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REPORT ON THE PROPERTY

OF

GOLIATH GOLD MINES LTD.

H EM LO AREA

DISTRICT OF THUNDER BAY

ONTARIO

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TABLE OF CONTENTS

INTRODUCTION

DESCRIPTION OF PROPERTY

LOCATION 6 ACCESS

TOPOGP.APHY 6 VEGETATION

EXPLORATION HISTORY

GENERAL GEOLOGY

LOCAL GEOLOGY t MINERALIZATION

SUMMARY f, CONCLUSIONS

RECOMMENDATIONS

ESTIMATE OF COSTS

EXPLANATION OF COSTS

BIBLIOGRAPHY

MAP REFERENCES

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HUDSON BAY

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THOMAS SKIMMING f, ASSOCIATES LIMITED

Topographic Plan

Bomby Township Claims


District of Thunder Bay, Ontario

July, 1981 Plan No. GML-81-2

INTRODUCTION

During the last several years, political and economic uncertainties throughout the world have created an unprecedented demand for gold and caused a dramatic increase in the free world price. As a result, many gold occurrences that were considered only mildly in

teresting during the 1940s and 1950s are being reassessed in light of present high gold prices and improved mining and milling technology.

The property of Goliath Gold Mines Ltd. adjoins that of Corona Resources Limited on which a gold- hearing pyritic zone within the Lake Superior Shear Zone is being delineated by diamond drilling a r i readied for production. Although existing evidence strongly suggests the favourable Lake Superior Shear Zone traverses the Goliath property, no systematic exploration appears to have been carried out in the past,

This report reviews the results of the earlier mineral exploration carried out in the area, particularly on the adjacent property presently under option to Corona Resources Ltd., and in addition, discusses the nature of the gold mineralization. An initial two phase ex ploration programme on the Goliath property is proposed herein to explore for zones of gold mineralization within the Lake Superior Shear Zone and generally to assess the mineral potential of the property.

This report is based on an examination of the Goliath and Corona properties by the writer, supplemented by a study of assessment work reports on file at the offices

of the Mining Recorder in Thunder Bay and Sault Ste. jftfie and the Assessment Research Piles Office in Toronto and on a review of all the pertinent technical

data published by the Ontario Ministry of Natural Resources.


The property of Goliath Gold Mines Ltd. consists of 58 contiguous, unpatented mineral claims which encompass an area of approximately 2,320 acres. The claims are

illustrated on Plan No. M33, (National Topographic Series 42C12), published by the Surveys and Mapping Branch of the Ontario Ministry of Natural Resources and titled "The Area of Molson Lake, District of Thunder Bay, r-ault Ste. Marie and Thunder Bay Mining Divisions".

The Goliath claims are identified on Plan No. M33 as

follows:

TD 57^847 - TB 576883 (37 claims)

SSM 576804 - SSM 576892 (9 claims)

SSM 577522 - SSM 577525 (4 claims)

SSM 577528 - SSM 577535 (8 claims)

These claims are outlined and coloured in yellow on a

current edition of Plan No. M33 accompanying this report.

All of the subject, unpatented mineral claims will require

annual assessment work to maintain the title. Title

searches were not carried out on any of the subject claims

by the writer or anyone commissioned Lv the writer; however,

it has been represented by the management of Goliath Gold

Mines Ltd. that the claims are in good standing until at

least July 24, 1982.

-J-

LOCATION AND ACCESS

The property is located along the north shore of Lake

Superior almost equidistant from Thunder Bay and Sault

Ste. Marie and, more specifically, in the northeast

quadrant of Bomby Township {Township 73) in the District

of Thunder Bay, approximately 5 miles by road, east of

the settlement of Memlo or one mile west of the Manitou

wadge cutoff (Highway 614).

Access to the propertv is by way of the Trans Canada

Highway (Highway 17), either from Thunder Bay for a

distance of 210 miles east or from Sault Ste. Marie for a distance of 230 miles northwest. Highway 17

passes through the centre of the property in a north

easterly direction and an unimproved gravel road

provides convenient access to the southeast portion of the claim group. Cedar Creek, which is navigable through

out most of its course, provides boat access to the north

and east portions of the property (see Photos l, 2 and 4).

The transcontinental line of Canadian Pacific Railways

passes through the ecstern portion of the property in

the vicinity of the Struthers railroad siding (see Photo 8).

The Struthers siding lies within claims TB 576880, TD 576881

and TB 576882. A hydro electric power line that was con

structed in 1975 is located approximately 800 feet from

the northwest corner of the property. The power line is

almost parallel to the northern boundary of the Goliath

claims.

The location of the Goliath property is shown on Provi

sional Map 42C/12 (Cedar Lake Sheet) published by the

Ontario Ministry of Natural Resources (and comprising part of Plan No. GML-81-2) and on Plan No. GML-81-1 pre

pared by Thomas Skimming i Associates Limited, both of

which accompany this report.

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Outline of


Claims

One ccnhmetri1 rrprnrntt one kilomi*lrp

THOMAS SKIMMING f, ASSOCIATES LIMITED

Topographic Plan




July, 1981 Plan No. GML-81-2

TOPOGRAPHY t, VEGETATIONm m l i -i m ——i li in - in.ua i a j 11 in— i i-1 *.m 1 '

The property is characterized by a gentle relief consist ing of rolling hills and rocky knobs separated by marshy ravines and bogs. The high ground is well forested with second growth black spruce and balsam fir and scattered jack pine. Large stands of white birch and poplar are common, particularly in areas previously ravaged by forest fires (see Photos 4, 5 and 7 accompanying this report).

Low ground and ravines are forested with black spruce, cedar, and tag alder with a ubiquitous labrador tea and sphagnum moss ground cover. Underbrush consists of a dense growth of moose maple, alder and witch hazel, particularly in "burn" areas.

Water is available in quantity from Cedar Creek which

flows through most of the Goliath property.

EXPLORATION HISTORY

The first recorded discovery of gold in the Hemlo area was made in the summer of 1945 by T. Ollmann of Heron Bay on the group of patented claims {The Ollmann-williams claims) in the immediate vicinity of Moose Lake which adjoins the claim group of Goliath Gold Mines Ltd. on the west. A limited amount of stripping and trenching was carried out on the Ollmann-williams claims during the summer of 1946 resulting in the discovery of a number of occurrences of gold within a strong, persistent, pyritic shear zone which has since become known as the Lake Superior Shear Zone. Subsequently, 15 short holes were drilled on the west side of Moose Lake using an X-ray rig and although the results were only mildly encouraging

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9

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(the best intersection was encountered in hole X-5 where 3.7 feet of core averaged .16 oz./ton in gold) the work

indicated the existence of a gold-bearing structural feature of consequence.

During the summer of 1947, Lake Superior Mining Corpora

tion carried out a systematic diamond drilling programme on the ground that is now encompassed by the Corona

Resources Ltd. claim group. The Lake Superior drill programme consisted of 13 x-ray holes (identified as X-l to X-13) totalling 1,846 feet of drilling along 1,500 feet of the Lake Superior Shear Zone. This drillir.j established a gold-bearing zone 1,200 feet in length, averaging 7.1 feet in width and containing .21 oz./ton in gold. On the basis of the promising results obtained in their initial drilling, Lake Superior Mining Corpora

tion completed an additional 4,022 feet of drilling in 10 holes during the fall of 1949 and the spring of 1950 (these are identified as E-l to F-10) to test the depth continuity of the gold-bearing zone indicated in the 19-17 drilling programme. The deeper drilling indicated a lesser strike length to the gold-bearing zone (400 feet) with an average width of 5.7 feet and containing .22 oz./ ton in gold. Based on the above drill results, Trevor W. Page, P.Eng., in his report on the property dated August 21, 1950, wrote the following summary and conclu sions:

"drilling on the main gold property of Lake

Superior Mining Corporation in the Hemlo area

has met with a large measure of success. As

an effort in pioneering a new district the

footage drilled has returned better than

average results. The indications of an ore-

shoot containing 76,653 tons grading 310.52

9

9

(uncut) are well substantiated and represent

only a small portion of the favourable and

partially explored ground extending for a

mile and a half to the east in Lake Superior

property. These facts, together with the

most desirable of transportation facilities

available and the possibilities of obtain

ing Hydro power in the near future make this

property one of the most obvious upon 'which

to complete development of mine potentiali

ties."

Further work on the property was undertaken by Teck

Exploration Company Limited in 1951. This consisted

essentially of a diamond drill -rogramme consisting of

15 holes which, with the exception of 3 deep holes of

questionable significance, was designed to substantiate,

and more accurately define the gold-bearing zone indi

cated in the earlier drilling carried out by Lake

Superior Mining Corporation. Although the writer was

unable to obtain the details of the Teck drilling,

reference is made to the results of this drilling in a

summary on the property prepared by Trevor W. Page, P.Eng. on June 25, 1951 as follows:

"Although the shear zone has been traced

for well over a mile through the Company

property, all drilling has been confined

to a section of some 1500 feet in length

on the western portion between a large

diabase dike and the property boundary.

Diamond drilling to date in the western

section of which 12,250 feet has been

completed, has indicated an orebody con

taining 83,283 tons with an uncut average

of 59.40 for a total indicated value of

5782,870.00."

-7-

This information leads the writer to conclude that 6,382 feet of drilling was carried out by Teck and that some encouraging results were obtained in the drilling since

Page increased his ore reserves from those stated in

his August 21, 1950 report.

From 1951 until 1973, the property lay dormant. In 1973, Ardel Explorations Limited drilled 3 closely spaced holes (100 feet apart) totalling 790 feet to test the Lake Superior Shear Zone approximately 400 feet east of the area explored by the Lake Superior Mining Corporation ' drilling. According to T. L. Muir in his summary on the work performed by Ardel Explorations Limited in Open File Report 5280, all three Ardel holes intersected the host shear zone and encountered grades of .15 to .21 oz./ton in gold over core lengths of 3.6 to 11.4 feet.

Cypress Resources Limited of Vancouver optioned the pro perty from prospector R. Newman of Kirkland Lake who staked the original Lake Superior Mining Corporation ground together with the ground immediately west of the Ollmann-Williams patented claims, during the summer of 1975. For reasons unknown, Cypress did not perform any

work on the property.

Subsequently, the Newman claims are believed to have been optioned by Copper Lake Explorations Ltd. of Vancouver in early 1977. Geological, geophysical and geochemical surveys were carried out by Robert E. Schaaf i Associates Inc. of Toronto on behalf of Copper Lake and R. Newman during May and June, 1977. However, this work was confined to ground west of the Ollmann-Williams patented claims. No work appears to have been done for Copper Lake or R. Newman on the known gold occurrence east of Moose Lake.

-B-

In 1980, the Newman claims were allowed to lapse. The ground was then staked by D. McKinnon of Timmins who optioned the claims to 435198 Ontario Corporation who,

in turn, it is reported, optioned them to Corona Resources Limited.

During the winter of 1980, Corona carried out ground magnetic and electromagnetic (VLF) surveys and initiated a diamond drilling programme to substantiate the results

of the earlier drilling and to attempt to extend the limits of the known zone of gold mineralization. By June, 1981, Corona had completed over 26,000 feet of diamond drilling (83 holes) and had outlined a gold-bearing pyritic zone within the Lake Superror Shear Zone, approximately 1,600 feet in length with widths varying from two to fifteen feet with an average grade of approximately .15 oz./ton in gold {verbal communication with David R. Bell). Narrower widths of higher grade material (i.e. 1.86 oz./ton over 2.0 feet in DDH 81-57) were intersected periodically in the Corona drilling. The easternmost hole to date drilled by Corona is approximately 1,500 feet from the western boundary of Goliath's claim group.

In 1950, Trevor W. Page, P.Eng. prepared a report on the so-called "Struthers" group of claims (now encompassed

by the southeast portion of the Goliath property) for

W.M.C. Thorns. The "Struthers" claims were staked in

1947 to cover the projected strike of the zone of gold mineralization outlined by Lake Superior Mining Corpora

tion (the same zone being investigated in detail by Corona Resources Ltd.). In his report on the "Struthers"

claims under the chapter on mineralization, Page states:

"To date the only mineralization of conse

quence has been found on the south side of

the east-west trending ridge that passes

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-9-

through the south portion of claim SSM

21470. This showing is located approxi

mately on the boundary line between SSM

21470 and SSM 21473 (writers note - this

showing appears now to be encompassed by

Goliath claim TB 576885 located in the

southeast corner of the claim group).

Relatively heavy silicification has taken

place throughout a zone some 30 feet wide.

Shearing of the sediments is noticeable

but not pronounced and mineralization in

the form of pyrite is localized in tt.e

more siliceous sections. Low values in

gold have been obtained from the portions

that are most heavily mineralized.

Exploratory work to date has been limited

to some stripping and trenching where the

zone is exposed on the face of the ridge.

Structural information would indicate

that this section is in line with the

gold bearing shear zone found on the

neighbouring Lake Superior Mining Corpora

tion proper ty."

In concluding his report, Page goes on to say:

"As yet, insufficient work has been under

taken to properly assess the potential

value of the Struthers group of claims.

Geologically and structurally they occupy

a favourable position in that they lie

astride the projection of the Lake

Superior shear zone, which has proven

gold values of commerical interest. The

present exposed section represents a very minute portion of the total strike length available for exploration."

GENERAL GEOLOGY

The regional geology of the Hemlo area is shown on Map

2220, "Manitouwadge - Wawa Sheet" published in 1972 by

the Ontario Division of Mines at a scale of one inch to

two miles. In 1978, a detailed mapping programme in

the Hemlo area was carried out by T. L. Muir and assis

tants of the Ontario Geological Survey. Information on

this programme was released in late 1979 as Open File

Report 5280. As part of this report, preliminary map

P2304 {Hemlo Area - Northern Half) illustrating the

regional geology of the Hemlo area at a scale of one inch to one-quarter mile, was issued.

In the area between Hemlo and Struthers within which the

Goliath Gold Mines Ltd. claim group is located, the

dominant rock types consist of medium to thickly lami

nated arkosic wackes and greywacke-type sediments inter

bedded with rhyolitic to dacitic tuffs and foliated flows

with intercalated lenses and pods of mafic metavolcanics

represented mainly by dark coloured variolitic flows and

lapi11 i-tuff. These rocks occur in a narrow belt trend

ing east-west, varying in width from one to three miles

and dip to the north at an angle of 60 degrees on the

average. In the vicinity of the Goliath claim group/

the belt is 1-3/4 miles wide and is bound on the north

by the Cedar Lake pluton, a hornblende-biotite grano

diorite and on the south by the P-jkaskwa Gneissic

Complex, consisting of a complex assemblage of porphy

ritic biotite hornblende granodiorite, quartz monzonite,

trondhjemite and a variety of hybrid rocks.

-li-

Feldspar porphyry and quartz porphyry dikes and sill- like masses, some up to 200 feet or more wide, intrude the metasediment-metavolcanic belt. Most of the rocks

in the Hemlo area have undergone medium-grade metamor phism.

A pronounced structural lineament, the Hemlo fault parallels the general strike of the rocks for several miles and passes through the southwest portion of the Goliath property, just north of Molson Lake. The Lake Superior Shear Zone is parallel to the Hemlo fault and may be genetically related.

LOCAL GEOLOGY S MINERALIZATION

The most detailed information available on the geology of the Goliath property is contained in a report by Trevor W. Page, dated December 20, 1950 on the Struthers group of claims (now the southwest portion of the Goliath property). In describing the geology, Page states :

"Rock exposures on the Struthers group of

claims are limited in extent by the presence

of considerable low lying ground in the

central and eastern portions of the claims.

Individual types appear limited to the sedi

mentary and intrusive members as are commonly

met with in the Hemlo Area. As an intimate

and detailed classification has not been

attempted only the more apparent types and

their distributions are discussed.

ST: This rock type, which is

presently believed to be one of the oldest

consists in general of an aggregation of

fine to medium grains of quartz together

with light colored mica in parallel to

subparallel Arrangement. The quartz ac

counts for up to 651 of the total volume

and the mica, while variable with other

f er r omagnes i un cons is ten ts , ranges up to

304. Due to the mica content and its

parallel arrangement, the rock, whil*

generally hard and firm, takes on a

gneissic to schistose appearance. Color

ranges from light buff to grey. Occa

sional garnetiferous bands have been

ohser ved .

This type is probably a continuation of a

similar band that has been observed in the

vicinity of mileage 36 on the C. P. R. some

two miles to the west. On the Struthers

group it forms a band some 600 feet wide

that trends northwestward through the cen

tral part of the property.

This type which

is in general most widely distributed in

the Hemlo Area is more or less limited to

a small section on claim SSM 21473 at the

east end of the ridge that passes Mirough

the central section of the claims.

Megascopica l ly , t hese sediments are a dark

grey, medium to fine grained, fairly hard

rock sometimes massive although more often

tending to be jointed and fissile. Locally

there may be a marked banding of these

rocks with increased content of dark

minerals.

-13-

5 EO.I MEN TS i This type of sediment, al

though quite prevalent on the Lake Superior

Min. Corp. ground some 2000 feet to the

northwest, is, except for a very minor

occurrence, almost entirely absent on the

Struthers group. In general this rock is

a rust grey to brown, usually fissile rock

in surface exposure. It consists almost

entirely of brown mica and quartz with

varying amounts of dark minerals as a

minor constituent. The quartz content at

times appears to increase considerably so

that the rock takes on a very siliceous

light colored appearance with minor bands

of extremely fine grained brownish siliceous

material. It is believed that this effect

may be due at least In part to silicifica

tion by hydrothermal agencies. Some light

colored sericitic mica is usually present

and also pyrite mineralization in sections

that show this effect.

Practically the entire

southwest portion of the group south of

the assun. d projection of the Hemlo Fault

is underlain by a medium to fine grained

dioritic rock which displays a banded

somewhat gneissic structure. Drag folding

is fairly prevalent and would indicate

further that these rocks have undergone

considerable metamorphism. Generally this

whole section shows little change in compo

sition of the rock type other than the band

ing effect noted.

fi^Si^GREEÎHKES: I n t he w"t central

portion of claim SSM 21473 a dark grey

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SUMMARY 6 CONCLUSIONS^^••••.^•••••••^••IMmBMHIIIIMMMVBaM^MBM^MHHIIMH^HIHB f

To date, diamond drilling on the property of Corona Resources Limited, which adjoins the Goliath claim group on the west, has outlined a gold bearing pyritic zone within a siliceous and sericitic fragmental tuff (Lake Superior Shear Zone) containing approximately one million tons of material grading .15 oz./ton in gold. The easternmost hole drilled to date by Corona is about 1500 feet from the western boundary of Goliath's claim group. Information contained in some of the earlier reports on the area strongly suggests the favourable Lake Superior Shear Zone underlies the Goliath property and, on the basis of the work by Trevor Page in 1950, may be gold bearing.

On the basis of the analytical work carried out by Lake Superior Mining Corporation and, more recently, by Corona, there appears to be a direct correlation be tween gold and pyrite within the Lake Superior Shear Zono suggesting the possibility of using an electrical geo physical survey as an indirect but possibly effective and inexpensive method of exploring for gold along the favourable horizon. A geophysical programme using a VLF (Geonics EM-16) electromagnetic unit and a fluxgate (McPhar MF-2) magnetometer, was conducted by Corona over their property. The VLF survey failed to delineate the gold zone; however, the ground magnetic survey recorded a weak, positive anomaly coincident with the zone and was considered useful in guiding their drilling. Because of the disseminated nature of the pyrite minera lization on the Corona property, induced polarization may be the only effective electrical method of detecting the gold-bearing pyritic zone.

The description of the gold occurrence in the southeast corner of the Goliath property by Page, resembles the description of the Corona mineralization, yet there is no evidence to suggest that the Goliath property has been explored since the limited work carried out by Page on behalf of W.M.C. Thorns in 1950. This probably is

accounted for by the fact that previous workers, with limited exploration funds, hesitated to explore much beyond the known gold occurrence under investigation by Corona.

Recent work on the Lake Superior Shear Zone suggests

that the zone may actually be a sericitized pyroclastic

horizon which, because of its foliated texture, has been

identified as a shear zone since it was first discovered

in 1945. In a report on the Corona property, D. Dell

describes the host rock as a fine grained, siliceous, sericitic and schistose fragmental tuff. Regardless of

its true nature, the favourable gold-bearing host will

probably have considerable geographic extent.

RECOMMENDATIONS

On the basis of the proximity of the Goliath property to the zone of gold mineralization being delineated by diamond drilling by Corona Resources, Inc. and on the evidence that strongly suggests the favourable Lake Superior Shear Zone (host pyroclastic horizon) extends onto the Goliath property, a comprehensive programme designed to explore for gold-bearing zo..es of the Corona type on the Goliath property is warranted.

A two phase exploration programme is envisaged wherein the first phase should consist essentially of geological

mapping, trenching, surface sampling and geophysical st rveys. The second phase will be contingent on favourable results from the first phase and should

consist exclusively of diamond drilling.

A grid to provide the necessary control for the pro posed exploration programme should be constructed over the ontire property. The grid should consist of a baseline oriented with an azimuth of 120O with cross- lines at intervals of 400 feet along the baseline. This should be reduced to intervals of 200 feet in the vicinity of any geophysical anomalies that are recorded and in the vicinity of any trenching that is carried out

Detailed geological mapping f all outcrops should be

carried out over the area encompassed by the control

grid. Special attention should be devoted to identify

ing and mapping alteration phenomena, including silici

fication, sericitization and pyritization within the

volcanic.'; and volcaniclastic sediments. Where any

evidence of these features is found, particularly

pyritization, trenching and systematic sampling should

be carried out.

Permission should be obtained from Corona Resources

Ltd. to conduct an experimental geophysical programme

using a variety of electromagnietic systems over their

known zone of gold mineralization to determine which

system most effectively delineates the zone. Follow

ing this, a ground magnetic and electromagnetic survey

should be carried out over the Goliath property in an

attempt to locate pyritic zones, which theoretically

should contain the highest concentration of gold,

within the so-called Lake Superior Shear Zone.

An effort should be made to locate the mineralized

zone south of'the Struthers siding (now believed to be encompassed by claim TB 576885) referred to in the December 20, 1950 report of Trevor Page. The zone should be exposed by trenching where practicable and

systematic sampling should be carried out.

If not already under option to Corona, an attempt should be made to acquire or to negotiate an exploration option

agreement on the Ollmann-Williams group of patented mineral claims to the west of the Corona property.

ESTIMATE OF COSTS

PHASE I

Control Grid $ 16,500 (1)

Geological Survey 11,250 (2)

Geophysical Surveys 23,000 {3)

Trenching f, Sampling 5,000 (4)

Chemical Analyses 1,500 (5)Transportation 5,500 (6)

Supplies 6 Equipment 6,500 (7)

Engineering S Supervision 3,600 (8)Contingencies 7,150 (9)

Total: S 80,000

PHASE II

Diamond Drilling 5125,000 (1)Engineering t. Supervision 4,500 (2)Chemical Analyses 3,750 (3)Contingencies 16,750 (4)

Total: 5150,000


The foregoing estimate of costs is based on an explora tion programme consisting essentially of geological mapping, experimental geophysics followed by systematic

ground geophysical surveys and a limited amount of trenching and sampling. The costs are further based on the assumption the field programme will require approximately 2 months to complete.

(1) The sum of $16,500 estimated for the construction of a control grid allows for 60 line miles (baselines and gridlinesj of cutting, chaining and picketing at a cost of 3275 per line mile.

(2) The sum of $11,250 estimated for the geological mapping allows for the employment of one senior geologist on a contractual basis for a period of 45 days at a rate of 5250 per day to carry out the proposed geological mapping and to supervise any trenching and sampling that is done .

(3) The amount of 323,000 estimated for geophysical surveys provides for 60 line miles of ground magnetic survey at 3100 per line mile (36,000), an allowance of S5,000 for geophysical experi mentation and an allowance of 312,000 for either 20 line miles of induced polarization survey (3600 per line mile) or 60 line miles of an acceptable electrical survey (maxmin, TURAM, etc.) at 3200 per line mile.

(4) The sum of 35,000 estimated for trenching andsampling includes the rental of a rock drillplus operator for approximately one week.

.

(5) The figure of 51,500 estimated for chemical analyses

provides 1 for a total of 100 gold-silver analyses

plus sample preparation costs at a unit cost of 515

per sample.

(6) The sum of 35,500 estimated for transportation

provides for the mobilization and demobilization

of personnel and equipment and all other field

transportation requirements for th*? duration of

the proposed field programme.

(7) The sum of 36,500 estimated for supplies and equip

ment includes the cost of accommodation, general

field equipment, equipment rental and all the food

and fuel lequired for the duration of the proposed

field programme.

(8) The sum of 33,600 estimated for engineering and

supervision allows for 12 days at S300 per day and

would include programming and logistical planning,

direct programme supervision and the compilation

and interpretation of all field data.

(9) The figure of 37,150 represents a contingency

factor of approximately 10i of the total estimated programme cost.

EXPLANATION OF COSTS (PHASE II)

Phase II of the programme proposed herein is contingent

on favourable results from the exploration programme

recommended in Phase I. The estimate of costs in Phase

II, which would consist essentially of diamond drilling,

is based on a nominal programme involving 5,000 feet of

drilling and on the assumption that the programme will

require approximately 2 months to complete. In the

event the results of the proposed diamond drilling in

Phase II are favourable, considerably more diamond

drilling will be required to assess the economic

significance of the property.

(1) The sum of 5125,000 estimated for diamond drilling

allows for 5,000 feet of drilling at an all inclu

sive price of 525 per foot. This includes con

tinuous, on site engineering supervision and

attendant transportation costs.

{2} As in Phase I, the estimate of 54,500 for engineer

ing and supervision is based on a rate of 5300 per

day for 15 days and would include the planning and

supervision of the entire programme and the compila

tion and interpretation of all the drill data.

(3) The figure of 53,750 estimated for chemical analyses

provides for a factor of 50.75 per foot against a

proposed diamond drill programme involving 5,000

feet of drilling.

(4) The figure of 516,750 represents a contingency

factor of 12^ of the total estimated programme

cost.

Respectfully submitted,

Thomas Skimming, P.

Toronto, Ontario August 20, 1981

BIBLIOGRAPHY

Bell, David R. May 5, 1981

Phase I - Progress Report Corona Resources Limited, Hemlo Property, District of Thunder Bay, Ontario

Greer, W.L.C. June 24, 1949

Memorandum on Property of Lake Superior Mining Corpora tion, Hemlo, Ontario

Greer, W.L.C. May 8, 1973

Report on the property of Ardel Explorations Ltd./ in Township 73, Near Hemlo in the Thunder Bay Mining Division, Ontario, unpublished report

Lyons, Edward M. July 6, 1977

R. Newman Hemlo Gold Property West Group, Molson Lake Area Thunder Bay Mining Division, OntarioRobt. E. Schaaf s, Associates, Inc., Geological, Geophysical and Geochemical Surveys unpublished report

Muir, T.L. 1978

Hemlo Area, District of Thunder Bay, Summary of Field Work, 1978, Ontario Geological Survey, Miscellaneous Paper 82 pp. 90-93

Muir, T.L. 1980

Geology of the Hemlo Area, District of Thunder Bay, Ontario, Ontario Geological Survey OFR 5280

Newbury, Michael June 3, 1974

Report on the Pronerty of Ardel Explorations Limited, Hemlo, Ontario unpublished report

- J! 1.^.'

Northern Miner Various Editions

Page, Trevor W. September, 1947

Summary of Geological Reconnaissance Survey

Page, Trevor W. December 20, 1947

A Report on the Ollmann- Williams Group of Claims Hemlo, Ontario

Page, Trevor W. April l, 1948

A report on the property of Lake Superior Mining Corporation Limited, Hemlo Area, Ontario unpublished report

Page, Trevor W, March 8, 1950

Outline of Results on Property

Diamond Drill Hemlo, Ontario

Page, Trevor W. August 21, 1950


Page, Trevor W. December 20, 1950

A Geological Report on the Struthers Group of Mining Claims, Hemlo Area, Ontario

Page, Trevor W. June 25, 1951

A report on the property of Lake Superior Mining Corporation Limited, Hemlo, Ontario unpublished report

Page, Trevor, W, undated

Interim Report on the property of Lake Superior Mining Corpora tion Limited, Hemlo, Ontario

Prospectus June 30, 1949

Lake Superior Mining Corporation Limited

MAP REFERENCES

Preliminary Map No. P 494

Manitouwadge Sheet Ontario Department of Mines Districts of Thunder Bay and Algoma Scale: l" to 2 miles

Map 2220

Geological Compilation Series Manitouwadge - Wawa Sheet Ministry of Natural Resources - Ontario Scale: l" to 4 miles


Geological Series Hemlo Area (Northern Half) Ontario Geological Survey Scale: l" to 1/4 mile

Map 2167G

Geophysics Paper 2167 Airborne Magnetic Survey Herrick Lake Sheet Geological Survey of Canada Scale: l" to l mile

Map 2156G

Geophysics Paper 2156 Airborne Magnetic Survey Heron Bay Sheet Geological Survey of Canada Scale: l" to l mile

CERTIFICATE OF QUALIFICATION

I, THOMAS SKIMMING, hereby certify:

1. that I am a consulting geologist employed by Thomas Skimming s, Associates Limited at Suite 306, 5233 Dundas Street, West, Toronto, Ontario

2. that I am a registered Professional Engineer inthe Province of Ontario and Manitoba and that I am a Fellow of the Geological Association of Canada

3. that I was born in Canada in the year 1935 and have been a Canadian citizen since birth

4. that I am a graduate of the University of Michigan i958, with the degree Bachelor of Science (B.Se.) in Geology

5. that I have been practising my profession as a geologist continuously for twenty-two years

6. that I do not have, nor do I expect to receive,directly or indirectly any interest in the- property reviewed herein or in the securities of Goliath Gold Mines Ltd.

7. that my report is based on an examination of theGoliath property on June 3 and 4, 1981 and on several on site investigations of the adjacent property being explored currently by Corona Resources, Inc. The report is also based on a review of all the pertinent technical data published by the Ontario Ministry of Natural Resources and a study of the assessment work reports on file at the Assessment Research Files Office in Toronto, Sault Ste. Marie and Thunder Bay.

8. a diligent effort has been made to obtain all records and technical data pertinent to the property reviewed herein and it is believed that these efforts have been successful and that the conclusions relating to the potential of the property have been reached with full recognition of the results of all the previous work, both positive and negative, carried out on the property.

Toronto, OntarioAugust 20, 1981 Y. T,K:,V..;-,!;-.JG T^pma s S k imprf ng , P

*

REPORT ON THE PROPERTY

OF

GOLDEN SCEPTRE MINES LTD.

fiUG- ZS.*************************

HEMLO AREA

DISTRICT OF THUNDER BAY

ONTARIO

TABLE OP CONTENTS

INTRODUCTION

DESCRIPTION OP PROPERTY

LOCATION S, ACCESS

TOPOGRAPHY 6 VEGETATION

EXPLORATION HISTORY

GENERAL GEOLOGY

LOCAL GEOLOGY S, MINERALIZATION

SUMMARY 6 CONCLUSIONS

RECOMMENDATIONS

ESTIMATE OP COSTS


BIBLIOGRAPHY

MAP REFERENCES

(9

HUDSON BATt

Location of


THOMAS SKIMMING K ASSOCIATES LIMITED

Property Location Map




August, 1981 Plan No. GSM-81-1

G

INTRODUCTION

During the last several years, political and economic uncertainties throughout the world have created an unprecedented demand for gold and caused a dramatic increase in the free world price. As a result, many gold occurrences that were considered only mildly in teresting during the 1940s and 1950s are being reassessed in light of present high gold prices and improved mining and milling technology.

The property of Golden Sceptre Mines Ltd. adjoins that of Corona Resources Limited on which a gold-bearing pyritic zone within the Lake Superior Shear Zone is being delineated by diamond drilling and readied for production. Although existing evidence suggests the favouiable Lake Superior Shear Zone traverses the Golden Sceptre property, no systematic exploration appears to have been carried out in the past.

This report reviews the results of the earlier mineral exploration carried out in the area, particularly on the adjacent Corona property and, in addition, discusses the nature of the gold mineralization. An initial two phase exploration programme on the Golden Sceptre property is proposed he.rein to explore for zones of gold mineralization within the Lake Superior Shear Zone and generally to assess the mineral potential of the proparty.

This report is based on an examination of the Golden Sceptre and Corona properties by the writer, supplemented by a study of assessment work reports on file at the offices of the Mining Recorder in Thunder Bay and Sault

(*

Ste. Marie and the Assessment Research Files Office in Toronto and on a review of all the pertinent technical data published by the Ontario Ministry of Natural Resources.


The property of Golden Sceptre Mines Ltd. consists of 98 contiguous/ unpatented mineral claims which encompass an area of approximately 3,920 acres. The claims are illustrated on Plans M33 and M1602 (National Topographic Series 42C12), published by the Surveys and Mapping Branch of the Ontario Ministry of Natural Resources and titled respectively: "The Area of Molson Lake, District of Thunder Bay, Thunder Bay Mining Division" and "The Area of Rous Lake, District of Thunder Bay, Thunder Bay Mini *g Division".

The Golden Sceptre claims are identified on Plans M33and M1602 as follows:

TB 528742 - TB S28749 (6 claims') TB 553735 - TB 553738 (4 claims) TB 568782 (l claim) TB 568784 - TB 568789 (6 claims) TB 576639 - TB 576700 (62 claims) TB 576803 - TB 576810 (8 claims) TB 576893 - TB 576896 (4 claims) TB 577536 - TB 577540 (5 claims)

These claims are outlined and coloured in yellow on current editions of Plans M33 and M1602 accompanying this report.

All of the subject, unpatented mineral claims will require annual assessment work to maintain the title. Title

searches were not carried out on any of the subject claims A by the writer or anyone commissioned by the writer; how-

^^ ever, it has been represented by the management of Golden ^^ Sceptre that the majority of the claims are in good stand

ing until at least July 21, 1982. Twelve of the claims expire on January 6, 1982 unless the required assessment work is performed or an extension is obtained CTom the Mining Commissioner.

0)

LOCATION AND ACCESS

The property is located along the north shore of Lake Superior almost equidistant from Thunder Bay and Sault Ste. Marie and, more specifically, in the northwest corner of Bomby Township (Township 73) and the northeast corner of Lecours Township (Township 74) in the District of Thunder Bay, approximately ^ ra-le by road, north of the settlement of Hemlo or 5 miles west of the Manitou wadge cutoff (Highway 614).

Access to the property is by way of the Trans Canada Highway (Highway 17), either from Thunder Bay for a distance of 205 miles east or from Sault Ste.'Marie for a distance of 235 miles northwest. Highway 17 passes through the centie of the property in an east-west direction (see Photos l, 2 and 5 accompanying this report) and an unimproved gravel road on the east side of Botham Lake, provides convenient access to the north central portion of the claim group. A hydro service road provides access to the remainder of the property.

The transcontinental line of Canadian Pacific Railways passes through the south eastern portion of the property in the vicinity of Cigar Lake just east of Hemlo (see Photo 3). A hydro electric power line that was con-

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•trotted In 197S oroaaea the centre of the property in M eeet-wett direction* approximately 3/4 nil e* north•f the Tt ana Canada Highway.

location of the Oolden fotptrt property is shown on Provincial Mr Ut Nap 4JC/WW (tthite liver Sheet) and 410/VS (Moron Bay fnect) published by tt* Ontario Kinlttry of natural Resources (and eonprisino, part of Nan no. om-ll-a) and on Man No. Om-ll-1 praparad by Tfconaa ninnlnf 4 Ataooiataa Unitad. both of which aooonpany thia raport.

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THa pf*a*fty la enaractaritad by a fantia raliaf conaiat- lAf of relit** Mila and rooky dnoba (aaa ^hotoa T , t and li) aaparatad by narahy ravlnaa and bofa. Tha hi^h fratmd ia val i foraatad with aaoond frowth black apryca and baiaan fir and aoattarad )acli pina (aaa rhoto 2)* tarta atanda of wnita birch and poplar ara connon* partiawiariy in araaa pravioualy favafad by foraat firaa (aa* rnotoa 10 and 12).

bow frovnd and ravtnaa ara foraatad with black apruca* aadar. and taf aldar with a ubiouitoua labrador taa and •pfc+ffiiMi noaa froand eovar. Undarbrvah conaiata of a d^naa frowtn af nooaa napla* aldar and witch hasal* partiavlariy ia 'burn* *raaa laaa fhotoa 10 and 12).

Matar ia available in quantity fron Cifar La*a, pala U*e and Ootnan U*e in t ha aaatarn half of tha property and fro* tooa taka and tha ii*cn liver in the antrane weatarn pt*tion of the property.

-5- ' ' " - ..

EXPLORATION HISTORY

The first recorded discovery of gold in the Hemlo araa was made in the summer of 1945 by T. Ollmann of Heron Bay on the group of patented claims (The Ollmann-williams claims) in the immediate vicinity of Moose Lake which adjoins the claim group of Golden Sceptre Mines Ltd. on the east. A limited amount of stripping and trenching was carried out on the Ollmann-williams claims during the summer of 1946 resulting in the discovery of a number of occurrences of gold within a strong, persistent, pyritic shear zone which has since become known as the Lake Superior Shear Zone. Subsequently, 15 short holes were drilled on the west side of Moose Lake using an X-ray rig and although the results were only mildly encouraging (the best intersection was encountered in hole X-5 where 3.7 feet of core averaged .16 02./ton in gold) the work indi cated the existence of a gold-bearing structural feature of consequence.

During the summer of 1947, Lake Superior Mining Corpora tion carried out a systematic diamond drilling programme on the ground immediately east of the Golden Sceptre property that is now encompassed by the Corona Resources Ltd. claim group. The Lake Superior drill programme consisted of 13 x-ray holes totalling 1,846 feet of drilling along 1,500 feet of the Lake Superior Shear Zone. This drilling established a gold-bearing zone 1,2*00 feet in length, averaging about 7 feet in width and containing .21 oz./ton in gold. On the basis of the promising results obtained in their initial drilling, Lake Superior Mining Corporation completed an additional 4,022 feet of drilling in 10 holes during the fall of 1949 and the spring of 1950 to test the depth continuity of the gold-bearing zone indicated in the 1947 drilling programme. The deeper drilling indicated a lesser strike length to the gold-bearing zone (400 feet) with an average width of 5.7 feet and containing .22 oz./ton in

'-.- '- ;-- .r .•'•

gold. Based on the above drill results, Trevor W, Page, P.Eng., in his report on the property dated August 21, 1950, wrote the following summary and conclusions:

Drilling on the main gold property of Lake

Superior Mining Corporation in the Hemlo area

has met with a large measure of success. As

an effort in pioneering a new district the

footage drilled has returned better than

average results. The indications of an ore-

shoot containing 76,653 tons grading S10.52

(uncut) are well substantiated and represent

only a small portion of the favourable and

partially explored ground extending for a

mile and a half to the east in Lake Superior

property. These facts, together with the

most desirable of transportation facilities

available and the possibilities of obtain

ing Hydro power in the near future make this

property one of the most obvious upon which

to complete development of mine potentiali

ties. "

Further work on the property was undertaken by Teck

Exploration Company Limited in 1951. This consisted

essentially of a diamond drill programme consisting of 15 holes which, with the exception of 3 deep holes of questionable significance, was designed to substantiate, and more accurately define the gold-bearing zone indi

cated in the earlier drilling carried out by Lake Superior Mining Corporation. Although the writer was unable to obtain the details of the Teck drilling, reference is made to the results of this drilling in a summary on the property prepared by Trevor W. Page, P.Eng. on June 25, 1951 as follows:

Although the shear zone has been traced

for well over a mile through the Company

- * -; .- . -7- ' - : , . ' , ?0- ,

property, all drilling has been confined to a section of some 1500 feet in length on the western portion between a large

diabase dike and the property boundary.

Diamond drilling to date in the western

section of which 12,250 feet has been

completed, has indicated an orebody con

taining 83,283 tons with an uncut average of 59.40 for a total indicated value of

S7S2,870.00."

This information leads the writer to conclude that 6,382 feet of drilling was carried out by Teck and that some encouraging results were obtained in the drilling since Page increased his ore reserves from those stated in his August 21, 1950 report.

From 1951 until 1973, the property lay dormant. In 1973, Ardel Explorations Limited drilled 3 closely spaced holes (100 feet apart) totalling 790 feet to test the Laice Superior Shear Zone approximately 400 feet east of the area explored by the Lake Superior Mining Corporation drilling. According to T. L. Muir in his summary on the work performed by Ardel Explorations Limited in Open File Report 5280, all three Ardel holes intersected the host shear zone and encountered grades of .15 to .21 02./ton in gold over core lengths of 3.6 to 11.4 feet.

Cypress Resources Limited of Vancouver optioned the pro perty from prospector R. Newman of Kirkland Lake who staked the original Lake Superior Mining Corporation ground together with the ground immediately west of the Ollmann-Williams patented claims, during the summer of 1975. For reasons unknown, Cypress did not perform any work on the property.

-.- ' . v ,- ' ' . ' .. .. - . , o -. . ..-.-,:.. .'r "t-'-l'

In 1980, the Newman claims were allowed to lapse. The ground was then staked by D. McKinnon of Timmins who optioned the claims to 435198 Ontario Corporation who, in turn, it is reported, optioned them to Corona resources Limited.

During the winter of 1980, Corona carried out ground magnetic and electromagnetic (VLF) surveys and initiated a diamond drilling programme to substantiate the results of the earlier Lake Superior and Teck drilling and to attempt to extend the limits of the known zone of gold mineralization. By June, 1981, Corona had completed over 26,000 feet of diamond drilling (83 holes) and had outlined a gold-bearing pyritic zone within the Lake Superior Shear Zone, approximately 1,600 feet in length with widths varying from two to fifteen feet with an average grade of approximately .15 oz./ton in gold (verbal communication with David R. Bell). Narrower widths of higher grade material (i.e. 1.86 oz./ton over 2.0 feet in DDH 81-57) were intersected periodi cally in the Corona drilling. Definition drilling employing two drills and metallurgical test -work by Corona is in progress.

In 1977, a systematic exploration programme consisting of geological, geophysical and geochemical surveys was carried out on the Newman property between Moose Lake and Botham Lake on ground now encompassed by Golden Sceptre claims TB528744 - TB528747 and TB553735 - TB553738. This work was performed by Robert E. Schaaf d Associates Inc. on behalf of Copper Lake Explorations Ltd. of Vancouver. An electromagnetic survey (VLF) was ineffective in locating any conductors and was restricted to some degree by the power line running through the centre of the survey area. In the geochemical soil survey, a weak multi sample gold anomaly, interpreted to be underlain by a porphyry intrusive, was located.

-9-

In addition, four single station gold anomalies, one of which analyzed 10,000 ppm in gold, were identified. Although the Newman claims covered the original Lake Superior Mining Corporation gold occurrence* no work was performed on the occurrence by Copper Lake.

In 1975, Noranda Exploration Company Limited carried out an airborne geophysical survey in the vicinity of Rous Lake. A number of airborne conductors were located in the Black River Valley approximately one mile north-northeast of Rous Lake (now believed to be encompassed by Golden Sceptre claims TB 576809 and TB 576810). Follow up ground geophysical surveys (magnetic and electromagnetic VLF) were carried out which resulted in the definition of four electromag netic anomalies. Three parallel magnetic anomalies were also outlined but were not coincident with the VLP anomalies. Whether or not these anomalies were investigated further by diamond drilling by Noranda or others is unknown.

In 1978, T. L. Muir of the Ontario Ministry'of Natural Resources, while mapping the geology of the Hemlo Area (Open File Report 5280) collected a number of grab samples from gossan zones along Highway 17 and had them analyzed for a variety of metals. One sample of pyritiferous felsic tuff collected on the north side of the highway about 2 km east of the Hemlo turnoff (now believed to be encompassed by Golden Sceptre claim TB 576674) assayed 0.32 oz./ton in gold and 0.48 oz./ton in silver. Although it was not known at the time, Photo 2 was taken in the vicinity of this gold-bearing gossan.

O!

-lo- . ' - - - - -GENERAL GEOLOGY

The regional geology of the Heralo area is shown on Map 2220, "Manitouwadge - Wawa Sheet" published in 1972 by the Ontario Division of Mines at a scale of one inch to two miles. In 1978, a detailed mapping programme in the Hemlo area was carried out by T. L. Muir and assis tants of the Ontario Geological Survey, Ministry of Natural Resources. Information on this programme was released in late 1979 as Open File Report 5280. As part of this report, preliminary map P2304 (Hemlo Area - Northern Half) illustrating the regional geology of the Hemlo area at a scale of one inch to one-quarter mile, was issued.

In the area between Rous Lake and Moose Lake within which the Golden Sceptre Mines Ltd. claim group is located, the dominant rock types consist of medium to thickly laminated arkosic wackes and greywacke-type sediments interbedded with rhyolitic to dacitic tuffs and foliated flows with intercalated lenses and pods of mafic metavolcanics represented mainly by dark coloured variolitic flows and lapilli-tuff. These rocks occur in a narrow belt trending east-west, vary ing in width from one to three miles and dip to the north at an angle of 60 degrees on the average. In the vicinity of the Golden Sceptre claim group, the belt is 1-3/4 miles wide and is bound on the north by the Cedar Lake pluton, a hornblende-biotite grano diorite and,on the south by the Pukaskwa Gneissic Complex, consisting of a complex assemblage of porphy ritic biotite hornblende granodiorite, quartz monzonite, trondhjemite and a variety of hybrid rocks. Feldspar porphyry and quartz porphyry dikes and sill-like masses, some up to 200 feet or more wide, intrude the metasediment-metavolcanic belt. Most of the rocks in the Hemlo area have undergone medium-grade metamorphism.

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A pronounced structural lineament, the Hemlo fault parallels the general strike of the rocks for several

/"^J miles and passes within approximately 200 feet of the south boundary of the Golden Sceptre property, just south of Cigar Lake. The Lake Superior Shear Zone is parallel to the Hemlo fault and may be genetically related.

Si

LOCAL GEOLOGY S MINERALIZATION

The most detailed information available on the geology of the Golden Sceptre property is contained in Open File Report 5280 by T. L. Muir and in the report pre pared by E. M. Lyons for Copper Lake Explorations Ltd. in 1977.

The property is underlain by an east-west trending assemblage oS interbedded foliated acid to mafic volcanic flows with.intercalated tuffaceous horizons and thick, but discontinuous sequence of volcaniclastic sediments consisting mainly of arkosic wacke with some thinly laminated beds of argillite and quartzite* All of these rocks dip steeply to the north {see Photos l and 5) at angles ranging from 60 to 80 degrees.

The volcanic-volcaniclastic assemblage is intruded by a variety of both conformable and discordant quartz- feldspar porphyry bodies which vary greatly in shape and size. A description of the porphyries on the Golden Sceptre property resembles that which appears to be structurally and perhaps genetically related to the gold mineralization on the adjacent Corona

property.

A small portion of the Heron Bay Pluton, a massive biotite-hornblende granodiorite, outcrops in the

-12-

southwest corner of the Golden Sceptre property along the north shore of Rous Lake. At this location,

sheeting or horizontal jointing in the granodiorite is common (see Photo 6).

Numerous north to northwesterly trending late stage

diabase dikes, ranging in width from a few feet to

200 feet or more, cut all of the volcanic and volcani clastic rocks on the Golden Sceptre property.

The gold occurrence discovered by Lake Superior Mining Corporation in 1947 and presently being delineated by diamond drilling by Corona Resources Limited on the

property to the east and immediately adjacent to the Golden Sceptre property, consists of a gold-bearing pyritic zone within a fine grained, silicified and

sericitized fragmental tuff. Scattered, deformed fragments of chert give a spotty and patchy appearance

to the tuff and, for this reason/ the unit is referred to as a "spotted mafic schist" by David R. Bell in his

work for Corona. The pyrite content varies from Q.5%

to occasional concentrations up to 101 and occurs as irregular patchy streaks and as fine to coarse grained disseminated crystals and crystal aggregates* Subor

dinate amounts of sphalerite, molybdenite and periodi

cally small grains of free gold occur within the pyritic zone. The fragmental tuff (spotted mafic schist) is

moderately sheared parallel to the bedding, has an

average strike of 107O (true azimuth) and dips north

at angles varying between 45 and 65 degrees.

SUMMARY fr CONCLUSIONS

To date, diamond drilling on the property of Corona

Resources Limited, which adjoins the Golden Sceptre

claim group on the east, has outlined a gold bearing

pyritic zone within a siliceous and sericitic fragmental tuff (Lake Superior Shear Zone) containing approximately one million tons of material grading .15 oz./ton in gold. The westernmost hole drilled to date by Corona is about 1,600 feet from the eastern boundary of Golden Sceptre's group. Information contained in some of the earlier reports on the area strongly suggests the favourable Lake Superior Shear Zone underlies the Golden Sceptre property. The gold occurrence sampled by T. L. Muir near Hemlo does not appear to be on strike with the- Corona zone and may be evidence of another zone of mineralization on the Golden Sceptre property.

On the basis of the analytical work carried out by Lake Superior Mining Corporation **nd, more recently, by Corona, there appears to be a direct correlation be tween gold and pyrite within the Lake Superior Shear Zone suggesting the possibility of using an electrical geo physical survey as an indirect but possibly effective and inexpensive method of exploring for gold along the favourable horizon. A geophysical programme using a VLF (Geonics EM-16) electromagnetic unit and a fluxgate (McPhar MF-2) magnetometer, was conducted by Corona over their property. The VLF survey failed to delineate the gold zone; however, the ground magnetic survey recorded a weak, positive anomaly coincident with the zone and was considered useful in guiding their drilling. Because of the disseminated nature of the pyrite minera lization on the Corona property, induced polarization may be the only effective electrical method of detecting the gold-bearing pyritic zone.

The description of the gold occurrence sampled by T. L. Muir of the Ontario Ministry of Natural Resources (pyritiferous felsic tuff) resembles the description of the Corona mineralization, yet no follow up sampling

-14- - - - . ' ,. - -

of the occurrence appears to have been carried out since the results of Muir's sampling were published in Open File Report 5280.

Although a number of weak, gold geochemical anomalies, including one significant anomaly of 10,000 ppm (albeit essentially one station anomalies) were outlined in the multi element geochemical survey carried out by Robert E. Schaaf S, Associates Inc. in 1977, no follow up work to assess the validity or the significance of these anomalies was attempted. A lack of adequate exploration funds and a depressed gold market in 1977 are believed to have discouraged further work on the property.

Recent work on the Lake Superior Shear Zone suggests that the zone may actually be a sericitized pyroclastic horizon which, because of its foliated texture, has been identified as a shear zone since it was first discovered in 1945. In a report on the Corona property, D. Bell describes the host rock as a fine grained, siliceous, sericitic and schistose fragmental tuff. Regardless of its true nature, the favourable gold-bearing host will probably have considerable geographic extent.

RECOMMENDATIONS

On the basis of the proximity of the Golden Sceptre property to the zone of gold mineralization being de lineated by diamond drilling by Corona Resources, Inc. and on the evidence that suggests the favourable Lake Superior Shear Zone {host pyroclastic horizon) extends onto the Golden Sceptre property, a comprehensive pro gramme designed to explore for gold-bearing zones of the Corona type on the Golden Sceptre property is warranted.

A two phase exploration programme is envisaged wherein the first phase should consist essentially of geological •apping* soil geochemistry, trenching, surface sampling and geophysical surveys. The second phase will be con tingent on favourable results from the first phase and should consist exclusively of diamond drilling.

A grid to provide the necessary control for the pro posed exploration programme should be constructed over the entire "*-operty. The grid should consist of a baseline oriented with an azimuth of 090O with cross- lines at intervals of 400 feet along the baseline. This should be reduced to intervals of 200 feet in the vicinity of any geophysical anomalies that are recorded and in the vicinity of any trenching that is carried out.

Detailed geological mapping of all outcrops should be carried out over the area encompassed by the control grid. Special attention should be devoted to identify ing and mapping alteration phenomena, including silici fication, sericitization and pyritization within the volcanics and volcaniclastic sediments. Where any evidence of these features is found, particularly pyritization, trenching and systematic sampling should be carried out.

Permission should be obtained from Corona Resources Ltd. to conduct an experimental geophysical programme using a variety of electromagnetic systems over their known zone of gold mineralization to determine which system most effectively delineates the zone. Follow ing this, A ground magnetic and electromagnetic survey should be carried out over the Golden Sceptre property in an attempt to locate pyritic zones, which theoreti cally should contain the highest concentration of gold, within the so-called Lake Superior Shear Zone.

-16-*

An effort should be made to locate the gold-bearing gossan xone sampled by T. L. Muir just east of Remlo (now believed to be encompassed by claim TB S76674). The zone should be exposed by trenching where practi cable and systematic sampling should be carried out.

A limited amount of detailed soil sampling should be carried out in the vicinity of the gold geochemical anomalies located by Robert E. Schaaf t, Associates Inc. to determine whether the anomalies are spurious or represent evidence of underlying gold mineralization.

As part of a geophysical survey proposed for the Golden Sceptre property, the Black River Valley, where a number of ground electromagnetic anomalies were outlined by Noranda, will be investigated. During this survey, special attention should be devoted to looking for evidence of diamond drilling in the vicinity of the Noranda work.

If not already under option to Corona or others, an attempt should be made to acquire or to negotiate an exploration option agreement on the Ollmann-Williams group of patented mineral claims between the Golden Sceptre and Corona properties.

ESTIMATE OF COSTS

Phase I

Control Grid S 27,500 (1)Geological t Geochemical Survey 15,000 (2)Geophysical Surveys 35,000 (3)Trenching d Sampling 10,000 (4)Chemical Analyses 3,500 (S)

i ' ^ "^ : "j*' - ^JSS- - —17— - - - - ' ^

Transportation 9 8 ,000 (6)Supplies 6 Equipment 10,000 (7) Engineering t Supervision 6,000 (8)Contingencies 10,000 ( 9)Total: 3125,000

Phase II^ ^^^-^^ *

Diamond Drilling 3125,000 (1)

Engineering d Supervision 4,500 (2)Chemical Analyses 3,750 (3)Contingencies " 16,750 (4)Total: 3150,000


The foregoing estimate of costs is based on an explora tion programme consisting essentially of geological mapping, soil sampling, experimental geophysics followed by syi-*-?:r,atic ground geophysical surveys and a limited amount of trenching and sampling. The costs are further based on the assumption the field programme will require approximately 3 months to complete.

(1) The sum of $27,500 estimated for the construction of a control grid allows for 100 line miles (baselines and gridlines) of cutting, chaining and picketing at a cost of S275 per line mile.

(2) The sum of 315,000 estimated for the geologicalmapping allows for the employment of one seniorgeologist on a contractual basis for a periodof 60 days at a rate of S250 per day to carry

-18-

out the proposed geological mapping, soil sampling and to supervise any trenching and trench sampling that is done.

(3) The amount of 335,000 estimated for geophysical~*surveys provides for 100 line miles of ground magnetic survey at S100 per line mile (310,000), an allowance of 55,000 for geophysical experi mentation and an allowance of 320,000 for either 35 line miles of induced polarization survey at approximately S600 per line mile or 100 line miles of an acceptable electrical survey (maxmin, TURAM, etc.) at 3200 per line mile.

(4) The sum of 510,000 estimated for trenching and sampling includes the rental of a rock drill plus operator for approximately two weeks.

(5) The figure of 33,500 estimated for chemical analyses provides for a total of 100 gold-silver fire assay analyses plus sample preparation costs at a unit cost of 315 per sample plus an allowance of 32,000 for soil sample analyses.

t

(6) The sum of 38,000 estimated for transportation provides for the mobilization and demobilization of personnel and equipment and all other field transportation requirements for the duration of the proposed field programme.

(7) The sum of 310,000 estimated for supplies and equip ment includes the cost of accommodation, general field equipment, equipment rental and all the food and fuel required for the duration of the proposed field programme.

-19-

(8) The sum of 56,000 estimated for engineering and

supervision allows for 20 days at 3300 per day and

would include programming and logistical planning,

direct programme supervision and the compilation and interpretation of all field data.

(9) The figure of 310,000 represents a contingencyfactor of approximately 8^ of the total estimated

programme cost.

EXPLANATION OF COSTS (Phase II)

Phase II of the programme proposed herein is contingent

on favourable results from the exploration programme

recommended in Phase I. The estimate of costs in Phase II, which would consist essentially of diamond drilling,

is based on a nominal programme involving 5,000 feet of drilling and on the assumption that the programme will

require approximately 2 months to complete. In the

event the results of the proposed diamond drilling in Phase II are favourable, considerably more diamond drilling will be required to assess the economic signi

ficance of the property.

(1) The sum of 3125,000 estimated for diamond drilling

allows for 5,000 feet of drilling at an all inclu

sive price of S25 per foot. This includes con

tinuous, on site engineering supervision and attendant transportation costs.

(2) As in Phase I, the estimate of 34,500 for engineer ing and supervision is based on a rate of 3300 per

day for 15 days and would include the planning and

supervision of the entire programme and the compila tion and interpretation of all the drill data.

. . -- - 20- y --'':- -V '

(3) The figure of S3,750 estimated for chemical analyses provides for a factor of SO.75 per foot against a proposed diamond drill programme involving 5,000 feet of drilling.

(4) The figure of $16,750 represents a contingency factor of 12Jj* of the total estimated programme cost.


Thomas Skimming, P J

Toronto, Ontario August 25, 1981

BIBLIOGRAPHY

Bell, David R. May 5 , 1 981

Phase I - Progress Report Corona Resources Limited/ Hemlo Property, District of Thunder Bay, Ontario

Greer, w.L.C. June 24, 1949

Memorandum on Property of Lake Superior Mining Corpora tion, Hemlo, Ontario

Greer, W.L.C. May 8, 1973

Report on the property of Ardel Explorations Ltd., in Township 73, Near Hemlo in the Thunder Bay Mining Division, Ontario, unpublished report

(Lyons, Edward M, July 6, 1977

R. Newman Hemlo Gold Property West Group, Molson Lake Area Thunder Bay Mining Division, OntarioRobt. E. Schaaf fi Associates, Inc., Geological, Geophysical and Geochemical Surveys unpublished report

Muir, T.L. 1978

Hemlo Area, District of Thunder Bay, Summary of Field Work, 1978, Ontario Geological Survey, Miscellaneous Paper 82 pp. 90-93

Muir, T.L. 1980

Geology of the Hemlo Area, District of Thunder Bay, Ontario, Ontario Geological Survey OFR 5280

Newbury, Michael June 3, 1974

Report on the Property of Ardel Explorations Limited, Hemlo, Ontario unpublished report

Northern Miner Various Editions

Page, Trevor w. September* 1947

Summary of Geological Reconnaissance Survey

Page, Trevor w. December 20, 1947

A Report on the Ollmann- Williams Group of Claims Hemlo, Ontario

Page, Trevor w, April l, 1948


Page, Trevor W. March 8, 1950

Outline of Diamond Drill Results on Hemlo, Ontario Property

Page, Trevor w. A-igust 21, 1950


Page, Trevor w, December 20, 1950

A Geological Report on the Struthers Group of Mining Claims, Hemlo Area, Ontario

Page, Trevor w. June 25, 1951

A report on the property of Lake Superior Mining Corporation Limited, Hemlo, Ontario unpublished report

Page, Trevor, W, undated

Interim Report on the property of Lake Superior Mining Corpora tion Limited, Hemlo, Ontario

Prospectus June 30, 1949

Lake Superior Mining Corporation Limited

HAP REFERENCES

Preliminary Hap No. P 494

Manitouwadge Sheet Ontario Department of Mines Districts of Thunder Bay and Algoma Scalei l* to 2 miles

Map 2220

Geological Compilation Series Manitouwadge - Wawa Sheet Ministry of Natural Resources - Ontario Scalet l" to 4 miles


Geological Series Healo Area (Northern Half) Ontario Geological Survey Scalei l' to 1/4 mile

Map 2167G

Geophysics Paper 2167 Airborne Magnetic Survey Herrick Lake Sheet Geological Survey of Canada Scales l" to l mile

Map 2156C

Geophysics Paper 2156 Airborne Magnetic Survey Heron Bay Sheet Geological Survey of Canada Scale: l" to l Mile

CERTIFICATE OF QUALIFICATION

I, THOMAS SKIMMING, hereby certify:

1. that I am a consulting geologist employed by Thomas Skimming 6 Associates Limited at Suite 306, 5233 Dundas Street, West, Toronto, Ontario

2. that I am a registered Professional Engineer inthe Province of Ontario and Manitoba and that I am a Fellow of the Geological Association of Canada

3. that I was born in Canada in the year 1935 and have been a Canadian citizen since birth

4. that I am a graduate of the University of Michigan 1958, with the degree Bachelor of Science (B.Se.) in Geology

5. that I have been practising my profession as a geologist continuously for twenty-two years

6. that I do not have, nor do I expect to receive,directly or indirectly any interest in the property reviewed herein or in the securities of Golden Sceptre Mines Ltd.

7. that my report is based on an examination of the Golden Sceptre property on June 3 and 4, 1981 and on several on site investigations of the adjacent property being explored currently by Corona Resources, Inc. The report is also based on a review of all *-he pertinent technical data published by the Ontario Ministry of Natural Resources and a study of the assessment work reports on file at the Assessment Research Files Office in Toronto, Sault Ste. Marie and Thunder Bay.

8. a diligent effort has been made to obtain allrecords and technical data pertinent to the pro perty reviewed herein and it is believed that these efforts have been successful and that the conclusions relating to the potential of the property have been reached with full recognition of the results of all the previous work, both positive and negative, carried out on the prope

Toronto, Ontario August 25, 1981 Thomas Skimming, P

'-*l l l ll l l l l l l l l3 l l lI l

GOLDEN SCEPTRE RESOURCES LTD.DIAMOND DRILLING

1982

Bomby Township Ontario

Or||| Hole GG-1 Drilled by

1 + 50N Bearing

Morrisette

ISO 0

D.portur. 0 + OOE Dip-75'

Logged by

Elevation Surface m

t , nnth 896 feet

David R. Bell Pog.

Dot. start t* Sept. 12. 1982

Dot. Flnl.h.d Sept. 18. 1982

FROM

. 0

3.65

28.0

86.1

t

TO

3.65

28.0

86.1

114.7

'

DESCRIPTION

Casing

Mafic Sediments - dark green to black biotiterich alterfcu jedimo.nts with patchy and mottled siliceous bands 37* - 40 0 C. A. Slump in bedding @ 14.5. Scattered streaks of py. and po. Some section of stretched or broken siliceous bedding. Porphyroblasts of quartz common.

Garnetiferous Mafic Sediments - as above, finegrained mafic sediments with scattered pink medium course grained garnets. Bedding 42 0 @ 38.0 M. Patchy brown staurolite to white sillimanite. 51 M. - 55 M. - Thinly bedded light to medium

grey-brown greywackes. Bedding 45" C. A.

64.1 M. - Three irregular quartz blebs. 67.8 M. - Siliceous bedding 55 0 C. A. 72.7 M. - 1 cm. quartz vein 55 0 C. A.

Greywacke - medium grey to medium green fine grained greywacke and mafic sediments. Some zones are more silicified than others. Bedding 55 0 - 57 0 to C. A. Intense staurolite and sillimanite alteration within the mafic sediments at the upper contact @ 85.6 - 86.1 M. 88.1 M. - 12.5 cm. white quartz vein, Tr. py.

po- 88.5 M. - 1.0 cm. quartz @ 65 0C.A. 3-5Z po/py

SAMPLE

NO.WIDTH

ASSAY VALUES

Au.

Drill Hole GG-1 Drilled by Morrisette by David R. Bell Pose

1 + 50N Bearing 180 Elevation Surface

Departure 0+OOE -75 896 feet

~ . e , Sept. 12/82 Daft Sforttd r____'

Sept. 18/821 ————————— ~-K ——— — ————————————— i.enqrn —— ^.^ — ,....— Dot* Flniihad

FROM

86.1

114.7

J

u

TO

114.7

179

i

1 — — - ————————————— - ————————————————————— —— ————————— I^/J.-L

DESCRIPTION

99.6 M. - 2.0 cm. irregular quartz, Tr. po/py. 104 M. - 56* bedding to C. A.107.3 - 107.7 2-3 mm. pyrite seam, Trace

disseminated pyrite. 107.7 - 109.2 1-2Z disseminated pyrite in

siliceous greywacke, scattered blue-grey quartz.

114.3 - 114.7 white barren quartz vein with rocky inclusions Trace pyrite.

Mafic Sediments - fine grained, thinly beddedaltered slatey-greywackes, medium green to grey green. Trace scattered garnets. Irregular narrow scattered quartz fractures. Bedding 60 C -63 0 to C. A Trace disseminated pyrite in more slatey sections. Increasing frequency in scattered siliceous solutioi brecciation from 129.0 M. From 137.0 M. onhematite alteration increases, along with the rare narrow 1-2 mm. calcite fracture, and apple green epidote alteration. 138.7 - 2.0 cm. white quartz fracture, Trace

pyrite 45 0 C. A. 140. 7 - 3.0 cm. quartz, 50 0 C. A., Trace pyrite 142. 7 -4.0 cm. quartz, Trace pyrite 1 4 6.9 - 147.6 - four 1-2.0 cm. quartz fractures

50" C. A. , Trace pyrite 149.8 - 150.6 - intense epidote alteration with

four white quartz fractures 55 0 -60 0 C. A., Trace pyrite

151 M. - from this point, there is less epidote, hematite and solution brecciation.

irerr-PH

SAMPLE

NO.

9701

9702

WIDTH

0.4

1.5

ASSAY VALUES

Au.

.002

.006

3 ^mWiDrm HOI* Wi-i nrin.d bv morrisette ( o eotd b y u-v*u *. — ** Paot - , .

Lotltu

Dtport

FROM

114.7

179

189.4

192.8

180 0 Surfaced* —— 1 * ciflN ————— Storing , Pleuatlnn

ur. ..0+OO.E mn -75 0 ,.n 9th896 feet (273.1 metres,

TO

179

189.4

192.8

211.65

DESCRIPTION

158.0 - Bedding 68 0 C. A. 161.4 - 9.5 cm. white quartz, Trace pyrite 178.2 - 1.0 cm. white quartz, 40 0 C. A. 173 M. - Bedding 70 0 C. A.

Interbedded Mafic and Siliceous Sediments- fine grained, green mafic beds interbedded with buff to white siliceous bedding 66 0 -68 0 to C. A. Siliceous beds are narrow from 0.5 - 2.0 c. m. Scattered irregular quartz fractures, several indicating boudinaging between bedding planes.181.8 - 181.9 - Diabase breccia, contact 25 0 -30 0

C. A. ,Trace pyrite 190.4 - 190.6 - Fine grained, medium grey chilled

diabase wedges.

Diabase Dyke - upper contact chilled light grey30"-35 0 C. A., general texture is dark grey to black, fine grained and uniform. Badly broken due to numerous irregular fractures. Lower contact badly broken.

Mafic Sediments - dark to medium green bedded maficsediments with scattered narrow section of thinly bedded siliceous sediments. Bedding 68" C. A. Scattered irregular quartz veins.203.6 - 204. 0 - 702 irregular quartz, Trace black

tourmaline, Trace pyrite. 208.5 - 6.0 cm. white quartz, Trace pyrite 211.65 - contact with diabase @ 50 0 C. A.

1-2 cm. fine grained chill margin

SAMPLE

NO.WIDTH

Dot* Sto

3of* Flnl

M. .Sept. 12/82

^ Sept. 18/82*h*d r

ASSAY VALUES

Au.

Drill Hole GG-1Drilled by

Bearing

Morrisette 180 0

Logged byDavid R. Bell Page

SurfaceElevotlon Oat* Started Sept.12/82

Deport

FROM

211.65

0

ur. o+OOE DIB -75 0 ,, ni? , h 896 feetOT\ i n mpt-r

TO

273.10

DESCRIPTION

Diabase - dark green, medium to course grainedp'yfoxehe rich diabase. Massive and uniform with scattered narrow irregular olive green epidote fractures. Trace po. and patchy disseminated magnetite. Magnetism is weak to moderate. Under .52 pyrite throughout/ possibly some pyrr. Fresh and unaltered. Occasional graphitic slips @ 20-45 0 C. A.

END OF HOLE #1

^ m ^. Acid Tropari AzimuthsD ip l e s c s : ——— —— c —— ——————100' -70 -74.5 -180 0 200' -63.5 -68 186 0 300' -56.5 —— 400' -52.5 -53 192" 500' -49.5 —— 600' -47.5 -47 700' -47 —— 800' -46 -54 177 0

SAMPLE

NO.

PR)

WIDTH

Date Flni.t.d SeP C ' 18 / 82

ASSAY VALUES

Au.

-

HOI. r.fi-9 by Morrisette Logged by Don Esson Pogt

Latitude.* 5 0N

Departure O * 50E

Bearing

Dip

180'

-80 0Surface Dot* 3tarftd Sept.

.. nn *h 396.85 metres ___(13UZ teet)

Dott cuii.h.nSept. 23/82

FROM TO DESCRIPTIONSAMPLE

NO.WIDTH

ASSAY VALUES

Au.

O

4.27

12.0

13.55

4.27

12.0

13.55

57.8

57.8 92.0

Casing

Mafic (Biotite) Sediments - medium grey to black- brown thinly bedded (slatey) mafic sediments. Narrow light grey greywacke beds. 35 C -36 C C.A. Well sheared @ same angle.

Diabase (Dyke) - well crystallized, chilled upper contact.Contact ground could be 45 e to C.A. Pyrite 1-2Z.

Mafic (Biotite) Sediments - as before23.8 - Miiior quartz-calcite veining

- Irregular 2 1 pyrite36.0 - Core angles changing gradually to 50 0 36.0-41.7 - More amphibolide41.7-57.8 - More siliceous and biotitic

- Numerous greywacke beds- Bedding less obvious than before

C.A. 55 C ±5 0

Mafic (Garnetiferous) Sediments - C.A. 60 059.8-60.0 - Alteration zone. Some brecciation

- Siliceous. Epidote veining.67.4 - 92.0 - Staurolitic.

71.75 - 71.95 - Brecciated.85.0 -85.5 - highly chloritic, carbonaceous

shear.

Drill HOle GG-2

Latitude.SON

Drilled by Morrisette

ISO 0

Logged by Don Esson Page

Departure O -* 50E

Bearing

Dip-80'

Elevation Surface

Length 396.85 metres

Dot* st*r*.d Sept. 14/82

Dott Flnlihid Sept. 23/82

FROM

92.0

116.37

9

TO

116.37

325. Of

DESCRIPTIOI*

Mafic (Amphibolitic) Sediments - garnetiferousand staurolitic.110.3-110.5 - k quartz vein. Sub-parallel to C. A.

Vuggy, 52 pyrite.

Mafic (Biotitic) Sediments117.2 - 117.35 - Highly altered. Bleached,

chloritic. Some calcite.118.25 - 121.0 - Staurolitic. No garnets.121.0 - 145.0 - Many chert beds, siliceous.

C. A. 60". Minor staurolite. 121.0-127.0 - Garnetiferous 133.08-133.25 - Bull quartz vein. C. A. 60":

Barren. 142.34-145.04- Solution breccia.

145.0 - 180.3 - Biotitic. Occasional scattered garnets. No staurolite. Cherty l disseminated pyrite.

153.6 - 6" brecciated. 160.6 - 6" brecciated. 162.0 - 6" brecciated.167.82 - 168.05 - Bleached, silicified.

Minor tourmaline crystals. 12 disseminated pyrite.

173.76 - 174.6 - Silicified, hematitic, chloritic. Some epidote.

SAMPLE

NO.WIDTH

ASSAY VALUES

Au.

DMIl Hole GG-2Drilled by

MorrisetteCogged bv Esson Poge

Lotltode

D . PO Mur. 5QE

Searing

Dip

180'

-80'Elevation

Length

Surface

396.85 metresDot* Started

Dart Flnlthtd

Sept. 14/82

Sept. 23/82

FROM

0

TO DESCRIPTION

174.6 - 175.47 - Bleached, massive, silicious, hematitic. Scattered epidote Shematitic veinlets.

175.5 - 176.8 - 3 minor quartz veins with hematite and epidote. 22 pyrite.

177.4 - 177.7 - Bull quartz. Minor pyrite and hematite at contacts. C. A. 50 0 .Slight MoS 2 on upper contact.

179.4 - 179.6 - Quartz vein. Minor hematite. C. A. 50".

180. 3 - 204.3 - Significant increase in alteration- quartz veins, calcite, epidote, hematization.

194.65 - 194.79 - Bull quartz vein. Few specks pyrite.

199.0 - 199.65 - Quartz hematite, chlorite, epidote zone. No sulphides. C. A. 50".

204.3 - 325.6 - Alteration as above continues butmuch less pronounced.

212.19 - 212.64 - Quartz veining, irregular. Some epidote.

213.58 - IV Quartz - chlorite vein. Barren.213.89 - 213.92 - Quartz - chlorite vein.

Barren .214.6 - 215.9 - Quartz "eyes".222.49 - 222.61 - Irregular quartz veins, k "

pyrite s'fjpp nn lower rnnfact.

SAMPLE

NO.WIDTH

ASSAY VALUES

AU.

Drill Hole GC-2

Lotltude.

Departure

SON

Drilled by Morrisette ISO 0

Scoring

Logged bv pQ" Esson

Surface

Poge

50EDip

-80'Elevation

Length396. o5 metres

Dot. start.. Sept. U/82

23 /82DO,. FinUH.d

FROM

9

TO DESCRIPTION

222.8 - 223.79 - Silicified zone with 22 pyrite as blebs and veinlets.

227.75 - 227.86 - Silicified, cherty, 42 pyrite228.17 - 229.3 - Bleached, weakly silicified.

Light green.233.47 - 234.3 - Bleached, weakly silicified.

Light green.235.4 - 252.58 - Increasing bleaching as beds

and bands. Occasional 1" chloriteband with weak calcite. Slight pyrite. C. A. 55" ± 5 0 .

252.58 - 253.20 - Intensely bleached. Strong epidote. Minor hematite.

254.00 - 254.28 - As above.256.40 - 257.42 - Bleached, chloritized.

Cherty beds.257.42 - 261.00 - Much reduced alteration.261.0 - 261.86 - Bleached. Chloritic.

Irregular quartz veins.261.86 - 263.45 - Much reduced alteration.

Some staurolite.262.95 - 1" quartz vein @ 50 0 . Minor pyrite and MoS 2

263.45 - 263.79 - No alteration. C. A. 45".Well bedded

SAMPLE

NO.

*

WIDTHASSAY VALUES

Au.

D'll! HOU GG-2

Lotltudt,SON


togged by Pogt

Bearing ElevotlonSurface

P* M rtur. 50E Dip-80 0

Length396.85 metres

Der, **.r*.j Sept. U/82

Dot. F,n..h.d SePt- 23/ 82

FROM

ft

TO DESCRIPTION

263.79 - 268.10 - Cherty, chloritic. Some staurolite. Minor bleach beds.

268.10 - 269.44 - Massive. Spotted mafic sediments.

269.44 - 269,65 - Cherty.269.65 - 270.26 - Cherty. Chloritic. Bleached

22 pyrite as veinlets and blebs.271.20 - 271.53 - Irregular bull quartz.

Chloritic. Minor epidote.272.20 - 272.91 - Cherty. Chloritic. 2 1 pyrite

as blebs.2^.61 - 275.05 - Bleached. Chloritic. Epidote.275.05 - 298.0 - Intermittent bleached,

chloritic zones. Occasional staurolite crystals. C. A. 60 0 ± 5 C .292.3 - 2" quartz vein. Barren. 294.4 - 1" quartz vein. Barren. 297.85 - 3" quartz vein. Barren. Chloritic, staurolitic.

298.0 - 300.8 - Increasing staurolite.304.4 - 304.6 - Bleached.305.0 - 306.3 - Occasional bleached zone.

Scattered staurolite. C, A. 50 0 .306.3 - 308.3 - Scattered staurolite. Occasion

al chloritic, pyritic bands. C. A. 60 0 .

SAMPLE

NO.

F9703

WIDTH

0.61

ASSAY VALUES

Au.

.004

Hi Hole GG-2

Latitude, l t- SON

Drilled by ^Morrisette ISO 0

Logged by —. Don Esson Pogt

Bearing Elevation Surface

Deporture 50E Dip-80'

Length396,85 metres

Dote Storied

Dote Flnlthtd

Sept. U/82

Sept. 23/82

FROM

J25^

TO

344.06

DESCRIPTION

308.3 - 317.7 - Increasing staurolite. Occasional bleached zone. 314.9 - 2" quartz vein, barren.

317.7 - 320.17 - Staurolitic and garnetiferous. Some sillimanite. More amphibolitic . Occasional bleached zone.

320.17 - 320.62 - Porphyritic. Indistinct.320.62 - 322.4 - Amphibolitic. Dark green.

Faintly phorphyritic or crystalline. No mineralization.321.6 - 322.0 - Quartz veining and silicified. Epidote veinlets.

322.4 - 325.06 - More siliceous and biotitic. Minor garnets. Fair sillimanite. Fairly well mineralized with pyrite 2-52. C. A. 60".322.85 - 322.98 - Porphyritic. Weak crystalline.323.81 - 323.93 - Porphyritic. Weak crystalline .324.13 - 325.06 - Much increased silicification. Pyrite 42.322.98 - 324.13 - Pyrite 22324.13 - 325.06 - Pyrite 42

Tuff, Siliceous S SericiticModerate to well sheared. C. A. 60 C . Well mineralized with ovrite and

SAMPLE

NO.

?-9704-•-9705

WIDTH

1.150.93

ASSAY VALUES

Au.

OZ/T

.002

Trace

Agg/t

Tr.Tr.

MoS,2

.002.003

Drill Hole GG-2

i a t it..n. l * SON

Oeporture Q * 5QE

Drilled by Morrisette 180"Storing

Logged by Don Esson

Surface

Pag*

Dip-80'

Elevation

Length

Dot* StartedSept. 14/82

396.85 metres Dore Flnlihtd Sept. 23/82

FROM

329.62

331.74

TO

331.7'

334. 7(

334.70.' 337.7

t

DESCRIPTION

molybdenite as noted.325.06 - 326.00 - 52 pyrite. Slightbedding @ 60 0 326.00 - 326.86 - very sericitic.52 pyrite.

326.86 - 327.04 - Porphyry. Nomineralization.

327. 04 - 328.04 - Increasing MoS 2 6pyrite 57.. 328.04 - 328.71 - Increasing MoS 2 Spyrite 52. 328 71 - 329.62 - Quartz vein. Barren.High MoS 2 and 5-lOZ pyrite.Frequent quartz veining.Very vuggy. Core recovery 90Z.329.62 - 330.66 330.66 - 331.74Same as above but much less vuggy and reduced pyrite, maximum 52.Badly broken, recovery 802 from331 - 334m., minor fuchsite.331.74 - 332.74 332.74 - 333.74 333.74 - 334.70

, Same as previous section but increased pyrite, local concentrations to 30Z. Average 107. -K

SAMPLE

NO.

F9706

F9707

F9708

F9709

F9710

F9713

F9714 F9715

F9716F9717 F9718

WIDTH

0.94

0.86

0.18

1.0

0.67

0.91

1.04 1.08

1.01.0 0.96

ASSAY VALUES

Au.

OZ/T

.002

.012

.006

.078

.139

.035

.237

.103

.187

.788

.369

Ag.g/t

Tr.

Tr.

Tr.

1.37

1.03

1.03

2.74 1.71

0.692.40 2.06

MoS 2Z

.003

.010

.007

.048

.090

.012

.095

.113

.205

.174

.242

CheckOZ/T

j

.079

.360

DHII HGle Don Esson 8

Lotltude ,50N

Oiporturt0 -r 50E

Drilled by uul l •Laei- l- c

180 0Bearing

-80 0DID

Loooed bySurface

Flevotion

396.85 metresLength ,

Pooe

Sept. 14/82Dot* Started .. ,, l lii-li ,, , il

Da f* plfîihfd oept . i. j Jot,

FROM

337.75

339.45

i

344.06i

&46.Si

TO

338.45

344.06

346.8

355.92

DESCRIPTION

Locally staurolitic. Frequent vugs. Occasionalfuchsite.334.70 - 335.70 335.70 - 336.70 336.70 - 337.75

Much more massive. Sericitic. Chloritic.Little MoS 2 . Pyrite - 1-22.337.75 - 339.45Much more molybdenite and pyrite. Occasionalvugs. Scattered fuchsite. Scatteredquartz veins.339.45 - 340,45 - Very heavy pyrite, 15-202and molybdenite .340.45 - 341.45 - Reduced pyrite (52) and MoS 2 .341.45 - 342.45 - Same as F9724.342.45 - 343.45 - Pyrite 52 and increased MoSj343.45 - 344.06 - Same as F9726 except last.25m. highly siliceous with quartz veining.

Porphyry - Weakly porphyritic. Dark grey. Massive346.55 - 347.47 - Ground Core. 6CZ recovery.344.06 - 346.8

Tuff, Sericitic. Siliceous- Heavily mineralized with pyrite S MoS;. Moderate!)well sheared. C. A. 66"

SAMPLE

NO.

F9719 F9720 F9721

F9722

F9723

F9724F9725F9726F9727

F9728

WIDTH

1.0 1.0 1.05

1.7

1.0

1.01.01.00.61

2.74

ASSAY VALUES

Au.

OZ/T

.357

.244

.518

.080

.419

.549

.265

.106

.059

.008

Agg/t

1.03 3.43 0.69

.69

2.74

2.741.031.030.69

Tr.

MoS 22

.195

.285 ,162

.008

.219

.239

.354

.172

.170

.003

Checkoz/T

.275

Drill HoltGG-2

Drilled by Morrisette Don Esson Peg*

Lotltude,SON

Dtportur*O -f 50E

Beorlng

Dip

180'

-80'

FI.—I™ Surface

.....K 396.85 metres

*... ...r,.- Sept. 14/82

B.,. ,, B ,.K.H Sept. 23/82

FROM

355.92

9

TO

i96.85

DESCRIPTION

346.8 - 347.37 - Mainly quartz vein with MoS 2 .347.7-347.9 - Quartz veining with fuchsite.

Pyrite on fractures.346.8 - 347.8347.8 - 348.8 - Very heavy pyrite 20Z+ and heavy

MoS 2 .348.8 - 349.8 - Ditto F9730 but less pyrite, 10Z+349.8 - 350.8 - Ditto F9730, pyrite 15Z350.55 - 350.74 - Chloritic dyke (sill?)350.8 - 351.8 - Ditto F9731, pyrite 10Z351.8 - 352.8 - Ditto F9731, pyrite 107.352.8 - 353.8 - Pyrite 102. Lost 0.5m core @

353.3-353.8 (Few segments left)353.8 - 354.8 - Less pyrite and MoS : .

354.23 - 354.59 - Weakly porphyritic dyke.Lost 0.15 m. probably g 353.8.

354.8 - 355.92 - More siliceous. Less MoS ? tpyrite except 355.8-355.9, Pyrite 40Z,Lost 0.6 m. core 355.0-355.7.Contact fairly sharp @ 60 0 . Vuggy @ contact.

Quartz Sericite Schist, Quartz Eyes- Siliceous, light , rey , well sheared. Indistinctbedding C. A. 60". Jonsiderable epidote. Tourmal ine common. ?',;ne staurolite. Occasionally vuggyand bleach.

355.92 - 357.0357.0 - 358.0358.0 - 359.0

SAMPLE

NO.

F9729F9730

F9731F9732

F9733F9734F9735

F9736

F9737

F9738F9739F9740

WIDTH

1.01.0

1.01.0

1.01.01.0

1.0

1.12

1.081.01.0

ASSAY VALUES

Au.

OZ/T

.200

.277

.206

.491

.3*9

.669

.212

.240

.339

.256

.010

.008

Agg/ 1

.1712.40

2.063.43

1.713.431.37

1.71

3.09

3.77Tr.n/a

MnS n Z

.187

.175

.220

.207

.246

.174

.299

.138

.380

.018

.010n/a

Check

.449

.325

Drill HoleGG-2

Lotltude, SON

Drilled by Morrisette 180 0

togged by Don Esson Pag* ^ 10

Bearing ElevationSurface

Dtpor' artO t 50E

-80'Dip Length

396.85 metresDate Started

Daft Finished

Sept. 14/82 Sept. 23/82

FROM

l

!

TO

*

DESCRIPTION

359. A3 - 360.86 - Dark grey feldspar porphyry.102 silicified sericite schist. Vaguelyporphyritic massive sills.

360.86 - 362.41 - Silicified bluegrey sericitictuff. Weak pervasive MoS 2 throughout withoccasional visible speck of MoS 2 .Scattered banding and sericitic fractures@ 65" to C. A.

363. 41 - 396.85 - Quartz eye sericite schist.Pale yellow-grey schistose tuff.

362.41-363.90 - Moderately sericitic +1Ztourmaline +.S to 1Z pyrite in upperpart17, s treaks of pyrite plus more silicifiedin lower part.

363.9 - 364.9 - Moderately silicified 1Zpyrite streaks yellowish-grey.

364.9 - 365.5 - Silicified 2-3Z pyrite streaksscattered coarse MoS 2 flakes.

365.5 - 367 - Weakly silicified moderatelysericitic .5 to 1Z pyrite Mafic dyke366.3-366.7 Sharp contacts 6 50 0 to C. A.More sericitic and tourmaline from 366.7

367 - 368.5 - Moderately silicified, sericitic 1Zvery fine pyrite scattered fine flakes ofMoS 2 .

SAMPLE

NO.WIDTH

ASSAY VALUES

Au. i

Drill HOUGG " 2

Drilled byMorrisette

Logged by Don Esson Pag* 11

i I.,I...H. -50N

Deportur* 50E

Bearing

Dip

180'

-80 0Elevation

SurfaceOar* Started

Sept. 14/82

Length396.85 metres oat. Finished Sept. 23 /82

FROM

9

TO DESCRIPTION

368.5 - 370 - Moderately sericitic, schistose trace fuchsite, MoS z 1-22 pyrite (streaks).

370 - 371 - Very sericitic, pyritic (52) grey, schistose, coarser grained. 370.33-370.64 vague feldspar porphyry.

371 - 372.5 - Highly sericitic schistose (55 0 to CA) 371.07 - 371.16 - Mafic dyke contacts sharp 50 0 to C. A.371.5 - 372.2 - Vague feldspar porphyry.

372.5 - 373.5 - Highly sericitic, rather coarse grained pyrite 2-52 coarse in places.

3^3.5 - 375 - Highly sericitic 3-52 pyrite Two narrow quartz veins, sericitic mud on contact of quartz vein at 374.2.

375 - 376.5 - Minor sericite. Minor pyritic bands. Minor fuchsite Pyrite 2-32 generally fine grained 20 cm. quartz vein at 376.3-376.5.

376.5 - 378 - Rather uniform, only weakly sericitic Trace fuchsite (wisps) .52 fine pyrite Minor quartz eyes.

378 - 379.5 - As at 376.5 - 378.379.5 - 381 - As at 376.5 - 378. 22 quartz eyes.381 - 382.5 - 22 quartz eyes. Minor tourmaline.382.5 - 384 - Moderately sericitic, slightly more

grey 3-52 quartz eyes 12 pyrite.

SAMPLE

NO.WIDTH

ASSAY VALUES

Au.

\

Drill Holt GG-2DHlled by Morrisette

Logged b yDon Esson Poge 12

Latitude

Departure

50N

50E

Bearing 180"

-80 0Dip

Elevation

Length

Surface

396.85 metresDote Started

Datt Flrithed

Sept. 14/82

Sept. 23/82

FROM

*

TO

396.85

DESCRIPTION

384 - 385.5 - Yellowish sericitic schist 5-102quartz eyes to 4 mm x 2 mm * scattered browntourmaline.

385.38 - 385.77 - 602 feldspar porphyry sill"^" coarse white feldspars set in a weaklychloritic ground mass. Feldspar phenocryst202 (up to 5 mm. in diameter)

385.5 - 387 - Tourmaline and quartz eye richsericite schist (highly sericitic) .52 pyriteUp to 52 tourmaline over short sections.

387 - 388.5 - 102 quartz eyes 3-52 brown-blacktourmaline .52 pyrite.

388.5 - 390 - As at 387-388.5 Minor MoS, fracture@ 389.62.

390 - 391.5 - As at 387-388.5 but 22 tourmalineSchistosity 60" 390.4-390.5 mafic dyke.390.69-391.08 mafic dykes (2) with tourmalineon contacts.

391.5 - 393 - 102 quartz eyes plus 32 fine blacktourmaline .5 to 12 pyrite

393 - 394.5 - As at 391.5-393393.8-394 - mafic feldspar porphyry hematizedfor 5-10 cm. on both contacts.

394.5 - 396 - As at 391.5-393 22 tourmaline.396 - 396.85 - As at 391.5-393 12 tourmaline.

END OF HOLE t l

SAMPLE

NO.WIDTH

ASSAY VALUES

Au.

Drill HoleGG-2

Lotltude. 50N


Logged by Don Esson Peg* 13


Deporture50E

Dip-80'

Length 396.85 metresDate Started

Dote Finished

Sept. 14/82

Sept. 23/82

FROM TO DESCRIPTION

Dip Tests: Acid Tropari Azimuths

50' -78 - —— ——100' -78 —— ——200' (61m) -73 -75" ISO 0300 1 -73 - — - —400' (122m) -73 -74' 181 0500' -70 ——600' (183m) -71 -70 0 194"700 ' -67^ -700 195 0800' (244m) -65^ -68 0 ——900' -64 —— ——

1,000' (304.8m) -61 -62 0 184 01,100' -56 ----1,200' (365.8m) -56 -58 0 197 01,300' (396.2m) -54 -53 8 197. 5 0

SAMPLE

NO.WIDTH

ASSAY VALUES

Au.

Drill HOU GG-3Drilled by Morrisette

L otlfudeION

Beorlng175'

Departure O * 15E Dip-80'

Don EssonLooaed by

r..*...*. Surface

L...,h 3 59 ' 3 metres

Poge

(lot. Start. 4 . , ®P

Sept Dote Finished v

1*

t. 19/82

. 26/82

FROM

0

3.66

TO

3.66108.18

•1

DESCRIPTION

Casing.Mafic ;Biotitic) Sediments- Ligh. -ârk grey to black. Garnetiferous.Scattered tourmaline crystals. Occasional stauro-litic zones. Light pyrite mineralization. Pervasivebiotite.3.66 - 7.9 - No bedding, very fractured.7.9 - 11.9 - Indisr.inct bedding. Core Axis 40".

Sheared parallel bedding.11.9 - 17.50 - Very garnetiferous. Some staurolite.

Occasional narrow bleached zones.17.50 - 21.68 - No garnets or staurolite.

20.11 - 20.23 - Fault brecciated.21.68 - 22.0 - Amphibolitic.22.0 - 26.5 - Garnetiferous. Staurolitic.26.5 - 28.35 - Quartz - feldspar rich. Very

biotitic. Numerous tourmaline crystals.28.35 - 50.60 - Garnetiferous. Staurolitic.

Narrow bleached zones.29.3 - 29.57 - Quartz. Badly broken up core31.85 - 32.05 - Bleached. Staurolitic.33.10 - 33.23 - Quartz veining. Some epidot41.05 - 41.29 - Quartz vein. Some epidote.

Barren.50.60 - 65.54 - More siliceous, sometimes cherty.

Light - medium grey. Core Axis 45". Lightstaurolite. Very few garnets. Occasionaltourmaline. Very little pyrite.60.54 - 61.0 - Cherty. Minor pyrite. Fair

epidote. 64.95 - 65.17 - Tourmaline rich zone.

SAMPLE

NO.

k- *

WIDTHASSAY VALUES

Au-

k

-

f****

Drill HOU

-f ION

OtpoMure

Drilled by ^ Morrisette

Bearing

Dip __

Logged by Don Esson

Eltvotlon Surface

-80'Length 359.3 metres

st,,,.* Sept. 19/82

Dot. PLUM* S eP c ' 26 '82

FROM

o

. TO DESCRIPTION

65.54 - 68.0 - Staurolitic. Garnetiferous. Morebasic. Dark grey - black. Core Axis 50 0.67.37 - 67. 49 - Tourmaline rich zone.

68.0 - 83.44 - Scattered garnets. No staurolite.Core Axis 50". More siliceous. Fairlywell -bedded.69.71 - 70.51 - Cherty zone with pyritebands. Approximately 42 pyrite.71.5 - 2" quartz tourmaline.72.0 - 3" quartz tourmaline.72.24 - 2" quartz tourmaline.73.65 - 74.10 - Weakly bleached zone.74.24 - 75.00 - Bleached. Silicified.2" quartz vein at 74.7. Brecciated in part.81.81 - 83.44 - Brecciated. Carbonated.Hematitic. No sulphides.

83.44 - 86.54 - Fractured at various angles.Occasionally brecciated. No garnets. Weaklyhematitic. Dark grey. Core Axis 50".

86.54 - 102.3 - Weakly garnetiferous. Occasionalstaurolite crystals. Dark grey. Occasionalbleached silicified zones.89.44 - 91.80 - Silicified. Partlybrecciated. Pyrite 52.99.64 - 101.71 - Weak porphyritic bedsinterbedded with mafic sediments.

102.3 - 108.18 - Amphibolitic. Occasional tourmal ine crystals.102.3 - 103.83 - Epidote zone.106.1 - 107.39 - Coarsely crystalline.Chloritic. Tourmaline. Irregular quartz.Pyrite 2-32.

SAMPLE

NO.

F9711

F9712

WIDTHASSAY VALUES

Au.

Trace

Trace

Drill Holt GG-3

ION

Drliitd by Morrisette 175"

by Esson Poo*

Btorlng Elevotlon Surface

15E Dip-80'

Length359.3 metres

Oat* Stortid

Dot* FlnUhtd

Sept. 19/82

Sept, 26/82

FROM

108. 1?

120.88

9

TO

120.88

246.65

DESCRIPTION

Greywacke- Light to dark grey. Very siliceous. Poorly defined bedding. Core Axis 60 0 . 116.1 - 116.21 - Quartz vein. Barren. 119.65 - 120.88 - Brecciated. Recemented with

epidote veinlets.Mafic (Biotitic) SedimentsCore Axis 50*. Frequent epidote veinlets. Light to dark grey. No garnets or staurolite. Pervasive biotite. Occasional cherty or greywacke beds. 126.5 - 126.7 - Brecciated. 128. A - 128.8 - Irregular quartz veins and hematitii

staining. 135.1 - U3.38 - Very dark and biotitic. Slightly

porphyritic Dike? Sill? 135.1 - 135.86 - Faintly porphyritic. 136.34 - 137.76 - Faintly porphyritic. 136.82 - 136.95 - Quartz vein. Slight

fuchsite. 140.85 - 2" quartz, calcite, biotite with

large pyrite crystals. 141.80 - 141.98 - Quartz veining. Barren.

143.38 - 173.0 - More siliceous. Bedding more apparent. Core Axis 60 0 . Chloritic. Well sheared. Considerable epidote. 160 - 160.8 - Bleached. Tourmaline. Chlorite 166.21 - 166.44 - 1" quartz sub-parallel

core. Barren. 167.0 - 168.02 - Bleached. Chloritic. 169.55 - 170.2 - Bleached. Chloritic.

SAMPLE

NO.WIDTH

ASSAY VALUES

Au.

Drill Holt GG-3

IONLotlfudt, Beorlng175'

Dtporture 15E Dtp-80'

Elevation

Length

Surface

359.3 metresDaft Storttd

Dart Finished

Sept. 19/82

Sept. 26/82

FROM TO DESCRIPTIONSAMPLE

NO.WIDTH

ASSAY VALUES

Au.

173.0 - 196.65 - Cherty beds. Chloritic. Biotitic. Occasional weak garnets. Core Axis 60*. Considerable epidote. Well-bedded for the greater part. 184.7 - 185.6 - Bleached. 185.24 - 185.43 - Brecciated.

196.65 - 208.14 - Siliceous. Light grey - greenish grey. Bleached? Well-bedded. Core Axis 60 0 . Considerable biotite and muscovite. Epidote common. Occasional narrow (to 12") beds faintly porphyritic. 207.57 - 208.03 - Porphyritic dike. Moderately well developed phenocrysts. Sheared at 60'. 209.0 - 209.11 - Quartz biotite, chlorite.

208.14 - 220.24 - More basic and massive. Biotitic. Bedding indistinct. Core Axis 50 C . Scattered garnets. Sparse pyrite. 219.0 - 219.39 - quartz chloritic vein. Barren.

220.24 - 225.07 - Bedding more apparent. More siliceous.

227.07 - 240.45 - More basic but still fairly well-bedded. Frequent chloritic bands. Occasional staurolite.240.0 - 240.45 - Bleached, quartz veined. Vuggy.

240.45 - 246.65 - More siliceous. Well-bedded. Core Axis 50 e . Frequent bleached and/or

DMII Hole GG' 3Drilled by Morrisette

175'Logged b y Don Esson

-,. .,. Surface

POO*

Sept. 19/82r

D...r,ur. 0 * 15E m o -80" i M-th 359.3 metres

FROM

J46.65

J49.45

285.30

J87.10

188.2

9

TO

249.45

285.30

287.10

288.2

291.39

DESCRIPTION

Basic Porphyry Dike- Fairly well developed phenocryst. Contact quite sharp, little alteration, slightly bleached. Core Axis 47 C .Mafic (Biotitic) Sediments- Light to dark grey. Fairly well-bedded. Core Axis 50 0 . Much staurolite. Scattered garnets. 254.5 - 282.2 - More siliceous. Reduced staurolite.

Scattered garnets. Light- medium grey. Scattered bleached zones (narrow) and minor quartz veins. Core Axis 47 e . 262,34 - 262.49 - Minor porphyritic dike. 265.66 - 266.14 - Bleached. Siliceous.

282.2 - 285.3 - Increasing staurolite, garnets, and sillimanite.

Porphyry Dike (Sill?)- Weakly porphyritic. Well sheared. Contacts indistinct.Mafic (Biotitic) Sediments- As before. Generally more siliceous. Core Axis47 a 287.15 - 287.29 - Minor porphyritic zone. Weak. 287.35 - 288.04 - Bleached. Epidote rich.Felsic Sediments (Biotitic)- Moderately to lightly serecitic. Well sheared. Core Axis 47 C . 2-4Z pyrite. Some tourmaline.288.6 - 288.68 - Minor porphyritic zone. Weak. 288.75 - 288.82 - Minor porphyritic zone. Weak.

SAMPLE

NO.

-

WIDTH

vut v si u

Daft Fin .h. d Sept. 26/82

ASSAY VALUES

Au.

Orl " Hole GG-

LoWude -Ljt

Departure

FROM l TO

•f 15E

Drilled bv Morrisette Logfled by Pon Esson175" Bearing i lj.-——-^—-

DESCRIPTION

288.2 - 288.90

291.39 307.3 Tuff,

- 291.39 - Dark, biotitic. Contorted. Chloritic. Garnetiferous. Minor pyrite. 1 *-——-s and Sereciti

. Core Axisto

- 296.39 - Less

300.39 - 39 . MoS to very heavy'

Surfacein

359.3 metres

ets

te.

d ry•y'air

entalental

mental

W

ive.

SAMPLEWIDTH

NO.

9768 9769

9770

9771

9772

9773 9774

0.7 1.56

0.93

1.0

Dot* Sforfed

Dot* Flnlihid

t y

Sept. 19/82

Sept. 26/82

ASSAY VALUESAu. Ag. MoS . ov . ,OZ/

Trac .036

.010

.0481.0 .159

1.0 1.0

9775 1.09776

9777 9778

9779

9780

9781

1.0

1.0 1.0

1.0

1.0

1.0

.516

.450

.275

.698

3.31 .740

.249

.344

.180

i y/ 1e

n/a

1.71

2.74 1.03

1.37

1.71

0.69 1.37

1.37

0.69

1.03

" T '

n/a

.295

.130

.135

.145

.087

.095

.080

.107

.140

.240

.064

5.179

Drill HoleGG-3

Lotltude. ION

DfilHd bv Morrisette Logged by 175 0

Don Esson Fog*

Bearing

Dfporturt 15E Dip-80 (

Elevation

Length

Surface

359.3 metresDote Storted

Dote Flnlthtd

Sept. 19/82

Sept. 26/82

FROM

307.3

309.8

0

TO

309.8

318.98

DESCRIPTION

302.39 - 303.39 - Pyrite 15Z. Heavy MoS 2 . Partlyfragmental .

303.39 - 304.39 - Pyrite 102. Heave MoS 2 . Partlyfragmental .

304.39 - 305.39 - Pyrite 52, very heavy in shortsections. Fair MoS 2 , Some quartz vein.

305.39 - 306.39 - Pyrite 5-102. Heavy MoSj.Core Axis 50 C .

306.39 - 307.30 - Pyrite 52. Very serecitic firstIV then very heavy molybdenite to end.

Mafic, Porphyritic Dike (Sill?)- Weakly porphyritic. Scattered pyrite. Sometimesquartz veined.307.3 - 308.46 - Two minor quartz veins with cubic

pyrite.308.46 - 308.72 - Quartz vein, vuggy contacts.

Sparse pyrite.308.72 - 309.8 - Two minor quartz veins.

Scattered pyrite.Tuff, Siliceous, Serecitic- As before except as noted. Scattered staurolite.1" vuggy quartz vein at contact. 309.8 - 310.8 - Pyrite 152. Heavy MoS 2 .310.8 - 311.8 - Pyric. 152. Heavy MoS,.311.8 - 312.8 - Pyrite 102. Lesser MoS 2 .312.8 - 313.8 - Pyrite 152. Increasing MoS 2 .313.8 - 314.8 - Pyrite 202. Very heavy MoS 2 .

Partly fragmental.314.8 - 315.8 - Pyrite 102. Heavy rfoS 2 .315.8 - 316.8 - Pyrite 102. Heavy MoS 2 . Mafic dike.

SAMPLE

NO.

9782

9783

9784

Q7Q Cy /o j

9786

9787

9788

9789

97909791979297939794

97959796

WIDTH

1.0

1.0

1.0

1.0

0.91

1.16

0.26

1.06

1.01.01.01.01.0

1.01.0

ASSAY VALUES

Au.oz/T.525

.453

.563

337* J^ *

.026

.008

.006

.012

.155

.075

.107

.151

.183

.380

.207

Ag.K/L1.71

1.37

1.03

1.71

n/a

n/a

n/a

1.371.370.691.031.37

2.401.03

MoS 2— z —.257

.195

.214

.142

.037

n/a

n/a

n/a

.071

.068

.048

.078

.090

.227

.138

CheckU6/ X

.035

.180

Drill HOllGG-3

Lotltude. IONDrilled by Mnrrisette

175 0Logged by Ppn Esson

Beorlng Elevation Surface

Departure O * 15E Dip-80'

Length 359.3 metresDate Started

Date Finished

Sept. 19/82

Sept. 26/82

FROM

3ia98

323.74

324.25

t)

TO

323.74

324.25

331.93

DESCRIPTION

316.05 - 316.35 - No mineralization, scatteredsillimonite.

316.8 - 317.82 - Pyrite 10Z. Lighter MoS 2 . Maficdike 317.6 - 317.82. No mineralization.

317.82 - 318.98 - Pyrite 5-10Z. Lesser MoS 2 .At 319. - 2" irregular quartz vein. Nomineralization.319. 48 - 319.62 - Sheared chloritic zone,may be remnant of dike.

Contact angle 45 C .Quartz Serecite Schist, Quartz Eyes-Core Axis 45 C .Siliceous, light - medium grey. Well sheared.Biotitic. Occasionally fragmental. 318.98 - 320.0 - Very sparse pyrite. 320.0 - 321.0 - Biotitic. Sparse pyrite. C. A. 45". 321.0 - 322.1 - Very siliceous. F

321,83 - 322.21 - Bleached. Quartz eyes.Porphyry Sill- Weakly porphyritic. Contains 1-2" bed of serecite shist. Contacts sharp, no alteration.Quartz Serecite Schist- As before.324.59 - 325.8 - Extremely siliceous. Massive.

Sparse serecite. Pyrite 22 as veinletsand crystal s. Some quartz eyes. GA 45 0 .

325. 8 - 329.38 - Increasing pyrite, as noted.325.8 - 326.8 - Pyrite beds. 2 1 pyrite. F

SAMPLE

NO.

9797

9798

9799 9800 48001

48002

WIDTH

1.02

1.16

ASSAY VALUES

Au.OZ/T

.336

.188

.036

.016 Trace

.012

Agg/ 1

2.05

0.69

n/a n/a n/a

MoS,l ?

.175

.162

n/a n/a n/a

Checkpz/T

.024

Drill HoleGG-3

i n.,...H, l -t- ION

O -t- 15E


Logged bv

Deporture

Storing

Dip ^

Elevation Surface-80'

Length359.3 metres

Sept. 19/82 Daft Storied ^---————-.,.^

Dot* Finithtd Sept. 26/82

FROM

J31.93

323.23

333.39

333.83

9

TO

332.23

333.39

333.83

357.15

DESCRIPTION

326.8 - 327.8 - Pyrite increasing to 52g 327.8.327.8 - 328.78 - Pyrite 5Z. Increasinglyserecitic.328.78 - 329.3 - Mafic schist. Chloritic.329.3 - 329.38 - Quartz vein. Large tour maline crystals. Some pyrite cubes.329.38 - Increasingly serecitic. Pyrite 21.

Porphyry Sill- Weak.Quartz Serecite Schist- As before. Quite serecitic.332.76 - 332.87 - Mafic Schist band.Porphyry Sill- Distinctly porphyritic.Quartz Serecite Schist- As before. Pyrite as veinlets and crystals. 2-32Quite serecitic. Very siliceous. Light grey. GA 45"34 A. 35 - 344.53 - Porphyritic. Weak. Chloritic.350.0 - 351.0 - Very siliceous. Minor pyrite 1-22.

Possible MoS 2 in some sections.351.0 - 351.35 - Serecitic. Biotitic. Some

tourmaline.351.35 - 352.4 - Very siliceous. Blue-grey, possibl

MoSj but not identified. Scattered pyrite.352.4 - 353.4 - Very siliceous but some biotite

and tourmaline. Minor chalcopyrite P 352.8. Scattered pyrite throughout.

SAMPLE

NO.

48003

48004

F48005

k

F48006F48007

WIDTH

1.0

1.0

1.0

1.051.0

ASSAY VALUES

AU.OZ/i.008

.014

.010

.006

.008

m

Drm Holt GG-3 Morrisette DonEsson poo* 10

Lotltu

Diport

FBOM

357.15

358.9

i. l * ION H. n ,, n? 175" ri . M(lflM Surface

u,. 0 * 15 E mo -80' ,.Mtt 359. 3 metres

TO

358.9

359.3

DESCRIPTION

354.3 - 355.11 - Massive hematite alteration. Scattered pyrite S stibnite?

Porphyry Sill, Quartz-Feldspar- Weakly porphyritic. Contact 45 0 , Sharp low indistinct.Quartz Serecite Schist- Very siliceous. Biotitic. No Serecite.

END OF HOLE f 3

Dip Tests: Azimuths Acid Tropari100' — -79.5 200 1 — -78,5 -78 e 300' — -79 400' 199 0 -76.5 -77* 500' — -77 600' —— -77 -76 e 700' — -71 800' 194 0 -71 -72 0 900' —— -71 1000' 195 0 -69 -69 0 1100' — -67 1177 204* -67.5 -67* 0

SAMPLE

NO.WIDTH

Dott Sfo

Doft Flnl

Sept. 19/82

Sept. 26/82

ASSAY VALUES

AU.

-

, ."". . ' .. -' -r.-;"'.-'--' ••••^;'^3f^PDrill Hole GG~^ Drilled by Morrisette LOOO. d bv Don Esson

Lotitu

Deport

FROM

0

3.65

8.21

9.59

23.15

25.6

*

,. 1 * 43N ,..,,., 180' r,...,,m Surface

... 1 + OOE B 1 . -85 ,...B 139. 29 metre.

TO

3.658.21

9.59

23.15

25.6

139.29

DESCRIPTION

Casing.Mafic (Biotitic) Sediments Core Axis 60 0- Dark-medium grey. Poorly bedded. Occasional narrow porphyritic beds.Amphibolite Core Axis 60 0- Massive. Dark green.Mafic Biotitic Sediments- As before. 9.59 - 10.33 - irregular quartz - tourmaline vein,

dirty, minor pyrite. 17.03 - 17.20 - porphyry, quartz-feldspar.

Coarse phenocryst. 20.71 - 22.0 - increasingly siliceous. Pyrite

scattered 22.Porphyry ^Quartz Feldsjjar- Moderately distinct.Mafic Biotitic Schist Core Axis 60 0- As before. Occasional garnets. 6" quartz vein at upper contact. Barren.37.4 - 38.6 - increasing amphibolite. 42.16 - 42.65 - amphiboJitic. 47.0 - Core Axis 50*. 50.0 - Core Axis 60 0 . 50.1 - 50.2 - amphibolitic. 55.0 - 63.7 - increasingly dark colored. Biotitic, chloritic. Well sheared. Core Axis 50 0 . Occasional very narrow porphvry beds.

SAMPLE

NO.WIDTH

Dote Sto

date Flnl

Page1 v - VC'

Sept. 24/82rim*

.H.,, Sept. 27/82

ASSAY VALUES

Au.

Drill HOU GG-4

43N


Bearing

Logged bv Dpn Esson

Surface

Page

Elevation

l "t- Dip -85 Length 139.29 metresDot* Started

Dote Finished

Sept. 24/62

Sept. 27/82

FROM

*

TO DESCRIPTION

63.7 - 70.14 - more siliceous with frequent amphibolite narrow beds.

70. 14 - 78.7 - more mafic, with quartz eyes throughout. 74.53 - 75.3 - weakly porphyritic.

78.7 - 88.0 - garnetiferous. Mafic. 88.0 - 95.0 - garnetiferous. Mafic, and staurolitic

89.05 - 90.65 - bleached. Brecciated. Sericitic.

95.0 - 97.2 - garnetiferous. Mafic. No staurolite. 97.2 - 101.85 - mafic. No garnets. Somewhat more

siliceous. Occasional amphibolitic beds. 101.85 - 122.54 - mafic. Garnetiferous. Staurolitic

Very chloritic, many chlorite crystals up to 5 mm. and staurolite to 10 mm.

122.54 - 128.85 - more siliceous. Garnetiferous. 128.85 - 130.42 - mafic. Garnets. Staurolite -

coarse. 130.42 - 139,29 - more siliceous. Occasional

staurolite and sillimonite. Core Axis 45". Chloritic.

END OF HOLE M

Dip Tests: Acid Tropari Azimuths100' -82 —— —— 200' -74 -76* 196' 300' -70 —— 400' -63 —— ——

SAMPLE

NO.WIDTH

ASSAY VALUES

Au.

DHii HOI* GG-5

. , t ...... l -H SON M

D.parm.l * 5 0W M

Oriiitd by Morrisette

Storing 1 8QO————1

Logged b y Dpn Esson

Surface

Pogt

-75 331.3 metresDot* Sfortid Sept. 27/82

Oct. 2/82

FROM

0

3.66

16.7

17.37

*

TO

3.66 16.7

17.37

131.40

Metric Measurements

Casing. Diabase- Dark black, fairly fine-grained. Lower contact @ 45" Core Axis.Contact Zone- Bleached, quartz veined. Chloritic. Mafic (Biotitic) Sediments Core Axis 50 0- Dark to medium grey. Fairly well sheared. Garnetiferous and staurolitic. Many thin chloritic beds . 17.36 - 17.64 - Brecciated. 20.5 - 21.6 - Contorted. Fragmental? 23.47 - 23.67 - Contorted. Chloritic. Quartz veined32.35 - 33.8 - Amphibolitic.

Very dark green. Massive. Coarse grained. 33.8 - 44.38 - No staurolite. Frequent narrow

bleached zones. 44.38 - 62.0 - Staurolitic. Garnetiferous..

46.82 - 47.4 - Brecciated. Quartz veined. Chloritic.

52.2 - Silicified. Epidote. 53.1 - Silicified. Epidote. (Quartz veined) 54.21 - 54.3 - Quartz vein. Minor epidote. 55.0 - Core Axis 50 0 . 60.5 - 61.23 - Bleached. Silicified.

61.0 - 76.8 - Much more siliceous. Core Axis 50 0. Light to medium grey. Weakly bedded. Scattered garnets and staurolite. Frequent bleached, serecitic beds, often

SAMPLE

NO.W.OTH

ASSAY VALUES

Au.

D'HI HOlC

Lotlfudt

Deportur*

GG-5Drilled by Mor r i se t Ce

1 -1- SON

. 0 * SOWBearing .

Dip

180 0

-75

Poge

SurfaceFlcuatlon

331.3 metresLength

Sept. 27/82rtflfa Sfort.d IMI r .

Oct. ^/82Dot* Flnlih*d ,. . ,.

FROM

17.37

9

TO

131.40

DESCRIPTION

Continuedwith epidote. Occasional 6"-12" mafic toamphibolitic beds.

76.8 - 100.23 - As above but no garnets or stauro lite.91.0 - 100.23 - More mafic, still massive.

Dark to medium grey.98.8 - 99.7 - Brecciated. Amphibolitic.

Quartz veined.99.8 - 99.0 - W fault gouge. GA 80 0 .99.1 - V 1 fault gouge.

100.23 - 117.39 - More mafic, somewhat chloritic.Core Axis 45 8 .110.7 - 111.84 - Quartz vein. Muscovite.

Barren.116.46 - 116.72 - Faintly porphyritic.

117.39 - 131. A - More siliceous. Massive. Poorlybedded. Black to medium grey.117.39 - 117.85 - Faintly porphyritic.

Epidote veined.117.85 - 120.77 - Frequent breccia zones.

Recemented by epidote and quartz.Epidote veined at random angles.Occasional hematite stained.

120.77 - 131.4 - Frequent epidote veinlets.Garnetiferous. Occasional elongatedfragments. Occasional hematite stain.Occasional tourmaline.

SAMPLE

NO.WIDTH

ASSAY VALUES

Au.

Drill Hole GG-5 Drilled by

Lotltudt. SON Bearing

Morrisette ISO 0

Logged by Don Esson Pag*

ElevationSurface

Departure 50W Dip-75 Length 331.3 metres

Dote Storied Sept. 27/82

Oct. 2/82Dott Finished

FROM

131.4

140.93

238.7

f

TO

140.93

238.7

240.56

DESCRIPTION

Greywacke- Faintly sheared @ Core Axis 45 0 . Massive, black, fine-grained. Biotitic. Frequent epidote veinletf . Frequent weakly porphyritic and occasional fragmental beds. Scattered quartz veins.Mafic (Biotitic) Sediments-Massive, dark-medium grey. Slightly sheared. Weakly bedded at Core Axis 45 0 . Frequent 2-4" chloritic beds. 150.71 - 151.07 - Bleached. Chloritic. 151.07 - 168.86 - More chloritic and epidote rich.

Occasional fragments or elongated porphyroblasts. Occasional sill tantite. 163.67 - Irregular quartz veins. Chloritic,

biotitic, tourmaline. 164.42 - 164.86 - Bleached with irregular

quartz veins. Vuggy in part. 164.86 - 167.1 - Increased epidote S chlori 167.5 - 168.86 - Increased epidote S chlori

Sparse garnets S sillimanite. 168.86 - 238.7 - More siliceous. Well-bedded @

Core Axis 45 0 . Light to dark grey to green. Cherty beds, frequent chloritic beds. Considerable epidote. Occasional narrow, barren quartz veins.

Quartz Feldspar Porphyry- Distinctly porphyritic. Phenocrysts to 3 mm. Dark grey. Barren.

SAMPLE

NO.

;ee :

WIDTHASSAY VALUES

Au.

-wÛffiDrill Hole GG-5


Logged by Don Esson Page

SON Bearing 180

SOW Dip-75

Elevation

Length

Surface

331.3 metresDate Started Sept. 27/82

Oct. 2/82Dot* Finished

FROM

240.56

292.4

C

TO

292.4

300.0

DESCRIPTION

Mafic (Biotitic) Sediments- Core Axis 45 0 poorly bedded. Intermediate to mafic. Medium to dark grey. Cherty beds, occasional garnet and amphibole beds.249.5 - 250.7 - Amphibolitic. Dark green.

Occasional staurolite and garnets. 252.08 - 252.33 - Quartz vein @ 30' Core Axis. 253.57 - 266.45 - Increasing chlorite beds.

Occasional staurolite. 261.16 - 261. A - Porphyritic. 265.07 - 266.45 - Bleached. Fractured.

Heavy epidote. 266.45 - 279.35 - Much reduced chloritic beds. 279.35 - 289.5 - Minor garnets and staurolite.

Occasional sillimanite. 289.5 - 292.4 - More siliceous. Minor pyrite.

Sericite increasing towards contact. 289.5 - 290.1 - Bleached. Serecitic. 291.1 - 292.1 - Siliceous. Minor pyrite. F 292.1 - 292.4 - Siliceous, serecitic,

slightly vuggy. 2Z pyrite.Tuff, Siliceous, Serecitic- Sheared at Core Axis 40 0 . Light grey to blue-grey. Slightly vuggy except as noted below. Well mineralized with pyrite and MoS, as noted. 292.4 - 293.4 - Siliceous. Serecitic. Pyrite 2 1.

Very little MoS 2 . 293.4 - 294.4 - Little serecite. Massive. PyritelOZ

Increasing MoS : .

SAMPLE

NO.

48009 48010

48011

48012

WIDTH

1.0 0.3

1.0

1.0

ASSAY VALUES

Au.

OZ/T

.012

.002

.042

.101

Phoolf

.092

OHII Holt Drilled by MorriseteLogged by Don Esson Poge

. ..it..*., l * SON 180 Surface

Deporture SOW m. -75 ,..., fc 331. 3 metresDot* Started

Dot* Plnl.h.d

Sept. 27/82

Oct. 2/82

FROM

300.0

301.2

303.7

*

TO

301.2

303.7

307.0

DESCRIPTION

294.4 - 295. A - No serecite, Pyrite 52, increasedMoS 2

295.4 - 296.4 - Vuggy, reduced MoS 2 , increasingserecite and pyrite.

296.4 - 297.4 - Serecitic, much reduced MoS 2 . FVuggy. Staurolitic. Pyrite 5-7Z.

297.4 - 298.4 - Ditto. MoS 2 increasing throughout. 298.4 - 299.4 - Massive, siliceous. Pyrite 10Z+.

Much increased MoS 2 .299.4 - 300.0 - Pyrite and MoS 2 reducing throughoutMafic Sediment?- Minor MoS 2 . Sparse pyrite. 6" epidote veiningat 300.9.Porphyry SilK?)- Weakly porphyritic. Massive, No mineralization.V quartz vein at upper contact. Lower contactindistinct @ Core Axis 50 0 .301.2 - 302.5302.5 - 303.7Tuff, Siliceous- Moderately sheared @ Core Axis 40 0 .Light grey, occasionally vuggy. Mineralization asnoted.303.7 - 304.4 - Mafic sediment composition. Dark F

grey to black. 3Z pyrite. Little MoS 2 .303.9 - 2" epidote staining.

SAMPLE

NO.

48013

48014

48015

48016 48017

48018

48019

4802048021

^8022

WIDTH

1.0

1.0

1.0

1.0 1.0

0.6

1.2

1.31.3

0.7

ASSAY VALUES

Au.OZ/T.137

.036

.042

.122

.024

.048

.018

.002

.002

.008

Check

.024

SOWoecortur* - - --" rii n '- JJ.L.J UICUJ.UO n O/RODlp ————— - —————————— Lenoth , ,. ,...., ,..,. ,. Dot. Flnlih.d Oct. 2/82

FROM••^••••MMM^M

303.7

307.0

9

TO

307.0

331.3

DESCRIPTION

Continued

304. A - 305.4 - Highly siliceous. Pyrite 102.Moderate MoS a .

305.4 - 306.4 - Reduced pyrite, increased MoS 2 .306.4 - 307.0 - MoSj and pyrite reducing, serecite

increasing to contact.Quartz - Serecite Schist- Typical, quartz eyed. Siliceous. Serecitic.(part) Scattered minor pyrite. Core Axis 55*.307.0 - 308.0 - Quartz eyes. Sparse tourmaline.

Little pyrite. Core Axis 45 0 .308.0 - 309.0 - Very siliceous. Quartz eyes.

308.6 - 308.9 - Mafic with garnets.310.2 - 310.6 - Amphibolitic bed.317.3 - 318.5 - Narrow, interbedded porphyritic

sills.321.5 -322.3 - More siliceous. Pyrite 2 1,

END OF HOLE J 5

SAMPLE

NO.

48023

4802448025

48026

48027

48028

WIDTHv* i w 1*1

1.0

1.00.6

1.0

1.0

0.8

ASSAY VALUES

Au.OZ/T

.022

.245

.265

.016

.008

.008

fhAolcoz/T

.045

.250

.017

100200300400500600700800900

1000

Dfin HOU GG-6 n,jiiid bv Morrisette i 0fl0 *d bv Don Esson

1 atltud. * * 4 3N B. a ,| nn 0* Fl.uaflflft 1015.0 Est.

Dtport

FROM

0 2.44

9.42

11.46

4

ur. * * O OE DIB " 9QO L.nîh 421.84 metres

TO

2.44 9.42

11.46

78.49

*

DESCRIPTION

Casing. Mafic (Biotitic) Sediments- moderately well-bedded. Core Axis 65*. Dark to medium grey. Siliceous. Occasional bleached zones. 5.61 - 6.13 - Siliceous. Fine disseminated pyrite

Amphibolite- dark green. Meissive. Mafic {Biotitic) Sediments-as before but more serecitic.11.58 - 19.81 - well sheared 9 Core Axis 75-90 0 .

14.42 - 14.97 - amphibolitic with 2" quartz vein.

19.81 - 24.38 - well sheared 9 Core Axis 75 C . Serecitic. 20.42 - 6" coarse quartz-porphyry. 24.23 - 24.38 - bleached.

24.38 - 27.13 - siliceous. Sheared. No bedding. Fine disseminated pyrite 1-21.

34.81 - 35.39 - quartz-feldspar porphyry. Well crystallized.

35.39 - 35.69 ^ quartz vein. Barren. 53.34 - Core Axis 65 e . 59.59 - 59.74 - amphibolitic. 64.62 - 65.87 - interbedded, weakly porphyritic sill; 73.76 - 76.05 - irregular quartz veins. Chloritic.

Minor pyrite. 77.57 - 77.94 - fragmental.

SAMPLE

NO.WIDTH

Daft '•ra

Dart Fin

Pag* 1

rtmA Sept. 27/82

.h.n Oct. 6/82

AiSAY VALUESAv.

^ "- - . ,.. JDrill Holt GG-6 Drilled by Morrisette Locoed by Don Esson Pog* 2

l * 43N O 0 1015.0 Est. Sept. 27/82Lotltud. A T n j " Bearing Fl.vaMnn not* Started

l H. OOE -90" 421.84 metres Oct. 6/82Dtoorturt * v D in L*n v th Oat* ttnlihAd

FROM

78.49

82.90

102.3

107.9

TO

82.90

102.3

107.9

154.4

4

ftCO^DlDTlrtlJU C d Unlf l lUn

More Felsic Sediment, Siliceous- indistinct bedding. Light to medium grey.Scattered, fine pyrite. Occasional weakly porphyritisills.81.44 - 82.91 - Quartz eyes.Mafic (Biotitic) Sediments- weakly bedded, sheared, Core Axis 40".86.72 - 87.17 - weakly porphyritic88.70 - 93.18 - interbedded with weakly porphyritic

sills.93.18 - 102.26 - more chloritic. Garnets, minor

staurolite.Felsic Sedments- siliceous, slightly serecitic.104.85 - 107.90 - staurolitic. Large chlorite crysta

towards end of section.Mafic Sedimoncs- black, almost graphitic. Very fractured at lowCore Axis 's. Very garnetiferous S, s taurolitic.Scattered tourmaline. Infrequent chloritic zones.117.96 - 118.26 - quartz-chlorite- tourmaline.

Contorted. Garnetiferous.118.32 - 118.69 - Ditto.122.53 -123.14 - fractured sub-parallel to core

axis.124.05 - 140.82 - very fractured at Core Axis O 0 to

30 0 . Mylonitic to talcose on slip planes. Heavily garnetiferous t staurolitic. Many large (to 10mm)

SAMPLE

NO.

t

.3

u/inTuwi u i nASSAY VALUES

Au.

Drill Holt GG-6 Drilled by Morisetteo*

Loggtd by Don Esson Pofl*

OOE Dip Length

1015.0 Est.

421.84 metresDot* Started Sept. 27/62

Oct. 6/82Date Plnl.h.d

FROM

154.4

4

TO

200.7

*

DESCRIPTION

chlorite crystals. Occasional narrow bleached zones. 140.82 - 154.38 - more competent. Few fractures.

Occasional narrow , sheared, serecitic zone?. Contacts heavily garnetiferous 6 staurolitic. 147.89 - 148.38 - porphyritic with 3" quartz vein at 30*. Barren.

Felsic Sediments- siliceous, massive, weakly bedded. Core Axis 45 0 . Occasional tourmaline and sillimanite, no garnets or staurolite. Epidote l chlorite common, occasional cherty beds. Occasional bleached zones. 158.71 - 160.29 - staurolite fi sillimanite. 161.09 - 161.36 - chloritic. Altered porphyry? 163.43 - 164.29 - scattered staurolite. 171.60 - 171.91 - bleached. Chloritic. 173.43 - 174.04 - weakly porphyritic. Brecciated,

recemented. 175.26 - 3" zeolite zone in vugs. Pyritic. 179.44 - 183.18 - more basic, darker black.

Scattered garnets, staurolite, epidote. 183.18 - 200.71 - dark to medium grey. Siliceous.

Occasional sillimanite i tourmaline. V.'ore Axis 4 S 0 . 190.04 - 190.50 - brecciated, recemente 192.15 - 192.33 - brecciated, recemente

Epidote. 196.29 - 196.60 - brecciated, recemente

Epidote.

SAMPLE

NO.

1. i.

k t

WIDTHASSAY VALUES

Au.

Drill HoltGG-6


Lotltudt

Otpor turt

Storing

Dip

Loggtd bv P"" Esson

1015.0 Est.

Pag*

-90'EItvo'lon

Length421.84 metres

Dart Sforttd Sept. 27/82 Oct. 6/82

Dot* FlnUhttf

FROM

200.7

TO

264.4

.

f

DESCRIPTION

Mafic Sediments- dark black to greenish. Same as above mafics plusfrequent epidote veinlets i crystals.Infrequent vuggy veins and hematitic stain.209.09 - 210.13 - marked increase in hematite

and quartz veining plus epidote.Suggestive of granitization.

210.46 - 212.75 - ditto plus calcitic.216.10 - 216.41 - brecciated. Recemented.218.85 - 224.33 - Ditto 209.9 - 210.01. Minor pyrite

in veinlets.223.57-224.33 - quartz veined. Redalteration.

226.22 - 229.06 - Ditto above.234.24 - 235.0 - Ditto plus brecciated, recemented.238.05 - 238.96 - brecciated. Heavy epidote and red

alteration.239.33 - 242.16 - numerous epidote veinlets and

blebs. Green stained quartz eyes and/orgarnets.

244.54 - 246.28 - heavily quartz veined. Brown/redalteration. Calcitic, pyrite 21.244.54 - 245.61 - slight magnetite.Pyrite Si.

246.28 - 249.20 - same as 209.9 - 210.01. Alterationmuch reduced from proceeding section.

249.2 - 264.41 - typical massive mafic sediments.254.51 - 254.72 - quartz-feldspar.Barren.261.46 - 263.44 - recemented by quartzand calcite.

SAMPLE

NO.

18029

18030

WIDTH

OZ/T

0.76

1.07

ASSAY VALUES

Au.

Tr.

.006

Drill HoleGG-6 Drilled by Morrisette

O 0Logged by Don Esson Page

Scoring Elevation1015.0 Est.

Departure OOE Dip-90' 421.84 metres

Doit

Daft Flnlihed

Sept. 27/82

Oct. 6/82

FROM

264.4

315.2

316.1

(

TO

315.2

316.1

367.7

.

DESCRIPTION

Felsic Sediments, Siliceous- dark to medium grey. Greenish beds. Bedding defined Core Axis 40 0 . Well sheared. Occasional amphibolitic beds. Occasional fragmental beds. 298.09 - 301.45 - increased epidote alteration,

brecciated in part. 304.62 - 315.16 - increasingly well-bedded with

alterating light to dark beds. Frequent green beds. General bedding k - i ". Core Axis 45 0 .

Porphyritic (Sill) Quartz-Feldspar- contacts clear. Core Axis 45*. Well crystallized Occasional sillimanite (?) crystals.Mafic (Biotitic) Sediments- light to dark grey, frequent greenish beds. CA 45 0 generally well-bedded. Occasionally fragmental. 325.37 - 325.98 - more siliceous. Light green.

Bleached? 326.75 - 327.29 - more siliceous. Light green.

Bleached? 333.97 - 334.98 - 2-10" porphyritic sills with

bleached contacts and epidote rich between sills.

334.98 - 344.27 - more mafic. Dark black. 334.27 - 344.42 - bleached. Serecitic. 344.42 - 348.69 - staurolitic. Sparse garnets. 354.48 - 359.51 - occasional 2-3" chloritic beds.

Occasional epidote. 359.51 - 361.10 - staurolitic. Sillimanitic.

SAMPLE

NO.WIDTH METRES

ASSAY VALUES

Au.

t

i

Drill Hole GG-6 Orilltd by Morrisette

Lotltud*. 43NScoring

Diporfurt l * OOE Dip-90'

Loggtd by

Eitvoflon

Length

Don Esson Pogt

1015.0 Eat.

421.84 metresOoft started .

Dot* Finished .

Sept. 27/82

Oct. 6/82

FROM

i

367.7

369.4

TO

369.4

378.3

*

DESCRIPTION

359.51 - 361.10 - occasional garnets fi epidote.361.10 - 363.17 - amphibolitic. Dark black-green.

Sillimanitic.363.17 - 367.71 - siliceous. Medium dark grey. Well

bedded. Core Axis 45 e . Scatteredgarnets d sillimanite. Occasionalchloritic beds. Recovery 1001.Mineralization as below.

363.17 - 364.97 - no significant mineralization364.97 - 365.88 - no significant mineralization365.88 - 366.8 - 31 pyrite. Veinlets, blebs,

crystals.366.8 - 367.71 - l-2% fine pyrite.

Felsic {Biotitic) Sediments- siliceous, chloritic, serecitic. Occasional maficbeds. 5% coarse pyrite crystals. Recovery 1001.367.71 - 368.50368.5 - 369.42Tuff - Siliceous, Serecitic- sometimes fragmental, sometimes bedded. Well sheared. Recovery 951. Occasional mafic beds withsillimanite. Grades to more chloritic with reducingserecite. Mineralization as noted. Virtually no MoS, 369.42 - 370.33 - siliceous. Occasional epidote.

Pyrite 21. Serecitic.370.33 - 371.25 - siliceous. Serecitic. Occasional

epidote. Pyrite 2%. 371.25 - 372.16 - becoming more mafic-chloritic s

biotitic. Reduced serecite. Pyrite 2%fine.

SAMPLE

NO.

'

4803148032

48033

4803448035

48036

48037

48038

WIDTH METRES

.91

.91

.91

.79

.92

.91

.92

.91

ASSAY VALUES

Au.OZ/T

.004

.012

.002

.002

.010

.002

.004

.056

CheqkOZ/T

.058

Drill HOU GG-6 Drilled by Morrisette Logged byDon Esson Pog*

Latitude, l -t- 4 3N Storing

D.nartur. Dip-90'

El.votlon 1015.0 Est.

421.84 metresOaf* Starttd Sept. 27/82

Length Dot* Flnlihtd Oct. 6/82

FROM

378.3

TO

385.7

f

DESCRIPTION

372.16 - 373.08 - becoming more mafic-chloritic 4biotitic. Reduced serecite. Pyrite 21fine.

373.38 - 373,56 - coarse muscovite, biotite,quartz. Minor grey sub-metallic mineralprobably sulphosalt (might be arsenopyrite) .

373.08 - 373.99 - Ditto, but more sheared g CoreAxis 40 0 . Pyrite 1-21.

373.99 - 374.90 - highly sheared. Chloritic. Lessthan H pyrite.

374.9 - 375.82 - more siliceous. Less sheared andchloritic. Minor pyrite. Possibly minor MoSj .

375.82 - 376.73 - More serecitic, still chloritic.Quartz eyes. Pyrite 51, minor MoS, .

376.73 - 377.65 - Chloritic, no serecite. Frequentfuchsite. Pyrite 2-4*. No MoS, evident.

377.65 - 378.32 - Reduced chlorite. Somewhat serec itic. Scattered fuchsite. Pyrite 3*. No MoS,.

Mafic (Biotitic) Sediments- medium to dark grey. Moderately well-bedded. Wellsheared. Core Axis 45*. Recovery 95%. Minor pyrite,no MoSj .378.32 - 379.17 - mafic, 1* pyrite.379.17 - 380.09 - mafic, H pyrite.380.09 - 381.0 - mafic, 3% pyrite.381.10 - 381.91 - mafic, 2 1 pyrite. Slight fuchsite

9 381.91.381.91 - 382.83 - less chlorite. Slight serecite.

Less than 11 pyrite.382.83 - 383.74 - more biotitic. Slight serecite.

11 pyrite.

SAMPLE

NO.

48039

48040

48041

48042

48043

48044

48045

48046480474804848049

48050

4^0503

WIDTH MBTPP*

.92

.91

.91

.92

.91

.92

.67

.85

.92

.91

.91

.92

.91

ASSAY VALUES

Au.OZ/T

.057

.024

.038

.124

. 298

.1-09

.091

.063

.088

.097

.069

.049

.089

Ag.g/ 1

0.69

MoS,t

Check3Z/T

.094

Drill Hole GG-6

43N


O 0Beoring

Logged b v

Elevotlon

Pogt 8

1015.0 Est. Doft Sforfed Sept. 27/82

Oiportuft GOE Dip-90'

Length 421.84 metres Oafl Fi n i,h t d Oct. 6/82

FROM

385.7

388.9

394.6

TO

388.9

394.6

399.98

f

DESCRIPTION

383.74 - 384.66 - fuchsite to 5%. Pyrit- l-2t.Talcose and bleached 9 383.74 and 384.34-384.66

384.66 - 385.42 - talcose 9 384.66 grading toargillaceous @ 385.42. Pyrite 2%.

385.42 - 385.72 - black. Quartz veined. Pyrite 101.Quartz-Feldspar PorphyryContact clean @ Core Axis 40 0 .- Fairly well crystallized. Hematite stained,particularly feldspar crystals for first 2} feet.No mineralization.385.72 - 386.79386.79 - 387.86387.86 - 388.92Lower contact clean 9 Core Axis 45 e .Tuff, Siliceous- occasionally fragmental. Weak to poorly bedded.Grey to blue-grey. Frequent fuchsite. Well mineral ized as not-ed.388.92 - 389.84 - pyrite 10*, slight MoS,.389.84 - 390.75 - ID-15% pyrite, increasing MoS,.

i" realgar (?) rich 9 3 90.60390.75 - 391.67 - ditto above, but more chloritic.391.67 - 392.58 - pyrite lS-20%, heavy MoS,.392.58 - 393.5 - ditto, except for weak porphyritic

sill 392.95 - 393.16 with no mineralization.393.5 - 394.56 - pyrite S-10%, relatively heavy MoS,Mafic Tuff (Sediment?)- black to dark grey. Very fragmental. Highlysheared 9 Core Axis 45 0 . Very biotitic.No appreciablcarbonate. Frequent minor fuchsite. Well mineralized

SAMPLE

NO.

49052

49053

49054

490554905649057

4905849059

490604906149062

49063

i

WIDTH METRF5.92

.76

.30

1.071.071.06

.92

.91

.92

.91

.92

1.06

ASSAY VALUESStu.'T

.139

.069

.248

.016

.020

.054

. 5041057

.5971.053.668

0.988

Dheckoz/T.180

.987

1.043

Drill HOU GG-6 Orilltd by Morrisette Logged byDon Esson Pagt

Latitude.43N

Bearing

l * Dip-90'

Elevation 1015.0 Est.

421.84 metres Length _____________.

Oat. tiarttd 522*1-12^21

Ooti Flnlshtd Oct. 6/82

FROM

399.98

400.96

401.4

408.4

TO

400.96

40L.4

408.4

409.4

^L™

DESCRIPTION

as noted.394.56 - 395.48 - pyrite 3 1, fine. No MoS,.395.48 - 396.24 - black. Fragmental. Pyrite 31.396.24 - 397.15 - more siliceous. Minor fuchsite

bands. Pyrite 2 \.397.15 - 398.07 - Ditto398.07 - 399.29 - more biotitic. No fuchsite.

Pyrite 2 1.399.29 - 399.71 - tuff. Siliceous. Pyrite 10t.

MoS, evident.399.71 - 399.99 - amphibolitic. No mineralization.

Tuff, Siliceous- same as 388.92 - 394.56Trace pyrite 15-201. Heavy MoS,.Contact Zone, Vuggy- minor fuchsite @ contact. Pyrite 10*. Minor MoS,.

Quartz Serecite Schist- massive, very siliceous, quartz eyes. Relativelylittle serecite except as noted. Light to mediumgrey. 401.42 - 402.34 - very fractured 9 low C. A. 's.

Very serecitic. Pyrite less than 1*.402.34 - 403.25 - light serecite. Somewhat fractured

and chloritic.403.25 - 408.43 - massive. Very little mineralizatio

Amphibolitic- black to dark green. Fragmental. Tourmalinecrystals. Very sheared. Chloritic. Slight carbonate.Pyrite 3*. 409.13 - 409.35 - semi-porphyritic.

SAHw,OTH

490644906549066

4906749068

49069

49070

49071

49072

49073

49074

M9397 49403

49075

.92

.76

.91

.921.22

.42

.28

.98

.44

.92

.91

5.18

1.0,0

ASSAY VALUES

Au.

.234

.042

.134

.164

.100

.335

.093

.126

.080

.049

.058

.006

0.64

MoS,

.002

ChecJ?oz/T

.105

i

D'llf Hole

i Le'lfJif ...,,/

Deporture 1 — i

GG-6

L * 43N

H OOE


O 0Rearing — , ,,

m, -90"

Logged by Don Esson Poge 10

Elevoflon 1015.0 Est.


Date star*.d Sept. 27/82

Oct. 6/82Dole Finished

FROM

409.4"

409.95

410.1

410.35

410.53

411.05

411.6

411.9

412.3

TO

409.95

410.1

410.35

410.53

411.05

411.6

411.9

412.3

416.05

t

DESCRIPTION

Quartz Serecite Schist- light grey. Massive, siliceous, no serecite. Nomineralization.Quartz Feldspar Porphyry- massive, distinctly porphyritic, no sulphides.Amphibolite

- as 408.43 - 409.44, pyrite 5-71.Quartz Serecite Schist

- As before.Quartz Feldspar Porphyry

- As before.Quartz Serecite Schist- dark grey, very siliceous. Scattered pyrite-fine.Quartz-Feldspar Porphyry- As above.Quartz Serecite Schist- As before. No sulphides.Amphibolite- as before. Sheared @ Core Axis 30*.412.33 - 413.0 - pyrite 5% 413.0 - 413.61 - pyrite 3-4t413.61 - 416.05 - no sulphides 413.61 - 414.92 414.9? - 416.05

SAMPLE

NO. ,

49030

49076

/49031\

49077 49078

49032 49033

WIDTHIRTRPR

1.65

.55

.73

.67

.61

1:311.13

ASSAY VALUES

Au.OZ/T

^303

.08

.0.19

.90 1.33

..113 •VO'08

MC-S*

.002

.002

.002

CheckOZ/T

.293

1.139

Drill Holt GG-6

43N

Q.nnrtu,. l *

Drilled by

Bearing .—

Dip .

Morrisette Loggtd by Don Esson Pogt

-90 (EUvotlon 1015.0 Est.

"21-84 metres

Dot* storttd Sept. 27/82

Oct - 6/82Dot. FlnUh.d

FROM

416.05

416.6

417.08

418.8

419.6

421.5

TO

416.6

417.08

418.8

419.6

421.5

121.84

•21.84

DESCRIPTION

Quartz Serecite Schist-medium grey. Massive, siliceous, quartz eyes,chloritic. Pyrite 3t.Amphibolite- as before. No sulphides.Quartz Serecite Schist- light to medium grey. Massive, siliceous, quartzeyes.417.09 - 417.94 - pyrite 201. Minor arsenopyrite.417.94 - 418.80 -'pyrite 31 fine.Amphibolite- as before. Pyrite heavy at contacts. Overallaverage 5%.Quartz Serecite Schist- medium to light grey. Massive, siliceous, quartzeyes. Serecite increasing with depth.419.59 - 420.62 - dark grey, possible MoS, .

pyrite in bands averaging 31.420.62 - 421.54 - DittoQuartz-Feldspar Porphyry- massive, distinctly porphyritic. No sulphides.421.54 - 421.84

END OF HOLE 16

SAMPLE

NO.

49079

49034

4908049081

49082

49083

49084

49035

WIDTH METRES

.58

.46

.55

.85

.79

1.04

.91

•;30

ASSAY VALUES

AU.

OZ/T

.06

.030

.001

.001

.02

.006

.004

Tr.

-

Drill Holt GG-6

Latitude.

Departure

Drilled by ^

Beorlng .^^

Dip .

Logged by

Elevation ^.

Length ——.

Pagt

Doft Starred

Date

FROM

1

J

TO

f

DESCRIPTION

TropariCollar Azimuths Dips Acid

0 —— -90100 —— —— -88200 1750 -830 -84.5300 —— —— -80400 343 0 -82 e -79*500 —— —— -80*600 212 0 -74%0 -75700 —— — - -73*800 060e -71*e -73900 —— —— -671000 363" -680 -691100 - —— —— -671200 008 0 -66 -671300 240 C ? -64 -62

SAMPLE

NO.WIDTH

ASSAY VALUES

Au.

Drill Holt GG-7

SON

p. Ba ,,u,. SOW

Drilltd by

Beorlng .—.

Dip -—---

Morrisette

-90 0

Logged bv B. Durham Pogt

Elevotlor. .


Dote Sforfed Oct. 2/82

Don Flnlthtd Oct. 10/82

FROM

0

4.27

23.47

9

TO

4.27 23.47

80.26

DESCRIPTION

Casing. Massive .Diabase Dyke-massive uniform coarse grained poikiloblastic grey-green diabase. Only rare magnetic patches. PoikilobL*: cics appear to be epidote. Broken core: 4.27 - 4.57

4.88 - 5.49 6.40 - 7.01

23.01 - 23.47 - fine grained chill margin.Mafic Sediments (Al Rich)- dark grey pelitic sediments altered to biotite, garnet, actinolite, staurolite -t- chloritoid. Somewhat heterogeneous i.e. some sections stauro lite or garnet rich while others contain very little, schistosity30* to Core Axis. 23.77 - 24.08 - late breccia white non-calcitic

matrix very angular fragments. 28.04 - 29.87 - broken core, some breccia,

scattered graphite and pyrite, schistosity 15* - 20 " to Core Axis.

29.87 - 32.31 - slightly more siliceous, no aluminum rich metamorphic minerals.

34.44 - 40.84 - lQ-15% garnets, schistosity 10 0 to Core Axis.

40.84 - 47.85 - scattered amphibole rich sections 45.42 - 3 inch quartz vein plus pyrite on walls

47.85 - 51.05 - amphibolite dike? 53.34 - quite sharp change in schistosity from 20 0

to 45 0 . 58.37 - 62.03 - 2% chloritoid. Schistosity 30 0 to C

IV

SAMPLE

NO.WIDTH

ASSAY VALUES

Au.

Drill HoleGG-7


Lotltude, SON

Deporture SOW

Bearing

Dip ——.

Loooed by

SurfaceElevation

419.71 metresLength

Page *-

Oct. 2/82flat* Start f il ,. , ,, . ,

n.t. P,,,.... Oct. 10/82

FROM

86.26

4

TO

184.56

DESCRIPTION

62.03 - 77.63 - 51 fine to medium grained garnet porphyroblasts plus some staurolite in narrow bands . Coarse staurolite @ 69.49 - 69.80. Heavy staurolite @ 71.93 - 72,09. Heavy staurolite 8 73.55 - 73.76.

Schistosity 35" to Core Axis. 77.63 - 78.24 - more siliceous greyish, epidote

altered. 78.24 - 81.69 - S-5% coarse garnet porphyroblasts. 81.69 - 86.26 - more bleached, grey much less

garnet, staurolite.

Wacke Sediments- grey to brown-grey, fine grained, bleached, weakly sericitic. These sediments appear to have been fine grained and quite brownish (biotite) but subsequent bleaching has left only scattered brown sections. 98.15 - 100.89 - light grey scattered quartz blebs

and veins. 51 pyrite and pyrrhotite minor sericite. Some brecciated sections. Schistosity 40 C @ 95.71.

100.89 - 122.22 - less altered but still frequent hairline bleached fractures, becoming pervas ive in places. 105.64 - 105.89 - weak in situ breccia.

122.22 - 131.98 - weakly fractured, grey, minor in situ breccia throughout, minor calcite (filling some fractures) .

131.98 - 150.27 - brown to grey-green, weak bleaching along micro-fractures, occasional

SAMPLE

NO.WIDTH

ASSAY VALUES

AU.

Drill Hole GG-1

. ntltnd. SON

Deporture O + S OW

Drilled bvMorrisette

Bearing ——-—-^.——.-.—.

Dip ^^--,.—-.-——.-

Logged by

Elevation —

Length -——.

Poge

Surface


Dore Finished

Oct. 2/82

Oct. 10/82

FROM

184.56

*

TO

239.88

DESCRIPTION

amphibole rich bands .5 to 2 inches. 141.12 - 147.83 - very minor hematite staining along some micro-fractures. 141.49 - 1" diabase e 15 0 to Core Axis (appears near vertical and striking O 0 ?) - strongly magnetic. 147.98 -2" diabase as above.

150.27 - 167.49 - brownish grey-green, moderately to well micro- fractured, some hematized,epidotized sections, some calcitic micro-veins, frequent weak breccia zones. 156.42 - 156.58 - quartz chlorite calcite vein. 161.00 - 1" quartz vein 9 1 5* to Core Axis.

Minor fluorite calcite, epidote in vein 161.54 - as at 161.00 162.06 - 163.98 - 70% quartz-chlorite, calcite

macro-veins, hematized wall rock, 1-21 pyrite in walls.

167.49 - 184.56 - more biotitic, moderately fractured, occasional breccia sections eg. 171.15-171.45 schistosity 35 0 to CA

177.94 - 178.37 - amphibolite dike?Mafic Sediments (Biotitic)- as above but significantly less altered, more biotite (and chlorite) rich. Bleaching parallel to schistosity and along micro-fractures persists but to a much lesser degree. No aluminum rich metamor phic minerals present. Schistosity 35 0 @ 197.82. 196.29 - 196.54 - pegmatitic calcite muscovite

quartz vein.

SAMPLE

NO.WIDTH

ASSAY VALUES

Au.

l

Drill HOU GG-7

* SONLotltude,

Diporfure Q -f SOW


Bearing .~———^^-~——^,

Dip ________________

Logged by Poge

ElevotlonSurface

i.n,th 419.71 metres n...

Oct. 2/82

' 10/82

FROM

239. 8 t

281.6,

4

TO

281.64

31-1.65

DESCRIPTION

199.19 - 203.45 - scattered amphibole - calcite rich bands. .5 to 3 inches.

205.44 - 210.92 - lighter grey weakly calcitic. 210.92 - 219.24 - frequent amphibole rich bands

(some calcitic) up to 301 interbanded Schistosity 35 0 at 218.54.

219.24 - 235.31 - biotite rich but increasing bleaching downhole. From 235.31 minor sillimanite.

Banded Mafic Sediments- laminated to coarsely banded brown, (biotite rich) whiteish (more sericitic) and greenish {amphibole rich) sediments. (Typical HW Corona West zone sections) Schistosity 35 0 -45 0 . 249.02 - 249.81 - epidote alteration plus quartz

veins. 254.08 - 254.23 - quartz vein. 265.66 - 265.76 - quartz vein. 266.52 - 266.64 - quartz vein. 270.54 - 271.52 - vaguely porphyritic (dike?) 273.16 - 273.25 - pegmatitic quartz vein.Mafic Sediments- thinly to thickly bedded (banded) brown (biotitic and green (amphibole rich) sediments. Generally the same as the overlying sequence but lacking the lighter bands (sericite altered, bleached). Schistosity 30 Q -35 C . 278.74 - 278.92 - quartz gashes. 284.87 - 285.02 - quartz vein at very shallow

angle.

SAMPLE

NO.WIDTH

ASSAY VALUES

Au.

Drill Hole GG-7

Lotltudt, SON

Otporturi SOW

Orflltd by Morrisette Lodged by

Storing .———.^—.—--——.——

Dip -^^^^—.--^.-.—-.

Pogt

SurfaceElevation

419.71 metresLength

Oct. 2/82pat* Started _ -u-

Oct. 10/82not* Flnl.h.d , . ,

FROM

314.6!

316.9:

363 -i

TO

316.93

363.57

371.64

DESCRIPTION

290.17 - 300.23 - scattered more massive sections (more biotite rich)

Quartz-Feldspar Porphyry- quite massive, unaltered uniform dike or sill. Lower contact @ 40 0 to Core Axis.Mafic Sediments (Green Banded)- bedded interbanded brown and green sediments. The brown sediments appear to be biotite rich in places, while other sections appear to contain up to 20% very fine staurolite. Green bands are large ly composed of amphibole and minor chlorite. Schistosity 40 0 to Core Axis. 320.04 - 320.22 - 801 barren quartz. 326.44 - 326.53 - barren white quartz. 334.67 - 334.82 - barren white quartz. 348.17 - 348.33 - barren white quartz. 351.83 - 351.98 - barren white quartz.More thinly banded from 352.35. 356.19 - 357.07 - .51 garnet porphyroblasts. 358.08 - 358.57 - definite cross-cutting dark

green mafic dike - cuts 3 30 0 and schistosity at 30 0 -50 0 .

358.57 - 359.36 - minor garnets. 360.88 - 361.98 - pseudo porphyry dark grey- grey

-green, flaky feldspar ghosts. 362.71 - 363.11 - as at 360.88 to 361.98 363.47 - 363.57 - as at 360.88 to 361.98Bleached, Sericitic Sediments, Mafic.- weakly mineralized light grey to brown schistose

SAMPLE

NO.WIDTH

ASSAY VALUES

AU.

Drill Hole GG-7

Lotltude — SON

Deporture SOW

Drilled by Morrisette Logged by

Beorlng _____________ Elevotlon

Dip ________________ Length _

Pogt

Surface

419.71 metres

Don Sforftd Oct. 2/62

Oct. 10/82Dott Flnlihed

FROM

371.64

373.78

TO

373.78

384.66

J

DESCRIPTION

and foliated mafic sediments becoming moresericitic toward 371.64.363.93 - 365.46 - moderately sericitic, 2-31 pyrite

No MoS, .364.57 - 364.69 - pseudo porphyry as at 360.88- 361.98.364.97 - 365.06 - grey quartz feldspar porphyrymoderately altered.

365.46 - 366.37 - moderately sericitic, 2-41 pyriteNo MoS, .

366.37 - 367.28 - quite sericitic, H pyrite.367.28 - 368.35 - quite sericitic, 3-51 pyrite.368.3.5 - 369.87 - weakly sericitic, .5 to 11 pyrite

minor garnet quite brownish. Minor arsenopyrite369.87 - 370.94 - weakly sericitic, quite brownish

H disseminated coarse arsenopyrite, .51 pyrite370.94 - 371.64 - quite sericitic. Minor very

coarse arsenopyrite, .5 to 11 pyrite.Sericitic Siliceous Tuff- schistose, very sericitic grey laminated tuffwith minor quartz eyes, arsenopyrite and MoSa .Schistosity 40 0 .371.64 - 372.86 - sericitic, 2-4% pyrite,

weak MoS] .372.86 - 373.78 - sericitic, vuggy fair MoS, on

occasional fractures, 5-71 fine pyriteSiliceous Tuff- dark to medium grey-blue, weakly to moderatelysericitic, moderately schistose, weakly foliated. No fragments visible. Pyrite occurs as very finedisseminated grains and also as coarser clots,

SAMPLE

NO.

49338

49339

490854908649087

4908849089

49090

49091

WIDTH

1.53

0.91

.911.07J. 52

1.070.7

1.22

0.92

ASSAY VALUES

Au.

02/T

.002

.042

.004

.016

.008

.004

.012

.042

.306

MoS a

1

.003

.003

.002

.002

.002

.025

.279

Checkoz/T

.045

.329

Drill HoleGG-7 Morrisette Drilled by

LotltutJt SON

Otporturi SOW

Beorlng

Dip ——.

Logged by Pooe

ElevationSurface Dote Starttd Oct. 2/82

Lenafh 419.71 metres D ott Plnt . h . d Oct. 10/82

FROM

*

TO DESCRIPTION

patches and seams generally trending parallel tothe foliation. MoS, occurs as a pervasive veryfine grains and smears along foliation planes.Green mica is present throughout as an alterationmineral in varying amounts parallel to foliation.In places, the green mica is vague but pervasive.Quartz veining is generally absent.Schistosity 40 0 -50 C to Core Axis.373.78 - 374.60 - 101 coarse pyrite, heavy MoS, ,

10% very fine pyrite, .2 mm. speck of VisibleGold at 374.08, 2 narrow brownish grey quartzveins.

374.60 - 375.82 - 2% coarse pyrite, S-7% finepyrite, heavy MoS a , dark grey-blue tracetourmaline.

375.82 - 376.73 - more greenish (green mica),moderate granular white irregular quartz(white) , minor biotite, 51 very fine pyrite.

376.73 - 377.95 - 3-51 coarse pyrite, 5-81 finepyrite, greenish-grey, weak to moderate MoS, ,minor biotite.

377.95 - 379.17 - 5% coarse pyrite, S-7% finepyrite, grey-green moderate MoS, , minor biotite

379.17 - 380.09 - 3-51 fine pyrite, quite sericitescattered granular quartz, minor biotite, fairgreen mica, weak MoSj , .6 ft. quartz vein at379.29.

380.09 - 381.00 - S-8% pyrite, ID-15% granularirregular white quartz, altered weak tomoderate MoS3 , some tourmaline.

381.00 - 382.22 - S-5% coarse pyrite, 3-51 finepyrite, moderate MoS a , greenish mica richsections.

SAMPLE

NO.

49092

49093

49094

49095

49096

49097

49098

49099

WIDTH

0.82

1.22

.91

1.22

1.22

0.92

0.91

1.22

ASSAY VALUES

Au.•W*

.295

.338

.159

.169

.215

.120

.364

.209

MoS a*

.726

.239

.085

.058

.080

.143

.153

•.145

Checkoz/T

.192

Drill Hole GG-7

LatitudeSON

Deporturt O * SOW

Drilled by

Bearing ,_

Dip ^—^

Morrisette Logged by Poge 8

SurfaceDot* Started

Oct. 2/82

i , not h 419.71 metres Dott pinl . h .d Oct. 10/82

FROM

384.66

387.71

TO

387.71

389.60

0~

DESCRIPTION

382.22 - 383.13 - 101 very fine pyrite, heavy MoS,fractures (not all parallel to schistosity) .1 cm. quartz vein plus realgar pyrite MoS,flakes at 382.95.

383.13 - 384.05 - S-8% fine pyrite, moderate toheavy MoS a , minor biotite plus tourmaline,patchy fine green mica. Schistosity 50*.

384.05 - 384.66 - 10% pyrite, fair amount of MoS,,fair amount of green mica. Minor biotite andtourmaline.

Mixed Tuffaceous Sediment- dark grey schistose, foliated moderately altered,sericitic showing some metamorphic banding oflighter and darker material. 20%-30% biotite, minortourmaline, patchy fracturing typical of sediments.384.66 - 385.27 - H pyrite.385.27 - 386.18 - 11 pyrite, some sillimanite.386.18 - 387.10 - . 51 pyrite, patchy alterations

along fractures.387.10 - 387.71 - 2-^ pyrite, more sericitic minor

tourmaline.Sericitic Siliceous Tuff- well mineralized, strongly schistose, sericitic,laminated grey to greenish tuff. Schistosity 50* toCore Axis.387.71 - 388.92 - lQ-15% fine pyrite, no MoS,,

minor tourmaline.388.92 - 389.60 - 10% pyrite, some epidote (due

to proximity of quartz-feldspar porphyry 'tracetourmaline.

SAMPLE

NO.

49100

49301

49302

493034930449305

49306

49307

49308

WIDTH

0.91

0.92

0.61

0.610.910.92

0.61

1.21

0.68

ASSAY VALUES

AU.QS/T .414

.392

.113

.010

.010

.016

.022

.061

.024

MoS,— t ——.344

.199

.090

.005

.002

.002

.003

.002

.002

Checkoz/T

.393

.017

Drill Holt GG-7

l * SON

Drilled by

Bearing ——

MorrisetteLogged by Poge

Deporture O * SOWElevation Surface


Oct. 2/82

Oct. 10/82

FROM

389.60

394. 95

' ———————— - ——————— ucnîn , _ ,,,,... Pfl*t Finished

ro

394.99

397.15

397.13 413.0

4

DESCRIPTION

Quartz Feldspar Porphyry (Sill)- medium grained uniform, very weakly foliated,dark grey sill. Upper and lower contacts at 50 0to Core Axis.389.60 - 390.14 - typical quartz-feldspar porphyry

but with fine grained section and 6 cm. bandof 101 banded pyrite near 390.14.

390.14 - 391.67 - typical quartz-feldspar porphyry391.67 - 393.19 - typical quartz-feldspar porphyry393.19 - 394.99 - typical quartz-feldspar porphyrySericitic Siliceous Tuff- light grey, quite sericitic, occasionally vuggyschistose and well foliated tuff. Little or novisible MoS 3 .394.99 - 395.94 - vuggy dark grey-green on quartz-

feldspar porphyry contact. More sericitictowards 395.94.

395.94 - 397.15 - very sericitic, vuggy patches,lQ-15% rather coarse pyrite. Light grey.

Siliceous Tuff- dark grey-blue schistose, weakly to moderatelyfoliated, fine grained siliceous (cherty?). Noobvious fragments. Pyrite occurs as mainly finedisseminated grains but also as coarser grainedblebs and seaiiis crudely parallel to foliation.MoSj occurs as very fine pervasive mineralizationand as massive smears along foliation planes.Green mica, although pervasive, is a minor compon ent, as is tourmaline.

SAMPLE

NO.

49309

493104931149312

49313

49314

W 1 0 T Mf* i w i n

0.54

1.531.521.80

.95

1.21

ASSAY VALUES

Au.OZ/T

.008

TraceTrace.002

.020

.073

MoS,s

.003

.005

.003

.003

.002

.007

CV*of"*V

oz/T

.015

i

Drill Hole GG-7 Drilled by Morrisette Logged by Pogt 10

, P.M. .H. l * SON

D. PO flur. SOW

Bearing

Dip ^-

Elevation

Length

Surface419.71 metres

Dot* Storted

Dot* Flnlthttf

Oct. 2/82

Oct. 10/82

FROM TO

-

DESCRIPTION

397.15 - 398.37 - 101 coarse pyrite scans plus5-71 fine pyrite, moderate amount of MoS, inS 1 2T fi 3. Jc S

398.37 - 399.29 - 7-101 coarse pyrite seams, S-5%fine pyrite, weak to moderate MoS, , moresericitic and banded 398.83 - 399.39.

399.29 - 400.20 -399.44 - 399.71 - brownish grey quartz vein

biotite, MoS,, pyrite on walls399.84 - 400.20 - pseudo quartz-feldspar

porphyry, trace pyrite. 400.20 - 400.81 - white fractured quartz vein,

trace MoSj in vein.400.81 - 402.03 - m fine pyrite, 101 quartz

(two macro-veins) containing realgar and minorstibnite, moderate to heavy MoSa .

402.03 - 402.95 - 10-151 pyrite, heavy MoS, wisps,dark grey.

402.95 - 403.86 - 1SI pyrite, heavy MoS, wisps,dark grey.

403.86 - 404.77 - 10t very fine pyrite, onlymoderate MoS, , minor tourmaline.

404.77 - 405.38 - 10t fine pyrite, fair MoS, onfoliation planes, some granular quartz.

405.38 - 406.45 - 151 fine pyrite, some very finegrained cherty sections, 20-25% pyrite, somegranular white quartz, heavy MoS,, minor realga

406.45 - 407.21 - 7-101 pyrite (some coarse),rinor MoS,, quite schistose.

407.21 - 408.13 - 101 pyrite, heavy MoS, on somefoliation planes, some realgar in quartzfractures,* some granular quartz.

SAMPLE

NO.

49315

49316

49317

49318

49319

49320

49321

49322

49323

49324*

49325

49326

WIDTH

1.22

0.92

0.91

0.61

1.22

0.92

0.91

0.91

0.61

1.07

0.76

0.92

ASSAY VALUESo^?

.081

.072

1.315

.104

.459

.484

.085

.118

.147

.145

.130

.185

MoS,

0.090

.075

.070

.002

.093

.177

.108

.063

.073

319. J A y

.095

.152

CheckOZ/T

1.225

1 on . loU

Drill Holt,

Lotltudt...

GG-7

SON

Deport.urt O 4- SOW


Storing .-———-^x-^^^^.

Dip ________________

togged by

Elevotlon ^

Length

II

Surface

419.71 metresDot* Storttd

Daft Flniihtd

O**. 2/82

Oct. 10/82

FROM

413.0

413.37

416.36

TO

413.37

ae. 36

117.33

*

DESCRIPTION

408.13 - 409.35 - ID-15% pyrite (some coarse) plusheavy MoS, in places, heavy realgar in quartzfractures, minor stibnite, tourmaline.

409.35 - 410.26 - ID-15% fine pyrite, pervasiverealgar and granular white quartz. Moderate toheavy MoS, .

410.26 - 411.18 - 151 fine pyrite, very heavyrealgar ( -t- orpiment?), weak MoS,, lighter grey,pervasive granular quartz.

411.18 - 412.09 - 15* fine pyrite, very heavyrealgar, weak MoS 2 , medium grey, 301 granular(granulated?) quartz.

412.09 - 413.00 - 15* fine pyrite, very heavy real gar, moderate MoS, (flakes), medium arey-orange30-401 granular quartz.

Mafic Dike- dark green chloritic medium ^rained dike, 501chlorite, 50t blueish quartz.Sericite Schist- greyish-white sericitic, foliated lapilli tuff,3% fine quartz eyes, plus 1-21 fine tourmalineneedles. .5 to 21 pyrite.413.37 - 414.53 - trace MoS,, 11 pyrite.414.53 - 416.36 - .5 to U pyrite.Mafic Dikes

-801 chloritic uniform mafic dikes or sills.416.36 - 417.27 - minor pyrite in 201 sericite

schist.

SAMF.E

NO.

49327

49328

49329

49330

49331

49332

4933349334

4933j

WIDTH

1.22

0.91

0.92

0.91

0.91

0.37

1.161.83

.97

ASSAY VALUES

Au.OZ/T.198

.343

.270

.367

.358

.101

.032

.010

.016

MoS al.143

.158

.125

.344

.454

.037

Checkoz/T

.347

.020

Drill Hole GG-7 Pogt 12

Lotltu

Dtpori

FROM

417.32

. 1 * 50N 0 , f l Surfaced* Bearing , Fl.untlno

0 * SOW 419.71 metresuri Dip L*n9fh

TO

419.71

419.71

*

DESCRIPTION

Silicified Sericite Schist- grey-blue very fine grained, weakly sericitic tuf417.33 - 418.49 - .8 foot quartz vein e 30* to

Core Axis. Minor MoS a , ^ pyrite streaks.418.49 - 419.71 - .5 to It pyrite, minor MoS, .

END OF HOLE 17

Collar ?5?iiulfr\s Dips Acid

-90100 - - -88200 089 0 True -87 0 -86300 - - -84400 092 0 True -84 0 -84500 - - -83600 032 0 True -82 0 -82700 - - -81800 303 0 Magnetic -80 0 -80900 - - -79

1000 253 0 Magnetic -78 0 -781100 - - -73?1200 083 0 Magnetic -71 0 -75?1300 - - -741377 282" Magnetic -74 0 -73.5

SAMPLE

NO.

?49336

49337

WIDTH

1.16

1.22

Oott Ste

Dot! Flnl

Oct. 2/82 "rt. A

Oct. 10/82 .h. d

ASSAY VALUES

AU.oz/T

.004

.002

OH,. HO,. G C - 8 n r|Iltd b v Morrisette | ooaed b v R. Kemp P flflt 1

1 * 50M. East , 8n * Surface Oct- 8/821 otlfud. Storing -tOU Fleuatlnn J ui Dot. Sfort.d

1 * 50H. North flfl * 421.54 metres Oct. 18/82Dtnortur* , . ,, Dip -oo ^ Length Dflf* Flnlphfd .— .,,,. ...,.,,

FROM ~ n WHB

03.66

TO

3.66

111.07

*

DESCRIPTION

Casing.Mafic Sediment- Well foliated with thinly bedded alternating unitsof sericite schist 4 sediment, minor sulphides-trace9 6.10 angle bedding to core axis 30*9 16.95 angle bedding to core axis 30*9 23.47 change in color from light to darker unit.

26.52 - 46.09 - garnet 4 staurolite bearing maficsediment - garnets are the first to come inwhile staurolite doesn't start to come inuntil 35.72, bedding ranges in size from 5 mm.up to 1.5 inches.© 27.16 - quartz vein. @ 30.48 angle beddingto core axis r 30*. d 37.80 angle bedding tocore axis r 30*. 9 46.09 - staurolite fallsout.

46.09 - 60.66 - mafic sediment, garnet bearing46.09 - 46.51 - mafic tuff zone( amphibolized)Upper contact 9 45* Lower contact 9 30*49.65 - 49.83 - coarse grained amphibolizedunit with bleached contacts.50.51 - 50.60 - quartz vein at high angle tocore 950.90 angle of bedding to core axis: 35V

60.66 - 66.35 - intermediate sediment, garnet bearincNoticeable decrease in mafic constituent 4interbedded sericitization, massive 4 pristinein appearance, disseminated 4 blebs of pyriteapproximately 2SJ. {4.47 - 66.35 - massive intermediate unit with

SAMPLE

NO.WIDTHW 1 W i H

ASSAY VALUES

Au.

Drill HOUGG-8

Drlllid by Morrisette Logged by R, Kemp Pogt

LoWude, Storing Elevotlon Dote Starttd

Departure Dip Length Dart Finished

FROM TO

*

DESCRIPTION

institial carbonate.66.35 - 83.76 - mafic sediment, garnet A staurolite

bearing - staurolite comes in ® 69.31 while garnet is always present. Staurolite occurs stronger towards sericite bearing zones. ®67.67 angle bedding to core axis s 30*. 3 74.37 - quartz vein, chloritized parallel to foliation .® 77.51 - quartz vein, chloritized parallel to foliation .

83.76 - 111.07 - mafic sediment - staurolite hasleft by 83.76 and garnet falls out by 84.61. Bleached intermediate in color zone which may

* by possible feldspar porphyry but due to alter ation, difficult to say - small feldspar phenocrysts exist. Upper contact O 15*. Lower contaca 10*.® 84.55- quartz vein at high angle to core. (D 90.65 - quartz vein.93.76 - 94.06 - feldspar porphyry, upper and lower contact ® 20*.94.06 - quartz vein. ® 105.22 - angle of bedding to core axis s 35* 107.29 - 107.90 - brecciated zone confined witha bounded bed.107.05 - 107.14 - mafic tuff, upper A lower contact at 35*.108.91 - 109.42 - quartz carbonate filled fractured zone.111.01 - 111.07 - brecciated horizon.

SAMPLE

NO.

t

WIDTHASSAY VALUES

Au.

Drill t

LQtltu

Deport

FROM

111.07

113.42

117.38

117.84

j n i, UG-B ' . .., . . Morrisette K. Kemp 0 s v-- i n| * , Driiitd bv Logged by Poot

Se Rearing, Flevatlan ,

urt Dip Length

TO

113.42

117.38

117.84

323.70

DESCRIPTION

Zone of Feldspar Porphyry- 111.07 - 111.86 - zone of alternating bedded feld

spar porphyry bearing units 4 mafic sediment. 111.86 - 113.42 - feldspar porphyry.Mafic Sediment- Mafic with a little bedding being present - occasional thinly bedded feldspar porphyry. 113.42 - 113.78 - bleached quartz carbonate fracture 115.49 - 115.61 - quartz carbonate injection 116.13 - 116.62 - mafic tuff { amphibolized) 116.62 - 116.77 - quartz vein plus bleached wallrock

Mafic Dike

-Upper contact at 35*. Lower contact at 30*.Mafic Sediment- Continuation of section 113.42-117,38. Quartz carbonate vein ® 117.29 - 117.38. d) 118.23 - tourmaline occurring within a fine grain

ed thinly bedded unit approximately 1" wide. From 117.84 - 121.55 - same description as 113.42-

117.38. 121.74 - 122.07 - mafic sediment, bleached with

approximately 255 disseminated pyrite within fracture parallel to foliation.

122.07 - 136.52 - interbedded thinly laminated feld spar porphyry unit as expressed by the occur rence of small, faint feldspar phenocrysts, bleached .

SAMPLE

NO.WIDTH

Doft Sto

Dote Flnl

rt.d

.h. d

ASSAY VALUES

Au.

Drill Hoi*GG-B Morrisette

Drilled by Logged byR. Kemp Pogt

L otltude. Beorlng Elevoflon Date Started

Departure Dip Length Date Flnlihed

FROM

9

TO DESCRIPTION

136.52 - 143.41 - garnetiferous, mafic sediment® 136.52 garnets start appearing in maficsediment horizon. 0 138.38 - staurolite comesin, co-existing with garnets.138.90 - quartz 4 chloritic vein142.16 - quartz vein.33 0 angle of foliation to core axis ® 127.71.40* angle of foliation to core axis 9 139.60.

143. 41 - 149.90 - intermediate sediment - lighter incolor than mafic sediment, bleached with thin ly interbedded (hematized) units.145.15 - 145.24 - feldspar porphyry - uppercontact 35*. Lower contact 40*.146.85 - 146.94 - quartz vein, through thissection coarse grained staurolite 4 garnetoccur randomly.

149.90 - 195.22 - mafic sediment: garnet 4 staurolitebearing .Mafic sediment with a stronger representationof garnet 4 staurolite.154.78 - 154.84 - quartz carbonate vein.40* angle bedding to core axis ® 176.78.185.32 - 185.68 - feldspar porphyry. Uppercontact ® 40*. Lower contact at 45*.188.06 - 188.27 - quartz carbonate vein.40* angle bedding to core axis ® 191.11.

195.22 - 290.66 - mafic sediment - falling out ofgarnet 4 staurolite, however occurs randomlywith more mafic horizons exist (amphibolizedmafic tuff zones)

SAMPLE

NO.WIDTH

ASSAY VALUES

Au.

:

Drill HoleGC-e Morrisette

Drilled by Logged byR. Kemp Pogt

Lotltude. Scoring Elevotlon Dote Storted

Oeporture Dip Length Do f e Finished

FROM TO

4

DESCRIPTION

Occurrence of garnet i staurolite ® 198.42 - 198.70199.22 -200.10, 204.22 - 205.40, 209.15 -211.50.211.50 downwards is mafic sediment with nointervening garnet or staurolite. Thinlybedded cherty zones exist randomly. With thesecherty zones, mafic sediment is found asswirls which has accumulations of up to 2?opyrite as dissemination, the zone has randomfractures and associated bleaching.45* angle foliation to core axis ® 215.49.226.31 - 227.78 - light grey brecciated zone.45* angle foliation to core axis 9 230.73.238.66 - 239.15 - fractured zone with quartzcarbonate filled fractures.239.76 - quartz vein.243.47 - quartz vein.45* angle foliation to core axis ® 243.69.245.73 - 246.52 - mafic sediment with smallfeldspar phenocrysts.250.09 - 250.27 - fractures filled with epidot265.97 - 267.00 - fractures filled with epidotplus quartz carbonate.274.38 - 275.30 - vuggy hematized zone. ISpyrite .278.89 - quartz vein.282.12 - quartz vein.282.31 - quartz vein.288.10 - quartz vein.

290.66 - 323.70 - mafic sediment to intermediatesediment. Distinct hematization occurring, providing a reddish hue to localized horizons.

SAMPLE

NO.

l

t

WIDTHASSAY VALUES

Au.

j

GG - 8Drm HOI. ft,Mi.H s v norraaeiie ( ^^ H u n. * B M, M P flfl ,

Lotlfu

Otport

FROM

323.7

333.9:

340.67

t

d* ———————————————— Bearing Elevation

ur* . . ... Din Length

TO

338.97

340.67

365.70

DESCRIPTION

The zone is commonly bleached and contains random hairline fractures. 302.36 - quartz vein, 304.07 - quartz vein. 60* angle foliation to core axis 0 292.00. 305.90 - 323.70 - mafic sediment, bleached/ reddish hue/ hairline fractures with assoc iated epidote, occasional thinly bedded argil laceous units with approximately 15c pyrite. 65* angle foliation to core axis ® 320.65. Quartz vein d 319.95 4 315.47 4 316.87 4 314.9

Mafic Sediment Plus Quartz Sericite Schist- Mafic sediment plus sericite schist beds with sericite schist forming thin beds, sericitic beds start coming in at 330.19. 65* angle foliation to core axis @ 333.51. 325.94 - 326.75 - intermediate unit, massive, possib

le feldspar porphyry but porphyry not evident. 326.96 - quartz vein. 327.20 - quartz vein. 325.71 - quartz vein.Feldspar Porphyry- Upper contact ® 55*. Lower contact @ 70*. Mafic Sediment with Interbanded Quartz Sericite Schi- Mafic sediment 4 interbedded quartz sericite schis with small white non-carbonate material standing out in sericite zones, a faint reddish hue imparted to thinly bedded zone. Staurolite oresent from 343.20 - 346.41.

SAMPLE

NO.

}

it

WIDTH

Dot* Sfo

Oar* Fin

rt t d

ih*d

ASSAY VALUES

Au.

Lotltu

Diport

FROM

367.31

368^

j.,. GG-B ^ .,, . . Morrisette D u *. mn o --. 7 ^ ole Drilled by Loaned bv R* Kemp Page /

at ———————————————— Bearing.,, Flevattan

ure ———— . . Dip. Length

TO

368.81

375.39

DESCRIPTION

From 348.84 to 365. 7- mafic sediments are well foliated 4 fine grained with interbedded cherty horizons, interbedded sericitic zones appear to fall out with depth. Quartz veins are granular (re-crystallized?) occurring at 348.23 - 348.57. 350.43 - 350.64 - porphyroblasts of white non-carbon

-ate material, appearing liko but not o feld spar porhpyry. 55* angle of foliation to core axis 9 351.13.

Quartz carbonate vein 9 354,54 - 354.85, 4 363.75 - 363.84

® 364.08 - staurolite and garnet appear, before this maybe staurolite existed, however only inter mittent within selected zones. 60* angle of foliation to core axis 9 364.08.

From 364.91 to end, garnetiferous mafic sediment/ fine grained/no interbedded quartz sericite schist .

365.7 - 366.40 - Mafic Sediment - coarse grained 4massive, no garnets.

366.40 - 367.31-Banded Mafic Sediment - bleached 4slightly chloritized/garnetiferous to end of section .

Quartz Sericite Schist 4 Interbedded Mafic Sediment- Thinly bedded with intermittent zones with garnets / arsenopyrite occurring within mafic sediment horizons. Pyrite 1SJ. Arsenopyrite 2X . 65* angle to core axis Q 367,89.Silicified Quartz Sericite Schist- Thinlv bedded with lenses, wisos 4 tlvLa of pyrite

SAMPLE

NO.WIDTH

Dote Sfo

Date Flnl

rt. d

.h. rf

ASSAY VALUES

Au.

1

Drm Hole GG-6 Drilled by Morrisette Logged byR. Kemp Poge

8

Latitude. Bearing Elevation Oat* Starred

Oipcrtur* Dip Length Oat* Finished

FROM

375.39

TO

387.10

*~

DESCRIPTION

chalcopyrite, arsenopyrite 4 pyrrhotite.Pyrite s 4S, Arsenopyrite s IS, Chalcopyrite s 0.55,Pyrrhotite s 0.5S.367.44 - 368.81 - garnets/interbedded sericite

schist/ arsenopyrite - 2%, pyrite - IS.368.81 - 369.42 - sericite schist, disseminated 4

blebs of pyrite, less than 3S.369.42 - 37U.33 - interbedded sericite schist plus

mafic sediment lenses 4 blebs of pyrite, lessthan 3S.

370.33 - 371.25 - mafic sediment, trace garnet,trace pyrite.

371.25 - 372.16 - mafic sediment with sericiteschist towards base of section. Pyrite IS.

373.16 - 373.38 - sericite schist. 3S pyrite.373.38 - 374.29 - sericite schist. BS pyrite374.29 - 375.21 - sericite schist. 3S pyrite.375.21 - 376.12 - mafic sediment /fragmental/wispy

4 bleby 4 disseminated pyrite, up to 8S.376.12 - 377. Pi - mafic sediment/f ragmental plus

fuchsite bearing sericite schist, plus small,less than 1" feldspar porphyry within serJciteschist horizon. Pyrite approximately 8S.

370.64 - 371,43 - mafic sediment - massive, pristineTrace garnet/ no sulphides.

371.43 - 375.39 - silicified quartz sericite schist/thinly laminated to thickly bedded with wisps,blebs and dissemination of pyrite, up to BS.

Mafic Sediment 4 Fragments^ Plus Fragmental BearingSericite Schist- Mafic sediment/dark/ lenticular fragments parallel

SAMPLE

NO.

49340

49341

49342

49343

43944

49345493464934749348

49349

WIDTH Metres

1.37

.61

.91

.91

.91

1.22.91.91.91

.91

ASSAY VALUES

Au.(OZ/T;

Trace

Trace

Trace

Trace

.OH

TraceTrac j.Oj6.004

.006

Drill Holt GC-0 Drilled by Morrisette Logged by R. Kemp Page

Lotltude.

Deportu/e

Storing

Dip ^— Length

Daft Started

Dote Finished

FROM

0

TO DESCRIPTION

to foliation, green color forming interstitial tofragments plus mafic sediment (chlorite?) fragmentsare cherty to mafic slivers. Pyrite less than 6S,Mafic sediments A fragments to 385.72.Sericite schist 4 fragments 385.72 - 386.55 -

fuchsite bearing.Mafic dike 386.55 - 386.64.Mafic sediments i fragments 386.64 - 387.00.377.04 - 377.95 - mafic sediments 4 fragments/

disseminated pyrite, blebs, wi?ps. Pyrite lessthan W ,

377.95 - 378.87 - mafic sediments 4 fragments/disseminated pyrite, blebs, wisps. Pyrite lessthan 6ifl.

378.87 - 379.78 - mafic sediments 4 fragments/disseminated pyrite, blebs, wisps, Pyrite lessthan 6Si.

379.78 - 380.70 - mafic sediments 4. fragments/, disseminated pyrite, blebs, wisps. Pyriteless than 5 3.

380.70 - 381.61 - mafic sediment 4 fragments/disseminated pyrite, blebs, wisps. Pyriteless than 5S.

381.61 - 382.52 - mafic sediment 4 fragments/disseminated pyrite, blebs, wisps. Pyrite lessthan 55X.

382.52 - 383.44 - mafic sediment 4 fragments/disseminated pyrite, blebs, wisps. Pyrite lessthan 6*.

383.44 - 384.35 - mafic sediment 4 fragments/disseminated pyrite blebs 4 wisps, plusfuchsite bearing fragments. Pyrite 6-7S.

SAMPLE

NO.

49350

49351

49352

49353

49354

49355

49356

49357

WIDTH Metres

.91

.91

.91

.91

.91

.91

.91

.91

ASSAY VALUES

Au.OZ/T;

.026

.008

.012

.016

.012

.060

.006

.010

Drill Hole CG-8Drilled by

MorrisetteLogged by R. Kemp Page 10

Latitude, Bearing Elevation Date Started

Departure Dip Length Dore Finished

FROM

387.1

388.77

TO

388.77

400.96

e

DESCRIPTION

384.55 - 385.27 - mafic sediment * fragments *fuchsite fragments.384.78 - 384.96 - sericite schist * fuchsite.Pyrite 6-755.

385.27 - 386.18 - mafic sediment * fragments /sericite schist -f fragments * fuchsite.Mafic sediment * fragments 385.27 - 385.72Sericite Schist 385.72 - 386.18.Pyrite 6-7S. t

386.18 - 387.10 - 65 to core axis 9 386.18.Pyrite 6-7S. Sericite schist * fragments *fuchsite fragments 386.18 - 386.55.Mafic dike 386.55 - 386.64. Pyrite-blank .Upper contact 9 80 . Lower contact 9 70 .Mafic sediments 4 fragments 386.64 - 386.85,pyrite 3-4S.Mafic sediment, no fragments, massive - 386.85- 387.10, pyrite s 0.5S.

Feldspar Porphyry- Massive/pristine.Mafic Sediment * Fragments388.77 - 389.05 - barren mafic sediment/massive.389.05 - 393.04 - mafic sediment * fragments *

pyrite 6-8S, with pyrite decreasing in amounttoward bottom of zone, cherty A mafic fragment/slivers. Q.8S arsenopyrite. 4-65 pyrite.

388.77 - 389.69 - mafic sediment * fragments.Pyrite 7SJ. Barren 388.77 - 389.05.

389.69 - 390.60 - mafic sediment * fragments. Pyrite 85!.

SAMPLE

NO.

49358

49359

49360

49361

49362

49363

WIDTH Metres

.91

.91

.91

1.68

.91

.91

ASSAY VALUESCU27T )

Au-

.004

.008

.004

.002

.028

.012

Drill HoltGG-8

Lotltudt.

Diporturt

Drilled by MorrisetteLogged by

R. Kemp Pogt 11

Storing

Dip —- Length

Oflt* Sforttd

Dott Flnlthtd

FROM

.

9

TO DESCRIPTION

390.60 - 391.52 - mafic sediment * fragments.Pyrite 75.

391.52 - 392.43 - mafic sediment * fragments.392.73 - 393.04 - feldspar porphyry/ very small to

negligible feldspar phenocrysts.Mafic Sediment * FragmentsMafic sediment plus fragments with thinly inter bedded quartz sericite schist zones, plus maficsediment zones devoid of fragments, plus occasionalquartz vein.393.04 - 393.34 - mafic sediment * feldspar porphyr)

(small phenocrysts) mafic/some fragments.Pyrite 1.0'*. Trace garnet.

393.34 - 394.26 - mafic sediment -i- occasionalfragment, 393,34-394.14, quartz sericiteschist (siliceous) 394.14-394,26 Pyrite 2. OS.

394,26 - 395.33 - mafic sediment * fragment.Quartz sericite schist 394.53-394.66.

4 395,14-395.20.Pyrite s 35!.

395.33 - 396.24 - mafic sediment * fragment *quartz vein 8 396.00 - 396.09. Pyrite s 25.

396.24 - 397.15 - mafic sediment * fragment.Pyrite 2-35.

397.15 - 398,07 - mafic sediment * fragment.Pyrite 2-35.

398.07 -398.98 - mafic sediment * quartz vein 9398.25, Pyrite 2-35.

398.98 - 399.90 - mafic sediment * fragment.Pyrite 25.

SAMPLE

NO.

49364

49365.

49366

49367

49368

49369

49370

49371

49372

49373

WIDTH Metres

.91

.91

.30

.91

1.07

.91

.91

.91

.91

.91

ASSAY VALUES

AU.,

.030

.016

.012

.029

.018

.048

.012

.024

.018

.042

GG-8 Morrisette R v . mn 1 2 '•' V'^s5OHM Hole n,m,d bv . o gg .d by R' K emp Poo* 1 Z

Lotlfud* .. Bearing Plcvatlon , not* Started

DiDortur* Din Length Dot* Flnlih.d

FROM

400.96

102.58

TO

402.58

403.86

*~

DESCRIPTION

399.90 - 400.81 - mafic sediment * fragment to399.96. 2?o' pyrite. Mafic sediment, fragmentsdying out 399.96 - 400.29. Mafic sediment *fragments 400.29 - 400.60 (End of Box 68)Pyrite 2S.

Mafic Sediment (Fragments) Plus Quartz SericiteSchist- Lighter in color than previous zone, much moresericitic with lenses 4 shards of fuchsite, pluscherty fragments plus quartz eyes, MoSt noted ®401.42 4 401.67. Pyrite r BK.400.81 - 401,73

400.81 - 400.96 -mafic sediment * fragmentsPyrite s 3SJ.400.96 - 401.73 - greenish color/sericitic *fragments * fuchsite * possible MoS Q 401.03,401.42, 401.67.Pyrite s 8?i. Fuchsite r 2S. MoS t s 0.1S.

401.73 - 402.58 - greenish color/sericitic/* frag ments * fuchsite. Pyrite 8S. Fuchsite O.OBSi.

Foliated Quartz Sericite Schist -f Interbedded MaficSediment- Mafic sediment is fine grained 4 provides thefoliated appearance, quartz sericite schist makesup the majority of the unit. 65* angle foliation tocore axis 0 402.95.402.64 - 403.56 - foliated, quartz sericite schist

with thinly bedded mafic units. Pyrite 1.0!*.403.56 - 404.47

403.56 - 403.86 - foliated, quartz sericite

SAMPLE

NO.

49374

49375

49376

49377

49378

WIDTH Metres

.91

.91

.91

.91

.91

ASSAY VALUES

n^T^.057

.126

.169

.052

.028

CheckOZ/T.070

.169

.054

Drill Hole GG-8 Drill.d by Morrisette Logged byR.. Kemp Page 13

Lotltude. Bearing Elevation Dot* Started

Departure Dip Length Dot* FInlihed

FROM

403.86

TO

411.51

•1

DESCRIPTION

schist * interbedded mafic units. Pyrite 1.0S5,403.86 - 404.47 - quartz sericite schist.0.05SS pyrite.

Silicified, Quartz Eye Sericite Schist- Massive plus silicified sericite schist withprominent quartz eyes/ breaking up the unit are409.47 - 409.56 - feldspar porphyry409.99 - 410.11 - amphibolized mafic sediment/

medium grained.410.14 - 410.78 - faint feldspar porphyry.411.18 - 411.30 - feldspar porphyry.Pyrite - l ?o localized, ie. not pervasive.404.47 - 405.38 - quartz eye sericite schist,

silicified, pyrite fractures, cross-cuttingfoliation 0 405.23 - 405.38.Pyrite - 1 .0S5, bluish tinge @ 405.23 -possibleMoS t .

405.38 - 406.3 - same as above. Pyrite fractures s2.0?i Pyrite, bluish tinge may indicate poss ible MoS^.

406.30 - 407.21 - same as above, ie. silicified,quartz eye sericite schist. Pyrite r 0.85.

407.21 - 408.13 - quartz eyes, silicified sericiteschist. Pyrite 0.083.

408.13 - 409.04 - silicified sericite schist.Pyrite r trace.

409.04 - 409.96 - ditto above * feldspar porphyry409.47 - 409.56.

409.96 - 410.87 - ditto above * amphibolized sed iment, green, medium grained from 409.99 - 410.11. Feldspar porphyry 410.14 - 410.17.

SAMPLE

NO.

49379

49380

49381

49382

49383

49384

49385

WIDTH Metre

.91

.91

.91

.91

.91

.91

.91

ASSAY VALUES

3 Au.( Q i./ T )

.016

.026

.014

.052

.026

.018

.046

Checkoz/T

.015

Drill Holt

Lotltudt

Dtporturt

GG-8 Morrisette R. Kemp Page

. ————————— . S toring . , ,

* Dip

Flevotlan

L*nnfh , ,,

,. ,,.., ,. O of * Storf *d , M

Dot* Plnl.h.d

FROM

111.51

(11.78

9

TO

All. 78

421.45

DESCRIPTION

410.87 - 411.78 - silicified sericite schist with feldspar porphyry units 411.21 - 411.30.

4 411.51 - 411.78. Small pyrite filled hairline fracture 0,83 Q 410.90.

Feldspar PorphyryUpper contact ® 65 ", Lower contact ® 65*. Quartz Eye, Silicified Sericite Schist- Quartz eye bearing silicified sericite schist with interbedded amphibolized zones A quartz vein fract ures filled by pyrite randomly occur along with zones with a bluish tinge which may indicate the presence of finely disseminated MoS*. Ground core between 414.83 to 415.14 approximately 50Si. Amphibolized mafic sediment/tuff 413.49 - 413.74. Amphibolized mafic sediment/tuff 415.93 - 415.99. Amphibolized mafic sediment/tuff 420.29 - 420.41. Quartz vein 0 418.67 - 418.76.411.78 - 412.70 - quartz eye sericite schist.

Trace pyrite. 412.70 - 413.61 -

412.70 - 413.49 - quartz eye sericite schist. 413.49 - 413.61 - amphibolized mafic sediment. Trace pyrite.

413.61 - 414,53 - quartz eye sericite schist with pyrite filled fractures * possible MoSj. surrounding pyrite zones. Pyrite s 2K, 413.61 - 413.74 - amphibolized mafic sediment tuff.

SAMPLE

NO.

49386

49387

49388

49389

WIDTH

.91

.91

.91

.91

ASSAY VALUES( uz/ T")

Au.

.028

.022

.004

.014

Drill Moll

Lotltudt

Dtporfuri

GG-8 Morrisette 15'* Drilled bv

———————— Rearing

1 Dip

. . tt. Kemp Loijaed by

Flcuatlan

,, , ,, Lingfh , ,

Poo* * J

— Dot* Slor**d _ ,..

Dot* Flnlihad ,

FROM

0

TO

.421.5^

DESCRIPTION

414.53 - 415.44 - quartz eye sericite schist.Pyrite filled fractures * possible MoS^.Pyrite - I S.

415.44 - 416.36 - quartz eye sericite schist. Tracepyrite. Amphibolized mafic sediment/tuff415.93 - 415.99.

416.36 - 417.27 - quartz eye sericite schist. Tracepyrite.

417.27 - 418.19 - quartz eye sericite schist. Tracepyrite.

418.19 - 419.10 - quartz eye sericite schist.Quartz vein 418.67 - 418.76, disseminated tobleby pyrite IS in chloritic quartz sericiteschist .

419.10 - 420.01 - quartz eye sericite schist.Pyrite l?i.

420.01 - 421.54 - quartz eye sericite schist.2?o pyrite, amphibolized mafic sediment/tufffrom 420.29 - 420.41.

END OF HOLE # 8

SAMPLE

NO.

49390

49391

49392

49393

49394

49395

49396

WIDTH

.91

.91

.91

.91

.91

.91

1.52

, A SSAY VALUES0//T) ——————————————— Au.

.010

.002

Trace

Trace

.002

.002

Trace

Drill Hole btj" y

i nm.m. 2 + 50N

Drilltd by . Morrisette Logged byR. Kemp Page

Beorlng180'

D.aortuf. 1+OOE Dip -90Elevation

Length

Surface


Dote Finished

October 13/82

October 25/82

FROM

0

4.88

ft

TO

4.88 303.22

DESCRIPTION

Casing. Mafic SedimentGarnetiferous fi. staurolite bearing with staurolite concentration in thin felsic zones/ garnet greater than staurolite, minor thinly bedded sericitic zones (staurolite areas), minor epidote bearing fractures. Bedding 25 0 to core axis @ 4.57. Bedding 12 0 to core axis @ 18.90.Mafic Sediment S Sericite SchistGarnet bearing still predominant feature with massive amounts occuring with mafic sediment units banding fi within sericite schist unit. 30.57 - 32.52 - serecite schist 32.52 - 32.74 - mafic sediment - garnets 32.74 - 33.68 - sericite schists. 33.68 - 33.89 - mafic sediment, garnets 33.89 - 36.82 - sericite schist 36.82 - 39.32 - mafic sediment, garnets 39.32 - 40.40 - a little felsic in nature - bleachin

apparent falling out of garnet @ 39.32. Bedding 20 0 to core axis @ 26.52. 40.40 - 41.39 - felsic zone, seritic to silicified 40.40 - 48.74 - mafic sediment, garnets 48.74 - 49.90 - bleached zone with small white

lapilli (feldspar phenocrysts) 49.90 - 51.94 - bleached zone, increase in pheno

crysts with interstitial CO, 51.94 - 52.55 - quartz vein with occasional pyrite

blebs

SAMPLE

NO.

J

WIDTH

-

ASSAY VALUES

Au.

Drill HoleGG-9

Drilled by Logged by R. Kemp Pogt

Latitude. Bearing Elevation Date Started

Departure Dip Length Date Finished

FROM

9

TO DESCRIPTION

52.55 - 52.73 - continuance from 49.90 - 51.9452.73 - 53.31 - petering out of felspar porphyry

ie. white feldspar phenocrysts fall outafter 53.31

53.31 - 55.53 - mafic tuff55.53 - 57.49 - feldspar porphyry zone, bleached,

not distinct [email protected] quartz vein

57.49 - 57.67 - mafic tuff56.67 - 58.30 - mafic sediment, massive with

interstitial C03Garnet falls out at 48.74 (from 41.39)Bedding 25 0 angle to core axis @ 55.41Bedding 25 0 angle to core axis ? 45.63

58.30 - 67.36 - mafic sediment with interstitialCOj (continuation of previous zone)62.94 - 63.00 - quartz carbonate vein

67.36 - 76.10 - felsic to intermediate sedimentlighter in color than above with lightmafic sediment fragments caught within,angular in shape, pyrite 2 \.68.15 - 68.28 - quartz carbonate veinwith very large books of biotite and verylarge euhedral crystals of pyriteMafic tuff horizon with interstitial CO,e 72.60 - 72.66, 73.15 - 73.24, 73.82-74.2274.62-74.86, 75.44-75.62.

76.10 - 76.87 - continuation of felsic to intermed iate zone

76.87 - 77.11 - mafic tuff (amphibolized)77.11 - 77.72 - ditto 76.10 - 76.8777.72 - 78.36 - ditto

SAMPLE

NO.WIDTH

ASSAY VALUES

Au.

Drill Holt GG-9 Drilled by Logged by R. Kemp POOt

Lotlludt-

Otporturt

Beorlng Eltvotlon

Dip Length

Dot* Starttd

Daft Flnlsltttf

FROM TO

^

DESCRIPTION

78.36 - 79.34 - mafic tuff (amphibolized)79.34 - 79.61 - intermediate felsic sediment,

same as previous.79.61 - 80.10 - mafic tuff amphibolized80.10 - 94.00 - mafic sediment with occasional

fragments fi interstitial quartz88.06 - 88.18 - quartz vein87.26 - 87.36 - quartz vein92.05 - quartz vein

94.15 - 111.80 - mafic sediment with interstitialCO,, intermittent quartz veins, fragmentss. small feldspar phenocrysts.

111.80 - 129.60 - mafic sediment with interstitialCO, S occasional quartz CO, vein andfragments , and small white feldsparphenocrysts to 126.10, where the unitbecomes a little lighter in color endingin well foliated mafic sediments to 129.60.40 0 @ 127.10 angle bedding to core axis.

129.60 - 147.20 - quartz sericitic intermediatesediment well foliated, minor quartzcarbonate veins4 O 0 @ 133.20 angle bedding to core axis40 0 e 144.78 angle bedding to core axis

147.20 - 158.90 - intermediate sediment ditto above40 C 8 154.53 angle bedding to core axis.

158.90 -.176.70 - interbedded mafic tuff and sericitsc.Ust, occasional quartz carbonate inject ion. Gritty in appearance.40 0 angle foliation to core axis S 163.3750" angle foliation to core axis S 174.35

SAMPLE

NO.

k

WIDTHASSAY VALUES

Au.

Drill HoleGG-9

Drilled by Logged by H. KempPag*

Latitude,

DepartureElevation —,

Length -

FROM TO

Bearing

Dip

DESCRIPTION

193.90 - continuation of above zone-ir.terbedded quartz sericite schist 6 mafic tuff with an incoming of garnet fi staurolite/ first appearance of garnet occurs within selected horizons ie. mafic sediment horizons.0 185.01 incoming of garnet within maficsediment horizons.f 193.30 incoming of staurolite s, garnetstill present.0188.52 - quartz vein.0192.05 - 192.57 - quartz veins.40" angle of bedding to core axis 0 188.06.

J194.16 - 243.38 - mafic sediments - thinly banded,weakly sericitic, schistose altered peliticsediments consisting of biotite, muscovite/actinolite i minor garnet, staurolite.Schistosity 45 0 to Core Axis.198.82 - 199.31 - fine grained amphibolitedike, schistosity 0 9* on upper contact.201.93 - minor pyrrhotite.203.21 - 203.42 - amphibolite dike plusquartz vein207.87 - 203.18 - quartz veining plus somebroken core.212.14 - 212.45 - quartz vein.217.32 - 228.90 - slightly more altered lessbanded, more granular, weakly fractured,plus scattered feldspar porphyroblaststhroughout.220.37 - 6" quartz vein.231.80 - 232.41 - quartz feldspar porphyry sill.

Dote Storted

Dot* Finished

ne-inter-

SAMPLE

NO.WIDTH ASSAY VALUES

Au.

Drill Holt GG-9Drilled by Logged by Poge

Lotltude. Scoring Elevotlon Dote Storttd

Deporture Dip Length Daft Flniihtd

FROM TO

J~

DESCRIPTION

233.17 - 237.44 - minor calcite, moregranular, scattered feldspar porphyroblasts

243,38 - 292.00 - mafic sediments f+garnet, stauro lite chloritoid porphyroblasts)Banded, porphyroblastic altered peliticsediments, schistosity SO 0 to core axis243.38 - 249.02 - 5% pink garnet porphyro blasts.254.05 - 258.47 - darker grey green, 31staurolite and more pervasive chloritoid(scattered fractures and some broken core* minor pyrite)260.3 - 267.0 - bedded pelitic grey sedi ments, only l \ small garnets, porphyroblasts267.0 - 286.51- 2-41 small garnet porphyro blasts * 1-31 staurolite. Minor chloritoid(.5 to X.5%)276.61 - 277.06 - coarse staurolite.286.51 - 292.00 - more abundant staurolite* 1-31 sillimanite, only l-2t garnet,generally lighter grey brown.283.95 - 284.07 - quartz tourmaline veinfollowed by '.6' quartz feldspart porphyry(poorly developed)

292.00 - 303.22 - mafic sediments (greenish, brownbanded) . Biotitic pelitic sediment whichhas undergone extensive fracture andschistosity controlled bleaching. Schistosity 50 0 to core axis. 211.23 - 211.47 - ragged quartz * tourmal ine vein plus minor pyrite, cuts core axisat 20".

SAMPLE

NO.WIDTH

ASSAY VALUES

Au.

Drill Hole GG-9

Lotltude.

Deporturi

Orllltd by

Beorlng ^

Dtp ————

Logged by

Elevation .—

Length -—--

Pogt

Dote Started

Dote Finished

FROM

303.2

304.5

9

TO

304.5

473.96

DESCRIPTION

Quartz Feldspar PorphyryLight grey, weakly fractured, quite massive anduniform.

Mafic SedimentsSame as 292.0 - 303.22.306.45 - 1 cm. band of magnetic pyrrhotite.335.68 - 335.83 - quartz tourmaline amphibole

veining.340.77 - 341.44 - four narrow quartz veins plus

minor pyrite.342.53 - scattered magnetite crystals over 2 cm.

346.86-349.0 - pinkish altered calcitic brecciasections, magnetite near 346.86.

361.34 - 361.95 - epidote altered breccia.363.32 - 364.85 - minor magnetite, schistosity 60 0364.85 - 368.05 - pink - red * green altered

breccia plus quartz veining along lowercontact.

368.20 - 370.03 - scattered magnetite.

375.51 - 384.35 - mafic sediment- grey to grey-green, more massive, muchless altered and banded. Scattered quartzveins, and pyrite.381.00 - 381.91 - 21 banded pyrite.382.46 - 7 cm. quartz vein * epidote onwalls

384.35 - 444.70 - mafic sediments (green fi brownbanded)

SAMPLE

NO.WIDTH

ASSAY VALUES

Au. j

Drill Holt

Lotltude. Bearing Elevation Date Started


FROM

0

TO DESCRIPTION

Bleached brown biotite rich sediments with interbedded amphibole (calc-silicate?) plus calcite beds generally less than 4 cm. 391.67 - 396.94 - amphibole rich - 20-3(H overall with some semi-massive sections Calcite is pervasive. 417.27 - biotite rich beds are less bleached. 422.64 - 433.12 - scattered white silêous beds. 422.94 - 423.61 - vague dark grey quartz feldspar porphyry 428.24 - 428.85 - vaguely porphyritic (porphyroblastic?) 442.26 - 444.09 - quartz feldspar porphyry - rather vague, massive, dark grey.

444.70 - 473.96 - mafic sedimentsGrey brown, weakly banded to 459.64, pelitic sedi ments containing 1-51 sillimanite, 30% biotite, minor sericite and scattered staurolite bands.

Schistosity 60 0 -65 0 . From 4 59. 64 thinly banded more very fine staurolite, very little sillimanite. 469.21 - 470.15 - epidote altered mafic sill, vaguely porphyritic. 471.53 - 473.96 - somewhat more bleached, weakly sericitic. 473.02 - 473.20 - dark grey pseudo porphyry

SAMPLE

NO.WIDTH

ASSAY VALUES

Au.

Drill H olt,

Lotlfudt-~

GG-9 6DfllUd by Loggtd by Pogt

Scoring Elevotlon

Dtporturt Dip Length

Dott Storttd

Doff Flnlthtd

FROM

473. 9(

477.62

TO

477.61

483.81

*~

DESCRIPTION

Sericitic Siliceous TuffGrey sericite altered pyritic tuff, moderatelybanded well foliated, becoming more siliceousdown hole.Foliation 60 0 -65 0 .474.33 - 474.67 - dark grey pseudo porphyry473.66 - 474.88 - 1-34 pyrite, weakly sericitic,minor quartz.474.88 - 476.10 - moderately -strongly sericitic

scattered quartz veinlets well foliated34 pyrite.

476.10 - 477.62 - strongly sericitic, scatteredtourmaline, quartz veinlets plus realgar,trace MoS,, stibnite.

Siliceous Sericitic TuffFine grained grey schistose realgar bearing unit.477.62 - 479.15 - 10-124 fine pyrite, minor MoS3 ,

minor realgar, weakly sericitic, minorgreen mica.

479.15 - 480.67 - 104 fine pyrite, moderatelysericitic. Minor foS, , green mica, MoS,479.33 - 479.60 - quartz plus MoS, realgarstibnite, green mica.

480.67 - 482.19 - 104 pyrite (coarse in places)granulated white quartz plus realgar,MoS,, green mica from 481.19.

482.19 - 483.81 - 154 pyrite (coarse in places)-moderate green mica frequent granulatedwhite quartz, heavy realgar in patches483.72-483.81 204 combined realgar, MoS,,*5t thnife f sphalerite?

SAMPLE NO.

49402

49403

49404

49405

49406

49407

49408

WIDTH

1.22

1.22

1.52

1.53

1.52

1.52

1.62

ASSAY VALUES

Au.OZ/T

.01

.028

.055

.116

.217

.480

.254

MqS,*

.003

.003

.045

.018

.065

.302

.430

56J?

.013

.028

.01?

.033

.395

Or/JJ HOU r!fl~9

Lofltude.

Departure

Drilled by

Storing —-

Dip -—--.

Logged by

Elcvotlon —

Length ,———

POOI

Dote Started

Dore

FROM

483.8}

486.2!

195.30

9

TO

486.25

495.30

496.73

DESCRIPTION

Quartz Sericite SchistQuite sericite rich, minor quartz eyes, wellfoliated, light grey, weakly banded schist.483.81 - 485.03 - J.% pyrite, minor MoS,485.03 - 486.25 - 1* pyrite.Siliceous Sericitic TuffGrey blue, fine grained tuff containing pyrite,MoSj , green mica and granulated white quartzsections.486.25 - 487.68 - 151 pyrite {m coarse) fair

realgar in places, minor-moderate MoS, .487.68 - 489.20 - 15-201 pyrite (10% coarse)

moderate MoS, , moderate green mica, minorgranulated quartz, minor realgar.

489.20 - 490.73 - 101 pyrite, minor MoS, , greenmica.

489.49 - 489.87 lean section, minor biotite.490.42 - 490.73 - 301 grey quartz.

490.73 - 492.25 - m pyrite, S-10% quartzveins plus granulated quartz. One smallspeck of Visible Gold @ 491.83.

492.25 - 493.78 - 101 pyrite, some fine grainedcherty bands moderate MoS, , green mica,granular quartz.

493.78 - 495.30 - 101 pyrite, fair to heavy MoS,,green mica, granular quartz, more sericiticnear 495.30.

Biotitic Tuffaceous SedimentDark grey-black, biotite, chlorite rich groundmass

SAMPLE

NO.

4940949410

49411

49412

49413

49414

49415

49416

WIDTH 109 ter

1.221.22

1.43

1.52

1.53

1.52

1.53

1.52

ASSAY VALUES

Au.Oz/T

.060

.060

.624

.560.

.346

.376

.311

.446

MoS,1

.167

.015

.513

.951

.399

.514

.822

.410

56*

043.016

.OA4

.032

.021

.018

.020

.033

Drill Hole GG-9Drilled by Logged by Fog*

Lotitudi, Bearing Elevation Oat* Started

Departure Dip Length Dote Flnishtd

FROM

496.73

498.41

501.05

TO

498.41

501.09

511.1

•l

DESCRIPTION

with occasional more felsic, cherty fragments.1-21 pyrite plus minor magnetite.495.30 - 496.73Siliceous Sericitic Tuff as at 486.16 - 495.30.Extensive granular quartz throughout, lQ-15% pyriteModerate MoS, , minor sphalerite.497.59 - 497.8 - mafic dike.496.73 - 498.41 -

Quartz Sericite SchistGrey foliated to massive quartz eye sericite richtuff sediment.498.41 - 499.87 - sericitic S-5% biotite. 21 pyrite

Trace MoS,. Mafic section from 499.57 -499.87. 2% pyrite cuts Core Axis e 30 0 .

499.87 - 501.09 - sericitic -H 51 quartz eyes..5 to U pyrite.

Quartz Sericite Schist (Silicified)Very fine grained, grey to vaguely blue-greysiliceous, weakly sericitic unit ± quartz eyes andminor pyrite.501.09 - 502.62 - silicified .51 pyrite.502.62 - 504.14 - silicified ,5i pyrite in streaks.504.14 - 505.66 - silicified .51 pyrite in streaks.505.66 - 507.19 - silicified .51 pyrite in streaks

and patches.506.43 - 506.76 - mafic dike.

507.19 - 508.19 - silicified 11 pyrite streaks.508.19 - 509.72 -401 quartz feldspar porphyry

bands. . 5% pyrite. 509.72 - 511.15 - 60% quartz feldspar porphyry

SAMPLE

NO.

49417

49418

49419

49420

49421494224942349424

4942549426

49427

WIDTH Tie ter s

1.43

1.68

1.46

1.22

1.531.521.521.53

1.01.53

1.43

ASSAY VALUES

Au.

.124

.198

.057

.042

.004

.006

.020

.024

.036

.053

.027

Mn R,

.016

.884

.077

.038

562

.013

.028

.007

bands. pyrite.

Drill HoltGG-9

Latitude,

Dtporturt

Drilled by

Bearing _

Dip ^———.

Logged by

Elevation —.

Length ———1

Root

Started

Date

FROM

511.15

520.9

9

TO

520.9

523.8

DESCRIPTION

Quartz Sericite SchistLight beige sericitic, moderately foliated, quartzeye, tourmaline bearing tuff.511.15 - 512.52 - faint green mica, darker grey

3-51 disseminated pyrite.512.52 - 513.59 - sericitic U tourmaline, 31

quartz eyes, .5 to 11 pyrite.513.59 - 514.65 - sericitic 11 tourmaline, ^

pyrite.514.65 - 516.33 - silicified, blue-grey, scattered

pyrite to \ \.516.33 - 517.86 - sericitic plus quartz eyes, 1-21

pyrite, 11 tourmaline. Coarse tourmalineplus bleached zone from 517.46 - 517.79.

517.86 - 519.38 - sericitic plus coarse quartz eyes11 pyrite.

519.38 - 520.90 - sericitic, 31 quartz eyes, 11pyrite.519.56 - 519.93 - mafic dike - 11 pyrite.

Siliceous Sericitic TuffFoliated, moderately sericitic grey containingpyrite, green mica, realgar, minor stibnite (inquartz veinlets) and granular white quartz.520.90 - 522.43 - lOi-15% rather coarse pyrite,

scattered realgar, moderate granular quartzplus 4 ' quartz vein containing green micarealgar and stibnite.

522.43 - 523.8 - 81 pyrite, trace MoS, , trace greenmica, more lean bands.

SAMPLE

NO.

49428

49429

49430

49431

49432

49433

49434

49435

49436

WIDTH

1.37

1.07

1.06

1.68

1.53

1.52

1.52

1.53

1.37

ASSAY VALUES

Au.OZ/T

.042

.004

.008

.014

.008

.012

.042

.140

.071

Drill Holt

Latitude

Diparturf

GG-9It nrilled by

. —————————————— Bearing

t D ip

i opaed by

Flcvatlan

Length

P00t -r

,- ,- DO** S tarted

Oatm Flnlih.d

FROM

523.8

9

TO

529.4

529.4

DESCRIPTION

Quartz Sericite SchistPale grey-white tourmaline, quartz eye bearing tuffscattered wisps of green mica. Tourmaline moreabundant along narrow mafic dikes.523.83 - 525.48 - l i tourmaline, 3% quartz eyes,

11 pyrite.525.48 - 527.0 - one wisp of green mica, li pyrite.527.0 - 528.52 - 3% tourmaline, trace pyrite,

minor green mica.528.52 - 529.4 - 2% tourmaline, trace pyrite.

END OF HOLE #9

SAMPLE

NO.

i

49437

4943849439

49440

WIDTH

1.65

1.521.52

0.88

ASSAY VALUES

Au.wz/T

.002

TraceTrace

Trace

Drill HOU GG-10

-f 50E

Drilled by

Lotllude

Morrisette

180'Logged by

R. Kemp Fog*

Deportur* 2 -f SON

Bearing __ -90"

Elevation 320.92 Dal* StarredOct. 21/82

Dip Length697.08 metres Dote Flnl.hed Nov - 6/62

FROM

0 4.88

0

TO

4.88 158.49

DESCRI B TION

Casing. Mafic Sediments4.88 - 24.38 - foliated, bleached along cross-cuttin

hairline fractures. Minor interbedded amphib olized carbonaceous mafic horizons. Garnet from 11.58 - 24.38. Staurolite from 18.59 - 24.38. Angle bedding to core e 20.12 - 25 e .

24.38 - 43.28 - massive, not well foliated, inter bedded, amphibolized horizons, biotitic, minor quartz carbonate veining and fractur ing. Disseminated pyrite, less than 21.

43.28 - 61.32 - garnet, staurolite, chloritoid bearing mafic sediments. Garnets in 3 43.28. Staurolite in e 53.19. Chloritoid in S 52.12 Zone is alternating mafic sediments and sericite schist, locally magnetic.

61.32 - 62.79 - amphibolized sediments, large bladed amphibole, coarse grained, dark green, interstitial carbonate.

62.79 - 74.67 - garnet, chloritoid, minor staurolite bearing sediments, very similar to 43.28 - 61.32. Angle bedding to core g 47.78 -20 0 Angle bedding to core @ 71.32 * 25*.

74.67 - 79.92 - lapilli tuff - small white feldspar lapilli, thickly bedded, light to dark alternating horizons, heavily garnetiferous and amphibolized zones from 75.80 - 76.29, 77.94 - 78.30.

79.92 - 83.30 - felsic tuff - massive, thinly laminated, thinly bedded, siliceous, carbon aceous.

SAMPLE

NO.

J

WIDTHASSAY VALUES

Au.

~',.. GG-10 Morrisette -. v~~,~ 0 ^V-- O'l" Holt nrjiud bv l fian .d hv R* KemP Poo* *

Lotltu

Deport

FROM

L58.49

fl * ———————————————— Bearing M ii Flcvatlnn , i nii

ur* . .. . .. ... Dta Length

TO

219.09

DESCRIPTION

83.30 - 91.16 - mafic sediment 83.30 - 85.83 - mafic sediments with inter bedded lapilli tuff from 85.53 - 85.83. 85.53 - 91.16 - garnet bearing maficsediments, thinly bedded with minor inter bedded lapilli tuff and amphibolized horizons. Pyrite less than 21, disseminated to bleby. Angle bedding to core e 87.48 *20 C

91.16 - 94.37 - lapilli tuff - coarse grained, lapilli*? mm. with interbedded amphibolized units from 92.63 - 92.87.

94.37 - 158.49 - biotitic mafic sediments - massive minor occurrences of lenticular shaped, cherty fragments. Minor quart*, carbonate zones. Scattered intermittently throughout are faint feldspar lapilli. Pyrite less thar 2%, bleby to disseminated. Angle bedding to core @ 219.48 * 25". Angle bedding to core 3 136.24 - 25 0 .

Felsic to Intermediate Tuffs/Sediments158.50 - 181.96 - intermediate tuffs/sediments,

very thinly bedded from 158.49 - 162.03, light grey in color, medium grained, thinly bedded hematized zones. Less than 21 pyrite, disseminated to bleby.

181.96 - 197.20 - intermediate to felsic tuffs/ sediments silicified with minor interbedded intermediate tuffs/sediments. 2% finely disseminated pyrite.

197.20 - 219.09 - biotitic, mafic fragments with disseminated pyrite. Zone ranges from a

SAMPLE

NO.WIDTH

Dot* Sto

Dot* Flfll

rt. d

•h. d

ASSAY VALUES

Au.

DHII Hole GG-10 Drilled by Morrisette Logged bv R- KemP Pag*

L otitudt.

Deporture

Beorlng

Dip ^^ Length

Started

Dor*

t FROM

219.09

t

TO

614.54

DESCRIPTION

massive silicified intermediate tuff tothinly bedded intermediate tuff, alternatingwith thinly bedded sericite schist.

181.96 - 183.18 - silicified felsic tuff, Udisseminated pyrite.

183.18 - 184.40 - silicified felsic tuff, Itdisseminated pyrite.

184.40 - 185.62 - silicified felsic tuff, 11disseminated pyrite.



188.06 - 189.28 - silicified felsic tuff, darkerzones may reflect presence of MoS, , pyrite21.

189.28 - 190.50 - silicified felsic tuff, "M ' II II It N W H

190.50 - 191.72 - silicified felsic tuff,II II II ' M H H N

191.72 - 192.94 - silicified felsic tuff, "II ' II II H II BM

192.94 - 193.85 - silicified felsic tuff,"li H II II H MM

193.85 - 198.73 - intermediate silicified tuff withdarker zones reflecting possible presenceof MoS, , pyrite 21.

Mafic Sediment219.09 - 246.79 - staurolite bearing mafic sediment.

Staurolite occurs as porphyroblasts within

SAMPLE

NO.

49036

49037

49038

49039

49040

49041

49042

49043

49044

49045

WIDTH metres

1.22

1.22

1.22

1.22

1.22

1.22

1.22

1.22

1.22

0.91

ASSAY VALUES

OZig/T.

Trace

Trace

Trace

Trace

Trace

Trace

Trace

Trace

Trace

Trace

Drm Hole GG-lo nrm.,* fr v Morrisette , n nnf1t b v R- KemP P fl fl" 4

LoMf'i

Otporf

FROM

0

di Rearing Elevation

urt Dip , Length

TO DESCRIPTION

thinly interbedded, sericite rich horizons. Staurolite comes in @ 221.89. Angle of bedding to core g 221.89 - 37 0.

246.79 - 247.77 - coarse grained, mafic amphibolite zone with minor quartz carbonate veining.

247.77 - 281.33 - staurolite and garnet bearing mafic sediments, staurolite dies out by 273.62. Zone is marked by interbedded mafic sediments and staurolite, garnet rich sericite schist. Garnets pinhead in size. Within zone are minor interbedded feldspar lapilli tuff. Angle of bedding to core axis 3 252.07 = 40 0 .

281.33 - 286.45 - mafic sediment, thinly bedded, minor sericitic schist.

286.45 - 288.04 - lapilli tuff - feldspar lapilli less than 7 cm. in size, bedded.

288.04 - 307.82 - mafic sediment 288.04 - 301.02 - mafic sediment with minorinterbedded feldspar lapilli turrs scattered randomly throughout. 301.02 - 307.82 - mafic fragmental, fragmentrange from mafic to cherty in composition with interstitial carbonate, minor feldspar lapilli tuff scattered randomly.

307.82 - 309.98 - intermediate to felsic sediments/ tuffs - minor quartz eyes exist throughout the horizon along with scattered feldspar phenocrysts.

309.98 - 321.35 - mafic sediments 309.98 - 314.06 - massive mafic sediment,no distinct beflding, minor fragments, feldspar lapilli randomly located.

SAMPLE

NO.

3

WIDTH

Dot* Sfo

Daft Flni

rt*d

ih.d

ASSAY VALUES

Au.

Drill Holt GG-10 n,|||*d bv Morrisette i 09 oed by R. Kemp Poof 5

LotMud* . Bearing , . Elevation .

D*ooMufi Din Lenofh 1

FROM

9

TO DESCRIPTION

314.06 - 321.35 - garnet bearing maficsediment with localized oieach, associated with cross-cutting hairline fracture.

321.35 - 326.44 - intermediate sediments - with minor amounts of garnet and staurolite porphyroblasts, minor epidotization, bleaching has obliterated any primary bed ding, zone is light grey-green in color due to epidotization 6 bleaching.

326.44 - 614.54 - mafic sediments 326.44 - 379.78 - staurolite, garnet,chloritoid bearing, fracturing (local) disrupts bedding. Quartz veining and feld spar porphyry -f minor amphibolized zones from 371.85 - 372.77. 379.17 - staurolite falls out. 379.78 - garnet falls out. 379.78 - 387.80 - mafic sediments inter bedded with hematized zones imparting a reddish hue to core, bleaching occurs along cross-cutting hairline fractures. Angle bedding to core axis @ 384.23 - 45 e . 387.80 - 391.12 - mafic sediment, garnetbearing, similar to above description. 391.12 - 405.20 - mafic sediment, bleachingoccurring along hairline fractures, hemat ized zones still exist with quartz carbonate filled fractures. 405.20 - 407.18 - quartz feldspar porphyry407. IS - 614.54 - the zone is marked byextensive bleaching and epidotization which occurs near and within fracture zones to

SAMPLE

NO.w i u i n

Dot* Sfa

Daft Fin!

rf. ri

*h*d

ASSAY VALUES

Au.

Drm HOI. GG-10 n,,,i.rf H. Morrisette ,^ k u R. Kemp paflf 6 ' ^;

Lflt/fu

Dtport

FROM

9

** i Bearing r , , , . . El*uotlftn . , . m

Uf* ........ .. . . Dlo Length

TO DESCRIPTION

pervasive through wide sections. Hematizatio as well occurs randomly, imparting a reddish hue. Solution breccias are quite pervasive in sections, ie. from 407,39 - 431.38, ranging in size from one inch to one foot wide (417,48 - 417.82). These zones have angular wall rock. Fragments randomly orientated within a fine grained cherty to siliceous matrix - often epidotized and associated with heavily bleach and fracture zones. Within the zones, minor unaltered biotite rich mafic sediments exist. Within the hematized, bleached, epidotized zones, up to 21 pyrite exists between 467.87 - 475.49.467.87 - 469.09 - hematized, coarse grainedwith epidote filled fracture and quartz carbonate veining, pyrite 2%, bleby to disseminated.469.09 - 470.31 - finer grained, epidotefilled fractures, zone of solution breccia, quartz carbonate veining, l \ pyrite.470.31 - 471.52 - fine grained, mafic, MoS,bearing zone "Between quartz carbonate vein ing, epidotized fractures, 1-21 pyrite.471.52 - 472.74 - fine to medium grained,quartz carbonate veining, minor hematization 21 pyrite.472.74 - 473.96 - hematized, carbonaceous,solution breccia zone with epidote, It pyrit

SAMPLE

NO.i

49441

49442

49443

49444

49445i

WIDTH •netres

1.22

1.22

1.22

1.22

1.22

Dot* Sto

Dot* Flnl

rt. d

.h. rf

ASSAY VALUES

OZ*"/!.

Trace

Trace

Trace

Trace

Trace

Drm Molt. ,. GG-10 nrmm h y Morrisette , n flflf 4 h v R. Kemp Pout 7 - ?

Lotltu

Dtport

FROM

9

At B earing Fttvntlnn

urt D ip Length

TO DESCRIPTION

473.96 - 475.49 - carbonaceous/minorepidbtized breccia zone and fractures, MOS S , 2\ pyrite.By 495.90 - bleaching, epidotization andhematlzation becomes less pronounced. Bleaching on a small scale exists near cross -cutting hairline fractures. Solution brecci @ 502.31 with associated alteration of surrounding wall rock.536.17 - 538.37 - quartz feldspar porphyry,lower portion epidotized and fractured with associated bleaching - hematization is strong towards the base. Angle bedding to core @ 529.44 - 45*.538.37 - 571.38 - biotite bearing maficsediment. 571.38 - 609.78 - interbedded mafic sedimentand cherty to siliceous felsic tuffs, wen foliated, thinly bedded with minor hematiz ation. Zone is sillimanite bearing. Angle bedding to core axis @ 575.16 - 45 0 . Pyrite less than 11, disseminated.609.78 - 614.54 - biotitic mafic sedimentwith thinly bedded, cherty units/ minor garnets with pervasive sillimanite. Pyrite less than 1.51, disseminated to bleby. Angle bedding to core axis @ 610.21 - 50 0 .

SAMPLE

NO.

49446

i

s

WIDTHmetre:

1.22

Oott Sfo

Dot* Flnl

rita

•h*d

ASSAY VALUES

OZAu./T

Trace

Drill HO,. W" nrm.* h* "0"i8ette l n^s ^ H . AW p flfl . - - * - -.^^

Lotllu

Deport

FROM

614.54

0

rt* ——————— Bearing Flcuatlnn .

uri .... Dip Length

TO

627.77

DESCRIPTION

Silicified to Sericitic Felsic Tuff614.54 - 618.13 - thinly bedded sericitic and

siliceous tuffs. Pyrite less than 6*, as dissemination, blebs and seams.609.78 - 610.51 - cherty bedded tuffs,2% pyrite. 610.51 - 611.43 - mafic biotitic sediment,minor amphiboiites, 2-31 pyrite. 611.43 - 612.34 - Ditto above.612.34 - 613.26 - mafic, amphibolized,bleached, garnets, 1* pyrite. 613.26 - 614.17 - mafic sediment i chertytuffs, minor epidotization, 2,5* pyrite. 614.17 - 615.09 - thinly bedded, maficsediment ant! cHert to 614.54. 614.54 - 615.09 - silicified minor inter bedded sericite schist. 11 pyrite.615,09 - 616.00 - thinly bedded, silicifiedto sericitic. Trace pyrite. 616.00 - 616.91 - ditto above with up to61 pyrite toward base of section - fcleny. 616.91 - 617.83 - ditto above with minormafic tuf F towards base of section,

618.13 - 626.21 - silicified/sericitic felsic tuff, heavily mineralized zone with pyrite up to lS-20% as blebs, and disseminations. MoS,

* ranges from very fine grained to massive

SAMPLE NO.

49447

49448

49449 49450

49701

49702

49703

49704

49705

WIDTHmetres

0.73

0.91

0.91 0.91

0.91

0.91

0.91

0.91

0.91

Dot* S i a

Doft Fin!

rt t ii

•h*d

ASSAY VALUES

ozAuyT.

0.16

0.002

0.020 0.10

0.004

Trace

0.002

0.008

0.002

Drill HOI. ^ A V n,M,.d h. "~——————— l MMii k w —————— P flflt v

LOflfu

Dtport

FROM

9

d. Bearing Pl.untlnn ,

ur* Dip Length ,,—

TO DESCRIPTION

blebs to individual discreet grains. Fuchsit locally very pervasive interbedded, primaril within the sericite schist zones', accompan ied by quartz eyes. Minor realgar noted. Quartzitic zones show signs of crystallizat ion as they appear coarse and granular. Visible gold noted as fir.* specks to blebs, commonly closely associntei to the more siliceous areas.618.13 - 619.81 - silicified quartz sericiteschist, dark quartz, pyrite less than It to trace. 7 specks of V.G. @ 619.32.3 specks of V.G. ^ 619.75.617.83 - 618.74 - silicified -i- sericiticschist, trace pyrite. 618.74 - 619.66 - silicified * sericiticschist, Q.5% pyrite, Visible Gold 619.66 - 620.57 - heavy pyrite, MoS, , pyrite15-201, silicified, Visible Gold. 620.57 - 621.49 - " " " "

621.49 - 622.40 - " "H u H

622.40 - 623,31 - heavy pyrite. MoS, , 10tpyrite, realgar 623.31 - 624,23 - heavy pyrite. MoS T , VisibleGold, lS-20% pyrite, silicified.

SAMPLE NO.

|

r

49706

49707

49708

49709

49710

49711

49712

WIDTH metres

0.91

0.91

0.91

0.91

0.91

0.91

0.91

Dott S i a

Dfltt Flnl

rt. d

Ih.d

ASSAY VALUESOZAu/T.

0.002

0.820

1.105

0.461

0.823

0.419

0.094

M?C

n/a

.003

.257

.344

.507

.115

.132

Drill Hole GG-10 Drilled by MorrisetteLogged by

R. Kemp Poge

Lotltude, Scoring Elevation Oatt Started

Departure Dip Length Dote Finished

FROM

627.77

t

TO

639.07

DESCRIPTION

624.23 - 625.14 - heavy pyrite, MoSa , lS-20%pyrite, silicified.625.14 - 626.06 - heavy pyrite, MoS,, VisiblGold, lS-20% pyrite, silicified.

626.06 - 627.77 - mafic tuff plus quartz feldspar porphyry (?) .626.06 - 626.67 - mafic tuff plus silicifiedintermediate to felsic zone. S-4% pyrite.626.67 - 627.77 - possible quartz feldsparporphyry, badly bleached and epidotized fractures, trace pyrite.

Mafic Fragmental- Cherty lenticular fragments to disrupted cherty beds in appearance, locally MoS,, pervasive pyrite throughout as blebs and disseminations up to 51.627.77 - 628.80 - mafic fragmental, cherty fragments

51 pyrite. 628.80 - 629.72 - ditto above description 629.72 - 630.63 - ditto above description 630.63 - 631.54 - ditto above description 631.54 - 632.46 - ditto above description 632.46 - 633.37 -633.37 - 634.29 -634.29 - 635.20 -635.20 - 636.12 -636.12 - 637.03 -637.03 - 637.95 -

SAMPLE NO.

49713

i

49714

49715

49716

49717

49718 49719 49720 49721 497224972349724497254972649727

WIDTH metres

0.91

0.91

0.61

1.10

1.04

0.91 0.91 0.91 0.91 0.910.910.910.910.910.91

ASSAY VALUES

OZAK/T.

0.207

0.124

0.135

0.060

0.098

0.048 0.004 0.016 0.018 0.0140.0040.0980.0060.0080.012

MOS3 I

.427

.719

.152

.018

.048

.015

.007

.017

.008

.007

.002

.002

.002

.003

.005

Drill 1

Lotltu

D*port

FROM

639.07

540.60

j 0), GG-JLU - .,. . . Morrisette ^. JXWMH m — :-,-.,^ 10IC . orilltd bv Logatd bv root -

di. ———————————————— Storing FUuntlon

uri Dip Length

TO

640.00

640.60

644.96

DESCRIPTION

637.95 - 639.07 - mafic fragmental, cherty fragments 5 l pyrite.

Felsic/Silicified Tuff- Cherty to silicified with tourmaline needles scattered throughout. Bluish hue imparted to core reflecting presence of MoS, . Minor quartz eyes/ minor fracture filling of epidote, spotty slivers of fuchsite, minor quartz eyes, 5% pyrite.Mafic, Massive, Biotitic bearing zone. Barren ofsulphides. Fuchsite Bearing Felsic Tuff- Cherty to siliceous zones, quartz eye bearing with cherty to siliceous fragments. Fuchsite strongly represented imparting a green color to core. MoS, present as faint bluish zones. Visible Gold notedat 642.40, Visible Gold noted at 643.58.Pyrite very pervasive ID-15%.640.60 - 641.30 - fuchsite, quartz eyes, fragments,

pyrite 51, MoS, . 641.30 - 642.21 - fuchsite, quartz eyes, fragments,

pyrite 5i, MoS,, Visible Gold. 642.21 - 643.13 - fuchsite, granular recrystallized

quartz, 10* pyrite, MoS,. 643.13 - 644.04 - fuchsite, granular recrystallized

quartz, Visible Gold, pyrite lQ-15%, MoS,. 644.04 - 644.96 -

644.04 - 644.35 - fuchsite, granular quartz,lQ-15% pyrite, MoS, .

SAMPLE

NO.

49728

49729 49730

49731

49732

49733

49734

49735

WIDTH metres1.13

0.93 0.61

0.70

0.91

0.91

0.91

0.91

Oott Sto

Don Flnl

rt a rf

.h. rf

ASSAY VALUESOZ AU7T

0.042

0.018 0.032

0.191

0.341

0.306

0.224

D. 235

MQS^

.003

.008 .003

.008

.007

.102

.128

.355

Drill M0 i, GG-10 . ... ^ ^ Morrisette R. KempM0f ——————————— Drill. d by r , loofltd bv

LoWudt ——————————————— Bearing FKwotlon

Diportur. ————————————— Dlo u.nath

FROM

644.96

647.94

648.67

TO

647.94

648.67

656.65

DESCRIPTION

644.35-644.96.- Blue Quartzitic Zones - swirledthroughout zone, pyrite 5-101 Silicified, Recyrstallized Granular Quartz- With darker siliceous zones appearing interswirled to fragmental in appearance, MoS, bearing, plus specks of Visible Gold note 3 647.94, MoS,, fine grained to granular - heavy. Pyrite S-8%.644.96 - 645.87 - dark, MoS, bearing zone plus

white siliceous recrystallized quartz (granular) S-8% pyrite.

645.87 - 646.78 - ditto above. 646.78 - 647.70 - ditto above.

Zone of Interbedded Dark, Mafic, MassiveAmphibolized Material- With a thin zone of silicified quartz sericite schist.647.94 - 648.06 - amphibolite, trace pyrite,

upper contact g 70 C , lower contact S 60 0 . 648.06 - 648.37 - silicified quartz sericite schist

8-101 pyrite, heavy MoS,. 648.37 - 648.67 - amphibolite, trace pyrite,

upper contact f? 55*, lower contact 3 55 C .647.70 - 648.61 - see above.

Silicified Quartz Sericite Schist- With heavy MoS, and ID-15% pyrite, 2 inch wide amphibolite zone from 649.22 - 649.59 with tourmal ine needles @ contact, 45* contact to core.

SAMPLE

NO.

49736

49737 49738

9739

WIDTH metres

0.91

0.91 0.91

0.91

Dot. Ste

Dot* Fin

Pogt

rt t a

12 ' - '^

i.h.d

ASSAY VALUESQZAUXT.

.255

.390

.415

.379

MOS, l

.520

.724

.409

.199

-

Drill Hole GG-10 Drilled by Morrisette Logged by R. Kemp Pogt 13

Lotltud*. Beorlng Elevation Oat* Started

Departure Dip Length Dot* Finished

FROM

656.69

9

TO

657.76

DESCRIPTION

648.61 - 649.53 - see above.649.59-656.69 - Silicified Quartz Sericite Schist

- With darker MoS, rich zones, silicified zonesrange from fine grained to recrystallized granularquartz. A marked decrease in i sulphide is notedtowards end of zone. Pyrite up to 151.649.53 - 650.44 - granular recrystallized quartz

with darker MoS, rich zones, 51 pyrite.650.44 - 651.36 - ditto above, heavy MoS,, e-7%

pyrite.651.36 - 652.27 - siliceous, less granulated,

recrystallized quartz, heavy MoS,, pyritelOt652.27 - 653.19 - ditto above, 101 pyrite.653.19 - 654.10 - ditto above, 101 pyrite.654.10 - 655.01 - siliceous, granular quartz, heavy

MoS, , 101 pyrite.655.01 - 655.93 - siliceous, quartz eye bearing

sericite schist, marked drop in 1 sulphides.S-8% pyrite.

Quartz Feldspar Porphyry (?)- Lightly sericitized at top of zone, faint feldsparphenocrysts present. No quartz eyes, no sulphides,lower contact @ 45 0 to core.655.93 - 656.84 - quartz eye bearing sericite schist

and quartz feldspar porphyry. 1-21 pyriteplus possible MoS, in quartz eye.

656.84 - 657.76 - ditto above, 11 pyrite in a thinlyinterbedded quartz eye sericite schist.

SAMPLE

NO.

49740

49741

49742

49743

497444974549746

49747

49748

49749

WIDTH metres

0.91

0.91

0.91

0.91

0.910.910.91

0.91

0.91

0.91

ASSAY VALUES

OZAU/T.

.157

.319

.159

.144

.103

.134

.140

.214

.008

.010

MoS,l

.410

.227

.212

.045

.252

.042

.082

.062

Drill Holt GG-10Drilled by

MorrisetteLogged by

R. Kemp Pag*

Latitude , Bearing Elevation Dote Started


FROM

657.76

9

TO

678.45

DESCRIPTION

Quartz Eye Bearing Quartz Sericite Schist- Well foliated with trace realgar within siliceouszone. MoSj bearing. Up to 751 massive pyrite from665.6 - 666,20. Two specks of Visible Gold notedat 666.35.657.76 - 658.67 - quartz eye sericite schist,

silicif ied, dark zones indicating MoS, ,S-8% pyrite.

658.67 - 659.59 - ditto above.659.59 - 660.50 - ditto above.660.50 - 661.42 - ditto above.661.42 - 662.33 - ditto above.662.33 - 663.24 - silicified to sericitic, quartz

eyes, 1-21 pyrite.663.24 - 664.16 - ditto above.664.16 - 665.07 - ditto above with realgar noted

within quartz vein at 664.46.665.07 - 666.20 - siliceous, minor quartz eye,

sericite schist, massive pyrite, up to 751from 665.62 - 666.20.665.07 - 665.62 - pyrite 2 Q*.

666.20 - 667.51 - silicified plus minor sericiteschist, locally heavy MoS, , two specks ofVisible Gold @ 666.35. Up to 601 localizedmassive pyrite. Pyrite disappears @ 667.51,marking the end of the sulphide rich zones.

667.51-678.45 - Quartz Eye Bearing Quartz Sericite S (,- Zone is recognized by pervasive quartz eyes withinsilicified to pristine sericite schist, locallythin slivers of fuchsite are noted. Pyrite occurs

SAMPLE

NO.

49750

4975149752497534975449755

4975649757

49758

49759

hist

WIDTH metres

0.91

0.910.910.910.910.91

0.910.91

1.13

1.31

ASSAY VALUES

OZAu/T.

0.002

0.0080.0220.0060.0080.004

0.0160.012

0.296

.324

MoS,

.222

.150

Drill Hole GG-10 Drilled by Morrisette Logged byR. Kemp Poge

15

Lotlrude. Bearing Elevation Oatt Started


FROM

678.45

9

TO

679.79

DESCRIPTION

occasionally at less than a.0%, commonly trace.Randomly interbedded throughout the zone are maficquartz feldspar porphyry sills, non to slightlymagnetic. Minor quartz veins St mafic dikes. Alter ation zones are localized as hematization t epidot ization associated with cross-cutting fractures.Tourmaline becomes a prominent constituent from679.79 - 697.08.

667.51 - 668.43 - quartz eye, quartz sericite schist668.43 - 669.34 - ditto above, plus trace pyrite,

plus trace fuchsite.669.34 - 670.13 - quartz eye, quartz sericite schist

plus mafic quartz feldspar porphyry sill.670.13 - 670.74 - mafic quartz feldspar porphyry

sill. Upper contact 3 40". Lower contact @40670.74 - 671.78 - quartz eyes, quartz sericite schis671.78 - 672.69 -672.69 - 673.61 -673.61 - 674.52 -674.52 - 675.44 -

675.31 - 675.37 - biotite rich mafic zone.675.44 - 676.35 - quartz eye sericite schist.676.35 - 677.72 -677.72 - 678.45 - hematized mafic dike, magnetic,

plus quartz feldspar porphyry.

Quartz Feldspar Porphyry Sill "A"; Feldspar- Phenocrysts less than 4 mm. in size, S-6%Phenocrysts in a chloritic green groundmass,non-magnetic.

SAMPLE

NO.

4976049761

49762

49763

:4976449765497664976749768497694977049771

49772

WIDTH metres

0.910.91

0.79

0.61

1.040.910.910.910.910.910.910.73

1.34

ASSAY VALUES

OZAu "T.

.026

.002

.008

.002

.002TraceTrace.004TraceTraceTraceTrace

Trace

MoSj,

.003

.002

.002

.002

.002

.003

.002

.002

.002

.002n/an/a

Drill Holt GG-10Drilled by

MorrisetteLogged by

R. Kemp Pog*16-

Lotltudt.

Deporture

Bearing

Dip ——

Elevation

Length —.

Datt Started

FROM

679.79

0

TO

692.08

DESCRIPTION

Quartz Eye Sericite Schist- Well foliated, tourmaline bearing plus minorepidotization and hematization.679.79 - 680.92 - tourmaline bearing quartz eye,

sericite schist, hematization to 680.53,minor quartz veins.

680.92 - 681.84 - tourmaline bearing quartz eyesericite schist.

681.84 - 682.75 - quartz eyes, tourmaline, quartzsericite schist, minor amphibolite, tracepyrite, biotite rich mafic zone 681.96 -682.23.

682.75 - 683.66 - quartz eyes, tourmaline, quartzsericite schist.

683.66 - 684.58 - siliceous quartz sericite schistplus tourmaline plus quartz eyes.

684.58 - 685.49 - siliceous quartz sericite schistplus tourmaline plus quartz eyes.

685.49 - 686.41 - ditto686.41 - 687.32 - ditto687.32 - 688.24 - ditto688.24 - 689.55 - slightly magnetic mafic quartz

feldspar porphyry from 688.94 - 689.00,within quartz eye quartz sericite schistplus tourmaline.

689.55 - 690.98 - silicified quartz sericite schistplus quartz eyes plus tourmaline plus maficquartz feldspar porphyry.

690.98 - 692.20 - quartz sericite schist plus quartzeyes, silicified, plus tourmaline.

692.20 - 693.42 - ditto

SAMPLE NO.

49773

49774

49775

49776

49777

49778

49779497804978149782

49783

49784

49785

WIDTH metres

1.13

0.91

0.91

0.91

0.91

0.91

0.910.910.911.25

1.43

1.22

1.22

ASSAY VALUES

OZAu/T.

Trace

Trace

Trace

Trace

.002

.002

.002TraceTraceTrace

Trace

Trace

Trace^

Drill Holt GG-IQ

Lotltude.

Otporturt

TO

Logged by

Elevoflon -^

Length _

DESCRIPTION

s :s' H"

END QF HOLE

R. Kemp___, Poge

Dote Stortid --

17

Dot* Finished .

"""-* W IOTH l————iSlA^VALUES N O. metresj OZftu./T |

49786 1.22 Trace

49787 0.9149788 1.52

Trace Trace

Drill Holt GG-11 Drilled by Morrisette Lnoo.d bv B. Durham Poot 1

Lotlfu H. 2 * 50N B.arlna P,.-,,™ SurfaCC

D...r.ur. 0 * 50E n, D " 90 , , nfl , h 566.32 metres

FROM

0

6.10

11.28

J

TO

6.10 11.28

56.60

DESCRIPTION

Casing. Mafic Sediments- Weakly banded, ^^derately biotitic, moderately siliceous sedimer , containing fine feldspathic grains in last I.. ". Schistosity 30 0 to Core AxisTuffaceous, Siliceous Sediments- Porphyroblastic or arkosic tuffaceous sediments. Finer grained, more massive to 13.11.13.11 - 13.41 - quartz vein. 13.41 - 32.19 - pervasive feldspathic grains or

porphyroblasts. lfl-20% overall with S-10% coarse obvious fragments of apparently varying composition, all of which appear to be quite fine grained and stretched. Minor pyrite and pyrrhotite scattered throughout.21.34 - 21.55 - chloritic, schistose,barren mafic dike. 24.35 - 24.57 - chloritic, schistose,barren mafic dike. 26.97 - 29.57 - quite calcitic, only vague,scattered feldspathic grains. 29.57 - 32.19 - interbedded coarse felds pathic material and narrow sections or biotitic sediments, only rare visible fragments.

32.19 - 35.91 - calcite rich, non-feldspathic, scattered fragments.

35.91 - 36.39 - chloritic schistose mafic dike. 36.39 - 38.40 - weakly calcitic.

SAMPLE

NO.WIDTH

Dot* Sto

Don Flnl

rt. d Oct - 28/82

.-.- Nov - 9/82ASSAY VALUES

Au.

1

Or... HOI. S0'" n,,,,.H h. MOrriSe"e , MM-k . B.Durham P flfl . 2'--V^

Lotltu

Otport

FROM

56.60

96.19

114.3

.

d* S toring E levation

ur* Din L*noth

TO

96.19

114.3

200.16

DESCRIPTION

38.40 - 43.98 - interbedded coarse feldspathic material and more biotitic material.

43.98 - 56.60 - quite calcitic, slight pink hue, scattered fragments to 31. 48.55 - 49.16 - chloritic schistose dike.

Mafic Sediments- Chlorite, biotite rich, foliated and locally folded sediments with occurring granular feldspathic sections. Some sections contain stretched fragments or broken beds. 81.17 - 82.33 - pink altered, epidote altered,

schistosity 30 0 to core axis.

Tuffaceous Siliceous Sediments- Weakly to moderately banded, fine grained, rather heterogeneous, moderately calcitic sediments with occasional narrow mafic sections and scattered tuffaceous fragments. Banding 30 C to core axis.

Sericitic Mafic Sediments- Banded to laminated, very schistose, quite uniform muscovite, biotite rich pelitic sediments. Schistosity 35" to core axis.123.75 - 124.36 - locally contorted 152.52 - 152.70 - amphibolite 160.93 - 161.54 - minor garnet and staurolite 170.14 - 170.29 - quartz feldspar porphyry (type A)

Coarse feldspar porphyroolasts (201) set in a biotitic, chloritic matrix.

SAMPLE

NO.WIDTH

Dot* Ste

Dot* FInl

rt. d

ih*d

ASSAY VALUES

Au.

Drill Holt GG-11 Drilled by

LoMudt.

Dtporturi

Scoring

Dip —--

Elevation

Length _

Started

Dote Finished

FROM

200.16

227.69

0

TO

227.69

284.07

DESCRIPTION

170.93 - 172.39 - mafic dike (amphibolitic) 174.65 - 177.15 - more siliceous - 3 cm.

Pegmatitic quartz muscovite vein on lower contact and minor pyrrhotite and tourmaline.

Mafic Sediments (Tuffaceous)- Dark green-grey chloritic biotitic schistose sediments with scattered tuffaceous fragments and feldspathic (granular) rich sections.212.29 - 212.75 - epidotized breccia zone. 212.75 - 227.69 - calcitic, more tuffaceous, some

feldspathic sections.

Mafic Sediments (Garnet, Staurolite Bearing)- Dark grey-brown to light grey (bleached), porphyroblastic pelitic sediments.227.69 - 233.02 - dark brown-grey, +5-7I coarse

garnets. 233.02 - 240.49 - bleached light grey with 2-41

staurolite where less bleached. 240.49 - 249.63 - garnet chloritoid? ( ± staurolite)

rich. 242.62 - 244.45 - some broken core (fractured

249.63 - 255.57 - only scattered fine garnets, scattered local solution breccias, only minor alteration. Minor pyrrhotite.

255.57 - 284.07 - 51 fine garnets ± staurolite (fine Heavier staurolite from 268.07 - 273.71.

SAMPLE

NO.

)

)

WIDTHASSAY VALUES

Au.

Drill Hole GG-11 Drilled bv Morrisette Logged by B. Durham Fog*

Lotltude, Bearing Elevation Oof* Started

Departure Dip Length Dot* Finished

FROM

284.07

0

TO

446.07

DESCRIPTION

Mafic Sediments (Bleached)- Pelitic, biotitic sediments in places quitebleached, both parallel to and across schistositygives the unit a banded, more siliceous appearance.Scattered sillimanite, staurolite patches.Schistosity 40* in upper section, 45 0 in lowersection.294.22 - 294.80 - mafic {biotitic, chloritic) cross

cutting dike, minor feldspar porphyroblasts,minor pyrrhotite.

295.75 - 295.99 - local solution breccia302.85 - 303.03 - weak breccia310.74 - 310.90 - quartz feldspar porphyry317.60 - 320.65 - scattered, narrow pyritic breccia

zones. Less bleached from 320.65.335.51 - -2.5 cm. quartz vein plus pyrite,

chlorite.336.07 - 336.50 - 301 quartz342.90 - 347.47 - more bleached, slightly greenish347.47 - 349.00 - blotchy alteration359.97 - 374.45 - breccia patches, weakly calcitic377.49 - 378.26 - moderately magnetic (fine magnetit360.12 - 360.43 - magnetite (cracked)381.49 - 382.77 - 2-41 banded pyrite, calcitic in

places, one hairline MoS, rich band.385.27 - 412.24 - frequent green amphibole rich

interbeds, less bleached. Schistosity 50 0to core axis.401.12 - 403.56 - scattered bleached section+1-2I pyrite.411.63 - 7 cm. quartz vein at 35 e to coreaxis.

SAMPLE

NO.

i)

S

WIDTHASSAY VALUES

Au.

rwin UAI. u(j-AA nuriisette o. uuiucuu ^ - i'i Drill Holt^ rallied by lagged by Poo* "

LOtitudt - . Bearing . Plcuatlnn

DiDorturt ... nin i * na th

FROM

446.07

447.54

482.41

TO

447.54

482.41

484.78

DESCRIPTION

413.13 - 413.77 - white quartz vein, sub-parallel to core axis.

436.93 - 437.27 - quartz vein and epidote, and minor pyrrhotite.

Quartz Feldspar Porphyry Sill- Equi-granular homogeneous sill, light green where bleached, grey where not so altered.Mafic Sediment- Fine grained, rather massive to thick laminated biotite, sillimanite rich, pelitic sediment i fine grained staurolite, garnet and scattered amphibole rich beds. Schistosity * bed - 55 0 to core axis.453.97 - 5 cm. white quartz vein. 456.80 - 457.02 - 50? white quartz vein material 458.63 - 459.24 - quartz -f pink feldspar? *

amphibolite vein. More thinly banded (bedded) from 466.65. 475.18 - 475.95 - 5t staurolite 476.40 - 478.08 - moderate epidote alteration 479.79 - 480.00 - pseudo-porphyry 480.97 - 482.41 - bleached, weakly sericitic,

11 pyrite, narrow sections of pseudo-porphyr Some epidote alteration.

Sericitic Siliceous Tuff- Fine grained, well banded, very light grey, mixed bleached sediments and sericite altered tuff. Schistosity 50 0 to core axis. 482.41 - 483.87 - 2-41 pyrite, moderately sericitic.

Minor tourmaline.

SAMPLE

NO.

49789

49790

WIDTH metre;

1.43

1.46

Dot* Ste

Doft Fin)

rt* d

ih*d

ASSAY VALUESoz/TSn'Au.

Trace

.016

MO S,

.002

.002

Drill Hole GG-11Drilled by

MorrisetteLogged by B. Durham Pagt

Latitude.

Departure

Bearing

Dip —-- Length

Storied

Dore K!

FROM

484. 7 t

489.66

*

TO

489.66

508.71

DESCRIPTION

483.87 - 484.78 - more foliated, 51 pyrite, quite

Siliceous Tuff- Very fine grained, light to medium grey, wellbanded, siliceous (cherty) tuff with occasionalcherty fragments in more pyrite rich matrix. Littleor no MoSj visible.484.78 - 486.31 - frequent lapilli, minor green mica

51- very fine pyrite, moderate sericite.486.31 - 487.53 - occasional lapilli, quite cherty,

101 very fine pyrite, minor green mica.487.53 - 488.75 - 104 very fine pyrite, moderately

sericitic, trace MoS, .488.75 - 489.66 - m pyrite, vague lapilli, quite

siliceous.Siliceous Tuff- Blue-grey to slightly greenish (due to presence ofgreen nica) , cherty to granular, siliceous tuffcontaining MoS, , realgar, green mica, minor sericiteand frequent granular white quartz sect.jns.489.66 - 491.19 - 101 blotchy and disseminated

pyrite, two coarse specks of VG e 490.09 indark quartz veinlet.

491.19 - 4S2.71 - frequent granular white quartzsections, ID-12% pyrite, some coarse moder ate sericite.491.86 - two specks VG.

492.71 - 494.08 - several dark quartz veins to 2"containing realgar, stibnite. MoS,. 10ft pyrite fsome coarse) , fair MoS,

SAMPLE

NO.

49791

49792

49793

49794

49795

49796

49797

49798

WIDTH rnptres.91

1.52

1.22

1.22

.91

1.52

1.52

1.37

ASSAY VALUESOZAu/T.

.042

.046

.034

.123

.215

.377

.582

.722

MoS,.015

.008

.007

.032

.073

.220

.544

.382

Drill Hole GG-11 Drilled by Morrisette Logged by B. Durham Pogt

Lotlfude. Bearing Elevation Daft Started


FROM

0

TO DESCRIPTION

494.08 - 495.30 - 81 pyrite, minor granular quartz,some dark stringers containing realgar,stibnite, MoS . Minor MoS, overall.

495.30 - 496.83 - lS-20% pyrite - mainly coarsergrained type. Minor to moderate MoSj ,scattered, granular quartz.

496.82 - 498.35 - ID-15% pyrite, mainly coarse grain'ed, heavy granular quartz, minor MoS,.497.80 - 498.20 - quartz feldspar porphyry,vague, weakly schistose.

498.35 - 499.87 - 5 specks VG 3 498.65, 101 pyrite.Up to .51 fine stibnite in places. MinorMoS, 499.57 - 499.87, vague quartz feldsparporphyry plus minor pyrite.

499.87 - 501.40 - 101 pyrite, patchy and disseminatecsome coarse. Some dark grey quartz richsections. Some MoS a . Two specks of VG@ 500.27.

501.40 - 502.92 - siliceous blue-grey, moderate MoS,10-121 pyrite, well banded.

502.92 - 504.20 - highly foliated, dark greenamphibolite. 20% actinolite (felty). 51pyrite. Very coarse pyrite plus one speckof VG in quartz vein at 506.36.

504.20 - 505T72 - dark grey, cherty plus granularquartz, moderate to heavy MoS,, 10t finepyrite.

505.72 - 507.19 - 51 pyrite to 506.49, much granularquartz 506.49 - 506.73, amphibolite, 5%pyrite, one speck VG at 506.67.506.73 - 507.19 - Brassy colored pyrite,heavy MoS, - sharp lower contact.

SAMPLE

NO.

49799

49800

49801

49802

49803

49804

49805

49806

49807

WIDTHW**-TYiS

1.22

1.52

1.52

1.52

1.52

1.52

1.28

1.52

1.46

ASSAY VALUESOSWT.

.513

.102

.668

.225

.594

.417

1.10

.275

.211

MoS,.527

.859

.581

.827

.339

737

.067

394

507

Drill t

Lotltu

D*port

FROM

508.71

*olt ™ " H 'illtd bv —————— ——— | a?Md b v "' ————— P oo .

fl* —————————— Rearing , , Flevatlan , , .

urt Dip Length

TO

533.70

DESCRIPTION

Quartz Sericite Schist- greyish yellow, well foliated, quartz eye, sericitic schist, more greyish to 511.61, more quartz eyes from that point. 507.19 - 508.71 - 14 pyrite, moderately schistose,

14 quartz eyes, medium grey. 508.71 - 509.93 - 54 pyrite over .5' in centre of

sample, minor MoS, . 509.93 - 511.45 - 54 quartz eyes, 14 pyrite, very

sericitic. 511.45 - 516.18 - very silicified, greyish, only

minor quartz eyes. 511.45 - 512.98 - narrow mafic dike, 24streaks ^"f pyrite. 512.98 - 514,50 - minor quartz eyes, 14pyrite. 514.50 - 516.18 - .54 pyrite, 515.51-515.78mafic dike.

516.18 - 521.51 - very sericitic, +S4 quartz eyes, 1-24 tourmaline. 516.18 - 517.55 - two mafic dikes, ,54pyrite517.55 - 510.07 - quartz feldspar porphyryfrom 517.61 - 518.07 -f 2 narrow quartz feldspar porphyrys. 519. C7 - 520.60 - .54 pyrite, two quartzfeldspar porphyrys to green mica.

520.60 - 522.12 - .5 to 14 pyrite, silicified in last 2'.

522.12 - 524.26 - as at 511.45 - 516.18 522.12 - 523.65 - 14 streaks of pyrite.523.65 - 525.17 - 1-24 pyrite streaks.

SAMPLE

NO.

49808

49809

49810

49811

49812

49813

49814

49815

19816

19817

19818 19819

WIDTHmetres

1.52

1.22

1.52

1.52

1.52

1.52

1.52

1.52

1.52

1.52

1.52 1.52

Dot* Sfo

Dote Flnl

rted

*h*d

ASSAY VALUES

OZ.AH/T.

.071

.057

.010

.018

.036

.014

.002

.016

.016

.022

.020

.014

MoS.,

n/a

n/a

Morriratte B. Durham

Lotltudt

Dtporturt

It ^'AA Or. M. H hy ""*"

Rtorlng .

i Dip

Logoed by

FlrvnUon

Length

Poo* y

pnta Started , ,

Dot* Finished

FROM

533.7

9

TO

539.65

DESCRIPTION

524.26 - 533.70 - sericitic525.17 - 526.69 - 10 cm. band of 101 pyrite@ 525.17.526.69 - 527.61 - 25 cm. section of silic eous tuff * I0i remainder l% pyrite.527.61 - 529.13 - quite sericitic -f 51quartz eyes, brown tourmaline. 529.13 - 530.05 - very sericitic 11 pyrite530.05 - 531.57" - very sericitic 11 pyrite,narrow silicified zone -t- tourmaline, 4 cm.quartz vein.531.57 - 532.79 - two quartz feldsparporphyry sills -f narrow mafic sill. 532.79 - 533.70 - very sericitic 11 dissem inated pyrite.

Siliceous Tuff- Very siliceous, cherty aphanitic to granular,weakly banded pyritic tuff (or chert) . Fine,disseminated to streaky pyrite is ubiquitous as isa very fine grained, grey submetallic mineral(stibnite?) which is too fine to identify. Minorpale green wisps of green mica occur sporadically.Schistosity 50 C - 55 0 .533.70 - 535.23 - m pyrite, trace realgar, tour

maline, some amphibole in upper 2'. 535.23 - 536.75 - very cherty, m pyrite, trace

realgar.536.75 - 538.28 - moderate amount of granular quartz

7-101 pyrite. 538.28 - 539.65 - 15* pyrite, minor tourmaline, more

sericitic in last 5' .

SAMPLE

NO.

49820

49821

49822

498234 OD O A7Ol4

49825

49826

49827

49828

49829

49830

WIDTH tetres

1.52

1.52

1.52

.911 52X . 3 f*

1.22

.91

1.52

1.52

1.52

1.37

ASSAY VALUESOZAu/T.

.016

.012

.002

.002

.006

.004

.046

.198

.023

.038

.058

Drill Holt GG-11 nailed bv Morrisette L 000 .d bv B- Durham Poot 10

Lotitu

Deport

FROM

539.65

551.54

556.32

557.88

9

d* Hearing , . , ., Elevation ,

uri Dip Length

TO

551.54

556.32

557.88

563.24

DESCRIPTION

Quartz Sericite Schist- Well foliated quartz eye, tourmaline bearing, pale yellow sericitic schist. Foliation 60 0 to Core Axis.530.65 - 541.02 - U pyrite. 541.32 - 541.72 - quartz feldspar porphyry -Type A

201 coarse porphyroblastic feldspar set in dark green-grey matrix.

547.60 - 547.66 - mafic sill. 548.94 - 551.54 - pale pink hue.Strongly Hematized Silicified Zone {of uncertainorigin) - Weakly chloritic, deep fire brick colored section This zone appears to be highly altered sericite schist. 551.69 - 551.81 - mafic dike.Mafic Quartz Feldspar Porphyry- 201 relatively small feldspar phenocrysts set in a dark grey, more biotitic groundmass. Weakly magnetic.Quartz Sericite Schist + Intsrmixed Mafic Sediments- Highly variable section of quartz eye sericite schist and more biotitic, more sedimentary material, some rather coarse fragments are present in places (vague) .557.88 - 558.09 - hematized. 558.09 - 559.31 - frequent quartz eyes. 559.31 - 560.25 - mixed sericitic and biotitic. 560.25 - 560.59 - vague mafic quartz feldspar porphy -ry

SAMPLE

NO.

49831

WIDTH

1.37

Date Sta

Date Flnl

rt. d

ih.d

ASSAY VALUES

TJ5 AU./T

.004

n.iii .j-,- OU-AA nui. j. iaeui-c o. uuiiidiu 11 '^v?; Ofl " HO", n'llltd bv iofiatd bv Poo* J"L * '

Latitude —————————————— Bearing rttvatlan nat. Started

Dioorture ———————————— Dlo L.n fl th Dot* Flniih.d

FROM

563.24

565.8

t

TO

565.80

566.32

566.32

DESCRIPTION

560.59 - 563.24 - occasional fragments, morebiotitic than above sections, .51 pyrite,schistosity 65 P to core axis.

Hematized Silicified Zone- Grey to brick red, very silicified quartz sericiteschist? Minor chlorite and quartz eyes. Trace .51pyrite.Mafic Quartz Feldspar Porphyry (Type 'A')- 20* coarse, subhedral feldspar porphyroblasts setin a much finer, dark grey groundmass of quartz(grey), biotite and feldspar.

END OF HOLE Oil

SAMPLENO.

WIDTHASS AV VALUES

Au.

t-ll

•1ll

GOLDEN SCEPTRE RESOURCES LTD.

l DIAMOND DRILLING

1982

lBomby Township Ontario

l

l

l

l

l l

l

l

l l

l

Drill Hole GS-1Drilled by Morrisette

Logged by B. Durham Peg*

POW ± Bearing180'

Elevation Surface Pfl ..

Dtporturt 90S Dip - 45 @ O Length 151 feet Oofe Finished

August 29/82

August 30/82

FROM

0

5.50

8.07

11.50

15.8

9

TO

5.50

8.07

11.50

15.8

17.47

All Assays gram/ tonnes J D ESCRIPTION

Medium Grey Porphyritic Quartz-Feldspar CrystalTuff - rather massive weakly fractured uintcontaining 202 blurred feldspar and quartz grains(pheno crysts). Minor biotite, 0.52 to 12 evenlydisseminated pyrite.Calcitic Mafic Tuff - highly schistose chloriticand calcitic mafic tuff. Calcite is pervasive to102. Scattered pyrite to .32 as disseminated grainsand along shear planes. Occasional barren whitequartz ve inlets and blebs. .1 m. very dark greynon-schistose section at 7.05 m.Medium-Grey Porphyritic Quartz-Feldspar CrystalTuff - quite massive. Occasional hairline chloriticslips. .5 to 12 disseminated fine pyrite. Minorchalcopyrite at 9.50, possible trace MoS 2 .10.6 - 10.7 - minor quartz blebs and chlorite,22 pyrite, scattered MoS 2 flakes.11.0 - hairline slip with heavy MoS 2 .11.2 - .03m. chloritic shear and pyrite (22)Biotitic Quartz-Feldspar Crystal Tuff- schistose, somewhat banded (due to biotiteconcentrations) .52 disseminated pyrite. Narrowchloritic shear at 13.43 M.Chloritic, Biotitic Meta-Sediraent- rather uniform chlorite and biotite richVery dark, grey-green weakly schistose peliticsediment. Rather evenly disseminated pyrite, .32to 12 schistosity, 60 0 to C. A.

- mgi-j.'SAMPLE

NO.

E59395940

594159425943

5944594559465947

5948 59495950595159525953

AJL ——— .

WIDTH

1.001.54

1.001.000.^9

0.920.501.001.00

1.00 1.001.001.001.000.90

ASSAY VALUES

Au.

0.340.34

0.140.210.14

0.690.620.340.21

0.14 0.210.140.210.410.14

Afi-

....

~---____

,.---••-~-..-.----

* V V. M

....----

0.69

From3.054.05

5.596.597.59

8.089,009.5010.50

11.50 12.5013.5014.5015.5016.50

To4.055.59

6.597.598.08

9.009.50

10.5011.50

12.50 13,5014.5015.5016.5017.40

Drill Hole GS-1Drilled by Morrisette B. Durham

oow±Dtc.nf.ur. A -t- 90S

Bearing

Dip

180'

-45 @

Loooed by

SurfaceFlevattnn

151 feetLength

Page

Aug. 29/82Oate Started a

Aug. 30/82Dot* Flnl.h.d

FROM

17.47

17.95

19.68

21.35

0

TO

17.95

19.68

21.35

25.37

i ————————————————————— -4U (g 151 ___________________ (46. O! m***-r**c!)All assays grams/tonne

DESCRIPTION

Silicified Chloritic Quartz Vein Zone- very siliceous, highly contorted and sheared (1stzone containing quartz, chlorite, pyrite, MoS 2 andve.Upper contact is very sharp and well defined at 35*to the core Axis, 2 specks of VG occur in thechloritic upper contact zone. Cne coarse speck ofJiC and several very fine specks occur near thelower contact associated with scattered MoS : .Note: some broken core -802? recovery.Silicified Medium and Light-Grey Quartz-FeldsparCrystal Tuff - minor biotite in medium-grey sectiom21 pyrite disseminated and streaky pyrite (morepyrite in non-biotitic sections). Scattered quartzveins (white with siliceous pyritized walls) from19.00. Occasional hairline chloritic slips.Medium-Grey Quartz-Feldspar Crystal Tuff- rather massive except possibly fragmental from20.9 - 21.2 M. .5 to 12 evenly disseminated pyriteInterbanded Medium-Grey Quartz-Feldspar CrystalTuff and Chloritic Tuffs (Dikes?)- the quartz-feldspar sections are slightly hematized. Some mafic sections are very fine grain ed and massive, while others are ârbonate

rich, and quite schistose.21.35 - 21.52 - very fine grained and massive21.52 - 21.86 - chlorite *:ich - minor carbonate

schistosity 60 0 to C. A.21,95 -21.97 - very fine grained and massive22.73 - 22.87 - carbonate-chlorite rich

SAMPLE

NO.

) 5954

5954(2nd)

5955

59565957

59585959 5960

WIDTH

1.10

1.10

1.20

0.800.85

0.651.50 1.50

ASSAY VALUES

Au.

32.02-32,8533. OS-32. 37

0.27

0.210.14

0.140.27 0.14

Ag.

22.97

-.-.

0.69

-.,.-- - ~-

---~

....

From

17.40

17.40

18.50

19.7020.50

21.3522.00 23.50

To

18.50

18.50

19.70

20.5021.35

22.0023.50 25.00

Drill Holt GS-1Drilled by Morrisette

Logged byB. Durham Pogt

l 4- OOW± Beorlng180 0

El*voflon Surface Dote Srorrtd

90S -45 151 feet

Aug. 29/62

Aug. 30/82

FROM

25.37

27.15

44.5

TO

27.15

44.5

46.02

,i

All assays grams/ tonne DESCRIPTION

23.40 - 23.72 - fine grained chloritic, lowercontact 65 023.72 - 24.42 - 1-22 pyrite24.42 - 25.37 - grey-green moderately chloritic12 pyrite.Fine Grained Quartz-Feldspar Crystal Tuff- dark grey vaguely porphyritic section.Occasional pyrite streaks -f .5 to 12 disseminatedpyrite.Medium to Dark-Grey Quartz-Feldspar Crystal Tuff- fairly massive and uniform alternating sectionsof medium and dark grey tuff.28 - 29 - occasional pyrite streaks and finer grain-sections 30.55 - 4 cm. carbonate vein 31,26 - 31.33 - fine grained and narrow quartz v*in* chlorite. 36.4 - 36.54 - white quartz vein cutting schistosity 38.71 - 39 - fine grained section bleached, silic ified, minor pyritic fractures, 12 fine disseminatedpyrite.39.6 - 39.75 - chloritic section with 22 1 mm.pyrite clots rimmed with epidote40.8 - 40.9 -

40.4 - 1" quartz vein cuts schistosity42.55 - 42.85 - 32 pyriteQuartz Eyes - Biotite Sericite Schist (Tuff)- basically the same as above but more schistose andsericitic. .52 pyrite. Schistosity 65 e

END OF HOLE H

SAMPLE

NO.

59615962

5963596459655966 59675968 5969 59705971 5972 5973

5974

WIDTH

'

1.501.50

1.501.501.501.50 1.501.50 1.50 1.501.50 1.50 1.50

1.52

JOIB ftniinva .

ASSAY VALUES

Au.

0.140.34

0.340.210.140.27 0.480.41 0.69

0.75 1.30 0.82

0.21

.,..

....

-,-.........----

v a. V M

.--.,

---~

From

25.0026.50

28.0029.5031.0032.50 34.0035.50 37.00 38.5040.00 41.50 43.00

44.50

To

26.5028.00

29.5031.0032.5034.00 35.5037.00 38.50 40.0041.50 43.00 44.50

46.02

Drill Holt GS-2Drilled by

LatitudeOOW

Bearing

Morrisette 180 0

Logged byB. Durham Pog*

:. t -- * v^tvâ

SurfaceElevation . 30/82

90S -75 @ O 200 feet Sept. 1/82

FROM

0

3.0

6.05

12.20

18.85

^

TO

3.0 6.05

12.20

18.85

23. AA

All assays grams/ tonne ' DESCRIPTION

Casing Medium-Grey Massive Weakly Silicified Quarts-FeldspaPorphyry - .3 to . 5Z pyrite (evenly disseminated)Occasional chlorite-sericite slips mineralized withpyrite.Light-Grey Silicified Quartz-Feldspar Porphyry- predominantly light grey to slightly blue-grey massive unit with some remnant less silicifiedsections which contain some pale biolite and minorchlorite.Pyrite 12 generally disseminated but with occasionalstreaks and pyrite on chlorite fractures. Finedisseminated MoS 2 is visible in some silicifiedsections. Some sericite developed in silicifiedzones.8.3 - MoS : - chalcopyrite and pyrite blebsWeak schistosity at 50-55*.10.75 - 10.85 - chlorite - carbonate shear roughlyparallel to C. A. - contains pyrite and trace MoS 2 .Light-Medium Grey Quartz-Feldspar Porphyry- as at 3.U-6.05 Biotite-chlorite patches through out - minor sericite.1A.6 - 15. A - 52 patchy chlorite, moderately silic ified, 12 pyrite, 2 small specks of VG associated with pyritic bleb containing pyrite, sericite,chlorite, MoS 2 and tourmaline.

Chlorite-Calcite Shear Zone (Mafic Tuff?)-highly sheared and foliated chlorite calcitebiotite unit Foliation averages AO 0 but varies

SAMPLE

NO.

5975

59765977 597859795980

5981

5982(1st) 5982

C2nd)5983598A

59855986

J —— 1WIDTH

3.00

1.501.50 1.501.001.00

1.50

1.00

1.00

1.001.50

1.301.70

ASSAY VALUES

Au.

0.62

0.3A0.3A 0.960.690.55

0.21

16.66-16.87 17.62-17.350.21O.A1

0 0 1 .3A0.1A

Ag.

— ~ ~ ~--.~..--

0.69

---~

....

--. -....

— — — —— — — —

From

3.00

6.007.50 9.0010.5011.50

.

12.50

1A.OO

1A.OO

15.0016.00

17.5018.80

To

6.00

7.509.00 10.5011.5012.50

1A.OO

15.00

15.00

16.0017.50i R AnJ. o . OU20.50

Drill Hole GS-2Drilled by

Bearing

Morrisette

180'Logged by

B. Durham Page

Elevation Surface Dote Storied

Departure f 90S -75 @ O 200 feet

Aug. 30/82

Sept. 1/82i fin OR

FROM

23.44

28.66

*

TO

28.66

35.9

i

All assays grams/tonne1 DESCRIPTION

from 10-70 0 . Some short sections within this unitare fine grained and by comparison are quite massiveQuartz veining occurs along the upper contact andwithin the unit from 20.7 - 21.2 m.Silicified Light-Grey Quartz-Feldspar Porphyry- well mineralized to weakly mineralized, fine grained silicified grey to blue sections, alter nating with light-grey sliliceous quartz - feldspar porphyry. Some remnants contain light brown biotite Pyrite in silicified sections - 2-3Z - in remnants.5 to 1Z.From 26.3 remnant material becomes more frequent.27.3 - 27.55 - three quartz stringers * 3-5Z pyriteminor MoS 2 , chalcopyrite28.63 - hairline MoS 2 streak and pyrite streaks(40 0 to C. A.)Medium to Dark Grey Quartz-Feldspar Porphyry- typical medium grained Quartz-Feldspar Porphyrywith more highly altered sections. These zonescontain occasional pyrite streaks and where assoc iated with quartz stringers, minor MoS 2 is alsopresent.Scattered siliceous sections occur to 32,65 m.29.8 - 30.15 - white quartz vein cut at very shallowangle * pyrite streaks, trace MoS 2 .30.15 - 31.2 - Scattered narrow siliceous zones,12 pyrite overall.32.3 - 32.7 - silicified zone centered alonga 2" white quartz vein containing trace MoS s .

mi* t* T* P c? )

SAMPLE

NO.

59875988

5989 5990 5991 5992 5993

59945995599659975998

WIDTH

1.501.50

1.50 1.00 1,00 1.00 0.70

1.001.001.500.501.30

ASSAY VALUES

AU.

0.070.62

0.89 0.41 0.34 2.06 0.75

0.55

0.620.140.41

Ag.

--.-

....

,.---,..-....

From

20.5022.00

23.50 25.00 26.00 27.00 28.00

28.7029.7030.7032.2032.70

To

22.023.50

25.00 26.00 27.00 28.00 28.70

29.7030.7032.3032.7034.00

Drill Hole GS-2

Lotltude, OOW


Storing

Logged bv B. Durham

Surface

Pogt

Elevation Date Started

Departure 90S -75 200 feet

Aug. 30/82

Sept. 1/82, ———— f rfin o*;

FROM

35.9

36.3

59.55

TO

36.3

59.55

60.96

*

All assays grams/tonne' 6 DESCRIPTION

33.23 - 33.55 - quite massive uniform fine graineddike or pelitic sediment. CT at 40 0 to C. A.Minor pyritic fractures in grey porphyry alonglower contact.Fault Zone- chlorite, epidote, calcite - fractured shearedzone.Intermediate Tuff(Poorly developed Quartz-Feldspar Porphyry)- dark grey weakly porphyritic, biotite rich(occasional chlorite rich), fine to medium grainedschistose tuff. Gradational changes from finegrained, more schistose sections to medium grainedsections of quartz-feldspar-porphyry.38.0 - 38.4 - medium grained chlorite rich section

contact at 40"39.65- 39.80 - fine grained 21 fine banded pyriteAA. 16-44. 9 - Fine grained pyritic chloritic, biotitituffaceous sediment banding 35* to core axis.Pyrite 21

Chloritic Tuff- Fine to medium grained schistose tuff with veryvague feldspar phenocrysts.

END OF HOLE t 2

TUP i-, r P B t ————————— ——

SAMPLE

NO,

59996000

^

WIDTH

0.501.50

ASSAY VALUES

Au.

0.3A0.89

-Ag ——*

— — — —

From

39.5055.90

To

AO.OO57. AO

Drill Holt Drilled by Morris P f; t-g Logged by B. Durham Pogt

Loflfu •f —— 2+OOW B* 0 , 11)fl 180 r,. u .,,^ Surface

Dtportur* .4.t9QS Din -45 0 L. nofh 150 feet

FROM

0

2.4.

9.20

10.4

16.0

-•J

TO

2.4

9.20

of

10.4

16.0

18.5

All assays grams/tonneDESCRIPTION

Casing

Medium Grey Quartz-Feldspar Porphyry-Rather indistinct weakly biotitic crystal or lapilli tuff. 0.52 disseminated pyrite 5.15-5.00 - Silicified Quartz-Feldspar Porphyry (1st light grey massive 22 pyrite (disseminated) and streak minor fine disseminated MoS 2 . (2nd

8.0-8.1 - Scattered coarse MoS 2 plus chalcopyrite plus pyrite in silicified zone and quartz veins. 8.77-8.90 - coarse MoS. flakes and pyrite in silicified zone along 2CM quartz vein.

Chlorite-calcite mafic tuffSchistose calcite altered dark green weakly pyritic tuff pyrite 52 schistosity 45*

Light grey silicified Quartz-Feldspar PorphyryScattered pale blue more silicified sections throughout minor pale biotite in less silicified sections. Pyrite 1-22 (very fine) disseminated and occasional streaks 11.4- hairline MoS 2 streak 12.5- hairline MoS, streak 13.9-15.4 - well silicified bluish grey 22 fine pyrite heavy pyrite MoS 2 15. 1-15. 6

Medium Grey Quartz-Feldspar PorphyryQuite massive, moderately biotitic with weakly silicified sections

SAMPLE

NO.

E5652 5653 5654

) 56553) 5655

5656 5657

5658 5659 5660 5661

E5845 /5662

WIDTH

0.501.00 1.05 1.51

1.51

1.24 1.00

1.00 1.50 1.50 1.00

1.10 1.00

Dot* S t a

Dor* Fin

r( .rf Sept. 2, 198

,h.d Sept. 2, 198;

ASSAY VALUES

Au.

0.750,21 0.14 15.63 15.57 13.99 13.78

0.34 0.07

0.41 0.27 0.21 0.27

0.34 1.65

Ag. From

- J J

- J J

5.10 5.60 6.60

7.65

9.16 10.40

11.40 12.40 13.90 15.40

16.40 17.50

To

5 SO

7.' 65

9.16

10.40 11.40

12.40 13.90 15.40 16.40

17.50 18.50

Drill HOlt GS-3

2+OOW

. 4+90S

Bearing ., ,. . m

m. -45*

180

Logged by B. Durham

Eievo.ion Surface

L , flnth 150 feet

Pooe

n... a,,,.., Sept.2. 1982

D.t. FI*I.Md SeP*- 2 ' 1982

FROM

18.5

24.5

26.27

27.10

^^w

TO

24.5

26.27

27.10

27.78

————————— —— ————————— - —— - — . — , . — . — — —— i M -i .

olseRnnfoN

Well silicified, mineralized Felsic TuffNon porphyritic vaguely fragmental, very siliceous very light grey tuffaceous unit. Wisps of palebiotite appear to rim relict fragments. Some sections are quite biotitic. Pyrite (*MoS 2 ) are concentrated in irregular wisps and bands in the mor siliceous sections.

18.5-19.5 - Well silicified bleached scattered Quartveins 42 pyrite and fair MoS 219.5-21.0 - Well silicified bleached sections (502)32 pyrite fair MoS 2 ,21.0-22.7 - Weakly mineralized chloritic and biotite12 pyrite22.7-23.7 - Well silicified bleached 52 pyrite heavyMoS j in places23.7-24.7 - Well silicified bleached 32 pyrite minorMoS 2 .

Moderately Chloritic TuffWeakly silicifed grey green tuff .5 to 12 pyrite (Is

Well silicified dark grey tuffWell mineralized to 26.7 - 3 to 42 pyrite (2nd)

Mafic DykeFine grained 10cm sections on both contacts centralpart is medium grained, weakly schistose and is insharp contact with finer grained sections (Mayactually be tuffaceous sediments).

IS IT1K.T

SAMPLE

NO.

5663

5664

5665 e 5666 56675668

r

5669:)5670

5670

5671

,i r.rtj — .

WIDTH

1.00

1.50

1.00 0.70 1.001.00

1.500.90

0.90

0.80

ASSAY VALUES

Au.

2.132.192.812.67 0.07 0.21 0.550.82

0.074 Qf\

. OU

4.73

4.804.59

0.07

AG.

-

.

-

-

-

j

}

1

—

From

18.50

19.50

21.00 22.00 22.7023.70

24.70

26.20

27.10

To

19.50

21.00

22.00 22.70 23.7024.70

26.20

27.10

27.90

Drm Hole GS-3

Lotlludt. 2+QQW

Drilled by Morisette

Beorlng 180---——

Logged bv B- Durham p oa .

Surface

4+90S -45 150 feet

Dot. st,,,.d Sept.2, 1982

. 2, 1982

FROM

27.78

30.45

30.90

38.7

39.33

39.82

TO

30.45

30.90

38.70

39.33

39.82

43.8


Felsic to Intermediate TuffQuite variable section of moderately siliceous tomoderately chloritic tuff -52 pyrite overall

27.95-28.15 - silicified zone 2 1 pyrite * 1" of 302pyrite at 28.1.30.15-30.45 - Interbanded silicified and chloriticmaterial 3-42 pyrite plus fair MoS 2 plus chalcopyrit

Fine Grained Mafic Tuffweakly schistose rather uniform unit containingminor epidote and up to 12 pyrite.

Intermediate TuffRather massive medium grained dark grey tuff -vaguelyporphyritic in some sections. 0.2 to 52 disseminatedpyrite33.15-33.30 - silicified minor pyrite streaks.Well preserved fragments to 2cm from 38.5-38.7

Chloritic Mafic TuffBanded dark green schistose tuff i containing 1-22pyrite.

Silicified Felsic Tuff1-2Z pyrite fine grained sections are blue grey dueto fine MoS 2

Intermediate Tuff- dark grey, fine to medium grained lapilli tuffwith a coarser well preserved tuff section from40.20 - 40.50 m.

SAMPLE

NO.

56725673 5674

j t

5675

5676

5677

5678

WIDTH

0.501.15 0.90

1.50

0.50

1.12

O f. Q . DO

ASSAY VALUES

Au.

0.550.07 0.89

0.27

0.07

2,332.40

0.69

Ag.

-

—

—

-

-

~

From

27.9028.40 29.55

30.45

33.00

38.80

OQ O Oj y . ot.

To

28.4029.55 30.45

31.95

33.50

39.82

40 S*f W . J

..-- '.-'- ' " ; ' Drill Holt Orlllid by Morrisetee Lo 9 fl.d by B. Durham Pog*

i O.....H. 2 * POW

t 90SBearing

180 0Eltvatlon Surface Dot* Sfarttd

150 feet

Sept. 2/82

Sept. 2/82

FROM

43.8

9

tt* 7 5 mAtrefii

TO

45.72

All assays erams /tonneDESCRIPTION

Fine biotite and minor silicification gives theunit its dark grey color.Intermediate Tuff(FG)- finer grained than previous section but other wise very similar. .5Z disseminated pyrite.

END OF HOLE #3

SAMPLE

NO.

E5679

WIDTH

1.92

ASSAY VALUES

Au.

0.07

Ag.

. ---

From

A3. 80

To

45.72

M ft

D'lll Hole GS-A

l nil...rt. 2 W

Drilled by

Bearing

Morrisette

180'bv B- Durham Pag*

ElevationSurface Dot* Stort*d Sept. 2/82

Dtportur. Dip-45 * (76.2 metresl Dot* Sept. 3/82

FROM

0

3.66

18. A18.58

19.1

21,32

9

TO

3.66

18. A

18.5819.1

21.32

34.0

DESCRIPTION

Casing,

Light to Medium Grey Quartz-Feldspar Porphyry- rather massive to weakly sheared, weakly biotitic, quartz- feldspar porphyry with scattered narrow, fine grained silicified sections. .52 disseminatedpyrite overall..5 era. pyritic fracture at 9.25.15.5 - 15.7 - blue-grey massive * pyrite, chalcopy rite, sphalerite fracture.17 - 17.2 - narrow chlorite shear at 20 0 to CoreAxis.Chlorite Calcite Altered Mafic TuffSilicified Medium Grey Quartz-Feldspar Porphyry- ,5Z fine disseminated pyriteChlorite-Calcite Altered Mafic Tuff- typically sheared, foliated and comprised essentially of chlorite and calcite. .52 to lidisseminated pyrite. Two narrow fine grainedmassive sections contain 2 1 pyrite.Silicified Light Grey-Blue Quarts Feldspar Porphyry- quite massive, rather uniform weakly fracturedgrey to grey-blue quartz feldspar porphyry * minor remnants of less altered quartz feldspar porphyry.21.32 - 22.5 - minor MoS,, 2 1 pyrite, occasional (Isstreaks

SAMPLE

NO.

5680

56815682 5683 5684 5685

5686

5687 5688

CtQQjooy56905691 5692:)5693

WIDTH

0.70

1.501.50 1.50 1.50 l.AO

0.70

l.AO 1.00

1.001.501.00 1.001.30

ASSAY VALUES

Au.

2.95-2.810.690.75 0.55 O.A1 0.07

Trace

Trace 0.07

0 3AW * *JH

0.1A0.21 0.073.70

-3.57

AS-

....

....*" ™ * —

....

From

A. 30

7.5012.50 1A.OO 15.50 17.00

18. AO

19.10 20.50

21.5022.502A.OO 25.0026.00

To

5.00

9.001A.OC 15. 5C 17. 0( 18. A(

19. K

20.51 21.51

22.5!24.025.0' 26.027.3

Drill HOll GS-4

Latitude.2 W

Drilled by

Btorlng

Morrisette 180 0

Logged byB. Durham Pag*

EKvotlon Surface

P.portur. 4 -l- 90S Dip -45 Length 3,50 feet Date Flnlthed

FROM

34.0

*

TO

43.85

L

DESCRIPTION

22.5 - 24 - Minor MoS 2 , 2Z pyrite occasional (2nd)streaks - some fine grained material.24 - 25 - trace MoS 2 , occasional pyrite streaks,pyrite 1-2Z.25 - 26 - scattered pyrite streaks, pyrite 3Z26-27-3 scattered biotitic remnants, 1Z pyrite27.3 - 28.5 - well mineralized and fine grainedsections - very siliceous - pyrite 3Z, frequentstreaks, minor MoS 2 and chalcopyrite.28.5 - 30 - well mineralized 3Z pyrite - frequentstreaks30 - 31.2 - weakly biotitic - 1Z disseminated pyrite31.2 - 32.4 - mixed silicified and biotitic

.5Z to 1Z pyrite32.4 - 33.4 - mixed silicified and biotitic

1Z pyrite - chalcopyrite * MoS 2 fractureat 33.35.

33.4 - 34.0 - grey biotitic quartz-feldspar porphyry.5Z pyrite

Felsic Tuff- schistose possibly fragmental unit with occasional well silicified and mineralized sections as noted. This unit contains wisps and plates of bio

.te(light colored) and chlorite where less silicif ied (or siliceous)

34 - 34.9 - weakly silicified .5Z pyrite 34.9 - 36.4 - moderately silicified .5Z pyrite

SAMPLE

NO.

5693

5694

56945695

5695

56965697

5697

5698

5699 5700 5846

' 5847 584858495850 5851

WIDTH

1.30

1.20

1.201.50

1.50

1.201.20

1.20

1.00

1.50 1.50 1.00 1.00 1.301.400.50 1.40

ASSAY VALUES

Au.

4.46-4.598.16 -7.688.30

83.66-85.7286.01-84.691.374.59-4.664.66-4,940.96

0.07 0.07 0.82 0.75 0.410.070.07 0.21

-Ag—

— — — —

-......~

.,....

... .

...-

,..--

....

~ — — ~

——

From

26.00

27.30

27.3028.50

28.50

30.0031.20

31.20

32.40

33.40 34.90 36.40 37.40 38.4039.7041.10 41.60

To

27.30

28.50

28.5030.00

30.00

31.2032.40

32.40

33.40

34.90 36.40 37.40 38.40 39.7041.1041.60 43.00

Drill Holt

2 W

GS-A

t o. it,.*.

Driiitd by Morrisette

Btorlng 1 8QO.——1-———

O.portu,. 90S m. "45

Loaacd by B. Durham

Surface

, ...n. A50 feet

POQt 3 ,

n... s,.,,.., S ep c - 2/82n... n.,.., S eP'- 3/ 82

FROM

A3. 85

58.5

59.0

9

TO

5;.. 5

59.0

60.35

DESCRIPTION

36.4 - 37. A - 2-10 cm. sections of heavy MoS 2 -fminor pyrite. Pyrite 1-2Z.37. A - 38. A - well silicified, 10Z pyrite in first20 cm. * fair MoS 2 .38. A - 39.7 - more chloritic, Acm. quartz vein at

39. A t 1 cm. quartz vein at 39.739.7 - 41.1 - chloritic felsic tuff

AO - A 1.27 fine grained chloritic tuff ordike - rather massive

A 1.1 - 41.6 - very siliceous fine grained pyritictuff * minor MoS : . Pyrite 5Z.

41.6 - 43 - moderate chloritic felsic tuff42.32 - 42.77 - schistose uniform mafic tuffschistosity 45 0 to Core Axis.

43 - 43.85 - scattered very silicified tuff * heavypyrite * minor MoS,. 3-5Z pyrite overall - mainly in silicified sections.

Vaguely Porphvritic - Medium Grey Felsic toIntermediate Tuff- more massive44.93 - 45.37 - chloritic schistose mafic tuff46.2 - 46.7 - 2Z streaky pyrite * minor sericitic -

fractures53.25 - 54.25 - well silicified * 3Z pyrite streaksChloritic Schistose Mafic Tuff-moderately chloritic fine grained.Dark Grey Tuffaceous Sediment- scattered felsic fragments in fine grained vaguelybedded sediment. Schistosity 50".

SAMPLE

NO.

5852

585358545855

5856

WIDTH

0.85

1.651.251.00

0.50

ASSAY VALUES

Au.

0.75

0.21O.A10.55

0.27

Ag.

M M W W

-.~----~-- . -

.......

From

43.00

A3. 85A5.5053.25

63.20

To

A3. 85

A5.50A6.755A.25

63.70

Drill HOU Drilltd by Morrisette Logged by B. Durham Pogt

*w iou aurrace q t 2; 821 etltud. Bearing Fl.untlnn flat. Start . d oeH u ' */"*.

D . BO ,,u,. A * 90S mn -A5 , M, ffc 450 feet n... p,.,.-., Sept. 3/82f76 2 m

r n wlw

60.35

65.15

72.8

e)

TO

65.15

72.8

76.2

76.2

U C9 w*t 1 1* 1 lUn

Vaguely Porphyritic Intermediate Tuff- very narrow silicified sections in weakly porphy ritic dark grey, biotitic quartz feldspar porphyry.63. A 3 - 1 cm. band of 50Z pyrite

Intermediate Tuff- dark grey moderately biotitic, fine to mediumgrained ground mass with scattered lapilli sizedmaterial which is often difficult to discern.Schistosity 50 068. 7A - 69.28 - mafic-chloritic tuff or dike -

contacts appear finer grained - contactsat A0 e (parallel to schistosity)

Less obvious tuff fragments and generally finergrained from 69.80.

Fine Grained Tuff? (or Dike)- fractured ground-broken core- quite massive and fine grained. May be a finegrained mafic tuff.

END OF HOLE /A

etres)SAMPLE

NO.w i v i n

ASSAY VALUES

Au. Ag. From To

Drill Holt GS-5

Lotltudt

Morrisette B. Durham

3 * 0 0 W

. 4 t 90S

Beorlng

D'P .

180 0

-45 @ 0

P ,. uo , lnn Surface

^50 feetLength

Dot* S

Dote F

Poge

Sept. 4/82

Dan Flnlihtd Sept. 4/82

FROM

0

2.4

8.6

12.6

23.46

^^W

TO

2.48.6

12.6

23.46

34.0

All assays grarts/tonneDESCRIPTION

Casing.Medium to Dark Grey Quartz-Feldspar Porphyry- only weakly silicified

Chlorite - Calcite Altered Mafic Tuff- schistosity 60"Medium to Light Grey Moderately Silicified QuartzPorphyry- generally quite massive but with occasionally more biotitic sections and finer grained sections15.34 - 15.38 - chlorite calcite shear * MoS 2 ,

pyrite, chalcopyrite and 5 specks of Visible Gold,

15.53 - 15.65 - fine grained dark grey dike-contacts at 65" .

15.13 - 16.22 - fine grained dark grey dike-contacts at 65-70"

18.9 - 5 cm. x 2.5 cm. fine pyrite lensFelsic Tuff- siliceous pale grey fine grained felsic material with varying amounts of pale biotite.23.70 - 23.90 - fine beige cherty fragments 25.15 - 25.52 - well silicified * quartz veins

MoSj, 3Z pyrite26.55 - 26.75 - well silicified * quartz veins

MoS 2 , 4Z pyrite.31.84 - 32.15 - mafic tuff chlorite rich, minor

calcite, finer grained along lower contact32.55 - 33.10 - mafic dike or tuff - fine grained

along contacts - contacts at 60*

SAMPLE

NO.

58575858

585958605861 586258635864

5865

58665867 5868

5869

58705871

587258735874

WIDTH

1.000.50

1.001.501.00 1.001.501.50

1.00

1.000.70 0.80

0.50

1.501.50

1.501.501.00

ASSAY VALUES

Au.

0.48113.83-116.5 1.10Trace0.07 Trace0.071.23

0.69

0.690.82 0.55

2.88-2.810.750.82

0.750.480.48

Ag.

— — — —

—— -~-~-

~ — ~ ™

,---....

..-~

-~--

.--~

--.--....

....

..-.— — — —

From

14.0015.00

15.5016.5018.00 19.0020.0021.50

23.00

24.0025.00 25.70

26.50

27.0028.50

30.0031.5033.00

To

15.0015.50

16.5018.0019.00 20.0021.5023.00

24.00

25.0025.70 26.50

27.00

28.5030.00

31.5033.0034.00

Drill Holt GS-5Drilled by Morrisette

Logged byB. Durham Page

POW Scoring

90S

ISO

-45 gElevation Surface Date Started

150 feet

Sept. 4/82

Sept. 4/82f45.72 metres)

FROM

34.0

38.1

m

TO

38.1

45.72

45.72


Chloritic Tuffaceous Sediment- scattered felsic fragments 10-20Z in fine grained schistose chlorite rich ground mass.Dark Grey Quartz-Feldspar Porphyry- rather vague dark grey massive to weakly schistose oorphyry (tuff) plus occasional more chi jitic tuff sections. Weakly silicified and mineralized zones at 38.30 - 38 40 32 pyrite streaks. 41 - 41.14 - 2 1 pyrite streaks 42. A - 42.7 - quartz veins 1-2Z disseminated pyrite

END OF HOLE #5

SAMPLE

NO.

5875 5876 5877

WIDTH

0.50 0.50 0.50

ASSAY VALUES

Au.

Trace Trace 10.42 -9.81

Ae, From

38.10 41.00 42.30

To

38.60 41.50 42.80

Orin HOU wo ftrin.d bv ™rrisecce , ftflfl . d h v a. uurnam P ofl( j. :,;

Lotlfu

Diport

FROM

0

3.04

21.22

21.50

29.60

d. 3 * OOW B. 0fin9 180 0 F l .v 0 i lflft Surface

ur. A * 90S mo -75 ,. Mtll 250' (76.2m)

TO

3.04

21.22

21.50

29.60

33.0

All assays grans/ tonne DESCRIPTION

Casing

Medium Grey Quartz Feldspar Porphyry- typical medium to dark grey rather uniform tuff with scattered, very narrow silicified zones as noted. Schistosity weak @ 40 0 . 5.66 - 5.82 - weakly silicified, minor pyrite *MoS 2 . 7.20 - 6 cm. quartz veins * pyrite * trace MoS 2 . 8.14 - 8.25 - silicified heavy MoS. -f quartz,

calcite, chalcopyrite, pyrite, 1 small speck of Visible Gold.

15.1 - 16.6 - lighter grey, minor sericitic fracture .5 to 12 pyrite.

18.1 - 19.1 - heavy MoS 2 (streaks * sericite, pyrite quartz veins) From 18.20 - 18.45 weakly silicified throughout.

Chlorite Calcite Altered Mafic Tuff- typical highly foliated sheared unit. .52 pyrite.

Medium Grey Quartz Feldspar Porphyry- as at 3.04 - 21.22 Medium to dark grey, weakly schistose quartz feldspar porphyry with occasional weakly silicified zones. 24.65 - 24.98 - fine grained - mafic.Felsic Lapilli Tuff- rather sharp contact to highly altered, foliated felsic lapilli tuff with lapilli up to 5 cm.

SAMPLE

NO.

E5890 5891 5892 5893 •5894

• 5894

5895 s5896 5897 5898 5899

5900••9001 9002

9003 9004

WIDTH

1.06 1.50 1.40 1.00 0.90

0.90

1.10 1.50 1.50 1.00 1.50

1.301.50 1.30

1.50 1.20

Dot* S I a

Dot* Flnl

, f-- Sept. 4/82

, h .d Sept. 5/82

ASSAY VALUES

Au.

Trace Trace 0.34 0.48 5.90

-6,03 5.49

-5.69 0.27 1.10 0.07 0.27 0.07

0.410.07 0.21

0.27 0.41

Ag. From

3.04 4.10 5.60 7.00 8.00

8.00

8.90 15.10 16.60 18.10 19.10

20.6027.50 29.00

30.30 31.80

To

4.10 5.60 7.00 8.00 8.90

8.90

10.00 16.60 18.10 19.10 20.60

21.9029.00 30.30

31.80 33.00

on,, HOI, w-" n,n..d bv ™""*™ ( b v D. uurnam P flflt ^ :^

Lomud. 3 t OOW B, nrlnfl 180' r, untIftB Surface ^. fitfl ,,. rf Sept. 4/82 ^

B. DO ,, U,. 4 * 90S ftlR -75 1 Maffc 250'(76.2m) ^ tlwi.^ Sept. 5/82

FROM

33.0

41.0

42.7

47.0

W

TO

41.0

42.70

47.0

49.88

-

All assays grams/ tonne ' DESCRIPTION

Matrix material is mainly brown biotite with minorlight green chlorite (matrix 20Z) .5 to 1Z finedisseminated pyrite.Fine Grained Felsic Lapilli Tuff- light grey, fine grained to aphanitic unit withonly occasional vague lapilli visible.Alternating aphanitic and weakly chloritic(•f actinolite) sections. Moderate calcite in lesssilicified sections.Chert or Highly Silicified Ashy Tuff- aphanitic to fine grained, well mineralized unit. Light grey-white to blue-grey. Coarse pyritic fractures and blotches plus very fine, disseminatedpyrite throughout. Minor quartz veins and gashes.41 - 42 - 10-152 pyrite plus fair MoS 2 .42 - 43 - 102 pyrite plus occasional MoS, streaks

to 42.70.Mixed Felsic and Intermediate Tuffs- as at 33.0 - 41.0 but becoming more mafic downhole43.76 - 43.80 - friable shear at 50 0 .Moderately Chloritic Mafic Tuff- fine grained calcitic schistose mafic tuff.47.33 - 47.50 - mafic dike- fine grained massive49.2 - 49.4 - 102 well bedded fine pyrite (in fine

sediment?)49.4 - 49,71 - medium grained mafic tuff weakly

schistose. 50"49.71 - 49.83 - fine grained tuff altered to sericit

fuchsite, tourmaline -i- 52 pyrite, tra

SAMPLE

NO.

9005900590069007900890099010 9011 9012 9013

90149015

90269016

9017

9018j:e MoS

WIDTH

1.001.001.500.501.501.501.00 1.00 1.00 1.00

1.000.50

1.001.50

0.20

0.30

7

ASSAY VALUES

Au.

3.633.220.610.89C. 480.550.75 0.48 1.51 0.96

0.210.14

0.410.21

0.62

0.27

Ag.

....---~....-~-----~-- -.

....

....

,..-----~

....

.--.

From

33.0033.0034.0035.5036.0037.5039.00 40.00 41.00 42.00

43.0044.00

44.5045.50

49.20

49.70

To

34.0034.0035.5036.0037.5039.0040.00 41.00 42.00 43.00

44.0044.50

45.5047.00

49.40

50.00

Drill Holt GS-6

Lotltude. OOW

Drilled bvMorrisette ISO 0

Logged bv B. Durham Page


Deporturi 90SDip

-75Length 250' (76.2 m.)

** a ,*n Sept. A/82

- 5/ 82Dot, FlnUh.d

FROM

A9.88

53.0

62.71

9

TO

53.0

62.71

76.20


Intermediate Tuff- moderately calcitic intermediate to felsic (silicified) tuff, moderately chloritic throughout. Lower contact marked by broken core and 20 cm. chloritic shear.Medium Grey Massive Quartz Feldspar Porphyry- quite massive and uniform medium grained tuff (crystal-lapilli) . 53.85 - 53.95 - 52 pyrite streaks t tourmaline

and sericite on fractures56.15 - 57.30 - 2 1 pyrite, trace MoS 2 , moderately

siliceous . 57.3 - 58.6 - 12 disseminated pyrite - occasional

streaks, minor sericite, tourmaline fractures 62.17 - 62. AA - chlorite - calcite shear - fine

grained.

Intermediate Lapilli Tuff (Vaquely Porphyritic)- dark grey intermediate lapilli tuff - crystal tuf: Gradational contact from above unit - occasionalremnant lapilli visible. 67.2 - 68.5 - weakly silicified - occasional

sericite and tourmaline fractures.72.8 - 73.22 - fine grained schistose mafic dike.75.28 - 76.20 - weakly silicified, moderately

fractured, more felsic tuff.

END OF HOLE i 6

SAMPLE

NO.

9019 9020

9021

902? 90 rt.3

902A

9025

WIDTH

1.50 1.50

1.00

1.15 1.30

0.60

0.92

ASSAY VALUES

Au.

0.3A O.A8

0.07

Trace 0.27

0.3A

0.69

Ag.

-...

..-.

-...

From

50.00 51.50

53.00

56.15 57.30

67.90

75.28

To

51.50 53.00

5A.OO

57.30 58.60

68.50

76.20

on,. HO,. GS -7 n, jljed b y Morisette , flnn . rf h w B.Durham p oflt 1 ;-

Lofltu

Dtporf

FROM

0

2. A3

3.72

A. 13

7.31

13.86

rt .. A t QQW B. nrinn 180' ,UwatlM Surface

Uf. A * 90S 0 |0 - A5 , .nn.h 48.76 metres

TO

2. A3 3.72

A. 13

7.31

. 13.86

20.73

All assays grams/ tonneDESCRIPTION

Casing. Medium Grey Quartz Feldspar Porphyry- quite massive - relatively fresh - .52 fine

disseminated pyrite.Chloritic, Calcitic Mafic Tuff- sheared, foliated (55") unit comprised essential ly of chlorite, calcite and .52 pyrite.Medium Grey Quartz Feldspar Porphyry (Vague)- weakly schistose, vaguely porphyritic Quartz feldspar tuff. Lapilli (porphyroblasts) decrease to 12 downhole.Fine drained Intermediate Tuff- lig tt grey - green, fine, ashy tuff with occas onal lapilli tuff sections. Weakly schistose (65 0 vo Core Axis). Pyrite trace - .32.10.1 - 10.36 - obvious lapilli - 502 lapilli are

fine grained white-beige and only one contains significant pyrite. Pyrite overall .52. Calcitic throughout.

Felsic and Intermediate Ashy and Lapilli Tuffs(Calcitic) - largely felsic tuffs with interbedded inter mediate tuffs (as above) . Felsic tuffs are not silicified and contain considerable calcite throughout. They also contain up to 202 chlorite (and fine amphibole) as ground mass material. There are no obvious fragmental sections.

SAMPLE

NO.WIDTH

Daft Sta

Daft Flnl

Sept. 6/82rttd . . r

Sept. 6/82•had

ASSAY VALUES

Au. Ag. From To

Drill Hole GS-7Drilled by

LotltudeOOW

Bearing

Morrisette ISO 0

Logged by6. Durham Page

Elevation Surface

90S Dip -45 Length 46.76 metres

Dote Started

Date Flnlihed

Sept. 6/82

Sept. 6/82

FROM

20.72

20.80

24.87

28.90

32.5

9

TO

20.80

24.87

28.90

32.60

39.7

All assays grams/ tonneDESCRlPTlbN

15.05 - 15.20 - fine grained massive mafic dike20.25 - 20.60 - medium grained dark green mafic

dike.Chloritic Shear Zone- shearing 35" to Core Axis.Intermediate Fine Grained Tuff-light grey green ashy tuff (as at 7.31-13.86)Felsic and Intermediate Ashy and Lapilli Tuffs(Calcitic) as at 13.86 - 20.72 25.43 - coarse MoS 2 flake on fracture26 - 27 - more silicified fine grained very minor

calcite . 57. pyriteSchistosity varies but is generally 50 0 .

Fine Grained Mafic Tuff- schistose fine ashy tuff with occasional remnantlapilli sized fragments. Moderate calcite through out. Schistosity 60".Fine Grained Intermediate to Mafic Tuffs- highly mixed sections of mafic, intermediateand occasional felsic tuffs.Some obvious remnant lapilli throughout.32.76 - 32.82 - medium grained mafic dike.33.36 - 33.58 - fine grained mafic dike.34.90 - 35.20 - medium grained mafic dike.39.1 - 39.55 - fractured, silicified calcitic gashe39.5 - 39.7 - 52 pyrite, no MoS 2 - dark grey.

SAMPLE

NO.

E5878

587958805881

5882

5883d5884

WIDTH

1.00

0.501.001.50

1.40

1.00

1.75

ASSAY VALUES

Au.

0.07

Trace0.343.910 QQ-j . y o

0.69

0.89

0.48

Ag.

~ — — —

....~---

-...

-.--

""

From

20.00

22.0025.0026.00

27.50

38.70

39.70

To

21.00

22.5026.0027.50

28.90

39.70

41.45

Drill Mole Ob-/

1 ntllurf. 4 * OOW

t . o ne DtDortufft " * 7wO

^ ,,, j ^ norrisecc Driiltd by

Raring ISO 0

mn -45

Looked bv B. Durham

r,.-.,,.. Surface

LvngtK 42-''^ 'HîtirBP

POO. 3 ^

Sept. 6/82Rat. Starf.d , r

Sept. 6/82Dot* Plni.h.d , , ,

FROM

39.7

41.45

46.3

9

TO

41.45

46.3

48.76

All assays grams /tonneDESCRIPTION

Medium Grey Quartz feldspar Porphyry (Vague)

Silicified Grey Quartz Feldspar Porphyry *Silicified Felsic Tuff41.45 - 42.2 - 2 1 s treaks of pyrite.42.47 - 42.80 - fine grained mafic dike.42.65 -47.10 - 502 quartz vein * 12 pyrite,

trace MoS 2 .47.20 - 47.28 - 5-102 pyrite streaks, no MoS z .45.1 - 46.3 - 20-302 quartz veins t 2-32 pyrite,

trace MoS 2 throughout.

Dark Grey Quartz Feldspar Porphyry (Vague)- typical vague quartz feldspar porphyry becomingfiner grained towards 48.76. .3-. 52 pyrite.

END OF HOLE /7

SAMPLE

NO.

5885

5886 5887

r-5888 1-5888

."889

WIDTH

0.75

1.30 1.50

1.30 1.30

1.00

ASSAY VALUESl

Au.

0.27

0.21 0.14

3.22 3.50

0.07

Ag.

....

.--.

From

41.45

42.20 43.50

45.00 45.00

46.30

To

42.20

43.50 45.00

46.30 46.30

47.30

Drill HoltGS-8

Lotitwde, OOW

Drilled by Morrisette 180*

Logged by B. Durham

Departure 90SBearing ,——

m. -75

Elevation Surface Daft Started

Page l

Sept. 6/82

250 feet Sept. 7/82r ( If. 1 m

FROM

03.04

9.03

9.74

12.70

36.3

*

TO

3.049.03

9.74

12.70

36.3

46.6


CasingMedium Grey Quartz Feldspar Porphyry {Lapilli Tuff)-vaguely porphyritic, weakly schistose.Trace to . 5Z pyrite. Schistosity 30 e to Core Axis.Chloritic, Calcitic, Mafic Tuff- sheared, foliated at 30 0 , minor pyrite.Medium Grey Quartz Feldspar Porphyry (Vague)- weakly schistose, vaguely porphyritic lapillito crystal tuff.Fine Grained Intermediate (to Mafic) Tuffs- fine grained calcitic, schistose tuffs of intermediate composition with lesser mafic sections (occasional felsic sections). Schistosity 40 0 to Core Axis. 13 - 14 - minor quartz veins t 1Z pyrite in

biotitic tuff.14 - 15.5 - weakly silicified - calcitic 1Z pyrite15.5 - 17 - mafic and intermediate tuff 1Z pyrite22.40 - 27.5 - more felsic25.7 - 26.15 - fine grained massive mafic dike.27.06 - 27.40 - chloritic, calcitic shear.Fine to Medium Grained Felsic Lapilli Tuff- coarser material to 40.6 m. From there, this unitis correlatable with the section from 33.41 inHole GS-6.Weakly silicified but calcitic throughout.Groundmass is pale biotite t chlorite -f amphibole.

g*-r**gj - - -SAMPLE

NO.

90279028 9029 9030 9031 9032 9033

90349035 ontfiyujo9037903890399040

WIDTH

1.001.50 1.50 1,00 1.50 1.50 1.50

1.501.00 1.501.501.501.501.50

ASSAY VALUES

Au-

0.270.75 0.41 Trace Trace Trace Trace

4.088.58 0.210.270.140.270.69

From

13.0014.00 15.50 23.00 24.00 25.50 27.00

36.3037.80 38.8040.3041.8043.3044.80

To

14.0015.50 17.00 24.00 25.50 27.00 28.50

37.8038.80 40.3041.8043.3044.8046.30


Bearing 180"-..——-,——.

Logged by B. Durham Pogt

Dip "75

Elevotlon Surface

Length 25fl

Dott storted Sept. 6/82

Dote Finished Sept. 7/82

FROM

46.6

53.24

56.75

67.9

t

TO

53.24

56.75

67.9

76.2

All assays^ms^tonne

37.8 - 38.8 - 1-2Z pyrite, trace MoS 2 , weakly fractured.

From 33-41 - very fine and fine grained material alternate.Mafic Tuff- fine grained schistose chloritic tuff with occasional felsic lapilli. Pyritic section from 46.6 - 47.6 probably correlate with section from 49.2-49.8 in GS-6.49.4 - 49.6 - fine grained massive mafic dike.Rather Massive Intermediate Tuff- light grey green fractured (calcitic) tuff -f 1-2Z pyrite.Medium Grey Quartz Feldspar Porphyry (Vague)- rather uniform weakly porphyritic crystal tuffs - generally medium grey except where silicified the unit becomes fine grained. 57.50 - 57.77 - quite massive fine grained mafic

dike.58.4 - 8 cm. fine grained section, minor pyrite

streaks.63.6 - 64.9 - fine grained silicified * calcitic

and chloritic fractures. .5Z pyrite. 67.7 - 2 cm. quartz vein -f MoSj on lower contact.Intermediate Tuff- rather vague and ill-defined variable unit with minor silicified sections. ,5Z pyrite throughout.

SAMPLE

NO.

9041

j

9042

9043 9044 9045 90469047

9048

WIDTH

1.30

1.50

0,60 1.50 1.30 1.501.50

1.50

ASSAY VALUES

Au.

0.55

0.21

0.96 0.21 0.27 0.890.07

0.21

From

46.30

55.25

61.50 62.10 63.60 64.9066.40

72.00

To

47.60

56.75

62.10 63.60 64.90 66.4067.90

73.50

Drill Holt GS-8Drilled by

Lolltiid. 4 -f

Departure 90S

Bearing —

-75

Morrisette

180'Logged by B. Durham

Elevotlon ^——-.

Poge

Surface Dot. Storttd ' 6/82

250 feet-. r-..-.. . . ,-- urn .- I*n0th fcrfv """ not. Plnl.h.d lJC^ U ' 7' U ' r?fi- 7 met-yeol

FROM

76.2

9

TO

—————————————————————— . ———————————————————————— UJB-uAll assays grams/tonneDESCRIPTION

Only rare lapilli visible (68.9). Medium grey with some greenish sections. Occasional vaguely porphyritic sections.

END OF HOLE /8

SAMPLE

NO.u/inTu ASSAY VALUES

Au. From To

Drill HOlf GS-9

5 -f POW

Dtportur* 4 -f 90S

Drilled bv Morrisette

Beorlng ISO 0--—-,.—

Dip

B. DurhamLoggtd by

Elevotlon Surface

Pogt

Dot* Storttd-45' 250 feet Sept. 8/82

FROM

0

3.04

10.70

13.8

19.45

*

TO

3.0410.70

13.8

19.45

22.6

All assay grams/tonne *DESCRIPTION

Casing.Mafic Tuff- dark grey - dark green tuff with occasional fel sic lapilli - may have a fair sedimentary component.52 pyrite. Scattered patchy bleached sectionsassociated with veining and fractures.8.55 - coarse carbonate veinlet, coarse pyrite

and chlorite.Intermediate to Felsic Tuff- weakly silicified medium grey lapilli tuff cutby occasional quartz veins. Pyrite .5.10.7 - 11.6 - 20 cm. of 802 quartz 4- 12 pyrite11.6 - 12.6 - minor chalcopyrite * MoS 2 in 2 cm.

quartz veinlet .5 to l i pyrite overall.12.6 - 13.8 - less siliceous except 13.6-13.75

Quartz veins * pyrite, trace MoSj.5 to l i pyrite overall.

Fine Grained Mafic Tuff- dark grey to grey-green moderately schistosetuff .52 pyrite.13.96 - 14.29 fine grained massive mafic dike.Intermediate Lapilli Tuff- light grey-green weakly silicified intermediate tuff with some more chloritic (mafic) sections.Some fine grained narrow siliceous sections. .5 to 12 disseminated pyrite.20.20 - 20.60 - Trace MoS 2 12 pyrite.

SAMPLE

NO.

90499050 9051

9052

9053

WIDTH

0.901.00 1.20

1.10

1.50

ASSAY VALUES

Au.

0.410.27 0.21

0.07

0.07

From

10.7011.60 12.60

20.00

21.10

To

11.6012.60 13.80

;

21.10

22.60

Drill HOlt

5 * OOW Lolltud*——————..— Beorlng180

Logged by

Elevoflon Surface

250 Feet

Dot. stortid Sept. 8/82

:. 8/82

FROM

22.6

24.6

34.9

t

TO

24.6

34.90

40.84


Schistose Fine Grained Mafic Tuff- calcitic chloritic weakly pyritic (.5 to 12)greenish grey tuff. Schistosity 60 0 to Core Axis.Intermediate and Felsic Tuffs- light grey to slightly blue-grey lapilli tuff Coarser lapilli tuff to 29.30 then pale grey-green aphanitic sections alternatingwith slightly coarser material (similar to GS-836.3 - 46.6)24.4 - 25.9 - 12 very fine pyrite, fine grained

medium grey tuffaceous.25.9 - 27.3 - 12 fine pyrite.27.3 - 28.3 - fine grained - 12 pyrite chlorite

calcite shear @ 27.728.3 - 29.4 - 2 1 f ine pyrite, trace MoS,

Minor quartz veins section is medium grey.29.4 - 30.9 - darker grey interbanded fine and

very fine material .52 pyrite.30.9 - 32.4 - coarser grained in lower part (more

felsic tuff) Minor pyrite streaks 12 pyrite.32.4 - 33.9 - felsic lapilli tuff 12 pyrite.

20 cm. mafic dike (medium grained massive)@ 33.7 - 33.9 Contacts at 75".

33.9 - 34.9 - well mineralized felsic tuff-blue grey from 34.3 * heavy MoS 2 streaks,fine pyrite quartz veinlets.

Intermediate Volcanic- rather massive, fine grained, relatively uniformlight green andesite.

ruotrsSAMPLE

NO.

90549055 9056 9057

9058

9059

9060

9061

90629063

sj ——— .

WIDTH

1.501.40 1.00 1.10

1.50

1.50

1.50

1.00

0.500.20

ASSAY VALUES

Au.

0.890.210.62 0.75

0.07

0.07

0.07

3.12

0.070.07

From

24.4025.90 27.30 28.30

29.40

30.90

32.40

33.90

34.9038.40

To

25.9027.30 28.30 29.40

30.90

32.40

33.90

34,90

35.4038.60

MI HOU GS-9

POW

Dtporturt -4 -f- 90S

Drill.d bv Morrisette

Storing 180 0————-—.

PI. -AS 0__________

Logged by B. Durham Pogt

Elevotlon Surface

Length 250 feet/7fi O

Do,. Storf.d

Do,. Fl...h.d

FROM

40.84

59.1

61.6

62.3

*

TO

59.1

61.6

62.3

76.2


Mixed Tuffaceous Sediments and Tuffs- highly variable mafic and intermediate tuffs with sections which appear to be predominantlysediments. Moderately schistose throughout 60-65 0 .41.50 - 41.75 - sericitic * tourmaline -f 1Z pyrite,

trace fuchsite.46.3 - 47.3 - sericitic, fuchsite, tourmaline,

11 fine pyrite.More Uniform Intermediate Tuff (tSediments)- light greenish fine grained l i pyrite.Well Silicified Tuff- blue grey quartz veined, fractured unit ofuncertain origin (due to silicification andveining) 3 or 4 tiny specks of Visible Gold ina cluster at 61.67.Moderately Sericitic Tuff (*Sediment)- dirty lapilli tuff and interbedded slightlypelitic sediment. This unit is typically very pale

freen and brown banded. Layers occur in 2-15 cm.ands. Schistosity 75* to Core Axis.Some sections contain scattered quartz? augens to.4 cm.

END OF HOLE #9

SAMPLE

NO.

9064

9065

90669067

9068

9069

WIDTH

0.30

1.00

1.501.00

0.90

1.00

ASSAY VALUES

Au.

0.07

0.07

TraceTrace

5.63

Trace

From

41.50

46.30

59.1060.60

61.60

62.50

To

41.80

47.30

60.6061.60

62.50

63.50 .

OHM HOI. GS-10 n, m-- b tf Morrisette , n (pfl . d b v R' Kem? Poo. 1 ""^

, ..i.,,*. 5 * OOW R. fl , lnfl 180' ruunflftn Surface

Dioortur. * * 90S mo -75 f 0^ ^ v | Ma|h 250 feet

FROM

0

3.04

3.56

4.26

6.03

6.22

8.53

10.26

9

-JO C iJU W.*, my ,^ , ^^

TO

3.04 3.56

4.26

6.03

6.22

8.53

10.26

10.87


Casing. Medium Grey Quartz Feldspar Porphyry- with vague feldspar phenocrysts/wlsps and lenses of biotite provide a sense of foliation, minor and local reaction to HCL along hairline fracture and grain boundaries.Chloritic/Calcitic Mafic Tuff- with swirls and injected quartz C0 3 zones. Medium Grey Quartz Feldspar Porphyry- with vague feldspar phenocrysts/ same as 3.04 - 3.56.Chloritic/Calcitic Mafic Tuff- saale as 3.56 - 4.26 angle of contact to core axis - 158 0 (21")

Grey-Green Mafic Tuff- more massive in appearance than 6.03-6.22 with localized quartz CO, injections, wisps and swirls. .012 disseminated pyrite - slightly chloritic angle of foliation to core axis " 158 0 (21*Feldspar Porphyry Sill- with laths of biotite providing a sense or foliation. Feldspar phenocrysts less than 5 mm. in size minor to local reactions to HCL at grain boundaries. Quartz C0 5 vein @ 8.87 - 9.06; barren.Mafic Tuff- medium grey in color with small biotite laths providing a sense of foliation - hairline fracture

SAMPLE

NO.

)

^ —— 1WIDTH

Dott S t a

Oatt Fin

ft . A Sept. 9/82

.-.- SePt- 9/ 82

ASSAY VALUES

Au. From To

Drill HOU GS-lP

. ......d. 5 * POW

by Morrisette L oggtd b v R. Kemp POO*

Bearing 180 Elevation Surface Dot* Starttd

90S "0 feet

Sept. 9/82

Sept. 9/82{/b. t metres)

FROM

10.87

12.26

13.41

L8.48

TO

12.26

13.41

L8.48

22.62

All assays grams/ tonne 'DESCRIPTION

parallel to the foliation contains chlorite and C0 3 , moderately strong reaction with HCL Pyrite occurs as fine disseminations approx. .01Z pyriMafic Tuff- bleaching is evident occurring along cross cutting hairline fracture Where close to these zones bleaching of the he st rock occurs, ghost relicts of feldspar phenocrysts are sllgntly evident but obscurred due to the bleach ing effect. Mafic constituents are biotite laths providing sense of foliation. Sulphides (pyrite) tei to come close to or within the hairline fracture and bleached zone. 0.02Z pyrite.Intermediate Tuff- bleaching appears to be more pervasive with a noticeable decrease in biotite content. Sulphides associated with cross-cutting hairline fracture which is the source for the bleached zones. Pyrite 0.02Z.

Mafic Tuff- biotite content decreases from the mafic tuff with more felsic zones in evidence. Biotite laths envelope stretched lenticular fragments, which are faintly evident. Quartz C0 3 vein @ 16.14-16.33 (barren).Intermediate Tuff- light grey In color with decreasing amount of biotite with depth. Ghost relicts of lenticular fragments are present (commonly less than 4 cm. long) Quartz C0 3 injection @ 19. 82-19. 90(barre

SAMPLE

NO.

A

ds

9101

9102 9103 9104 n)

WIDTH

1.15

1.001.00 1.00

ASSAY VALUES

Au.

0.21

0.340.21 0.14

From

12.26

18.48 19.48 20.48

To

13.41

19.48 20.48 21.48

- Drm N.I. GS ' 10 B,,,,. d bv Morrisette | ofloedbv R. Kemp POO. 3

Lotlfu

Dtport

FROM

22.62

23.14

24.10

26.17

5 * OOW 180 0 . .U* Benrlng Pl.vnflnn Surface

"" 4 * 9 0S D" ~56 I ^50(76 2 m) '--"i". 250 feet^ ^ ,

TO

23.14

24.10

26.17

27.54

All assays grams 7 tonneDESCRIPTION

22.10 - 22.80 - very fine grained tuff zone with MoSj wisps and small lense of pyrite; portions of intermediate tuff (wallrock) fragments caught up within this fine grained MoS 2 bearing zone.

Pyrite content disseminated 0.10Z pyrite.

Mafic Dyke- angle of contact to core axis

upper contact: 39 0 (219 0 ) lower contact: 42 0 (221 0 )

Intermediate Tuff- same as 18.48 - 22.62 Mafic component more pervasive towards lower contact in biotite. Biotite provides a sense of foliation and tends to wrap around and outline the lenticular fragments. Sulphids 0.1Z pyrite disseminated.Massive Mafic Tuff- pristine in appearance and homogeneous in contact with small, less than 2 mm., light grey feldspar scattered throughout as ghost outlines.

Slight reaction to HCL.Intermediate Tuff- light grey in color, faintly foliated due to alignment of biotite laths, (biotite content decreasing in amount from the massive mafic tuff) . Pyrite occurs as fine disseminations 0.01Z. Angle foliation to core axis 45*.

SAMPLE

NO.

9105 9106 9107

9108

WIDTH

0.600.30 0.24

0.96

)ot* Sfa

DOT* Flnl

r ,. H Sept. 9/82

ASSAY VALUES

Au.

0.140.07 0.07

Trace-

From

21.48 22.08 22.38

23.14

To

22.08 22.38 22.62

24.10

OrlH Hole GS-10 Drilled bv Morrisette Logged by R' KemP Page

POW Bearing180'

Elevation Surface

90S -75 @ O 250 feetDC?* Storftd Sept. 9/82

•01* FI,I.I..,I Sept. 9/82Ob P /DU ( 76.2 m ) n t -) n,o4-^ e \

FROM

27.54

29.30

33.28

33.76

0

TO

29.30

33.28

33.76

36.09

All assay grams /tonneDESCRIPTION

Intermediate to Felsic Tuff- light grey in color with zones cherty in composition, these more fine grained felsic zones lack biotite, while other zones in sectionare swirled with biotite within felsic zones

fiving a fractured appearance ie. @8.34 - 28.48 - quartz C0 3 injection29.10 - 29.30 - quartz C0 3 injection

Massive Mafic Tuff- dark grey, pristine and massive in appearance.Mafic component - biotite with thinly interbeddedand localized quartz C0 3 lenses. Less than 5 mm.wide. Locally hairline quartz CO, fracturecross-cutting foliation blebs and wisps of pyriteoccur along foliation planes. Less than 0.12.Intermediate to Felsic Tuff- fine grained, light grey zones interswirledby seams of maf : cs (biotite). Wisps and lensesof quartz C0 3 cross-cut foliation. Localizedreaction with HCL. Finely disseminated grains ofpyrite. Less than 0.02Z.Intermediate Tuff- light grey in color with a slight but noticeable decrease in mafic component (biotite). Chloriteoccurs along foliation planes which appears tohave a higher concentration of pyrite, wherethese chloritic planes occur. (34 .57-34 .6. )Locally biotite will accumulate to jform thinlybedded units rich in biotite, commonly less than5 mm. thick. Locally quartz C0 3 injection occuryh-f^h nnnf-fl'fri wall rnnk material.

SAMPLE

NO.

91099110 9111

9112

9113 91149115

WIDTH

0.80 0.14 0.82

0.48

1.00 1.000.33

ASSAY VALUES

Au.

0.07 0.410.07

0.21

0.14 Trace0.21

From

27 54b 9 V J*f

28.34 28.48

33.28

33.76 ?4 . 7635.76

To

28 34^-O * J*?

28.48 29.30

33.76

34.76 35.7636.09

Drm HOU GS-10 nniied by Morrisette i ftfln .d hv R- Kemp Pooc ^ . - : "s

LOtltM

Deport

FROM

36.09

36.78

41. AA

9

fl* —— H-QQ V Bearing. , IPf) 0 Flivnllnn , SlirfaCP

urt A+sos mn -J-J @ 0 L h 2 SO feftf. n fi 2-3D e Z3u (7o,2 m) metres)

TO

36.78

A 1.4 ';

A3. 00


Small felsic brecciated appearing zone from 35. Al -35. A9 with cherty felsic fragments separated by darker biotite rich swirls. Lenticular cherty fragments occur at bottom of section.

Intermediate to Felsic Tuff-light grey in color with very fine grained chertj looking zones, with cross-cutting hairline fractures, along which pyrite accumulation occurs. These cherty zones are separated and are interswirled by biotite richer zones. HCL reaction interstitially in biotite rich zones, while cherty zones are locally reactive along hairline fracture In chert zones, fine dissemination of pyrite speckles throughout, as well as along fracture. Speck of molybdenite at 36. A7. Pyrite less than l.OZ

Massive Mafic Tuff-dark grey-black in rolcr with disseminated pyrite throughout. Description of zone is same as previous massive mafic tuff horizons. Towards the base of the section, quartz CO, veinlets and injection parallel to the schistosity come in with accumulations of pyrite.

Intermediate to Felsic Tuff- fine grained silicified tuff - with laths of biotite and chloritic injections along schistosity planes. Faint cherty fragments spotty throughout section but visible. Sulphides, pyrite, occur throughout as disseminations and tend to accumulat near to and within cross-cuttinE hairline fracture

SAMPLE

NO.

9116

9117 9118

WIDTH

0.69

0.99 0.57

Date Sta

Date Flnl

rtm A Sept. 9/82

.h. H Sept. 9/82

ASSAY VALUES

Au.

Trace

0.27 Trace

1

From

36.09

Al.AA A2.A3

TO

36.78

A2.A3 A3. 00

as well as disseminated throughout the unit.

onii HOU GS-10 nrm,* by Morrisette , o nfl . d b v R. Kemp P oflt 6 : 1

Lotltu

Dtport

FROM

43.00

A3. 12

43.73

AA. 33

AA. 66

*

rt. 5 * o ow R^rm, 18QO P..v 0 H 0ft Surfaceuf . A * 90S -. -75 @ 0 250 feetUrt ——————————————————————— DID ,, ~ /j-fl . -.f 0 , lenffh

-jfc g ^Û ( /O.*, m} , 7fi 5 mo*-r**l

TO

A3. 12

A3. 73

AA. 33

AA. 66

A5.09


Fragments are lenticular in shape, stretched parallel to the foliation. Zone of quartz CO, injection plus chloritic materia at A2.A3 - A2.65. U pyrite.Massive Mafic Tuff- dark in color (black) with fine dissemination of pyrite and localized calcitic veinlets and fractures parallel to the foliation. Interstitial reaction to HCL.Intermediate to Felsic Tuff- light grey in color with finer grained, lighter colored lensoid shaped fragments parallel to foliation faintly evident. Chlorite invasion along grain boundaries. Laths of biotite provide a sense of foliation. Biotite content increases towards upper and lower contact. 1Z pyrite.Mafic Dike- upper contact @ A5" Dark and massive. - lower contact @ 33 0Mafic Tuff Massive- similar to other like zones. Approximately less than 12 pyrite as disseminated grains.Felsic Tuff- very fine grained cherty to silicified tuff with local cross-cutting hairline fracture of white COj. Bluish hue may indicate fine grained disseminated MoS 2 . Pyrite disseminated and blebs along hairline fracture. Less than 12 pyrite.

SAMPLE

NO.

1

9119

9120

WIDTH

0.61

0.63

Dot* Sto

Dot* Flnl

r*. A Sept. 9/82

•h- SeP c - 9/ 82

ASSAY VALUES

Au.

0.21

3.56

From

A3. 12

AA.A6

To

A3. 73

A5.09

Drill Hole GS-10

Lotlfude. OOW


Bearing

Deporture 4 -f 90S Dip -75 @ O

Logged by___R. Kemp

Elevation Surface

..^.K 250 feet

____ Poge _7

Dott Sturm Sept. 9/82

Do,. F.nl,h.d Sept. 9/82-Sfi 0 250 ( 7 6. 2 M ) i -jc o M4...A .,i

FROM

45.09

45.39

45.86

47.43

47.72

9

TO

45.39

45.86

47.43

47.72

52.96

All assays grfms^TO

Intermediate to Felsic Tuff- zone in which biotite content increases and chloritic fragments still faintly evident with sulphides occurring along hairline fracture sub-parallel to foliation. Less than 12 pyrite.Felsic Tuff- zone in which biotite content decreases to provide a silicified cherty appearance to core, pale colored lenticular fragments still present. Less than 1 7. pyrite.Intermediate to Felsic Tuff-lenticular fragments still evident less thc?n 1" in length sub-parallel to foliation, biotite present as mafic constituent slightly chloritic. Zone appears to become brecciated at bottom of zone. 46.87 - 47.13 - fragmented zone, swirled with

biotite encompassing lighter grey cherty. Fragments bluish hue - possible MoS 2 .

Intermediate Tuff- medium grey in color. Biotite content increases from previous zone. Pyrite accumulation along fracture parallel to foliation. Less than 1Z pyriteFelsic to Intermediate Tuff- interbedded zones at

48.83 - 48.99 - dark massive mafic tuff upper contact: 50 0 lower contacts 50 052.35 - 52.57 - dark mafic dike upper contact: 50 0 lower contact: 50 0

SAMPLE

NO.

9121

9122

9123 9124 9125

9126 9127 9128 9129 9130 9131

WIDTH

0.30

0.47

1.01 0.26 0.30

1.11 1.00 0.91 1.00 0.45 0.39

ASSAY VALUES

Au.

0.62

Trace

0.27 0.21 0.34

0.07 0.55 0.07 0.07 0.75 0.62

From

45.09

45.39

45.86 46.87 47.13

47.72 48.99 49.99 50.90 51.90 52.57

To

45.39

45.86

46.87 47.13 47.43

48.83 49.99 50.90 51.90 52.35 52.96

' MM H.,. OS-10 n, |Mt , bv Morrisette ,.... lli . R. Kemp P00 . 8 !

Lotltu

Dtport

FROM

47.72

52.96

55.18

55 f

c i flfiTj i PH**

4 * 90S m -75 g 0 k 250 ft.urt Dlo r, n Orn /7r 0 ml Length-jo 6 2jO (70. Z ra; * (76.2 metres)

TO

52.96

55.18

55.38

55.79


Continued- medium grey-green in color, with variable amounts of mafic constituents (biotite) along zone, locally interstit'ially reactive to HCL. 52.57 - 52.96 - fractured zone especially towards

centre of this section with injected quartz C0 3 vein material and chlorite, plus possible MoS 2 , Sulphidest 2 1 pyrite. Fragments are not discernible.

Intermediate Tuff- dark grey in color, noticeable feature is the pervasiveness of light colored, lenticular in shape, fine grained cherty fragments less than 1" in length x k " wide. Parallel to foliation. 54.92 - 55.18 - chloritic plus quartz C0 3

injection providing a swirly appearance to the core, small speck of Visible Gold@ 55.09.

Stronger sulphide accumulation towards upper contact of zone as blebs and dissemination of pyrite. Section locally reactive to HCL interstitially

21 pyrite.Intermediate to Felsic Tuff- light grey in color, fine grained, becoming more sericitic and chloritic at base of section. Biotite " mafic constituent. Pyrite 1 -21 t finely disseminated pyrite.Dark Mafic Tuff (massive)

SAMPLE

NO.

9132 9133 9134

9135

WIDTH

0.98 0.98 0.26

0.20

Oat* Sta

Dot* Flnl

Sept. 9/82rt. A V

Sept. 9/82• had

ASSAY VALUES

Au.

0.75 0.07 224.1

1.44

From

52.96 53.94 54.92

55.18

To

53.94 54.92 55.18

55.38

OHM HOI* GS-10

5+QQW

Drilled by Mnr^ Logged by K or Poge

Deporture 4+9QS

Bearing

Dip

ISO

-56 g 250 (76.2 M)

Elevotlon Suyfape

L*nflth2SQ f t. ( 76.2

Dote Started SeptQ/82

Finished _______

FROM

55.79

59.99

63.09

9

TO

59.99

63.09

67.48


Intermediate - Felsic Tuff-with discernible lenticular shaped fragments,finely disseminated pyrite approximately 2 7, a sblebs and smears parallel to foliation.Quartz * C0 3 vein g 59.20 (9 cm. wide).

Quartz Feldspar Porphyry (Lapilli Tuff?)-light grey in color with distinct small (lessthan 1mm.) hazy white quartz 0 - feldspathic lapilllocally hairline fracture cross-cuts foliation,here a bleaching of the bounding core exists.Finely dissemination of pyrite is pervasive, lessthan 1 7. pyrite.

Intermediate-Felsic Tuff-mixed zone of felsic, intermediate and mafictuffs. No distinct beds or zones, rather the mafituffs appear interswirled through the section withintermediate to felsic tuffs bounding and enclosedwithin the mafic tuffs. Cross-cutting hairlinefractures are pervasive with bleaching of thesurrounding rock near these fracture zones.Mafic tuff zones are coarser grained with blebsand specks of pyrite standing out while felsicto intermediate horizons are finely disseminatedwith pyrite.@65. 49-65. 59 - intermediate to felsic tuff bounded

by two thin beds of mafic tuff. Betweenthe mark hairline fractures run parallel tocore axis with heavily sulphide.

SAMPLE

NO.

9136913791389139

i/

t

9140

WIDTH

1.001.001.001.20

0.30

ASSAY VALUES

Au.

0.691.440,820.96

0.34

From

55.7956.7957.7958.79

65.37

To

56.7957.7958.7959.99

65.67

Drill H OU GS-10 Drilled bv Morrisette Logged bv R- KemP Pogt 10

oow 180'

Dtportur.

Bearing

m* -75 * O

Elevation Surface

...... 250 ft.

.1... .t...... Sept. 9/82

- 9/82Ob 0 ^DU (76. 2m) ( Tfi. J met-r**cs1

FROM

63.09

67.48

68.28

68.56

0

: TO

67.48

68.28

68.56

76.2

76.20


Continuedrich wisps which stop at the upper and lowercontact. Pyrite less than 8-102.Quartz Feldspar Porphyry (Lapilli tuff?)- same as 59.99 - 63.09 with cross-cuttinghairline fractures producing bleached zone in core.Mafic Tuff- dark" massive with blebs and specks of pyriteless than 3 7.,Same as 63.09 - 67.48 in Felsic to Intermediatetuff with intermixing of mafic tuff zones.

68.56 - 69.20 - heavily fracturedand bleached zone.

END OF HOLE #10

SAMPLE

NO.WIDTH

ASSAY VALUES

Au. From To

*

Drill Holt GS-11 by Morrisette Logged by B. Durham Page

POW Bearing 180

Departure DOS Dip-45

Elevation

Length

Surface

137.16 M.Date Started

DJfe Finished

Sept. 10/82

Sept. 11/82

FROM

05.49

11.7

16.90

35.65

9

TO

5.4911.7

16.90

35.65

39.5


Casing.Medium Grey Lapilli Tuff- weakly sericitic and moderately biotiticfine to medium grained tuff. Minor quartz eyes. Biotite-chlorite patches 1-3 mm. give the unit asomewhat speckled appearance.Pyrite . 5-1Z disseminated.Quartz Eye Sericite Schist (Tuff)- moderately siliceous, buff to grey massive to moderately schistose lapilli-ash tuff.Very weak bluish hue in places may indicate atrace of MoS 2 Schistosity 55" to Core Axis..5 to 12 fine pyrite mainly disseminated butoccasional patches present (associated withbiotite patches) .Light-Medium Grey Lapilli Tuff- rather uniform weakly sericitic dirty lapilli tuff. Occasional fragments visible. Biotite patches to 4mm. throughout. Disseminated pyrite to 12 Scattered chloritic wisps and fracturesthroughout .17.99 - fuchsite wisp * tourmaline.30.50 - minor MoS 2 in chloritic fracture.Felsic Lapilli Tuff- as above but less homogeneous (presumably coarser) lighter grey and somewhat more silicified. Minor sericite, chloritic fractures.

SAMPLENO.

9070907190729073 9074

907590769077

90789079 9080 9081 9082 9083

90849085 9086 9087 9088

WIDTH

0.511.501.501.50 1.20

1.501.501.50

1.501.50 1.50 1.50 1.50 1.50

1.501.50 1.50 1.50 1.50

ASSAY VALUES

Au.

Trace0.070.550.07 Trace

Trace0.756.13

0.27Trace Trace 0.21 0.14 0.07

0.210.75 0.82 1.30 0.21

From

5.496.007.509.00

10.50

11.7013.2014.70

16.2017.70 19.20 20.70 22.20 23.70

25.2026.70 28.20 29.70 31.20

To

6.007.509.00

10.50 11.70

13.2014.7016.20

17.7019.20 20.70 22.20 23.70 25.20

26.7028.20 29.70 31.20 32.70

Drill Hole GS-11

3 * OOWLotltude.


Bearing

Logged by B- Durham

Surface

Poge

Deporture OOS Dip-45

Elcvotlon

Length137.16 M.

Dote Sept. 10/82

Dot. Finished Sept. 11/82

FROM

39.5

47. 0

0

TO

47.0

63.80


Some sections are vaguely porphyritic. 35.7 - 37.2 - . 51 pyrite37.2 - 38.7 - .52 pyrite38.7 - 39.5 - l i pyrite. Moderately siliceous.

Silicified Blue-Grey Lapilli Tuff- as above but more silicified, vaguely porphyriticand blue-grey (MoS 2 content).39.5 - 41 - 3 cm. quartz vein * MoS 2 , 1-22 very

fine pyrite, 41 - 42.5 - more blue-grey from 41.95. 21 very

fine pyrite.42.5 - 44 - Blue-grey scattered MoS 2 flakes. 3-52

very fine pyrite. Minor quartz fractures (* heavy MoS 2 fractures)

44 - 45.5 - blue-grey siliceous 2-32 very finepyrite, frequent chloritic patches andfractures.

45.5 - 47 - 7cm. white silicified zone t MoS :flakes. Blue hue decreases toward 47.0.45.85 MoS 2 * chalcopyrite streak.

Light Grey Quartz Feldspar Porphyry- silicified light grey to blue-grey porphyriticlapilli tuff? Some sections are quite porphyritic,others only vaguely so. 47.0 - 48.5 - scattered pale blue sections

.5-12 pyrite.48.5 - 50.0 - weakly silicified minor MoS 2 stain.

.52 pyrite.

SAMPLE

NO.

9089 909090919092 9093

9094909590969097 9098

F9099 9100

F9801

WIDTH

1.50 1.501.301.50 0.80

1.501.501.501.50 1.50

1.50 1.501.50

ASSAY VALUES

Au.

0.070.960.480.27 0.55

0.340.210.410.69 6.61

1.17 2.360.89

From32.70 34.2035.7037.20 38.70

39.5041.0042.5044.00 45.50

47.00 48.5050.00

To34.20 35.7037.2038.70 39.50

41.0042.5044.0045.50 47.00

48.50 50.0051,50

Drill Hole GS-11

3 -f OOW .otltude————.——.

O.Bartuf 3 * OPS

Drm.d bv Morrisette180 0

Scoring ._________——--45"

Logged byB. Durham Page

Elevotlon

Length

Surface

137.16 M.Date Started Sept. 10/82

Date Finished Sept. 11/82

FROM

63.80

9

TO

77.5

All assays gramsônne

50.0 - 51.5 - vague fragments 12 pyrite51.5 - 53.0 - minor pale blue silicified patches

* chloritic patches and fractures.53.0 - 54.5 - 3 cm. very siliceous walls * very

fine pyrite -f MoS 2 . Minor pale blue sections.54.5 - 56.0 - pale blue, moderately siliceous

22 very fine pyrite, occasional pyritepatches -f MoS 2 flakes.

56.0 - 57.5 - fine grained mafic dike at 56. 04-56.28,56.28 - 57.5 - weakly silicified.

57.5 - 59.0 - weakly silicified minor pyrite *MoSj.

59.0 - 60.0 - finer grained very blue-grey heavyMoS 2 streaks 52 very fine pyrite.

60.0 - 6 J. 8 - less silicified light grey minorpale blue patches ,5Z to 12 fine pyrite.

Light-Medium Grey Lapilli Tuff- moderately schistose. Moderately biotitic(patchy and wispy around remnant lapilli?) Schistosity 65 0 .65.10 - 65.5 - minor pyrite streaks, i ilicified,

fine grained.68.5 - 69.2 - fine grained moderately silicified

22 pyrite, trace MoSj.69.2 - 70.5 - rather barren occasional chloritic

fractures.70.5 - 72.0 - rather barren occasional chloritic

fractures.72.0 - 72.8 - 2 cm. quartz vein * coarse MoS 2 flake

Section is fine grained * 2-32 very fine pyri

SAMPLE

NO.

9802

98039804

9805

98069807

980898099810

9811 98129813

9814

9815

9816

9817:e.

WIDTH

1.50

1.501.50

1.50

1.501.00

1.501.501.50

1.50 1.501.00

0.70

1.30

1.50

0.80

ASSAY VALUES

Au.

4.80

0.480.07

0.07

0.070.75

0.270.890.69

1.17 0.550.14

1.17

0.48

0.62

1.03

From

51.50

53:0054.50

56.00

57.5059.00

60, CO61.5063.00

64.50 66.0067.50

68.50

69.20

70.50

72.00

To

53.00

54.5056.00

57.50

59.0060.00

61.5063.0064.50

66.00 67.5068.50

69.20

70.50

72.00

72.80

Drill Hole GS-11 Drilled by Morrisette B. Durham

POW 180'

Departure 3 -f OOS

Bearing

m* -45'

Logged by

Elevation Surface

Page

,, nBth 137.16M.

Dott Starred Sept. 10/82

Cat* Flnlihed Sept. 11/82

FROM

77.5

86.7

91.8

^h^^

TO

86.7

91.8

94.5

All assays grams/tonne0 c 5 CRlfilON

72.8 - 74.3 - rather barren, uniform74.3 - 75.8 - rather barren, uniform75.8 - 77.3 - vaguely porphyritic

Light Grey Quartz Feldspar Porphyry- vaguely porphyritic light grey to vaguely grey-blue, moderately silicified lapilli tuff.77.3 - 78,8 - .52 pyrite weakly silicified78.8 - 80.3 - vaguely blue-grey minor quartz

fractures .52 pyrite.80.3 - 81.8 - weakly silicified .52 pyrite81.8 - 83.3 - minor chlorite fractures .5 to 12

pyrite fine grained mafic dike82.25-82.55 contacts 60* to Core Axis.

83.3 - 84,8 - pale blue grey .52 to 12 pyrite84.8 - 86.7 - pale blue grey 1-22 fine pyrite

- disseminated and streaks- occasional sericitic fractures, traceMoS 2 .

Pink Feldspar Porphyry Sill- massive, uniform medium grained pink - darkgreen dike or sill.91.0 - 91.8 - chloritic calcitic shear material

mixed with dike.Felsic Lapilli Tuff (Rather Coarse Fragments in Pla- fine grained to coarse material set in calciticto chloritic groundmass.Narrow light blue-grey silicified zones containmoderate MoS, and up to 52 pvrite.

SAMPLE

NO.

981898199820

9821

9822

98239824

982598269827

9828

:es)

9829

U/lftTUw i w i n

1.501.501.50

1.50

1.50

1.501.50

1.501.000.90

0.80

1.00

ASSAY VALUES

AU.

1.580.890.07

0.41

0.82

0.480.62

0.210.140.07

0.07

0.34

From

72.8074.3075.80

77.30

78.80

80.3081.80

83.3084.8085.80

91.00

91.80

To

74.3075.8077.30

78.80

80.30

81.8083.30

84.8085.8086.70

91.80

92.80

Drill HOU GS-11

3 * POW

Drilled by ^Morrisette 18P 0

beorlng

togged bv B- Durham

SurfacePogt

Elevation

n. BO Mu,. 3 -f OPS Dip-45*

Length137.16 M.

Dott Started Sept. 10/82


FROM

94.5

102.5

TO

1P2.5

137.16

•1

All assayj grams/tonneINSCRIPTION

91.8 - 92.8 - fine grained silicified zones atboth ends f pyrite MoSj.

92.8 - 98.8 - minor silicified sections l i pyrite93.8 - 94.5 - 32 pyrite * trace MoS 2 in last

.3m. of sample.Felsic to Intermediate Lapilli Tuff- felsic lapilli tuff with chloritic wispsthroughout from 94.5 - 96. From 96 - 1PP.5, theunit is vaguely porphyritic (lapilli tuff).95. 2P - 95.37 - fine grained massive mafic dike

contact 6P 0 .96.98 - 99.28 - fine grained calcitic weakly

schistose Contact 55* finer grained contact99.40 - 99.66 - dark green schistose mafic dike

contact @ 6P 0 .1PP.1 - 1P0.3 - chlorite calcite shear.101.55 - 2 cm. section of sericite schist * 102

tourmaline.Intermediate Lapilli Tuff- dark grey matrix 702 * lighter .5 cm. lapilli .5 to 12 pyrite throughout.104.3 - 104.9 - more silicified scattered pyrite

C f* * Q g l/ O

107.38 - 107.7 - 702 chlorite calcite.Finer grained from 108.13.114.5 - 118 - weakly sericitic sections

Schistosity 60 0 .114.76 - 114.96 - quartz calcite muscovite,

tourmaline vein. 135.6 - 137.16 - vaeuelv porphyritic, dark grey.

SAMPLE

NO.

9830

9831

9832

9833S9834

9835

9836

WIDTH

1.00

0.70

1.00

0.501.50

0.60

0.6"

ASSAY VALUES

Au.

0.14

0.07

0.07

0.750.07

0.07

0.82

From92.80

93.80

94.50

95.5096.00

109.00

104.30

To93.80

94.50

95.50

96.0097.50

LOO. 60

.04.90

END OF HOLE i ll

DHll Hole fiS - 12

* oosLotltude.


by R. Kemp POO.

Dtporture B -f QOW

Bearing

Dip -50 O O

ElevationSurface

-Ai iSfiLength 450 ft.

/177

Sept. 13/82 Date Started ^—^^——^——,


FROM TOAll assay grams/ tonne

DESCRIPTIONSAMPLE

NO.WIDTH

ASSAY VALUES

Au. From To

0

7.92

9.83

21.59

24.13

31. 84

32.61

7.929.83

21.59

24.13

31.84

32.61

63.72

Casing. Mafic Tuff- dark black in color, massive, with minor amounts of localized bleaching. Lower contact @ 55 0 .Intermediate Mafic Tuff- greenish-grey in color/featureless in appearance- many places with bleaching and chloritized/ sulphides are fine grained and disseminated with occasional blebs and wisps.Zones change in character from pristine featureless zones to highly fractured by cross-cutting hairline fracture bleaching the core and chloritized to provide a greenish color. Less than 12 pyrite.Quartz Feldspar Porphyry- pristine bluish-grey in colour with quartz- feldspar phenocrysts. Less than 5 mm. in size. Upper contact @ 40 0 . Lower contact @ 60 0 . Bull quartz vein 22.01 - 22.51.Intermediate Tuff- similar to 9.83 - 21.59. Quartz Feldspar Porphyry- pristine - contacts hazy, phenocrysts less than 5 mm. in size.Intermediate Mafic Tuff- ranges from greenish color to dark grey-black.

D'lll HOlC GS - 12

/ 4.


Bearing

Logged bv R*

Surface

Poo*

Elevation Date Started Sept. 13/82

onu Dip -SO (3 O Length 450 ft. Dot* Finished Sept. 14/82

FROM TOAll assays grams/tonne

DESCRIPTIONSAMPLE

NO.WIDTH

ASSAY VALUES

Au. From To

33.18 - 38.31 - chloritized green coloured zone. Chloritization pervasive with many small cross-cutting hairline fractures.

Intermediate-Mafic Tuff is rather non-descriptive -commonly massive with intercalated bleached and chloritized zones. With intermittent mafic tuff horizons thinly bedded. Pyrite occurs as blebs and fine disseminations. Minor zones of sericitiz ation. Pyrite less than 1Z.44.49 - 44.54 - quartz C0 3 vein. 44.86 - 44.92 - mafic angular fragments in a fine

grained felsic tuff@ 45.39 - mafic tuff.45.89 - 46.50- chloritized plus slightly hematized

zone by cross-cutting hairline fractures. 46.66 - 46.83 - chloritized zone plus quartz C0 3

vein @ 46.71. 47.23 - 47.30 - mafic tuff with white feldspar

phenocrysts. 47.54 - 47.79 - mafic tuff with white feldspar

phenocrysts.48.21 - 48.32 - mafic tuff with chloritic blebs. 50.24 - 50.32 - chloritized and slightly sericitic 53.54 - 53.71 - quartz COj veining and sericitic

alteration and chloritic alteration.Less than 1Z pyrite.

54.19 - 54.24 - chloritic and quartz C0 3 injection 57.09 - 57.16 - mafic tuff. 57.44 - 57.59 - mafic tuff. 61.24 - 61.31 - biotite-sericite schist. Less than

1Z pyrite.

a"" note CS-12 Ofl||td b y Morrisettet *v A A l A /\ O. -ft..*. * * oosgDeparture .jL OOW

Bearing ,

m - 50 fi 0 Dip .441 fl

Logged bv R- KemP

Surface Elevation ---———--————.

Page

Date StartedSept. 13/82

450 ft. Dat. Flnl.hed Sept. 14/82

FROM

63.72

66.87

68.06

76.65

TO

66.87

68.06

76.65

78.20

•1

———————————————————————————————————— \ ±*i. All assay grams/tonne

3 ^ DESCRIPTION

62.96 - 63.07 - biotite-sericite schist. Less than17. pyrite.

63.07 - 63.72 - zone of quartz C0 3 injection atsteep angle to core.

Biotite Sericite Schist- ranging from white to olive green in colour with fine dissemination of pyrite accumulating along the foliation planes. 2-3Z pyrite.63.72 - 63.91 - quartz C0 3 vein.64.98 - 65.18 - quartz CO, vein.66.00 - 66.38 - quartz C0 3 vein.Intermediate Tuff- occasional quartz eyes seen less than 5 nun. insize.Biotite-Sericite Schist S Intermediate Tuff- felsic to intermediate in color with the occasional quartz eye present. Pyrite is finely disseminated throughout concentrating along planes of foliation. Throughout section, small inter bedded intermediate tuff zones are present - too narrow to outline. However, the majority of the zone is sericitized highly or slightly. (Pyrite 2-3Z Therefore, this zone is a mixed bag of intermediatetuff and localized altered sericitized zones.Quartz eyes are evident in the sericitized zones.73.46 -73.53 - quartz C0 3 vein.Intermediate Tuff- massive in appearance, pristine, unaltered.

j inafcj SAMPLE

NO.

91419142 9143

91449145 9146 9147 9148 9149 9150 9151 9152

as f — — j

WIDTH

1.00 1.00 1.15

1.001.00 1.00 1.00 1.00 1.00 1.00 1.00 0.59

ASSAY VALUES

Au.

0.210.48 0.14

0.890.07 0.41 0.21 Trace Trace 0.07 Trace Trace

From

63.72 64.72 65.72

68.0669.06 70.06 71.06 72.06 73.06 74.06 75.06 76.06

To

64.72 65.72 66.87

69.0670.06 71.06 72.06 73.06 74.06 75.06 76.06 76.65

Hole GS-12

Loiltud*.

Dtporturt

A ' O PS

8 * OOW

Driiitd by Morrijette 180 0

Scoring

Loggtd by R- Kemp

Surface

Poge

Elevotlon

-50(3 0WL A50 ft.Dot* Sfort*d Sept. 13/82

Dot. Finlsh.d Sept. 1A/82-HS^ t; HjU " ' M 77 T ' mo^Y-ec

FROM

78.20

116.91

117.29

118^.

TO

116.91

117.29

118. Al

120.18


Biotite-Sericite Schist Plus Intermediate Tuff- zones preferentially sericitized moderately to highly. Pyrite content 2-3Z as fine disseminatedblebs. 8A.83 - 85.82 - highly sericitized zone. As you get lower in the section, from 87. A8, the intermediate tuff/sericitic unit becomes somewhat , better foliated between light felsic coloured seri- .4citic zone to medium grey intermediate tuff band, commonly less than 3 cm. thick but up to 12 cm. wide beds with the felsic sericitic zones providingthe greater proportion.Bedding to core axis - 61 0 . Sericitic alteration much more pervasive lower in section with quartz eyes quite evident in the sericitic zones. Sericitic zones provide the major part of the lower horizon with thinly bedded faintly contacted intermediate tuff zones. Less than 5 cm. wide. Finely disseminated pyrite lessthan 2-3 l .

.Quartz Feldspar Porphyry- white quartiD-feldspathic phenocrysts in a darkerbiotitic groundmass.Sericite Schist- intermediate in color. Less than 12 pyrite.Mafic Quartz Feldspathic Porphyry- phenocrysts less than 2 mm. in size, massive.

SAMPLE

NO.

9153 915A 91559156 9157 9158 9159 9160 9161 9162 9163916A916A 9166 9167 9168 9169 9170 917191729173917A

9175

9176

1

WIDTH

1.00 1.00 0.811.00 1.00 1.00 0.82 0.99 0.62 1.00 1.001.001.00 1.00 0.97 1.00 1.00 1.05 1.001.001.001.05

1.00

1.13

ASSAY VALUES

Au.

0.21Trace TraceTrace 0.07 0.07 0.1A 0.07 0.07 0.21 TraceTraceTrace Trace Trace 0.21 Trace 0.27 0.1ATraceTraceTrace

0.07

0.21

From

78.20 79.20 80.2081.01 82.01 83.01 8A.01 8A.83 85.82 102.8* 03. 8AOA.8A105. 8* 106.8* 107.8* 108.8] 109.8] 110.8] 111. 8f112. sej113. StiiA.se116.28

117.28

To

79.20 80.20 81.0182.01 83.01 8A.01 8A.83 85.82 86. AA 103.8 10A.8105.8106.8 107.8. 108.8 109.8: 110.8: 111.81 112. 8(113.8111A.8(115.9:117. 2 i

118. A3

Drill H OI* GS-12

4 * DOS

Drilled by

Lotlfudt. Beorlng

Morrisette

180'Logged b y R. Kemp

Elevotlon Surface Dott StorttdSept. 13/82

8 * OOW -50 @ O 450 ft. Dot* Flnlthid Sept. 14/82— —- ---- -- -Q43 g Q3Q ————— ........ ^^

FROM

120.18

TO

135.99j

135.99

136.60

*

L36.60

L37.30

137.30


Sericite Schist (Quartz Eye) Sericitic IntermediateTuff - with quartz eyes less than 3 mm. in size.Pyrite occurs along foliation planes. Sericitiz ation ranges from weak to pervasive. Pyrite lessthan 3 Z.

Intermediate Tuff- massive and pristine.Sericite Schist- same as 120.18 - 135.99.

END OF HOLE #12

SAMPLE

NO.

91779178917991809181918291839184918591869187

9188

Q )

WIDTH

1.001.000.821.001.001.001.001.001.001.000.64

0.70

ASSAY VALUES

Au.

TraceTrace0.070.210.480,07TraceTrace0.270.070.14

Trace

From

124.9:125.9:126.9:128.3!129.3!130.3!131.3!132. 3f133.3!134.3!135.3!

136.60

To

125.9;126.9."127. 7f129.3!130.35131,35132.35133.35134.35135.35135.99

137.30

Drill HOU GS-13

12 * OOWLatitude,

Drilled by

Bearing .—.

Morrisette ISO 0

Logged byB. Durham Poge

Deporture l * SON

Elevation

Length

Surface

137.19 metres

Dote Started Sept. 16/82


FROM

0

3.66

9

TO

3.6634.85

All a s Bays grams 1 tonneDESCRIPTION

Casing.Moderately Chloritic Intermediate Tuff- moderately to strongly calcitic, and chloritic-litfht greyish-green quite inhomogeneous fine tomedium fragmental material.Frequent chlorite and chlorite calcite fracturesthroughout. Schistosity 50 C . Pyrite .52. 8.0 - 9.0 - . 57. pyrite trace bluish colour near

8.120.0 - 21.5 - chlorite calcite shear 20.32 - 20.61

.52 pyrite21.5 - 23 - scattered chlorite calcite slips23.0 - 2 k. 5 - scattered chloritic calcite fractures

Hairline MoS 2 fractures. From 23.8 to 34.1Pyrite . 57. to 1 2.

24.5 - 26.0 - coarse remnant intermediate fragments(small bombs?) in more biotitic groundmassChloritic fractures * .52 fine pyrite.

26.0 - 27.5 - MoS 2 rich fracture at 26.5 M..52 pyrite.

27.5 - 29 - occasional chloritic fractures29 - 30.5 - slightly more mafic - occasional

chlorite fractures .52 pyrite30.5 - 32.0 - frequent chloritic fractures

.52 pyrite. Broken quartz vein materialat 31.8.

32.0 - 33.5 - trace MoS z .52 pyrite. Moderatelysilicified.

33.5 - 34.85 - chlorite calcite shear (mafic tuff)from 34.16 - 34.40 .52 pyrite overall.

SAMPLE

NO.

9837 983898399840

9841

984298439844

9845

9846

9847

WIDTH

1.00 1.501.501.50

1.50

1.501.501.50

1.50

1.50

1.40

ASSAY VALUES

AU.

0.48 2.810.553.01

0.69

0.270.691.85

1.51

0.55

1.37

From

8.00 20.0021.5023.00

24.50

26.0027.5029.00

30.50

32.00

33.50

To

9.00 21.5023.0024.50

26.00

27.5029.0030.50

32.00

33.50

34.90

Drill Hele GS-13

12 * OOWLotltude.


Bearing

Logged by B. Durham

Surface

Pagt

Deporture l * 50N

Elevotlon

Length —

— D ote Storttd Sept. 16/82

137.19 metres O ott Fmiihed Sept. 17/82

FROM

34.85

35.9

38.40

40.8

*

TO

35.90

38. 40

40.8

47.97


Mafic Tuff- dark green fine grained uniform chloritic tuff

.5 to 1Z pyrite.Felsic Lapilli Tuff- vague fine grained fragments in more biotiticground mass. Moderately siliceous.35.9 - 37.4 - moderately silicified 1Z pyrite

* trace MoS 2 .37.4 - 38.4 - moderately silicified . 57, - li pyrite

Scattered blue patches.Fine Grained Mafic Tuff- grey-green uniform - quite homogeneous mafictuff.Sericitic Mafic Tuff- schistose fine grained, light to dark grey tuffaceous unit. Sericitic sections contain 5-202fine biotite some of which appears to pseudomorphtourmaline. Pyrite 1-22 overall (up to 5-72 overshort sections) .40.8 - 42.3 - l i pyrite (fine)42.3 - 43.8 - quite mafic 1-2Z pyrite 12 cm.

barren quartz vein43.8 - 45.3 - moderately sericitic 2 1 pyrite

rare quartz eyes.45.3 - 46.8 - weakly sericitic 12 pyrite46.8 - 48.0 - more altered near 48,0 * quartz vein

(2 cm.)

SAMPLE

NO.

9848

9849

9850

98519852 9853

98549855

WIDTH

1.00

1.50

1.00

1.501.50 1.50

1.501.20

ASSAY VALUES

Au.

0.82

0.48

0.41

0.960.48 0.62

0.480.62

From

34.90

35.90

37.40

40.8042.30 43.80

45.3046.80

To

35.90

37.40

38.40

42.3043.80 45.30

46.8048.00

Drill HOU GS-13

Dtporturt

12 * POW

l * SON

Driiltd by Morrisette 180 0

Loggtd by B. Durham Pogt

Scoring

Dip ,——

Surface

Length 137.19 inures pot.

Sept. 16/82 ''

Sept. 17/82

FROM

48'. 0

49.65

ft

TO

49.65

68.25

All assays grams f tonneDESCRIPTION

Mafic Tuff- rather massive fine grained, uniformFelsic (Cherty) Tuff- fine and medium grained felsic material.No obvious fragments. Minor calcite and pale brownbiotite gives some sections a medium grainedappearance. Some sections are aphanitic andbluish white. Schistosity 70* to Core Axis.49.65 - 51 - mixed felsic and mafic material

.5 to 1Z pyrite.51 - 52.5 - 1Z pyrite weakly calcitic occasional

aphanitic sections52.5 - 54 - 3-4 1 f ine pyrite. Minor bluish

alternation frequent aphanitic sections.54 - 55.5 - 1-2Z pyrite except 2 cm. band of

102 pyrite * tourmaline @ 54.6.55.5 - 57 - 1Z pyrite chalcopyrite on fracture

(3 55.9557 - 58.5 - minor bluish alternation. 1Z pyrite.58.5 - 60 - mainly aphanitic, 1Z pyrite scattered

bluish alternation.60.0 - 61.5 - mainly aphanitic .5 to 1Z pyrite

Frequent bluish alternation.61.5 - 63 - mainly aphanitic. 1Z pyrite overall

10Z pyrite over 6 cm. @ 61.9663 - 64.5 - mainly aphanitic 1-2Z pyrite overall.

Pervasive blue alternation * MoS 2 onfractures.

64.5 - 66.0 - patchy MoS 2 alternation. .5Z pyritecherty

SAMPLE

NO.

98569857

985898599860986198629863

9864

WIDTH

1.351.50

1.501.501.501.501.501.50

1.50

ASSAY VALUES

Au.

0.140.27

0.480.410.480.550.070.55

0.6*

From

49.6551.00

52.5054.0055.5057.0058.5060.00

61.50

To

51.0052.50

54.0055.5057.0058.5060.0061.50

63.00

Drill H Olt GS-13

i atit..n. 12 * POW

Dtportur* l * SON

Oriiltd by Morrisette

Bearing 18Q "^^^

Dip

Logged by B- Durham

Surface

Pogt

Elevotlon Sept. 16/82

-45 137.19 metres••m^^MII* •••••^•••••••mMMMHBHBlBMa

Dote Stoned .


FROM

68.25

71.20

73.6

76.05

TO

71.20

73.6

76.05

78.05

.


66.0 - 67.5 - chloritic mafic dike to 66.35Weakly fragmental, MoS 2 wisps, cherty.

67.5 - 68.25 - cherty fragmental IZ pyriteOccasional chloritic fractures.

Mafic Tuff- weakly sericitic and biotitic, chloritic mafic tuff. Weakly to moderately schistose .5 to IZpyrite throughout.Cherty Tuff- blue-grey fine grained siliceous unit with occasional fragments discernible.71.2 - 72.2 - blue-grey MoS 2 rich fracture at

72.40. Pyrite IZ. Fi'ie grained siliceous.72.2 - 73.6 - more fragmental, minor MoS 2

1-2Z fine pyrite.Mafic Tuff- rather massive, fine grained and uniform.52 pyrite overall. Gray-green quite chloritic,minor epidote alteration rimming pyrite.Felsic Lapilli Tuff (Vaguely Porphyritic)- light to dark grey, fine to medium grainedlapilli tuff, vaguely porphyritic in sectionfrom 76.05 - 76.60.76.05 - 77.05 - .5 to IZ pyrite. Fine grained ir

place., .77.05 - 78.05 - fractured, fine grained * quartz

vein in upper part, lower part mixed felsic and mafic tuff. 2Z pyrite.

SAMPLE

NO.

986598669867986898699870 9871

9872

Qft"7^y o f j9874

9875

9876

WIDTH

1.50

1.501.500.751.501.45 1.00

1.40

1.500.95

1.00

1.00

ASSAY VALUES

Au.

0.69

1.440.890.070.410.55 0.48

0.14

1.170.82

0.41

0.69

From63.0064.5066.0067.5068.2569.75 71.20

72.20

73,6075.10

76.05

77.05

To64.5066.0067.5068.2569.7571.20 72.20

73.60

75.1076.05

77.05

78.05

Drill Holt GS - 13

. ........ 12 t POW

1+ 50NOiparturt

Dritltd by .

Bearing __

Dip ^^^

Morrisette

180*

-45

Logged by B. Durham_______ Poet 5

Elevation Surface Dot* Started Sept. 16/82

137.19 metres Oaft nm.h.d Sept. 17/82

FROM

78.05

93.75

TO

93.75

137.19

13701


Mafic Tuff- grey to grey-green, fine grained section withoccasional lighter (sericitic) sections.Some short sections are silicified or moresiliceous tuffs. Pyrite is more abundant in themore mafic sections.81.0 - 82.8 - scattered sericitic sections and

silicified sections. Schistosity 70 0 .

Intermediate Tuff (Similar to GS-8 @ 36.3-46.6)- pale green-grey fine grained intermediatematerial with minor more chloritic and lessfrequently siliceous matrix (inter-pillow?)Schistosity 70".93.75 - 95.25 - 12 pyrite fine grained,

siliceous in upper part.102.0 - 102.5 - pyrite, MoSj, possible specks

of Visible Gold in quartz vein insilicified andesite.

102.5 - 104 - fragmental andesite. .52 pyrite.104 - 105.5 - moderate silicified trace blue

alternation. .52 pyrite. 3 cm. band of102 pyrite at 105.4.

105.5 -107 - moderate silicified vaguelyporphyritic .52 pyrite.

107 - 108.06 - patchy blue alternation -fragmental .5 to 12 pyrite. Minorfracturing.

END OF HOLE J 13

SAMPLE

NO.

9877

9878

987998809881

9882

WIDTH

1.50

0.50

1.501.501.50

1.06

ASSAY VALUES

Au.

0.21

0.07

0.210,270.14

0.07

From

93.75

102. OC

102. 5C104. OC105. 5C

107.00

To

95.25

102.50

104.00105.50107.00

108.06

••••^——'————————— —

OH,, HO,. GS-1A onn.d b. Morrisette L oflfl . dby Kemp pogt

Lotlfu

Dtport

FROM

0

2. AA

16.38

22.50

23.50

^

i. A * SON ..a,,.. 180* P l . uflfln. Surface

u,. 1 2 * OOW m. -5?S0 - 00 -1-2 i i ——— 500 ft.-3J e JUU \13Z.4 in) MI; 9 J

TO

2. AA 16.38

:?.2.50

23 . 50

A0.2?

A8.06


Casing. Intermediate Tuff- felsic to Intermediate in color, due to the sericitization of the unit, providing a banded appearance but not well bedded. The unit is garnetiferous less than 1 mm. in size/ falling out of garnets @ approximately 8. A3. Two thin zones @ 3.71 and 13.83 have finely disseminated magnetic grains with a sericitic unit. Trace pyrite.Intermediate Tuff- more massive in appearance compared to previous zone, with localized bleached zones eminating from cross-cutting hairline fracture, minor thin units of sericitized tuff. Trace pyrite.Mafic Volcanic- dark green in color, massive, with a quarz C0 3 injection in centre of section 22.88-23.05. Trace pyrite.Intermediate to Mafic Tuffaceous Sediment-grey-blue in color, massive and pristine to zones locally bleached where fracturing occurs, medium to fine grained with the majority of the mafic constituent being biotite. Small lenticular frag ments sub-parallel to parallel to foliation. Trace pyrite.Inter-mediate Tuff-.light grey in color, fine to medium grained

mofrogl

SAMPLE

NO.WIDTH

Oat* Sta

Dor* Flnl

rtmf Sept. 18/82Sept. 19/82 .H. d r

ASSAY VALUES

Au. From To

or,,, HOU GS-14 Drilled by Morrisette Logged byR. Kemp Poflt

i B tit.,n.- 4 * SON B.-rinfl 180 8 r,. un t. nft Surface ftflf . Sfol. t . rf Sept . 18/82

n.Bfrtur. 12 * OOW D |o -50 @ 0 L enflth 500 ft. Do,, wnl.h.d SeDt. 19/82-35 c 500 fl3Z.4 m) /leo ^

CD AIJr n Vm

40.27

48.06

TO

48.06

51.06


Continuedwith localized bleached, mafic tuff and chloritizecfractured zones. Pyrrhotite, Pyrite content 1Z.Small cherty lenticular fragments present parallelto foliation, mafic tuff horizons commonly containsinterswirled and injected quartz C0 3 material andchloritized.40.27 - 40.81 - chloritized, quartz C0 3 zone with

intervening intermediate tuff withlenticular fragments.

40.81 - 41.73 - chloritized quartz C0 3 zone at topof zone - becoming bleached and finegrained to bottom of section. Preferential ly bleached zones appear to outlinefragments .

43.38 - 43.53 - mafic tuff with injected quartzCO j ve in .Upper contact @ 65 0 Lower contact @ 67 C .

45.88 - 45.96 - mafic tuff with chloritized quartzCOj injection.

46,17 - 46.32 - mafic tuff and chloritized quartzC0 3 swirls.

Intermediate Tuff- fractured zone light grey in color, cross-cuttinghairline fracture occur commonly throughout withpyrite occurring in chloritized C0 3 zones as blebs and lenses. Approximately 22 pyrite. Pyrite alsooccurs around lighter colored cherty fragmentswhich are common throughout the zone.48.03 - 48.06 - sheared zone, granular with small

•{•/•Mir^/-) whiffl *3U8Tt"3T*'f sldspfl t"hi c f rflfltnftnt" s

1 mofryoc 1

SAMPLE

NO.

F918991909191

91929193 9194

WIDTH

1.001.001.00

1,000.72 1.05

ASSAY VALUES

Au.

0.550.750.27

0.210.14 3.77

From

45.8846.8847.88

48.8849.88 50.60

To

46.8847.8848.88

49.8850.60 51.65

Drill HOI* GS-14 Orilltd by Morrisette Logged by R. Kemp Poo*

Lomud.JLjÔN ———— B eor(nfl 180* flevatlon surface rfff ,fflfff rf Sept. 18/82

Dtoorriir. . 12 * OOW D lo -50 @0 , ..^ 500ft. e __ 1 0 , 00 Ulp ,4S M snu iHJ.d ml Length— —————————— Dart Flnlihtd Sept. 19/82

FROM

48.06

51.06

J

TO

51.06

58.27

* — I

All assayi^m^conne

Continued@ 50.21 - MoS 2 occurring along hairline fracturesparallel to sub-parallel- to the foliation,- somequartz C0 3 injection is in close proximity to the molybdenite Although molybdenite found within thequartz C0 3 , it has no bearing on presence of themolybdenite.51.10 - 51.65 - zone of fragmentation

heavily interswirled quartz C0 3 materialand tuff material gives the impression offragmentation. MoS, occurs at 51.10, 51.17,51.44, Visible Gold g 51.62.MoS, - 0.02ZPyrite, Pyrrhotite - less than 21.

51.06 - 56.92: Intermediate-Felsic Tuff Zonesranging from intermediate tuff to bleachedfine grained felsic horizons. Lenticularshaped cherty fragments still evident.Pyrite occurs as streaks and fine dissem ination, approximately 12.

56.92 - 58.27: Intermediate Tuff with biotitecontent making a marked increase. Bleached felsic zones still present but not pervas ive. As seen in previous zones, with theincrease in the biotite content, fragmentstend to stand out as the biotite richzones swirl about the lighter coloredframental zones.

Angle to core axis - 67 C .

mof ye

SAMPLE

NO.

9195919691979198

C21670

21671 21672

*v

U/lrtTU

1.001.001.001.001.00

1.00 0.62

ASSAY VALUESAu.

2.331.170.340.270.96

0.55 0.75

From

51.6552.6553.6554.6555.65

56.65 57.65

To

52.6553.6554.6555.6556.65

57.65 58.27

. .. .. ..--..., ——————————— "— -"-" —— - — ' ———— '" -. '••••'•.^••:r:V i^^K^jp8

orni Mat. GS-14 n I 11 , k Morrisette R. Kemp 0 4 ; 1 Drill Hole rvnied oy loaned bv r Pofle

Lotlfu

Deport

FROM

58.27

58.92

60.87

74.41

i

i.* * SON B. BrjM 180" ri . BatlM Surface

-r. 12 * OOW m o -50 @0 , MJIfh 500ft.-JD P 9UU(1~3Z.4 mj M 59 d me*-Y

TO

58.92

60.87

74.41

102.41


Mafic Dike- pristine, dark, massive, medium grained. Angle of upper contact: 63* Angle of lower contact: 57 C Non magnetic.Intermediate Tuff- same as 56.92 - 58.77 with a distinct decrease in the amount of biotite present - decreasing down the hole to the end of the section. li pyrite - fragments still evident.Intermediate Tuff- ranging from fine grained cherty horizons to fine-medium grained intermediate tuff zones richer in mafics. Fragments still apparent. 1-22 pyrite. Biotite content spotty - prevalent in mafic zones, absent in fine grained cherty horizons.Intermediate Tuff- the fine grained felsic cherty zones appear absent. Biotite is the prominent mafic constituent In places the biotite swirls about fragments - highlighting the features. Mafic tuffs - thinly bedded appear localized throughout section. Pyrite occurs as fine dissemination to large blebs, common to lighter felsic horizons. Pyrite 1-22. This unit varies from bleached, thinly bedded zones with minor biotite to zones medium to coarse grained with biotite speckled throughout. Mafic Tuff - 87.50-87.74 - with quartz C0 3 inject

ion.

SAMPLE

NO.

21673 21674

21675 21676 21677 21678 21679 21680

p Q \

WIDTH

1,001.00

1.00 1.00 1.00 1.00 1.00 1.00

Date Sto

Date F!nl

, ^.r

ASSAY VALUES

Au.

1.921.30

0.41 1.58 0.27 0.07 1.30 0.69

From

58.92 59.92

60.92 61.92 62.92 63.92 64.92 65.92

To

59.92 60.92

61.92 62.92 63.92 64.92 65.92 66.92

r-v ':- l', ,. ,?X r iTSrWÎKM i',' •-•' - -.' -. i' 1 "*'.^!-^.^

Drm HOI. CS-U nriii.d b. Morrisette , o flfled b v R. Kemp Poo. 5 ?"^

Lotllu

Otport

FROM

74.41

102.41

102.56

.09.29

14.11

125.2!

*

- 4 * 50N B, nrlft? 180" F1 . un ,lnn Surface

ur . 12 * OOW n lB -50 @ 0 . .. 500 ft.urt ————————————— D |D — -ii A * AA j i tn i L Length-JD e PUU {iDi;.^ m; fi*;9 ^

TO

102.41

102.56

109.29

114.11

125.25

125.4

All assays grams/tonneJ D ESCRIPTION

Continued88.20-88.30 - mafic tuff

Sections are medium grained and gritty. No distinct bedding.

100.33-100.53 - chloritized and sericitic with wall rock fragments - no sulphides.Mafic Dike- massive, dark -b lack Upper contact @ high angle to core @ 20 C Lower contact @ 45 to core axis.Intermediate Tuff- similar to 74 - 102 m. zone, no distinct bedding. Ranges from felsic zones lightly speckled in biotite laths to massive grey zones with pervasive mafics (biotite) and cherty fragments present in the more felsic zone.Intermediate Tuff- chloritized and" fractured zone locally/ 1Z pyrite / swirled by chloritic and chloritized zones, Pyrite concentrated in chloritized fractured zones.Intermediate Tuff- light grey in color with interswirled units of injected chlorite and C0 3 . Bedding not present - cross-cutting fractures occur randomly. Where bleaching is closely related, biotite laths prevalent, fragments present.

i Intermediate to Mafic Tuff- dark, fine grained, minor quartz C0 3 stringers sub-parallel to foliation.

1 l

SAMPLE

NO.WIDTH

Dor. Sto

Dot. Fin!

. , Sept. 18/82

Sept. 19/82ihad

ASSAY VALUES

Au. From To

D'HI Hole GS-UDrilled by Morrisette Logged b y * Kemp Page

l n.ltn*. 4 -t- SON

r, —— ,..... 12 * OOW

Beorlng180'

-50 @ OElevation Surface Dot* Started

Sept. 18/82

500 ft.' —— '3 g 300 (152.4 m) " " M so /i

FROM

L25.45

L26.52

.38.15

0

TO

126.52

138.15

152.40

152.40

DESCRIPTION

Intermediate Tuff- bleached, fine grained with white cherty sections Pyrite 1 7., finely disseminated, cross-cutting hairline fracture.Intermediate to Mafic Tuff- dark grey, massive, medium grained with sections prominent with cross-cutting quartz COj hairline fracture. Dark sliver-like marie shards present parallel to foliation/ ghost outlines of feldspar? are present, increasing in amount towards base of section.Felsic to Intermediate Tuff- light grey in color with variable mafic content (biotite) felsic zones, very fine grained, cherty, less than 12 pyrite, fine cherty lenticular shaped fragments parallel to sub-parallel to foliation. 148.04 - 148.18 - mafic tuff, with injected

quartz C0 3 . 148.18 - 149.48 - intermediate tuff, small

lenticular fragments. 149.48 - 149.62 - mafic tuff with small wisps of

quartz C0 3 .

END OF HOLE #14

mgfcrfys iSAMPLE

NO.WIDTH

ASSAY VALUES

Au. From To

Drill Hoi* GS ' 1 5 nriimrf h v Morrisette i 000 *d bv R- Kemp Poo. 1 '

Lolllu

Diport

FROM

0 4.27

5.36

5.77

6.86

9.43

12.86

4

-. 16 * OOW * farlna 180* F,. untlnn Surface

ur.2 * OON D la -45 0 l en(?th 1 2 i.92 metres

TO

4.27 5.36

5.77

6.86

9.43

12.86

13.03

All assays giams/tonneDESCRIPTION

Casing. Felsic Tuff- very fine grained, D.01% pyrite with darker wispy sections/unit white - cherty in appearance, with an increase in mafic constituents {grey- brown chlorite) towards bottom of zone.Intermediate Tuff, Fragmental- mafic constituent is biotite, lighter colored, very fine grained cherty fragments approximately 3 cm. long stretched parallel to foliation.Intermediate Tuff- felsic at top of section but stronger in mafic constituent towards base, mafics (biotic/ appear swirled into the unit. Pyrite Q.01%.

Mafic Tuff- very dark medium grained, massive, with hairline injections and interswirled CO, (carbonate) common ly hosting disseminated to bleby pyrite Q.1% along foliation plane, pyrite is smeared. Angle of lower contact to core axis s 63 0 .Intermediate Tuff- intermixing of swirled in fine grained cherty unit with a coarser, more mafic biotite, chlorite, carbonaceous host. Trace pyrite.Intermediate Dike- massive, medium grained, above the dike , from 12.81 - 12.86 is a thin mafic tuff unit, as well

SAMPLE

NO.WIDTH

Dot* S t o

Doff Fin!

Sept. 21/82r*. d

, h . d Sept. 22/82

ASSAY VALUES

Au.

o,,,, HOI. GS-15 n,,,,.- K. Morrisette , ™, R' Kerop POO. 2"""^

LOtMu

Oiport

FROM

13.03

25.73

27.46

31.05

- 16 * OOW R MrlBf 180" F( . untlft. Surface

ur . 2 * OON D |D -45 0 i..n fl th 121.92 metres

TO

25.73

27.48

31.05

31.33

31.95

All assays grams/tonneJ D ESCRIPTION

at the base of section from 13.03 - 13.05. Intermediate Tuff- intermixing of mafic biotite and chlorite S CO, (carbonate) unit with a finer grained cherty unit, beige colored lenticular shaped fragments parallel to foliation is found intermittently throughout section, commonly less than 2 cm. long, . 5* pyrite 16.10 - 16.20 - hairline fracture cross-cutting

foliation has a bluish hue, possible MoS, . @22. 33 - speck of Visible Gold found in a fine

grained cherty unit with a dark hue, fine disseminated pyrite occurs here along sub-parallel hairline fracture zone approximately 10 cm. wide

11 pyrite.Mafic Tuff- dark, medium grained with injected quartz CO, swirls, pyrite coarse grained approximately .11. 26.21 - 26.29 - coarse grained felsic unit with

slivers plus rectangular shaped quartz CO, fragments.

Intermediate Tuff-medium to fine grained, with fine grained cherty fragments Q.03% pyrite.Mafic Tuff

- dark, medium grained, carbonaceous, disseminated pyrite, 0.034 pyrite.Intermediate Tuff

— trip pnr"f•^rtn r\f ^pot* \ nn i *s ^''QCfVj v**ry Îmlâi" t~o

SAMPLE

NO.WIDTH

Oatt Sta

Dote Flnl

Sept. 21/82 rttd r

.H.,, Sept. 22/82

ASSAY VALUES

Au.

Drill HOU GS-15

16 * OOW

Drilled by Morrisette Logged by..__R. Kemp

Eifvotion Surface

Peg*

D.portur. 2 * DON Dip -45

Dott Storied Sept. 21/82

121.92 metres D flf . FIft|.ht- Sept. 22/62

FROM

31.95

32.24

33.95

35.99

41.10

9

TO

32.24

33.95

35.99

41.10

46.46


27.48 - 31.05, Q.01% pyrite. Mafic Tuff- with injected and interswirled quartz CO, , pyrite content Q.1% pyrite.Intermediate Tuff, Fragmental- medium grained, with a preponderance of felsic fino grained fragments, cherty in composition. Commonly less than 3 cm. long, stronger towards top of section.Mafic Tuff- dark black, medium-coarse grained, approximately 11 pyrite following foliation planes/upper contact has quartz CO, injected vein/ pyrite occurs as blebs and disseminations.Intermediate Tuff- massive, medium grained with finely disseminated and streaked pyrite along foliation planes. Q.03% pyrite.Intermediate to Felsic Tuff- this zone ranges from a true intermediate tuff to cherty, very fine grained zones. Fine grained lenticular shaped beige in color, lenticular fragments are common throughout the section, within or close to the cherty units along hairline fract ure cross-cutting the foliation. MoS, S 41.94, 43.09, 41.79, 44.33 - 44.49, 15.67 - 46.17, approximately 0.08 to 0.11.

SAMPLE

NO.WIDTH

ASSAY VALUES

Au.

Drill HOU GS-15

16 -t- POW

Oriiltd bx Morrisette Logged byR. Kemp Pug*

Departure OON

Bearing

Dip

180'

-45'Elevation

Length

Surface

121.92 metresDote Storted Sept. 21/82

Dote Flnlthtd Sept. 22/82

FROM

41.10

46.46

50.49

4

TO

46.46

50.45

75.31


Two zones were found to be heavily laden with pyrite, and stronger in mafic constituent, ie. 3 44.66 - 44.81, 45.34 - 45.44. Pyrite content here 51. Constituent of mafic zones * biotite, chlorite, CO, (carbonate)Mafic Tuff- fine to medium grained, massive, dark, with CO, stringers cross-cutting foliation/ becoming more intermediate towards base of section with intro duction of quartz CO, injection.Intermediate to Felsic Tuff- zone varies from an intermediate zone rich in chlorite, biotite, C0 5 and staurolite to felsic cherty massive zones, fine grained with areas having cross-cutting hairline fractures containing finely disseminated MoS, providing a bluish hue to the fractures. Restricted portions have been silicified. Pyrite accumulations occur more heavilj in the mafic sections along foliation planes - smeared disseminations and blebs. Pyrite approximately 1.0*. Coarse grained mafic tuff @ 53.00-53.60 at high angle to core axis. Zones with MoS, @ 52.80.fo'fl? " A?'n2 ~") This does note reflect pervasivt ci ci ~ A rZ i MoSi zones but 20nes in which c A i n Sn'Sf f many cross-cutting hairline 64.10 - /u.jfl j fractures occur which (may tend)

to contain MoS, .

SAMPLE

NO.WIDTH

ASSAY VALUES

Au.

m

Orlll Holt GS-15 Drilled by Morrisette logoed by R* Kemp Poge

16 -t- P OW Bearing 160'

Deporture DON Dip-45

Elevation

Length

Surface

121.92 metresDote Started

Dote Finished

Sept. 21/82

Sept. 22/82

FROM

9

TO DESCRIPTION

50.49 - 51.46 - felsic tuff, massive, 0.01* pyvrt*51.46 - 52.46 - felsic tuff, massive to biotite,

staurolite ri oh, 0.011 pyrite52.46 - 53.60 - felsic tuff to 53.00, mafic tuff

53.00-53.60, .011 MoS, along fracture plane,mafic tuff coarse grained with dark maficphenocrysts. Pyrite .014.

53.60 - 54.60 - felsic tuff, occasional fractureprovides fragmented appearance, .01* pyrite.

54.60 - 55.60 - felsic tuff, alternating zoneswith bleached zones to biotite, staurolite richzones, occas -' trial fragments.

55.60 - 56.60 - intermediate tuff, occasionalfragments, biotite, staurolite, occasionalinjected quartz CO, zone. .011 pyrite.

56.60 - 57.60 - intermediate - felsic tuff:trending towards felsic tuff/biotite, stauro lite, 0.02* pyrite.

57.60 - 58.60 - intermediate to felsic tuff:occasional fragments/ biotite, staurolite,D.01% pyrite.

58.60 - 59.60 - intermediate to felsic tuff to 59.0559.05-59.60 * felsic tuff/ possible MoS, alonghairline fracture. 0.02* pyrite.

59.60 - 60.60 - intermediate-felsic tuff/ biotiteplus staurolite, 0.021 pyrite.

60.60 - 61.60 - intermediate-felsic, tending felsicto base of section. MoS, along hairlinefracture. .02* MoS,. .01* pyrite.

61.60 - 62.60 - felsic tuff/cherty to siliceouswith hairline fracture containing MoS, .03*.Pyrite 0.01*.

SAMPcE

NO.

99809981

9982

9983

9984

9985

9986

9987

, 9988

9989

9990

9991

WIDTH (M.)

0.971.00

1.14

1.00

1.00

1.00

1.00

1.00

1.00

1.00

1.00

1.00

ASSAY VALUES

AU.

Tr.0.07

0.07

Tr.

0.07

0.27

0.14

0.55

0.14

0.27

0.21

1.17

Drill Holt GS-15

16 * P OW


2 -f OON

Scoring

Dip —--

180'

-45 0

Logged bv R' KemP

Surface

Pogt

Elevotlon

Length121.92 metres

Dot* StartedJ pt. 21/82

Dott Flniihtd Sept. 22/82

FROM

9

TOAll assays grams/tonne

DESCRIPTION

62.60 - 63.60 - felsic tuff/cherty to siliceousvery fine grained with bluish hue along hair line fracture. Q.04% MoS, . Q.01% pyrite.

63.60 - 64.60 - felsic tuff/cherty to siliceousat top of zone plus increases in small CO,grains towards base of section. Many smallMoS, fractures. Pyrite disseminated to blebs,one large dark fragment at base of rection.Pyrite D.03%. MoS, D.10%.

64.60 - 65.60 - felsic tuff/cherty to siliceous,

SAMPLE

NO.

9992

9993

9994hairline fractures with MoS, Q.08%, Pyrite .011

65.60 - 66.60 - felsic tuff/minor intermediate tuffl 9995within zone, biotite * staurolite, MoS, . 03i,Pyrite .011.

66.60 - 67.60 - felsic tuff/same as above.67.60 - 68.60 - felsic tuff/same as above.68.60 - 69.60 - felsic tuff/same as above with

carbonaceous fragments standing out due tomafic envelope about them.

69.60 - 70.60 - felsic tuff/a slight increase inthe amount of intermediate tuff present,MoSj ^, pyrite .11, silicification towardsbase of zone.

70.60 - 71.60 - felsic tuff/top portion silicified,interbedded mafic tuff zones (thin) many alongfracture planes, MoSj . 31, pyrite .11.

71.60 - 72.60 - felsic tuff /fractured with CO,.Pyrite Q.02%, MoS, Q.08%.

72.60 - 73.60 - felsic tuff/fractured with a wellfragmented zone, MoS, 2.01, Pyrite Q.02%.

73.60 - 74.60 - felsic tuff/similar to above.

999699979998

9999

10000

49101

49102

49103

WIDTH (M.)

1.00

l.UO

1.00

1.00

1.001.001.00

1.00

1.00

1.00

1.00

1.00

ASSAY VALUES

Au.

0.55

0.62

0.27

0.41

0.481.230.21

0.62

0.14

0.21

0.34

0.62

Drill Holt GS-15

Lotltude—JJL POW

D.portur. 2 -f DON

Drilled by —

Beorlng 160'

-450

Morrisette Logged by R. Kemp Poqt

Dip

Elevotlon Surface————


21/82Dot*

Dot* Finished Sept. 22/82

FROM

75.31

9

TO

82.63


74.60 - 75.31 - felsic tuff /occasional fragmentshairline fracture may carry MoS, - .8*,Pyrite - .021.

Intermediate Tuff- dark grey, coarse grained due to pervasiveness oicherty fragments occurring throughout the section.Pyrite 1.04, fragments less than 4 cm. long.77.82 - 77.97 - felsic zone with pure white rhomb

shaped orthoclase, small dark blue to blacksub-metallic specks are found within zone,non-magnetic, galena? specular hematite? zinc?

75.31 - 76.31 - intermediate tuff /large {less than4 cm. long) fine grained cherty fragments,carbonaceous, pyrite disseminated to blebs andstreaks parallel to foliation. Pyrite - 1.0*.

76.31 - 77.31 - intermediate tuff /same as above.77.31 - 78.31 - intermediate tuff /same as above

with a quartz C03 injected vein with whiterhomb shaped crystals, with small sub-metallicspecks, possibly zinc, galena, specularhematite?77.52 - zone heavier in pyrite within a carbon aceous zone, approximately ID-15% pyrite/white zone pyrite ** 2.01.

78.31 - 79.31 - intermediate tuff /similar to 4910579.31 - 80.31 - intermediate tuff /same as above

Pyrite ^ 3.0*.80.31 - 81.31 - intermediate tuff /same as above

Pyrite 1.0*.81.31 - 82.63 - intermediate tuff /same as above

Pvrite - 1.5*.

SAMPLE

NO.

49104

49105

4910649107

1910819109

19110

19111

WIDTH (M.)

0.71

1.00

1.001.00

1.001.00

1.00

1.32

ASSAY VALUES

Au.

0.27

0.48

0.210.41

0.270.21

0.07

0.27

Drill Hole GS-15 Drilled by Morrisette Logged by R. Kemp Poge S

16 -t- POW

Oeporrure 2 OON

Beorlng 180 0

-45 0

Eievotion Surface Dote Started Sept. 21/62

Dip ,, nnth 121.92 metres Doft cln,. h ..,Sept. 22/82

FROM

82.63

.

87.70

9

TO

87.70

95.62


Felsic to Intermediate Tuff- cherty to silicified, medium to fine grained,cherty sections are very fine grained, beige incolor, fragments are of this composition, MoS,ranges from coarse crystalline veinlet to veryfinely disseminated on foliation planes. MoS, .51.Pyrite 1-21, pyrite occurs as blebs, disseminatedand smears - heavy along foliation planes.82.63 - 83.63 - intermediate-felsic tuff:

intermixing of intermediate tuff and felsicat top of section. Felsic is cherty, beige incolor with many small hairline fractures withpossible MoS,. Pyrite 11, MoS, crystallineveinlet present, MoS, 1-2*.

83.63 - 84.63 - felsic tuff /cherty to siliceouswith hairline fractures with MoS,, MoS,. l-2%,fragments, pyrite 11.

84.63 -85.63 - felsic tuf f/silicified with beigecherty fragments/finely disseminated pyriteQ.8%.

85.63 - 86.63 - felsic tuf f /tending towards a dirt ier section at base due to increase in maficcontent, fragments, MoS, .3*, pyrite 1.0*.

86.63 - 87.70 - felsic to intermediate tuf f /bluishhue to core may indicate MoS,. becoming moreintermediate towards end of zone, pyrite 2 \,MoS, Q.8%.

Intermediate Tuff- medium grained/fragments apparent in upper portioof section/localized quartz C03 veins at highangle to core axis. Tourmaline needles pervasive

SAMPLE

NO.

49112

49113

49114

49115

49116

i

WIDTH (M.)

1.00

1.00

1.00

1.00

1.07

ASSAY VALUES

Au.

0.48

0.41

O tr) . Of.

0.34

0.07

Drill Holt GS-15 Drilled by

Lotltude16 * OOW

Denture 2 * DON

Beorlng

Dip

Morrisette 180 0

-45'

Logged bv R' KemP__________ P"*' 9 ^

Eievofion Surface __ O flf , sforf.d Sept. 21/82

Length 121.92 metres Ooft fr|n |sr)t(j ' 2 2 /82

FROM

95.62

97.02

TO

97.02

102.02

.

All assays^rgmpônne

Pyrite as blebs, smears and disseminations. Pyriteless than 11.87.70 - 88.70 - quartz COj vein plus fragments

(cherty beige) Pyrite 1.01 blebs t disseminatec88.70 - 89.70 - quartz CO, vein, tourmaline,

fragments, pyrite 1.01, blebs S. disseminated.89.70 - 90.70 - massive, pristine foliation to

core axis 59 0 , Q.01% pyrite.90.70 - 91.70 - massive/quartz CO, vein at high

angle to core axis/tourmaline, Q.01% pyrite.91.70 - 92.70 - massive/pristine, Q.01% pyrite.92.70 - 93.70 - massive/pristine, Q.01% pyrite.93.70 - 94.70 - massive/pristine, 0.031 pyrite.94.70 - 95.62 - massive/quartz C0 3 vein/fragments

Q.03% pyrite.Mafic Tuff- dark/very mafic with interstitial CO, , blebs todissemination of pyrite, large cubes close toquartz CO, injections.95.62 - 96.62 - dark/swirly injected CO,, dissemin

ated to blebs of pyrite/pyrite 2 1,96.62 - 97.02 - dark/swirly injected CO,, dissemin

ated to blebs of pyrite/pyrite 21.Intermediate Tuff- top part of section is carbonaceous with felsicfragments/slightly chloritic, with depth zonebecomes more pristine, with the occasional quartzcarbonate injection and an incoming of ghost out lines of feldspar, from 100.32 to 102.02, pyrite less than 0.011.

SAMPLE

NO.

49117

49118

49119

49120

49121491224912349124

49125

49126

WIDTH (M.)

1.00

1.00

1.00

1.00

1.001.001.000.92

1.00

0.40

ASSAY VALUES

Au.

Tr.

0.07

Tr.

0.07

Tr.Tr.0.070.27

0.21

Tr.

Drill Mole GS-15 Drilled byMorrisette togged bv R- KemP Poge 10

16 -f POW Bearing180*

Elevation Surface

Departure Dip-45' 121.92 metres

Dot* Storied

Oflt .

Sept. 21/82

Sept. 22/82

FROM

102.02

103.34

117.62

120.99

t

TO

103. 3'

117.62

120. 9*

121.9:

.21.92

All aS8aysD ff3OT^pne

97.02 - 98.02 - mixed zone of chloritic mafic tuffwith fragments, Q.08% pyrite.

98.02 - 99.02 - pristine intermediate tuff withoccasional vuggy carbonate zone, pyrite D.01%.

99.02 - 100.02 - same as above with injectedquartz carbonate vein, pyrite D.01%.

100.02 - 101.02 - same as above with the incomingof ghost outlines of feldspar phenocrysts.

101.02 - 102.02 - same as above with ghost outlinesbeing more pronounced, pyrite D.01%.

Quartz Feldspar Porphyry- massive and pristine.Intermediate Tuff- distinguishable by the presence of ghost outlinesof feldspar phenocrysts, common to the section arethin sliver like mafic shards, trace pyrite.

Quartz Feldspar Porphyry- slightly hematized, definite phenocrysts offeldspar - massive.Intermediate Tuff- same as 103.34-117.62.

END OF HOLE #15

SAMPLE

NO.

49127

49128

49129

49130

49131

WIDTH (M.)

1.00

1.00

1.00

1.00

1.00

ASSAY VALUES

Au.

0.41

0.07

0 *-\ *.34

0.21

0.07

j

Drill Hole

Latitude

GS-16 Drilled oy Morrisette B. Durham Poge

3 * OON B , 180 0. . Rearing

. 20 * OOW mn ~ 45

Surface ^ Sept. 22/82 'Flu/otlnn Rate Started r

L .n,th 121. 92 metres D o ,. FlB ,, h .d Sept. 23/82

FROM

03.7

7.2

9.4

10.92

14.44

14.8

L5.1

tf

TO

3.77.2

9.4

10.92

14.44

14.80

15.1

20.3


Casing.Felsic Lapilli Tuff- weakly chloritic, moderately foliated fragment packed coarse tuff. Fine grained grey section from 3.7 - 3.77, contains 101 fine pyrite 4 trace MoS3 . Pyrite overall .51, chlorite occurs as patches and wisps. Foliation 55 0 .Mafic Tuff- dark green fine grained, weakly schistose tuff with minor felsic tuff sections.Coarse Felsic Tuff- mixed lapilli and bomb sized aphanitic, light colored siliceous fragments with only minor ground mass material. Pyrite ^ to l i. MoS, bleb at 10.02Mafic Tuff- dark green fine grained, weakly schistose tuff.Coarse Felsic Tuff- as at 9.4 - 10.92.Mafic Tuff- as at 10.92 - 14.44.Felsic Lapilli Tuff- mixed fine and moderately coarse lapilli, weakly chloritic throughout, plus minor biotite, minor tourmaline on scrnie fractures, pyrite .5 to 11.

SAMPLE

NO.

9885

9886

9887

9888

9889

9890 9891 9892

WIDTH

1.18

1.52

0.80

1.59

1.56

1.50 1.50 1.30

ASSAY VALUES

Au.

0.21

0.14

0.27

0.14

0.69

0.21 0.27 0.55

t

From

3.70

4.88

6.40

9.35

14.44

16.00 17.50 19.00

To

4.88

6.40

7.20

10.94

16.00

17.50 19.00 20.30

Drill Holt GS-16

Loll.'ude. DON


180 0

Departure 20 * OOW

Bearing ^.

DIP -45*

Logged by B. Durham

Surface Elevoflon ____________.

Length 121. 92 metres

Pogt

s.,,,., Sept. 22/82

Dote Flnlihed Sept. 23/82

FROM

20.3

32.31

9

TO

32. 3J

46.5


Mafic Tuff- fine grained dark green chloritic tuff. Quitemassive and uniform. Occasional eh lori te-ca lei tefractures.

*Note - Box 4 spilled -26.31-33.91Felsic Lapilli Tuff

- rather heterogeneous, fine and coarse lapillituffs, some aphanitic sections, some sectionsmoderately biotitic (pale brown) . Pyrite concen trations quite variable from .5 to 5% over shortintervals.32.31 - 33.91 - trace MoS,, .51 pyrite, 34 cm.

quartz vein.33.91 - 35.0 - minor MoSs on one fracture, 1-21

pyrite overall - concentrated in 3-6 cm. bands35.00 - 36.2 - 1* pyrite overall, 3 cm. band of

20* pyrite @ 35.76 (calcitic).36.2 - 36.7 - finely bedded, cherty 21 pyrite

bedding 60 C -65 0 .36.7 - 38.2 - .5 to li disseminated pyrite.38.2 - 39.7 - It pyrite, trace chalcopyrite, trace

MoS, (faint) .39.7 - 41.2 - .5 to 11 disseminated pyrite.41.2 - 42.0 - f 5 to 1 1 disseminated pyrite plus

hairline MoS, fracture.42.0 - 43.5 - only vaguely fragmental43.5 - 45.0 - 2 cm. pyritic band 9 4 4.83

.54 pyrite overall.45.0 - 46.5 - . 51 pyrite - vaguely fragmental.

SAMPLE

NO.

9893

9894

9895

9896

98979898

98999900

99019902

9903

WIDTH

1.60

1.09

1.20

0.50

1.501.50

1.500.80

1.501.50

1.50

ASSAY VALUES

AU.

0.07

0.14

0.21

0.82

0.340.21

0.340.07

0.210.14

0.07

pr-nm

32;-31

33.91

35.00

36.20

36.7038.20

J9.7011.20

12.0043.50

45.00

To

33.91

35.00

36.20

37.70

38.2039.70

41.2042.00

43.5045.00

46.50

Drill HoleGS-16


Logged by B. Durham Fog*

QON180'

Dtporrure 20 * POW

Storing —

Dip "45

ElevoflonSurface


Dote Sforted Sept. 22/82


PROM

46.5

49.0

62.23

55.88

168.80

"*

————— TO

49.0

62.23

65.88

68. 8(

71.70

83.2


Mafic Tuff- dark green, fine grained, quite massive, non-calcitic tuff. .51 fine pyrite.Intermediate Lapilli Tuff- rather heterogeneous, intermediate lapilli(light grey to grey-green) set in a more chloriticgrey groundmass. 49.0 - 50.5 - .51 pyrite, obvious lapilli.50.5 - 52.0 - . 51 pyrite mafic tuff 51.28-51.34

no obvious lapilli.52.0 - 53.5 - weakly silicified .5 to \ \ pyrite.53.5 - 55.0 - obvious fine lapilli, l% pyrite55.0 - 56.5 - Jinely bedded in upper part, \ \

pyrite.56.5 - 57.2 - some finely bedded sections.

Mafic Lapilli Tuff- medium to dark green chloritic groundmass withoccasional scattered beige (fine) and greenishlapilli. Scattered 3 cm. pyritic sections.Intermediate Lapilli Tuff-light greenish to yrey, weakly silicified and sericitized lapilli tuff, pyrite 1*.Mafic Lapilli Tuff- rather massive and uniform mafic, chloritic tuffwith occasional obvious lapilli.Heterogeneous-Mafic and Intermediate Lapilli Tuffs- dark arev-oreen mafic laoilli tuffs interbedded

SAMPLE

NO.

99049905

990699079908

9909

9910 9911

WIDTH

1.501.50

1.501.501.50

0.70

1.42 1.50

ASSAY VALUES

Au.

0.210.07

TraceTrace0.07

0.07

0.27 0.14

frrnm

49.0050.50

52.0053.5055.00

56.50

65.88 67.30

Tn

50.5052.00

53.5055.0056.50

57.20

67.30 68.80

Drill Hoie^GS-16

i *tit...... 3 * OON

Or i lit d by Morrisette 180 0

Logged by B. Durham POflt

Storing Elevation Surface

Dtportur* 20 * OOW Dip-45

Length121.92 metres

Dot* Sforrtd

Dot* Flnlihtd

Sept. 22/82

Sept. 23/82

FROM

83.2

88.3

9

TO

88.3

121.92

All assays grams/ conneDESCRIPTION

with beige-grey intermediate tuffs.Pyrite .5 to l i, up to 5i in narrow chlorite, cal cite rich material. Schistosity 75 e .73.5 - 75.0 - 1-21 pyrite, mixed intermediate and

mafic tuffs.Intermediate to Felsic Lapilli Tuffs- rather heterogeneous aphanitic, beige-grey,felsic material with intervening more chloriticmaterial. Some more massive sections could besmall pillows.83.0 - 84.5 - possibly pillowed. .51 pyrite.84.5 - 85.0 - aphanitic, beige85.0 - 86.0 - scattered MoS, wisps, 21 pyrite.86.0 - 87.5 - mixed felsic and mafic lapilli tuffs87.5 - 88.3 - 1-21 pyrite, minor grey aphanitic

sections, trace MoS, .Medium Grey Quartz-Feldspar Porphyry (Lapilli Tuff)- quite sharp contact to rather porphyriticquartz-feldspar porphyry. Feldspar, quartz porphy-roblasts (lapilli?) generally 1-3 mm. Matrix isbiotitic giving spotted medium grey appearance.Quite massive and uniform.88.3 - 89.0 - It pyrite, trace MoS,.95.60 - 97.78 - mafic tuff or dike, fine grained

uniform, massive.98.70 - 9 cm. white quartz vein - sharp contacts

at 30*.Less porphyritic from 100.63, more tuffaceous,

weak schistosity 3 70*.103.2 - barren 8 cm. quartz vein.

SAMPLE

NO.

9912

99139914991599169917

9918

WIDTH

1.50

1.500.501.001.500.80

0.70

ASSAY VALUES

Au.

0.21

0.550.821.580.550.82

0.62

From

73.50

83.084.5085.0086.0087.50

88.30

To

75.00

84.585.0086.0087.5088.30

89.00

All assays grams/tonne3 6 DESCRIPTION SAMPLE

NO.

121.9;

From 108.0 there are widely scattered mafic lapilli up to several cm. (stretched). These mafic lapilli account for only 21 of the unit while the felsic lapilli account for up to 201 or 301 of the unit. From 108.0, the unit is dark grey.

END OF HOLE 116

WIDTH ASSAY VALUES

Au.

Drill Holt GS-17

DON

Drill.d bv Morrisette Logged by B' Durham 180 0

Bearing

D.onrtu,. 20 * POW Dip-45

Elevotion Surface--—.—-


DJ** Storted Sept. 24/62

Doft FiBi.ti*dSept. 26/82

FROM

03.04

11.7

32.2

35.42

t

TO

3.04

11.7

32.2

35.42

56.0


Casing.Mafic Tuffs and Sediments- mixed dark grey-brown sediments with someobvious mafic to intermediate tuff sections.Bedding (schistosity) 70 0 to Core Axis.Some bleaching of the sediments has occurred alongmicro- fractures.Mafic and Intermediate Tuffs- chloritic, biotitic unit with occasional obviousfragmental sections (intermediate lapilli).18.66 - 18.77 - chlorite calcite shear or tuff.18.77 - 18.97 - fine grained mafic dike - massive.

Schistosity 70* to Core Axis.27.70 - 28.20 - chlorite calcite shear, minor MoS, ,28.20 - 28.24 - 201 pyrite plus some MoS,.28.90 - 29.13 - quite mafic (chloritic)29.13 - 32.20 - 301 chlorite calcite shear material

20% white quartz.29.26 - minor MoS, in quartz vein.

Thinly Bedded Felsic Tuffs and Sediments- beige-grey, very fine grained siliceous sedimentsBedding @ 70" to Core Axis.34.0 - 34.52 - chlorite calcite shear.Intermediate Tuffs (Some Flows?)- fine grained grey-beige unit with chlorite - biotite patches and occasional bands to 3 cm. 40.6 - 41.2 - chloritic, calcitic, S-5% pyrite.44.9 - 46.3 - scattered 5 cm. pyritic chloritic

SAMPLE

NO.

9919992099219922

9923

9924 9925

WIDTH

1.51.51.01.0

0.9

1.1 1.4

ASSAY VALUES

Au.

0.270.210.210.14

0.21

0.07 0.14

Froro

27.529.030.531.5

33.7

40.4 44.9

To

29.030.531.532.5

34.6

41.5 46.3

Drill Hole GS-17 Drilled by MorrisetteLogged by B. Durham Poge

Lotltude.5 4- DON

Bearing180'

ElevationSurface

O.DQMur. 20 * POW Dip-45*

Pfl f star,.- Sept. 24/82

Length 121.92 metres Doft Flfl|lhtd Sept. 26/82

FROM

56.0

58.0

66.7

71.0

9

TO

58.0

66.7

71.0

75.24

All assays grams/ tonne' DESCRIPTION

sections, 21 pyrite overall.46.3 - 47.8 - scattered 5 cm. pyritic chloritic

sections. 2% pyrite overall.47.8 - 48.8 - trace MoSa , .51 pyrite.48.8 - 50.2 - .51 pyrite.50.2 - 50.6 - \ b\ pyrite, no MoS,.50.6 - 52.1 - .5 to 11 pyrite, possible trace MoS,.52.1 - 53.6 - .5% pyrite.53.6 - 55.1 - .51 pyrite.Fine Grained Mafic Tuff- very dark green chloritic, quite massive.Intermediate to Felsic Tuffs- light grey-beige, quite fine grained withscattered chloritic patches and rimming possible fragments.60.0 - 60.6 - \ 5\ pyrite over 8 cm., disseminated

in chloritic section.Chloritic Mafic Tuff- dark green rather uniform, fine grained schistoseunit - no visible fragments, \\ disseminated pyrite67.38 - 69.08 - intermediate to felsic tuff.

Intermediate to Felsic Tuffs- medium grey, fine to medium grained, ratherheterogeneous mixture of fine cherty material and weakly calcitic, chloritic material. No obviousfragments. 71.4 - 72.0 - 6 cm. section of 201 medium grained

pyrite.

SAMPLE

NO.

9926992799289929993099319932

9933

49201

WIDTH

1.51.01.40.41.51.51.5

0.6

0.6

ASSAY VALUES

Au.

Tr0.210.070.140.07Trace0.07

0.14

3.09/3.29

From

46.347.848.850.250.652.153.6

60.0

To

47.848.850.250.652.153.655.1

60.6

r oriii HOU G5-17 n,,, ud b y Morrisette , 0 (?fltd b v B. uurnajn Pflfl . —j - ::?*^

i otitiid. ^ * OON R,a ,in fl 180 0 f,. untl ~~ Surface

Dtport

FROM

75.24

77.14

83.35

85.5

u,. 20 * OOW DID -45 0 t.npth 121.92 metres

TO

77.14

83.35

85.5

90.74

All assays grams/ônne

72.0 - 73.5 - 21 pyrite. 73.5 - 75.24 - 1-21 pyrite.Chloritic Mafic Tuff- dark green rather uniform fine grained schistose mafic tuff. No visible fragments, .5 to 11 evenly disseminated pyrite.Intermediate and Felsic Tuffs- quite heterogeneous, vaguely fragmental, grey- beige unit fragments (lapilli), vary from 1-4 cm. 77.6 - 79.0 - 1* disseminated pyrite plus obvious

fragments. 79.0 - 80.0 - ^ to 11 disseminated pyrite

chlorite calcite shear 79.62-79.96 80.0 - 81.18 - .5* pyrite, some lapilli. 81.18 - 81.9 - chloritic tuff. 81.9 - 83.35 - .51 pyrite, occasional lapilli.Chloritic Mafic Tuff- fine grained uniform chloritic tuff with occasional visible lapilli.Fine Grained Felsic Tuff- fine grained to aphanitic (cherty in places) , heterogeneous to moderately bedded tuff with some obvious lapilli. 85.5 - 87.0 - heterogeneous, .51 disseminated

pyrite. 87.0 - 88.0 - heterogeneous, some beige lapilli

. 5t pyrite. 88.0 - 89.5 - more bedded scattered blue patches

1 ft nvi*1 1* t*

SAMPLE

NO.

49202 49203

49204

49205

49206

49207

49208

49209

49210

WIDTH

1.5 1.74

1.4

1.0

1.18

1.45

1.5

1.0

1.5

Oof* S i a

Do tt Fin

M . d Sept. 24/82'

.h.* Sept. 26/82

ASSAY VALUES

AU.

0.480.55

0.41

0,21

0.27

0.41

0.27

0.07

1.92/ 2.13

Drill Hole GS-17 Drilled by Morrisette B. Durham Page

OON

Deporture 20 * POW

Bearing

Dip

180'

-45*

n.*..i M Surface

L....H 1 21 ' 92 metres

nat. Start. rf , SeP fc ' 24/82

FROM

90.74

92.4

L18.87

9

TO

92.4

118.87

.21.92

121.92


89.5 - 90.74 - fine grained 11 pyrite.Chloritic, Calcitic Mafic Tuff- fine to medium grained schistose unit plus minorquartz veins.Intermediate Lapilli Tuff- more uniform medium grey, moderately biotiticunit.93.50 - 94.0 - chloritic -f 501 quartz, 11 pyrite.94.0 - 95.5 - .51 pyrite95.5 - 97.0 - .5% pyrite97.0 - 98.0 - MoS, on one slip face, .51 pyrite98.0 - 98.75 - MoS, on one slip face, l% pyrite98.75 - 100.35 - .51 pyrite, MoS, on one slip face100.35 - 101.35 - mafic tuff, .51 pyrite101.35 - 102.9 - mafic tuff, .51 pyrite102.9 - 104.4 - minor bleached sections, .5 to l%

pyrite, occasional lapilli104.4 - 105.9 - 11 pyrite, frequent lapilli * ash105.9 - 107.4 - more bleached .51 pyrite107.4 - 108.9 - 31 pyrite in last 17 ft., no MoS,108.9 - 110.4 - coarser lapilli, 1-21 pyrite.110.4 - 111.9 - grey-green .51 pyrite112.5 - 118.87 - lighter beige-green trace .51

pyrite.

Mafic Tuffaceous Sediment- dark grey green fine grained tuff S sediment.Schistosity 80 0 to Core Axis.

END OF HOLE 1 17

SAMPLE

NO.

49211

492124921349214492154921649217492184921949220

4922149222492234922449225

WIDTH

1.24

0.51.51.51.00.751.61.01.551.5

1.51.51.51.51.5

ASSAY VALUES

Au.

0.34

0.070.210.140.270.820.140.270.340.14

0.410.550.270.480.21

From To

DHII Hole GS-18 nfiii.d h v Morrisette , ftnnt d b v R. Kemp Pooe - * -V

Lotltu

Dtport

FROM

0

2.44

28.89

29.26

48.55

*

i. 16+OOW n. fl ,iB fl ifln- iri. W ati An Surface

Ur. 6 * OON DID -45 0 L.fiftn 167.64 metres ,

TO

2.44 28.89

29.26

48.55

57,33


Casing. Intermediate Tuff- altered in appearance with bleached and chloritized sections quite pervasive, bedding faintly evid ent, minor hematization, thinly bedded mafic tuff zones, less than 1-2" wide occur randomly, as does injected quartz carbonate veins, sub-parallel to the foliation. Thinly bedded mafic tuff zones quite commonly contain 2-3t pyrite, while other zones are less than Q.04% pyrite.Mafic Tuff- medium grained, dark green, pristine b massive. Intermediate Tuff- zone very similar to 2.44-28.89 zone, bleaching 6 chloritization continue with interswirled mafic tuff zones. Minor amounts of interbedded felsic tufface ous beds - which have bleached contacts. Chloritized zones are coarse grained and contain large biotite plates, and intermixed quartz. Fragments are faintly evident due to bleaching effect, pyrite occurs as seams, blebs and disseminations less than .22.Intermediate Tuff- very similar to above with the exception that it appears lighter in color, unit still contains the occasional fragmental zone. Wisps 6 swirls of chlorite are common, localized quartz carbonate vein (2) are noted, contains coarse grained biotite fc shards of wall rock. Pyrite less than 0.021.

SAMPLE

NO.w i y i n

Date Sfo

3ote Flnl

rt. A Sept. 27/82

.m Sept. 28/82

ASSAY VALUES

Au.

Drm HOI* GS-18 n, i H, d bv Morrisette l ono .d hv R' KemP Poot * ' ••'"- Wi\~*.

Lotlfu

Depart

FROM

57.33

77.24

87.54

- 16 * OOW ...r.., 18QO ,u un ,, ftn Surface

-r. 6 * O ON m. - 450 ,.BBfh 167.64 metres

TO

77.24

87.54

87.96


Intermediate to Felsic Tuff- intermixed zone of intermediate 4 felsic tuffs which range from pristine intermediate tuff, unaltered to sericitic zones which are bleached St contained interbedded intermediate tuff horizons. Mafic tuff zones are thinly interbedded, grain size varies from fine in the felsic zones to medium grained in the intermediate zones. Pyrite less than 0.021. Angle of bedding to core axis 361.69 - 80 0 .60.65 - 62.68 - zone predominantly sericite schist

(barren) with interbedded S bleached intermed iate tuff.

68.55 - 70.10 - felsic tuff, bleached with an inter mixing of intermediate tuff. 69.37 - 69.52 - intermediate dike, upper

contact 3 75" to core axis. Lower contact @ 80 0 to core axis.

70.10 - 73.03 - intermediate tuff- pristine and massive.

Intermittent zones, if not mentioned above, are intermixed intermediate to felsic tuffs.Intermediate Tuff- light grey in color, fine to medium grained with the occasional fragment. Pyrite Q.02%.Mixed Zone- quartz carbonate vein plus intermediate tuff, plus mafic tuff zone is relatively barren in sulphides within all three units, intermediate tuff is light grpy plus fine grained. Mafic tqff has a swirled

SAMPLE

NO.WIDTH

Dot* Sto

Dart Flnl

rt . rf Sept. 27/82

ASSAY VALUES

Au.

DMII Holt GS-18 rolled * * Morrisette i 0fl oed by R' KemP P fl fl* 3 ^^

16 + O OW 180 0 Surface Sept. 27/82"'

.. , 6 * OON ril -45 0 167.64 metres o *. 5 0/03Otporfur* Dlo Length Data Finished oept. t.Q/04

FROMr R w lw

87.96

88.79

89.39

0

TO

88.79

89.39

121.31

All assays grams/ tonneytwCKirTI wN

appearance, quartz carbonate vein injected.Pyrite less than Q.01%.Quartz Carbonate Vein- with intermixed tuff ie. wall rock caught up invein material, portions of the vein have beenhematized imparting a pinkish color. Zone is barrenof mineralization, pyrite less than Q.01%.Mafic Tuff- black, coarse grained with interswirled carbonate.Q.01% pyrite.Intermediate Tuff to Felsic Tuff- lighter grey in color than the intermediate tuffzone 77.24 - 87.54, a slight increase in pyrite isnoted occurring as fine dissemination Q.02%-0.03%pyrite. Fracturing occurs as hairline breaks cross cutting to sub-parallel to the schistosity, unit isgenerally .iner grained, bleached zones occurrandomly associated with the hairline fracture,fragments occur randomly throughout . Minor MoSj .89.39 - 90.40 - swirled zone of intermediate tuff

and carbonate fractures, fine grained, lightgrey, fragments, Q.01% pyrite.

90.40 - 91.40 - intermediate tuff, light grey,fragments, quartz carbonate vein at high angleto core, pyrite Q.01%.

91.40 - 92.41 - intermediate tuff, light grey, finegrained, minor fracture, Q.02% pyrite.

92.41 - 93.27 - intermediate tuff, light grey, finegrained, minor fracture, Q.02% pyrite.

SAMPLE

NO.

49132

49133

49134

49135

U/IHTUw l \j l n(M.)

1.00

1.00

1.00

0.85

ASSAY VALUES

Au.

0.27

0.21

0.89

0.48

i

Drl " Holt

16 * POW


Bearing

Olp

180*

.450

Logged by ^

Elevation Surface

R. Kemp Pogt

tength 167.64 metres

Dot* Started Sept. 2 7/82

Dote Finished Sept. 2 8/82

FROM

**


DESCRIPTION

93.27 - 94.27 - intermediate tuff, light grey, finegrained, cross-cutting hairline fracture,Q.02% pyrite.

94.27 - 95.28 - intermediate tuff, light grey, finegrained, fragments, small quartz carbonateinjection, pyrite 0.021.

95.28 - 96.31 - intermediate tuff, light grey, finegrained with cross-cutting hairline fracture,pyrite Q.03% disseminated.

96.31 - 97.22 - intermediate tuff, light grey, smallquartz carbonate vein, cross-cutting hairlinefracture, disseminated i bleby pyrite Q.03%.

97.22 - 98.33 - intermediate tuff, light grey,fragments, hairline fracture with bleachedzones, 0.01* pyrite disseminated.

98.33 - 99.36 - intermediate tuff, light grey,fragments, cross-cutting bleached hairlinefracture, Q.01% pyrite disseminated.

99.36 - 100.37 - intermediate tuff, light grey,fractured plus bleached, seams plus dissemin ated pyrite, 0.031, fragments.

100.37 - 101.38 - intermediate tuff, light grey,fine grained to medium grained in a smallinterbedded mafic tuff zone. Q.03% pyrite.

101.38 - 102.41 - intermediate tuff, fine grainedto cherty in sections, minor fragments, cross cutting hairline fracture, thin zone with 2lenses of disseminated MoS, in cherty zone atbase of section. Pyrite Q.02%.

102.41 - 103.42 - intermediate tuff, fine grainedto cherty zones, fractures, minor fragment,one small lense of MoS j at top of section,pyrite Q.02%.

SAMPLE

NO.

49136

49137

49138

49139

49140

49141

4 0 142

49143

49144

49145

WIDTH (M.)

1.00

1.00

1.04

1.00

1.00

1.04

1.00

1.00

1.04

1.00

ASSAY VALUES

Au.

0.07

0.69

0.41

0.27

0.55

0.82

0.34

D. 21

J. 07

).27

Drill Holt GS-18 Drilled bv Morrisette ^^ b y R. Kemp Pogt

. atltu.1.. 16 * POW

a. PO ,tur. 6 -f DON

Storing180'

Elevoilon Surface

Dip-45 167.64 metres

Do,, storttd Sept. 27/82

Pflt . Sept. 28/82

FROM TO

•1

All assays grams/tonneDESCRfPTION

103.42 - 104.42 - fine grained, grey, cherty zoneswith brecciated to fragment zone, pyrite Q.02%many hairline fracture.

104.42 - 105.46 - slightly coarser grained due toan increase in mafic constituent (biotite) ,some fine grainei. cherty fragment, 0.011 pyrite

105.46 - 106.47 - continuation of slightly coarsergrained intermediate tuff with intermedia'' efiner grained bleached zones, pyrite O.Olfcpyrite.

106.47 - 107.47 - coarser grained tuff continues,mafic slivers (biotite) are common, bleaching

, at top of zone, Q.01% pyrite.107.47 - 108.50 - continuation of above zone with

minor bleaching, pyrite Q.01%.108.50 - 109.51 - continuation of above zone with

minor bleaching, pyrite 0.01*.109.51 - 110.52 - continuation of above zone with

minor bleaching , pyrite D.01%.110.52 - 111.56 - continuation of above zone with

minor bleaching and fragments, a slightincrease in pyrite content D.03%.

111.56 - 112.56 - coarser grained at top of sectiongiving way to a finer bleached zone towardsbase with cross-cutting hairline fracture inbleached zone, pyrite Q.02% disseminated.

112.56 - 113.57 - medium grained with minorcoarser grained mafic tuff horizons, bleachingoccurs along cross-cutting hairline fracture,fragments occur as fine grained t, cherty.Pyrite Q.03% disseminated.

SAMPLE

NO.

49146

49147

49148

49149

49150

49151

49152

49153

49154

49155

WIDTH 1M.11.00

1.04

1.00

1.00

1.04

1.00

1.00

1.04

1.00

1.00

ASSAY VALUES

Au.

0.55

0.07

0.07

Tr.

0.27

0.21

O f\ t.34

0.21

0.55

O f, Q .07

Drill HoleGS-18

Drilled by Morrisette Logged by R' KeroP Pag*

L o 1 1 1 u d t Bearing 180'

Departure 6 Dip -45'

Elevation Surface.———


Dote Storted Sent. 27/82

Dot* Finished Sept. 28/82

FROM

121.3

9

TO

122.22

All assavs grams/tonne DESCRIPTION

113.57 - 114.60 - a darker more massive, coarsergrained intermediate tuff uait with chertyfragments and bleached zones. Q.01% pyritedisseminated.

114.60 - 115.61 - darker in color, massive, withminor carbonate bearing hairline fracture,mafic fine grained unit at base with seams ofdisseminated pyrite. Pyrite 0.041,

115.61 - 116.61 - similar to above, giving way toa finer grained lighter zone towards bottomof section. Pyrite Q.02%.

116.61 - 117.65 - light grey, finer grained inter mediate tuff with minor fragments. Pyrite Q.02%.

117.65 - 118.66 - light grey, fractured plusbleached, pyrite Q.02% disseminated, approximatebedding to core axis * 85 0, fragments.

118.66 - 119.66 - fine grained, light grey in colorminor fragments and bleached zones, Q.01%pyrite.

119.66 - 120.70 - mafic tuff zone, .7 ft wide withdisseminated, bleby i smeared pyrite, inter mixed with interswirled carbonate, pyritecontent Q.5%-1.0%, bounding this zone isa finer grained light grey intermediate tuff.Pyrite Q.01% zone is bleached towards base.

120.70 - 121.31 - intermediate tuff, fine grainedlight grey, thinly bedded S. bleached , finelydisseminated pyrite Q.03%.

Intermediate Tuff Zone- with fragmented, brecciated zone bounding a quartzcarbonate vein from 121.86 - 121.95, pyrite occursas ^c!SPrMn*fPri R t-H1n spams . pvritft Q.10% —————————

SAMPLE

NO.

49156

49157

49158

49159

49160

49161

49162

49163

WIDTH (M,)1.04

1.00

1.00

1.04

1.00

1.00

1.04

0.60

ASSAY VALUES

Au.

0.41

0.27

0.75

1.10

0.41

0.21

1.03

0.69

Drm HOU QS-JtS nailed by Morrisette i oflo .d bv R. Kemp

LotMu

Depart

FROM

122.22

122.62

123.38

124.75

*. 16 * OOW B. n ,lnn 180" n.un ,lftn Surface

6 * O ON ^, -45 0 167.67 metresart D in L*n9fh

TO

122.6:

123. 3f

124.75

137.0'

*

All assay^jaj^nne

121.31-122.22 - same as described above.Mafic Tuff- dark black with interstitied carbonate, quartz carbonate vein with pinkish hematized zone at base of section. Pyrite 0.51.Intermediate Tuff- light grey in color with bleached zone bounding small cross-cutting hairline fracture. Narrow quartz carbonate vein cuts zone in half cross cutting schistosity at a high angle to the core. Tourmaline found within vein, fragments. Pyrite .051 122.22-123.38 - combination of the two zones

described above.Massive Mafic Tuff- massive, dark, pristine mafic tuff with very finely disseminated pyrite Q.05% plus small hairline carbonate fracture.Intermediate Tuff- light grey in color, medium grained with trace MoSj S 135.60, intermediate dike with bleached contacts 3 127.56-127.68. Fragments are common to the section as are small hairline fractures filled with carbonate. Pyrite occurs as blebs, seams 6 disseminated. 1.0* pyrite, minor interbedded mafictuff zones. 124.75 - 125.76 - medium grey, minor fragment,

Q.01% pyrite.

SAMPLE

NO.

49164

19165

49166

WIDTH (M )

0.91

0.91

1.00

Dot* Sto

Dote Flnl

Pogt

rt. d Se

7 ' •'•'A3;

pt. 27/82

,h.d Sept. 28/82

ASSAY VALUES

Au.

0.27

0.14

).21

Drill Hole GS-18

Lotltud. 16Drilled by Morrisette

180 0Logged by R. Kemp

El.votlon Surface

Length ——

All asj

125.76 - 126.78

tonne

Dote Stqrted Sept. 27/82

Dot* Finished Sop*- 7R/R2

NO.WIDTH(M.)

—-..~ medium grey, oieached fractures, fragments, D.08% pyrite.

126.78 - 127.80 - medium grey, bleached fractures,fragments, Q.08% pyrite dike 3 127.56-127.80.

127.80 - 128.80 - medium grey, minor fragments,bleached along fracture, pyrite D.05%.

128.80 - 129.84 - medium grey, minor fragments,bleached along fracture, pyrite Q.05%.

129.84 - 130.85 - medium grey, minor fragments,bleached along fracture, minor interbeddedmafic tuff, 0.081 pyrite.

130.85 - 131.86 - medium grey, fragments, pyrite .02 49172 1.00 131.86 - 132.89 - medium grey, fragments, carbonate 49173 1.04

filled fracture @ high angle to core, pyriteC.02%.

132.89 - 133.89 - medium grey, fragments, massive pyrite 0.021.

133.89 - 134.9 - medium grey, bleached light green zones, hairline fracture near base of zone. Pyrite, minor fragments.

134.90 - 135.94 - medium grey, fractured zones by hairline fracture, MoS, g 135.60. .021 pyrite.

u*---i---nairnne fracture, MoS, @ 135.60. .02* pyrite.

135.94 - 137.04 - medium grey, bleached, near hair line fracture, fragments, pyrite Q.02%.

|l37.04 141.67 Massive Mafic Tuff

- black, massive with minor CO, hairline fracture. 41.67 142.25 Intermediate to Felsic Tuff

- medium grey, medium grained with minor quartzcarbonate injection.ixi c -,.*.* ~ me as above| pyrite D.03%.

1.04

1.00

1.00

1.04

4917l|l.OO

49174 1.00

49175 1.00

49176 1.04

49177 k).91

19178 D.58

ASSAY VALUES

Au.

0.62

0.27

0.41

0.34

0.89

0.14 0.07

0.41

O.A8

1.17

0.34

Drill HOI, GS-18 Drilled by

16 * POW Scoring180 (

D.pnrtu,. 6 -K DON Dip-45'

Elevotlon

Length

Surface

167.67 metresOott

Dot* Flnl.had

Sept. 27/82

Sept. 28/82

FROM

142.25

143.77

TO

143.71

153. 4^

153 *w 154 * 4]

All assays grams/tonne DESCRIPTION

Massive Mafic Tuff- same as 137.04 - 141.67.Intermediate to Felsic Tuff- light to medium grey in color with a mixed zoneappearance of intermediate tuff, mixed with light er cherty felsic tuff material, faint hairlinefractures occur, along which some of them containMoSj , fragments are pervasive. Pyrite contentis relatively low, G.03%.143.77 - 144.78 - cherty fragments intermixed

intermediate tuff, Q.02% pyrite, fracture.144.78 - 145.79 - cherty fragments intermixed

intermediate tuff, Q.02% pyrite, fracture.145.79 - 146.79 - cherty fragments, intermixed


intermediate tuff, Q.02% pyrite fracture.147.79 - 148.80 - cherty fragments, intermixed



intermediate tuff, 0.021 pyrite, fracture,and MoS, along faint hairline fracture, anoted decrease in intermixed intermediate tuff

150.82 - 151.82 - same as above.151.82 - 152.83 - same as above.152.83 - 153.44 - same as above.Mafic Tuff-massive black to black with interstitial CO, .

SAMPLE

NO.

49179

49180

49181

41982

41983

41984

41985

419864198741988

WIDTH (M.)

1.00

1.00

1.00

1.00

1.00

1.00

1.00

1.001.000.60

ASSAY VALUES

Au.

0.75

0.21

0.07

0.14

0.27

0.21

0 . 27

0.480.210.41

Drill Hole GS-18 Drilled by jMorrisette Logged bv R* KemP Page 10

l ntl...^, 16 -f POW

Otporturi 6 -f DON

Beorlng ISO 0

.450

Elevotlon Surface Dot* Storted Sept

Dip Length 167.67 metres Dote FlnUhed Sept. 2S/82

FROM

154.41

157.52

9

TO

157.52

163.37


Felsic Tuff- light grey, very fine grained, cherty, with finehairline fracture containing MoS, 0.031, pyriteO.Olt. Fragments are present.154.41 - 155.42 - fine grained cherty with hairline

MoS, bearing fracture, 0.011 pyrite, minorcarbonate.

155.42 - 156.42 - same as above.156.42 - 157.52 - same as above.Intermediate to Felsic Tuff- top part of zone is intermediate in nature withfine grained cherty fragments and some minor MoSjoccurring along schistosity pl'.nes. With depth, unitbecomes progressively more cherty i felsic in naturewith zones higher in pyrite, many cross-cuttinghairline fractures contain MoSj , pyrite * Q.03-0.05%157.52 - 158.53 - intermediate tuff, light grey,

0.03* pyrite, fragments 6 fractures.158.53 - 159.53 - intermediate tuff, light grey,

Q.03% pyrite, fragments fi. fractures, MoS,along schistosity plane.

159.53 - 160.54 - intermediate to felsic tuffbecoming more cherty S. fine grained, fine hair line fracture with MoS, Q.03% fine disseminatedpyrite.

160.54 - 161.54 - felsic tuff, fine grained withMOS, bearing hairline fracture. Pyrite Q.03%.

161.54 - 162.55 - felsic tuff, with faint MoSjbearing fracture, minor fragments, pyrite D.03%

SAMPLE

NO.

49189

4919049191

19192

49193

19194

49195

49196

WIDTH (M.)

0.85

1.161.16

1.00

1.00

1.00

1.00

1.00

ASSAY VALUES

Au.

2.06/1.92

1.78/10.96

0.55

0.21

0.41

).75

).62

65

Drill HOlt GS-18 Drilled by

LOtltUde16 * OOW

Oeporture - 6 * OON

Bearing —

DIP -45"

Morrisette ISO 0

Logged bv R* KemP

ElevationSurface Sept. 27/82

167.67 metres

Datt Started

O.M.MJ. 1O l O **Doti Finished Sept. 4 O/Q2

FROM

163.37

163.68

0

TO

163.68

L67.64

167.64


162.55 - 163.37 - felsic tuff with minor inter bedded mafic tuff zone bearing pyrite/hairlinefracture with MoS 2 , pyrite Q.05%.

Mafic Dike- fine grained, massive, pristine.Felsic Tuff- light grey in color, fine grained with MoS,bearing hairline fracture, interswirled carbonatebearing fracture, minor small cherty fragments.163.68 - 164.68 - fine grained cherty to siliceous

with many fine MoS, bearing hairline fractures,fragments. Pyrite 0.02*.

164.68 - 165.69 - same as above.165.69 - 166.69 - a marked change in appearance.

Very fine grained, massive with fine hairlinefractures bearing carbonate, core has a bluishhue which is pervasive, which may indicate avery finely disseminated MoS, throughout thesection from here to end of hole. Pyrite Q.01%.

166.69 - 167.64 - same as above. Pyrite D.01%.

END OF HOLE #18

SAMPLE

NO.

49197

49198

4919949200

49251

WIDTH fM. )

0.82

1.00

1.001.00

0.94

ASSAY VALUES

Au.

0.34

0.69

0.410.89

0.48

Drill Hole Drilled by

i ..titui*. 4+OOW Bearing 180

Logged bv R. Kemp

Elevation Surface

2+00 N -55 O 304.8metres

Don start** Sept.30/82

Oct.5/82


DESCRIPTIONSAMPLE

NO.WIDTH

ASSAY VALUES

Au. Au

O

3.05

3.05

21.34

Casing

Intermediate Tuff

-the zone ranges in nature from fine grainedcherty and bleached material to coarse grainedbiotite, chlorite C0 3 rich zones. Fragments arecommon to the zone as all pervasive cross-cuttinghair line fracture3.05-4.99 - bleached zone eliminating any originalfeatures. Quartz CO, vein @ 3.38-3.54 tourmalinenoted in cherty section of sample 0.01Z Py.Note: Approx. 3 feet of ground core between theabove sample is only 3.4 ft. long4.99-5.30 - Mafic Dyke - lower contact atupper contact at 65 to core axis.5.30-6.30 - Intermediate Tuff; fine to mediumgrained chloritized and bleached, tourmalinewithin bleached zones fine disseminated pyriteo.on6,30-7.31 - fine to medium grained with small fine grained cherty fragments; bleached zones with cross-cutting hair line fracture Pyrite 0.01Z 7.31-8.23 - Fragments are most pronouaded-feature in a much more unaltered section of non-bleached pyrite Q .021.i 23-9.24 - top portion is a continuation of above zone but gives way to a fine grained cherty unit interbedded with the fragmental material MoS 2 noted with Pyrrhotite Pyrite 0.02Z.

49252

49253

49254

49255

49256

1.95

1.00

1,00

0.91

1.00

0.55

1.23

0.69

1,03

0.55

g/t

Drill Hole

Latitude—

GS-19 Drilled by Logged by Page

Bearing Elevation

DID Length

Date Started

Dote FInlih.d

FROM

4


DESCRIPTION

9.24-10.24 - very fine grained cherty zones withcross cutting hair line fracture to slighty coarsegrained C0 3 bearing zones Pyrrhotite, Pyrite,Chalcopyrite. Chalcopyrite and Pyrrhotite occurritogether in sulphide filled hair line fracture,well fragmented zone. Pyrite 0.022 Trace chal copyrite, Pyrrhotite 0.02210.24-11.28 - fine grained cherty zone, similar tcabove . Visible Gold at 11.2511.28-12.28 - fine cherty zone with intermixedcoarse grained CO, units (Subordinate) ChalcopyritPyrrhotite, MoS 2 found within hair line fractureat top of zone. Pyrite 0.052 Pyrrhotite 0.102Trace MoS 2 . Section is magnetic to very magneticdue to the preponderance of Pyrrhotite.12.28-13.29 - Cherty fine grained with mineralizechair line fracture of Pyrite, Pyrrhotite andtrace of Chalcopyrite. MoS a occurs along foliaticplanes and fractures finely disseminated. Chloritbleached zones occur randomly - not very widePyrrhotite 0.12, Pyrite 0.052 Trace ChalcopyriteMoS.(?)13.59-14.33 - fine grained cherty zone at base ofsection as seen above but changing to a medium

trained massive and pristine intermediate tuff

SAMPLE

NO.

r

ng

49257

49258

e

49259

nic

49260

.022 Pyrite and Pyrrhotite (4926114.33-15.33 - bleached zone providing fine grained cherty appearance with some dark blue hair linefracture Pyrite 0.02215.33-16.34 - fine to medium grained with minorfragments thinly bedded cherty section Pyrite 0.02Pyrrhotite 0.022

49262

l49263^^^.^

WIDTH

1.00

1.04

1.00

1.00

1.04

1.00

1.00

ASSAY VALUES

Au.

0.48

2.13/2.33

0.75

0.69

1.79/1.71

0.89

0.62

Au

g/t

Au

g/t

Au

g/t

Drill Hole flS.19 Drilled by Logged by Pag*

latitude, Bearing Elevation Date Started

Departure Dip Length Cat* Finished

FROM

21.34

22.00

t)

TO

22.00

70.71

All assays crams/tonne DESCRIPTION

16.34-17.37 - same as above 17.37-18.38 - same as above to 17.62 then changes character to a medium to coarse grained biotite, staurolite, chlorite ana interstitial C0 3 unit Pyrite 0.01Z. Pyrrhotite 0.01Z 18.38-19.39 - medium-coarse grained zone to 18.98 then back to a finer grained bleached cherty section Pyrite 0.02Z 19.39-20.42 - fine grained cherty to medium graineo with fragments Pyrite 0.03Z 20.42-21.34 - cherty fine grained to 20.69 then changes to a coarser grained fragmented zone a little more mafic in appearance Pyrite 0.5Z

Mafic Tuffcoarse grained, dark, with wisps, disseminated, and blebs of pyrite along with interstitial C0 3 Pyrite 1.02/upper and lower contact brecciated, bottom contact at High angle to core (5 0 )

Intermediate Tuffcontinuation 6F previous mentioned tuff zone a little more mafic in appearance with interbedded cherty zones pyrite accumulates along hair line fracture and foliation planes. Pyrite 0.03Z to l.OZ in localized sections. Fragments are nearly pervasive to common throughout. 22.00-23.01 - upper portion of zone has interswirle mafic tuff material. Well fractured and fragmented from 22,0-22.70 as expressed by lenticular shaped cherty fragments and cross cutting C0 3 hair line fracture, needles of tourmaline are common to the fplsir •sprfions seen on fpl,iation planes

SAMPLE

NO.

49264

49265

49266

49267

49268

i

WIDTH

1.04

1.00

1.00

1.04

0.91

ASSAY VALUES

Au.

0.48

0.8*

0.96

0.34

0.48

Aug/t

Drill GS-19 Drilled by Logged by Fog*

Lotltude, Bforlng Elevation Oat* Started

Departure Dip Length jet* Finished

FROM TO

*

All assav|s gram^tonne

Pyrite 0.01Z.-74.8 to end is intermediate to felsicand bleached23.01-24.02 - upper portion of zone if bleached,a continuation of above grading downw.-^rd to afragmented zone with interbedded fine chertysections with cross cutting hair line fracture at23.47. Pyrite occurs as seams filli.ig fractureand disseminated 0.5Z.24.02-25.02 - continuation of fracture and fragmentzone with interbedded cherty zones co 24.66 whereit changes character to a little coarser grainedunit with bleached C0 3 bearing zones. Pyrite O.SZ25.02-26.03 - medium grained bleached zone withzone intercalated with C0 3 and hair line fracturewhich have bleached margins. Pyrite 0.02Z26.03-27.04 - medium gray and grained with faintcherty fragments, bleached sections with maficclots of Biotite. Pyrite 0.02Z27.04-28,04 - medium grey and grained- same asabove28.04-29.05 - same as above with a chloritizedcarbonaceous fracture. Slighty sheared zone from28.92-29.05 bearing Pyrite and tourmaline. Angleof zone to core axis upper contact * 50'lower contact * 45 C Pyrite 0.05Z29.05-30.05 - a little darker in color with inter mittent cherty zones, cross cutting CQj bearinghairline fracture 0.08Z pyrite.30.05-31.06 - similar to above with interbeddedcherty zones, bleached zones, hair line fractureand fragments. Tourmaline occuring along schistoci planes. Pyrite 0.08Z

SAMPLE

NO.

49269

49270ed

49271

49272

49273

49274

49275

49276

cy 49277

W.OTH

1.00

1.00

1.00

1.00

1.00

1.00

1.00

1.00

1.00

ASSAY VALUES

Au.

0.27

0.07

0.14

0.07

0.21

0.27

0.21

0.14

0.07

Aug/ c

Drill Hole GS-19 Drilled by Logged by Poge

LoWude. Scoring Elevotlon Dcfe Sforted

Deporture Olp Length Daft Finished

FROM TO

•j

All assays grams } tonneDESCRIPTION

31.06-32.06 - same as above32.06-33.07 - dark-more pristine in nature thanprevious zone, medium grained, with the occasionalfragments to 32.89. 32.89-33.07 fragmented withintercalated cherty zone section comes inTourmaline bearing felsic lense at 32.89 Pyrite 0.(33.07-34.08 - Fragmented zone above continues to33.49 where it then changes character to a morepristine zone with minor fragments and then thefragment zone comes back in at 33.86-34.08 -chergy lenses, fragments and disseminated to blebypyrite 0.082Intermediate to Mafic Tuff34. 08-35. 0^ - massive with some cherty fragmentsPyrite 1.0235.08-36.09 - Quartz C0 3 veins at high angle tocore. Trace pyrite.Intermediate Tuff36.09-37.09 - with cherty fragments MoS 2 at 37.09Trace pyrite.37.09-38.1 - with cherty fragments MoS 2 at 37.64Trace pyriteIntermediate to Mafic Tuff38.1-39.1 - cherty fragments Trace pyrite39.1-40.11 - cherty fragments 1.02 pyrite disseminato bleby.40.11-41.15 - cherty fragments 0.82 pyrite41.15-42.06 - cherty fragments 45 C angle to coreaxis at 41.76 MoS a , pyrite 1.0242.06-42.98 - cherty fragments and cherty horizonsMoSj/ pyrite 2.02 disseminated

SAMPLE

NO.

49278

4927952

49280

49281

49282

49283

49284

49285ted4928649287

49288

49289

WIDTH

1.00

1.00

.1.00

1.00

1.00

1.00

1.00

1.00

1.001.04

0.91

0.91

ASSAY VALUES

Au.

0.62

0.48

1.10

0.75

0.48

0.21

1.58

0.41

1.100.34

0.69

0.75

Aug/ 1-

Drill Hole GS-19 Drilled by Logged by Pogt

Lotltudt. Searing Elevation Daft Starttd

Departure Dip Length Dote Flniihed

FROM

0


DESCRIPTION

Intermediate Tuff42,98-43.89 - cherty zones and fragments MoS,Pyrite 1243.89-44.80 - cherty zones and fragments MoS 2Pyrite 1 .5144 .80--'t5, 72 - cherty zones and fragments and MoS 2Pyrite 1.0245.72-46.63 - cherty zones and fragments and MoS 2and pyrite 1.0246.63-47.55 - cherty zones and fragments and MoS 2and Pyrite 1.0247.55-48,46 - cherty and fragments and pyrite trace48.46-49.38 - cherty and fragments and MoS 2and Pyrite trace49.38-50.29 - cherty and fragments and MoS 2 andPyrite 1.0250.29-51.20 - cherty and fragments and MoS 2 andpyrite 1.0251.20-52.12 - cherty and fragments and pyritetrace52.12-53.04 - cherty and fragments and pyritetrace53.04-53.95 - cherty and fragments and MoS 2 andtrace pyrite53.95-54.86 - cherty and fragments and MoS 2 andtrace pyrite.54.86-55.78 - cherty and fragments/chloritic tracepyrite55.78-56.69 - Intermediate to mafic tuff - chertyand fragments trace pyrite56.69-57.60 - cherty and fragments trace pyrite

SAMPLE

NO.

49290

49291

49292

49293

4929449295

49296

49297

49298

^9:99• 9300

.9451

.9452

.9453

(9454.9455

WIDTH

0.91

0.91

0.91

0.91

0.910.91

0.91

0.91

0.91

0.91

0.91

0.91

0.91

0.91

0.910.91

ASSAY VALUES

Au.

1.03

0.41

0.89

1.44

1.78/10.55

0.48

0.62

0.21

0.75

1.99/1

0.27

0.55

0.41

Tr.).27

Aug/t

.85

.99

Aug/t

Aug/t

Drill Hole flS-19 Drilled by Logged by Page

Latitude , Bearing Elevation Dart Started


FROM

70.71

*

TO

75.68

All assays erams/ tonne DESCRIPTION

57.60-58.52 - cherty and fragments trace pyrite58. 52-59. 44 - cherty and fragments trace pyrite59.44-60,35 - cherty and fragments and MoS 2 tracepyrite60.35-61.26 - cherty and fragments and MoS 2 tracepyrite61.26-62.18 - cherty and fragments and trace pyrite62.18-63.09 - cherty and fragments and trace pyrite63.09-64.00 - cherty and fragments and trace pyrite64.00-64.92 - cherty and fragments and MoS 2 andtrace pyrite64.92-65.84 - cherty and fragments and MoS 2 andtrace Pyrite65.84-66.75 -cherty and fragments and brecciatedzone 66.32-66.51 and MoS 2 and 12 pyrite66.75-67.67 - cherty and fragments trace pyrite67.67-68.58 - cherty (dark-MoS 2 ?) and fragmentsand 1.52 pyrite68.58-69.49 - cherty (dark-MoS 2 ?) and fragmentsand 1 .51 pyrite69.49-70.40 - cherty (dark-MoS 2 ?) and fragmentsand 1.02 pyrite70.40-71.32 - cherty intermediate tuff to 70.71pyrite trace 70.71-71.32 mafic tuff 1.52 pyriteMafic Tuffvery dark in colour pyrite occurs as blebs anddisseminatior.s, unit is massive .Pyrite 2-3Z asection of intermediate to mafic tuff occurs from72.82-74.0671.32-72.24 - massive 22 pyrite72.24-73.15 - massive 22 pyrite to 72.82 - 72.74 to73.15 intermediate to mafic tuff trace pyrite

SAMPLE

NO.

4945649457

49458

49459494604946149462

49463

1.9464

49465.9466

.9467

(9468

.9469

i9470

.9471

.9472

WIDTH

0.910.91

0.91

0.910.910.910.91

0.91

0.91

0.910.91

0.91

0.91

0.91

0.91

0.91

0.91

ASSAY VALUES

Au.

0.410.21

0.07

0.140.070.210.14

0.41

0.21

0.340.07

0.55

0.21

Tr.

0.89

1.03

0.02

ku g/ 1

Drill HOU GS-19 Orilltd by Logged by 8

Lotltude. Btorlng Elevotlon Oat* Srartfd

Dtpartur* Dip Length Dot* F'nlshtd

FROM

75.68

TO

86.23

6~

DESCRIPTION

Intermediate to Mafic Tuff73.15-74.06 - Less than 1Z pyrite74.06-74.98 - Mafic Tuff - massive 2Z pyrite74.98-75.89 - Mafic Tuff - massive 2 1 pyrite to75.68 - r.afic to intermediate tuff, cherty,fragments 75.68-75.89 trace pyrite

Intermediate Tuffmedium grey in color/ranging from felsic chertyzones to intermediate zones biotitic, chloriticand carbonaceous, cherty lensoid shaped fragmentsare common with MoS 2 concentrating in the cheryfine grained horizons providing, a blush tinge tothe section, cross-cutting hair line fractures areAu. common with associated bleaching.75.89-76.80 - medium grey/cherty fragments/tracepyrite76.80-77.72 - medium grey with cherty zones andcherty fragments, fine grained 0.05Z/ cherty zoneshave a bluish hue ie. possible fine grained MoS 277.72-78.64 - same as above pyrite l.OZ78.64-79.55 -medium grey, cherty zones and frag ments pyrite trace79.55-80.47 - darker grey with cherty fragments andzones pyrite trace.80.47-81.38 - same as above trace pyrite81.38-82.29 - grey, cherty zones and fragments,dark bluish hue in cherty zone ie. possible MoS 2pyrite l.OZ82.29-83.21 - same as above pyrite l.OZ83.21-84.12 - cherty zones and fragments bluishhue along cross cutting fracture possible MoSjpyrite l.OZ

SAMPLE

NO,

4947349474

49475

!i9476

i9477^9478

.9479

i9480.9481

.9482

.9483

•94:84.

WIDTH

0.910.91

0.91

0.91

0.910.91

0.91

0.910.91

0.91-0.91

0,91

ASSAY VALUES

Au.

0.271.44

1.67

0.07

Tr.0.07

O f\ t.34

0.550.07

0.140.82

0.07

Au R/

j

Drill Hole Drilled by Logged by Pogt

Lotltude, Bearing Elevation Oat* Started


FROM

86.23

9

TO

95.95


84. 12-85. 03 - very cherty and fine grained zonedark bluish color probably due to high amounts ofMoS, pyrite 1-2Z85.03-85.95 - same as above with chloritized Co 3zone approx. 3" wide.Intermediate to Felsic Tuff85.95-86.87 - fine grained cherty dark blue horizonto 86.23. 86.23-86.87 is a felsic tuff zone,cherty, fine grained more pyrite in intermediate zone 2 1 pyrite and MoS 2 felsic zone l.OZ pyrite.

Felsic Tufflight grey in color/ fine grained to cherty inappearance with occasional fragments. MoS 2 isheavy within the zone from approx. 91.44 to 95.95occuring as very fine disseminated providing abluish hue to the cherty zones. Biotite occurs inthe less cherty zones Minor CO, exists Pyrite 1-2Z86.87-87.78 - cherty with minor biotitic chertyzones trace pyrite87.78-88.69 - same as above88.69-89.61 - same as above with minor C0 3 zone89.61-90.53 - cherty zone with MoS 2 , minor fragmentpyrite 1.0290. 53-91. AA - cherty zone with bluish hue ie. MoS 2pyrite l.OZ91.44-92.35 - cherty zone with bluish hue ie. MoS 2pyrite 1.0292.35-93.27 - same as above pyrite trace93.27-9A.18 - same as above pyrite trace94.18-95.09 - cherty/minor C0 3 / bluish hue to coreie. MoS 2 / pyrite trace

SAMPLE

NO.

49485

49486

49487

1948849489i94905i9491

.9492

.9493i9494.9495

.9496

WIDTH

0.91

0.91

0.91

0.910.910.91

0.91

0.91

0.910.910.91

0.91

ASSAY VALUES

Au.

0.07

0.48

0.64

0.14

0.07

0.14

0.07

0.750.340.07

0.07

Aug/c

Drill HOl* Drilled by Logged by Pag* 10

Latitude. Bearing Elevation Oat* Started

Departure Olp Length Oat* Finished

FROM

95.95

96.32

96.93

TO

96.32

96.93

106.77

•I


95.09-96.32 - same as above to 95.95, becominga little more mafic towards 95.95

Intermediate Dyke - massive, coarse grainedupper contact @ 70 0 lower contact 60

Mafic Sediments - massive, brown in color, fineto medium grained dyke? with disseminated pyrite0.52

Felsic Tuff - light grey in color/cherty to biotitechlorite, C0 3 rich horizons, MoS 2 heavy towardstop of section 96.93 to 100.28,96.93-97.84 - light grey, cherty fragments pyritetrace. 96.93-97.78 felsic tuff. 97.78-97.84intermediate dyke (see below)97.78-98.05 - Intermediate Dyke - massive, coarsegrained, upper contact @ 75" lower contact @ 70 0(same as dyke at 95.95 -96.32)Felsic Tuff97.84-98.76 - same unit as 96.93 - 106,77, cont'dcherty with fragments heavy in MoS 2 as core has blush hue pyrite 1.5Z disseminated98.76-99.67 - cherty to biotitic and chloritic andCOj and cherty fragments heavy in MoS 2 at top ofsection trace pyrite.99.67 - 100.58 - same as above/ heavy in MoS 2towards top of section.100.58-101.49 - cherty with biotite and C0 3 tracepyrite some MoS 2101. 49-102. 41 - same as above

SAMPLE

NO.

49497

i

49498

49499

49500

49501

4950249503

WIDTH

1.22

0.91

0.91

0.91

0.91

0.910.91

ASSAY VALUES

Au.

0.07

0.14

0.07

TrXL.

Tr.

Tr.0.07

Au g/ 1

'"

Drill Holt GS-l q Drilled bv io ?0 td by Poo* 11

Lflflfudt . Bearing Flet/atlon

DtDorturt .. Din Lenoth

FROM

106.77

.11.80

4

TO

111.80

115.70

AU ..WfcffiWAfe-n..

102.41-103.33 - cherty with minor fragments/fine grained with bluish hue ie. MoS 7 , biotitic and CO,, trace pyrite 103.33-104.24 - same as above 104.24-105.16 - same as abova 105.16-106.07 - same as above 106.07-106.98 - Felsic k Mafic tuff - felsic tuffcherty/fine grained with cherty fragments towards base of unit at 106.77 - mafic tuff from 106.77 106.98. pyrite l.OZ see mafic unit description below

Mafic Tuffmassive dark to black in color with mafic shards/ sliver's pervasive throughout minor quartz C0 3 veining. trace pyrite 75 angle of foliation to core axis at 106.98 106.98-107.89 - same as above 107.89-108.81 - same as above 108.81-109.73 - same as above 109.73-110.64 - same as above 110.64-111.56 - same as above 111.56-112.47 - Mafic/Felsic Tuff - 111.56-111.80mafic and felsic tuff zorie/chlbritic/cherty zones and fragments/possible MoS a / o.5Z pyrite.

Felsic Tuffcontinuation of 96.93-106.77 zone a little more chloritic and carbonaceous with MoS 2 and 1Z pyrite 112.47-113.69 - chloritic/cherty with fragments/ hair line fracture with MoSj trace pyrite 113.69-114.60 - same as above trace pyrite

SAMPLE

NO.

49504 49505 49506 49507

49508

49509 49510 49511 49512 49513

49514

49515 49516

WIDTH

0.910.91 0.91 0.91

0.91

0.91 0.91 0.91 0.91 0.91

0.91

1.22 0.91

Dot* Stfl

Daft Flnl

rita

lh*d

ASSAY VALUES

Au.

0.07 0.210.27 0.14

1.65

0.21 0.07 0.07 0.14 0.07

0.96

0.82 0.48

Au

Drill Holt 03,10 Drilled by togged by Pag* 12

LoMtud*. Bearing Elevation Date Started


FROM

115. 7(

123.44

123.7!

TO

123.44

123.75

155.08

l

4f


114.60-115.51 - same as above trace pyrite115.51-116.43 - Felsic-Intermediate Tuff - felsictuff to 115. 70/ chloritic and C0 3 with chertyfragments trace pyrite, cross cutting hair linefracture with MoS, Intermediate Tuff see description115.70-116.43 below.

Intermediate TuffGrey in color coarse to medium grained withoccasional cherty fragments, cross cutting hairline fractures with assoc. bleaching Pyrite lessthan 2Z, mafic shards and sliver fragments pervasivtrace fuchsite, minor Quartz C0 3 veining.116.43-117.35 - tiame as above117.35-118.26 - same as above118.26-119.18 - same as above119.18-120.09 - same as above120.09-121.00 - same as above121.00-121.92 - same as above121.92-123.44 - same as above

Mafic Dykedark, massive, 85" at upper contact80 0 (3 lower contactIntermediate Tuff123.75-125.27 - same as 115.70-155.08125.27-126.79 - same as 115.70-155.08126.79-128.32 - same as 115.70-155.08128.32-129.84 - same as 115.70-155.08129.84-131.37 - same as 115.70-155.08131.37-132.89 - same as 115.70-155.08132.89-134.42 - same as 115.70-155.08

SAMPLE

NO.

9517

49518

t

.9519

.9520

.9521• 9522.9523.9524.9525

.9526

.9527i9525.95299530i95319532

WIDTH

0.91

0.91

0.910.910.910.910.910.911.52

1.521.521.521.521.521.521.52

ASSAY VALUES

Au.

0.27

1.03

0.550.410.270.340.140.270.41

0.070.070.07Tr.0.07D. 07Fr.

Aug/t

Drill HOI* GS-19 Drilled by Logged by Pogt 13

Latitude, Bearing Elevation Dote Started

Departure Dip Length Dote FlAitnetf

FROM

155. Of

t

TO

157.67


134.42-135.94 - same as 115.70-155.08 fuchsite not*135.94-137.46 - same as 115.70-155.08 fuchsiteat 136.64.137.46-138.99 - same as 115.70-155.08138.99-140.51 - same as 115.70-155.08140.51-142.04 - same as 115.70-155.08142.04-143.56 - same as 115.70-155.08 fuchsiteat 142.65143.56-145.08 - same as 115.70-155.08145.08-146.60 - same as 115.70-155.08146.60-148.13 - same as 115.70-155.08148.13-149.66 - same as 115.70-155.08149.66-151.18 - same as 115.70-155.08151.18-152.70 - same as 115,70-155.08152.70-154.23 - same as above core bearing bleached154.23-155.75 - 154.23-155.08 intermediate tuffbleached trace fragments, trace pyrite.- 155.08-155.75 - coarser grained feldspar porphyryunit see description below.

Feldspar Porphyrythe margins are well bleached ie. the unit tends toslowly die out rather than a definite contactfeldspar phenocrysts are pervasive trace pyrite155.75-157.28 - same as above157.28-158.19 -

157.28-157.67 feldspar porphyry/ 157.67-158.19bleached and fractured quartz eye bearing schist.see description below

SAMPLE

NO.

#9533

49534495354953649537

4953849539495404954149542495434954449545

49546

• 9547

.9548

WIDTH

1.52

1.521.521.521.52

1.521.521.521.521.521.521.521.52

1.52

1.52

0.91

ASSAY VALUES

Au.

Tr.

0.070.07Tr.0.14

Tr.Tr.Tr.0.07Tr0./30. *10.27

Tr.

Tr.

0.21

AuS/i.

Drill HoU Drilltd by Logged by Page 14

Latitude, Bearing Elevation Date Started

Departure Dip Length Dote Flnlihed

FROM

L57.67

65.08

TO

165,08

178.30

e|


Silicified Quartz sericite schist quart v eye bear ircross cutting hair line fracture with associatedbleaching occurs throughout Fuchsite is presentwithin the zone occuring along schistocity planesand as wisps and lenses 11 to schistocity/ pyriteoccurs as disseminations approx. 1Z158.19-159.10 - bleached and fractured zone .tracepyrite159.10-160.02 - bleached and fractured zone, tracepyrite fuchsite towards base of zone160.02-160.93 - bleached and fractured zone, tracepyrive ,quartz eyes, fuchsite bearing160. 9 J- 161. 85 - bleached, fuchsite bearing as swirland lenses 1.02 pyrite161.85-162.76 - bleached, chloritic, fuchsitebearing, pyrite less than l.OZ162.76-163.68 - same as above163 68-164.59 - same as above164. 59-165. 50 - bleaching less pervasive, quartzeyes to 165.08, pyrite less than l.OZ 165.08-165.50intermediate tuff see description below

Intermediate Tuffdark grey in color, fragments .biotite, chlorite andminor C0 3 occasional quartz CO. vein. Tracefuchsite. Pyrite less than 2Z disseminated to blebs165. 50-166. 42 - small feldspar Phenocrysts, biotitetrace pyrite, fragments .166. k 2- 16 7. 34 - same as above l.OZ pyrite167.34-lu8.25 - same as above l.OZ pyrite168.25-169.16 - grey biotite and chlorite, l.OZ dissemenated pyrite

SAMPLE

NO.

g

49549

49550

49551549552

!i9553i9554i9555

• 9556

.9557

.9558

.9559

.9560

WIDTH

0.91

0.91

0.91

0.91

0.910.910.91

0.91

0.910.910.91

0.91

ASSAY VALUES

Au.

0.14

0.41

0.21

0.55

0.071.100.14

0.07

0.82Tr.0.07

Tr.

Aug/ 1

'

Drill Drilled by Logged by Pose 15

Latitude, Storing Elevation Daft Started


FROM

L78.30

t

TO

238.93


169.16-170.08 - same as above 1.52 pyrite170.08-170.99 - same as above 1.52 pyrite170.99-171.90 - same as above pyrite 2.02, smalllenses of fuchsite171.90-172.82 - same as above 1,52 pyrite172. 82-173. 74 - same as above173.74-174.65 - same as above less mafic constituerfragments, pyrite 1.02 174. 65-175. S6 - same as above pyrite less than 1.03175.56-176.48 - same as above feldspar (Small,phenocrysts back ia Pyrite less than 12176.48-177.39 - same as above

Felsic Tuff - light grey to blue due to the presencof fine disseminated MoS 2 along hair line fractureZone has faint white phenocrysts of feldspar lessthan 1mm. in size within a silicified unit. Pyriteless than 12 disseminated.177.39-178.30 - same as above MoS 2178.30-179.22 - same as above MoS,179.22-180.14 - same as above MoS,180.14-181.05 - same as above MoS,181.05-181.97 - same as above MoS,181.97-182.88 - same as above MoS,182.88-183.79 - same as above MoS,183.79-184.70 - same as above MoS,184.70-185.62 - same as above MoS,185.62-186.54 - see description, MoS, falling out,incoming of faint feldspar phenocryst trace pyrite.186.54-187.45 - same as above187.45-188.37 - same as aboveNote: felsic in nature from 188.37 onward withfaint to distinct feldpoar phenocrvsts. Ipterbedded-

SAMPLE NO.

4956149562

495634956449565t49566 49567

4956849569

e

495704957149572495734957449575495764957749578

495794958049581

WIDTH

0,910.91

0.910.910.91

0.91 0.91

0.910.91

0.910.910.910.910.910.910.910.910.91

0.910.910.91

ASSAY VALUES

Au.

0.070.07

0.07Tr.0.21

0.14 0.07

0.070.14

0.210.270.140.210.140.210.140.210.07

0.070.140.07

Aug/t

Drill Hole GS-19 Drilled by Logged by Pogt 16

LQtltudt. Storing EHvotlon Oat* Started

Departure Dip Length Dote FInlihed

FROM

t


DESCRIPTION

amphibolized mafic tuff occur 189.70-190.68trace pyrite in felsic feldspar porphyry zones192.20-192.54 12 pyrite disseminated in amphiboliz.zones. 194. 16-194. 65., 196.35-196.54188.37-189.89 - silicified quartz-feldspar porphyrfaint to pristine 189.7- 189.89 amphibolized mafictuff.189.89-191.41 - same as above 189.89-190.68amphibolized mafic tuff. 190.68-191.41 silicifiedquartz-feldspar porphyry191.41-192.94 - same as above amphibolized mafictuff 192.2-192.54192.94-194.46 - same as above amphibolized mafictuff 194.16-194.46194.46-195.99 - same as above amphibolized mafictuff 194.46-194.65195.99-197.51 - same as above amphibolized mafictuff 196.35-196.54197.51-199.03 - same as above silicified faint topristine feldspar porphyry199,03-200.56 - same as above silicified faint topristine feldspar porphyry200.56-202.08 - same as above202.08-203.60 - same as above203.60-205.13 - felsic tuff with biotite, silicifieminor cherty zones trace pyrite to 12205.13-206.65 - same as above with hazy feldsparphenocrysts trace pyrite to 12206.65-208.18 - same as above trace pyrite208.18-209.70 - to . . . . , ./208. 73-210.49 quartz eyesericite schist trace pyrite, fuchsite209.70-211.23 - quartz eye sericite schist to210.49/210.49-211.23 prev faint feldspar porphyry

SAMPLE

NO.

d

49582

49583

49584

49585

49586

49587

49588

495894959049591d49592

4959349594

49595

49596

WIDTH

1.52

1.52

1.52

1.52

1.52

1.52

1.52

1.521.521.52

1.52

1.521.52

1.521 S9

ASSAY VALUES

Au.

0.07

0.41

0.34

0.62

0.34

1.03

1.44

0.480.690.21

1.44

0.270.21

0.14

0,21

Aug/c

.

Drill HOU HS..1Q Drilled by Logged by Poge 17

Latitude, Bearing Elevation Dot* Started


FROM

9

TOAll assays grams/ tonne

DESCRIPTION

211.23-212.75 - grey in color with pristine to faitfeldspar phenocrysts to quartz eye (quartz-feldspaiporphyry) less than 12 pyrite212.75-214.27 - same as above quartz-feldsparporphyry less than 12 pyrite214. 27-215. 79 - quartz-feldspar porphyry faint topristine less than 12 pyrite215.79-217.32 - quartz-feldspar porphyry faint topristine less than 12 pyrite217.32-218.48 - quartz-feldspar prophyry light greywith bleached zones contacts 12 pyrite disseminatecand MoS, (possible)218.48 to 218.85Mafic Dykefine grained dark upper contact at 80" lowercontact at 80 C218.85-220.37 - quartz feldspar porphyry grey incolour pristine phenocrysts of feldspar less than12 pyrite220.37-221.89 same as above with chalcopyriteoccuring at bottom of section as blebs approx.0.52 chalcopyrite 1.02 pyrite221.89-223.42 - quartz feldspar porphyry faint topristine phenocrysts.223.42-224.94 - same as above229.94-225.86 -7 224.94-225.55 feldspar porphyrywith porphyry dying out to 225.55. 225.55-225.86silicified felsic tuff, minor biotite and ghostrelicts of feldspar.225.86-227.77 - silicified felsic tuff ghost relictof feldspar porphyry 0.52 pyrite

SAMPLE

NO.

t

49597

49598

49599

49600

49601

49602

49603

49604i9605

.9606i.9607

WIDTH

1.52

1.52

1.52

1.52

0.91

1.52

1.52

1.521,52

1.52

0.91

ASSAY VALUES

Au.

0.14

0.27

0.21

0.34

0.55

0.48

8.71/9

44. 92/1.58

9.74/1D. 55

Aug/ 1

39

• 5.26

).01

Au6/t

.

Au61 L

Drill Hole Drilled by Logged by Peg* 18

Latitude. Bearing Elevation Dote Started


FROM

38.93

t

TO

262.86


227.77-227.69 - feldspar porphyry to 227.23, 227.23to 227.69 silicified felsic tuff with lenses, blebsand disseminated pyrite and MoS 2 pyrite 1-1.52227.69-228.6 - silicified felsic tuff with ghostrelicts of feldspar porphyry less than 2Z pyriteand MoS,228.6-229.51 - silicified felsic tuff with ghostrelicts of feldspar porphyry 2-32 pyrite MoS 2229. 51-230. A3 - same as above 2 1 pyrite MoS,230.43-231.34 - same as above to 230.73 where thezone becomes biotitic and silicified 2 1 pyriteand possible MoS 2231.34-232.26 - biotite feldspar porphyry, darkerthan above felsic zone with intermittent bleachedand CO j zones less than 12 pyrite232.26-233.17 - same as above233.17-234.09 - same as above234.09-235.0 - same as above235.0-235.92 - same as above235.92-236.83 - silicified tuff, felsic to inter mediate, bleached, minor biotite, pyrite less thanli236.83-237.74 - same as above237.74-238.66 - same as above to 238. 08/238. OS-238. 66 amphibolized mafic tuff with interswirledCO, less than l i pyrite238.66-239.57 - 1 238.66-238.93 amphibolized mafictuff 238.93-239.57 intermediate tuff and fragmentsIntermediate Tuffdark grey in color, cherty fragments, fine diss eminated pyrite 12, to zones with ghost relicts ofporphyritic feldspar

SAMPLE

NO.

49608

49609

4961049611

49612

49613196144961549616i9617

4961849619

i9620

49621

WIDTH

0.91

0.91

0.910.91

0.91

0.910.91-0.911.220.91

0.910.91

0.91

0.91

ASSAY VALUES

Au.

0.41

O f. 0 .DI

1.3712.557

33. 05/

0.210.270.750.480.21

0,140.07

D. 21

D. 14

Aug/ 1

L2.75

53.67

Aug/c

Aug/ c

Drill Hoi* r;g-i o Drilled by Logged by Poge 19

Lotltude. Bearing Elevation Oat* Starred


FROM

f

TO

.'t


239.57-240.49 - same as above silicified tuff tocherty with lenses of pyrite 2Z and possible MoS.to 240.27/240.27-240.49 arnphibolized mafic tuff wiinterswirled CO*. 240.49-241.40- fragments/cherty/biotitic/ and minoCO, pyrite l.OZ241.40-242.31 - same as above pyrite 1Z242.31-243.23 - same as above pyrite 1Z243.23-244.14 - same as above, fragments lost asapparent pyrite less than 1Z244.14-245.05 - dark grey biotitic massive, minorCO, no fragments less than 1Z pyrite 245.05-245.97 - same as above245.97-246.89 - same as above246.89-247.80 - same as above247,80-248.72 - same as above to 248.47. 248.47-248.72 intermediate to felsic/silicified withminor fragments (cherty) 1-2Z pyrite248.72-249.63 - intermediate to felsic tuff /minorfragments same as above 1-2Z pyrite249.63-250.55 - intermediate to felsic tuff to250.24/250.24-250.55 intermediate tuff dark grey,

biotitic 1.5Z pyrite250.55-251.46 - minor fragments 1Z disseminatedpyrite251.46-252.37 - same as above less than 1Z pyrite252.37-253.29 - same as above less than 1Z pyrite253.29-254.20 - same as above/silicified 1Z pyrite254.20-255.12 - same as above 1Z pyrite255.12-256.03 - same as above 1Z pyrite256.03-256.95 - same as above less than 1Z pyrite256.95-257.86 - intermediate tuff /no fragments

SAMPLE

NO.

h49622

i*

496234962449625

49626

49627 496284962949630

49631

49632

49633

4963449635496364 96: V 7496384963949640

49661 1

WIDTH

0.91

0.910.910.91

0.91

0.91 0.910.910.91

0.91

0.91

1.22

0.910.910.910.910.910.910.91

0.91

ASSAY VALUES

Au.

.41

3.04.07.48

.41

.75

.14

.82

.14

.44

0.96

0.27

0.690.751.102.88/21.231.30).55

l,f)7

Au8/t

95

AuK/i.

AuB/ L

^KH ^^H ^ m HMM

Drill HOlt Drilled by Logged by Poo* 20

Lollfude, Scoring Elevoflon Oof* Storttd

Dtporrurt Dlo Length Dflt*

FROM

262.86

264.66

275.50

f

TO

264.66

275. 5(

277. 34

All assa^âms^tonne

257.86-258.78 - intermediate tuff/biotitic/tracepyrite258.259.69- intermediate tuff /minor C0 3 / tracepyrite259.69-260.60- same as above260.60-262.13- same as above/amphibolized mafictuff 260.82-261.12,262.13-263.65- intermediate tuff to 262.86 sameas above/262.86-263.65 amphibolized mafic tuff.

Amphibolized Mafic Tuff - interstitial CO, 12pyrite263.65-265.18 - amphbolized tuff to 264.66/inter-roediate tuff 264.66-265.18, faint feldsparphenocrysts.Intermediate Tuffmedium grained faint feldspar phenocrysts withminor CO, trace pyrite 265.18-266.7 -same as above266.7-268.22 - same as above268.22-269.75 - same as above269.75-271.27 - same as above271.27-272.79 - fine grained, olive green in colortrace pyrite272.79-274.32- same as above with feldspar porphyry267.68-273.98 feldspar porphyry274.32-275.84 - same as above to 275.50/275,50-275.84 feldspar porphyry

Feldspar Porphyry275.84-277.34 - feldspar porphyry

SAMPLE

NO.

49642

4964349644

49645

49646

49647

49648496494965049651

49652

49653

49654

49655

WIDTH

0.91

0.910.91

1.52

1.52

1.52

1.521.521.521.52

1.52

1.52

1.52

1.22

ASSAY VALUES

Au.

0.41

0.480.21

0.14

0.07

1.44

0.210.340.070.62

3.70/

0.21

0.07

0.07

Aug/t

.70

Aug/ i-

Au-jrr-

Drill H ole GS-19 Drilled by Logged by Page 21

Lotltude. Beorlng Elevotlon Dolt Started

Oiporturt Dip Length Dote Finished

FROM

277.34

TO

277. 9f

.

A11 assîcftTO6tonneIntermediate277.34-277.98 - Intermediate tuff/silicified tocherty in places/ zones showing feldspar porphyryas ghost outlines 2-32 pyrite as seams and lensesat to section277.98-278.89 - Intermediate Tuff - same as above1-22 disseminated and bleby pyrite278.89-279.80 - same as above 12 disseminate pyrit279.80-280.72 - same as above with minor quartzCO, ve in ing.280.72-281.64 - Intermediate tuff - same as above1-22 pyrite281.64-282.55 - same as above 12 pyrite282.55-283.46 - fine grained massive trace pyrite283.46-284.38 - same as above284.38-285.29 - same as above trace pyrite285.29-286.20 - same as above trace pyrite286.20-287.12 - same as above trace pyrite287.12-288.03 - same as above trace pyrite288.03-288.95 - Quartz, C0 3 vein, less than 12pyrite288.95-289.86 - quartz, C0 3 vein, biotitic lessthan 12 pyrite289.06-290.78 - same as above, ghost outlines offeldspar less than 12 pyrite290.78-291.69 - same as above, less than 12 pyriteminor interbedded quartz sericite schist291.69-293.22 - medium grey minor interbeddedquartz sericitic schist trace pyrite293.22-294.74 - same as above trace pyrite294.74-296.27 - same as above trace pyrite296.27-297.79 - same as above trace pyrite297.79-299.31 - same as above trace pyrite

SAMPLE

NO.

49656

49657.49658

49659

4966049661496624966349664496654966649667

49668

49668

49669

49670

4967149672496734967449675

WIDTH

1.22

0.910.91

0.91

0.910.910.910.910.910.910.910.91

0.91

0,91

0.91

0.91

1.521.521.521.521.52

ASSAY VALUES

Au.

0.75

0.550.27

0.21

0.340.070.070.14Tr.0.270.340.07

Tr.

Tr.

Tr.

0.07

Tr.Tr.0.070.07Tr.

Aug/ 1

,

'..-. . " ,rf - VJjiX .'j' ' - 't)' -

Or Ml Hole

•'•••^^^îlKSS-19

Latitude.

Departure

Drilled by

Bearing .—

Dip ————

Logged by

Elevation ,—

Length ___

POfl*

Date Started

Dote Finished

FROM

1

TO

-

304.8

1


299.31--300.84 - same as above trace pyrite 300.84-302.36 - same as above trace pyrite 302.36-303.89 - same as above trace pyrite 303.89-304.8 - same as above quartz vein with a marked increase in pyrite within quartz eye sericite schist 2-2.52 pyrite

END OF HOLE #19

SAMPLE

NO.

49676 49677 49678

49679

WIDTH

0.910.91 0.91

0.91

ASSAY VALUES

Au.

0.070.14 0.07

0.21

AusA

prill Hole GS-20

Latitude. L48 -f OOW

Drilled by

Bearing

Morrisette

ISO 0Logged b, R' Ke*P

Surface

Poge

Elevation

Departure 6 -f SON Dip -45' Length 116.87 metres

Daft Started CCL. 29/82

Dot. Flfll.hed O**' 30/82


DESCRIPTION SAMPLE!

NO. !WIDTH

ASSAY VALUES

Au.

2.44

29.38

34.62

2.44

29.38

34.62

100.70

Casing.

Biotitic Mafic to Intermediate Sediments2.44 - 14.32 - biotitic mafic sediments with minor

interbedded amphibolized mafic tuffs.14.32 - 16.76 - intermediate to mafic sediments,

minor interbedded amphibolized mafic tuffs and fine grained muscovite bearing zones and biotitic mafic sediments bleaching occurring randomly. Angle bedding to core axis e 14.93 - 70*.

16.76 - 29.38 - intermediate to biotitic mafic sediments, minor bleaching/ possible fragments.

Intermediate Sediments, Cherty Tuffs s Fragmental29.38 - 29.78 - intermediate tuff/fragments, cherty

zones, trace pyrite.29.78 - 33.83 - biotitic intermediate tuff, bleachec33.83 - 34.62 - intermediate tuff, fragments,

cherty interbedded tuffs, trace pyrite.

Mafic Biotitic Sediments, Minor Interbedded Tuffs Fragments Locally34.62 - 38.10 - intermediate to mafic sediments,

biotitic, minor interbedded cherty zones, occasionally bleached trace pyrite.

38.10 - 45.41 - biotitic mafic sediments, fine _____grained, possible fragments, interbedded

Drill Hole GS-20 Drilled by Morrisette Logged bv Pag*

Lotltude, Bearing Elevoflon Daft Sfarftd

Departure Dip Length Daft Finished

FROM

.

TO

m ~


38.10 - 45.41 Cont'd.cherty horizons, pyrite 2.01, possible MoSj .38.10 - 39.32 - minor bleaching, minorinterbedded cherty horizons, minor amphib-olites, less than 11 disseminated pyrite.39.32 - 40.54 - fine grained, possiblefragments 6 MoS,, bleby pyrite 21.40.54 - 41.76 - fine grained, mafic,disseminated to bleby pyrite 2%, carbonaceou41.76 - 42.98 - fine grained, mafic withinterbedded cherty zones, minor amphibolitespossible fragments, MoS, , minor carbonate.42.98 - 44.20 - fine to medium grained,minor chert and carbonate:, bleby pyrite 2%.44.20 - 45.41 - epidotized and bleached,associated with fracturing, minor quartzcarbonate veining, possible fragments.trace pyrite. '

45.41 - 46.63 - grey wacke, brown in color, mediumgrained, massive, minor cross-cutting,carbonate fractures. Angle bedding to core0 42.98 - 75*.

46.63 - -17.85 - mafic sediments, chloritized andbleached. Trace' pyrite.

47,85 - 49.07 - Ditto above to 48.4648.46 - 49.07 - cherty zone and possiblefragments, li pyrite.

48.46 - 62.48 - biotitic mafic sediments withcherty horizons interbedded along withpossible fragments.

SAMPLE

NO.

49681

49682

49683349684

49685

49686

49687

49688

49689

WIDTH METRE5

1.22

1.22

1.22

1.22

1.22

1.22

1.22

1.22

1.22

ASSAY VALUES

Au.

0.07

o.-,:0.21

0.41

4.05/t i c4 .250.48

0.27

0.55

0.21

1

Drill HO.. ^-^ n,m.,, M, "or"se"e , ... ., K. R. Kemo Poo. -^ ^

Lotltu

D.porf

FROM

9

Elt Bearing Fl.untlnn ,

urt Dip Length

TOAll assays grams j tonne

DESCRIPTION

49.07 - 50.29 - fragments, mafic sediments.\\ pyrite. 50.29 - 51.51 - mafic sediments, \ \ pyrite.Si.Sl - 32.73 - bleached cherty zone, maficsediments. Bleby to disseminated pyrite 1.51 52.73 - 53.95 - fragments, minor carbonate,1.51 pyrite. 53.95 - 55.17 - bleached mafic sediments.Locally epidotized, Q.5% pyrite. 55.17 - 56.39 - fragments, mafic sediment.Less than 11 pyrite. 56.39 - 57.60 - biotitic mafic sediment,pyrite less th. 11. 57.60 - 58.83 - biotitic mafic sediment,pyrite less than 11. 58.83 - 60.04 - biotitic mafic sediment,pyrite less than 11. 60.04 - 51.26 - biotitic mafic sediment,pyrite less than 11. 61.26 - 62.48 - biotitic mafic sediment,pyrite less than 11.

62.48 - 79.58 - biotitic mafic sediments, minor localized bleaching, minor interbedded mafic tuff, bedding to core e 72.24 - 75 0 .

79.58 - 83.21 - intermediate to mafic sediments, bleached, epidotized along many cross cutting hairline fractures, commonly carbonate filled.

83.21 - 88.09 - biotitic mafic sediments, bleaching associated with cross-cutting hairline fractures. 86.87 - 87.48 - cherty fragment

SAMPLE

NO.

49690

49691 49692

49693

49694

49695

49696

49697

49698

49699

49700

*

WIDTH dETIES

1.22

1.22 1.22

1.22

1.22

1.22

1.22

1.22

1.22

1.22

1.22

Dot.'Sto

Dot. Flnl

rt id

.h. rf

ASSAY VALUES

Au.

0.55

0.27 0.89

0.27

0.07

0.21

0.07

0.82

0.07

0.27

0.21

4

•V.-: '-'-'Drill H oi* GS-20

Lotltudt,

Deporture

Drilled by

Bearing ..^

Dip ——^—

MorrisetteLogged by

Elevation ,—

Length .-—-—

R. Kemp Pagt

Dote Started

Date Finished

FROM

100. 7C

106.01

9

TO

106.01

118.87


bleby, pyrite less than 21, biotitic/bedding to core e 84.43 - 75 C .

88.09 - 100.70 - mafic biotitic sediments, epidotized, minor fragments.91.74 - 91.93 - solution breccia.

Quartz Feldspar Porphyry

Biotitic Mafic Sediments- Fragments, locally bleached, epidotized and hematized.

END OF HOLE #20

SAMPLE

NO.WIDTH

ASSAY VALUES

Au.

Drm HOI. GS-21 n,m-d o v Morrisette ( ft , oftd b v R. Kemp Poot 1 ' *?l

, .H,,,-. 51 4- OOW a..,,., 180" P, ufltlftn Surface

D. 00 r, u,. 6 * SON B la -45 t mnnth 91.46 metres

FROM

0 3.05

14.21

26.52

33.39

t

TO

3.05 14.21

26.52

33.39

41.40


Casing. Biotitic Mafic Sediment- Localized bleaching and minor quartz carbonate injections/massive/foliation to core axis 3 16.77 - 60 0 .

Interbedded Biotitic Mafic Sediments and Inter mediate to Felsic Tuffs

- Tuffs are thinly bedded and chalk white in appearance. Minor seams of pyrite/localized hematized zones associated with fracturing. Less than 1* pyrite. Minor interbedded amphibolites. Foliation to core axis @ 25.0 - 60 0 .

Fragmental (Mafic)- Cherty fragments hosted in a mafic biotitic groundmass/fragments lenticular in shape, stretched parallel to the foliation. 11 bleby and dissemin ated pyrite. Interbedded biotite bearing mafic sediments occur randomly at 26.92 - 27.74, 30.79 - 31.07, 32.41 - 33.47.

Intermediate Biotite Bearing Sediments- Interbedded with biotitic mafic sediments similar to 14.21 - 26.52, minor interbedded felsic to intermediate tuffs, trace pyrite. Foliation to core axis 0 38.72 - 60*.

SAMPLE

NO.WIDTH

Oott Sfo

Dot* Fin!

Oct. 31/82rf. d

.h.* Nov. 1/84

ASSAY VALUES

Au.

Drill Hole GS-21

•'^•^^jj^

Pag*

Lotltudi

Dtporturt* Din

Pl*uotlnn

l *nqfh

P nt * Started

Dot* Plrl.h.ri

FROM

41.40

51.04

9

TO

51.04

58.69


Biotitic Mafic Sediments- Locally epidotized possible fragments, less than 21 disseminated seams and blebs of pyrite. Zone is slightly magnetic to locally very magnetic, due to grains of magnetite.41.40 - 42.68 - 21 disseminated to bleby pyrite,

tourmaline, magnetic 42.68 - 43.90 - 21 disseminated to bleby pyrite,

tourmaline, magnetic 43.90 - 45.12 - 21 disseminated to bleby pyrite, 45.12 - 46.32 - 2-31 disseminated to bleby pyrite,

magnetic 46.32 - 47.56 - 1.5t disseminated to bleby pyrite 47.56 - 48.78 - 1-1.51 disseminated to bleby pyrite 48.78 - 50.00 - l.S-2.0% disseminated to bleby

pyrite 50.00 - 51.22 - 1.0% pyrite, disseminated to bleby,

magnetic/ fragment s

Mafic Fragmental- Fragments highlighted by lighter colored lentic ular fragments set in a biotitic groundmass. Pyrite found within groundmass less than 2%.51.22 - 52.44 - fragmental, It disseminated pyrite 52.44 - 53.66 - fragmental, l-2t disseminated

pyrite, slightly magnetic 53.66 - 54.88 - fragmental, 1.5t disseminated

pyrite 54.88 - 56.10 - fragmental, 1.01 disseminated

pyrite

SAMPLE

NO.

49047

49048

49049 49050

49226 49227 49228

49229

49230 49231

49232

49233

WIDTHASSAY VALUES

Au.

Tr.

1.10

0.07 0.55

0.27 0.21 0.27

0.07

0.14 0.07

0.07

0.14

Drill Hole GS-21 Pogt

Latitude

Dtporturt

—————————— Rearing

. Olo

Fl.untlnn

Length

,., ,. , ,. Oof* S tart md l iiini , ,, , , ,

..M--, D of * Fln!**i*d . , , , , .,

FROM

58.69

9

TO

91.46


56.10 - 57.32 - fragmentalÔ.5%-1.0% disseminatedpyrite

57.32 - 58.54 - fragmental, 1.01 pyrite

Biotitic Mafic Sediments- Occasional quartz carbonate veins/localizedepidotization/trace to 11 disseminated pyrite/locally slightly magnetic due to pyrrhotite.58.54 - 59.76 - biotitic mafic sediment, trace

pyrite59.76 - 60.97 - biotitic mafic sediment, 11

disseminated to bleby pyrite60.97 - 62.19 - biotitic mafic sediment, trace

pyrite.

END OF HOLE #21

SAMPLE

NO.

49234

49235

49236

49237

49238

WIDTHASSAY VALUES

Au.

0.41

1.03

0.34

0.07

0.96

GEOCHEMICAL REPORTON

THE MOLSON LAKE JOINT VENTURE CLAIM GROUP HEMLO AREA

DISTRICT OF THUNDER BAY ONTARIO

L

Timmins, Ontario By: David R. Bell, B.Se., December 28, 1982 Consulting Geologist

-I . Introduction

11. Property

III Method

IV Geology

V Results

VI Recommendations

INDEX

Page No. l

1-2

2

2-3

3

L

L

Maps: Map No. lMaps: Map No. 2Maps: Map No. 3

Scale: 1"-200'Scale: 1"-400*Scale: 1"-400'

-1-

INTRODUCTION

The geochemical survey stemmed from the results of earlier prospecting during May and June of 1982. Panning

j soils indicated colours in gold leading to a sampling program l of the "B" horizon soils over favourable geological structures.

The first phase of the sampling program was concent rated over an area of sparce outcropping, but shallow overburden. Unusually high values in gold (p.p.b.) were encountered, extending the collection of soils regionally on wider spacing over the rest of the property, restricting the program to geological

l formations interpreted from the summer mapping carried out over the claim group.

The unusual high values encountered on claims TB : 553736 and TB 553737, north of the 0+00 Base Line (Map No.l)

lead to a detailed induced polarization survey, trenching and i later diamond drilling.

The program has been successful in outlining stratigra-^ phic zones anomalous in gold. Depths and types of overburden will

present problems over areas of interest. Within these areas, basal till sampling is recommended.

l II PROPERTY

The claim group covered by the geochemical survey covered a potential four mile east-west trending felsic volcanic environment on the Golden Sceptre claim group (Map No. l and 2),

; . and a potential three mile east south-east trending volcanoganic i sedimentary environment on the Goliath claim group (Map No. 3)

j III METHOD

The"B" horizon was sampled using an auger. Wet swampy areas with humic layers greater than ten feet resulted in a no sample area. The samples were dried and sent to Bell-White Analytical Laboratories Ltd. in Haileybury, Ontario, and analyzed

for gold (p.p.b.).

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Samples were dried and sieved using an 80 mesh screen. The -80 fraction was than used for analysis.

For gold assaying, a ten (10) gram sample was fused and cuppelled using a standard fire assay method. The resulting bead was then dissolved and the concentration read using atomic absorption.

IV GEOLOGY

The Golden Sceptre Resources Ltd. claim group is underlain in whole by an east-west trending assemblage of in terbedded foliated felsic to mafic tnetavolcanic flows, fragmentals and related tuffs. Intercalated with these volcanics and occasionally discontinuous, are a sequence of volcaniclastic sediments consisting mainly of arkosic wackes and thinly laminated argillites.

All of the above units are generally dipping steeply to the north with foliations parallel to bedding and striking from 060 0 NE to 117 e ESE. Minor drag folding in the mapping area suggests that the overall complex is lying within one limb of a homocline, dipping and with probable f.ops to the north.

The volcanic and sedimentary complex is intruded by diabase dykes and a variety of both conformable and discordant feldspar porphyries. Fringes of :he Heron Bay and Cedar Lake Plutons consisting of highly altered felsic to intermediate intrusive rocks, cut all units.

Pyrite has been observed in most of the above units, but concentrations of pyrite anamalously high in gold and molybdenum have been traced in what would appear to be hydrothermally altered felsic pyroclastics.

Overall recrystallization of the volcanic and sedi mentary assemblage indicated that they have undergone an app reciable degree of metamorphism (probably amphibolite facies).

V " RESULTS

A long geochemical anomaly with values greater than 25 o.p.b. An has been traced on the Golden Sceptre claim'group

. - , ^ V ;-from 0+00, west, almost continuously through to L 64 -f 00 W,

1 v y north of the 0+00 Base Line. (Map No. 1) ' s ;

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Samples were collected on 50 foot centres along pre-cut grid lines every 400 feet with fill-in lines over the anomalous areas every 200 feet.

Values as high as 3400 p.p.b. Au. were encountered with many exceeding 100 p.p.b. Au. between Lines 2 W and 28 W. A silicified felsic tuff zone has been identified by napping and trenching. Recent diamond drilling returned many anomalous gold values along this zone. The shallow overburden over the zone would indicate that the higher than normal geochemical re sults are probably due to a more typical "basal till" type environment that the usual "B" type soil horizon.

Care in interpreting anomalous results, elsewhere over the claim groups in the Hemlo area should be taken with depths of overburden in mind.

A gap in collecting samples between Lines 64 W and 80 W exists and should be filled in to follow the continuation of the anomaly located on L 64 W between 5 * DON and 10+00 N.

.Cue to the high percentage of outcropping on claims 528745, 553738, and 553735 (Map No. 1); sampling was restricted to spot checks.

Sampling within the area of Map No. 2 was collected on 100 foot centres along pre-cut grid lines every 1200 feet north-south. Values greater than 25 p.p.b. Au. would indicate that the east-west trend traced on the easterly attached Map No. l exists, but in a more broken nature through to L 200+00 W, 22 +00 N.

Greater depths of overburden were encountered on the Goliath claim group (Map No. 3) resulting in scattered low values over the area covered by the survey. On lines 176+00 E and 186+00 E, between 70+00 S and 84+OOS, several low values in gold p.p.b. do appear. This is over the projected easterly exten sion of the "Corona" zone, hosting gold bearing volcanoganic sediments. VI RECOMMENDATIONS . ' ' ' .

More detailed sampling will be required to bet.ter define the westwardly extension on the Golden Sceptre claim : n

i

group from L 64 W through to L 220+00 W using the existing 400, i x .1 n f

foot grid lines. Sampla intervals should be collected a t :i'ss

liWfifty (50) foot centres.

Analysis for molybdenum, mercury and arsenic should also be considered .

Recent induced polarization surveys have assisted in better defining the anamalous geochem zones and should be used to identify future geochem anomalies.

Due to the depths of overburden on the Goliath group. (Map No. 3), basal till sampling should be considered. An induced polarization survey should be conducted east along the east southeast projection of the mineralized main "Corona" zone.

Respectfully submitted by,

Timmins, Ontario David R. Bell, B.Se., F.G.A.C. December 28, 1982 C nsulting Geologist

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CERTIFICATE

I, David R. Bell, hereby certify:

1. That I am a consulting geologist employed by David R. Bell Geological Services Inc., Suite 6 251 Third Avenue, Timmins, Ontario.

2. That I am a graduate of Carleton University, Ottawa Ontario, with a degree Bachelor of Science (B.Se.) in geology, 1973.

3. That I have been practicing my profession as a geologist continuously since 1973.

A. That I am a Fellow of the Geological Association of Canada (1991), and a Memeber of the Canadian Institute of Mining and Metallurgy.

5. That the author owns directly 30,000 shares of Golden S^ptre Resources Ltd.

C. That this report is based on field work performed by the author and his crews during the calender year of 1982.

Timmins, Ontario. December 28, 1983

David R. Bell, (B.Se.) Consulting Geologist.

SUMMARY REPORT 1982 MOLSON LAKE JOINT VENTURE

HEMLO AREADISTRICT OF THUNDER BAY

ONTARIO

Tlonins, Ontario By: DAVID R. BELL GEOLOGICAL SERVICES INC. January 28, 1983

tnINDEX

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I

II

III

IV

V

VI

VII

VIII

IX

Summary

Introduction

Property

History of Exploration

Geology IV- 1 Regional Geology IV-2 Property IV- 3 Legend IV-4 Recommendations

Geophysics 1. Magnetometer Survey 2. Electromagnetic Surveys 3. Self -Potential Surveys tt. Induced Polarization Surveys

Geochemistry

Diamond Drilling VII-1 Goliath Gold VII-2 Golden Sceptre

Conclusions

Recommendations

IllustrationsProperty S Claim Map Magnetometer Map t EM Maps Self -Potential Maps Trench Maps

Page No.

1

2

2-3

3-4

4 4-5 5-8 8

8 8 8-9 9

9-10

10-11 11-13

13

13-16

in pocket In pocket In pocket In pocket

Appendices"Report on EM and Magnetometer surveys (Goliath section)

Appendix A

INDEX Con't

Appendices con*t

Report on EM and Magnetometer surveys (Golden Sceptre section)

Report on Induced Polarization surveys i Maps

Report on Geochemical Surveys S Maps

Geological Maps

Diamond Drill Logs and Sections

Page No.

Appendix B

Previously submitted

Previously submitted

In Pocket

In Pocket

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SUMMARY

David R. Bell Geological Services Inc., guided anexploration program on the Golden Sceptre Resources Ltd. and Goliath Gold Mines Ltd. properties, in the Hemlo area of northwestern Ontario, from inception in late 1981 to late 1982. Early in the program, the two companies amalgamated their properties and efforts under the "Molson Lake Joint Venture".

The exploration techniques employed on this property (and on others in the area) consisted of:

1. Geological mapping and prospecting2. Magnetic surveys3. Electromagnetic Surveys, both HF and VLF. A. Self-potential surveys5. IP surveys6. Geochemical surveys7. Diamond drilling

As is detailed herein and in earlier reports, some of these techniques were found wanting as guides to gold mineralization, while others have proven to be valuable gold exploration tools.

The Molson Lake Joint Venture exploration program resulted in the discovery of encouraging, but not-yet-economic, areas of gold mineralization on one section of the properties. Diamond drilling down-dip from a discovery on an adjoining property resulted in the delineation of a major gold orebody.

This Report recommends exploration techniques and areas to be explored, based upon the experience of David R. Bell Geological Services Inc. in the Hemlo camp.

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I INTRODUCTION

David R. Bell Geological Services Inc. ("D.R.B.G.S. 11 ) was retained by Golden Sceptre Resources Ltd. and Goliath Gold Mines in 1981 to provide geological consulting and exploration services for their claims adjoining the Corona Resources (now International Corona) gold discovery in Bomby Twp., Thunder Bay Mining Division, Ontario. At that time the properties comprised 58 claims (Goliath) and 98 claims (Golden Sceptre).

Early in 1982, Golden Sceptre and Goliath entered into a joint venture agreement under which the two properties were pooled and expenses shared under the Molson Lake Joint Venture Agreement.

D.R.B.G.S. conducted an expanding program of exploration of the Joint Venture properties, including geophysical and geochemical surveys, geological mapping and diamond drilling during 1982 up to Nov. 21, 1982. Subsequent to that date, Noranda Exploration Co. Ltd. assumed management of the exploration/ development program under another joint venture agreement with the Molson Lake Joint Venture partners.

This Report is a summary of the work performed under the direction of D.R.B.G.S. from inception to November 21, 1982.

II PROPERTY

The Molson Lake Joint Venture ("M.L.J.V.") property lies astride the TransCanada Highway (Ontario Highway 17) north of Lake Superior and more or less equidistant between Sault Ste. Marie and Thunder Bay. Marathon and Manitouwadge are the closest towns. As the intended recipients of this Report are intimately aware of the location, topography and local services it would be redundant to repeat those details herein.

The M.L.J.V. property consisted of 156 Crown-granted mining claims as shown on the plan S legend with the geology maps. It is the writer's understanding that Noranda have over-staked the total property and that the claims may no longer bear the original numbers. Accordingly, this Report will not discuss

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the original claims nor their status as regards assessment work due dates. As at Nov. 21, 1982 the claims were all in good standing to the writer's knowledge.

Ill HISTORY OF EXPLORATION

Gold was first discovered in the area about 1926 when a C.P.R. employee is reported to have found gold within a few hundred ft. of the railway. There is no record of any further activity until 1945, when T. 01 Imann discovered gold on the Ollmann Williams claims near Moose Lake (Now the Lac Minerals property). A few drill holes on this property showed gold mineralization but not in then-economic quantities

Lake Superior Mining Corp. found gold on the property east of the 01Imann-Williams claims about 1947. This discovery was drilled several times in the period 1947-1973 by several companies. This deposit is now the International Corona West Zone.

In 1975 and 1977, the claims west of the 01Imann-Williams (now part of the M.L.J.V. claims) were explored by two companies, but were not drilled.

In 1981, persistant exploration and diamond drilling by Corona Resources, under the direction of D.R.B.G.S., succeeded in locating the Corona East Zone, of significantly higher grade and tonnage than any previous deposit in the area. Subsequently, Teck Corp. took over exploration management of this property.

Long Lac Minerals explored and diamond drilled the Williams-Ollmann claims in the late winter and spring of 1982. In August 1982, that Company announced that they had outlined a deposit of 1.8 million tonnes averaging 0.146 oz. Au./T over an average width of 77.7 ft. to a vertical depth of 492 ft.

The results on the Corona property during 1981, prompted Goliath and Golden Sceptre to explore their properties in earnest. As is detailed elsewhere herein, there followed geological mapping, prospecting, trenching, geochemistry and geophysics in early 1982. Subsequent to formation of the M.L.J.V.,

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diamond drilling conmenced on favourable geology coupled with co-incident geochemical anomalies on the portion of the property west of the Long Lac ground. This program resulted in some encouraging intersection but continuity had not been established when the Long Lac discovery was announced. - It soon became apparent to D. R. B. G. S. personnel that the Long Lac discovery was close to the boundary of the M.L.J.V. property and that a -down-dip extension of the deposit could pass onto the M.L.J.V. property (former Goliath portion).

Two diamond drills were mobilized to commence testing down dip from the Long Lac discovery. In the period Sept. 12 to Nov. 9, 1982, eleven drill holes were completed of which 7 intersected the main ore zone. By Nov. 16, it was postulated that an orebody had been indicated of 6.5 million tons averaging 80 ft. true width and grading 0.261 oz. Au. /T. This zone was fairly well defined on strike but open down dip.

Noranda Exploration assumed direction of the exploration/ development program after Nov. 21, 1982. The writers have had no direct involvement in the program since that date. It is understood that drilling has been continuous and even accelerated and that definition of the orebody has been continued down dip with grades improving with depth.

IV GEOLOGY Regional Geology

LThe regional geology is best described by Muir S

-JT fO. G. S. Report GR-217"Hemlo" 1982) accompanied by Map l ' 2452. The general geology of a broader area is shown on Map j ; 2220 "Manitouwadge-Wawa Sheet" (O.M.N.R. 1972). [ i The interested reader is referred to those publications

! for further detail.

t V& Propertyl l The Molson Lake Joint Venture claim group is underlainv" A) in whole by an east-west trending assemblage of interbedded,t \ foliated felsic to mafic metavolcanic flows, fragmentals and related" i tuffs. Intercalated with these volcanics and occasionally

-5-

disc.scontinuous, are a sequence of volcaniclastic sediments, consisting mainly of arkosic vackes and thinly laminated argillites.

All of the above units are generally dipping steeply to the north with foliations parallel to bedding and striking from 060* NE to 117* ESE. Minor drag folding in the mapping area suggests that the overall complex is lying within one limb of a homocline, dipping and with probable tops to the north.

The volcanic and sedimentary complex is intruded by diabase dykes and a variety of both conformable and discordant feldspar porphyries. Fingers of the Heron Bay and Cedar Lake Plutons, consisting of highly altered felsic to intermediate intrusive rocks, cut all units.

Pyrite has been observed in most of the above units, but concentrations of pyrite anomalously high in gold and molybdenum have been traced in what would appear to be hydrothermally altered felsic pyroclastics.

Overall recrystallization of the volcanic and sedimentary assemblage indicate that they have undergone an appreciable degree of metamorphism (probably amphibolite facies).

IV3 Legend

i The stratigraphic sequence utilized for mapping of the j properties is based on the Ontario Geological Survey Map 2452, : and the Open File Report /5280 by T.L. Muir (1980).

The precise chronological order of the various unitscannot be derived from the field evidence due to the overall lack

1 of good primary structures, but the following units are herein i listed: l l* Mafic Metavolcanics

The unit is generally characterized by its massiveappearance with medium to coarse grained recrystalized amphibole.The high^propertions of recrystalized mafics suggest that this

j unit is a metamorphosed basalt. Highly deformed pillows havebeen noted, but due to the intense stretching, tops were difficultto determine.

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Fine grained schistose mafic units mapped as "IF" with accasional garnets suggest a mafic tuff and in some areas are difficult to distinguish from altered argillaceous sediments.2. Intermediate to Felsic Metavolanics

This unit is by far the most interesting and active assemblage in the area. Map No. 5 was mapped on 200 foot centres and has detailed a felsic assemblage consisting of fragmenCals, tuffs and minor cherts. Samples collected by G.C. Patterson, Resident Geologist, Ontario Geological Survey have indicated the felsic complex has been hydrothermally altered. Volcanoclastic sediments (2c) exhibit highly deformed and stretched fragments making it difficult to determine whether this unit is a fragmental or conglomerate or a combination of both. Patterson (O.G.S) suggests that the source of the fragmentals could be due to slumping in a volcanic environment. The matrix is variable, consisting of sericite and quartz with varying degrees of hydrothermal alteration. In the field, many of the units appear to be homogeneous and lack definable bedding and occasionally exhibit quartz eyes and feldspar phenocrysts. In diamond drill hole sections however, these units suggest a hydrothermally altered tuffite and lapilli appearance. The porphyritic zones appear to be crystal tuffs.

Mineralization is generally in concentrations associated (1-10Z) with the fragmental units and consists of pyrite, trace chalcopyrite, molybdenite, tourmaline, green-mica (fuchsite?) and the occasional wisp of native gold. Assays in silver have been noted, and in some cases suggest that separate silver minerals may be present.

On the Golden Sceptre Section, gold values may be more related to fracture patterns, rather than the stratabound mineralization common to the Goliath-Corona deposits.3. Metasediments

The metasediments and metavolcanics of the mapped area represent, a gradual and often diffuse continuum between purely pryoclastic and purely epiclastic units. The precise identification of the various rock types at the field level was usually a very subjective process.

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The classification of these units have best been described by Muir (1978, O.G.S), and to maintain consistency in mapping his classifications have been noted and used.

According to G.C. Patterson's notes (1982) some of the units are siliceous tuffites with sedimentary features including rip-up clasts and scour channels. Many of the more mafic sediments appear to be pelites indicating a mid-amphibolite grade metamorphism.

Pyrite within these units appears to be coarse, generally barren and secondary. Stringers of sulphides are commonly associated with intense alteration. 85i9 Heron Bay and Cedar Lake Plutons

As indicated earlier, only fringes of these two intrusives hav been mapped. In general they consist of a medium grained granodiorite with roughly equal portions of quartz, feldspar, biotite and hornblende. Occasionally medium grained cubic pyrite has been observed, but very little mineralization within this complex has been noted to date. Future exploration and prospecting should look for zones of alteration and mineralization within these two plutons keeping in mind similar environments in other gold camps. 10. Feldspar Porphyry

This unit is more commonly located north of Highway No. 17 between Botham Lake and east towards Moose Lake. The feldspar porphyry unit is massive, red to dark grey in colour, sub-euhedral pink to white plagioclase phenocrysts, and occasionally 5-101 quartz-eyes in a fine grained siliceous matrix.

Rusty sections north of the highway, southeast of Botham Lake, exhibit disseminated cubic pyrite from which several samples have assayed 300 to 1000 PPB in gold. Clasts of this porphyritic material have been observed (G.C. Patterson, O.G.S.) within the adjacent volcanoclastic sediments returning assays from 300 to 7000 PPB in gold. The structure and stratigraphy in this area is somewhat complex and will require more detailed mapping,

i*

sampling and geophysics. 11. Diabase Intrusive

The diabase dykes generally striking north-south with the exception of a west-north-west striking dyke on Map No. 10,

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A southwest quarter. Fairly good correlation between the magnetometer j highs and the diabase dykes are evident and provide an effective 1 mapping tool.

RecommendationsThere appears to be an increase of hydrothermal activity

in the Map No. 5 area indicating a potential alteration pipe in this area. The flanks of this proposed pipe, especially to the west should be explored in more detail, looking for gold in stratabound and hydrothermal fracture environments.

V GEOPHYSICS

1. Magnetometer SurveyDuring 1981, the total M.L.J.V. properties were surveyed

by magnetometer over 400 -f t. spaced north-south lines. The reports and maps of these surveys were completed and carried out by Prospecting Geophysics of Val D 'Or, Quebec, copies are available from the same .îv^f

In 1982, a more detailed magnetic survey was conducted over a 17 claim portion of the former Golden Sceptre ground and a A claim portion of the former Goliath property. Reports on this work are appended hereto as Appendices A and B. Plans of results are in the pockets hereof.

In general, magnetic surveys have proven to be marginally useful as an aid to geologic mapping but of little benefit in defining areas of interest for gold mineralization.2. -Electromagnetic Surveys

In 1982, a horizontal loop EM survey was conducted over 17 claims of the former Golden Sceptre property and 4 claims of the former Goliath property. Reports on this work are appended hereto as Appendices A and B. Plans of results are in the pockets hereof.

, The E. M. nurveys did not locate any significant conductors and were not found to be diagnostic of either geology nor gold mineralization. 3. Self Potential Surveys

Self Potential surveys were conducted over the same 17 claim (Sceptre) and 4 claim (Goliath) groups over which the

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magnetometer and E.M. surveys were run.Maps of the results of these surveys are included herein

(in pocket).The anomalies indicated do not appear to be coincident with

the geochemical and IP survey results as discussed later in this Report. Nor do they appear to be diagnostic of underlying bedrock nor gold mineralization.

The SP surveys, as applied to the M.L.J.V. properties, do not appear to be a useful tool for gold exploration. However, some additional testing of this system should be applied over known deposits to determine the parameters which may possibly be interpretable as diagnostic of mineralization associated with gold. A. Induced Polarization Surveys

A report and maps on Induced Polarization Surveys has been prepared previously and forwarded to the recipients of this Report. (D.R. Bell Dec. 1982). Therefore, it is not reproduced herewith.

The IP method, developed by Newmont Mines utilizing time domain and dipole-dipole array with short "a" spacings has been found useful in outlining finely disseminated mineralization and alteration in the Hemlo camp.

An extension of this type of IP surveys is recommended as a useful guide to diamond drilling of '^©logically-favourable horizons.

VI GEOCHEMISTRY

D.R. Bell has reported on the results of geochemical sampling (December 1982) over portions of the M.L.J.V. property. That report has been forwarded to recipients of this report and is not reproduced herein.

Analysis for gold was the only element utilized in the areas of shallow overburden over which the surveys were conducted.

f It is believed that the sampling was, in effect, almost that of ! basal till sampling. In areas of deeper (plus 10 ft.) overburden,

reverse-circulation basal till sampling is recommended.

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It is also suggested that in areas of greater overburden and/or less rock exposure, analysis for molybdenum, arsenic antimony and mercury, as well as gold, could be useful as indicators of gold mineralization. The mobility of mercury could reduce its usefulIness in this regard.

It is recommended herein that the geochemical surveys be extended and used in conjunction with IP surveys as the primary guides to drilling of geologically favourable horizons.

VII DIAMOND DRILLING

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DDK. NO.

VII-1 Goliath SectionDiamond Drill Logs and sections for holes GG-1 to GG-11,

directed by D.R.B.G.S., are appended hereto. Holes GG-12 and GG-13 were spotted and in progress at the time of the Noranda agreement, but results of same have not been made available for this report.

Results of this drill program, which probed the down dip extension of the Long Lac Minerals' discovery, are summarized as follows:

RESULTS. OZ. AU./T Diabase, did not reach ore zone 0.254/88.5 ft. True width 0.314/68 ft. True width Headed off property, not to ore zone 0.245/5.25 ft. Fringe of zone Cut 0.237/113.2 ft. True width 0.19/95.1 ft. True width 0.148/5.9 ft. Fringe of Zone 0.272/72.2 ft. True width 0.212/69 ft. True width O) Cut 0.386/65.6 ft. True width

GG-1GG-2GG-3GG-4GG-5GG-6GG-7GG-8GG-9

GG-10GG-11

Total Footage 14.947

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From this very limited drilling, it was estimated that some 6.5 million tons of ore grading 0.261 oz. Au./T had been drill-indicated, with all assays over 1.0 oz. cut to 1.0 oz. The average true width of the zone was 80 ft. A strike length of 650 ft. appeared to have been fairly-well defined but the deposit was unexplored at depth. The tonnage was estimated to be 5.400 tons per vertical foot or 4300 tons per ft. on dip. Significant assays in molybdenite, averaging 2-3 pounds per ton, accompany the gold.

Drilling of this remarkable gold deposit is continuing to date. The authors are not conversant with recent results and are unable to express an opinion on current tonnages and grades.

VII-2 GOLDEN SCEPTRE SECTIONDiamond drill logs and sections for holes GS-1 to GS-21,

as directed by D.R.B.G.S., are appended hereto.Results of this drilling, which probed several different

features of the property are summarized as follows:DDH NO. SECTION DEPTH, FT. RESULTS OZ. AU./T

WIDTH FT.

coupled with coincident IP anomallyGS-1 GS-2 GS-3

GS-4

GS-5

GS-6

GS-11 GS-7

GS-8

1+OOW 1+OOW 2+OOW

2+OOW

3+OOW

3+OOW

3+OOW 4+OOW

4+OOWGS-19 lower

section 4+OOWSub-total

ificant goldanomally151200150

250 Cut

150

250

490160

250

10003051

values in surface trenches

0.95/3. 6 j do not appear0.50/3.2J to be related.0.43/5.0 0.07/8.2 0.14/3.00.336/21.0

3.36/1.6 1 0.08/1.6 0.30/1.60.67/3.0 0.10/3.20.09/24.60.11/4.9 0.10/3.20.17/8.2

0.37/36.0

i Continuity not established

No apparent continuity

Could possiblyline up

DDH. NO. SECTION

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DEPTH FT. RESULTS OZ. AU./T WIDTH FT.

GS-9 5+OOW

l GS-10 5+OOWij GS-12 8+OOWi TOTAL

j B. Sceptre North Zone-over 5600 ft. strike

GS-13 12+OOW GS-14 12+OOWGS-15 16+OOWGS-18 16+OOWGS-16 20+OOWGS-17 20+OOW

TOTAL

C. Sceptre North Zone,IP anomally stronger

GS-20 48+OOWGS-21 51+OOW

i TOTAL

250

250

4504001

con incident IP dlength, open to w*

450 5004005504004002700

West- coincidentthan usual.

390300690

0.09/3.2;0.16/3.0; No apparent0.10/2.0 continuity 6.54/0.9No signifigant assay

Geochemical anomaliesJSt

0.09M.9] No co-relation 0.09/6.7!No signifigant assaysNo signifigant assaysNo signifigant assays0.09/2.0

IP d Geochemical anomalies,

0.12/4.0No signifigant assays

TOTAL A, B 7,391

Diamond drilling to-date on the former Golden Sceptre property has failed to reveal any continuous body of economic gold mineralization.

^ Several signifigant intersections in the "South Zone" require further work (see "Recommendations"). It is noted that the close association of gold with molybdenite in the Goliath- Corona deposits is not, so-far, evident in the Golden Sceptre intersections.

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The "North Zone" has so far proven unproductive. However this Zone should be drilled-off in a regular pattern and the IP and geochemistry surveys should be extended westward, (see also "Recommendations").

VIII CONCLUSIONS

A variety of exploration technicques have been utilized in the Hemlo camp to explore for the apparently stratabound pyritic gold deposits of the Goliath-Long Lac-Corona type. These techniques have included geological and structural mapping, prospecting, magnetic-electromagnetic-S.P. - IP surveys and geochemistry. To-date, D.R.B.G.S. have found magnetic, electromagnetic: (both HF d VLF) and S.P. surveys to be of little use.

Geological mapping and prospecting are the foundation upon which a sound exploration program can be based. In the camp so far, it has been found, that felsic volcanics and pyroclastics in association mafic to intermediate sediments are required for the occurrence of ore.

After definition of favourable host rocks, induced j polarization and geochemistry have been found useful in delineatingl

j drill targets.l There is a rather remarkable increase in grade with; depth in the Long Lac-Goliath deposit, e.g. the Long Lac deposit

averages approximately 0.15 oz. Au./T. (to 500 ft. depth) while 1 the deeper drilling suggest that a grade of 0.30 oz. Au./T is common : . at 2000 ft.. This same tendency of increased grade with depth is l also apparent, albeit to a less marked degree, in the Corona j deposit. Appreciation of this factor is important in design of an ! exploration program in the camp. j The following Recommendations are based on the abovet

considerations and other results as noted in this report.

IX RECOMMENDATIONS

1. Induced Polarization SurveysThe results of trial induced polarization surveys over

a portion of the former Golden Sceptre ground are covered in an

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earlier report. (D.R.Bell, Dec. 1982).This Report recommends that all of the M.L.J.V.

property be surveyed using this method. The reader is referred to that report for details. The survey coverage might be restricted to those areas underlain by more favourable geology as outlined on the maps included herewith.

In particular the Golden Sceptre "North Zone" and "New North" Geochem (line 64W, 10+OON) should be extended westward at 200ft. spacings.2. Geochemical Surveys

The results of geochemical surveys on the former Golden Sceptre property are covered in an earlier Report (D.R. Bell, Dec. 1982

That report recommends:a) detailed smapling on lines 64W to 220W to extend the

previously located geochemical anomally north of the base line.b) basal till sampling, using reverse circulation drills,

on the former Goliath property due to the greater depths of over burden in that area. It is suggested that the area of basal till sampling might be guided by the results of IP surveys in the area.

The reader is referred to the earlier report for details.It is also recommended that whole rock geochemistry of

drill cores as well as surface rock by commenced as a guide to regional as well as on property future exploration. A preliminary start on this project had been made on behalf of the M.L.J.V. by D.R.B.G.S., however the work was in conjunction with another mining company and the results have not been made available at this time. It seems probable to the writers that, in light of the volumes of gold which have been concentrated in the Goliath deposit, that there should be diagnostic increases and decreases in some of the rock forming minerals as one approaches and retreats from the ore deposit.3. Diamond Drilling

3-1 Goliath Sectiona) As is so obvious as to be almost redundant, the Goliath

deposit should be expanded by deep drilling to indicate its ultimate tonnage potential as a guide to production rate.

-15-

Similarily, fill-in drilling and wedging of deep holes is required as a guide to future development design and mining, as well as to improve the confidence level of ore reserve tonnages and grade.

At some time, the parallel sericitic horizon 4-500 feet south of the zone currently being tested should be examined by extending existing holes of the above program.

b) Exploratory drill-testing of the "Hemlo-Corona Horizon" should be extended along the north boundary of the International Corona property at 500 ft. intervals. While this program will, at the eastern end, result in quite deep holes (3000 ft. ±), the signifigant increase in grade with depth of the Goliath deposit warrants testing this horizon in a routine fashion.

c) The eastern extension of the "Hemlo-Corona Horizon", southeast of the International Corona property, should be tested by diamond drilling in a regular pattern. Based upon the known strike lengths of the Goliath and Corona deposits, a spacing of 500 ft. between holes would provide a reasonable probability of detecting signifigant mineralization. East of the eastern boundary of the Corona property, the holes will be shorter than in (b) above and can be guided, at least in part, by the results of the IP and geochemical surveys as in l fc 2 above.

3-II Golden Sceptre Sectiona) Limited testing of the Highway Zone at depth is

warranted on a few sections to test for improved grades and widths. This program should be guided by completion of IP surveys of the zone but some testing is warranted even if the surveys are not positive.

b) The moderately encouraging values in GS-20 (.121 oz. Au./T over 4 ft.) should be followed up by a deeper hole on this section.

c) The "North Zone" coincident I.P. and Geochemical anomally, should be drilled at 400 ft. centres on a routine pattern west of line 20-fOOW every third section being drilled by two holes, one shallow and one deep. This program would be extended west of 56+OOW should the anomallies be found to continue in that direction.

L

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d) The Golden Sceptre North Zone (lines 12W to 0+OOW, just north of the Base Line) coincident IP and Geochemical anomalies, produced a number of anomouslly high gold assays in DDK's GS-13, 14 and 19 (upper section). Some additional assays in GS-14 would appear warranted, particularily at depth. This north zone should be drilled on 200 ft. centres and at depth in the section 10W to 0+OOW.

e) The Sceptre "South Zone, line 5W to OW south of the Base Line, appears to be characterized by narrow ore-grade intersections in the shallower holes with a possible tendency to wider intersections at depth, (eg GS-19 i 11) GS-4 produced a signifigant intersection at a shallower elevation. The trend of better values at depth is particularily evident on section line 4+OOW although GS-19 should be surveyed in order to determine the precise location of the deep intersection.

Re-logging of the core from holes in this area may assist in rationalizing the geology and structure from section to section.

More drilling, particularily at. depth to follow-up the deeper intersections in GS-19, is recommended for the South Zone. During the program, consideration should be given to the possibility that gold mineralization in this area may be fracture-controlled. 4. Rock-mechanic (Compressibility) tests should be conducted on representative samples of drill-core from the hanging wall, orebody and footwall. The writers believe that the hangingwall and ore rocks should not cause unusual problems but are somewhat concerned about the stability of the footwall in light of the signifigant amounts of sericitic schist present.

It is recommended that a pilot hole be drilled to the total projected depth of the future shaft.

It is also recommended, again due to concern about the footwall schists, that test stopes be opened and allowed to stand unsupported prior to a final commitment to any mining method using large open stopes.

RespexftfulNly submitted,DAVID R. BELLEGtLOGICAL SERVICES INC.

Timmins, Ontario. David R. Bell, B.Se. January 28, 1983. Consulting Geologist.

••REPORT ON EM17L AND

MAGNETOMETER SURVEYS

rGOLIATH GOLD hINES LTD.

HEMLO PROPERTY

THUNDER BAY MINING DIVISION

July 12 1982 Timmins, Ontario

Bruce lAirhamProject GeologistD.R.Bell Geological Services Inc

l*r*l i

-i-

INTRODUCTION

L L

A magnetometer survey of the Goliath Gold Mines property near Hemlo was done during 1981 by Prospecting Geophysics Ltd. using north-south grid lines at 400 foot intervals. As a result of this work it was decided that a more detailed magnetic survey and some HLEM profiling were required on the four claims covered by this report.

The additional line-cutting, rechaining, and geophysical surveys were carried out by Mid-Canada Exploration Services Ltd. of suite 8-251 Third Avenue Timmins, Ontario, during Feburary 1982, Bell Geological Services of Box 1250, Timmins, Ontario, was commissioned by Goliath Gold Mines to write this report.

PROPERTY LOCATION AND ACCESS

The Goliath Gold Mines property consists of 58 contiguous unpatented mineral claims located in the Molson Lake Area in the Thunder Bay and Sault Ste. Marie Mining Divisions. The work covered by this report was done on a group of four claims immediately east of the Corona Resources gold property. The claims covered by this report are: TB576869, TB576870, TB576878, TB576887.The recorded holder of the claims is R.A. Schiralli, Suite 420 181 University Avenue, Toronto, Ontario.

Access to this portion of the Goliath Gold Mines Ltd. property is via a railway access road which leaves Highway 17 at a point approximately two miles west of the Junction of Highway 614.

GEOLOGY

* The geology of the property is described in a report by Thomas Skimming, P. Eng. dated August 20, 1981, The geology of the area covered in this report is illustrated on Map 2439

-2-

published by the Ministry of Natural Resources of Ontario. The area covered by these detailed geophysical surveys is currently being mapped using the existing north-south grid lines for control. Since a full report covering the geological survey will be submitted in the near future no further mention of the geology is made at this time.

SURVEY PROCEDURE AND INSTRUMENTS

Approximately 2.5 miles of additional line cutting was done to establish grid lines at 200 foot intervals across the four claims. Magnetometer and EM17L readings were taken at 100 foot intervals along the north-south grid lines.

A Barringer GM-122 proton magnetometer was used for the magnetic survey. A magnetometer base station was established at L 128E 40S and was assigned a value of 59620 gammas. Loops were read and regular tie-ins made to the base stations at intervals generally less than one hour apart. From this data a graphical diurnal correction was applied to all data.

A Geonics EM17L Horizontal loop system using a 400 foot coil separation was employed for the HLEM survey. In phase and guadrature readings were taken at each station.

Copies of the instruments' specifications accompany this report. (appendix).

SURVEY RESULTS

The data obtained from the magnetometer survey more or less correlates with the previous work done by Prospecting Geophysics Ltd.. Better definition of the southeast trending magnetic anomaly was obtained using the 200 foot spaced lines. This magnetic trend appears to be offset between lines 134E and 136 El with the east side being shifted south. Geological mapping to date indicates the cause of this anomaly to be a southeast trending diabase dyke. The magnetic anomaly which

.

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-3-

roughly parallels line 164E from 52S to 63S is most likely due Co a north trending diabase dyke.

At this point it is difficult to say if the areas which gave background readings which are .in the range of 750 gammas to 850 gammas are underlain entirely by metasediments or a combination of metasediments and felsic to intermediate volcaniclastics

The EM17L horizontal loop survey failed to delineate any real bedrock conductors.

CONCLUSIONS AND RECOMMENDATIONS

L

No further work is recommended until the geological mapping program has been completed and fully evaluated.


Bruce DurhamProject GeologistBell Geological Services Inc.

tfe

REPORT ON EM17L AND

MAGNETOMETER SURVEYS

l

GOLDEN SCEPTRE RESOURCES LTD.

HEMLO PROPERTY

THUNDER BAY MINING DIVISION

July 12, 1982 Timmins, Ontario

By: Bruce DurhamProject Geologist David R. Bell Geological Services Inc.

t i[J -1-INTRODUCTION

A magnetometer survey of the Golden Sceptre Resources Ltd. property near Hemlo was done during 1981 by Prospecting Geophysics Ltd. using north-south grid lines at 400 foot intervals. As a result of this work it was decided that a more detailed magnetic survey and some HLEM profiling were required on the seventeen (17) claims covered in this report.

The additional linecutting, rechaining, and magnetometer and EM17L surveys were carried out by Mid-Canada Exploration Services Ltd. of Suite 8- 251 Third Avenue Timmins, Ontario, during February and March 1982. Bell Geological Services of Box 1250 Timmins, Ontario was commissioned by Golden Sceptre Resources Ltd. to write this report.

PROPERTY LOCATION AND ACCESS

n

L

L

The Golden Sceptre property consists of 98 contiguous unpatented mineral claims located in the Molson Lake Area in the Thunder Bay and Sault Ste. Marie Mining Divisions. The work covered by this report was done on a group of seventeen claims on the eastern portion of the property immediately north of Highway 17. The claims covered by the current surveys are TB 528742 to 528748 inclusive, TB553735 to 553738 inclusive, TB576669, TB576674, TB576675, TB576680, TB576681, TB 576686. R.A. Schiralli of 420-181 University Avenue, Toronto, Ontario, is the recorded holder of all claims. Highway 17 cuts through the south tier of claims approximately four miles west of the junction with Highway 614.

GEOLOGY

The geology of the property is described in a report by Thomas Skimming, P. Eng., dated August 20, 1981. The geology of the property and surrounding area is shown on map 2439 published by the Ministry of Natural Resources of Ontario. The

i;-2-

area covered by these detailed geophysical surveys is currently being mapped using the existing north-south grid lines for control. Since a full report covdring the geological survey will be submitted in the near future no further mention of the geology is made at this time.

SURVEY PROCEDURE AND INSTRUMENTS

The surveys were conducted over rechained summer grid lines, which had been established at 400 foot spacings and new in between lines giving survey coverage at 200 foot intervals. Magnetometer and EM17L readings were taken at 100 foot intervals along the north-south grid lines.

A Geonics EM17L Horizontal loop system using a 200 foot coil separation was used for the HEM survey. In phase and guadrature were read at each station.

A Barringer GM-122 proton magnetometer was used for the magnetic survey.

A magnetometer base station was established at BLO, LO and was assigned a value of 59620 gammas. Loops were made and regular tie-ins made to the base stations at intervals generally less than one hour apart. From this data a graphical diurnal correction was applied to all data.

Copies of the instruments' specifications accompany this report. (appendix).

SURVEY RESULTS

The data obtained from the magnetometer survey more or less correllates with the previous work done by Prospecting Geophysics Ltd., with somewhat better continuity from line to line particularly along the south limit (Hwy. 17) of the detailed area. The closer line spacing gave better resolution of the strong magnetic anomaly on claims TB528742 and TB 528743. Diabase dykes (north trending) appear to be the cause of narrow

L

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-3-

anomalies parrallel to the grid lines on L50W from 3S to 8N, L3W from 21S to 15S, and L6W from 5S to 7N. Background readings in the area range from 59650 gammas to 59750 gammas. The widespread background readings appear to conincide with felsic to intermediate volcanic flows and tuffs as well as a variety pelitic, wacke and arkosic metasediments which often contain volcanic debris. The magnetic anomaly along the south limit of the detailed area appears to be directly associated with a chloritic (amphibolitized) group of volcanic flows and/or tuffs. Some portions of the northern edge of this anomaly may be cau?ed by thin magnetite band within thinly bedded sediments ne?.r the mafic volcanic contact.

The highly anomalous readings across claims TB5287A2 and TB528743 appear to be due to abnormal amounts of magnetite within mafic (amphibolitized) volcanics.

The north trending anomalies are due to the presence of late Precambrian diabase dykes.

The EM17L survey failed to delineate any real bedrock conductors.

CONCLUSIONS AND RECOMMENDATIONS

As previously recommended, a geological survey is currently being done over this area. Some geochemical sampling is also in progress as is some mechanical stripping. If the results of this work are encouraging a diamond drill program will be recommended.


Bruce Durham,Project Geologist,Bell Geological Services Inc.

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1984 06 21 Your Flits 164-84 Our F1lt:2.672l

Mrs. H.V. St. JulasMining RecorderMinistry of Natural Resources875 Queen Street CastP.O. Box 669Sault Ste. Marie, OntarioP6A 5N2

Dear Madam

RE t Notice of Intent dated July 24, 1984.Geological Survey on Mining Claim SSM 607770 et al 1n the Tovmship of Brothers.

The assessment work credits, as listed with the above mentioned Notice of Intent, have been approved as of the above date.

Please Inform the recorded holder of these mining claims and so Indicate on your records.

Yours sincerely,

S.E. YundtDirectorLand Management Branch

Whitney Block, Rooa 6643Queen's ParkToronto, OntarioK7A 1H3Phone: (416) 965-6918

S. Hurst:se

cci Lac Minerals Limited P.O. Box 5800 Manitouwadge* Ontario POT 2CO

ccs Mr. 6.H. FergusonMining i Lands Commissioner Toronto, Ontario

ccs Resident GeologistSault Ste. Marie, Ontario

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32

0

6 ±00 S 54-005 44-00 S

64-20S 5-J-75 S 4 4 90S

SOUTH NORTH

S.S. 1-45*

o.:

G.S 2 -75'

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0.89

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42c M O-0023*DAVID R. BELL GEOLOGICAL SERVICES INC,

GOLIATH-GOLDEN SCEPTRE JOINT VENTURE

VERTICAL SECTION, looking west

LINE ItOOW

D.DH G S 182 *SCALE 1:250 OCTOBER, 1982

42C12NW8705 42C12NW0023 BOMBY 330

SOUTH NORTH

7+OO S5+OOS

4+90 S 4KJOS

E0H. 457meters G.S-3

E.O.H. 76.22 meters GiS.-4

Z K) U) -0023 /5

DAVID R. BELL GEOLOGICAL SERVICES LTD.



D.D.H. GS-3a 4 Line 2tOO

SCALE OCTOBER, 1982

BOUBY 340

SOUTH 5+OOS44-DOS 34-OOS

NORTH

3d

TR10.11

E.O.H. 45.72m GS-5

GS 6 -75 GS 11

.69 EQH. 76.20m GS-6

GS-11 E.O.Kl3716m

42C12NW870S BOMBY 350



VERTICAL SECTION, looking westL3 t OOW

OS D.D.H.,5,6 a II

SCALE: t-250 OCTOBER , 1 982

54-O

OS

44-O

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E.OH. (J, 76.2 meters GS. -9(-45*)

E.O.H. Q 76.2 meters GS.-10(-75*)

42C/I2DAVID R. BELL GEOLOGICAL SERVICES LTD.



D.D.H. GS-9aiO Line StOOW

*SCALE 1 = 250 OCTOBER, 1 982

42C12NWS735 BOMBY 370

SOUTH NORTH

OOS 7+00 S 6f OOS 5-1-00 S 4 + 00 S GS 12

3H-OOS

EQH l37.Ometers OS-12

in molt........42C12NW8705 42C12NW8023 BOMBY

380

42 C 12. WU) -0025 * 19DAVID R. BELL GEOLOGICAL SERVICES LTD.


VERTICAL SECTION looking west

D D. H. GS- 12 Line StOOW

SCALE 1=350 OCTOBER, 1982

SOUTH

3+OOS 24OOS 14OON

GS 14

NORTH ^

5+OON

EO.H.(a, 1 37.4 meters G.S. 13

EP.H. @, 152.4 meters G.S. 14

l42C12NW8705 42C12NW®a23 BOMBY 390

42 C/ 12 K)lO - 0023*20DAVID R. BELL GEOLOGICAL SERVICES LTD.


VERTICAL SECTION-looking west

D.D.H. GS-l3ai4Line IZtQOW

SCALE h500

3 W A

™ PK v^ l /^ f* f\^*OCTOBER; 1982

14-DON 240ON 34-OON 44-OON 54-OON 64-00 N

NORTHSOUTH

GS15 G6 18

24a

EjQH. 121.9m GS-15

GS-18EQH. 1677m

420 * 21DAVID R. BELL GEOLOGICAL SERVICES INC


VERTICAL SECTION, looking westDD.H GS 1 5 S 18 f

LINE 16+-OOW

SCALE l 250 OCTOBER, 1982

400

2+OON 3 + OON 4* OON 5 + OON

SOUTH NORTH

GS16 GS 17

0.55.82

1.580.55

0.820.62

E.O.H. 121.9m GS 17

EO.H. 121.9m GS 16

42 C/l 2 K)U)-0023DAVID R. BELL GEOLOGICAL SERVICES INC



LINE 20-l- OOWD.D.H. G. s. is a 17

SCALE |:250 OCTOBER, I982

42C12NW8705BOMBY

5 4-00 N 6+0 ON 64- SON

SOUTH NORTH

GS 20

E.O.H. 116.67 m GS 20

4-2C/I2WOJ-O023DAVID R. BELL GEOLOGICAL SERVICES INC



LINE 48-4-OOW

DD.H. GS. 20

SCALE 1:250 OCTOBER, I982

42C12NW8705 42C12NW0023 BOMBY 420

4IOON 5J-OON 64-OON 6+50N

SOUTH

E.O. H. 91.46m GS 21

NORTH

GS 21

42 C// 2 - 0023 *2-tDAVID R. BELL GEOLOGICAL SERVICES INC



LINE 5I +OOW

D.D.H. GS 2!

SCALE h250 OCTOBER, 1982

42C12NW8705 42C12NWCB23 80M0Y 430

f

12000 N (CORONA-ORIGIN )

B

CO-ORDINATES ARE RELATIVE TO CORONA RESOURCES POINT OF ORIGIN MO .000 N , 10 .000 E ) AT N 0 2-TB 32159

BASE LINE AND GRID LINE MEASUREMENTS ARE SHOWN IN 'MET R fc] BUT PLOTTED IN T' M'PERJAJL]( 50 m : 164.04 FT.)

ELEVATIONS ARE REFERRED TO CORONA ORIGIN (N 0 2-TB 32159 ELEV. IO48.59'. SURVEY INFORMATION TO SEPTEMBER 15,1983'TJWILL HOLE

Stationer Drill Hole

IB 2-32159Corona Origin SSIB 1 -32159

1000Sta. D.H. Sta. D.H. D.H. Sta. D.H. D.H. Sta. D.H. D.H.

#W221001#17-3AIBA'WIS

1002BA1003#W21 C

Baseline

1 + OON1 + 50N 2+OON 2+OON2 + OON 2 + OON 1 + 50N 1 + 50N 1 + 50N1 + 50N 1+50N2 + 50N 2+50N 2+50N 2 + 50N 2 + 50N2 + 50N 2+50N 2+50N3 + OON 3 * 5 O K 3 + 50N 5 + 50N 3 + 50N 3+50N 3+50N 3 + 50N 3 + 50N

0+50E 1 + OOE 0+50W 0+50W 0+50E 1 + OOE 1 + 50E 2+OOE

0+50W 0+50E 1+OOE 1 + 50E 2+OOE 2+50E 3 + OOE

3 + 5. 0 f."4+00 N 4+-OON4+50N 4+50N4 + 50N 4+50N 4 + 50N 4+ 50 N 4+50N 4 + 50NGG #1GG 4GGGGGGGGGGGG

0+50W 0+50E 1+OOE 1+50E 2 + OOE2 + 50E3 + OOE 3+50E4 + OOE

1+OOE 0+50E 1+OOE 1+50E2 + OOE 2+50E 3+OOE3 + 50E4 + OOE

#3#4#5#6#7#8

MOLSON LAKE JOINT VENTURE

BOMBY TOWNSHIP

Northing Ft.

1010101010101010.10.10,10,10,10,

,000,842782763

.770666810750723790736786782

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, 138,302,467.467.467.467.302,302,302..302..302.,631 ..631 ..631 ..631 ..631 .631 .631 .631 .795.959.959.959.959.959.959.959.959.959.959.123.123.287.287.287.287.287.287.287.287.325.307.177.281 .301 .280.303.306.

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Easting Ft.

10,000.0009,925.0359,410.2789,453.7139,308.7789,313.6689,306.2049,140.6399,161 .4169,159.2519,021 .2739,009.2649,024.941

99999999999999999

10109,9,9,9,9,9,9,

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C 'OP t it C ASING G L - -iftOUNO Lf VE L

MOLSON LAKE JOINT VENTUREPLAN SHOWING

BASE LINE AND GRID LINES DRILL HOLE LOCATIONS S ELEVATIONS

SCALE - 1 INCH iOO FEET

H SUTCLIFFE LIMITEDCONSULTING ENGINEERS -ONTARIO LAND SURVEYORS

NBW LI3Hf*RO ONTAHIO

42C12NW87K5 42C12NW0023 BOMBY ocTo*rn e ,i9a2 122* 1229 PL AH" CJlrtl /*5401 C

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80189324022367

10201045105210261004105210661070.661068.6110691072101810161002.191033.571054 .601066107910741074107710761006104910181043.831058.731071 .051073107210821081

10061010100710131005

91776604528934

29834303

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1047.661046.74

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100810141006101410061046

8251076583165

* 25

REVISED- NOVEMBER 13,1982

ool

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DAVID RBELL GEOLOGICAL SERVICES INC.GOLDEN GIANT

DRILL PLAN

SCALE 1.1250 MARCH. 1983

42C12NW8705 42C12NW0023 BOMBY 450

o * sow 0+ 00 O+ 50 E 1 -l- OOE 1 -H 50 E 2 -f OOE 2 -h 50E 3 -t- OOE 50E

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Axis ofCORONA RESOURCES INC

Gold Zone

420/2100-0023*27*GOH Goliath Gold M ines L td.Gold M ines L td

ICR Internationat Corona Resources L td LLE Long Lac E xploration L td.

SOW 00 0+ 5OE OOE 1+ 50E 24- OOE Z+ 5OE OOE 3* 50E

DAVID R. BELL GEOLOGICAL SERVICES LTD

GOLIATH GOLD MINES LTD

PLAN OF SURFACE DIAMOND

DRILL HOLE LAYOUT

SCALE: l: I250 OCTOBER , I982

12C12NWS705 42C12NW0023 BOMBV

46027

42 C/l 2MU)-QQZ3*28DAVID R. BELL GEOLOGICAL SERVICES LTD.


GOLIATH CLAIM N 0 TB 5 76849

PLAN VIEW . 350 Meter Level

Projection of Diamond Drill Intersections to th350 Meter ElevationAssays in Gold, ounces per ton

SCALE l 50 OCTOBER, 1982

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GOLIATH—GOLDEN SCEPTRE JOINT VENTURE

VERTICAL SECTION- looking west LINE 0 +I5E

SCALE |:500 OCTOBER, I982

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W 12-45* W l -45* Elev. 326m W13 -60* Elev. 326m

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200

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32DAVID R BELL GEOLOGICAL SERVICES LTD.


VERTICAL SECTION - looking westLINE I 4-OOE f

SCALE h 500 OCTOBER , I982

III II PI* M . -. ..-^

42CI2NW87B5 42CI2NW0ia23 BOMBY 510

100

-45* El*v. 321

4-2C/I2NIO-0023DAVID R. BELL GEOLOGICAL SERVICES LTD.


VERTICAL SECTION, looking westf

LINE 0-I-50W

SCALE I'SOO OCTOBER, 1982

42C12NW8705 42C12NW0023 BOMBY520

o oro

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42CI2NW8785BOMBY

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DAVID R. BELL GEOLOGICAL SERVICES INC.



LINE 1+50 E

SCALE 1=500 OCTOBER, 1982

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100

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DAVID R. BELL GEOLOGICAL SERVICES INC



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HEMLO PROPERTY-BOMBY TWP

DISTRICT OF THUNDER BAY, ONTARIO

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TRENCH CONTINUES 300 FEET FURTHER

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-45* Clcv. 1049'

42C/I2 K) 10-0023DAVID R. BELL GEOLOGICAL SERVICES LTD


VERTICAL SECTION

04

'.

-06 T

06

OB

oe 110

08 l

08 l

l

O8 ;

-O6-

--06

"06

06

06-04

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O4

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"04

••06

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-OB

412

r 06i f04

--O8

5] t

TIE LINE 15 t 00 N

BASE LINE OtOO

CEDAR CREEK

BASE LINE 6 f 00 S

DAVID R. BELL GEOLOGICAL SERVICES INCMOLSON LAKE JOINT VENTURE

GEOCHEMICAL SURVEYSOIL SAMPLING

(B) HORIZON

Values in gold - pp. b

DATE DECEMBER, 1982 SCALE l '^ 400 CREEK or STREAM

4-2 C/12 W U) -0023

Documents

42C12NW8705.pdf - Geology Ontario