42E13NW8352 63.3860 CASTLEWOOD LAKE 010

GEOLOGICAL REPORT

ON

ONAMAN GROUP OF CLAIMS

ONAMAN LAKE, JELLICOE AREA

THUNDER BAY MINING DIVISION

December, 1972 H. Petak

INTRODUCTION

A geological survey was conducted on September 7, 1972 by the

writer on four (4) contiguous claims called the Onaman Group, held by

Am ax Exploration, Inc. The purpose of the survey was a detailed

geological napping of the property to assist in checking out an AEM

conductor and ground EM conductors. The ground EM conductors were

located by a Radetn VI. P survey executed by Araax prior to the geologicalf - i

survey.

LOCATION AND ACCESS

The property is located on the south end of Onaman Lake, about

17 miles north of Jellicoe, NW Ontario. (see accompanying map) Access

is provided by aircraft only. Ontario Northern Airways Ltd. with two

seaplane bases located several miles west of Jellicoe, offer charter

services with Cessna 180 and Reaver aircraft. Minimum charter rate for

Beaver is 520/25 rolled.

PROPERTY

The Onaman Group of claims consists of four (4) unsurveyed contiguous

claims numbered 3350^9, 335060, 335061 and 335062. Comprising an area of

approximately 160 acres or 0.2S aq, miles, this claim group was staked

and recorded in April 1972, and is since owned by Amax Exploration, Inc.,

Suite 1302, 7 King St. East, Toronto l, Ontario. The property is covered by

claim map M-1850.

PREVIOUS WORK

Other than a very old claim post, there is no indication of any

ground work prior to the ground acquisition by Amax Exploration, and there

is no assessment work on file at the Mining Recorder's office.

2.

After staking In April 1^72, Amax Exploration completed 19,400 ft.

(3.5 Hnc miles') o*" 1inecuttlng (Hnc spacing is 400') and the same

amount of ground marnetics and Radem Survey. Geophysics was followed

up by a geochemical soil sampling program of which results are not yet

on hand. Geophysical readings or soil samples respectively w*re generally

taken on 100' station*) and In some cases, on 50" stations.

GENSRAL GaOLOGY

The property IB located In a belt of chiefly volcanic rocks com

prising lavas of basic to acid composition, related Intrusive*, and

tuffs. Sediments representing a minor p.roup In the regional 11thol oglcal

picture however, may dominate In some parts over rock* of volcanic origin

(e.g. Cow Greek area). These sediments are conglomerates, quartzite,

greywacke and slate. They are velieved to be generally younger than the

suite of volcanics (W.W. Moorhouse, OOM Report Vol. XLVII, Part VIII, 1938,

page 4). A series of granitic Intrusions within the volcanic - sedimentary

belt are younger than the volcanic rocks. Their age relation to the sedi

ments however, Is uncertain. A few diabase dikes cut all the previously

described units .md thus represent the youngest known of the Precambrian

basement rocks In the region.

Varying In thickness, unconsolidated glacis), lake, stream, and i

swamp sediment H cover lar^a areas of Precambrian rocks and create un

fortunately all too often, extremely poor outcrop conditions.

Grade of metamorphism changes strongly from one place to another,

affecting mainly the volcanic - sedimentary sequences. Strong silicific

ation can be noticed almost everywhere.

W.W. Moorhouse, (page 15, 1038), mainly for reasons of structural

analogies existing amongst other Keewatin and Timiskaming regions In the

Canadian shield, believed the gross structure in the South Onaman area

3.

to be a "faulted, synclinal zone". Vany outcrops exhibit drag folding

caused by faulting, which In some Instances, (e.g. dost to the boundary

of the belt), become* very Intensive. The regional strike of the belt

is NW- SE with mostly vertical to steep northerly dips.

DETAILED GF. O LO??

Most of the property Is covered by t'ocensol idated glacial, Jake

nnd 3vamp sediments, Precambrian basement rocks are exposed only in

two outcrops. One occurs on the west shore of Onaman Lake in the NE

corner of claim No. 335062. The other ono is traversed by BL-0 from

l -'60!*. to 3-'-60!S, In the .SV corner of claim No. 335059, The following

rock types were

LO'VED (?) ANDES TT;; (ip)

Brownish-grey on the weathered surface and dark greenish-grey on

the fresh surface, this very fine-grained rock is composed of the

minerals chlorite, biotite, hornblende (?) and very Jittl* plagioclase.

Some traces of very fine disseminated gulf idea (py?) can be noted here

and there. Generally, the rock looks very massive. In some places,

the weathered surface shows structures which possibly are distorted

pillows. They however, did not allow top determinations.

This rock type forms t*ic centre, outcrop on the lakeshore. Its

colours are dar!f hrowninh-grey on the weathered surface and dark green

on the fresh. The rock Is f Ine-prained nnd consists of chlorite, horn

blende and sore pi sftloclflsf!. The tuffaceous texture is visible only on

the weathered surface,

GRBYWACKE (2)

Light grey on both weathered and fresh turface, this rock is

fin* to medium grained and consists of plagioclase, quarts, biotite, some

hornblende (?) , chlorite (?) and sericite. On the weathered surface

plagioclase and quart* occur as unsorted angular to sub-rounded frag

ments with grain sice of coarse sand, and occasionally slightly coarser.

TONALITE (3)" . *- -i

Light grey to pinkish on the fresh surface, this medium to coarse

grained, massive rock weathers with light grey colour. Its mineralogical

composition consists of feldspar (both plagioclase and K-feldspar),

quarts, biotite, and aotne hornblende.

STRUCTURAL GEOLOGY

The volcanic-sedimentary series outcropping in the SW corner of

claim No. 335059, strikes and dips with 160/70W. A local fault with

the same strike direction bisects this series into an eastern portion

with predominantly volcanic rocks and a western part with a higher ratio

of sediments to volcanics. Small conformable intrusions of tonalite

occur in both parts.

The well developed schistosity in the basic tuffs outcropping on

the lakeshore strikes 700 and dips 65O to the NNE. The structural re

lationship of these tuffs to the rocks previously mentioned is unknown.

The very close vicinity of the claim group to a regional granitic con

tact, illustrated in Pig. l, however, is suggestive of rather complex

structures.

Gi;''i.'.)OiCAi. SKETCH MAf OF THE SOUTH O:;AMAS; AREA SHOWING THE DOMINANT STRUCTURAL TRENDS (INDICATED HY THE STRIKE AND IMP OK THE SCHISTOSITY AND REDDING, ZONES OFSHEARING, AND FAULTING) AND THEIR RELATIONSHIP TO THE PRINCIPAL GEOLOGICAL BOUNDARIES.

Fig. 1: taken from W.W. Moorhouse, ODM Report Vol. XLVII, Part VIII, 1938

CONCLUSIONS

(1) Unconsolidated glacial, lake and swamp sediments cover

nearly 1007, of the property, masking most of the t-recambrian bedrock

geology.

(2) For that sane reaaon, neither the ARM conductor* nor the

Radem conductors could be explained as a result of this geological

survey.

RECOMMENDATIONS

No definite recommendations regarding further work can be made

at this stage. They depend on results of a complete data compilation

which l* not yet possible since peochenical results have not been

received.

Horst Petak.

STATEMENT OF QUALIFICATIONS

I hereby state that I have graduated from Karl-Franzen"s

University, Graz, Austria, with the degree of Ph.D. in Geology,

and that I have been practising my profession for four (4) years

in Canada.

Horst W. Petak

111 Illllll II Hill.,. ——. -.__42E13NW8352 63.3860 CASTLEWOOD LAKE 030

GEOLOGICAL REPORT

ON

ALTITUDE GROUP OP CLAIMS

ALTITUDE LAKE, JELLICOE AREA

THUNDER BAY MINING DIVISION

December, 1972 H. Petak

INTRODUCTION

A geological survey was conducted on September 9th and 10th, 1972,

by the writer on six (6) contiguous claims called the Altitude Group,

held by Amax Exploration, Inc. The purpose of the survey was a detailed

geological mapping of the property to assist in checking out two AEM

conductors and ground EM conductors. The ground KM conductors were

located by a Radeto VLF survey executed by Amax prior to the geologicalt. -

survey. '

LOCATION AND ACCESS

The property is located about one mile west of Altitude Lake,

and approximately IP miles to the NNE of Jellicoe, Northwestern Ontario.

Access Is provided by aircraft only. Ontario Northern Airways Ltd.,

with two seaplane bases located several miles west of Jellicoe, offer

charter services with Cessna l BO and Beaver aircraft. Minimum charter

rat* for Beaver Is 520/25 miles.

PROPERTY

The Altitude Group of claims consists of six (6) unsurveyed con

tiguous claims, numbered 335081, 335082, 335083, 335084, 335085, and

335086. Approximately 1/3 of the property, (i.e. parts of the claims

335084, 335085 and 335086), is under water, while the othtr 2/3 are on

land. Comprising an area of approximately 240 acres or 0.375 sq. miles,

this claim group was staked and recorded In April 1972 and Is since

owned by Amax Exploration, Inc., Suite 1302, 7 King St. East, Toronto 1,

Ontario. The property is covered by the claim map M-1850.

An old campsite located on 1,122, 17-120N, on an old 400' spaced

grid with the base line running E-W, and two diamond drill set-ups

were found by the writer and are indicative of rather intensive

previous exploration activity at least in the eastern half of the

property. From drill core (site A Q'.l le/t on one of the sites (150*

south of L28E, 23), this hole is estimated to be at least 3SO 1 Ion.;.t-"~-

Drilled to the north, this helicopter-supported hole has the number

B-5 and intersected basic to intermediate lavas and tuffs. Sulfide

mineralisation, consisting of very little and finely disseminated py,

is insignificant and insufficient to explain the conductors. However,

the possibility exists that eventual better intersections have been

removed. The only information obtained concerning the other hole is

its location, which Is about 200* W of Mo. l claim post of claim

335084, in the NE corner of the property.

Despite all work performed on that ground, there Is no assessment

work on file at the Mining Recorder's office.

After staking in April 1972, Aniax Exploration completed 22,300 ft.

(4.2 line miles) of linecutting, (line spacing is 400') and the same

amount of ground magnetics and Radem survey. Geophysics was followed

up by a geochemical soil sampling program. However, at the time of

writing, results of the survey are not available. Geophysical readings

a* well as soil samples were generally taken on 100' stations and in some

Instances, on ^0' stations.

GENERAL GEOLOGY

The property la located In a belt of chiefly volcanic rocks

coapriaing lavaa of basic to acid composition, related Intrusives,

and tuffa. Sediments representing a minor group in the regional

llthological picture however, may dominate in some parts over rocks

of volcanic origin (e.g. Cow Creek area). Theae sediments are con

glomerates, quartzite, greywacke and slate. They are believed to be* tgenerally younger than the suite of volcanics (W.W. Moorhouse, ODM

Report Vol. XLVII, Part VIII, 1938, page 4). A series of granitic

intrusions within the volcanic - sedimentary belt are younger than the

volcanic rocks. Their age relation to the sediments however is uncertain.

A few diabase dikes cut all the previously described units and thus re-

present the youngest known of the Precambrian basement rock* in the

region.

Varying in thickness, unconsolidated glacial, lake, stream, and

swamp sediments cover large areas of Precambrian rocks and create un

fortunately all too often, extremely poor outcrop conditions.

Grade of metamorphism change! strongly froot one place to another,

affecting mainly the volcanic - sedimentary sequences. Strong silicific

ation can be noticed almost everywhere.

W.W. Moorhouse (page 15, 1938), mainly for reaaona of structural

analogiea existing amongst other Keewatin and Timiskaming reglona in

the Canadian Shield, believed the gross structure In the South Onaman

area to be a "faulted, synclinal tone". Many outcrops exhibit drag

folding caused by faulting, which In some instances, (e.g. close to the

boundary of the belt), becomes very intensive. The regional strike of the

belt is NW-SE with mostly vertical to ateep northerly dips.

DETAILED GEOLOCT

Precambrian rocks are only exposed in the southeastern part

of the property with the exception of one outcrop found In the

northwestern portion of the property. The estimated outcrop ratio

for the whole claim group is around 101. For the southeast part

alone, it is considerably higher.

Unconsolidated glacial, lake, stream and swamp sediments cover**~i

9OX of the property, masking the underlying Precambrian rocks.

Although varying in thickness, the overburden coverage is generally

expected to be shallow.

The following classification and description of the Precambrian

rocks is baaed on macroscopic observations only.

v

BASIC VOLCANIC ROCKS (1)

MASSIVE ANDESITE (l np

The bulk of this rock type was found on L20E, between 19N and 22N.

Slightly west of L16E, between the stations 25N and 27N, the same rock

type was found interbedded with basic tuffs (It ). A small outcrop

composed entirely of massive andesite (1m) is located on BL 0400, east

of L12E. As surrounding outcrops to the ME suggest, it represents a

basic flow (1m) intercalated in basic tuffs (It). Weathering dark green

ish grey, and dark green on the fresh surface, this rock is very fine

grained and consists mainly of hornblende and chlorite and occasionally

minor amounts of plagioclase.

BASIC TUFF (It)

Besides the two locations as mentioned above, where basic tuff

(It) was found to be associated with massive andesite (Im), an isolated

outcrop of basic tuff (It) occurs slightly west of the north end of

LAW. The tuff weathers dark greenish-grey, whereas on fresh surface,

4.

it is dark green. The tuffaceous texture Is best visible on the

weathered surface exhibiting a well developed lamination or banding.

The tuffaceous fragments are less than l mm In slse. Their shape

Is angular. The mineral composition of the tuff consists mainly of

fine grained chlorite, some hornblende, and little plagioclase.

INTERMEDIATE VOLCANIC ROCKS (2)

Intermediate phases seen to make up the majority of the volcanic

rocks, at least in the area SE of the lake.

INTERMEDIATE MASSIVE FLOWS (2m)

Closely associated with tuffs of the same composition (2t) , an

intermediate flow is exposed in a large outcrop located at the north

end of L24E. This exposure, forming a high ridge, extends to the east

beyond the property boundary. Three smaller elongated outcrops,

roughly located on a line from L20E, 12N, to L24E, 17N, most likelyN

represent one flow. There is a chance that this flow la the offset

western extension of the one mentioned above. However, no tuffs were

found in direct contact with them, which of course could be due to lack

of outcrop.

This rock type weathers light grey to brownish-grey, with light

"* green td medium greenish-grey colour on the fresh aurface. Very fine

plagioclase and quarts, with approximately equal proportion of mafic

to felsic components. Traces of finely disseminated pyrite are not

uncommon.

INTERMEDIATE TUFF (2Q

The bulk of intermediate tuff outcrops in the extreme aouthwest

corner of the claim group (i.e. southern half of claim 335083).

Light grey to brownish-grey on the weathered aurface, and light

green to medium greenish-grey on the fresh, these tuffs are usually

very fine grained and thinly bedded. They are composed of chlorite,

plagioclase and quartz in about equal proportions, plus some horn

blende. Traces of finely disseminated pyrite can be observed in

many hand specimens.

INTERMEDIATE FRAGMENTAL TUFF (2f)

Outcrops exposing this rock type were found 'around the north end

of L12E and the SE corner of the claim group. The rocks in the latter

area suggest a slight facies change from the fine clastic variety (2t)

to a coarse fragmental variety (2f) from east to west. "Fragmental"

refers to fragments of over 4 cm in diameter. The matrix looks the

same as the tuff described aa (2t). The fragments either subrounded

or lens-shaped average 6" x 4" and weather slightly lighter than the

matrix. On the fresh surface, however, there is no difference.

ACID VOLCANIC ROCKS (3)

The volcanic series underlying the claim group seems to be

characterised by a atrong deficiency in acid phases. Li68 around 17N

traverses the only outcrop encountered in the area exposing this group.

The rock type is classified as:

ACID PRACMKNTAL TUFF (3.f j

The matrix weathers light grey to white. The fresh surface is

buff to greyish. The weathered surface exhibits a laminated to thinly

bedded granular texture, whereas the fresh surface is extremely fine

grained t rather massive, and very siliceous in appearance. This matrix

surrounds generally subrounded to lens-shaped fragments, averaging

4" to 6" in aiie. Fragments and matrix are of the aaaa composition

which makes it impossible to differentiate them from each other on

the fresh surface. A slight difference in weathering and massive texture

even on the weathered surface makes them easy to recognise on the outcrop.

BASIC ROCKS OF UNCERTAIN ORIGIN (4)

A medium to coarse crystalline basic rock composes several out

crops sporadically distributed over the SB portion of the property,

weathering dark brownish to grey, the colours on the fresh surface

are dark to medium greenish-grey. The highly crystalline rock is

medium to coarse grained and very massive in appearance, with

granitoid texture. Its Mineral assemblage comprises hornblende,

plagioclase and possibly pyroxene, with ratios indicative for gab

broic composition. The relationship of thll rock type to the sur

rounding basic and Intermediate volcinica is in all but one outcrop,

doubtful. In this one particular case, (N end of L24E), however, a

gradatlonal contact shows that the questionable rock is a coarse

crystalIced phase of a basic volcanic flow grading into a tuffaceousV

Intermediate phase. For the others, an intrusive relationship is also

possible. The outcrop located on TL13N, 23E, has to be included here.

The exposed contact is a shear contact and does not reflect the true

primary relationship between the two rock types on each side.

STRUCTURAL GEOLOGY

The most significant structural features in this area are strong

faulting, folding, and consequently, shearing.

A strong fault Kona occurs SE of the lake between the lines 16B

and 20B, and is possibly identical to the northwest extension of the

fault south of Altitude Lake, as presumed by W. W. Moorhouse * , (page 15,

1938). Fig. l illustrates the location of the Altitude group of claims

in relation to this fault system,

(1) W.W. Moorhouse, 1938: Geology of the South Onaman Area, ODMReport Vol. XLVII, Part VIII, 1938

Folding which is the strongest on both aides and in the clove

vicinity to aforementioned fault zone, appears to be drag folding

caused by both lateral and vertical movements along the fault zone.

All the fold axes observed plunge SW with a 45 to 500 dip.

Moderate shearing can be observed in many outcrops. A strong shear

cone crossing TL13N between the lines 20E and L24E, strikes 90O .

ECONOMIC GEOLOGY f~"

Besides trace amounts of finely disseminated pyrite, no signific

ant sulfide mineralization was noticed.

CONCLUSIONS

(1) The presence of an environment generally considered favour

able for massive sulfide typo of base metal deposits could be proved

for a large part of the claim group. It consists of a series of vol

canic rocks of intermediate composition,

(2) Although no significant salfides have been found to date,

more prospecting, including some trenching, particularly in contact

ones, could change that situation.

(3) Surface geology failed to explain AEM and Radem conductors.

RECOMMENDATIONS

No definite recommendations regarding further work can be made

at this stage. They depend on results of a complete data compilation

which Is not yet possible since geochemical results are not presently

available.

Horst Petak.

Gii'-i.c-oic/.i, SKrrc r MAI- or Tin: S'yurir ONAMAN- AHI:A Sm.v. i-.'. Tiii; DOMI.-.-AST STKVC'IUHAI, TREND? (INDICATED BY THE STRIKE AND Du1 OF THE SCHISTOSITY AND BEDDING, ZONES OFSHEARING, AND KA' J.TINX;) AND THKIK KI-I.ATIONSIIIP TO THE PRINCIPAL GKOLOGICAI, BOUNDARIES.

Fig. 1: A Fault Zone south of Altitude Lake and its possible extension into the Altitude Group of claims(Geol. sketch map after W.W. Moorhouse, ODM Report Vol. XLVII, Part VIII, 1938 - Geology of the South Onaman Area)

• II l l BIB II II 1 M .. .. ,. __. -.--

•42E13NW8352 63.3868 CASTLEWOOD LAKE 030

GEOLOGICAL REPORT

ON

LAPIERRE GROUP OP CLAIMS

LAPIERRE TOWNSHIP, JELLICOE AREA

THUNDER BAY MINING DIVISION

December, 1972 H. Petak

INTRODUCTION

A geological survey waa conducted on September 12th and 14th,

1972, by the writer on thirteen (13) out of fifteen (15) contiguous

claims called the Lapierre Group, held by Anax Exploration, Inc.

The purpose of the survey was a detailed geological mapping of the

property to assist in checking out ground EM conductors located by

a Radem VLP survey executed by Amax prior to the geological survey.*~ t

LOCATION AND ACCESS

The property is located near the south boundary of Lapierre Twp. ,

NE of Jellicoe, Ntf Ontario. It is accessible from Highway 11 via good

gravel road (logging road), located about 8 miles E of Jellicoe.

PROPERTY

The Lapierre Group of claims consists of fifteen (15) unsurveyed

contiguous claims with the numbers 32A243 to 324253 inclusive, and

329592 to 329595 inclusive, Two of these claims, namely 329592 and

329593, are almost totally under water and are excluded from this

geological survey. Comprising a total of approximately 2,100 acres, or

9.94 square miles, this claim group was staked and recorded in April,

1972, and is since owned by Amax Exploration, Inc., suite 1302, 7 King

St. E., Toronto l, Ontario. The property is covered by claim map M-1791,

PREVIOUS WORK

A very old drill site (no core]), located about 50' W of L-44E,

3450S and line-cutting (about 2 to 3 years old) paralleling the Amax

grid, indicate that at least part of the area has been worked in the

past. However, there Is no assessment work on file at the Mining

Recorder's office.

After staking in April 1972, Amax Exploration completed 80,800 ft.

(15.4 lin* eolith) of Hneeuttlng with a line spacing of 400 ft, and the

game amount of ground magnetics and Radem Survey. Geophysics was followed

up by a geochemical soil sampling program of which results are not yat

on hand. Geophysical readings or soil samples respectively, were gener

ally taken on 100 ft. stations and in some cases, on 50 ft. stations.

GENERAL GEOLOGY~ "' ,- t-—-t

The property is located in a belt of chiefly volcanic rocks com

prising lavas of basic to acid composition, related intrugives, and

tuffs. Sediments representing a minor group in the regional lltholog-

icai picture however, may dominate In some parts over rocks of volcanic

origin (e.g. Cow Creek area). These sediments are conglomerates,

quartcite, greywacke and alate. They are believed to be generally

younger than the suite of volcanics (W.W. Moorhouse, ODN Report Vol.

XLVII, Part VIII, 1938, page 4). A series of granitic intrusions within

the volcanic - sedimentary belt are younger than the volcanic rocks.

Their age relation to the sediments however is uncertain. A few diabase

dikes cut all the previously described units and thus represent the

youngest known of the Precambrian basement rocks in the region.

Varying in thickness, unconsolidated glacial, lake, stream, and

swamp sediments cover large areas of Precambrian rocks and create un

fortunately all too often, extremely poor outcrop conditions.

Grade of metamorphism changes strongly from one place to another,

affecting mainly the volcanic - sedimentary sequences. Strong silicific

ation can be noticed almost everywhere.

W.W. Moorhouse (Page 15, 1938), mainly for reasons of structural

analogies existing amongst other Keewatin and Timiskaming regions in

the Canadian Shield, believed the gross structure In the South Onaman

area to be a "faulted, synclinal cone". Many outcrops exhibit drag

folding caused by faulting, which in some instances, (e.g. close to

the boundary of the belt), becomes very intensive. The regional strike

of the belt is HW-SE with noatly vertical to steep northerly dips.

f..-

DETAILED GEOLOGY

In the entire property, the Precambrian basement is exposed only in

one location, namely on L36E, 78, in the southwest part of claim No. 324250.

PILLOWED ANDESITE (Ip) comprises an outcrop forming a small and very

narrow E-W striking, moss-covered ridge. Brownish-grey on the weathered v

surface and dark greenish-grey on the fresh surface, this very fine

grained rock Is of homogeneous composition. Microscopically visible

are the minerals hornblende, chlorite (T), plagioclase, quartt, (mostly

a product of secondary silicification), and traces of extremely fine

disseminated sulfldes (pyt).

The weathered surface of the outcrop exhibits pillow structures,

Stretched and sheared the pillows are 2 to 4 ft, long and up to l foot

wide. Top determinations were negative. Foliation which parallels the

stretch axes of the pillows, was 85-900 .

CONCLUSIONS

(l) Unconsolidated glacial, lake and swamp sediments were found

to cover nearly 1001 of the property. This most unfortunate fact mini

mised the possibility to gain detailed information concerning the Pre

cambrian basement geology during this survey.

(2) For the same reason, all EM conductor* remain unexplained.

(3) The old DDH found on 50'W of L44E, 3+50S la collared between

150' to 200* south of an Aaiax multiline Raden conductor. This position

ing suggests very strongly that this hole was designed to teat that

sane conductor. Whether or not it really intersected it is not known

due to lack of any core. To test that target from that given collar

the hole would have had to be 350* long and drilled with 45O Inclination

to the north. *~"

RgCOMMENDATIONS

No definite recommendations regarding further work can be made

at this stage. They depend on results of a complete data compilation

which is not yet possible since geochemical results are not back.

Horst Petak.

42E13NW8353 63.3060 CASTLEWOOD LAKE040

GBOLOGICAL REPORT

ON

CASTLEWOOD CROUP OF CLAIMS

CASTLEWOOD LAKE, JBLLICOE AREA

THUNDER BAY MINING DIVISION

December, 1972 H. Petak

INTRODUCTION

A geological survey was conducted on September 17th and 18th,

1972, by the writer on eight (8) contiguous claims called the

Castlewood Croup, held by Amax Exploration, Inc. The purpose of

the survey was a detailed geological mapping of the property to

assist in checking out ground EM conductors located by a Radem VLF

survey, executed by Amax prior to the geological survey.t-* i

LOCATION AND ACCESS

The property is located north of Castlewood Lake, about 18 miles

to the NNW of Jelllcoe, Northwestern Ontario. It is easily accessible

by road (Highway li, gravel road to Auden, Northwestern Ontario, and

private logging roads).v

PROPERTY

The Castlewood Group of claims consists of eight (8) unsurveyed,

contiguous claims numbered 335054 to 335058, inclusive, and 329596 to

329598, inclusive. Comprising a total of approximately 320 acres or

1/2 square mile, this claim group was staked and recorded in April, 1972

and is since owned by Amax Exploration, Inc., Suite 1302, 7 King St. E.,

Toronto l, Ontario. The property ia covered by claim map M-1839.

PREVIOUS WORK

Part of the property is covered by two different previous grids.

One, with lines cut approximately N-S, seems to be older than another

on* that parallels the present Amax grid, A diamond drill hole with

core (site AQ) left on the site, has been drilled to the SW. it was

collared on a line of the younger grid.- The location in reference to

the Amax grid is 30 feet East of L-8E, 7470S. The core does not show

any conductive material and apparently intersected tuffaceous sequences

of basic to Intermediate composition throughout the hole. Mo

assessment work is on file at the Mining Recorder's office.

After staking in April, 1972* Amax Ixploretion completed

39*200 feet (7.4 line milea) of llnecuttIng (line specing Is 400')

and the same amount of ground magnetics and ladem survey. Geophysics

was followed up by a geochemical soil sampling program* reaults of

which are not available at the present time. Geophysical readings or

soil samples respectively were generally taken at 100* atationa and

in seme cases st 50* stations.

The property is located in a belt of chiefly volcanic rocka com

prising lavas of basic to acid composition* related intrusive** and"V

tuffs. Sediment* representing a minor group in the regional litholog-

ieal picture however, may dominate in some parts over rock* of volcanic

origin (*.g. Cow Gr**k ar*a), Th*** **dim*nts are conglom*r*t*a*

fuaruit** gr*ywack* and slat*. Th*y at* believed to b* g*n*r*lly

younger than th* suit* of voleaniea (W.W. Noorhou**, ODH loport fol.

Kuril t Part fZZX, 1938, pat* *). A serl** of granitic intrusions within

the volcanic - **dim*ntary belt are younger than the volcanic rocks.

Their age relation to th* sediments how*v*r, i* uncertain. A few diabase

dik*s cut all the previously described units and thus represent the

youngest known of the Precambrian basement rocks in the region.

varying in thickness, unconsolidated glacial, lake, stream, and

swamp sediments cover large areas of Precambrian rocks and create, un

fortunately all too often, extremely poor outcrop conditions.

Ored* of metamorphism changes strongly from on* plae* to another,

affecting mainly the voleenic - **dim*nt*ry sequences. Strong slliclflc-

*tion can b* noticod Almost *v*rywh*r*.

W.V. Noorhouaa, (Pago 15* 1938), Minly for raaaont of

atruetural analogic* exiating among* t othor Keewatin and Timiakaming

ragiona in tha Canadian Shiald, baliavad th* grot* atruetura in tha

South Onaman araa to ba a "faulted, ayaclinal tone", Many outcrop*

axhibit drag folding caoaad by faulting, which in aome inatanoaa,

(a. g. cloaa to tha boundary of tba halt), baco*a vary intanaiva.

Tha regional atriko of tha bait ia HW- gf with moatly vortical to ttaapr-northarly dip*.

PtjAIUD CTOLOGT

Precambrian rocka ara axpoaad along tha gravol road eroaaing tha

proparty in HW- gf diraction north of baaaliaa 0+00, and in tha aouth-

cantral and touthaatt part of tha claim group. Tho outcrop ratio iax.

estimated to ba roughly batvaan 5 and 101. Unconsolidated glacial

aedimcnt* (cand, graval, and bouldara) and swamp sediment* cover* 901

to 951 of tha property, Making tha underlying Precambrian rocka.

Although varying in thiekaaaa* tha overburden coverage ia generally ex

pected to ba very (hallow.

Tha following clarification and daacription of tha Precambrian

rook* it baaed on macroscopic observation* only.

IASIC VOLCAMIC ROMS (1)

AMUglTB (Im)

Thia rock type outcropa in aaveral placaa on both K aide* along tha

gravel road north of baaaliaa 0+00. It occura aa 2* vida band* Inter

calated ia tuff a. Vaathariag dark graeniah-grey, and dark green on tha

Iraah aurfaea, thia rock ia vary fine trained and eoaalata chiafly of

horablaada and chlorite, aad minor plagioclase. A tuffacaoua variety

outcropa in the *outhw*at corner of the claim group on tho northweat

id* of tht road on both sides of th* lin* 81* The tuffaceous

character it viaibla only on the weathered surf act,

i)

This rook type was found only in on* outcrop located 150* east

of lin* 12E and 100' K of BL 0400.

Microscopically th* Mineralogy does not differ fro* the en* ob

served in the Massive type deacribed above. The pillows are stretched

to an extent that makes top determinations impossible.

BA11C TUfT (It)

The very fine elastic variety of this rock type was observed

only in on* exposure located at L-0, 3M. Th* tuffaceous sequence in

this outcrop is intercalated with a 2* thick massive andesltlc flow,

Th* tuff* weather dark greenish-trey. The fresh aurfac* is dark green.

Th* tuffaceous character la best vlslbl* on th* weathered eurfaee, *x-

hlbltlng a well developed lamination as beading. Th* tuffaceous frag-N

ments average laaa than l mm In slie. The mineral compoaition of the

tuffs conslata mainly of fin* grained chlorite, aom* hornblende and

little plagioclase.

BASIC ntAOMCTTAl. TOFFS (If)

This form la uaed for tuffa containing fragments larger than 4 em

in di ami ter. They were encountered at two different placeai

(1) on L8B, around 6+50H

(2) on the linea L20B and 2 AE, around 114508 and 13S respectively

Averaging around 6 inches, eome of the fragment* reach a diameter

of l foot. They are either well rounded or ellipsoidal in outline. In

their mineralogy, they differ little from the matrix la which they 11*

and it makes them generally impossible to recognise on the fresh surface,

5.

The fragmental character, however, la usually well documented on the

weathered surface.

Dark greenish to brownish-grey on the weathered surface and dark

green on the fresh, the rock is generally very fine grained, It la

composed of the nlnerals chlorite, sons hornblende and little plagio*

claae. In hand specimens, these fragmental tuffs are very difficult

to distinguish from the regular baalc tuffa (It) described before.

BASIC LAPILLI TUFF (It)

Bsslc lapilli tuff la exposed In several outcrops occurring on

both aides of the road northeast of BL 0400. A very fine grained matrix

weathers light grey to medium greenish-grey, and Is of dark grey colour

on the fresh surface. On the weathered surface, the thinly layered

character of this tuff Is well preserved. Chlorite making up over 801

of the mineralogy of the matrix gives It a schistose appearance on the

fresh surface. Minor minerals are plagioclase and quarts, and possibly•i

some local hornblende. Generally of much more felsic composition than

the matrix, the lapilli are easy to recognise on the weathered and fresh

surfsee. They sverege in sice around 2 mm, the largeat onea range up

to 2 cm. They occur in all aorta of ahapes from rounded to angular.

Oval or otherwise elongated-shaped fragments ere usually well oriented

in the bedding planes.

IKTERMSDIATE VOLCANIC KOCK8 (2)

In the field mainly two criteria were used to classify these rocks

aa a sepsrate groupi (1) degree of silicification in compariaon to the

most basic aa well as most felsic volcanic rocka observed In the area;

(2) colour on weathered and freah surface.

6.

INTERMEDIATE TUFF (2t)

Thia rock typa was found to ba exposed In thraa outcrops on tha

north and aaat side of a ridga croaaad by L4E, north of BL 0400,

and In aavaral outcrops In tha SB cornar of tha proparty (on Una* 20K,

24E. 28B, and on BL 0400 between L28B and L32E). A narrow band of

such tuff Is axposad on L16K, 4+BON (Just north of tha road). That

same band appears to grada into a coarsa fragmental tuff further to* *

tha aast. An Isolated outcrop exposing intemediate tuff occurs on

tha TL168 just aast of L-0.

In addition to thasa exposures composed antiraly of intermediate

volcanics, there ara quite a few outcrops in which bands of inter

mediate tuffa alternate with ones of acid composition. The width of

thasa bands varias but usually ranges from l" to 3".

Weathering light gray to brownish-gray, with light graan to medium

greenish-grey colour on the frash surface, these intermediate tuffs

ara usually very fine grained. They ara generally thinly budded and

consist of the same minerals as tha more baaic phases. Tha ratios

though ara different, baing chloritai (plagioclase 4- quart*) -lil

with plagioclaaa somawhat higher than quart*.

ItmtKHEDIATE FKAQHSMTAL TUFF (2f)

Tha biggest outcrop exposing this rock typa is located on tha

south boundary of the property, slightly aast of claim post Ho. 3 of

claim 329598. "fragmental", as dascribad under basic fragmental tuff,

(If) - again rafars to fragments of A cm or more in diameter. Tha

matrix looks the seme as the tuff described ss (2t). The fragments

either subrounded or lens-shaped average 6" x 4" and weather slightly

lighter than the matrix. On tha fresh surface however, they are very

difficult to differentiate.

ACID VOLCANIC ROCKS (3)

Their exposure* form two parallel Bones. On* outcropa along

the road north of BL 0400, and the other one l* located along and

south of TL16S. In decreasing order of abundance, thla group comprises

the rock types fragmental tuffa (3f), regular tuffa (3t) , and rhyolite

(3-).

RHTOLITE (3m)f-— - l

A. Massive flow of rhyolite, approximately 10 ft. wide, was found

in only one outcrop located on LSI, 64-8011 (north of the road). It la

in sharp contact with the basic fragmental tuff in the 8V. To the Ht

the rhyolite grades into an acid fragmental tuff.

ACID TUFF (3t)

A band about 60 ft. wide of add tuff was delineated north of the

road paralleling BL 0400. The tuff la bounded by a thin layer of basic

flow In the south and by basic lapilli tuff in the north. Ixpoaed from

line 161 to 201 its full strike length is not known. While it is com

pletely open to the 91, it is not expected to continue much more than

a couple of 100 feet to the HW.

la moat of the other outcrops exposing acid phases of tuffs, they

ware found closely associated with tuffs of Intermediate composition,

Both phases form bands of l" to 3" in width alternating with each

other, weathering light grey to white, the acid tuffa are originally

thinly bedded. Thla primary texture la well documented on the weathered

surface. On the fresh surface however, the rock la buff to greyish,

extremely fine grained, rather massive, and very siliceous.

ACID FKAOgJTCAL TUFF Of)

The bolt exposures of this variety of acid tuff outcrops on both

Id** of tb* road jugt v**t of ci*t* 335058, and south of claim 335054

ID axtansion of TL168 to tha SK. Both locations ara outslda tha

proparty boundarias.

In tha Matrix tha fragmental tuff doas not diffar fro* tha ragular

acid tuff dascribad bafora. Tha fragments avaraga about 4" to 6" andf-— iara generally subroundad and lens-shaped. Thay ara difficult to ident-

ify on tha frash surfaca. On tha weathered surfaca however, thay show

up wall.

BASIC ROCKS PT UKCBRTAIH ORIGIH (4)

A medium to coarsa crystal l ina-basic rock cosipriaas aa vara l out*

crops locatad along a bait slightly MB of TL16S paralleling tha lina.

350 ft. to 400 ft. vida in tha HW portion, this bait l* thinning out

towards tha SI.

weathering dark brownish to gray, tha colours on tha frash surfaca

ara dark to medium graaniah-gray. Tha highly crystallin* rock is

medium to coarsa grainad and vary massive in appaaraoca, with granitoid

taxtura. Its mineral aasemblage comprises hornblanda, plagioelasa

and possibly pyroxana with ratios indicative for gabbroic coaiposition.

Rocks outcropping on both sidas and intaraactad in a DDi ME of tha

bait ara of dafinita volcanic origin. Thay ara tuffs of intermediate

and acid composition in the SW and baaic in tha tt. Unfortunately,

however, no contact against the gabbroic rock was found to assist in

establishing the relationship between the gabbroic rock and the volcanics

on either side.

At laaat two poaalbllltiea offar thaaaalvaa for conaldoratlont

(1) tha questionable rock i* part of tba volcanic aaquanca

and repreaenta a coaraa cryatallisad phaaa of a basic

volcanic flow;

(2) wa ara looking at a trua gabbro and tha ralatlonahlp

la of an Intrualva natura

mPCTUlAL OROLOGY J*

tha Precambrian rocka undarlying tba Caatlawood Group of

clalaa eoBpriae a aariaa of volcanic rocka of pradeailnantly tuff-

acaoua character, vbloh atrika batvaan 110O and 100O (avaraga 1200),

with dip varying froai vartical to SOOMB (avaraga 7SO IB), Although

not confirmed in individual outcropa (top dataminationa vara impoaalble),

it la fait that in general, tha atratlgraphie top of tha volcanic aa

quanca of thla araa la in tha IB, while tha lower portlona occur to

tha SW. Tha corralation of outcropa along atrika la In *oat eaaaa

axtreattly difficult. Tha aa*a roek typaa do not aaaai to ba eontlnooua

ovar long diataneaa. Thla could probably ba dua to rapid atratabound

faeiaa changaa. Tba poaaibllity of vary tight iaoclinal folding alao

exleta, contributing ita ahara to tha atructural complexity of tha araa.

A daflntta change in tha allica ratio can ba notad in atratlgraphloally

vartical diractlon. Fro* tha aouthweat baaic volcanica grade ^Lnto acid

phaaaa around TLl6g. IB of thla Una a naw aaquanca atarta with baaic

rocka changing to a predominantly acid aaaemblage outcropping on both

aidaa of tha road north of BL 0400. Located between tha baaic aide of

thia northeaatern volcanic aaquanea and tha acid and of tha aouthvaatam

one, liaa the belt of gabbroic roeka. Thia particular eetting auggeata

an interpretation aa a coarae cryatallisad phaae of u baaic volcanic

flow initiating tha northeaatern aequence, rather than an Intrusion.

10,

Shaaring vaa found to ba vary Minor aa4 of vary raatriatad loaal

iaaofftanaa. tha aawi ia trua far faulting. A abort loaal fault

i, atrikin* 1000 , la travaraad by Una 28E on atatloa 4*508.

aaidaa aaaw aaoradia traoa avauata of fiaaly diaaaainatad

pyrita, aa alfalfltaat awlfida aiiaaralUatioo waa aotiaad.

(1) At laaat tvo-thirda of tha proparty la undarlain by volcaaie

roaka. Vor oa*-tblrd aoaariaiaf alaiai 3293W aad tba ME aan of alaia

DSOM, tbta awrvay failad U tatalaa lafomatloa aa to tha aatuva of

ita badrock taalofy* dna to lade af autaroa,

(t) tha volaaaia roaka* baair to aetd ia aoafoaitton, raaja fro*

aaalva fIowa to aoaraa fragaaatal tuffa* thua arovidiftf a haaiaally

favourabla aaviroaaunt for haaa atttala*

(9) Onfortuaataly! outerafa U coataet ftanaa* baiag tba atoat

iataraatinf portioaa* ara axtraaaly rara*

(4) tadaai Vtr eoaduatara aaaaot ha axalalaad vith aay aonfidaMoa

by tha raaulta of thia aurvay.

m dafUita rainaajiaiatioaa ratardUf futfhar work oaa ha vada

at thia ataja. thay dafaad an raaulta af a caaflata data aoaollatiaa

idiiah ia not yat aoaaihla aiaaa gaathaalaal raaulta hava not haaa

racaivod.

iorat fatal.

43E13NW8352 63.31860 CASTLEWOOD LAKE 0B0

GEOLOGICAL REPORT

ON

ATIGOGAMA CLAIM GROUP

LAPIERRE TWP.

THUNDER BAT MINING DIVISION, ONTARIO

March, 1973 J.E. Steers

INTRODUCTION

A geological survey was carried out over four (4) contiguous t

unpatented mining claims registered In the name of Amax Exploration,

Inc., Suite 1302, 7 King St., Toronto, Ontario.

LOCATION AND ACCESS

The property is located in the northwest portion of Lapierre

Twp., Thunder Bay Mining Division, some eight miles north of Highway 11.

The property is readily accessible from Hwy. 11, via a Domtar haulage

road and a quarter-mile winter road.

PROPERTY

The property consists of four (4) contiguous mining claims

numbered TB 335050-335052, inclusive. The claim group was acquired to

cover a weak, single line ASM response.

PREVIOUS WORK

No record Is available of previous exploration carried out on

the property.

GENERAL GEOLOGY

The property is located on the northeast limb of a southeasterly

trending anticlinorium. Government compilation maps indicate that the

bulk of the rocks in the area should be intermediate to felsic volcanic

rocks.

PROPERTY GEOLOGY

Only one outcrop area was found on the property. The rocks

were massive, fine grained, dark green, somewhat chloritic andesite.

2.

TOPOGRAPHY AND OVERBURDEN

The whole area is generally low-lying. The northern half

of the group is a low sand plain where young second growth jackpine

predominate. The rest of the group is a very wet spruce or cedar

swamp most difficult to traverse.

CONCLUSIONS

No conclusions could be drawn from geological observations

as to the cause of the AEM anomaly.

X

42E13NWB352 63.3860 CASTLEWOOD LAKE 060

SUMMARY REPORT

FOR

M8R MAJESTY TUB QUEEN IH RIGHT OF OITTARIO

AS REPRESENTED BY THE MIKISTRR OP NATURAL RKSOORCES

SCOVERINO COHTRACT fOB-2t

#GB-30

tout*. Exploration, Inc. , Roc* 204 - 231 Arthur 3t. Thunder Bay (P). Onturlo. P7B 1A7

J.E. Stft*rt, FOAC, P.Entr. Dlttrtct Geologist:, March 20, 1973.

t

INTRODUCTION

The following report encompasses a ground exploration program

carried out under Contracts #GB-21 s GB-30 of the Government Assistance

Program.

The purpose of the vork carried out was to examine the economic

potential of seven (7) claim groups acquired following an airborne mag

netic and electromagnetic survey carried out over an area north of

Jellicoe, Ontario.

In general, the program consisted of linecutting, electromagnetic

and magnetic surveying, geological mapping and soil sampling with minor

variations from group to group.

SUMMARY AND CONCLUSIONS

One claim group, (Eight Lake Group), was eliminated from further

consideration after a re-flight by the A.E.M. Contractor. It was deter

mined that the anomalies originally detected were caused by instrument

malfunction.

Of the six (6) remaining groups, drill targets were outlined

on five (5) of the six groups.

A total of seven (7) drill holes were drilled to test the

anomalies. All anomalies were found to be caused by non-economic sulphide

mineralization and/or graphite.

Some additional geophysical work was performed on five (5)

groups prior to drilling.

GENERAL

The individual claim groups will be discussed separately.

Individual geological reports have been prepared for each group; however,

geophysical and geochemical reports have not.

f Locution, access, general geology and previous work ara

adequately covered in the Individual geologic report a and will not be

repeated.

The Irwin Group cone i tt a of twenty (20) contiguous uapatented

claim* located in th* southwestern portion of Irwin Twp. and numbered

aa follow* i

329586-91, inclusive; and 349258*349271, inclusive

Geological napping, aotl saatpling , Rede* BM survey a and fluxgate

•agnetomster fturvays were carried out during the aomser of 1972.

Fourteen (14) clalns were added to the original alx (6) claim group in

Movember of 1972.

Hie geology of the six claim sro'p it described in the accompany

ing report by O. Youtnga.

OjStgKRVATIONJ

Ranges end anomaly threshold values of the trace elements

determined in soils of the Irwin group are tabulated below:

f

Ho-1 lCu 4-1 SO ?fO 100Kl 4-36 40Co 4-2tfHu 60-2400 1000 2000P* 0.5-2.9Ag "^.5Z& U-260 100 200Pb 8-32

A email number of samples have Cu and Zn contents outside the

ranges stated above. Two samples contain 2BB and 366 ppn Cu whilst four

Ccurry 520, 570, f20 and 3600 n* Zn respectively. A general covariance

is evident between Cu and Kl although sew* moderately anomalouti Cv values

ar* associated with only background HI, The majority of the mor*? prcwln-

*nt En anova11 ea are associated with enhanced (1000*2000 ppa) Mn,

A prominent 7,n anomaly la p r a cent in t ha west of the area

lyiiu- mainly within claims 329S89 and 329590. The pattern t* elongated

roughly LW and includes peak values of 470*520 ppm Zn. A Moderate Cu *

weak Ni Anomaly partly coincides with this En pattern; Ou values range

front M3-W ppw.

A weak Cu anomaly, partially supported by Zn, la present fring-

ing a drainage channel in the south of the area (data 329191). A Moderate

Cu anooMty (140-2M ppei), this tine unsupported by Kn, occur* n short

distance to the NE of the prominent En anomaly deacrihod above.

with the exception of a few weak Cu values (^0-76 ppat) aoils

from the two eastern claims (3295R* and 329587) return only background

•etal values.

The tone of exploration interest ta clear from the geochemical

data, i.e., a little over one claim in the west of the area, the 7n values

obtained here are clear!y anomalous and merit preliminary follow-up.

However, the absence of Pb and Ag in anomalous quant11 lew is a negative

feature. Similarly, the general enhancement of Cu and Ni with the anomalous

7,n is suggestive of a metal source other than mineral i cat f on. These values

c (xi Id, quite probably, he obtained from an unml netallied carbonaceous and

sulphur bearing argillaceous rock (e.g., a graphite carrying barren Fe

sulphide*). Weaker Cu anomalies in low*lying swampy ground ara likely to

reflect metal accumulation in organic toils and hence be of no exploration

significance.

f(b) .

TVo very veil defined radet* anomalies exist on t h* northern

for** of thtf property.

Both are probably du* to the comb In* d effect* of shear tones

and/or lake hot toot condactfve aoiiine-nt*.

In general, th* other a nema H ea are reflected by t ho dip angle*

profile only and are therefore to be vi owed vfth suspicion. However,

anomalies ' A' , "B" and 'C" lie in an ara* of interfingering f*laic t, mafic

volcanic rocks. Hit* general ar*a alao display* enhanced trace eleaent

value*.

(c) Majnjitjc dajta

Maximum magnetic relief In th* area i* If .780 gamut; however,

if one reading on Una 288 at 6*5011 la ignored, the relief ia only

7,620 gaoata*. It J a suggested that thi* particular a tat ion be ignored

as the reading wa* probably taken over a aMt^oatlte bearing boulder.

The general background of 700 to l ,000 gamia* probably reflect*

dontnantly felsic to interned tato rock* whila the areaft where readings

in eccoss of 1,000 (^anna* vara obtained, are area* underlain by dotefnantly

mafic lavas and/or mafic intrusive rock* probably occurring a* din-

continuous all la.

It ia reeoMtended that additional detailed napping and pros

pecting be carried out in the area* where anoaalou* trace element value*

were obtained and l ri the area* where culphide miner* H** 1 1 on wa* en

countered in the cour*e of t h* original napping.

During th* auajaer of 1973 geological napping and geochemical

•ampling ahould be carried out over the *ixt*en (H) ci ala)* not covered.

5.

The Atigogana Group c on* l t t* of four (4) contiguous on-

petented wining claim located in Northwestern Lapierre Twp.

Geological Mapping, partial soil sampling, RadsM BM and

magnetic surveys vara carried out over the group.

SBS&SM&XiSi

Cu, ph, Zn and Ag values ara uniformly low. Many of the P*

values are low, suggesting a virtually barren exotic overburden; (e.g.

fi uvio- glacial aand) that precludes the application of conventional

surface soil geochemistry.

O*) Ma&QftJLc*

Tha mafneeic background is low and Mxlsmsi relief only 930

tf AflMftAflt B**™"""""*

TWo features ara obvious. The first is a narrow linear

feature with a northerly strike which is probably a Mf le dike.

The rocks underlying the northern quarter of the property have

considerably nore roiief than the southern portions. In the absence

of concrete geological data, the northern portion i* probably underlain

by a mafic unit containing slightly store Magnetite than the southern

portions.

Three (3) weak, nebulous conductive cones were detected which

lack significant fluid strength anomalies. These sones are probably

surficial conductors.

the AIM anomaly located on the property is probably du* to

surficial effect*. No further work i* recoamended on the property.

Pb, ?n And An content* of th* tolls of this group fall well

within background ranges. A swill nustber of aaiaplea have anoiialoue CM

contents; (60-220 ppn, with s peak of 340 ppsi) , which are generally

associated with enhanced (21-56) ppn Hi.

These data do not suggest the occurrence of significant near*

surface Mineral t E* t ion.

00

Magnetic relief in the area is relatively high, appxoxiauitely

26,700 gamut t. The individual features have relatively stron? aaiplitude

but stull wavelength, suggestive of narrow bands of conductive or sewi-

conductive materiel, probably pyrrhotite and/or aom* magnetite.

The area was covered by a Radarn survey and later with a JKH

aurvay to try to sort out the SMUiy Raden conductor*.

The Raden VLK survey indicated a nuaiber of abort, dlscontinuoita

conductive features which had direct Mgnetic coincidence or flanked

magnetic anosuiliea.

Later JEM surveys indicated two cones, each of which has

three (3) probable conductors. Integrated interpretations indicate

they are narrow, vnrtical to steeply dipping bodies of fair conductivity.

Two (2) hoi** were apotted to teat t h* Major aooaa of con

ductivity. Theae were aa follows:

AL -l Una 241. USOS, ~4SO Or l d M - 250* At -2 Una 4W, 5*7511, -450 Grid K - 500*

Conductivity in tiolo on* vat found to b* du* to (1) a pyrrhotite

network in iMta-andeaitea and (2) a aulphld* iron formation.

Conductive tones in hoi a two vara cauaad by pyrrhotite con-

cantrationa in graphitic aedtaentary rocka.

No economically significant concent ra t i ona vara encountered.

Mo further work la warranted on thia property.

Cu, Pb, ?n and Ag valuea are uniformly background. Many of

the Pe valuaa are extremely low auggeating a virtually barren exotic overburdan

(e.g. fluvioglacial sand), that precludea the application of conventional

aurface aoil gaocheaitatry.

Magnetic relief ia generally low, ma* taw M* relief being 4000

. The Magnetic features and available geological data auggeat a

aeriea of intermediate to felaic volcanic rocka which have a aoutheeaterly

strike.

Only the linear anomaly in the south -central part of the area i a

considered to be significant.

The initial radea survey waa not i|rfinitive, aince it indicated

several surficial conductive von* a In t ha northern portion of the

area and en anomaly in the eouth*central portion having Magnetic

correlation but a very peculiar electromagnetic expression.

A JIM aurvey w* a then carried out which indicated only one

anoaialy in the south-central portion of the area.

Thia anomaly ia atrike li*! ted, narrow* direct magnetic

coincidence and a conductivity-thickness product of about 24 Mho a.

One hole was spotted to teat this anoetaly.

A tone of 10-131 pyrrhotite Mineral i tattoo over a core

length of 23 ft. was encountered in en Intermediate tuff.

Mo further work ia recoBaended aince the conduct lv* cone

haa been adequately teated and no economically aignificant mineral!*

at ion watt encountered.

A few positive, or weakly anomalous, Zn valuea are preaent

(80-140 pptn) but no Cu, pb or Ag anomaliea occur, f e valuea ere "norwal"

•uggeating that barren exotic overburden ia unlikely to he a aifnificant

factor. The*** data do not auggeat that the area poaeenaee amy obvious

Hineral potential.

fieveral narrow, atrike limited, anoattliea are evident.

M*xlBi'im relief on cho property i a 3610 gamut.

The contoured data ere euggeative of narrow form* t Ion* l

tone* weakly Mineral ited with pyrrhotite.

The Hade* Survey yielded several anowalies which are dif

ficult to correlate Iron lin* to line. All either flank Magnetic

BoofMlie* or have direct Magnetic coincidence.

The JEN aurvey carried out utilising a 300- foot coil aepar-

ation and a frequency of 1630 H* failed to conflm the anoMHe*.

Prior to drilling selected line* were run using A !KX)*foot

coil separation and 5010 HE. The awin, aouth*rnmo*t Aiumaly wu a COB-

firmed. It i a likely that the other* could be detected ueinjf 5010 Wx

tind a 200 -foot coil separation.

DIAHOW) MELLING

One hole waa apotted to teat the ctrongeat anoawly. Three

narrow aoite* containing pyrrhotite were encountered. Host rock* were

mafic to andealtic volcanic rock*.

No further work i* warranted on thl* property.

With the exception of a few acattered weakly poaitlv* 9En

values, (70-85 ppw), only background level* are evident. Many of the

fe value* are extremely tow *ugge*tini a barren exotic overburden,

probably fluvioglacial cand.

lo.

00Maximta relief in the area i* 8960 gam* e.

Four, relatively narrow gone* having Moderate magnetic

relief and en easterly strike are evident. It ia likely that form-

atlonal pyrrhotite is the cause of the anomalies.

The Radem survey indicated the praaence of four (4) conductora.

However, only vary weak field strength anomalies were detected.

Prior to drilling, lines 20K ft 48B were read using a Crone

CRM unit utilising a 300-foot coil separation and frequencies of 1830

am) 390 Hs to obtain dip and conductivity data.

Three (3) holes were drilled to test the anomalies. All

holes encountered pyrrhotite and pyrite mineralization and/or graphite.

No further work is recommended for this property.

Respectfully submitted,

APPENDIX l

t

"B" Horicon material i* sampled thus organic- rich top soil

and leached upper subsoil arc avoided. Occasionally organic-rich

samples have to be taken frost swampy areas.

Sasiples are taken by hand Iron a SIM 11 excavation wade with

a cast iron mattock. Approximately 200 grans of the finer grained

material is taken and placed in a numbered, high wet strength kraft

paper bag. The bsgs are closed by folding and do not have setal tabs.

Observations as to the nature of the sample and the environ

ment of the sample site are made In the field.

Normally, samples are taken at 200-foot intervals on 400-foot

grid lines. Even- numbered stations are sampled on alternate lines.

The minus 30 mesh fraction of the dried, sieved samples is

analysed by Atomic absorption spectrometer, following digestion with

hot HC104 - HNOg.

Routinely, Mo, Cu, Mi, Go, Mn, Fe, Ag, Zn, Pb content is

recorded.

Comp

Collector

Dote ——

RECCE SAMPJrf^DATA SHEET

Project, ATM doke.highwcy.etc).

Plotted (mop, photo) —NvMW

SompleNumber

T

M Oo tt

o tn

it*

\~ o ±

0b

o b

0b c

0b c

0b c

0b c

0b c

0bc

o b c

o b c

0bc

o >

Lxvti**

General

N

N

N

N

N

H

N

N

N

N

N

Sample Site

E

E

E

E

E

E

E

E

E

E

E

CwlnMMrt

TOPOTerroin-

T YPE

— -

DIRECTION-Drainage-

TYPE

S*-** DMcr*NM

SIZE— Texture -

TYPE

-

TONE- Coloor-

BASE

- - — ———

. . ————

-— - ———

ArPH

lalyticol ResultsMo t Cu

Remarks

(Otology, GtomorpK, Culture , Float)8 i

10

General Remorks:

Form JAH-67

tABBREVIATION INDEX FOR CBQCBPMICAL SAMPLES

GAS - ALTITUDE

HAS - ATIGOGAMA

HCR - CASTLEWOOD

HIS - IRWIK

HLS - LAPIERRE

HOS - ONAMAN

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OCT2' 0197?/IROJpQU

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AMAX EXPLORATION INC. ANALYTICAL REPORTBURNABY LABORATORY - 2225 SPRINGER AVE. - BURNABY 2, B.C.

TYPE SAMPLES

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DATE SAMPLES RECEIVEC DATE REPORTS MAILED-

ANALYST __________

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TYPE SAMPLES

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DATE SAMPLES RECEIVEL DATE REPORTS MAILED -

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l AMAX EXPLORATION INC ANALYTICAL REPORTBURNABY LABORATORY - 2225 SPRINGER AVE.' - BURNABY 2, B.C. AUG 1 O 1972

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DISPOSITION OF REJECTSEQUESTED BY

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TYPE SAMPLES

LOCATION

DISPOSITION OF REJECTS

DATE SAMPLES RECEIVED- DATE REPORTS MAILED — ANALYST, —-x^,_____

AMAX EXPLORATION INC. ANALYTICAL REPORTBURNABY LABORATORY - 2225 SPRINGER AVE. - BURNABY 2, B^^

DATE . /7/f^ /# f 7Z - __ __-^^--™-. TYPE SAMPLES Jib// ___________

OJECT ____^——-57?-——-——— LOCATION -

EQUESTEDBY ———^*-- ^T^^-^S —————— DISPOSITION OF REJECTS

DWTE SAMPLES RECEIVED- DATE REPORTS MANNED — ANALYST .', ., i . t ...J——

AMAX EXPLORATION INC. ANALYTICAL REPORTBURNABY LABORATORY - 2225 SPRINGER AVE. - BURNABY 2, B.C.

DATE -W ...-i/U-W-- OJ t J.y2Q—...- ——____' TYPESAMPLES

?OJECT -—. —-^-.-—,-^ri/Y __ ____ LOCATION

REQUESTED BY

AUG 1 f) 197?

DISPOSITION Of REJECTS' b "

AMAX EXPLORATION INC. ANALYTICAL REPORTBURNABY LABORATORY - 2225 SPRINGER AVE. - BURNABY 2, B.C.

TYPE SAMPLES

LOCATION

DISPOSITION OF REJECTS L

DATE SAMPLES RECEIVEC DATE REPORTS MAILED.

ANALYST ' , \

? EXPLORATION INC. ANALYTICAL REPORT \SBURNABY LABORATORY - 2225 SPRINGER AVE;. - BURNABY 2, B.C. n.,p ,- AUG 1 o W)

A 11 ZLI IQ7V *-—. ' w{\\MAJ, gijjyjxL J ^4by

TYPE SAMPLE

/UMAX EXPLORATION INC. ANALYTICAL REPORTBURNABY LABORATORY - 2225 SPRINGER AVE. - BURNABY 2, B.C.n i ir -f

DATE •^•L,. IrJJUJ, .., S) t Jy7fQ—— .-j- TYPE SAMPLES.————

OJECT -——.

EQUESTED BY

197?

LOCATION

ISPOSITION OF REJECTS

No.

01

02

03

04

0506

07

08

09

10

11

12

13

14

15

16

17

, 18h-20

21

22

23

24

25

26

27

28

29

30

31

32

33

34

35

36

37

38

3,

WCO

Sample

MlS~3olj8Q Q?)O

#LS331

MMENT:

X

•— -

-— --

,

Mo ^

Y-1-

1

— - - -

--- - -

s Cujy

y^t/*

.

V

' N.^b

/2-

/^

y*

- — —

— —

-Co9

2g

•*.

'

tyyju~oj ' &Q

\J /^y c^** Y~ty

S&&

~.

mO'ti(6t'f/.r

*

, DA DA

' - . . : ' \ AN

flfl.j--P-V

i'

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fa,

,0

PJ?

22?**

,

•^ -

TE SAMPLES RECE TE REPORTS MAIL Al VST ' ' ' '

fk*t^f*

j,

'

No.

01

02

03

04

05

06

0708

09

10

11

12

13

14

15

16

17

18

19

20

21

22

23

24 25

26

27

28

29

30

31

32

33

34

35

36

37

38

39

40

1 V E D ___________ —— _ - ED

S t-fto

AMAX EXPLORATION INC. ANALYTICAL REPORTBURNABY LABORATORY - 2225 SPRINGER AVE. - BURNABY 2, B.C.

T&4-TYPE SAMPLES

-..-y.--...-- LOCATION

lj?FH-Z4*

D1SPOSITIOHOF REJECTS

DATE SAMPLES RECEIVEC DATE REPORTS MAILED -

AMAX EXPLORATION INC. ANALYTICAL REPORTBURNABY LABORATORY - 2225 SPRINGER AVE. T BURNABY 2, B.C.

4fc^' ^ /^ S? J CVDATE ^JMfafr/y/SA ^. . .^ ______ TYPE SAMPLES—±_____^^//L-

OJECT ———.-__- — y^ - . ..J___ LOCATION —T--—

EQUESTED BY — , ^^/^t^ 3 J ^^/^^J /JZLjj DISPOSITION OF REJECTS

DATE SAMPLES RECEIVED- DATE REPORTS' MAILED ^~ANAL,YST ,.., "- ——*——

,~:t'

AMAX EXPLORATION INC. ANALYTICAL REPORTBURNABY LABORATORY - 2225 SPRINGER AVE. - BURNABY 2, B.C.

TYPE SAMPLES

LOCATION

DISPbSITION OF REJECTS

DATE SAMPLES RECEIVED, tiATE REPORTS MAILED —

3 AMAX EXPLORATION INC. ANALYTICAL REPORTBURNABY LABORATORY - 2225 SPRINGER AVE. - BURNABY 2, B.0^p l g

TYPE SAMPLES.

LOCATION

AMAX EXPLORATION INC. ANALYTICAL REPORTBURNABY LABORATORY - 2225 SPRINGER AVE. - BURNABY 2, B.C.

TYPE SAMPLES

LOCATION

S If l

DISPOSITION OF REJECTS -

DATE SAMPLES RECEI^ED- DATE REPORTS MAILED —ANALYST . .y.., . ,.'—--——

,.~ v,.v;-.V;i* L- - "- '•--

AMAX EXPLORATION INC ANALYTICALBURNABY LABORATORY - 2225 SPRINGER AYE. - BURNABY

REPOR12, B.C.

ft ^Jfy

— LOCATION

DISPOSITION OF REJECTS

No.

01

02

03

04

0506

07

08

09

10

11

12

13

14

15

16

17

k ' 8

f 191 "

1"22

23

24

25

26

27

28

29

30

31

32

33

34

35

36

37

38

39

L 40

Sample

72 HO^ 3;S?j;j^-0

4" f-j^

tt-*f\4-54-b

W- Jtl

--— — --

I COMMENT:

PH

i

-

Mo

3

f

J

yfj

-L A

tt 1fff

Cu

2/^sjfy

M

_ _

if

APLV

A

•— ——

Ni

2 \2

J-0

2

so/2.

6*/o4-/o

^6^L

C*

ut.t?tf(f(y^(0(f(f

f ' fe A

b'

. ———

/*7wbcto*

2. 0**-JMs-

^0

t 00

j oc(T0f"

Jro

:

T-'/.a.ts-2.7O'-tf

0'^/r 2

-?'±

0,±

/- 7S**

3.0/•v

DA

- DA

AN

th

-r

,,-^J-

iff(f

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-^

^

3/if**

-5 O3p3-63.2.Jz^*?.12.

3^/^

TE SAMPLES RECE TE REPORTS MAIL Al Y^T

^^^

_ ^^/o

__^_^xi^/o

^

No.

01 "02

03

04

05

06

07

08

09

10

11

12

13

14

15

16

17

18

19

20

21

22

23

24

25

26

27

28

29

30

31

32

33

34

35

36

37

38

39

40

IVEDED . .

.. , .

AMAX EXPLORATION INC. ANALYTICAL REPORTBURNABY LABORATORY - 2225 SPRINGER AYE. - BURNABY 2, B.C.nQj g O 197^

TYPE SAMPLES ——

DISPOSITION OF REJECTS

DATE SAMPLES RECEIVED- D'ATE REPORTS RAILED —ANALYST —-._____:__

7-V

Cj•.

;i

H

^

)ATE

LROJ

!EQU

No.

01

02

03

04

0506

07

08

09

10

11

12

13

14

15

16

17

l 18! 19

20

21

22

23

24

25

26

27

28

29

30

31

32

33

34

35

36

37

38

39- 40

1 ————————————————

'3" AMAX EXPLORATION IFBURNABY LABORATORY - 222,5

EC r t? 1 yk - ^~-

ESTED BY —s/ —

Sample

QTU ffoS 9lQ^Cf^

?Ua^ay

??fjhq

1 PT*HiuffcS /D/

^7 *~/1'^ f

COMMENT:

\X

S/f C-^?S 1 R F H (j- -——. 1 ——r

P*

-• ——

.

- ————

————

- ———

—————

Mo

f

f

/

1

i

f

-J -

L1

Cu ^^

2 ^p

^/r — *#^-—

f-

22P1^Itf/i

\

Ni J

LZ3^

S3.Fgx^

/j-/0

6*

dog-

2 fi

f^^^^IrfiZ' l0

s

— , —

1C. .SPRING

TYPESA

LOCATK

DISPOSI

A/H

/5cIZlpj^^ol^f-fl^(\If sif-^r'S kc34-fa77 ctt P1 2o

.

ANER/

MPLE

IN

TION

F.

ALYTICAL REPORTWE. - BURNABY 2, BX^ U '

• c . . WTlOiqns ^15/C W?

.Tfftwbe-G'' fcfl-yOF REJECT

e*5

^tf^

/.4*'

J ^

?

0.1

y/^'./7ir

/•XP'%/,o

DA

DA

AN

l faf r

:. .\\

.—**L Y

^^^•r,f

^ " - i' '

^22

'. 9 Z.4*3/.' /r

.-3 23^9f^x'^^?e

7^

TE SAMPLES RECE TE REPORTS MAIL AI.XST . , . ,.

Pi. /o^0/.iX-^-

; ^,

ffso/^/^^

66*

IVED —— F D

No.

01

02

03

04

05

06

0708

09

1011

12

13

14

15

16

17

18

19

20

21

22

23

2425

26

27

28

29

30

31

32

U33

34

35

36

37

38

39

40

"

i 1

\

ox/

a•o. iOo l

INDEX MAP ! SCALE M INCH :I6 MILES

LEGENDFELSIC INTRUSIVE ROCKS

3 TONALITE

SEDIMENTS

2 j 2 GREYWACKE

BASIC VOLCANIC ROCKS

Ip PILLOWED ANDESITE

It BASIC TUFF

SYMBOLS

l m l CLAIM POST

|TvT| SWAMP

FV~-1 LOW WET GROUND

l c:? l OUTCROP

|~~~| SHEAR ZONE

i —*— \ BEDDING

42E13NW6352 63.3063 CASTLEWOOD LAKE 200

f AMAX EXPLORATION INCORPORATEDTYPE OF SURVEY' GEOLOGY

GROUP-JELLICOELOCATION 1 NORTH WESTERN ONTARIO

SCALE'400 300 200 CO O 400

l INCH s 400 FEET800

DRAWN BY-'KP

TRACED BY: H.S.

MAP No.; 72-69

DATE"'NOVEMBER 17,1972

REVISE D:

NTS. No-:

TO ACCOMPANY^

BY-—^—^^ DATE :-

S A N o y

S6Co * 0" G R O Vi t

t

Mixeo Fo*^

42E13NW8352 63.3060 CASTLEWOOD LAKE 210

INDEX MAP SCALE.) INCH - 16 MILES

LEGEND

4 BASIC ROCKS OF UNCERTAIN ORIGIN

LI

3f ACID FRAGMENTAL TUFFS

INTERMEDIATE VOLCANIC ROCKS2m MASSIVE VOLCANIC ROCK21 INTERMEDIATE TUFF

2f INTERMEDIATE FRAGMENTAL TUFF

BASIC VOLCANIC ROCKS

Im ANDESITE MASSIVE

H BASIC TUFF

SYMBOLS

CLAIM POST

SWAMP

LOW WET GROUND

OUTCROP

DIAMOND DRILL HOLE

SHEAR ZONE

BEDDING

GLACIAL STRIAE

DRAG FOLD

AMAX EXPLORATION INCORPORATEDTYPE OF SURVEY^ GEO LOG Y

GROUP-JELLICOELOCATION 1 NORTH WESTERN ONTARIO

SCALE'400 300 200 100 0 400 BOO

INCH S 400 FEETDRAWN BY : H.P

TRACED BY: H.S.

MAP No. : 72-60,

DATE NOVEMBER 17,1972

REVISED'

NT. S. No- :

TO ACCOMPANY

DATE 1—

SPRUCE

LEGEND

BASIC VOLCANIC ROCKS

BASIC PILLOWED ANDESITE

SYMBOLS

[""•"~| CLAIM POST

DIAMOND DRILL HOLE

SWAMP

LOW WET GROUND

OUTCROP

BEDDING

42E13NW8352 63.3060 CASTLEWOOD LAKE 220

\ r- *f M . .

GEOLOGYLAPIERRE GROUP-JELLICOE ONT

NORTH WESTERN , NTARIO

H.P

H.S.

l INCH " 400 FEETp-

72-70

42E,I4

NOV. 17, i

w3ne

R U C E

INDEX MAP SCALE l INCH'16 MILES

LEGEND

4 BASIC ROCKS OF UNCERTAIN ORIGIN

ACID VOLCANIC ROCKS

3m RHYOLITE 3t ACID TUFF 3f ACID FRAGMENTAL TUFF

INTERMEDIATE VOLCANIC ROCKS

Zt INTERMEDIATE TUFF21 INTERMEDIATE FRAGMENTAL TUFF

BASIC VOLCANIC ROCKSl j tm ANDESITE MASSIVE

Ip ANDESITE PILLOWED It BASIC TUFF [f BASIC FRAGMENTAL TUFF l ItBASIC LAPILLI TUFF

SYMBOLS

l m~~\ CLAIM POST

SWAMP

LOW WET GROUND

GEOLOGICAL CONTACT INTERPETED

BEDDING

OUTCROP

DIAMOND DRILL HOLE.J

42E13NW8352 63.3060 CASTLEWOOD LAKE

AMAX EXPLORATION INCORPORATEDTYPE OF SURVEY'GEOLOGY

AREA CASTLEWOOD GROUP-JELLICOELOCATION ; NORTH WESTERN ONTARIO

SCALE: 400 30C ?00

INCH ^ 400 FEETDRAWN B Y : H. P

TRACED BY' H.s.

MAP No. ;

DATE 1 NOVEMBER 17,1972

REVISED :

TO ACCOMPANY- BY : DATE :

230

i.L.0+00

LEGEND

l l j MASSIVE ANDESITE

SYMBOLS

tf ^ SWAMP

^-~^ GEOLOGICAL BOUNDARY'INTERPRETED

m CLAIM POST

ATTIGOGAMA GROUP

INDEX MAP SCALEM INCH^I6M1LES

42E13NW8352 63.3060 CASTLEWOOD LAKE 240

AMAX EXPLORATION INCORPORATEDTYPE OF SURVEY: GEOLOGY

AREA'ATTIGOGAMA GROUP-JELLICOELOCATION - NORTH WESTERN ONTARIO

SCALE 14OO 30O 200 MO O 400

l INCH = 400 FEET800

DRAWN BY:J.E3.

TRACED BY: K.G.

MAP No.- 73-41

DATE 1 MARCH 29,1973

REVISED

NTS.

TO

BY .DATE J

INDEX MAP' SCALE M INCH -\6 MILES

LEGENDFIELD STRENGTH SCALE'llNCH^OO

DIP ANGLE SCALE:|INCH:200 .————. INDICATES FIELD STRENGTH PROFILE .———.. INDICATES DIP ANGLE PROFILE

FIELD STRENGTH BASE SETTING'100TRANSMISSION STATION:SeATTLE,WASH1NGTON

———— iNDICATES CONDUCTOR AXIS m——— INDICATES CLAIM POST AND CLAIM LINE

ILLUSTRATION

- 130

ei -

N.+ 100

-STATION ON GRID LINE

•DIP ANGLE PROFILE•FIELD STRENGTH PROFILE

125

V FIELD STRENGTH VALUES

120-DIP ANGLE

NORTH DIP ANGLES ARE INDICATED BY NUMERALS ONLYSOUTH DIP ANGLES ARE INDICATED BY NUMERALS FOLLOWED BY THE LETTER S

S.-100

4?

42E13N*B352 63.3060 CASTLEWOOD LAKE 250

AMAX EXPLORATION INCORPORATEDTYPE OF SURVEY-'RADEM

AREA ONAMAN GROUP-JELLICOELOCATION 1 NORTH WESTERN ONTARIO

SCALE-400 300 200 100 O 4OO

INCH : 400 FEETDRAWN BY'KCG.

OPERATOR^R-H

MAP No. : 72-34.

800

DATE : SEPTEMBER 6,1972

REVISED 1

NT. S. No- !

TO ACCOMPANY

DATE ; -

r

INDEX MAP'SCALEH INCH;|6MILES

LEGEND

l MEASUREMENT STATION ON PICKET LINE

RELATIVE VALUE OF THE VERTICAL COMPONENT OF740

flOOO

THE EARTHS MAGNETIC FIELD IN GAMMAS

MAGNETIC CONTOUR

MAGNETIC DEPRESSION

100GAMMA CONTOUR INTERVALINSTRUMENT: MC PHAR M-500 FLUXGATE MAGNETOMETER

42EI3NWS352 63.3060 CASTLEWOOD LAKE 260

AMAX EXPLORATION INCORPORATEDTYPE OF SURVEY^ MAGNETOMETERAREA'ONAMAN GROUP-JELLICOELOCATION'-NORTH WESTERN ONTARIO -

SCALE: 400 300 200 100 O 40O

INCH = 400 FEETDRAWN BY-K.C.G.

OPERATOR : R.G.

MAP No. !-T2-46

DATE : OCTOBER 2,1972

REVISED 1

NTS- No- : ~42E!3

TO ACCOMPANY

BY :_ —--^ DATE :-f * t— *-

80O

42E13NW8352 63.3060 CASTLEWOOD LAKE

f

50*00'-

, ^ ^ONAMAN

GROUP

INDEX MAP: SCALE'1 INCH 'WHILES

LEGEND

FREQUENCY!390 Lo.

COIL SPACING: 300 FEET

SCALE-

ILLUSTRATION

\"—t&M. STATIONS ON GRID t-1 HE

JE.M PROFILE

READINGS IN DEGREESPLUS READINGS PLOTTED NORTH OF GRID LINE MINUS READINGS PLOTTED SOUTH OF GRID LINE

AMAX EXPLORATION INCORPORATEDTYPE OF SURVEY J.E.M "COAXIAL SHQOTBACK AREA.ONAMAN GROUP-JELLICOELOCATION: NORTH WESTERN ONTARIO

SCALE'400 300 200 DO O 400 800

l INCH s 400 FEETDRAWN BY' K CG

OPERATOR 1 R.J.PaR.D.M.

MAP Na*..72-74

DATE: DECEMBER 13,1972

REVISED-

42EI3

TO ACCOMPANY'.

BY*———————. DATE:.

O x/

INDEX M AP : SCALE: i INCH: 16 MILES

ILLUSTRATION

SAMPLE t STATION A

COPPERVALUE V

•NICKEL VALUE

VziNC VALUE S

SOIL SAMPLE NUMBERHCJS-/O-S.-+

SOIL SAMPLE —ONAMAN GROUP SAMPLER'S INITIAL

42E13NW8352 63.3060 CASTLEWOOD LAKE 280

AMAX EXPLORATION INCORPORATEDTYPE OF suRVEY'GEOCHEMISTRYAREA ONAMAN GROUP-JELLICOELOCATION - NORTH WESTERN ONTARIO

SCALE-' 400 300 200 100 O 400 800

INCH s 400 FEETDRAWN BY-K.C.G.

OPERATOR-' R.H.

MAP No. !-12l39-

DATE ! SEPTEMBER 12,1972

REVISED 1

N.T.S. No- :

TO ACCOMPANY^

BY :____^. . , . DATE ; -

f?offALTITUDE J?" GROUP

INDEX MAP SCALED INCH^6 MILES

N?

4^E13NWa352 63.3060 CASTLEWOOD LAKE 290

LEGENDFIELD STRENGTH SCALE' l INCH * 200

DIP ANGLE SCALE* l INCH : 20OINDICATES FIELD STRENGTH PROFILEINDICATES DIP ANGLE PROFILEFIELD STRENGTH BASE SETTING'100TRANSMISSION STATION - SEATTLE .WASHINGTON

INDICATES CONDUCTOR .AXIS

INDICATES CLAIM POST AND CLAIM LINE

ILLUSTRATION

as :

10 - l 95

IDS

N.-HOO

•DIP ANGLENORTH DIP ANGLES ARE INDICATED BY A NUMERAL ONLY SOUTH DIP ANGLES ARE INDICATED BY A NUMERAL FOLLOWED BY THE LETTER S.

100i——7^—— STATION ON QRID LINE

IK) ^-DIP ANGLE PROFILE

FIELD STRENGTH PROFILE FIELD STRENGTH VALUES

95f

-lOO-S.

AMAX EXPLORATION INCORPORATEDTYPE OF SURVEY^ RADEM

AREA'ALTITUDE GROUP-JELLICOELOCATION ' NORTH WESTERN ONTARIO

400 300 200 IOO 0 400 800

INCH - 400 FEETDRAWN BY : K.C.G.

OPERATOR - R.H.

MAP No. :-Z2;3!

DATE 1 AUGUST 30,1972

REVISED-

NT.S. No. : -42E13.

TO

— DATE 1 -

42EI3NW83SE 63.30G0 CASTLEWOOD LAKE300

INDEX MAP SCALE'1 INCH -- 16 MILES

LEGEND

f MEASUREMENT STATION ON PICKET LINE

l TArt RELATIVE VALUE OF THE VERTICAL COMPONENT OF T 740 EARTHS MAGNETIC FIELD IN GAMMAS

MAGNETIC CONTOUR

MAGNETIC DEPRESSION

100 GAMMA CONTOUR INTERVAL

INSTRUMENT- MC PHAR M-500 FLUXGATE MAGNETOMETER

AMAX EXPLORATION INCORPORATEDTYPE OF SURVEY: MAGNETOMETERAREA'ALTITUDE GROUP-JELLICOELOCATION' NORTH WESTERN ONTARIO

SCALE :400 3OO 2OO 100 O 400

l INCH = 400 FEET800

DRAWN BY: K G

OPERATOR : R.G.(OCT)aRJP {JAN.

MAP No. ! 72-55

DATE'OCTOBER 6,1972

REVISED- JANUARY 19,1973

N.T.S.TO BY : DATE 1.

v

MtLEGEND

FREQUENCY:

COIL SPACING'300 FEET

COAXIAL SHOOTBACK

SCALE'l INCH:200

ILLUSTRATION

-5

J.E.M. PROFILE __/A LOW FREQUENCY^

LOW FREQUENCY READINGS

"S—/-J.E.M. STATIONS ON GRID LINE

/-rvi )——J.E.M. PROFILE

-4 - 1

-5 .J s

l/ HIGH FREQUENCY

HIGH FREQUENCY READINGS

NOTE : READINGS ARE IN DEGREESPLUS READINGS PLOTTED NORTH SIDE OF GRID LINE MINUS READINGS PLOTTED SOUTH SIDE OF GRID LINE

42E13NW8352 63.3060 CASTLEWOOD LAKE 310

AMAX EXPLORATION INCORPORATEDTYPE OF SURVEY'J.EM SURVEY

AREA ALTITUDE GROUP-JELLICOELOCATION : NORTH WESTERN ONTARIO

SCALE-400 30O 200 100 O 800

INCH- 400 FEETDRAWN BY ; J.F

OPERATOR^ R.J.PaG.H.P

MAP No. : 72-56

D AT E : SEPTEMBER 1,1972

REVISED'

N.TS. No. ; 42EI3

DATE-'

\J

INDEX MAP SCALE, l INCH : 16 MILES

r

V

42E13N*835a 63.3060 CASTLEWOODLAKE 320

ILLUSTRATION

SAMPLE/STATIONS,

icfCOPPER/ VALUE \ ,

se

NICKEL VALUE

.-*V-2121MC VALUE

J —— SOIL SAMPLE NUMBER

—SOIL SAMPLE-ALTITUDE GROUP

-SAMPLER'S INITIAL

AMAX EXPLORATION INCORPORATEDTYPE OF suRVEY'GEOCHEMISTRY

GROUP-JELLICOELOCATION ' NORTH WESTERN ONTARIO

SCALE- ____ - -....--

400 300 200 100 0 400 800

INCh^ 400 FEETDRAWN BY'KCG

OPERATOR' R.G.

MAP

DATE 1 SEPTEMBER 8,1972

REVISED'

NTS. No.-42.EI3

TO ACCOMPANY

DATE 1

" J r^. i"a?ZS*^^ f^S'-^S

- —-Mh ——

FIELD STRENGTH SCALE: l INCH - 200 DIP ANGLE SCALE: j INCH^O0 INDICATES FIELD STRENGTH PROFILE INDICATES DIP ANGLE PROFILE FIELD STRENGTH BASE SETTING'100 TRANSMISSION STATION' SE ATT LE, WASHINGTON INDICATES CONDUCTOR AXIS INDICATES CLAIM POST

STATIONS ON GRID LINE

DIP ANGLE PROFILE FIELD STRENGTH PROFILE

FIELD STRENGTH VALUES '

r-DIP ANGLESNORTH DIP ANGLES ARE INDICATED BY NUMERALS ONLY

\ SOUTH DIP ANGLES ARE INDICATED BY NUMERALS FOLLOWED BY THE LETTER "s"

EXPLORATIOo p SURVEY RADEMLAPIERRE GROUP -JELLICOE ONT

'./N NORTH WESTERN ONTARIO

K.C.G.

OPERATOR R.H.

l INCH"400 FEET OATfJULY 20,107;

72-24 i '-' \42E,I4

INDEX MAP SCALE'1 INCH^I6 MILES

42E13NW8352 63.3060 CASTLEWOOD LAKE 330

-VO nt (S-tt?

LEGEND

j MEASUREMENT STATION ON GRID LINEB.L.0+00 B.L.0+00&CX3

324244OF THE EARTH S MAGNETIC FIELD IN GAMMAS

MAGNETIC CONTOUR

MAGNETIC DEPRESSION

LAPIERRE .GROUP

100 GAMMA CONTOUR INTERVAL

INSTRUMENT: MC PHAR M-500 FLUXGATE MAGNETOMETER

AMAX EXPLORATION INCTYPE OF SURVEY: MAGNETOMETERAREA LAPIERRE GROUP-JELUCOE ONTLOCATION^NORTH WESTERN ONTARIO

DRAWN BY K.C.G.

SCALE l INCH-400 FEET DATE-i JUNE 33t l972

OPERATOR: J. F

MAP No 72-25

; NTS REF 42EJ4.REVISED

INDEX MAP SCALED INCH: 16MILES TO ACCQMPANYBY: vJCv/fc^ DATE

42E13NW3352 63.3060 CASTLEWOOD LAKE 340/s

LEGENDFREQUENCY: 1830 Hi.

COIL SPACING' 300 FEET

COAXIAL SHOOTBACK

SCALE-l INCH:200

ILLUSTRATION

J.E.M. PROFILE —/\ LOW FREQUENCY^.

LOW FREQUENCY/ READINGS ——\

V

J.E.M. STATIONS ON GRID LINE

'O——AE.M. PROFILE l/ HIGH FREQUENCY

W- HIGH FREOUENCY READINGS

NOTE-PLUS READINGS PLOTTED NORTH SIDE OF GRID LINE MINUS READINGS PLOTTED SOUTH SIDE OF GRID LINE

J.E.M.-COAXIAL SHOOTBACKLAPIERRE GROUP-JELLICOE ONT

NORTH WESTERN "ARK'.

J.F

OPERATORR.J. P

INCH" 400 FEET

72*58AUG. 30,1972

INDEX MAP SCALE:

42E13NW8352 63.3060 CASTLEWOOD LAKE 350

LEGEND

FREQUENCY:

COIL SRftCING'300 FEET

HORIZONTAL SHOOTBACK

SCALE'1 INCH* 20*

ILLUSTRATION

A.+21-

J.EJJ. PROFILE —A LOW FREQUENCY^

LOW FREQUENCY ' READINGS

. STATIONS ON GRID LINE

~ 4J.E.M. PROFILE

\y HIGH FREQUENCY

} — HIGH FREQUENCY READINGS

NOTE 1 PLUS READINGS PLOTTED NORTH SIDE OF GRID LINE MINUS READINGS PLOTTED SOUTH SIDE OP GRID LINE

y T \ P ; " P ^ "j" , . f\; ' \i i,.... ' . ' *~ . fj ^J.E.M.-HORIZONTAL SHOOTBACK

LAPIERRE GROUP-JELLICOE ONTNORTH WESTERN v'NTARIO

J. F

OPERATORR.J-P

l INCH "400 FEET

72-59AUG. 30,1972

.INDEX MAP SCALE:] INCH-IGMILES

42E13NW83S2 63.3060 CASTLEWOOD LAKE 3B0

OPERATOR^ R.H. S R.G.

INDEX MAP SCALER INCH^MILES

SAMPLE NUMBER

MLS-t+5 S+

Y ZINC VALUE

SOIL SAMPLELAPIERRE GROUP

SAMPLER'S INITIAL

iAMAX EXPLORATION ;N': GEOCHEMISTRY

LAPIERRE GROUP-JELLICOE ONT.; - NORTH WESTERN ONTARIO

l INCH H 400 FEET

72-33

42E,I4

42E13NW8352 63.3360 CASTLEWOOD LAKE 370

O x/

42EI3NW3352 63.3060 CASTLEWOOD LAKE

INDEX MAP SCALE l INCH "WHILES

LEGENDFIELD STRENGTH SCALE 1 1 INCH = 200 DIP ANGLE SCALE* I INCH E 200 INDICATES FIELD STRENGTH PROFILE INDICATES DIP ANGLE PROFILE FIELD STRENGTH BASE SETTING'100 TRANSMISSION STATION:SEATTLE,WASHINGTON INDICATES CONDUCTOR AXIS INDICATES CLAIM LINE

— m—— INDICATES CLAIM POST

ILLUSTRATION NOT TO SCALE

3S

-,6S -\

ft* 100

170

- STATION ON GRID LINE

-——DIP ANGLE PROFILE

- FIELD STRENGTH PROFILE

FIELD STRENGTH VALUES

•DIP ANGLESNORTH DIP ANGLES ARE INDICATED BY NUMERALS ONLY SOUTH DIP AN6LES.ARE INDICATED BY NUMERALS FOLLOWED BY THE LETTER^.

S.-IOO

AMAX EXPLORATION INCORPORATEDTYPE OF SURVEY: RADEM

AREA'CASTLEWOOD GROUP-JELLICOELOCATION -'NORTH WESTERN ONTARIO

SCALE! 400 300 200 100 0 400

1 INCH s 400 FEETBOO

DRAWN BY' KG

OPERATOR^ F

MAP No.' 72-28

DATE : AUGUST 23, 1972

REVISED:

N.T.S. No- i42E|3

TO ACCOMPANY'

BY- ^ DATE'-

380

X/

tk/

INDEX MAP SCALE l INCH-W MILES

LEGEND

-810

MEASUREMENT STATION ALONG PICKET LINE

RELATIVE VALUE OF THE VERTICAL COMPONENT OFTHE EARTHS MAGNETIC FIELD IN GAMMAS

C22!) MAGNETIC CONTOUR

MAGNETIC DEPRESSION

100 GAMMA CONTOUR INTERVAL

ENT' MC ?HAR M-500 FLUXGATE MAGNETOMETER

42E13NW8352 63.3060 CASTLEWOOD LAKE330

AMAX EXPLORATION INCORPORATEDTYPE OF SURVEY: MAGNETOMETERAREA:CASTLEWOOD GROUP-JELLICOELOCATION ; NORTH WESTERN ONTARIO

SCALE: 400 300 200 .00 0 400 800

INCH: 400 FEETDRAWN BY'K.G

OPERATOR^ R.H.

MAP No. :-72-36

DATE : AUGUST 24,1972

REVfSED :

NTS. No- :

TO ACCOMPANY

BY :______-..- DATE : -

a

INC.EX MAP -CALE llNCH'l6MtLES

J.E.M. PROFILE LOW FREQUENCY

LOW FREQUENCYREADINGS

LEGEND

FREQUENCY;'ffg [^

COIL SPACING ' 300 FEET

COAXIAL SHOOTBACK

SCALE'l INCH'200

—— ^— INDICATES CONDUCTOR AXIS

ILLUSTRATION

. STATIONS ON GRID LINE

J.E.H PROFILE l HIGH FREQUENCY

-4

r 5 ,READINGS IN DE8REES-HIGH FREQUENCY B LOW FREQUENCY

PLUS READINGS PLOTTED NORTH OF BRIO LINE MINUS READINGS PLOTTED SOUTH OF ORO LINE

1' l

ft/ s*0 1^

X/

- N/

^

^ ^ ^

^ *,vx/

AMAX EXPLORATION INCORPORATEDTYPE OF SURVEY J.E.M. SURVEY

AREA CASTLEWOOD GROUP -JELLICOELOCATION ' NORTH WESTERN ONTARIO

^^M ^^^ ^^^^^^^^^^^^~

400 300 ^00 00 C 400

SCALE: 1 INCH -- 400 FEETaoo

DRAWN BY : J.F OATE : OCTOBER 12,1972

OPERATOR: R.J.P a G.H.P REVISED'

MAP No/ 72 57 NTS- No- :42EI3

TO ACCOMPANY'.- " ^'i r~; ,BY : - x+^^t-W DATE : '

V

42EI3NW8352 63.30EC CASTLEWOOD LAKE 400'QO

™

INDEX MAP SCALE l INCH'16 MILES

LEGEND— •—INDICATES CLAIM POST———— INDICATES CLAIM LINE—— INDICATES DIRECTION OF DRAINAGE

\ INDICATES STATION ON GRID LINE

incs-13 NUMERALS INDICATE STATION NUMBER

ILLUSTRATION

SAMPLE __y STATION V

COPPER,/ VALUE ~"A

/-NICKEL VALUE

BHCS-70-sa

VSAMPLE NUMBERe f HCS-7HS

. V ZINC VALUEHCS-72-is

^- SOIL SAMPLES— CASTLEWOOD GROUP•SAMPLER'S INITIAL

^/*5^— — —— - i **., J \ **^L *c'Ss^ -- ^*rs^m —— *A. ^v ^-^-•^--^—-^^ ^^5 V\ *". s

f t ^^

X/

^^ 4f1 Illlil Illilll Illllllll III III ^ ^42EI3NWS352 63.3860 CASTLEWOOD LAKE 410 '

AMAX EXPLORATION INCORPORATEDTYPE OF suRVEY'GEOCHEMISTRYAREA'CASTLEWOOD GROUP -JELLICOELOCATION 1 NORTH WESTERN ONTARIO

^^^400 300 200 .00 0 400 800

SCALE: 1 INCH - 400 FEETDRAWN BY'K.c.G.

OPERATOR: R.H- -

MAP No.'-?2-30

DATE : AUGUST 29,1972

REVISED^

NTS. No. ;42EI3

TO ACCOMPANY :—.- . ....

BY : DATE :

B.L.0+00 RL.O*00LEGEND

FIELD STRENGTH SCALE -l INCH - 200 DIP ANGLE SCALE-l INCH = 200 INDICATES FIELD STRENGTH PROFILE INDICATES DIP ANGLE PROFILE FIELD STRENGTH BASE SETTINGMOO TRANSMISSION STATION' SEATTLE,WASHINGTON INDICATES CONDUCTOR AXIS INDICATES CLAIM POST

ILLUSTRATIONNOT TO SCALE

"l68

K* i oo

noSTATIOMS ON WU? UNE

-Oft* ANGLE PROFILE HELD STRENGTH PROFILE

KX)FIELD STRENGTH VALUES

DIP ANGLESNORTH DIP ANGLES ARE INDICATED BY NUMERALS ONLY SOUTH DIP ANGLES .ARE INDICATED BY NUMERALS FOLLOWED BY THE LETTERS

S.-100

ATTIGOGAMA GROUP

INDEX MAP SCALE:! INCH^6MILES

42E13NW6352 63.3060 CASTLEWOODLAKE

AMAX EXPLORATION INCORPORATEDTYPE OF SURVEY: RADEM

GROUP-JELLICOELOCATION' NORTH WESTERN ONTARIO

SCALE'400 500 ZOO 100 O 400

l INCH = 400 FEET800

DRAWN BY t K.C.G.

OPERATOR' J. F

MAP No.-- 72-26

DATE'JULY 25,1972

REVISED

NTS. Na--42-EJ4

TO BY: DATE*

63-3060

^-——355Q5I ^760 ^~~~——- TOO

LEGEND

MEASUREMENT STATION ALONG PICKET LINE

RELATIVE VALUE OF THE VERTICAL COMPONENT OF THE EARTH'S MAGNETIC FIELD IN GAMMAS

MAGNETJC CONTOUR MAGNETIC DEPRESSION100 GAMMA CONTOUR INTERVAL

INSTRUMENT' M*PHAR M.-500 FLUXGATE MAGNETOMETER

:s DIABASE DIKE P

—— MAFIC CONTACT

ATTIGOGAMA GROUP

INDEX MAP SCALEM INCH^SMILES

42E13NW3352 63.3060 CASTLEWOOD LAKE 430

AMAX EXPLORATION INCORPORATEDTYPE OF SURVEY: MAGNETOMETER

AREA'ATTIGOGAMA GROUP-JELLICOELOCATION' NORTH WESTERN ONTARIO

SCALE'l INCH = 400 FEET

DRAWN BY-K.c.G.

OPERATOR: R-H.

MAP No.-' 72-45

DATE'SEPTEMBER 18,1972

REVISED^

NTS. Ng:42EI4

TO ACCOMPANY^.DATE*.

f sz 'f

LEGENDFREQUENCY:

COIL SPACING^ 300 FEET

SCALE 'l INCH'200

ILLUSTRATION

J.E.M. STATIONS ON GRID LINE

- JE.M. HIGH FREQUENCY PROFILE

READINGS IN DEGREESPLUS READINGS PLOTTED TO THE LEFT OF GRID LINEMINUS READINGS PLOTTED TO THE RIGHT OF GRID LINE

ATTIGOGAMA GROUP

INDEX MAP SCALE:i INCH^6M!LES

42EI3NW8352 63.3060 CASTLEWOOD LAKE -4-40

AMAX EXPLORATION INCORPORATEDTYPE OF SURVEY: J.E.M. COAXIAL SHOOTBACK

GROUP-JELLICOELOCATION' NORTH WESTERN ONTARIO

SCALE*4O0300 206

l INCHO 406

400 FEETaoo

DRAWN BY'- K.C.G.

OPERATOR : R J P

MAP No.-' 73-15

DATE 1 JANUARY 9,1973

REVISED

N.T.S.

DATE*.

OoUJ UJ

00-JUJ CM

LJ (O

o

S

UJoPJ -J

UJ hJ

.J

*

i

^

m

l ie 'aHAS-46-j*L rapa^HAS47-is

fii a

o HAS-48-B4-

c

e * HAS'49"'-*

i

t HAS. 50-"*

a

' HAS'51-RB

1 K X.eHAS-52-eo HaS-53-jeoa"

— — — -

HAS45-M*

e aHAS-44'rf* HAS-43-IE

i(t

L, 3350^)HAS-37-a \\

\*

^AS-56-ao

iA

*

6

HA8-54-IE i

•~

335051

/^^^ ______ -41

o j y ^HAS-40-ia

rf 'Pj *HAS4I-ifV

(i AS -39 B4'i f

e

^AS-58'iK

w

S AS -3T-*i

NV *

K NN

h AS- 36^*

\ -

HAS-35^

HA6-34 J4 M ———

l 1a\u\\l! 1 1i i

||!

^"^

- —— ——————— .

HAS-7IB

HAS-6-ift'

HAS- 5 40

HAS-45*

HAS-3*

A HAS- E W i

HAS-lsn

X~\^

^

^s Sf s

**- — — -

VH HAS-8*t

iat

iA

4

J:

II

\ ^\

^

\\

1 l//'

^

^\f,'V "^ s'*'

8 —— HAS-9-t*

IK* HA8-42'Tt

US -10 -aa

f'HAS-II ee

3i

HAS -12 10

rHAS-I3'B4

4

HftS-14-io

33

' ~ — — — — ~-

~ — — - . _ __ i •P

RAS-19***""' 20'*0

6

H AS 18 6

15053 **RAS-17a

^

B

HAS-I5-BO

^

5052

^^-— — — .

6

H AS -22 w

IB

H AS -23i*

H AS -24*0

1'HAS-258

^

HAS-26**

4

——— — ,

-H

RA;

HAS

HA!

HA!

HAS

HAS

HI

133*o

•32'ie

31 a*

-30ao

29 B*

ae *oi

LEGEND—B—- INDICATES CLAIM POST

———— INDICATES CLAIM LINE——— INDICATES DIRECTION OF DRAINAGE

l INDICATES STATION ON GRID LINE JHAS-25 NUMERALS INDICATE STATION NUMBER

ILLUSTRATION

SAMPLE- STATION

COPPER VALUE

y-NICKEL VALUE

HA8-I2 .o

V-SAMPLE NUMBER

a H AS-13 M

K HAS-J4 ic

ZINC VALUE

V\ SOIL SAMPLE ATTIOOOAMA GROUP

SAMPLER'S- INITIAL

ATTIGOGAMAGROUP

INDEX MAP SCALEM INCf^ 16 MILES

42E13NWS352 63.3060 CASTLEWOOD LAKE

AMAX EXPLORATION INCORPORATEDTYPE OF suRVEY'GEOCHEMISTRY

GROUP-JELLICOELOCATION-NORTH WESTERN ONTARIO

SCALE1INCH = 400 FEET

DRAWN BY- K.C.G.

OPERATOR-R.H.

MAP No.--72'32

DATE'AUGUST 31,1972

REVISED

NTS. Ma* 42 E14.

TO ACCOMPANY BY'- DATE:

\

INDEX MAP SCALE:l INCH^6MILES

LEGENDFIELD STRENGTH SCALE' l INCH^200 DIP ANGLE SCALE M INCHED0 INDICATES FIELD STRENGTH PROFILE INDICATES DIP ANGLE PROFILE FIELD STRENGTH BASE SETTING'IOO TRANSMISSION STATION- SEATTLE.WASHINGTON INDICATES CONDUCTOR AXIS INDICATES CLAIM POST INDICATES CLAIM LINE

ILLUSTRATION

(OBt l

ioe

ZHSTATION ON GRID LINE

— FIELD STRENGTH PROFILE

100

N.+100 S.-100

DIP ANGLES

FIELD STRENGTH VALUES———DIP ANGLE PROFILE

AMAX EXPLORATION INCORPORATEDTYPE OF SURVEY: RADEM

AREA: IRWIN GROUP-JELLICOELOCATION^ NORTH WESTERN ONTARIO

SCALE*4OO 30O 2OO IOO O 4OO

l INCH * 400 FEETDRAWN BY: K.G

OPERATOR: R.J.P

MAP Na.1 73-24

DATE- FEBRUARY 8,1973

REVISED:

N.TS. ^TO ACCOMPANY: BY'. DATE:.

42E13NW8352 63.3050 CASTLEWOOD LAKE 460

\

V INDEX MAP SCALED INCH^ISMILES

LEGEND

MEASUREMENT STATION ALONG PICKET LINE

RELATIVE VALUE OF THE VERTICAL COMPONENT OF THE EARTH'S MAGNETIC FJELD IN GAMMAS

MAGNETIC CONTOUR

MAGNETIC DEPRESSION-

O MINUS: 500 GAMMA CONTOUR INTERVAL O TO 1000 i 100 GAMMA CONTOUR INTERVAL 1000 TO 3000: 500 GAMMA CONTOUR INTERVAL 3000 PLUS : 1000 GAMMA CONTOUR INTERVAL

INSTRUMENT : SCINTREX MF- 2 FLUXGATE MAGNETOMETER

AMAX EXPLORATION INCORPORATEDTYPE OF SURVEY^ MAGNETOMETERAREA: IRWIN GROUP-JELLICOELOCATION^ NORTH WESTERN ONTARIO

SCALE'4OO 3OO 200 100 O 400

l INCH ' 400 FEET800

DRAWN

OPERATOR - R.J.P

MAP No: 75-25

DATE* FEBRUARY 14,1973

: APRILI3 ' 1973 - MAY |

N.TS. No.f 42EI2

TO

BY: DATE'.

42E13NW835S 63.3360 CASTLEWOOD LAKE470

^

\

<.

INDEX MAP SCALED INCH^6MILES

LEGEND

CLAIM POST———— CLAIM LINE

-*-—— DRAINAGE DIRECTION

l His-iz STATION ON GRID LINE

ILLUSTRATION

SAMPLE^/ STATION

COPPER VALUE

^^NICKEL VALUE

HIS-55-*o

>SOIL SAMPLE NUMBER

HIS-56-5* o.o

'"— SILVER VALUE IN OUNCES a, --ZINC VALUE HIS-57-iS\v. SAMPLES

GROUP NAME-IRWIN SAMPLER'S INITIAL

anomaly-

i42E13NW8352 63.3860 CASTLEWOOD LAKE •480

AMAX EXPLORATION INCORPORATEDTYPE OF suRVEY'GEOCHEMISTRYAREA: IRWIN GROUP-JELLICOELOCATION 1 NORTH WESTERN ONTARIO

SCALE-400 300 200 100 O 4OO 800

INCH - 400 FEETDRAWN BY'- K.C.G.

OPERATOR' R H

MAP

DATE'-SEPTEMBER 6,1972

REVISED-

N.T.S. No.* 12

TO ACCOMPANY

BYV .DATE :-

ss

34*937 134*93*94*939~~ ~ |TB '

^^ J349942 134994M 349940^

j3*990* (3*9907 9*990*fr* I7s~Tfi

3*3643 l 3*3*44 l 383*49

- ,.-

193)303494•54 M j303499 30349*

. ITBl l

1094**' 8034*9 3034*41*034*3

42EI3NW8352 63.3868 CASTLEWOOD LAKE

T8

IRWIN MCCOMBER

..i42E13NW8353 63.3860 CASTLEWOOD LAKE

- M jso

IT,

500

Id l"

5 M4 M

3M2M

-5M

f?Lakt

-30!

LAPIERRE TP.

42E13NW8352 63.3060 CASTLEWOOD LAKE