GEOLOGICAL AND GEOCHEMICAL REPORT ON THE TOM GROUP by · The glacial deposits in the project area consist of a series of NW trending ridges that strongly suggest small drumlins. These

52N«8swei«e9 2.82«7 SATTERLY LAKE 010

GEOLOGICAL AND GEOCHEMICAL REPORT ON

THE TOM GROUP

by

Richard Cote

m - . ( : K t V ! . l >

MINING U K I K SI CIfOU

LABRADOR EXPLORATION (ONTARIO) LIMITED

Toronto, Ontario November, 1984

52N«i8sweee>9 2.sa«7 SATTERLY LAKE 010C

CONTENTS

INTRODUCTION

LOCATION AND ACCESS

PREVIOUS ACTIVITY

SURFICIAL GEOLOGY

GEOPHYSICS

GEOLOGY

Map Units Structure Interpretation

GEOCHEMISTRY

Whole Rock Geochemical Analyses Soil Sample Geochemical Analyses

CONCLUSIONS AND RECOMMENDATIONS

1

2

3

4

5

6

6 12 13

17

17 19

20

APPENDIX I

APPENDIX 11

APPENDIX III

APPENDIX IV

APPENDIX V

CERTIFICATE

PERSONNEL

TIME DISTRIBUTION

ROCK SAMPLE ASSAY RESULTS

SOIL SAMPLE ASSAY RESULTS

22

23

24

25

30

IN POCKETS:

Figure 1

Figure 2

Figure 3

1:2500 Tom Group Geology

1:2500 Tom Group Assay Plan

1:2500 Tom Group Geochemical Survey

INTRODUCTION

This report is a summary of a geological mapping program carried

out on the Tom Group of claims for Labrador Exploration (Ontario)

Limited. The property consists of 24 contiguous mining claims, of which

not more than 5% is water covered. Mapping was conducted by a two

person crew working from an aircraft supported camp located on the

north east shore of Exit Bay, Birch lake. Grid lines cut and chained in

the fall of 1983 were used for mapping control.

The program was carried out from May 23 to completion on June 30,

1984.

2

LOCATION AND ACCESS

The Tom Group is in the Red Lake Mining Division, Northwestern

Ontario. It is a contiguous rectangular block of 24 mining claims, 6

claims to the south by 4 claims to the west (Figure 1). The north

boundary is partly covered by the waters of Wagner Bay, Birch Lake.

The southern boundary of the property runs approximately parallel to

the northeastern shore of Exit Bay, also of Birch Lake.

The property lies approximately 100 air-km east of the town of Red

Lake and access was by bush-plane. Aircraft support was supplied by

Green Airways Ltd. of Red Lake. Alternate basis for support could be

either Uchi Lake or Confederation Lake (South Bay), both approximately

35 air-km from the property, but support facilities at these two locations

may be inadequate.

3

PREVIOUS ACTIVITY

The earliest activity on the property is reported in ODM Annual

Report, 1936. The property was first staked in 1930 by L. Wagner,

J . Kerr and H. Mayo. That same year it was optioned to the

consolidated Mining and Smelting Co. Ltd. which carried out a program

of str ipping, trenching, and sampling. The highest gold valve reported

was $13.65, at a time when the gold price was $20.67/ounce.

No further activity is known of until the reconnaissance mapping

and staking of the Tom Group by Labrador Mining and Exploration Ltd.

in the summer of 1983. Grab samples taken from the now caved-in

trenches assayed as high as 5322 ppb Au. A grid was cut over the

property and ground geophysical surveys were performed, both proton

magnetometer and VLF/EM-16.

4

SURFICIAL GEOLOGY

The glacial deposits in the project area consist of a series of NW

trending ridges that strongly suggest small drumlins. These ridges are

10 to 30 meters wide, 3 to 5 times that in length, and only 2 to 3 meters

in height above the surrounding terrain. In t ransverse section the

ridges are symmetrically rounded while in longitudinal section a number

of ridges appear to have good stoss-ee profiles with the direction of ice

movement from 290° to 310°. These ridges are made up of a reddish

brown silty to sandy fill with a wide variety of rounded pebble and

cobble sized rock clasts (5 - 15%). Clay content is highly variable (nil

- 25%).

Striations on polished bedrock surfaces, and in one instance good

chatter marks, indicate a direction of ice flow of 210° to 220°,

approximately perpendicular to the above mentioned direction. This

difference may be explained by either of two glacial histories.

1) There were two episodes of ice movement. The first ice sheet

flowed from the NE to the SW as indicated by striations. This was

followed by a change in flow to the NW producing the drumlins.

2) The ridges may in fact be end moraine and were deposited parallel

to the melting ice front. This is supported by the frequent paveity

of clay which suggests an ablation till ra ther than basal till.

The differences in these two glacial histories will be significant in

the event that a drift exploration program is undertaken.

GEOPHYSICS

5

Geophysical coverage over the Tom Group consists of a proton

magnetometer and VLF/EM-16 surveys carried out in the fall of 1983 by

CDI Surveys Inc. of Val D'Or, Quebec.

At least 5 strong conductive zones have been identified by the

electromagnetic survey constituting a total of 68 conductor axes of

various intensity. These conductive zones are all approximately parallel

and strike NW-SE extending diagonally across the proper ty . This t rend

is also parallel to that of the geological s t ructure and topography, and it

is felt that the majority of conductors may be due to conductive swampy

areas between glacial r idges. It is equally possible that these swampy

areas coincide with graphitic and/or sulfide rich less resistant bedrock

that has not yet been identified.

Zones of high magnetic susceptibility have been identified in the

central and southern parts of the surveyed area. One very strong

trend consists of 4 long narrow magnetic high striking NW-SE to N-S

running from the southern end of the property through to the nor thern .

This trend is approximately parallel to that of both s t ructure and the

electromanetic conductors, and the indicated dip is steeply to the SW.

The central and most magnetically susceptable area is centered on the

trench area on 9 & 50W between L128N and L140N where magnetite and

iron sulfides (possibly some pyrrhoti te?) are present . This trend would

constitute a single lineament were it not discontinuous.

6

A second zone of high magnetic susceptibility is centered on

tie-line 16+OOW. It crosses all grid lines along the tie-line, interrupted

only between L150N and L154N. The anomaly pattern is much less

linear. Numerous spot lights fall on a broad, generally NW-SE trending

contour pat tern. Here though the dip is steeply to the SW, to vertical.

GEOLOGY

MAP UNITS

The following map units have been identified from surface mapping

1. Miscellaneous Sediments

(a) Argillite - black to dark gray on both fresh and weathered

surfaces, aphanitic to very fine grained, thinly laminated,

moderately phyllitic and with very fine crenulations on cleavage

surfaces.

(b) Sandstone - medium gray weathering to buff, moderately to poorly

sorted with fine to coarse grained quartz sand supported in a very

fine sand to silt matrix. The sandstone overlies the argillite across

a wavy contact suggesting a scour surface. Thin upward fining

beds are facing SW and the sandstone appears to grade upward into

a second argillite bed. Rounded platty pebble sized clasts of

argillite are also found within the sandstone.

7

2. Intermediate Metavolcanics and Sediments

(a) Intermediate tuff - light brown on the weathered surface, pale

green to gray on the fresh, inequigranular and very fine to medium

grained with subangular felsic fragments. In outcrop bedding is

frequently seen and in one instance there is a distinct upward

fining (facing SW) of the fragments.

(b) Conglomerate - monomictic orthoconglomerate to moderately

polymictic and paraconglomerate. Clasts are well rounded,

elipsoidal to spherical and consist for the most par t of a fine to

medium grained felsic intrusive and possibly some rhyolite. These

clasts are pebble to cobble sized, and occasionally boulder sized.

Sedimentary clasts when present do not exceed 20% of the total clast

content and are pebble sized quartzi te , char t , and siltstone.

The clasts are supported in a tuffaceous to chloritic greywacke

matrix. The matrix becomes increasingly chloritic both up the

sequence and along the strike from north to south.

The conglomerate is intimately interbedded with the tuff.

8

(c) Mudstone - greenish gray on the fresh surface weathering to light

brown or buff. It is very fine to fine grained and typically very

good thin bedding, and upward fining is common in hand specimen.

3. Conglomerate

(a) Conglomerate - a polymictic orthoconglomerate with a distinct

dominance of mafic (gabbro? basalt?) clasts over felsic clasts,

Mafic clasts are elipsoidal, rounded, and made up of medium to

coarse grained subhedral dark green hornblend in a pale green fine

grained to aphanitic matrix. The felsic clasts are aphanitic to very

fine grained, pinkish gray weathering to buff, and very hard .

The clasts are supported in a highly foliated siltstone to greywacke

matrix.

(b) Mudstone - dark green, highly chloritic and weakly magnetic. It is

massive to poorly bedded, strongly foliated, and always found

immediately above 2c.

( c ) Undifferentiated siltstone/sandstone - medium gray weathering to

buff and light brown, massive, very poorly sorted, non-magnetic.

9

(d) Magnetite sandstone - a fine to very fine grained sandstone. It is

banded, medium to dark gray and weathers to light gray . It is a

very hard and dense rock containing 10% to 15% magnetite and 1% to

2% disseminated sulfides. The rock also contains conspicuous glassy

blue quartz eyes. It also has a vigorous and pervasive reaction to

HCL. This rock is found only in and around the trenches of 9 +

50W between L130N and L140N for a strike length of approximately

300 meters. A possible facies equivalent of the magnetic sandstone

can be found at 7 - 50W/L158N. Here the rock is dark green, and

banded carbonate and fine magnetite sandstone to siltstone.

4 • Greywacke

(a) Greywacke - medium to dark green on the fresh surface weathering

medium to dark brown. It is very fine to medium grained, highly

chloritic, probably after biotite, and strongly foliated.

Reaction to HCL is spotty to pervasive. The greywacke is usually

massive in outcrop but occasionally supports rounded pebble sized

quar tz , cher t , and siltstone clasts.

10

(b) Siltstone - pale green to medium gray weathering to buff and

reddish brown. It is fine grained well sorted and moderately

laminated to massive. Chlorite content is highly variable and

directly related to the degree of foliation. Reaction to HCL is

spotty and usually restricted to veinlets.

(c) Mudstone - texturally indentical to 2c. It differs in that it is

intimately interbedded with the greywacke (4a) and siltstone (4b) .

Contacts may be sharp but are predominantly gradational, and

lateral variations between all these units appear to be very rapid

and complex interfingering is assumed.

(d) Basalt - dark green weathering to medium green, very fine to fine

grained equigranular, massive in outcrop to moderately foliated.

Parallel alignment of fine mafic crystals to foliation suggests a flow.

Blue quartz eyes are present but ra re . The rock is non-magnetic

and exhibits a vigorous pervasive reaction to HCL.

11

5. Quartz-Feldspar Porphyry

This unit is mottled white, light to dark gray on the fresh surface

and buff to pink on the weathered. It is inequigranular

porphyritic with phenocrysts of blue to gray anhedral quartz and

light gray to white subhedral feldspar, both medium grained, set in

a very fine to fine grained groundmass of quar tz , feldspar, and

biotite. This porphyry is found as conformable sills 0.4 to 1 meter

thick, that can be seen to pinch and swell. The porphyry appears

almost aphanitic when foliated (sheared?)

6. Biotite Lamprophyre

This rock is mottled gray to black, weathering to very dark brown.

It is essentially a fine grained felsic groundmass supporting fine to

medium grained subhedral biotite. The lamprophyre is this ( 1

meter) conformable sill or dyke.

7. Gabbro

12

The gabbro is medium to dark green and white on the fresh

surface, and dark brown on the weathered. It is equigranular,

medium to slightly coarse grained, hypidiomorphic, and locally

ophitic. Occasionally it reacts quite vigorously with HCL, and

gabbro boulders have been found to be moderately to strongly

magnetic.

STRUCTURE

Structural data was collected for foliation and bedding. Foliation in

this case is taken to include both slaty cleavage and schistosity. The

foliation trend is 150° and varies from site to site by usually not more

than 15°. Dip is always to the SW and ranges between 40° and 60°.

This is assumed to normal random variation along a generally NW trend.

Bedding measurements appear to be similar to the foliation. Graded

bedding from the sandstone, mudstones, and tuffs indicate that beds are

upright .

Thus the area appears to be on the southwest limb of an anticlinal

s t ructure with a fold axis trending nortwest. No evidence for minor

folding or faulting was identified in the field.

13

INTERPRETATION

The sediments and pyroclastics found on the Tom Group represent

an upward fining basin fill sequence.

At the base of the sequence are the Miscellaneous Sediments

(Unit 1). This sandstone and argillite unit is found in only one location

and its role in the stratigraphic history is naturally ambiguous. Never

the less, it is my impression that this unit is fluvial in nature and

possibly indicates the basins margin.

Overlaying the Miscellaneous Sediments are the Intermediate

Metavolcanics and Sediments (Unit 2) . The tuff member is waterlaid as

indicated by excellent upward fining, and it is intimately associated with

a polymictic ortho- to paraconglomerate. The majority of the

conglomerate clasts are fine to medium grained felsic intrusives ,

supported in a massive tuffaceous to a highly foliated chloritic greywacke

matrix. The clast assemblage becomes increasingly polymictic from N to

S as the matrix becomes predominantly sedimentary. With regards to

OGS Preliminary Map P. 2387 an area designated Intermediate

Metavolcanics can be found to the NW of the proper ty . The tuff member

may be an extension of this unit , or the Intermediate Metavolcanics may

be the provenance for the reworked tuff and sediments. The tuff

member is overlaid by a thinly laminated mudstone.

Above Unit 2 is the Conglomerate (Unit 3) which consists of a

polymictic conglomerate, fine sandstone and mudstone. The latter two

14

lithologies are rich in magnetite and the boundary of unit is defined by

both contacts seen in outcrop, and by the magnetic anomaly pat tern .

Where the contact can be seen, it is between thinly laminated silicious

mudstone (2C) and weakly magnetic chloritic mudstone (3b) .

Although the distribution of outcrop for Unit 3 is poor there

appears to be a facies relationship between the members of this unit . In

the SE conglomerate clasts are predominantly mafic and weakly magnetic

but become increasingly felsic towards the N and NW. The magnetite in

the magnetite sandstone (3C) and mudstone (3b) may be derived from

the same mafic source area as the conglomerate, and are themselves

distal facies equivalents of the conglomerate. One outcrop of banded

magnetic siltstone carbonate (L156N/7+50W) may be an even more distal

facies of the magnetite sandstone.

Also found within the magnetite sandstone is trace amounts of

pyrite and pyrrhot i te . These minerals along with magnetite are

interpreted as distal detrital concentrations in a debris flow environment.

If this is the case it may be that the gold present in the trench area is

also detrital in nature and derived from the same mafic provenance. A

large metavolcanic terrain lies to the east of the property (OGS

Preliminary Map P.2387) and may be the provenance area for the heavy

minerals.

15

Above the conglomerate is the Greywacke (Unit 4 ) . This unit

consists of a monotonous assemblage of rythmicly laminated mudstone,

massive siltstone, and foliated chloritic greywacke, all occupying the

western half of the property. The outcrop distribution is generally poor

but even in areas where the exposure is good there appears to be very

little lateral continuity of uni ts . Locally the mudstone exhibits fine

upward fining with younging to the southwest. This upward fining is

only seen in individual outcrops and is not apparent on a property

scale. The Greywacke assemblage represents a distal basin fill

environment with some turbidite units i . e . laminated mudstone.

Three distinct intrusive units crop out on the proper ty ;

Quartz-feldspar Porphyry, Biotite Lamprophyre, and Gabbro (Units 5,6,

and 7 respectively). The Quartz feldspar porphyry is a thin (< 1

meter) sill that is frequently seen to intrude the mudstone (Unit 2C)

near the Units 2/3 contact. This association appears along BL 10W from

L96N to 116N (600 meters) and again at L150N. It is not yet clear

whether there is a single sill, either pinching and swelling or displaced

by faulting, or a number of parallel sills. In either case if the

porphyry is found in the trench area it would be a useful marker

horizon. The Biotite Lamprophyre is also a thin sill also occuring near

the Units 2/3 boundary between L146N and L150N. It also may be a

useful marker but so far has a strike length of only 120 meters.

16

The Gabbro (Unit 7) is found in the western half of the property

and appears as large eliptical subconcordent stocks trending NW-SE.

The boundries from this unit are defined by both outcrop distribution

and magnetic anomaly pat tern. The Gabbro is only weakly magnetic in

outcrop but it does coincide with very high erratic NW trending anomaly

pat tern. The highest magnetic anomaly, located in the NW corner of the

proper ty , is completely covered by bog but because it is adjacent to an

area of exposed Gabbro, it too is interpreted as Gabbro.

17

GEOCHEMISTRY

WHOLE ROCK GEOCHEMICAL ANALYSES

A total of 90 rock samples were selected from throughout the

property and assayed for gold in parts per billion. (See Appendix I I ) .

The samples are considered to be representative of each particular

outcrop.

Statistical analyses performed on the assay results yielded the

following:

Standard Deviation SD = 7.57

Variance S2x = 58.03

Mean x = 8.47

x + 2SD = 23.61 p . p . b . Au.

The mean plus two standard deviations is used as the basis for

determining anomalies values. Of the 90 samples assayed, 18 have so far

been determined as being anomalous. These are shown in Table 1.

Table 1

ANOMALOUS GOLD ASSAYS

Sample No.

F57651

F57653

F57654

F57657

F57658

F57660*

F57661

F57664

F57673

F57672

F57673

F57676

F57677

F57680**

F57681

F57683

F57822

F57840

Assay Au/ppb

51

421

819

67

29

469

143

192

33

41

36

30

Value Au/oz

0.319

0.062

0.122

0.048

0.118

0.500

Location

Trench 4

Trench 4

Trench 1C

Trench IB

18W/133N

Trench 5

Trench 5

Trench 5

Trench 1C

9+60W/134N

Trench 5

Lithology

Magnetite Sst

Magnetite Sst

Magnetite Sst

Quartz vein

Quartz vein

Magnetite Sst

Siltstone/Sst

Siltstone/Sst

Magnetite Sst

Quartz vein

Magnetite Sst

Quartz vein

Quartz vein

Magnetite Sst

Magnetite Sst

Int. Tuff

Conglomerate

Mudstone

* Repeat Sample of F57651 ** Repeat Sample of F57671

19

SOIL SAMPLE GEOCHEMICAL ANALYSES

A follow-up soil sample survey was undertaken over the Tom Group

grid by C. Davis and J. McNaughton from August 22 to 25, 1984. A

total of 379 soil samples were collected and assayed for gold in par ts per

billion. (See Appendix V).

Statistical analyses performed on the assay results yielded the

following:

Standard Deviation SD = 5.3

Variance S2x = 28.2

Mean x = 7.84

x + 2SD = 18.44 p . p . b . Au

The mean plus two standard deviations is used as the basis for

determining anomalous values. Of the 379 soil samples assayed, only 14

have so far been determined as being anomalous. A contoured plot of

the geochemical results at 10 p . p . b . intervals is shown in Figure 3.

20

CONCLUSIONS AND RECOMMMENDATIONS

The Tom Claim Group is underLain by northwest t rending,

southwest dipping sequence of basin fill pyroclastics and sedments. The

sequence consists of Intermediate Metavolcanics and Sediments (Unit 2) ,

exhibiting an intermediate to felsic provenance, followed by Conglomerate

(Unit 3) which exhibits a strong mafic provenance. The Greywacke

(Unit 4) represents a moderately distal basin environment and the

lithologies are simply monotanous basin fill, a large par t of which is

probably turbiditic. The Miscellanous Sedmiments (Unit 1) may

represent a fluvial system on the margin of the basin but this unit 's

exposure is too restricted to establish this interpretation.

The gold mineralization appears to be almost exclusively found

in the magnetitie sandstone. It is interpreted as being a facies

equivalent of the conglomerate and mudstone. This rock frequently

exhibits a colour banding between dark gray to black magnetite rich and

lighter gray magnetite poor laminae. Also small amounts of pyrite and

possibly other sulfides are disseminated throughout the rock. It is

possible that the gold is detrital in nature and par t of the heavy

minerals concentrated in the magnetite sandstone. Quartz veins in the

trench area also appear to be associated with anomalous gold values but

their role in mineralization is not yet known.

A total of 90 rock samples were selected from throughout the

property and assayed for gold. Eighteen samples returned anomalously

high gold values (Table 1) . Of these 18 samples, 10 are from the

trenches found and sampled in 1983. These anomalous values range from

21

143 to 819 ppb/Au, and 0.084 to 0.319 oz/Au (0.500 Au/Au on repeat

sample of the la t te r ) . These values reconfirm the presence of significant

gold mineralization on the property but fail to extend laterally the

showing.

One high anomalous gold value was returned for a sample outside

the trench area. At 18W/133+16N a samll outcrop of siltstone/greywacke

produced an assay of 469 ppb/Au. No other assay results for the

property exceed 100 ppb/Au.

Fourteen out of 379 soil samples taken over the grid returned

anomalous values greater than 18.44 p . p . b . Au. A contoured plot of the

geochemical assay results outlines a large haloe surrounding the trenches

as well as several other interesting areas.

Assuming that the diamond drilling program carried out in July 1984

is successful in extending the mineralized zone it is my recommendation

that an extensive program of stripping and trenching be considered for

the trench area. Equipment need should not be more than one small

bulldozer with back-hoe, and one high pressure water pump and hoseing

to wash off stripped areas. This should be followed by detailed

geochemical sampling, mapping and petrographic examination. Fur ther

work would naturally depend on the results of the above.

Also detailed prospecting and sampling should be considered in and

around the area of sample F 57664, at 18W/133-16N.

APPENDIX I

CERTIFICATE

This is to certify that:

I am a resident of Toronto, Ontario, since 1979.

I have been engaged in mineral exploration since 1976.

I am a graduate of Concordia University in Montreal and hold a B.Sc. degree in Geology.

This report is based on geological mapping carried out by myself.

I have not received, nor do I expect to receive, any interest , either directly or indirectly, in the Tom Group, property of Labrador Mining and Exploration Company Limited.

Signed in Toronto

- ? )

J . P. Richard Cote, B.Sc, Geologist

Date

APPENDIX II

PERSONNEL

Richard Cote 1216 York Mills Rd. Apt. 405 Don Mills, Ontario M3A 1Y6

Geologist 23 May-30 June 1984

Tel. 416-447-6823

Martin Cuda Assistant 23 May-30 June 1984

Chris Davis Geologist 22-25 August 1984

Jay McNaughton Assistant 22-25 August 1984

APPENDIX III

TIME DISTRIBUTION

3. Cote and Cuda

Job Description

Camp set-up Mapping Drafting and office duties Weather days Days off

2. Davis and McNaughton Job Description

Soil Survey

Total Man-days Tom Group

25

APPENDIX IV

ROCK SAMPLE ASSAY RESULTS

BELL-WHITE ANALYTICAL LABORATORIES LTD.

26

P.O. BOX 187. HAILEYBURY. ONTARIO TEL: 672-3107

Qfrrttfirat? nf Attaints NO. B603-84

SAMPLE(S) OF: R o c k < 1 9 >

DATE: July 6, 1984

RECEIVED: June, 1984

SAMPLE(S) FROM: Labrador Mining and Exploration Co. Ltd. RE: #9440-19

Sample No.

F57685 6 7 8 9

F57690 1 2 3 4 5 6 7 8 9

F57700

F57801 2 3

Au/ppb

2 2 3 4 8 3 2 4 3 4 8 5 3 3 3 4

2 10 14

IN ACCORDANCE WITH LONG-ESTABLISHED NORTH AMERICAN CUSTOM, UNLESS IT IS SPECIFICALLY STATED OTHERWISE SOLD AND SILVER VALUES REPORTED ON THESE SHEETS HAVE NOT BEEN ADJUSTED TO COMREN-SATE FOR LOSSES AND GAINS INHERENT IN THE FIRE

ASSA V F*ROCCSS.


PCR_

27

BELL-WHITE ANALYTICAL LABORATORIES LTD. P.O. BOX 187 HAILEYBURY. ONTARIO TEL: (705) 672-3107

POJ 1KO

Labrador Mining and Exploration Co. Ltd. 4600, Toronto-Dominion Centre TORONTO, Ontario M5K 1E5

INVOICE N2 16 572

ORDER NO.

DATE July 6, 1984

CERTIFICATE NO. DATE DESCRIPTION AMOUNT

B603-84 July 6/84

RE: #9440-19

19 Au, 19 sample preparations $ 190.00


28

JU

P.O. BOX 187, HAILEYBURY, ONTARIO

Qkrttfteat* of Analgata

TEL: 672-3107

NO. B635-84

SAMPLE (S) OF: Rock {37;

DATE: J u l y 1 1 , 1984

RECEIVED: J u l y , 1984

SAMPLE (S) FROM: Labrador Mining and Exploration Co. Ltd.

Sample No.

F57804 5 6 7 8 9

F57810 1 2 3 4 5 6 7 8 9

F57820 1

Au/ppb

3 4 2 5 3

15 4 4 5

10 8

10 5 7

22 16 8

11

Sample No.

F57822 3 4 5 6 7 8 9

F57830 1 2 3 4 5 6 7 8 9

F57840

Au/ppb

36 15 11 2 5 7 4

20 18 18 5 4 8

23 3

20 11 5 30

IN ACCORDANCE WITH LONG-ESTABLISHED NORTH AMERICAN CUSTOM, UNLESS IT IS SPECIFICALLY STATED OTHERWISE GOLD AND SILVER VALUES REPORTED ON THESE SHEETS HAVE NOT BEEN ADJUSTED TO COMPEN-SATE FOR LOSSES AND GAINS INHERENT IN THE FIRE

ASSAY PROCESS.


29

BELL-WHITE ANALYTICAL LABORATORIES LTD. P.O. BOX 187 HAILEYBURY. ONTARIO TEL: (705 ) 672-3107

POJ 1K0

Labrador Mining and Exploration Co. Ltd. 4600, Toronto-Dominion Centre TORONTO, Ontario M5K 1B5

INVOICE N2 16 609

ORDER NO.

DATE J u l y 1 1 , 1984


B635-84 Ju ly 11/84

RE: #9440-19

37 Au, 37 sample preparations $ 407.00

^^2-- \°i

30

APPENDIX V

SOIL SAMPLE ASSAY RESULTS

BELL-WHITE ANALYTICAL LABORATORIES LTD. P.O. BOX 187, HA1LEYBURY. ONTARIO TEL: 672-3107

Qfcrttfiratr nf Analgatfi NO. B 9 6 4 - 8 4

SAMPLE(S) OF: S o i l ( 9 2 )

SAMPLE (S) FROM:

DATE:

RECEIVED:

31

August 30, 1984

August, 1984

Mr. T. P. Ryan Labrador Mining and Exploration Co. Ltd.

Sample No.

TOM-01 -02 -03 -04 -05 -06 -07 -08 -09

T0M-10 -11 -12 -13 -14 -15 -16 -17 -18 -19

T0M-20 -21 -22 -23 -24 -25 -26 -27 -28 -29

T0M-30 -31

Au/ppb

14 14 10 26 20 18 14 28 20 4 14 30 28 20 10 4 4 2 6 8 4 2 2 2 2 4 2 4 6 6 2

Sample No.

T0M-32 -33 -34 -35 -36 -37 -38 -39

T0M-40 -41 -42 -43 -44 -45 -46 -47 -48

T0M-50

T0M-201 -202 -203 -204 -205 -206 -207 -208 -209

T0M-210 -211 -212

Au/ppb

10 8 4 8 12 2 10 14 12 12 8 14 16 4 8 6 2 4

6 14 6 2 10 10 20 14 12 10 8 6

Sample No.

T0M-213 -214 -215 -216 -217 -218 -219

T0M-220 -221 -222 -223 -224 -225 -226 -227 -228 -229

T0M-230 -231 -232 -233 -234 -235 -236 -237 -238 -239

T0M-240 -241 -242

T0M-250

Au/ppb

12 4 8 12 14 6 4 4 4 20 16 4 8 12 4 4 6 4 12 4 8 8 4 2 4 2 6 10 2 8 4

I N ACCORDANCE W I T H L O N G - E S T A B L I S H E D N O R T H A M E R I C A N C U S T O M , UNLESS IT IS S P E C I F I C A L L Y STATED O T H E R W I S E G O L D AND SILVER V A L U E S REPORTED ON THESE SHEETS HAVE NOT BEEN ADJUSTED TO C O M P E N -SATE rOR LOSSES AND GAINS INHERENT IN THE FIRE

ASSAY PROCESS.


32


POJ 1K0

Labrador nining and Exploration Co. Ltd. 46o0 T. D. Centre TOii'JiiTO, Ontario

INVOICE N2 17142

ORDER NO.

DATE August 3 0 , 1984


B964-84 Aug. 30 /84 92 Au a t $ 8 . 5 0

92 sample preparations at $1.25

$ 782.00

113.00

$ 897.00

BELL-WHITE ANALYTICAL LABORATORIES LTD. P.O. BOX 187. HA1LEYBURY. ONTARIO TEL: 672-3107

Gfrrttfirai* ttf A l ta i te

33

NO. B988-84 DATE: September 6, 1984

SAMPLE(S) OF: Soils(88) RECEIVED: August, 1984

SAMPLE(S) FROM: Mr. T. P. Ryan, Labrador Mining & Exploration Co. Ltd.

Samp .No.

TOM-49 TOM-51

52 53 54 55 56 57 58 59

TOM-60 61 62 63 64 65 66 67 68 69

TOM-70 71 72 73 74 75 76 77 78 79

* Checked.

Gold ppb

8 5 12 4 8 6 1 2 2 8 2 2 4 8 4 6 8 2 10 8 8 10 6 2 4 10 6 4 2 2 14

Samp .No.

TOM-80 81 82 83 84 85 86 87 88 89

TOM-90 91 92 93 94 95 96

TOM-100 TOM-243

244 245 246 247 248 249

TOM-251 252 253 254 255

Gold ppb

4 14 4 4 12 6 1 0 16 6 2 10 6 4 2 4 4 6 1 2 16 0 O

8 14 8 16 4 14 10 20 4 8

Samp .No.

T0M-256 257 258 259

TOM-260 261 262 263 264 265 266 267 268 269

TOM-270 271 272 273 274 275 276 277 278 279

TOM-280 281

TOM-290

JM84-67

Gold ppb

6 4 4 1 0 2 16 16 4 1 0 1 2 6 4 6 8 8 4 4 1 0 12 6 10 1 2 6

2 36* 10 8 4

8

IN ACCORDANCE WITH LONG-ESTABLISHED NORTH AMERICAN CUSTOM, UNLESS IT IS SPECIFICALLY STATED OTHERWISE GOLD AND SILVER VALUES REPORTED ON THESE SHEETS HAVE NOT BEEN ADJUSTED TO COMPENSATE FOH t - csses M<VO GAUSS IHH£RE.NT IN T H E r/R£

ASSAY PROCESS.


34

BELL-WHITE ANALYTICAL LABORATORIES LTD. P.O. BOX 187 HAILEYBURY. ONTARIO TEL: ( 705 ) 672-3107

POJ 1KO

Labrador Min ing and E x p l o r a t i o n Co. L t d . , 4600 Toronto-Dominion Cen t re , To ron to , O n t a r i o . M5K 1E5

INVOICE N2 1 7 1 9 3

ORDER NO.

DATE September 6, 1984


B988-84 Sept .6 /84 88 Au (geochem) 9 $8.50 each 88 sample p r e p a r a t i o n s @ $1.25 each

$ 748.00

no.oo $ 8 5 8 . 0 0

' -_^>A'< <-> * 1 < > /


35

P.O. BOX 187, HAILEYBURY, ONTARIO TEL: 672-3107

Qfrrttfirat* of Analgflta NO. B1033-84

SAMPLE(S) OF: Soil (199)

Page 1 of 3 DATE: September 17, 1984

RECEIVED: September , 1984

SAMPLE (S) FROM: Mr. T. P. Ryan Labrador Mining and Exploration Co. Ltd

Sample No.

TOM-9 7 -98 -99

TOM-101 -102 -103 -104 -105 -106 -107 -108 -109 -110 -111 -112 -113 -114 -115 -116 -117 -118 -119 -120 -121 -122 -123 -124 -125 -126 -127 -128

Au/ppb

4 4 4

10 8

10 10 10 14 12 8

12 10 2

14 2

10 14 28** 6 6

16 10 4

16 18 6 4 4 4 8

Sample No.

TOM-129 -130 -131 -132 -133 -134 -135 -136 -137 -138 -139 -140 -141 -142 -143 -144 -145 -146 -147 -148 -149 -150 -151 -152 -153 -154 -155 -156 -157 -158 -159

Au/ppb

4 2 8 2 8 8 6 4 6 4 6 8 6 2

12 8 4 4 6

12 10 4 2 4 2 2

10 4 6 4

12

Sample No.

TOM-160 -161 -162 -163 -164 -165 -166 -167 -168 -169 -170 -171 -172 -173 -174 -175 -176 -177 -178 -179 -180 -181 -182 -183 -184 -185 -186 -187 -188 -189 -190

Au/ppb

8 14 8

10 2 14 12 12 16 6 4 2

10 16 6 4 4

10 2 6 8 2

12 2 6 8

10 2

10 4 4

IN ACCORDANCE WITH LONG.ESTABLISHED NORTH AMERICAN CUSTOM, UNLESS IT IS SPECIFICALLY STATED OTHERWISE GOLD AND SILVER VALUES REPORTED ON THESE SHEETS HAVE NOT BEEN ADJUSTED TO COMPENSATE FOR LOSSES AND GAINS INHERENT IN THE FIRE

ASSAY PROCESS.


BELL-WHITE ANALYTICAL LABORATORIES LTD. 36

P.O. BOX 187, HAILEYBURY. ONTARIO TEL: 672-3107

Qfrrttfirat* nf Analpta NO. B1033-84

SAMPLE(S) OF: S o i l (199)

Page 2 of 3 DATE: Sep tember 1 7 , 1984

RECEIVED: S e p t e m b e r , 1984

SAMPLE(S) FROM: Mr. T. P. Ryan Labrador Mining and Exploration Co. Ltd.

Sample No.

TOM-191 -193 -194 -195 -196 -197 -198 -199 -200

TOM-282 -283 -284 -285 -286 -287 -288 -289

TOM-291 -292 -293 -294 -295 -296 -297 -298 -299 -300

Au/ppb

2 2 2

12 12 10 6 6 14 2

10 2

18 8 6 2 8

16 8

10 4 2 4 6 6 4 8

Sample No.

TOM-301 -302 -303 -304 -305 -306 -307 -308 -309 -310 -311 -312 -313 -314 -315 -316 -317 -318 -319 -320 -321 -322 -323 -324 -325 -326 -327

Au/ppb

2 12 2 8 2

40** 8 2 2 4 2 8 6 16 6 8 6

10 6 8 4 6 2 2 2 4

12

Sample No.

TOM-328 -329 -330 -331 -332 -333 -334 -335 -336 -337 -338 -339 -340 -341 -342 -343 -344 -345 -346 -347 -348 -349 -350 -351 -352 -353 -354

Au/ppb

12 8 8

18 6 8 2

10 8 8 2 6

10 10 2 2

12 2 6

10 10 6 4 2 2 4 4

IN ACCORDANCE WITH LONG-ESTABLISHED NORTH AMERICAN CUSTOM, UNLESS IT IS SPECIFICALLY STATED OTHERWISE GOLD AND SILVER VALUES REPORTED ON THESE SHEETS HAVE NOT BEEN ADJUSTED TO COMPENSATE FOR LOSSES AND GAINS INHERENT IN THE FIRE

ASSAY PROCESS.



37

P.O. BOX 187, HAILEYBURY, ONTARIO TEL: 672-3107

(Htvtxfkntt of Analgflte NO. B 1 0 3 3 - 8 4

SAMPLE(S) OF:

SAMPLE (S) FROM:

P a g e 3 o f 3

S o i l ( 1 9 9 )

DATE: S e p t e m b e r 1 7 , 1984

RECEIVED: S e p t e m b e r , 1984

Mr. T. P. Ryan Labrador Mining and Exploration Co. Ltd

Sample No.

TOM -355 -356 -357 -358 -359 -360 -361 -362 -363 -364 -365 -366

Au/ppb

8 6

10 8

18 8

12 4 6 4 8 2

Sampl

TOM

TOM

e No.

-367 -368 -369 -370 -371 -372 -373 -374 -375 -376 -377 -380

Au/ppb

10 8 2

10 12 16 4 6

10 4

10 18

** Checked

IN ACCORDANCE WITH LONG-ESTABLISHED NORTH AMERICAN CUSTOM, UNLESS IT IS SPECIFICALLY STATED OTHERWISE GOLD AND SILVER VALUES REPORTED ON THESE SHEETS HAVE NOT BEEN ADJUSTED TO COMPENSATE FOR LOSSES AND GAINS INHERENT IN THE FIRE

ASSAY PROCESS.


Pen.


POJ 1K0

Labrador Mining & Exploration Co. Ltd., 4600 Toronto-Dominion Centre, Toronto, Ontario. M5K 1E5

INVOICE N? 17 285

ORDER NO.

DATE S e p t e m b e r 1 8 , 1984

ERTIFICATE NO. DATE DESCRIPTION AMOUNT

B1033-84 Sept.17/84 199 Au @ $8.50 each 199 sample preparations @ $1.25 each

$ 1691.50 248.75

$ 1940.25

^

f)

f i

r,

SELECTION

[A:H GRP

TOM TOM TOM TOM TOM TOM TOM TOM TOM TOM TOM TOM TOM TOM TOM TOM TOM TOM TOM TOM TOM TOM TOM TOM

FOR CLAIM GRP=TOM SORTED ON RECORD tt

RECORD tt

RL696812 RL696813 RL6968I4 RL696815 RL696816 RL696817 RL6968I8 RL6968.1.9 RL696820 RL697044 RL697045 RL697046 RI... 69 7 04 7 RI. 69 7 048 RL697049 RL697050 RL697051 RI... 69 705 2 RL697112 RL697113 RL697114 RL6971J5 RL697116 RL697117

'AGE

Documents

GEOLOGICAL AND GEOCHEMICAL REPORT ON THE TOM GROUP by · The glacial deposits in the project area consist of a series of NW trending ridges that strongly suggest small drumlins. These