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52F08NW0385 21 KAWASHEGAMUK LAKE 010

Diamond Drilling

Area Kawashegamuk Lake Report NO 21

Work performed by: Esso Resources Canada Ltd.

Claim NQK 762809

K 762805

K 762804

K 762803

Hole NOFJlFJ2FJ3FJ4FJ5FJ6FJ7FJ8FJ9FJ10FJ11FJ12FJ13FJ14FJ17 .FJ18MK-1MK-2MK-3ZG-7ZG-8FJ15FJ16SK-1SK-2ZG-4ZG-5ZG-1ZG-2ZG-3ZG-6ZG-9ZG-10

Footage17m23.5m29m .38m71m35m71m47m68m44m53m44m71m74m44m44m29m20m20m83m

101m17m29m68m68m

101m50m99.5m80m60m80m

101m86m

DateFeb/84

Note

Mar/84 Mar/84 Feb/84

Oct/83 H

Mar/84 M

Feb/84 ii

Oct/83 Oct/83

(1) (i) (1) (l) (i) (l) (1) <D (l) (1) (l) (1) (1) (1) (l) (1) (l) (1) (l) (1) (l) (l) (l) <D U) (l) (1) (1) (1) (1)

Nov/83

Notes: (1) #43-85

AWL. 00517-69) rev. 9-72

II

.........1.111 iiMffl If IIS2F08NWa385 21 KAWASHEGAMUK

LAKE

THE SNAKE BAY DRILL PROGRAMME

IF: :

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OCTOBER 1983

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9 III

JANUARY 16, 1983

File #16.70

Doc. 170202

P.A. TYLER

ESSO MINERALS CANADA

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DnWiConWntB 5aF08NW03BS 21 KAWASHEGAMUK LAKE

020C

Introduction

Conclusions & Recommendations

Results

1. The Zig Zone

2. The South Katisha Zone

3. The Main Katisha Zone

Appendix I Diamond drill logs

II Assay sheets

Table 1 Summary Snake Bay Drilling - October 1983

Figures 1. Katisha Grid

2. Drill Sections ZG1 & ZG3 1:250

3. Drill Sections ZG2 & ZG6 1:250

4. Drill Sections ZG3, 9, 10, 4 1:250

5. Drill Sections ZG7 & ZG8 1:2506. Drill Sections ZG4 & ZG5 1:250

Page

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Between 1 and 2

Between 1 and 2

In Back Pocketn

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- 1 -

INTRODUCTION

Ten BQ diamond drill holes, for a total of 841.5 m of drilling, were

completed between October 19th and November 2nd by Longyear Canada Ltd.

Borehole logs are attached, hole locations are given on Fig. 1 and results

summarized on Table 1. The average cost was $62.31 per metre drilled.

Of the various zones located during the 1983 exploration programme, only

the Zig, south Katisha and Main Katisha were drill tested. The Fiji

Kawijekiwa and 0 veins will be tested in early 1984.

Results from the Zig and South Katisha confirm the low grades obtained

from trenching. The South Katisha, however, was wider and stronger than

surface mapping had indicated. Interpretation of results from the Main

Katisha is complicated by a number of felsic dykes and further drilling is

required.

A core logging and storage facility has been established at Pine Sunset

Lodge, Dinorwic.

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TABLE I

SUMMARY SNAKE BAY DRILLING -

HOLE /

ZG 1

ZG 2

ZG 3

ZG 4

ZG 5

ZG 6

ZG 7

ZG 8

ZG 9

ZG 10

ANGLE

45*

45"

45'

45"

45"

45*

45°

45'

45*

45'

AZIMUTH

065°

060"

245*

065°

065°

065°

003'

003°

267"

087°

OCTOBER 1983

DEPTH (M) TARGET ZONE SIGNIFICANT ASSAY. CCfNENTS

99.5

80.0

60.0

101. 0

50.0

80,0

83.0

101. 0

101.0

86.0 "84775"

lOz Per t/m)xx

Zlg 0.04/0.9

Zlg ']•'

Zlg

South Katlsha

South Katlshe

Zlg

Main Ketlsha & Portage

Main Katlsha

Zlg

South Katlsha

0.03/0.65

Nil

0.02/0.70

0.05/4.0

Tr

Tr

0.68/0,55

0.03/1.00

0.02/1.10

Narrow zone of slllclflca- tlon In Carbonatlzed shear zone

.

Slllclfled zones adjacont to felslc dykes, In a pervasive zone of cerbonetlzetlon

As ZG 1 & ZG 2

Narrow zones of sll Iclf Icatlon localized edjecent to felslc dykes, In zones of carbonization

As ZG 1 & ZG 2

As ZG 4 & ZG 5

Average of 30 m per shift

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CONCLUSIONS AND RECOMMENDATIONS

The .gold values obtained in the drilling were comparable to those

obtained by surface sampling in both the Zig and South Katisha zones and in

both these zones the surface and sub-surface geology could be related. This

was not the case with the Main Katisha however, where the surface and

sub-surface could not be connected and where the down-dip continuation of the

zone was not located.

It is recommended that;

(i) Two further holes be drilled on the south Katisha structure, one 30 *

metres to the north of ZG 5 and the other 30 metres south of ZG 4, for a

total of 160 metres of drilling.

(ii) At least three short holes, for a total of 60 metres of drilling, be

drilled to better define the down-dip extension of the Main Katisha.

The regional and detailed geology of the Katisha area has been described

in a report by Randy Hall, November 1st, 1983.

The three zones drill tested are localized along minor structural zones

within a 350 m thick, differentiated gabbro sill. Within the structural zones

the gold is localized within zones of silicification, which have overpinted an

earlier, more pervasive carbonatization and sericitization. The gold is

associated with pyrite, arsenopyrite and traces of chalcopyrite and

sphalerite. Extensive zones of mariposite are developed in places and

occasional TourmaTene has been noted. |

- 3 -

1. THE ZIG ZONE

Where exposed, the Zig is a 5-20 m wide zone of sericitized, pyritized

and silicified sheared meta gabbro within a wider, foliated structural zone

striking at 340°. Channel samples ranged from 0.02 to 0.24 oz/ton Au over 50

cm. The average grade was 0.02 oz/ton Au.

To the south of the road drilling from the east, which would have allowed

for shallower holes, was not possible because of the presence of cedar swamp.

ZG 1 and ZG 2 were collared 50 m apart to intersect beneath the north and

south ends of the trenched area. Results are summarized on drill sections -

Figs 2 and 3. A zone of strongly foliated and carbonatized gabbro 20 to 30 m

wide corresponding to the surface feature was intersected in both holes. The

zone contained narrow sections up to 2 m in width with a 20-90% silicification

overprint and containing generally 5-10% disseminated pyri'te. No

aresenopyrite was noted. Four intersections of above trace were obtained;

0.01 oz/ton Au/0.95 m, 0.03 oz/ton Au/0.65 m, 0.015 oz/ton/3.50 m and 0.04 oz

ton/0.90 m. All of these were within zones of silicification.

ZG 6 was collared 55 m south of ZG 2 and intersected the continuation of

the same structural zone. However the intensity of both the foliation and

carbonatization had decreased markedly. Two narrow zones of weak

silicification with 1-2% pyrite were intersected, both assayed trace.

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1. THE ZIG ZONE (Cont'd)

ZG 3 and ZG 9 were drilled to intersect the northern extension of the

zone. ZG 9 was also part of, a fence of twoholes between the Zig and South

Katisha zones. ZG 3 intersected only weakly carbonatized metagabbro centred

on a narrow zone of foliation, which seems to correspond to the eastern

boundary of the foilated zone Intersected in the holes to the south. ZG 9

intersected two zones of strong foliation. The most easterly of these

contained three narrow zones of silicification with 1-5X pyrite. All assayed

trace. Four close spaced 0.5 - 1 cm wide quartz/carbonate veins with

Tourmaline, specks of disseminated chalcopyrite and minor mariposite were

Intersected in the westerly foliated section. A 1 metre sample centred on one

of these veins returned an assay of .03 oz/t Au. The others assayed trace.

2. THE SOUTH KATISHA ZONE

Surface mapping had outlined a wide zone of pervasively carbonatized,

sericitized and silicified netagabbro striking at 335°. Except for a single

value of .06 oz/ton Au, sampling returned values of Nil to 0.02 oz/ton Au.

Three holes, ZG 5 north of the road and ZG 4 and 10 south of the road,

have intersected the zone.

- 5 -

2. THE SOUTH KATISHA ZONE (Cont'd)

ZG 4 and 10, drilled approximately on section, intersected a zone of

20-90% silicification 14 to 23 in in width and dipping 45c-55° to the west.

The sil.icification occurs at the base of a wider zone of pervasive

carbonatization and is post-carbonatization in age. A number of thin banded

or coloform carbonate veins were intersected. Many of these were silicified.

Some of the silicified sections were brecciated and re-cemented with silica

indicating a prolonged period of tec^dnj-efn and mineralization. The

silicified sections generally contain 2-5% pyrite. A 3m wide felsic dyke was

intersected in both holes within the silicified zone. Gold values, generally

associated with the most intensely silicified and pyritized sections, were

sporadic and ranged between 0.01 and 0.02 oz/t Au.

ZG 5 intersected 18 m of similar alteration between 20.5 and 37.5 m,5 m

of which graded .04 oz/t Au from 20.5-25.5, including .09 oz/t Au over 1.2 m.

This section is faulted to the west at 20.5 m with 0.5 m of sheared, Talcose

silicified gabbro between 20.00 and 20.5 m. A carbonatized felsic dyke was

intersected near the base of this section.

- 6 -

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3. THE MAIN KATISHA ZONE

On surface the zone consists of a 10-300 cm wide zone of foliated,

sericitized and pyritized rock striking at 300°, sub-parallel to the north

contact of the metagabbro and the overlying metasedimentary rocks and striking

into the metasediments at the eastern end of the trenching. The lamination in

the metasediments dips 70° N.

The zone has been traced over a strike length of 100 metres. The channel

sample results ranged from nil to 3.42 oz/ton Au, which averages to 0.21

oz/ton Au over 1.5 m for 42 m uncut or 0.07 oz/ton Au cut. The Au values are

associated with silicification.

To the south of the Main Katisha at the eastern end of the zone as

exposed, a discontinuous zone of sericitization and silicification is exposed,

the Portage zone. The zone contains up to 10% pyrite with traces of

sphalerite. Channel samples returned 0.10 to 0.50 oz/ton Au.

Two holes, ZG 7 and ZG 8, were drilled to test the down-dip extension of.5

the zone-Fig. 6. This was not found In either hole either because;

I) The zone is dipping at 75° to the north on less. Surface mapping(

) suggests this Is unlikely.

-7 -

3. THE MAIN KATISHA ZONE (Cont'd)

11) The zone does not continue at depth, possibly having an en echelon

relationship to the gabbro-epiclastic contact. If this IB the case then the

down-dip continuation of the contact and not the vein may be the target.

ill) The vein is cut-off or displaced along the felslc dykes Intersected

in both holes. The dip and strike of these is unknown and cannot be tied in

with surface outcrop conclusively.».

ZG 7 was collared to test for a possible down-dip extension of the

portage zone. This was not seen in the core. A similar looking section,

which averaged 0.25 oz/ton Au over. 1.55 o, including 0.68 oz/ton Au over 0.55

m, was however intersected in ZG 8 between 13.05 and 14.60 m. Any up-dip

continuation of this zone has not be seen on surface.

Short holes, drilled from the north, are planned for the winter 1984

programme.

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APPENDIX I

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APPENDIX II

CUSTOM FIRE ASSAYINGPAULOKANSKI.Assayer

Box 253, Cochenour, Ontario POV ILO

Esso Mineeiis Canada ASSAY CERTIFICATE

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iltfd L»U Prml,r| Co Lid.

iAu *4

Esso Mineral Can. Ltd.



ASSAY CERTIFICATE

Phone: Bus. 662-8171 Res. 662-3361

Date: Oct. 31-83

*mple No. Description oz/tonAu oz/ton Ag

race

25

1 26

27

.01Trace

-52-

w

U3

Aiujrtr. f: ^^^\

IW.

1Ii i

_--._ ——— ..•_!!• (•Illglll II

52F88NW«385 21 KAWASHEGAMUK LAKE

030

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SNAKE BAY WINTER DRILL PROGRAMME

JANUARY - MARCH 1984

> • f• ! i '— •"-*

I..-'"\ •. •

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File: 16.7

Doc. #0805

P. MORETON


i - 1 -

I I I I I I

INTRODDCTION

Twenty-three diamond drill holes, for a total of 1035m were drilled

between January 30th and March 14th, by Longyear Canada Ltd. Eighteen of the'

holes were drilled testing the Fiji vein, two the South Katisha structure, and

three the Main Katisha structure (Fig. l).

All eighteen holes (FJ-1 to 18) drilled (at/>/25m spacings) intersected

the Fiji vein with sporadic gold values obtained over narrow widths. The two

holes drilled on the South Katisha vein vere collared 30m along strike from

holes drilled (ZG 4, 5) during the 1983 fall programme. The three holes

(MK-1, 2, 3) drilled on the Main Katisha zone were collared (•< 10m) close to

the surface trench in order to find any down dip extension of which none was

found.

• Result of the above holes are summarized in Table #1, hole logs and

assays are in Appendices 3 and 4, and drill sections are located in the back

II

I

pocket.

Average cost of drilling was 72.39$ per metre drilled.

ii

ISSO»ill II (111 Ulllim (Hill 11111(1

Mosnci, DIAMOND DRILL HOLE LOCATIONS SNAKE BAY PROPERTY

O Verticol hole *--O Verticol and Inclined holes, same collar

memo

LAKE K 762809

1I

11 ' " 'II11

•V™:: •r«

i, ;• •

1 •

•f%4^B1 • 'BI'm

1: "

11", "

II£ '

IIits'

y .

1f •f."

- 3 -

•^^fc TABLE 1

HOLE f

FJI

FJ2

FJ3

FJ4

FJ5

FJ6

FJ7

FJ8

FJ9

FJIO

FJII

FJI2

FJI3

FJI 4

FJI5

FJI6

FJI7

FJI8

SK-I

SK-2

J"K-I

KK-2

WC-3

•^

AW3LE

45'

90*

45'

90»

45'

90'"

45*

90*

45*

90*

45°

45*

90*

45"

45°

45"

45'

90s

45°

45"

45°

45*

45*

Total

AZIMUTH

015'

015*

015*

015'

015*

015"

015*

015*

015*

015*

015*

030'

030'

015'

015'

015*

015*

065*

065*

003*

003 *183*

Meterage

SLW.RY

DEPTH (M)

17

23.5

29

38

71

35

71

47

68

44

53

44

71

74

17

29m

44

44m

68

68

29

20

20

1035m

SKAKE BAY DRILLINS - FEBRUARY, KARCH 1983

TARGET ZONE

FIJI

FIJI

FIJI

FIJI

FIJI

FIJI

FIJI

FIJI

FIJI

FIJI

FIJI

FIJI

FIJI

FIJI

FIJI

FIJI

FIJI

FIJI

South Katlsho

South Katlsha

Main Katlsha

Main Katlsha

Kaln Katlsha

SIGNIFICANT ASSAYCAu (Oz/Ton)/Hetre)

0.05/0.4«

-

0.09/0.37m

Tr

.045/1. 25m, 0.07/0. 5m

Tr

Tr

Tr

.04/l.46ro

Tr

Tr

.06/4 2m

,05/1/1. 03m

Tr

.14/.l5m,.03/.6m

.04/0. 5m, ,03/0. 3m

Tr

.06.1.00m, .04/1 .28m

Tr

Tr

Tr

Tr

COWEKTS

- sll lclfled,cerbonltlzed gabbro, py-espy

- slllclfled zone 5£ aspy

- slllclfled zone 2f a spy.- cerbonltlzed gebbro, py.

- slllclfled gebbro, 2 % py

pyasp

-

- visible gold In quartz-cb stringer cutting slllclfled-zone

- qz-cb vein In pyrltlzedgabbro

- slllclfled zones, 5£ aspy_ H n H

. py"

- slllclfled, pyrltlzed basalt

- slllclfled, pyrltlzed basalt5- 10* py

•

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CONCLUSIONS AND RECOMMENDATIONS

Drilling on the Fiji vein indicates that it IB a continuous, although

anastomozing structure, for over 280m of strike length. The assay values

obtained from drill intersections are consistently lower (Tr. to 0.14 oz/ton)

than those obtained from surface trenching (Tr. to 0.28 oz/ton 50 cm). The

vein with its accompanying alteration and mineralization has been tested down

dip from 20 to 70 metres along its strike length with no economic gold values

obtained over mineable widths.

Drilling on the South Katisha structure indicates a proven strike length

of 100 metres with good potential for strike extension, particularly to the

'southeast. It is recommended that further stripping, trenching, sampling and

mapping be carried out along the southeastern extension of the South Katisha

structure in order to outline possible future drill targets.

The Main Katisha structure was not intersected in any of the three holes

drilled, therefore indicating that the zone does not extend down dip greater

than 10 meters. No further work is recommended on the zone.

I

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I I I I I I I I I

- 5 -

FIJI VEIN

A series of eighteen diamond drill holes were drilled on the Fiji vein

| covering a strike length of 285m. The drilling consisted of ten - 45° holes

• drilled at 015°, seven vertical holes, and one hole oriented at 030° and 45*.

Foutree,n of the holes were drilled on Howie Lake and four on land (Figs 1 and

• 23). All holes intersected the Fiji vein which confirm the apparently

continuous nature of the vein on surface. This continuous nature and overall

• strike of 115° is complicated by two "breaks" located at 1+25W and 0+25W

• (Fig. i?2). These "breaks" are defined by a sharp strike change from 115"

to 160°. They may represent a primary change in attitude of the vein or

• possibly late offsets along NNW trending faults.

Alteration and Mineralization - The alteration zone associated with the

Fiji vein dips from approximately 25° to 45° to the southwest and is defined

by the appearance of disseminated leucoxene (0.5 to 5. OX) in the hanging wall

and footwall gabbro adjacent to the vein. The formation of the leucoxene is

accompanied by weak, non-pervasive carbonitization of the gabbro. The

leucoxene alteration zone varies in width from 7 to 16 metres (Table

Immediately adjacent to the vein then, ^.2m wide, carbonitized zones are

developed in the gabbro. These carbonitized zones are creamy grey-white in

colour and contain from 1 to 5% disseminated pyrite as well as leueoxene,

tourmaline and minor fuchsite.

II•:;•

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- 6 -

FIJI VEIN (Cont'd)

The alteration zones are cored by a series of colliform-texturedIcarbonate veins which range in width from 0.05 to 1.25m and are composed of

grey to white carbonate with minor pyrite.

The colliform-textured carbonate veins have been extensively brecciated

and stockworked by a series of quartz veinlets (5 to 80% quartz veinlets).

Local zones (<^10cm) of quartz flooding are developed in the brecciated areas.'

The quartz veining is most strongly developed at the margins of the carbonate

veins with subsequent zones of silicification developed in the previously

carbonatized gabbro wallrock adjacent to the vein.

Pyrite found as disseminations and in thin, irregular stringers in' • • amounts ranging from 2 to 15% is ubiquitous (,in the quartz-flooded and

: M' silicified zones. Less common is arsenopyrite which was found in eleven of

the holes occuring in thin (<120cm) zones associated with extensive quartz

veining and/or silicification. It is present as -fine needle-like

disseminations with pyrite and in thin bands of massive arsenopyrite. Minor

amounts of fuchsite and tourmaline are' associated with the quartz stockwork

and silicified zones.

II I I I II

I I II

- 7 -

I I I I I

FIJI VEIN (Cont'd)

Native gold was found as two 1.00mm grains in the margin of a

quartz-carbonate vein in d.d.h. FJ-12. The vein is crosscutting an

arsenopyrite-pyrite bearing silicified zone.•,

Minor scheelite, chalcopyrite, sphalerite and pyrrhotite were found as

disseminations in thin quartz-carbonate stringers in some holes.

No zones of pervasive tectonism (foliated, schistose zones) are

associated with the Fiji Vein and the zone appears to have formed in a

tectonically quiescent fracture system. Thin, <2.0m fine-grained, felsic

dykes were found within the altered zones in four of the eastern most holes

(FJ-11, 12, 13, and 18).

Thin, less pervasive and presumably parallel alteration zones were

intersected 5 to 35m below the Fiji zone in seven of the holes. Two of these

zones (FJ-9, 12) are gold-bearing. No surface expression of these zones has

been found by field mapping.

M

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ASSAY RESULTS

Overall assay results from the holes drilled on the Fiji vein indicate

that to the depth drilled, the vein contains low and sporadic gold values.

Assay results range from trace to a high of 0.14 oz/ton. The majority of the

assay results which have values greater than trace were obtained from thin

silicified zones which contain abundant arsenopyrite.

SOUTH KATISHA (84-SK-1.2) ZONE

Two holes were drilled thirty metres along strike on the South Katisha

structure from the two holes collared (ZG-4.5) in the 1983 fall drilling

program (Fig. #1). The structure is continuous for the 90m of strike length

it has been tested. The intersections in d.d.h. 84-SK-l and 2 indicate that

the South Katisha structure developed along the approximately vertical contact

between a fine-grained mafic rock (basalt ?) to the south and a medium to

coarse-grained gabbro to the north. Along the contact a quartz-dioritic

dyke/sill has been intruded.

In SK-2 the contact zone is intruded by a thick (16m in 84-SK-2) quartz

dioritic dyke/sill which is weakly altered. To the south the quartz dioritic

dyke/sill) progressively thins, being only 2m thick in 84-SK-l (Figure #24).

Ijp;

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- 9 -

Alteration and Mineralization - The alteration zone is centred along the

basalt/gabbro contact. It is present on a weakly to intensely silicified

and/or quartz veined zone. The silificication occurs over widths of 2m in

84-SK-Z, to 30m in 84-SK-l. The zones of intense silicification (>70% quartz)

are generally no greater than 1.5m in thickness and have from 2 to 15%

disseminated pyrite. The silicification is overprinting an earlier pervasive

and more widely developed carbonitization.

Foliated zones are common adjacent to the silicified zones within the

carbonatized basalt and gabbro. In drill core, the foliation is consistantly

oriented 40-60° to the s.c.a. which identifies a relatively steep orientation

(75°W-75°W) to the zone, which is consistant with the field data (Fig. 24).

Assay Results - show that gold mineralization is associated with

intensely-silicified pyritized zones. Two zones in 84-SK-l (0.06 oz/ton over

1.00m and 0.04 oz/ton over 1.28m) occur is silicified zones with 2-10%

disseminated pyrite.

IIs

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I 1III

jjjp

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- 10 -

MAIN KATISHA ZONE

Three diamond drill holes were collared in order to test the immediate

• down-dip extension of the Main Katisha zone (Figure 1, ddh section ZG-7, MK

1-3). .Two of these holes (MK-1, MK-2) were collared approximately 10m south

• of the zone and intersected massive gahhro with only minor carhonitized and/or

foliated zones with no associated gold mineralization. One hole (MK-3) was

• collared to the north of the zone in epiclastics and was drilled through the

• epiclastic/gabhro contact with no mineralized zones intersected.

It is clear that the Main Katisha zone which is continuous on surface for

over 100 metres along strike does not have a down-dip extention of more than

10m under the most intensely mineralized/altered portion. The Main Katisha

zone may therefore be a flatly plunging rod-like zone found at the

intersection of two structures or alternatively a lens-like structure which

extends down-dip into a weakly carbonitized and/or foliated zone with no

associated gold mineralization.

The Main Katisha zone is the only structure drilled on the property which

does not have a down-dip extension consistant with the surface geology.

i - 11 -

p• Jfe1 •(11

*.

HOLE /'S

!• FJH ' 2-',:

1|: FJ-3,4 ^11, FJ-5,6

II- '

i|| FJ-7, 8

:"-

I|l FJ-9, 10

iI!

TABLE 2

FIJI AND LOWER ZONE WIDTHS

THICKNESS OF LEUCOXEKE ALTERATION ZONE SILICIFIED ZONES

FIJI Zone - 7m FJ-IFJ-2

FIJI Zone - 10m FJ-3FJ-4

FIJI Zone - 9n> FJ-5Lower Zone - FJ-6

(FJ-5) 7m FJ-5

FIJI Zone - 12m FJ-7FJ-8

Lower Zone.- FJ-7 (FJ-7) 26m

FIJI Zone - 6m FJ-9FJ-IO

Lower Zone - FJ-9

In2, l/2m

2mIm, 3/4ra

l/2m, 2, l/2m2m l/2m

l/2m, 3/4m2ml/2m (3)

3ml/2m1, l/2m

I

APPARENT DIP

40*S

35*5

25*S

25*S

25*S

Doc. /I805

(FJ-9) 13.5m

FJ-I2,I3 FIJI Zone - unknown FJ-12 1/2(2) 35*SFJ-13 Im (2)

Lower Zone - FJ-12 I/2m, I, I/2m 35»S (FJ-12) 8m (Total) FJ-I} l/2m (FJ-13) 30m

tsso(ill II (It) ilttiKH (HIM imlll

msKci:DIAMOND DRILL HOLE LOCATIONS SNAKE BAY PROPERTY

O Vertlcol hole »-O Vertlcol ond Inclined holes,some collar

lOIOktO

MM

LAKE K 762809

CSSO HII.HHJ C»NW tin ii mi Minim IIIMI limn

•:DIAMOND DRILL HOLE LOCATIONS SNAKE BAY PROPERTY

O VertlcolholeVertlcol end Inclined holes,some collar

LAKE K 762809

mo unions C»HWin i ir nil mmm IMIII

DIAMOND DRILL HOLE LOCATIONS SNARE BAY PROPERTY

0 Vertical holeVertical and Inclined holes,tame collarLAKE

K 762805K 762802

K 7.62803 K 762804

LAKE K 762809

38 ROAD

tSSO mmm C'MDA tin i r mi IIIHKII pun until

: DIAMOND DRILL HOLE LOCATIONS SNAKE BAY PROPERTY

O Vertlcol holeVertlcol ond Inclined holes,some collar

1010*10 III 11

LAKE K 762809

I I

Drill Logs

I

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PROPERTY

NTS CODE

Sn£ke LOCATION . .Howie 'Lake

HOLE NO.

LATITUDE . 2t9°.W. ......... AZIMUTH

DEPARTURE . . 1 .8 **. s ?v? t.h . ...... DIP .".

ELEVATION

SECTION

REF. GRID

l85 'PURPOSE

STARTED

Test Fiji Zone (West End)

Feb. 2nd, 1984

CORE .B P. ............... COMPLETED .F(: b/ .? r.d .' A98 *

LOGGED BY . ?'. ?lc? r.e f:c? n.

DIP TESTS

FOOTAGE

TEST FROM

/

TO TOTAL

DIP

CORP.

LATITUDE

CUM.

DEPARTURE

CUM.

FROM

0.0

2.0

6.1

7.0

9.0

9.5

TO

2.0

6.1

7.0

9.0

9.5

9.7

LITHOLOGY

CASING

Medium-coarse-grained GABBRO -massive, unaltered -57, magnetite

Fine-grained GABBRO

LEUCOXENE-BEARING GABBRO -weakly foliated > -5% carbonate stringers

CARBONATIZED GABBRO -tr. pyrite

SILICIFIED GABBRO-5 to 7% pyrite disseminated-aspy bands, locally up to 10% aspy-silicified carbonatized gabbro fragments

9.7 10.1 BRECCIA ZONE-composed of carbonatized gabbro fragments with quartz matrix

10.1 10.5 SILICIFIED ZONE-massive texture-2% disseminated aspy, abundant fuchsite

10.5 10.8 Weakly SILICIFIED ZONE- as silicification decreases foliation increases-foliation 75 to c.a.

10.8 13.0 Leucoxene-bearing GABBRO-10% leucoxene, 2% pyrite, 5% carbonate stringers

13.0 17.0 Massive, equigranular, unaltered GABBRO

17.0 E.O..U.

ASSAY RESULTS

SAMPLE // FROM TO WIDTH ASSAY OZ/TON

00010002000300040005

8.89.49.810.010.6

9.49.810.010.611.9

0.60.40.20.61.3

0.20.50.20.1Tr.


PROPERTY . ??a.k .e . B.a y LOCATION

NTS CODE HOLE NO.

LATITUDE

DEPARTURE

2+OOW

18M South

AZIMUTH 1 9 .5 ° '. PURPOSE Test ^iji Zone (West Zone)

Q|p - 90° ....... STARTED 1?c.b ; . 3.r ^». -1 ? 8/1 .

ELEVATION CORE . B.Q. ............... COMPLETED .F <: 1V. 3. r.d i

SECTION .

REF. GRID

LOGGED BY

DIP TESTS

FOOTAGE

TEST FROM

i

TO - -TOTAL

DIP

•

CORR.

LATITUDE

CUM.

DEPARTURE

CUM.

FROM TO LITHOLOGY

0.0 2.5 CASING

2.5 6.8 Unaltered Coarse-grained GABBRO

6.8 8.2 Unaltered Medium-grained GABBRO

8.2 10.5 Leucoxene-bearing GABBRO-1 to 5% leucoxene, 5% carbonate stringers

10.5 13.1 CARBONATIZED-SILICIFIED GABBRO- well banded 50 to c.a.-2 to 10% pyrite-12.2 to 12.5 colliform-textured carbonate vein

13.1 14.2 CARBONATIZED-PYRITIZED GABBRO-3% disseminated pyrite

14.2 14.5 Brecciated CARBONATE VEIN-arsenopyrite in stringers

14.5 14.6 Carbonatized Pyritized GABBRO-57. pyrite

14.6 16.3 Weakly to Intensely CARBONATIZED GABBRO

16,3 17.1 CARBONATE VEIN-5% quartz stringers with pyrite, pyrrhotite and arsenopyrite-contact 90 to c.a,

*

17.1 18.7 CARBONATIZED GABBRO —•••- medium-grained abundant leucoxene

18.7 19.4 / Weakly altered GABBRO

19.4 25.0 Unaltered Coarse-grained GABBRO-5% magnetite

25.0 E.O.H.

SAMPLE // FROM TO WIDTH ASSAY OZ/TON

000600070008000900100011001200130014

10,10.11.

14, 16,

12.412.914.0

16.5

10.711.512.412.914.014.515.016.517.0

0.30.8 0.9 0.5 1.1 0.5 0.-5 0.3 0.5

Tr.Tr.Tr.Tr.Tr.0.02Tr.Tr.0.01


PROPERTY

NTS CODE

Snake Bay Howie, LakeLOCATION

HOLE NO. , , F.J 73. <? 9.'?«>,

LATITUDE r ..r.. r .YTr.1^ . AZIMUTH

O e:cDEPARTURE . .... ..........

ELEVATION ...............

SECTION

REF. GRID

DIP TESTS

. ?l 5. ........... P URPOSE ' , v.L ^. i. ,z?n.c .

DIP . 7 ? ?*. . ............. STARTED Fe.b : . 4 .«. l 9 .8^ . .

CORE D Q. ................ COMPLETED .Fc. b;.V.i 98 f

LOGGED BY ?•. .M? r.e .t ?n. .

FOOTAGE

TEST FROM

i

TO TOTAL

DIP

CORR.

LATITUDE

CUM.

DEPARTURE

CUM.

FROM

0.0

2.5

9.4

10.15

11.1

12.3

13.4

16.2

16.3

16.85

17.0

TO

2.5

9.4

10.1

11.1

12.3

13.4

16.2

16.3

16.85

17.0

17.8

17.8

18.2

23.0

18.2

23.0

23.2

LITHOLOGY

CASING

Coarse-grained GABBRO

Fine-grained unaltered GABBRO

Leucoxene-bearing GABBRO-minor carbonate stringers

Fine-to-medium grained GABBRO

Weakly CARBONATIZED GABBRO

CARBONATIZED GABBRO- foliation 80 to c.a.

Laminated QUARTZ-TOURMALINE VEIN-contact 90 to c.a'.-abundant pyrite in adjacent wallrock

PERVASIVELY CARBONATIZED GABBRO-fuchsite-bearing bands 80 to c.a.

SILICIFIED GABBRO-10 to 20% arsenopyrite, banded 90 to c.a.

Brecciated-silicified colliform-textured CARBONATE VEIN-15% quartz stringers-locally abundant tourmaline

Well-banded Pyritized-Silicified GABBRO-banding 90 to c.a.-trace arsenopyrite,2% pyrite

Weakly Carbonatized Leucoxene-bearing GABBRO- thin quartz stringers

SILICIFIED GABBRO-5% pyrite in quartz, stringers-abundant fuchsite, coarse pyrite ------'

FROM

23.2

26,8

27,0

27.2

28.5

29.0

TO

26.8

27.0

27.2

28.5

29.0

LITHOLOGY

Weakly altered Leucoxene-bearing GABBRO

Colliform-textured CARBONATE VEIN-crosscut by quartz-tourmaline stringers

Pyritized GABBRO

Weakly altered Leucoxene-bearing GABBRO-minor disseminated pyrite

Unaltered Medium-grained GABBRO

E.O.H.

SAMPLE FROM TO WIDTH ASSAY OZ/TON

0015001600170018001900200021002200230024

10.410.715.816.116.5316.917.718.122.626.6

10.710.916.116.5316.9017.718.118,6223.127.05

0.30.20.30.430.370.80.40.520.50.45

Tr.Tr.Tr.0.010.09Tr.Tr.Tr.Tr.Tr.


PROPERTY

NTS CODE

LOCATION

HOLE NO. •« 7

LATITUDE . .1 t5.0^ B.-!) » s.cHn.e . . AZIMUTH PURPOSE

DEPARTURE . ?6M South. ...... DIP y9r. t .1 9 n.1 . ............ STARTED F, c,

ELEVATION ............... CORE ? Q. ................ COMPLETED

Zne

5c1 '

SECTION LOGGED BY . , p.'. t10 .r ? t.0 .n

REF. GRID

DIP TESTS

FOOTAGE

TEST FROM

i

TO TOTAL

DIP

CORR.

LATITUDE

CUM,

DEPARTURE

CUM.

FROM TO LITHOLOGY

0.0 1,5 CASING

I.5 11.0 Coarse-grained GABBRO

II.0 14.0 Fine-grained CABBRO

14.0 16.8 Leucoxene-bearing GABBRO-locally intensely foliated 80 to c.a.

16.8 17.7 Silicified Brecciated CARBONATE VEIN-10% quartz stringers-well developed banding 50 to c.a.-5% pyrite

17.7 18.1 Carbonatized GABBRO-well developed foliation 50 to c.a.

18.1 19.3 Leucoxene-bearing GABBRO

19.3 20.0 SILICIFIED GABBRO-well banded 90 to c.a.-minor disseminated pyrite


23.4 28.7 Massive unaltered GABBRO

28.7 29.3 Foliated GABBRO-5% magnetite-foliation 50 to c.a.

29.3 33.1 , Mngnetito-benring GABBRO-7% magnetite

33.1 37.0 Feldspar-phyric GABBRO

37.0 E.O.H.

I I I I I I I I I I I I I I I I I II

o fr*o

^

0C

O

co

Ov

O

! nil


PROPERTY

NTS CODE

Snake Bay Howic LakeLOCATION

HOLE NO. , . F.J7 5. .<? V

LATITUDE 1.+.2 ? v! P: 15.3 .8 ! 1.1^ . . . AZIMUTH . :°. 1 .5 . ........... PURPOSE T0.^ .^^ .z?n. e.

DEPARTURE . . ?5M. South ...... D )P .7 .45° ."....,..,...,. STARTED ?*>.• A^>, ,1 ? 8.^.

ELEVATION .......'........ CORE ?9 ................ COMPLETED .Feb..7th, .1984

SECTION .

REF. GRID

LOGGED BY . f.\

DIP TESTS

FOOTAGE

TEST FROM

/

TO TOTAL

DIP

CORR.

LATITUDE

CUM.

DEPARTURE

CUM,

FROM TO LITHOLOGY

0.0 4.2 CASING

4.2 10.3 CARBONATIZED GABBRO-pyritic zone at 7.8 to 8.1 and 9.4 to 9.6

10.3 12.05 SILICIFIED GABBRO-overprinting carbonate vein-10% aspy from 10.5 to 10.8-brecciated, abundant fuchsite

12.0 13.4 Carbonatized GABBRO-disseminated pyrite-5% carbonate-pyrite stringers

13.4 13.6 Pyritized GABBRO-20% pyrite

13.6 14.8 Carbonatized GABBRO-massive, non-foliated

14.8 15.00 SILICIFIED GABBRO'

15.0 17,3 Carbonatized GABBRO

17.3 17.5 Brecciated Silicified GABBRO-10% pyrite in quartz stringers

17.5 18.8 Weakly Carbonatized GABBRO

18.8 20.0 Massive Fine-grained GABBROi

20.0 22.5 Massive medium to coarse-grained GABBRO

22.5 23.8 Medium-grained GABBRO

23.8 24.3 Fine-grained GABBRO

FROM

24.3

25.2

26.5

27.8

30.5

35.5

43.2

46.5

47.5

53.6

54.0

58.3

TO

25.2

26.5

27.8

30.5

35.5

43.2

46.5

47.5

53.6

54.0

58.3

61.0

61.0

71.0

71.0

LITHOLOGY

Medium-grained GABBRO

Fine-grained GABBRO

Feldspar-phyric Intermediate DYKE

Intensely foliated GABBRO-foliation 50 to c.a.

Fine-grained GABBRO

Anorthositic GABBRO-65% feldspar

Massive fine-grained GABBRO

Pyritized GABBRO-pyrite in thin stringers 75 to c.a.

Massive medium-grained GABBRO

Silicified GABBRO-well banded (75 to c.a.)-alternating layers of

Fine-grained Leucoxene-bearing GABBRO

Unaltered fine-grained GABBRO-6% magnetite


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PROPERTY

NTS CODE

LOCATION

HOLE NO.

LATITUDE

DEPARTURE

ELEVATION

SECTION . .

REF. GRID

K25W 15-baseline

AOS

AZIMUTH . .°.1 ?. ....,'.!,... PURPOSE ?.s ? .W .z ?n.c.

DIP r. 9.0 .* .."........;..... STARTED ^b. .7, § 1984 . .

CORE ?Q ................ COMPLETED . l: c,b : ,8 .' , 1.9 .84

LOGGED BY P. Morcton

DIP TESTS

FOOTAGE

TEST FROM

i

TO TOTAL

DIP,

CORR.

LATITUDE

CUM.

DEPARTURE

CUM.

FROM

0

9,6

11.5

13.1

15.0

16.9

17.9

22.0

23.0

32.0

35.0

TO

9,6

11.5

13.1

15.0

16.9

17.9

22.0

23.0

32.0

35.0

LITHOLOGY

CASING

Weakly altered GABBRO-streaky carbonatization

Carbonatized GABBRO


SILICIFIED GABBRO BRECCIA-10 to 30% quartz stringers-banding 70 to c.a.-1 to 5% pyrite

Carbonatized GABBRO

Leucoxene-bearing GABBRO

Fine-grained Magnetite-bearing GABBRO


Fine-grained GABBRO

E.O.H.

SAMPLE # FROM TO WIDTH ASSAY OZ/TON

003900400041

15.016.217.4

16.216.917.9

1.2 0.7 0.5

Tr.Xr. Tr.

IMPERIAL OIL LIMITED - DIAMOND DRILLJiO.LEJ.OG

PROPERTY

NTS CODE

sn *° LOCATION .

HOLE NO. ™:7. .TO

LATITUDE

DEPARTURE . /.°.S

1+OOW B-baseline

ELEVATION

SECTION .

REF. GRID

AZIMUTH . . ? \ 5. . ........... PURPOSE

DIP 7 A5 ! ..".............. STARTED ?&: ? ..

CORE B.Q. ................ COMPLETED . F.e^. .9 !

LOGGED BY . p.'. h!0,r ? t. 0.n .

DIP TESTS

FOOTAGE

TEST FROM

f

TO TOTAL

DIP

CORR.

LATITUDE

CUM.

DEPARTURE

CUM.

FROM

0.0

11.2

12.0

13.1

13.3

13.4

13.6

15.2

15.7

16.0

TO

11.2

12.0

13.1

13.3

13.4

13.6

15.2

15.7

16.0

16.1

LITHOLOGY

CASING

Carbonatized GABRRO-foliation 70 to c.a.

Carbonatized Leucoxene-bearing GABBRO

Brecciated CARBONATE VEIN

CARBONATIZED GABBRO

Carbonate-stringer zone -25% carbonate veins-3% disseminated pyrite

Carbonatized-Leucoxene-bearing GABBRO

Silicified GABBRO-overprinting carbonate vein -5% pyrite well developed breccia fabric

Carbonatized GABBRO

Pyritized GABBRO-15% disseminated pyrite

16.1 17.1 Carbonatized GABBRO-well developed foliation

17.1 20.5 Unaltered fine-grained GABBRO-5% magnetite

20.5 33.0 ' Massive unaltered Medium to coarse grained GABBRO

33.0 42.5 Massive unaltered medium grained GABBRO

42.5 49.5 Massive Leucoxene-bearing GABBRO

FROM TO LITHOLOGY

49.5 50.4 Brecciated Silicified Carbonate VEIN-well laminated 45 to c,a.-quartz-pyrite-fuchsite

50.4 52.5 Moderately Carbonatized GABBRO-foliation 45 to c.a.

52.5 52.6 LAMPROPHYRE DYKE

52.6 54.0 Foliated Carbonatized GABBRO-foliation 50 to c.a,

54.0 54.3 Intensely Foliated GABBRO-foliation 55 to c.a.

54.3 54.6 Carbonatized GABBRO-weakly foliated

54.6 55.0 Foliated GABBRO30% carbonate stringers parallel to foliation

*55.0 56.5 Massive Carbonatized GABBRO

56.5 60.0 Pyritized-Silicified GABBRO-weakly to well banded 60 to c.a.-containing up to 20% pyrite-well developed breccia texture


61.0 61.7 Silicified-Brecciated Carbonate VEIN-well banded 70 to c.a., less than 3% pyrite

61.7 62.7 'i Leucoxene-bearing GABBRO

62.7 62.8 Silicified GABBRO-57. pyrite

ft-

SAMPLE #

004300440045004600470048

FROM

13,215.147.061.462.566.70

TO

13.615.847.8561.8562.867.10

WIDTH

0.40.70.850.450.30.40

ASSAY oz/ton

Tr.Tr, Tr. Tr. Tr. Tr,


PROPERTY

NTS CODE

LOCATION

HOLE NO.

LATITUDE . 1 T°°.W . 1!- b7T.1 :n.e . . . AZIMUTH ° 5 Te3 °ne

DEPARTURE

ELEVATION

60S

SECTION

REF. GRID

.......... PURPOSE

DIP .:??•..'............. STARTED^:-.9 ?. 1 .9 ? 4...

CORE . B.Q. ............... .COMPLETED . F.e !>: .™\ .1984

LOGGED BY ?•

DIP TESTS

FOOTAGE

TEST FROM

/ /

TO TOTAL

DIP

CORR.

LATITUDE

•

CUM.

DEPARTURE

CUM.

FROM T£ LITHOLOGY

0.0m 12.5m Casing/overburden12.5m 14.8m - Massive unaltered, fine-grained GABBRO14.8 15.60/ Foliated leucoxene-bearing GABBRO

-foliation 45 to c.a.-intensely foliated at 15.4m-tr. tourmaline, and pyrite

15.6 15.87 Carbonatized-foliated GABBRO-2 to 1 7, d isseminated py

15.8 15.9 Silicified Carbonate Vein-20% quartz stringers-2% fuchsite in.wallrock adjacent to vein-5% pyrite-foliation and quartz stringers 7 0 t o c.a.

15.9 16.3 Carbonatized-Pyritized GABBRO-foliation 55 to c.a.

16.3 16.4 ,- Banded Silicified GABBRO-5 to 10% pyrite-banding ( qz-fu-py ) 50 to c.a.

16.40 17.1. Brecciated CARBONATE VEIN-weakly Silicified colliform-textured vein-2 to 25% quartz in irregular stringers-1 to 5% py, tr. tourmaline

17.1 17.7 Silicified GABBRO-abundant fuchsite, tr. py

17.7 18.2 Colliform CARBONATE VEIN-5 to 15% quartz stringers

18.2 18.35 Car'bonatized GABBRO

FROM

18.35

TO

18.45

18

22

22

28

28

37

37

47

.45

.0

.7

.0

.1

.3

.4

.0

22

22

28

28

37

37

47

.0 '

.7

.0

. 1

.3

.4

.0

LITHOLOGY

CARBONATE VEIN-contact 70 to c.a.-10% quartz-tourmaline stringers-minor fuchsite, trace pyrite

Variably Carbonatized Leucoxene-bearing GABBRO

Carbonatized GABBRO-30% carbonate stringers

Leucoxene-bearing Medium-grained GABBRO-weakly foliated

QUARTZ-CARBONATE VEIN-pyritized haloes


QUARTZ_CARBONATE VEIN

Unaltered medium-to-coarse - grained GABBRO

END OF HOLE ———————————————————————————

"152*0

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HldlM

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0'9T0'9T

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9500 5500 *7SOO £500 2500 1500 0500 6VOO

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PROPERTY . . s.n?*e.

NTS CODE .....

LOCATION , H.°l*e. !*k.e .

FJ-9 (68M)HOLE NO.

LATITUDE °.f ? 5W. . B:.b^.Un.e . . . AZIMUTH..-. 01.5 .0 TC

DEPARTURE

ELEVATION

SECTION .

REF. GRID

5

,.,-...... PURPOSE .

DIP 7.V. ............... • STARTED

CORE . B.Q. ............... COMPLETED . Feh .1 } t. lV. 198A

LOGGED BY . E.-F-. M.-. . . .

DIP TESTS

FOOTAGE

TEST FROM

,'

TO TOTAL

DIP

CORR.

LATITUDE

CUM.

DEPARTURE

CUM.

FROM

0

19

22

25

.0

.0

.0

TO

19

22

25

25

.0

.0

.0

.3

25.3

25.7

26.3

26.35

26.60

26.90

27.2

25.7

26.3

26.35

26.60

26.90

27.2

27.65

LITHOLOGY

CASINGi


Weakly Carbonatized Leucoxene-bearing GABBRO

Banded, pyritized, SILICIFIED GABBRO-2 to 10% pyrite-irregular pyritic stringers

CARBONATIZED GABBRO-tr pyrite

Partially silicified, CARBONATIZED GABBRO-10 to 35% quartz stringers-5% pyrite

Colliform-textured CARBONATE VEIN

SILICIFIED GABBRO-5 to 10% fine pyrite-10% carbonate vein fragments

CARBONATE VEIN-contact 80 to c.a.

Carbonatized GABBRO

Colliform-textured CARBONATE VEIN-contact 75 to c.a.-1% pyrite-weakly foliated ( 75 to c.a. )

27.65 30.85 Weakly altered Leucoxene-bearing GABBRO

FROM TO LITHOLOGY>'

30.85 33.7 Fine-grained Unaltered GABBRO- dk-green, mt-ilm - bearing-some weakly foliated zones

33.7 36.0 Unaltered massive Medium-grained GABBRO

36.0 39.8 Unaltered Fine-grained Dk-green GABBRO-cut by thin qz-stringers ( 50 to c.a. )

39.8 40.4 Leucoxene-bearing, foliated, CARBONATIZED GABBRO-bands of chloritic schist near contact at 40.4

40.4 40.8 QUARTZ-CARBONATE VEIN-contact 65 to c.a.

40.8 43.0 Foliated Leucoxene-bearing GABBRO-5% quartz-carbonate stringers, foliation 45 to c.c.

43.0 46.0 Weakly-foliated Leucoxene-bearing GABBRO

46.0 47.5 Massive CARBONATIZED GABBRO-non foliated-disseminated pyrite and tourmaline

47.5 50.1 Weakly Silicified CARBONATE BRECCIA-40 to 75% carbonate fragments in a quartz-chlorite matrix-1 to 3% disseminated pyrite-contact with wallrock 45 to c.a.

50.1 51.3 Fine-grained MAFIC DYKE-massive-contact 45 to c.a.

51.3 51.9 Leucoxene-bearing GABBRO-5% coarse pyrite disseminated near contact with above dyke

51.9 52.6 Stockwork Zone-10 to 30% quartz-carbonate veinlets

FROM

52.6

53.2

54.3

59. 1

65.0

68.0

TO

53.2

54.3

59.1

65.0

68.0

LITHOLOGY /

Leucoxene-bearing GABBRO-massive

Fine to medium grained Unaltered GABBRO

Massive medium-grained Coarse-grained GABBRO

Unaltered Fine-grained GABBRO-thin quartz-carb stringer at 63.5 with disseminated sphalerite


END OF HOLE ————————————————————————————————

WOTO'O

eofoSL'LZ 96*92 W92

96*92 179*92

*9282 TS

92 S2

82 T9 €6

S2 I72

egoo29001900090065008500

AVSSV01


PROPERTY . . .s !lij ke .

NTS CODE .......

LOCATION . H.°»*e. H*k.e

HOLE NO. ."7 1. 0

LATITUDE .°t 7. 5^. b.-.bi? s.cMn.e . . . AZIMUTH . W . .....',..... PURPOSE T.e?t .W. ?<i n.e .

DEPARTURE . . , 7 .3 ? .......... DIP 7 . 9.°? ..'....,........ STARTED .F?b.«. -11.'. } 9. 8.4 .

ELEVATION ............... CORE

SECTION .................

B COMPLETED

LOGGED BY

eb l 1 '

E.P.M.

REF. GRID

DIP TESTS

FOOTAGE

TGST FROM

/

TO TOTAL

.

DIP

conn.LATITUDE

CUM.

OEPARTUnE

CUM.

FROM

0.0

22.

31.

32.

32.

33.

33.

35.

38.

40.

0

5

3

7

2

6

2

0

5

TO

22

31

32

32

33

33

35

38

40

43

.0

.5

.3

.7

.2

.6

.2

.0

.5

.0

LITHOLOGY

CASING/

Massive unaltered Coarse-grained GABBRO


CARBONATIZED GABBRO

Stockworked Section-10 to 25% quartz-carbonate stringers, 65 to 90 to c.a.-2 to 3 % pyrite in carbonatized wallrock

CARBONATIZED GABBRO

Brecciated, silicified CARBONATE VEIN-5 to 35% quartz stringers and matrix infillings-1% pyrite

Leucoxene-bearing, weakly Carbonatized GABBRO-minor quartz-carbonate veining

Unaltered, massive medium-grained GABBRO

Weakly altered Leucoxene-bearing GABBRO-weakly pyritized

43,0 44.0 Unaltered Medium-grained GABBRO

SAMPLE //

006500660067

FROM

32.6533.6236.46

TO

33.4535.5936.97

WIDTH

0.80m 1.97m 0.51m

ASSAY Oz/ton

Tr. Tr. Tr.

IMPERIAL OIL LIMITED .'- DIAMOND DRILL HOLE LOG

PROPERTY

NTS CODE

LOCATION . 1J°.W^ .L?He.

HOLE NO. .'W.-U <?3M)

LATITUDE .°^°.W . 1!-.b tlb: c.1 frl e. . . AZIMUTH . 9 1.5 " ......'..,... PURPOSE Test .Fiji Zone,

DEPARTURE . f*9 S. ........... DIP :. A.5 .° ..'............. STARTED *&'. IWt

ELEVATION ............... CORE ? Q. ................ COMPLETED F°.b; . 1.2 .tl?». .198A

SECTION

REF. GRID

LOGGED BY E.P..M.,

DIP TESTS

FOOTAGE

TCST. FROM TO ' TOTAL

DIP

CORR.

LATITUDE

•

CUM.

DEPARTURE

CUM.

FROM TO LITHOLOGY

0.0 "13.5 CASING ;

13.5 15.0 Massive Leucoxene-bearing GABBRO-weakly foliated (75 to c.a.)-1% pyrite

15.0 16.0 Massive unaltered GABBRO-medium-grained, magnetite

16.0 17.70 Massive weakly carbonatized GABBRO-non veined, sharb contact with vein at 17.70m (75 to c.a.)

17,70 19.1 Variably silicified CARBONATE VEIN-from 17.7 to 18.4 brecciated-silicified section with 5 to 40% quartz stringers

-well banded 60 to c.a.-1 to 3 % pyrite in quartz veins and infillings-minor fuchsite-from 18.4 to 19.1 less intensely brecciated

19.1 19.6 CARBONATIZED GABBRO-weakly carbonatized

19.6 20.4 Pervasively CARBONATIZED GABBRO

20.4 21.5 Massive variably carbonatized GABBRO-abundant (5%) leucoxene

21.5 22.1 Carbonatized-Pyritized Fine-grained Dyke-dk. brown in colour, contact 75 to c.a.

22.1 23.5 Fine-grained Leucoxene-bearing GABBRO

23.5 24.4 Coarse-grained, weakly-altered GABBRO

24.4 25.0 Unaltered Medium-grained GABBRO

25.0 26.0 Weakly altered GABBRO-weak leucoxene alteration of mt/ilm.

FROM TO LITHOLOGYt

26.0 28.2 Unaltered medium-grained, dark-green GABBRO

28.2 29.2 Carbonatized, leucoxene-bearing GABBRO-massive, contact with dyke 55 to c.a.

29.2 29.35 MAFIC DYKE, dark brown

29.35 29.60 Pyritized GABBRO-2 to 5% pyrite

29.6 31.30 MAFIC DYKE

31.30 31.70 Foliated carbonatized GABBRO

31.70 32.00 CHLORITE-CARBONATE VEIN-banded, foliation 45 to c.a.-minor pyrite

32.00 33.40 Fine-grained carbonatized GABBRO

33.40 37.40 Foliated dark green GABBRO-chloritic zones foliation 30 to c.a.

37.40 37.70 Quartz-Carbonate Stockwork Zone-30% quartz-carbonate veins

37.70 38.10 Foliated Zone-chloritic, foliation 35 to 45 to c.a.

38.10 40.5 Carbonatized GABBRO-minor pyrite

40.5........ ..4J.O Quartz Stringer Zone - 30% Quartz Veins

41.0 42.0 Foliated Carbonatized GABBRO-foliation 55 to c.a.

FROM

42.0

42.3

43.2

44.0

49.5

50.3

58.0

TO

42.3

43.2

44.0

49.5

50.3

58.0

LITHOLOGY

Intensely Foliated - Veined GABBRO-foliation 45 to c.a.

/Massive weakly foliated Carbonatized GABBRO

Foliated Carbonatized GABBRO-foliation 45 to c.a.-5% quartz veins parallel to foliation

Massive weakly altered, medium-grained GABBRO-partial leucoxene,development

Unaltered Magnetite-bearing GABBRO

Medium to coarse-grained GABBRO

END OF HOLE ———————————————————————

SAMPLE // FROM TO WIDTH ASSAY Oz/ton

006800690070007100720073007400750076

14.2717.6618.5019.1320.0921.4429.1331.5332.30

14.6718.5019.1320.0920.6622.2029.6431.9732.77

0.40m0.84m;0.63

0.960.57m0.76m0.51m0.44mO.,47m

Tr. Tr. Tr. Tr. Tr. Tr. Tr. Tr. Tr.


PROPERTY

NTS CODE

Snuke BayLOCATION

HOLE NO. **«

LATITUDE °+25W B-bascline

75SDEPARTURE

ELEVATION

AZIMUTH . 93.0 . ..,....'...... PURPOSE ^e.sf .

DIP -. < 5.°. ./......,...... STARTED W ; A2 i ,1984

CORE W .,....,.....,.,, COMPLETED Feb, ,. 1.3, ,

SECTION .

REF. GRID

LOGGED BY

DIP TESTS

FOOTAGE

TEST FROM

/

TO TOTAL

~- ——— '• — ••,

DIP

-::^.

CORR.

LATITUDE

•

CUM.

DEPARTURE

CUM.

FROM TO LITHOLOGY ''I

0 9.8 CASING

9.8 10.0 SILICIFIED CARBONATE VEIN ,

10.0 10.9 Carbonatized Fine-grained GABBRO-minor disseminated pyrite

10.9 11.1 Carbonatized GABBRO-weak foliation 35 to c.a.

11.1 13.8 Weakly Carbonatized, leucoxene-bearing GABBRO-weakly pyritized

13.8 14.0 SILICIFIED GABBRO-wallrock adjacent to vein'contains up to 10% pyrite-contact 85 to c.a.-Visible gold found in late-carbonate stringers crosscutting silicified zone

14.0 14.6 Leucoxene-bearing fine-grained GABBRO-dark green, cut by 3% carbonate veins

14.6 14.7 Pyritized GABBRO-5 to 10% pyrite

14.7 15.30 Carbonatized Mafic Dyke-5% disseminated pyrite

15.30 17.00 Pyritized GABBRO-chloritic

17.00 18.60 Weakly Carbonatized leucoxene-bearing GABBRO

18.60 23.00 Massive Unaltered GABBRO

23.0 24.3 Weakly Foliated and altered GABBRO

24.3 25.15 Well-foliated leucoxene-bearing GABBRO-medium grained, foliation 45 to c.a.

25.15 28.00 Massive Unaltered medium-grained GABBRO

FROM

28.00

TO

28.60

28.60

29.4

35.30

36. 10

36.25

37.6

38.90

44.0

29.40

35.30

36.10

36.25

37.60

38.90

44.0

LITHOLOGY

Brecciated Silicified CARBONATE VEIN ,-20 to 25% quartz stringers and silicified zones-27, a rsenopyrite-banding 75 to c.a;

Leucoxene-bearing weakly altered GABBRO

Unaltered medium grained GABBRO\

Weakly altered leucoxene-bearing GABBRO

Foliated pyritized chloritic GABBRO-foliation 45 to c.a.-2 to 5% disseminated pyrite

Brecciated Silicified GABBRO-10% pyrite-banded 50 to c.a.

Carbonatized GABBRO cut by Carbonate etockwork-20% veins-foliation 50 to 55 to c.a.

Unaltered medium to coarse grained GABBRO

END OF HOLE

SAMPLE #

00770078007900800081008200830084008500860087

FROM TO WIDTH

9.8110.2010.8813.413.714.1214.5927.9828.7036.2036.91

10.2010.8811.2313.714.1214.5915.3228.7028.9936.9137.84

? 0.39m0.68m0.35m0.30m0.42m0.47m0.73m0.72m0.29m0.72m0.93m

ASSAY Oz./ton

Tr.Tr.Tr.Tr.0.060.01Tr.Tr.Tr.Tr.0.01


PROPERTY

NTS CODE

LOCATION! .,H,°yJ;e,V0,k,e .

FJ-13 (71M)HOLE NO.

LATITUDE AZIMUTH .°3.°. ......'...,.. PURPOSE ^st Fiji Zone

DEPARTURE. ? 5S "T .M? 8 .°? . 03 ?°. )

ELEVATION

SECTION

REF. GRID

DIP- 90°

STARTED 3 '

CORE . ,B 9. .............. COMPLETED ?eb. .14, .1984

LOGGED BY . E/.p :"'.'

DIP TESTS

FOOTAGE

TCST FROM TO TOTAL

••

DIP

CORR.

LATITUDE

CUM.

DEPARTURE

CUM.

FROM

0.0

14.25

17.30

17.70

19.0

TO

14.25

17.30

17,70

19.0

20.4

LITHOLOGY

CASING

Leucoxene-bearing ; GABBRO, medium-grained ' -weakly brecciated at 16.1m

Weakly Silicified GABBRO

Massive Leucoxene-bearing GABBRO

Brecciated - pyritized GABBRO-3% pyrite-stockworked zone at 19.4m

20.4 21.5 Foliated Stockworked GABBRO-5 to 10% quartz veins-tr py, tourmaline and chalcopyrite-foliation 30 to 60 to c.a.

21.5 22.2 Leucoxene-bearing Coarse-grained GABBRO

22.2 23.2 Weakly pyritized leucoxene-bearing GABBRO

23.2 23.5 Silicified Brecciated CARBONATE VEIN-banded - 90 to c.a.-2 to 5% pyrite

23.5 24.1 Pyritized Foliated GABBRO-5 to 10% "pyrite-foliation 70 to c.a.

24.1 29.6 Leucoxene-bearing GABBRO-medium-grained, nonfoliated

29.6 30.0 Foliated GABBRO-foliation 30 to 45 to c.a.

30.0 30.7 Weakly altered GABBRO

30.7 34.6 Unaltered medium-grained GABBRO-magnetite-ilmenite bearing

w if;

FROM TO LITHOLOGYi


35.0 35.1 Chloritic Schist Zone-foliation 45 to c.a,

35.1 39.8 Weakly foliated Leucoxene-bearing GABBRO-foliation 45 to 60 to c.a.-2% quartz-tourmaline stringers


40.1 40.2 Carbonatized GABBRO-weakly brccciated

40.2 40.7 Brecciated GABBRO-composed of 70% carbonatized gabbro fragments in a quartz chlorite matrix.

40.7 42.0 Massive fine-grained FELSIC DYKE-both contacts cut by quartz-chlorite stringers

42.0 42.1 Pyritized GABBRO-10% pyrite


45.2 46.6 Carbonatized GABBRO

46.6 46.8 Pyritized GABBRO-5 to 10% pyrite, trace arsenopyrite

46.8 47.44 Leucoxene bearing GABBRO

47.44 47.70 Pyritized - carbonatized GABBRO-2 to 5% arsenopyrite,2 to 3% pyrite

47.70 55.70 Carbonatized Brecciated GABBRO-50 to 60% carbonate stringers-2 to 5% pyrite

55.70 56.20 Arsenopyrite-bearing Brecciated GABBRO

56.20 60.00

-20 to 35% arsenopyrite, 15 to 20% pyrite-contacts 50 to c.a. ;-matrix of quartz and calcite

I

Carbonatized GABBRO Breccia-35% carbonate stringers

60.0

63.7

63.7

65.4

65

65

70

7 1

.4

.50

.00

. nn

65

70

71

.5

.00

.0

Weakly veined GABBRO-weakly carbonatized, 2 to 15% carbonate stringers

Leucoxene-bearing, GABBRO-minor quartz-carb.: veins

Medium-grained GABBRO

Weakly altered Leucoxene-bearing GABBRO-magnetite-ilmenite bearing-non foliated


END OF HOLE

SAMPLE

0088008900900091009200930094009500960097009800990100010101020103010401050106010701080109

FROM TO WIDTHASSAY Oz/ton

14.30 16.10 19.00 20.20 22.90 23.11 24.14 30.69 39.53 39.86 40.62 46.62 47.10 47.34 47.70 48.34 51.06 54.46 55.70 56.18 63.24 65.26

14.77 16.83 20.20 21.60 23.11 24.14 24.34 30.94 39.86 40.32 41.98 47.10 47.34 47.70 47.92 48.89 52.15 55.70 56.18 57.11 63.70 65.63

0.47 0.73 1.20 1.40m 0.21m 1.03 0.20m 0.25 0.33m 0.46m 1 . 36m 0.48m 0.24m 0.36m 0.22m 0.55 1.09m 1.24m 0.48m 0.93m 0.46m 0.37m

Tr. Tr. Tr. Tr. Tr. 0.05 Tr. Tr. Tr. Tr. Tr.

. 0.01 Tr. 0.02 Tr. Tr. Tr. Tr. 0.04 Tr. Tr. Tr.


PROPERTY

NTS CODE

Sn£kc LOCATION . .??W.1?, I?!»

HOLE NO.

LATITUDE .°.H '.1 ?': i 1 T b.u ?° 1.1^ . . AZIMUTH . ?! 5.°. .....'.,,,,, PURPOSE T?f. W. (, a.r ? e.n°Pyrite > v iew

DEPARTURE . \°9* . .......... DIP ". 5?°. ............... STARTED F^.', 1, 5.'

ELEVATION ............... CORE B COMPLETED Fe

SECTION

REF. GRID

LOGGED BY .E :^*.M :

DIP TESTS

FOOTAGETEST FROM

{

TO TOTAL

DIP

CORR.

LATITUDE

•

CUM.

DEPARTURE

CUM,

FROM TO LITHOLOGY

0.0 11.23 CASING/

11.23 13.60 Brecciated Carbonatized GABBRO- composed of 50% carbonatized gabbro fragments, 50% carbonate veins- 2 to 10% pyrite

;'i ,

13.60 14.00 Carbonatized GABBRO-trace pyrite

1A.OO 14.10 Silicified GABBRO

14.10 14.60 Carbonatized GABBRO ';-10% carbonate veins-trace pyrite

14.60 14.70 Leucoxene-bearing GABBRO-trace pyrite, weakly foliated

14.70 15.00 Massive Leucoxene-bearing GABBRO-medium-grained

15.00 15.10 CARBONATE PYRITE VEIN-contact with gabbro 75 to c.a.-10% pyrite

15.10 16.90 Massive Foliated Leucoxene-bearing GABBRO-foliation 55 to c.a.-chloritic slip zones parallel to foliation

16,90 17.00 CARBONATE VEIN-parallel to foliation ( 75 to c.a. )

17.00 19.40 Massive Weakly Foliated GABBRO-5% leucoxene

19.4 20.00 Carbonatized Pyritized GABBRO-2 to 5% pyrite-foliation sporatically developed 45 to 60 to c.a.-5% quartz-carbonate stringers

:.:'('FROM TO LITHOLOGY

20.00 20.35 Stockworked GABBRO-20% quartz carbonate veins

/20.35 20.50 Banded Carbonatized GABBRO

-banding 45 to c.a.-trace pyrite

20.50 20.80 QUARTZ TOURMALINE VEIN-2% pyrite

20.80 22.00 Intensely Carbonatized Banded GABBRO-1 to 3% disseminated pyrite-weak anastomosing ailicified zones-disseminated fuchsite-banding 20 to c.a.

22.0 23.8 Weakly altered GABBRO-partial alteration of magnetite-ilmentite to leucoxene

23.8 23.95 Carbonatized GABBRO-5% quartz-carbonate veining, minor pyrite

23.95 24.40 Carbonatized Pyritized GABBRO- 5% pyrite

24.40 27.40 Unaltered Medium grained GABBRO-10% magnetite ilmenite

27.40 33.40 Weakly foliated Leucoxene-bearing GABBRO-numerous irregular foliated zones 65 to 75 to c.a.-5% quartz carbonate stringers

33.40 33.60 Silicified Pyritized GABBRO-well developed breccia texture-extensively silicified, 10% pyrite

33.60 35.80 Weakly altered Leucoxene-bearing GABBRO

35.80 36.3 Unaltered medium grained GABBRO


FROM

40.8

41.3

42.8

45.5

45.8

47.8

56.4

57.1

60.0

60.5

70.7

71.0

TA n

TO

41.3

42.8

45.5

45.8

47.8

56.4

57.1

60.0

60.5

70.7

71.0

74.0

LITHOLOGY

Stockworked GABBRO -20% quartz-carbonate stringers

Foliated GABBRO - foliation 45 to c.a.

Weakly altered GABBRO

QUARTZ CARBONATE VEIN -contact 45 to c.a.


Coarse to medium-grained Unaltered GABBRO -minor foliated zones cutting at 45 to c.a.

Weakly Carbonatized/Silicified GABBRO -disseminated pyrite (3%) -weak foliation ,65 to 75 to c.a.

Unaltered Medium grained GABBRO

Foliated GABBRO -foliation 75 to c.a.

Massive unaltered fine-grained GABBRO

QUARTZ CARBONATE VEIN

Unaltered GABBRO

SAMPLE //

01100111011201130114,011501160117

FROM

11.2313.0320.1821.1423.9033.2556.3660.01

TO WIDTH

13.0314.5821.1422.1724.5534.2357.1660.60

1.80, 1.55, 0.96; , 1.03

0.650.880.80

1 0.59

ASSAY OZ/ton

Tr. Tr. Tr. Tr. Tr. Tr. Tr. Tr.


PROPERTY

NTS CODE

ay LOCATION . l!°.wf«

HOLE NO. FJ-15 (17M)

LATITUDE2+25W IJ-bnseline 015 Test Fiji Zone

DEPARTURE ° S

AZIMUTH . ... ......'...,.. PURPOSE

DIP :. 4.5 .°. . '.,.....,..... STARTED ^"'l ?! - 1 ?? 4.

ELEVATION ............... COREBQ

SECTION .

REF. GRID

COMPLETED

LOGGED BY

March 9, 1984

DIP TESTS

FOOTAGE

TEST FROM

,

TO

•

TOTAL

DIP ,. .' :

CORR.

^

• n

r

LATITUDE

CUM.

DEPARTURE

CUM.

FROM

0.0

4.2

7.1

TO

4.2

7.1

10.1

10.1

10.2

10.25

10.70

11.6

12.3

17.0

10.2

10.25

10.70

11.6

12.3

17.0

LITHOLOGY

CASING

Leucoxene bearing medium-grained GABBRO

Massive Carbonitized GABBRO-quartz tourmaline vein at 8.6ra

Pyritized - Silicified GABBRO-3 to 5% pyrite :

Arsenopyrite - bearing Zone-1 to 3% arsenopyrite in eilicified gabbro-5% pyrite-irregularily banded

i

Extensively. Brecciated CARBONATE VEIN contact with wallrock 45 to c.a.-50% carbonate fragments in a fine quartz matrix-10% arsenopyrite disseminated in quartz matrix-5% pyrite

i !*. •

Weakly Pyritized Leucoxene-bearing GABBRO

Leucoxene-bearing GABBRO fI;

Massive unaltered, medium-grained GABBRO

END OF HOLE ———————n———————————————————-

Ji

SAMPLE #

0151015201530154

FROM TO WIDTH ASSAY Oz/ton

8.510.110.2510.40

9.610.2510.4011.0

l.lm0.15m0.15m0.60m

Tr.0.010.140.03


PROPERTY ..

NTS CODE . .

Snake Day LOCATION

HOLE NO.

llowie Lake

FJ-16 (29M)

LATITUDE . ?t 5.0!? . B:!?u. s.u i- 1,n .e . . AZIMUTH ° 1

DEPARTURE . . 1/',S . .......... DIP- 45*

PURPOSE ^.w.y?1.0 .STARTED .M.»rch 10..1984

ELEVATION . .

SECTION

REF. GRID

CORE Bq ................ COMPLETED ^la.r .c1} , 1 9

LOGGED BY E.P.M.

DIP TESTS

FOOTAGE

TEST FROM TO TOTAL

DIP '-I;

•

QO.RR.

; h '' .

':'''

(j '

'•'•:

LATITUDE

CUM.

DEPARTURE

• CUM.

i;

,ear

4.5

5.0

14.2

U.55

14.77

14.9

5.0

8.0

8.0

9.1

12.6

13.7

9.1

12.6

13.7

14.2

14.55

14.77

14.9

15.0

Foliated GABliRO-foliation 45 to 60 to c.a.-well banded with alternating chlorite-carbonate bands

Weakly altered Leucoxene-boaring GABBRO-medium to coarse-grained-magnetite-ilmenite present

Leucoxene-bearing, medium-grained GABBRO-leucogabbro - 50% feldspar

Weakly altered GABBRO-magnetite-ilraentite still present

Carbonatized fine-grained GABBRO

Banded Silicified GABBRO-moderately to intensely silicified gabbno>-2 to 10% pyrite-banding 80 to c.a.-fuchsitic streaks '

Colliform-textured CARBONATE VEIN-weakly to intensely silicified and brecciated-2 to 10% pyrite ,

Silicified Pyritized GABBRO-weakly banded 70 to c.a.-banding 70 to c.a. : •-minor fuchsitic streaks

i|!Weakly Pyritized GABBRO jl

f.! Banded QUARTZ-TOURMALINE-CARBONATE VEIN

FROM TO LITHOLOGY

15.0

17.1

17.2

18.8

17.1

17.2

18.8

19.1

19.1

20.0

20.9

20.0

20.9

21.5

21.5 .

24.55

24.55

25.20

25.20 26.1

26.1 29.0

29.0

-2% pyrite-banding 80 to c.a

Weakly-altered, leucoxene-bearing GABBRO

QUARTZ-CARBONATE VEIN

Weakly altered leucoxene-bearing GABBRO

Foliated GABBRO-foliation 45 to c.a.-2% disseminated pyrite

Massive leucoxene-bearing GABBRO-minor foliated zones (45 to c.a.)

Silicified CARBONATE VEIN-30 to 40% quartz stringers

Foliated GABBRO 'J-foliation 45 to c.a. '-fine-grained '

Massive, fine-grained, Leucoxene-bearing GABBRO,f' r

Foliated Stockworked GABBRO,-35% carbonate stringer?- ( 40 to c.a. ) parallel to foliation '•-minor fuchsitic zones >i

Massive medium-grained GABBHO-minor loucoxeno present;';I'M

'{if Massive unaltered, coarse-grained GABBRO

END OF HOLE

I

O O

O

O

O

H^

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i OJ

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3

3

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it

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I

I

I

I

I

I

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I

I

I

I

I

I

I

I

I


PROPERTY

NTS CODE

Snake 3iayLOCATION

HOLE NO. • , F.J:l 7.

Howie Lake

LATITUDE 1°t3. 5.E . 1)-.bl. lb: ii.14no. . . AZIMUTH . - 0. 1 ?. .....'...... PURPOSE Tesf .Appy. J

DEPARTURE . !9°.s . .......... DIP . ".

ELEVATION ............... CORE 1JQ

STARTED

COMPLETED

SECTION .

REF. GRID

. • •' \DIP TESTS

FOOTAGE

TEST FROM

_ ' /

TO . TOTAL

DIP,!

r CORR.

':!

! |,

!i

LATITUDE

CUM.

DEPARTURE

CUM.

LOGGED BY .'. .

'=„, .

1i:

y

F'i1

$

i.

tr

1

1 f

i' "- si •

FROM

0.0

11.0

14.2

15.5

17.0

17.5

18.4

21.0

21.3

11 A

TO

11.0

14.2

15.5

17.0

17.5

18.4

21.0

21.3

22.0

11 £

m

23.65

24.00

24.80

25.10

24.00

24.80

25.10

25.80

LITHOLOGY

CASING

Weakly altered, leucoxene bearing GABBRO

Unaltered medium-grained GABBRO


Extensively Carbonatized GABBRO-10% quartz-tourmaline stringers 90 to c.a.- 2 to 3% pyrite


Chloritized GABBRO-abundant leucoxene

Weakly Carbonatized GABBRO-minor disseminated pyrite

Foliated, Carbonatized, Pyritized GABBRO-foliation 80 to c.a. jv-2 to7% pyrite 1

Colliform-textured CARBONATE VEIN-5 to 15% gabbro fragments-contact with wallrock 80 to c.a.-less than 2% pyrite :

Massive, leucoxene-bearing. GABBRO-5 to 10% pyrite ,, ,,i ,

Massive fine-grained GABBRO-5% carbonate stringers 80 to c.a.. '•!*• •

Colliform-textured CARBONATE VEIN-10% irregular quartz .stringers-trace pyrite '

Weakly Carbonatized GABBRj)-5% carbonate sti

*• .-.i-ilH'

FROM

25.80

26.5

26.70

27.70

28.10

28.20

29.5

TO

26.50

26.70

27.70

28.10

28.20

29.15

29.15 29.50

30.3

30.0 34.70

34.70 35.10

LITHOLOGY

Extensively Carbonatized GABBRO-20% quartz-carbonate stringers (45 to c.a.)

Foliated GABBRO-foliation 85 to c.a.-3 to 5% pyrite

Carbonatized-Stockworked GABBRO-20% carbonate stringers-10% pyrite in stringers

CARBONATE VEIN / REPLACEMENT ZONE-20% gabbro fragments-contact with wallrock 80 to c.a.

Foliated - Pyritized GABBRO foliation 80 to c.a. minor pyrite I '

I;' '

CARBONATE VEIN '<-colliform-texture-up to 50% replacement by quartz-1 to 15% pyrite S ;-well-developed colliform texture

.li-j!'r '

Massive Leucoxene-bearing' GABBRO-chloritized i1,' 1

, Vi Carbonate-Stockwork Zonef

-50% irregular carbonate veinlets-minor silicified zones-up to 10% pyrite iii 'Isilicif led zones

1 •'$ Massive weakly altered ,. l!eucoxene--bearing GABBRO

}!: Carbonate Stockwork Zone I

-60 to 70 % carbonate .veins-20% overprinting quartz stringers-3% pyrite in stringers

39.10

39.50

39.90

40.3

41.1

42.2

43.0

39.50

39.90

40.3

41.1

42.2

43.0

Weakly carbonatized, fine-grained GABBROi -. . i i

Extensively Carbonatized GABBRO-20% carbonate stringers-10% overprinting quartz stringers

Leucoxene-bearing medium-grained GABBRO


Massive leucoxene-bearing GABBRO

Weakly foliated, Leucoxene-bearing GABBRO

HOLE ABANDONED ———————————————————-

a! it

FTr\"

m?';

k

•11•11•11

TO'O TO'O•H•II

ZO'O TO'O•H•H•11

X.VSSV

uiQ9 ' 0

sno08'6€ 08 'SG 01 *SG 0'0€

o^•6^50*8^se1^ 08'9^09'S^ 08>17Z Si'GZ 00'G2

UIQS'O

01

09 '

08 '92 08 §SZ

SO'U

ono69TO 89TO

99TO S9TO

C9TO

T9TO 09TO

IMPERIAL OIL'LIMITED ~ D IAMOND

PROPERTY

NTS CODE

SnuUu

llowie LOCATION ,,..-•

HOLE NO.

LATITUDE

DEPARTURE

ELEVATION

SECTION .

REF. GRID

OI-75K B-b»uul.l«o.•••••" AZIMUTH

_ (JDIP,

CORE

PJ-1B

PURPOSESTARTED

COMPLETED

LOGGED BY

Aiy

2 »

-cut by 10% carbonate stringers

5.6 6.0 Foliated Zone-foliation 45 to c.a.


7.0 7.1 QUARTZ-CARBONATE VEIN-45 to c.a.

7.1 8.0 Leucoxene-bearing GABBRO-10% quartz-carbonate veins

8.0 8.8 Stockwork Zone-15-20% quartz-carbonate veins-majority of veins 45 to c.a.


11.0 11.3 Weakly foliated GABBRO-foliation 45 to c.a'.

11.3 19.5 Massive Leucoxene-bearing,GABBRO-medium-grained '' ,

19.5 20.0 Weakly carbonatized GABBRO-thin irregular silicified zones

20.0 21.2 Silicified CARBONATE VEIN '-well developed colliform texture-up to 70% quartz replacement-disseminated arsenopyrite at 20.3

21.2 21.55 SILICIFIED GABBRO '?,well banded, 45 to c.a. 2% pyrite {,,{

1 'L 11

ft>\

FROM

21.55

21.75

22.0

27.0

28.1

28.6

29.4

TO

21.75

22.0

27.0

28.1

28.6

29.4

30.8

30.8

34.0

LL n

34.0

44.0

LITHOLOGY

FELSIC DYKE

Carbonatized - Pyritized GABBRO-contact with above dyke 80 to c.a.-2 to 5 7. pyrite-banding 40 to 60 to c.a.




Carbonatized Zone-irregular foliation 45 to 60 to c.a.-20% carbonate

Weakly silicified / Carbonatized GABBRO-irregular foliation 45 to c.a.-1,0% pyrite in foliation parallel stringers

Massive unaltered, medium-grained GABBRO

Massive Unaltered, Coarse-grained GABBRO

END OF HOLE ——————-———————————————•

SAMPLE //

017801790180018101820183

FROM

,3 ,6

20.20.21.221.7528.929.9

TO

20.621.221.7522.029.230.8

WIDTH

0.30m 0.60m 0.55m 0.25m 0.30m 0.90m

ASSAY

Tr. Tr. Tr. Tr. Tr. Tr.

Oz/ton

i i'l'!'.•'

IMPERIAL OIL LIMITED 1'- DIAMOND DRILL HOLE LOG

PROPERTY . . S'Y' kc: .Bf y.

NTS CODE .........

LOCATION .

HOLE NO. . S.K."1

LATITUDE

DEPARTURE

ELEVATION

SECTION .

REF. GRID

AZIMUTH065'

PURPOSE Test South Katisha Zonu

.....

DIP

CORE

-.''*?". '............. STARTED ?e.b ; A7

BQ COMPLETED ,F« b;

LOGGED BY

DIP TESTS

FOOTAGE

TtST FROM

/

TO TOTAL

DIP

CORR.

LATITUDE

CUM.

DEPARTURE

CUM.

FROM TO LITHOLOGY

0.0 6.1 CASING

6.1 8.7 Massive BASALT ( Fine-grained GABBRO ? )-aphanitic weakly pyritized

8.7 8.9 Brecciated, weakly carbonatized BASALT-basalt fragments in quartz-carbonate matrix-up to 3% pyrite

8.9 9.8 Silicified BASALT ,.,,-Intensely brecciated and silicified-2 to 7% pyrite-silicified fragments in a quartz-carbonate-chlorite matrix

9.8 11.2 Massive weakly-carbonatized BASALT-5% carbonate stringers

11.2 12.0 Weakly brecciated, Carbonatized, Pyritized BASALT-2% pyrite

12.0 12.4 Weakly-Carbonatized BASALT

12.4 13.4 Silicified Brecciated BASALT-well banded 45 to c.a.-banding defined by elongated silicified basalt fragments-2 to 10% pyrite

13.4 14.00 Foliated Carbonatized GABBRO- moderately to intensely foliated 45 to 60 to c.a.- 1% pyrite

14.00 18.40 Weakly Carbonatized BASALT

18.40 18.70 Pyritized BASALT- 5 to 10% pyrite- banding 45 to c.a.

18.70 20.00 Carbonatized BASALT-pervasively carbonatized, light grey in colour

FROM TO LITHOLOGYi

20.0 20.5 Weakly Carbonatized and Foliated GABBRO-foliation 45 to c.a.

20.5 20.8 Well banded Silicified BASALT- banding 45 to c.a.- 3 to 5% disseminated pyrite- in sharp contact with weakly altered basalt

20.8 23.1 Massive weakly foliated , Carbonatized BASALT- in sharp contact with silicified basalt in hanging-wall and footwall

23.1 24.0 . Silicified BASALT-locally well brecciated- in gradational contact with foliated zone

24.0 27.5 Well foliated Carbonatized BASALT-locally brecciated, foliation 45 to c.a.

27.5 28.5 Schistose - Chloritic Gouge Zone ,, /-steep foliation 20 to 30 to c.aK-50 to 60% chlorite, 25% carbonate-sphalerite-chalcopyrite bearing quartz-carbonate stringers-0.5 to 5% chalcopyrite, 3% pyrite, sphalerite

28.5 29.1 Brecciated BASALT-weakly Carbonatized, minor pyrite

29.1 29.4 Broken Rusty Ground, BASALT Fragments

29.4 29.7 Chlorite-carbonate Schist-schistosity 40 to 70 to c.a.-composed of 50% carbonate, 30% chlorite, 10% pyrite-marks contact between basalt and intermediate dyke

29.7 33.4 QUARTZ DIORITE DYKE-composed of feldspar-chlorite and minor quartz-crosscut by numerous pyritic stringers-becomes foliated at contact with Silicified zone, foliation 70 to c.a.

FROM TO L1THOLOGY

33.4 37.9 Silicified Pyritized BASALT-weak to extensive breccia development-0.5 to 10% pyrite-foliation 45 to 80 to c.a.

37.9 40.5 Weakly altered Leucoxene-bearing DYKE-20% irregular quartz-carbonate stringers

40.5 40.8 Moderately Carbonatized-Foliated BASALT-foliation 50 to 55 to c.a.-foliation paralle quartz-carbonate stringers-3% pyrite ' ; •'

40.8 41.5 Pyritized Silicified BASALT-irregularily banded ( 30 to 90 to c.a )- 2 to 10% pyrite-quartz-fuchsite stringers

41.5 43.8 Massive weakly foliated, Leucoxene-bearing GABBRO-weakly carbonatized-foliation running 40 to 50 to c.a.-5% quartz-carbonate veins

43.8 44.8 Foliated Zone-strong foliation 45 to c.a.-3% pyrite in fine-stringers

44.8 47.1 Variably Carbonatized Fine-grained BASALT-well foliated 80 to c.a.-fine disseminated leucoxene

47.1 49.0 Foliated Leucoxene-bearing GABBRO-foliation 45 to c.a.

49.0 52.0 Non-foliated Leucoxene-bearing GABBRO

52.0 54.5 Unaltered medium-grained GABBRO

54.5 68.0 Unaltered Coarse to medium grained GABBRO?••£''!;

68.0 ——————— END OF HOLE —————r——————————————

SAMPLE //

0118011901200121012201230124012501260127012801290130013101320133013401350136013701380139

FROM

8.528.859.8511.8212.1613.4418.8619.6320.3022.8827.3227.5828.7533.6235.1135.6336.2637.1037.8440.2043.5244.66

TO WIDTH

8.859.85

10.1112.1613.4414.1719.6320.1821.2124.2127.5828.7530.1035.1135.6336.2637.1037.8438,1441.5144.6645.07

0.33m1.00m0.26m0.34m1.28m0.73m0.77m0.55m0.91m1.33ra0.26m1.17m1.35m1.49m0.52m0.63ra0.84m0.74m0.30ra1.31m1.14m0.41m

ASSAY Oz/ton

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!:


PROPERTY . ? I.lu,k Is . B.a y

NTS CODE

LOCATION . , S.°? t: h,

HOLE NO.

LATITUDE . .l t5.5!*. ......... AZIMUTH . .°.6 .5 ! .....'...,.. PURPOSE Test .South Katlsha

DEPARTURE . .'t 1,0?. ......... DIP r.'1.5 .". .............. STARTED ?e,b ; - 1 .9 !

ELEVATION ............... CORE ?S ................ COMPLETED F^'V . 2.°.»

SECTION

REF. GRID

LOGGED BY .

DIP TESTS

FOOTAGE

TEST FIIOM TO • TOTAL

DIP, i

CORR.

,<:'

•I

LATITUDE

CUM.

DEPARTURE

CUM.

.

*•

FROM

0.0

1.9

8.6

9.0

TO

1.9

8.6

9.0

23.8

LITHOLOGY

CASING

Massive Carbonatized Basalt -minor foliated zones -5% carbonate stringers

Extensively Carbonatized BASALT - primary textures destroyed

Massive Carbonatized BASALT-minor disseminated pyrite-thin foliated zones

23.8 24.9 Pyritized Foliated BASALT-weakly foliated, partially slllcified-cut by thin irregular pyritic stringers ( up to 5% pyrite )

24.9 25.4 Carbonatized BASALT-foliation 65 to 60 to c.a.

25.4 29.5 Massive Carbonatized QUARTZ DIORITE-weakly to moderately foliated-minor disseminated pyrite-foliation 25 to 40 to c«a.,'.'.' :

29.5 30.7 Unaltered QUARTZ DIORITE 'p,,'' ">' '

30.7 33.0 Massive Carbonatized QUARTZ DIORITE-composed of 20 to 35% 'chlorite phenocrysts (pseudomorphs ) in a carbonate rich matrix, minor free quartz

33.0 34.1 Carbonatized - Sericitized QUARTZ DIORITE-chlorite pseudomorphs!replaced by fuchsite- cur by milky quartz stringers cutting 90 to c.a.

' ''i 34.1 35.6 Carbonatized QUARTZ DIORITE;.

35.6 39.7 Unaltered QUARTZ DIORITE

39.7 43.5 Carbonatized QUARTZ DIORITE!'

FROM

A3.5

45.3

45.9

48.8

49.2

55.4

60.0

60.7

64.0

68.0

TO

45.3

45.9

48.8

49.2

55.4

60.0

60.7

64.0

68.0

LITHOLOGY

Unaltered Plagioclase porphyritic QUARTZ DIORITE

Foliated Carbonatized QUARTSZ DIORITE-foliation 45 to c.a.-strongly carbonatized

Fine-grained Massive QUARTZ DIORITE

Silicified GABBRO-contact with Quartz Diorite dyke 80 to c.a.-50 to 80% quartz stringers-5% pyrite-disseminated leucoxene

Foliated Leucoxene-bearing GABBRO-crosscut by 30 to 50% carbonate stringers-1 to 5% fine-disseminated pyrite

Foliated weakly silicified GABBRO-intensely foliated foliation 45 to 60 to c.a.-lamination defined by alternating quartz -chlorite-carbonate and leucoxene

Strongly foliated Carbonatized GABBRO-foliation running 30 to 50 to c.a.

Moderately-foliated,weakly"altered GABBRO

Unaltered Medium grained GABBRO

END OF HOLE ——————————^————————————————————

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PROPERTY

NTS CODE

LOCATION!

HOLE NO.

Ktisla

MK-1 (29M)

LATITUDE

DEPARTURE .

ELEVATION ..

Ut'/5W 003'

SECTION

REF. GRID

Test Main Katisha PURPOSE ...........AZIMUTH

DIP :.«.' ............... STARTED **!>: . 2,°> ,.

CORE ?9 ................ COMPLETED .Ff:b.- . 2.°.

LOGGED BY .E '. p.-":

DIP TESTS

HOOTAG6

TEST FROM

/

TO TOTAL

DIP ,

CORR.

'.(

.•' '.

»..iii! '',

i

LATITUDE

CUM.

'" DEPARTURE

CUM.

FROM TO

0.0 4.2

4.2 6.3

6.3 14.0

14.0

16.7

25.0

25.5

•)« n

16.7

25.0

25.5

28.0

LITHOLOGY

CASING

Foliated weakly-altered GABBRO-foliation running 55 to 65 to c.a.-1% pyrite

Massive medium-grained GABBRO-strongly magnetic, 10% pyrite-minor carbonate stringers

Massive BASALTi!» '


Foliated GABBRO-cut by 25% carbonate stringers-minor disseminated pyrite


END OF HOLE ———————————————

SAMPLE it

0144

FROM

24.68

TO

25.30

WIDTH

0.62m

ASSAY Oz/ton

Tr.


PROPERTY .

NTS CODE

Snake Hay LOCATION

HOLE NO.

Main Katisha

LATITUDE

DEPARTURE

ELEVATION

04-63 W

5-1-1 OS

SECTION .

REF. GRID

AZIMUTH .

-45°

003' PURPOSE Ma ' n Kataha0DIP . TV. ............... STARTED

CORE »Q. ................ COMPLETED F*b; . 2.0.'. l.9 ? 4

LOGGED BY

DIP TESTS

FOOTAGE

TEST FROM

fl

TO TOTAL

DIP ,j. i

CORR.

!il i

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J '

LATITUDE

CUM.

DEPARTURE

CUM.

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FROM

0,0

6.9

8,8

9.1

14.0

20.0

TO

6.9

8.8

9.0

14.0

20.0

LITHOLOGY

Massive Fine-grained GABBRO-magnetite-ilinenite bearing-minor carbonate veinlets

Weakly pyritized medium-grained GABBRO-1% pyrite disseminated

Quartz Stockwork Zone-irregular quartz-carbonate veins cutting gabbro-up to 5% pyrite in wallrock adjacent to veins

Massive unaltered Fine-grained GABBRO-abundant magnetite


END OF HOLE ————————————————————————————-

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PROPERTY

NTS CODE

Snfl « LOCATION

HOLE NO.

IH-75W 183* Test Main KatishaLATITUDE . rvr:.......... AZIMUTH .. ,*rr........... PURPOSE

DEPARTURE . W? .......... DIP ' '. 7 A5 ! .............. STARTED .*?»>•. ?°.. 1984

ELEVATION ............... CORE ?q ................ COMPLETED .Feb.. 21,.

SECTION LOGGED BY E.P.M.

REF. GRID

DIP TESTS

FOOTAGE

TEUT FnOM TO TOTAL

DIP ;-CORR.

I

LATITUDE

CUM.

DEPARTURE

CUM.

FROM

0.0

2.2

7.2

8.2

9.2

12.5

13.4

15.5

20.0

TO

2.2

7.2

8.2

9.2

12.5

13.4

15.5

20.0

LITHOLOGY

CASING

Fine to coarse-grained EPICLASTICS-10 to 60% feldspathic and quartz-rich clasts

Dark-Grey Banded SILTSTONE-banding ( bedding ) 85 to c.a.-minor carbonitized sections-minor disseminated pyrite

Dark-green, massive MAFIC VOLCANIC-minor disseminated pyrite-20% quartz-carbonate stringers

Bleached and Brecciated MAFIC VOLCANICS-variably brecciated-weak silicification at 11.4 and 12.0m-minor disseminated pyrite

Extensively Silicified Zone-minor quartz-carbonate veining

Massive unaltered MAFIC VOLCANICS

Massive unaltered GABBRO

END OF HOLE —————————————————————————•

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Date: Feb. 7-84r ——

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A ^ A CUSTOM Fl RE ASSAYINt«•> ^ *•* PAULOKANSKI.Assayer

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.•ample No.

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CUSTOM FIRE ASSAYINGPAULOKANSKI.Assayer : :

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ASSAY CERTIFICATE Date: Feb. 20-84

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Esso"Minerals Can. Ltd. ASSAY CERTIFICATE Date: Feb. 27-84

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ASSAY CERTIFICATE Date:

Phone: Bus. 662-8171 Res. 662-3361

Mar. 13-84

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CUSTOM FIRE ASSAYING Phone: Bus. 662-8171 Res. 662-3361

PAULOKANSKI.Assayer *• Box 253, Cochenour, Ontario POV ILO

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ASSAY CERTIFICATE Mar. 15-84

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Ministry of Natural

Report of Work

Thefof Recorded Holder

tion • separate form for each ri»d (see table below).

t it

900

^..^ »«M>. "-v nv+\.^\yi * *•»>*'/ 'P»OMTt> O"«T '•

Summary of Work Performance and Distribution of CreditsTotal Work Dayi Cr. claimed

for Performance of the following work. (Check one only)

Q Manual Work

PI Shaft Sinking Drifting or other Lateral Work.

[] Compressed Air, other Power driven or mechanical equip.

QPower Stripping

|TfDiamond or other Core drilling

QjjLand Survey

All the work was performed on Mining Clsim(s):

Required Information eg: type of equipment, Names, Addresses, etc. (See Table Below)

Certification Verifying Report of Work

ir

f

I:

f

———————————————————————————————————————————————————— r ——————— * ————————1 hereby certify that 1 have a personal and intimate knowledge of the facts set forth In the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion end the annexed report Is true.

Name and Postal Address of Person Certifying

ttf, AUnfeTo/J V» eW e MI^O*^*-* r.o &e>f *^6Z9 Tce?0A>Ifc , 6HT n^feU Ucl' Date Certified jf>rtW*d-bv(SI

Table of Information /Attachments Required by the Mining Recorder ^-—y^

Type of Work

Manual Work

Shaft Sinking, Drifting or other Lateral Work

Compressed air, other power driven or mechanical equip.

Power Stripping

Diamond or other core drilling

I Land Survey

Specific information per type

Nil

Type of equipment

Type of equipment and amount expended. Note: Proof of actual cost must be submitted within 30 days of recording.

Signed core log showing; footage, diameter of core, number and angles of holes.

Name and address of Ontario land surveyer.

Other information (Common to 2 or more types)

Names and addresses of men who performed manual work /operated equipment, together with dates end hours of employment.

Names and addresses of owner or operator together with detes when drilling/strippingdone.

Nil

natu/e)

*

' Attachments

Work Sketch: these •re required to show the location end extent of work in relation to the nearest claim post.

Work Sketch (as •bove) In duplicate

Nil

69 (81 /3)

fcrMining Claims - Distribution of Credits - MW8 man days/Claim

Meggisi Lake (M2553) Kawashegarauk Lake (M2573) Wapageisi Lake (M2056) Boyer Lake (M2582)

|,N43831*^43830*^43827 •N43833*V43832*V743829*\43828*

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V?1800>?71798»>771785 •>71786»

,Nl89.07 •^71787 •

KVo.6169*\51120 •^95896*NS95895*V62802 •^62805 •N62808.\26961 *\26872 •

\?71790»

V28138 ••^28137 •V28136 •^28135 *V76952 •X32089 •

732090 *^28141%

\28143 * ^28131 • V28132* \28133 • \28134 •

KV62803 *

^726962* V26963 •

176954 V32087 •

^^32084 • Ntf2085* X32086 *

^731139 • >931141 •

0003A 0045A

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AKE BAY

KAT SNA GRID

DDH GEC7ION

ZG-6, ZG-2

AC

CO

UN

T N

2 M

G70

FILE

N

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AP

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1:25

0 0

10 M

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icom

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B

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Dot

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r.

sw NE

EOH 17m

EOH 25m

52F0BNW6J385 21 KAWA5HEGAMUK LAKE

Esso

r: SNAKE BAY FIJI ZONE

DDH SECTION FJI E; FJ2

a*: v / . JACK^SN MAR. '84 52 F/8

SCAL£

I: 2OO O 5m

SNAKE BAY FIJI ZONE

52F08NWB385 21 KAWASHEGAMUK LAKE

-;-:T SNAKE BAYFIJI ZCr.'E

DCrl SECTION FJ5 FJ6

ESSO MINERALS C ANADA

'N O F €350 RESOURCES C ANADA LIMITEDUOOW B-Boseline, 60S

PROSPECT: SNAKE BAY

FIJI ZONE

DDK SECTION FJ-7,FJ-8ACCOUNT N?M670 FILE N2QNT 70 TORONTO

LAKE DATE

MARCH'84NTS

52F/8DRAWN BY:

P. MORETON

DWG. N? 10,781

\ 200 0

To Accompany A Hipart 8j '.

Ool«d:

47.0m E.O.H

0*75W B-Boseline, 75S 0-75W B-8aseline, 60S ESSO MINERALS CANADA

OF ESSO RESOURCES CANADA LIMITED

PROSPECT: SNAKE BAY .

FIJI ZONE

DDH SECTION FJ-9,FJ-IOACCOUNT N2M670 FILE N90NI70TORONTO

NTS52F/8

DATEMARCH'84

DRAWN BY: P MORETON

LAKE N |o,782

44.0m E.O.H

68.0m ED.H52F0BNW0305 21 KAWASHEGAMUK LAKE290

0*50W B-Baseline, 60S

ESSO M INERALS CANADADIV'N OF ESSO RESOURCES CANADA LIMITED

PROSPECT: SNAKE BAY

FIJI ZONE

DDH SECTION FJ-IIACCOUNT N2M670 FILE N9QNT70TORONTO

NTS

52 F/ 8DATEMARCH'84

DRAWN BY:P. MORETON53.0 m E.O.H

DWG. N ? '0,783

To Accompany A Rtporl Bf :52F08NW«3B5 2 ! KAWASHEGAMUK LAKE

sw0»a5W B-Base!ine,75S*Q5S on 030°)

61*

6a

6 In

Scb

ecb

6cb

60=

6a

0095

0098

01 03

0104

010501060107

0108

0109

71.OM E.O.H.

52F88NWC385 21 KAWASHEGAMUK LAKE 310

44.0 M E.O.H.

ESSO MINERALS CANADAOiv'N OF ESSO RESOURCES CANADA LIMITED

PROSPECT: SNAKE BAY

FIJI ZONE

DDH SECTION FJ-I2,FJ-ACCOUNT F!LEDRAWN BY:P. MORETON

DWG, N«, 0 '784

DATEMARCH'84

NTS

52 F/

MAP N«

To Accompany A Rtport By

SW

52F08NW33B5 21 KAWASHEGAMUK LAKE

ESSO M INERALS CANADAOIV'N OF ESSO RESOURCES CANADA UMlTEO

PROSPECT: SNAKE BAY

FIJI ZONE

DDH SECTION FJ-14ACCOUNT N? M 670 FILE N9ONT.7OTORONTO

DRAWN B Y:P. MORETON

DWG.10.785

DATE

MARCH'84NTS

52F/8

MAP

; 2oo o / "-y."o i-C3™»a«i A Rtpott flf:

;^ff4 -

swU05W, 8 *103

84-SK-l

52FC8NW0365 21 KAWASHEGAMUK LAKE 330

o • » • . . ° °. e • • a '. o.o. 0

.OM E.O.K

^W

ESSO MINERALS CANADADIV'N OF ESSO R ESOURCES C ANADA LIMITED

PROSPECT: SNAKE BAY

SOUTH KATISHA

DDH SECTION SK-IACCOUNT N?M 670 _ FILE N^ONI70 TORONTO

DRAWN BY: P. MORETON

DWG. N ? 10,786

DATEMARCH'84

NTS52F/8

MAP N9

1=200

^

M

TO AccoMpany A N«port By

ESSO MINERALS CANADADIV'N OF ESSO'SESOUPifES CANADA LIMITED

PROSPECT: SNAKE BAY

SOUTH KATISHA

DDH SECTION SK-2FILE N*ON~T70TORONTOACCOUNT N2 M670

NTS

52F/8DATE

MARCH'84DRAWN BY:

P. MORETCN

5aF06NWe38S 8, KA*ASHEGAMUK LAKE

68.0M E.O

2»25W B-Bcseline, I6S

FJ-15

52F0BNW0385 21 KAWASHEGAMUK LAKE 350

17.0m E.O.KESSO M INERALS CANADA

Div'fl OF ESSO R€SOu«CES CANADA LIMITED

PROSPECT: SNAKE BAY

FIJI ZONE

DDH SECTION FJ-15ACCOUNT N9M670 FfLE N»ONT.70 TORONTO

DRAWN B Y: PMORETON/REG

DWG. N^ , 0 J88

DATE

MARCH'84NTS

52F/8

MAP N9

To Accompany A Rtpo/t 8 1

2»50W B-Baseline, 14S

FJ-16SW

29M E.O.H.

S2F08NW0385 2 1 KAWASHEGAMUKLAKE

3G0


Dtv'N OF ESSO RESOURCES CANADA LIMITED

PROSPECT: SNAKE BAY

FIJI

DDK SECTION FJ-16ACCOUNT N9 M 670 RLE NSONT70 TORONTO

DRAWN BY: RMORETON/REG

DWG N 9 10,789

DATEMARCH'84

NTS '52F/8

MAP N9

SCALE

1=200 £_ IOM

To Accawpany A Riparl By'

0-35E B Baseline, IOOS

FJ-17SW

44m E.O.H.

52F&8NW0385 21 KAWASHEGAMUK LAKE 370

ESSO MINERALS CANADA DIV'N O F esso RESOURCES CANAO* L IKITEO

PROSPECT: SNAKE BAY——^.

FIJI ZONE^2^_]_

DDH SECTION FJ-17ACCOUNT N« M670 F1LE N*ONT70TORONTODRAWN B Y: PMORETON /REG

DWG. N? 10,790

DATE

MARCH'84NTS

52 F/8

MAP

SCALE

l'200 0 1DM

To Accompany A Rtport

0-75E B-Baseline,63S

FJ-18SW

•l

filx

6°:I 6lx

qi-cb vnn 6U

qi-cb v n

61 *

6cb _6 ill ,cb vn I

6 cb ,py — -

6tx

60

6l7

ecb;6>>l,cb -

So

\ i

60

" 0180 : OIBI

: 0182

_ 0183

-

NE

44.0m E.OH

52F08NWe385 21 KAWASHEGAMUK LAKE380

ESSO MINERALS CANADAOIV'M O F ESSO RESOURCES C ANADA L IMITED

PROSPECT: SNAKE BAY

FIJ ZONE

DDH _SECTION FJ-18ACCOUNT N» M670 F II-E NfiONT70TORONTO

DRAWN BY; RMORETON/REG

DWG. N« 10,791

DATEMARCH'64

NTS

52F/8

MAP N«

1 = 200 0SCA1E

To Accompany A Rtport By

Doliri :

0*63W, 5+IOS

MK-2

20.0m E.O.H.

52F08NW8385 21 KAWASHEGAMUK LAKE 390

ESSO MINERALS CANADAOI1T1- OF E SSO I ESOUKCES CAIAOA LIHIfEB

PROSPECT: S NAKE

MAIN KATISHA

DDH SECTION MK-2

ACCOUKT Hi M670 FILE ** ONT. 70 T OROHTQ

SCALE 1:200 Q ION

AUTHORP. MORETON

NTS 52F/8

DATE MAR. 8 4

DIG.10,931

0.75W,

MK-

20.0m E.O.H.

29.0m E.O.H.

S2F88NIV03a5 21 KAWASHEGAMUK LAKE •400

GEOLOGIC LEGEND

|Q6a 7a 80

aspycb

cb vnchl-sc

epifx

silsits

BasaltUnaltered Gabbro Felsic Dyke, Quartz Diorite Mafic Dyke

Arsenopyrite Carbonalized Carbonate Vein Chlortte Schist Epiclastics Leuccxene Silicified SMlsfone

ESSO MINERALS CANADAOF ESSO RESOURCES CANADA LIMITED

PROSPECT: SNAKE BAY

MAIN KATISHA

DDH SECTION ZG-TJMK-I.SACCOUNT N5M670 FILE N?QNT.70 TORONTO

DRAWN BY: RMORETON/REG

DWG.

DATEMARCH'84

NTS52F/8

MAP N?

^250

To Accompany A Report By :

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