rpt on geol mapping prog of the cooper w grid …...1989; bond gold canada inc. completed ground em...

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a.iasee KAWASHE LAKE 010

. 1380&

REPORT ON THE GEOLOGICAL MAPPING PROGRAM

OF THE

COOPER WEST GRID

MUSKEG WEST PROPERTY

21)990

Submitted by:Bond Gold canada Inc.

December, 1990

S2086NWMM 2 .13886 KAWASHE L AKE

TABLE OF C...——...

l l

Introduction l

" Location and Access l

m Topography and Vegetation 2

Exploration History 3

l Regional Geology 5

Grid Geology 7

l Mineralization 11

m ~ Summary and Recommendations 11

— LIST OF MAPS AND TABLES

Map l - Ontario Location Map

H Map 2 - Golden Patricia Area

Map 3 - Golden Patricia/Muskeg Property Compilation

l Back Pocket - Cooper West Grid Geology Map

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COOPER WEST GRID - GEOLOGY REPORT 1989

INTRODUCTION

lll l

The Cooper West Grid was mapped, in an intermittent fashion,

l between July 18, 1989 and August 7, 1989, at a scale of 1:5000.

The baseline of the grid strikes 0450 , with crosslines turned off

l at 100m intervals. A total of 22.7km of line were mapped, and

m ~ compass traverses were used occasionally to extend lines to ensure

complete mapping coverage. Also, the shorelines of the lake and

l its islands were mapped by boat. All claim posts were located and

tied into the grid.

lm A wide range of rock-types were encountered and include

hornblende gabbro, diorite, quartz diorite, tonalite, granodiorite

l pillowed, massive and sheared mafic metavolcanic flows, minor

felsic to intermediate agglomerate, the occasional feldspar/quartz

l feldspar porphyry dyke, and rarely magnetite-chert iron formation.

Mapping was done by J. Lukosius-Sanders, J. Ackert, P. Chiles

l and J. Gray, under the direct supervision of the author.

l LOCATION AND ACCESS

The Cooper West Grid is centrally located within the Muskeg

l West Claim Group, immediately north of Cooper Lake. It is

contiguous with the Cooper Lake Grid to the southeast, and the Meen

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Lake grid to the west-north west. The Cooper Lake Area is located

B in northwestern Ontario approximately 380km northwest of Thunder

m Bay, (Map 1) 75km west of Pickle Lake and 15km northwest of the

Golden Patricia Mine, which is owned and operated by Bond Gold

l Canada Inc. The Muskeg West Group consists of 520 contiguous

claims that are directly adjacent to the Golden Patricia Mine lease

l (Maps 2 and 3) . The Cooper West Grid covers approximately 26

m ~ claims of the Muskeg West Group.

l Access to the grid is by float or ski-equipped, fixed-wing

aircraft, or helicopter, from Pickle Lake, Sioux Lookout or Red

l Lake. Drill roads, and cut trails, allow snowmobile access to the

m grid during the winter from the Golden Patricia Mine.

l TOPOGRAPHY AND VEGETATION

l Much of the Cooper West Grid is underlain by hummocky,

g kettled, recessional moraine, trending roughly ENE-WSW, that is

* forested with a mature growth of jack pine, and locally trembling

l aspen. Small, swampy lakes and ponds surrounded by black spruce,

cedar and tag alder, now occupy the roughly circular kettle

l depressions within the moraine. The margins of the moraine exhibit

moderate, black spruce and white birch-covered, slopes that drop

quickly into black spruce, cedar and alder swamps. The swamp-edged

l Meen River meanders across the northern limits of the grid. Cooper

Lake forms the southern boundary of the grid and is usually lined

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ONTARIO LOCATION MAP

KENORA

DRYDEN

500 kilometres

, 200 miles ,

MAP l

Z

91'

LANG LAKE

00' October 199O

GOLDEN PATRICIA AREA

GITCHE GROUP

Dobie Zone301,000tgrading 5.50 g Au/1

CENTRAL PATRICIA GOLD MINE

THIERRY MINE CCu,Ni)

GOLDEN PATRICIA * p| k | proven and probable reserves -^ Lake 1,215,871t grading 23.62g

MUSKEG EAST

POWER ^ . , MAGPY ^J

PANTHEON 127VIESTLENS

GOLDEN PATRICIA LEASE

BAMAJI

JEWETT LAKE JV

PICKLE LAKE CAMPpast production 2 million ounces

PICKLE CROW GOLD MINE

r DONA LAKE MINEproven and probable reserves685,500 t grading 8.2

r\WAi KASAGIMINNIS GOLD ZONEJOVAL 997,300 f

JL grading 6.51 gAu/tA 51 0 15

KOVAL

LAKE471,589 t

grading5.18gAu7t

VALLAS LAKE

IRON FALLS

AUGUST NORTH

AUGUST CREEK

20 miles

GREENBUSH fiLAKE JPJEMIMA

PASHKO LAKE

WEBB LAKE PROJECT(Cameco to'earn-in 50*fc)

40 kilometresGold OccurrencePast Producing Gold Mine

COOPER LAKE AREA

GPZ HORIZON 127 WEST LENS

DOBIE AREA

COOPER

DOROTHY6 EAST LENS X

DOBIE NORTH ZONE

DOBIE ZONEDRILL INFERRED ^ 20 WEST LENSMINERAL INVENTORY301,1011grading 5.5 g Au/1


POWERLINE ZONE

ESKER Z 20 EAST LENS DRILL INFERRED MINERAL INVENTORY 48,939 t grading 15.58 g Au/1

LEGEND

IP Axis

HLEM Axis

5 kilometres

MEEN LAKE AREA October 1990

GOLDEN PATRICIA- MUSKEG LAKE PROPERTY

COMPILATION


GOLDEN PATRICIA DRILL INFERRED MINERAL INVENTORY 1,215,871 t grading 23.62 gAu/t

MUSKEG EAST

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*with a thick growth of cedar.

There is less than S-5% outcrop exposed within the grid area.

Most of the rock occurs along or near the shoreline of Cooper Lake,

near the Meen River or Pitu Lake. Outcrop areas

by a mixed forest growth of jack pine, black

birch.

EXPLORATION HISTORY

are characterized

spruce and white

1962; Jorsco Explorations completed geological mapping,

ground magnetometer and EM surveys

of the eastern arm of Meen Lake,

of the Cooper West Grid.

immediately north

about 1.5km west

1973; A joint venture between Umex Corp and Inco Ltd.

contracted a base metal-oriented regional

aeromagnetic survey over the Meen

Area.

Lake/ Cooper Lake

1974 to 1976; Umex Corp. tested numerous airborne conductors,i

detected during the 1973 survey, by diamond

drilling. Some of these holes were drilled south

of the main Cooper Lake Grid and

Meen Lake Grid area.

1977; Cominco Ltd. contracted Questor

others within the

Surveys to fly a

lregional airborne magnetometer survey.

M 1978/1979: Cominco Ltd. completed regional geological

mapping; follow-up ground Max-Min, magnetometer,

l and gravity surveys were completed in selected

areas; several diamond drill holes were completed

l a short distance south of Meen Lake.

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1984: St. Joe Canada Inc. (now Bond Gold Canada Inc.)

l contracted Questor Surveys to fly EM and

magnetometer surveys over a large area that included

l the Meen Lake/Cooper Lake region.

1984 to 1986: Duration Mines Ltd. completed geological

l mapping, ground magnetometer and EM surveys, and

diamond drilling on a 6 claim group coincident with

l the work Jorso Explorations completed in 1962.

1985 to 1986: Van Horne Gold Exploration, Moss Resources, and

l Power Explorations conducted airborne VLF-EM and

magnetometer surveys; ground VLF-EM and

l magnetometer surveys; some geological mapping; and

. diamond drilling on a group of properties adjacent

* to the southern boundary of the Muskeg West Group

l south of the Cooper Lake Grid.

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1987/1988; Umex Corp. completed geological mapping, sampling,

" surface stripping, trenching and considerable

U diamond drilling on their Dorothy Lake Property.

This work outlined a small shear zone-hosted gold

l deposit within a large sill-like diorite body near

the northern boundary of their property.

m ~ 1988; Bond Gold Canada Inc. completed geological mapping,

some outcrop stripping, and a reconnaissance drill

l program on the adjacent Cooper Lake Grid, and ground

Max-Min and magnetometer on the Cooper Lake and

l Cooper West Grids.

1989; Bond Gold Canada Inc. completed ground EM and

l magnetometer surveys on the Meen Lake Grid; and IP-

EM surveys on the Cooper Lake Grid.

lM REGIONAL GEOLOGY

l The Cooper West Grid is located at the Northwestern end of the

Meen-Dempster Greenstone Belt, that occurs within the Archean-age

l Uchi Subprovince of the Superior Structural Province. The belt is

g 95km long, 6 to 10km wide, and forms part of an irregular cluster

* of linear to arcuate volcanic belts situated at the margins of

l late-stage, diapiric, felsic batholiths. It is bounded in the

south by the Carling Granite, the Obaskaka Lake Pluton, and the

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Southern Pluton; on the north by the Dobie Lake Batholith; and

l on the west and northwest by the Hammerton Lake Pluton.

The supracrustal rocks of the Meen Lake area are subdivided

l into the Upper and Lower Meen Lake Group, and the Dorothy Lake

Group. The Lower Meen Lake Group, the oldest cycle, consists of

l massive to pillowed, tholeiitic flows, interbedded with oxide

m ~ facies iron formations, and small volumes of felsic to intermediate

flows and tuffs. The Upper Meen Lake Group is composed of

l predominantly intermediate to felsic pyroclastics and subordinate

flows. The Dorothy Lake Group, which occupies a synclinal portion

l of the greenstone belt, is chiefly composed of metasedimentary

g rocks, such as wackes, arenites, conglomerates, and reworked

pyroclastics, with minor, interbedded, mafic and felsic tuffs, and

l mafic to intermediate flows.

l Metamorphism within the belt is generally upper greenschist

. facies, but locally reaches mid-amphibolite facies near the

" surrounding plutons and batholiths.

lStratigraphic units are thought to be recumbently folded about

l an east-southeasterly to southeasterly synclinal axis\that occurs

near the centre of the belt. The complete sequence has been

overturned, with foliation and bedding dipping steeply, to

l subvertically north, but younging to the south.

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The northern contact of the belt, defined by the Dobie Lake

l Batholith, focuses a major, dextral, shear/deformation zone known

m as the Bearhead Fault Zone (Osmani and Stott, 1988) . It is

suggested that a splay from this zone hosts the gold-bearing vein

I at the Golden Patricia Mine, but the relationships between the two

structures are still unclear. Another possibility may be that

l movement along the Bearhead Fault Zone reactivated an older

m ~ structure within which the gold was concentrated. Another possible

splay, or subparallel reactivated structure may be responsible for

l Umex's Dorothy Lake gold zone near Cooper Lake.

l Gold mineralization occurs in several geologic environments

H within the Meen-Dempster Belt. The most significant is Bond Gold

Canada Inc. 's Golden Patricia Deposit, containing reserves of about

l 370,000 tons at 0.60 oz. Au/ton, where visible gold occurs within

a narrow, laterally very extensive, shear zone-hosted, cherty-

I appearing quartz vein. Two other significant deposits are Bond

Gold Canada Inc.'s Dobie Zone, containing approximately 300,000

" tons at 0.16 oz. Au/ton? and LAC Minerals's Bancroft Lake Deposit.

l These two deposits are associated With sheared, silicified and

sulphidized zones in close association with iron formations. A

J fourth possibly significant gold deposit is the recently

discovered, Umex Corp. Dorothy Lake Property, where gold occurs

" within a sheared, highly altered and mineralized diorite.

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GRID GEOLOGY

m The lithologic units encountered during the 1989 Cooper West

Grid mapping program include: mafic metavolcanic flows;

l intermediate fragmental rocks with felsic fragments; mafic to

intermediate intrusive rocks; some felsic to intermediate feldspar

l porphyry dykes; aplite dykes; and rare chemical sediments.

m ~ Both massive and pillowed mafic metavolcanic flows were

observed, however, the massive varieties appear to dominate. The

l massive flows (Unit la) are fine-grained, dark grey-green to dark

green, weakly to moderately chloritic, variably foliated, locally

l sheared, and locally plagiophyric. Rusty, oxidized foliation

M planes are common, although sulphides are generally not visible.

Occasional narrow, barren, oxidized quartz veinlets occur parallel

l to the foliation. The pillowed mafic flows (Unit Ib) are similar

to the massive flows in colour and texture, but differ due to the

l presence of distinctive, biotitic, locally garnetiferous selvedges.

These selvedges are straight, to gently curvilinear, and l-2cm in

* thickness. Deformation has stretched and elongated the pillows to

l the point where the rocks become banded in appearance. . Top

determinations are impossible. A trace very finely disseminated

J pyrite occurs locally. Localized, discrete, ductile shear zones

have produced chlorite schist (Unit In) in both the massive and

* pillowed flows.

lA well-foliated, pyroclastic metavolcanic rock, possibly a

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lapilli tuff, is exposed in two locations along the eastern

B shoreline of Pitu Lake (Unit 2k). This unit contains up to 701,

m highly elongated, cherty, felsic metavolcanic fragments, up to

1.5cm in thickness and 20cm in length, within a silicified,

l intermediate to mafic matrix. The silicification is pervasive and

lensoidal in nature. Approximately 2% blebby pyrrhotite, pyrite

8 and chalcopyrite is observed within the matrix. Minor quartz

veinlets, oriented parallel to the foliation, occur locally.m

l A few outcrops of chert-magnetite iron formation, (Unit 4c)

hosted by massive to sheared, mafic metavolcanic flows occur near

l Cooper Lake. The BIF units are composed of well-laminated to

H bedded, dark blue-green, magnetite-rich bands, and bluish,

* deformed, recrystallized chert bands. Thickness of the three units

l observed ranges from 10cm to 2m. A trace of disseminated to blebby

pyrite occurs rarely.

l. Hornblende gabbro (Units 6c and d) occurs in three sill-like

bodies that have been emplaced subparallel to regional foliation

l and are probably synvolcanic in nature. This mafic intrusive rock-

type is fine to coarse-grained, massive to well-foliated, dark

l green, and spotted to mottled in appearance. Plagioclase content

varies between 2 0* and 50%. The dominant primary amphiboles

" (probably hornblende) are commonly altered to actinolite, chlorite

l and biotite. The rock is usually strongly magnetic due to the

presence of primary, interstitial magnetite; and contains trace

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to 2%, locally up to ICtt, pyrrhotite and pyrite. Locally, the

l gabbro is highly sheared and silicified, and can contain some

m narrow, boudinaged white quartz veinlets. Shearing is commonly

focused near the contacts of the gabbro bodies. Xenoliths of

l variably deformed and altered mafic metavolcanics occur locally.

l The northern 30-4(tt of the grid is underlain by the marginal

m ~ rocks of the Dobie Lake Batholith comprising granodiorite,

tonalite, quartz diorite, and diorite. The most common variety of

l intermediate intrusive rock within this part of the batholith is

diorite (Unit 8e), which is massive to porphyritic, locally

l sheared along narrow, discrete zones, and composed of approximately

g equal amounts of white plagioclase and green amphibole. Biotite,

quartz and chlorite are minor constituents. The diorite becomes

l porphyritic, near the contact with the metavolcanic rocks,

containing up to 4mm long light-coloured, subhedral to euhedral,

l plagioclase laths. Trace finely disseminated pyrrhotite is present

g throughout. The diorite grades into tonalite (Unit 8d) in the

northeastern part of the grid. The tonalite is massive to

l moderately foliated, locally sheared and silicified, and contains

greater than 2 (tt quartz. Biotite and chlorite are minor

l constituents, and some of the plagioclase has been saussuritized.

Minor amounts of granodiorite (Unit 8b) occur in the northern-most

areas of the grid. It is similar to the tonalite but contains 10-

I 35% potassium-feldspar, and considerable biotite. The progression

of rock-types from diorite to tonalite to granodiorite implies that

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.the diorite only occurs in quantity in the marginal areas of the

l Dobie Lake Batholith. Occasionally large, altered (amphibolitized;

m locally silicified) xenoliths of mafic volcanics occur near the

margins of the batholith, generally within the diorite and

tonalite.

Tonalite, granodiorite, feldspar porphyry and quartz-feldspar

porphyry dykes commonly intrude the mafic metavolcanic rocks.

MINERALIZATION

l l l l l* No significant sulphide mineralization was observed within the

l area of the grid. Localized shears can contain up to 21

disseminated pyrite in association with silicification, and/or

l carbonatization. Disseminated pyrite and pyrrhotite are a common

accessory within the mafic metavolcanics; l-2% disseminated

' pyrrhotite is common within the intermediate intrusive bodies;

l while 1-101 disseminated pyrrhotite, pyrite and locally

chalcopyrite are observed within the hornblende gabbro bodies.

l Twelve grab and chip samples were taken of various sheared

" and/or mineralized and/or altered rock-types, however, no anomalous

j gold values were encountered (Table 1).

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SUMMARY AND RECOMMENDATIONS

m Poor outcrop exposure within the Cooper West Grid area makes

evaluation difficult. The area's location marginal to the Dobie

l Batholith, the presence of discrete shears within all rock types

and some association with sulphide mineralization and alteration

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suggests better potential than indicated by the poor assays

returned. The following recommendations are warranted:

l 1) Re-evaluation of prior ground geophysics in light of the

rock types and structure observed during mapping, with

l attention paid to the weak to moderate max-min, and

M magnetometer anomalies within the margins of the Dobie

* Lake Batholith, or associated with gabbro/metavolcanic

l contacts.

l 2) IP-EM surveys should be run over favourable geology

coincident with the weak to moderate max-min and

" magnetometer anomalies.

l3) The above anomalies should be drilled if IP-EM results

J are good.

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CERTIFICATE OF QUALIFICATION

I, Allan MacTavish of 548 McMaster St., due hereby certify that:

1. I am a graduate of Laurentian University hold an Honours Bachelor of Sciencesciences (1977) .

Thunder Bay, Ontario

, Sudbury, Ontario and degree in geological

2. I am a geologist employed by Bond Gold Canada Inc. and have practised my profession continuously since graduation.

3. I am a fellow, in good standing, of the Geological Association of Canada.

4. I personally supervised the fieldwork described herein.

^9f^(Â^2^Âl MacTavîsh

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l— ,- , . - .-.-•.-•••••K B m im

S2006NW0008 2 .13806 KAWASHE LAKE O2O

GEOLOGICAL MAPPING REPORT

MUSKEG EAST GRID

MUSKEG EAST PROPERTY

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l —— — ™~ ^ l S R O~ MTTfilTFa F&RT PROPRPTV ^^ * J^ t^ V/! W

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lRECEIVED

" DEC 21

l MINING LANDS SECTION

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l A.D. MacTavish

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Thunder Bay, Ontario October, 1990

ll VB TABLE OF ' ssoeewweees 2. i sees KAWASHE LAKE 020C

l Introduction l

M Property, Location and Access l

™ Topography and Vegetation 2

l Exploration History 3

Survey Method . 4

l Regional Geology 5

— ~ Property Geology . 8

™ Summary 11

lLIST OF MAPS AND TABLES

J Map l - Ontario Location Map

Map 2 - Golden Patricia Area

" Map 3 - Golden Patricia/Muskeg Property Compilation

•j Back Pocket - Muskeg East Grid Geology Map

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MUSKEG EAST GRID - GEOLOGY REPORT 1990

INTRODUCTION;

g The Muskeg East Grid was mapped, at a scale of 1:5000, between

* September 27, 1990 and October .11, 1990. A total of 90.735 km of

l grid were mapped and 16 rock samples were taken and sent for assay.

g Little outcrop was observed with most of the grid underlain

— j- by swamp, bog or deep glacial overburden. Rock types observed, in

' order of relative abundance are: hornblende gabbro, massive to

l pillowed mafic metavolcanic flows, diorite to quartz diorite,

tonalite, granodiorite and the occasional quartz porphyry dyke,

l intermediate dyke or mafic dyke.

PROPERTY. LOCATION AND ACCESS:

M The Muskeg East Grid is contained within the Muskeg East

portion of the large Muskeg Claim Group, which totals 754

l contiguous, unpatented mining claims. The Muskeg Group surrounds

the 192 claim Golden Patricia Mine Lease on three sides. The

8 Muskeg East portion of the group consists of 184 contiguous claims,

m with the Muskeg East Grid overlying 69 of those claims. The Grid

is located in Northwestern Ontario approximately 3.4 km southeast

l of the Golden Patricia Mine, 60 km west-southwest of Pickle Lake,

and 365 km northwest of Thunder Bay (Maps l, 2 and 3).

m Access to the grid is by all-weather road from the Golden

Patricia Mine site, or by boat from Hour Lake or Muskegsagagen

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MUSKEG EAST GRID PICKLE LAKE

KENORA

DRYDEN

TORONTO

500 Kilometre*

, 200 miles ,

MAP l

91

LANG LAKE

00'

Dobie Zone301,000tgrading 5.50 gAu/t


THIERRY MINE (CufNi)

GOLDEN PATRICIA * p, .. proven and probable reserves ___ Lake 1,215,8711 grading 23.62g Au/tl n^"1

rf^-*? l DONA LAKE MINE

'JEWETT LAKE JV

GITCHE GROUP

POWERMAGPY ,

PANTHEON 127VESTLENS

MUSKEG EAST


BAMAJI

20 miles

October 199O

GOLDEN PATRICIA AREAPICKLE LAKE CAMPpast production 2 million ounces


proven and probable reserves 685,500 t grading 8.22 g Au/1

KASAGIMINNIS GOLD ZONE 997,800 t grading 6.51 gAu/t 51 0 15

'BANCROFT LAKE.,~,,../ ^ 4 71,5891 KOVAL' ^ grading

5.18 gAu/t

VALLAS LAKE

IRON FALLS

AUGUST NORTH

AUGUST CREEK

GREENBUSH [l,——— LAKE "jpJEMIMA ^ JPASHKO f fP LAKE\ ^ LAKE l ^ ^

ct f ^*~^*^ WEBB LAKE PROJECT ^--- (Cameco to-earn-in 50%)^ l1^- ^ li^

Gold OccurrencePast Producing Gold Mine

MEEN LAKE AREA

LAKE AREA

October 1990


COMPILATIONGPZ HORIZON 127 WEST LENS


COOPER LAKE ZONEDOROTHY LAKE ̂ SP//CE

DOBIE NORTH ZONE

GOLDEN PA TRICIA DRILL INFERRED MINERAL INVENTORY 1,215,871 t grading 23.62 gAu/t

DOBIE ZONE DRILL INFERRED MINERAL INVENTORY 301,101t grading 5.5 g Au/1

MUSKEG EAST

3 m iles

.___5 kilometres

DOBIE AREA

6 EAST LENS

20 WEST LENS


POWERLINE ZONE

LEGEND

IP Axis

HLEM Axis

ESKER Z( 20 EAST LENS DRILL INFERRED MINERAL INVENTORY 48,939 t grading 15.58 g Au/1

lThe Golden Patricia Mine site can be accessed by float, ski

or wheel -equipped aircraft. The grid can be reached by winter road

l from Pickle Lake. Numerous drill roads cross-cut the grid.

™ TOPOGRAPHY AND VEGETATION:

l Most of the Muskeg East Grid is underlain by flat black spruce

swamps and bogs, locally supporting a growth of tamarack, alder or

P cedar. Lakeshores and the edges of ponds commonly consist of

— r floating mats of sphagnum, locally supporting a sparse growth of

" black spruce and tamarack. Rivers and streams connecting lakes,

l ponds and wet bogs are commonly lined, or choked with tag alder,

dwarf willow or cedar. The southcentral part of the grid is

J characterized by a long, narrow, glacially moulded drumlinoid form

— with a relief of 15-20 m above the surrounding areas of black

" spruce swamp. This drumlin is forested with black spruce, white

M birch, and locally, jack pine. Irregular areas of dry, gently

rolling deep overburden, forested with black spruce, trembling

l aspen, white birch and balsam fir, are scattered throughout the

grid area, generally in the northwest and northeast. Outcrop

B comprises about l* of the grid area and occurs as isolated, low

—j relief islands within areas of swamp, as small, narrow exposed

areas along lakes and streams, and as small, localized

l concentrations. Vegetation generally consists of black spruce and

balsam fir in these areas.

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EXPLORATION HISTORY:

1960 to 19631 New Jersey Zinc Exploration completed

l geological mapping, trenching, and 6 diamond

— drill holes, totalling 212.8m, on what is now

' the Golden Patricia Mine Lease; two of the six

drill holes intersected the Golden Patricia

mineralized horizon.

l~- 1971; Union Miniere Explorations (UMEX) completed an

B airborne EM and magnetometer survey over much

l of the Meen - Dempster Greenstone Belt; Umex

also did some reconnaissance geological

l mapping.

l l

1978 and 1979; Cominco Ltd. completed an airborne magnetometer

survey; and as follow-up did ground

magnetometer, EM and gravity surveys over

l selected areas; one of the areas covered by

ground geophysics now lies within the northwest

l corner of the Muskeg East Grid.

1984; St. Joe Canada Inc. (now Bond Gold Canada Inc.)

l contracted a Questor Airborne Input and

Magnetometer Survey, and began ground

l geophysical HLEM and magnetometer surveys,

m within the central area of the Golden Patricia

Mine Lease.

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1985; Noranda Exploration Canada Ltd. completed

geological mapping, geochemical sampling, and

ground magnetometer and EM surveys on two

blocks of claims, one located within what is

now the southwestern corner of the Muskeg East

claims, and the other directly south of the

southeastern portion of the present grid.

1985 to 1988; St. Joe Canada Inc. (now Bond Gold Canada Inc.)

completed considerable ground geophysics, and

diamond drilling that led to the discovery,

underground exploration and eventual

development of the Golden Patricia orebody.

1985 to present;

completed

St. Joe Canada (now Bond Gold Canada)

considerable ground geophysics,

geological mapping and diamond

drilling on the Muskeg Claim group,

including magnetometer, HLEM and

diamond drilling within the Muskeg

East Grid area.

SURVEY METHOD:

A geological map of the area was prepared, at a scale of

1:5000, using a cut grid as geological and topographic control.

The Muskeg East Grid consists of;

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.

9 1 ) 4.30 km of baseline striking 1150 true;

2) 90.735 km of crosslines, striking at 0250 true ;

crosslines are turned off the baseline at 100m intervals

with stations at 25 m intervals along the lines ; and

3) 7.85 km of tie lines , parallel to the baseline, to be

used as additional control.

Lakeshores, streams and rivers, tree types, vegetation

~ boundaries, topographic changes, roads, bridges, outcrops

locations, drill collars, and claim posts were all tied

grid as an integral part of the mapping process.

REGIONAL GEOLOGY:

, sample

into the

The rocks that underlie the Muskeg East property are centrally

located within the Meen-Dempster metavolcanic belt of the Archean

age Uchi subprovince. The belt was originally mapped by Harding

in 1935; then by Sage, Breaks, and Troup in 1972 (Sage et al,

1976) ; and by Stott and Wilson during 1984 and 1985 (Stott and

Wilson, 1986) .

The Meen-Dempster belt forms part of an irregular cluster of

linear to arcuate volcanic belts situated at the margins

stage diapiric felsic batholiths. The belt is 95 km long

of late-

and 6 to

10 km wide. It is bounded on the south by the Carling Granite, the

Obaskaka Lake Pluton and the Southern Pluton and on the

the Dobie Lake Batholith.

ftiorth by\

l

l

l

ll V The geology consists of a northwest-southeast trending

overturned homoclinal sequence representing two mafic to felsic

g volcanic cycles. The cycles are capped by a chemical-sedimentary

H horizon, expressed geophysically as a formational electro-magnetic

' conductor. These cycles, termed the Meen-Jacknife Lake Cycle and

B Dempster Lake Cycle are dominantly mafic volcanics with relatively

narrow intermediate to felsic components.

l~ The Muskeg East property lies entirely within the Meen-

™ Jacknife Cycle volcanics and the Dobie Lake Batholith. The basal

l mafic volcanics are interbedded with a laterally continuous package

of iron formation that can be traced geophysically across the

l property.

The mafic volcanics grade laterally into gabbroic rocks and

other intrusive equivalents, particularly in the Cooper Lake and

Muskeg East areas. Elsewhere they are dominantly pillowed to

l massive flows, commonly intruded by feldspar porphyry dykes and

sills.

m The chemical-sedimentary horizon that caps the Meen-Jacknife

Lake Cycle has been drill-tested by Bond Gold Canada Inc. and by

l Umex. In the Cooper Lake area it consists of a 5 m thick unit of

massive pyrite-magnetite-chert. On the Umex property it consists

l of massive pyrite up to 20 m thick.

The metamorphic grade within the belt is generally of

l l

ll Wgreenschist facies, with amphibolite-grade mineral assemblages

occurring marginal to the Dobie Batholith, and in areas with a

l significant mafic intrusive component.

™ A regional deformation zone is believed to occur at the

l northern margin of the Meen-Dempster volcanic belt. This

structure, which the Ontario Geological Survey (O6S) has called the

g Bearhead Fault Zone, (Osmani and Stott, 1988) is mapped along the

— ~ intrusive contact and within the Dobie Batholith. Another major

" deformation zone is known to enclose the auriferous vein presently

l being mined at the Golden Patricia Mine. The relationship between

these two structures is unclear, although it has been suggested by

g the OGS that the Golden Patricia Zone may be a splay off the

Bearhead Fault Zone, or possibly an older structure reactivated by

* the formation of the Bearhead Fault Zone.

lGold mineralization occurs in several geologic environments

l within the Meen-Dempster Belt. The most significant is Bond Gold

Canada Inc's Golden Patricia Mine presently containing reserves of

B about 446,000 tons at 0.61 oz. Au/ton, where gold occurs within a

M narrow, laterally very extensive, shear zone-hosted quartz vein.

Two other significant deposits are Bond Gold Canada Inc. 's Dobie

l Zone, containing approximately 300,000 tons at 0.16 oz. Au/ton, and

LAC Minerals Ltd. 's Bancroft Lake Deposit containing about 149,000

l tons at 0.19 oz Au/ton. These two deposits are associated with

m sheared, silicified and sulphidized zones in close association with

iron formations. A fourth possibly significant gold deposit has

l l

ll ^recently been discovered by Umex Corp. (now owned by Major General)

near Dorothy Lake, where gold ' occurs within a sheared, highly

altered and mineralized diorite.

™PROPERTY GEOLOGY:

l Lack of outcrop made interpretation of the data, and contact

placement difficult and uncertain. The general picture that

g emerges from beneath the swamp indicates that the northern SO-35%

— - of the grid is underlain by marginal regions of the Dobie

™ Batholith, composed of tonalite, quartz diorite and diorite.

l Directly south of the Dobie Batholith occurs a 300 to 800 m thick

body of hornblende gabbro that contains numerous slices, wedges,

l blocks and xenoliths of highly altered, generally sheared mafic

metavolcanic rocks. The contact between the batholith and the

* gabbro body is undulatory and strikes roughly 115 to 1300 Az. A

•j narrow, 25-50 m thick, sliver of mafic metavolcanic rocks is wedged

between the diorites and the gabbros in the central portion of the

l grid. The margins of the gabbro tend to be fine-grained and

sheared, whereas the internal regions are medium to very coarse-

I grained and massive. The southern contact of the gabbro is

m undulatory and usually strikes between 105 and 1206 Az. Much of the

southern 30 to 40% of the grid is underlain by variably deformed

l and sheared, usually pillowed, mafic metavolcanic flows. There is

a relatively narrow gabbro body present in the southwestern part

l bf the grid. This body appears to be surrounded by mafic

m metavolcanics and may be two cross-cutting dykes rather than one

bifurcating body. It ranges from 75-200 m in thickness, and

l l

ll ^apparently thickens to the west, where it may eventually join up

with the larger gabbro intrusion discussed previously.

l— The most abundant rock-type observed during the mapping

™ program was hornblende gabbro. This rock-type is mottled in

M appearance, light green to dark green in colour, massive to vari-

l l

textured to locally sheared, and composed of 20 to 1 Q\ greyish to

I slightly greenish, subhedral to euhedral plagioclase feldspar, 30

- to 80% altered, dark green, subhedral hornblende, and trace, to

B locally 11, disseminated pyrrhotite, and minor chalcopyrite. The

•j plagioclase is commonly saussuritized and the wide variation in

content causes the rock to range from leucogabbro to melagabbro in

l composition. The hornblende is rarely preserved and has altered

to dark green actinolite and chlorite. Locally the chlorite has

B further altered to biotite. Shearing quickly destroys the mafic

m minerals and forms pressure shadows around the plagioclase

crystals. Intense shearing can give the rock a well-foliated,

l locally banded appearance and dramatically decreases grain-size.

Narrow, highly deformed,, greyish quartz stringers and veinlets, of

l limited extent, occur locally where the gabbros are sheared.

•j Shearing tends to be focused along the margins of the gabbro bodies

or where dykes cross-cut the intrusions.

lThe next most abundant rock-type are the pillowed locally

l massive, mafic metavolcanic flows. These rocks are green to dark

m green, weakly to moderately, locally intensely sheared, chloritic,

weakly to moderately carbonatized, and locally epidote-rich.

ll p'illows tend to be stretched and deformed, and with increased

shearing tend to form a rock with a well-banded appearance.

J Numerous, narrow, highly boudinaged, generally disrupted, white to

grey-coloured quartz veins, containing trace to 2% disseminated

B pyrite, occur where the pillows are most sheared.

lThe last of the major rock-types in abundance are the

l tonalites and diorites. These two rock varieties occur in close

~ proximity to, and are gradational with, each other. They are light

m buff-grey to cream in colour, locally hematite-stained, massive to

m moderately sheared, locally highly sheared, and occasionally

feldspar porphyritic. Both contain 40-50* subhedral locally

l euhedral, cream-coloured plagioclase, 2 0-40* fibrous amphibole,

(actinolite), chlorite, biotite, and variable quantities of quartz.

m The tonalites and diorites are almost identical in appearance,

except that the tonalites contain 20-30* interstitial quartz, and

l the diorites contain trace to 201 quartz. The diorites do not

resemble the hornblende gabbros in any way, and do not appear to

l be genetically related to one another.

Minor quantities of sheared, felsic to intermediate, quartz

l or feldspar porphyry dykes occur in all rock-types. Narrow,

irregular dykes and veinlets of diorite and tonalite cross-cut

l rocks near the contact with the Dobie Batholith. Rarely

M plagiophyric, or hornblende-phyric, mafic dykes are observed.

l

l

l

l

l

l

l

l

l

l

l

ll ^P Mineralized shears and quartz veins are not common,

Mineralized shears and all quartz veins encountered were sampled,

g however, they returned no anomalous gold values. A total of 16

— chip and grab samples were taken.

SUMMARY?lOver 90 km of grid line were mapped with about l* outcrop

l observed. Most of the grid is underlain by swamp, bog or deep

- overburden. Rock-types in order of abundance were hornblende

l gabbro, mafic metavolcanic flows, tonalites and diorites, with

B subordinate felsic to mafic, porphyritic dykes. Locally weakly

mineralized shearing is common within the mafic metavolcanic rocks,

l along or near major lithologic contacts, or focused by narrow

dykes. Quartz veins are observed locally, and tend to be weakly

mineralized and white to grey in colour. Sixteen grab and chip

samples were taken but no anomalous gold values were forthcoming.


CERTIFICATE OP QUALIFICATION

I, Allan MacTavish of 548 McMaster St., Thunder Bay, Ontario due hereby certify that:

1. I am a graduate of Laurentian University, Sudbury, Ontario and hold an Honours Bachelor of Science degree in geological sciences (1977).


3. I am a fellow, in good standing, of the Geological Association of Canada.

4. I personally supervised the fieldwork described herein.

Al Mac


a.iaeee KAWASHE LAKE 030

2.1380^

REPORT ON THE

1990 GEOLOGICAL MAPPING AND PROSPECTING PROGRAM

MEEN LAKE GRID,

MUSKEG WEST PROPERTY

RECEIVED

Submitted by:

Bond Gold Canada ino. December, 1990

l l l l l l l l l l l l l l l l l l

REPORT ON THE1990 GEOLOGICAL MAPPING PROGRAM

MEEN LAKE GRID

INTRODUCTION

A geologic napping and prospecting program was completed on the Meen Lake Grid portion of the Muskeg West Property between August 7 and 14, 1989, and between June 5 and August 4, 1990. A total of 288 line kilometres were mapped at a scale of 1:5000 and 377 rock samples were collected and fire assayed for gold. Mapping was performed on a cut line grid spaced at 100 metre intervals, oriented at 30" azimuth. Mapping was assisted by M. Trudzik, M. Rosatelli, and F. Longpre, under direct supervision of the author.

No values of economic interest were encountered, although 10 samples yielded anomalous values between 0.01 and 0.06 02 Au/ton. In addition, several interesting structures and geological environments were examined that may hold potential for gold and base metal mineralization.

PROPERTY LOCATION AND ACCESS

The Meen Lake Grid is cut over the western 40% of the Muskeg West claim group. It is located in northwestern Ontario about 380 km northwest of Thunder Bay, 80 km west of Pickle Lake, and 15 km northwest of Bond Gold Canada Inc.'s Golden Patricia Mine (Maps l S 2). The Muskeg West Group consists of 520 contiguous claims that are directly adjacent to the Golden Patricia Mine Lease (Maps 2 and 3).

Access to the grid is by float or ski-equipped fixed-wing aircraft, or helicopter, from Pickle Lake, Sioux Lookout or Red Lake. Drill roads and cut trails allow access to all parts of the property in winter by snowmobile from the Golden Patricia Minesite.

TOPOGRAPHY AND VEGETATION

The Meen Lake Grid covers a considerable area and exhibits a wide range of terrain and vegetation types. The eastern and southeastern areas are comprised chiefly of deep, hummocky, locally kettled, glacial moraine forested with a mature growth of jackpine, black spruce and occasionally stands of trembling aspen. The areas south of Meen Lake tend to be low, flat to gently rolling, swampy, and treed by black spruce, tamarack and alder. The northern and central regions are characterized by bedrock-cored ridges and hills, exhibiting up to 20 m relief and the occasional low cliff. The ridges are treed with trembling aspen, black spruce and jackpine, while the intervening swamps are covered with black

l l l l l l l l l ll

*:

l

l

l

l

l

l

l

l


KENORA

DRYDEN

TORONTO

500 kilometres , 200 miles ,

MAP l

\

GITCHE GROUP

LANG LAKE

00' October 199O

GOLDEN PATRICIA AREA,, Dobie Zone

301,000t grading 5.50 g Au/1


MUSKEG EASTPOWER

MAGPY PANTHEON


THIERRY MINE CCu,Ni)

GOLDEN PATRICIA * pick|a proven and probable reserves __ Lake 1,215,871t grading 23.62g Au/tjn 3̂ *'-^^ A

r-f^-f IDONA LAKE MINE\lJEWETT LAKE JV

PICKLE LAKE CAMPpast production 2 mi f lion ounces


proven and probable reserves 685,500 f grading 8.22 gAu/1

t f\\r A i KASAGIMINNIS GOLD ZONE JpVAL 997^00 t

grading 6.51 g Au/1p—l l T yiauiiiy v.

, —J Ir l ~~ij^SBANCROFT LAKE L-J ^^*,../ ^ 477,589 fU l^/^l/AI/ A —l~^s~~

51 0 15,

KOVAL grading 5.18 g Au/1

VALLAS LAKE

IRON FALLS

AUGUST ' NORTH

AUGUST CREEK

GREENBUSH fiLAKE JPJEMIMA

PASHKO l rJ-p LAKE LAKE

WEBB LAKE PROJECT(Cameco to'earn-in 50*fc)

A Gold Occurrence* Past Producing Gold Mine

\MEEN LAKE AREA

COOPER LAKE AREA

October 1990


COMPILATIONGPZ HORIZON 127 WEST LENS GOLDEN PATRICIA LEASE

COOPER LAKE-ZONEDOROTHY LAKE -*C SPIKE ZONE

DOBIE NORTH ZONE

GOLDEN PATRICIA DRILL INFERRED MINERAL INVENTORY 1,215,871 t grading 23.62 gAu/t

DOBIE ZONE DRILL INFERRED MINERAL INVENTORY 307,707* grading 5.5 gAu/t

MUSKEG EAST

3 m iles

5 kilometres

DOBIE AREA

6 EAST LENS

20 WEST LENS


POWERLINE ZONE

LEGEND

IP Axis

HLEM Axis

ESKEf? ZONE 20 EAST LENS DRILL INFERRED MINERAL INVENTORY 48,939 t grading 15.58 gAu/t

l l l l l l l l l l l l l l ll l l l

-2-

spruce, tamarack and alder. A very large black spruce swamp separates the central and far western bedrock areas.

Locally outcrop abundance can approach 401, however, the overall average for the grid is about S-5%. Lakes, large and small, constitute 15-2(^ of the area.

EXPLORATION HISTORY

1962;

1973:

1975/1976:

1977;

1978-1979;

1984-1986;

1985-1986;

Jorsco Explorations completed geological mapping, ground magnetometer and EM surveys a short distance north of the eastern arm of Meen Lake.

A joint venture between Umex Corp. and Inco. Ltd. contracted a regional base metal-oriented aeromagnetic survey over the Meen Lake area.

Umex Corp. diamond drill-tested numerous airborne conductors detected during the 1973 survey. Some of the holes were drilled within the area of the present Meen Lake Grid.

Cominco Ltd. contracted Questor Surveys to fly a regional airborne magnetometer survey.

Cominco Ltd. completed regional geological mapping; and in selected areas completed follow-up ground Max-Min, magnetometer, and gravity surveys; several holes were drilled a short distance south of Meen Lake.

St. Joe Canada Inc. (now Bond Gold Canada Inc.) contracted an airborne EM and magnetometer survey over a very large area that included the Meen Lake region.

Duration Mines Ltd. completed geological mapping, ground magnetometer and EM surveys, and diamond drilling on a 6 claim group located immediately north of the eastern arm of Meen Lake.

Van Horne Gold Exploration, Moss Resources, and Power Explorations conducted airborne VLF-EM and magnetometer surveys; ground VLF-EM and magnetometer surveys; some geological mapping; and diamond drilling on a group of properties adjacent to the southern boundary of the Meen Lake area.


-3-

1989; Bond Gold Canada Inc. completed ground EM and magnetometer surveys over the Meen Lake grid; these surveys provided the targets for a 17-hole drill program completed during the summer of 1989.

REGIONAL GEOLOGY

The Meen Lake Grid is located at the northwestern end of the Meen-Dempster Greenstone Belt, that occurs within the Archean-age Uchi Subprovince of the Superior Structural Province. The belt is 95 km long, 6 to 10 km wide, and forms part of an irregular cluster of linear to arcuate volcanic belts situated at the margins of late-stage, diapiric, felsic batholiths. It is bounded on the south by the Carling Granite, the Obaskaka Lake Pluton, and the Southern Pluton; on the north by the Dobie Lake Batholith; and on the west and northwest by the Hammerton Lake Pluton.

The supracrustal rocks of the Meen Lake area are subdivided into the Upper and Lower Meen Lake Group, and the Dorothy Lake Group. The Lower Meen Lake Group, the oldest cycle, consists of massive to pillowed, tholeiitic flows, interbedded with oxide facies iron formations, and small volumes of felsic to intermediate flows and tuffs. The Upper Meen Lake Group is composed of predominantly intermediate to felsic pyroclastics and subordinate flows. The Dorothy Lake Group, which occupies a synclinal portion of the greenstone belt, is chiefly composed of metasedimentaxy rocks, such as wackes, arenites, conglomerates, and reworked pyroclastics, with minor, interbedded, mafic and felsic tuffs, and mafic to intermediate flows.

Metamorphism within the belt is generally upper greenschist facies, but locally reaches mid-amphibolite facies near the surrounding plutons and batholiths.

Stratigraphic units are thought to be recumbently folded about an east-southeasterly to southeasterly synclinal axis that occurs near the centre of the belt. The complete sequence has been overturned, with foliation and bedding dipping steeply, to subvertically north, but younging to the south.

The northern contact of the belt, defined by the Dobie Lake Batholith, focuses a major, dextral, shear/deformation zone known as the Bearhead Fault Zone (Osmani and Stott, 1988) . It is suggested that a splay from this zone hosts the gold-bearing vein at the Golden Patricia Mine, but the relationships between the two structures are still unclear. Another possibility may be that movement along the Bearhead Fault Zone reactivated an older structure within which the gold was concentrated. Another possible splay, or subparallel reactivated structure may be responsible for Umex's Dorothy Lake gold zone.


-4-

Go,ld Mineralization occurs in several geologic environments within the Meen-Dempster Belt. The most significant is Bond Gold Canada Inc. 's Golden Patricia Deposit, cpntaining reserves of about 446,000 tons at 0.61 oz Au/ton, where visible gold occurs within a narrow, laterally very extensive, shear zone hosted, cherty- appearing quartz vein. Two other significant deposits are Bond Gold Canada Inc.'s Dobie Zone, containing approximately 300,000 tons at 0.16 oz Au/ton; and LAC Minerals' Bancroft Lake Deposit containing about 149,000 tons at 0.19 oz Au/ton. These two deposits are associated with sheared, silicified and sulphidized zones in close association with iron formations. A fourth, possibly significant, gold deposit was recently discovered by Umex Corp. on their Dorothy Lake Property, where gold occurs within a sheared, highly altered and mineralized diorite.

PROPERTY GEOLOGY

The Meen Lake Grid covers two cycles of volcanic rocks: the dominantly mafic Lower Meen Lake Group and the dominantly intermediate to felsic Upper Meen Lake Group. - The grid also covers the boundaries of two peripheral plutonic complexes, the Dobie Lake Batholith to the north and the Hammerton Lake Pluton to the southwest). The rock types encountered on the property are described below:

i) Mafic Metavolcanic Rocks:

The mafic metavolcanic rocks of the Lower Meen Lake Group are well exposed and form the bulk of the outcrop on the Meen Lake property. These rocks extend across the central part of the property north of Meen Lake in a fairly continuous band up to 1.5 km wide. Both massive and pillowed flows are observed. The massive volcanics are generally fine-grained and dark greyish-green to dark green in colour. The typical mineral assemblage is amphibole-plagioclase-chlorite, locally with accessory biotite and calcite. The rocks are variably foliated and locally sheared. Rusty, oxidized foliation planes are common, although sulphides generally occur in only trace amounts. Coarse-grained varieties occur locally and represent the central sections of thick flows.

Pillowed mafic flows are similar in colour and composition to the massive flows but differ due to the presence of distinct dark grey to green pillow selvedges. These selvedges are typically straight to gently curvilinear in form and 1-3 cm in width. Deformation has structured the pillows into ovoid shapes with length to width ratios from 2:1 to 6:1. Saussuritization of pillow selvedges and pillow cores is very common (light green to yellow- green in colour) and likely reflects deuteric alteration. Interpillow material is occasionally observed, typically composed of very rusty, recrystallized, saccharoidal chert which may be magnetiferous. The pillowed flows are typically too deformed to


-5-

ailow for reliable top determinations. There are, however, rare occurrences of weakly deformed pillows and amygdaloidal pillows which indicate that tops are dominantly south facing.

Pillow breccias occur sporadically throughout the mafic pile. These are typically clast supported, monolithic breccias composed of subangular fragments (generally ^20 cm in thickness) that exhibit portions of pillow selvedges. The matrix is a fine grained, strongly saussuritized material. There are also minor occurrences of mafic volcanic breccias with no obvious selvedge fragments that may represent flow top breccias.

The mafic volcanics are variably foliated and locally strongly sheared, creating chloritic schists. Shearing of pillowed flows and pillow breccias likely gives rise to the banded mafic flows that occur near the margins of the supracrustal sequence and within rafted segments of volcanics within the Dobie Lake Batholith. The banded flows are composed of narrow, discontinuous, alternating bands of amphibole-rich and epidote-rich material, best observed on weathered surfaces.

ii) Intermediate to Felsic Metavolcanic Rocks:

Intermediate and minor felsic metavolcanics belonging to the Upper Meen Lake Group are interpreted to underlie most of the south property area. These rocks are poorly exposed due to the presence of thick glacial deposits which cover much of the property south of Meen Lake. Lapilli and ash-tuffs and pyroclastic breccias of intermediate composition are the most commonly exposed rocks in this area. The ash-tuffs are typically light greyish-green to grey in colour, fine to medium-grained, and well foliated. The typical mineral assemblage is plagioclase-chlorite-quartz-sericite + biotite. Lapilli tuffs are commonly heterolithic and usually display a strongly, pitted, greyish to buff-coloured weathered surface.

Coarse pyroclastic rocks are exposed immediately south of the Meen Lake narrows. Pyroclastic breccias in this area typically display a light green chloritic matrix with subrounded to angular fragments that are usually more felsic than the matrix. Bombs and fragments up to l m in diameter were observed.

Exposures of felsic metavolcanic rocks are limited. The principle occurrence is a 100-300 m thick, east-west trending band of sporadic outcrop immediately north of Tie Line 20+OOS between lines 265+00 w and 274+00 W. Here, massive to weakly foliated flows and lapilli tuffs are intercalated with intermediate volcanics and gabbroic intrusives. The flows display a distinctive buff coloured, polished, weathered surface and a blocky fracture pattern. They are typically composed of a fine-grained assemblage of quartz-plagioclase-sericite and may contain quartz phenocrysts.


-6-

The presence of rhyolitic flows, coarse pyroclastic rocks, and subvolcanic intrusives (quartz ± feldspar porphyries) which occur stratigraphically above and below the intermediate-felsic package, are all evidence for a volcanic centre within or proximal to the south property area.

iii) Chemical and Clastic Metasedimentary Rocks:

Chemical sediments occur as discontinuous bands of varying thicknesses, interlayered with mafic metavolcanics of the Lower Meen Lake Group in the central property area. Chert-magnetite iron formation occurs in bands usually less than a metre wide, although locally they can attain widths of up to six metres (eg. Line 270+00 W, 5+30 N). The iron formation units are usually interbedded with chlorite-biotite schists or dark grey mudstones. They often contain minor sulphide mineralization (locally up to 5%, mostly pyrite) and are rarely garnetiferous. Lean iron formation and chert occurs rarely in thin bands and also as an interpillow material.

Clastic sedimentary rocks are of very limited occurrence on the property. Outside of the fine-grained sediments associated with iron formation, the only other clastic sediments observed were narrow, discontinuous bands of interflow wackes and siltstones.

iv) Subvolcanic Intrusive Rocks:

Gabbroic sills of varying size are common on the Meen Lake property. The most extensive exposures occur within the Lower Meen Lake Group, extending westward from "Pitu" Lake to an area immediately north of the Meen Lake narrows. Smaller sills intrude the Upper Meen Lake Group and are likely westward extensions of a large gabbro body situated along the south shore of Cooper Lake. The gabbros are composed of varying amounts of hornblende and plagioclase, occasionally with accessory magnetite and chlorite. They are typically massive but are locally sheared and strongly chloritized. A strongly porphyritic gabbro with plagioclase phenocrysts up to several centimetres wide was also observed in one outcrop.

Quartz-feldspar porphyries occur sporadically on the property, although locally dykes can be traced for distances of up to 200 metres. The majority of the porphyry outcrops occur within the Lower Meen Lake Group, in close proximity to the contact with the Upper Meen Lake Group. The porphyries typically display a medium to dark grey, fine-grained siliceous matrix surrounding varying amounts of yellowish to white feldspar and pale blue to colourless quartz phenocrysts, best recognized on weathered surfaces.

Minor, fine-grained, mafic to intermediate dykes and possible lamprophyre dykes also occur on the property, mainly within the Lower Meen Lake Group metavolcanics.


-7-

v) Felsic to Intermediate Intrusive Rocks:

The northern portions of the Meen Lake Grid are underlain by the marginally complex, felsic to intermediate intrusive rocks of the pretectonic to syntectonic Dobie Lake Batholith. This is essentially a granodioritic to tonalitic body, with diorite common along the margins of the batholith. Contacts between the different phases are gradational, often making classification of the granitoid rocks in the north property area difficult.

The late to post-tectonic Hammerton Lake Pluton intrudes the southwest portion of the grid. This consists predominantly of massive, potassium feldspar and/or guartz-porphyritic granodiorite. In the Meen Lake area the rock contains abundant biotite. Various lobes of this intrusion pinch and eventually truncate within the mafic metavolcanic rocks of the Lower Meen Lake Group northwest of Meen Lake.

STRUCTURE

The overall trend of the supracrustal rocks on the property varies from west-northwest to east-west, or subparallel to the granite-greenstone contacts. The metavolcanic rocks are folded around a major syncline that is coaxial with the Upper Meen Lake Group. The synclinal axis is slightly curved, strikes between 090" and 1350 , plunges 2 5-50" east and southeast, and is generally parallel to mineral stretching and intersection lineations. The rocks north of Meen Lake dip subvertically to steeply south, while south of the lake dips are moderate to steep to the north. The northern contact of the metavolcanic rocks with the Dobie Batholith is marked by the trace of the Bearhead Fault Zone, which is usually located within the granitoid rocks but occasionally curves into the metavolcanic rocks. The numerous shear zones observed within the metavolcanics are possibly splays, subparallel systems, or reactivated older structures associated with the Bearhead Fault Zone. Many of the subsidiary shears are located along lithologic contacts exhibiting some sort of competency contrast.

DISCUSSION OF RESULTS

A total of 288 line km of geological mapping and prospecting was completed on the Meen Lake property at a scale of 1:5000. Mapping has outlined two cycles of east-west trending metavolcanic rocks and the boundaries of two surrounding granitic plutons.

The main focus of sampling included quartz -f- carbonate veins, sheared and altered zones, iron formation, and gossanous, iron- stained horizons. A total of 377 grab and chip samples were obtained and fire assayed for gold by Paul's Custom Fire Assay Ltd. in Red Lake, Ontario. No gold values of economic significance were


-8-

encountered, although ten samples returned weakly anomolous values (X).01 oz Au/ton) (The ten anomolous samples are described in Table I). The highest value obtained was a 0.06 oz Au/ton from a weakly sheared quartz-feldspar porphyry- dyke crosscutting mafic flows. The dyke contains thin quartz veinlets and trace to i.% disseminated pyrite. Resampling of this feature yielded a value of 0.03 oz Au/ton. However, sampling of other rocks along strike and in the immediate vicinity yielded no economic values. The remaining anomolous values are associated with disseminated sulphides (mainly pyrite and pyrrhotite) in various lithologies and also with small, rusty quartz veins which are very common on the property, particularly north of Meen Lake.

The Bearhead Fault Zone was recognized in the north property area, manifested by a series of strongly sheared to mylonitized granitoid rocks in close proximity to the granite/greenstone contact. Alteration and sulphide mineralization in these rocks is minimal. In the metavolcanics of the Meen Lake Group several small shear zones, possibly associated with the Bearhead Fault Zone, were mapped and sampled. These shears are often carbonatized and/or silicified and occasionally host large quartz ± carbonate ± tourmaline veins. Sulphide mineralization, however, is generally weak and sampling of these zones did not return significant gold values.

The seventeen hple 1989 drill program tested several of the stronger geophysical anomolies on the property, but did not intersect any significant zones of gold mineralization. The majority of the EM conductors that were drilled proved to be associated with bands of variably sulphidized, sheared and deformed oxide facies iron formation, interbedded with pillowed mafic flows. Minor values (up to 0.02 oz Au/ton) were returned from the iron formation horizons, however, there is no readily apparent correlation between sulphide content, the presence of quartz * carbonate veinlets, and the occasional anomolous assay result. Subsequent sampling of numerous iron formation outcrops in the present program returned two anomolous gold values from widely separate locations (see Table I). None of the surface values obtained in the mapping program appear to correspond to anomolous zones intersected in the drill program.

1 -9-

"

1

1

1

1

I .-

1

1

1

1

1

1

1

1

1

1

1

1

••w

SAMPLENUMBER

JLS-26

JLS-27

JLS-28

PJC-01

JAG-03

JAG-04

16919

16927

2688

14378

16852

TABLE 1MEEN

: ANOMOLOUS ROCKLAKE GRID, MUSKEG

SAMPLES (5*0.01 ox /ton Au)WEST PROPERTY

ASSAYLOCATION

325+OOW,10+80S

325+10W,1H-25S

325+05W, 14+90S

328+90W,4+20S

327+25W,2+40S

325+OOW,0+10S

258+OOW,O+IOW

252+96W, 10+OOS

243+OOW,4+90N

267+92W0+78S

260+05W

TYPE

Grab

Grab

Grab

Grab

Grab

Grab

Grab

20 cm chip

Grab

Grab

Grab

DESCRIPTION (oz/ton Au)

Quartz vein in mafic flow,trace pyrite

Disseminated pyrite in maficflows

Sheared iron formation, trace pyrite and pyrrhotite

Quartz vein in mafic flow(xenolith)

Pillowed mafic flow, a-2%disseminated pyrrhotite,trace pyrite

Pillowed mafic flow, xenolithin granodiorite, trace py

Iron formation, tracedisseminated py

Quartz-feldspar porphyry dyke - crosscutting granodiorite

Quartz-feldspar porphyry dykein pillowed mafic flows, minorquartz veinlets, trace - \\disseminated py

Quartz pods and lenses in maficflows, trace - 1\ pyrite

Quartz veins and stringers insheared diorite, trace pyrite

0.01

0.02

0.02

0.01

0.01

0.02

0.033

0.03

0.060.03

0.01

0.01

l l ll l l l l l l l l l l l l l l l

-10-

SUMMARY AND RECOMMENDATIONS

The geologic mapping and prospecting program carried out on the Meen Lake Grid portion of the Muskeg West property did not uncover any significant zones of gold mineralization. A variety of features of potential economic interest were sampled, including quartz veins, shear zones, iron formations, and disseminated sulphide zones. Of the 377 samples collected, only 10 returned anomolous values between 0.01 and 0.06 oz Au/ton.

The highest value of 0.06 oz Au/ton was obtained from a weakly sheared and mineralized quartz-feldspar porphyry dyke crosscutting mafic flows. It is recommened that this zone be stripped and sampled thoroughly. In addition, more prospecting should be performed over the entire peninsula on the west side of "Pitu" Lake where the showing is situated. This area is covered by thick vegetation and it is quite likely that a significant amount of outcrop can be uncovered between grid lines.

In the south property area, the presence of coarse pyroclastic rocks, rhyolitic flows and subvolcanic quartz-feldspar porphyries suggest the existence of a volcanic centre within or proximal to this area. An effort should be made to assess the potential for gold and base metal mineralization within these rocks. This would include additional prospecting and stripping south of Meen Lake and limited, widely spaced I.P. profiling over selected areas within the Upper Meen Lake Group. I.P.. profiling should also be performed over the contact between the Upper and Lower Meen Lake Groups, which is largely covered by water. The contact between these two volcanic cycles is a potential site for gold and base metal mineralization. Follow-up diamond drilling to test any new geophysical/geological targets in this area is also recommended.

ET/mj

F:SARAH\VP\R-MUSKES.TIM

1111111111111111111

t

CERTIFICATE OF QUALIFICATION

I, Allan MacTavish of 548 McMaster St. due hereby certify that:

, Thunder Bay, Ontario

1. I am a graduate of Laurentian University, sudbury, Ontario and hold an Honours Bachelor of Science degree in geologicalsciences (1977) .


3. I am a fellow, in good standing, of the of Canada.

4. I personally supervised the fieldwork

/(^fl/lifevw^C——— ̂Al Mactavish j\C^O^La-'

Geological Association

described herein.

'

. j

Acton ot Work

(Geophysical, Geological a.iaaee KAWASHE LAKETypeotSurv.

CrSOÔd/ Ctf*-Mining t*Kiwvni ,,v^.^..^.. . —

ReoorJedHoldefts) prospector s Licence NO.

/W/A PryTS CVW/9&/? }*)C. T-c&OBAddress

Survey Company/^to/oA GCXA cft

Telephone No.

^;A^T STE. TD^rw^Tn M^c^r^ 3&--/OZIrv/yÂ^ yA/C

'Name and Address of AuttSr^fGeo-Technicai Report) . oat* of Burvey (troi

jfedits Requested per Each Claim in Columns at right Mining Claims Traversed•pedal Provision*

For first survey: —

Enter 40 days. (This includes Vne cutting)

For each additional survey: using the same grid:

Enter 20 days (tor each)

Man Days

Complete reverse side and enter totals) here

Airborne Credit*

Note: Special provisions credits do not apply to Airborne Surveys.

Geophysical

- Electromagnetic

~ Magnetometer

-Other

Geological

Geochemical

Geophysical

- Electromagnetic

- Magnetometer

• Other

Geological

Geochemical

Electromagnetic

Magnetometer

Other

Total miles flown over claim(s).o** RnS?tx5!Ajry 23/^0 -ffflm

Certification Verifying Report of Wl

Dssr

40Days per

Claim

0^

Days per Claim

ttor or Aoeni (Stonahtft)

•dL

Mining ClaimPrefix Number

PL&flSg

R

——— MINU

T /o ô0*y 1 Mo 1 Vi

List in numerical sequence)Mining CWm

Prefix

S&5

tdJtO i

IChtAiN

Number

SfclMS^c

- -

IVEDS tiflO

rv vWy i il/li

Mining ClaimB*^KM rivuX

UZL *

Total number of mining claims covered by this report of work.

Number

ft"

^-3

l hereby certify that l have a personal and intimate knowledge ot the facts set forth in this Report of Work, having performed the work or witnessed same during and/or after Its completion and annexed report is true.Name and Address of Person Certifying

/07OTelephone No. Date

For Office Use OnlyTJOISIAIQ ONINW

VIOiyJ d30dOD3a

low uayi Cr. Recorded

Date Approved as Recorded81 :2d OCAONOE

Provincial Manager, Mining

SCHEDULE "A"

Pa. 777854777855777856777857777858777859777860777861777862777863777864777865777866

Pa. 851234851242851243851244851252851253851254851255851256851276

Pa. 868905868906868907868908868909868910868911868912868913868914868915868916868917868918868919868920868921868922868923868924868925868926

MUSKEG EAST QRID MUSKEG LAKE PROJECT

Pa. 868927868928868929868930868931868932868938868939868940868941

Pa. 869088

Pa. 872790

Pa. 883521 883522883525883526

Pa. 886547886548886549886550886551886552886576

Pa. 886689

Pa. 890477890478890479890480

NOISIAIQ 9NINIIA1

U3QdOD3b ON1NI1AI

B) :2d OCAONOE

i'VOt j, .rn Df'BBfcment

OntarioDOCUMENT NO.

Report of Work ~ Mining Act (Geophysical. Geological and Geochemical Surveys)

Iristiuctions- Please type or print ^- Refer to Section 77. the Mmmg Act for at

md maximum credits allowed per survey l- if number of mining claims traversed ex

attach a list, . Technical Reports and maps in duplicate should be submitted to

Mining Lands Section. Mineral Development and Lands Branch:Type ol Surveys) Mining Division Township or Area

6-21*2Recorded Holdens)

fa)AU\ CpoC)Prospector's Licence No.

Telephone No.

//on- - /OB/Survey

Credits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)Special Provisions '

For first survey:

Enter 40 days. (This includes line cutting)

for eacn additional survey: using the same gno:

Enter 20 days (for each)

Geophysical

- Electromagnetic

- Magnetometer l i . OtheriJ Geological

i Geochemical

Days per Claim

Man Days

Complete reverse side ana enter totaHs) here p P

Geophysical i Days per Claim

itometer

j Geological

MINING tAW^ SECTIONAirborne Credit*


Days per Claim

. Electromagnetic

Magnetometer

l Other

Total miles flown over claim(s).

Mining ClaimPrefix j Number

j

i teens*iiii.i'i ii

i

l

r

Mining ClaimPrefix

' ^

. Number

ze Sttfi

Mining ClaimPrefix

:f2*l

j

Total number of mining claims covered by this '*pon of work.

Number

fe M"

508l hereby certify that l have a personal and intimate knowledge of the facts set forth m this Repon of Work, after its comoietion and annexed report is true.

having performed the worn or witnessed same during and/or - ^

Name ano Address of Person Certifying

For Office Use Only

61 :?d OCAON06

"l

SCHEDULE "A"

-Pa, 841317841318841319841320841321841322841323841324841325841326841327841329841330841331841332841333841334841335841336841337841338841339841340841341

841401841402841403841404841405841406841407841408841409841410841411841412841413841414841415841416841417841418841419841420841421841422

MEENMUSKEG

wai *ei•Pep. 841423 -Pa-.

841424841425841426841427841428841429841430841431841432841433841434841435841436841437841438841439841440841441841442841443841444841445841446841447841448841449841450841451 Pa.841452841453841454 KL841455 -Per.841456841457841458841459841460841461841462841463841464841465841466841467841468841469

LAKE GRIDLAKE PROJECT

*ei-841470 -Per.841471841472841473841474841475841476841477841478841479841480841481841482841483841484841485841486841487841488841489841490841491841492841493841494841497841498

841690841691841692

869001869002869003869004869005869006869007869008869009869010869011869012869013869014869015

86901686901786901886901986902086902186902286902386902486902586902686902786902886902986903086903186903286903386903486903586903686903786903886903986904086904186904286904386904486904586904686904786904886904986905086905186905286905386905486905586905*869u5T869JQS8865W98690608694618690)62

*a. 869063869064869065869066869067869068869069869070869071869072869073869074869075

872858872859872860872861

115137611513771151378115137911513801151381

Pa.

lAIO ONINIW /d 9NINIIAI

OBAONOe

o!Norinern Development and Mines

Ontario

RU&DOCUMENT

w eport of Work —————Mining Act (Geophysical. Geological and Geochemical Surveys)

- Please type i- Refer lo Section 77. the Mining Act torTssessineni work requirement

and maximum credits allowed per survey type.- If number of mining claims traversed exceeds space on this form,

attach a list.- Technical Reports and maps m duplicate should be submitted to

Mining Lands Section. Mineral Development and Lands Branch:Type of Survey!*)

Recorded

j Mining Division Township or Area62122

Holdertsl

^ /A/C.Prospector'1 Licence No.

Address

A'/ftCaTkTelephone No.

Survey Company

COcA /A/C,Name and Address of Author (o Gee-Technical Report)

M&OJ7W/SM MsCredits Requested per Each Claim in Columns at right

Special Provisions

For trst survey:

Enter 40 days. (This includes line cutting)


Enter 20 days dor each)

Geophysical

- Electromagnetic

- Magnetometer

- Other

Geological

Geochemical

Days per Claim

Man Days

Complete reverse sioe and enter totaKs) here

j Geophysical

l - Electromagnetic

• li

Days per Claim

RE C E l!Vt*"1"1"

DEC l- Other

l Geochemical

Airborne MWNG lANDp 3CCT10N Days per Claim


Electromagnetic

Magnetometer i j Other'

Total miles flown over

Certification Verifying R

Mining Claims Traversed (List in numerical sequence)

l hereby certify that l have a personal and intimate knowledge of the facts set forth m this Report of Work, having performed the work or wnnessed same during and/or after us completion and annexed report is true.Name and Address of Person Certifying

For Office Use Only

Total Days j Date Recorded ICr. Recorded

81 :2d OCAONOE

841345841346841347841348841356841357841358

-Pa-. -041406"

841495841496

Pa.

i841505841506841518841519

841683841684841685841686841687841688841689

041003841693841694841695841696

872851872852872854872855872856

• •078050

SCHEDULE "A"

COOPER WEST ORID MUSKEG LAKE PROJECT

eo

NOISIAIO ONlNlAi VIDIdiVd

ei :2d OCAOUOE

Ontario

Ministry ofNorthern Developmentand Mines

Ministere du Developpement du Nord et des Mines

Mining Lands Section4th Floor, 159 Cedar StreetSudbury, OntarioP3E 6A5

Telephone: (705) 670-7264 Fax: (705) 670-7262

Your File: Our File:

W. 9003. 295, 296, 298 2. 13806

April 9, 1991

Mining RecorderMinistry of Northern Developmentand MinesCourt House BuildingP. O. Box 3000Sioux Lookout, OntarioPOV 2TO

Dear Sir/Madam:

RE: Notice of Intent dated March 6, 1991 for GeologicalSurveys on mining claims KRL 841317 et al in the township of Teefy.

The assessment work credits, as listed with the above-mentioned Notice of Intent have been appr/Tj&d^as of the above date.

Please inform the recorded hoi indicate on your records.

sincerely,

Ron. C. Gashinski, Provincial Manager, Mining Lands Mines Se Minerals Division

f JM/jl

claims and so

cc: Bond Gold Canada Inc. Toronto, Ontario

Resident Geologist Sioux Lookout

Ttohntul AiM*n*nt WorkCrftfiti

ffi*

BonoLGold

Stotfen 77 (19) it* "Minim Cwm AMMW^ Mhnm

KRL'841317 to 326'iricri 841331'toX341 1ncl. -841401.S9 1ncU 84142.3-424t 841428 to 439 Incl 841441 to 443 1ncl l 841446. to ; 454 JncU

'841460 to 462 1ncls'84l468;to'467 lnc \\'841469; 841476,! 841478-to .481-1ndi 841485^86,

841490191,841493:494, '841498/84W91-692, 869003 to 009 1ncU 869013 to 018 IncU 869023 to 036 1ncU 869039i 869041 to 045 Incl;

'869048 to 075"1hc1 J872860 -161',, P* 1151876 to 380 lncV.

jag; rag0,; S8S:'S!J8: 8K8: 8181'

Q AMtMfnctoAtfy *ovw*d br ** *"^W

VIDWXVdONIN1W

f) KBffi^***™01 Work Crwjlo ^ w i"*™* i 2.13806

March fi/01

Bond Gold Canada Inc.

tophytkal

Intfuettf po

Othw.

77 (18) *f -Mlnlnf CMlW AtMmtf" MtofM

Sp*cW Q

(Q OrtdKitiMtlMiAr*duc*db*c*Mt*9fp*nW

Q w woft tfttM tnd ftfluf** c* tppikvn.

PA' 841345 to 348 1ncU 841356 to. 358MOCT;

KRL 841495-496

Pr 841505-506', 841518-519

KRC 841683 to 689-1nil;

Pa 841693 to 696 Inc].

KRL 872851-852'872854 to 856 1ncl,

*t •ftdttt uikkf t*rton 77 (K) ter On fotk*Moa mtntna drimt

Q iwt Mtnctefttlv *OM***d by th* wuviyila.

Til Mnlf* fWwdtf nwy t**ie* th* itev* er^hi N Memwy M W*r thM thi totll MWttf *f i moKM on M* d*bn (tow MI

ft/01

toetion 77 (IB) tH*M(iMo|CWfniAMMMr whnm

3 AktonwQ

3 . *tt*O

Q ttt*tit**b*flr**w**"u"otP*'*' ••vfrtpofcMifli.

Q CiwH*l*vibwnndw*dbieiMiMfton**tl**

und* wctton 77 (U) ter tfvi

20 days Geological KRL 841497, 869002, 869011, 869038, 869040, 869046

30 Days Geological KRl 841327. 841330, 841457, 841468, 841477, 841492, 841690,869012, 869019, 869022,; 869037, 869047, 8728S9Pa 1151381

KRL 841426, 841459, 869010, 869020

ON!NM VIO!b.lVd

March 6/91 .9QQ3.2.9.6.

Gold CanadA Inc.

Kawashe LakeMoray tnt miitabtr d

.dm

tndutttf pollution.

Pa 777855 to 866 1ncl; 851243, 851262 to 266 Incli 868905 to 912 *ne; 868914 to 916 1ncl; 86S92Q-927 Jnc.lt 868929 to 932 1nc1 i

' 868938 to 941 1nd j 869088. 872790, 883625-526; 88.6547,,'886549, 886551-552; ' 886576, 890477 to 480 1nd.

(10) It* "Mlnlno qrin* A*MH*d" tttoam

Q

AhtonwQ

OroundQ

Q OrtdltitMvib*fnr*duMdb*e*u*t9f|MnW'

Q

p*eltt cwUttmxw **ctteft77 (16) forth* foflowog mlntmdiltm

10 days Geological pa 851242, 868918, 886550

20 days Geological Pa 777854, 851244, 851276. 868917, 868919, 883522

30 days Geological Pa 851234, 868913, 868928, 883521, 886548, 886689.

locTtdHi hw b*tn rtowtd fer thifotlowlM mlnlntcUlmt Q not wfftcfentfy eovtrtd by tN mnty {

..aaoaosaa

Tn* Mink* ft*4ord*r rrwy rtAio* th* *6ov, cw)Hi K MOMMry M ori* t^*t tht t*W fMiHb*t *f W (teyt fKMttMl M MOh *1*Jrt do** nn

l^CM No'ntvimt)eveio|Jtoj

Ontario rvp "A j "

falfl&W/' fWfning ActType of Surveys)

Recorded Holder(s)

•Address* 1 1 c^r^\ ~ "5fT*1 1 ^J^J A CL

i,K . -..,-... ...,... . Instructions - •••.-.— ^ ,,,^

Report of Work(Geophysical, Geological ant

DOCUMENT No i " P lease lype or print 'ivwvxwtvii-iii mw. i . fte(er ,0 section 77. the Mining Act tor assessment work requirements VA/QOn'"!* ? Q ^ and maximum credits allowed per survey type. VVtJUUO A i *J \ . H number of mining claims traversed exceeds space on this form.

i Geochemical Surveys)anach a list. Technical Reports and maps in duplicate should be submitted to Mining Lands Section, Mineral Development and Lands Branch:

1 Mining Division Township or Area i P/-} 77? /C//"? /^/f^CX/ 0*9^"^ \9~2ljL2.

Prospector's Licence No.

Telephone No.

, /^se^/A^ 55T^. TO/frÔTO ^KC^Tlo ,^^WOB/Survey Company . - '

AÂJA Cn;U\ C&rJft&Pi /AJC ; : . Vi: . :..,, . i ,Name"~ana Address of Author (of Geo-Techmcal Report) Oat* of Survey (from 4 to) tt O

ftL MMT/WlSM t /9S /fcto*^ •U'.^r^ltfr'S.^.Credits Requested per Each Claim in Columns at rightSpecial Provisions *

For first survey:

Enter 40 days. (This includes iine cutting)


Enter 20 days (lor each)

Man Days

Complete reverse side and enter total(s) here

Airborne Credits


Geophysical

- Electromagnetic '

•- Magnetometer

- Other

Geological

Geochemical

Geophysical

- Electromagnetic

- Magnetometer

- Other

Geological

Geochemical

; Electromagnetici

Magnetometer

j Other

Days per Claim

4oDays per

Claim

Days per Claim

—————

Total miles flown over clajm(s).

ArOV Z^/9^ :JM^7?1^^1Û-C.. — -

Mining Claims Traversed (List In numerical sequence) -Mining Claim

Prefix j Number

/\ .

i __ __ ^(^'{T}]^)^\^~ ' ii

iii!

Mining Claim"Prefix

— - ^~

NumberMining Claim

Prefix

^-TXV]

Number

ter'V?"

1


^08Certification Verifying

1 hereoy certify that 1 have a personal and intimate knowledge of the facts set forth m this Report of Work, having performed the work or witnessed same during and/or after ns completion and annexed report is true.Name and Address of Person Certifying

RL

For Office Use Only

Total Days i Date Recorded Cr. Recorded \

as Recoraea , Provincial Manager. Mining

.8-1.2.2-d OeAONOe

"i*

SCHEDULE "A"

~Pa

^rc***

WL841317^ -Pan841318v-841319'841320^841321^841322^841323-"841324'- -841325'841326-841327^841329^841330^84 13 3 l/841332 ̂841333 ̂841334 '841335^841336^841337^841338^841339^841340^841341-

841401 ̂841402^841403K841404^-"841405^841406^841407^841408X841409^841410^841411^841412^841413^841414*^841415^841416^841417^841418 ~"841419 -'841420^841421-v841422^

MEENMUSKEG

8414234^^841424iX841425"?F841426^8414274841428^841429^841430-^841431^841432 ̂841433-/841434V841435^841436^-841437^841438-^841439^841440^841441^841442^841443^8414444841445|841446^841447^841448^841449^841450^'841451-" Pa.841452"-841453*^841454^ fat841455-i *fr.841456?841457^841458^841459X841460 X841461i-^841462^841463^841464i:841465^841466i/841467^841468^.841469/

LAKE GRIDLAKE PROJECT

l Kfc*. 841470^- -Pa-.841471-^841472^841473^841474^841475^-841476^841477^841478^841479^841480^841481^841482^841483^841484^841485^841486^841487^841488^841489^-841490^841491^841492^841493^0841494V/841497 'i841498^

(841690^841691^841692^

869001?869002^869003^869004^869005^869006^869007 ̂869008^869009^869010^869011 4869012^869013^869014^869015^

869016--869017 ^869018^869019^869020X869021^8 69 02 2/869023^869024^869025 ̂869026^869027^869028869029 ̂ j869030^.869031^869032^869033 ̂869034 ̂869035^869036^8690377869038/869039^^869040^869041 —869042 -~869043^-869044v/869045^869046^869047^869048^-869049^869050^869051-"869052^869053 ̂869054 r"o o 9 055

86^ftf^lAI869U5v^'**^?JQ5fi r86yrov^^869060 ̂

869to52*J2

Pa.

869063^869064 ̂869065 ^869066^869067^869068.^869069^869070-^869071-^ 869072 t--" 869073- 869074 l^ 869075'^'

872858^ 872859 4- 872860^- 872861^

1151376^1151377^1151378^1151379^1151380 ̂1151381^

ONINIW

OCAON06.

l DOCUMENT No!"

Report of Work lining Act (Geophysical, Geological and Geochemical Surveys)

Instructions- Please type or print- Refer to Section 77. the Mining Act tor assessmeni work requirements

and maximum credits allowed per survey type.- If number of mining claims traversed exceeds space on this form,

attach a list.- Technical Reports and maps in duplicate should be submitted to

Mining Lands Section. Mineral Development and Lands Branch:Type of Survey(S)' j Mining Division Township or Area

62122Recorded Holderis)

/A/c.Prospector's Licence No.

Address Telephone No.

Survey Company

COcA /A/C,Name and Address of Author (ol Geo-Technical Report)

Credits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)Special Provisions

For first survey: . , w

Enter 40 days. (This includes line cutting) -



Man Days

Complete reverse side and enter totat(s) here ~

Airborne Credits

Note: Special provisions credits do hot apply to Airborne Surveys.

Geophysical

- Electromagnetic -

- Magnetometer

- Other

Geological

Geochemical

Geophysical

- Electromagnetic

- Magnetometer

- Other

Geological

Geochemical

Electromagnetic

: Magnetometer

Other'

Days per Claim

HoDays per

Claim

Days per Claim

1

Total miles flown over clajm(s). jDate 1 Rj

2r?ffi^^!32HIt J I f v\Jf^f^V^^" "*"

Q

Mining ClaimPrefix'

Number

Ptense- '

'j

# C/*'.** S^ovu-

4^ oky* ^**

A-vukfe^' tt A f n t/v;

.rgvn/7

/Ir y

.

Mining ClaimPrefix

56

" tVtv

f ' i rytttJ

*lt

•rf)s

t Number

f J * Lw *4TCAiK.

^t M ̂ 4 4 C 09^^^^f

J AJ t nl/ru

Mining ClaimPrefix

^VFT

-

--4aJLLz

Number

V?"

.

HJirt t^ kM tf^Y*f

jjjj


3321Certification Verifying Report of

l hereby certify that l have a personal and intimate knowledge of the facts set forth m this Report of Work, having performed the work or witnessed same during and/or after its completion and annexed report is true.Name and Address of Person Certifyi

For Office Use Only

Total Days i Date Recorded Cr. Recorded

Provincial Manager. Mining Lands

8| :2d OCAONOE

•36i (89/061

841345^- 841346^ 841347^ 841348 *H 841356 # : 841357^ 841358 l

•Pa-. -8444-86-i 841495^ 841496^

Pa.

i841505^' 841506-*" 841518^ 841519 \

841683^ 841684^ 841685V 841686V841687^ 841688^ 841689 .X

To.. -844-694- -844-69S- 841693^ 841694^ 841695 i: 841696-i

872851^872852^872854872855?872856i

lSCHEDULE "A"

COOPER WEST GRID MUSKEG LAKE PROJECT

ooT

NO IS l A 10

0UYrw**-O /L ;8| ODAQNQE

Ontaric

Report of Work j \^i Mining Act {Geophysical, Geological

• ^•- 5 -v * f.. . (

- nt'Ci' ic- ouCiioit ' /. ittc ivnjitii^ /iCl iu o^sebsiiifcrii v. UK i tnuiieii't-and maximum credits allowed per survey type.

. tl number of mining claims traversed exceeds space on this to? anach a list.

- Technical Reports and maps in duplicate should be submitted Mining Lands Section, Mineral Development and Lands Branch

Type of SurvevfsK

C ^TOuOO/XC:rfcRecorded Holder(s)

f^rw/A OocA cyw/Address '

n #2^Survey Company

/to^JA COLA c/9

M ning Division Township or Area

Prospector's Licence No.

Telephone No.

&1&6 vSTf. TDrf^/OTO MXC. AT^ S&^-'/OS/T^\ftbP, /A/C

Name and Address of Author (of Geo-Technical Report) . Date of Survey (tror

Credits Requested perSpecial Provisions

Each Claim in Columns at right

For first survey: —

Enter 40 days.- (This includes line cutting) •-••-•-



Man Days ...,. .

Complete reverse side and enter total(s) here

Airborne Credits

Note: Special provisions p credits do not apply to Airborne Surveys.

Geophysical

- Electromagnetic

- Magnetometer

-Other

Geological

Geochemical

Geophysical

- Electromagnetic

- Magnetometer

- Other

Geological

Geochemical

Electromagnetic

Magnetometer

Other

Total miles flown over claim(s).Date

Days per Claim

40

Days perClaim

^L&f

Days per Claim

iRecBrdad Holger or Aoenl fStonati^rel

Mining Claims Traversed iMining Claim

Prefix

-t

Number

Pt&fcg,

^(f))[p)^7

i A to) - II 10 ^0Day | Mo. | Yr

List in numerical sequence) :Mining Claim

Prefix

SEE

Number

^CMC&C

- Mining Claim

Prefix

L& *

...- ,

. ,. . ,-


' Number

ft,,

^3Certification verifying Repprt of

1 hereby certify that 1 have a personal and intimate knowledge of the facts set forth in this Report of Work, after its completion and annexed report is true.

having performed the work or whnessed same during and/or

Name and Address of Pereon Certifying

fa. TO^O/OTOTelephone No. Date

For Office Use OnlyONINl

VIDIdJVdONINIW

Total Days Cr. Recorded

2VO

Date Recorded

//o*/. 30/90Date Approved as Recorded

Mining rocord

81 :?d OCAON06Provincial Manager, Mining

1362(88/06}

SCHEDULE "A"

Pa,

Pa.

Pa.

7778544777855^777856^x"777857^777858"-777859X"777860^777861X777862^777863 v"777864 ix777865 vX 777866X

851234-^851242^851243-851244?851252^^851253^851254^851255vx851256^851276^

868905X868906^868907^868908^868909^868910X"868911^"868912^^868913^868914^868915^

8689174868918^868919i868920 v"868921V-868922^868923^868924v^868925^868926X

MUSKEG EAST GRID MUSKEG LAKE PROJECT

Pa. 868927*--" S68928/ 868929V"868930^ 868931^

8689381^ 868939 ix-

868941 ""

Pa. 869088 ̂

Pa. 872790^

Pa. 88352li 883522 i 883525^ 883526*^

Pa. 886547^ 886548^ 886549^ 886550 3 886551-- 886552vX886576 -~

Pa. 886689^

Pa. 890477-^ -890478^^ 890479^ 890480,^"

NOISIAIQ ONINIW VIDIdlVd

81 :2d OCAONOE

—5I 0 30'

MCVICAR LAKE.- G-2121

———hr-——"j;"™""

—-4 Z *MZ\Jt4*^ \94t4lA±9*t49t l j*\ 1**^ l**4 ' l***-, |**~ "W4

l^î^L-iS'SL'JL^

i*****',!*****9 r/ " \ v i~"~ ' "^rr'*r—rn V- *i j,-^-i v ri i/f/m 'f*/** i :*V J —"*v, 'JX" K" '/Jfer/H

fy- /*gg yi^/jgtyat*~, r"" ~-—]—r 51-

^***^ *î /*g**^g Lf *iiiî.

l 107327

_~~ —— ""~———'

^^ *"^^^ "*^ "^^ ^ - - —i ^. -l — ' ^^ ..^-[^ —' f ^ ̂b ^^^

~t7f i f ~,~i*H'"3~i*vyff*r|

OX-4i:-:i:

R*^yf^rr* ____ —^~

i tuftiyr- ! K59I i.Kami^bi i*3882

NABEMAKOSEKA520*6NWeHB08 2.13606 KAWASHE LAKE

THE INFORMW1ON THAT ? ' APPEARS ON THIS MAP

HAS BEEN COMPILED FROM VARIOUS SOURCES, AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE M1N-

' ING CLAIMS SHOULD CON SULT WITH THE MINING RECORDER, MINISTRY OF

. NORTHERN " DEVELOP- N *MENT AND MINES, FOR AD-

4 DmONAL INFORMATION ON THE STATUS OF THE

. LANDS SHOWN HEREON.

!isv. v "-v- - ; ;--: j-.,. -- -.-.- .. --^ w-* -- ; T - '-'

. 4 . .-•- . ."C - - - - -v J' *,* - — , -^ . - - ~. "

LEGEND

HIGHWAY AND ROUTE No - OTHER ROADS. \ TRAILS J - '

-SURVEYED LINESTOWNSHIPS. BASE LINES. ETC. LOTS. MINING CLAIMS. PARCELS. ETC

^NSURVEYED LINES LOT LINES PARCEL BOUNDARY MINING CLAIMS ETC -

RAILWAY AND RIGHT OF WAY - UTILITY LINES* f

-ÔN-PERENNIAL STREAMFLOODING OR f LOODiNG RIGHTSSUBDIVISION Oft COMPOSITE PLAN RESERVATIONS ~~ ORIGINAL SHORELINE^ " MARSH OR MUSKEG , ^ MINES - ^ ^-,

TRAVERSE MONUMENT ^* ^ ^ .

DISPOSITION OF CROWN LANDS

TYPE OF DOCUMENT.

SYMBOL

FATENT, SURF ACE 4, MINING -RIGHTS -^^'—^L^ \ - , SURF ACE RIGHTS ONLY. .^.^JL^L." ..g

r .' - , MINING RIGHTS ONLY,CEASE,SURFACE 4 MINING ' ^" .SURFACE HIGHTSpNLY...^^^™___~.™l B

* \ MINING BIGHTybNLY.-~-.-J-,-—^- -. J7-^. BLICENCE OF OCCUPATION ,ORDERÎW-COUNCIL ^^-.;RESERVATION ^^..^...^CANCELLED V':--:.ll y. ', -..

^ V

SAND a GRAVEL -^L.-.^-™. "\.^ ~-4 O.MOTC: MINHMO W4GMTS IN r AH CCL* PATCNTCO^mOfl TO

~^*IJ. VCCTED tN OHK*1HAL ÂTCNTEC W Tt**LANDS ACT. HX.O l*T*. CMA* WO. BCC.*V*4 *V**S*C 1.

^-u . - - * * - - *-~ - ' . - v "- - f -t - ~

R E F E; R.: E JMAREAS WITHDRAWN FROM

- - . ^M.R.Q. - MINING RIGHTS ONLY

". * S.R.O. -SURFACEJWGRTSONtY^ ^/I ^ ^ ^^ '

. *L* S. v-MINING AND SURFACemGHTS*

TIJX - TRAPUNE 'i - OUTPOST

. 2 - OUTPOST CAMP

SCALE 1 INCH^WCwiv

ôoe aooQ MOO

O 7OO •MCTHfS.

2000KM.

ARfA ;-.--..-* !" : .; -^,. ' -- ;-' ,-/

MEEN LAKE 1MN R. ADMINISTRATIVE DISTRICT ^ - H

SIOUX LOOKOUT '^r|MINING DIVISION V ' ' ' j'^

MBI iaMIS/PATRICIA ,LAND TITLES/ REGISTRY DIVtSlD^, ' , ^:

KENORA (PATRICIA PORTION)

\ ^Natural ,, Resource

Ontarip

MARCH

11 ~

NA

BE

MA

KO

SE

KA

LA

KE

G

-213

5

j—

——

j ^,

-

lv S

' *

;Y

S

i o

M

i r\

.

w '

..Si-'

-.

'j..l

'.r

fji

u

- ^

l -

- —

—l

- —

WR

IGH

T LA

KE

G

-227

1

Hou

r La

ke

yen

~j b

oulde

rs

rl

Ok

*

y B

IOW

dOW

D-y

-^

3d 6

a (p

eg. d

yke)

V

^

Sb,W

t(we

A

' ""

XS

b(F

bK)-

-V —

A-

— T

\X

i i^

^

V y

^-

ON'M

EB

9-I

2

"6 '

Sb-Fb

GO

LDE

N P

ATR

ICIA

MIN

E

LEA

SE

BO

UN

DA

RY

BA

SE

LIN

E

00+

00

II50

azim

uth

Y

Sb,

Bw

y P

JM

E88

-03

-\M

E8

8-0

9 .

^

kS

b, l

swam

p ;'\\

Sb

fail JL

AX

!

Sb

X.

swam

p

LEG

EN

D

TREE

TY

PE SYMBOLS

Jack pine

Sb

l Black

spru

ce

Fb

l Ba

lsam

fir

Tama

rack

(L

arch

)

Cedar

Tag

alder

Whit

e bi

rch

Trembling

aspen

FELSIC TO

INTERMEDIATE IN

TRUSIV

E RO

CKS

Alkali feldspar granite

Tona

lite

Diorite

INtermediate dy

ke

Quar

tz diorite

Outc

rop:

la

rge/

sme

ll

Cont

act:

ob

ser

ved/

assumed

Shea

ring

Samp

le lo

cation

Samp

le nu

aber

0 149

9.7

Dril

l hole a

nd number

FELSIC PORPHYRKIC IN

TRUS

IVE

ROCK

S

Quar

tz porphyry

Quar

tz

- feldspar po

rphyry

s" s

Over

burd

en slope: pr

onou

nced

/sli

ght

Bond

Gol

d Ca

nada

Inc.

Vegetation/tree-type bo

unda

ry

Swam

p, bog

Cla

im

post

: ob

serv

ed

Cla

im

po

st:

not

obse

rved

Witn

ess

post

Road

, ^

Drill

road

, brill

pad

868

93

0

Cla

im

723.

Folia

tion:

no d

ip o

bse

rve

d/in

clin

ed/v

ert

ica

l

MU

SKEG

EA

ST P

RO

PER

TYM

USK

EG E

AS

T G

RID

NO

RT

HW

ES

TE

RN

ON

TA

RIO

, N

.T.S

. 5

2O

/6

MAHC INTRUSIVE

ROCKS

Horn

blen

de gabbro

6f

l Ma

fic

dyke

MAFI

C METAVOLCANIC RO

CKS

I a

l Ma

ssive

flow

lb

l Pi

llowed

flow

CO

MPI

LATI

ON

MA

P

2.1

38 G

Cooper L a/(e

Mapped

Previously

LEGEND

FELSIC TO INTERMEDIATE INTRUSIVE ROCKS

85l Granodiorite

Trondhjemite

Tonalite

Diorite

FELSIC PORPHYRITIC INTRUSIVE ROCKS

Feldspar porphyry

/r- l Quartz f e Idspar porphyry

MAFIC INTRUSIVE ROCKS

6c l Hornblende gabbro

CHEMICAL METASEDIMENTS——i4c l Magnetite - chert iron formation

INTERMEDIATE rtETAVQLCANICS

Massive flow

2k l Pyroclastic, fragments more mafic than matrix

-41* Y "h*or s.' Sb "Jo - , ' \Q q tz. carl i

Mapped

Previously

MAFIC METAVQLCANICS

Massive flow

Pillowed flow

Coarse-grained flow

Chlorite schist

Amphibolitized flow

Sb.Pj yjut; r-op: large/smal l

Contact: observed/assumed

Shearing

Sample location

Sample number

Claimpost

84I5C3 a m "umber

S st y( Foliation: no dip observed/inclIned/vertical

Cooper Lake

Cooper Lake

v^. x" Overburden slope: pronounced/slight

Vegetation/tree-typie boundary

Swamp, bog

TREE TYPE SYMBOLS

Jack pine

Black spruce

Balsam fir

Tamarack (Larch)

Cedar

Tag alder

White birch

Trent)l ing aspen

Mapped Previously

Bond Gold Canada Inc.MUSKEG WEST PROPERTY

COOPER WEST GRIDNORTHWESTERN ONTARIO, N.T.S. 52O/6

COMPILATION MAP

52086NWe088 2 .13626 KAWASHE LAKE S30

2.1380&

FELSIC TO INTERMEDIATE ROCKS 8a Alkali feldspar granite 8b Granodiorite Bc Tronjhemite 8.d Tonalite Be Diorite Bf Granite pegatite 8h Biotite rich granodiorite 8i Intermediate dyke

FELSIC PORPHYRY INTRUSIVE ROCKS 7a Quartz porphyry 7b Feldspar porphyry 7c Quartz-feldspar porphyry

MAFIC INTRUSIVE ROCKS 6a Gabbro6c Hornblende gabbro 6d Hornblende melagabbro 6e Magnetite-hornblende gabbro 6f Mafic dyke

CLASTIC SEDIMENTS B Unsubdivided 5b Siltstone 5c Mudstone 5d Conglomerate 5e Biotite-quartz schist 5f Sericite-biotite-quartz schist 5g Garnet-biotite-muscovite schist 5h Chlorite-quartz-biotite schist

CHEMICAL METASEDIMENTS 4a Ferruginous chert 4b Metachert 4c Magnetite 4d Sulphide ironstone 4e Massive sulphides 4f Marble

FELSIC METAVOLCANICS 3a Massive flow3b Flow top breccia, flow breccia 3c Tuff3d Lapilli tuff 3e Crystal tuff 3f Tuff breccia

silcarb, cc

ep

gntmag

pypocpy

cblqv sh

LEGEND

INTERMEDIATE METAVOLCANICS 2a Massive flow 2b Tuff2c L apilli tuff 2d Tuff breccia 2e Lithic tuff 2g Monolithic pyroclastic 2h Heterolithic pyroclastic 2j Pyroclastic, fragments more

mafic than matrix 2k Pyroclastic, fragments more

felsic than matrix 21 Agglomerate 2m Crystal tuff 2o Sericite schist

MAFIC METAVOLCANICS la Massive flow Ib Pillowed flow le Pillowed breccia Id Amygdaloidal flow le Banded flow lg Coarse-grained flow l h Tuff1m Plagioclase feldspar phyric flow In Chlorite schist lo Araphibolitized flow Is Amphibole-muscovite-chlorite schist It Ta-lc-chlorite-biotite-muscovite schist

ABBREVIATIONS

SilicificationCarbonization

EpidoteGarnet

MagnetitePyritePyrrhotite ^

ChalcopyriteChloritization

Quartz veinShearing

B Q WP

0.01 Au

SYMBOLS

Claim post, witness post, post not found

Outcrop

Outcrop area

Drill hole

Geological contact: observed, assumed

Sample location

Assay result (oz/ton Au)

Bedding, inclined

Bedding, vertical

Foliation, inclined, vertical

Mineral lineation with plunge

Shearing

Pillow tops

TIE LINE 10+00

2.13

SHEET INDEX

100Metres

100 200 300l l — l 400

500E—

500 1000

Feet


MUSKEG LAKE PROJECTMEEN LAKE PROPERTY

NORTHWESTERN ONTARIO, N.T.S. 52O/6

GEOLOGYSHEET 1

DRAWN BY :

DATE t NOV/90

DRAFTED BY :J.M.

REVISIONS DATE

2.13886 KAWASHE LAKE 240

LEGEND

FELSIC TO INTERMEDIATE ROCKS 8a Alkali feldspar granite 8b Granodiorite 8c Tronjheraite

Tonalite 8e Diorite 8f Granite pegatite 8h Biotite rich granodiorite 8i Intermediate dyke

SilicificationCarbonizationEpidoteGarnetMagnetitePyritePyrrhotiteChalcopyriteChloritizationQuartz veinShearing

FELSIC PORPHYRY INTRUSIVE ROCKS 7a .Quartz porphyry 7b Feldspar porphyry 7c Quartz-feldspar porphyry

MAFIC INTRUSIVE ROCKS 6a Gabbro6c Hornblende gabbro 6d Hornblende melagabbro 6e Magnetite-hornblende gabbro 6f Mafic dyke SYMBOLS


Outcrop

Outcrop area

Drill hole


Sample location

Assay result (oz/ton Au)

Bedding, inclined

Bedding, vertical



Shearing

Pillow tops

CLASTIC SEDIMENTS 5 Unsubdivided 5b Siltstose 5c Mudstone 5d Conglomerate 5e Biotite-quartz schist 5f Sericite-biotite-quartz schist 5g Garnet-biotite-muscovite schist 5h Chlorite-quartz-biotite schist

Sjtdyke 8b(sheored*chl,ser)

sheared8j,lo,py 8b 8b(sheartd

CHEMICAL METASEDIMENTS 4a Ferruginous chert 4b Metachert 4c Magnetite 4d Sulphide i ronstone 4e Massive sulphides 4f Marble


INTERMEDIATE METAVOLCANICS 2a Massive flow 2b Tuff2c Lapilli tuff 2d Tuff breccia 2e Lithic tuff 2g Monolithic pyroclastic 2h Heterolithic pyroclastic 2j Pyroclastic, fragments more


felsic than matrix ' 21 Agglomerate 2m Crystal tuff 2o Sericite schist

MAFIC METAVOLCANICS la Massive flow Ib Pillowed flow le Pillowed breccia Id Amygdaloidal flow le Banded flow lg Coarse-grained flow l h Tuff1m Plagioclase feldspar phyric flowIn Chlorite schistlo Ampnibolitized flowIs Amphibole-muscovite-chlorite schistH Talc-chlorite-biotite-muscovite schist

Buggy - Muggy Lo'Ae

— BASE LINE 00+00s * i

— .—i—— - TIE LINK 10+00 S

|I445I-50|DV T M 4450

MEENMEEN

L A K EL A K E

Bond Gold Canada Inc



GEOLOGYSHEET 2

ET, MR, MTSHEET INDEX

52006NWCe08 2 .13866 KAWASHE LAKE 250

LEGENDFELSIC TO INTERMEDIATE ROCKS 8a Alkali feldspar granite fib Granodiorite 8c Tronjheniite 8d Tonalite 8e Diorite 8f Granite pegatite 8h Biotite rich granodiorite 81 Intermediate dyke


SilicificationCarbonizationEpidoteGarnetMagnetitePyritePyrrhotiteChalcopyriteChloritizationQuartz veinShearing

INTERMEDIATE HETAVOLCANICS 2a Massive flow 2b Tuff2c Lapilli tuff 2tJ Tuff breccia 2e Lithic tuff 2g Monolithic pyroclastic 2h Heterolithic pyroclastic 2j Pyroclastic, fragments more


felsic than matrix 21 Agglomerate 2m Crystal tuff 2o Sericite schist

FELSIC PORPHYRY INTRUSIVE ROCKS 7a Quartz porphyry 7b Feldspar porphyry 7c Quartz-feldspar porphyry

MAFIC INTRUSIVE ROCKS 6a Gabbro6c Hornblende gabbro 6d Hornblende melagabbro 6e Magnetite-hornblende gabbro 6f flafic dyke

8o(qtz dior)

SYMBOLS


Outcrop

Outcrop area

Drill hole


Sample location

Assay result {oz/ton Au)

Bedding, Inclined

Bedding, vertical



Shearing

CLASTIC SEDIMENTS 5 Unsubdivided 5b Siltstone 5c Mudstone 5d Conglomerate 5e Biotite-quartz schist 5f Sericite-biotite-quartz schist 5g Garnet-biotite-muscovite schist 5h Chlorite-quartz-blotite schist

SHEET INDEXMAFIC METAVOLCANICS la Massive flow Ib Pillowed flow le Pillowed breccia Id Araygdaloidal flow le Banded flow lg Coarse-grained flow l h Tuff1m Plagioclase feldspar phyric flow In Chlorite schist lo Araphibolltlzed flow Is AmpMbole-muscovlte-chlorite schist It Talc-chlor1te-b1otite-muscov1te schist

-CHEMICAL METASEDIMENTS 4a Ferruginous chert 4b Metachert 4c Magnetite

Sulphide ironstone 4e Massive sulphides 4f Marble

felsite dykes sh

Mer kin 8a,sh 8a(sh)

l-2VopyO

3e,sh(qtz d ior.f.g.)

5b lithic S \wachem.g.

3*. f.a 0Xo py

l I43TO-73I (Q

4c

Ib(sh) 81 dyke

l. oggiom. ep.po+py

()MC 89-11

2Vopy,fil stringersJ6837

la

16885Ig(agglom) la l b'd

xo\x lb

aevt. altn. lens

6a,la,2o(*)porph

L('WER\WEEN LAKE GfMGROUP

L1AKE GFOUPUPPER M

MEEN

LAKE16622.231 7b,4b

Ph,aiHlS364-67| 80 C) MC89-I!

lofrogments

Pomogron/fe

Bond Gold Canada Inc.MUSKEG LAKE PROJECTla, d carb

amygdules

MEEN LAKE PROPERTYNORTHWESTERN ONTARIO, N.T.S. 52O/6

GEOLOGYSHEET 3

ET, MR, MT

52006NW0883 3 . 13806 KAWASHE LAKE 260

8b,8o (pegmatite

8b(d] 8a dyke

y ineiBO. —^. m —r" —S""

Syket **he . (4b lens?

16862 j A9

le(4blen;E)efj 8* *-43 .-r?-'

sh q.v. 1.5m - 8b

x lb(8d dykes)

8d qtz.slips

f la xenos)

sheared, tightly folded ib,8d(bx) plunge

x x la'8dlox (

,-^ ^ f^^—^

"* ^ ^^TO^X ____ 60\

PI ru

LAKE

tOcm folded felsite dyk

6a sheared, chloritic

8e qtz diorite

Im la 50Xo po

Cooper Lake

LEGEND

FELSIC TO INTERMEDIATE ROCKS 8a Alkali feldspar granite 8b Granodiorite 8c Tronjhemite

Tonalite 8e Diorite 8f Granite pegatite 8h Biotite rich granodiorite Si Intermediate dyke

INTERMEDIATE METAVOLCANICS Za'Massive flow

Tuff 2c Lapilli tuff 2d Tuff breccia 2e Lithic tuff 2g Monolithic pyroclastic 2h Heterolithic pyroclastic 2j Pyroclastic, fragments more


felsic than matrixAgglomerate

2m Crystal tuff 2o Sericite schist

SYMBOLS


Outcrop

Outcrop area

Drill hole


Sample location

Assay resuU (oz/ton Au)

Bedding, inclined

Bedding, vertical



Shearing

Pillow tops

FELSIC PORPHYRY INTRUSIVE ROCKS 7 a Quartz porphyry 7b Feldspar porphyry 7c Quartz-feldspar porphyry

MAFIC INTRUSIVE ROCKS 6a Gabbro6c Hornblende gabbro 6d Hornblende melagabbro 6e Magnetite-hornblende gabbro 6f Mafic dyke

MAFIC METAVOLCANICS la Massive flow Ib Pillowed flow le Pillowed breccia Id Amygdaloidal flow le Banded flow lg Coarse-grained flow l h Tuff1m Plagioclase feldspar phyric flow In Chlorite schist lo Amphibolitized flow Is Amphibole-rouscovlte-chlorite schist It Talc-chlorite-biotite-muscovite schist

CLASTIC SEDIMENTS 5 Unsubdivided 5b Siltstone 5c Mudstone 5d Conglomerate Se Biotite-quartz schist 5f Sericite-biotite-quartz schist 5g Garnet-biotlte-muscovite schist 5h Chlorite-quartz-biotite schist

CHEMICAL METASEDIMENTS 4a Ferruginous chert 4b Metachert 4c Magnetite 4d Sulphide ironstone 4e Massive sulphides 4f Marble

SilicificationCarbonizationEpidoteGarnetMagnetitePyritePyrrhotite

ChalcopyriteChloritizationQuartz vein

Shearing

Bond Gold Canada Inc.FELSIC METAVOLCANICS 3a Massive flow3b Flow top breccia, flow breccia 3c Tuff3d Lapilli tuff 3e Crystal tuff 3t Tuff breccia



GEOLOGYSHEET 4

ET, MR, MTSHEET INDEX

2.13606 KAWASHE LAKE 2Z0

\ground \

TIE LINE 10+00 S

B H aWP

Black spruce

Balsam fir

Jack pine

Larch, tamarack

Trembling aspen

Balsam poplar

Tag alder

White birch

Bog, muskeg, wet ground

Vegetation type boundary

Gradual to moderate change in slope

Scarp, cliff

Esker


2*1138

SHEET INDEX

100 O \—l l—It—l

Metres 100 200 300 400

500 500 1000

Feet




TOPOGRAPHY MAPSHEET 1

DRAWN BY .

DATE NOV/90

DRAFTED BY: J.M. REVISIONS DATE

520a6NW00BB 2.13886 KAWASHE LAKE 280

SBltBw,Ffl

TIE LINE 10+00 N -

- BASE LINE 00+00

hummocky and 8 boukfen

E E NMEEN

L A K EL A K E

Black spruce

Balsam fir

Jack pine

Larch, tamarack

Trembling aspen

Balsam poplar

Tag alder

White birch



Gradual to moderate change In slope

Scarp, cliff

Esker


S.13800





SHEET INDEX

a.13806 KAWASHE LAKE 230

SHEET INDEX

TIE LINE 20+00 N

SB.A!

Black spruce

Balsam fir

Jack pine

Larch, tamarack

Trembling aspen

Balsam poplar

Tag alder

White birch

, muskeg, wet ground


Gradual to moderate change in slope

Scarp, cliff Esker


2.^1380*3

Metres100______O l—l l—l l—' 100 200 300 400

500 500 1000

Feet





DRAWN BY :' ET, MR, MTDATE : NOV/90

DRAFTED BY' J.M. REVISIONS DATE

52006NW0008 2.13806 KAWASHE LAKE 300

sand a boulders | S B. AT.PJ

blowdown SBJ,BW ,WT i AB

sand f boulders

- -ir- X

LAKE

Black spruce

Balsam fir

Jack pine

Larch, tamarack

Trembling aspen

Balsam poplar

Tag alder

White birch



Gradual to moderate change tn slope

Scarp, cliff

sand outwash ,̂ \ 7-


2.138Gb





SHEET INDEX

52006NWee03 2 . 13806 KAWASHE LAKE 310

rpt on geol mapping prog of the cooper w grid …...1989; bond gold canada inc. completed ground em...

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