RECEIVED NOV 2 v w MINING LANDS SECTION€¦ · 538l6swe0ei 010 report on geological mapping, prospecting and trenching four square property district of kenora, patricia mining division

538l6SWe0ei 010

REPORT

ON

GEOLOGICAL MAPPING, PROSPECTING AND TRENCHING

FOUR SQUARE PROPERTY

DISTRICT OF KENORA, PATRICIA MINING DIVISION

NORTHWESTERN ONTARIO

FOR

POWER EXPLORATIONS INC.

RECEIVEDNOV 2 v w

MINING LANDS SECTION

August, .1 S'87 Paul S. Newman, P.Se.

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TABLE OF CONTENTS

Page

l.O SUMMARY l

Figure No. l - Location Map 3

2.0 INTRODUCTION 4

Figure No. 2 - Property Location andRegional Geology 5

3.0 PROPERTY DESCRIPTION 6

4.0 LOCATION, ACCESS AND SERVICES 6

Figure No. 3 - Claim Sketch 7

5.0 TOPOGRAPHY AND VEGETATION 8

6.0 PREVIOUS WORK 8

7.0 REGIONAL GEOLOGY AND ECONOMIC MINERALIZATION 9

8.0 PROPERTY GEOLOGY AND MINERALIZATION 12

8.1 General Geology 128.2 Volcanics 138.3 Sediments 148.4 Intrusives 158.5 Structure 168.6 Geophysical Summary 178.7 Economic Mineralization 18

8.7.1 Trench FS-1 18

Figure No. 4 - Stripped Area A 19

Figure No. 5 - Trench FS-1 Detail 20

8.7.2 Trenches FS-2 and FS-3 21


Figure No. 6 - Trenches FS-2 and FS-3 Detail 22



TABLE OF CONTENTS (Cont'd)

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8.7.6 Stripped Area B 24



Figure No. 10 - Stripped Area B 27

8.7.7 General Discussion 28

9.0 CONCLUSIONS 29

10.0 RECOMMENDATIONS 29

10.1 Phase I 2910.2 Phase II 29

11.0 ESTIMATED COST OF RECOMMENDED EXPLORATION PROGRAM 30

11.1 Phase I 3011.2 Phase II 30

12.0 REFERENCES 31

APPENDICES

A

B

C

D

CERTIFICATE OF QUALIFICATIONS

TECHNICAL DATA STATEMENT

ROCK SAMPLE DESCRIPTIONS

ROCK SAMPLE ANALYTICAL CERTIFICATES

LIST OF DRAWINGS

Back of report

DRAWING NO. l - GEOLOGY-FOUR SQUARE PROPERTY In map pocket

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l.O SUMMARY

The following report describes the results of a geological mapping, prospecting and trenching program carried out over

the Four Square property for Power Explorations Inc. in June and July, 1987.

The property is located 100 miles north-northwest of Pickle

Lake in Northwestern Ontario. Access may be gained by float

plane from Pickle Lake or from Weagamow Lake, 40 miles to the west. A winter road has been constructed into the Mussel-

white property from Highway 808, and provides winter access

to within 12 miles south of the property.

The property lies on the south limb of a synclinal fold which

parallels the North Caribou Lake greenstone belt along its central core. It straddles a north-northwest trending

contact between the South Rim Metavolcanics and Eyapamikama

Lake Metasediments (Breaks et al., 1986). The South Rim

Metavol- canics in this area are comprised of pillowed and massive mafic volcanics and intermediate to felsic flows and

tuffs with large intercalations of clastic metasediments and

oxide facies banded iron formation. Stratigraphically overlying this package are cross-stratified, epiclastic sedimentary accumulations (Eyapamikama Lake Metasediments) in

the axial portion of the large syncline. The intrusive

contact of the tonalitic North Caribou Lake batholith lies in the extreme southwest corner of the property (Fig. No. 1).

Numerous anomalous gold values, ranging up to 790 ppb, were obtained from grab samples of moderately deformed, highly

gossaned banded iron formation at 77*OON,4-HOOW. Grab samples

at a similarly deformed and gossaned zone of banded iron formation at GS+OON^+OOW had gold values ranging up to 235 ppb.

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Six old trenches that were re-exposed, mapped and sampled in

detail, either within or at the contact with overlying mafic

volcanics, yielded anomalous gold values of up to 190 ppb.

Other anomalous gold values of 100, 235 and 170 ppb were

derived from a gossan zone in wackes, a quartz vein and a

shear zone in basalts, respectively.

Further exploration is warranted to better determine the

significance and extent of gold mineralization, shear zones

and vein systems on this property. Differing tectonic styles

manifested in different zones of the banded iron formation,

as a result of megascopic boudinization, provide abundant

dilatant zones critical for the passage and deposition of

epigenetic auriferous fluids. The on-property strike length

of banded iron formation is over three miles and should be

investigated along its length.

Based on geological similarities and proximity to the Musselwhite, Snoppy Lake and Opapimiskan gold discoveries to

the south, the property merits additional exploration. A

two-phase program of I.P. surveying and diamond drilling is

warranted and recommended to better assess the potential of the Four Square property.

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FOUR SQUARE PROPERTYLAKE

, O N T A R

C^X~*,M"ATTABI

C.X*""^. j KIRKLAND " ,s LAKE*

UNITED

STATES

SAULT STE MARIE

Greenstone Belts

lOOmiies


FOUR SQUARE PROPERTYPatricia M.D., Ontario

LOCATION MAP

SCALE; l i IQOmiDATE: Auo.1987

BY: H.H./R.T.M FIG. No. 1

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2.0 INTRODUCTION

The following report describes the results of a geological exploration program, comprised of geological mapping (at a scale of l inch to 400 feet), prospecting and trenching on the Four Square property for Power Explorations Inc. The program was carried out by Geocanex Ltd. in June and July, 1987, following an earlier program of linecutting, ground magnetic and VLF-EM surveying in January and February, 1987 (Fig. No. 2).

The program was carried out from June 11 to July 3, 1987.

The following personnel were involved in the work.

P. Newman Project Geologist Windsor, OntarioC. Burk Geologist London, OntarioD. Hopkins Geological Assistant Whitby, OntarioP. Gammell Geological Assistant Calgary, AlbertaP. Latta Geological Assistant Toronto, OntarioR. McKelvey Geological Assistant Kirkland Lake, Ontario

All work was carried out on a picket line grid with baseline orientation N20 0W, and perpendicular cross lines every 400 feet.

Grab and chip samples were taken of features of potential

economic interest, including quartz veins, shear zones and

sulphide-bearing metavolcanic and metasedimentary rocks.

Several old trenches were re-exposed, mapped and sampled in

detail.

The time breakdown in man-days for the work performed is as

follows:

Mapping 28 Man-daysProspecting 21 Man-daysTotal 49 Man-days

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Metavolcanic rocks

Metasedimentary rocks

Iron formation

Gold occurrence

~- Fault zone

x \ ^—X \ \

Property Location

-*"GOLD DISCOVERY

\ SNOPPY LAKE ^ \DEPOSIT

MUSSELWHITE DEPOSITS

EXPLORAtlOMS

POOR SQUARE PROPERTY Patricia M.D., Ontario

PROPERTY LOCATION AND REGIONAL GEOLOGY

GEOCANEX LTD TORONTO. CANADA

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OPAPIMISKAN LAKE

Metavolcanic rocks

Metasedimentary rocks

Iron formation

Gold occurrence

Fault zone

Property Location

GOLD DISCOVERY

\ SNOPPY LAKE 1 \DEPOSIT

MUSSELWHITE DEPOSITS

EXPLORAtlOMS tHC.

SQUARE PROPERTY ricia M.D., Ontario

*PERTY LOCATION REGIONAL GEOLOGY



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3.0 PROPERTY DESCRIPTION

The Four Square property consists of 64 contiguous, unpatented mining claims situated between Lundmark Lake and Akow Lake (Fig. No. 3). The claims are recorded on the Ministry of Natural Resources North Caribou and Akow Lakes claim sheets (G-2147 and G-1928, respectively), Patricia Mining Division, Kenora District. The claim numbers and recording dates are shown below.

Claims Recording Dates

Pa 857635 to 857686 inclusive (54) August 27, 1985 Pa 893275 to 893284 inclusive (10) November 27, 1986

Total 64 Claims

Power Explorations Inc. of 1003-34 King Street East, Toronto,

Ontario, M5C 1E5, has the right to earn a 50% interest in the

property under the terms of a joint agreement with the

present owners, The Four Square Syndicate, consisting of H.J. Hodge, W.G. Beach, T. Jensen and J.H. Adams.

4.0 LOCATION, ACCESS AND SERVICES

The property is located in Northwestern Ontario (Lat.52*48'N, Long.90 0 20'W), approximately 100 miles north-northwest of Pickle Lake, 180 miles northeast of Red Lake and 40 miles east of the Weagamow Indian Reserve No. 87, Access to the property can be gained by float or ski-equipped aircraft from Pickle Lake, Red Lake and Weagamow Lake.

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86768 857678 857677.V — — ——'** — ——l— — -S3

576^7 857679i*!JI57686 J^ 857680 j 857675

17681 18576731657672 T85767I———r— ——

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8576j2Te57668 l 857669 j 857670**/ t W9& i V iJ t W Om,e87688 l 85766.7 857666 i 85766517666 l B!

857684 l 857.661 i 857662 l 857663i 857662 l 857663 857664— —— ——

J93275 1857660 ' 857659 857658*

857654

w^837648 l 857647 1857^42^837639——

89328018576491857646 l 857643 ifp —i——r—r T-

! I'll!.693262 693283 l 893284 l 857645 J 8S7644lJeS76

05 l mile


POUR SQUARE PROPERTYPatricia M.D., Ontario

CLAIM SKETCH

OEOCAN6X LTD TORONTO. CANADA

BY: RT. M.PATE: AUG. 87 SCALE: T* 2640' FIG. No' 3

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A winter road from Highway 808 to the Musselwhite gold property 12 miles to the south, provides winter road access to the area.

Services, supplies and manpower can be obtained from Pickle Lake. The town is a mining and transportation centre with a population of approximately 350.

5.0 TOPOGRAPHY AND VEGETATION

Outcrop is exposed over 5 to 7% of the Four Square property and is mainly confined to a large north-northwest trending ridge along the central portion of the property. Banded iron formation and mafic volcanics are very well exposed along this ridge, in contrast to felsic volcanics and sediments which are recessively weathered and poorly exposed in the low-lying eastern and western areas. Hummocky pine-covered sand and boulder ridges mantle outcrop areas, and form well-drained hills dissected by muskeg plain.

6.0 PREVIOUS WORK

The first significant work recorded on the property was in the form of a government reconnaissance mapping program by Satterly (1939) at a scale of l inch to l mile. An aeromagnetic survey (ODM-GSC, 1960) was also completed over the area at a scale of l inch to l mile.

In 1982, Cominco Ltd. carried out an overburden drilling program on an area which now encompasses the present Four Square property and the northern half of the present Akow North property, held by Moss Resources Ltd. and Power


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Explorations Inc. A 61-hole, 755 foot program was completed, on which basal till geochemistry for Au, Cu, Pb and Zn was done on samples from 53 holes. The highest gold content of till samples from the holes ranged from 24 to 86 ppb Au along the northwestern shore of Akow Lake. Base metal values were very low and indicated no subcropping base metal mineraliza tion of interest. There is no further record of work by the company.

In the second year of a three-year interdisciplinary program, Breaks et al., (1986) mapped the area at a scale of l inch to 1/2 mile. The same year, the Ministry of Northern Affairs and Mines (1986) conducted an airborne magnetic and electro magnetic survey over the North Caribou Lake belt.

The most recent work done on the property consists of a ground magnetic and VLF-EM survey conducted by Geocanex Ltd. during January and February 1987.

7.0 REGIONAL GEOLOGY AND ECONOMIC MINERALIZATION

The Four Square property is located in the north-central portion of the North Caribou-Opapimiskan-Neawagank Lakes greenstone belt. Due to the relative remoteness of the area, the belt has not been extensively worked by mining and exploration companies. Most of the available geological information on the area is from government funded geological/ geophysical surveys. The Ontario Geological Survey has recently completed a three year geological/geophysical survey of the area, manned by staff from the Precambrian Geology, Engineering and Terrain Geology, and Mineral Deposits sections.


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The belt forms part of the Sachigo Subprovince, which is composed of several small, irregularly shaped sequences of supracrustal rocks. The rocks in this subprovince are evolutionarily distinct and probably older than the rocks of the Uchi and Wabigoon Subprovinces to the south (Bartlett et al., 1985).

The belt forms an arcuate, horn-shaped assemblage of metavolcanic and metasedimentary rocks which has been synclinally folded about an axis approximately coincident with Eyapamikama Lake (Satterly, 1939). The syncline is rimmed by mafic volcanics on the north and south, and filled with trough cross-stratified, epiclastic sedimentary accumulations in the axial portion. Two fairly continuous bands of iron formation and chemical sediments mark the contact between the metavolcanics and metasediments (Bartlett et al., 1985).

Regional geological maps indicate that the belt is bounded by paragneiss and migmatized rocks in the north, and felsic intrusives in the west and south (Map 2292, Big Trout Lake - North Caribou Lake).

The entire belt extends from Weagamow Lake in the northwest, to Opapimiskan Lake in the southeast. South of Opapimiskan Lake, the belt bifurcates into two major lobes; one extending south through Libert Lake, the other through the Forester and Neawagank Lakes area.

Airborne electromagnetic and magnetic surveys (MNAM, 1986) indicate that the centre of the property contains the main magnetic trend interpreted to be the same iron formation that hosts the Musselwhite, and Snoppy Lake deposits, located twelve miles south-southeast of the property on Opapimiskan


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Lake. Here, a consortium of companies headed by Dome Mines Ltd. has outlined a combined total of 5.4 million tons of ore at an average grade of 0.20 ounces gold per ton in structu rally controlled gold-quartz-sulphide mineralization in iron formation.

In 1985, Van Horne Exploration Inc. announced a golddiscovery the same band of iron formation, on the propertyadjoining the Musselwhite to the north.

At the western end of the Weagamow-North Caribou Lakes belt, two gold showings (Agutua Arm, Teal) have been partially explored. They consist of gold-silver mineralization in sulphide-bearing quartz-carbonate veins in shear zones within mafic volcanics.

Further to the east in the McGruer Lake area, Northern Dynasty Explorations Ltd. have discovered a polymetallic Ag-Pb-Zn bearing shear zone hosted in lean iron formation.

Towards the southeastern extremity of the belt on the Neawagank Lake East property of Van Horne Gold Exploration Inc. and Power Explorations Inc., gold has been discovered in arsenopyrite-bearing quartz veins hosted in a sheared/ silicified gabbro. Numerous anomalous assays have been reported, including a value of 1.79 ounces Au per ton over 1.0 feet.

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1 O*8.0 PROPERTY GEOLOGY AND MINERALIZATION

8.1 General Geology

The Four Square property lies on the western limb of a majorsynclinal fold whose axis parallels the belt. The axialtrace of the north-northwest trending syncline lies neareastern periphery of the claim group.

the

Eight lithological units strike across the Four Squareproperty. From west to east they are:

1. tonalite

2. pillowed and massive mafic volcanics

3. intermediate to felsic flows and tuffs

4. clastic metasediments

5. oxide facies banded iron formation


7. clastic metasediments


Unit 8 is not exposed on surface but is interpreted onbasis of geophysics to lie along the eastern claim margin

thein

the southeastern corner of the property. Similarly, inter mediate to felsic flows and tuffs (Unit 3) are not exposedsurface, but are interpreted from geological mapping onAkow North property to the south (Adams and North, 1985)the Erichsen Lake property to the north (Newman, 1987).

ontheand


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The development of amphibole metacrysts in mafic volcanics, and garnet, cordierite and staurolite in aluminous metasediments, indicates that the rocks on the property are regionally metamorphosed to amphibolite facies.

Localized shearing and quartz veining have resulted in alteration in many of the rocks to assemblages containing retrograde sericite, chlorite and carbonate.

Drawing No. l (in map pocket) shows the geology and structural features as determined from this program.

8.2 Volcanics

Apart from the pillowed and massive mafic volcanic unit found in contact with the banded iron formation along the central ridge of the property, volcanic rocks are very poorly exposed on the property.

A basal mafic volcanic unit that outcrops along the western margin of the property has a minimum thickness of 2,500 feet and is composed of light green-gray weathering, fine to medium grained massive and pillowed mafic flows. Mildly deformed pillows average less than 3 feet in length, have dark green chloritic selvages and locally developed epidote infillings of selvages and more vesicular pillow tops. The 200 to 600 foot thick mafic volcanic unit in the central portion of the property is very similar and indicate a east-facing stratigraphy. Both units have a grey-green fresh surface and are composed of subequal proportions of hornblende (or actinolite) and plagioclase with subordinate amounts of chlorite and quartz.


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Intermediate to felsic volcanic rocks are not exposed on surface, but are interpreted to comprise a 1,000 foot thick assemblage of flows and tuffs. On the Akow North property to the south of the Four Square property, exposures of white to buff,banded, foliated felsic volcanics containing intercalations of mafic volcanics and greywacke are noted (Adams and North, 1985).

8.3 Sediments

Clastic sediments are exposed into two 1,500 and 2,500 foot thick units located on the western and eastern flanks, respectively, of the main outcrop ridge that extends down the central portion of the property.

Exposures at L8*OON,94-50E and L64*OOS,14*50E of knobby- weathering wackes and subordinate pelites have coarse, pink-grey porphyroblastic cordierite crystals that measure, in places, up to 6 cm long.

These crystals are ovoid, locally exhibit sinistral rotation of up to 40 e and can comprise lQ-15% of the light-brown weathering rock. In addition, euhedral staurolite porphyroblasts, apparently unrotated, are found disseminated throughout the quartz-feldspar-biotite groundmass.

Small intercalations of garnet-biotite schist were noted in contact with banded iron formation at various locations on the property. One exposure at 63*20N,2*10W displays sub-5 mm euhedral garnet porphyroblasts in a fine-grained biotite* quartz+feldspar matrix.


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Banded iron formation is very well exposed on the outcrop ridge along the centre of the property and is typically composed of 1/2 to one inch thick buff-to-white weathering chert laminae intercalated with 1/4 inch thick, grey to brown weathering magnetite+grunerite laminae. In general, the iron formation is leaner towards the eastern margin of the unit. The prominent aeromagnetic anomaly associated with this unit exhibits a pinch-and'-swell shape, attributable to large-scale boudinization. Rocks in neck zones of lower magnetic intensity have undergone conversion of magnetite into grunerite to a greater degree than rocks associated with adjacent magnetic highs (Breaks et al., 1986).

8.4 Intrusives

Clear to milky white, concordant quartz veins constitute the bulk of intrusive rocks on the property and are generally less than 12" wide, contain trace sulphides and occasionally, carbonate. Tourmaline was noted in a number of discordant quartz veins in mafic flows at 63+4013,0+651^.

Two forty foot wide concordant mafic dykes intrude pelitic and clastic sediments at L60+OOS,13+OOE. These are typically medium-grained gabbroic intrusives composed predominantly of pyroxene and feldspar with minor quartz and are very weakly magnetic.

A twelve inch wide lamprophyre dyke concordantly intrudes banded iron formation at L24+OQIH, 0+50E. The light brown-weathering dyke is composed of fine-grained biotite and quartz and hosts small lenses and stringers of calcite.


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An outcrop at L56+OOS,54+OOW exposes massive, medium-grained tonalite of the North Caribou Lake Batholith that is light grey on weathered surface, dark grey on fresh surface and composed of subequal proportions of quartz and plagioclase with 15 to 2(U biotite.

8.5 Structure

The rocks on the property strike north-northwest at approx imately 325* and generally dip steeply west from 75* to 85*.

Geological mapping during the present program and by Breaks et al. (1986), suggests that the property straddles a synclinal fold axis which strikes 325*. The axial plane of the fold dips steeply west and plunges south. Drag-fold axes in banded iron formation plunge 45* to 70* south.

On the basis of truncations in magnetic signature, a large east-west trending, 300 foot dextral offset is interpreted to lie at L16+OON, base line 0. It is not certain whether or not the VLF-EM response supports this interpretation. The location of the offset coincides with the point where the magnetic signature of the banded iron formation is at its thinnest, due to megascopic boudinization of the unit. The effect of this large-scale deformation is manifested in differing tectonic styles observed in the banded iron formation. Outcrops near the necking point of these mega scopic boudins are dominated by abundant small-scale boudinage whereas outcrops in the "centre" of the boudin tend to show intense folding and dextral shearing.

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Macroscopic closed to open Z-folds in banded iron formation have an axial plane striking at 300* to 310* and dipping steeply southwest at 70* to 85*. A moderately developed superimposed crenulation cleavage observed in grunerite-rich bands strikes at approximately 300* and dips 45* south-west. A locally developed axial planar fracture cleavage is present in folds of the first phase and, in places, hosts small quartz-pyrrhotite veinlets similar to those found at the Musselwhite and Snoppy Lake deposits.

Zones of shearing are observed on difference scales in all lithologies, but are best developed in the brittle banded iron formation unit. Sub-1 inch concordant limonitic shear zones are commonly observed. In addition, dextral shearing along axial planar fracture cleavages exhibit displacements up to 8 inches. The widest zone of shearing, however, is a concordant brittle deformation zone up to 12 feet wide located at 63+50N,2+15W. Angular clasts of chert up to 6 inches long are preferentially oriented parallel to the strike of the zone in a chert matrix.

8.6 Geophysical Summary

Results of the VLF-EM and magnetic survey indicate that the Four Square property hosts a unit of banded iron formation that thickens in the north and south and thins, presumably as a result of megascopic boudinization, in the central portion of the property. The magnetic signature is very high along this unit, reaching amplitudes of 84,000 gammas. Filtered inphase VLF-EM contours associated with the unit are simi larly high, reaching +203I in places.

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Numerous north-northwest trending VLF-EM conductors occur concordantly to subconcordantly to the stratigraphy and may represent unexposed sulphide facies iron formation, graphitic and/or sulphide-bearing volcanics and sediments, or sulphide- bearing concordant shear zones (Medd, 1987). Two cross cutting west-northwest trending faults/shears and one subconcordant, north-northwest trending fault/shear are interpreted on the basis of magnetic and VLF-EM discontinu ities. Two areas of small scale, tight folding within iron formation are interpreted on the basis of magnetic and VLF-EM data. The locations for these are?

L96+OON to L52+OON; 2+OOE to 10+OOW

L16+OOS to L52+OOS; 6+OOE to 2+OOW

8.7 Economic Mineralization

Rock sampling and prospecting were focussed along the wide band of iron formation trending north-northwest through the centre of the property. Six old trenches were re-exposed, mapped and sampled. A brief description of each trench and associated mineralization follows. Trenches FS-1 to FS-4 are located in stripped Area A {Fig. No. 4), while trenches FS-5 and FS-6 are located further south.

8.7.1 Trench FS-1

Located along the northern claim margin of the Four Square property at L96+OON,6+OOW, Trench FS-1 exposes weakly gossaned oxide facies banded iron formation containing up to D.5% disseminated pyrrhotite (Fig. No. 5), Fourteen grab samples from the mildly deformed area yielded low gold values, the highest of which analyzed 60 pb.

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— 4W

8W

Open muskeg with small iackpine

12443- *5 —-^T-T /*

Shallow sand 8 boulders s

4W —

IOO ZOO

FEET

FS-1

Oxide facies Banded Iron formation

Garnet - Chlorite schist

Hornblende schist

Trenches: see detailed maps

I245O-5

—2OOO—

Grab sample: No-Auppb

Magnetometer contour-gamma

VLF-EM conductor

For symbols See grid geology map


FOUR SQUARE PROPERTYOpapimiskan Lake Area

Ontario

STRIPPED AREA 'A'


BY:P.S.N.XR.T.M.DATE: SEPT. 87 SCALE: l "sIOO' FIG. No. 4

1 fl l l l

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96N

12464-35

12393-4512394-1512395-1012396-2512397-10

12463 - 60 12440- 20 12441 -25

Pa 857678

Immature jackpine, sprue* ond poplar

12460-20

"•s

12462-30

•12442-40• 96N

FEET

Oxide faciesBanded Iron formation

Trench


For symbols See grid geology mop



Ontario

TRENCH FS-1 DETAIL

OEOCANEX LTD TORONTO. CANADA

J! l"t.RG^JoTS

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8.7.2 Trenches FS-2 and FS-3

Trench FS-2 straddles the contact between moderately deformed banded iron formation and garnetiferous hornblende schist at 94*OON,5H-15W (Fig. No. 6).

The contact is marked by the occurrence of sub- l inch con cordant pyrrhotite and pyrite veinlets. Trench FS-3 exposes weakly gossaned banded iron formation in the same outcrop at 934-90N,5*40W. Deformation exhibited in the iron formation becomes more intense towards the western edge of the outcrop where shearing and Z-folding are abundant.

Out of 21 samples taken over the area, nine analyzed 50 ppb Au or better. Values ranging from 50 to 190 ppb Au were obtained from samples in the vicinity of Trench FS-2, most being directly at the contact or within proximal banded iron formation. Samples from Trench FS-3 failed to yield anomal ous gold values. The highest gold values from the outcrop area, however, were taken from and dilated, limonitic, axial planar fracture cleavage in the deformed iron formation. Two samples taken from the' same location assayed 350 and 240 ppb Au.

8.7.3 Trench FS-4

Trench FS-4 located at 85+OON,3+25W, straddles the same contact between banded iron formation and hornblende schist as found in Trench FS-2 (Fig. No. 7). Out of eight samples taken for assay, two anomalous gold values 50 and 70 ppb were derived from samples taken at, and slightly below, the con tact in the banded iron formation. Again, the contact is marked by the occurrence of small pyrite and pyrrhotite veins. In addition, a sample taken from a small gossan zone located 17 feet to the west of the contact analyzed 50 ppb Au.

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^ Q A M

wC

77401-10 77402- 95

12445-350 12451-240

*84

N —

77401-10

Oxide faciesBonded Iron formation

Garnet - Chlorite tchlit

Hornblende schist

Trench

Grab sample: No-Au ppb




OntarioTRENCHES FS-2 ft FS-3

DETAIL


BY! P.S.N.DATE! SEPT. 87

FIG. No. 6

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wf.

9

12471 -10-v t l2472-l5-\\\

12473- 50 -x\\\ 12474- 70 "x"\VA^ FS -4

12475-50-^ ^^SS^3

85N -j —— ; —— ,....-'V ———

•~...*f~../ ^ .12476-10 —— \ i \

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s o*^ • ***frt*

' V'*'

\-l2456-25

a ̂ LJ

0 20 40

FEET

1

i

. Oxide facie* l Bonded Iron formation

2 G arnet - Chlorite ichltt

3 Hornblende *chlit

(^JYnV Trench'L

12471 -10 Orflb lomple . No .Au ppb

Tor tymboli See qrldjêletiMftop

[l/M^GE g J

\^^xll^//\^1o:(O^X


FOUR SQUARE PROPERTY Opapimiskan Lake Area

Ontario

TRENCH FS-4 DETAIL

-tfftf BY:C.f?B,XR.T,M,Ifi^fj DATE: 5E.PT 87

SJ?^ QEOCANEX LTD 86ALE:|"iô!.,' ^ TORONTO. CANADA FIG. No. 7 ^™


- 24 -

8.7.4 Trench FS-5

Trench FS-5 is located at 75+50N,4+60W and exposes a magnetite-rich gossanous section of banded iron formation hosting up to J.0% sub- 1/4 inch ankerite veinlets and 11 pyrite (Fig. No. 8). One anomalous gold value (80 ppb) was found out of ten samples taken.

8.7.5 Trench FS-6

Trench FS-6 exposes a pervasively carbonatized section of gossanous banded iron formation at 47*15N,(H40W (Fig. No. 9) values of 40 and 35 ppb Au were derived from a concordant shear zone cutting across the trench and a fractured, pyrrhotite and arsenopyrite-rich (5% combined) section of iron formation, respectively.

8.7.6 Stripped Area B

A large outcrop area at 29+OON, base line zero exposes the thickest continuous section of banded iron formation stratigraphy found on the property (Fig. No. 10). In addition to taking samples of quartz veins, gossan and shear zones, character samples of banded iron formation were analyzed to assess any changes in background gold value. Although no systematic change in background values was detected, a number of anomalous values were encountered. A small gossan zone, a concordant shear zone and a character sample of mafic tuffs analyzed 158, 45 and 55 ppb Au, respectively.

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- 25 -

75*50N

**wOf.

Open muskeg

77418-35- 77419-10

77420-5/t

FS-5

77417-10 77416-20 77415-5 77414 -^ 77413 -80 77412 -5-

77412-5

Oxide faciesBanded Iron formation

Trench


For symbol* Set grid geology map

Sand ft boulders

75* SON —

77421 - 10



l Ontario

TRENCH FS-5 DETAIL


DATE! SIie,SCALE: l"*2FIG. No. B


48 N

— 47N

- 26 -T"Pro

Poplar, alders, spruce muskeg

12497-10

12498-40

12489-15 12490-10

12438 ^5 12491-5

12492-10 12493-10

12496- 10

20 40

FEET

Oxide facies iron formation

Trench


for symbols See grid geology mop



••'M:- Ontario!^'

TRENCH FS-6 DETAIL


DATE: SttSCALE; l " *#y ILJlo^S___

w ro

- 27 -

ro9

— B .LOO

-- 12380-5*

*——12381-5 .J

Oxid* facie*Bonded Iron formation

Massive basalt

Massive tuffs


—2OOOO- Magnetometer contour-gamma




Ontario

STRIPPED AREA 'B*

OEOCANEX LTDTOBOMTO. CANADA

SCALE: |"a4O'FIG. No. l O


- 28 -

8.7.7 General Discussion

Two large outcrop exposures of banded iron formation yielded a number of anomalous gold values. These are discussed further.

The first, located at 77+OON/4+OOW, exposes a wide section of moderately-deformed, heavily-gossaned banded iron formation. Along with anomalous gold values of 225, 175, 140 and 100 ppb taken from gossan zones, the highest value on the property (790 ppb) was obtained in a gossan zone oriented parallel to an axial planar fracture cleavage in a well- folded area. A small outcrop located just north of this area exposes a highly brecciated zone of magnetite and grunerite- rich iron formation that assayed 165 ppb.

The second large outcrop area is located at 63+0013,2+001*7 and straddles the contact between moderately-deformed banded iron formation and overlying pillowed and massive mafic flows. The contact itself is highly sheared and hosts a 6 inch wide, smokey, arsenopyrite-bearing quartz vein which assayed 215 ppb. Stratigraphically overlying this, below the mafic unit, is a 6 foot wide band of garnet-biotite schist that analyzed 100 ppb Au. Other anomalous values of 235, 160 70 ppb Au were from gossan zone samples within banded iron formation close to the sheared contact.

The only anomalous gold values encountered during the present program that were not derived from banded iron formation were from a gossan zone in wackes (100 ppb), a quartz- tourmaline vein and a shear zone in basalts (235 and 170 ppb Au, respectively).


- 29 -

9.0 CONCLUSIONS

The property is underlain by a north-northwest trending sequence of mafic to felsic volcanics, clastic sediments and iron formation which has been synclinally-folded about an axis which strikes north-northwest - south-southeast and plunges steeply south. One thick, continuous band of iron formation flanks the fold axis on its west side.

Numerous anomalous gold values, ranging up to 790 ppb, were found in moderately deformed, highly gossaned banded iron formation at a number of locations on the property.

In light of the association of significant gold mineraliza tion with iron formation on the Musselwhite, Snoppy Lake and Van Horne properties on strike to the south, the Four Square property has good potential for economic gold deposits.

10.0 RECOMMENDATIONS

A two phase exploration progam is recommended.

10.1 Phase I

Should consist of I. P. surveying to better define drill targets.

10.2 Phase II

This should consist of diamond drilling of selected geophysical/geochemical targets. The location of drill holes will be contingent upon the results of Phase I. It is estimated that a minimum of 3,000 feet will be required.

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- 30 -

11.0 ESTIMATED COST OF RECOMMENDED EXPLORATION PROGRAM

11.1 Phase I

B I.P. Survey, 12 days at $l,500/day•————————$ 18,000.00

l Contingency 20%————————————————————————? 3,600.00

H Total Cost of Phase I ——————————————————— ? 21,600.00

l n' 2 Phase II

Diamond Drilling - 3,000 feet at l ?357foot all inclusive——————————————————$105,000.00

m Contingency 20%————————————————————————? 21,000.00

Total Cost of Phase II-——————————————————$126,000.00

B Total Cost of Phase I and Phase II ————————— ?147,600.00

lB Respectfully submitted,

l— . Paul S. Newman, B.Se. l Geocanex Ltd.

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- 31 -

.0 REFERENCES

Adams, J.H. and North, J.W., 1985. Report on Geological Mapping, Prospecting and Trenching, Akow Lake - North Property, District of Kenora, Patricia Mining Division, Northwestern Ontario, Moss Resources Ltd. for 635479 Ontario Ltd.; unpublished report of Geocanex Ltd.

Bartlett, J.R., Breaks, F.W., DeKemp, E.A. and Shields, H.N.,1985. Precambrian Geology of the Eyapamikama Lake Area (Opapimiskan Lake Project), District of Kenora (Patricia Portion); Ontario Geological Survey, Map P.2834, Geological Series - Preliminary Map.

Breaks, F.W., Bartlett, J.R., DeKemp, E.A. and Osmani, I.A.,1986. Precambrian Geology of the Doubtful-Akow Lakes Area (Opapimiskan Lake Project), Kenora District (Patricia Portion); Ontario Geological Survey, Map P.2965, Geological Series - Preliminary Map.

Medd, S.B., 1987. Report on Magnetic and VLF-EM Surveys, 4-Square Akow Lake Property; Private Report, Explora-Five Limited Partnerships.

Ministry of Natural Resources, 1983. Map 2292? Big Trout Lake - North Caribou Lake, Geological Compilation Series, l inch to 4 miles.

Ministry of Northern Affairs and Mines, 1986. Opapimiskan Lake Area, Airborne Electromagnetic Survey, Total Intensity Magnetic Survey, District of Kenora, Patricia Portion.

Newman, P.S., 1987. Report on Geological Mapping and Prospecting, Erichsen Lake Property, District of Kenora, Patricia Mining Division, Northwestern Ontario. Private Report, Moss Resources Ltd. and Power Explorations Inc.

Ontario Department of Mines - Geological Survey of Canada, 1960. Map 919G; North Caribou Lake, l inch to l mile.

Ontario Geological Survey, Resident Geologist Files - Toronto and Sioux Lookout. Various unpublished assessment reports.

Satterly, J., 1939. Geology of the Windigo - North Caribou Lakes Area; O.D.M., Vol. 48, Part 9, pp.1-32.

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APPENDIX A


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THIS IS TO CERTIFY THAT:

I have been a resident of Windsor, Ontario since 1967.

I am a consulting geologist employed by Geocanex Ltd.

I have worked as an exploration geologist since 1985. I have worked intermittently in gold exploration in Northwestern Ontario since 1985.

l am a graduate of the University of Windsor with a Bachelor of Science (Honours) degree in geology.

I supervised geological mapping and geochemical sampling programs on the Four Square property from June 11 to July 3, 1987.

My report is based on a personal examination of the property in 1987, and upon a diligent search and review of all available pertinent technical data published by the Ontario Ministry of Natural Resources, and in the Assessment Records Libraries in Sioux Lookout and Toronto; as well as private company reports.

In this report, I have disclosed all relevant material, descriptive and interpretive, which is to the best of my knowledge, necessary to gain a complete understanding of the viability of the project and the recommendations.

DATED THIS 22*^ DAY OF

Paul S. Newman, B.Se. Geologist

APPENDIX B

TECHNICAL DATA STATEMENT

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Ministry ofNorthern Developmentand Mines

Geophysical-Geologlcal-Geochemical Technical Data Statement

File.

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

T f o , . GeologicalType of Survey(s) _____I.—————————^————————.Township or Area North Caribou Lake St Akow Lakeî - u ij i \ Power Explorations Inc.Claim Holder(s)_________l___________________

Surveyrnmpany Geocanex Ltd.——-^-———————Author of Report Paul S. Newman.————————————Address of Aiithnr 734 Wallace Ave., Windsor, Ont. Covering Dates of Survey June 11 to July 3, 1987

(linecutting to office)47.8 MilesTotal Miles of Line Cut.

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.

Geophysical—Electromagnetic.—Magnetometer-.—Radiometric———Other^—————

DAYS per claim

GeologicalGeochemical.

AIRBORNE CREDITS (Special provision credits do not apply to airborne turveyi)

Magnetometer. .Electromagnetic(enter days per claim)

SIGNATUReport or Agent

Res. Geo I.. .Qualifications,Previous Surveys

File No. Type DateU

Claim Holder

MINING CLAIMS TRAVERSED List numerically

.. (prefix) (number)

TOTAL CLAIMS g 4

837 (85/12)

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A SELF POTENTIALInstrument————————————————————————————————————— Range. Survey Method ——————————————————————————————————————————

Corrections made.

RADIOMETRIC

Instrument.——.Values measured.Energy windows (levels),——.—-—.—^-———^---.—-—.—-.-———.———---—-——. Height of instrument—,—-—-—.-————.—-.—-—.—^—--Background Count. Size of detector_________________________________________Overburden ——————————————.-—..———..^-^.—.———-..———™.^————..-—

(type, depth - include outcrop map)

OTHERS (SEISMIC, DRILL WELL LOGGING ETC.) Type of i Instrument. Accuracy.—Parameters measured.

Additional information (for understanding results).

AIRBORNE SURVEYS Type of survey(s) ——— Instrument(s) —————

(specify for each type of survey) Accuracy———————————^™

(specify for each type of survey) Airrraft used.

Sensor altitude.Navigation and flight path recovery method.

Aircraft altitude.————.—.———..——.—.——.——.——.^——— LineMiles flown over total area———-————-———^--——..™—-.—Over claims only.

GEOCHEMICAL SURVEY - PROCEDURE RECORD ^

Numbers of claims from which samples taken Pa 857638, 857639, 857645, 857655, 857658 f857659, 857662, 857663, 857666857679, 857680, 893284, 893283

T"tal Nnm*""- "f Sample 2 3 !Type nr sampie Rock

(Nature of Material)A verage Sample weight 2 kgMethod of Collection Grab and Chip

Soil Hnrjrnn Sampled

Horizon DevelopmentSample Depth

Terrain

Prainagf Development T

Estimated R^ng*- nf OverhiirH^n Thirkncss., ,

SAMPLE PREPARATION(Indudes drying, screening, crushing, ashing)

M*"*b w,* of fr^f-tion iis^rl for analysis .

-200 mesh on 10 gr weight

r,fnfra\

, 8 57669, 857670, 857673, 857675, 857678,

——— ANALYTICAL METHODS—— ' Values expressed in: per cent D

p. p. m. Qp. p. b. 123

Cu, Pb, Zn, Ni, Co, Ag, Mo, As.-(circle)

Oth™ Au

Field Analysis ( tests)

Extraction MrtbnA .

Analytiral Mftthnrf

Rragrnte Used

Field Laboratory AnalysisNo { tests)

Extraction Method

,, , . Analytical Method

Reagents Used

Commercial Laboratory ( tests)Nam,nfT.aKnM,™.y Bondar Clegg s Co. LtdV.vtrartion MethoH AqU3 Regia

AnalytJral MetK^H FA~AA

Reagents TIseH - ll .ll . ....

General ————————————————————————

1 1

1

1

1 1

1 1

1

1

1 1

1

1

1 1

1

1 1

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Pa 857635857636857637857638857639857640857641857642857643857644857645857646857647857648857649857650857651857652857653857654857655857656857657857658857659857660857661857662857663857664857665857666857667857668857669857670857671857672857673857674857675857676857677



MINING CLAIMS

Pa 857678857679857680857681857682857683857684857685857686857687857688

Pa 893275893276893277893278893279893280893281893282893283893284

Total 64 Claims

APPENDIX C

ROCK SAMPLE DESCRIPTIONS

111111111I111111111

*Sample No.

12326

12327

12328

12329

12330

12331

12332

12333

12334

12335

12336

12337

12338

12339

Type

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

FOUR SQUARE

Location

BLO,344-75N

1+40E.29-I-40N

4+50E.32+50N

3400E,24*50N

3+50E,24+70N

3+05E.24+OON

04-40E.24+10N

0+50E.24+OON

0+30W.47+30N

4-fOOE,47*OON

3+80E.50+20N

3*90E,504-30N

0+40E.53+80N

5*20E,54*80N

SAMPLE DESCRIPTIONS

Description j

Gossan zone, 3-5", concordant, veryminor cc stringers, traceable for6', tr.-0.55K asp.(?)

Quartz vein, 12" wide avg. , irregular, concord., white, sugary, abundantlim. , no visible sulphides

Quartz vein, 12" x 24", deformed,clear, minor concord, qtz-cc stringers,lim. , tr. py. 6 asp.

Quartz vein, chert (?) , clear,concordant, 1/8 py. Si asp.

Quartz vein, Z- folded, lim. , novisible sulphides, no cc.

Chert horizon, 12", concordant, minorlim. , no visible sulphides

Gossan zone, in wackes, 4" x 5', novisible sulphides, no cc.

Lamprophyre dike, 12" x 30', minor cc stringers, ^ dissem. pyrrhotite.

Gossan zone, in BIF at old trench,lean BIF, concordant, euhedral asp.(1/0 and tr.-O^ pyrrhotite instringers and disseminated.

Gossan zone, in pillowed flow, 15" x20', tr. diss. po. d asp., tr. cc.

Quartz vein, in pillowed flow, irreg ular - generally concord., 12", minorlim. , no visible sulphides

Gossan zone, in basalt flows, 2* x 4 1 ,concord., abundant lim., tr. asp.

Gossan zone, in BIF, 3' x 25', minordeformation, concord., abundant lim.,no visible sulphides

Gossan zone, in basalts, 2* wide,concord. , no visible sulphides

Au ppb

35

105

100

45

20

10

10

1 111111111111111111

*Sample No.

12340

12341

12342

12343

12344

12345

12346

12347

12348

12349

12350

12351

12352

12353

12354

Type

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

FOUR SQUARE

Location

2+25E.55+80N

2+20W.59+60N

2+20W.59+40N

1+10E.58+10N

1+20E.58+60N

2+OOE.59+70N

2+60W.63+10N

2+1 OW, 65+1 ON

2+60W.65+10N

3+OOW.68+40N

2+80W.68+50N

3+20E.64+40N

4+80W,75+60N

S+IOW^+OON

6+20E,20+60N

SAMPLE DESCRIPTIONS

Description

Felsic dike, 7' x 40', qtz. porphy ritic, tr. cpy., tr.-0.5% py,contains small irreg. q.v.'s.

Gossan zone in BIF, abundant lim., concordant

As above

Quartz vein, 18", irreg., discontin uous, milky, minor lim., no cc, novisible sulphides

As above, 12" x 6'

Gossan zone in basalts, 3' x 50',concordant, minor chert inter calations, no visible sulphides

Gossan zone in BIF, 12" x 36",concordant, no visible sulphides

Gossan zone in BIF, 16" x 15', asabove

As above, 4' x 15'

Tectonic Breccia in BIF, .10' wide,minor lim. , no visible sulphides

Gossan zone in BIF, 3' x 40',concord., no visible sulphides

Felsic dike in basalt flows, 2.5'wide, abundant limonite

Gossan zone in BIF, small carbonateveinlets ptygmatically foldedthroughout, no visible sulphides

Gossan zone in BIF, highly deformedarea, 5* x 40', parallel to axial planar fracture cleavage

Quartz vein, 12" in metaseds., milky,discordant, no cc, no visible sulphs.

Au ppb

O

O

5

O

o10

10

5

*15

10

10

^

225

10

1111111111111I11111

W FOUR SQUAI

Sample No. Type Location

12355 Grab 0+70W, 8+OON

12356 Grab 0+60W, 7+OON

12357 Grab 0+30W, 6+20N

12358 Grab 0+30E, 3+60N

12359 Grab 0+00 3+80N

12360 Grab 0+50E, 2+80N

12361 Grab 0+85E, 1+15N

12362 Grab 8+40E, 4+10N

12363 Grab 7+30E, 5+15N

12364 Grab 3+40E, 1+90S

12365 Grab 3+20E, 3+OOS

12366 Grab 1+OOE, 7+50S

12367 Grab 0+00 3+80E

12368 Grab 4+OOE.12+OOS

12369 Grab 6+30E.28+80S

Description

Gossan zone in BIF, 1' x 4', concordant, no visible sulphides, no cc.

Gossan zone in BIF, Z- folded, 6" x 15', generally concordant, no visible sulphides

As per #12355

Gossan zone in BIF, near contact with basalts

Shear zone in BIF, 3' wide, concordant, lim. , very fissile

As per #12358, 2' x 6'

Gossan zone in BIF - near contact with basalts

Quartz vein, 8" - in wackes, milky, deformed (s-folded) , generally concordant

Quartz vein, 6", hosted in wackes, milky, deformed

Felsic tuffaceous horizon in pillows, 3* wide - bifurcates into two horizons - possibly a dike, tr. asp.

Quartz vein, 16", milky, irregular - generally concordant

Quartz- Feldspar Porphyry Dike, 14", concordant, minor lim., tr.-O^ disseminated asp.

Gossan zone in basalts, 12" x 3', concordant

Quartz vein, 3", hosted in basalts, concordant, no visible sulphides

Intermediate Dike(?), 8' x 60' exposed, lim. , slightly discordant

Au ppb

10

5

10

75

1 111111111111111111

W FOUR SQUARE SAMPLE DESCRIPTIONS

Sample No.

12370

12371

12372

12373

12374

12375

12376

12377

12378

12379

12380

12381

12382

12383

12384

12385

12386

Type

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Location

S+OOEê+OOS

5+70E.23+90S

9+20E.21+OON

9+90E, 9+OON

H47E,28-f88N

1+36E.28+88N

1+25E.28+88N

1+11E.28+88N

04-93E,28*88N

0*80E,29-H39N

0+62E.29+09N

0+49E.29+34N

0+27E.29+49N

0+06E.29+45N

BLOO 28+50N

0+10E.28+55N

1+19E.30+48N

Description

Quartz vein, 10", milky, deformed,hosted in pillows, minor lim.

Shear zone in basalts, 2", discordant,lim.

Quartz vein in wackes, 8", clear tomilky, irregular - generally discor dant, no cc, no visible sulphides

Quartz-albite vein in wackes, 5" x 20'milky, concordant, no cc, no visiblesulphides

Character sample of BIF - Stripped Area A

As above, including a 3" gossan zone



Character sample of BIF

As above, very mt.-rich

As above, very mt.-rich

As above, incl. a 10" gossan zone

As above, incl. a small gossanousshear zone


Shear zone in mt.-rich BIF, concord.,abundant lim. , includes a 1" milkyq.v. , no cc, no visible sulphides,fissile

Gossan zone in in termed, to felsictuffs, concordant, lira., tr.-0.5%diss. po., tr. asp.

Quartz-Pyrrhotite veinlet in BIF,1/4", discordant at 25 0 to bedding,clear, deformed

Au ppb

0

170

20

, 5

10

O

10

5

O

O

5

5

5

15

45

25

O

1 1 11I11111111111111

9Sample No

12387

12388

12389

12390

12391

12392

12393

12394

12395

12396

12397

12398

12399

12400

77401

77402

77403

. Type

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

FOUR SQUARE

Location

0+09E,28+64N

0+30E.27+15N

0+25E.27+15N

1+56E.29+61N

0+24W.19+04N

29+06W, 0+46W

96+09N, 5+85W

96+08N, 5+8 7W

96+07N, 5+89W

96+06N, 5+91 W

96+05N, 5+9 3W

96+04N, 5+9 5W

94+0 3N, 5+1 8W

94+30N, 5+0 4W

94+30N, 5+1 3W

94+29N, 5+1 7W

93+98N, 5+3 2W

SAMPLE DESCRIPTIONS

Description Au ppb


Gossan zone in BIF, concord., 1.5' x5', fissile, abundant lim.

Quartz-Tourmaline vein in BIF, 12"max. x 5', boudinaged, concord.,milky, minor chl. inclusions

Gossan zone in deformed BIF, 1' x 3',concordant, no cc, no visiblesulphides

Character sample of mafic tuffs,chloritic, well foliated, tr. sulphides

Gossan zone in BIF, very weathered,fissile, tr. py.(?)

Trench FS-1 - through BIF, vfg. tr.-Q.5% pyrrhotite

As above, heading W

As above, heading W, abundant limonite

As above, heading W, abundant limonite

As above, heading W, abundant limonite,tr. cc.

As above, heading W, abundant limonite,tr. cc.

Trench FS-2, Sample of BIF containingup to 1" stringers of po., tr. asp.,tr. cpy. Near contact with hbl. schist5% po.

Character sample of hbl. schist, Q.5%diss. po., cc.

As above

Weathered contact zone between BIF andhbl. schist, 5 7, po. in stringers andblebs

Character sample of BIF, vfg. tr.-Q.57,pyrrhotite

20

35

15

10

55

15

5

15

10

25

10

35

120

20

10

95

40

1 111111111111111111


Sample No.

12426

12427

12428

12429

12430

12431

12432

12433

12434

12435

12436

12437

12438

12439

32440

32441

Type

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Location

BLO , 35N

BL0.32+80N

32+OON.50E

31+80N.50E

31+80N.65E

31+50N.30E

31+15N.60E

30+80N.60E

30+70N.40E

30+20N,50E

28+80N, 1+OOE

29+10N.90E

47+30N, 0+30W

44+80N, 4+OOE

96N, 5+50W

96N, 5+50W

Description

Glassy quartz (chert?) . Thick bou-dinaged horizon in BIF. Extensivelimonite infilling of fractures.

Gossan in BIF concordant to bedding,± 2' wide



Gossan in BIF. Dense fracturing con cordant to bedding, ± 2 ' wide

Gossan in BIF. Dense fracturing con cordant to bedding, ± 2' wide

Gossan in BIF, disseminated magnetitet 1 ' wide

Gossan in BIF, ± 1 ' wide

Gossan in BIF, disseminated magnetite

Gossan in BIF, disseminated magnetite

Gossan in BIF, ± 2' wide

Gossan in BIF, ± 2' wide

Gossan in BIF. Found in an approx.15 year old trench (py, arsenopyrite)± 3' wide

Medium grained gossan zone in basalticflow, ± 2 ' wide

Oxide Facies BIF, gossan zone thereinbrown to black limonite staining. 5%euhedral magnetite. Gossan concordantto bedding.

Fractured (carbonate-quartz filled)gossan zone in BIF. Small veinlets ofquartz form ptygmatic folds. Tracepyrrhotite, arsenopyrite.

Au ppb

O

10

15

^

10

O

10

5

20

158

10

0

O

5-

20

25

1111111111111111111


Sample No.

12442

12443

12444

12445

12446

12447

12448

12449

12450

12451

12452

Type

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Location

96N, 5+50W

92N, 6+50W

92N, 5+2 5 W

92N, 5+7 5W

92N, 5+OOW

92N, 5+OOW

88N, 5+OOW

88N, 5+OOW

88N, 5+OOW

92N, 5+2 5W

92N, 5+25W

Description

Small gossan zone, brown to blacklimonite staining, 70% quartz, 30%magnetite.

Gossan zone, 60% quartz, 20% grun. ,2Q7, mt., fine grained

In a shallow trench (± 1 ' deep) 80% qtz., 155K iat.,^% grun., gossan inBIF

Gossan in BIF, quartz 60%, mt. 205S,grun. 20%. Found in axial fold hingefracturing which was dilated.

Quartz-magnetite-hornblende schist,carbonatized, hbl. 50%, qtz. 25%,mt. 10/S, calcite (or ankerite) ± 5%,pyrrhotite, arsenopyrite, chalcopyrite- 5%, contains saccharoidal qtz.stringers.

Quartz stringer in qtz, mt, hbl.schist, saccharoidal qtz., minorsulphides .

Garnet-biotite-schist, concordant toBIF, very fine matrix of foliatedbiotite with garnet as 5 to 10 mmporphyroblasts; garnet ± 20%

Gossan zone in BIF. Extensiveweathering to talc. Foliated withmicaceous mineral concordant withbedding.

Smokey quartz contains ± 25% albite,deformed in a z-fold.

Re-sampled dilated axial planar clea vage; qtz. 60%, mt. 20%, grun. 20%,similar sample as 12445

Boulder sampled very similar descrip tion to 12445 and 12451 but smallerscale. Boulder part of outcrop at92N, 5+25W.

Au ppb

40

-C5

350

10

10

10

240

15

1111111111111111111

™ FOUR SQUARE SAMPLE DESCRIPTIONS

Sample No.

12453

12454

12455

12456

12457

12458

12459

12460

12461

Type

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Location

88N, 5+OOW

88N, 5+OOW

88N, 5+OOW

84N, 3+OOW

84N, 3+OOW

72S, 9+OOW

72S, 7+50W

96N, 5+50W

96N, 5+50W

Description j

Gossan staining in BIF, quartz 60%mt. ± 10/5, grun. 20/2, weatheredproducts of grun. 10/L Extensivelydeformed. No bedding preserved.

Small gossan. Intercalated peliticseds. and BIF. qtz. 50%, grun. 30%,pelites 20%.

Very lean BIF, qtz. 75%, grun. 207,,mt. 5%, bedding obliterated by exten sive deformation. Minor amounts ofdisseminated sulphides.

Boudin rich in qtz. hbl. , grun, bio.,all medium grained, concordant folia tion to boudin shape.

Trench blast rock. Fine grained qtz.-hbl. schist. Foliation 310/vertical.Qtz. as saccharoidal stringers. Tr.arseno. , chalco, pyrrhotite, very finegrained stringers. Carbonatized.Locallized med. grained sulph.

Clear quartz in QV. Moderately frac tured in deformation of vein. Moderatelimonitic staining. 2" wide in apelitic metasedimentary unit.

Finely fractured quartz in a one cmwide deformed QV. QV contains tour maline. QV Z- folded.

6' interval in BIF. Qtz. 50/2, mt. 407., grunerite ± 1 0%. Qtz. exemplifiesextensive brecciation of BIF bedding,small scale Z-folding. Locallizedlimonitic staining.

6' interval in BIF. Qtz. 80/2, mt. 1052,grun. .10/2 . Very chert-rich BIF.Chert-rich beds are boudinaged andlocally brecciated. Small mt-grun-rich pods in chert as well.

Au ppb

140

20

10

25

35

15

10

20

40

1111111111111111111

™ FOUR SQUARE SAMPLE DESCRIPTIONS

Sample No.

12462

12463

12464

12465

12466

12467

12468

12469

12470

Type

Grab

Grab

Grab

Chip

Chip

Chip

Chip

Chip

Grab

Location

96N, 5+50W

96N, 5+50W

96N, 5+50W

94N, 5+1 5WFS- 2

94N, 5+1 7WFS- 2

94N, 5+2 OWFS-2

94N, 5+2 2WFS-2

94N, 5+2 4WFS-2

94N, 5+20W

Description

Qtz. 50/2, mt. 30/2, grun. 205?,thinly laminated chert/mt. Chertshows up as brecciated boudins.Extensive limonitic staining.

Qtz. 70%, mt. 30/2. Finely laminatedchert-mt. BIF - immediately south ofTrench FS- 1 .

Gossan Zone in BIF. Qtz. 70%, mt.2552, grun. ± 5/L Zone exhibitssluffing of bands approx. 5" thickthat break off in bands concordantwith bedding.

2' wide chip sample of coarse grainedhornblende schist. In immediate con tact with mafic pillowed volcanics.Coarse grained (~ 1 cm) hbl. hostssacchroidal qtz. stringers containingminor amounts of sulphides (pyrrhotite,chalcopyrite, arsenopyrite). Extensivecarbonatization.

Hornblende schist finer grained than12465. Euhedral grains -~ 2-5 mm.Sulphides constitute ± 2%. Chalco pyrite, pyrrhotite, arsenopyrite.Carbonatized. Pyrrhotite stringersupwards of 2" wide.

BIF + Pyrrhotite Stringers. BIF 507,,pyrrhotite 40%. Large 12 inchpyrrhotite-rich stringer runs throughsample location. Concordant with bedding of BIF.

BIF. Qtz. 50/2, mt. 40/K, grun. 5/2,sulphides 5/2. Very fine grained andfinely laminated BIF.

BIF. Finely laminated chert-mt.Qtz. 50/2, mt. 40/2, grun. 10/2. Lastsample in Trench FS-2.

Gossan zone material to SW of trench.Finely laminated BIF. Qtz. 50/2, mt.40/2, grun. ~ 1052.

Au ppb

30

60

35

15

50

160

55

190

85

1111111111111111111


Sample No.

12471

12472

12473

12474

12475

12476

12477

12478

12479

12480

Type

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Location

85+08N, 3+2 1WFS-4

85+0 7N, 3+2 3WFS-4

85+06N, 3+25W

85+0 5N, 3+2 7W

85+0 2N, 3+40W

84+9 ON, 3+40W

SON, 4+80W

80N, 4+80W

79N, 4+OOW

79N, 4+OOW

Description

Trench Sample: garnet-quartz-hornblende schist. Fine to mediumgrained. Quartz-carbonate stringersmake up 25%. Chloritized to minorextent. Sulphides ± 55S; pyrrhotite,chalcopyrite, arsenopyrite.

2' interval. Very fine grainedquartz-biotite schist. Minorsulphides. Qtz. 405?, biotite 50%,chlorite 5%. Very fine grainedsulphides. Sacchroidal texture inquartz.

2' interval. Fine grained magnetite- grunerite schist. Mt. 402!, grun. 50%,small quartz stringers ± 5%.

2' interval. Fine grained mt. qtz.grunerite schist. BIF.

Gossan zone in BIF. Qtz. 50%, grun.302, mt. 207..

Shear zone material. Shear zonedisplaced — 2' sinstral sense.Width -2*.

Very magnetite and grunerite-richhorizon in brecciated zone. Foliationin grunerite and minor chlorite isparallel to bedding.

Sheared BIF, 3" dextral displacements

Gossan in finely fractured BIF.Quartz 707,, magnetite 205?, sulphides<5%. 6" wide and concordant tobedding.

Gossan in BIF. Extremely weatheredand chlorite-rich. S. G. low. Con cordant to bedding. — 2' wide.Limonite staining at surface.Green-yellow staining below 6".

Au ppb

10

15

50

70

50

10

165

55

40

30

lFOUR SQUARE SAMPLE DESCRIPTIONS

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

Sample No.

12481

12482

12483

12484

12485

12486

12487

12488

12489

12490

12491

Grab

Grab

Grab

Location

79N, 4+OOW

78N, 3+75W

Grab 77+75N, 4+1OW

77N, 3+OOW

Grab 76+80N, 2+65W

Grab . 76+90N, 2+65W

Grab 77+1ON, 2+65W

Grab 77+15N, 2+65W

Grab 47+15N, 0+33W Trench FS-6



40

790

175

Description Au ppb

Gossan in BIF. Altered BIF 25 stratigraphically below but adjacent to 12482.

Gossan in BIF. Sulphide-rich pod. 100 Qtz. 60%, mt. 10X, grun. 10X, biotite - 10/L Sulphides - 105S - chalcopyrite, pyrrhotite, arseno pyrite. Follows a curvilinear shear discordant to BIF bedding.

Gossan in BIF. BIF bedding obliterated. Qtz. 60%, mt. 20%, clays 207,. 2 ' x 4 1 pod.

Gossan in BIF. Trend 330 0 discordant to bedding which is- 350 0 .

Extensively fractured. Blue-green weathering as well as limonite staining. Fracturing on o/c- 290 0 .

Fracturing at 290 0 . Fracturing 140 dilated (~3"). Centred at axial planar cleavage of fold. Fracturing randomly oriented.

Dilated axial planar cleavage in- 25 filled with quartz, grun., minor pyrrhotite.

Dilated axial planar cleavage, 20 limonite staining, quartz, grun.

2' interval. Lean BIF. mt. - 15X. 15 f.g. diss. carb. ~5Ji t f . g. po., arsenopyrite <5%, grun. 10X.

3* interval. Lean BIF, black chert, 10 mt. 10%, vfg. grun <5%, carb. ~5X. Sulphides -5X.

2' interval. Lean BIF, black chert, 5 mt <JO%, grun. •~10%, arseno. —5%, carbonates -55L Sample in SZ 2' wide. Staining green to blue to rust. 1" wide steel grey gouge concordant to bedding at 320, SOW.

1111111111111111111


Sample No. Type

12492 Grab

12493 Grab

12494 Grab

12495 Grab

12496 Grab

12497 Grab

12498 Grab

12499 Grab

12500 Grab

Location

47+15N, 0+40W

47+1 5N, 0+4 1WTrench FS-6

47+1 5N, 0+4 3WTrench FS-6

47+1 5N, 0+45W Trench FS-6

47+1 5N, 0+48WTrench FS-6

47+34N, 0+40W

47+1 7N, 0+38W Trench FS-6

48N, 3+60E

49+75N, 3+70E

Description Au

1' interval. Lean BIF, mt. ~5JS,carb. -105S up to 20% locally asstringers. Arsenopyrite disseminated.Minor limonite staining.

2 1 interval. Lean BIF,mt. *C^ (diss.)grun. -~5X, carb. -^. Sulphides ~^,vfg arsenopyrite, pyrrhotite.

Lean BIF, mt. "CIO/?, grun. -10X,sulphides - pyrite, arseno. -~55K f. g.in quartz veinlets as well as mt-rich laminae.

3' interval. Lean BIF, mt. -55K, carb. <5%, sulphides <5%, pyrrhotite,arsenopyrite. Badly fractured.

2' interval. Lean BIF, mt. IQ-15%,carb. ~5JS, sulphides <5%, diss. arseno.

Lean BIF, bio. 10/S, gnt. -5!K, mt. ~ 107.,grun. 10%. Extensive limonite staining.

SZ gouge. WS limonite staining. FS steel grey. Vfg sandy material-1" wide.

QV in flow basalt. Locallizedlimonitic staining.

Fg to mg basalt flow disc. QVsurrounded by limonitic staining.QV black qtz. , coarse grained,oriented 100 az. Foliation asymptotic to QV suggests sinstral movement ofbasalts.

ppb

10

10

^

35

10

10

40

^

5

1111111111111111111

FOUR SQl

Sample No. Type Location

77301 Grab 67+70N, 1+OOW

77302 Grab 67+40N, 1+OOW

77303 Grab 69N, 2+05W

77304 Grab 69+OON, 2+15W

77305 Grab 68+65N, 1+75W

77306 Grab 68+90N, 2W

77307 Grab 69+30N, 1+50W

77308 Grab 69+20N, 1+50W

77309 Grab 69+20N, 2+20W

77310 Grab 64N, 1+60W

77311 Grab 68+75N, 2+25W

FOUR SQUARE SAMPLE DESCRIPTIONS

Description Au ppb

Quartz-tourmaline lens in flow 235 basalt. (290/V) Tourmaline -103!. Euhedral crystals 4 mm - 8 mm long. Chlorite O52. Vfg sulphides.

Quartz-tourmaline lens in flow O basalt. Same description as 77301.

Quartz Vein, average thickness —1". O Smoky as well as recrystallized quartz. Gossan along the length of q.v. Sample interval ^-10', 30 0 to bedding.

102' wide unit of BIF of deformed and brecciated chert in a grunerite-mt. matrix. Chert 505?, grun. 305S, mt. 2 07,.

Quartz Vein, SE extension of q.v. sampled in 77303, flanked on the east side by a very grunerite-rich and limonitically stained BIF.

Quartz Vein. Same q.v. as 77303 and 77305. 4 foot interval in central part of o/c flanked by dominant fracture set. Oriented 270775 CN

Quartz lens in flow basalt. Oriented 270/V. -3" wide. Prismatic tourmaline up to 1 cm long, ~15L

Same as 77309 but maximum thickness

Quartz Vein in BIF. Course grained, 10 black, discordant. BIF bedding. Altitude 150/80W, q.v. orientation: 10/V. Surrounded by extensive limonite staining.

Gossan in BIF. Limonite and blue to 10 green staining on small fold hinge in BIF. Fracturing convergent with fold. Qtz. 85%, grun. 10/2. Extensively weathered po ~^. Qtz. saccharoidally textured.

Quartz-Garb, lens in BIF. Cone, to So. 5 6" wide, traceable for 15'. Qtz. 40/S, ank. 507, , grun. TO-15%. Minor sulph. <1%. Limonitic staining flanking lens.

1 1 11111111111111111


Sample No,

77312

77313

77314

77315

77316

77317

77318

77319

77320

77321

77322

77323

77324

Type Location

Grab 68+76N,

Grab 68+75N,

Grab 69+1 ON,

Grab 68+80N,

Grab 68+80N,

Grab 68+80N,

Grab 68+35N,

Grab 68+08N,

Grab 68+30N,

Grab 68+53N,

Grab 68+53N,

Grab 68+65N,

Grab 67+64N,

2+36W

2+50W

2+6 OW

2+70W

2+80W

2+85W

2+60W

3+0 4N

3+30W

3+30W

3+45W

4+0 3W

3+35W

Description Au ppb

Gossan in BIF. Chert 752, mt. -52 ^f g, diss. grun. -202. BIF - blockyfracturing.

Gossan in BIF. Qtz. 702, grun. 252, 10limonite in vugs —52. 3 1 interval.

Gossan in BIF. Recrystallization of Oqtz. Saccharoidal texture. Grun.and diss. mt. qtz. 702, grun. 252,mt. 52, ochre + limonite.

(15* interval) Tectonic Breccia Oqtz. 702, mt. 102, grun. 202, sulph.-52. f. g. chalc. py. Limonite stainingthroughout. Minor carb.

(6 1 interval) Tectonic Breccia OSame description as 77315.

(6 1 interval) Tectonic Breccia ^Same as 77315.

Gossan in Tectonic Breccia. Qtz. 802, Omt. 102, grun. 52, limonite -52.Fractured.

Gossan in BIF. Vfg. recrystallized ^5chert 802, mt. 102, grun. 102, blue-green staining.

Gossan in BIF. Recrystallized chert 5̂802, mt. 102, grun. 102, sulph. -02 (calc. po.) minor chlorite.

Gossan in BIF. Chert 702, mt. 202, ^grun. 102, sulph. 52, f. g. chai, po.Carbonate as stringers.

Gossan in BIF. Chert 802, recrystal- Clized mt. 102, diss. grun. 102.

Chert 702, grun. 202, mt. 102, 35 gossan in BIF.

Gossan in BIF. Same as 77323 5

1 1 111111111

1111111

9Sample No

77404

77405

77406

77407

77408

77409

77410

77411

77412

77413

77414

77415

77416

77417

77418

77419

77420

77421

. Type

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

FOUR SQUARE

Location

93+91N,

93+89N,

93+60N,

93+53N,

93+86N,

93+83N,

93+77N,

92+25N,

75+48N,

75+48N,

75+48N,

75+48N,

75+48N,

75+48N,

75+55N,

75+54N,

75+53N,

75+44N,

5+40W

5+44W

5+4 3W

5+6 2W

5+52W

5+5 8W

5+6 3W

6+90W

4+53W

4+5 5 W

4+5 8W

4+60W

4+6 2 W

4+65W

4+7 3W

4+80W

4+88W

4+4 4W

SAMPLE DESCRIPTIONS

Description Au ppb

Trench FS-3. Sample of BIF,abundant lira., D.5% po.

As above

Quartz vein, 1" x 2', smokey, dis cordant, deformed ptygmatically, tr.po. , no cc.

Character sample of garnet-chloriteschist. 5" wide, no visible sulphides

Character sample of BIF as per #77403increased grunerite content.

As above, heading west

As above, heading west

Gossan zone in deformed BIF, 2' x 3' ,irregular, abundant lim. , no visiblesulphides

Trench FS-5. Character sample of lean,undeformed BIF

As above, mt.-rich gossaned BIF, minorcc veinlets, no visible sulphides

As above, leaner BIF, up to 10%sub-1/4" cc. veinlets

As above

As above, including an 8" gossan zone in BIF, less cc. , 1^ py.

As per #7741 2

As per //77412

Gossan zone in BIF, 3" x 5 1 , concord.,no cc., tr. po. 4 asp.(?)

As above, 1' x 6' in mt.-rich BIF

As per #77412

20

20

25

40

40

30

20

^5

5

80

O

5

20

10

35

10

5

10

1 1 11111111111111111


Sample No

77422

77423

77424

77425

77426

77427

77428

77429

77430

77431

77432

77433

77434

77435

. Type

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Location

76+OON,

7 6+9 ON,

75+60N,

74+65N,

93+55N,

63+30N,

63+95N,

63+75N,

63+75N,

63+75N,

63+75N,

63+75N,

62+70N,

62+85N,

3+40W

3+30W

3+40W

3+60W

5+4 3W

2+1 OW

2+1 5W

1+OOW

1+OOW

1+OOW

1+OOW

1+OOW

1+OOW

1+OOW

Description Au ppb

Quartz vein, 12" max. x 125'exposed, clear to milky white,sugary, slightly discordant at345/90. No visible sulphides.

Quartz vein, sampled previously insouth as 1/77422

Shear zone in BIF, 4" x 12' exposed,concordant, smoky quartz infillings,highly carbonatized

Shear zone in BIF, 10" x 3 1 , concor dant, qtz.-ab. infillings, minor cc.

Shear zone in BIF, muscovite-rich,discordant, fissile, possibly aconductor (?)

Quartz vein in BIF, 1" x 3', orientedparallel to axial planar direction indeformed BIF

Shear zone in BIF, 10" wide x 75',boudinaged, no cc., no visible sulph.

Gossan zone in BIF, very lean BIF,deformed, sucrosic, no cc, no visiblesulphides

As above, minor cc.

Quartz vein in BIF, 6" wide, smoky,concordant, sheared contacts, abundantchl. inclusions, tr. asp. d py.

Garnet Biotite Schist, 6' thickcharacter sample, local tr. asp. Stpy. , minor cc.

Basalt, massive - character sample

Gossan zone in BIF, qtz. infillings,3 1 x 6', O.S-1% po., tr. cc.

Banded Iron Formation character samplewith very high cc. content, It. green,slightly rusty

5

^

^

O

90

O

^

70

160

70

20

10

20

15

11 '11111111111111111

^ FOUR SQUARE SAMPLE DESCRIPTIONS

Sample No

77436

77437

77438

77439

77440

77441

77442'

77443

77444

77445

77446

77447

77448

77449

Type Location

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab.

Grab

Grab

Grab

Grab

Grab

Grab

63+40N,

63+20N,

63+50N,

63+75N,

64+1 5N,

65+OON,

66+20N,

59+70N,

60+60N,

63+50N,

63+20N,

6 3+2 ON,

63+20N,

63+50N,

0+6 5 W

0+65W

1+35W

2+55W

2+1 5W

2+1 OW

2+70W

2+OOE

2+OOE

2+30W

2+1 OW

2+1 5W

2+0 8W

2+1 3W

Description Au ppb

Quartz-Tourmaline vein in massivebasalts, irreg., 3" x 6', discordantat 290", lira., up to 5 7, py.

As above, no visible sulphides

Sample along fracture cleavage indeformed BIF, gossanous, dextraloffsets

Gossan zone in BIF, mt.-rich, concord.,minor qtz. veinlets within, r/, p o. blebs

Quartz Pod in boulder beside o/c ofBIF, appears downstrike from #77428.

Shear Zone in BIF, 2" x 30', fissile,concordant, lim., minor quartzstringers

Gossan Zone in BIF, 6' x 20', concor dant, no visible sulphides

Quartz Vein in basalt, 12" x 10',milky to clear, discordant, chl.inclusions, no visible sulphides

Quartz Vein in basalt, 2' x 15', con cordant, milky, lim., no cc, novisible sulphides

Gossan Zone in BIF, concordant,1' x 3', no visible sulphides

Garnet-Biotite Schist, minor quartzveinlets, tr. asp (?)

BIF, slightly limonitic, no visiblesulphides

Basalt, mg, massive, tr.-0.5% po.

Deformation Zone in BIF, brecciated,12' wide x > 100', continuous, con cordant shearing, mt-poor, 6' sampleinterval

15

10

O

15

15

O

25

^

^

15

100

15

•cC5

^

111111111111I111111


Sample No.

77450

77451

77452

77453

77454

77455

77456

77457

77458

77459

77460

77461

Type

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Grab

Location

63+50N, 2+19W

63+85N, 2+1 3W

63+85N, 2+1 9W

63+40N, 2+20W

62+85N, 2+1 OW

63+75N, 1+OOW

63+75N, 1+OOW

63+75N, 2+70W

66+008,1 4+OOE

64+108,1 2+OOE

57+508,1 2+50E

63+20S.13+70E

Description Au

As above, 6' sample interval

As above, 6' sample interval

As above, 6 f sample interval

Gossan Zone in BIF, adjacent toDeformation Zone, 1 1 wide x 30',white sugary chert, tr. sulphides

Gossan Zone in BIF, 4' wide x 8'long, concord., no visible sulphides,no cc.

Quartz Vein with carbonate, abundantepidote, tr. asp. 4 py - as per 77431

As above, 15K py 6 asp.

Gossan Zone in BIF, 2' x 3', novisible sulphides

Quartz-Ab Vein, max. 1 1 wide, irregular,hosted in leucogabbro, clear to milkywhite, minor chloritic inclusions, no cc, no visible sulphides

Quartz Vein in metapelites, slightlydiscordant at 341/90. Garnetiferousmetapelite inclusions, clear tomilky white, 16" x 5'

Quartz Vein in metapelites, 3" x 20',slight lim. , minor chl. inclusions,no cc.

Character sample of leucogabbro, mg.

ppb

*C5

O

5

15

40

215

^

^

O

O

O

10

l l lll l l l l l lll l l l l l

APPENDIX D

ROCK SAMPLE ANALYTICAL

CERTIFICATES

l4

Bomtar-On A Comptny IJd.5420 Canolek Rd.. Ollawa, Onlario, Canada Phone ( Tclci: 0

BONDAR-CLEGG Geochemical Lab Report

lMl 0 17-2744

PROJECT: FOUR- SQUARE

REFERENCE INFO:

SUBMITTED BY: P. NEWMAN Ml PRIMED: 29-JUN-87

l

lf ll

l

l

lm

l

ORDER ELEMENT

l Au Gold

NUMBER OF LO'JERANALYSES DETECT ION LIMIT EXTRACTION

24 5 PPB AQUA REGIA

METHOD

FA-AA 3 10 911 weight

SAMPLE TYPES

ROCK

NUMBER

24

SIZE FRACTIONS

-200

NUMBER SAMPLE PREPARATIONS NUMBER

24 CRUSH,PULVERIZE -200 6

P; -^HEANB LESS THAN,

REPORT COPIES TO: H. HODGEPAUL NEMAN

INVOICE 10: H. HODGE

li

l i

Bondtr-Otn A Comptny Ud.5420 Canotek Rd.. Otiawa. Ontario. Canada Phone: ( Telex: 053-

BQIMPAR-CLEGG^î^)^

Geochemical Lab Report

REPOH: 017-2/44 PROJECT: FOUR SQUARE PAGE l

li.141

l1ll1l4

SAMPLE ELEHEHTNUMBER UNITS

1232612327 123281232912330

123311233212333 1233412335

12426124271242812429 12430

12431 124321243312434 12435

1243612437 1243812439

.

AuPPB

(535 5

1055

^5100

5 4520

ffi .1015

10'

105 -

20 158

.

10(5 O5

. .

j

,i

l

t

ftnfldir-tVgg A Company i Id.

5430 f amuck Ril., Ouaâ, OntRiio. (anad.l Phone I lclcv 05'

BONDAR- CLEGG Geochemical Lab Report

t

l

l

i ii i

iiii i ii i i i i i

REPORT: 017-2879 ( COMPLETE )

CLIENT: GEOCANEX LIMITED PROJECT: FOUR SQUARE

ORDER ELEMENT

l Au Gold

SAMPLE TYPES NUMBER

ROCK 5G

REMARKS: < MEANS LESS THAN.

REPORT COPIES TO: H. HODGEPAUL NEUMAN

REFERENCE INFO: -

SUBMITTED PY: P. NEWMAN HATE PRINTED: 7-JUL-87

NUMBER OF LOWERANALYSES DETECTION LIMIT EXTRACTION

56

SIZE FRACTIONS

-200

5 PPB AQUA REG IA

NUMBER

56

METHOD

FA-AA 9 10 9iB

SAMPLE PREPARATIONS NUMBER

CRUSH,PULVERIZE -200 56

INVOICE TO: H. HODGE

1111

f " - "

" Afe1i11i V

1J

1i

II

1

1f ' "

1

1

1

1

;

1i

1

fton4*r4.tettt Ce.npiiif lid.*410 CanolcV Ri)., Onawa. Onia^^~ Canada Kl J ^^^Phone: 1613)^0220 Teltx: 053-323)

REPORT: 017-2379SAMPLE NUMBER

1233612337 123381233912340

1234112342 123431234412345

123461234712348 1234912350

12351123521235312354 12355

12356 12357123581235912360

1236112362 123631236412365

123661236712368 1236912370

1237112372123731244012441

k;VVv1;*; -^ .

ELEMENT Au UNITS PPB

tttt 1010(5

tt5

tttt10

.. , . .. . . . , . . ..,. ,,10

5<5 1510

10G

225 -10 10

5 10<5tt75

(5

(55

tt

tt5

(5 tttt

17020

52025

flEONDAR-CLEGG 'JBftSS!J|..--.-- •-.-••-••. . •.-——ra. .••..v;.-. .-~.-,.v—— .^.'^

i j PROJECT: FOUR SQUARE PAGE 1

SAMPLE ELEMENT Au NUMBER UNITS PPB

12442 " " ""TO ~"" "12443 <5 12444 tt12445 35012446 1012447 ........... ?s .-....-...-.................-..........—

12448 10 12449 1012450 512451 24012452 " •15"""" "~" " "" "~ "" ~12453 14012454 20 12455 1012456 25

12457 35 '

T omptn) l Id.5420 tanoiek Rd,. Onawa. Onlaij Canada Klj| Phone: d Telex: 05V.'2iT

BONDAR-CLEGG Geochemical Lab Report

l ll i l l l l l l l

REPORT: 017-3009 ( COHPLEIE rCLIENT: GEOCANEX LIMITED PROJECT: FOUR SQUARE

REFERENCE INFO: .

' SUBHITIED BYl'P.' DATE PRINTED: 16-JUL-87

ORDER ELEMENT

l Au Gold

'SAMPLE WES

ROCK

ANALYSES DETECTION LIMIT EXTRACTION

53 5 PPB AQUA REGIA

NUMBER

53

SIZE FRACTIONS

-200

NUMBER

53

METHOD

FA-AA l? 10 911 weight

SAMPLE PREPARAnQNS"TttJH6Er~

CRUSH,PULVERIZE -200 53

REMARKS: < MEANS LESS THAN.

REPORT COPIES TO: H. HODGEPAUL NEWMAN

INVOICE 10: H. HODGE

T l

ompint Ltd,."o.

J42(l Canplck Ril., Ollaua. Onl; Canada KIJI Phone: Tdo: O

EONDAR-CLEGG Geochemical Lab Report

f l l l l l l l l l l

REPORT: 017-3009 PRflJECt: FOUR SQUARE" PAGE l

SAMPLE NUMBER

ELEMEfil UNITS

Au PPB

SAMPLE NUMBER

ELEMENT UNITS

Au PPB

1247712478124791248012481

1248212483124841248512486

12487"12488124891249012491

1249212493124941249512496

1249712498124991250077412

7741377414774157741677417

7741877419774207742177422

77423"77424774257742677427

55403025

10040

790175140"25

2015105

'10"

10v'5

35 10

40tf55

5201035"

105

105

O ^ 90 (5

'77428-

77429774307743177432

7743377434774357743677437

77438"7743977440

"?5 —— "

701607020

"10""

20 15 15 10

1515

omptn) l.ld.

5420 Canoiek Rcl., Ouaâ, Ontario, Canada KJ Phone: Telex: (

BPNPAR-CLEGG Geochemical Lab Report

l 'REPORT: 017-3001 ( COMPLETE!" "" " j REFERENCE INFO: —-—U" "CLIENT: GEOCANEX I,111IIED" " ' " "~" "~"~ "—"" ~ -----—--——- sUPBmEDlYri.lOLliFFE

l PROJECT: FOUR SQUARE HATE PRINTED: 16-JUL-87j.—...- .......,..^..™..™................. ....^^.. ^̂. .^.........^^ .... m... ..—..... ...——————————————

ff ORDER ELEMENT ANALYSES DETECTION LIMIT EXTRACTION METHOD

j l Au Gold 57 5 PPB AQUA REGIA FA-AA g 10 99 weisht

F ' SAMPLE TYPES " NUMBER"" SIZE FRACTIONS NUMBER ' SAMPLE 7REFARATIOH3" NUMBER"

l ROCK 57 -200 57 CRUSH,PULUERIZE -200 57

l ^. REHARKS: (- HEANS LESS IHAN ' ^ .^__ . __

• REPORT COPIES TO: H. HODGE INVOICE TO: H. HODGE T. JOLLIFFE

j|M-.-~ ...,..-~--,, — , . — — __ __ __

ii"'"" -------—-——----~——i.......——:-.--—.........———ii.............._.^..^.^..^_^^^^.....^^^^__i

i

Bondar-CVgjt * Company Lid. r̂hn^^ 5420 Onolrt M .. WM Ollaua, Ontario, {llW////!

I Phnnc: (MJl ^^^0 fi*,'^(' Telex: 05.1-12^^

1

1

1

1

1

1

1

1

1

1

1

1

1

1

\

1

REPORT: ol7-30oiSAMPLE ELEMENTNUflBER UNITS

1237412375 123761237712378

123791238012381 1238212383

-"12384"""" ' ~ ~"

123851238612387 12388

12389 12390123911239212393

1239412395 123961239712398

1239912400124581245912460

124611246212463 1246412465

12466 12467124681246912470

•"Sâ mHf*- flBONDAR-CLEGG CMSQtf**mMiM**fafr

..................jAu

PPB

1(5tf105•'5

^555 5

15- w— — — — — -— - .

25^520 35

— 15"-- ---------- 1055 .15tf

1510 251035

12020151020

403060 3515

50 16055

19085

^^s^^fe^***:*

|SAHPLENUMBER

1247112472 124731247412475

................, 1 24?6

7740177402 7740377404

77405774067740777408 77409

77411

•M&wM&W

PROJECT: FOUR SQUARE PAGE iELEMENT Au '

UNITS PPB1

10 |15 l 507050

1095 4020

20254040 30

^

1

1 omptny Ltd..•-b

5420 Carrick Rd..Ollaua. Oni;

• Canada Klj iHhont: (ftlJ) Ittln: 05K'233

3NDAR-CLEGB'*li^--#i^

l

l

l

l

l

l

l

::m..

l

iiixiiii

i

" REPORT:' 017-3079" TCofiflEiE "i"

PROJECT: FOUR SQUARE .

REFERENCE INFO:

SUBKIIIED Bif: P. NEMAN DATE PRINTED: 21-JUL-87

ORDER ELEMENT

1 Au Gold

R OF ANALYSES DETECT ION LIH1T EXTRACTION

41 5 PPB AQUA REGIA

HETHOB

FA-AA B 10 gti weight

SfiflFLE "TYPES '~—"""

ROCK 41

.REMARKS: < KFWJS-IF.SS THAN. .

200 41 CRUSH, PULVERIZE -200 40

REPORT COPIES TO: H. HODGET, JOLLIFFE

INVOICE TO: H. HODGE

1-i111 11 111 1111 11t1 1

5420 Onolel Rd., W/m?/ Oiiawa. Ontario. Ullu/L( .in,iHa k! 1 1 jdl^ - * '* fPhone: (MJllH^n 1-;*,-*,:

REFCfcl: 017-3075

NUMER UKIK

77302 77303 77304 77305

77305 77307 7730S 77305 77310

77312 77313 77314 77315

77317 77318 77319 77320

77322 77323 77324 77441

77443 77444 77445 77446

77447 ~ ' 77118 77449 77450 77451

77433 77454 7745577435

p.-S^M —— Vf^— iBONDAR-CLEGG (SflSB*-'(j*i.o:*--J^||^—^BJp.iI ;;iVX'f*"'.-;:f.v:J*'.. 1-^ ; ,' 1 ;. w -., M̂C.-- .v U.^,. v\, •;-(.-., .•v,-:jvv : ; 1 ,f .-^

i j PF'CJECI: ? [W SGLlftRE- PAGE i

FFF HUMFER L'fiJJS PPE

10';s

:

'•1 '

(5

10 10

j

10

(5

(5 (5 .

1 -i

(r,35

5

•;5 (5is :

100

(5 (5 {5 (5

5 ••"" ' ' ' ' ---— , 15 40

215

Ontario

Ministry ofNorthern Developmentand Mines

53B16SW0001 900

Ministere duDeveloppement du Nord et des Mines

-UiX

December 17, 1987 Your File: 87-178 Our file: 2.10583

Mining RecorderMinistry of Northern Development and MinesCourt HouseP.O. Box 3000Sioux Lookout, OntarioPOV 2TO

Dear Sir:

RE: Notice of Intent dated December 2, 1987Geological Survey on Mining Claims PA 857635 et al in the Areas of North Caribou Lake and Akow Lake

The assessment work credits, as listed with the above-mentioned Notice of Intent, have been approved as of the above date.

Please inform the recorded holder of these mining claims and so indicate on your records.

Yours sincerely,

W.R. Cowan, Manager Mining Lands Section Mines and Minerals Division

Whitney Block, Room 6610 Queen's Park Toronto, Ontario M7A 1W3

Telephone: (416) 965-4888

RM:plEnclosure: Technical Assessment Work Credits

cc: Mr. G.H. FergusonMining b Lands Commissioner Toronto, Ontario

Power Explorations Inc. Suite 1003 34 King Street Toronto, Ontario M5C 1E5

Resident Geologist Sioux Lookout, Ontario

•Ministry ofNorthern Development

MinesOntario

Technical Assessment Work Credits

Date

December 2, 1987

File

2.10583Mining Recorder's Report of Work No.

87-178

Recorded Holder

Power Exploration Inc.ttifciXJWy^X Area

North Caribou Lake and Akow LakeType of survey and number of

Assessment days credit per claimGeophysical

electromagnetic rtayf

Mxgnetometer , rtayf

Other. rlays

Section 77 (19) See "Mining Claims Assessed" column

- , . . 40 Geological * v ttxyt

Georhemira! rfaysf

Man days [~~| Airborne |~|

Special provision ("X] Ground Jx]

Q Credits have been reduced because of partial coverage of claims.

l l Credits have been reduced because of corrections to work dates and figures of applicant.

Mining Claims Assessed

PA 857644 to 647 inclusive 857649 to 650 inclusive 857652 to 656 inclusive 857658 to 659 inclusive 857662 to 666 inclusive 857669 to 670 inclusive 857673 857675 to 678 inclusive 867681 893276 to 277 inclusive 893283 to 284 inclusive

Special credits under section 77 (16) for the following mining claims30 Days Geological 20 Days Geological 10

PA 857636 PA 857635 857642 to 643 inclusive 857641 857648 857657 857651 857661 857660 857672 857671, 857679, 857682, 857674, 857680 857688, 893278, 893282 857683, 893279 to 281 inclusive

Days Geological PA 857637 to 639

inclusive 857667 to 668

inclusive 857684 893275

No credits have been allowed for the following mining claims0 not sufficiently covered by the survey Q Insufficient technical data filed

PA 857640 857685 to 687 inclusive

The Mining Recorder may reduce the above credits if necessary In order that the total number of approved assessment day* recorded on each claim does not exceed the maximum allowed as follows: Geophysical - 80; Geologocal - 40; Geochemical - 40; Section 77(19)-60.

828(85/12)

Mi' /.'try of Northern Affairs and Mir.es

Report of Work

(Geophysical, Geological, Geochemical and Expenditures) W #7

Mining Act

Instructions: — Please type or print. , t ^ . *^y— If number of mininc/^CkMms Ar^vgl'sed

exceeds space on this form, attach a list. Mote: — Only days credits calculated in the

"Expenditures" section may be entered in the "Expend. Days Cr." columns.

— Do not use shaded areas below.Vpe of Survey(s)

Geological:iaim Holder(s)

Power Explorations Inc.

To^Ârca North Caribou Lake E, Akow Lake _ C,-il28

Prospector's Licence No.

T 4642

Company

1003-34 King Street, Toronto, Ontario, M5C 1E5[Date of Survey (from St t o)

Geocanex Ltd. 11 06 .87 103 09 ,87_______l Day J Mo. | Yr. j Day J Mo. | Yr.

Total Miles of line Cut

47.8Jame and Address of Author (of Goo-Technical report)

Paul Newman, 734 Wallace Avenue, Windsor, Ontario N P\ ^ ' ^redits Requested per Each Claim in Columns at rightSpecial Provisions

For first survey:Enter 40 days. (This includes line cutting)

For each additional survey: using the same grid:

Enter 20 days (for each)

Man Days

Complete reverse side and enter total(s) here

Airborne Credits

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

1

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Electromagnetic

Magnetometer

Radiometric

Days per Claim

40

Days per Claim

Days per Claim

Expenditures (excludes power stripping)Type of Work Performed

Performed on Claim(s)

Calculation of Expenditure Days Credits

Total ExpendituresTotal

Days Credits

InstructionsTotal Days Credits may bo apportioned at the claim holder's choice. Enter number of days credits per claim selected in columns at right.

D.i RecdTWcd H6|dor or Aênl (Signature!

Certification Ven'tying Report of \VOflc

Mining Claims Traversed (List in numerical sequence)(^

Prefix

See

-;::;:;Y

-~.v-.-...~

.' - ' l "-.

,.,,;;:

U t

•;. ' ' , - - - ;

MK11M

/lining ClaimNumber

Attached S

.. L: l V b 1- i - , -, /'

5 1 j * 1 r*. J-S. ^\f *N*fLANDS SECT

Expend.Days Cr.

heet

ji

AKION

.

1'

NPrefix

"-

.^..-.:., -

PATRK

nSE

.M.ivlVliy

lining ClaimNumber

^•1,-wrt.... 4, ..^^ —— . ——————*"it]i v'-'-"

" ---fTilii9.\ "(\^'i^\ --i

\i

Expend.Days Cr.

~.^w- :

•^ '

^^ff .

j

;/ j

l hoit'by certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after us completion and the annexed report is true.

n mo .nut I'ost.il A.Mross of Person Cortityimr"' . ^^~

H. J. Hodge, 100/3-34.- King Street East, Toronto, Ontario, M5C IBS/'/Diito Certified

&S? /'//J 7Certit

Â*-**-

POWER EXPLORATIONS INC


MINING CLAIMS TRAVERSED

Pa 857635857636857637857638857639857640857641857642857643857644857645857646857647857648857649857650857651857652857653857654857655857656857657857658857659857660857661857662857663857664857665857666857667857668857669857670857671857672857673857674857675857676857677

Pa 857678857679857680857681857682857683857684857685857686857687857688

Pa 893275893276893277893278893279893280893281893282893283

Total 64 Claims

Q) E IIIA.M.''.n:C;

^

90930'

.pQ ^ ,a ^r r——^ il*1 - ^T":-S. ?i.*-*/ WU-*! ' J* 5 *

jtOC fi 3 SBgass i Msoht

i ^ l^^

4~t7oobiHoT" 5;^ 69 ,''

S2045'

900 45' 900 3O'

A.^ - .") O

y 1^.- *-

HIGHWAY AND ROUTE No.

OTHER ROADS

TRAILS

SURVEYED L!NES:TOWNSHIPS, BASE LINES, ETC.LOTS. M INING CLAIMS. PARCELS. ETC.

UNSURVEYED L INES;LOT LINESPARCEL BOUNDARYMINING CLAIMS ETC.,

RAILWAY AND RIGHT OF WAY UTILITY LINES NON-PERENNIAL STREAM

FLOODING OR FLOODING RIGHTS, SUBDIVISION OR COMPOSITE PLAN

RESERVATIONS

ORIGINAL SHORELINE MARSH OR MUSKEG ^*

, KKKi JessgfvSi

TRAVERSE MONUMENT

DISPOSITION OF CROWN LAI

TYPE O F DOCUMENT SYMBOL

PATENT. SURFACE a MINING RIGHTS _____ .^.... __ *- .SURFACE RIGHTS ONLY ______ . __ ..^.^. ©

, MtNING RIGHTS ONLY __________ :.... _ ̂ OLEASE, SURFACE 4 MINING RIGHTS— —.——..———••tt

" , SURFACE RIGHTSONLY. __ ...........1".'.*........ H

" , MINING RtGHTS ONLY.,. _ — ̂ .—....^..... __ . B

LICENCE OF OCCUPATION . __ .. ____ ... __ .™ __ . T QRDER-IN-COUNCIL ...^....... __ . ____ ™™...—— OCRESERVATION ___ ...,... ___ ...... __ ..— ......... __ . C

CANCELLED ___ ,...... ___ — ....................... SSAND S GRAVEL ___ ..,. ____ ..... __ .....—....,.....

HOTE: M INING RIGHTS IN PARCELS PATENTED PR:OR TO MAY t 1913 V ESTED IN O RIGINAL PATENTEE B Y T HE P UBLf LANDS ACT. R S. O 1 970. CHAP 380. SEC. S3. SUftSEC 1

REFERENCESAREAS WITHDRAWN FROM D ISPOSITION

M.R.O. - MINING R IGHTS ONLY

S.R.O. - SURFACE RIGHTS ONLY

M.+ S. - MINING AND SURFACE RIGHTS

Description Order No. Date Disposition Pitt

".-1C 'fi P "

Au G- p.w.

53B16SW000I

SCALE; l INCH * 40 CHAINS

FEETD 1OOO 2CX10 60OC aooc

o ?ooMETRES

1OOO M KLM!

2OOO I2 KM)

^V^f l j***.- A ^** f f^Si ^^. tTH CARIBOI(NORTH -EAST PART)

M. H. R, ADMINISTRATIVE DISTRICT

OOKOUT Division 7. \058l

PATRICIALAKD TITLES/ REGISTRY DIVISION

(PATRICIA PORTION

Ontario

Ministry ofNaturalResources B ranch

Bat* t (i

U} fieri vSK C- 2245

90 Q 30 90 7 15

52 0 52'30"52 0 52' 3-

52 045'

— . - 7~ — "T .— —

* /"r?* l"' .P-

Pa i \ ' ) Po i. P

K

V

K 2-22/0

LEGENDHIGHWAY ANO ROUTE M-

OTHE^ ROADS

TRAILS

SURVE> tO LINESTQWNSHlPS. 3ASS LINES r. TC.LOTS M'VNG CLAIMS 'ÂRCELS F TC

UNSUR'- t VEC LiîES

LOT LiNESPARCEL BOUNDARY 'MINING CLAIMS ETC.

RAiLWAv AND RIGHT Of WAY

UTILITY ,!NES

NON-PERENNIAL STREAM

FLOODING OR FLOODING RIGHTS

SUBDIVISION OR CCU?OSf T E PLAN

RESERVATIONS

ORIGINAL SHORELINE

MARSH OP MUSKEG

MINES

TRAVERSE MONUMENT -

DISPOSITION OF CROWN LANDS

TYPE OF DOCUMENT

PATENT, SURFACE fe MINING RIGHTS .SURFACE RIGHTS ONLY _. .MINING RIGHTS ONLY ... ...

LEASE, SURFACE S MINING RIGHTS .:E RtGHTSONLY. .,..

RIGHTSONLY. .....

LICENCE OF OCCUPAT.ON .... .—ORDER-IN COUNCIL .....,. ,.........

RESERVA T !ON .... ..... ..,.

CANCEL L fcO ___.^... ... ......

SAND&GRAVEL .......,.. ,...... ...

SYMBOL

B B

- ...—.O

NOTE: M NiNQ R IGHTS IN PARCELS PATENTED B " O fl TO MAY S, 1913. VESTED I N OfliGiNAL "ATENTEE B- THE PUStiC UANDS ACT flSO 1970 C HAP 3 8O. S &C 53 S oBSEC 1.

REFERENCEAREAS WITHDRAWN FROM DISPOSITION

M.R.O. - ViNING R .GHTS ONLY

S.R O. -SURFACE R IGHTSONLY

M.-*- S. - MiMNG AND SURFACE fiiGH'S

man Order No. Oaie O iiaosmon R!s

S10

'JUN25 1987A.M. p f,

SCALE. 1 1\CH - 40 C HAINS

sooo 30 DC

ooo *. v

AREA ,/

KOW 1\ r \ w v v i _M.S.R. ADMINISTRATIVE DISTRICT

SIOUX LOOKOUTl M!3!ttG DIVISION

i O A T ̂ r f l** \ A i ^^^. i n l w l M

l LATiO TITLES/ REGlSTat DIVISION

HORA ( PATRICIA f

Ontario

Ministryof LandNatural Management

Resources Branch

Dele F EBRUARY, 1 984.

527902 l

PROPERTY LOCATIONO Z 4 Miles

stand ; Open

Open spruce, jack pine , alders

Jack pin spruce, tamarack

LEGEND North Caribou LakeAREA 'A;

QUATERNARYWapuskeyo

LakeStream, lake , bog deposits Glacial, glaciofluvial lacustrine sediments

LATE PRECAMBRIAN (Keeweenawan?)

Ile Diabase

EARLY PRECAMBRIAN

Intermediate and. Felsic Intrusives

857677

Jack ptme, ^ spruce:,

\ \ tamarack

\I0a Granite pegmatiteiOb AplitelOc GranitelOd SyenitelOe Quartz monzonitelOf GranodioritelOg TrondjemitelOh Quartz dioritetOi Diorite10k Unsubdivided gneiss10 l Granite gneiss

857687A- ^ckpmer^/ ^

Boulders Jack pine,

\ spruce, poplar,

.alders

) 857676i i

\ ^ ———:

ii*/ Poplar, V

8/5 76 7 9Spruce, poplar, jock pine

x FS-5 Q!;\ So :

Mafic Intrusives9a Unsubdivided9b Gabbro9c Leucogabbro9d Plagioclase-phyric gabbro9e Peridotite9f Pyroxenite

. Jack pine, l poplars :2di /; --.--.

:/ ': A Jack pine l 'J:. \ | 1

'•- '-- ) \ ^.i-.-/ \

•::-*~ '857686Iron Formation8a Oxide facies8b Carbonate facies8c Silicate facies3d Sulphide facies

Chemical Metosediments Birch, poplar forest

7o Chert7b Calcitic marble7c Dolomitic marble

Clastic Metasediments6a Clast supported conglomerate6b Matrix supported conglomerate6c Oligomictic conglomerate6d Polymictic conglomerate6e Sandstone, Unsubdivided6f Wacke6g Arenite6h Mudstone, argillite6j Feldspathic wacke6k Feldspathic arenite61 Quartz arenite6m Schistose rock ± amphibole,± biotite

i garnet, ± chlorite of probablesedimentary origin

Spruce, poplar,

\ \ a iders

f \ J ack pine , 1 alders, poplai

-.1 ''- —- - - -^-L :-:;. 6f

Lundmork Lake

857680

857685Boulders \

Spruce j/ Open birch /l

X

Jack pinealderspoplars

Felsic and Intermediate Subvolcanic Rocks5a Unsubdivided5b Quartz - feldspar porphyry5c Quartz porphyry5d Feldspar porphyry

^^ ( Muskeg l

,d..:;::j VU, \-•-

85768 857673Felsic Metavolcanics

4a Massive fine-medium groined flow4b Pyroclastic breccia, tuff breccia4c Tuff, lapilli tuff

Intermediate Meta volcanics3a Massive fine-medium grained flow 3b Flow breccia3c Pyroclastic breccia, tuff breccia 3d Tuff , lapilli tuff

Poplar, aiders, birch spruce

l a lders,y sprucei f orest Jack

l pine

Alders, spruce . birch,

poplarsMafic Metavolcanics

2a Massive fine-medium groined flow2b Amygdaloidal flow2c Variolitic flow2d Pillowed flow, pillow breccia2e Flow breccia2f Medium-coarse grained flow centres2g Plagioclase-phyric flow2h Amphibolite2i Co-magmatic sills, dikes2j Pyroclastic breccia, tuff breccia2k Tuff, lapilli tuff21 Chorite ± amphibole schist

Alders, f ' spruce,

dead standing

\ trees(muskeg)'

N t1 i '

Open , poplars, birch, alders

857682'spr;cebirch

/ J ack pine, alders,

Stump \trunk S- f - , ^^

tamarack l ; , . ir . ../-. .,——,....rForest / 'fii Tamarack, '

— j s pruce, /Open tamarack,', 7 i ' o pen open '

/ A lders f-y s

V 857669t S pruce K 84Ultramafic Metavolcanics

la Massive fine-medium grained flow Ib Spinifex textured flow c Talc-carbonate ± magnetite ± amphibole

± serpentine ± chlorite schist STRIPPEDAREA 'B 1857670

Spruce, alders,

. birch

Popliar, jackpine spruce, alders

SYMBOLS

Shoreline

Creek, showing flow

Swamp

Beaver Dam

Break in slope ..

Claim post, line,witness post

Township line.

Trench, pit

Diamond drill hole

Highway, bush road....,

Power transmission line

857667Spruce forest 81 alders

/^Sand, C: V boulders'*

Open poplar, jackpine

^ \ Sond S l \boulders \J j857666

Outcrop, outcrop area ... .... .,..-.. x

Geological boundary, observed,.— Spruce forest

Open poplar,

' jackpine857684Inferred, inferred from geophysics.—— —— — G—G

Surficial feature boundary

Rock sample location Snumber.... *I750I

Assay for Au(ppb), Ag(ppm)

Pillow; tops known , unknown

Bedding; inclined, vertica).

Foliation, cledvage;

Inclined, vertical, unknown50y^ yf /

Gneissosity; incl., vert., unknown. . S j f

Lineation , plunge

Fracture; inclined, vertical

Shear zone ; dip

Shear fracture; inclined,vertical.

Fault zone; dextral , sinistral.... __

Anticline , syncline; plunge......... —J- — -|Drag folds with plunge

Dyke ; width , dip

Vein; width, di p, quartz , carbonate

Glacial striae

, ,. ... p \\ l Poplar9'••-.. \ l a lders l

85766

••"i t ; . - \j O pen popliar, /l 8a;'f "'-' : \ \

i l : .t. . .'. \Spruce forest

893275 V 857.663Spruce forest, f alders

Sond boulder i ridge l

Open poplar, N-^ ,- —, -, -, —857660 l a lders,

birch857664

High sand, boulder ridge

893276 Jack pine forest

Alders, spruce

(boulders)

Poplars, alders, spruce, jackpine

Spruce, tamarack, alders, birch

ABBREVIATIONS l 8 57659Silicification-.....,.. SIL, sSericitization........ S E R , serCorbanatization ,. .. .CAR ,corChloritization..... ...CHL, chl

/ l strong weak

Pyrite.......... /.... ......,... pyPyrrhotite . .. ... ...... .... . . poChalcopyrite..... ..,... ...... cpArsenopyrite ... ..... ...... ospSphalerite ................. .sphGalena . ., ..... ...,..., ,,... gaBornite .. ..................,.. brMalachite ........ ....... . malGraphite ..,........... . ... grChrysocolla ,.. ... .,..... ..chryMagnetite ........... ....... mtLim-onite . . ..... ... .. .... . .. li mHematite ,.....,............ hemMolybdenite . .......,.,..... moGrunerite .......,,.,,.,,.. grunSiderite...,........,,....... sidDolomite ..... ,. ............. dolAnkerite . ............,,,... .ankGarnet... ........... ,......' gntEpidote.... ........ .,. ....... epTourmaline ... ,....... ....... tlXenolith...................... xnMylonite .........,..,....,... ,mylShearing .,......,.......,.... sh

Corbonatized ,.......,........ cc

, '•l ' '-- - .-. - \8a !U '- j : \1 ' ' : 857658857653 O pen X Poplar,

X alders, \ spruce \

spruce. , alders '

893277

Spruce , tamarack alders , birch

Spruce, alders 857654 rounq

jiack pine

Poplars, alders, spruce 857655

20|d -\ \857652

Spruce, 4 tamarack \

893278 Spruce, birch, alders forest

857651i Small jackpine i on shallow ridge

Jack pine ,birch,spruce

Alders, ' jockpine

M857650

Alders, jackpine893279

M(j-hBoulders

Jackpine on T shallow sand f

boulder f

Spruce, tamarackOpen

\ areo l

857648

893280Poplar, alders

Jackpine, poplar on sand 8 boulder ridge 8576408 5\7 647

Spruce forest

893282857642

;t J ockpine

857649\ i Spruce Alders J forest

Spruce, birch , alders forest

Openbirch, i \ alders, ; \ ^ Spruce boulders/ \ *,

' V\

857639Open sprucebirchalders , l o.f i\

l l

857646Alders , spruce, jackpine893283

B o u l d e rs

Spruce, tamarackAlders^

\spruce) \ (birch ] \

l \

l J ackpine t forest i 8 93284

l A lders, birch , spruce, tamarack

t O pen,alders, spruce,jackpine

857638857645

Birch,spruce,tamarack 857635

857644

857637

POWER EXPLORATIONS INC.857636

Jackpine, i spruce

4- ...,FOUR SQUARE PROPERTY Opapimiskan Lake Area,Ontario Jackpine ,

spruce, poplar, birch

Geology

BY: PN./R.TMDATE: SEPT. 87SCALE: 1 :4800GEOCANEX LTD

TORONTO, CANADA DWG. No: FS-

Documents

RECEIVED NOV 2 v w MINING LANDS SECTION€¦ · 538l6swe0ei 010 report on geological mapping, prospecting and trenching four square property district of kenora, patricia mining division