RESULTS OF 1992 EXPL WORK EM (VLF) & MAG SUR · PDF filezinc and copper-nickel prospects in the surrounding area. ... TB 1142831 ... deformed zone flanked by intermediate to mafic

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42C13SW{*e2 2 .M649 W ABIKOBA LAKE 010

RESULTS OF 1992 EXPLORATION WORK ELECTROMAGNETIC (VLF-EM1G) AND MAGNETIC SURVEYS

SUMMERS LAKE PROPERTYWABIKOBA LAKE AREA, NORTHWESTERN ONTARIO

N.T.S. 42 C 13 f SW

Written by: Pierre 3-309, Thunder P7E 1K7 Phone: (807)

(807)

Simoneau Catherine st. Bay, Ontario

June 1992

623-7496 623-1692 (messages 1)

/err

JUL O 8 1992

MINING

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SUMMERS LAKE PROPERTY

ABSTRACT

The property consists of 8 unpatented mining claims which include a base metal occurence.

The property is located l'l km north-north-east of the famous Hemlo gold mines site on l ho Trans-Canada Highway 17. Access to the property is by the Highway 614 which extends north- south through the western half of the property, 12.5 km north of the corner of highways 17 (Trans-Canada) and 614 {to Mani touwadge).

The Summers Lake claim-group lies on the southern limb of tlie Dead Otter Lake anticline, in a package of volcanosedimentary rocks similar to the Manitouwadge-Geco area which hosts several significant base metal deposits.

VLF and magnetometer surveys were completed along cut and topofill chained pace with stations flagged at 25 metre intervals during the beginning of april 1992.

The survey should provide good assistance in locating potential base-metal and gold targets. Two (2) significant VLF conductors (B and H) coincide with magnetic anomalies and are consistent with the results of prior AEM surveys. They are probably stratigraphic conductors within mafic to intermediate volcanics. The anomaly H also coincide with a prior IP anomaly. The main copper-zinc occurence west of Season Lake didn't show on the survey. It is maybe not conductive enough to cause appreciable EM effect. Prospection with a Beep Mat should provide more accurate information.

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42C!3SWeeea 2 .14649 WABIKOBA LAKE

Table of contents

Abstract. . .... .. . . . .... . .. . . . . . . . . . . . . . . . . . . . . . . . . lTable of contents... . . . . . . . . . . . . . . . . . . , . . . . . . . . . . . 2

1. Introduction................. . . . . . . . . . . . . . . . . . . . . . 32. Location and Access........ . ... . , , . . . . . . . . . . . . . . . . 43. Claims......................... . . . . , , . . . . . . . . . , . , , 74. Vegetation and topography........ . . . . . . . . . . . . . . . . . 95. Regional geology.................................lO6. Previous work....................................127. 1991 work program................................15

7.1 Li necutting.................................157.2 Geophysical surveys..... .. .... . . . .. . . . . , . . . . 15

7.2.1 Survey methods........................157.2.2 Interpretation............ . . . . . . . . . . . . l 6

Magnetic survey...... . . . . . . . . . . . . . . . . . l 6Electroniagnetic survey. ...............17

8. Property geology.................................208.1 Volcano-sedimentary rocks. . . ............. . ..208.2 Intrusive rocks. . . . . . , . . . . . . . . . . . ........ . ..208.3 Structure............................... . . ..208.4 Alteration..................................208.5 Mineralization.............................,22

8. Conclusion. . . . . ...... . . . ... ......................239. Recommendations..... .... . . . . ... . . . , . . ....... . . ...23

Selected References........,......,..............24Certificate of Qua]i fications.............. . . . . . . 26

LIST OF FIGURES

Figure 1. Genera.! location map. . . . . . . . . . . . . . , . . . . 5Figure 2. Detailed location map.............. . ...6Figure 3. Claim map. . . . . . . . . . . . . . . . .. . . . . . . . . . . . . 8Figure 4. General geology map of Hemlo area.....11Figure 5. Compilation map of mag-vlf anomalies..19Figure 6. Property Geology......................21

LIST OF MAPS (in pocket)

Plan Plan Plan Plan Plan Plan Plan Plan Plan Plan Plan

l .2.3.4.5.6.7.8.9.1011 ,

Magnetometer Magnetometer MagnetometeiMAG MAG VLF VLF VLF VLF VLF VLF

survey, survey, survey, survey, survey, survey, survey, survey,

survey, profiles S postings survey, total field contours survey, vertical gradient contours

colored total field contours colored vertical gradient contours profiles S postings, Cutler station profiles S interpretation, Cutler st. colored Fraser Filter contours, Cutler profiles S postings, Jim Creek st. profiles fc interpretation, Jim Creek colored Frazer Filter contours, Jim Cr

O1OC

2,5002,5002,5002,5002,5002,5002,5002,5002,5002,5002,500

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l. INTRODUCTION

There has been continued prospecting interest in the Manitouwadge area since the discovery of Geco orebody in 1953. The claims were .slaked to cover a copper-zinc showing, and much interest has recent]y been shown in copper, copper- zinc and copper-nickel prospects in the surrounding area.

The following report gives the results of a limited ground VLF-EM and magnetometer surveys carried out between April 9th to 12th, 1992 over the Summers Lake Property. The author of this report supervised and performed the survey work .

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2. LOCATION AND ACCESS

The property is located approximately 325 kilometres east of Thunder Bay (figure 1) and 14 km riorth-riorth-east of the famous Hemlo gold mines site on the Trans-Canada Highway 17. The property is located on a northerly extension of the same belt of rocks.

Access to the property is very good, The claim group is located about 12.5 km north of the corner of highways 17 (Trans-Canada) and G14 (to ManiLouwadge) [figure 2]. Highway 614 to Manitouwadge extends north-south through the western half of the property arid the Canadian Pacific Railway spur line, extending from the main line at Struthers to Manitouwadge, also passes along the western boundary of the property.

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HUDSON BAY

•KitMond lake

LAROE


LOCATION MAP

WABIKOBA LAKE AREA

SCHREIBER-HEMLO DISTRICT

N.W. ONTARIO

N.T.S. 42 C 13 l SW

FIGURE 1.

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Property

FIGURE 2.


DETAILED LOCATION MAP

WABIKOBA LAKE AREA

N.W. ONTARIO

SCALE l : 10,000


3. CLAIMS

The property consists of 8 unpatented mining claims which were all covered by a limited geophysical survey (figure 3).

List of Claim Numbers and Due Dates

1. TB 1142831................,,............August 3, 1992

2. TB 1142832..............................August 3, 1992

3. TB 1142833.....,........................August 3, 1992

4. TB 1142834........ . . . . . . . ... .. . . ........August 3, 1992

f). TB 1142835. . . . . . . . . . . . . . . . . . . . . . . . . . . . . .August 3, 1992

G. TB 1142836..............................August 3, 1992

7. TB 1142837..............................August 3, 1992

8. TB 1142838. . . . . . . . . . . . . . . .. .. . . . ........August 3, 1992

The claim holder of the mining property covered by the survey is:

M. Dave Saunders 309, Catherine st. Thunder Bay, Ontario P7E 1K7


TB ;ra l"111*4283) l H Vt83l

FIGURE 3.


CLAIM MAP

WABIKOBA LAKE AREA

N.W.

SCALE

ONTARIO

l : 31,680


4. VEGETATION AND TOPOGRAPHY

The vegetation on the property is quite dense and appears to have been burned or partially logged in the nineteen thirties or forties. The high ground cover now consists of older hardwood, mostly trembling aspen and white birch, mixed with a dense younger growth of softwoods, predominently black spruce, balsam and jackpine. Cedar, tamarack and black spruce are found in the swampy eastern section of the claim group.

The property lies between elevations of 335 and 500 metres above sea level. The topography is variable. The area west of Season Lake consists of bedrock scarps and ridges with a relief of 30 to GO metres and steep 5 to 25 metre cliffs. The ridges are covered by a thin overburden of silt and clay. The cliffs outline the Jenny Creek valley, which is the main drainage for the area, flowing north to the Black River. The Jenny Creek valley is a flat, low lying 250 metre wide area, composed of glacio-lacustrine sands, silts and varved clays. The topography of the eastern half of tlie property consists of low rolling ridges interspersed with swampy area characterized by silt and clay overburden, 3-10 metres thick and little rock exposures.

Outcrop exposure over the western half of the property is estimated to be about 20?o of the covered area.


5. REGIONAL GEOLOGY

The Black River area, as described by V.G. Milne (1968) is underlain by an assemblage of Archean greenstones, intruded by granitic plutonic rocks (figure 4), The mafic inetavolcanics formation, which includes pillowed units, has been interpreted as the oldest and lowermost horizon of a gradational sequence. The mafic inetavolcanics grade upwards into intermediate inetavolcanics, felsic metavolcanics, pyroclastic rocks (agglomerates) and sediments.

The Summers Lake property lies on the southern limb of the Dead Otter Lake anticline, an east-west trending anticlinorium developped within the Archean aged Heron Bay Greenstone Belt. The anticline is flanked to the west by the Gowan Lake and to the south by the Musher Lake Plutons.

Rocks within the anticline have locally attained an upper amphibolite grade of metamorphism. The core of the anticline has locally been intruded by several late Archean felsic complexes, some batholitic size, composed of hornblende-biotite, biotite granodiorite, arid quartz monzonite. Finally, several ages of post-Archean diabase dykes intrude the entire sequence.

The Hemlo Mining Camp, situated in the Wawa- Shebandowan subprovince, specifically occurs in a highly deformed zone flanked by intermediate to mafic volcanic rocks in the footwall and volcaniclastic rocks in the hanging wall. It lias been suggested that the mineralization is at the contact of the crystal tuffs and sediments, where the tuffaceous rocks wedge out against the sedimentary rocks. The mineralization is zoned both across dip and along strike.

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ITJ71 alkalic complexgranitoid rocks, gneiss, migmatite mafic and ultramafic Intrusive rocks

7] Intermediate lo felsic metavolcanlcsmafic lo Intermediate metavolcanlcs, amphibolitemetasediment— — fault, lineament

GOWANLAKE

PLUTON

\

CEDAR LAKE PLUTON

OHERON BAY PLUTON

PLAYTERHARBOUR

GROUP

PUKASKWA GNEISSIC COMPLEX

Ltkt Super/or

Map courtesy of OGS

Figure U* Geological map of the Hemlo area by T.L. Muir, 1993. (Modified after OGS Maps 2220, 2^39, 2Jf52, P.2701, P.2702, P.2738, P.2739).

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6. PREVIOUS WORK

Little is known about history of the property prior to 1961 except that, since discovery of the orebodies in the Manitouwadge area in 1953, the whole district generally has been regarded with interest.

1961-1962 Including the eastern half of the Summers Lake property, 134 claims were staked by Cecil Von Klein and his associates and the property was optioned to Mcintyre Porcupine Mines Ltd. who has done some ground geophysical work and investigated the copper-nickel showing by diamond drilling in 1962.

1964 - Car-ravel le Mines Ltd. acquired control of the Mcintyre property and called it the Pulfa prospect. The Pulfa prospect consists of 253 contiguous claims including the whole Summers Lake property. Associate companies have carried out evaluation work over the area of the claims in summer 1964. The work consisted of photogeological and aeromagnetic interpretation, reinterpretation of previous information and ground geological reconnaissance. The results were compiled into reports by V. Wierzbicki (1964, 1964b).

1964-1965 Geologists of the Geological Branch, Ontario Department of Mines carried out field mapping of Black River area during the summers seasons (Milnes 1968) .

1965 - A combined airborne geophysical survey was flown between June 11 tli and 13th, 1965 for Carravelle Mines Ltd. by Selco Exploration Company Ltd. with a Mark IV INPUT and 200 metres spacing and variable line directions. A number of weak anomalies were detected whose characteristics are difficult to interpret (Domzalski, 1965).

1966 - Arrangements for further developments on the mining property were taken with Falconbridge Nickel Mines, dated January 31st, 1966. A ground magnetometer and AFMAG-Longwire surveys were carried out over the claims by Central Geophysics Limited of Winnipeg (Kilburn, 1967, 1967b). The claims over Summers Lake area were soon dropped.

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1982 - As a result of the gold discoveries during the summer of 1982 in the Henilo area, claims covering the Summers Lake property were staked by two seperate companies: llarlin Resources Limited covered the eastern half and Key Lake Exploration Limited covered the western half called the Dillman C]aim Group. An airborne magnetometer and electro magnetic survey was done over the area by Aerodata Surveys Limited. Work has been conducted on the surrounding claim groups exploring for copper- nickel and copper-1 ond-y. i ne mineralization. The survey yielded significant information as to probable bedrock conductors and the extent and conductivity of probable conductive overburden, as well as generalized magnetic features. The potential for gold bearing rocks on the Key Lake property appears to be likely in the southeast corner of the property (central part of the Summers Lake Property).

1983 - Dillman Claims (Key Lake Expl. Ltd.)Three grids were cut on the property.

Detailed mapping of the property carried out by Chris Richardson (1983) has largely confirmed the geology of Milnes (1908) while providing greater details as to volcanics subunits. Both intermediate and mafic units are observed considerably more intermingled than the OGS map would suggest. Several occurences of pyrite and/or pyrrhotite in the volcanics were noted, 47 rock samples were collected. Soil Geochemical sampling at 30 metre intervals on the grid has been done over the volcanics rocks. Work was done by S.J. Bortnick and Associate. A VLF and magnetometer surveys were carried out over the property and J. Roth (1984) recommended IP and subsequently test by drill ing.

Harlin Resources LimitedMagnetometric and Electromagnetic (VLF)

surveys were performed in winter 1983 (Giroux, 1983). Two major magnetic zones were observed. The VLF survey has outline 10 anomalies. Three of which crosses in the Summers Lake Property.

Montgomery Consultants Limited of Vancouver B.C. undertook to conduct a detailed multi-element geochemical soil survey for Harlin Resources Ltd. which was done during the period June 9th to July 15th, 1983 (Montgomery, 1983). A total of 2500 soil samples were taken. A total of 25 areas which contain anomalous metal values were further examined and sampled.

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1983 - Harlin Resources Limited (continuation)

A Geological mapping was done in conjunction with geochemical surveys (Montgomery, 1983b). Laminated pyrjte-chalcopyrite-sphalerite mineralization occurs in interbedded chert- argil l ite. A chip sample from this outcrop assayed fl.14% zinc. Disseminated pyrite also occurs in felsic volcanics. A sample of this material assayed Q.20% nine. Roth of these occurences are in the southwest corner- of the map-area and indicate some potential for a volcanogenic massive sulfide deposit.

During the period of July Gth to August 8th 1983, Phoenix Geophysics Limited have completed a reconnaissance induced polarization and resistivity survey on the grid (Hallof, 1983) covering a portion of Summers Lake Property. The background IP effects in the general Hemlo area are low in magnetude: this must be due to the low level of metallic minerals (pyrite, magnetite, etc.) in the country rocks. The survey lias detected anomalies of definite interest.

A total of 1707 feet were drilled in five holes during the period October 11 to October 28, 1983 by N. Morissette Diamond Drilling Limited of Haileybury, Out. (Montgomery, 1985). Five holes were drilled to test combined geological, geochemical and geophysical targets. Only minor zinc values were encountered and the claims in the vicinity of Summers Lake soon came open.

1985 - Key Lake Exploration Limited acquired 5 new mining claims contiguous to their original 33 claim group. These 5 claims are north of Summers Lake, staked on the previous Marl in's property. During June and July 1985, the new claims were geophysically surveyed by VLF-EM and magnetometer survey equipment (Baker, 1986). Following the geophysical survey, the claims were then prospected and mapped geologically (Baker, 198Gb). As well, a total of 245 geochemical soil samples were collected at various intervals over the 5 claims and some 38 rock samples were taken from the outcrop exposures.

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7. 1992 WORK PROGRAM

7.l Linecutting

During the beginning of april 1992, a grid (cut and flagged lines) was established over the claim-area with a line-spacing of 100 metres and a station interval of 25 metres. Two kilometres of l i neciitti ng was undertaken on the western half of the Baseline and the eastern half of the tieline 6 + 50 S. All the other lines were flagged (17 km) for a total of 19 line-kilometres.

7.2 Geophysical surveys

7.2.1 Survey methods

A geophysical program was initiated on the Summers Lake property to evaluate the economic potential of the claim block.

A grid of north - south lines spaced 100 metres apart was established as reference stations for the geophysical surveys. A total of 1.9 km of lines including the base line and tie line was completed. The ground geophysical surveys including a magnetometer and an electromagnetic VLF-EM 16 survey were carried out by the author of this report.

The geophysical survey was conducted with a Scintrex OMNI-PLUS. The OMNI-PLUS Magnetometer/VLF System is a ruggedized compact, portable instrument designed specifically for field operation. It allows for quick surveying capability without sacrificing accurancy arid quality data. It contains several microprocessors and associated circuitry for monitoring, processing and storing data. The OMNI-PLUS has two memories: the tie-line points and field measurements of the survey.

The magnetometer system measures the value of the total magnetic field with a precision of 0.1 gamma with a statistical error alarm flashing over 0.2 gamma. If the error is larger than 2.0 gammas, another reading must be taken. The OMNI-PLUR contains high technology circuits which allow for automatic, fine tracking (tuning) over the entire field strength from 18,000 to 110,000 gammas, under cumputer control. The readings were taken systematically every 12.5 metres along the cut - flagged and chained lines. The base station is located east of the highway 614, on the shore of Summers Lake, near line 2+00 W. The magnetic readings have been automatically corrected for diurnal variations when the data was dumped.

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The magnetic results are presented on a profile map (Plan 1) and two contour maps {Plans 2 and 3) at the metric scale of 1=2,500 in pocket. Extra couloured contour maps (Plan 4 and 5) were added to the report at the metric scale of 1=2,500.

The electromagnetic VLF-EM 16 survey was carried out with the OMNI-PLUS using Cutler, Maine station (frequency 24.0 kHz) and Jim Creek, Washington station (frequency 24.8 kHz). The vertical components (in phase and quadrature) of the secondary field are measured with a precision of -f or Q.2%. The OMNI-PLUS has been designed whereby, if a weak station is selected, the instrument will automatically increase the measurement period to produce higher quality results. The readings were taken systematically every 12.5 metres along the grid lines.

The results of the electromagnetic survey are plotted for the Cutler station on Plan 6 and the interpretation on Plan 7 with an extra coloured contour map 8 representing the Fraser filter. The Jim Creek station results are on Plan 9 and the interpretation on Plan 10 with an extra coloured contour map 11 representing the Frazer filter. All the maps are at the metric scale of 1=2,500 in pocket. Profiles at the scale of l cm = 2096 have been drawn for the in phase and quadrature readings. The possible conductors have been interpreted and marked by a bolder line.

7.2.2 Interpretation

Magnetic Survey

The contoured magnetic data reveal 3 general magnetic domains:

1) Broad, relatively featureless areas consistent with narrow bands of felsic volcanics and/or volcaniclatic sediments interbanded between stronger sub-linear anomali es.

2) Strong, linear magnetic high, reflection of diabase dykes like the one trending northwest and intruding the fault zone c rossing through Season Lake. A number of outcrops northwest of Season Lake allow confirmation of that anomaly.

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3) Strong, sub-linear features correlating with the belt of interbanded series of mafic volcanic rocks, mainly basalts. The continuity of magnetic units is broken by other anomalies due to diabase dykes and those due to magnetic stratigraphy. The genera] strike direction range from north-east to an eastern direction in the eastern part of the property. The anomalies arise predominantly from mafic volcanics may also be causative. In at least one instance on l,j ne 700 W around 550 S, an anomaly partially coincide with an outcrop of mafic volcanics with minor pyrrhotite.

Minerals having strong magnetic susceptibility are generally magnetite and pyrrhotite, and are usually, but not necessarily, associated as primary or accessory minerals in massive sulphide deposits; thus, coincident magnetic and electromagnetic anomalies could be i mportant.

Electromagnetic Survey

The VLF electromagnetic method is usually used in area of poor conductive overburden being very sensible to it. This method is capable of delineating geological structures as fault zones, shear zones, as well as sulphides or graphite conductive zones and other interfering conductive features like power lines... Normally, a VLF anomaly is not a drilling target. It is suggested to confirm a VLF anomaly wit}) other geophysical method prior to drilling.

The VLF results for the western portion of the property are significantly perturbed by the railroad track and accompanying telegraph line acting not only as a passive conductor but also as an active transmitter precluding readings in its proximity. A strong response is observed along Highway 614 which runs parallel to the railroad. A buried telephone cable is suspected to be the source.

The remaining VLF Em-16 anomalies, designated A to H, resulting from the ground surveys and their characteristics are as follows on next page:

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1111111111111111111

Anomaly Length CentreNo . ( metres )

A 400 L4+OOW

R 100 L7+OOW

Bl ]00 L4+OOW

C 200 L2+OOW

D 100 L7+OOE

E ^00 L7 + OOE

FI MOOO L8 + OOW

F MOO TL6 + 50S2

F3 M 200 Ll + OOE

G MOOO L4 + OOE

H MOO L6+OOE

The VLFtopographic corr

6 + 75S

5 + OOS

4 + 24S

1+OOS

6 + 25S

5 + OOS

1+OOS

6 + 25W

1 + 75S

l+GOS

0 + 50S

anomel at i o

parallel to strati grap probable bedrock condweak INPUT anomal

Figure 5anomalies result!

ies ani

pi'eS'ng froi

Remarks

Narrow linear swamp

Weak one line anomaly, Weak INPUT and Moderate Magnetic anomaly. Outcrop with pyrrhotite nearby. Weak one line anomaly, possibly related to anomaly B but cut by the road interference. Narrow linear valley.

Swamp.

Narrow Linear swamp.

Cross fault known as the Jenny Creek Fault. Smal l fault 7,one .

Cross fault known as the PinegroveLake Fault.Weak, follow flat swampy area, isprobably caused by conductiveoverburden.Weak bedrock conductor, INPUTanomaly on Line 5+OOE, follows amagnet i c anomaly.

l ies B and H lack of clear-cut i fall within volcanics and are f. Therefore they are judged to be ;torK. The anomalies coincide with moderates magnetic anomalies.

sents a compilation of the geophysical

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l li -~- . -__ ' ft. *

VI f

FIGURE 5


GEOPHYSICAL COMPILATION

Wabikoba Lake Area Schreiber-Hemlo Distric

N.W. Ontario

Scale l : 10,000

O 100 i 00 300

N.T.S. 42 C 13 X SW


8. PROPERTY GEOLOGY

8.1 Volcano-sedimentary rocks

Fi'om compiling assessment work data, the property can be shown to be underlain by a package of mafic volcanics rocks in fault contact with intermediate to felsic volcanic rocks intercalated with narrow bands of greywacke. argillite and chert (figure 6).

8.2 Intrusive rocks

Minor gabbroic plugs, granodiarite-quartz-diorite sills, quartz-feldspar porphyry dykes intrude the metavolcani.es. Also, all these formations were intruded by north and northwest trending diabase dykes.

8.3 Structure

Rocks within the property have undergone intense complex folding and have been metamorphosed up to the amphibolite facies. Pillow top determinations indicate a south facing direction while the foliation is 90 degrees to the pillows; the foliation trends north-northeast {35 degrees) dipping 80 to 85 degrees SE.

Faulting in the report area is directly related to the major north-south trending .Jenny Creek Fault situated west of the property and the northwest trending Pinegrove Lake Fault crossing the center of the property (Season Lake). This fault is one of the most extensive in the area and produces a right-handed offset of the pyrodastic-acid metavolcanic formations spectaculare]y seen by the magnetic trend on the maps. The younger Jenny Creek fault appears to be a left- handed strike-slip fault.

8.4 Alteration

Alteration of the rocks on the claim group is related to metamorphism, intrusives and structural movements. The predominent alteration present on the property is a strong hematination and epidotization of the rocks most notably in the Jenny Creek fault area.

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K)

FIGURE 6


Wabikoba Lake AreaSchreiber-Hemlo Distric


8.5 Mineralization

Minor mineralization of pyrite, pyrrhotite and magnetite were present, mainly in the Jenny Creek Fault area. Laminaled pyri te-cha] copy r i lo-sphaleri le mineral ization occurs in interbedded chert-argil l j le.

Feldspar porphyry and diabase dykes are strongly magnetic and the diabase dykes contain up to 596 pyrite and pyrrhotite.

The metasedi menlary rocks of the property are somewhat similar to those in the Hem]o Gold Camp and have a good potential for gold and base metal mineralization.

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9 CONCLUSIONS

The combined VI.,F nnci magnetometer survey has detected 3 anomalies, 2 (B and H) of which coincide with weak INPUT and magnetic anomalies that may host base metal and gold mineralization. The anomaly 11 also coincide with an IP anomaly which is making it the best target for drilling.

In light of the location of the mining property, the potential Tor base metal and gold mineralization in the vicinity of the VI,F anomalies is considered to be good but the main copper-zinc occurence didn't show on the surveys. It is believe to be of too small volume or not conductive enough to cause appreciable EM effect.

The host rocks and structural feature shares; similarities with economic deposits in the area. Further ground work should evaluate the potential for an economic zone .

10 RECOMMENDATIONS

The property should be mapped at 1=2,500 scale and prospected with a Beep Mat (a miniaturized electromagnetic survey instrument used for surface prospecting in detection of conductive mineral i seed outcrops hidden under up to 1.5 metres of overburden). Further stripping, sampling of the occurences should be performed.

The planning of more advanced work, including diamond drilling, would be based upon the ground survey results.

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SELECTED REFERENCES

Baker, N.W.,

Baker, N.W.,

Domzal ski , W.

Giroux, M.

Hallof, P.G.

Kilburn, L.C.

Kilburn, L.C.

Milne, V.G.

1986. Report on Geological Mapping and Geochemical Survey, Hemlo Area Property, Ontario. Company report for Key Lake Kxplornti on Limited and Brandy Brook Mines Ltd. l report 4 l map. MNDM assessment File No. 2.9213, Thunder Bay.

1986b. Report on VLF and Magnetometer Surveys, Hemlo Area Property, Ontario. Company report for Key Lake Exploration Limited and Brandy Brook Mines Limited. l report -f 3 maps. MNDM assessment File No. 2,9213, Thunder Bay.

1965. Report on Combined Airborne Geophysical Survey Over Pulfa Group of Claims. Company report for Carravelle Mines Limited. l report -f l map. MNDM assessment File No. G3.1G98, Thunder Bay.

1983. Magnetometric and Electromagnetic (VLF) Surveys, Company report for Marl in Resources Ltd. l report * 2 maps, MNDM assessment File No. 2.6030

1983. Report on the Reconnaissance Induced Polarization and Resistivity Survey on a Portion of a Claim Group, Hemlo Area, District of Thunder Bay, Ontario. Company report for Harlin Resources Ltd. l rep. * l map MNDM assessment File No 2.6030

1966. Report of Geophysical Assessment Work, Dead Otter Lake Claims, Thunder Bay Mining District, Ontario. Company report for Falconbridge Nickel Mines Limited, l report -f 1 map, MNDM assessment File No. 63.2003, Thunder Bay.

1966b. Report of Geophysical Assessment Work, Phil Lake - Wabikoba Lake Area, Thunder Bay Mining District, Ontario. Company report for Falconbridge Nickel Mines Limited, l report * l map, MNDM assessment File No. 63.2105, Thunder Bay.

1968. Geology of the Black River Area, ODM GR 72 68 p. 5 maps (2143-2144-2145-2146-2147).

Montgomery, J.H. 1983. Geological Report on Claims Nos. TB660401-405 incl., Claims Nos. TB660502-520 incl. Claims Nos. TB644129-144 incl., Thunder Bay Mining Division, Province of Ontario, Company report for Harlin Resources Limited, l report t 2 maps, MNDM assessment File No. 2.6030, Thunder Bay.

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Montgomery, J.H. 1983b. Geochemical Report on Claims Nos. TB660401-405 incl., Claims Nos. TB660502-520 incl. Claims Nos. TB644129-144 incl., Thunder Bay Mining Division, Province of Ontario. Company report for Harlin Resources Limited, l report 4- 16 maps, MNDM assessment File No. 2.0030, Thunder Bay.

Montgomery, J.H. 1985. Report on Diamond Drilling Program (1983) Hemlo North (Pine Grove Lake) Project, Thunder Bay Mining Division, Province of Ontario. Company report for Hnrlin Resources Limited, l rep, * logs and sketches, MNDM assessment File No 63.4388.

Mn i r T. L .

Richardson, C.

Roth, J.

Wierzbicki

1983. Geology of the Hemlo - Heron Bay Area: pp. 230-239, in The Geology of Gold in Ontario; edited by A. Colvine, Ontario Geological Survey, Miscellaneous Paper 110, 278p.

1983. Geology of the Dillman Claim Group. Company report for Key Lake Exploration Limited, l report * 3 maps, MNDM assessment File No. 2.7408

1984. Report on VLF and Magnetometer Surveys, Hemlo, Ontario. Company report for Key Lake Expl . Ltd. and Brandy Brook Mines Ltd. l report f 6 maps MNDM assessment File No. 2.7409, Thunder Bay.

Wierzbicki', V. 1964. Report on Pulfa Arthur Mining Division, Canada. Company report MNDM Assessment File No.

Group of Claims, Port Province of Ontario,

for Carravelle Mines Ltd. 03 E.6, Thunder Bay.

V., Domzalski , W. 19(i4b. Report on Preliminary Evaluation of Pulfa Prospect. Photogeological report + G maps. Company report for Carravelle Mines Limited, MNDM assessment File No. 63 E.6.

25


CERTIFICATE OF QUALIFICATIONS

THIS IS TO CERTIFY THAT:

l am a resident of Thunder Bay, province of Ontario, Canada {2-309 Catherine si, Thunder Bay, Out. P7K 1K7).

T have been engaged in base and precious metal exploration as a geologist since 1987 and as a geophysicist since 1991.

I am a graduate of University of Quebec at Chicoutimi, Chicoutimi, Quebec {M.Se. Earth Sciences, 1987) and University of Montreal, Montreal, Quebec (B.Se. Geology, 1982).

t am a member of the Professional Association of Geologist and Geophysicist of Quebec (APGGQ).

APGGQ

P1ERRE SIMONEAU

\ N* 319

Signed in Thunder Bay, June 30 1992

Pierre Simoneau Geologist, M.Se.

2G

ntario 42CI3SWeee2 2 .M649 WABIKOBA LAKE 900

Ministry of Ministere duNorthern Development Developpement du Nordand Mines et des Mines

Mining Lands Branch Geoscience Approvals Section 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5

Telephone: Fax;

(705) 670-5853 (705) 670-5863

September 28, 1992 Our File: 2.14649Transaction #W9240.0129

Mining RecorderMinistry of Northern Developmentand Mines435 James Street SouthThunder Bay, OntarioP7C 5G6

Dear Si r/Madam:

Subject: APPROVAL OF ASSESSMENT WORK CREDITS ON MINING CLAIMS TB1142831 ET AL. IN THE WABIKOBA LAKE AREA

The assessment work credits for the Geophysical Survey and Other Authorized Work filed under sections 14 and 18 of the Mining Act Regulations have been approved as originally filed.

The approval date is September 24, 1992.

Please indicate this approval on your claim record sheets.

Yours sincerely,

Ron C. GashinskiSenior Manager, Mining Lands BranchMines and Minerals Division

JLJ/jl Enclosures:

cc: Resident Geologist Thunder Bay, Ontario

Assessment Files Office Toronto, Ontario

tylnlstry ofNorthern Developmentand Mines

Ontario

Report of Work Conducted After Recording Claim

Mining Act

DOCUMENT No.M/ 9240-06/4 f

'ersonal Information collected on this form Is obtained under the authority of the Mining Act. This Information will be used for correspondence. Questions about ill collection should be directed to the Provincial Manager, Mining Lands, Ministry of Northern Development and Mines, Fourth Floor, 159 Cedar Street, Sudbury, Ontario, P3E 6A5, telephone (705) 670-7264. .

instructions: - Please type or print and submit in duplicated fiN t*t G /**JQ*tbS- Refer to the Mining Act and Regulations for requirements of filing assessment work or consult the Mining

Recorder.- A separate copy of this form must be completed for each Work Groupf) 1 4 O 4- Technical reports and maps must accompany this form in duplicate. J& * A ** ^ - A sketch, showing the claims the work is assigned to, must accompany this form.

(•corded Holders) Client No.

S9/U3leNo.\ddress

sr fareephone (f*?)

fining Division Township/Area M or Q Plan No.

G 6Zoates

Work Performed

From:Af/ZlL 1 To: tz

/ork Performed (Check One Work Group Only)Work Group

X

/

Geotechnical Survey

Physical Work, Including Drilling

Rehabilitation

Other Authorized Work

Assays

Assignment from Reserve

Type

LlfG" C.oTr/^6 f 6&0 rn'rJ IC4L s^/zvty

RFCEIV^nIiC.wU.1 v CO/w/V LATtO^

JUL 0 8 1992

' ; ' "i ; "' MINING LANDS BRANCH

)tal Assessment Work Claimed on the Attached Statement of Costs S?te: The Minister may reject for assessment work credit all or part of the assessment work submitted if the recorded

holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.

jrsons and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name Address

12 30*? sr

, O"r. Pit? Ik?

tach a schedule If necessary)

rtlficatlon of Beneficial Interest * See Note No. 1 on reverse sidecertify that at the time the work was performed, the claims covered In this work (port were recorded In the current holder's name or held under a beneficial Interest y the current recorded holder.

Date

rtlficatlon of Work Report -* C. . O ?- r, i

certify that l have a personal knowledge of the facts set forth In this Work report, having performed the work or witnessed samedurln{parjd7orcafter i completion and annexed report is true.___________________________________________J^ ^ -.y ~ne and Addres* of Person Certifying ,-M r,

ST.ipone No.

C2-J-

Date Certified By rSpnature)

Office Use OnlyotaTvalue Cr. Recorded

ts Sent

Mining Recorder

Oat* Approved

Received Stamp

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^ ^ ^ ^ ^ — ^ —

Credits you are claiming in this report may be cut back. In order to minimize the adverse effects of such deletions, please indicate from which claims you wish to priorize the deletion of credits. Please mark (^) one of the following:1. D Credits are to be cut back starting with the claim listed last, working backwards.2. Ga Credits are to be cut back equally over all claims contained in this report of work.3. D Credits are to be cut back as priorized on the attached appendix.

In the event that you have not specified your choice of priority, option one will be Implemented.

Note 1: Examples of beneficial interest are unrecorded transfers, option agreements, memorandum of agreements, etc., with respect to the mining claims.

Note 2 : If work has been performed on patented or leased land, please complete the following:

] i certify that the recorded holder had a beneficial Interest In the patented Signature Dale

Ontario

ofNorthern Development and Mines

Mi.Developpement du Nordet des mines

Statement of Costs for Assessment CreditEtat des coOts aux fins du credit devaluation

Mining Act/Lol sur les mines

Transaction No./N 8 de transaction

Personal Information collected on this form is obtained under the authority of the Mining Act. This information will be used to maintain a record and ongoing status of the mining claim(s). Questions about this collection should be directed to the Provincial Manager, Minings Lands, Ministry of Northern Development and Mines, 4th Floor, 159 Cedar Street, Sudbury, Ontario P3E 6A5, telephone (705) 670-7264.

Les renseignements personnels contenus dans la presente formule sont recueillis en vertu de la Lol sur Its mines et sen/iron! a tenlr a jour un registre des concessions minleres. Adresser toute question sur la collece de ces renseignements au chef provincial des terrains mlnlers, minlstere du Developpement du Nord et des Mines, 159, rue Cedar, 4* etage. Sudbury (Ontario) P3E 6A5, telephone (705) 670-7264.

1. Direct Costs/CoOts directs

Type

Wages Satalres

Contractor's and Consultant's Fees Drolts de ('entrepreneur •1 de I'expert- consell

Supplies Used Fournltures utilities

Equipment Rental Location de materiel

Description

Labour Main-d'oeuvreField Supervision Supervision sur le terrain

Type

U^f c^r i i-s t

Type Pi ut j f no TOO f let

*WP /urAZ*0îTu*v

Type O/MV, PL v J e**, / fc

f Sw/fVWi

Amount Montan!

3200

3200

3V. *W

M S, 1,0,

loVt.?!

Total Direct Costs Total des coOts directs

Totals Total global

3ôo, *

5j2c***

/

^<?7. ttt

iof^?iiww.is

l/

2. indirect Costs/CoOts Indirects* * Note: When claiming Rehabilitation work Indirect costs are not

allowable as assessment work. Pour le remboursement des travaux de rehabilitation, les coOts Indirects ne sont pas admissibles en tant que travaux d'evaluation.

Type

Transportation Transport

MlFood and Lodging Nourrlture et hebergementMobilization and Demobilization Mobilisation et demobilisation

DescriptionTyp*

'VxV r/cv.'/r

it^v^C.1 v rzt *

JUL 0 8 1992

ÎNG LANDS BRAfPI/VO w k*. neic*r f /tfJr#.^~rj

Amount Montan!

H mo,-"

;CH

t 3 Si. H

Sub Total of Indirect Costs Total partlel des coots Indlrects

Amount Allowable (not greater thin 20H of Direct Costs) Montsnt admissible (n'excedant pas 20 tt des coOts directs)Total Value of Assessment Credit Vileur totals du credit (Total of Direct and Allowable d'evaluation Indirect eoilit ftolil du coflli dlrieti

Totals Total global

^20 ^.

^ 3W.IV

ISi.N

7?yjiy?sw.w

*t Mlrtclt •dmliilbl*!

Note: The recorded holder will be required to verify expenditures claimed In this statement of costs within 30 days of a request for verification. If verification is not made, the Minister may reject for assessment work all or part of the assessment work submitted.

Note : Le tltulalre enreglstre sera tenu de verifier les depenses demandees dans le present etat des coCils dans les 30 jours sulvant une demande a cet effet. Si la verification n'est pas effectuee, le minlstre pout rejeter tout ou une partie des travaux devaluation preserves.

Filing Discounts

1 . Work filed within two years of completion is claimed at ^ 00% of the above Total Value of Assessment Credit.

Remises pour depot

1. Les travaux deposes dans les deux ans suivant leur achevement sont rembourses a 100 Vo de la valeur totale susmentionnee du credit devaluation.

2. Work filed three, four or five years after completion is claimed at 500A of the above Total Value of Assessment Credit. See calculations below:

Total Value of Assessment Credit Total Assessment Claimed

x 0.50

2 . Les travaux deposes trois, quatre ou cinq ans apres leur achevement sont rembourses a SO "/b de la valeur totale du credit devaluation susmentionne. Volr les calculs cl-dessous.

Valeur totale du credit d'evaluationx 0,50 -

Evaluation totale demandee

Certification Verifying Statement of Costs

l hereby certify:that the amounts shown are as accurate as possible and these costs were incurred while conducting assessment work on the lands shown on the accompanying Report of Work form.

that as J&(Rscordsd Holder, Agsnt, Petition In Compiny)

to make this certification

Attestation de l'6tat des coOts

J'atteste par la presente :que les montants indiques sont le plus exact possible et quo ces depenses ont 6td engagees pour effectuer les travaux devaluation sur les terrains Indiques dans la formule de rapport de travail ci-joint.

J M* l dee. \ am authorized Et qu'a titre de je suis autoris6(titulilri enngiiM, npriitnlinl, poiti occupi dim li compignli)

a faire cotte attestation.

Slgnstur* Date

Noia : Dans cetle rormule, lorsqu'il deslgne des personnes, le masculin esl utilise au sens neuue. A

W.R.O. - MINING RIGHTS ONI.Vf..H.O. -SURFACE RIGHTS ONLYW.+ 5. ^ MIMING AND SURFACE RIGHTS

Dwcripuon Order ho. Due Qiipoaition

SEC 36/BO W 28/63 20/10/83 S-B.O

SEC 36/60 W22/84 I4/OJ/B4 SB O

SCC 36/80 WIO/85 2/10/85 S R f;

SEC 36/^0 Wil/85 I8/I2/85 S BM B

Fik

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l ft TB 1 ti[*4444lll94441

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7V8GI . 1177862 l n 4 o29Ete

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LEGEND

.HIGHWAY AND PO'.n; Nr

OIHtH R OADS

TRAILS

SUHV[ YtD UNLSTOWNSHIPS BASE L INl^ tTC LOTS, M INING CLAIM''-. VARCE .S

UNÛRVEYID HUES LO 1 L INES PARCEL BOUNDARYM'MNG CLAtMI- t If

PA'i ^/.^ AN'.'. Mi,,HI O* *A/' i

UTILITY L IV S

NON-PE FfCNMAi. S " ^fcAM

FLOODING CH f LOODING PIGHTG SUBDIVISION OR cur,' pos"f PLAN"r st h", /. ' iOKS

OHIO.. A L SH:.:-FLIr,'

VA^SH OR Mi'SKf - .

M IN t i, TRAVf'lSl M ' - "' •- 1

4,...,-...-

?^ OF CROWN LANDS

XDCU M E NT SYMBOL

PATFNT, SURF A*":r h MnJNG H 1GHTS

,SURf ACE e

"!jy *î s"j'?7jT?4T~ - - l ^ ^'615

BOMBY TWP. G-3173 PROTHERS TWP. G-3172

, MINJN:., RIGHTS ONIYLEASE'. SURF ACf ft VI'. I NG r'tG

" .SURfACt R IGHTS ONLY......

" .MINING r.lGHlSONLY. ..,.

L ICE NCfc Of OCCUPATION ...... .

ORDEP 1N-COUNCIL .....RES: F VATION .... .... ... .. . .CANCELED . ........ . .....

. GC

(J-

SAND&GRAvf !. . ... ... ,. ... .. ....LAND USE PERMIT;. r *,# COMMEhCtAI TOUWSM.OOTPC-^1 S

MlN'NCi ftlGMlS if, y i C CFLS PA^f NTtC 1 PMIO* 1O M*,V 6 1913 vLSTf!. 'K O^^'ÂL PATi^^tf iV -* H t K J* i. K LANDb ACT *, C , 7 8:0, CH^P S*C S IC &J. *'..'*..M C "

f*OTE:

SCALE: 1 INCH -- 40 CHAINS

6OOC

O .00 '/t. T Hi i.

SOLGNG LAKE SUBJECT TO F LOOfJiNfe " O E.tVA^ GSC 3 23.75 M ETRE S

Lards o ijrrouoded by Thl* Mor'-'''T or* Su^*Qf to — 5*c. 189 Easement *S4-IO.

Sea Bomby Landrail.

Lands Surrounded by TKts MwMftg ar* Subject to Qnd o1h*r right*, 01 j*r S*e.. i89 E

. S** Whitv l.aVa N. Part

MOT F: The f.ôve Eofeemerts Ru,- Wilfi T*ypi '..^R-S And Will Attest ' Bfnes A fii'

THE INFORMATION THAT APPEARS ON THIS MAP HAS B EEN C OMPILED FROM VARIOUS SOURCES, AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SUIT WITH THE MINING RECORDER, MINISTRY OF NORTHERN DEVELOP WENT AND MINES. FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEHEON

A P E A

M.N.R. ADMINISTRATIVE DISTRICT

TERRACE BAYMlMNGDIVIStOll

THUNDER BA\RECE'wcLAND TITUS/ R EGISTRY Q UHV 8*1992

THUNDER BAY

MinistryofNatural

ResourcesOntario

Dell AUGL'iT 1964

e.i4649 WABIKOBA LAKE

200

TB

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PRO

JECT

. AR

EA

^ DI

STRI

CT

N.

T. S

.SC

ALE

1: 25

00

SUM

MER

S LA

KE P

ROPE

RTY

WAB

IKO

BA

U\K

E TH

UNDE

R BA

Y.

N.W

, ON

T.

42

C 13

X

SW-—

——

—25

50

75

10

012

5™

Mie

04—

97

06-9

2EX

ECUT

ED

BY

P.

SIM

ONE

AU

DRAW

N BY

P.

SI

MQ

NEAU

—

——

—

REVI

SED

BY

-—

——

——

——

——

——

AP

PRO

VED

BY

P.

SIM

ONE

AU

06

-92

FOR

DAVE

SA

UNDE

RSPL

AN

NO10

4S

C1

3S

W0

0*2

2

.14

64

9

WA

BIK

OB

A

LAK

E310

614

42837TB 1 142836 42833 TB 1142832

650 S

TB 1142834SummersTB 1142831

TB 1142835 LakeTB,1142838

200

100

L O

-100

-200

300

-400

-500

-600 . 650 S

-700

Approximate mean declination in 1992 for center of map.

Annual change increase 1.5'.

65000 gammas

60000

59900

59850

59300

59750

59700

59650

59600

59550

59450

59350

59300

59250

59200

59150

59100

59050

59000

59950

59000

58800

58700

58600

58500

Geophysical Legend

TOTAL FIELD 58750 -L

Legend

a

TB 1H2831

Fault

Flagged and or c u tie d survey linea

Main Highway 514 to Manitouwadge

Canadian Pacific Railroad

Lake

Creek

Claim post

Witness daim past

Property limits

Claim line

Claim number

LOCATION MAP 1 : 700 000

EXPERTS-CQHSEIUS EN GEOPHYSIQUE

MAGNETOMETER SURVEYCOLORED TOTAL FIELD CONTOURS

PROJECT S UMMERS LAKE PROPERTY AREA ______WABIKOBA LAKE DISTRICT N. T. S.GCALE1: 2500

THUNDER BAY. N .W. ONT. 42 C 13 X SW^—^

9 25 50 75 100 1^5

EXECUTED BY P. SIMONEAU n4-g? DRAWN BY P. SIMONEAU 06-92 REVISED BY ———————-— ^^—. APPROVED BY P. SIMONEAU 06-92FOR DAVE SAUNDERS

PLAN NO 4-

S3042C13SW00B2 2.14649 WABIKOBA LAKE

Documents

RESULTS OF 1992 EXPL WORK EM (VLF) & MAG SUR · PDF filezinc and copper-nickel prospects in the surrounding area. ... TB 1142831 ... deformed zone flanked by intermediate to mafic