S2008NW9170 2.1000 KAPKlCHl LAKE RECEIVED 010 TRANSTKRRB EXPLORATIONS LTD* AU6291972 (no ptTMnil liability) PROJECTS SCCTION

A OEOLOOICAL AND OEOJWSICAL REPORT on tbt PICKLE LAKE PROPERTY, XAPKICHZ LAKE AREA Group No. 4, Twp. plan No. M-2246 KENORA DISTRICT, ONTARI(ONTARIO r

MARC 0. TANOUAT, Eng., Ph.D.

OCTOBER 1971 ©rvJ©^vV©^w - •:--~~"-'! -- -- '- -1.. r-©-1- - " ; '-' TRAX3TERRE EXPLORATIOXS LTD. (no personal liability)

A GEOLOGICAL AMD GBOPIOSICAL REPORT on the PICKLE LAKE PROPERTY, XAPKXCHX LAXB AREA Claim* Group No. 4, Twp. plan No. M-2246 KENORA DISTRICT, ONTARIO

by Mare O. Tanguay, ing., Ph.D.

1. INTRODUCTION

The Transterre Exploration! Company Ltd. (the company) holds a block of seventy-eight (78) contiguous claims located in the south-*est corner of Township M-2246 of the Kapkichi Lake Area, District of Kenora, Ontario. These claims are located some twelve (12) miles south-vest of the town of Pickle Lake and fourteen (14) miles from the former Central Patricia Mine.

The purpose of this report is to assess the merits of this property based on the geophysical and geological work conducted on these claijns during the svraaer of 1971. The report is to oake recommendations based on the favourable conditions that exist end the geophysical charac teristics. It will be the aim of this report to attempt to establish the potential of this property in terns of the nature, the results and the significance of the exploration work conducted to date and in terns, also, of the considerations bearing on the geological character of volcanic meta sediment* affiliated base metal sulfides and the presence of a recently- discovered mineralised body in the neighborhood. This report is based on information of a published and unpublished nature and on personal knowledge of the geology on ore deposits of the Pickle Lake area. A party of six peoples© including one geophysicist, one geologist and the author, spent more than five weeks on the Company©s claims, during which were made the observations and surveys required for this report of evaluation.

2. LOCATION. ACCESS AND GENERAL DESCRIPTION OF THE PROPERTY (SEE FIG. 1)

This group of claims hereafter called claim group No. 4, is located in the south-west corner of township M-2246, at longitude 900 30 fV

and latitude 5l0 22*30" N, in the District of Patricia© Ontario. It is situated imnediately south of Kawinogans River which cuts across the north-west corner of the property.

This claim group No. 4 is adjacent to tfaa north to the property of Union Miniere Explorations (UMEX) on which a mineralised

discovery was made recently.

©* The property is accessible by air only. It is a 22 air-mile distance from the Severn Entreprises airbase at Pickle Lake. From Montreal the region is reached by the Trans Canada Highway to Dinorwic and then by gravel roaa to Pickle Lake. This distance can be also travelled by train to Savant Lake on the CNR line and then on by car or by bus, or by regular airlines to Thunder Bay and on by bush plane. * * ( The topography of this property is characterised by a local relief of some 50 feet. The west half is very flat and covered by numerous 2a.

S3* 4- w 90- e.;je HC ft)* H. NOKTH NORTH SPIRIT WUNNUMMIN! CAKIKHI UKC LAKE 1 LAKl *2* l sj* rrr ———njjy ——— n-H*^ S J *( LAKt MIMINISKA 1 TROUT LAKE ,,*T.JO*tPM LAKt 1 M* . :'-"^ -•••'-^:'/. Ut* M K M j SIOUX H LAC f CUL ARMST*ONO 1 LOOKOUT J M* "i * ,1* 90" W" Indti IOKf|Oinin| ihtttt o* Nilion*! ______lM*"io'"t SmttiB ——— ^ —.

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Scale 1:250,000 Tichellc llll t t s W Milk* rJ -.-.;::.-.:.: .-.i:. ::~ - -Jrrrrz^r^:— pr^-i - ^•i\^'i-": —ij.; '-.-."..i-tJ^LI.rjmnzi"^-rj'..*r.L r' KllonttiKi l 10

FIGURE l : LOCATION MAP OF TRANSTERKE EXPLORATIONS LTD'S GROUPS OF CLAIMS. •lyi-;;?..--;-.-'--

swamps. v Kawinogans River* cuts across the north-west corner where sporadic outcrops were mapped. The east half is flat with a 50 feet escarpment of glacial moraine,which borders a small lake and has a N300 trend. The lake is large enough for the landing of small bush ai re rafts. |0ut.crops were more numerous in the east half.. A power-line crosses over the property just south of the river. t

3. THE PROPERTY

Claim group No. 4 property includes 78 claims numbered 287627 to 287651 inclusively, and 289626 to 289678 inclusively. AU are duly registered with the Ontario Dept. of Mines, as is witnessed by©the Abstracts of Mining Titles, included in^appendix to this report.

This claim group has the configuration of the letter L and is limited to the north by the Kawinogans River aad claims held by UMEX. To the east the claim groups terminates at the small lake on which landing is possible. To the south the property is adjacent to James Bays Mining Corp. claims. To the west, it terminates near Carpenter River, a small river with rapids flowing to the north.

4. HISTORY OF PREVIOUS WORK

The area was the object of a regional geological map by the Ontario Dept. of Mines at a scale of l inch = 4 mi. and report by V.S. Dyer in 1933. It also was mapped by the Geological Survey of Canada at a scale of eight miles to one inch in 1963 (GSA Paper 63-5). No further details of a geological or geophysical nature were reported or filed with the Ontario Dept. of Mines as statutory work. No drilling was reported on these claims and no piping or drilling activity could be noticed in the field.

A ground magnetic and electro-magnetic report however was filed with the Ontario Dept. of Mines for the claims adjacent to the south. A weak anomaly both magnetic and electromagnetic was detected, trending north east and which seemed to cut across the base leg of the L of this r property. The anomaly reported seemed to decrease going north. Geophysics work was not extended on the claim group No.4 except for a few hundreds of feet, probably because the geophysical instrument did not have sufficient penetration and seemed to loose the anomaly. In the report filed with the IVnt.. nf Mi TIPS, one .short diamond drill hole is reported for these claims to the south but no chemical analyses are given.

In other words, the general geological trends and rock types are known but it appears that no specific detailed assessment work has been previously reported on these claims. This can be considered highly favorable particularly !at the light of an anomaly terminated at the claim boundary and at the light of a new discovery JS the nearly grounds. 5. GEOLOGICAL ASSESSMENT

5.1 Regional Geology

The rocks of the Pickle Lake region consist of volcano-sedimentary rock assemblages with foliated granitic rocks and younger intrusive masses.

A The meta-volcanics are principally fine to median grained dark green to grsy-green basalts and andesites. The pillowed varieties are common. The volcanic pyroclastic and brecciated rock varieties associated * with the previous volcanic flows are relatively abundant. The more acidic varieties are lets common and they are strongly foliated when they occur.

The meta-sedimentary rocks are fine-grained impure siliceous pelitic beds. Local!/ some tuffaceous dark colored beds appear as interbedded facies within the volcanic rocks. Examples of primary sedimentary structures are present such as cross bedding and graded bedding. Conglomerates are not common. \ Iron formations principally made of fine grained quartz, chert and magnetite are common in small amounts. They generally are interbedded with the volcanic sequences.

Foliated granitic to granodiorite rocks are very widespread. There are many variations in quarts and mafic minerals. The quartz diorite facies is the most predominent. Biotite is the principal mafic accessory mineral. The volcanic and sedimentary belts associated to the foliated granitic rocks generally exhibit a foliation concordant with these rocks. Some well-banded gneisses occur within this rock unit. ;f^Vv i ---.-: -^*.. v - - ; -- - ©-"C©V "." ©

Associated to these rocks, thor* art numerous intrusive bodies either acid masse* of porphyritic granitic rocks and froth muir* equigranular granite!, or ••all masses of gabbro with tho related dioritio facies.

5*2 Local Ooologr and Structure

Thor* la a particular meta-volcanic - meta-sedimentary belt with an oral *hap*, locatod to tho south and tho touth^wtst of Pickle Lake, shown on the geological sketch Map, which has an increased interest at tho moment. The Pickle Crow Ooid Nines and Central Patricia Mines are locatod to the north-east of this oral belt and the recent discovery by IMEX at Kapkichi Lake is locatod on north side of this belt. Coincident to this belt, there is a series of Dagnetie anomalies superposed to the meta- voleanic rocks. The claim group no. 4 owned by Transterre lixp. is locatod to the west side of this oral belt and it is also coincident: to a magnetic anomaly.

The two principal rock types are the meta-Tolcanics and the foliated granitic rocks. The geology on claim group No. 4 appears to be relatively simple but at the same time it is difficult to study it because of a rather small number of outcrops. Outcrops are fairly abundant to the south-east of this property where most of the geological work was conducted and where a very consistent and prosdsJiing electromagnetic conductor was detected. They are also quite abundant in the north section of this property. The principal series of outcrops to the east and south-east is located about 250 feet east of the baseline of the survey grid. It occurs as a set of more or less continuous outcrops 200 feet wide by a little more than 1000 feet long, with a general trend on a N-40O E bearing. Another set of outcrops was found on some 50 feet wide by 100 feet long, about 1000 feet east of the previous one. t

The first rock type is a sequence of interstratified tuffs and rhyolites. They strike at N-40O-E and the dips range between 70 to 75O to the north-west. The tuffs are made up of a succession of light grey and * dark green thin beds. The lighter beds take a buff color on weathering and both the light and dark layers vary from about one millimeter to 20 millimeters. The tuffs represent the major portion of the rocks equivalent to some 75/6 of the outcrops. The alternation of dark and light bands is characteristic. Th*?s? ti©ffs am fine grained and very strongly foliated. They are highly silicified at places and some quartz veins are present sometimes parallel to the bedding and sometimes making a sharp angle with the beds. The combination*of quartz veins partly parallel partly at an angle gives a resulting structure closely similar to dragfolds.

Dragfolds with a low amplitude and an angular fold crest were mapped, sometimes interrupted by quartz veinlets. Minor amounts of pyrite occurred near these folds. These rocks are less competent than the rhyolites and they are only lightly folded in the deformation zones where the rhyolites arc strongly folded and fractured. 7-av ""-f''.

© ' '-'''^••^i

TABLE OF FORhLVTIONS

QUATERNARY: muskeg and peat glacial drift (ground moraine of till, sands and gravels).

Unconformity

PRECAMBRIAN: (1) Foliated granitic rocks (2) Metavolcanic rocks: metatuffs metarhyolites •M;

rhyolitea occur aa long and continuous bands within the tuff beds. The thicknMa of the rhyolitea vary from l inch to 3 fact vbara it occurred. On fraah trokan turfaca, thaaa rbjolitaa ara light gray in color and thay ahov tha buff color typical of tha lighter tuffa on waatharad aurfaca.

MinaraliaatiLon of pyrita and poasibly of pyrrhotita occurred in tha tuff bada particularly vhara chlorita vaa aoat abundant* Tha pyrita vaa generally fine-grained and thinly disseminated* Tha suspected pyrrhotita appeared aa sdnute specs in the tuff layers, displaying a sat of irridescent colors* The mineralisation vaa not sustained* One grab surface sample vhere pyrite occurred was analysed and gave

The foliated granitic rocks were napped on this claia group at a location 2000 feet to the east of the baseline, towards the south boundary. This rock unit is characterised by nediun-grained pinkish grey material shoving sons 30Jf of quarts, white and pink feldspars and ndnor amounts of biotite. Foliation of the rock is evidenced by the dark minerals and the foliation trend is N-40-E with a 750 dip to the north-west. The outcrops are small and flat and most hare to be uncovered from the moss in order to be seen. Near this location, a few large (about 6 ft.) boulders were seen with l to # disseminated pyrite. This is tha only location on the property where such material was seen.

The geological contacts between the meta-volcanica and the foliated granitic rocks ware located using the magnetometric data, on both sides of the anomaly. Mor* foliated granitic rocks vert mapped in the section of tut property* There, they occurred with a more consistant and pronounced foliation and they presented the characteristics of granite- gneisses.

5*3 Geolojor of th,e conductor

Besides the snail amounts of sulphides present in the tuff beds, there is no surface evidence that can explain the presence of an Of conductor. No traces of graphite could be detected by visual means and the surface rock did not show any grey or black staining on rubbing. As is the case in this region, the sulphides are frequently associated with the iron formations and it is quite evident that a magnetic anomaly aa described below most likely is produced by magnetite. Thus it seems that a favounfcle situation occurs for sulphides to be present since both magnetic and electromagnetic anomalies are coincident in this case.

5.4 Implications of the Geological Environment

The claim block No. 4 is located within a greenstone belt which is made of rhyolite! and tuff beds. Minor amounts of sulphides were seen at the surface and a magnetic anomaly coincident to an E.M. conductor were detected. This property is located in the greenstone belt where ore bodies were found previously, the Pickle Grow Gold Mines, for which the gold bearing sulphides were intimately related to an iron formation, the Central Patricia Mines in a closely related geological situation and more recently a new orebody discovered by UMEX near Kapkichi Lake, just north-east of the present claim group and on the same strike of rock formations* 6. 080PHISICAL ASSESSMENT

6.1 Description of the Geophysical surveys

A preliminary examination of group No. 4 wo Made and tht location of the southern limits was verified following the claim* linea* A tuffaceous outcrop wu found around 1800* north of that limit over which an E.M. set-up was made, An B.M. conductor was located (anomaly No* l) and established to run parallel to the outcrop 300 feet to the west. Subsequent work involved preliminary conductor tracing by pace and compass method for 4400*.

For the second period of surveys, a baseline 8800* long was cut at N-28O-E based on the information gathered on the first survey. A complete conductor trace out then was made from the center of the grid to the northern and to the southern limits. Parallel checks were made every 1200* on the east and west side. The final lay-out of the grid was done according to this information which is plotted as the "E.M. Survey Part A Claim Group No. 4". The position of the conductor on this drawing is not exactly the same aa in the part B because the position of the cross-overs was evaluated by pacing in part A and along chained lines in part B. The positions of the cross-overs in the field are the same* A reconnaissance magnetic survey to the west of the property was nade and the result of this survey is plotted as "Reconnaissance Magnetic Survey, Group No. 4".

The detailed E.M. survey was conducted using a fan pattern with 400* - 800* - 1200* spreads and taking one extra reading at 25 feet on each side of the cross-over. The readings were made at every 100 feet extending to 500 feet on each side of the cross-over. This survey is plotted as "E.M. Survey, Part B, Claim Croup No. 4M. The magnetic survey was done with a vertical component flux-gate magnetometer and the stations were also read at every 100 feet. A 25* station interval is used near the cross-over. This survey is contoured with a 1000 Y intervals (see "Magnetic Survey, Claim Group No. 4"). One of the grid's section No. 36N was cut to the Lake on the cast side in order to get the exact location of the grid. The baseline is 3290 feet from the lake at section 36N and is running N-280-E. The azimuth has to be taken away from the center of * the grid because of the magnetic anomalies. The mean length of the north- south claim lines is actually longer than the theoretical 13201 as* seen on the location map.

The instruments used include a Sharpe magnetometer model MF-1. vertical component flux-gate type with a rang* of "p t.o 100.000 gammas and a sensitivity of 20 gammas,, with a relative scale continuously adjustable datum. The E.M. system was composed of a custum made vertical loop, a transmitter with a 3000 amp. turn-ft flux using a 1050 hz frequency. The receiver was a Sharpe model SE-200. The maximum spread was 1200 ft. and the maximum distance transmitter-receiver was 1500 ft. under average noise conditions.

6.2 Geophysical Results

From the part "A" of the E.M. survey, the following results were obtained: " ^-''"-•'•''vv-?'''^';-"-V^iT^*^ "' ••"••• ' -- '•''-'"- -" •"•""-" fii '

1. A conductor baring a strike length of 8400* inside the Had t of the property along the geological strike (see note 1) and dipping at various angles between 65*and 900 with a plunge to the north-vest. On tne grid of cut lines, it has a depth of approximately 35 feet at section 16 S (1600* South) and 250 feet at section 64 N (6400* North). There is a magnetic association coincident vdth this electro-oagnetic conductor.

2. No major parallel conductor could be found on the east nor the west of the first conductor.

3. A minor conductive zone might exist at 200'-300 f on the west of the first conductor on section 1QJ, 29N, 32K and 60N.

4. The conductivity of the overburden is much lover than the conductivity of die body responsible for the main anomaly] the quadrature component of the secondary field is caused only by this body and not by the overburden.

Kpte It The presence of a high magnetic permeability material (as evidenced by the magnetic survey) in close proximity to a conductor has an inverse effect on the inphose response (P) of the resultant formation while not affecting the quadrature response (w). The net result of this distortion is to lower the apparent conductivity of the conductor under observation by raising the y/P ratio so that the possibility of good conductivity should not be excluded. This effect will also bias the axis depth calculation toward higher depth than the real situation.

The data from part B of the E.M. survey have been tabulated on the "Sumary of geophysical datas and results". The depth of the induced current axis and the upper limit of the dip of the current axis are found together with the figure of merit of the conductor. The estimated depth •fr,:*"

NO ANOMALY NO

SUMMARY OF GEOP H Y S II;AL DATAS AND R E S lJ L T S SECTION Peak E.M. Peak-tp-Peak Current a xis de] pth calculation Spreai d/Ratio Fig. of Curre nt axii Peak-to-Peak Mag. Anomaly /Broadness E.M. peak Value Depth Derivative Depth Merit Pair Dip (at x-o) , i P Dip Y jjva ' 9i 9P-P * "o/lOO' j 81'- 800' —75— U H —E 20 S - 36^i20 39?140 7s0 170 ' 3QO 1.146 67' .064 6.3 4 10,125 160r ' 52' 900 16 25^14o 30/120 550 80' 240 1.338 50' 400' .125 6.9 4 10,100 ISO'' 102' 900 12 3S^i20 36?240 740 210' 380 .704 108' 1200' .090 6.7 e 4,300 165' 106' 800' 820 W 8 32^i60 27?220 590 180 ' 280 .596 116 '- .145 8.6 4 1,600 225' 114' 400' 900 4 S 21^2 20 12^16o 330 160' 190 .314 168' .420 13.8 4 3,750 ISO' 138' 900 0 21^240 24^240 450 200' '' 210 .490 118' 1200' .098 4.4 8 5,225 55' 230' 800' 4 N iT/'ls0 17)22o 340 300' 150 .174 260' .325 11.0 e^w 2 4,950 100' 198' 400' 8 6^1 20 7?120 130 220' 60 .104 210' ' .525 6.8 850 W 6 ' 2,600 ISO' 178' 12 20^26o 23^260 430 270' 230 .314 179' 1200' .149 6.4 840 W 8 2,600 160' 150' 400' 860 W 16 9?100 9?140 180 180' T0 .140 193' .483 8.7 4 4,200 205' 139' 800' 20 2 2 /'lg0 23/-220 4s0 210 ' 230 .456 123' .154 6.9 SS0 W 4 7,675 140' 114' 24 34^i20 35?140 690 220' 350 .562 130'' 1200' .108 7,45 780 W 4 4.450 345' 151' 760 W 28 29?160 35/22 0 640 290' 350 .562 130' 1200' .108 6.9 2 12,300 70' 184' 800' 32 26)16o 28/20" 540 310' 280 .420 152' .190 10.0 750 W 4 2,900 ISO' 130' 400' 830 W 13 /T Qo 18A60 3l0 180 ' 180 .348 136' .340 10.5 4 8,550 75' 147' 40 , 16^ go 2lJ22o 370 210' 200 .268 197' 1200' .164 6.1 8f\i 2 4,050 55' 44 , 8'A2o 6^12o 140 200' 8G 173' .174 140' 400' .350 4.9 650 W 6. 3,550 240' 252' 800' 860 W 48 15/1 go I3)18o 280 330' IS0 .136 298' .372 10.4 1 3,100 185' 52 19)14o 21^220 400 310' 210 214' .208 254' 1200' .212 8.5 ST0 W 1 2,100 265' 178' 400' 56 j 6/go 2l)14o 290 260' 210 .244 216' .540 15.6 8S0 W 2 1,150 120' 60 1S^120 25^180 430 160' 250 102' .509 117' 800' .146 6.3 800 W 4 2,700 275' 246' 850 W 64HA NM i -"-/lo11 O ~0 24A60 3SO 380 ' 240 .278 208' 1200' .173 6.1 2 1,400 165' 1 to the conductor's top is drawn on tho bottom r'rwing of "E.M. survey part B1*. As shown on this drawing the most int .,-:- - lg sections (P.M. > 10) are the following ones: 4S, 4N, 32N, 36N, 48N, 56N (see Note 2). The estijnatcd depth to the conductor's top varies from 20' to 250*. The frequency of the E.M. transmitter was at 1050 ht and the E.M. response of the conductor was appreciably below saturation.

Note 2; A vertical loop survey made with a fan pattern has good resolution along the sections but poor across. Therefore, even if section 36N has * good E.H. response the break in the magnetic body could also correspond to a local break in the conductor.

The magnetic survey shows a closely associated magnetic anomaly with the peak exactly on the cross-over on some-sections. But the peak is slightly displaced to the west on section 125, I6S, 203 and t* the e** t on section 40N to 56N. This displacement however is in general less than one hundred feet and it is consistent with the dip of the E.M. conductor. The exact dip and depth* of the magnetic body could not be evaluated here with simple methods: because the magnetic profiles show clearly that some strong remanent magnetisation effects are present. The causative body is probably made of several parallel bands having different remanent magneti sation directions resulting in a profile with much steeper gradient than normal. The low area near section 36N probably corresponds to a break in the magnetic body, the discontinuity being less than 200' wide. The value tabulated for the magnetic survey arc the pcak-to-pcak anomaly in gammas over each section and the width in feet of the value midway between the high and the low ovc.* that section. C ' j. ^ M-) The reconnaissance magnetic survey to the west of the property has shown another magnetic anomaly (anomaly No. 2) on the two claim lines traversed about 8500 feet west of the anomaly No. 1. Anomaly No. 2 is located on a poorly drained part of the property and is therefore classified as a winter proposition.

*

6.3 A Geophysical Assessment

The geophysical surveys show an important E.M. conductor of low to moderate conductivity closely associated with a magnetic anomaly. Considering the homogeneity of the readings (1700-1800 gammas) for the foliated granitic rocks to the east and to the west, the conductor would be located in the vicinity of the contact between these rocks and the

The strike of the conductor is consistent with the airborne magnetic anomaly. This airborne anomaly extends onto properties where considerable work is being done presently and to the north where a discovery of a new copper mineralized body was found. Keeping these factors in mind, this anomaly commands a high priority as far as further evaluation is concerned.

In order to do so, further geophysical work could be recommended but the results might not be worth the expenses for the following reasons. A turam survey would give the conductivity thickness product of the conductor. Provided suitable set-ups are made it *ill permit a discrimination between the macnetio and oonduotive reaponae of the oausatiYe body* But thia type of awnrey la moat expenaiTe and never glvea the certainty that drilling doea provide*

A gravity survey might be indicated but the magnetic aaaooiated to the conductive body would oaak the gravity anomaly and the results night become misleading* For these reasons a diamond drilling program is more preferable.

6.4 An Exploration Aasesmen^

It is considered that thia claim group No.4 aerits a diamond drilling program of exploration. In view of the information obtained both geological and geophysical, a diamond drilling program has a much greater than average chance to meet with a certain degree of success.

7. CWdJUSIONS

It has been die ain of this report to outline the geological and geophysical characteristics of this claim group No. 4 of Tranaterre Explorations Ltd. The results and considerations have underlined the favourable conditions on the property for the occurrence of sulphide base metal deposits in a sequence of volcanic rocks. It is concluded that a diamond drilling program la warranted without delay and that further geophysical (mag. and EH.) surveys are necessary to determine the presence of additionnal anomalies. 8. RECOMMPiDED DRILLING AND GEOPHYSICS PROGRAMS;

Phase I It is recommended that the following drilling program be performed as an efficient approach to further evaluate the anomaly No. l on claim group no. 4, as detailed in a) and b). The geophysical surveys should include both magnetic and EM measurements as detailed in c).

a) Diamond drilling on anomaly No. l Section No. Footage 4N 350' 24N 250' 28N 250' 36N 250' 48N 400' 56N 350'

Total 1850 feet

b) Drilling costs "',- i) immobilization $ 3,200- ii) 1850'D drilling 13,600. at $7.35/ft iii) moves 1,200. iv) core logging, sampling supervision, engineering 3,000. v) contingencies 1,500.

Phase I $ 22,500. ~ .- : ~: ;; -© .©" .-. .. -.© : , }©- - © . . © © , ~ : - lit©© o:\"..©., .rf-©*-©??-©/.-f-

c) - Geophysical surveys on anomaly No. 2 (vertical IM and magnetic surveys: 35 mi at S265.7mile $ 4,500. - Mobilization costs for geophysical surveys 1,500. - Supervision, interpretation, contingencies 1,500. SL2,275. TOTAL: $34,775.

Phase II

Depending on the results of Phase I, and if it warrants, a second phase program is recoiiriondeu LO include uic Tullunltig vllcu.~i.vi drilling: a) Elaboration and organization of program $ 1,500. b) Drilling on additional sections of anomaly No. l Section No. Footage ''-' Section No. Footage 12S 200' ' 20N 250' 6S 200' 40N 250' 4S 250' 44N 250' OfOO 250' 52N 350' 8N 350' 60N 350' 12N 350' 64N 350'

t ^ tt i ai —^^^••••^^ 16N 35Q1 ' Total: 3,650 feet V-Y,;'.'.'*.'~,"'^-.'.: " 1;-"i''.'-iY-:y?5l'1 ^^^fS^^j^^^^^^'^^^^S'^ •, , '•"-'••"''t''-; C- r-'-'"'-.' .C':','.",

c) Drilling costs

i) immobilization nil ii) 3650'D drilling at $7.10/ft $25,900. iii) moves 2,400. iv) core logging, sampling supervision, engineering 6,000. v) contingencies 3,000. $37,300.

TOTAL:

January 25, 1972. (Signed) m

A P P EN DIX

ADDITIONNAL INFORMATION ON TRANSTERRE'S CLAIM CROUP #4 KAPKICHI LAKE AKEA. KENORA. DISTRICT ONTARIO

a) Location and access;

Claims of this group are located 12 mi. west-south-west of Pickle Lake. Access by road to Pickle Lake and there on by small bush plane to the Kawinigans River, or to a nearby lake. Access is possible also using the transmission line path, going from Pickle Lake to Sioiix Lockout. b) Property holder;

Transterre Explorations Ltd 117 St-Catherine St. W., Suite 910 Montreal 110.

* c) Party submitting the survey reports;

Marc G. Tanguay, Eng., Ph.D. Consulting Geological Engineer 13 Greenwood St. . Ste-Therese, P.Q. d) Numbers of ciaimsi

licence nos. 287627 to 2S7651 inclusive 289626 to 289678 inclusive. total of 78 claims. ,-T ' ' "' "-- . '. i vwir-s**e- " - -" ''' " '^- "

e) Dates of survey (field york)

July 3rd to July 26, 1971.

f) Table of formations

(included inside report) g) h) Rock descriptions and structural features;

(included inside report)

i) Previous work

None reported in government's files, None that could be deduced from field

j) Mineralized zones;

(As described inside report)

k) Personnel

Two geologists, one with 9 years of experience and a Ph.D. degree. One geophysicist with 4 years of experience Four assistants One draftsman Two secretaries 3;' " y' "T'^71 "^-^ . ;: 21. -- , -?-\^

1) Geologist in charge;

Dr Marc G. Tanguay, Eng., Ph.D. has a B.Se.A.degree in geological engineering from Ecole Polytechnique, Montreal; a M. Se. A. degree in mineralogy and economic geology from the same; and a Ph.D. degree from Purdue University.

January 27, 1972 lay ., Loc AT ION n^p : TWP

4 fcMOflAU'V NO. l l*\*TWlcf v XlHCMA

SC.ALt i 'l* *KUC * \* C.M. CoMO^*c•r•*^ t —-~ in f r&peiV of j/f.

To July 15 July 20 6 ?vu.y t s juuy ao July 15 July 20 6 Tiiuy 15 xuuy 20 July 15 Juily 20 6

. .

, AWO LINt CUTTihS t STAKING CQ.XTRACTOR HEAD OFFICE: VAL D©OR, P.QU6. TEU 824-4060

TWP.- Pic^loPICKLE PROV:C:.i.:-li. DATE: July 23, 1S?1*

iViios at ? Total $ Grand Totdl: e.4 Wiles at S 95.00 Total ? 798-00

j NCRTrt ! SOUTH j TOTAL IN FEtT j TOTAL IN FEET TRANSIT LINE ~~!' ————————————————t-TIE L:NE i TIE LINE j PICKET u\c i

BASI Li ME: O 8800

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TRANSTERRH EXPLORATIONS LTD. BREAKDOWN ANALYSIS OF 1971 SUMMER OPERATIONS-PICKLE LAKE AREA

GROUP NO l GROUP NO 2 GROUP NO 3 GROUP NO 4 207. 45* 10* 25*

Line cutting (Appendix A) 556.60 1,298.75 NONE 795.15 (as per mileage) Fees and salaries (Appendix A) 2,629.00 5,915.00 1,315.00 3,286.00 Disbursements (Appendix B) 752.26 1,692.60 376.13 940.34 Sub-total 3,937.86 8,906.35 1,691.13 5,021.49

Administration fee - 57. 196.90 445.32 84.55 251.07 34.134.76 S9.351.67 SI.775.68

BODNAR A CIC ^fr

TRANSTERRE EXPLORATIONS LTD. APPENDIX A PICKLE LAKE AREA

LINE CUTTING - Jean Alix Ltd -

Mileage basis - Length y. Amount Group No 1 $ 313.05 217. $ 556.60 Group No 2 715.45 497. 1,298.75 Group No A 444. 90 307. 795.15

,ES AND fALARIES EXPENSES DURING SUMMER 1971

PAID PAYABLE TOTAL A. Robin 1,000 100 1,100 J.M. Dube' 690 690 J. Robillard 2,850 2,850 F. Ray 960 960 J. Ray 4,150 4,150 M.G. Tanguay 1,600 1,600 3,200 Indian Charly 195 195

Applicable to Group No l

Group No 2

Group No 3

Group No 4

cdrl. aooNAR A cic OOMPTAMLM ' "" '

TRANSTERRE EXPLORATIONS LTD. APPENDIX B

PICKLE LAKE AREA

DISBURSEMENTS -

Truck rental 700.00 ^Equipment rental (E.M. and Mag) 300.00 Air transportation on site 422.75 Maps 44.20 Travelling, food, lodging and supplies 2.294.38 S3.761.33

Applicable to Group No l 207. 752.26

Group No 2 457. 1,692.60

Group No 3 107. 376.13

Group No A 257. 940.34 S3.761.33

cfirt aooNAR A etc •:i

52008NW9170 2.1800 KAPKICHI LAKE 020

Surveys

on ih,e property of

WANS TERRS EXPLORATIONS LTD.

Kapkichi Lake Jiogion N. W, Ontario

Group IV

July 20th, 1972.

- "-if *- -p* i, * CONSTANT1NE BALAMIS, P.ENO.

INTRODUCTION

Geophysical surveys were carried out on two properties controlled

by Transterre Explorations Ltd. in the Pickle Lake area.

The two properties are designated as IV and III respectively.

Group IV is located fifteen miles south-west of Pickle Lake while group III

ir, located nine miles south-east of the town (see attached index map).

The most accessible way into the two properties is by air. The

beet lakes for transport lie on the western margins of the two groups.

These were used by the Geophysical crews for the surveys described in this

report.

This report deals only with those surveys in group IV. The Trans-

terre holding in this p;roup are an follow;:.: Seventy-eight claims numbering ;'?JY627 to W(tj'jl inclusive and 289626 Lo ^89678 inclusive, on township plan

'A'^'.'hC. The r.urveyr, cover the south-west part of the group.

The methods chosen for the surveys were the vertical loop electro-

n-irnetic L-y.stem :ir. well ;is magnetics.

The- r.urvcys were carried out between March 25th and April 21st.

A total of I'Y-7 miles of line was cut (including base lines and tie lines).

in addition, P.'?, "i miles of geophysical surveys was completed over this

.iruup.

The Pickle Lake area has been the site of considerable explora tion over the punt year. As part of a systematic search for base metal " "- - -j,^'— ——— s;,-," — ' — SJA 3'

NORTH SPIRIT NOW1H WUNNUMMIN CARlliniJ LAKf lAKt LAKt 42" ———— S? r M* 4JN MIMINISKA IROUT lAKt ST. JObtTM LAKt

if M* t} K l 1?J S? SIOUJ LAC 5CUI AMMS1RONQ I lOOKOUI VI™ ,.....[ . __ ...... — ,.^- JO* 94* o?" 9-A 88^ Indr* U* *.1|pintn4 thcctt of NitiOflAl

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M.lf. t Scale 1:250,000 FchclU It Mill'1 t —l:--;-Ji^:z^'—— -—:——l l t—1 l——l !————— :o 19 KiloMrttrft

F ] G l! R K l : LOCATION MAP OF TKANS7EURE EXPLORATIONS LTD'y CHOUi'S 01-' CLAIMS. C: -'- . -- ' '- . - ' ' ' -.' . . -'. "" - -"''V y.- ' -' -"-"•- -*'" •-—'•'."-.'^•'.f-'^--

CX^NSTANTINE 8AI.AMIS, P.KNG.

deposits within Precambrian greenstone belts, UMEX discovered a mineral deposit "now estimated to contain 10,000,000 tons of sulphide ore with an average of 1.6J5 copper and Q.2% nickel". The company recently made the decision to sink a shaft on the deposit in order to more effectively develop it at depth. The site is eight miles north-east of group IV. Unfortunately no data is available regarding the geological or geophysical characteristics of the deposit.

GENERAL GEOLOGY

The general geology of the area is described in a number of pub lications. Of particular interest are the following:

(1) Ochi;; Lake Aeromagnetic r. Geophysics Paper 923 Scale: One mile to the inch

(2) Preliminary Series Geology Map 51-1960 Lake St. Joceph Area, Ontario Geology by R. F. Ernslie - C.C.C. Scale: Four miles to the inch

(b) Preliminary Series Geochemistry Map 50-1963 (Copper in Bedrock) L-.il,-: Hi. Joseph Area, Ontario Compilation by R. H. C. Holman, 1960-61 Scale: Four miles to the inch (k) Red Lake-Lansdowne House Area, Northwestern Ontario, Bedrock Geology, Geophysical and Geochemical Investigations G.S.C. Paper 63-5, with two maps.

On group IV the western third of the claims is underlain by granite (exposed on the south shore of Kapkichi Lake). The central part of the claims is mapped as basic volcanics, although no outcrop is apparent. The -' :: "'" ;::^'-' : "'''-'" ; -' : : - ''''

CONST ANTING SALAMIS, P.ENG.

eastern third of the claims is covered by a broad esker. The ground is generally low and swampy, particularly to the south-west.

The granitic rocks are typified by low magnetic susceptibilities. The mafic volcanics give rise to linear anomalies having medium to low magnetic susceptibilities. Iron formation produced anomalies in the range between 62,000 and 76,000 gammas on the aeromagnetic sheet,

The iron formation was an important control for the old gold mines of the Pickle Lake area (e.g. Pickle Crow Gold Mines, and Central Patricia Cold Mines). The gold occurred free in irregular quartz veins cutting mafic pillowed lava flows and interbedded iron formation.

MAGNETOMETER SURVEY

The- surveys were carried out using an Ask an i a torsion-type magnet ometer. The results arc indicated on the enclosed maps on a scale of two hundred feet to the inch.

t On group IV the data is presented in profile form {four hundred

gawrius to the inch).

The magnetic relief is extremely low in this area with the except ion of the south-west corner (area of Zone "V").

Zone "G" is interpreted as underlain by granite. Profiles of magnetic intensity over this zone are typically smooth. Tanguay noted the presence of granite on the south shore of Kapkichi Lake, a half mile north of the grid. frj:*-'-'~\^'-'''^y?'^

. ' - ' " •-''' * •"-.~ ** ; iV.".'* *''*\*!'*-^V*'?/^. CONSTANTING SAI. AMIS, P.KNO.______©______-______: :: © © '' \©4©^-©^© l* "•^/•••:

Zone "V" is interpreted as underlain by volcanics. The profiles are typically irregular and show amplitudes up to 2300 gammas. In general they indicate medium to low magnetic susceptibility. The volcanics are likely highly granitized because of the enclosing granites. They likely represent a relatively thin remnant of an ancient greenstone belt,

The magnetic maxima are irregular and do not show continuity from line to line. Unfortunately none of these coincide with any significant electro-magnetic anomalies.

Tlie local magnetic anomalies are therefore due to magnetite rather than magnetic sulphide mineralization.

ELECTROMAGNETIC SURVEYS

The ucintrcx SE-300 vertical loop was used for the surveys. A constant, separation of 1(00 feet was mo ; 'tairied in a broadside configuration over botli grids. The? instrument has two operating frequencies (1*00 and 160C Hz). The higher frequency wan maintained for the surveys described hero.

Used in the "broadside" configuration the vertical loop has min imum coupling with 'lat lying conductors such as rverburden. Anomalies are indicated by the presence of "cross-overs", i.e. the coiltilts away from the conductor on both .tides, forming an "anticlinal" pattern (if one used the dipping bed analogy) wiitn crossed by the receiver coil.

The tilt-angles are plotted on the enclosed maps on a scale of CONSTANT1NB BAL.A.MI8, P.ENO.

ten degrees to the inch.

Five weak electromagnetic conductors were located by the survey {EJL to E5 ).

The responses are marginal since all have very lov peak-to-peak amplitudes. All of the conductors are confined to one line, and usually to just two or three stations.

The conductors fall close to the operator "noise level" in their response. None have magnetic correlation.

The "anomalies" are probably caused by overburden and are there

fore of no further interest.

CONCLUSIONS AMu RIQCOMMENDATIONS

The ceophysical surveys on the south-west part of group IV

revealed that moot of the area of this particular grid is underlain by

granite. The volcanics are interpreted'as underlying the western third of

the survey area and are probably granitized basic volcanics or their

metamorphic equivalents. The electromagnetic survey failed to reveal

any significant I'M anomaly that could be caused by a massive sulphide

de-posit. No further work is recommended within the part of group IV covered

by this survey.

A survey, under the supervision of Dr. M. Tanguay, was carried

out in the eastern part of this group in 1971. p|f^^v;: :^i^;|;^ v:- ,:- r-••/- ;v'-"-4;^v^^|:^:^4|:'4?li^^ii|

CONSTANTINB 8A.1.AM1S, P.ENO. ' /-V " "*.'"•'"' ' : ''',-"- - : ' ' " :;' . ; ""' " """ " '^ . ' '' •"•"; | ; " '.. "'-' ••••'.:.- " : :'" ,.. '^' . " ; .- ", "" ' 6

This report does not deal in any way with the results of Dr. Tanguay's survey.

Respectfully submitted,

CON SALAMIS, P.Eng. STATJMBIT OF COST

TRAHSTERRE EXPLORATIOMS

in account vitb

C. 3ALAMIS t ASSOCIATES DtC.

Jun* 27, 1972. lo accordance vitb letter-contract signed January 26th, 1972. Geophysical surreys - Group IV (Kapkichi Lake area)

Ling cutting

27.7 miles 6 375 per mile 4 2,077.50

OeopbyeicB

Electromagnetics - 22.3 miles Q 1105 per mile 2,3*1.50 Magnetics - 22.3 miles g l 80 per mile 1.76^.00

TOTAL l 6,203.00 i .'. i^Atf *M^ A* c* TRANSTERRE EXPLORATIONS LTD. (no personal liability)

52088NW9170 2.1888 KAPKICHI LAKE

A GEOLOGICAL AND GEOPHYSICAL REPORT on the PICKLE LAKE PROPERTY, KAPKICHI LAKL AREA Claims Group No. 4, Twp. plan No. M-2246 KKNOR\ DISTRICT, ONTARIO

by MARC G. TANGI'AY, Eng., Ph.D.

JANUARY 25, 1972 1NO SiMSOLS

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EM SURVEY PART "A CLAIM CROUP "4 ANOMALY '1 TRANSTERRE EXPLORATIONS LIMITED s c'oji ovin ~—- PICKLE LAKE REGION. ONTARIO

T W P PLAN No M 2246 (* OKDuCtM CV '04^^1*1^1* !.TATIOIIt COMOUtIO* (K *.'i'.—4 sn'iohs **o crrsc 205 16-5 125 'BS 45 4-N BM 12-N 16*4 20 N 24 N 28 N 3? N 36 M 4O H 44 N 48 N " S? N 56 N SON 64 M 68 N 12-W

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•4 t If MCOvxit SUTiM ANOMALY TRANSTERRE EXPLORATJONS LIMITED * ic*j loo' -r to* —1" v C"0*"" t*-I* C H CO*Dvt'OI PICKLE LAKE FtCION. ONTARIO

*uwrt*(D Jut* 'M '•* —S T W P PLAN No M 2246 - —— —— —— —— — .— H(*|-0 ttltttuTiC tlXVC' •OO-*00-"IOC '** *4TTl'1

CURRENT AXIS DEPTH VI dlCt*. IX((|01,Ck II *f cootc'te to* TOO' - t* DI'lx Of to* O" COMOVCIO* ?0 ? 16-S 12-S 8-S 4-S 4-N 8-N 12-N 16-N 2O-N 24-N 28 N 12 N 36-N 40 K 44 N 48 M 52 N 56-N 6O N 64 M 68 N 12 W e w

4-W

MAGNETIC SURVE-l CLAIM ANOMALY TRANSTERRE EXPLORATIONS LIMITED *. f ix * v .r1' **to**v *'OJ* *i't***t tODO f - — PICKLE LAKE REGION. ONTAAiO ULi^t *2*WwTM H ?t* f jut* 'ri TWP PLAN No M 2246 f MAbM f OMC Tt* M4tMMt STATtO (H :j**oucto* "•t UM

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• ooo y- TRANSTCRRC EXPLORA sS LTD PICKLE LAKE DC CON Jooo y - CLAIM CNOVJ* ** TW PLAN : tooo i - MACNCTK JUtrVtT f HOU MMUM IO OtSTIWI lUMt O* P*O- K*i* AUOH* i* *oa *" IAST-WCST cuu** imcs

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4- 1 * S20a8NW9l7a 2.10*0 KAPKICHI LAKE 900 GEOPHYSICAL - GEOLOGICAL - GEOCIIEM1CAL TECHNICAL DATA STATEMENT

TO BE ATI ACHED AS AN APPENDIX TO TECHNICAL REPORT FACTS SHOWN IIEKF. NEED NOT BE REPEATED IN RETORT TECHNICAL REPORT MUST CONTAIN INTERPRETATION. CONCLUSIONS ETC.

Type of Survey fii*nphy*H Pftl smA Township or Area Kapkichi Lake M-2246 Claim hoifi.-r(s) Transtcrre Explorations Ltd——-——————. MINING CLAIMS TRAVERSED in? St-Catherine St.W. #910, Montreal no. List numerically Author of M-G. Tanguo tt Hr^ n Smi 13 Greenwood Rd. 917. Wilder ave. • •^•^'••'••M^wk^VtM***'****"**********'**"**"'****"**'PA - 287627 p* - 289636 St Thre Pt MflrtT f ffi !L\ j FA - 2S7B28 PA - 289637 Covering Dales of Snrvcy July 3 to 26/71 j March ?? tft AjvHI (linccultinx lo office) 21/^2 PA - PA - 289639 Total Miles of Line nn fi.4 mi nnA 27.7 mi rni p'A"-"2876"32"PA - 287631 'PA "-" 289641"

SPECIAL PROVISION'S DAYS PA - 287634 'PA "-"289643 CREDITS REQUESTED 'PA"-"287636" Geophysical PA -289645 40 'PA"-"287638" ENTER 40 days (includes 20 PA -269647 Illite cutting) lor tnsi —Magnetometer 'pA"^"2e764o' survey. PA -289649 4 -OiiuT 'pA"-"287642' ENTER L'O days for each PA - 289651 additional survey using ?.0 PA -'287644 PA - 289653 ni-iirlirmir.il, "PA'T'267646* A l R BO R N E CRED1 l S (Spit ial provision irrdiU do not apply lo airborne lurveyt) PA ~ 269655 MajjriClonu'ter.- . Radiometrii (ciiu-r days per claim) PA -287648 PA - 289657 PA - 287650 PA - 28*659 I)ATE:AiiJMSj.2J^-l222 . SIGNATURE; Al1"10' of K/'0" / PA,r...287.fc5,l...... PA..—2S0660. Marc C. PA - 280661 "TA'-'-Zfe'SfPA - 28962 PA -

I'lcvious Surveys JPA A -

PA - 289632 "S. Checked l*v———— — .dale™ "FA"-

•f. c;E(JI.O(;!CALBRANt:U. PA - 269673 *C^V Aiwrn'.i'i! l(\.- — -••'i r\ - i^ .pA——2^ \'\ ~ iS'jti??.!.

TWAl.C-l MM*i.- 78 GEOPHYSICAL TECHNICAL DATA

GROUND SURVEYS Number of Station* Mae (530H249) EM f48O4-1220i_____Number of Readings .—1429,..——————— Station interval———100*———————————————————————————————————————————————————— Line spacing____400*.——..—..—....^...—...—-———-—————,—--—...... -——^—----—..—..—-—.-.^ Profile scale or Contour iniprvah T* s 1QO ; l" a 4QO pnmnns; and 1000 gammas______. (ipccify for each type ol survey)

,MAGXKT1C Instrument ftharpe MF-3 and Asknnia torsion type______m______^.^^ Accuracy - Scale rnntiant 20 gammas and 2.1 cantnas______;______. Diurnal correction method datum continuously adjusted______Base station i..r;..i,.n at center of grid on baseline______;-——---^—-————-——-

ELKCI'ROM AGN ETIC Initirtimpni Tr^nstp't t.f.****; .^OQO flmp~t.iirn-ft? vith receiver ShflrpC 3^*~?00t and SP—300 ^yanscei,ver

Coil ronfiguralion Vertical lOQP______-... i! srp^ratioM 400 ft. (max. 800 and 1200)______A ccuracy Method: E Fixed transmitter and brol^s^niooii back D In line D Parallellinc Frequency I05Q hz and ICiQO hz.-———.--—^—-—.--..-.——-—..-.—.--.-—-.—^....^.—---——.— (ipccify V.I..K. tuiion) Parameters measured tilt anjgj.c______GRAVITY Instrument. Scale constant. Corrections made,.

Base station value and location.

Klevatiun accuracy JN'DV-T.KI) POhAKIX.-VllON RF.SISTlVl'i'Y

Instrument ______————— Time domain.————————————————————————————— Frequency domain. Frequency______———————————————— Range————————

Klecinule array Klectrtidf spacing. 'l') j)f of '-l (a)

Authors of reports Marc C. Tanguay, Ens.. Ph- (report of Jam/27/72) Con. Salamis, geophysicist (report of July 20th,X?2)

Dates of Surveys first survey (July - Jan.) a - Electromagnetic field 3/7/71 to 23/7/71 line cut. 1/7/71 to 14/7/71 office 1/6/71 to 20/6/71 1/9/71 to 26/1/72 b - Magnetic field 3/7/71 to 23/7/71 line cut. 1/7/71 to 14/7/71 office 1/6/71 to 20/6/71 1/9/71 to 26/1/72 c - geology field 3/7/71 to 23/7/71 line 1/7/71 to 14/7/71 office 1/9/71 to 26/1/72

second survey (July/72) field 3/25/72 to 4/21/72 office April to July/72

Instruments used

first survey EM. vertical loop at 1050 hz, transmitter flux 3000 amp.-turn, ft? receiver Sharpe SE-200 Mag. Sharpe MF-1 second survey EM. Scintrex SE-300 "transceiver" Mag. Askania torsion type.

Total expenditure; 55,000. and S6,203. Sil,203.00 Room W 1617 Parliament Building* Toronto, Ontario •4TARK) M7A 1X1 intetry Matura! 4161965-6918 January 29, 1973

Mr. W. A. Buchan Mining Recorder Court House Sioux Lookout, Ontario

Dear Sir: Re: Mining Claims Pa. 287627 et al, Kapkichi Lake Area. Pile 2.1000-——^—————

The Geophysical (Electromagnetic 6 Magnetometer) and Geological assessment work credits as listed with my Notice of Intent dated January 12, 1973 have been approved as of the date above. Please inform the recorded holder and so indicate on your records.

Yours very truly,

Fred W. Matthews Supervisor O J /nw Projects Unit

cc: Transterre Exploration Limited cc: Dr. Marc C. Tanguay cc: Resident Geologist Kenora, Ontario (a)

Authors of reports Marc C. Tanguay, Eng.. Ph.D. (report of Jan.X27X72) Con. Salamis, geophysicist (report of July 20th,X72)

Pates of Surveys first survey (July - Jan.) a - Electromagnetic field 3/7/71 to 23/7/71 line cut. 1/7/71 to 14/7/71 office 1/6/71 to 20/6/71 1/9/71 to 26/1/72 b - Magnetic field 3/7/71 to 23/7/71 line cut. 1/7/71 to 14/7/71 office 1/6/71 to 20/6/71 1/9/71 to 26/1/72 c - geology field 3/7/71 to 23/7/71 line 1/7/71 to 14/7/71 office 1/9/71 to 26/1/72

second survey (July/72) field 3/25/72 to 4/21/72 office April to July/72

Instruments used

first survey D4 vertical loop at 1050 hx, trai jmitter flux 3000 amp.-turn, ft? receiver Sharpe SB-200 Mag. Sharpe MF-1 second survey EX. Scintrex SE-300 "transceiver" Mag. Askania torsion type.

Total expenditure; S5,000. and S6,203. 511,203.00 v..- .- -'"5-^iii^^2^ :-- -1-,-^Jr^q,.g,^^tfSSft-vtti^ffXf-i^.LS^i^7^F^ ^^yf~ \ —Thi^ —— .—— ; — )— ——— l--- V& .'l Mt. t f*, t f*. * VK ~.?-'t ^'3^7^333®® s 'iioT7i;1**jrri .MSr V \ -' \ o'---}^?^\--^?i**S'il r———— - Hf—— ^ — lj ————*- r, - •r—— — ?H — — — l- — p*4*017SOirJ...oit.l ^T** |4*OZ* . o*•jffisaj44WJ2I r- **03t|L*iia^****^fe^grg i .k. ^k^. B A *y^ ———'--XF IT ~

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' PA1RICIA MINING DIVISION -- *-- *- - ~': '-'fr- SCALE: l-INCHrz40 CHAINS^ FOR

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.. LEGEND AND SYMBOLS

UNCONSOLIDATED QUATERNARY DEPOSITS i MORAINE , MUSKEG

METVOLCANIC ROCKS 287637 (METATUFFS, METARHYOLITES )

FOLIATED GRANITIC ROCKS.

DISSEMINATED SULPHIDES.

SCHISTOSITY OR SHEARING AND DIP

JOINTING WITH DIP.

BEDDING WITH DIP

FAULT

S-TYPE DRAG FOLDING

ASSUMED GEOLOGICAL CONTACT

RI3-I T-22 SAMPLE NUMBERS

X SMALL OUTCROP

OUTCROP AREA

CLAIM POST

SWAMP

M-41 TRAVERSES WITH J-43 —— }—DIRECTION

\ GROUND MORAINE \ \

GROUND MORAINE

TRANSTERRE EXPLORATIONS LTD.

PICKLE LAKE AREA PROPERTY

TWP PLAN No. M-2246

GEOLOGICAL MAP

CLAIM GROUP #4

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