ea15 JANES 010

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REPORTon

Property of TR1LLER EXPLORATIONS LIMITED

JANES TOWNSHIP SUDBURY MINING DIVISION

ONTARIO

lToronto, Ontario

D. W. Esson, P. En g.

September 25, 1968

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41 leSNWSiae? 8815 JANES 010f* ' --"

INDEX

SUMMARY l

PROPERTY Z

LOG.. iION AND ACCESS Z

TOPOGRAPHY Z

RESOURCES 3

HISTORY 3

GENERAL GEOLOGY 3

GEOPHYSICAL SURVEYS 5

MAGNETOMETER SURVEY 5

RESULTS OF MAGNETIC SURVEY 6

ELECTROMAGNETIC SURVEY 6

RESULTS OF ELECTROMAGNETIC SURVEY l

CONCLUSIONS 8

RECOMMENDATIONS 8

CERTIFICATE 9

ACKNOWLEDGEMENTS 10

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SUMMARY ;

TriDer Explorations Limited acquired a mining

property consisting of 17 unpatented mining claims in Janes

Township, Sudbury Mining Division of Ontario during early 1968.

This group of seventeen (17) claims is located in

an area of mafic rocks (norite) that are intrusive into metamorphosed

Huronian and Keewatin sediments. The identification of norite was

a result of thin section study of samples blasted from an outcrop

east of the Sturgeon River near the common boundary of claims

S 147 :-30 and S 147431 to the west of the subject property.

The company has recently completed a program of

line cutting, magnetometer surveying, test electromagnetic-4

surveys and is presently carrying a program of prospecting,

trenching and sampling. Particular attention is being paid to

areas of interest indicated from the geophysical work completed

to date and results of work completed on properties adjoining to

the east and west.

It is therefore recommended that stripping,

trenching and sampling be carried out to completion to allow an

evaluation for diamond drilling as warranted.

INTRODUCTION: f .-.\''~.

——— — — —— —This -report-was-authorized-by

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PROPERTY:

Consists of seventeen (17) unpatented contiguous

mining claim;; of approximately 40 acres each.

S 147435 to S 14744Z include S 147445 to S 147447 inclusive S 147416 and S 147695 S 147707 to S 147710 inclusiv ;

Total

8 claims 3 claims 2 claims 4 claims

17 claims

LOCATION AND ACCESS:

The claim group is located in the west central part

of Janes Township in the Sudbury Mining Division of Ontario near

the junction of the Sturgeon and Chiniguchi Rivers.

It lies l - 1/4 miles north of Chudleigh on the main

line of the Canadian National Railways which passes through the

s outhern part of Janes Township. It is readily accessible by a

good gravel road which passes through the property from Sturgeon

Falls or Warren on Highway 17. The distance fi^m Sturgeon Falls

by road is approximately 37 miles.

TOPOGRAPHY:

Generally rugged, particularly at the junction of the

two rivers with le cal relief of about 150 feet. Relief is due mainly

to ridges and hills of Precambrian sediments and sills and masses

•- ••;;--.: . - ";". ' ' -- - ;,v',. ^. ." - ; 3 ••'- •'"' ' /••. '. ••'" ' M '

of basic rocks typical of the area between Lake Temiskaming and

Lake Wanapitie.

RESOURCES:7

The district is timbered with secondary spruce,

pine, balsam, birch and maple. Local lumbering operators are

active. Power is available from the North Bay-Sudbury grid of

Ontario Hydro.

HISTORY:

Prospecting and some exploration has been carried

on for several years in the area, more especially in Davis Township

to the west.

Minor showings of copper and gold have been found

in quartz veins in crush zones in gabbro and old sediments in

Janes Township. A 30 foot shaft was sunk north of Sargesson Lake

one mile to the east but no values were reported.

This discovery of base metals in norite warrants

further investigation and the large areas of mafic rocks seen on

tlie property require careful investigation. This discovery of

sulphides in rock of the Sudbury type is the first known indication

in this area.

GENERAL GEOLOGY;

- -All the rocks in the area are Precambrian in.age.'/-' ,V/'- f —

' - 4 -

The Grenville Front crosses the southern part of Janes Township

and tlie Ess Creek Fault coincides with the Front. A relatively

strong north-south fault extends from Ess Creek up the Sturgeon

River and is evident in the field on the east side of the river.

The rocks south of the Ess Creek fault are Killarnean

(Grenville) and consist of granite gneiss, migmatites, amphibolites

and metasediments. North of the fault in the area of the property

the rocks consist of metamorphosed Cobalt and Keewatin sediments

intruded by diabase, gabbro, amphibolite (Sudbury gabbro) shown

as mafic intrusives on O. D. M. Map P-367(1966).

The mafic intrusives cover a large area in Janes

Township as were seen by the writer during field examinations

on June 24th - 25th and August 14th, 1968.

It is of particular interest to note that the large area

of mafic intrusives between Lake Temiskaming, Gowganda and

Sudbury, show variations in composition from quartz diabase

to quartz norite (Sudbury norite) with the latter type increasing

from northeast to southwest approaching the Sudbury base metal

area (see G. S. C. Memoir 95, pp. 88 - 91). As mentioned earlier,

a sample from a test pit on the common boundary of mining claims' 1. ",

S 147430-431 of an adjoining property has been identified as norite ,. . . -,y

of the Sudbury type. This sample showed from a thin section and :""; -,*/' -: .

polished section study to have 37c intersticial sulphides (chalcopyrite,'. ?X'/'. - i--.'-. '. , ,. .. ;. - . --.- ...---,- : : .-. .-'. ' -' - -- - '- v' .vj--,^'--^) 1"*'./^.^- .*" "

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-,-.:-, -. y,.-.. - :\,-- -. :, - --y, y- . -•••y-^-v.^ -: - - . --*:-j* ~^ - -^ - - fc'-^*^^^ V ^ , ; ,, .^, i-{^^k^^^:^!K;:iti

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pentlandite, pyrrhotite), 50"^ plagioclase, 4 Q 0fc hypersthene and

minor biotite, hornblende, chloritCi ilmenite and quartz (see

photomicrographs). The above determinations were done for the

Company by the Geological Survey of Canada and given to the

\vriter for his study.

It would appear that the large areas of basic intrusive

mapped as diabase and gabbro east-northeast of the Sudbury nickel

area warrant careful examination since they appear to be in part

related to the favourable Sudbury norite. Careful examination of

the larger intrusive masses or sills should be made for possible

magnetic segregation? within them which may contain concentrations

of base metal sulphides.

GEOPHYSICAL SURVEYS:

North-south picket lines were cut on the property at

intervals of 300 feet with stations established every 100 feet along

the lines. East-west base line controls were established.

MAGNETOMETER SURVEY:

A g round magnetic survey utilizing a Sharpe MF1

Fluxgate magnetometer was completed using the pre-established

picket line grid. The usual corrections for instrument drift and

diurnal variations were applied and readings were recorded to the

6 -

nearest 5 gammas. Technical details of the instrument used\

arc outlined in Appendix "A" bf this report.

RESULTS OF MAGNETIC SURVEY:

As will be noted on the accompanying magnetometer

map there arc at least four areas of magnetically high relief.

The first and most extensive of these extending

from cast of the Sturgeon River in claim S 147708 to the eastern

boundary of the claim S 147710 with a range of 2100 gammas or

some five times background.

The second area of high magnetic relief is located

in claims S 147695 and S 147707 with a east-northeast trend and

relief to 1400 gammas.

The third area of magnetic relief extends east-west

along the common boundary of claims S 147437 and S 147438 with

a maximum relief of 4000 gammas.

There are other smaller areas with lesser relief that

require further investigation.

ELECTROMAGNETIC SURVEY:

This survey was conducted in the areas of magnetic

relief utilizing the same grid pattern as was used for the

magnetometer survey. The instrument used -was the Ronka^ _,~*''.

7 -

E. M. 16 series and technical details relative to this equipment

are to be found in Appendix "B" to this report.

RESULTS OF ELECTROMAGNETIC SURVEY:

The accompanying electromagnetic map indicates three

(3) significant electromagnetic conductors both in the northwest

portion of the property and both related to areas of above normal

magnetic relief.

Conductor "A" is located on claim S 147438 extending

from Line 36E to Line 42E and trending generally in an east-west

direction. This particular conductive zone is known to extend

into the properties adjoining to the cast and west.

Conductors "B" and "C" located on claim S 147439

both extending from Line 36E to Line 42E and related to an area

of above normal magnetic relief. Bovh these conductors are known

to extend east and west into adjoi.ung properties.

The overall picture indicates the possible existence of

sulphide zones a nd requires that additional exploration be

undertaken.

CONCLUSIONS:

The results of exploration to date justifies the

continuation of the recommended program of stripping, trenching

and sampling. This phase of the program is currently underway

and will be reported upon separately.

Since the area is known to contain basic rocks

including Sudbury type norite and since it is known that copper

nickel sulphides are associated with these basic rocks to the

east and west of this property the property should be systematically

mapped geologically. This geological information along with the

information Irom the stripping, trenching and sampling currently

underway will provide ample information to recommend subsurface

exploration as warranted.

RECOMM ENDA TIONS:

It is therefore recommended that the stripping,

trenching and sampling be completed along with the systematic

geological mapping as set out in a report by D. W. Sullivan

dated April 23rd, 1968.

The results of the above will then provide sufficient^

information to initiate stage two of the program outlined in a

report dated April 23rd, 1968. *- ~ :;?^.x-',"~*'-:*:-' \ . .,. , ^ .. .. ..~ ~ R e sp~e ctf ally's u'Bmi tfed ,*^"

.,..- ,. ... . . . .. . . ,^^^-.;Vv : ;^^-^:^..-V.^:^^ ' •••^:-.v v- r -- -\- - ' : . .-•'.. ..'. - . /. .''

r.' ' -*'' ' ' ' ' .-'. - . ~ , -'. . . l- " 'l V '' J ".v -* ' ' . "' '.,. . ^-' v ' ' ' - ' ,. . *- ':'-- '-..'.;''.- •••. -^.''.. . '-r •'^." t:r'~- - •~'-'^'."-- .s,;..!.'.-.'.'^^-. -:'.- . -'..i.-'-- . - '' .'.-, --.'- --^ - .-- ' - r.j .: . -, . .--. . . ,v.:.; •'•'••-, v^:-''-:^ ; :^- ;; ' ; -^ J'"' ~V:.-o:i\.^'..'.?'-'"V.'" . . - ~ , . l:',' " - -..,-"- -'". "-".-- ". •• ;-- ' -'—: ;'; r-'--"-.--.- -v' •-.••.vr1 -^------ CERTIFICATE '""' '

I, Donald W. Esson, of the City of Toronto, in the County of York,

in the Province of Ontario, hereby certify:

1. That I am a consulting geological engineer and reside at 122

Dlythwood Road, Toronto 12, Ontario.

2. That I graduated from the University of Toronto in 1957 with

the degree of B. A. Se. in Mining Geology and have practised '

my profession as field geologist, mining securities analyst

and consulting geologist continuously since graduation with

the exception of the year' o2-64.

3. That I am a member of The Association of Professional

Engineers of Ontario.

4. That my ^eport on the Janes Township property of Triller

Explorations Limited is based on review of maps and reports

as listed in the attached Acknowledgements, on personal

visits to the property and surrounding area during June and

August, 1968 and on my specific knowledge of exploration

programs being conducted by others in the same general area.

5. That I have no direct or indirect interest, nor do I expect to

receive any direct or indirect interest, in the properties described

herein, I do not own beneficially, directly or indirectly, any, '"' :..-' .-•••^ -shares in Triller Explorations Limited, nor shares in any

, affiliate of that Company.' '

^r~DA"TErjr"at"T676nt6" this' 3 Oth"da"y"bf~SepternBeF," T96ST""

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ACKNOWLEDGEMENTS:

Ontario Department of Mines

Ontario Department of Mines

Report of D. A . Duff, B. Se. , P. Eng.

Report of D. W. Sullivan, B. Se. , P. Eng. , F. G. A. C .

Department of Mines, Geological Survey,

Ontario Depariment of Mines

Photomicrographs (4), Sample #BA-D-3

Report of D. W. Sullivan, B. Se. P. Eng. , F. G. A. C.

Vol. XL1 Part IV 1932

Geological Report 15, 1963

Dated November 13, 1967, Janes Township

Dated March l, 1968Janes Township

Memoir 95

Preliminary Report P. 367(1966)

Thin section and polished sections carried out by Geological Survey of Canada.

Dated April 23, 1968 Janes Township

APPENDIX "A"

VERTICAL INTENSITY FLUXGATE MAGNETOMETER MF-1 SPECIFICATIONS

Model MF-1 Standard surveying and prospecting magnetometer with self-levelling sensor.

Ranges: Plus or minus - l, 000 gammas f. se. 3, 000 "

10, 000 " 30, 000 "

100, .000 "

Sensitivity: 20 gammas per div.50

200 " 500

2000 "

Meter: Taut-band suspension, l, 000 gamma scale: l 7/8" long 50 div.3,000 " " l 11/16" long 60 div.

Accuracy; l, 000 to 10, 000 gamma ranges - 0. 57r of full scale 30, 000 to 100, 000 gamma ranges t I 07r of full scale

Operating Temperature:

Temperature Stability:

Bucking Adjustments;

o o-40 C to 40- 400 F to 1000 F

Less than 2 gammas per C {l gamma/ F)

10, 000 to 75,. 000 gammas by 9 steps of approximately 8, 000 gammas and f'ne control by 10-turn potentiometer. Convertible for Southern hemisphere or i 30, 000 gammas equatorial.

Batteries: 12 x 1. 5V - flashlight batteries ("C" cell type)(AC Power supply available)

Consumption:

Dimensions:

Weights:

50 milliamperes

Instrument: 6 1/2" x 3 1/2" x 12 1/2" - 165 x 90 x 320 mm

Battery Pack: 4" x 2" x 7" -- 100 x 50x : " -180 mm - i

Shipping Container: 10" dia. x 16" -255 mm dia. x 410 mm

Instrument: 5 Ibs. 12 o z. - 1. 6 kg. Battery Pack: 2 Ibs. 4 oz^ - l kg. ^^ Shipping: J3 Ibs.

. . :'. . APPENDIX "B" '

PRINCIPLE OF OPERATION (RONKA EM 16)

The VLF-radio stations operating for communications

with submarines have a vertical antenna. The antenna current is thus

vertical, creating a concentric horizontal magnetic field around them.

When these magnetic fields meet conductive bodies in the ground, there

will be secondary fields radiating from these bodies. This equipment

measures- the vertical components of these secondary fields.

The EM16 is simply a sensitive receiver covering the

frequency band of the new VLF-transmitting stations, with means of

measuring the vertical field components.

The receiver has two inputs with two receiving coils

built into the instrument. One coil has normally vertical axis and the

other is horizontal.

The signal from one of the coils (vertical axis) is first

minimized by tilting the coil. The tilt-angle is calibrated in percentages.

The remaining signal in this coil '3 finally balanced out by a measured

percentage of a signal from the other coil, after being shifted by 90 .

The axis of this coil is at right angles to the axis of the first coil.

This coil is kept normally parallel to the primary field.

Thus, if the. secondary signals are small compared to .

the primary horizontal field, the mechanical tilt-angle is an accurate

measure of the vertical real-component, and the compensation~IT72-

-coil-itr-a

SPECIFICATIONS

APPENDIX "B" (Cont'd)

Primary field:

Frequency range:

Station selection:

Measured field:

Accuracy of readings:

Range of measurements:

Output readout:

Batteries:

Size:

Weight:

Accesso ries:

Horizontal from any selected VLF- transmitting station.

Approximately 15 - 25 kc.

By plug- in units. Two stations selected by a switch on front panel.

Vertical field, in-phase and quadrature components.

- l^r resolution.

In-phase -150ft or -90O , quadrature -

Null-detection by an earphone, real and quadrature components from mechanical dials.

6, size AA penlight cells, about 200 hours.

Life

16 x 5. 5 x 3. 5 in. (42 x 14 x 12 cm).i

2. 4 Ibs. (1. l kg).

l earphone and cord, l carrying bag. l set of batteries.

1 Manual of Operation.2 plug-in units for station selection

-- additional optional units available.

ea 15 JANES 020

SUMMARY H K POUT

Property o fJJ .

ONTARIO

Toronto, Ontario

SUMMARY

j The following summary is provided by D. W. Sullivan, P. F,ng. ,

F. G. A. C. whose full report is available in the Public Files of the |( '

Ontario Securities Commission.

•' Triller Explorations Limited has acquired by outright purchase

a contiguous group of seventeen (17) unpatcntcd mining claims in the west

central part n t T ™" * Tfl^il ' '"f* 1*"*1*^'"- -" Mining Division of Ontario.

j They aro known more precisely as follows:

S147435 to S147442 inclusive 8 claims^ S147445 to S147447 inclusive 3 claims

S147416 and 5147695 2 claimsS147707 to S147710 inclusive ^4 claims

17 claims

The claim group is readily accessible by a good gravel road

j which traverses the central part of the property. This road joins

Highway 17 at Sturgeon Falls and Warren. It is 37 miles by road from'''i•^ Sturgeon Fa 11 B. The C. N. Railway passes through .the southern part of

fi! Janes Township.V '•f

HISTORY--A " ™ '———"*~™

•tt; ."i•— P rospecting has been carried out in this general area foi

; j several years but no early work has been'reported on this property. In

tho fall of 1967 a small pit was blasted on a sulphide showing in maficfi . 'U

' reckon tho common boundary between claims S147430nnd S147431 a

^'i - v '

t) quarter mile west of claim S147438. The latter claim forms part of the

property under consideration here. Y

sri '-: ; ' - ^-" '-. " '''- .-''l' -' -. ; ' ' ' "' -. -' -'- - 'V-l?t'*4''i5*. ̂if]-'"1'- •'••' ' :- .' "' v'" -v' ''" . ' '. ' ,. ' ' " ' - - " ' . ' ' '-'' -" - '^^V.S.-iltf*aiHj.:-V, , . ^: : ' -- '-..-' '"'v-y^ -''-: .- '-' '-' :- ;; f' :!:'"' -' ••;" v - -Vv " .V.:/ ' " : ;":.;."':,; .; ^VS^f^

d-.i

Microscopic examination of this milphidc bearing rock by

the Geological Survey of Canada indicated the rock to bc a norite similar

to the Sudbury norite which is known to contain copper and nickel sulphides.

Similar ui.sic roe.k v,a.^ seen by the wriler in the area of the claims during

a p*;rs'j:,ai visit February 2 ?., l 9oR.

i-Oj^'l-' ; S iO ̂ ' S.

On the basis of the presence in the area and immediately

adjoininz; the property of favourable mafic rocks some of which hiive

been identified as norite, the property is considered worthy of careful

exploration lor economic roneent raiion.s of hajie metal .sulphide.';.

RECOMN1ENDATIONS

It i .s recommended ihat the entire properly be geologically

mapped and any promising occurrences of sulphides be trenched and

sampled.

It iff also recommended that the whole claim group bc

covered by a geophysical magnetometer survey on lines cut at 300 foot

spacing and readings taken every 100 feet,

A t est programme of electromagnetic geophysical surveying

should be clone over any showings.

•. v; ';. - ••••'"!-:-:^f^"'. ;'~ -" ~- : ••-••~ , - ' ' - - -''-l?."-''^''-'''"'" c ' ' ;'.'.''.V."^^- ;- *' - '.-•.,: ; -' -- ; ; -, - - " ••v; . .., - - :' ' T -

- 3 -

The estimated cost of the above exploration is as

Lin c cuttingsurvvy

mappinj; Trenciiinc nnd sampling Electromagnetic test survey

Total estimated cost

5\ , 7 00. 00 ?, , .3. 0 0. 00 J , j Ut). DU 2, -t 00. 001,300. 00

__ o 00. 00

^10, OOP. 00

•l

If t}ic above exploration should indicate that diamond

drilling is warranted, the following cost estimate is recommended:

l, 5 00 feet nf diamond ('rillinf,at S o. D O /f t. :j,|-5, OUO. 00

Engineering nnd contingencies 2 , 5 00. 00

Ki-speclfiilly submitted,

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D. W. Sullivan, P. Eng, F. G. A. C.

- 4-

CERTIFICATE

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1. IX V,r . SULLIVAN, of the Township of Esquesing, in the County o f ll.xlton, Province of Ontario, hereby certify:

L That I am a Mining Engineer and re.sidn at R. R. //3, f'lh Line, Georgetown, Ontario.

2. That I am a graduate of Queen's University with a B. Se. degree and that l have been practicing my profession as a Mining Engineer for the past luenly years.

3. That I have no interest, cither directly or indirectly, no r do I expect to receive any interest, cither directly or indirectly in the property of Trillcr Explorations Limited or any affiliated company.

•l. Thai I do not beneficially ov-n, either directly or indirectly, any securities of Triller Explo rationa Limited o i4 any affi liated company.

5. That the following report is based on a personal vir-it to theproperly on February ?.?.nd, l 9'iH and upon available geological reports and maps of the general area. Photomicrograph:; of the rock types and sulphides were given to the writer by the O.mpany for his study.

6. That J am a member of the Association of Professional Engineers of the Province of Ontario and ilia Geological Association of Canada.

Oi

Dated this 23rd day of April, 1968.

D. W. Sullivan", B. Se, , P. En g. F. G. A . C.

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"M"

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AC K N1 0 W LE DO EM E N T S

Ontario Dopnrtmeiit of Minos

Ontario Department of Mini's

Vt.il. X IJ Part IV 1932

Geological Report 13, 1963

Report of D. A. Duff, B. Se. , P. Y.n*. , dated Novel n bo r 13, l l)67,Janes Township

j'if:;.orl of J). \V. Sullivan, li. Se. , l\ Kn;;. , F. G. A. C. dated March l, l O o S.laiii-ri Township

Department of Minos, Geological Survey, Memoir 95.

Ontario Pv-pa rt mont of M inns Preliminary Uuport p, 367(1966)

l ^jHiiunnc roi; i-a|)lis ( -t), Sample : ;' A- D- i. 'i'hiu :.i-c't:on anrl si'c t loii.s carru'd out by Cleolo^jicti! Survey ol ('a.'i.uM.

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