DIGHEM SYNDICATE ONAMAN JOINT VENTURE SOUTH … · 2017. 1. 17. · Thin inatruioont Bjeaauree the...

2.3334 COUGHLAN LAKE 010

i" -''

PROJECTS UNIT

BIMKS

DIQHSM SYKDICATZ

SOOTH OgAKAK HR8A

PKOKHBBK 29. 1.976. PUDIPIM AND COMPANY

3?be property on which tba preaant aurvay out ie ooapriaad of tbt following 30 '

Mt .LTiJu ;: -- ; :...... . - . ;-.-.Total area of tba olaio* liatad li about 1560

The olaiwft art loontefl in th* Soutb Ojiwwn River nbout 8 ra! l a e west of the weat*8*atr*OL Bay of Onaman fffeimdor Buy Mining Dlvitlon, QttHili**'."

The Village of Beardaoro i* about 30 oilo aoutb-eouthwoflt of the property, on tttmi Oanadft Higbirtiy So, 11," i '- : ' ' " - *4"' . r . .\ . . .

The property aay bil fraaeboa by grate! road via High way No. 301 and Abitibi Pa pa r Oo* road nortb f roa Highway 11 and 801 function, for ?5 olloe, tbaw 11 ailta uortbaaatward on Abitibi Paper Co, f.revel road *rtiidb oroaBaa th* property, A network of haulage roade occur on the proparty Wbiob at pree*nt it baing horveoted ,ot

property le loontad vitbin a band of wata vol- oanio and eodiwentsry rooks whiob nay b* Intarpratad aa tha folded l iwb joining two aa 4 or volcanic belt* ~ tbo Armstrong ~ Kowkaeh and tho Bonrdmor* - Garaldton belts*

f ha rooke in tha aran of tb* property ara ooopriead

largely of intermediate to baeio toloanlo f low* and atea, with 00910 tuffs end fragaOTital*. BOO* rhyolitlo tufffl ero looslly present* Seat interflow tediaenta and lyon for mation alto occur*

the property is largely underlain by intermediate volcanic rooke. They strike it* i north-south direction, paral leling the oontoot of a granitic batholith underlying the area to the east. ?he contact le bvlievtd to lie within the prop erty, itesr the eaatern boundary,

A north-south baseline vius out aoroft* the property, ooftt-weat picket linea at 200 ft* intervea*,

Readlnge vert tmken along the picket liuee at 100 ft* intervale,

The intruffient uaed wafl im ABKK, Denlgun, hori*ontal loop type eleotroiaognotic unit at a ooil *eparatiou of 200 ft. end eaploylng a frequency of fto^O H*/

Thin inatruioont Bjeaauree the 'In Jhose* ejid 'Quad- - returo 1 ootapononte of the aeooadmry eleotroBagnetio field net up in the preoence of a conduct or* Head ing e are plotted ae ft direct percentage of the primary field at the receiver* The receiver it ooa&eeted to the trenemitter by a reference cable which allows total f i aid at the receiver to be compared with the primary field,

In general, * conductive gone will produce a pea- it ive responae near the edgea aad a wegatlve reaponee over m conductor.

Results are plotted on eoooffipanylng Plane 158 and 159 on a eoale of l in* to 200 ft*

Peg*.,.3

Readings, other than background or vbat i* inter preted a* 'noise', ar* profiled on a scale of l in, to ttJC, In-Phase reading* art pi otto a on the loft tide tf tilt line, Quadrature on the right*

A total tf t* conductors vtvt located by the survey, varying froo one-line indiofctions tt about 690 ft, long whioh re designated lo4 o t -f 2 for r+foronoo purpotti* not in or- dtr tf priority, In tAittittt* ttftftl wook, narroir, ntrfinal ooourranots of conductivity oootur*

Conductor 1 i* about 500 ft* Itag* It uppotro tt tt oomptood of up tt 3 ttfttftf partiotdwrly on lin* W* It it of foir to eood qunlity on tint i8f Ittt oo on lino* 8S and 103*

Conductor 2 it about 600 ft, long, foirly narrow, of gocd quality on linoi tS mnd 48, lo*t on lint *0, It it flan ked by tatb *Uo by parallel oonduotor* of poor pnatt-ratio,

Conduotora 3* ^i 5 *nd 6 ooour stft or loaa along trikt tf tooa ttbtr in nortn-touth trtading tone of higher, irregular Magnetio9. they are moderate tt itrong oonduotera vith generally good phaae imtitt*

Conductor 7. it about 4tO ft* long, noderote tt weak with fair pheee ratio.

Conductor 0 it about 250 ft, Itng, it narrow. It occur at the edge tf t nngnetio anomaly. Pbaie ratios ore fair tt poor*

Conductor 9 it about BOO ft, long, variea up tt poo* aibly 60 ft, wide in placet. It ttrlkoa north-touth, except for the northerly end which ewinga northwest. It ia tf good quality on linea 503 and 52if leat ao on the remainder. It generally follow* ft aagnttit anomaly.

Conductor 10, fairly tRall, but of good quality on lint W58, ooderate etrength.

Conductor 11 about 500 ft* long by 150 ft, wide,

4

mod ore t o atren&th, oooura in a wsgnttio low,

Conductor 12 i narrow, strong on linea J&B, 568 and 56S. Xt oooura along the en B t Bide of a band of probable Iron Forme t ion,

Conductor 13 of fair atrongth and Quality, i* narrow on line 688, Lines 668 ond 6fc8 were not run due to forest oper- atlona at time of survey* fhie anomaly could extend further northward B.

Conductor 14, fairly narrow, strong on line 688, good quality, oooure along a bend of probable Iron Forme t i on, AB C-13, it probably continue* northward,

Conductors 15 and 16 one line occurrences, about 50 ft, wide, fair phase ratio*

Conductor 17, narrow, week,

Conductor IB, narrow, moderately atrong, good phase ratio*

Conductors 19 and 20, weak, probable bedrock topo graphy,

Conductor 21, one-line ooourranoe, possibly up to 50 ft. wide but not clear, le aeeooiated with a email magnetic anomaly.

Conductor 22* generally wide, weak scattered e one. It ooinoidea roughly with a moderate to weak magnetic anomaly, probably disseminated sulphidea with *oae magnetite.

It i ei recommended that all enoraeliea of Moderate to strong conductivity, where pbaae ratios are fair to good, (iet where Out-Phaae value doea not approach oloae or surpnee In* llnaee) ahould be further inveatigated, fhia ehould take the form of overburden drilling and sampling, or by etripping if found feaaable*

asv

aq ^Cq p*AtdS9Jt aq ^ouuuo eao^onpuoo poo^

s u a y it JP A t

work woe carried out froa August l? to Sgptcflaber ? inol,,

A total of 56.5 mi* of picket lin* wtre traversed in the sur vey, involving **,363 reading**

Personnel involved in carrying out the worki

Fiold t J. Bosum, C, Wcpnoh, A4B. Pudifin, Val t*Or, Qu*,

Draughting and officet B, toodtr,W* Peiga,

42L03SW0013 2.2334 COUGHLAN LAKE

!

020 MAR ,. -, u, ,

PROJECTS .UNH

REPORT ON

MINERAL EXPLORATION PROGRAMME

ONAMAN LAKE AREA, THUNDER BAY MINING DIVISION

ONTARIO

JULY-DECEMBER, 1976

FOR

DEJOUR MINES LIMITED-DIGHEM SYNDICATE JOINT VENTURE

(M.E.A.P. CONTRACT G.B.-61)

R. E. Routledge, M.Se.

January - 1977 Toronto, Ontario

This report may not be reproduced, in whole or in part, without the written permission of Derry, Michener ft Booth.

DEKRY. MICHENER ft BOOTH

12L03SW0013 2.2334 COUGHLAN LAKE

TABLE OF CONTENTS

020C

Paee

INTRODUCTION

LOCATION AND ACCESS

PROPERTY STATUS

HISTORY

EXPLORATION PROGRAMME

REGIONAL PHYSIOGRAPHY-TOPOGRAPHY

REGIONAL GEOLOGY

PROPERTY GEOLOGY

MINERALIZATION

MAGNETOMETER SURVEY

LIST OF ILLUSTRATIONS

Location Plan

Table of Formations

l

1

2

2

4

6

6

7

10

11

Following Page l

Following Page 8

LIST OF APPENDICES

A - Schedule of Claims, Thunder Bay Division

B - Sketches of Basal Overburden Sampling Locations: Conductors D-2, D-3, D-10, D-20, D-24.

C - Description of Lithologic Units

D " Results of Geochemical Analyses

LIST OF MAPS

Map l - Geological Compilation (North and South Sheets), Scale 1'^ 200'. (In Pocket).

Map 2 - Magnetometer Survey (North and South Sheets), Scale 1'^ 200'. (In Pocket),

L)riii\'Y. MICili.'NKR ft BOO'll-i

INTRODUCTION

At the request of Dejour Mines Limited, Derry, Michener Et Booth

carried out a programme of line cutting, geological, electromagnetic and

magnetic surveying and basal overburden sampling on behalf of the Dejour

Mines Limited-Dighem Syndicate Joint Venture. This programme was undertaken

on the Joint Venture property situated in the vicinity of Onaman Lake,

Thunder Bay Mining Division, northwestern Ontario, during the period

July 7, 1976-December 8, 1976.

LOCATION AND ACCESS (Long. 87 O39'30"W; Lat. 50O00'00"N; (Figure 1) ~ N.T.S. 42/L/4; 42E/13)

The property straddles the common boundary between the south-

central portion of the Coughlan Lake area (M1409) and north-central portion

of the Castlewood Lake area (M1850), approximately 25 air miles north-

northeast of Beardmore. Excellent all-weather road access to the property

is achieved by travelling 15 miles east on Highway 11 from Beardmore to

the intersection with gravelled Highway 801, the Paint Lake Road. Highway 801

is then taken north for 29 miles to a junction near Abitibi Camp 40, thence

12 miles east and northeast, on the Tashota Road which traverses the northwest

portion of the claim group. Alternatively, the Domtar Pulp Company Camp 58

access road departs from Highway 11, 5 miles east of Jell leo, and reaches

the Tashota Road, approximately l 1/2 miles east of the Abitibi Camp.

Good access on the property itself is provided by numerous lumber/

winter roads branching from the Tashota Road as well as from the West Bay

Road, immediately south of the claims, and the Abitibi Company haulage roads

nos. 8 and 9, constructed during the summer of 1976.

n'l-.RR'f, f.'iciu i\!i:.K ft BOOTS;

- DIGHEM PROPERTYAUDEN TASHOTA

—A

VDomtar Cp SB

JELLICOE GERALDTON

LAKE SUPERIOR

Thunder f J a y7

LOCATION KHY

2

PROPERTY STATUS

j The property, covered completely or in part by the explorationl; programme descr ed herein, comprises 40 contiguous mining claims, the

; bulk of which were staked by D. Thorsteinson and N, Cox of Beardmore in

; July 1975 and subsequently transferred to Lynx-Canada Explorations Limitedl

j as nominee for the Joint Venture. A list of the claims, expiry dates andl

ownership is provided in Appendix A.

HISTORY

The region has been prospected for gold since the early 1900's

and numerous showings were discovered through the 1930*s. Small, old

prospecting pits on barren quartz veins at several locations attest to this

initial exploration on the claim group.

Located approximately four miles north of the property, the Tashotai1 Mine, the only mine in the area, produced some 50,000 tons of ore containing'

! approximately 13,000 02. of gold, 15,000 oz. of silver and 510,000 Ibs. of

' copper from 1927 to 1929 and from 1934 to 1937.

', In the early 1950's a sub-economic lead-zinc deposit was discoveredl

on the Headway Red Lake Gold Mines Ltd.-Coulee Lead 6* Zinc Mines Ltd. property,

about one mile to the north of the claims.

Palomino Explorations Ltd. drilled a total of 1,107 ft. in two

holes, numbered 67-1 and 67-2, following a programme of ground VLEM and

magnetometer surveying on the west-central portion of the property during

1967. Hole 67-3 intersected massive pyrite and pyrrhotite (sulphide iron

DI K'K'V. MICHF'K'l-.H t- BOOfM

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formation) within "Temiskaming metasediments" close to their contact

with basic volcanics on the western margin of the claim group. Hole 67-1

investigated Dcjour-Mghcm HLEM conductor no. D-10 and intersected a shear

zone in "gabbro" but only trace sulphide mineralization.

As part of a larger programme to re-evaluate the Headway-Coulee

and adjacent grounds during 1971 to 1974, Noranda Exploration Limited

carried out geological mapping, geochemical soil and silt sampling and

magnetic, VLF and VLEM geophysical surveying on a scale of l" s 400' on

the northern half of the property. This was followed by 881 ft. of diamond

drilling. Two holes, numbered H72-3 and 7 on the northwest portion of the

property, intersected sulphide iron formation consisting of barren, massive

pyrite-pyrrhotite and minor interlayered magnetite hosted by felsic

volcanics. A third hole, H72-8, on the north-central margin of the claim

group tested thin bands of Cu-Zn-Ag mineralization in quartz veins and

silicified zones within mafic volcanics.

j The southern half of the property was covered only by reconnaissance

; geological mapping along claim lines. The Noranda claims lapsed in July

1975 whereupon the ground was restaked on behalf of the Dejour-Dighem Joint

Venture.

Recently, in late 1975, two small Cu-Ag-Au deposits were discovered

approximately one-half mile north by the Lynx-Canada Explorations Limited-

Dejour Mines Limited-Canadian Reynolds Metals Company Limited Joint Venture.

This find precipitated a minor staking rush and prompted such companies as

Amoco, Mattagami Lake Mines and Mcintyre Mines to commence exploration in the

i immediate area.

n'.UiiV. r,',ir.HF.-:Ni:.r\

The exploration programme was designed specifically to detect

and evaluate small disconcordant or subconcordant Cu-Ag-Au bearing massive

sulphide bodies of the type discovered in the mafic metavolcanics on the

Lynx-Dejour-Reynolds ground to the north. Exploration on the property

consisted of close interval line cutting, detailed geological, magnetometer

and horizontal loop electromagnetic surveying over the newly cut grid,

followed by a limited amount of basal overburden geochemical sampling.

Contract: line cutting was carried out by Phil Blaze Enreg. of

Rouyn, Quebec under the direction of Alcide Thibault. During the period

July 7-August 6, 1976 a grid totalling 64.7 line miles was cut, including

a 9,600 ft. base line, 2 tie lines and 49 cross lines cut at 200 ft.

intervals. Following line cutting, a magnetometer survey was conducted by

A. Koskela of Thunder Bay and R. E. Routledge of Toronto between July 20ij "nd September 28, ]97^.

j From August 15 to September 3 and September 29 to October 18, 1976,il R. K. Routledge carried out detailed geological mapping on a scale of

l" = 200'. Mapping was terminated following heavy snowfalls and this

resulted an a small portion in the east-central map area remaining only

reconnaissance mapped. In addition, the grid had been cut over during

logging operations causing slow progress in this area and to the west.

Pud i f in S Company of Val d'Or, Quebec, under sub-contract to the-

Joint Venture, carried out 58.5 miles of HLEM surveys from August 17 to

September 7, 1976. With the exception of lines 64S and 66S, which could

hi I-;!\'Y. MICI-llINt/K l- UOOTrl

- 5 -

not be surveyed due to active logging operations in the vicinity, a total

of 4,365 readings were completed on all cross-lines employing the A,B.E.M,

demi-gun at a coil separation of 200 ft. and transmitter frequency of.

2640 Hz. Pudifin tt Company's covering report and maps for the HLEM survey

are attached separately.

Basal soil overburden sampling,using an Atlas Copco rock drill

and soil sampling kit, was undertaken by prospectors Thorsteinson and Cox

from November l to December 8, 1976, whereupon this survey was discontinued

because of extremely low temperatures and adverse snow conditions. Depending

on the length of the conductor to be tested, a tier,or more,of holes were

drilled from up to down-ice across, as well as on the conductor, to detect

ionically and clastically dispersed base and precious metal mineralization.

A total of 29 samples over conductors D-2, 3, 10, 20 and 24 were collected

by this method and analysed for Cu, Pb, Zn, Ag and Au by Bondar-Clegg S

Co. of Ottawa. Anomalous values of 380 ppm Pb in the vicinity of conductor

D-2, and values of 580 and 122 ppm Cu, 120 ppm Zn, 2.0 and 3.0 ppm Ag over

conductor D-24, were the only results which could be considered significantly

above background. Unfortunately, conductor D-24 is west of the property

boundary on Dighem Syndicate ground and conductor D-2, by geological and

geophysical inference, is suspected to be iron formation. Sketch diagrams

showing the location of basal overburden sampling points for the conductors

tested and a tabulation of Bondar-Clegg analyses are attached as Appendix B.

Ni'iuir,', wich! Nt.f; ft HOOT 11

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REGI ONAL PjIYSI OGRAPllY-TOPOGRAPHY

Topography in the area is typical of other Shield terrain underlain

by Archean greenstone. Relief is relatively low, seldom varying in excess

of 50 ft. Extensive strip cutting in 1970-1971 and current total cut

logging operations by Abitibi Pulp S Paper Company have removed much of

the spruce, balsam, poplar and birch forest in the area and, in particular,

in the southern half of the property. Outcrop is sparse, approximately

5% of surface area, and in general bedrock is covered by thin glacial

overburden composed of till, outwash, glacial lacustrine and glacial fluvial

deposits, ranging locally to a depth of 60 ft. Glacial ice direction,

deterr.ined from bedrock striae and chattermarks measured on the property,

vary from 240 to 264 . Limited recent fluvial sediments, swamps and marsh

border the fault-controlled streams which flow north and west to join the

South Onaman River and eventually the Lake Nipigon-St. Lawrence River regional

\ drainage system.

The c] aim group lies within the south-central portion of a north

to northeast trending Archean metavolcanic belt. This greenstone belt

extends north to Oboshkegan Township where it widens and joins the east-

west trending O'sullivan Lake-Caribou Lake belt, and south to Conglomerate

Lake where it widens and bifurcates around a felsic stock, eventually

joining the east-west Beardmore-Geraldton-Long Lac greenstones, some 20

miles south. In the vicinity of the property the belt is approximately

DFKUY, MIOHI'N^R fv BOOT!!

- 7 -

2 3/4 miles in width and is bounded on the east and west by batholiths

ranging in composition from biotite-quartz-monzonite to trondhjemite.

In general, the metavolcanic rocks of the area comprise maf ic ' f lows

with intercalated mafic tuffs, occasional oxide and sulphide facies of iron

formation, and rare thin dacitic tuff and agglomerate layers. Centred

within the mafic volcanics is a I/A mile wide band of intermediate to felsic

flows and pyroclastics exposed on surface to the north and along strike for

about three miles. To the south the felsic rocks are represented by two

narrow bands separated by mafic volcanics. On the west, the felsic rocks

are unconformably overlain by metaconglomerates exposed in the vicinity of

Conglomerate Lake, and Con Creek areas, which extend as far north as

MacDonald Lake. The belt appears to be synformal and isoclinally folded

about a southwesterly plunging axis. It has been proposed by Thurston

(1972) that the trace of the axial plane on surface coincides with the

band of felsic rochr.. Volcanics j.n the area have undergone region 'i T

metamorphism to mid to upper greenschist facies, except adjacent to their

margins with granitic intrusives, where the grade may approach almandine-

amphibolite facies.

LJ^J11 Y J^LOGY (Map //l)

Bedrock exposure on the north half of the Joint Venture property

averages about \7a . South of the west-flowing creek, which bisects the

ground, outcrop approaches Id-15% of the surface area, particularly in

the central portion of the map area where concentrated logging operations

r* [soon i

- 8 -

have stripped the forest and overburden covering. The higher ground and

outcrop density in the south possibly suggests transverse faulting in

which the northern half of the property represents the down-thrown block

with the creek physiographically marking a location of a buried consequent

or resequent fault scarp.

The property is underlain by Archean rocks largely comprising

north trending, steeply westerly dipping, mafic metavolcanics of basalt

to andesite coriiposition. These are intruded in several localities in the

east by diabase sills and along the entire eastern property margin by the

batholith of granite to quartz-monzonite.

Although rarely exposed, narrow bands of dacitic pyroclastic rocks

are intercalated with the mafic flows and vary in texture from the lapilli

tuffs and tuff breccias to blue quartz-eye porphyry. Intermediate flows

within the mafic volcanics in the east-central map area are distinguished

from the mafic volcanics by harder, apparently more siliceous, character

l of the aphanitic surfaces and the blocky nature of weathered surfaces.

Enclosed within the mafic volcanics to the west, amygdaloidal

intermediate flows occur on the hanging walls and footwall s of a 100-150 ft.

wide quartz-feldspar porphyry dacite quartz muscovite schist unit,

stratigraphically and lithologically correlatable to the Headway-Coulee

felsic rocks, hosting the lead-zinc mineralization to the north. Well-

foliated to sheared amygdaloidal dacite flows underlie the western margin

of the south half of the property and continuity is traced by sparse

outcrops of dacitic to rhyodacitic pyroclastics and diamond drilling to

l

LJi.HI.'Y. MIOHLNi.K fi; DOOTH

TABLE OF FORMATIONS

PRECAMBRIAN

6 Mafic intrusive rocks

a Diabase sill, fine to med. grainedfresh to amphibolide

b Diabase sill , porphyritic 6/or withrosettes of plagioclase (glomeroporphyritic)

c Diorite dyke

Felsic intrusive rocks Granite to quartz monzonite

Metasedimentory rocks

o Conglomerateb Chert, thinly beddedc Magnetite-quartz iron formation, chert

with hematite partings on bedding planes, lesser greywacke 8i siliceous tuff.

d Arkose, conglomeratic arkose, interbedded tuff breccia a orkosic tuff.

Felsic metavolconic fi pyroclastic rocks

a Quartz — feldspar po.rphyryb Amygdaloidal dacite; foliate to shearedc Quartz - muscovite schistd Dacitic to rhyodacite lapilli tuff to tuff brecciae Cherty dacitic tufff Dacite

Intermediate metavolcanic rocks

a Andesite; massive to foliateb Andesite; pillowedc Andesite to dacited Andesitic tuffe Amygdaloidal andesite

CDa b c d e fgh

Mafic to intermediate metavolcanic rocks

UnsubdividedBasalt to andesite; massive to foliateBasalt to andesite; pillowedBasalt to andesite ; schistose, shearedBasalt to andesite; porphyritic to porphyryBasalt to andesite; amygdaloidalChlorite-- talc schist (ultra mafic?)Mafic tuffBreccia , (flow?)

- 9 -

tuffaceous arkosic metasediments in the. northwest. The felsic rocks are-

succeeded to the west by mafic volcanics which are in turn unconformably

i overlain by a polymictic metaconglomerate. A detailed description of theii principal rock types j s presented in Appendix C.

; Measured attitudes of schistosity in metavolcanic rocks arelconsistently NNW-SSE at. 60-75 westerly dip. This direction is sub-parallel

to the bedding of intercalated cherty iron formation, generally striking

10-20 more N-S than schistosity,in unconformably succeeding volcanic flows.

The penetrative foliation transects the N-S trending rock units, a

reflection of folding on a regional scale, whereas the apparent cross-

striking relationship of lithologic contacts and bedding of cherts to the

regional trend is probably the result of smaller amplitude asymetrical

folding.

Drag-folding and/or transverse shearing observed in outcrop is

evidence of E-W faulting in two locations, 11S/13E and 86S/7E,, -uid

' NW-SK faulting at 17S/17W. The latter aligns with a major lineamentij which traverses the property to the southeast. Additional assumed

faults are interpreted from apparent displacement of locally restricted

lithologic units, such as the breccia at 86S/19K, and by displacement or

abrupt termination of local magnetic patterns in areas mantled by overburden.

Three separate units of oxide-facies sedimentary iron formation

within the mafic, volcanics have been identified in outcrop and a fourth

sulphide-facies iron formation within the most westerly band of felsic

rocks has been previously established by diamond drilling. The easterly

rNtcf* tt BOOTH

- 10 -

band of cherty and magnetite-quartz oxide facies iron formation can be

traced magnetically and electromagnetically north to sulphide facies iron

formation outcropping on the Lynx-De jour-Canadian Reynolds Metals ground.

Virtual lack of magnetic expression, which verifies the absence of iron

oxide or sulphide mineralization in exposures of the westerly band of

cherts, suggests this may represent silicate facies. Under classic

concepts of Archean basin development in which oxide grades to sulphide

facies iron formation towards the basin centre, the greenstones appear to

be synformally folded about a southerly plunging axis. Thus the metavolcanics

in the property are progressively younger to the west and the felsic rocks

would, by this interpretation, occupy the centre of a basin and the core of

the synform. This hypothesis is in agreement with regional interpretations

outlined in previous reports on the area and is supported by westerly top

determinations from pillow packing and shape in the mafic volcanics, as

we.11 as angular unconformable relations between bedded cherts (I. F.) and

succeeding mafic flows in two locations on the property.

Excluding the sulphide and oxide facies iron formation, very little

significant mineralization was observed in outcrop on the property. Minor

amounts of disseminated pyrite or pyrrhotite are observed in the matrix

and foliation planes of mafic volcanics and spotty sulphides may be seen

in fracture intersections at 84S/3E, 86S/6E and 91S/8W. Weathered

disseminated sulphides and sulphur burn occurs in the quartz-feldspar

i)::i;r;Y, MICHKNFR a BOOTH

- 11 -

porphyry at 72S/15W and may be related to weak HLEM conductor D-18.

In the quartz-muscovite schist of the northern extension of this same

j felsic, unit at 16S/19W, approximately S-10% disseminated pyrite is

weathered to limonite. By extrapolation the patchy mineralization in the

quartz-feldspar porphyry to the south is probably of the same type. Pyrite,

pyrrhotite, chalcopyrite and quartz-rich float, located at 2N/2 to 4W,

is likely related to the mineralization drilled by Noranda in HLEM

conductor D-l.

EY (Map #2)

The magnetometer survey, utilizing a Scintrex MF-2 fluxgate

magnetometer, was conducted over all newly-cut grid lines on the property.

Approximately 6,800 readings of vertical component of the earth's magnetic

field were taken to the nearest 4 5 gammas at 50 ft. intervals. Base line

control stations wore established at the intersection of base end '..ross

i lines. The grid datum base control station is located at BL 0+00 at which

the magnetometer was set to read 520 gammas. This setting is in reference

i to the datum station setting of 500 gammas, located one-half mile north at

base camp, which was used in surveys on other grids in the area carried out.

by the Lynx--l)ejour-Reynolds Joint Venture.

Instrument drift and diurnal corrections were effected in the

following manner :-

A close-loop traverse was done in which two sub-stations were read,

then the two lines going away from the base line on the first grid line,

;-:i;:iY. (vilCfii Isi.fi ft BOOTH

- 12 -

returning to the base line on the second grid line, then the same two

sub-base stations are read again. Generally, the time interval between

the first and second readings of the sub-base station was 40 to 60 minutes.

The average difference between the first and second readings of the base

line station are taken to be the diurnal drift variation. This variation

is divided by the number of readings taken on a grid line to find the

variation per grid line reading. The final correction is: reading +

variation/grid line reading x number of grid line stations ^ final reading

to the nearest jf 5 gammas.

The contoured corrected data shows a magnetic pattern corresponding

to the northerly regional trend of the underlying lithology. Readings

varied from -4885 gammas to 4-22,815 gammas with extreme values generally

correlatable to magnetite-chert iron formation.

Intermediate values reflect the magnetic susceptibility range of

j the various principal lithologic mits, jrovidiug a guide in establishing

continuity of various lithologic units and their contacts, as well as

interpretation of structure in areas covered by overburden. The assumedl! magnetic susceptibility range of the principal rock units is tabled

as follows:-

Rqc^k Tyjpe Average Range

Mafic to intermediate volcanics Felsic volcanics 6 pyroclastics Oxide iron formation Sulphide iron formation Felsic intrusive

200-600 gammas 140-700 gammas 1015-22,815 gammas 1090-15,430 gammas 208-250 gammas

January - 3977.y

ZJfr-.-

R. E. Routledge, M, Se. DERRY, MICHENER S BOOTH

{x

overburden cornplc location; -OOrncsh analysis, heavy rnincrol seporate. analysis.

Values: Cu, Fb,7.n, Ag In ppm, Au In ppb

Conductor A. N.

DEJOUR-DIGHEM JOINT VENTURE

ofBASAL OVERf3UF?DEN SAMPLING LOCATIONS -conductor D- 2

Scolc.-l"200' Jan. 1977

G1

/p*

overburden sample location; -SOcriesh analysis, heavy mineral separate analysis.

Volucs: Cu, Pb,2n, Ag in ppm, Au In ppb

Conductor A. N.

DEJOUR-DIGHEM

SKETCH ofBASAL OVEIRBUF?[)EN SAMPLING LOCATIONS -conductor D-3

Scale; l" 200* :r Jan. 1977

at-

s*S'

\i f i\ni.37,0.2,10

67-2 O

TB- 383677

8,15,11,03,10

-e/tt, 73, 77, 0.9, f

O A Basal overburden sample location;-OOrncsh analysis, heavy mineral separate analysis.

Values: Cu, Pb,2!n,Ag in ppm, Au In ppb

f/f Conductor A. N.

DEJOUR-DiGHEM JOINT VENTURE

SKETCH ofBASAL OVERBURDEN SAMPLINGLOCATIONS -conductor D-10

———j.——.————,—————————— ScoUj; 1=200 J[ Jon. (977

8.1

6.L.

O A Basal overburden sample location;-BOmesh analysis, heavy mineral seperate analysis.

Values: Cu, Pb,Zn, Ag in pprn, Au in ppb

Kt Conductor A. N.


SKETCH ofBASAL OVERBURDEN SAMPLING LOCATIONS-conductor D-20

Scale: l =20O ...J. Jan. 1977

TB

TB

t.ws

X /

x x-432069

865

ns

105MS.\ faff. 70,10, IS Ill, 30.120.3.0, Mbf j j t y f f j

-432068

US

SWJX, W, /'IJ-S 50,^,3^ 1-7,1.5. U} 11, HO /.C-,, 1-5.

ws TtV

O A Rasa] overburden sample location;-60mesh analysis, heavy mineral sepcrate analysis.

Values: Cu, Pb,Zn, Ag in pprn, Au In ppb

ffi Conductor A. N.

DEJOUR-DIGKEM JOINT VENTURE

SKETCH ofBASAL OVERBURDEN SAMPLING LOCATIONS -conductor D-24

C-- - - - ——^,™^,^.,M,^,-. Jan. 1977

APPENDIX C

l)i:i\'K-Y. MICHKNf.i; 6 HOOTi !

DESCRIPTION OF LITHOLOGIC UNITS

Rock type nomenclature is essentially field terminology based on

empirical criteria such as colour, hardness, fabric characteristics and

tectonic relationships recognizable in the field.

(l) MajjLc to Intermediate Metavolcanic Rocks

The mafic metavolcanic rocks of basalt to andesite composition are,

in general, greenish-gray with the texture of individual flows ranging from

aphanitic to fine-grained amphibolitic and massive to schistose. The

classification basalt to andesite has been retained in conforming with

previously published reports although whole rock analysis performed on

diamond drill core of similar rocks on the Lynx-Dejour-Reynolds ground

indicate these are low-silica basalts.

Large, 2-3 ft., irregular, elongate to regular l ft. bun-shaped

pillow?, or absence of pillows serve to distinguish individual flows. Flow

i top direction determinations by pillow top rounding and packing could rarelyibe achieved. Chloritic, schistose, carbonate-rich varieties occurring in

ij contact with massive mafic flows are probably the result of shearing or,

jif thinly and conspicuously layered with fine fragments, have been termed

mafic tuffs. Porphyritic flows were noted at L86S/14E and 18E and a

porphyritic to porphyry basalt occurring on the footwall of the easterly

felsic unit ("Coulee felsics") features quartz and feldspar phenocrysts,

standing in relief on the weathered surface, set in a dark greenish-gray

chloritic, matrix. The silica content of this rock may qualify it as an

andesite rather than a basalt.

DLl.iv'V, f.-ilCH!.: iJi:-.H ft BOOTH

C-2

Three outcroppings of chlorite-calc-schist exhibited uniformly

light greenish-gray, carbonate-stained, rhombic-hatchured, or rope-like,

l weathered surface and waxy, light greenish, fresh surfaces. Spatial

relationship of two of these outcrops to schistose mafic flows and apparent

displacement of mafic breccia in the. southeast corner of the map area,

suggests the unit may be related to a fault zone. Alternatively, this

unit may represent a thin altered ultramafic flow or hypabyssal sill.

Amygdaloidal flows Outcropped only at 86S/14E and although vesicular

basalt to andesite was observed in float in the same area, none was

recognized in outcrop.

(2) ln t ermed i ate Vo l cani c s

These rocks are distinguished from the typical mafic volcanics by

medium gray, hard (siliceous) aphanitic texture and blocky light brownish-

gray weal herod surface in the case of the 100-450 ft. thick andesite to

andesite-dacite unit, extending from 30S/9E to 56S/11E and at 80S/19E, and

by fine-grained equigranular texture in which a mafic (amphibole) content

of about 305? or Jess imparts a lighter greenish-gray colour to slightly

foliated pillowed and non-pillowed andesites, located at 17S/18W.

Amygdaloidal andesite intermittently outcrops along the hanging wall

(west contact) of the "Coulee felsics". These are medium gray, aphanitic

to very fine-grained and slightly foliated with 2-5 mm. amygdules of fine

granular quartz.

Kuy. MicnrtJFK K uoom

C-3

! One exposure of andesite tuff, interbedded in mafic volcanics

j along the roadside at LO/8W, is fine-grained with medium gray layers

alternating with discontinuous lenses of mafic material of about l cm. inl

i thickness.

(3) Felsic Metavolcanics and Pyroclastic. Rocks

The more easterly continuous felsic unit, herein termed "Coulee

felsics", consists of a 100-150 ft. thick quartz-feldspar porphyry in

the south which is correlated with a dacite to porphyritic dacite and

quartz-muscovite schist in the north. The "Coulee felsics" could be

considered as comprising the suite of rocks which includes, from east to

west, the. porphyritic to porphyry basalt and amygdaloidal andesites on the

footwall; the quartz-feldspar porphyry and the amygdaloidal andesites on

the hanging wall.

The quartz-feldspar porphyry is schistose and almost entirely

composed of feldspar and quartz, identifiable only on the white, glacially-

polished surface. Freshly broken planar fresh surfaces are predominantly

muscovite and light buff-gray in colour. It is unclear whether this is a

flow or sub-volcanic intrusive sill, as field relationships where the

porphyry is exposed have been obscured by logging dirt and debris.

In the southwest corner of the property a few outcrops of foliated

to carbonate-altered and sheared dacite, bearing 3 mm. to l cm., spherical

to irregular amygdules of pink granular carbonate, form part of the 500-

2,000 ft. thick westerly felsic unit. In view of the alteration, these

i'.K'RY. MICHL:NC:K ft BOOTH

C-4

dacites arc possibly more intermediate in composition. A nor.hern extension

of this unit appears to represent a volcanic facies change to dacitic or

rhyolitic pyroclastics, reported in previous diamond drilling and exposed

at 30S/26W.

These appear to correlate with the well-bedded, light pinkish-

gray, tuffaceous metasediments comprising arkose, conglomeratic arkose

and interbedded tuff breccias and arkosic tuffs, exposed at 2S/23W on

the northwest corner of the property.

(4) Metasedimentary Rocks

One outcrop of polymictic conglomerate was located at approximately

32S/A1W. Cobbles to boulders of foliated granite and medium-grained, non-

foliated, quartz-feldspar porphyry, in addition to elongate mafic volcanics,

are set in a strongly schistose chloritic matrix. This unit appears to be-

part, of the same mctasedimentary unit of oligomictic and polymictic

conglomerates and arkoses outcropping along the Tashota road to the south.

The cherty facies of magnetite-quartz iron formation is characterized

by alternating 1-2 mm., white and bluish-gray beds. The thickness of this

chert unit probably does not exceed 50 ft. and in outcrop has been

measured to widths as narrow as 8 ft. Black magnetite-quartz iron

formation, with beds of very fine magnetite up to 2 cm. in thickness, are

separated by 1-2 mm. layers of fine granular quartz. The magnetite-quartz

facies may be undeformed or occur complexly folded. Undeformed cherty

facies with hematite partings on bedding planes have been traced to

tCU l* BOOTH

C-5

contorted magnetite-quartz facies in outcrop within 100 ft. This suggests

that the contorted folding in the magnetite quartz could be a primary

slump feature.

Felsic Intrusive Rocksl -

! Three outcrops of medium-grained, equigranular, roassive-textured,i iwhitish-gray, quartz- monzonite were located east of the grid in the

southeast map area. The intrusive contact with the mafic volcanics along

the eastern margin of the property has been magnetically inferred.

(6) Maf ic Intrusive Rocks

Diabase sills on the property are distinguished from volcanic

flows by their characteristic massive textures, greater topographic

relief and brownish weathering surfaces. The two narrow sills in the

southeast have weathered surfaces which are similar to pillowed mafic

flows in the vicinity and have been classified as diabase sills through

local cross-cutting contacts and relief of outcrop. A glomeroporphyritic

diabase outcropping at 46S/7E carries phenocrysts of 2-5 cm., greenish-

wlrjtc plagioclase in rosettes or clusters about 15 cm. in diameter.

n;-;;;r,', MICMKNKIJ fi- noon i

rv" (

* B D NDAR -CLEGG PA NY LTD.VB1 [3 EL F ART ROAD, OTTAWA. ONTARID, K1R DTTi PHDNF: PB7-C-311U

Geochemical Lab Report

Method A. A. t

Fraction Used

SAMPLE NO.

L805~3*50)S

L805-li^)C

L815-V80B

Ti805-5*50}i:

i^gj-Bo+oow

LS)05r31.,oow

W25^0*OOW

L925-31-HOW

L9H5-30',OOW

L9H5-31-J-20W

WH5-32+7W

1.0.q...rot:

Mt. ir

.17 f

.158

.08g

.10(5

. ...

.-A '.-A. A

l:s,J[ tH

CuVp'31

...7.2 ....

1*8

W

20

.-122.

^

29

66

50

580

li ^

J^

*-

Lynx Cannon T**\wV*r* j*a,

.t). pate NoY'V^SJ* ?.ii t 19 'l -J

Fb JPP-i

.-12......

15

10

20

SO

1510

17

3-9

25

22

-v------

praa

HO

30

HO

. 120.

.. 70-..

HO58

80

37

90

5A^;

-

t

AB

l.U

1.3

1.5

1.2

..J5L.O

2.0

1.0

l.U

1.6

1.7

l.H

0 -

-.

----- ~-

t t'

AuPpla

15

T. S.

HP- Ne

I.S.

ID

I.S.

pI.S.

I.S.

I.S.

I.S.

M

Tnoxiffi

tJB?i.e.c

"

REMARKS

Te. 3 S3 50 4-II

2 J.C*3i v *5 vvJjil^JLG

wQ4a ____ M

323&&13B35rr?

Hu

H

II

II

4-37.0 fct^

. ^^i

n m. F-AST F^OAD. OTTAWA, ONTARIO. KIG

Geochemical Lab ReportPHONE: 237-311O

^^^^.^^ Report No. ^.

Method .-... - —A .A... .^.... F . A.^-A. A .... .... - ... ...^....,..- .^. _ From

Fraction Used... _ .... . ~80.j;pils ...,. ..^^- .. . Date., _ .^^^..ecemer^j 19 6

SAMPLE NO.

I,6S 8-1- 5 OF,

9+50E

11+50E

L8S 9+50E

10+50E

12E

L10S 6+OOE

9+50E

10+50E

11+50E

L28S 31H-30W

L50S 1J+50E

L52S It+OOE

L5'4S ln-OOE

6+50)5

Lr;6s UOOE

6+603;;

L58S 5+OOE

1

Cu-Ppm

18

22

15

11

20

26

28

7

19

17

50

ill

37

8

55

8

21

'IT

gU

:-^

pbppm

22

23

ali

17

23

22

16

16

23

380

!i8

21

25

15

73

17

16

12

I.S.

ND No

J j Me a

o.-V-

Knppm

32

39

li h

17

32

28

23

147

33

20

51

37

39

11

77

18

16

30

[nsuffii

b Detec."

IB ICKS

Cv*e^

Ag ppm

1.7

1.6

1.5

l.lt

1.5

1.3

l.lt

1.3

1.5

1.3

0.9

0.2

l.H

0.7

0.9

l.l

l.l

O.H

dent s;

-,ed.

than .

( s-\v~

Au ptDb

L 5

L 5

10

ND

L 5

L 5

10

KD

L 5

5

I. S.

10

10

10

5

5

L 5

5

mple

)" ~

w-*/-. Ail- gramsf&p-fwt-

10

7

10

10

10

10

1.5

10

10

It

10

10

10

10

10

10

8

1

REMARKS

Ta 43414-0^s'-nscfli

ttII

K

M 3 m3~/u

43M-13&II

LIMSMO^3?36~?7

u

K

II

3l^(olO\\

l*

a.

j ^ .... .......... ... ..-...--- ... - .

Appendix "A 1

Schedule of Claims - Thunder Bay Division

Claim No.

TB-383501-09

TB-383514

TB-383673-85

TB-434731

TB-434732-35

TB-U34736-42

TB-434743 S 44

TB-451714

TB-445402-3

No, of Claims Expiry Date

9

1

13

1

4

7

2

1

2

July

Aug.

July

July

July

Aug.

July

Sept.

Dec.

24,

28,

24,

24,

24,

28,

24,

4,

1978

1980

1978

1980

1977

1978

1978

1977

1977

D.

D.

N.

D.

D.

N.

N.

A.

A.

Staker

Thorsteinson

Thorsteinson

Cox

Thorsteinson

Thorsteinson

Cox

Cox

Theriault

Lafontaine

Current Ownership

Lynx-Canada

Lynx- Canada

Lynx-Canada

Lynx-Canada

Lynx-Canada

Lynx-Canada

Lyn x- Canada

Lynx-Canada

A. Lafontaineoption agreement with Lynx-Canada)

Total 40 claims

TB- 434736

Q Basal overburden sompla location, -COmesh analysis

Values: Co, Nr ,2n, Ag In ppm, Au In ppb

(X Conductor A.N.


SKETCH ofBASAL OVERBURDEN SAMPLINGLOCATIONS -conductor D-4

Scale: l" 200' | Sept. 1977

/^7t D-6 ; r* j i

fe/WVf .47 7 7IS'i

XX

TB- 434733

TB- 383675

L3BS

1.40 S

IA2S

O BosoJ overburden sample location, -BOmesh analysis

Values: Cu, Ni,2n,Ag In ppm, Au In ppb

Conductor A. N.


SKETCH ofBASAL OVERBURDEN SAMPLING

LOCATIONS -conductor D-Q

Scoie; l"200* ' " "j Sept. 1977

5—(

Basal overburden sample location, -OOmesh analysis

Volues: Cu, Ni,Zn,Ag In ppm, Au In ppb

Conductor

TrenchOutcrop ~ /nafft mit* tSoltTwiretk, ft fer to

AA. N.

DEJOUR-D1GHEM J01NTVENTURE

of TKENCHfAIG BASAL OVERBURDEN SAMPLINGLOCATIONS -conductor

Scole; 1=200* j Sept. 1977 ~

J' ..*\m

-432068 * 1,''

-CIDasol overburden sample location;

I51J -8Omesh analysis, heavy mineral seperate analyslsf/976)

Wuej:Ac,Cu, Pb,Zn,Ag In ppm, Au In ppb

Conductor

Dd./,.

AA. N.

DEJOUR-DtGHEM JOINT VENTURE

SKETCH ofBASAL OVERBURDEN SAMPLING LOCATIONS -conductor D-24

i Sept.. I97T

DERRY, MICHENER fit BOOTHMINING GEOLOGICAL CONSULTANTS 2302 - The Simpson Tower

401 Bay Street Toronto, Canada M5H 2 Y4

OVERBURDEN DRILLING LOG

SkMPLt NO: OH ILL hlOLt NO: P7?25*MPi.c DEPTH:

. 4+30 -g.LOCATION;

POINT STARTED:

POINT STOPPED:

POINT EXTRACTED:

DRILLING TIME

SAMPLER STARTED:

SAMPLER STOPPED:

SAMPLER EXTRACTED:

FOOTACE

FROM

0t

11

'

TO

*

^

OVERBURDEN DESCRIPTION

ol^^-if 3? f

'

SAMPLE

DESCRIPTION

ORGANIC tt

CLAY 1, ™

S UT *1

nut SAHD t.

Mtl IVM IAHB K

COAM9C SAND 1,

CHAVtt ft '

Pt Bel. IS K

REMARKS:

383505 383504

TB- 383508

TB- 383509

l f On format mn :-t*trft I.f-, irtkh'itt tind 6 '-4-V*r '

•' sn-(fa.Oo(cAntc fock

DEvlOUR-DIGHEM JOINT VENTURE

SKETCH of

D "21,23

Sept. 1977

TB- 383681

/T—r^TV. /WffA t", Wtyf* 2fi, W}f* Mi, (g.; 'I, ; ?-4 ^m "r* **ff* wL'

Basol overburden sample location, -CO mesh analysis DEJOUR-DIGHEM JOINT VENTURE

of Tf?ENCHIWG BASAL OVERBURDEN SAMPLING

Values: Cu, M;,Kn,Ag In ppm, Au In ppb Conductor

Trench -

^olt^nilrockf f-eftrfo

LOCATIONS -conductor D-14-.16

TB- ' 383601

TB- 3836O2

TB- ^ 383506

o Basol overburden sample location, -80 mesh onalyois

Volues: Co, Ni ,Zn,Ag In ppm, Au In ppb

Conductor A. N.


li of Baf-khoz Trtnthts ^ BASAL OVERBURDEN SAMPLING LOCATIONS -conductor D-19,12

Scale.-1*200* ___j Sept. 1977

DERRY, MICHEXER St BOOTHM1NINO OUOLOOICAI, CONSULTANTS 2502 - Tilt

401 Bay Street L^" - Toronto, Canada M5H

OVERBURDEN DRILLING LOO

Tower \

•v . J*"*-

J*M\lt DEPTH :

I., lit:

POINT STAWTEDi

POINT STOPPED:

POINT EXTnACTEO:

on it. l "no 1 1 no:

7 C

/x 7 7LOCA1IOH:/o o

DRILLING TIME ^.tfv /;', , VV ,s

SAMPLER STARJEDl

SAMPLER STOPPED!

EXTRACTED!

FOOT/

FROM

(T4

C

'

-

ntMARKS:

ICE

TC

^/•Q{J (l/lAJji.. C"f t'Lf'i-^--'!

. (-^ ., y

.. , ] ' j ,1 ffffl 'CA-^.' j'i-x*-'^f V^.L/"/ ^ f T' C-* -^ / 7 i" f sf i ,*

^ ^

'

SAMPLE

DESCRIPTION i;

Cl*Y t, (

9 1 UT H

fINt SUMO T,

MlDIUl* 8 AH D *T,

COAX91 S AH O 1,

OBAVtk H

Ptntats \

DERRY, MICHENER S? BOOTHMINING ouoLooxcAi, CONSULTANTS 2S02 - The Simpson Tower \

401 Day Street \^/^-—' - Toronto, Canada M5K 2Y4 .j

OVERBURDEN DRILLING LOG -it,,

1 VAMI'lt MO: i

t

SAMI'LC 0[l"THl?# '

,*~ ijUINt:

III! ilk HOkl. NO:

b*MI'l.U)D:

T^nr/eWw f ci XSt AT 10H:

UAft! y

ann^S/V'SCOHtltAcfr . y'

LOCATION;

T)~zt- Cfs-^fa.ff.-'

POINT STAWTEOi

POINT STOPPED!

POINT EXTRACTED!

DRILLING TIMESAMPLER STAR,

SAMPLER STOPPED!

EXTRACTED'

FOOTAOE

FROM

, rt

f

-

'

,.

'

Tl-

*L.9.

— (


U flA-U r r ( CL.y-*XXA

O. -PcAAJ P)^.lf(fAV'^

W-ft-fi!//?^ /O-?) *-NAr.v L:6'-^;- -

1

SAMPLE

DESCRIPTION -

OKCA'ilt T,

CI.AT T. '

9H.T V,

r m t SAND r.

MtOIUM BJkNO n'

CO A* 9 t 4M(0 r. -'

OUAVtV *. .

ctimm T, •1 - '

- r

.

; DERRY, MICHENER Se BOOTH lCONSULTANTS 2302 - The Simpson Tower \

401 Bay Street ' Toronto, Canada M5H 2Y4 \

OVERBURDEN DRILLING LOG . -

DERRY, MICHENER Se BOOTHOISOLOOICAI. CONSULTANTS #302. T/ic Simpson Tower \

401 Bay Street j Toronto, Canada M5H 274 .i

OVERDURDEN DRILLING LOG l

:'T#';fo^fe

Z, ?ff ^UA—W /X li - ^-*

Onttl. KOVi NO;

S T AT i ON L '

DATtl

CONTnACT:

f /l - -"^ -DRILLING TIME " '

POINT STARTED: S AMPLER ST A RT EOl

POINT STOPPEOl SAMPLER STOPPED)

POINT EXTRACTED: 3AMPLEF* EXTRACTED!

FOOTAGE

FROM TOOVEROVROEN DESCRIPTION

, SAMPLE

DESCRIPTION

, j'^'p^sjliftik

i-uvr —

*7 ^

?'

' POINT STARTED:

; POINT STOPPED!

POINT EXTRACTED;t

mFOOTACE

pn ntut TO

Oil ILL "01. L NO:

^Sw/^ftK^XSTATION:23 '/- 75"

DATtl

CONTRACT: ,

L 0 C A T t 0 Hi yy

DRILLING TIME '

SAMPLER STARTEOl

SAMPLER STOPPED!

- BAMPLCrt EXTRACTED!

SAMPLE OVERBURDEN DESCRIPTION

TOOTAGE

FROM

, O-

^

'

'

TO

^

ovEnounoEN DESCRIPTION

u^yy

, SAMPLE

DESCniPTION ''

ORGANIC f,

t\.*1 f, '

SII.T H

riKt SAND Vk

MtOIUM *AND *,' '

COAflSl 9AHO V,

ONAVtV ^ .

rtnnt.il i,

,

FOOTAOE

FROM

. O-

'

'

TO

/A

OVEROURDEN DESCRIPTION

Uajj . ±;i(J(\ '

SAMPLE

OEScntPTlO^4 '

016ANIC T.

ci.Ay r, i'

9II.T *.

r IX t S AN B T,

MtDIUM BAHO fi

eOAHSt SAMt" *.

OUAVtl fi -

rtn*'. ts ',

'

DERRY, MICHENER 8e BOOTH ' TMININO OtfOLOOXCAJ. CONSULTANTS ^Qg . TllC SimpSOH TOWCT i

401 Bay Street ' Toronto, Canada MSH 2Y4 .1


(lil H. l. HO Lt NO:

07 X-*T f X Jfcfr

LOCTION!

POINT STARTED;

POINT STOPPED)

POINT EXTRACTED:

DRILLING TIME -

SAMPLER STARTED!

SAMPLER STOPPEOi

SAMPLER1 EXTRACTED)

FOOTAGE

FROM

0.

TO

/.y-OVERDVJRDEN DESCRIPTION

Cl,^,, , cy;^,.,!

^j'0. 1/, j,Ye(-n /A,flXfo\ ,,,nf(! vfv!,e.'h fi i 1

SAMPLE

DESCRIPTION '

0, a A N ,C

CLAY K '

sat y.

rmt SAND ^

MEDIUM *AH6 V '

COAIUt SAMP X

OBAVtl. H 4

Pt.nti *

1

nUMAHKS: ' '

DERRY, MICHENER S; BOOTHMININO oiiotooxcAi. CONSULTANTS 5502 . The Simpson Tower \

401 Bay Street \, Toronto, Canada M5H 2Y4 ,\

OVERBURDEN DRILLING LOG i

DRILL MOLt MO:

^J^L, c^/ S

POINT .STARTED!

POINT STOPPED!

POINT EXTRACTED;

DRILLING TIME

SAMPLER STARTED!

SAMPLER STOPPEOi

SAMPLER EXTRACTED!

FOOTAGE

FROM

0

.

'

'

T l-

CL^


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OCSCRIPTION '

0 1 C AN 1 C T.

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rmt SAWD T.

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rtnBtts *.

DERRY, MICHENER ft BOOTHMIKINO oisotooTCAL CONSULTANTS 2502 - T/ic Kwjjson Tower

401 Bay Struct Toronto, Canada M5H 2YJ,

OVERDURDCN DRILLING LOO

"~~^T/;\in 'L. t HO 1.1. NO

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DERRY, MICHENER ft BOOTHMINING OUOLOOXCAX. CONSULTANTS 2305 - T'lC tftf

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O

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-y.—— ——

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DERRY, MICIIENER S: BOOTHMINING 01IOr,OCUCAL CONSULTANTS 2302 - T (1C iV'tHl/WOM

401 Bay Strfet Toronto, Canada. M5H S

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cv

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DERRY, MICHENER Sg BOOTHMINING ouoLooicAL CONSULTANTS 2302 - The Simpson Tower

401 Bay Strait Toronto, Canada MCH 2YJ,

OVERDURDEN DRILLING LOG

POINT STAMTEDl

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POINT EXTNACTEOr

DRILLING TIMESAMPLEn STAHT'SOl

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DERRY, MICHENER S: BOOTHMINING cKoi.ooicAi. CONSULTANTS 2302 - The Simpson Toivci

401 Kay Street Toronto, Canada M5H 2Y,

OVERBIDDEN DRILLING LOG

OH 'L L HO Li HO;

/L

POINT STARTED:

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POINT EXTRACTED-

DRILLING TIME

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.0

f ri't SAND

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'-PY4l BDNDAR-GLEGG S. COMPANY LTD.1V-J "BELFAST ROAD. OTTAWA, ONTARIO. K1G OZ5

Geochemical Lab ReportPHONE: B37-3110

Cu,Zn,JIi,Ag,Au - H1JO ~KC1 D .. 1590-7 xtraction._____L-..L... J..Jr.! ^ ___ -3-—___-—_____ Report No._______±rr ..L.

Method —- A.A. F.A.-A.A.

Fraction Used M..- -80 soils.

^ p rom _Dsrry, Hicheaey fc Booth

_ Date_______September 8, .1911.

SAMPLE NO.

E ~ ^

33

89

90

92

93

E - 9'iU

85

88

89

uuppia

13

36

56

7

32

51*

20

10

15

23

L iriea

inzszz-

Vsa ppm

16

53

65

15

7U

53

35

2H

33

-3? ,

is less

-X-^i-oa

in ppm

19

20

20

e18

22

23

13

3-9

19

than

Wvjn

Ag ppai

0.8

1.3

0.6

0.5

0.8

0.6

0.6

0.3

1.3

0.6

't/o-

Au•DT3b

L 5ios

•t 5

10

iro ^25

10

L 5

J1D

L 5

__

^^m^f^^m

9

(t dot e c

REMARKS

TB. ^-3M 137stofolT3^3507

li

ted Uh

3835053?35ob^3M133sgsGol

Ontario

RECEIVEDMinistry of Natural Resources

APR l 4 W APR l 4 ft//GEOPHYSICAL - GEOLOGICAL - GEOCHEMICALPROJECTSWHNICAL DATA

5 SECTION

) C /"* C l W F H C ^

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

TECHNICAL REPORT MUST CONTAIN INTERPRETATION. CQNCLUSIONSJETC, LANDS ADMINISTRATION -

Type of Survey(s) Geological S Geophysical_____

Township or Area Coughlan Lake 6 Castlewood LakeClaim Holder( s) Lynx-Canada Explorations Ltd.

A. Lafontaine (under option to " ) Survey Company Derry, Michener 6 Booth _______ __ Author of Report R * E. RoutledgeAddress of Author Sulte 2302 " ^ Bav Styeet Toronto

Covering Dates of Survey July ? - December 8, 1976(linecutting to office)

Total Miles of Line C.ut 6t** 7 ____ : _____________ -

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.

ENTER 20 days for each additional survey using same grid.

DAYSper claim,, . , . . Geophysical

—Electromagnetic

(l ) —Magnetometer—Radiometric

—Other .———— (l ) Geological

(2) Geochemical __ . __ 2

20

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

Magnetometer. .Electromagnetic. . Radiometric

nATF; February 2/77 sir.N ATITRF. ;

(enter days per claim)

. ^0Author of Report or Agent

Res. Geol.. .Qualifications.

Previous Surveys File No. Type Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

(prefix) (number)TB-383501 - 09 inclusive '

TB-383673 - -85

TB-43U731 - 44 inclusive

- 03

TB-451714

Note: Report on

and Magnetometer Surveys for

TB-445402 - 03 has been .................*.................. .,...... ................

previously submitted for

assessment credits. (Jan. 1977

(2) Geochemical Survey credits

.to claims

TB-383504

TB-383677

76-38368^0

TB-434737

- 81

inclusive

3

c

TOTAL CLAIMS.

GEOPHYSICAL TECHNICAL DATA

GllOUND SURVEYS — If more than one survey, specify data for each type of survey

Number of Stations^ U36S _____________________ Number of B^rfing.^800 (mag) .-3200 (HLEM)

Station interval ____ 1^2 ______________________ Line spacing ______ 00' ———————————.Profile ...IP l"-l(ft (HLEM) _____________________________________________Contour interval 200 gammas (magnetometer)

Instrument _____ Scintrex MF-2 Fluxgate

Accuracy — Scale constant — 5 gammasC^ Diurnal correction method closed-loop*"'?;| Base Station check-in interval (hours) 0'66 - l hours

Base Station location and value BL/0+00 520 gammas

'J: Instrument A.B.E.M demi-gun

Coil configuration Horizontal co-planar

Coil separation 200

Accuracy, ^ 0—————Method: Q Fixed transmitter CD Shoot back CD In line CD Parallel line

0 2640 Hz.___________________________________________(specify V.L.F. station)

Parameters mp^.irpH In Phase and quadrative in % of primary field._____________

Instrument __________________________________________________________Scale constant.Corrections made.

Base station value and location .1

Elevation accuracy.

Instrument _________________________________-_______________ * Method CD Time Domain [~l Frequency Domain

Parameters - On time ^_________________________ Frequency —..——— Off time __________________________ Range ———-.-.—— Delay time, ————————,—.—————.——-L.

— Integration time ——..——..—..————..———...—....—.—•S:

Power _______________:____________________————————————— Electrode array.——————————————————————————————————————————— Electrode spacing ———————————————————————————————————————————— Type of electrode ————————————————————————,—————————————————

GEOCHEMICAL SURVEY - PROCEDURE RECORD

CNumbers of claims from which samples

445H02.

TB-38350H. 383677, 383680 - 81, U34737 - HO,

Total Number of Samples Type of Sample. soil

ANALYTICAL METHODS

(Nature of Material)Average Sample Weight. variable

Values expressed in:

Method of rnlWHnn Atlas Copco rock drill and deep soil sampling kit .______^__

Soil Horizon sampl PH Basal soil adjacent to bedrockOthers

per cent p. p. m. p. p. b.

Co, Mo, As.-(circle)

Horizon Development Sample nPpth l

Field Analysis (-'58*

1QW relief, swampy

low density, glacially jmeHp.H to structurallDrainage

Estimated Range of Overburden ThicknessO - 60'

Nil

Extraction Method^. Analytical Method— Reagents Used———.

controlled.Field Laboratory Analysis

Nn ( Nil-—--^^

Extraction Method——— Analytical Method ——— Reagents Used.—-———.

.tests)

.tests)

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

Mesh size of fraction used for analysis ~ 8Q mesh for 18 samples^^^^^^^^^—^^^^^^^^^^^^^^ -100 for 11 samples (H.M.S.)

Commercial Laboratory (Name of T.ahnratory Bondar-Clegg fe Co.

Extraction Method^—^———————i

-tests)

Analytical Method-atomic absorption. Reagents ric.H f*** assay for Au.

Bagged and dr*ied J-n shipped to General.Bondar-Clegg 5 Co. in Ottawa where screened

to - 80 mesh and analyzed

H. M. S. samples pulverized to - 100 mesh,

density separated by methylene iodide , heavy

mineral separate analyzed.

Ministry of Natural Resourcft^ File.

OntarioGEOPHYSICAL - GEOLOGICAL -

TECHNICAL DATA,J;MICALtf-ANDS SECTION

TO BE ATFACTS S

TECHNICAL REPC

42L83SW0013 2.2334 COUGHLAN LAKE 900Type of Survey(s). Township or Area. Claim Holder(s)—

Geophysical

1 APR j 4 1977j

PROJECTS UNIT

Coughlan Lake c^ Castlewood Lake

Lynx-Canada Explorations Ltd.

A.Lafontaine (under option to ")Survey Company Derry, Michener Se Booth ———^^^ Author of Report R. E. Routledge,^..—^^^.^^^—.^. Address nf Author Suite 2302 - 401 Bay Street, Toyont 3 Covering Dates of Survey July 7 - December 8, 1976

(linecutting to office)

Total Miles of Line Cut 64.7______________________


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

Geophysical—Electromagnetic.—Magnetometer_—Radiometric———Other—————-

DAYS per claim

4020

Geological.Geochemical.


Magnetometer .Electromagnetic. Radiometric(enter days per claim)

HATR. Feb. 2/77 STOMATTTRF. /77,Author of Report or Agent

Res. Geol..


(prefix) (number)

TB38354

TB383673 - 85 inclusive

TB445402

.TO.4.4.5.4.0.3..........

Qualifications.Previous Surveys

File No. Type Date Claim Holder

•l

TOTAL CLAIMS. 40


GROUND SURVEYS — If more than one survey, specify data for each type of survey

^^^ Number of Station* ^ 4365___________________Number of Readings 6800 (mag) . 3200 (HLEM

Station interval _____100 '———^———^—.——————^——Line spacing-—————^..^-..—.—...—.-——.....— Profile scale_______l" -10^ (HLEM)_________________________________________ Contour interval____200 gammas (Magnetometer)_______________________

u Instrument______Scintre* MF-2 Fluxgate_________________________________

H Accuracy - Scale constant.. - 5 gammas_________________________;_______________typ

Q Diurnal correction method ____closed-loop—.—...——-—..—.———.^—————.———.-———-—^—-—— *ji Base Station check-in interval (hours) 0.66 - l hours^^^.^-^-—^——-—.^^—^.^————.-——

Base Station location and value _____BL/0+00_____520 Cfammas

U Instrument A.B.E.M. demi-gun

Zsh

Coil configurationCoil separationArnirary — l%

Method:

Horizontal co-planar200'

CD Fixed transmitter Q Shoot back D In line CD Parallel lineFreniionrv 2640 HZ .

Parameters measured in phase and quadrative in ?6 of primary field.

Instrument

Scale constant.Corrections made.

^5 Base station value and location .

Elevation accuracy.

NDUCED POLARIZATION

Instrument

Method 1 1 Time DomainParameters — On time

i* Of f t impH ^ — Delay time

rf, — Integration timew:W Power

Electrode arrayElectrode soacine .. — -.

O Frequency Domain FrequencyRange

Type of electrode

ft Kt*. La

Ministry of Natural Resourc^^ . 4 File.

OntarioGEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL

TECHNICAL DATA STA^fcKffiSlLANDS SECTION


TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

GeologicalType of Survey(s) —Township or Area Coughlan Lake Se Castlewood LakeClaimHolder(s) Lynx-Canada Explorations Ltd.

A.Lafontaine (under option to ") Survey Company Derry, Michener Se Booth——————Author of Report R. E. Routledge_______________Address of Author Suite 2302-401 Bay St./ Toronto. Covering Dates of Survey July 7 - December 8, 1976


Total Miles of Line Cut 64.7____________________



Geophysical—Electromagnetic.—Magnetometer——Radiometric———Other—————

DAYS per claim

Geological 20Geochemical.


Magnetometer. .Electromagnetic, . Radiometric(enter days per claim)

HATR- Feb. 2/77 SIGNATURE:Author of Report or Agent

Res. Geol.. .Qualifications.Previous Surveys


APR l 4PRQIECTS. .UNIT


(prefix) (number)

.m^sAQA........::...................

TB445402 - 03 has been

p reviously, submi11ed t

TOTAL CLAIMS.


GROUND SURVEYS - If more than one survey, specify data for each type of survey

Number of Stations ———————-——^———^^——————————Number of Readings —

Station interval ______________________________Line spacing^^——^

Profile scale——^——.—.—-^^———^-——^^——.^.^-—..——^———————-^———————Contour interval.

,,. Instrument.w

w

Z C

Accuracy — Scale constant. Diurnal correction method.Base Station check-in interval (hours). Base Station location and value ____

.ECTROMAGNETIC

Instrument

fV(il rnnfignratirm

Coil separation

Method: d Fixed transmitter d Shoot back d! In line FrermerifV

d Parallel line

Parameters measured.

Instrument.Scale constant ——

^Corrections made.

^ Base station value and location

Elevation accuracy,

Instrument ————Method d Time Domain d Frequency Domain

Parameters — On time __________________________ Frequency ————- Off time ___________________________ Range ————————

— Delay time __________________________— Integration time

Power.Electrode array — Electrode spacing .

Type of electrode

Ministry of Natural Resources

GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT

File.



GeochemicalType of Survey (s) —Township or Area Coughlan Lake c* Castlewood LakeClaim Hnlder(s) Lynx-Canada Explorations Ltd.

A. Lafontaine (under option to ") Survey Company Derry, Michener Se Booth—————— Author of Report R - E. Routledge____^__^___ Address of Author Suite 2302 - 401 Bay St. f Toronto Covering Dates of Survey July 7 - December 8, 1976


.Total Miles of Line Cut 64.7___________________



ENTER 40 days (includes line cutting) for first survey.

ENTER 20 days for each additional survey using same grid.

Geophysical

—Electromagnetic.—Magnetometer™.—Radiometric——

—Other———^—

DAYS per claim

Geological ———. Geochemical—2CL


(prefix)

TB 383504(number)

.TB...3.8.36.7.7............

TB383680

TB434737

TB445402

l

1 I

Magnetometer. .Electromagnetic, . Radiometric(enter days per claim)

DATE: Feb.2/77Author of Report or Agent

Res. Geo I.. .Qualifications.Previous Surveys


TOTAL CLAIMS.



Number of Stations ———————-———-——--.———-—-——.Number of Readings -Station interval——-—-—-—————..^————-.-.—..—^-—.—Line spacing-.^——-—Profile scale______________________________________________

fContour interval.

- Accuracy — Scale constant.ZO

z;5?s

O

S

oo

g

Instrument.

Diurnal correction method.Base Station check-in interval (hours)- Base Station location and value ____

InstrumentCoil configuration ,^--^-—^—-——.^———^——-^-.——-———^——™^^^-.-—.^—.——^—.———-..—.^—..——^^— Coil separation -—^—-—^———-.—--———-^^—-——^..———.——————.....^^-—.^^—..-..^—-^—-—.—Accuracy ———————————----——^--———--——^——.—.^——————-——-——-.———-——.—.-—.———^^Method: C] Fixed transmitter CH Shoot back O In line D Parallel line

Freq u en cy ______________________________________________________________(specify V.L.F. station)

Parameters measured_______________________________________________________

Instrument.Scale constant,Corrections made.

Base station value and location .

Elevation accuracy.

Instrument —^———-^^—-——^———-——^————-——.——————.^———-—2; Method D Time Domain D Frequency Domaino ———

Parameters — On time ___________________________ Frequency ...—^^.— Off time ———--———--—--.^-——-^————— Range.— Delay time ——^—^.^——--—.—.^^-—^—————— Integration time —^——.^^—-.———--——^———.^—.

Power.Electrode array — Electrode spacing .

Type of electrode


Numbers of claims from which samples taken. ______TB434737 - 40. 445402

TB-383504. 383677. 383680. 383681

Total Number of Samples 29 Type of Sample_______soil

(Nature of Material)Average Sample Wright variable———————-Method of finiwtinn Atlas Copco rock drill

and deep soil sampling kit—————Soil Horizon s^mpi^H Basal soil adjacent to Horizon Development——^:——————————^—Sample Depth l' - 58 '________________ Terrain low relief, swampy__________—————————————low density/—glacially

ANALYTICAL METHODS

Values

"~^\^ CU^CP

Others '?feld/

expressed in

V*(Zn^) Ni

AuAnalysis (.

: per cent O p. p. m. S p.p. b. g]

, Co, C^Ajp Mo, As.-(circle)

Nil -tests)Extraction Method. Analytical Method- Reagents Used——

DrainageEstimated Range of Overburden Thickness__________O - 60',^^..^^

impeded to structurally Field Laboratory Analysis controlled No 7_ .tests)

Extraction Method. Analytical Method - Reagents Used,——.


Mesh size of fraction used for analysis -80 mesh for 18 samples—..———.-—,—.—^^-^———— -100 for 11 samples (H.M.Si)______

tests)Commercial Laboratory {———29—————— Name of Laboratory Bondar-Cleqg S Co. Extraction Method ——————————.-—'.————Analytical Mpthr.d atomic absorption, ReagentsTTgPH fire assay for Au.

Bagged and dried in field shipped General - to Bondar-Clegq St Co. in Ottawa wherej ———— screened to -80 mesh and analyzed — ——— H. M. S. samples pulverized to -100 mesh^. ———— density separated by methleneheavy mineral separate analyzed.

SELF POTENTIAL

Instrument.———^———————j—^^———————^———^——'.———————— Range.Survey Method ———————————————————————————————————————————

Corrections made.

RADIOMETRIC

Instrument ———.Values measured.Energy windows (levels)—-——-————™———.-———-——————-^^—.————.———Height of instrument____________________________Background Count, Size of detector-^————^-————————..———,^—-———.—.^———-—-—.—Overburden —-———————--^——...———.——————-—..——.-——,—————^.,—

(type, depth — include outcrop map)

OTHERS (SEISMIC, DRILL WELL LOGGING ETC.)

Type of survey———————————————————————————————————Instrument —————-—^—.^-———...-..——-^—..—-^.—————-—. Accuracy.———-^-—————.—————————---————————.——Parameters measured.

Additional information (for understanding results).

AIRBORNE SURVEYS

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

(specify for each type of survey) Accuracy——————————.————.

(specify for each type of survey) Aircraft used ——-^——-——————————-——-^^———^^—-——

Sensor altitude.Navigation and flight path recovery method.

Aircraft altitude_______________________________Line Spacing—— Miles flown over total area__________________________Over claims only.

Ontario



File.



Type of Survey(s) Township or Area Claim HnlHer(s)

Survey fhmpny

Author of Report Address of

. "Z- SCCOI S T.

Covering Dates of Survey.

Total Miles of Line Cut.—office)



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

DAYSper claim


AIRBORNE CREDITS (Special proviiion crediti do not apply to airborne turveyi)

Magnetometer .Electromagnetic.

DATE

(enter dayt per claim)

. W T 15} r- SIGNATURE:^

. Radiometric

Author of or Agent




x) .-j (number)ST..

.LlUiH

TOTAL CLAIMS.



Number of Stations _________________________Number of Readings - Station interval -^——..^-—^——^————.—-^-—,.^—I ine spacing ————— Profile scale _________________________!__________________'Contour interval.

o

s Si ^

— Delay time

Instrument.Accuracy — Scale constant. Diurnal correction method.Base Station check-in interval (hours). Base Station location and value ———

InstrumentHW ZSjj5

X

Bwe

Coil configurationToil separation

Accuracy ,Method: D Fixed transmitter CD Shoot back O In lineFrequency , ,.. .,,....

(specify V.L.F. station)

D Parallel line

Parameters measured.

Instrument.Scale constantCorrections made.

Base station value and location .

Elevation accuracy.

Instrument ___________________________________ ; ———————————— Method D Time Domain D Frequency Domain Parameters - On time ____________________ : ____ ' Frequency —————

-Off time ___________________________ Range

Integration time.Power.Electrode array — Electrode spacing . Type of electrode


Numbers of claims from which samples taken

?

Total Number of S Type of

pies

(Nature of Material)Average Sample Weight- Method of Collection.

Soil Horizon Horizon Development Sample Depth. Terrain

-t

Estimated Range of Overburden Thickness_____ O-


Mesh size of fraction used for analysis^—^—

ANALYTICAL METHODSValues expressed in: per cent

p. p. m. p. p. b.

Mo, As,-(circle)

Field Analysis (Extraction Method. Analytical Method- Reagents Used——

Field Laboratory AnalysisNo. (———————Extraction Method Analytical Method, Reagents Used

Commercial Laboratory (. Name of Laboratory, Extraction Method Analytical Method. Reagents Used__

tests)

.tests)

tests)

GeneraL General.

SELF POTENTIAL

Instrument_______________________________________ Range.Survey Method .^^—-———-——————————^-—-.—————^—^^————.....—..——

Corrections made.

RADIOMETRIC

Instrument ———.Values measured.Energy windows (levels)-———————————^—^——————..——^^^^——.——..—Height of instrument____________________________Background Count, Size of detector————-————-———-—-—————————.———.—.—..—.^^—————-Overburden -^-^^^—^^————-—^^^^———..——-—.————^—-..—.——..—..————


OTHERS {SEISMIC, DRILL WELL LOGGING ETC.)

Type of survey———————————————————————Instrument —^^^———————————^————Accuracy.-———-—.-——————--—-————————-—Parameters measured.


AIRBORNE SURVEYS

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

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

(specify for each type of survey) Aircraft used.———————————————————-——-——————

Sensor altitude-Navigation and flight path recovery method.

Aircraft altitude______________________________Line Spacing—— Miles flown over total area__________________________Over claims only.

Ontario



File.


TECHNICAL REPORT MUST CONTAIN INTERPRETATION. CONCLUSIONS ETC.

Type of Survey(s). Township or Area. Claim Holder(s)^

d &&SMINING CLAIMS TRAVERSED

List numerically

Survey Company. Author of Report. Address of Author Covering Dates of

Total Miles of Line Cut.

. f

X^ JH/V(linecutting to office)



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

DAYS per claim


AIRBORNE CREDITS (Special provision credit! do not apply to airborne surveys)

Magnetometer. .Electromagnetic. . Radiometric

DATE:.

(enter days per claim)

SIGNATURE:

'(prefix)' (number)

Author of Report or Agent



TOTAL CLAIMS.


GROUND SURVE1YS — If more than one survey, specify data for each type of survey

Number of Stations_________________________Number of Readings ______-.—~—-————.Station interval ______________;-————-———.————.Line spacing——.——-————-—..-——.—————Profile scale ________'._____:_______;_____' ^——————————————^————.—.————.Contour interval.

InstrumentAccuracy — Scale constant, Diurnal correction method.Base Station check-in interval (hours). Base Station location and value ^——-

Instrument ——^— Coil configurationCoil separation.S

^ Accuracy.Method: CD Fixed transmitter D Shoot back D In line C] Parallel line

Frequency —————————————————————————————-.————————————————————————————{specify V.L.F. station)

Parameters measured_________.____'.___'._______:———:———————————————————————

Instrument.Scale constant

,, .Corrections made.

Base station value and location

Elevation accuracy.

[NDUCED POLARIZATION

Method di Time DomainParameters — On time .

* Off timpC

— Delay time

V) — Integration time

H Pnwpr

Elect r^H*" arr^yElectrode snacine — . . ——— ...— ————

D Frequency Domain FrequencyRange

.-

Type of electrode


Numbers of claims from which samples taken.

%

Total Number of Samples Type of R.mpi,

(Nature of Material)

Average Sample Weight Method of CollectiontaufSoil Horizon Sampled. Horizon Development Sample Depth____

xTerrain______f

iX

Drainage Development——-Estimated Range of Overburden Thickness.

x.^^^m--^n-

General


Mesh size of fraction used for analysis____

ANALYTICAL METHODSValues expressed in: percent CH

p. p. m. p. p. b.

As.-(circle)

Field Analysis (Extraction Method. Analytical Method- Reagents Used——

tests)

Field Laboratory AnalysisNo. ___________Extraction Method. Analytical Method - Reagents Used ——,

Commercial Laboratory (Name of T.ahnratnry

Extraction M^thnH

Analytical Method Reagents Used -—

General

.tests)

tests)l/ffi JU~f\

SELF POTENTIAL

Instrument.^-^——————.^———-—--————-—————^————.-——^— Range.Survey Method ___________________________________________.

Corrections made.

RADIOMETRIC

Instrument—-—Values measured.Energy windows (levels)_________________________________,—-———.— Height of instrument____________________________Background Count.Size of detector—————.^——^————————-———-——————.——.————.Overburden —^-^-—^———...-.—^-———-.——-—-.—.—...———.—.—.—^—-——


OTHERS (SEISMIC, DRILL WELL LOGGING ETC.)

Type of survey——————————————————————— Instrument ————————————————————————— Accuracy__________________________Parameters measured.


AIRBORNE SURVEYS

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

{specify for each type of survey)Accuracy——^^—^—^—^—^-——.

(specify for each type of survey) Aircraft used———-—-————.^—————.—-——————.-..—..—.

Sensor altitude.Navigation and flight path recovery method.

Aircraft altitude_______________________________Line Sparing Miles flown over total area———.————————-—————————Over claims only.

870 45'

50 0 0730 —i

50 000'—J

T—500 0730

OBOSHKEGANFOR^-. STATUS REFER TO TWP. PLAN

V..

K-i-^-

386264 386260'386256l 386253.396246

\W62TI' 386267(3862 63 386259

y^TB ITB TB

TB TB l TB

6296,386285 3862841435418 (4354171386303

386301 386298 386293 'TB l -B 336288

300 38629! 386290 383663

Onaman

2424 /3B3656 ^ 383655 , 383654^434727 JM3692

43474'; '4347*1

l I0 Jt

1434736 (434737 '*3473 6 i 4 1*731

B"434732TFa 4J4r?33~IT?383675!38ySr74lTB3B3673"ITB 431514 TB 431511 ITB 416526

or

L- 500 OO'

870 30'

42L03SW0013 2.2334 COUGHLAN LAKE 200

AREA OF

COUGHLAN LAKE

DISTRICT OFTHUNDER BAY

THUNDER BAYMINING DIVISION

SCALE: 1-INCH-40 CHAINS

LEGEND

PATENTED LANDCROWN LAND SALELEASESLOCATED LANDLICENSE OF OCCUPATION

MINING RIGHTS ONLYSURFACE RIGHTS ONLYROADSIMPROVED ROADSKING'S HIGHWAYS

RAILWAYSROWER LINESMARSH OR MUSKEGMINESCANCELLED

C.& Loc.

L.O. M.R.O.

S.R.O.

c.

NOTES

40O' suifgce rights reservation around oil lakes ft rivers

NATIONAL TOPOGRAPHIC SERIES 42 L

PLAN NO. M "l 409

- -A . ONTARIOT. - X - ,

^NISTRY OF NATURAL RESOURCESSURVEYS AND MAPPING BRANCH

NOTES

400' surface rights reservation along the shores of all lakes and rivers.

J87 0 45'

COUGHLAN LAKE M.140967 0 30'

500 00'—

O* ro00

UJ

o:

490 52' 30'

431514 I43I5II 1418528

\ M l i tioat i i -l-f-/- — L-- — --L

7 TB l TB

1455670 l 455569

Conglomerate Lake 432070 l 432 069

iTB ~~ ~~~ _ __ l__ - JOJ31TB ^-"TB ~~ ~ ~^ —

.4320661 431534 (431527 |43I

JTB

Onaman

i i ' l ^"\ l 434644 1434643^ J' 434641 I^5O' - - -

r—™"""!"""' __ l A"D l TO

i-rv*-*D rf-r^j-jj i~~~ ~

349941 l 349940

4*5567 155566 J455564

386240 l 386237"386234 l l

38624! .386238|386235)

493| 30349454 M .303495 ,— \— — __ L, ^—-.J

"TR lTR \

Term/nation f

6s449644 - 449647 '44964B ,4496s!

TB : TB i TB ' TB

449645'449646 ' 449649 1449652

Castlewood Lakeo"

i 449650 U49653 I449656 , 449657

Silhouette L,

449654 .449655 449658

Crooked

Green

tastbrookL.

500 00'

59'

58'

57'

00

UJ

o:UJ

55'

54'

53'

•490 52'30'

87 0 45'44' 43' 42 4I 40 39 38

37' 36' 3534' 33' 32 3I'

87 0 30*

KABY LAKE M. 187342L03SW0013 2.2334 COUGHLAN LAKE 210

l J.S.H. 498873

LEGEND

HIGHWAY AND ROUTE No.

OTHER ROADS

TRAILS

SURVEYED LINES:TOWNSHIPS, BASE LINES, ETC. LOTS, MINING CLAIMS, PARCELS, ETC.

UNSURVEYED LINES: LOT LINES PARCEL BOUNDARY MINING CLAIMS ETC.

RAILWAY AND RIGHT OF WAY

UTILITY LINES

NON-PERENNIAL STREAM

FLOODING OR FLOODING RIGHTS

SUBDIVISION

ORIGINAL SHORELINE

MARSH OR MUSKEG

MINES

-O

DISPOSITION OF CROWN LANDS

TYPE OF DOCUMENT

PATENT, SURFACE 4 MINING RIGHTS

SURFACE RIGHTS ONLY

MINING RIGHTS ONLY

LEASE, SURFACE S MINING RIGHTS

SURFACE RIGHTS ONLY

MINING- RIGHTS ONLY

LICENCE OF OCCUPATION

CROWN LAND SALE

ORDER-IN-COUNCIL .

RESERVATION

CANCELLED

SAND S GRAVEL

SYMBOL

9

mB

• HT c.s. oc

SCALE : 1 INCH - 40 CHAINSO 5QO IOOO 1 000

FEET METRES

O ZOO 4OO COO 80O l KM

ACRES HECTARES

AREA

CASTLEWOOD LAKE

DISTRICT

THUNDER BAYMINING DIVISION

THUNDER BAY


Ontario Surveys and Mapping BranchDate FEB. 1975

National Topographical Series 42 E 13

Plan No.

M. 1850

43

47

29

2 N

O

4730

6 S

8S 10 S I2

S

4S 6S

8S 20S

22S

24S

43

47

41

43

47

42

r

L5

6W

/2IS

38

35

14

mas

sive

py

, po

(m

t)\

(ve

rt.p

roj.)

44

54

02

A x/

/y

4 4

5 4

O43 4

73

63836

87

— _

~ s

43

47

33

383675

43

47

3

2

41852

6

383678

434735

LE

GE

ND

*S

SY

MB

OLS

AB

BR

EV

IAT

ION

SFe

lsic

m

etov

olca

mc

S

pyro

clas

tic

rock

s

a Q

uartz

- fe

ldsp

ar

porp

hyry

b A

myg

dalo

idal

daci

te;

folia

te

to

shea

red

c Q

uartz

-mus

covi

te

schi

std

Oac

itic

to

rhyo

daci

tic

lapi

lli

tuff

to

tuff

brec

cia

e Ch

erty

da

citic

tu

fff

Dac

ite

Qua

tern

ary

glac

ial

depo

sits

;

mor

aine

s,

gioc

io

fluvi

al,

glac

iola

cust

rine

dnd

outw

ash

Dep

osits

, re

cent

org

anic

5

allu

vial

de

ps.

Dia

mon

d dr

ill

hole

8 n

umbe

r

O

Tren

ch ,

pros

pect

pi

tPR

ECA

MB

RIA

Nl

G

O

Cla

im

post

, lo

cate

d cu

rren

t, no

t lo

cate

d cu

rren

t, la

psed

(C

laim

s pr

efix

ed '

TB

')

Inte

rmed

iate

m

eta

volc

anic

ro

cks

L-2

6 S

L-2

8 S

L-

30 S

L-3

2S

L-3

4S

L-3

6 S

L-

38 S

L-4

0S

L-4

2S

L-4

4 S

L-4

6S

L-4

8 S

L-5

0S

L-5

2S

Magnetic

D

ecl

ina

tion

l

'/2

0 W

12

L0

3S

W0

01

3

2.2

334

CO

UG

HLA

N

LAK

E320

a A

ndes

ite;

mas

sive

to

fo

liate

b A

ndes

ite;

pillo

wed

c A

ndes

ite

to

daci

ted

And

esiti

c tu

ffe

Am

ygda

loid

al

ande

site

M

Maf

ic

to

inte

rmed

iate

m

eta

volc

anic

ro

cks

l U

nsub

divi

ded

a B

asal

t to

an

desi

te,

mas

sive

to

fo

liate

b B

asal

t to

an

desi

te;

pillo

wed

c B

asal

t to

an

desi

te;

schi

stos

e, s

hear

edd

Bas

alt

to

ande

site

; po

rphy

ritic

' to

po

rphy

rye

Bas

alt

to

ande

site

; am

ygda

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alf

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orite

— t

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st

(ultr

a

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ic?

)g

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ic

tuff

h B

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(f

low

?)

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se sill

, fin

e to

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. gr

aine

dfre

sh t

o am

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base

si

ll ,

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ft/or

with

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of

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c

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rite

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Fels

ic

intr

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cks

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nite

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qu

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m

onzo

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ased

imen

tary

ro

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a C

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b C

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, Th

inly

be

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c M

agne

tite-

quar

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iron

form

atio

n,

cher

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ith

hem

atite

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rting

s on

be

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g pl

anes

, le

sser

gre

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ilice

ous

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d A

rkos

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cong

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se,

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rbed

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tuff

brec

cia

B

arko

sic

tuff.

fh 3orp

nyri

tic)

Bedr

ock

outc

rop;

sm

oll,l

arge

(*

20'

dia

met

er)

Area

of

sh

allo

w

subc

rop

Strik

e B

dip

of b

eddi

ng

Stri

ke

B

dip

of

folia

tion,

schi

stos

ity

Stri

ke

B

dip

of

join

ting,

di

p un

know

n

Str

ike

B

dip

of

shea

r zo

ne

Strik

e of

lon

g ax

is

of

pillo

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va

flow

to

p di

rect

ion

indi

cate

d fr

om

j*

pillo

w

shap

e B

pa

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g

Geo

logi

c bo

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ry ;

obs

erve

d,

assu

med

, ge

ophy

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infe

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, flo

w

cont

act

Cre

ek

Spr

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m

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, w

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it of

hi

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gr

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,

rbed

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Ang

ular

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ity

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top

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n

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g fo

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g

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cial

st

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ice

di

rect

ion

unkn

own

©

Min

eral

ized

flo

at

5

*

Min

eral

oc

curr

ence

j

HLEM

co

nduc

tor

8k

desi

gnat

ion

no.;

wid

e, n

arro

w

Ag

Silv

er

Au

Gol

d

cp

chal

copy

rite

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Cop

per

IF(S

) Iro

n fo

rmat

ion

(Sul

phid

e)

Lm

Lim

onite

mt

mag

netit

e

Pb

Lead

po

pyr

rhotit

e

py

pyrit

e

qv

quar

tz

vein

S S

ulph

ides

spti

spha

lerit

e

Zn

Zin

c

gn

gale

na

KE

YK

200

400

F E

c!T

60

0

800

N.T

.S.

42 -

L-4

DE

RR

Yf

MIC

HE

NE

R

a

BO

OT

H

DE

JOU

R

MIN

ES

LT

D.

DIG

HE

M

SY

ND

ICA

TE

JO

INT

V

EN

TUR

E

GEO

LOG

ICAL

C

OM

PILA

TIO

NA

ug..

1976

By:

R.

Rou

tledg

eM

ap N

o.

38

36

78

38367

9

L-6

4S

L- 6

6 S

43

20

69

38

35

'\ \

5

carb

onat

est

ringe

rs

Ag.Z

n.Pb

.Cu.

py,

432068

Car

bona

te

alte

ratio

n

43

15

20

43

15

35

431534

NA

MA

N

LA

KE

Long

La

cA

BB

RE

VIA

TIO

NS

S Y

M B

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SLE

GE

ND

Fels

ic

met

avol

cam

c a

pyro

clas

tic

rock

sC

EN

OZO

IC20

dia

met

er)

LOC

ATI

ON

O

F D

EJO

UR

MIN

ES

LTD

.- DI

GHE

M

SYND

ICAT

E J.V

PR

OPE

RTY

Dia

mon

d dr

ill

hole

8i

num

ber

Tren

ch ,

pros

pect

pi

t

Bedr

ock

outc

rop;

sm

allja

rge

Are

a of

sh

allo

w

subc

rop

Stri

ke

S

dip

of

bedd

ing

Stri

ke

S

dip

of

folia

tion

, sc

hist

osity

Stri

ke

S

dip

of

join

ting,

di

p un

know

n

Str

ike

S

dip

of

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ne

Stri

ke

of

long

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of

pillo

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Ag

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copy

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Cu

Cop

per

IF(S

) Iro

n fo

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(Sul

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Lm

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mag

netit

e

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py

pyrit

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e

Zn

Zinc

an

gale

na

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par

porp

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b A

myg

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daci

te;

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to

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Qua

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mus

covi

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d D

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rh

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citic

la

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mor

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fluvi

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glac

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outw

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, re

cent

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anic

a

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Cla

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post

, lo

cate

d cu

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t ,

not

loca

ted

curr

ent,

laps

ed

(Cla

ims

pref

ixed

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RE

CA

MB

RIA

N

Maf

ic

intr

usiv

e ro

cks

Cre

ek

Spr

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ft/o

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der

swam

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open

m

uske

g

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d,

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el

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Pro

perty

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pl

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lom

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orph

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iorit

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Fels

ic

intr

usiv

e ro

cks

//.

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nite

to

qu

artz

m

onzo

nite

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met

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cam

c ro

cks

Inte

rmed

iate

a A

ndes

ite;

mas

sive

to

fo

liate

b

And

esite

; pi

llow

edAn

desi

te

to

daci

teA

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itic

tuff

Am

ygda

loid

al

ande

site

Lava

flo

w

top

dire

ctio

n in

dica

ted

from

pi

llow

sh

ape

a

pack

ing

Geo

logi

c bo

unda

ry;

obse

rved

, as

sum

ed,

geop

hysi

cally

in

ferr

ed,

flow

co

ntac

tM

ag

ne

tic

Decl

inatio

n

l /2

0 W

DE

RR

Y ,

M

ICH

EN

ER

a

B

OO

TH

Fau

lt,

shea

r zo

ne

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amen

t

Ang

ular

un

conf

orm

ity

S

top

dire

ctio

n

Dra

g fo

ldin

g

Gla

cial

st

riae,

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di

rect

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unkn

own

Min

eral

ized

flo

at

Min

eral

oc

curr

ence

HLE

M

cond

ucto

r ft

de

sign

atio

n no

.; w

ide,

na

rrow

Met

ased

imen

tary

DE

JOU

R

MIN

ES

LT

D.

DIG

HE

M

SY

ND

i G

AT

EJO

INT

V

EN

TU

RE

Maf

ic

to

inte

rmed

iate

m

etav

olca

mc

rock

sC

ongl

omer

ate

Che

rt, t

hinl

y be

dded

Mag

netit

e-qu

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iro

n fo

rmat

ion,

ch

ert

with

he

mat

ite

part

ings

on

bedd

ing

plan

es,

less

er g

reyw

acke

a

sili

ceou

s tu

ff.A

rkos

e,

cong

lom

erat

ic

arko

se,

inte

rbed

ded

tuff

brec

cia

8 ar

kosi

c tu

ff.

Uns

ubdi

vide

d a

Bas

alt

to

ande

site

, m

assi

ve

to

folia

te

b B

asal

t to

an

desi

te;

pillo

wed

Bas

alt

to

ande

site

; sc

hist

ose,

she

ared

d

Bas

alt

to

ande

site

; po

rphy

ritic

to

po

rphy

ry

e B

asal

t to

an

desi

te;

amyg

dalo

idal

Chl

orite

— t

alc

schi

st

(ultr

a

mafic

?)

Maf

ic

tuff

Bre

ccia

,

(flo

w?)

GE

OLO

GIC

AL

CO

MP

ILA

TIO

N

Aug

., 1

97

6B

y!

R. R

outle

dge

N.T

.S

42-

L-

4,

42-E

-I3

UJUJ

UJ

L-2

N

L-O

L-O

L-2

S

L-4

S

L-6

S

L-8

S

L-10

S

L-10

SL-

I2

S

L-I

4S

L-I

6S

L-I

8S

L-2

0S

L-2

0 S

L-2

2 S

L-2

4S L

-26S

L-2

8 S

L- 3

0 S

L-3

2 S

L-3

4 S

L-3

6S

L-

38 S

L-4

0 S

L-4

2 S

L- 4

4 S

L-4

6S

L-4

8 S

L-5

0 S

L-5

0 S

L-5

2S

L E

6 E

N D

A.

N.

Mag

neti

c

Decl

inatio

n

l '/

20

W.

IDS

170

Instr

um

en

t -

Scin

tre

x

MF

-2

(Flu

xgat

e)-

*V

alu

es

in

ga

mm

as

(Pos

itive

re

adin

gs

on

right

si

de o

f lin

e)

Ma

g

Ba

se

520

gam

mas

(B

L

0 +

00)

KE

Y

Base

sta

tio

n

500

gam

mas

(B

ase

Cam

p)

Conto

ur

inte

rval

200

ga

mm

as

Accura

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DIGHEM SYNDICATE ONAMAN JOINT VENTURE SOUTH … · 2017. 1. 17. · Thin inatruioont Bjeaauree the...

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Transcript of DIGHEM SYNDICATE ONAMAN JOINT VENTURE SOUTH … · 2017. 1. 17. · Thin inatruioont Bjeaauree the...