52Na4SEeei82 2 .7616 BALMER TWP 010

GOLDQUEST EXPLORATION INC.

REPORT ON THE GEOLOGY OF THE PINDAR CLAIM GROUP

SOUTHERN PORTION

BALMER AND BATEMAN TOWNSHIPS

RED LAKE MIMING DI.VISI.ON

RED LAKE, ONTARIO

RECEIVED

^C 28 1984

MINING LANDS SECTION

OCTOBER 1983 BY: Stephen McGibbon

INTRODUCTION;

The Pindar Claim Group was staked for Dickenson Mines Limited in 1979.

The property adjoins an extensive area of patented and staked claims that

together make up part of the holdings of Goldquest Exploration Incorporated.

The present survey was conducted on twenty-one claims located at the

southeast corner of the group, and was primarily interested in mapping the

geology, as well as relocating old work (trenching, drilling) performed by

previous operators.

The claims are located fourteen kilometres northeast of the community

of Red Lake, and can be reached via a winter road branching off of Johnson Road,

which intersects Nungesser Road at a point 8.6 kilometres from highway 125.

(See Figure l).

This area is largely covered by swamp, muskeg, and glacial till, with

bedrock having about two percent surface exposure, and found almost exclusively

on the six most easterly claims.

PRESENT WORK;

Geology and VLF surveys were conducted concurrently by the author,

W. Wirowatz, and l. Spooner, during August, Setpember, and October 1983.

These surveys were performed by traversing 25 metre picket lines spaced 100

metres apart, and the data plotted at a scale of 1:2500.

Interpretation and evaluation of the VLF survey is not included in

this present study; two map sheets showing results of the geology survey are

appended.

Claims examined in the survey are listed in Table 1; not all are

part of the Pindar Claim Group.

[tOLDCHJEST EXPLORATION INC.

RED E AREA,ONTARIO

PROPERTY MAP

DISTRICT OF KENORA

SCALf ' I'7850O O i t

DUCHESNE—y————. BALARD l

COMMANDER

cDONOUGH TWP.

PRESENTMCDOUGALL

CAMPBELL RED LAKE MINES LTD.

DICKENSON MINES LTD.

TOWNSHIP CORNER' LOCATED TWELVE MILES,(19.J KU) CUE WEST OF THE NORTHEAST CORNE OF DOME TOWNSHIP

INSET SCALE-SAME

SOUTHEASTROWAN GROUP

KEG LAKE

fp'

TABLE

K.R.L. 22236

K.R.L. 22237

K.R.L. 222*12

K.R.L. 16903

K.R.L. 5095***l

K.R.L. 5095**5

K.R.L. 5095^6

K.R.L. 5095*17

K.R.L. 5095*48

K.R.L. 563850

K.R.L. 563851

K.R.L. 563852

K.R.L. 563853

K.R.L. 563854

K.R.L. 563939

K.R.L. 5639**0

K.R.L. 5639^1

K.R.L. 5639*12

K.R.L. 5639*13

K.R.L. 5639*1**

K.R.L. 5639**5

HISTORY OF PREVIOUS WORK;

No less than five operators have carried out work on portions of the

claim block covered by this survey.

O'Keefe Red Lake Mines, in 19^6, performed magnetic and geological

surveys over a group of 27 claims at the extreme northeast corner of Balmer

Township; two of which (5^39^2 and 5639^3) are held by Goldquest. The magnetic

survey, and subsequent drilling (three X-ray holes totalling 6^ m) helped to

define the greenstone-granite contact. No economic mineralization was intersected,

Also in 19^*6, Janet Red Lake Mines Limited carried out a magnetometer

survey and detailed surface examination over fifteen claims situated west of the

O'Keefe group. Their results indicated the property was underlain by rocks of

the Keewatin volcanic assemblage as well as a narrow band of sediments with iron

formation. Geological and geophysical evidence also suggested the presence of a

northeast trending fault zone eminating from the Clicker property to the south

and extending to a deep narrow embayment of volcanics in the Trout Lake Batholith

northwest of Walsh Lake.

In 195^, a block of 18 claims, covering a large part of the present

survey was optioned to New Dickenson Mines Limited by Charlie Peterson and

John Gomez. The work carried out consisted of a systematic channel sampling

program in a trench exposing predominantly copper mineralization in carbontized,

resilicified, sedimentary rock. Results indicated mineralization to be erratic,

and generally lacking in the exposed rock.

During 1957, Cordoba Mines Limited carried out a major drill program

over their holdings in Balmer, Bateman, and Ranger Townships. The drilling was

concentrated within four claims which just overlap the extreme southeast corner

of the Goldquest claims (KRL 5639^3) near Adam's Lake. The drill logs show the

geology to be mainly mafic volcanics with numerous narrow silicious bands con

taining variable amounts.of iron sulphides, magnetite, and graphite. Some

clastic sediments and felsic intrusives were also noted. The best assays returned

from dril l ing were:

2.76 ozs. Au/5.0 feet

0.17 ozs. Au/2.6 feet

0.06 ozs. AuA.8 feet

The southeast portion of the Pindar Claim Group is part of a large block

HISTORY OF PREVIOUS WORK: Cont'd

of claims staked for Dickenson Mines Limited between August 1979 and October 1981

Since then, linecutting, magnetometer, and horizontal loop surveys have been

conducted over the twenty-one claims comprising this study.

LOGY;

Regionally, the map area is located in the lower mafic sequence

{predominantly tholeiitic) of the Red Lake greenstone belt. Locally, the

geology consists of mafic metavolcanic sequences and metasedjraentary .strata.

intruded by rocks of felsic to mafic composition.

The mafic metavolcanic sequences consist of green to black, fine

grained pillow basalts and flows intercalated with minor mafic lapilli tuff.

These units are often chloritic, display variable degrees of biotite alteration,

and occasionally exhibit localized carbon! t ization, silicification, and

calcification. Homogeneous mafic flows are most commonly observed, however,

on weathered surfaces, light and dark flow bands can sometimes be discerned.

Pillow basalts are rarer and deformed so as to obscure stratigraphic tops.

Lapilli tuff is observed on two outcrops only. The unit appears banded and

contains less than five percent lap! 1 1 i -sized fragments.

Intercalated clastic and chemical metasedlmentary rocks are common

in the map area. The clastic unit, an argillite, is best identified by distinct

banding of laminae, strong folding, and differentially weathered outcrop surfaces.

Laminae bands and wisps are the only primary sedimentary structures observed.

Fine grained biotite, amphibole, and pyroxene, as well as medium to coarse -

grained, pink to red subhedral garnets are common in argillites on the eastern

boundary of the property, near the Balmer-Bateman township line. This mineral

ogy reflects the thermal metamorphic aureole of the Trout Lake batholith, and

represents a change from greenschist to amphibolite facies metamorphism.

The chemical metasedimentary units are represented by oxide and sulphide

facies iron formation. These are most often contained within the argillites, are

two metres (or less) in width, and are often covered by rust or yellow coloured

gossan. Common minerals within these horizons are finely to coarsely crystalline

pyrite, finely disseminated magnetite, pyrrhotite, and chalcopyrite. Aresenopyr i te

is rare. Barrren chert horizons are often found adjacent to iron formation, and

may be an unmineral i zed sequence of the same unit.

The metavolcanic and metasedimentary rocks are intruded by at least

two generations of felsic to mafic dykes (and sills?). The most extensive of

these is a series of massive to very well foliated gabbroic intrusives which

generally strike north-south across the eastern portion of the map area. Massive

varieties range from fine - to coarse - grained, and contain subhedral crystals of

pyroxene. Considerable alteration of pyroxene to hornblende and biotite is common.

GEOLOGY: Cont'd

Another late intrusive body, confined to an area just north of Adam's

Lake, contains phases ranging from gabbro to granodiorite. Although many phases

intermediate to these are observed, the rocks are inferred to represent separate

intrusive bodies. The gabbro is massive, medium - to coarse - grained, and

contains subhedral to euhedral hornblende phenocrysts in a groundmass composed

of quartz, anorthite, tourmaline, and sphene. The granodiorite is also massive,

medium - to coarse - grained, but contains hornblende and biotite phenocrysts in

a groundmass of quartz, alkali feldspar, and plagioclase. Inclusions of a fine

- grained mafic rock, varying in size from 0.5 cm to 15 cm, are found within

the granodiorite. Rock similar to the granodiorite, but lacking the mafic

inclusions, is found at the north property boundary. Some doubt remains as to

whether these are outcrop or boulder.

STRUCTURE;

Fabrics developed in the mafic metavolcanic and metasedimentary

sequences suggest the presence of east-west field of compression, possibly

related to the intrusion of the Trout Lake batholith.

Locally, a belt of intense drag folding, producing "M" and "W" style

folds, run parallel to lithologic units at the eastern end of the property.

Strongest folding is largely confined to meta-sedimentary units near the Balmer-

Bateman Township line (See Figure 2). Well developed boundinage, trending 012 0 ,

is also found near the township boundary, within argillites in contact with

iron formation.

Drag folds within mafic sequences are not as well pronounced, but the

generally shallow plunge of the folds toward the south is consistent with those

in the metasediments. Pillow flattening in basalts west of Adam's Lake trend

at 15 1* 0 .

A pervasive, north-south striking, steeply east and west dipping fol

iation is sympathetic to the outline of the Trout Lake intrusive; it turns slightly

to the southeast at the southern claim boundary of the property.

A lower hemisphere stereonet projection of joint and dyke orientations

show that while jointing is widely dispersed, mafic and felsic intrusives are

limited to two orientations {See Figure 3). Gabbro and diorite dykes strike

predominantly north-south, while felsic dykes strike north-south and east-west.

Faulting occurs north of the township line where a tectonic breccia,

trending at 211 0 and at least one metre in width, is exposed. Whether or not

this breccia represents a major northeast-southwest trending structure across

the property to the west is uncertain.

TREND AND PLUNGE OF FOLD AXES

FIG. 2

'JOINT AND DYKE ORIENTATIONS

-.—J-o-—.

FIG. 3 POLE TO JOINT

POLE TO DYKE o FELSIC

AMAFIC

ECONOMIC GEOLOGY;

Although mineralization was encountered in all environments, the most

significant quantities were confined to iron formation, argillites, and quartz

veins.

Within the iron formations, minerals such as magnetite, pyrite, pyrrhotite,

chalcopyrite, and bornite were observed. In most cases the mineralization was

fine grained and disseminated. The copper minerals occurred in trace amounts.

Within the argillites, pyrite, magnetite, and arsenopyrite were present,

the latter of which was finely disseminated and occurred in trace amounts.

Qjjartz veining occurred sporadically, in widths up to 30 centimetres,

in all environments. Magnetite, pyrite, chalcopyrite, and malachite were

observed. The copper minerals again occurred in trace amounts.

Mineralization within mafic sequences was rare (Sample P4l), but when

encountered included trace amounts of finely dissiminated pyrite and/or arseno

pyrite. This rock was often silicified, but no gold values were returned.

Traces of pyrite were sometimes present in the mafic and felsic

intrusive rocks.

Select grab samples from all environments were assayed for gold and

silver. No visible gold was observed. Only one gold assay returned was above

"trace" in amount. Sample P28-1 assayed 0.03 ozs.:.AuXton, and was located in

a si ightly si lici f ied metasediment near the contact with a diorite dyke. Several

silver assays returned values in the 0.50 ozs. Ag/ton range, but only one

sample, P-l^S-B-Z, was above one ounce. Specifically, this assay of l.OA ozs. Ag/

ton was located in a foliated metagabbro containing less than one percent dis

seminated pyrite.

CONCLUSIONS AND RECOMMENDAT I ONS;.

Much of the area comprising the south east section of the Pindar Claim

Group has no surface exposure of bedrock. In the eastern most claims, where

outcrop is abundant, the present survey was successful in outlining a series of

sub-parallel chemical and clastic metasedimentary units which can be correlated

with known geophysical anomalies. Similar anomalies exist in areas where bed

rock is not exposed, and may represent more metasedimentary horizons. Previous

operators have investigated parts of these units, mainly in an area just north

of Adam's Lake. High, yet erratic gold values were returned.

Conductors identified by geology and/or geophysics currently represent

the best exploration targets, and will require being tested by diamond drills.

Those not exposed on surface should be given priority so that geological information

can be recovered from areas with thick overburden. Beyond this, development of

new exploration targets on the property will be necessary.

As a means to this end, the following preliminary guidelines are

suggested:

1. In conjunction with a more regional program, samples from outcrop areas and

recovered drill core should be collected, described, and analyzed using whole

rock geochemistry. With this, geochemical "background values" can be assigned

to rock types in a certain area.

2. When gold mineralization is encountered, a similar program can be applied to

identify minerals associated with the gold, and zones of alteration surrounding

it. Hopefully, a geochemical signature can be identified with this mineral-

izat ion.

The above, if carried out with future mapping and drilling, may

provide tools identifying mineralization which lacks geophysical expression, and

serve as a basis for developing new exploration targets.

OCTOBER 1983 STEPHEN McGIBBON

CERTIFICATE OF QUALIFICATION

l, Stephen McGibbon, fulfilled the requirements for a B.Se. (Honours,

Geological Sciences) degree from Queen's University in May 1983.

l have worked in the field of mineral exploration since the summer of

1981, and am presently employed by Goldquest Exploration Inc., as a contract

geologist.

l have no financial interest in the properties or securities of Goldquest

Exploration Inc.

October 31, 1983

Signed: Stephen McGibbon

52Ne4SE0002 8 .7616 BALMER TWP

Mining Lands Section

Control Sheet

File No J?

900

TYPE OF SURVEY

MINING LANDS COMMENTS:

GEOPHYSICAL

GEOLOGICAL

GEOCHEMICAL

EXPENDITURE

Signature of Assessor

Date

i

f" , X v Ministry of |C0 J Natural

" y\7^// Resources Ontario

, Report of Work(Geophysical, Geological, Geochemical and Expenditures)

The Mining Act

f*- 8 c. o ^ f.Instructions: — Please type'or pfint.

— If number of mining claims traversed exceeds space on this form, attach a list.

/yNote: — Only days credits calculated in the "Expenditures" section may be entered in the "Expend. Days Cr." columns. Do not use shaded areas below.

Type of Survey(s) Townsffip or Area

Claim Holder's)

(S-0 JLDQUZSTAddress

y/ C.

(Prospectors Licence No.

l 7" A? .2. O

Survey Comparg ;t^oo ..A? 0.^0.* A/f/,0*. .-.vfTT. J^rr, To^o^ro. 0/tr, Ms 4 3ny A Date of Survey (from Si to) Total Miles of line *B*.

Name and Address of Author (of Geo-Technical report): l ffi l 0& l M? l Vr3 V*

— /iorxf-tj X?Credits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)Special Provisions

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

- Electromagnetic

For each additional survey: using the same grid:

Enter 20 days (for each)

Complete reverse side and enter total (s) here - Electromagnetic

DMINING IVe c E i y'

Note: S pecial provisiocredits do not apply 4 to Airborne Surveys.

romagnettc

Magnetometer

Radiometric

Expenditures (excludes'power stripping)Type of Work Performed

Performed on Claim(s)

Calculation of Expenditure Days Credits

Total Expenditures

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

Recorded Holder or Agent (Signature

Certification Verifying Report of Work

BATEMAN TR -M.2I39

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LEGEND

- FFI ST TO irJTpRMfniATr PI innwir INTRUSIVE

8 . 8A GRANITE .QUARTZ MONZONITE

l^ww , rp| cir TO iwTrRurniATF HYPABYSSAI INTRUSIVES

7 ;. : 7A QUARTZ PORPHYRY

7C QUARTZ- FELDSPAR PORPHYRY

7D PEGMATITE, FELSITE, APLITE

.^jM^fi— MAFIC TO ULTRAMAFIC INTRUSIVES

H^Bfcll GA GABBRO, DIORITETS"ffllHiy 'frJ Am^

^^^^v m 6C PERIDOTITE

n6D LAMPROPHYRE

,". ,. — THFMir*! UFTA*;FniMFHTfi

g - 5A CHERT H5B OXIDE FACIES IRON FORMATION

' - 5C CARBONATE FACIES IRON FORMATION 5D SULPHIDE FACIES IRON FORMATION

56 GRAPHITE .

p- CLASTIC METASEOIMENTS

ff||l||p i - 4* ARGILLITE , MUDSTONE

I^V^1! J 4B ARENITE, ARKOSE, GREYWACKE^

^^ 4C CONGLOMERATE

i FFI SIC UFTAV01 CAMICS

3 '- " 3A HOMOGENOUS TO PORPHYRITIC FLOWS

—————— [ ^ 3B PYROCLASTIC BRECCIA, TUFF BRECCIA , AGGLOMERATE

| ^ 3C TUFT, LAPILLI TUFF, LAPILLISTONE

3D SPHERULITIC FLOWS

3E RHYOLITIC

5F DACITIC

,,, .,. |NTFRMFm*TF UFTAVOI CAWICfi

2 1 2* HOMOGENOUS TO PORPHYRITIC FLOWS

—— ---— a ^0 2B PYROCLASTIC BRECCIA, TUFF BRECCIA, AGGLOMERATE

— 9H 2C TUFF; LAPILLI TUFF, LAPILLISTONE

20 AMYGDALOIDAL FLOW

2E ANDESITIC

2F DACITie

2P PILLOWED FLOWt

. ., . ..— MfiFIC TO ULTRAMAFIC MFTAVOI CANICS

1 -,V ' A HOMOGENOUS TO PORPHYRITIC FLOWS* - *t ' - - 1- _———— ̂ ^ ^PB B PYROCLASTIC BRECCIA, TUFF BRECCIA, AGGLOMERATE

^9 C TUFF, LAPILLI TUFF, LAPILLISTONE

D AMYGDALOIDAL FLOWS

E FLOW BRECCIA

m F CHLORITE 1 T ALC-CHLORITE SCHIST

P PILLOWED FLOWS

V VARIOLITIC FLOWS

I! X SPINIFEX

BH I.6A MASSIVE FLOW POSSIBLY INTRUSIVE

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GOLDSUfSTDICKENSON

FELSIC TO INTERMEDIATE HYPABYSSAL INTRUSIVES

7A QUARTZ PORPHYRY

7B ' FELDSPAR PORPHYRY

7C QUARTZ- FELDSPAR PORPHYRY

7D PEGMATITE, FELSITE,APUTE

MAFIC TO ULTRAMAFIC INTRUSIVES

6A GABBRO, DIORITE

6B PYROXENITE

6C PERIDOTITE

6D LAMPROPHYRE

CHEMICAL METASEDIMENTS5A CHERT5B OXIDE FACIES IRON FORMATION

CARBONATE FACIES IRON FORMATION

SULPHIDE FACIES IRON FORMATION

GRAPHITE

METASEDIMENTS

ARGILLITE .MUDSTONE

ARENITE, ARKOSE, GREYW AC KE

CONGLOMERATEu)|TW ORIENTATION

FELSIC METAVOLCANICS

3A HOMOGENOUS TO PORPHYR1TJC FLOWS

|^ J] 38 PYROCLASTIC BRECCIA.TUFF BRECCIA, AGGLOMERATE

TUFT, LAPILLI TUFF, LAPILLISTONE

SPHERULITIC FLOWS

RHYOL1TIC

DACITIC

INTERMEDIATE METAVOLCANICS

2A HOMOGENOUS TO PORPHYRITIC FLOWS

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