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BEARDMORE AREA LARSON PROPERTY

RICKABY TOWNSHIP FRANK HOUGHTON ft-trf-

K FELDSPAR ALTERED; SILICEOUS. CHLORITIC MAGNETITE PYRITIC ZONES IN GRANODIORITIC INTRUSION. No APPARENT STRONG

DEFORMATION; BUT POSSIBLE ALTERED ROOF PENDANTS - INCLUSIONS ETC - IN INTRUSION.

ZONES MAY OR MAY NOT BE ALIGNED OR ASSOCIATED WITH PALEO STRATIGRAPHY-STRUCTURE.

NUMBER I - NORTH ZONE; TRENCH (45 METERS) ACROSS POSSIBLE N.W. TREND; TWO 3-5 METER ALTERED ZONES IN GRANODIORITE.

DESCRIPTIONSAMPLE(GRAB)

227316

227317

K felds,

silica -

quartz, chlorite,

U magnetite,

IX Py

approximately 3-4

meters; East

sjde^of-trench.

Highly siliceous

with gray

silica megacrysts

- porphyry;

K feldspar;

magnetite seams

and Py.

3 meters

approximately- West

side of

trench.

ASSAY Au PPB

706

'

MAIN ZONE: LARGE TRENCH 30x50 METERS WITH HIGHLY SILICIFIED K FELDSPAR. CHLORITE ROCK WITH CONGLOMERATE INCLUSIONS.227318

Silicified K

felds chlor

weakly sheared

rock, 2-3Z

Py

227319 Highly

silicified -

megacrystlc quartz,

21 Py

227320 Contact

highly altered

(sil -

K felds

- chlor?)

and Lahare

or conglomerate

- 21

Py

227321 Silicified,

pyrltic fine

grained sediment,

3-4Z Py

227322 Highly

silicified -

K felds

- granodiorite,

21 mag;

21 Py

227323 Highly

altered granodiorite

or sediment

(sil -

K felds)

3Z Py

2974-

1399 -

829-

4874-

1258 -

401

Z A

BEARMORE AREA - LARSON PROPERTY CON'T

KiNOHORN ZONE; EXTENDS TO THE KINGHORN ROAD. TRENCHED "ACROSS TREND" IN K FELDS QUARTZ - CHLORITE GRANODIORITE FOR

———————

SOME 60 METERS. INCLUDING A 6 METER SHEAR OR INCLUSION - HIGHLY CARBONATIZED - WITH 20* QUARTZ STRINGERS.

SAMPLE DESCRIPTION

ASSAY————

————————

AUL-ERE227324

Highly carbonatlzed

- K

felds -

quartz rock

- foliated;

20* quartz

strlngtrs, 1-3Z

sulphldt 368"0'

227325 Ditto

977 - tt9

LINE 2 TRENCH; K FELDS. CHLORITE, QUARTZ (8 METERS) IN ALTERED GRANODIORITE.

227337 Quartz

- 95Z

quartz eyes,

some 1nterst1al

K felds,

carbonate patches,

<^H magnetite,

21 pyrite.

308

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LEGEND

PHANEROZOICCENOZOIC* * "——'

QUATERNARY HECENT

Swamp, lake, and i/ioa/n iloposih

PLEISTOCENEStintl. yiavol, tntl clay

UNCONFORMITY

PRECAMBRIAN 6MIDDUETO LATEfKCCAMBRIAN

(PROTEROZOIC)

LATE INTRUSIVE ROCKS

St 0/oftaso.1 l f b Feldspar-quail l porphyry iclaled lo

diabase.INTRUSIVE CONTACT

EARUY PRECAMBRIAN (ARCHEAN)

FELSIC TO INTERMEDIATE INTRUSIVE ROCKS

Crtuiudioiilv, ttontlliicnutc. quailldiorite, dioflleGranito, qutrti monionllu

4c Feldspar porphyry ana qutrttfrit/spar porphyry dikes

4tl Giamlic and peumalilic didci MInlvd lo in and lit.

•ft1 HytinJ leluc lo inli'imcili.ilu inliuwe locus

MAFIC INTRUSIVE ROCKS

3i Dionlo, quar/; diorlle, gabbro. 3b Gubbto. , 3c Malic dike*INTnUSIVt CONTACT

METAVOLCANICSc FELSIC TO INTEUMfDlATC

METAVOLCANICSf V/nauvuiviuvwla lull breccia and pyroclastic bice

?fi Lapilli lullle Crystal lull.Id laminated lullle Amygdaloidal lava.21 Pillow lava and related brecciatg Massive and flow banded lavas.In Spherulitic and How banded lavasfi Quartt feldspar iiorphyry.Ik feldspar porphyryim Derived sericitic schist

CONPORMAPLE CONTACT INTERCALATtP IN PART

MAFIC TO INTERMtOIATC METAVOLCANICS

l Unwbdivlded la Massive lava t b Amygdaloidal lava le Volcanic breccia and agglomerate td Pillow lava lo Derived chloritic schist lg TullKBOui, chert associated with

mafic molavolcanlci

SilvfColdBonnie.CuibonalCChalcopyriteCopper.GalenaMolybdenumNickelleadPyrrhotitePyriteQuaitlSphaleriteSpeculariteSulphide riunlotuinalinvlllll

'Unconsolidated deposits. Cenozoic deposits are rep resented by the lighter coloured parts ol the map ^Bedrock ooolouy. Outcrops and Interred oitenslont ol etch map rock unit are shown respectively In deep and light tones ol the same colour. Where In places a formation Ik loo narrow lo show colour and must be represented In lilac k. t i,hort black bar appotts in Ihe appropnale block"Hacks In those groups ara subdivided lilhologlcally and the order doun not Imply age riiatlanihlp within

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HOUGHTON OPTIONIP/RESISTIVITY SURVEY

PROJECT: HOUGHTON OPTION PROJECT # : 2265 BASLLINL AZIMUTH : 155 Deg.

SCALE ^ 1 : 2500 DATE : 11/25/91 SURVEY DY : JM/MM/MS NTS :

RLE: M2265CHNORANDA "