: other ( j claim no. hole no. footage date note€¦ · m-sh-2 summary log o -4m 4 - 961 m 961 -...

11M6NWe06S 10 SHEPPARD

TOWNSHIP; FALCONBRIDGE ) s Ko^l dt k *

WORK PERFORMED FOR: FALCONBRIDGE LTD.

RECORDED HOLDER: SAME AS ABOVE

: OTHER ( J

010

REPORT NO: 1 0

CLAIM NO.

1157854 *

1157853 H-

1157852

HOLE NO.

M-SH-2

FOOTAGE DATE NOTE

2200 m SEPT-NOV/91 (1)

NOTES;(1) W9270.00029, FILED NOV/92.

o o

oCM

M-SH-2

0.00m.

Go^>ganda Fm.

Nipissinj Diabase

l Gowganda

Espanola Fm,

Bruce Fm.

Mississagi Fm. McKim Fm.

Matinenda Fm.

fM-SH-2'^4

o? o

/ Serpent Fm.

FALCONBRIDGE LIMITEDEXPLORATION

Mirage PropertySheppard Twp.

SECTION LOOKING NORTH

TrtccJ kj

•.Km mst Kit 1 1/92

Sujxrvlwd li; 11. TXOSCon

terixi kj :J

PUn M.

l : 1 (000 (mctrei) JOO

M-SH-2 SUMMARY LOG

O -4m

4 - 961 m

961 - 1141 m

1141 - 1449 m

1449 - 1558 m

1558 - 1763 m

1762 - 1784 m

1784 - 1828 m

1828 - 1836 m

1836 - 1900 m

1900 - 2200 m

2200 m

Overburden (casing).

Gowganda Formation- interbedded sequence of conglomeratic wacke with siltstone and arkosic beds.

Nipissing Diabase- fine to medium grained greenish - grey gabbro, trace amounts of pyrrhotite and chalcopyrite are locally disseminated. Contacts are sharp and chilled.

Gowganda - Serpent Formation- conglomeratic wacke interbedded with siltstone and arenite in increasing amounts with depth.

Espanola Formation- rhythmically interbedded laminated white limestone, siltstone and less abundant greywacke.

Bruce Formation- polymictic conglomeratic greywacke with mudstone and wacke beds.

Transition to Mississagi Formation- dark grey massive beds of mudstone increasingly more chloritic with depth.

Mississagi Formation- commonly crossbedded sandstone and arkose interlaminated with minor argillite.

Ramsey Lake Formation- polymictic paraconglomerate

McKim Formation- greywacke rhythmically interbedded with argillite

•~. *Matinenda Formation

- interbedded sequence of medium to coarse grained sandstone and arkose with minor laminae of siltstone.

End of hole.

HOLE NUMBER: M-SH-002FALCONBRIDGE LTD

DRILL HOLE RECORD IMPERIAL UNITS:DATE: 07/20/1992

METRIC UNITS:

PROJECT NAME: MIRAGEPROJECT NUMBER: 6-249

CLAIM NUMBER: S.1157854,1157853,1157852LOCATION: SHEPPARD TOWNSHIP

PLOTTING COORDS GRID: FALSE GRIDNORTH: 1000.00NEAST: 1000.00EELEV: 335.00

COLLAR ASTRONOMIC AZIMUTH: O' O' O"

DATE STARTED: 09/12/1991DATE COMPLETED: 11/13/1991

DATE LOGGED: / /

COLLAR SURVEY: YES MULT ISHOT SURVEY: NO

ROD LOG: NO

ALTERNATE COORDS GRID:NORTH: 0+ O EAST: 0+ O ELEV: 0.00

GRID ASTRONOMIC AZIMUTH: 0- O' O"

PULSE EM SURVEY: YES PLUGGED: NO

HOLE SIZE: NO

COLLAR DIP: -90* O' O"LENGTH OF THE HOLE: 2200.OOM

START DEPTH: O.OOMFINAL DEPTH: 2200.OOM

CONTRACTOR: LONGYEAR CANADA INC.CASING: HQ, 3.95m

CORE STORAGE: FALCONBRIDGE,FALCONBRIDGEUTM COORD.: 5198320N, 538500E

COMMENTS :WEDGES AT: No. 1 a 221.6; No. 2 3 238.7; No. 3 3 164.6

DIRECTIONAL DATA:

Depth (M)

11.2826.5241.7660.0578.3396.62133.20163.78164.60200.25221.59229.21238.66248.11308.15369.11420.93484.94548.95609.91670.87731.83792.79853.75978.71

Astronomic Dip Type of Azimuth degrees Test

195' 0-222- 0'228" 0'241* 0'231* 0'253* 0'247- 0'253- 0'253* 0'256* 0'261- 0'262- 0'264* 0'262* 0'272- '273- '275- '274* '273* '273* '274- '274' '274- '275- '277* '

0" -88-75'0" -88-75'0" -88*40'0" -88*35'0" -87*90'0" -87-50'0" -85-95'0" -85-25'0" -85*20'0" -83*80'0" -83-30'0" -84-30'0" -82*30'0" -82* 0'" -79- 9'" -79* V" -78* 3'" -77- 9' i .77. i" -76* 5'" -76-25'" -75- 9'n .75. ii. -74- v" -72* 8'

0"0"0"0"0"0"0"0"0"0"0"0"0"0"nH

H

H

H

M

nIIH

II

H

SSsssssssssssssssssssssss

FLAG Conments

OKOKOKOKOKOKOKOKOK WEDGE #3 OFF M-SH-2OKOK WEDGE #1 OFF M-SH-2OKOK WEDGE #2 OFF M-SH-2OKOKOKOKOKOKOKOKOKOKOKOK

Depth CM)

1039.671094.541157.631221.641282.601343.561404.521465.481526.441593.491648.361709.321770.281831.241892.201953.162044.602105.562166.522200.05

Astronomic Dip Type of FLAG Azimuth degrees Test

278* '0* '0- '

278- '0- '

280- 5-285* '

0- '287- '291- 5'293* '294- '295- '300- 5'302* 5'300- 0'312* '312*30'315- '316-30'

-

H .72- 91 nH -72- 71 Mn * t H" -72- ' "II * 1 H

i. .71 . 2, .." -70* 5' " l * 1 H

" -69- 4- "H .66- 5! .

H .65' . M

" -62* ' " i .6T 31 i.n -60- 2' "" -58* 8' "" -58* 2' "M .56. V 1.

H .55. 5, Hn -54. 3. nII .53- 71 K

-

Ssssssssssssssssssss

OKDO

OK

OKOK

OKOKOKOKOKOKOKOKOKOKOKOK

Comments

DIP ONLYBAD TEST

BAD TEST

BAD TEST

E.O.H.

HOLE NUMBER: M-SH-002 DRILL HOLE RECORD LOGGED BY: R. MEECHAM, D. TRUSCOTT PAGE: 1

HOLE NUMBER: M-SH-002 DRILL HOLE RECORD DATE: 07/17/1992

FROM TO

ROCK TYPE TEXTURE AND STRUCTURE

ANGLE TO CA ALTERATION MINERALIZATION REMARKS

0.00TO

3.95OVERBURDEN CASING

Till, unconsolidated sand with pebble to boulder- size clasts

3.95TO

960.75

PEBBLY WACKE

GOWGANDA FORMATION 3.95 TO 960.75

3.95-186.00Light to dark greywacke matrix contains ":15*i sub-angular to rounded clasts consisting of granite, tonalite, gabbro, mafic volcanics and a variety of sediments ranging from 1cm to 15cm in diameter grainsize of matrix particles but no siltstone material is evident. The unit is rhythmically laminated to bedded, ranging in thickness from 1cm to less than 1m at 90* 10' to c.a.

Quartz-carbonate-feldspar veinlets up to 2cm thick at various angles are spaced at 2.0 - 5.0m intervals. Narrow veinlets at 25*-50*, wider veinlets at 60*-80* to c.a.

34.4-37.65 Intersect DDH M-SH-1

221.6#1 Wedge

238.7#2 Wedge

Tr to IX scattered Py cubes to 1cm

Weak carbonate and quartz halo with chlorite associate usually with veinlets.

Tr Cp, Py, gal in most larger (1-2cm) veinlets

186.00TO

265.00PEBBLY WACKE/ PEBBLY/ SILTSTONE

Matrix as 3 .95 to 186.00 interval but subintervals of siltstone are common and gradational.

- bedding sometimes apparent, generally vague, to 65* to 70* to c.a.

- narrow cross-cutting quartz-carbonate-feldspar veins to 5cm a 30* to 80* to c.a., generally 60*, 50cm spacing, becoming more frequent with depth. Larger veins a 80* quartz with K-feldspar rims.

- wide silicified haloes to 5cm chlorite

- local weak carbonatization

Trace - 1X Cp * Py * Po * Gal. One vein 2-355 with trace galena and Py at 278.0m at 50* to c.a.

HOLE NUMBER: M-SH-002 DRILL HOLE RECORD LOGGED BY: R. MEECHAH, D. TRUSCOTT PAGE:

HOLE NUMBER: M-SH-002' DRILL HOLE RECORD DATE: 07/17/1992

FROM TO

265.00 TO

280.00

280.00 TO

302.00

302.00 TO

311.50

311.50 TO

698.00

.

ROCK TYPE

SUDBURY BRECCIA

PEBBLY WACKE/ PEBBLY/ SILTSTONE

SUDBURY BRECCIA

PEBBLY WACKE/ PEBBLY SILTSTONE

TEXTURE AND STRUCTURE

Good fluidal textures in matrix.

As 186.00 to 265.00 interval

Fragments well-rounded and conprised of laminated wacke/siltstone (micro faulted), pebbly wacke, pebbly siltstone, diabase.

As 280.00 to 302.00 interval. Occasional Sudbury Breccia veinlets and dikelets throughout section.

455.0 - 505.0 Strongly fractured and micro faulted. Indicative of fault? Mainly pebbly siltstone within this zone.

480.0 - 494.0m Sudbury Breccia contains scattered, narrow quartz-carbonate veins.

499.5-500.0 Broken core.

498.0-505.5 Mainly fine pebbly wacke, abundant microfractures (annealed), and quartz-calcite veinlets with K-feldspar or epidote selvedges (45'- 60' to c. a.). Many calcite-rich veinlets have large plates of Py H plane of fracture/veinlets.

504.6 1cm thick band of chlorite-rich rock (pseudo- tachylite?) at 60' to c. a.


Broken core; numerous fractures, possible fault zone.

HOLE NUMBER: M-SH-002 DRILL HOLE RECORD LOGGED BY: R. MEECHAM, D. TRUSCOTT PAGE:

HOLE NUMBER: M-SH-OOi DRILL HOLE RECORD DATE: 07/17/1992

FROM TO



514.75-550.0Mainly pebbly siltstone or very fine grain pebbly wacke (grades into finer rock over ^ 30cm). Relatively uniform with -eSX clasts 2mm - hairline epidote fracture fillings common - local calcite and quartz veinlets with epidote or K-feldspar selvedges and Py flakes.

550.0 - 660.0Massive pebbly wacke - grey to black. Lacks veining as in 1st 500m, but contains several narrow (2mm) quartz-carbonate veinlets at 25'- 30" to c.a.

562.0 - 565.0 Broken core.

614.0 - 629.0 Black matrix.

629.0 - 636.0 Broken core.

668.0 - 683.0Sections of broken core.

684.0 - 689.0Sudbury Breccia - high percentage of matrix - very good fluidal textures. Above and below the rock is strongly fractured and altered.

524.72-525.2 Strong epidote alteration.

550.0 - 550.0 Moderate pervasive epidote alteration and broken core (moderate).

535.4 - 536.5 Moderately broken core

- 1X disseminate Py- several sulphide clasts or sulphide- bearing clasts

Moderate to strong fracture controlled to pervasive epidotization.

698.00TO

780.00INTERBED GREYWACKE AND SILTSTONE

Rhythmically interbedded greywacke, siltstone and narrow (20cm) arenaceous beds, that are rich in epidote and chlorite. Bedding is at 60* to c.a. Minor Sudbury Breccia dikelets.

Occasional microfaulting (approx. 1 per 2m) with consistent dextral displacement, usually along steep planes at 30'- 40' to c.a.

720.0 - 780.0

Soft sediment deformation of epidote-rich beds at 720m - 771m.

Some disseminated Py and Po with trace of Cp especially in epidote/chlorite zones. Trace - 1X Cp * Po in Sudbury Breccia

HOLE DUMBER: M-SH-002 DRILL HOLE RECORD LOGGED BY: R. MEECHAM, D. TRUSCOTT PAGE:


FROM TO

780.00 TO

807.00

807.00 TO

960.75

960.75 TO

1U0.65

ROCK TYPE

wSDBXw SUDBURY BRECCIA

wAREw SILTSTONE/ ARENITE

wGAB* NIPISSING DIABASE


Predominantly siltstone with graded beds to fine grained wacke. Bedding thickness averages 2cm, dipping at 60'- 70'. Colour is primarily dark grey to black with minor light grey to pale green arenaceous beds.

Networks of multi -orientated 1mm fractures are increasing towards 780m.

Various sedimentary structures such as cross- bedding, graded bedding, soft sediment deformation structures, slumping, rip-ups, and flames, are evident throughout this unit.

780.0 - 807.0 Fragments are siltstone, wacke and arenite. Good fluidal textures.

Interbedded siltstone, arenite and minor quartzose wacke. Arenaceous beds alternate at 1-2m intervals, ranging in thickness from 15cm to 150cm (avg. 30-40cm). Graded bedding is common with arenite/siltstone equal proportions towards 900m. Occasional pebbles and minor Sudbury Breccia. Arenite dominates base of unit.

Greenish-grey, medium to coarse grained equigranular, massive to weakly foliated rock with sharp, fine grained - chilled margin. 10m wide.

Pegmatitic patches occur occasionally. Variations in grain size may be due to layering.

Scattered (*:1mm) reddish-purple mineral trace only - garnet?

At 1000m the rock is primarily coarse grained gabbro.

Minor randomly orientated quartz veins up to 7cm wide are scattered throughout. The veins are sometimes brecciated.

ANGLE TO CA ALTERATION

Minor epidote alteration.

MINERALIZATION

Commonly IX Cp * Po within matrix of Sudbury Breccia.

Trace to 1X Cp * Po as fracture fillings and within 1mm thick quartz veins.

Trace Cp * Po dissemination.

Occasionally Z-3% Cp+Po+Py within veins.

REMARKS

Good core recovery.



FROMTO

.

ROCKTYPE TEXTURE AND STRUCTURE

1029.0 - 1045.0Gabbro is sheared and fractured.

1045.0-1048.0White quartz vein, generally fractured (healed).uniform minor patches of chlorite and albite (?),commonly some white mica in indistinctsegregations and along fracture plane. Uppercontact at ~ 40" to c. a. Lower contactirregular. Gabbro in hanging wall to quartz veinis altered more strongly than further uphole.

1048.0 - 1049.0Fine to medium grained, foliated, with chlorite.epidote and quartz ribbons at 25* to c. a. Minor Ocm quartz vein with epidote * plagioclaseselvage.

1049.0-1050.48Coarse foliated gabbro with semi-planar clots ofmafic-rich material set in irregular groundmassof plagioclase * quartz. Last 0.5m much coarser.dottier and more mafic. Mafic component isfoliated on fine mm scale also and blobs appearto have been rotated.

1050.48 - 1093.4Abrupt change across 1cm quartz vein to massive.uniform medium grained (average 2-3mm) gabbro, CI* 50, equigranular, minor quartz and/or epidoteveinlets at 45' - 65* to c. a. throughout (mostabundant in top 40cm). Some quartz-carbonateveins to 7cm thick around 1085m.

1119.0-1124.6Several 0.5-1. Ocm quartz-carbonate veinlet at 15*- altered.

1131.0-1140.65Gabbro getting finer-grained. Chill zone -dmfeldspar is epidote altered.

ANGLETO CA ALTERATION

Pale green-grey alteration product maybe epidote with some ser - not as hardas epidote alone.

Feldspars appear to be epidotealtered.

MINERALIZATION

1084.53-1084.63 Several cubes ofpyrite 2-5mn along a 1.5cm thickquartz-calcite-chlorite vein, and inadjacent gabbro.

Trace Py as tiny specks locally.

Minor Po grains.

REMARKS

Felsic component formed by segregationof quartz and plagioclase at and aftertime of foliation formation.

Few breaks in core, solid ground.

Test at 3591' (1094.54m). Check forMag or Po at 137*/ -72.7*



FROMTO

1140.65TO

1448.69

1175.85TO

1448.69

ROCKTYPE

^ANDwSANDSTONE

^LST*SILTSTONE

*tf)WKEwPEBBLYWACKE/SILTSTONE/


GOWGANDA - SERPENT FORMATION1140.65 TO 1448.69

1140.65-1141.7Strong epidote alteration, possibly quartzalteration too. Fine to medium sandstone(possibly feldspathic arenite).

1141.7-1149.85Fine grained dark greywacke with 1-2X -eO.Snmleucoxene throughout. Rock is massive anduniform with local Py blebs to 5mm. Around1149m, * 50cm section of grey, mediumgrained sandstone: Very diffuse grain boundaries- quartz-rich - gradational to lower unit.

1150.68-1175.85Generally fine grained, dark green to greyquartz-carbonate hairline fractures throughout.very fine to locally fine, ragged leucoxene.

1156.64-1157.01Alteration Zone.

1159.99-1160.40As 1156.64-1157.01 interval; epidote less intenseand decreasing with depth. 1cm white.recrystallized quartz veinlet/band at 10' to c. a.contains fine, sub to anhedral Py grains 0.5mmwide. Appears to be altered sandstone bed as1140.65 to 1150.68.

1164.03-1164.18Weak epidote alteration bands to 1.5cm widealternate with 3 -5mm unaltered bands at 25* toc. a.

1173.41-1173.50Dark grey, pebbly wacke interbed; vague beddingat 45" to c. a. Very weakly calcareous.

1175.85-1448.69Alternating beds with occasional granitoiddropstones to 4.5cm; fine leucoxene throughout;bedding locally contorted/micro faulted.


Quartz-epidote alteration - pervasiveQuartz veinlets: colourless.

Local patches of pervasive epidote (*quartz) alteration towards end ofinterval. Quartz-calcite seams at50'- 70' to c. a.

Green-yellow epidote * weaksilification

Epidote, spotty altered blebs to 0.6cm

MINERALIZATION

1X Py - tiny specks.

Trace very fine grained Pydisseminated; 1 3, locally, mediumto fine grained.

Trace 15C fine to medium grained Py.

Trace - IX fine grained Py.

REMARKS



FROM TO



WACKE1175.90-1176.22Alteration zone, wacke/siltstone

1178.996cm wacke pebble with 2-3/J whispy to blebby Py

1185.88-1191.37Pebbly wacke horizon; upper contact at 30* toc.a.; occasional sub to euhedral Py to 4mm.

1191.37-1194.30Siltstone bedded at 70' to c.a.

1194.30-1194.70Light green to grey arenite; upper contactindistinct. Lower contact at 75* to c.a.

1200.75-1209.24Slight increase in leucoxene (?) content, locally to 30X and medium grained; locally reflects bedding at 30" to c.a. with alternating leucoxene-rieh and poor bands to 3mm wide.

1223.10-1233.58Intercalated siltstone/wacke; siltstone uniformly fine grained; wacke fine to medium grained and feldspathic with 1 to 3/S leucoxene; upper contact siliceous; siltstone beds fractured and infilled by wacke to 1224.30. Wacke finer grained downhole. Siltstone to wacke * TO/S/30%. Medium grained leucoxene defining bedding at 50*- 60* to

1240.04-1240.54Pebbly wacke band with feldspathic clasts to 2mm.

1261.58-1261.84Siltstone weakly brecciated and infilled withchlorite?

1261.84-1278.0Siltstone, wacke and pebbly wacke laminae at 45*-60* to c.a.

1278.0-1278.10

Moderately green to yellow epidote Trace - 1/5 fine to medium grained Py; rare Cp in pebbles.

Bedding at 15*- 25* to c.a.

Weak chloritization; epidote

Weakly siliceous at upper contact; weak chlorite throughout siltstone portions

Trace very fine grained Py.

Weakly to moderately chloritic.

Siltstone/wacke = 75V25X

HOLE RUMBER: M-SH-002 DRILL HOLE RECORD LOGGED BY: R. MEECHAM, D. TRUSCOTT PAGE: 8

HOLE NUMBER: M-SH-002; DRILL HOLE RECORD DATE: 07/17/1992

FROM TO

ROCK TYPE TEXTURE AMD STRUCTURE


Cream/, white medium to coarse grained granodiorite/tonalite cobble.

1297.52-3mm wide carbonate veinlet at 50* to c.a.

1281.35-1286.70Siltstone with scattered pebbles throughout.

1284.99-1285.22Creamy white, medium to coarse grained tonalitecobble.

1293.20-1293.38Microfaulting and folding of narrow (to 2cm)bedding - subparallel siliceous bands;

1294.02-1294.06 Siliceous band at 60* to c.a.

1297.95-1298.62Slight increase in fine leucoxene needles.

1298.98Possible slumped structures in siltstone; numerous hairline carbonate-filled fractures in 10cm halo above structures; uphole bed brecciated over Son. Weakly calcareous.

1300.87-1301.95Weakly fractured and calcite-flooded siltstone;narrow veinlets to 1mm form lattice.

1307.76-1307.86Coarser grained siltstone in contact with finegrained siltstone. Moderately calcareous.

1308.06-1317.1Alternating leucoxene-poor and narrow leucoxene- rich siltstone bands/beds; leucoxene-rich beds 1mm to 2cm and generally coarser grained, locally fine grained wacke, rare pebbles.

1309.81-1309.84 Quartz-carbonate band at 55* to c.a.

2 cm Py bleb in fracture plane.

1292.97-1294.42 may be slightly more chloritic

2-3X medium to fine grained subhedral Py

Several pyritic clasts to 4nm.

Rare fine to medium grained. Py dusts with carbonate rims in wacke bands.

Bedding at 55*- 60* to c.a.; siltstone/wacke and coarse siltstone 60X/40X.

Local moderate bleaching (epidote?)

No leucoxene.



FROM TO



1309.89-1310.42Medium grained siltstone bed irregular upper contact, lower contact at 48" to c.a.; few narrow carbonate stringers.

1311.19-1311.22As above; contacts at 55'- 60' to c.a.

1311.49-1311.57As above; irregular contacts

1312.15-1312.22As above; contacts at 45"- 50* to c.a.

1312.99-1313.05As above; irregular contacts; bedding at 60' toc.a.

1315.05-1315.06Quartz-carbonate band at 70* to c.a.

1317.73-1317.78Medium grained siltstone pebble; subrounded.

1317.82-1317.86Coarse grained wacke bed at 45* to c.a.

1317.86-1369.01Generally uniform massive to well-beddedfine grained si Itstone/mudstone. Locally up to 5XgranitoidC?) granules and rare pebbles; rareargillaceous pebbles. Leucoxene relatively rare.Local intervals to 10cm slightly worecoarse grained, local wacke beds to 5cm.

1326.27-1326.64Medium grained granodiorite/tonalite boulder.

1346.62-1349.051-2mm carbonate fracture parallel to c.a.2cm angular Breccia at lower contact, moderatelychloritic and carbonate infilled.

1354.42-1358.34Fine grained - very fine grained leucoxene specsto 1-235. Siltstone appears slightly finer-grained

As above, pervasive

As above, pervasive

As above, pervasive

As above, pervasive Trace fine grained Py and chlorite in cross-cutting hairline fracture.

Trace specks Py.

Locally weakly graphitic along narrow, carbonate-filled fractures.

Trace specks Py.

Trace speck Py. Rare granule-sized carbonate-rimmed subangular to angular clasts Py.

Local slickensides carbonatized and weakly graphitic.

Very weakly chloritic.

HOLETIUMBER: M-SH-002 DRILL HOLE RECORD LOGGED BY: R. MEECHAM, D. TRUSCOTT PAGE: 10


FROM TO



than elsewhere.

1367.47-1369.01Irregular slumping and development of chloriticslicken sides to lower contact.

1369.01-1380.18Fine grained wacke, locally pebbly, irregularupper contact. Indistinct bedding. Numeroushairline to 1mm carbonate veinlets, variablyoriented.

1369.21-1369.30 Quartz-carbonate-chlorite void-filling.

1370.11-1370.16Banded greenish-grey opalescent cherty clast;subangular.

1371.63-1371.74Quartz-carbonate band/vein at 60' to c.a.

1371.85-1371.89 As above.

1373.540.4cm quartz-carbonate band at 60* to c.a.

1375.30-1375.33Brecciated mudstone band hosting quartz- carbonate void-filling at 60* to c.a.

1376.57-1376.59Fractured siliceous band at 50* to c.a.; quartz- carbonate filling.

1379.37-1379.40Quartz vein at 70* to c.a.; 5/4 carbonate.

1380.19Lower contact at 50* to c.a.

1380.19-1422.68Green-grey siltstone as 1317.86 to 1369.01interval; occasional quartz granules.

Locally weakly silicified.1-2X fine grained, Py at upper contact in carbonated slip plane.

Weak chloritization at upper contact and lower contact.

2-3X fine to medium grained Py.

Occasional carbonate-rimmed, fine grained, angular Py clasts to 1.5 x 1.2cm

HOLE (JUMBER: M-SH-002 DRILL HOLE RECORD LOGGED BY: R. MEECHAM, D. TRUSCOTT PAGE: 11

HOLE NUMBER: H-SH-002 DRILL HOLE RECORD DATE: 07/17/1992

FROM TO



1380.19-1381.211-2X medium grained leucoxene laths.

1380.71-1380.79Two 0.4cm wide quartz-chlorite-carbonate veins at20* to c.a.

1384.97-1392.03Slump-brecciated and dark green to blackchlorite-infilled.

1396.345cm medium grained diorite pebble; rounded.

1396.74-1397.07Slump-brecciated as 1384.97 to 1392.03

1399.48-1399.88 As above.

1403.87Small quartz pebble with narrow, fine grainedPy Po rim.

1406.17-1406.45Medium grained impure wacke and quartz wacke pebble paraconglomerate horizon hosted by identical siltstone matrix. Irregular bedding and micro-faulting.

1409.86-1409.88Siltstone bed, micro-faulted, at 45* to c.a.

1409.97-1411.95Pebbly siltstone/wacke horizon, upper contact at 65* to c.a., lower contact at 15* to c.a. 3-5/J pebbles and coarse granules of quartz.

1416.58-1416.60Narrow fine wacke bed at 30* to c.a.

1421.35-1422.68Alternating siltstone/pebbly wacke beds to 3cmthick. Bedded at 60* to c.a.

1422.68-1448.69

2-3/C fine grained blebby Py.

Bedding contacts marked by 2-4mm quartz-carbonate bands.

Locally fine grained Py associated with hairline quartz-carbonate infilled fractures.

Bedding at 35*- 40* to c.a. Moderately calcareous.

HOLE SUMBER: M-SH-002 DRILL HOLE RECORD LOGGED BY: R. MEECHAM, D. TRUSCOTT PAGE: 12


FROM TO



Fine-grained, granular to locally pebbly feldspathic wacke. Beds 10-50cm thick and bounded by 1-3nm quartz-carbonate bands.

1436.37Flame structures at upper bedding contact.

1438.09-1438.30Wacke bed finer grained downhole. Load castlower contact. Upper contact at 50" to c.a.

at

1441.78-1442.07Narrow lenticular siltstone beds in wacke at 45'to c.a.

1443.15-1448.69Narrow 1-4cm wide fine to medium-grained arkose/subarkose beds in wacke. Strongly calcareous. Generally bedded at 45* to c.a. Pale pink to light greenish-grey.

Flame structure at 1446.36: tops uphole. Moderately calcareous.

1448.69TO

1494.40wLSwLIMESTONE/ CALCAREOUS WACKE AND SILTSTONE

ESPANOLA FORMATION 1448.69 TO 1558.33

1448.69-1494.40Rhythmically alternating beds of grey, buff or white limestone with dark grey siltstone and greenish-grey calcareous wacke ranging in thickness from a few mm to 100cm. Siltstone laminae are often slumped and contorted.

1448.70-1494.40Laminae defined by 1mm wide black chlorite) bands with 0.2 to 2.0cm intervals (Siltstone). Distinct, microfaulted upper contact at 30* to c.a.

Trace fine grain Py disseminated throughout.

1456.34-1456.38Coarse siltstone bed at 40"calcareous.

to c.a. Moderately

1457.18-1457.28As above, few quartz-rich granules; moderatelycalcareous.

Similar to narrow beds in 1443.15 to 1448.69 interval.

Bedding at 35* to 45" to c.a.

Coarse siltstone component increasing down hole from 1471.95m

Fine Wacke?

Fine Wacke?

HOLE WUMBER: M-SH-002 DRILL HOLE RECORD LOGGED BY: R. MEECHAM, D. TRUSCOTT PAGE: 13


FROM TO



1471.11-1471.19As 1456.35-1456.38; 40* to c.a.

1471.30-1471.35 As above.

1471-47-1471.53 As above.

1471.86-1471.90 As above.

1471.95-1476.19As above. Occasional narrow wacke beds at 40050* to c.a.

1476.19-1479.50Contorted wacke beds with narrow siltstonelaminae up to 1cm wide.

1478.47-1479.14 Coarse siltstone.

1479.50-1494.40Alternating wacke/subarkose beds with wackegenerally predominating.

1487.27-1487.29.Glassy quartz vein/quartz band at 50* to c.a.

Rare 1-2mm Py clasts.

Rare specks cpy in wacke to 2mm. Wacke weakly to locally moderately magnetic.

1494.40TO

1558.33

otUKE/SLSTwWACKE/SILTSTONE

1494.40-1520.14Fine massive wacke/coarse siltstone as in1479.50-1494.40. Rare, narrow, subarkose beds.Occasional silt to claystone beds of narrowwidth.

1506.64-1506.91Fining uphole sequence with claystone grading to siltstone to wacke to wacke with poorly sorted quarts clasts to 0.5cm. Contacts at 45* to c.a.

1510.74-1510.89Lenticular claystone beds to 3ntn wide with balland pillow structured quartz-carbonate.

Trace very fine to fine grained Py Cp disseminated throughout.

Bedding at 40* - 55* to c.a.

Wacke locally weakly magnetic.


HOLE NUMBER: M-SH-002: DRILL HOLE RECORD DATE: 07/17/1992

FROM TO



1515.70-1515.97Fine wacke/coarse siltstone hosting granule to small pebble-sized, cream-coloured feldspathic arenite (?) clasts (angular). Clasts aligned at 35* to c.a.

1516.82-1518.40Fining uphole sequence of claystone to coarsegrained wacke. Well sorted with increasingly coarse grained subangular quartz-carbonate granules; increasing carbonate content downhole. 5itm quartz- carbonate vein at 25* to c.a. Upper contact at 40* to c.a., lower contact at 45* to c.a.

1518.70-1518.92Arenite with irregular upper and lower contactsat 55' to c.a.

1520.14-1558.33Fine grained light greenish-grey carbonate-rich arenite as in 1448.69 to 1494.40 interval. Fine siltstone beds to 2.5cm throughout. Bedding generally at 45* to 55* to c.a. Rare, concordant, clear quartz bands to 3mm. Unit locally massive beds to 0.5m. Chloritic matrix, local microfaulting.

1520.29-1521.44Siltstone horizon hosting 1-3X angular quartz- carbonate granules. Bedding at 45* to 50* to c.a. Quartz-carbonate veinlet at 20* to c.a. at 1521.01. Siltstone, carbonate-rich.

1523.88-1524.41 Siltstone as above.

1527.72-1528.29Massive siltstone as above with 10cm raft ofsiltstone-laminated arkose (limestone).

1530.30-1530.96Massive siltstone as above.

1530.96-1531.09 Massive limestone.

Fine to medium grained Py clasts.

Trace fine grained Py disseminated throughout.

Upper contact at 35* to c.a.



1-3X very fine grained Py and trace



FROM TO



1540.37-1540.89Intercalated, lenticular-bedded siltstone andarenite.


1551.78-1553.52Siltstone laminated limestone. Contorted bedding.

1553.52-1553.56 Massive siltstone.


1554.70-1554.85 3-15mm quartz vein.

1554.85-1558.33As 1551.78 to 1553.52 interval.contact at 60* to c.a.

Abrupt lower

fine grained arsenopyrite(?)

Trace very fine grained disseminated Py.

Trace very fine grained Py dissemination throughout.

Trace very fine grained Py dissemination throughout.

Trace very fine grained disseminated Py.

4nm bleb fine grained Po.

Trace IX blebby Py, 1-2* fine grained Po.

1558.33TO

1584.03

CONGLOMER ATE/ PEBBLY WACKE

BRUCE FORMATION 1558.33 TO 1762.86

1558.33-1584.03Polymictic, poorly to moderately sorted pebble para- to orthoconglomerate with beds grading into coarse lithic wacke. Distinct upper contact at 50* to c.a. Medium to fine grained wacke to coarse siltstone matrix.

Clasts are comprised of:medium to coarse grained diorite/granodiorite -

405Sfine grained argillaceous sediments and mafic

volcanics - 40X medium grained arenaceous sediments - 20Z

Clasts range from angular to rounded.

Trace - IX Po, trace - 1X Py as clasts throughout.

No carbonate.



FROM TO



1563.77-1565.43Fine, laminated siltstone (1-3mn), bedded at 60'to c.a.

1568.50-1576.60Alternating graded beds of coarse grained areniteand fine lithic wacke.

1579.16-1580.06Medium grained lithic wacke. Upper contact at45* to c.a., irregular lower contact.

1580.18-1580.43As above, irregular upper contact and lowercontact.

Trace very fine grained Py disseminated throughout. Trace very fine grained Po in rare hairline carbonate-filled fractures.

Trace - 15J fine grained Py disseminated throughout. Bedding at 23* to c.a., hosting hairline veinlets of Po.

T-3% fine to medium grained clastic rounded to subrounded Py.

As above.

1584.03TO

1718.25

*CONG* CONGLOME RATE

1584.03-1716.20Medium grained pebbly wacke. Pebbles generallyarenaceous (arkosic).

1584.60-1584.63Glassy quartz vein/quartz band at 60* to c.a.

1586.88-1587.00Fine grained arkosic bed. Possibly silicifiedwacke. Irregular upper and lower contacts.

1587.51-1587.54Quartz vein as 1584.60 to 1584.63 3 50* to c.a.

1588.13-1588.56Fine orthoconglomerate. Upper contact a 35* toc.a.; lower contact 3 30* to c.a.

1590.01-1591.08Medium grained arkosic bed as 1586.88 to 1587.00interval.

1592.25-1592.28Quartz vein as 1587.51 to 1587.54 interval at 60*

Trace - 1X fine to medium grained Py disseminated throughout. 1-2X very fine to fine grained Po disseminated throughout. Trace galena in association with clastic Po.

Sulphide clasts contain quartz (possible vein material)

1-2X blebby Po a core of vein.

1-2X fine to medium grained Po * Py disseminated throughout.

Upper contact at 35* to c.a.; irregular lower contact.

Trace - IX blebby Po



FROM TO



1606.41-1606.60Fine grained, chloritic, quartz veined mafic volcanic C?) boulder. IS-20% fine grained opaque mineral throughout.

1607.33-1611.70Fine grained beds at upper contact with increasing grain size of matrix and pebbles downhole. Upper contact 3 60* to c.a. Lower contact marked by narrow (4mm) carbonate band at irregular but high angle to c.a.

1634.20-1634.32Narrow bed of orthoconglomerate in fine grain silty matrix. 1.5cm sulphide clast (Py Cp) with fine grained Py mineralization in cherty pebbles.

1634.50-1634.60 As above.

1670.86-1670.89Fine grained green-grey siltstone bed 9 45* toc.a.

1670.32-1670.94Fine grained siltstone as above. Upper contact 3 40- to c.a. Bedded a 40'-50' to c.a. 1-2X fine to medium grained leucoxene throughout. Lower contact intercalated with wacke.

1672.17-1672.23 As above.

1675.68-1677.67Lenticular - bedded fine grained intercalated siltstone/fine grained wacke. Rare carbonate stringers host Po * trace Cp to 45* Po disseminated throughout interval.

1677.67-1679.62Fine to medium grained arkose; calcareous. Bedding a 35* to 70' to c.a. Upper contact a 60' to c.a. Irregular lower contact, strongly chloritic over lower - most 12 em's.

1602.00-1607.33Increasing proportion Z grain size ofmatrix (fine to medium grained)

T-2% very fine to fine grained detrital Po *Py

Fine grained, massive Po locally rims cherty pebbles.

Trace Po in narrow bands in bedding plane.

1-2X fine grained Po disseminated throughout.

Trace - 13S Po disseminated throughout.

Trace - 151 fine grained Po Py.

HOLE RUMBER: M-SH-002 DRILL HOLE RECORD LOGGED BY: R. MEECHAM, D. TRUSCOTT PAGE: 18


FROMTO

1718.25TO

1729.80

1729.80TO

1762.86

ROCKTYPE

*ARTEwARENITE

*PWKEwPEBBLYWACKE


1679.62-1716.20Pebbly wacke and paraconglomerate dominate butlocally grade into coarse grained arkose overnarrow intervals.

1689.89-1689.9Quartz vein/band at 75* to c. a. Glassy.

1703.69-1707.76Quartz vein hosting 3-5X Po * trace Cp. Severalpebble to granule-sized clasts in thevein increase in amount downhole.

1710.20-1710.21Quartz-carbonate vein a 305; to c. a.

1716.19-1718.25Fine grained variably bedded siltstone.

1716.71-1718.25Chloritic siltstone- 1-3X fine grained leucoxene.

1718.25-1729.80Fine grained, light green-grey arenite. Locallygrading into impure massive wacke. Bedded at 70*to 60* to c. a.

1720.85-1721.18Fine grained massive wacke. Locally weaklychloritic.

1729.28-1729.80Chloritic siltstone as 1716.71 to 1718.2interval. IX fine to medium grained leucoxene.Upper contact at 60* to c. a., lower contact atSO* to c. a.

1729.80-1762.86Pebbly wacke as 1584.03 to 1718.25 interval.Rare quartz-carbonate veins. Rapidly gradinginto medium grained quartz-granular wacke withintercalated coarse grained siltstone beds to 8cm


Strongly chloritic.

MINERALIZATION

IX blebby Po

Trace blebby Po.

Trace fine grained Po.

Carbonate stringer - trace Po.

Trace very fine to fine grained Pydisseminated throughout.

1-2X fine grained Py.

Trace - 1X fine Py disseminatedthroughout, local coarse grainedblebs.

Trace IX fine grained Py disseminatedthroughout, locally blebby. Trace Poin veinlets and in quartz-carbonateclasts (vein material?)

REMARKS

Occasional subangular, Po-mineralizedquartz vein clasts throughout.

Similar to mineralized quartz veinclasts

HOLE HUMBER: M-SH-002 DRILL HOLE RECORD LOGGED BY: R. MEECHAM, D. TRUSCOTT PAGE: 19


FROM TO

1762.86 TO

1783.93

ROCK TYPE

*ARG I w MUDSTONE/ ARGILLITE


wide. Siltstone intervals locally appear cherty.

1752.55-1752.85 Medium grained calcareous arkose. T-2% medium grained opaques. Upper contact 3 25* to c. a.; lower contact 3 35* to c. a.

1756.18-1556.98 As above, gradational contacts.

1759.25-1759.88 Coarse grained arenite pebbles.

1759.88-1760.39 Coarse-grained quartz arenite. Weakly calcareous. Reverse grading. Irregular upper contact; gradational lower contact.

1760.42-1760.73 Granular quartzo-feldspathic arkose. Similar to above, but with feldspathic clasts. ID-15% dolomitic (?) granules. Lower contact at 50* to c. a.

1761.64-1761.68 Clear quartz vein at 55* to c. a.

1761.94-1762.15 Fine grained locally argillaceous arenite. Occasional argillaceous bands.

1762.15-1762.86 Coarse grained granular to pebbly arenite as 1759.88 to 1760.39 interval. 5-10X rounded to sub-angular mudstone granules and pebbles. Moderately calcareous. Narrow, discontinuous pyrite bands at lower contact a 60* to c. a. Gradational lower contact.

TRANSITION TO MISSISSAGI FORMATION 1762.86 TO 1783.93

Fine to medium grained dark grey to light green/khaki mudstone/argillite. Locally fractured and quartz-carbonate infilled with trace 2X Po in

ANGLE TO CA ALTERATION MINERALIZATION

Trace very fine grained Py disseminated throughout.

2-3JS very fine grained Py in matrix.

As Above.

IX blebbly Py.

Trace fine grained Po in argillaceous bands.

Trace -15J very fine grained Py in matrix.

REMARKS

Possibly calcareous analogue to surrounding wacke.

Granules are fine grained, sil i ecus mudstone; olive green; grey-brown weathering.

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FROM TO



veinlets. Generally massive beds. Becoming less argillaceous, but increasingly chloritic downhole.

1770.34-1770.44Weakly to moderately calcareous.

1778.47-1778.50 Microfaulted siliceous band. 3-5X blebby Po.

1783.54-1783.93 Weakly brecciated, talcose?).

intensely chloritic (weakly

1783.93TO

1828.26*SANDw SANDSTONE

MISSISSAGI FORMATION 1783.93 TO 1828.26

1783.93-1867.93Fine to locally medium grained wacke; massive to poorly laminated. Locally granular to pebbly. Occasional arkose and narrow arenite and argillite beds. Indistinct upper contact. Bedding at 45* to 55* to c.a. Angular to subrounded arenite granules to pebbles hosting blebby Po and rare Cp mineralization are scattered throughout. Units generally intercalated or possessing gradational contacts. Hairline carbonate fractures, variably oriented, found throughout. Argillite begins to predominate downhole.

1785.91-1786.35Fine grained greenish-grey arenite. Bedding at 50* to c.a. Upper contact at 60* to c.a., irregular lower contact, gradational.

1786.81-1787.16Argillaceous wacke interval as 1762.86 to 1783.93 interval. Upper contact at 55* to c.a.; lower contact at 45* to c.a.

1787.16-1787.47Medium grained arenite bed.

1804.54-1805.60

Trace ZX, fine grained Py disseminated throughout. Occasional POT i eh quartz clasts (vein material) in granular/pebbly beds (Trace Cp).

Trace - IX fine grained Py, (trace Cp?) disseminated throughout.

1-2X whispy Py disseminated throughout. Trace very fine grained disseminated Py.

HOLE WUMBER: M-SH-002 DRILL HOLE RECORD LOGGED BY: R. MEECHAM, D. TRUSCOTT PAGE: 21


FROMTO

1828.26TO

1856.41

1836.41TO

1900.44

"

ROCKTYPE

vCONG"CONGLOME RATE/WACKE

*WKE*WACKE


As above.

1805.60-1814.28Intercalated arenite, wacke and arkose.

1814.28-1816.54Coarse grained arenite, grading downhole intoarkose.

1816.54-1818.18Arkose grading into arenite.

1818.18-1819.56Arenite, coarsening downhole.

1819.56-1819.85Dark green to black chloritic contact with coarsegrained arenite-filled mud cracks at 35* to 40*to c. a.

1819.85-1828.26Intercalated coarse grained siltstone andsiliceous argillite. Argillite locally verysiliceous, possibly fine grained arenite, darkgreen-grey. Narrow medium to coarse grainedwacke bands intercalated throughout. Detrital Pomineralization shows marked preference for wackeintervals. Grading downhole into granular wackewith occasional blue quartz eyes.

RAMSEY LAKE FORMATION1828.26 TO 1836.41

Fine to medium grained lithic and conglomeraticwacke (locally coarse grained). Generallysiliceous matrix resembling argillite in1819.85-1828.26 interval. Upper contact at 70* toc. a., gradational lower contact at 55" to c. a.

McKIM FORMATION1836.41 TO 1900.44

1836.41-1867.66Fine to medium grained siliceous argillite with

ANGLETO CA ALTERATION MINERALIZATION

Trace blebby Po, trace - 1X very finegrained Py disseminated throughout.

2-3X blebby Po.

Trace - IX fine grained Pydisseminated throughout.

Coarse grained Po and Cp spots andstringers in siliceous interval(1824.42 to 1824.70)

Trace - locally 2X fine to mediumgrained detrital Po disseminatedthroughout. Trace Py.

Trace to IX very fine grained Py,

REMARKS

Argillite massive to vaguely bedded.

Numerous up to 1cm angular quartzclasts.

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FROM TO



ARGILLITE intercalated lithic wacke (rare leucoxene in wacke). Increasingly coarse grained downhole. Argillite locally becomes cherty where fine grained. Lower contact at 60* to c.a.

1867.66-1867.93Medium to coarse grained laminated arenite bedded at 65* to c.a. Narrow ( fl.Sctn) argillaceous bands parallel to bedding. Lower contact at 75* to c.a.

1867.93-1900.44Granular dark green-grey siliceous lithic wacke. Matrix resembles siliceous argillite above. Granules comprised predominantly of clear, milky and blue quartz and rare lithic fragments. Increasing mudstone granules and angular pebbles with argillaceous bands and matrix material increasing from 1870.62 metres; Wacke locally grades, arkose with decrease in amount of lithic fragments.

1870.57-1870.62 Silty mudstone band.

locally in narrow bands.

Trace - 1X fine grained Po * Py in thin argillaceous bands.

Trace - 1X fine grained Py. Trace 1X fine to medium grained Po.

Weakly calcareous.

Occasional trace fine grained disseminated leuxocene.

1900.44TO

2200.00

SANDSTONE/ARKOSE/SILTSTONE

MATINENDA FORMATION 1900.44 TO 2200.00

Medium to coarse grained pinkish, grey to predominantly greenish mica-rich sandstone. Most are quartzites, greywacke and arkose with minor conglomerate and siltstone. Thickness of beds ranges from 10 to 100cm.

1900.44-1901.69Medium grained subarenite with fine grained siltymatrix, upper contact at 20* to c.a.;gradiational lower contact. Occasionallenticular very fine grained mudstone bands (mudchips?)

1907.46-1908.90Medium grained quartz-granular arenite locally grading into subarenite. Quartz granules to 5X, generally monocrystalline. Occasional argillaceous pebbles. Gradational upper and lower

Trace - IX fine grained Py. Trace - 13. fine to medium grained Po.

Trace Py.

Occasional trace fine grained disseminated leuxocene.

Box 398

HOLE DUMBER: M-SH-002 DRILL HOLE RECORD LOGGED BY: R. MEECHAM, D. TRUSCOTT PAGE: 23


FROM TO



contacts. Vague bedding at approximately 40" to 45- to c.a.

1913.20-1916.29As above, but more typical quartzite. Irregular upper contact at high angle to c.a. Fine grained 1cm-wide pyrrhotitic mudstone band at upper contact (trace Cp). Gradational lower contact.

1916.97-1917.24As 1907.46 - 1908.90 interval. Locally silty. Gradational upper contact over 4cm at 50* to c.a. Vague bedding at 50* to 55* to c.a. Gradational lower contact at 50* to c.a.

1921.93-1922.87Arenite as 1913.20 to 1916.29 interval; locally silty over 2-4mm widths. Weakly calcareous with carbonate spots throughout to 3am in size. Upper contact at 60* to c.a.; lower contact irregular at 50* to c.a.

1923.09-1923.38As above. Upper and lower contact at 60* to c.a.

1927.00-1931.70As 1907.46 to 1908.90 interval. Upper contact at 35* to c.a. Gradational lower contact into silty lithic wacke.

1931.70-2046.88Fine grained silty to mediun grained granular siliceous lithic wacke; grading to arkose. Local irregular mudstone bands to 1.5cm. Occasional arenite bands as 1921.93 to 1922.87 interval. Angular mud chips to 2.5cm throughout. Spotty, skeletal-appearing carbonate to 5mn locally, as 1921.93-1922.87. Feldspathic arenite beds throughout with gradational contacts with arkose.

1945.06-1946.66Feldspathic arenite. Gradational upper contact at 60* to c.a. 2X, 1-2nm mafic particles. Gradational lower contact.

Trace fine grained Py, local Po * Cp.

Trace - 1X very fine grained disseminated Py.

Trace fine grained Py disseminated throughout.

Trace - IX fine grained Py.

Trace fine grained Py; trace very fine grained Po disseminated throughout.

Trace fine grained Py. Trace -IX fine to medium grained blebby Po -i- Cp in wacke beds.

White, ragged carbonate spots appear to be arenite matrix.

Bedding at 60* to c.a.

Bedding at 45* to 55* to c.a.

Trace fine grained Py, occasionally euhedral disseminated throughout.

Carbonate spots.


HOLE NUMBE*: H-SH-002: DRILL HOLE RECORD DATE: 07/17/1992

FROM TO

t

ROCKTYPE TEXTURE AND STRUCTURE

1947.14-1947.42Paraconglomerate. Subangular to subroundedsiltstone, wacke, very fine grained arenitepebbles in wacke matrix.

1950.42-1951.22Intercalated laminae of wacke and feldpathic-arenite at 1cm intervals.

1952.32-1953.34Coarse grained arkose with spotty carbonate asabove. Upper contact and lower contactgradational to wacke.

1954.61-1956.39Feldspathic arenite/subarenite with 4-8mm wackebands at 1 to 1.5cm intervals!. Gradational upperand lower contacts to arkose and wacke over 10cmintervals.

1957.0-1058.47As above. Gradational upper contact at 55* toc. a. Gradational lower contact.

1959.53-1964.16As above, locally grading into wacke and arkoseover 10cm intervals. Gradational upper contactand lower contact from 1964.0. Bedding at 50* toc. a.

1964.16-1964.28Fine grained, medium green-grey siltstone. Veryweakly calcareous.

1964.39-1964.42As above. Contacts at 55* to c.a.

1964.54-1966.45As 1954.61 to 1956.39 interval. Arkose gradinginto feldspathic arenite by 1965.30 withaccompanying "spotty" carbonate. Gradationallower contact over 25cm.

1968.34-2077.12Similar pattern of interbedded feldspathic-arenite with gradational contacts to arkose and

ANGLE TO CA ALTERATION MINERALIZATION

1-2X fine to mediun grained roundedPy.

Trace, fine to coarse grained detritalmineralization disseminated

REMARKS

Spotty carbonate throughout withpossible slight preference for arenitebeds.

"Spotty" carbonate to 1958.75.

"Spotty" carbonate in more quartzoseportions of interval.

HOLE KUfJBER: M-SH-002 DRILL HOLE RECORD LOGGED BY: R. MEECHAM, D. TRUSCOTT PAGE: 25


FROM TO



wacke as above. Bedding thicknesses is usually less than 3.0m. Rare rounded to subrounded fine to medium grained siltstone pebbles resembling 1783.93 to 1867.93 interval.

1993.25-198.58Fine to medium grained quartzose silty wacke.Gradational upper and lower contacts to arkose.

2046.88-2052.09Feldspathic arenite/silty feldspathic arenite with narrow fine grained lithic wacke beds to 0.5cm to 2046.98. Bedding at 40* to c.a. Spotty carbonate in quartzose intervals. Becoming increasingly silicified from 2047.49 with trace - IX fine grained leucoxene in silicified wacke bands. Apparent gradations to feldspathic arkose, partly obscured by silicification. Core becomes increasingly fractured and vuggy with spaces locally being infilled by 1cm euhedral, locally prismatic white quartz crystals. Bedding at 45* to 55* to c.a. is accentuated by silicification. Arenite grades through arkose to lithic wacke, at 2049.30. Lithic wacke hosts 3-5X medium grained euhedral leucoxene? scapolite?, crystals. Silicification decreasing downhole from approximately 2051.38 and disappears by 2052.09.

2071.15-2077.12Silicified as above, though not vuggy. Alteration identifiable by silicification along planes of parting (bedding?) at nwderate to high angles to c.a. Carbonate spots in cleaner arenites and 2-3X medium grained white crystals in wacke intervals are present throughout.

2077.12-2200.00Medium to coarse grained arenite becoming predominant lithology; locally weakly to very weakly calcareous. Generally silty, locally with medium grained feldspar laths to lithic fragments up to 4-5X. Massive to moderately -well bedded at 40' to 50* to c.a.; narrow (up to 1.5cm) wacke bands/beds define bedding plane. Arenite locally grades into medium to coarse grained arkose and fine to medium grained wacke as above in beds

throughout.

Increasing silicification from 2047.49

Rounded to subangular white quartz pebbles and granules to 2X from 2000.22.

Possible dilatant zone.

Silicification much more noticable in wacke, along bedding/parting planes.

Essentially same lithology as 1931.70 to 2046.88 interval.

Trace to locally ZZ f ine to medium grained detrital Py * Po * Cp

Carbonate spotting noted throughout arenite sequences.

Matrix in wacke and arkose ^ silt with ^X fine grained biotite? crystals.

HOLE RUBBER: M-SH-OOZ DRILL HOLE RECORD LOGGED BY: R. MEECHAM, D. TRUSCOTT PAGE: 26

HOLE NUMBER: M-SH-002

HOLE NUMBER: M-SH-002

DRILL HOLE RECORD DATE: 07/17/1992

FROMTO

2200.00TO

2200.00

ROCKTYPE

*EOHwEND OF HOLE


ci. Om on average.

2200.00Foot of hole at 2200.00m.

ANGLETO CA ALTERATION MINERALIZATION REMARKS

DRILL HOLE RECORD LOGGED BY: R. MEECHAM, D. TRUSCOTT PAGE: 27

MAP SHOWING BLOCK

OF CLAIMS

WITH APPLIED VALUES OF

SUBMITTED ASSESSMENT WORK

BY FALCONBRIDGE LIMITED,

JULY 1992.

t*

Ao:o. o.

Ministry ofNorthern Developmentaid l-flnesOnt'

Report of Work Conducted After Recording Claim

Mining Act

Transaction Number

L) W?o.Personal information collected on this form Is obtained under the authority of the Mining Act. This Information will be used for correspondence. Questions about this collection should be directed to the Provincial Manager, Mining Lands, Ministry of Northern Development and Mines, Fourth Floor, 159 Cedar Street, Sudbury, Ontario, P3E 6A5, telephone (705) 670-7264.

Instructions: - Please type or print and submit in duplicate.- Refer to the Mining Act and Regulations for requirements of filing assessment work or consult the Mining Recorder.- A separate copy of this form must be completed for each Work Group.- Technical reports and maps must accompany this form In duplicate.- A sketch, showing the claims the work is assigned to, must accompany this form.

Recorded Holder(s)

Address 7-^7. Q A/TAQ/O .

Client No.

Telephone N

Mining Division Township/Area M or 0 Plan No.

Datesformed M 12.

^/? & S99/Work Performed (Check One Work Group Only)

Work Group

V

Geotechnical SurveyPhysical Work, Including Drilling

Rehabilitation

Other Authorized Work

Assays

Assignment from Reserve

Type

-p/rtMOA/P ~PRlt~UMG- ONTARIO GFOLOGICAL SURVEYGIS- ASSESSMENT FILES

AUG171992

—— RECEfVED ——

\

Total Assessment Work Claimed on the Attached Statement of Costs SNote: The Minister may reject for assessment work credit all or part of the assessment work submitted if the recorded holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.Persons and Survey Company Who Performed the Work (Give Name and Address of Author of Report)

Name Address

ffi. &OK 33 o

(attach a schedule If necessary)

Certification of Beneficial Interest * See Note No. 1 on reverse sideRecorded Holder or Agent (Signature)

(L,

l certify that at the time the work was performed, the claims covered in this work report were recorded In the current holder's name or held under a beneficial Interest by the current recorded holder.

Certification of Work Report! l certify that l have a persona! knowledge of the facts set forth in this Work report, having performed the work or witnessed same during and/or afteri its completion and annexed report is true. nsTinTe"and~Ao'dress o! Person Certifying

Certified

For Office Use OnlyTola!"Value Gr. Recoraed[Date Recorded

Date Notice for Amendments Sent

r-'-SLiryn-.M^YReceived Stamp , .

tr -

Ministry o)Northern Developmentand Mines

irvfinistere du Developpement du Nord et des mines

Statement of Costs for Assessment CreditIztat des coOts aux fins du credit devaluationMining Act/Lo) sur les mines

Transaction No./N 0 de transaction

Personal information collected on this form is obtained under the authority of the Mining Act. This information will be used to maintain a record and ongoing status of the mining clalm(s). Questions about this collection should be directed to the Provincial Manager, Minings Lands, Ministry of Northern Development and Mines, 4th Floor, 159 Cedar Street, Sudbury, Ontario P3E 6A5, telephone (705) 670-7264.

Les renseignements personnels contenus dans la presente formule sont recueiilis en vertu de la Lo) sur les mines et sen/iron! i tenir a jour un registre des concessions mlnieres. Adresser toute quesiton sur la collece de ces renseignements au chef provincial des terrains miniers, ministere du Developpement du Nord et des Mines, 159, rue Cedar, 4 e etage. Sudbury (Ontario) P3E 6A5, telephone (705) 670-7264.

1. Direct Costs/CoQts directs

Type

Wages Salalres

Contractor's and Consultant's Fees Drolls de ('entrepreneur et de ('expert- consell

Supplies Used Fournltures utlllsees

Equipment Rental Location de materiel

Description

Labour Main-d'oeuvreField Supervision Supervision sur le terrain

Type

T?#fcUAff

Type

^Mfrtc*.

Amount Montan)

JI6.S**

17^9/3f

I)A77

Total Direct Costs . Total des couts directs

Totals Total global

*IG.3S*

*Mf98

1277'tfy&i

2. Indirect Costs/CoQts Indirects* * Note: When claiming Rehabilitation work Indirect costs ere not

allowable as assessment work. VJ Pour le remboursement des travaux de rehabilitation, les couts Indirects ne sont pas admissibles en tant que travaux devaluation.

Type

Transportation Transport

Food and Lodging Nourrlture et hebergement

Mobilization and ~Damgt)lll*atlonMobillsatl6A'i!demobilisation

DescriptionType

CAMP

Amount Montant

Sub Total of Indirect Costs Total partlel des couts Indirects

Amount Allowable (not greater than 20H of Direct Costs) Montant admissible (n'excedant pas 20 H des coOts directs)Total Value of Assessment Credit (Total of Direct and Allowable Indirect costs)

Valeur totale du criditdevaluation(Totil del coOti dlrecti*l Indirect! idmlnlblet

Totals Total global

#4,5-09

3 tt J 32

Note: The recorded holder will be required to verify expenditures claimed in this statement of costs within 30 days of a request for verification. If verification is not made, the Minister may reject for assessment work all or part of the assessment work submitted.

Note : Le titulaire enregistre sera tenu de verifier les depenses demandees dans le present etat des coOts dans les 30 jours suivant une demande b cet effet. Si la verification n'est pas effecluee, le ministre peut rejeter tout ou une partie des travaux devaluation presents.

Filing Discounts

1. Work filed within two years of completion is claimed at 1000Xo of the above Total Value of Assessment Credit.

Remises pour d6pdti

1. Les trevaux deposes dans les deux ans suivant leur achievement sont rembours6s a 100 CA de la valeur totale susmentionnee du credit devaluation.

2. Work filed three, four or five years after completion is claimed at 500xb of the above Total Value of Assessment Credit. See calculations below:

Total Value of Assessment Credit Total Assessment Claimedx 0.50

2. Les travaux deposes trois, quatre ou cinq ans apres leur achievement sont rembourses a 50 Vo de la valeur totale du credit devaluation susmentionne Volr les calculs ci-dessous.

Valeur totale du credit devaluation Evaluation totale demandeex 0,50 -

Certification Verifying Statement of Costs Attestation de l'6tat des couts

l hereby cert!:',that the amounts shown are as accurate as possible and these costswere incurred v. rille conducting assessment work on the lands shownon the accompanying Report of Work form.

that as .-^'^'Y^^^-^.^^.^'__ l am authorized(Reccrcea Ho.'aer. Agent, Posiii&n in Company)

to make this certification

J'atteste par la presente :que les montants indiques sont le plus exact possible et que ces d6penses ont 6te engagees pour effectuer les travaux devaluation sur les terrains indiques dans la formule de rapport de travail ci-joint.

Et qu'a litre de.. je suis autonse(litulaire enregistr6, reprisentant, poste occupS dans la compagme)

a faire cette attestation.

;Signatur

Nota : Dans cetle formule, lorsqu'il ei^signe des personnes, le mascuhn esrJ'.His* BJ sens neutre

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ased

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pate

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riorit

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Mississagi Fm. McKim Fm.

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FALCONBRIDGE LIMITEDEXPLORATION

Mirage PropertySheppard Twp.

SECTION LOOKING NORTH

Traced by

Drawn by :JOHN ROSE JULY 16/92

Supervised by :D. TRUSCOTT

Revised by

Approved by : P.SNAJDR

Plan no.12:SECT8.5xli MIRSECT3.DffG

Scale :O 100

l : 5000 (metres) 200 300 400

4III6WWC865 10 SHEPPARD 200

: other ( j claim no. hole no. footage date note€¦ · m-sh-2 summary log o -4m 4 - 961 m 961 -...

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