geophys rpt on the garrison property located in garrison … · 32d12sw0047 2 16794 garrison 010...

32D12SW0047 2 16794 GARRISON 010

GEOPHYSICAL REPORT

ON THE

GARRISON PROPERTY

LOCATED IN

GARRISON TOWNSHIP - LARDER LAKE MINING DIVISION

FOR

MONETA PORCUPINE MINES INC.

2.16794

V

Submitted by: S.D. AndersonRayan Exploration Ltd Aug.,1996

RECEIVED

X OCT 9 - 1996

MINING LANDS BRANCH

32D12SW0047 2.16794 GARRISON Q-l QQ

TABLE OF CONTENTS

INTRODUCTION. . . . . ... . . . . . . . . . . . . . . . . .. . . . . ... .. . . . . . . . . lLOCATION AND ACCESS.................................... lPERSONNEL. . . . . . .. . . ... . . . . . . . .. . . . . . . . . . . . . . . . . . . . . . . . . lCLAIMS... . . . . . . . . . . . . . . . . . . . .. . . . . . . . . . . . . . . . . . . . . . . . . . 2GEOLOGY. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3GEOPHYSICAL WORK PROGRAM. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4SURVEY RESULTS......................................... 5,6RECOMMENDATIONS AND CONCLUSIONS. . . . . . . . . . . . . . . . . . . . . . . . 6CERTIFICATE. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7

LIST OF FIGURES

LOCATION MAP FIG. lREGIONAL LOCATION MAP FIG. 2CLAIM AND GRID SKETCH FIG. 3

APPENDIX

MAGNETOMETER SPECIFICATIONS....................APPENDIX A

LIST OF MAPS

CONTOURED and POSTED MAGNETOMETER. . . . . . . .. . .. . . . . . . l:5000

INTRODUCTTON

Rayan Exploration Limited of Timmins, Ontario was hired by Monet a Porcupine Mines Inc. to conduct a Total Field Magnetometer Survey on their Garrison Property. This property is located in the northeast portion of Garrison Township, Larder Lake Mining Division, District of Cochrane. This work was carried on a contract basis and was performed between June 18 and 21, 1996. A total of 43 kilometres of previously established grid lines were purveyed.

The purpose of this project was to provide a detailed ground magnetic map to aid in geological interpretation of the claim block.

This report deals with the logistics of the Magnetometer Survev and resuIts of same.

LOCATION AND ACCESS

T'-,o Property j? located in the northeast, portion of Garrison Townshio, Larder Lake Mining Division, District of Cochrane. It is situated arm t-r, x i in.-j t e l y 100km. east of the city of Timmins, an ci 40km. east of the town of Matheson. Hwy 101 East runs generally eas L west through the northern portion of the block. Thackery free': flows through the extreme southeast corner of the grid. ArcF-Rs to the pronerty was gained via HWY 101 east from the city of Timmins to the town of Matheson. From the town of Matheson Hwy 1 01 con!: i nue.c east to the Province of Quebec. At approximately the 40km point east from Matheson this Hwy passes through theri o r H-, rn no r t ion f the Local t.he grid is situated aboutkm. east of Garrison Creek.

PERSONNEL

The people directly involved in this program were all employed by Rayan Exploration Limited, and are as follows:

Lanny Anderson..........................TimminsDanny Brazeau. . . . . . . . . . . . . . . . . . . . . . . . . . .Ti mmins

A ll work was supervised by R.J. Meikle.

89 80 83 80 79

53

90-

U.S.A.

•99

•49

O 90 100190 nllet

80 89 80

PROV NCE OF ONTARIO

FIG l

MONETA PORCUPINE MINES

GARRISON PROPERTY

LOCATION MAP

"-//^f Gravrf. h *.a v^-..•^fr^n—Hij-L_~7i -^-

FIO 2

ient: MOWETA PORCUPINE MINESPrOMf-t.u: GARRISON PROPERTYTiLU:

REGIONAL LOCATION MAP

RAYANEXPLORATION LTD

CLAIMS

The Garrison Property covers or partially covers a total of 27 contiguous, unpatented. patented and leased mining claims (56 units), all located in Garrison Township, Larder Lake Mining Division. District of Cochrane. The claim numbers are listed in numeric order below.

Claim of units T vi

2580 3258042580525937250 3 P25939250402 5 9 4 12 5 9 4 236074 — ———— —————2607;-2607 62 6 3 3 426385263863057640273428064230"4280806106 ———————————p z. rj p *-f ri

1 193851120105 3120105 612067551 2067^6

11l111111tL

11111L

ll1

111L4

1

1 51 521

patentpatentpatentpatentpat entpatentpatentpatentpatent

——————— pateulpatentpatentpa ten tpa t en tp a t e n tpa ten tpa tentpatentpat entpat en t

——————— pa t v LI l, T

unpatentedunpat en tedunpat en tedunpat en tedunpat en t e d

^ Claims Un itpL-

1201053

1201056

- l

MONETA PORCUPINE MINESGARRISON PROPERTY

CLAIM SKETCH

RAYANEWLCRATICN LTD

GENERAL GEOLOGY

The property is shown on the Timmins-Kirk l and Lake Map No. 2205, to be situated within the Abitibi Greenstone Belt which covers much of northeastern Ontario and northwestern Quebec.

Generally this belt is underlain by a variety of mafic to felsic volcanics and related sediments as well as felsic to ultramafic intrusive.

Locally, The Geology of Garrison Township Map 1949-1 shows tlie north central portion of the grid to be underlain by generally east- west striking sediments with some iron formation. Several parallel east-west fault zones are shown to occur within this unit. These faults have been interpreted to be a portion of the Des t or Porcupine Fault-. To the north and south, this geological unit is paralleled by a variety of mafic to felsic volcanics. The ^xtreme northern portion of the grid is shown to be underlain by an ultramafic intrusive while the southern portion of the grid is shown to be primarily granite.

GEOPHYSICAL PROGRAM

A total of 43 kin. of grid lines were surveyed with a Total Field Proton Magne t ome ter. Only the cross lines were surveyed which ran in a north-south direction. This g'rid was established using a 100m line interval with 10m station intervals.

Tile following1 is a brief description of the Geophysical S LI r ve v Method used:

MAGNETOMETER SURVEY

An EDA Omni Plus Proton Precession magnetometer was used to carry out the magnetometer survey. The instrument, is synchronized with an EDA recording base station to help eliminate magnetic diurnal variation. This should ensure an accuracy of less than 10

The Proton Precession method involves energizing a wire coil immersed in a hydrocarbon fluid. Tli i s causes the protons in the proton rich fluid to spin or process simulating spinning magnetic d; po l pp , when the current is removed the protons precess aboi.it the direction of the earth's magnetic field, generating a signal i. n the same coil which is proportional to the total magnetic field intensity. In this way. the horizontal gradient of the earth"? magnetic field can be measured and plotted in plan form with values of equal intensity joined to form a contour map.

This -ire-sen t a t i on is useful in correlating* with other data sets to aid. in structural interpretation. Individual magnetic re;-".onse? pan be interpreted for dip. depth and width estimates a f t e r p ro f i l i ng t he da. t a .

The following parameters were employed for the survey:

Instrument - EDA Omni Plus Proton Precession Magnetometer St.at ion Interval - 10m Line Interval - 100mDiurnal Correction Method - EDA Recording Base Station Data Presentation - ^ag*netic Data Posting and Contour Map

- 1:5000 scale

SURVEY RESULTS

The Total Field Magnetometer survey conducted on the Harrison Property outlined various geological structures and units occurring within the block, as shown by the Geology of (Garrison Township Map 1949-1.

There are two main magnetic features that stand out, both having strong magnetic high signatures. The first of these strikes roughly from L50W/200N to L6BW/200S, remaining open in hot]"! directions. This is coincident with the sediments shown to extend through the block. The strongest magnetics occur between T 55W anr1 fi?,W, and may be responding to zones of iron formation known to occur within the sediments. This feature is flanked on both sides by a number of magnetic lows. Although these lows may be a shadow effect from the strong magnetic highs, they could ft ] sn he marl-; ing some of the fault zones shown to be associated with this geological unit.

The second area of interest outlined is a series of erratic ni.-i g:i e t i c highs running generally east-west across most, of the grid between 400S and 1000S and from L53W to Lfi9W, remaining open to ^he vest. This feature is more or less coincident with the volcanics shown to occur to the south of the sediments. The iimgne t j r response may be due to areas of mineralization or some type of geological structure or structures extending through t '-ii c n p ; t- . Wjthin this zone of erratic magne tics it may be possible to roughly out l ine a number of individual trends. At t h i s point in t i me two such trends may be out lined. Both are marked by magnetic highs with the first running from L54W/950S to LF,R\V /^50? . and the second Prom T.54W/400S to L60W/950S. Although these features are not very we l l defined they could be responding t-o '-:'eo l o e' i ea l structures within the volcanics. In order to help determine if these are legitimate trends, as well as to outline any other similar trends, this data should be compiled with any other geological or geophysical information available on the o r o "i e r t y .

To the south of this volcanic unit the magnetics remain more or l^ss at background, showing little change. This area to the south is shown to be underlain by granite. As a result, the southern limits of the previously discussed feature are likely marking the contact between these two rock units.

The two main magnetic features outlined are thought to be responding to two separate geological rock units, sediments and volcanics. For the most part these two geological units are separated by weak magnetic low that extends across much of the grid just south of the base line. This weak low may be marking either the contact between the sediments and the volcanics, or a portion Destor Porcupine Fault, or both.

The only other significant magnetic feature outlined is a high located within the extreme northern section of the grid. Tt extends from L p)2E to LR3E. at roughly 1000N. remaining open to the north east and west. This zone is likely marking the change in rook, type between mafic volcanics and ultramafios, as shown by Geology of Garrison Township. Map 1946-1.

RECOMMEND AT T ON,S-JAND- CONCLUSIONS

As mentioned under results, it would appear as though this o'eophys i C.R l wo r!-i program vas successful in outlining the main geological units and struct ares shown to occur wit li in the grid a rea .

At this point in time, the two main zones outlined are of•vi o c 1 - inter-'?*. The first zone discussed is thought to be responding to a band of sediments and related iron formation, as ve' ' s s a port Ion of the Destor Porcupine Paul t or related faults. The second feature discussed appeal's to be coincident

•,.. i i -- i-ne TO l can i c 5 *o the south. These magnetics are more erratic arid. ^ re thought to be the resul t of mineralization within the••o l i .-in i f-c ,--,\- geological structures extending through the area. Both these features would apnear to be indicating a geological• : nvi ropment ^avourable for gold, deposi t ion

Although the magnetic survey has helped in isolating the•na i r; ar^as of interest . this data should be compiled with any other information available on the property. This may help in f u r t h e r r e s o ' v i n g some of the z o ri e s described as well as p r o v i d e possible targets for follow-up work. If after this, any areas of interest remain unresolved, further testing should be done.

If it is felt that additional information is required, an Induced Polarization Survey should Lie considered. This would help detect any areas containing sulphide mineralization, and when correlated with the magnetics may outline areas of possible alteration or silicification.

As mentioned earlier, because of the favourable geological environment of the Destor Porcupine Fault, no areas of interest should be dismissed without further testing.

CERTIFICATION7

I, Steve Anderson of Timmins, Ontario hereby certify that:

1. I hold a three year Technologist Diploma from Sir Sandford Fleming College , Lindsay, Ontario, obtained in May1 O P "i i ,-j o ± *

2. I have been practising my profession since 1979 in Ontario. Quebec. Nova Scotia, New Brunswick, Newfoundland. NWT, Manitoba, and Saskatchewan.

3. I have been employed directly with Asamera Oi l Inc. T'ran^el lschaf t Canada Ltd.. Nanisivik Mines Ltd., R . S . Middleton Exploration Services Ltd...and Rayan Exploration Ltd.

4. I have based conclusions and recommendat ions contained in this report on knowledge of the area, my previous experience ?nr! on the results of the field work conducted on the property d u i- i n ? 1990.

Dated this 10th day of August, 1996

at Timmins. Ontario.

APPENDIX A

EDA OWNT PLUS MAGNETOMETER

Major Benefits of the OMNI PLUS* combined VLF/Magnetometer/Gradiometer

System

9 No Orientation Required

9 Three VLF Magnetic Parameters Recorded

* Automatic Calculation of Fraser Filter

9 Calculation of Ellipticity

9 Automatic Correction of Primary Field Variations

Measurement of VLF Electric Field

Specifications*Frequency Tuning Range.

Transmitting stations Measured.

Recorded VLF Magnetic Parameters

. 15 to 30 kHz, with bandwidth of 150 Hz; tuning range accommodates new Puerto Rico station at 28.5 kHz

. Up to 3 stations can be automatically measured at any given grid location within frequency tuning range

Standard Memory Capacity

Display

.. .Total field strength, total dip, vertical quadrature (or alternately, horizontal amplitude)

... 800 combined VLF magnetic and VLF electric measurements as well as gradiometer and magnetometer readings

... Custom designed, ruggedized liquid crystal display with built-in heater and an operating temperature range from -400Cto n-55 0 C. The display contains six numeric digits, decimal point, battery status monitor, signal strength status monitor and function descriptors.

RS232C Serial I/O interface ...... 2400 baud rate, 8 data bits, 2 stop bits, no parity

Test Mode .................... A. Diagnostic Testing (data and programmablememory)

B. Self Test (hardware)

Sensor Head ................. .contains 3 orthogonally mounted coils withautomatic tilt compensation

Operating Environmental Range ...................... -400cto +55 0C;

O - 10007o relative humidity; Weatherproof

Power supply ................. Non-magnetic rechargeable sealed lead-acid 18VDC battery cartridge or belt; 18V DC disposable battery belt; 12V DC external power source for base station operation only.

Weights and Dimensions instrument console .......... 2.8 kg, 128 x 150 x 250 mmSensor Head................. 2.1 kg, 130 dia. x 130 mmVLF Electronics Module........ 1.1 kg, 40 x 150 x 250 mmLead Acid Battery Cartridge ... 1.8 kg, 235 x 105 x 90 mm Lead Acid Battery Belt ........ 1.8 kg, 540 x 100 x 40 mmDisposable Battery Belt ....... 1.2 kg, 540 x 100 x 40 mm

preliminary

EDA instruments inc., 4 Thorncliffe Park Drive, Toronto, Ontario Canada M4H1H1Telex: 06 23222 EDA TOR, cables: instruments Toronto (416)425-7800

in USA,EDA instruments inc.,5151 ward Road,Wheat Ridge, ColoradoU.S.A. 80033(303)422-9112

Printed in Canada

2. l 67 932D12SW0047 2.16794 GARRISON 020

MONETA PORCUPINE MINES INC GARRISON PROPERTY

DDK MG96-01 AND CLAIM LOCATION

FE;? M,-,T j UN

ONETA PORCUPINE MINES INCGARRISON PROPERTY

DDH MG96-01 PLAN/SECTION

Date: 9 Aug, 1996

Northing:Easting:Elevation:

Collar Azi.: Collar Dip:

140-5900

O

180-45.0

HONETA PORCUPINE MINES INC.

DRILL HOLE RECORD

*** Dip Tests *** Depth Azi. Dip

Drill Hole:

Page: 1 of 14

HG96-01

Hole Length: 264Property: LINTON OPTIONLogged by: K.A. JENSENComments:Date Completed: APRIL 4, 1996NTS:Date(s) Logged: APRIL 3-4, 10-12, 15, 1996Company: BENOIT DIAMOND DRILLING LTDCore storage: MONETA CORE FACILITY ON HWY 655, TIMMINS

50150264

180 -43.0180 -40.0180 -37.0

Northing:Easting:Survey:Core Size:Measure:Claim:Grid:Township:Purpose:Date Started:Assay Type:

1+40N59+OOwNONQMETRICL40273/26016LINTONGARRISONTESTING IP ANOMALYMARCH 30, 1996Au by FIRE ASSAY

From (m)

.00

23.00

23.90

26.70

30.30

GeologyTo (m)

23.00 CASING

23.90 CHLORITE SCHISTFine-grained, medium green to blackish green with bluish hue, non-magnetic Locally contorted, chloritic to locally talcose, occasional quartz to fracture-filling, trace to scattered up to 0.5X pyrite.

26.70 ARKOSE23.90 FAULT GOUGE at contact 50 degrees to core axis.Fine-grained, black to blackish green, hard, locally weakly to moderately magnetic, massive, poorly developed bedding, with inclusions of CHLORITE SCHIST altered reddish brown at 15 to 50 degrees to core axis, siliceous, minor contorted up to 1 mm quartz-carbonate fracture-filling stringer. Overall IX to 27. fine-grained pyrite locally up to 3/i to 5X with minor pyrrhotite.26.21 26.25 CHLORITE SCHIST with upper contact 70 degrees to core axis, lower contact 85 degrees to

core axis.

30.30 HEMATITIZED ARKOSIC WACKEFine-grained, reddish brown to purp red brown, massive, uniform, poorlypervasively hematitic, hard to very hard, siliceous,magnetic, CHLORITE SCHIST up to 27.30 m, very fineoccasional 1 to 2 mm pyrite cube, chloritic fracture-filled slip at 57 to 65 degrees to core axis.Overall V/. to 27, pyrite locally up to S'/, fine-grained pyrite.26.70 Upper contact at 55 degrees to core axis.26.70 28.30 Brecciated to fragmental.

28.30 30.30 Massive.28.33 Greyish quartz-carbonate stringer at 48 degrees to core axis with

pyrite.

32.05J LITHIC SUB-ARKOSIC WACKEFine-grained, quartz and feldspar labile fragments up to 1mm in aphanitic matrix, poorly developedFine-grained, quartz

, moderately hard.i quartz-carbonate

c, massive, poorly5 to 50 degrees tostringer.

itact 85 degrees to

developed bedding,;akly to moderatelyninated pyrite with:es to core axis.

to 27, fine-grained

*, poorly developed

Sample

3770137702

3770337704

37705

From(m)

27.0028.00

29.0030.00

31.00

To(m)

28.0029.00

30.0031.00

32.00

Lngt(m)

1.001.00

1.001.00

1.00

AUPPB

55

3627

27

AGPPM

.1

.1

.1

.1

.1

ASPPM

1.03.0

2.73.5

1.6

MG96-01 (continued) Page: 2 of 14

From (m)

32.05

34.54

36.50

37.39

38.22

40.75

43.00

T. l(m)

34.54

36.50

37.39

38.22

40.75

43.00

50.22

Geology

bedding, greyish to greyish green, minor contorted fracture-filled greyish white quartz-carbonatestringer with hematitic alteration on contact, massive, hard, siliceous, non magnetic.Overall up to Q.5'/, fine-grained pyrite locally up to S'/..31.27 31.60 Extremely fractured with 3X to 5X fine to medium-grained pyrite, gradual change in

colour, weakly to moderately magnetic.

HEMATITIZED ARKOSIC WACKEGreyish red to reddish brown changing to reddish grey, hard, siliceous, pervasively hematitic.massive poorly developed bedding, moderately to strongly magnetic, GROUND CORE at contact, minorquartz-carbonate fracture-filling at 50 to 75 degrees to core axis.Scattered D.5% to V/. fine to medium-grained pyrite.34.45 Quartz-carbonate stringer 4 mm with minor chlorite and hematite, 55 degrees to core axis

LITHIC SUB-ARKOSIC WACKEFine-grained, quartz and feldspar labile fragments up to 1mm in aphanitic matx, poorly developedbedding, greyish to greyish green, massive, non-magnetic, hard, siliceous, minor pyrite associatedwith quartz-carbonate fracture-filling stringer.Overall scattered to up to Q.5% fine-grained pyrite.

HEMATITIZED ARKOSIC WACKEFine-grained, reddish brown to reddish grey, moderately hematitic, non-magnetic, minorquartz-carbonate fracture-filling stringer with hematite, poorly developed bedding, massive,gradual alteration contact.Overall Q.5% to V/. fine-grained pyrite locally up to 2'/, pyrite.37.10 Fractures at 60 degrees to core axis.

LITHIC SUB-ARKOSIC WACKEGrey, non-magnetic, similar to above 34.54 to 36.50, trace to nil pyrite.

HEMATITIZED ARKOSIC WACKEFine-grained, reddish brown to purplish red brown with dark reddish brown magnetic aphaniticfragment, nil to poorly developed bedding, massive, pervasively hematitic.Overall 2'/. to Y/, fine-grained pyrite locally up to 10X very fine to fine-grained pyrite 39.3 to40.75.

ARGILLITEFine-grained, greyish red to grey, brecciated to locally fine-grained bedding at 40 to 45 degreesto core axis, minor quartz-carbonate fracture-filling with hematite alteration on contact, poorlydeveloped bedding.Overall up to Q. S'/, fine-grained pyrite, locally 1X to 27. fine-grained pyrite.

BANDED MAGNETITE IRON FORMATION43.00 Sharp contact 70 degrees to core axis.Aphanitic to fine-grained, black, strongly magnetic, hard, siliceous, 1 to 5 mm laminae of bandedmagnetite iron formation and ARGILLITE to greywacke, locally contorted bedding at 30 degrees tocore axis, minor quartz-carbonate fracture-filling crosscutting bedding at 37 to 60 degrees to coreaxis with minor parallel to bedding usually non contorted.Overall scattered to trace pyrite, locally V/, fine-grained to coarse-grained pyrite.45.90 46.25 Fine-grained matrix with white phenocrysts, moderately hard to moderately soft.

non-magnetic, porphyry with 1 cm chilled upper contact at 60 degrees to core axis,lower contact GROUND CORE.

Sample

37706

3770737708

377093771037711

3771237713

:

From (m)

32.00

33.0033.75

38.2239.0040.00

41.0042.00

To (ra)

33.00

33.7534.75

39.0040.0041.00

42.0043.00

Lngt (m)

1.00

.751.00

.781.001.00

1.001.00

AU PPB

=s=*=.=±

5

1058

2055

55

:

AG PPM

.3

.2

.1

.1

.2

.3

.2

.1

AS PPM

1.0

1.68.7

1.52.71.0

1.01.2


From (m)

To (m)r Geology

50.22 77.85

47.65 47.78 Medium-grained to coarse-grained pyrite in siliceous stringer zone at 80 degrees tocore axis.

48.00 48.79 Scattered reddish hematitic stretched blobs. 48.54 48.70 Bands of hematitic stretched blobs parallel to bedding at 25 degrees to core axis.

HEMATITIZED ARKOSIC WACKE50.22 Lower contact at 20 degrees to core axis.Fine-grained, brownish red to reddish brown, massive, uniform, nil to poorly developed bedding,pervasively hematitic usually moderately magnetic, siliceous, hard, occasional aphanitic ARGILLITEweakly to moderately magnetic fragment.Moderately hematitic section brownish-grey to dark grey, fine-grained, massive, hard, siliceous.Gradual alt contact with pervasively hematitic and moderately hematitic section.Minor scattered section of quartz-carbonate fracture-filling up to 1mm.Very fine to fine-grained up to D.5% pyrite locally up to 3/i to 57. fine-grained pyrite.50.22 54.77 Weakly to moderately hematitic, scattered V/, to Z'/, fine-grained pyrite.50.22 50.42 Irregular banded magnetite iron formation.50.32 Irregular quartz-carbonate 2 cm veinlet.51.10 51.17 Altered, light brown to medium brown with quartz-carbonate fracture-filling stringer at

60 degrees to core axis.51.67 Quartz-carbonate stringer 2 cm at 55 degrees to core axis. 52.30 Q and chlorite 5 mm stringer with scattered fine-grained pyrite, spks of chalcopyrite

and fine-grained ars, 22 degrees to core axis.53.40 Quartz-carbonate 4.5 cm veinlet at 39 degrees to core axis, nil pyrite. 53.70 Quartz-carbonate 2.5 cm veinlet at 35 degrees to core axis. 54.10 Quartz-carbonate 2 cm veinlet at 28 degrees to core axis. 54.13 54.24 Fine-grained uniformly disseminated pyrite S'/, to 107,. 54.77 59.20 Uniformly pervasively hematitic, hard, siliceous, with aphanitic fragment, disseminated

2V. to y/, fine-grained pyrite with scattered 1 mm pyrite band, moderately magnetic. 56.07 Quartz veinlet 2 cm at 70 degrees to core axis. 56.35 Quartz veinlet 3 cm at 40 degrees to core axis. 58.10 59.20 Very fine to fine-grained pyrite y/, to T/,.58.46 Orange carbonate stringer with 2'/. fine-grained pyrite at 25 degrees to core axis. 59.20 62.00 Moderately hematitic, hard, siliceous, with aphanitic fragment, weakly magnetic,

occasional quartz-carbonate fracture-filling, trace to 27. fine-grained pyrite. 59.20 59.40 Chlorite and carbonate fracture-filling, vuggy. 62.00 70.00 Moderately to pervasively hematitic, hard,

moderately magnetic.62.80 End of occasional aphanitic band and fragment.63.23 Graded bedding aphanitic and fine-grained, sharp contact at 15 degrees to core axis. 63.74 Graded bedding aphanitic and fine-grained, sharp contact at 22 degrees to core axis. 63.85 Quartz-carbonate with chlorite 1.5 cm at 10 degrees to core axis terminated at 63.95

fracture at 60 degrees to core axis. 70.00 77.20 Gradual decrease in hematitization to fine-grained, greenish grey to dark grey, nil to

weakly magnetic, uniform, massive, nil to poorly developed bedding, scatteredquartz-carbonate fracture-filling at 10, 70 and 85 degrees to core axis,fracture-filling at 70 degrees to core axis crosscutting bedding, bedding at 50 degreesto core axis, minor hematite associated with fracture-filling stringer, scattered to upto 1/i fine-grained pyrite.

73.50 Irregular quartz veinlet 2 at 1.5 cm at 55 to 60 degrees to core axis. 75.00 77.85 Increasing aphanitic ARKOSE. 75.55 Quartz-carbonate veinlet 4 cm with fragment at 65 degrees to core axis.

siliceous, with aphanitic fragment.

Sample From (m)

Lngt (m)

AU PPB

AG PPM

AS PPM

MG96-01 - (continued) Page: 4 of 14

To (m)

77.85

78.30

83.46

84.00

86.83

88.40

78.30

83.46

84.00

86.83

88.40

93.20

Geology I Sample From To |Lngt AU l AG l (m) (m) (m) PPB PPM

77.20 Aphanitic weakly hematitic contact with fine-grained hematitic ARKOSE at 20 degrees to core axis.

77.20 77.85 Fine-grained, hematitic, quartz-carbonate fracture-filling stringer crosscutting bedding, overall 5'/. fine-grained pyrite over 5 cm at contact.

CARBONATED ULTRAMAFIC METAVOLCANICS77.85 Contact 30 degrees to core axis.Similar to above 23.00 to 23.90, fine-grained, blackish green, carbonatized, soft to moderatelysoft, occasional white and pink carbonate stringer, non-magnetic, schistose, chlorite and talcose,sheared and brecciated, nil to trace pyrite.78.33 Lower contact GROUND CORE.

HEMATITIZED ARKOSIC WACKESimilar to above 50.22 to 77.85, fine-grained with occasional aphanitic section, hematitic,scattered 2 ram to 5 mm quartz-carbonate fracture-filling stringer usually at 60 to 70 degrees tocore axis, massive, uniform, poorly developed bedding.Disseminated fine-grained pyrite Y/, to 2Z locally up to y/, to 5/i.82.28 82.40 Quartz vein 6 cm at 50 degrees to core axis crosscut by 3 mm quartz-carbonate stringer

at 30 degrees to core axis and displaced by 2 cm, scattered fine-grained pyrite. 83.10 83.20 Dark green, carbonated mafic to ultramafic band at 27 degrees to core axis.

HORNBLENDE SYENITE DIKEFine-grained, black brown matx with 0.5 to 1.0 mm black lathe phenocrysts hornfels altered tochlorite hard, non-magnetic, massive, uniform.Upper contact irregular at low angle, lower contact with quartz stringer at 70 to 75 degrees tocore axis.

ARKOSIC WACKEFine-grained, brownish black, weakly hematitic, non-magnetic, hard, siliceous, massive, uniform,nil to poorly developed bedding, occasional quartz-carbonate fracture-filling stringer at 50degrees to core axis usually 2 to 3 mm.Scattered to disseminated V/, to 27. fine-grained pyrite.

ARGILLITE 86.83 contact fine-grained hematitic and aphanitic non hematitic at 25 degrees to coreSharp

axis.Similar to above, fine-grained, blackish green to greenish black, very fine-grained to aphanitic, massive, uniform, hard, siliceous, occasional quartz-carbonate fracture-filling stringer. Overall up to V/. disseminated very fine to fine-grained pyrite. 87.33 Chlorite band 2 to 3 cm at 15 to 20 degrees to core axis with quartz-carbonate

fracture-filling stringer crosscutting and krinkled.

HEMATITIZED ARKOSIC WACKE88.40 Lower contact sharp at 24 degrees to core axis, contact with aphanitic and hematitic

fine-grained wacke bedding crosscut by quartz-carbonate fracture-filling stringer at 50degrees to core axis.

Similar to above, fine-grained, massive, uniform, hard, hematitic, non-magnetic to locally weakly magnetic, moderately developed bedding. Locally 2 to 57. quartz-carbonate fracture-filling stringer at 70 to 85 degrees to core axis, crosscutting stringer at 30 degrees to core axis usually with 3X to 5'/. fine-grained to medium-grained pyrite.

AS PPM


-ir From (m)

93.20

95.95

99.10

To l (m)

95.95

99.10

111.20

Geology

89.45 Bedding at 40 degrees to core axis.89.50 90.50 Intensely q and quartz-carbonate veinlet with fine-grained pyrite, Y/, to 5X

disseminated pyrite in matx.

ARGILLITE93.20 Gradual contact at 35 degrees to core axis.Fine-grained, dark green to pale brownish green with occasional weakly hematitic section, mm withstrongly magnetic section, locally minor quartz-carbonate fracture-filling stringer, occasionalaphanitic section.Scattered to disseminated 1X fine-grained pyrite, locally up to 27, to 3/J fine-grained pyrite.93.20 4.00 Cm band of fine-grained to medium-grained pyrite y/, to 57..94.14 Bmaf 1 to 1.5 cm band, bedding at 30 degrees to core axis.

BANDED MAGNETITE IRON FORMATION95.95 Sharp lower contact at 32 degrees to core axis.Similar to above, fine-grained, black, hard, strongly magnetic, contorted bedding with slip planescrosscutting bedding at 20 degrees to core axis, 1 to 5 mm band of grey to greyish black ibARGILLITE.Scattered up to l'/, fine-grained to medium-grained pyrite, locally up to 27..96.35 96.42 Brownish green ARGILLITE.96.72 96.93 Brownish green ARGILLITE.96.95 2.00 Cm disseminated band of 5/i fine-grained pyrite crosscutting banded magnetite iron

formation.97.08 Sharp lower contact at 20 degrees to core axis.97.08 99.10 Reddish brown hematitic ARGILLITE and wacke strongly magnetic with black mif band with

fine-grained pyrite parallel to bedding at 30 degrees to core axis.98.12 Coarse-grained pyrite at banded magnetite iron formation section.98.56 98.80 Banded magnetite iron formation with 3/i to 5X pyrite, bedding at 32 degrees to core

axis, stringer of disseminated pyrite crosscutting banded magnetite iron formation at35 degrees to core axis.

98.98 99.05 Banded magnetite iron formation with quartz-carbonate stringer parallel to bedding.

HEMATITIZED ARKOSIC WACKE99.10 Lower contact sharp with quartz-carbonate veinlet at 42 degrees to core axis.Similar to above, fine-grained with aphanitic section, reddish brown, hematitic, non-magnetic.hard, siliceous, massive, uniform, scattered quartz-carbonate stringer and section of 5 intenselyfractured, quartz-carbonate stringer usually at 50 degrees to core axis, occasional chloritestringer usually at 40 degrees to core axis crosscut by fractures.Overall 1X to 27. fine-grained pyrite, locally Y/. to 5X disseminated very fine to fine-grained pyrite103.00 104.40 Gradual decrease in hematite.104.40 111.20 Fine-grained to locally aphanitic, weakly hematitic.104.90 Bedding at 35 degrees to core axis.105.60 Quartz veinlet 2 cm at 30 degrees to core axis.105.70 105.90 Mafic dike grey chilled contact.106.60 Quartz veinlet 2.5 cm at 30 degrees to core axis with speck of chalcopyrite, contact

blackish green ARGILLITE and hematitic ARKOSE based on grain size and colour at 20degrees to core axis.

107.70 Platey pyrite on chlorite fractures at 20 degrees to core axis.108.10 111.20 Increasing quartz-carbonate fracture-filling stringer and quartz-carbonate veinlet,

weakly magnetic, minor chlorite, trace to scattered pyrite in veining, decreasinghematitization, overall 2'/, to 3X fine-grained pyrite.

: -| Sample

37714

37715

37716

37717

377183771937720

;

From (m)

89.50

95.95

97.00

98.00

108.00109.00110.00

TO l (m)

90.50

97.00

98.00

99.10

109.00110.00111.00

;™mLngt (m)

1.00

1.05

1.00

1.10

1.001.001.00

AU PPB

5

5

5

167

ccc

AG PPM

.1

.1

.2

.3

.1

.1

. 2

AS PPM

1.0

1.2

1.9

2.3

5.38.31.2


From I (m)

111.20

133.46

143.33

144.78

To Geology(m) L l33.46

143.33

144.78

155.26

110.40 Bedding at 25 degrees to core axis.

ARKOSIC WACKESimilar to above, fine-grained, black brown with reddish brown section, weakly hematitic, mmaphanitic section of ARGILLITE, occasional quartz-carbonate fracture-filling stringer at 40 degreesto core axis, parallel to bedding and crosscutting bedding.Trace to scattered V/. to 2X disseminated fine-grained pyrite.113.80 124.20 Increasing hematitization.119.50 Bedding at 40 degrees to core axis.124.50 Bedding at 30 degrees to core axis, V/, to 2/i pyrite at 30 degrees to core axis.126.50 Aphanitic to fine-grained contact at 25 degrees to core axis.127.03 127.16 Quartz-carbonate fracture-filling stringer at 40 degrees to core axis.129.20 Chlorite fracture at 10 degrees to core axis.129.30 131.65 Hematite fracture-filling.131.60 Bedding at 60 to 65 degrees to core axis.131.65 133.46 Medium brown, weakly hematitic with section of buff to pale green brown, V/,

disseminated fine-grained pyrite, locally up to 2'A to 3X fine-grained pyrite,chlorite fracture-filling crosscut by quartz-carbonate fracture-filling stringer.

131.65 132.00 Bleached.132.50 Chlorite seam at 33 degrees to core axis.132.67 Quartz-carbonate veining 2 cm at 70 and 75 degrees to core axis.132.80 Quartz-carbonate stringer 1.5 cm at 65 degrees to core axis.133.20 Quartz-carbonate stringer 1 cm at 50 degrees to core axis with quartz-carbonate

fracture-filling at 50 degrees to core axis.

ALTERED ARKOSIC WACKEFine-grained, dark to medium green with pale brownish green and light green alteration due toquartz-carbonate stringer and quartz-carbonate fracture-filling, occasional hematite alteration onvein contact, massive, uniform with occasional aphanitic fragment or band.Overall trace to Q.5% fine-grained pyrite, locally up to 1X to 2'/, fine-grained pyrite.133.46 141.27 Hematite alteration and fine-grained pyrite ARKOSIC WACKE quartz-carbonate stringer.134.70 135.05 Soft, carbonated ultramafic metavolcanic with carbonate stringer parallel to contact

at 20 degrees to core axis.137.34 137.41 Soft, carbonated ultramafic metavolcanic void of stringers contact at 60 degrees to

core axis.141.27 143.33 Pale green and buff alteration at stringer and vein contact, older quartz-carbonate

stringer contorted with later quartz-carbonate stringer with minor chlorite andpyrite at Q.5% to 1.0X, hematite fracture-filling with pyrite, veining at 4 to 6pervasive 30 cm usually at 33 degrees to core axis.

ARKOSIC WACKESimilar to above, fine-grained, black to dark grey to greyish green, with aphanitic section, bandedmagnetite iron formation at.143.39 Banded magnetite iron formation at 40 degrees to core axis non contorted, V/, to 2X gm

pyrite.143.51 To 143.58 banded magnetite iron formation at 40 degrees to core axis non contorted.

T/, to 2'/. medium-grained pyrite.144.00 144.78 Quartz-carbonate fracture-filling with pale green to buff alteration, occasional

hematite fracture-filling stringer with pyrite, overall up to V/. pyrite.

BANDED MAGNETITE IRON FORMATION

Sample

l

37721

37722

37723377243772537726

37727

From (m)

131.65

132.50

139.25140.25141.27142.27

143.33

To (m)

132.50

133.46

140.25141.27142.27143.33

144.00

Lngt (m)

.85

.96

1.001.021.001.06

.67

AU PPB

5

5

55

1627

12

AG I AS PPM PPM

.2

1.0

.1

.1

.2

.1

.1

1.7

1.7

1.01.61.01.0

1.5


———rFrom I (m)

——— ——— IL

155.26

156.97

159.89

162.75

164.63

"T. "f

(m)

156.97

159.89

162.75

164.63

166.10

Geology

144.78 Sharp contact at 43 degrees to core axis.Similar to above, fine-grained, black, hard, siliceous, strongly magnetic, occasional band reddishjasper iron formation at 146.50 to 146.56, uniform, well developed bedding at 41 to 42 degrees tocore axis, 1 to 3 mm laminae, minor quartz-carbonate fracture-filling stringer parallel to bedding.occasional carbonate stringer crosscutting bedding.Occasional dark green ARGILLITE to greywacke band from 152.00 to 152.37 and 153.32 to 153.68.Scattered to trace pyrite.146.00 Pyrite stringer parallel to bedding at 42 degrees to core axis.151.70 To 151.80 jasper laminae, 1 to 2 mm at 40 degrees to core axis.

155.00 155.26 Crushed zone - brecciated with quartz-carbonate stringer with specular hematite andminor pyrite ARKOSIC WACKE stringer crosscutting bedding, occasional pyrite from 1 to2 mm.

155.00 Quartz stringer at 70 degrees to core axis.

ALTERED ARKOSIC WACKE155.26 Sharp contact at 65 degrees to core axis.

Similar to above, pale green, hard, siliceous, non-magnetic, massive, uniform.Overall 17, to 27. fine-grained pyrite.

HORNBLENDE SYENITE DIKE156.97 Sharp baked contact at 45 degrees to core axis.

Fine-grained matrix, dark brown to reddish brown with up to 0.5 mm white phenocrysts, hard,siliceous, locally specular hematite with fine-grained pyrite in vug at upper contact, moderatelyto strongly magnetic, massive, uniform, homogeneous, numerous quartz-carbonate fracture-filling.Overall scattered to up to V/. fine-grained pyrite.

ALTERED ARKOSIC WACKE159.89 Sharp lower contact at 40 degrees to core axis.

Similar to above 155.26 to 156.97.161.75 162.75 Overall 2/i to 3/i pyrite, locally up 5X very fine to fine-grained pyrite.161.90 162.75 Pale green with minor medium brown alteration ARKOSIC WACKE quartz-carbonate

f racture-f i lling.

BANDED MAGNETITE IRON FORMATION162.75 Lower contact at 40 degrees to core axis.Similar to above, scattered carbonate stringer parallel to bedding, jasper fragment at 162.87 and163.10.Overall scattered to up to Q.5% pyrite.163.10 Bedding at 15 to 20 degrees to core axis.163.52 Jasper band crosscut by by slip plane parallel to core axis and 35 degrees to core

axis ARKOSIC WACKE carbonate stringer.

HEMATITIZED ARKOSIC WACKE164.63 Lower contact at 15 degrees to core axis.Similar to above, fine-grained, extremely altered, hematitized and bleached section, chlorite on

Sample

3772837729

3773037731

377323773337734

377353773637737

From (m)

153.00154.00

155.26156.00

156.97158.00159.00

159.89160.75161.75

To(m)

154.00155.26

156.00156.97

158.00159.00159.89

160.75161.75162.75

Lngt (m)

1.001.26

.74

.97

1.031.00.89

.861.001.00

AU PPB

532

55

955

55

10

AG PPM

.2

.2

.1

.1

.1

.1

.1

.2

.2

.3

AS PPM

1.01.2

1.01.0

1.01.01.0

1.21.21.2


From l (m)

166.10

184.00

184.65

"T01

(m)

84.00

184.65

198.30

Geology

fracture, hard, siliceous, non-magnetic, scattered fine-grained pyrite. Locally minorquartz-carbonate fracture-filling at low to moderate degrees to core axis.

LITHIC SUB-ARKOSIC WACKE166.10 Lower contact at 40 degrees to core axis.Similar to above, fine-grained with locally aphanitic section, dark green, chlorite, buffalteration ARKOSIC WACKE quartz-carbonate fracture-filling at 50 to 70 degrees to core axis, whitequartz-carbonate fracture-filling at 50 to 70 degrees to core axis, siliceous, moderately hard,non-magnetic, massive, uniform with occasional hematitic alteration along fracture, minor localbrecciation.Overall trace to up to 17, fine-grained pyrite, locally up to 3X very fine to fine-grained pyrite.174.10 175.85 Buff green alteration locally intense ARKOSIC WACKE quartz-carbonate fracture-filling

with up to V/* pyrite.177.58 Quartz-carbonate stringer 1 cm at 70 degrees to core axis.178.82 Quartz-carbonate stringer 1 cm at 40 degrees to core axis.178.85 Quartz-carbonate stringer 1 cm at 45 degrees to core axis.179.00 Cleavage at 45 degrees to core axis.179.04 180.20 Intense fracture-filling ARKOSIC WACKE buff green alteration, overall up to Q.5%

pyrite locally up to 2'/,.179.45 Quartz-carbonate stringer 5 mm at 70 degrees to core axis.183.00 184.00 Patchy buff green atln, increasing hematitization.

HORNBLENDE SYENITE DIKE184.00 Sharp lower contact at 15 degrees to core axis.Similar to above, scattered to up to Q.5% pyrite, locally coarse-grained.

LITHIC SUB-ARKOSIC WACKE184.65 Wavey lower contact at 15 degrees to core axis.Similar to above, fine-grained, chlorite, moderately soft to moderately hard, non-magnetic, darkgreen to pale green with buff green alteration ARKOSIC WACKE some quartz-carbonatefracture-filling, minor chlorite fracture-filling.Overall scattered to up to Q.5% fine-grained pyrite.184.65 185.50 Overall 27. to y/, fine-grained pyrite.184.90 185.10 Low angle wedge of medium-grained hematite with up to 3X pyrite.189.32 189.44 Buff alteration band at 55 degrees to core axis and contorted quartz stringer with 3X

to S'/, fine-grained pyrite.193.50 Buff green to buff alteration ARKOSIC WACKE quartz-carbonate fracture-filling.194.34 194.80 Contorted bedding with aphanitic section and randomly orientated pinkish buff hard.

siliceous, felsic stringer.194.80 194.90 Medium-grained, medium to dark green, Vf, medium-grained pyrite, chloritic masses.194.90 Contorted carbonate stringer 2 to 3 mm at 20 degrees to core axis.195.20 195.65 Low angle contorted carbonate stringer from 1.5 cm to 5 mm.196.25 To 198.30 medium brown to reddish medium brown atln ARKOSIC WACKE quartz-carbonate

fracture-filling and stringer with section of unaltered dark green wacke to arkose.scattered fine-grained pyrite.

196.80 White quartz-carbonate 2 cm veinlet nil pyrite at 30 degrees to core axis.

197.95 198.30 Greyish white veining at 25 to 35 degrees to core axis crosscut by 2 mm whitequartz-carbonate tension fracture-filling stringer at 50 degrees to core axis with upto V/. fine-grained pyrite.

Sample!

37738

37739

37740

37741

3774237743

1

1 From (m)

174.00

175.00

185.60

196.10

197.00197.80

-TT1(m)

175.00

175.85

186.40

197.00

197.80198.30

:Lngt (m)

1.00

.85

.80

.90

.80

.50

AU PPB

5

5

5

C

55

AG PPM

.2

.1

.2

.3

.1

.1

ASPPM

1.0

3.0

1.5

2.1

3.01.0

HG96-01 (continued) Page: 9 of 14

From To (m) (m)

Geology

98.30 199.30

199.30

200.50

202.60

202.90

204.95

205.25

200.50

202.60

202.90

204.95

205.25

205.60

BANDED MAGNETITE IRON FORMATIONSimilar to above, gradual contact, bedding at 30 degrees to core axis, scattered quartz-carbonatestringer parallel to bedding, scattered fine-grained to medium-grained pyrite.198.34 Quartz-carbonate stringer 1 cm at 25 degrees to core axis.198.50 Scattered to disseminated pyrite band.198.62 198.69 Quartz-carbonate veinlet at 20 to 25 degrees to core axis with 1 to 2 cm hematitic

alteration on contact, with trace pyrite. 198.75 198.91 Fine-grained pyrite 0.5X. to U.198.83 Contorted quartz-carbonate stringer from low to 35 degrees to core axis. 199.17 199.30 Scattered 2'/. medium-grained pyrite.

LITHIC SUB-ARKOSIC WACKE199.30 Lower contact at 35 degrees to core axis. Similar to above, fine-grained to aphanitic, quartz-carbonate fracture-fi l ling. Scattered to Q.5% to V/. pyrite locally up to 27.. 200.33 Banded magnetite iron formation 2 cm

alteration.

black, hard, non-magnetic to wm, minor

at 28 degrees to core axis, weak hematitic

HORNBLENDE SYENITE DIKE200.50 Sharp lower contact at 18 to 20 degrees to core axis.Fine-grained brownish matrix with black to blackish green phenocrysts hornblende altered tochlorite, moderately soft to moderately hard, non-magnetic, scattered pyrite, minorquartz-carbonate fracture-filling and hematitic alteration.201.00 201.50 Inclusion of fine-grained hematitic altered metasediments.201.50 202.60 Increase in phenocrysts.

BANDED MAGNETITE IRON FORMATION202.60 Sharp lower contact at 18 to 20 degrees to core axis.Similar to above, low angle contorted bedding.

LITHIC SUB-ARKOSIC WACKE202.90 Sharp lower contact at 23 degrees to core axis.Similar to above, aphanitic to 203.34.203.34 Contact at low degrees to core axis.203.95 204.95 Fine-grained, massive, uniform, reddish brown, weakly magnetic, nil fracture-filling,

overall l'/, disseminated pyrite.204.49 Vuggy quartz-carbonate fracture-filling 5 mm at 20 degrees to core axis. 204.80 Vuggy quartz-carbonate fracture-filling 5 mm at 65 degrees to core axis.

HORNBLENDE SYENITE DIKE204.95 Sharp lower contact at 27 degrees to core axis.Similar to above 200.50 to 202.60, medium-grained phenocrysts.

ARGILLITE205.25 Lower contact broken core.Aphanitic, black to greyish black with occasional black banded magnetite iron formation, graded bedding ARGILLITE to ARKOSE at 20 degrees to core axis displaced with carbonate fracture-filling at 40 degrees to core axis, above displaced by two 2.5 cm carbonate veinlet at 205.60 contact at 25 degrees to core axis.

Sample

37744

From (m)

198.30

To (m)

199.30

Lngt (m)

1.00

AU PPB

8

AG PPM

.2

AS PPM

2.3


om j To li) (m)

From (m)

Geology

205.60 207.46

207.46

207.80

208.54

208.62

208.86

215.15

207.80

208.54

208.62

208.86

215.15

216.24

HEMATITIZED ARKOSIC WACKESimilar to above, fine-grained, hematitic, massive, uniform, homogeneous. T/. fine-grained disseminated pyrite locally up to 3X with minor quartz-carbonate fracture-filling, wm. 205.80 Crushed zone at 25 degrees to core axis ARKOSIC WACKE two 2.5 cm wide pink carbonate. 206.10 206.30 Aphanitic stretched clast at 25 degrees to core axis with up

fine-grained pyrite.

BANDED MAGNETITE IRON FORMATION207.46 Sharp lower contact at 43 degrees to core axis.Similar to above, non contorted bedding, fine-grained laminae magnetite and fine-grained magnetichematitic ARGILLITE to ARKOSE.

HEMATITIZED ARKOSIC WACKE207.80 Sharp lower contact at 35 degrees to core axis. Similar to above at 205.60 to 207.46.208.16 Banded magnetite iron formation 1 cm at 30 degrees to core axis. 208.21 Band of fine-grained pyrite 1 mm at 30 degrees to core axis.208.30 Black chlorite band with fine-grained pyrite at 40 degrees to core axis crosscutting

pyrite band at 208.21.

BANDED MAGNETITE IRON FORMATION208.54 Sharp lower contact at 27 degrees to core axis.Similar to above.

HORNBLENDE SYENITE DIKE208.62 Sharp lower contact at 30 degrees to core axis.Similar to above, chloritic, soft, non-magnetic to weakly magnetic.

HEMATITIZED ARKOSIC WACKE208.86 Lower contact with pink carbonate stringer at 35 degrees to core axis.Similar to above, fine-grained, weakly magnetic.208.86 208.96 Fine-grained to medium-grained, pink brown to reddish brown, hematitic.208.96 Sharp contact at 25 degrees to core axis.208.96 215.15 Minor and occasional hematitic ARKOSE, locally up to 2'/. fine-grained pyrite.209.00 210.00 Broken core.210.20 Banded magnetite iron formation 1 cm with 2'/. fine-grained pyrite at 50 degrees to

core axis. 211.16 211.30 Banded magnetite iron formation upper contact at 55 degrees

contact at 15 degrees to core axis. 211.70 212.05 Banded magnetite iron formation upper contact at 25 degrees to core axis, lower

contact at 10 degrees to core axis. 212.05 215.15 Increasing quartz-carbonate fracture-filling at 20 degrees to core axis crosscutting

stringer at 72 and 35 degrees to core axis. 214.00 214.30 Banded magnetite iron formation upper contact at 50 degrees to core axis, lower

contact at 20 degrees to core axis. 214.32 214.45 Banded magnetite iron formation contact at 25 degrees to core axis, quartz stringer

at 25 degrees to core axis with 2'/. fine-grained pyrite.

BANDED MAGNETITE IRON FORMATION215.15 Fracture at 38 degrees to core axis crosscutting lower contact at 25 degrees to core

axis and displacing 1.5 cm.

I Samp l e

very fine to e-filling, wm. ink carbonate. y/, very fine to

rained magnetic

is crosscutting

rite,

t 50 degrees to

ore axis, lower

ore axis, lower

is crosscutting

ore axis, lower

quartz stringer

degrees to core

From F To fLngtJAU j AG (m) (m) l (m) PPBJ PPM

AS PPM

MG96-01 (continued) Page: 11 of

Geology

216.24

216.50

217.17

225.40

226.06

216.50

217.17

225.40

226.06

231.20

Similar to above with hematitized arkosic wacke.215.19 216.14 Wispy magnetic band fracture and sheared.215.80 Fracture at 12 degrees to core axis displaces 2 mm quartz-carbonate stringer at

215.92 with contact at 78 degrees to core axis, displacement 4 cm. 216.07 216.14 Banded magnetite iron formation at 30 degrees to core axis crosscut by 1 to 2

quartz-carbonate stringer 10 in 20 cm, 65 to 70 degrees to core axis. 216.14 216.24 Hematitic ARGILLITE to ARKOSE.

HORNBLENDE SYENITE DIKE216.24 Sharp lower contact at 32 degrees to core axis.Similar to above, carbonatized, chloritic, fine-grained to medium-grained.

BANDED MAGNETITE IRON FORMATION 216.50 Contact at 35 degrees to core axis.Similar to above banded magnetite iron formation and hematitized arkosic wacke.216.50 216.76 Low angle fracture displaces quartz-carbonate fracture-filling and stringer at 65

degrees to core axis.

HEMATITIZED ARKOSIC WACKE217.17 Sharp lower contact at 40 degrees to core axis.Similar to above, fine-grained, reddish brown, hematitic, hard, siliceous, quartz-carbonatefracture-filling with and without buff contact alteration usually with quartz-carbonate stringer at37 degrees to core axis and quartz-carbonate with chlorite at 65 degrees to core axis crosscut byquartz stringer at 20 degrees to core axis.Overall up to 1X fine-grained pyrite.217.86 Banded magnetite iron formation 2 cm upper contact at 25 degrees to core axis, lower

contact fractured at 17 degrees to core axis. 218.35 219.00 Quartz-carbonate stringer 1 cm and 1.5 cm ARKOSIC WACKE buff alteration at 65 degrees

to core axis.219.01 219.09 Banded magnetite iron formation with contact at 45 to 50 degrees to core axis. 220.56 220.80 Banded magnetite iron formation contact at 30 degrees to core axis. 222.46 222.60 Banded magnetite iron formation and hematitized arkosic wacke laminae at 20 degrees

to core axis. 222.84 223.00 Banded magnetite iron formation and hematitized arkosic wacke laminae at 30 degrees

to core axis, crosscutting fractures at 50 degrees to core axis. 223.00 225.40 Medium brown to medium green, moderate quartz-carbonate fracture-filling, extremely

fracture-filling from 223.00 to 223.40, overall 1X to 2'/. fine-grained pyrite in matrix 225.00 225.40 Felsic alteration.

HORNBLENDE SYENITE DIKE225.40 Sharp contact 44 degrees to core axis.Similar to above, fine-grained to medium-grained, pink brown with coarse-grained black phenocrystsof hornblende altered to chlorite, weak pervasive chloritic alteration, nil to trace pyrite.

ALTERED ARKOSIC WACKE226.06 Sharp contact at 40 degrees to core axis.Fine-grained, medium green to brownish green hematitic alteration ARKOSIC WACKE quartz-carbonatefracture-filling with overall IK to 2'/. fine-grained pyrite locally up to 3X hard, siliceous,non-magnetic, massive, uniform to 228.30.226.30 Greyish quartz-carbonate stringer 1.5 mm with chlorite at 20 degrees to core axis.226.80 Grey quartz stringer 2 mm with l'/, fine-grained pyrite at 33 degrees to core axis.

1at

mm

65

te at by

er

es

es

es

iyix

ts

tps,

Sample

37745

37746

;~1

From I (m)

226.10

227.10

To 1 (m)

227.10

228.30

Lngtl (m)

1.00

1.20

AU l PPB

6

5

AG|PPM

.2

.2

E

AS PPM

2.6

4.0


231.20 236.80

236.80 247.65

Geology

227.56 227.74 Felsic.228.10 Quartz-carbonate stringer with 57, fine-grained pyrite at 7!

displaced 4 cm by chlorite fracture-filling at 22 degrees to core axis. 228.30 231.20 Buff to pale green buff alteration ARKOSIC WACKE quartz-carbo

scattered to V/. fine-grained pyrite.

BANDED MAGNETITE IRON FORMATION231.20 Sharp lower contact at 40 degrees to core axis.Similar to above, fine-grained black laminae banded magnetite iron formation and fine-grained blackto greyish black ARKOSE laminae, minor to locally moderate quartz-carbonate fracture-filling, hard,siliceous, strongly magnetic, locally contorted bedding.Scattered to up to 0.5X fine-grained pyrite in ARKOSE, minor streaks of pyrite parallel to beddingat 40 degrees to core axis.231.74 232.10 Nil magnetite band.232.00 Quartz-carbonate stringer 2 mm at 50 degrees to core axis.233.00 Fracture at 52 degrees to core axis terminates banded magne

bedding at 47 degrees to core axis.233.05 233.73 Nil magnetite band, graded bedding at 45 degrees to core axis. 233.80 234.52 Nil magnetite band, moderate quartz-carbonate fracture-filling

buff green alteration, scattered fine-grained pyrite.234.37 234.52 Felsic dike, sharp lower contact at 35 to 40 degrees to core axis. 234.52 234.57 Crushed quartz-carbonate filled shear zone.234.66 Banded magnetite iron formation bedding at 37 degrees to core axis. 235.30 236.80 Massive ARKOSE, upper contact sharp at 50 degrees to core axis,

degrees to core axis with quartz-carbonate stringer parallel tdeveloped quartz-carbonate fracture-filling usually ARKOSIC MAalteration and trace to scattered fine-grained pyrite.

BANDED MAGNETITE IRON FORMATION236.80 Sharp lower contact at 30 degrees to core axis.Similar to above, fine-grained, 1 to 2 mm black magnetite laminae locally withue, hard, siliceous, strongly magnetic, ARKOSIC WACKE minor black to greyishwell developed bedding ARKOSE locally contorted bedding, weak toquartz-carbonate fracture-filling, locally vuggy carbonate stringer.Trace to scattered pyrite locally T/, to 27, medium-grained with minor fine-grained pyrite.237.50 Bedding at 47 degrees to core axis.237.53 239.20 Moderate developed quartz-carbonate fracture-filling, minor di

by fractures, locally contorted bedding, occasional fracture-filling stringer parallel to bedding and crosscutting bedding.

237.54 Low angle pyrite stringer.237.54 237.88 Hematitic, reddish brown hue.238.27 Chloritic zone at 50 degrees to core axis.238.80 Pyrite masses.240.10 240.20 Chloritic zone, fault at 65 degrees to core axis crosscut

parallel to core axis. 240.20 Quartz-carbonate stringer at 62 degrees to core axis crosscutti

core axis. 240.65 Quartz-carbonate stringer at 62 degrees to core axis crosscutti

core axis.240.80 Pyrite fracture-filling. 241.00 241.20 Vuggy quartz-carbonate stringer.

grees to core axisIS.

k f racture-f i lling,

fine-grained black •ure-f i lling, hard.

jarallel to bedding

tite iron formation

ARKOSIC WACKE pale

.owen contact at 30 3 bedding, moderate CKE pale green buff

h reddish hematitic black fine-grained moderate developed

pyrite.

acements of bedding iloritic stringer, ing.

g contorted bedding

redding parallel to

bedding parallel to

Sample From (m)

To (m)

.ngt (m)

AU PPB

AG PPM

AS PPM


Fromnri To ) (m) l

Geology Sample! From j To (m) (m)

247.65

248.87

258.57

248.87

258.57

264.00

bedding and non contorted bedding at 40 degrees to

241.60 Bedding at 40 degrees to core axis. 241.88 242.00 Medium-grained pyrite up to V/,. 243.20 Sharp contact between contorted

core axis.243.50 247.65 Contorted bedding parallel to core axis to low angle. 243.70 244.10 Vuggy quartz-carbonate stringer and fracture-filling. 245.00 Quartz-carbonate stringer 2 cm at 42 degrees to core axis. 245.40 Quartz-carbonate stringer 2 cm at 40 degrees to core axis. 246.00 246.25 Jasper iron formation. 246.47 246.50 Felsic dike, contact irregular to 60 degrees to core axis.

HORNBLENDE SYENITE DIKE247.65 Sharp contact at 80 degrees to core axis crosscutting bedding at 45 degrees to core

axis. Similar to above fine-grained, dark brown, massive, phenocrysts, non-magnetic.

BANDED MAGNETITE IRON FORMATION248.87 Sharp contact at 45 degrees to core axis crosscutting banded magnetite iron formation

bedding with 2 mm quartz-carbonate stringer at 60 degrees to core axis. S i mi lar to above. 248.87 253.12 Contorted bedding. 252.35 252.50 Fine-grained hornblende syenite dike crosscutting banded magnetite iron formation

bedding at upper contact 70 degrees to core axis and lower contact at 62 degrees tocore axis, lower contact displaced 4 cm by fracture at 12 degrees to core axis.

253.08 253.12 Medium-grained hornblende syenite dike, parallel to bedding, sharp contact at 40degrees to core axis.

253.12 257.47 Less contorted bedding.253.44 253.56 Vuggy carbonate band with 5'A to 10X fine-grained pyrite. 254.62 254.68 Aphanitic blackish green mafic dyke at 75 degrees to core axis crosscutting bedding

at 25 degrees to core axis. 255.20 255.90 Grey to greyish black ARKOSE Less banded magnetite iron formation, magnetite, bedding

at 40 degrees to core axis. 257.02 257.47 Massive, fine-grained, hard, siliceous, non-magnetic, dark grey ARKOSE, upper contact

at 24 degrees to core axis, with minor quartz-carbonate fracture-filling crosscuttingbedding at upper contact at 35 degrees to core axis.

257.47 258.57 Contorted bedding, banded magnetite iron formation to ARKOSE 60 40.

ALTERED ARKOSIC WACKE258.57 Sharp contact at 40 degrees to core axis displaced 1 cm by fracture at 75 degrees to

core axis.Similar to above, fine-grained, massive, nil to poorly developed of bedding, hard, siliceous, poorly to moderate developed of quartz-carbonate fracture-filling to 260.00, brownish to reddish brown, hematitic.Overall V/. fine-grained pyrite locally up to 3X to 5X pyrite. 258.86 Quartz stringer 1 cm contorted at 40 degrees to core axis with minor fine-grainec

pyrite.259.14 Quartz stringer with specular hematite contorted at 70 degrees to core axis. 259.22 259.30 Q veinlet at 40 degrees to core axis with fragment, 3 7, fine-grained pyrite in

matrix, V/, in veinlet. 259.52 Q. veinlet 1.5 cm at 30 degrees to core axis with specular hematite.

Lngt (m)

AU PPB

AG PPM

ASPPM

37747

3774837749

258.56

259.56260.56

259.56

260.56261.56

1.00

1.001.00

7

cc

.2

.2

.2

1.4

1.51.8

M696-01 (continued) Page: 14 of 14

I From (m)

264.00

To (m)

Geology

260.60 Decreasing quartz-carbonate fracture-filling.262.50 263.29 Pale green sericitic alteration of matrix.263.29 263.35 Pale green, hematitic, reddish brown.263.29 Sharp contact at 55 degrees to core axis.263.35 263.68 Fine-grained, grey, non-magnetic, bleached zone.263.68 Sharp contact at 65 degrees to core axis.263.68 264.00 Fine-grained, reddish brown, V/. to 25! fine-grained pyrite.

END OF HOLECASING LEFT IN HOLE.

Sample

3775037751

From (m)

261.56262.56

To (m)

262.56263.29

Lngt (m)

1.00.73

AU PPB

574

AG PPM

.2

.2

AS PPM

1.01.9

CertificatBondar Clegg InP'fcPfmPfin of

C-J t—' l j; ,u..:_. .^. 'JL, ; LLLiL l Ir! A 1Inchcape Testing Services , ; ,, ?" inn , j h AnaiYsls .................................................................................................................................................^

HONETA PORCUPINE MINES INCP.O. BOX 1756TIMMINSONTARIOP4M 7U9

Bondar-Clegg A Company Ltd. 5420 Canotek Road, Ottawa, Ontario, KIJ 9G2, Canada

Tel: (613) 749-2220, Fax: (613) 749-7170 """~""'~'""ilb s'i'r

CertificatiBondar Clegg of

^ Inchcape Testing Services Analysis

REPORT: T96-57179.0 ( COMPLETE ) REFERENCE:

CLIENT: MONETA PORCUPINE MINES INC SUBMITTED BY: RS PROJECT: NONE DATE PRINTED: 23-APR-96

NUMBER OF LOWER ORDER ELEMENT ANALYSES DETECTION LIMIT EXTRACTION METHOD

1 Au30 Gold 37 5 PPB Fire Assay of 30g 30g Fire Assay - AA Z Ag Silver 37 0.1 PPM HCL:HN03 (3:1) ATOMIC ABSORPTION

3 As Arsenic 37 1.0 PPM HCL:HN03 (3:1) HYDR. GEN/AA

SAMPLE TYPES NUMBER SIZE FRACTIONS MUMBER SAMPLE PREPARATIONS NUMBER

:zvzz:.iiRiLi:'JcM^PULVERIZATION 37

REPORT COPIES TO: P.O. BOX 1756 INVOICE TO: P.O. BOX 1756

TO FAX:705-267-7490

Bondar-Clegg Si Company Lid. 5420 Canotek Road, Ottawa, Ontario, KIJ 9G2, Canada

Tel: (613) 749-2220, Fax: (613) 749-7170 ——~. ——----——~.~.-.————-—

Bondar CleggInchcape Testing Services

CertificattofAnalysis

REPORT:

SAMPLE NUMBER

T96-57179.0 ( COMPLETE )

ELEMENT Au30 UNITS PPB

AgPPM

DATE PRINTED: 23-APR-96

PROJECT: NONE PAGE 1

As PPM

37701 37702

: 37703 ; 37704 i 37705

<5

36 27 27

•eO.1

<0 . 1 ^.1

^•1

3.0 2.7 3.5 1.6

37706 i 37707

37708 ; 37709

37710

^ 105

8 20

0.30.2

•eO.I

0.2

•O.O 1.6 8.7 1.5 2.7

37711 37712 37713 37714 37715

^

<5 <5

^

0.3 0.2

•^0. 1

^. 1

•O.O 1.2

1.2

37716 37717

i 37718 i 37719 : 37720

<5

167

<5<5

0.2 0.3

0.2

1.9 2.3 5.3 8.3 1.2

: 37721 : 37722

37723 37724 37725

^

<5 <5

16

0.2 1.0

O.1

0.2

1.7 1.7

•d.O 1.6

37726

37727 37728 37729

: 37730

: 37731 i 37732

37733 37734 37735

2712

32^

<5

9

^ <5

0.2 0.2

^. 1

<0 . 1

^. 1

^.1

0.2

1.5

1.2

1.2

37736 37737

<5

100.2 0.3

1.2 1.2

Bondar-Clegg A Company Ltd.

5420 Canotek Road. Ottawa, Ontario, KIJ 9G2, Canada , 1 -i S ^^' Y ^^tr-

Td : (6 1 3) 749-2220, Fax : (6 1 3) 749-7 1 70 ub Supervisor

Certificate^ Bondar Clegg of

"^^ Inchcape Testing Services AnalysisDATE PRINTED: 23-APR-96

REPORT: T96-57179.0 ( COMPLETE ) PROJECT: NONE PAGE 2

STANDARD ELEMENT Au30 Ag As NAME UNITS PPB PPH PPM

ANALYTICAL BLANK ^ •eO.1 ^.0ANALYTICAL BLANK - 0.1 ^.0

Number of Analyses 122

Mean Value 2.5 0.08 0.50Standard Deviation - 0.035 tO.OOI

Accepted Value 5 0.1 O.1

BCC GEOCHEM STD 4 - 0.6 29.9 Number of Analyses - 1 1

Mean Value - 0.56 29.89 Standard Deviation Accepted Value - 0.8 30.0

CANMET GTS-2 273Number of Analyses 1Mean Value 272.9Standard Deviation -Accepted Value 263 1.0

BCC GEOCHEM STD 3 - 5.0 320.6 Number of Analyses - 1 1 Mean Value - 5.00 320.59

Standard Deviation Accepted Value - 5.8 310.0

Bondar-Clegg & Company Ltd. 5420 Canotek Road, Ottawa, Ontario, KIJ 9G2, Canada

Tel: (613) 749-2220, Fax: (613) 749-7170 ......,-...-.™——-...--...---......................-

Bondar CleggInphcape Testing Services

CertificateofAnalysis

REPORT: T96-57179.0 ( COMPLETE )

DATE PRINTED: 33-APR-96

PROJECT: NONE PAGE 3

SAMPLE

NUMBER

ELEMENT Au30

UNITS PPB

A9

PPM

As

PPM

37710 Duplicate

37727

Duplicate

0.2 2.7

0.3 2.9

12 0.1 1.5 1.1

37733 Duplicate

Bondar-Clegg Si Company Ltd.5420 Canotek Road, Ottawa, Ontario, KIJ 9G2, Canada

Tel: (613) 749-2220, Fax: (613) 749-7170 Lab Supervisor

Bondar CleggServices


HONETA PORCUPINE MINES INC

HR. RAINIER SKERIES

P.O. BOX 1756

TIMMINSONTARIO P4N 7W9

Bondar-Clegg A Company Ltd.5420 Canotek Road, Ottawa, Ontario, KU 9G2, Canada

Tel: (613) 749-2220, Fax: (613) 749-7170 Lab Siqjerviaor

Certificates- Bondar Clegg of

•TT _____ *——J ^——-^ A 1 "

^ Inchcape Testing Services Analysis

REPORT: T96-57207.0 ( COMPLETE ) REFERENCE: - .1

CLIENT: MONETA PORCUPINE MINES INC SUBMITTED BY: R.S. PROJECT: NONE DATE PRINTED: 3-MAY-96

NUMBER OF LOWER ORDER ELEMENT ANALYSES DETECTION LIMIT EXTRACTION METHOD ;

1 Au30 Gold 64 5 PPB Fire Assay of 30g 30g Fire Assay - AA :2 Ag Silver 64 0.1 PPM HCL:HN03 (3:1) ATOMIC ABSORPTION i

3 As Arsenic 64 1.0 PPM HCL:HN03 (3:1) HYDR. GEN/AA :

SAMPLE TYPES NUMBER SIZE FRACTIONS 'NUMBER SAMPLE PREPARATIONS NUMBER

ZZZZV.VDRlLlVi'bREZ^PULVERIZATION 64 \

REPORT COPIES TO: MR. RAINIER SKERIES INVOICE TO: MR. RAINIER SKERIESTO FAX:705-267-7490 ;

Bondar-Clegg & Company Ltd.5420 Canotek Road. Ottawa, Ontario, KU 9G2, Canada

Tel: (613) 749-2220, Fax: (613) 749-7170 Lab Supervisor

^^ Bondar Clegg^^ Inchcape Testing Services


DATE PRINTED: 3-HAY-96 REPORT: T96-57207.0 ( COMPLETE J PROJECT: NONE PAGE 2

STANDARD ELEMENT Au30 Ag As STANDARD ELEMENT Au30 Ag AsNAME UNITS PPB PPM PPM NAME UNITS PPB PPM PPM

1990 AU STD-2 265Number of Analyses 1Mean Value 264.6Standard Deviation -Accepted Value 260

BCC GEOCHEM STD 3 - 6.2 306.7Number of Analyses - 1 1Mean Value - 6.24 306.73Standard Deviation -Accepted Value - 5.8 310.0

ANALYTICAL BLANK ^ -:0.1 <1.0ANALYTICAL BLANK - -eO.1 <1.0Number of Analyses 1 2 2Mean Value 2.5 0.05 0.50Standard Deviation - -eO.OOI <0.001

Accepted Value 5 0.1 -:0.1

AFTON TAILS AU STD 78

Number of Analyses 1Mean Value 78.0Standard Deviation -Accepted Value 70

BCC GEOCHEM STD 2 - 40.7 8.2Number of Analyses -11Mean Value - 40.67 8.23 Standard DeviationAccepted Value - 34.0

Bondar-Clegg St. Company Ltd.5420 Canotek Road, Ottawa, Ontario. KIJ 9G2, Canada

Tel: (513) 749-2220, Fax: (613) 749-7170 Lib Supervisor

CertificateBondar Clegg ofInchcape Testing Services Analysis

DATE PRINTED: 3-MAY-96 REPORT: T96-57207.0 C COMPLETE ) PROJECT: NONE PAGE 1

SAMPLE ELEMENT Au30 Ag As SAMPLE ELEMENT Au30 Ag As NUMBER UNITS PPB PPM PPM NUMBER UNITS PPB PPM PPM

37660 160 0.5 1.437738 ^ 0.2 *:1.037739 *5 O.1 3.037740 ^ 0.2 1.537741 ^ 0.3 2.1

37742 ^ 0.1 3.037743 ^ O.1 ^.037744 8 0.2 2.337745 6 0.2 2.637746 ^ 0.2 4.0

37747 7 0.2 1.437748 ^ 0.2 1.537749 ^ 0.2 1.837750 ^ 0.2 *:1.037751 74 0.2 1.9

P

(3 oS

-o Ov

LilI I a

5 -o c~

15s

Bondar CleggCertificate of

~3^r Inchcape Testing Services Analysis

REPORT: T96-57207.0 C COMPLETE )

SAMPLE ELEMENT NUMBER UNITS

Au30 PPB

AgPPM

As PPM

DATE PRINTED: 3-MAY-96 PROJECT: NONE PAGE 3

SAMPLE ELEMENT Au30 Ag As

NUMBER UNITS PPB PPM PPM

37740 Prep Duplicate

37744 Duplicate

^

87

0.2

0.2 0.1

1.5 1.3

2.32.4

Ministry of.Northern Development and Mines

Ontario

Report of Work Conducted After Recording Claim

Mining Act

Transaction Number

Personal Information collected on this form Is obtained under the authority of the Mining Act. This Information will be used for correspondence. Questions abo this collection should be directed to the Provincial Manager, Mining Lands, Ministry of Northern Development and Mines, Fourth Floor, 159 Cedar Strec Sudbury. Ontario, P3E 6A5. telephone (705) 670-7264. ^ -\ f **J f^ r*2. l b? ^ iInstructions: - Please type or print and submit in duplicate. "^

- Refer to the Mining Act and Regulations for Recorder.

- A separate copy of this form must be comp- Technical reports and maps must accompa- A sketch, showing the claims the work is ai 32D12SW0047 2.16794 GARRISON 900

cllen' No-Recorded HoWer(s)

Telephone No.Address .w r: M r/, z,, fit.***M or d Plan No.Mining Division Township/Area .

C -Dates Work Performed

From:s

: f id \J rM-t*L '',

To:

Work Performed (Check One Work Group Only)Work Group

X Geotechnical Survey

Physical Work, Including Drilling

Rehabilitation

Other Authorized Work

Assays

Assignment from Reserve

Type

yfc^.We* U&MttifM. bkC*#**.f '

Total Assessment Work Claimed on the Attached Statement of Costs S

iRECElVFU

uCT 9 - 199G

/MiNgflfrlvANDS BRANCH

Note: 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

., 7#t*S*s, ^ 7^2

/CO

-t————l.T

(attach a schedule if necessary)

Certification of Beneficial Interest * See Note No. 1 on reverse side

1 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.

Date f

^ 'i, nRecorded Holder or Agent (Signature)

/9^^^Certification of Work Report

1 certify that 1 have a personal knowledge of Its completion and annexed report Is true.

Name and Address of Person Certifying

Telepone No. Date

the facts set forth In this Work report, having performed the work or witnessed same during and/or after

/of fi/'np 5J. C. fldjt /75(* T'Wtu wS i d&T' PfyfJlipl

Uj. IQ ) /99CCertified By (Signature) , .

For Office Use Onlytalue Cr. Recorded ///i^ piping Recorder

yyovi.B.yy W, ///faNotice tor Amrfndmertts SAnyAndrnerits Sent

Date Approved

Received Stamp

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Claim Number (see Note 2)

co la HO:

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Credits you are claiming In this report may be cut back. In order to minimize the adverse effects of such deletions, please Indicate from V which claims you wish to priorize the deletion of credits. Please mark (s) one of the following: *\

1. D Credits are to be cut back starting with the claim listed last, working backwards. f\ 'S2. D Credits are to be cut back equally over all claims contained In this report of work. \r ^3. CD Credits are to be cut back as priorized on the attached appendix. V P

In the event that you have not specified your choice of priority, option one will be implemented.

lote 1: Examples of beneficial Interest are unrecorded transfers, option agreements, memorandum of agreements, etc., with respect to the mining claims.

*ote 2: If work has been performed on patented or leased land, please complete the following:——————.———————*—-—,—————————————___rt——..—— - --7

..-......--j l Sionalure l fi—f ~~~-~ - in,i-l certllv thnl Iho rororrlorl hnlHwr hart a

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Credits you are claiming In this report may be cut back. In order to minimize the adverse effects of such deletions, please Indicate from which claims you wish to priorlze the deletion of credits. Please mark (^) one of the following:1. D Credits are to be cut back starting with the claim listed last, working backwards.2. D Credits are to be cut back equally over all claims contained in this report of work.J. D Credits are to be cut back as prlorlzed on the attached appendix.f JET" VaAj^m— AtL--e-w^—In the evenTtnat you have not specified your choice of priority, option one will be Implemented.

ile 1: Examples of beneficial Interest are unrecorded transfers, option agreements, memorandum of agreements, etc., with respect to the mining claims.

ile 2: If work has been performed on patented or leased land, please complete the following:

certilv thai the recordort holdor hnd a honnflrlni i,,io, n^i i~ .t.~ ,,-.~...~~. ISIanalura P~V-T^^

D Ontario Ministry ofNorthern Developmentand Mines

Statement of Costs for Assessment Credit

transection Number (oJilcf UM)

sonal Information collected on (hit lorm Is oblalned under the authority ol subsection 6(1) of the Assessment Wort Regulation 9/99. Under 1ton 8 of Ihe Mining Ad. the Intoimallon Is a public record. This Information will be used to review the assessment work and correspond with mining land holder. Questions about this collection should be directed lo Ihe Chief Mining Recorder. Ministry of Northern Development and

ie*. 6th Floor, 933 Ramsay Lake Road. Sudbury. Ontario. P3E 6B5.

Work Type

^ uJfSu* .(J

^IXfc /fa*4*tto*)J-Jf

Units of WorkDepending on Ihe type of work, list the number ol hours/days worked, metres of drilling, kilo metres of grid line, number of samples, etc.

"*? f *""5 J

V3 fa*.

? - - -

soclated Costs (e.g. supplies, mobilization and demobilization).

Transportation Costs

RFood and Lodging Costs

MIN

Cost Per Unit

' XSO/fr. * A9s

So/tut + Kfrtf.

2- ~Zd f ctmf.f r

2t l fi**" A o i

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Total Value of Assessment Work

Total Cost

^oscA-Vb - 7 d f3^0+600-- LtO Lt(

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ilculatlons of Filing Discounts:

Work filed within two years of performance Is claimed at 1000̂ of the above Total Value of Assessment Work. If work Is filed after two years and up to five years after performance, it can only be claimed at 50^ of the Total Value of Assessment Work. If this situation applies to your claims, use the calculation below:TOTAL VALUE OF ASSESSMENT WORK x 0.50 - Total S value of worked claimed.

ote:Work older than 5 years Is not eligible tor credit. . A recorded holder may be required to verify expenditures claimed in this statement of costs within 45 days of a quest for verification and/or correction/clarification. If verilicalion and/or correction/clarification is not made, the

Mnister may reject all or part of the assessment work submitted. —-—.———

edification verifying costs:

f?Q,Ve,r Skene s________________ , do hereby certify, that the amounts shown are as accurate as may(please print full name)

easonably be determined and the costs were incurred while conducting assessment work on the lands indicated on

19 accompanying Declaration of Work form asr

o make this certification.

, —— ̂(recorded holder, agent, or Hals company pojilion wtlh signing aulhority)

l am authorized

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O -J-J) o -Si JgS81*1

o^ 5 I ga?'

Credits you are claiming In this report may be cut back. In order to minimize the adverse effects of such deletions, please Indicate from which claims you wish to priorlze the deletion of credits. Please mark (^) one of the following:

1. D Credits are to be cut back starting with the claim listed last, working backwards.2. O Credits are to be cut back equally over all claims contained In this report of work.

3. D Credits are to be cut back as prlorlzed on the attached appendix.

In the event that you have not specified your choice of priority, option one will be Implemented.

[Note 1: Examples of beneficial Interest are unrecorded transfers, option agreements, memorandum of agreements, etc., with respei to the mining claims.

4ote 2: If work has been performed on patented or leased land, please complete the following:

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Credits you are claiming in this report may be cut back. In order to minimize the adverse effects of such deletions, please Indicate from which claims you wish to prlorlze the deletion of credits. Please mark (^) one of the following:

^. D Credits are to be cut back starting with the claim listed last, working backwards.

2. D Credits are lo be cut back equally over all claims contained In this report of work.

3. D Credits are to be cut back as priorlzed on the attached appendix.

In the everihfliKyouJiavenms^dned your choice of priority, option one will be Implemented.

ate l: Examples of beneficial Interest are unrecorded transfers, option agreements, memorandum of agreements, etc., with respect to the mining claims.

ote 2: If work has been performed on patented or leased land, please complete the following:

Ministry ofNorthern Developmentand Mines

October 22, 1996

Roy SpoonerMining Recorder4 Government Road EastKirkland Lake, ONP2N 1A2

Ministere du Developpement du Nord et des Mines Ontario

Geoscience Assessment Office 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5

Telephone: Fax:

(705) (705)

670-5853 670-5863

Dear Sir or Madam: Submission Number: 2.16794

Subject: Transaction Number(s): W9680.00399

After reviewing the Work Report(s) we have prepared this letter and the attached summary, which lists the results of our review. Requirements of the Assessment Work Regulation may not have been fully met. Please examine the summary to determine the next course of action concerning the identified Work Report(s).

NOTE: The 90 day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, is no longer in effect for this submission.

PLEASE NOTE ANY REQUESTED REVISIONS MUST BE SUBMITTED IN DUPLICATE.

If the anniversary dates for the mining claims affected by this correspondence have not passed, a number of options are available. Please contact the Mining Recorder to discuss these options.

If you have any questions regarding this correspondence, please contact Steve Beneteau at (705)670-5855.

Yours sincerely,

C (Z 42

ORIGINAL SIGNED BYRon C. GashinskiSenior Manager, Mining Lands SectionMines and Minerals Division

Correspondence ID: 10294

Copy for: Assessment Library

Work Report Assessment Results

Submission Number: 2.16794

Date Correspondence Sent: October 22, 1996 Assessor: Steve Beneteau

Transaction Number

First Claim Number

W9680.00399 L.26075

Section:

14 Geophysical MAG

Township(s) l Area(s)

GARRISON

Status

Approval

Approval Date

October 21, 1996

Correspondence to:

Mining Recorder Kirkland Lake, ON

Resident Geologist Kirkland Lake, ON

Assessment Files Library Sudbury, ON

Recorded Holder(s) and/or Agent(s):

MONETA PORCUPINE MINES INC. TIMMINS, Ontario

Page: l

Correspondence ID: 10294

cor rv i CD01

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MAY 17, 1995

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^^-r^ \ ' -- .-rC 0^ \ THE INFORMATKD \)l^X \ APPEARS ON Th

jAt \ HAS BEEN CO I* V1^ \ FROM VARIOUS S

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rtpnV^VeCV^ ' WISHING TO STA Vt^rtOSfB^ - 'NG CLAIMS SHOU

v rajt^ SULT WITH THE *tt\^ - RECORDER, MINIS

NORTHERN BE MENT AND MINES, DITiGNAL INFOR ON THE STATUS LANDS SHOWN HE

IC.VNSHIP ^* 1 Q 1^ Q A

GARRISONM N R AOMIN^SlTiATIVE DISTRICT

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1300 NORTH

1200 NORTH

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1000 NORTH

900 NORTH

800 NORTH

700 NORTH

600 NORTH

500 NORTH

400 NORTH

300 NORTH

200 NORTH

100 NORTH

BflSE LINE

100 SOUTH

200 SOUTH

300 SOUTH

400 SOUTH

500 SOUTH

600 SOUTH

700 SOUTH

TL 800 SOUTH

900 SOUTH

1000 SOUTH

1100 SOUTH

1200

1300 SOUTH

1400 SOUTH

l 500 SOUTH

TL 1600 SOUTH

LEGEND

INSTRUMENT: EDA OMNI PROTON PRECESSION MAGNETOMETER

PARAMETERS MEASURED: EARTH'S TOTAL MAGNETIC FIELD (NANO-TESLAS)

READING INTERVAL: 10 n

CONTOUR INTERVAL: 50 NANO TESLAS

DIURNAL CORRECTION METHOD: RECORDING OMNI BASE STATION

DATUM SUBTRACTED FROM ALL PLOTTED READINGS: 57000 nT

PEAK MAGNETIC HIGH: *

PEAK MAGNETIC LOW: *

TOPO LEGEND

D

CIolm Li ne

Clotm Post Lacoted

Claim Past. Assumed

Highwoy

P F C F ' V F

MINING LANDS BRANCH

. 16794

GAR32D12SW0047 2 16794 GARRISON 210

200 i ae se IBB 2BB

C l lent: MONETA PORCUP NE M NES NC

Property: GARR SON PROPERTYTitli

TOTAL FIELD

MAGNETOMETER SURVEY^ l^o'vxW

Processed:RJM

Date:JULY 1996

ProvinceONT.

Scale:l:5.000

Checked:RJM

Tawnship: ____QARR l SON

N.T.S. :42A/NE

Draw ing:R339MAG

RAYANEXPLORATION LTD.CONTRACT/CONSULTlsD GeOPHYSCS

TIMMINS. ONTARIO

(7051-268-4866

geophys rpt on the garrison property located in garrison … · 32d12sw0047 2 16794 garrison 010...

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