malamute prop assessment submission 1999 prog · 2017-01-17 · ecei ved feb o 7 2001 a.m. p.m....

ECEI VED

FEB O 7 2001A.M. P.M.

MALAMUTE PROPERTY

Tannahill and Dokis Township

Eric Marion/Alain Carrueau

NTS 32D/5

48 0 24'N 790 38'E

Prepared by: Eric Marion

L/ S00\

32D05NE2019 2.20896 DOKIS 010

Index

Property Location................................................................................................5Access.................................................................................................................5Claims................................................................................................................^General Geology.................................................................................................5,10Work Done.......................................................................................................... 10Site "G"...............................................................................................................10Site'-H"........,,...............,.,..,........,.......................................................................10Magnetometer Survey.........................................................................................13DDH-99-1...........................................................................................................13DDH-99-2...........................................................................................................13Conclusions........................................................................................................ 17Assay Sheets Appended

FiguresFig-1 Location Map............................................... lFig-2 Claim Map....................................................2Fig-2A Claim Map-Tannahill Twp.........................3Fig-2B Claim Map-Dokis Twp...............................4Fig-3 General Geology..........................................6Fig-4 General Geology..........................................7Fig-5 Blake River Area...........................................8Fig-6 Claim Area Geology And Reference Map....9Fig-7 Site "G".......................................................l lFig-8 Site "H".......................................................12Fig-9 Drill Hole Location Map.............................14Fig-10 DDH-99-1..................................................15Fig-11 DDH-99-2..................................................16

Section B- Magnetometer Survey

Section C- Drill Hole Logs DDH-99-1 and DDH-99-2

32D05NE2019 2.20896 DOKIS 010C

KIRKLAND LAKE RESIDENT GEOLOGIST'S'S DISTRIC'

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1213861LARDER LAKE

. MIHINO DIVISION

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NORTHERN DEVELOPMENT' AND MINES

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REFERENCES

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Property Location

This property is located in the Larder Lake Mining Division and is in the Kirkland Lake Resident Geologist District. It covers the east central part of Tannahill Township and the west central part of Dokis Township and can be found on NTS 32D/5 with the geographic center being at approximately 48 0 24'N and 79 0 38'E.

Access

To get to this property, one would drive east from Kirkland Lake for 13km on Highway 66 then turn north on Highway 672 (Esker Park Road). Driving north for 30km will bring you to a reasonably well maintained logging road heading east. (Rosko Road #39). Following this for 6 172km will take you to Rosko Road #46 which continues easterly, following this for 4 172km will take you to the western boundary of the property. The road continues through the property. Previously extreme limited access (helicopter) and rugged terrain discouraged prospecting and most of the property is virgin ground.

Claims

This property is comprised of 14 contiguous unpatented mining claims being 1220022, 1220023, 1220024, 1220025, 1225450,1225451, 1225892, L1213920,1225872,1225871, L1221835, L1221837, L1221838 and L1221839. They are recorded on plain M-342 Dokis and plan G-3717 Tannahill. They are held by Eric Marion K22502 and Main Carreau K22280. As the Internet maps are difficult to read. I have enclosed an older (1998) map as well as the Internet maps.(REF. Figure 2)

Deposit Type and Geology

This property lies in the Blake River group of the Abitibi Greenstone Belt. To the north about 10km is the Porcupine-Destor Deformation zone- a prolific source of gold in the region, to the south approximately 7km are what are believed to be two volcanic vental areas which may be the source of some of the Blake River Rocks. Mafic intrusives are present throughout the area and ryolitic rocks, though more extensive and abundant in the vental areas, are also present through the area. To the west of the property in Tannahill Township there is a syenite intrusive which is possibly associated with a gold showing. There are many strike faults in the area trending north east which may be splays of the Porcupine-Destor Fault. The Murdock Creek Fault- a splay of the Larder-Cadillac Fault passes through the south east corner of Dokis Township. Several north east trending fault are present on the property. The rocks are also folded in a series of anticlines and synclines which tend to define or reflect the domal areas to the south.

The property itself is mainly pillowed and flow calc-alkaline basalts. Some mafic intrusives are present as well as a diabase dike on claim L1213920 in Dokis Township. A shear zone cuts across the property in a north east direction up through Webster Lake, as well as associated cross faults. The southern portion of the claims cover the northern bounds of a lens shaped area of volcanic-pyroclastic sedimentary rocks which is approximately 10km long and

LS. JENSEN

' i*1 ^*^****i

LEGEND

Lo

ProterozoicKeeweenawan diabase (not shown)

12 Cobalt Group Archean

Matachewan diabase (not shown) Granitic rock!

11 Granodiorite, monzonite, quartz monzonite,syenite

10 Massive to gneissic quartz diorite, tonalite,trondhjemite

Upper Supergroup9 9a* Timiskaming Group, 9b" Destor-

Porcupine Complex8 8a, Sn, Blake River Group, 8c*" Blake

River (Upper Fm., Tisdale Group)

•a refers to Kirkland Lake Area, south limb of synclinorium (Jensen"b refers to Kirkland Lake Area, north limb of synclinorium (Jensen*"c refers to Timmins Area (Pyke, 1980)."" (Goodwin. 1965).

7 7a, 7b, Kinojevis Group, 7c Kinojevis Group,(Middle Fm., Tisdale Group)

6 6a Larder Lake Group, 6b StoughtonRoquemaure Group, 6c Lower Fm., TisdaleGroup

5 5c Porcupine Group tnr Supergroups 4 4a Skead Group, 4b Hunter Mine Group, 4c

Upper Fm., Deloro Group 3 3a Catharine Group, 3c Middle Fm., Deloro

Group 2 2a Wabewawa Group, 2c Lower Fm. Deloro

Group 1 la Pacaud tuffs""

1978c, 1979). 1976, 1978b). FIGURE 3

A MUTE ERTY

Geological map of the Timmins-Kirkland Lake area showing the distribution of volcanic successions.

CENTRAL FAULT BLOCK

:::::::::::

ANCMCAN OxMtow MriHMm

Oonoaiixil*. MMUow* (M O Tool* (M CZ3 Ouitli ambta iM Olorll.

EH PorcuoM Oraw nM

S3 SmM MM Humtr UM Ornip* Anttalkw ——— FIIM Zone

-*- StrillgiiDMc ToolHwiM Otow

'•cand ridli

. Geological map of the Kirkland Lake-Noranda area. C J -

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LEGEND

Syncline

Anticline

Fault

Location

BLAKE RIVER GROUP

Intrusive Assemblage

Qtz diorite

Gabbro, qtz gabbn and diorite

Layered Assemblage

. '///l Sedimentary rocks'

Dacite and rhyolite

Basalt and andesite

Iron-rich tholeiitic basalt

oo Map of Blake River Group in the Magusi River map-area.

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3km wide and goes through Tannahill and Dokis Townships above the previously mentioned domal areas. It is believed that this unit is unique.

Work Done/Results

During the past season two sites were stripped trenched and sampled, some grid was cut and old grid lines refreshed, a magnetometer survey was done on 6km of grid and two drill holed totaling 1207' were done unfortunately the west grid area was not worked. This year as the program was cut short in November due to health reasons.

Site "G" reef ra T)

Stripping and trenching were done at this site and samples were blasted out. The outcrop here was previously mapped by L. S. Jensen as pillowed andesite. The work was done in order to study what appeared to be silicious mildly altered rock. As stripping was done, a north- south trending QZ-calcite vein cutting across the pillows was encountered. There were wall rock inclusions in the vein and some appear bleached. The vein was mineralized with some chalcopyrite and malachite. Out in the wall rock to the west approximately l meter from the vein were areas within the pillows with pinkish discoloration which, by the results of the Do-12 sample, are most likely the result of elevated potassium.

Recommendations

The elevated copper in the sample taken here,(Ref DO-11) is not significant enough to warrant further work here. Perhaps geophysics done in a tight area around this outcrop may indicate an area of higher mineral concentration.

Site "H" (Ref Fig-8)

Stripping and trenching was done here to test mineral potential in a bleached looking andesite. No interesting mineralization was encountered here and a sample was done for comparative geochemical analysis only.

RecommendationsNo further work recommended here.

10

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Magnetometer Survey (Ref section B Mag survey)A mag survey was done on 6km of grid in the region of highest probability of the

location of the 1988 OGS hole. Several magnetic trends were encountered. Finally, after 3 work programs, a geophysical response cam be correlated with the OGS road which may indicated the alteration present in the OGS hole. A mag low on line 24E at 215-249S over to line 25E at 2 10- 246S crosses the OGS road in an area of organic overburden cover this fits well with the drill logs of the OGS hole. A magnetic break on line 21E-485S, Line 22E-437S, Line 23E-387S and L400S-234E seems to correlate well with a heavy chloritic alteration present in DDH-99-1 possibly associated with hydrothermal activity along a fault present in this hole (Ref Fig 9)

RecommendationsIt is highly recommended that a hole be drilled at 24+35E - 1+50S to test this magnetic

anomoly. A 175m hole at a -50 0 dip at azimuth 180 0 would cross this target area, and confirm the existence and extent of the alteration present in the OGS hole.

DDH-99-1

This hole was drilled to test the cause of an IP response present in this area. After logging and observation of the core, it was determined that the cause was most likely pyrite and pyrolite concentrations in brecciated andesites. (Ref drill log DDH-99-01 200' to 460') four of eight samples from this section showed elevated zinc with one sample being anomolous. (Ref- assay sheets) Faulting increases towards the base of this unit and below in the next lithology a pervasive chloritic alteration extends down to 500' and shows elevated nickel. (Ref sample DO- 99-01). Fluctuating sodium, barium and potassium levels in the whole rock analysis of sections in this hole (Ref 99-01-99-04), would tend to indicate hydrothermal activity in this area.

Recommendations

More geochemical and geological investigation is required here to determine the potential of this alteration and mineralization, and to possibly locate economic concentrations of mineral in this hydrothermal system.

PDH-99-2

This hole was drilled to test the cause of a magnetic low present on line 21+OOE between 3 23S. To 3 55S.. The rock unit which appears to correlate with this response would be from 60 feet to 162 feet in the hole (Ref drill log) The cause of the low seems to be calcite and minor chlorite alteration in a massive andesite flow.

RecommendationsAs no structure or elevated values were encountered in this hole, no further work is recommended at this time.

13

DRILL HOLE LOCATION MAP

7: p

DDH 11 1 JD/Prso 0 l

AZI90 C-AST. 1(7)4- - — 50M - - -L

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Conclusions

This years program was a success in that we have finally located a target for the sericite- iron carbonate alteration present in an OGS hole, and several other magnetic anomolies have been mapped. The drill hole DDH-99-1 revealed chloritic alteration and metal enrichments which definitely enhance the base metal potential of this area, and seem to point to a hydrothermal system being present on this property. Because of these nickel and zinc enrichments, the base metal potential of this area should be considered to be above average. It is essential that more work be done on the Malamute Property to further define this exciting prospect.

17

Swastika LaboratoriesA Division of Assayers Corporation Ltd.

Established 1928 Assaying - Consulting - Representation

Geochemical Analysis Certificate 9W-1182-RG1Company: E. MARION Date: MA Y-19-99Project:Attn: E. Marion

We hereby certify the following Geochemical Analysis of l Rock sampled submitted M A Y-14-99 by .

Sample Au Mult i W*A Number PPB ElementDO-10 3 Results Results

to tofo 11 ow fo 11ow

One assay ton portion used.

Certified by

l Cameron Ave., P.O. Box 10, Swastika, Ontario POK l TO Telephone (705)642-3244 Fax (705)642-3300

E.MARIONAttention: E. MarionProject:Sample: Rock

Sample Number

DO-10

Ag Al As Ba Be Bi ppm Oh ppm ppm ppm ppm

TSL Assaj j Swastikal Cameron Ave., Swastika, Ontario, POK 1TO Tel: (705) 642-3244 Fax: (705) 642-3300

MULTI-ELEMENT ICP ANALYSISAqua Regia Digestion

Ca Cd Co Cr Cu 96 ppm ppm ppm ppm

Fe K Mg Mn Mo Na Ni P Pb Sb Se Sn Sr It 'fa Ik ppm ppm % ppm ppm ppm ppm ppm ppm ppm

Report NoDate

9W1182 RJMay-26-99

V W Y Zn Zr ppm ppm ppm ppm ppm

2.83 30 tO.S 1.79 31 658 67 3.98 0.14 1.92 540 6 0.07 104 300 10 47 0.31 99 55 16

A .5 gm sample is digested with 10 ml 3:1 HC1/HNO3 at 95c for 2 hours and diluted to 25ml with D.I.H20.

Page l of l Signed:

E. MARIONAttention: E. MarionProject:Sample: Rock

TSL Assayt Swastikal Cameron Ave., Swastika. Ontario, POK l TO Tel: (705) 642-3244 Fax: (705) 642-3300

ICP Whole Rock AssayLithium Metaborate Fusion

Report No Date

9W1182 RLMay-26-99

(Sample jNumber

ioo-io

Si02

53.88

AI203"k

17.88

Fe203 CaO •X. MgO Na 20 TiO2 K2O MnO P205 LOI

7.45 9.30 3.47 2.20 0.81 0.99 0.10 0.08 3.39

Ba ppm

240

Sr ppm

350

Zr ppm

Se ppm

Yppm

15

Be ppm

Co ppm

Gr ppm

95

Cu ppm

10

Ni ppm

10

V ppm

185

Zn ppm

Rb Nb ppm

Total

10 99.66

Sample is fused with Lithium Metaborate and dissolved in dilute HNO3

Page 1 of 1 Signed



Geochemical Analysis Certificate 9W-1531-RG1Company: E. MARION Date: JUN-22-99Project:Attn: E. Marion

We hereby certify the following Geochemical Analysis of 2 Grab samples submitted JUN-14-99 by .

Sample Au Au Check Mil t i \\RA Number PPB PPB ElementDO- 11 ~~~~~~~9~~~~~~~~~7~"fesuIts"~ResuIts~~"~~"~

DO-12 3 to tofo 11ow fo 11ow


Certified by


E. MARIONAttention: E. Marion

Project:Sample: Grab

TSL Assjiyt Svvsistiksil Cameron A\ c . Swastika. Onlario. POK ITO

Tel: (705) 642-3244 Fax: (705) 642-3300

MULTI-ELEMENT ICP ANALYSISAqua Rcgia Digestion

Report IN o

Dale

9W15JI R,l

Jun-29-99

Sample Number

DO-11 DO-12

Ag ppm

<0.2 •cO.2

Al As Ba Be Bi "56 ppm ppm ppm ppm

0.911.06

10

10

•eO.5•;0.5

<5

Gay,

0.431.55

16 M

:ram

774509

Cu ppm

3149

Fe

1.501.29

K •X,

0.010.02

Mg •X,

1.31MS

Mn ppm

215180

Mo ppm

64

Na •X,

0.020.06

Ni P Pb Sb Se Sn Sr ppm ppm ppm ppm ppm ppm ppm

5963

200400

105

•clO•-10

733

Ti •X.

0.130.17

V W Y Zn Zr ppm ppm ppm ppm ppm

6175 -1U

10 -1

A .5 gm sample is digested with 10 ml 3:1 HCI/HNO3 at 95c for 2 hours and diluted to 25;n! with ID l 020

:. MARION.Uciition: E. Marion

roject:

ample: Grab

ample lumber

KD-12

l SI- Assaye. .SwsistiksiCameron Avc.. Swastika. Ontario. I'OK l TO

Tel: (705) 642-3244 Fax: (705) 642-3300


Report No

Dale

•JW1531 KL

Si02 AI203 Fe203 CaO MgO Na 2O Ti02 K2O MnO P2O5 LOI Ba Sr Zr Se Y Be Co Cr Cu Ni V Zn "it ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm

Rb Nb ppm

Total "fa

57.43 16.14 3.52 6.76 4.25 6.49 0.81 1.39 0.04 0.10 2.40 460 400 90 15 20 15 500 95 70 230 <5 20 99.SI

Sample is fused witli Lithium Metaborate and dissolved ir, dilute HNO3



Geochemical Analysis Certificate 9W-3015-RG1Company: E. MARION Date: OCT-18-99Project:Attn: E. Marion

We hereby certify the following Geochemical Analysis of 4 Core samples submitted OCT-10-99 by .

Sample Au Milti \\RA Number PPB ElementCO-99-01 3 Results ResultsDO-99-02 7 to toDO-99-03 Nil follow followDO-99-04 Nil

Certified by

l Cameron Ave., P.O. Box 10, Swastika, Ontario POK l TOTelej?hpjLe.CZ05164^-3244^ Fax (705)642-3300

E.MARIONAttention: E. MarionProject:Sample: Core

TSL Assaj Swastikal Cameron Ave., Swastika, Ontario, POK ITO Tel: (705) 642-3244 Fax: (705) 642-3300

ICP Whole Rock Assay Lithium Metaborate Fusion

Report NoDate

9W3015 RLOct-29-99

: Sample ^Number

i DO-99-01 -fl-DO-99-02 Hao-DO-99-03 2'T -DO-99-04 1 '.a -

5iOj A12O3 FejOj"fa 'b Ik

41.0947.8752.3453.45

10.7115.6016.2816.54

13.879.448.427.79

CaO MgO Na2O TiO2 Ik Ik '!k Ik

4.70 20.89 0.06 0.687.59 5.75 l 0.74 0.87

11.65 4.20 ^0.49^ 1.228.32 4.65 2.74 1.51

K2Oft

0.012.890.401.36

MnO PjO, LOI BaZ* Ik *fc ppm

0.170.130.130.13

0.10 7.330.13 8.790.15 4.300.19 2.61

10370

50340

Sr ppm

105040

270

Zr Se Y He Co Cr Cu Ni V Zn Rb ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm Ik

709090

110

10151515

10151520

S555

70 112530 19030 22535 85

25757040

805756065

105150190210

110 0.01225 0.03345 0.01555 0.03

Nb Total ppm 96

•:10 99.85. -:10 99.96^0 99.70•clO 99.50

f-PY-po-

Sample is fused with Lithium Metaborate and dissolved in dilute HNO3.

Page l of l Signed:


TSL Assa. 5 Swastikal Cameron Ave., Swastika, Ontario, POK 1TO Tel: (705) 642-3244 Fax: (705) 642-3300


Report NoDate

9W3015 RJOct-29-99

Sample Number

DO-99-01 DO-99-02 DO-99-03 DO-99-04

Ag Al As Ba Be Bi Ca Cd Co Cr Cu Fe ppm ft ppm ppm ppm ppm ft ppni ppm ppm ppm ft

^.2 4.940.2 3.32

-:0.2 3.74•eO.2 2.45

^^^^

10 <0.520 <0.510 *:0.520 *:0.5

<5 0.40^ 4.72<5 2.26^ 1.30

1<l<l•el

65 96230 12629 15626 57

36 7.2264 6.2557 5.6253 3.67

K Mgft ft

"CO.Ol 9.090.14 3.280.06 2.470.11 1.89

Mn

805905735510

Mo Na Ni )pm ft ppm

^ 0.01^ 0.01

2 0.01^ 0.09

878906859

P Pb Sb Se Sn Sr Ti V ppm ppm ppm ppm ppm ppm ft ppm

400480520610

•c21242

1555

•cS

1 *:104 -clO6 ^02 -clO

7 0.0732 0.13

8 0.3623 0.33

6964

12588

W Y Zn Zrppm ppm ppm ppm ppm

•clO

•elO

6 944 845 1035 104

6121617


Page l of l Signed

. 'V.



Geochemical Analysis Certificate 9W-3133-RG1Company: E. MARION Date: OCT-27-99Project:Attn: E. Marion


Sample Au Au Check Mil t iNumber PPB PPB ElementDO-99-05 --------------------~------------------------

DO-99-06 3 - toDO-99-07 5 - followDO-99-08 19 22DO-99-09 15


Certified by-



TSL Assay Swastikal Cameron Ave., Swastika, Ontario, POK 1TO Tel: (705) 642-3244 Fax: (705) 642-3300


Report NoDate

9W3133 RJOct-29-99

Sample Number

DO-99-05 DO-99-06 DO-99-07 DO-99-08 DO-99-09

Ag Al Asppm ft ppm

10.2 3.94 150.2 4.70 15

10.2 2.78 150.4 2.51 15

Ba Be Bippm ppm ppm

40 10.5 1540 10.5 1520 10.5 1520 10.5 15

Ca*

2.822.17

12.438.36

Cd Coppm ppm

11 371 351 221 21

Cr Cuppm ppm

232 81171 55171 45129 56

Fe K•Sk Ik

5.98 0.148.03 0.174.72 0.125.37 0.15

Mg Mn Mo% ppm ppm

4.45 945 124.45 955 22.75 885 12l. 94 830 2

Na Ni Ptfa ppm Ppm

0.02 174 460O.Ol H9 640O.Ol 86 300O.Ol 62 500

I'b Sbppm ppm

6 530 5

6 528 5

Se Sn Srppm Ppm ppm

7 110 215 110 95 110 474 110 41

Ti V WIb ppm ppm

0.32 109 1100.12 90 1100.16 63 1100.11 52 110

Y Zn Zrppm ppm ppm

5 70 IS4 207 95 49 85 128 11

0.6 4.22 10 10 10.5 2.85 •ei 70 66 75 9.81 0.01 2.69 750 0.01 127 720 28 8 ilO 0.40 138 110 82 29


ge l of l Signed:

Swastika Laboratories LtdEstablished 1928 Assaying - Consulting - Representation

Geochemical Analysis Certificate OW-0673-RG1Company: E. MARION Date: MAR-08-00Project:Attn: E. Marion

We hereby certify the following Geochemical Analysis of 5 Core samples submitted MAR-03-00 by .

Sample Au Au check Mil t i \\RA Number PPB PPB ElementDO-99-ii "Nil ~~~~"~~""itesults~~~Results~~~~~~~~~"~~~~~~

DO-99-12 Nil - to toDO-99-13 Nil - follow followDO-99-14 NilDO-99-15 Nil 2


Certified by

l Cameron Ave., P.O. Box 10, Swastika, Ontario POK l TO Telephone (705) 642-3244 Fax (705) 642-3300

E. MARIONAttention: E. MarionProject:Sample: Core

Swastika LaL atories Ltd.l Cameron Ave., Swastika, Ontario, POK 1TO Tel: (705) 642-3244 Fax: (705) 642-3300


Report NoDate

OW0673 RJMar- 16-00

Sample Number

DO-99-11 DO-99-12 DO-99-13 DO-99-14 DO-99-15

Ag Al As Ba Be Bi ppm 96 ppm ppm ppm ppm

Ca Cd Co Cr Cu ^ ppm ppm ppm ppm

Fe K Mg Mn Mo ppm ppm

0.2 1.690.2 0.430.2 2.210.2 2.920.2 2.55

5 •eS

30 •elO

40 40 20

0.5 0.5 0.5 0.5 0.5

•e 5•cS

•eS

2.4511.003.513.042.72

•el445

444027

11234112515883

841791

10687

5.501.846.596.174.54

0.150.020.200.180.10

1.090.261.532.401.95

820470865825585

Na Ni P Pb Sb Se Sn Sr 'fa ppm ppm ppm ppm ppm ppm ppm

Ti V W Y Zn Zr 96 ppm ppm ppm ppm ppm

•e 2

0.040.010.030.090.12

22331

25818958

32040

640520200

801814168

55555

51585

^0•elO

^0^0•:10

8 0.2041 0.0112 0.2421 0.2419 0.13

699

7013689

^0•elO•clO

clO•elO

3•:1

654

8218

1229247

143

181411


Page l of l Signed:

E. MARIONAttention: E. MarionProject:Sample: Core

Swastika Lab. atories Ltd.l Cameron Ave., Swastika, Ontario, POK 1TO Tel: (705) 642-3244 Fax: (705) 642-3300


Report No : OW0673 RLDate : Mar-16-00

Sample Number

DO-99-15

Si02 A1203 CaO MgO Na2O TiO2 K2O MnO P2O, LOI Ba Sr Zr Se Y Be Co Cr Cu Ni V Zn Ve "fa fa 1& Ik 'fc Ve fc ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm

Rb Nb Total9o ppm 9f

40.73 18.39 12.23 11.11 8.37 2.80 0.76 0.71 0.20 0.09 3.53 220 150 60 30 10 40 250 90 105 210 60 .eO.Ol 10 99.08


Page l of l Signed^



Geochemical Analysis Certificate 9W-3015-RG2Company: E. MARION Date: OCT-18-99 Project:Attn: E. Marion

We hereby certify the following Geochemical Analysis of l Core samples submitted OCT-10-99 by .

Sample Pt Pd Number PPB PPB


Certified by




Geochemical Analysis Certificate 9W-3284-RG1Company: E. MARION Date: NOV-04-99 Project:Attn: E. Marion


Sample Au Au Check Mil t i W*A Number PPB PPB ElementEO-992-6I 2~ """"""i" "Results """Results"

DO-992-02 Nil - to toDO-992-03 2 Nil follow followDO-992-04 Nil

One assay ton portion used for gold.

Certified by


j E. MARIONi Attention: E. Marion j Project: 'Sample: Core

Sample Number

DO-992-01 DO-992-02 DO-992-03 00-992-04

TSL Assay Swastikal Cameron Ave., Swastika, Ontario, POK 1TO Tel: (705) 642-3244 Fax: (705) 642-3300


Report No Date

9W3284 RJNov-17-99

Ag Al As Ba Be Bi Ca Cd Co Cr Cu Fe K Mg Mn Mo Na ppm Ik ppm ppm ppm ppm % ppm ppm ppm ppm 'X* Ik 'K ppm ppm It

0.6 4.23-CO. 2 3.93•cO.2 4.49•^0.2 3.74

^^^^

10 tO.S40 <0.510 <0.510 ^.5

^ 3.67 <^ 4.33 <<5 2.88 <<5 1.63 <

1 401 451 391 32

179170153110

66 5.37 0.01 4.21 100090 5.15 0.12 2.31 93568 5.72 0.01 4.57 94073 4.39 0.01 3.77 495

^ 0.03c2 0.03e 2 0.05e2 0.03

Ni P Pb Sb Se ppm ppm ppm ppm ppm

190150187175

340 ^370 ^340 ^310 ^

^ 2^ 9^ 3^ 2

Sn Sr Ti V W Y Zn Zr ppm ppm 96 ppm ppm ppm ppm ppm

•clO•elO-clO•clO

34 0.248 0.38

27 0.2226 0.17

118 tlO158 ":10120 ^069 *:10

26.22

60595844

10171010


Page l of l Signed:


TSL Assay j Swastikal Cameron Ave., Swastika, Ontario, POK ITO Tel: (705) 642-3244 Fax: (705) 642-3300

ICP Whole Rock Assay Lithium Metaborate Fusion

Report NoDate

9W3284 RLNov-17-99

Sample Number

DO-992-01 DO-992-02 DO-992-03 DO-992-04

SiO2 A12O3 FejO,K, "X, Ik

CaO MgO Na2O TiO2 K2O MnO P2OjTP /P TP nl nf TP TP

LOI Ba Sr Zr Se Y Be 9( ppm ppm ppm ppm ppm ppm

49.0050.0748.5050.29

16.4019.7517.9317.13

8.176.638.448.23

10.987.129.11

10.66

6.243.527.026.89

1.303.821.931.65

0.670.830.740.72

0.081.630.090.02

0.150.120.140.11

0.08 6.650.06 5.810.08 5.820.08 3.65

306004030

340150260280

60706060

15202020

l t5555

Co )pm

35403535

Cr Cu ppm ppm

200215185190

15251010

Ni V Zn Rb Nb ppm ppm ppm *fa ppm

ISO120170150

165210185175

70 -:0.0175 tO.Ol70 <0 1 0155 •tO.Ol

•ao101010

Total'X,

99.8499.5299.9099.53


Page l of l Signed:

Swastika Laboratories LtdEstablished 1928 Assaying - Consulting - Representation

Geochemical Analysis Certificate OW-0663-RG1Company: E. MARION Date: MAR-06-00Project:Attn: E. Marion

We hereby certify the following Geochemical Analysis of l Core samples submitted MAR-05-00 by .

Sample Au Au Check Mil t i \\RA Number PPB PPB ElementDO-992-05 bffl - ftf 50 45 Results Results

&-.-FF A 1~- OT tO tOf O l l OW f O l l OW


Certified by

l Cameron Ave., P.O. Box 10, Swastika, Ontario POK l TO Telephone (705) 642-3244 Fax (705) 642-3300

i E. MARIONl Attention: E. Marion'Project:l Sample: Core

Swastika Lab atories Ltd.l Cameron Ave., Swastika, Ontario, POK 1TO Tel: (705) 642-3244 Fax: (705) 642-3300


Report NoDate

OW0663 RJMar- 16-00

i Sample ' Number

DO-992-05

Ag Al As Ba Be Bi Ca Cd Co Cr Cuppm ^ ppm ppm ppm ppm 5fc ppm ppm ppm ppm

•;0.2 2.77 ^ 10 -cO.5 ^ 3.97 <•i

Fe K Mg Mn Mo ppm ppm

Na Ni P Pb Sb Se Sn Sr ^ ppm ppm ppm ppm ppm ppm ppm

Ti W Zn Zr% ppm ppm ppm ppm ppm

33 167 120 3.90 0.01 1.68 675 0.03 139 270 96 -;10 20 0.13 83 ^0 55 10


Page l of l Signed:


Swastika Lab atories Ltd.l Cameron Ave., Swastika, Ontario, POK 1TO

Tel: (705) 642-3244 Fax: (705) 642-3300


Report No Date

: OW0663 RL: Mar-16-00

Sample Number

DO-992-05

Si02 AI 203 CaO MgO Na20 TiO2 K2O MnO P2OS LOI Baft ppm

47.41 18.90 6.94 14.67 2.91 1.99 0.72 0.05 0.12 0.08 5.73 60

Sr ppm

270

Zr Se Y Be Co Cr Cu Ni V Zn ppm ppm ppm ppm ppm ppm ppm ppm ppm ppm

Rb Nb ppm

Total

70 15 30 225 95 125 150 50 70 99.65


Page l of l Signed:

REPORT

ON

MAGNETIC TOTAL FIELD SURVEY(October 1999)

Malamute Property

Dokis Township Larder Lake Mining Division

North-eastern Ontario

NTS 32D

UTM Grid Zone 17, NAD. 27

For

Eric Marion

Douglas Robinson P. Eng. Doug Robinson Consulting

TABLE OF CONTENTS

l.O SUMMARY................................. . . . . . . . . . . . . . . . l

2.O LOCATION AND ACCESS.................................... l

3.O PHYSIOGRAPHY AND VEGETATION............................ l

4.O REGIONAL AND PROPERTY GEOLOGY.......................... 2

5.O EXPLORATION RATIONAL................................... 2Magnetic Survey........................................ 2

6.O EXPLORATION PROGRAM.................................... 2Grid................................ . .. . . . . . . . . . . . . . . . . 2Magnetic Survey........................................ 3

7.O DISCUSSION OF RESULTS.................................. 4Magnetic Survey.................................... . .. . 4Magnetic Survey........................................ 5

8.O Recommendations . . . . . . . . . . . . . . . . . . 6

9.O REFERENCES.............................. . . . . . . . . . . . . . . . 7

CERTIFICATE OF QUALIFICATIONS . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 8

LIST OF TABLES 6c FIGURES

Location Map: (After Ministry of Natural Resources)

Magnetic Total Field Profiles: Scale 1:5000Line 2100E 0+OON-600SLine 2200E 0+OON-600SLine 2300E 0+OON-600SLine 2400E 0+OON-600SLine 2500E 0+OON-600SLine 2600E 0+OON-600SLine OOON 2100E-2600ELine 200S 2100E-2600ELine 400S 2100E-2600ELine 600S 2100E-2600E

Base Station Values along 000 Base Line

Contoured Total Magnetic Field Strength Map: Scale 1:2500

Compilation Map: Scale 1:2500

l.O SUMMARY

This exploration project of the Malamute Property north east of Kirkland Lake, Ontario; consisted of magnetic

total field strength magnetic survey to supplement IP surveys and mapping by Eric Marion. The author conducted this magnetic survey and prepared this report.

2.0 LOCATION AND ACCESS

The property is located at 5362254 mN and 0603204 mE (NTS 30/D5, approximately 16 km east of Highway 672.

The property is accessed via Highway 672 leading 31.5 km north from Highway 66. Turn east onto the J. Roscoe Road 39 (uncorrected 0586389 mE, 5359000 mN) . Proceed 5.5 km and turn right. Proceed an additional 11.2 km to the junction with road #79 (to the right). Continue (3.2 km total distance) straight ahead avoiding road #79 crossing over the Magusi River bridge and taking the first right turn and proceed to the end of the road and

park (0602256 mE, 5363474 mN) . Take the trail to the

left (former OGS access road) to the property.

3.0 PHYSIOGRAPHY AND VEGETATION

The property is flat with a few rare high relief outcrops. Clay and glacial deposits with swampy areas

comprise the survey area except for a high outcrop at approximately 450S on lines 2500E and 2600E. Boreal forest provides the main forest cover.

Doug Robinson Consulting

4.0 REGIONAL AND PROPERTY GEOLOGY

The property is located in calc-alkalic massive and pilled flows, tuffs, lapilli tuffs, and pyroclastic breccias of calc-alkalic volcanics consisting of

intermediate (to felsic) Blake River group.

See OGS map P.3398.

5.0 EXPLORATION RATIONAL

This magnetic survey was conducted to assist interpretation and tracing of bedrock geology under the overburden and to aid in the identification of collar

location of an OGS overburden hole that intersected

bedrock sericite carbonate alteration (44 meters).

6.0 EXPLORATION PROGRAM

The magnetic survey was plotted on 1:5000 scale profiles at 50 nanoTeslas per cm vertical scale. The magnetic data is also supplied in a 1:2500 scale contour map. A

1:2500 scale compilation map is also provided.

The location of an access OGS access road used as access

in an overburden survey program was traced onto the compilation map. The OGS hole was collared in humus overburden. The area of humus overburden is shown as a darkened road symbol. The location of the road and humus overburden was provided by Eric Marion.

Grid

The survey was conducted on a metric grid consisting of100 spaced lines with pickets spaced at 25 meter


intervals. The grid lines are oriented approximately

165-345 degrees azimuth.

Line 2100S at 215S is located at uncorrected UTM co ordinates 0603204 mE, 5362254 mN.

Magnetic Survey

The author of this report conducted a total field strength magnetic survey of the property September 30,

1999. A Scintrex Envimag in walkmag mode was used. Total field strength Magnetic readings were measured at 2 second intervals along lines 2100-2600E and lines DOON, 200S 400S and 600S. This 2 second interval rendered readings spaced at approximately two-meter intervals.

Base stations were established along the Base Line 0+OON at the intersection of each grid line (at 100 meter

intervals). Each base reading was established standing on the east side of the picket while facing north. See appendices for base station values.

The survey traverses were interrupted at the base line

to measure the base stations. All base stations were quiet and all base station readings were within 8 nT of established base station values. The survey values were corrected.

Interpretation was performed from 1:5000 profiles. A 1:2500 contour plan is provided to supplement the profiles.


7.0 DISCUSSION OF RESULTS

Magnetic Survey

The grid has a low relief magnetic signature. The outcrop area at approximately 450S on lines 2500E and 2600E have spiky data due to close proximity to outcrop.

Short ^5m) magnetic fabric is generally masked by deep

overburden. Intermediate length magnetic fabric is most evident on profiles. The broad magnetic responses ^25 meters) are most evident on the contour maps.

The broad magnetic trend appears to be roughly grid east-west direction. This is interrupted by a magnetic high along line 2400E south of 400S.

Eric Marion indicates strong sericitic alteration was

intersected in an OGS overburden hole drilled through humus overburden along the access road between 2350E and 2475E. This is roughly coincident with a magnetic

low at 2400E-215-249S -^ 2500E-210-246S . Line 2400E

has the strongest magnetic low signiture; however the

location of the road indicates the OGS hole was drilled between lines 2400E and 2500E. This magnetic low is

located north of the magnetic high on line 2400E (south of 400S) . This magnetic high and magnetic low may be related to a common alteration/structural system.

The following magnetic breaks may exist at 064 degreesdegree azimuth:

. Lines 2100E-485S -^ 2200E-437S -^ 2300E-387S -^ 400S-


2340E (-^ S possibly 2400E-321-351S -^ 2500E-278-295E

2600E-225S)

* Lines 2100E-134S -^ 2200E-036S

. Lines 2400E-035S -* OOON-2440E

* Lines 600S-305E -* 2400E-574S -^ 2500E-555S -^ 2600E-

532S (possably 2100E-323S ans 2200E-255S also)

An additional magnetic break may exist at grid azimuth

142 degrees at 2100E-123S -^ 2200E-255S -^ 2300E-387S.

Magnetic breaks may indicate:

natural or fault contacts between rocks of dissimilar magnetic character

sharp vertical subcrop drops in areas of moderate to strong vertical magnetic gradient (caused by underlying magnetic rocks)

edges of alteration defined by replacement of magnetic minerals (non magnetic replacement minerals may include

sericite, iron-magnesium carbonates, albite and silicification minerals).

A distinct magnetic low a 2100E-323-335S appears to be a distinct contrast to the property fabric.

IP responses (Remy Belanger 1997 survey) at 2100E-450S and 2500E-575S have weak and neutral magnetic responses respectively. These would be caused by magnetically neutral rocks or alteration.

Diamond Drilling

Diamond drilling was in progress at 350S-2060E when the magnetic survey was in progress.


5

8. O RECOMMENDATIONS

The magnetic breaks represent possible structural targets for gold mineralization. The break at 2100E- 485Smay have been intersected in the hole that was in

progress during the magnetic survey. The author

observed strong alteration within the core drilled. This break should be identified in the core. The magnetic data indicates the geological formations and/or alteration in this hole could logically strike at grid azimuth 064 or 093 degrees. This alteration

could be related to either gold or base metal

mineralization.

The pronounced magnetic low at 2100E-323-335 south is an exploration target for alteration. It is unknown if this negative magnetic signature is caused by

alteration or rocks having reversed magnetic polarity.

This location of the OGS access road and the

information from the OGS overburden drilling program

should be confirmed in the field and related to this magnetic survey report. A hole should be drilled to

confirm the existence, location and extent of alteration intersected by the OGS hole. A 175 meter diamond drill hole azimuth 180 degrees, dip 50 degrees collared at 2435E-150S would test this zone.


9.O REFERENCES

Jensen, L.S.1978: Thackeray, Elicit, Tannhill, and Dokis Townships, District of Cochrane. Ontario Geological Survey Report 165.

Map 2367 Tannahill and Dokis Townships, Scal3 1:31,680.

MERQ-OGS, 1983. Lithostratigraphic Map of the Abitibi

Subprovince;Ontario Geological Survey/Ministere de 1'Energie et des

Ressources, Quebec; scale 1:500,000.

Map 2543. Bedrock Geology of Ontario East-central Sheet. Ministry of Northern Development and Mines

Scale 1:1,000,000


CERTIFICATE OF QUALIFICATIONS

I, Douglas Robinson, of 24 Victoria Avenue, Swastika, Ontario hereby certify that:

1. I am a registered professional Engineer of the province of Ontario, No. 39322011.

2. I am a graduate of Queen's University in Kingston Ontario with an Honours Bachelor of Science, Geological Engineering 1975, andNorthern College, School of Mines in Haileybury, Ontario, 1970.

3.

4 .

I have been practising graduation.

my profession since

The information contained in this report is the result of work done by myself and the references cited.

5. I own no direct or indirect interests in and do not expect to receive any interests in the Malamute Property.

Respectfully submitted "^ -

Douglas Robinson, P. October 01, 1999


Malamute Property: Dokis Tp. Line 2100E

57500 -i — —— —— —————————————————

m 574*50*V \J f *TWW

to 0)i— *i74nn•^ O f Hww

C CD cTocrtc 57350 -

57300 - ———————————————————————————————————— — -

r\N/ V\ ^vr"

A^A 7

V

^^^,"X ,s^

t^r^ ^^-^

-600 -500 -400 -300 -200 -100 0

Northing


57500 n —— — —— ——————

jj 57450 - w5 57400o(0C C7Ocno/ JoU -

57300 - ——————————————————————————————————————

^^\

^X r-~^W

\ t"W

fs^-^f^^^^

V^^,^^-x

-600 -500 -400 -300 -200 -100 0Northing

(O

H

(O

57500

57450

57400

57350

57300


-600 -500 -400 -300 -200

Northing-100

Maiamute Property: Dokis Tp. Line 2400E

cycnnvj t \J\J\J

18 57450 -w5 57400 -ocRtc 57?50^ v f OwW

57300- -— T-

/^\I ^"Vj' ^v ^^-^——Vv^^-—— ̂ —x ^

vx-xx^-^-Vy

x^ ~V"V"~Wvwv^

————^

-600 -500 -400 -300 -200 -100 0

Northing


gj 57450 -W5 57400 -oc(0c "5775O H*" O t O*J\J

57300 -

M

^/Jy1|-

f

*-\V" \ S^^~~~\ r-J-

\ f]1 ^\f ^^^Y

-600 -500 -400 -300 -200

Northing-100


57500 —————— — — — - - — — -

m 57450(y \J 1 ^TvJW . /\ . -

r̂\\

\ ^'^

.l ~ \r~

^SW

^WW-^,^(O 0)

oc(Oc

57400

57300-600 -500 -400 -300 -200

Northing-100

Malamute Property: Dokis Tp. Line DOON

57500 -i ——————————————————————————————————

52 *5745n(0 Or *rOU

ToP 57400 -c re c 57T50 -Of OOw

57300 - —————————— — ——

r — "^'••'v-\-^~~~J ^ •v^X^Avv~'

yw^^y-V^-V^^^

^-v^w^^-^~' 1 — x~^~ -

^^"^^v

2100 2200 2300 2400 2500 2600 2700

Easting

Malamute Property: Dokis Tp. Line 200S

KTcnn .,O t \J\J\J

w ^74^0 -(0 Of fOU

To0i— *s74nnQ Of *TWW

C (0C S7^*50 -O f OOU

57300 —— —— -- ̂ - —— — — — —— —— ^

^—^^ ~^^~^-^^ ————~^. JlXx^

2100 2200 2300 2400 2500 2600 2700

Easting


57500 ————————— —— —— —

w ^7/mn(Q Of tOU"w0)

1— *i74nO -A O 1 *TWVJ

C (0 C 57^0 -O f OOw

57300 n .-r- — ^ —— —————————————————————

y^^Y\ -S^ fi ^

C^Svv^

2100 2200 2300 2400 2500 2600 2700

Easting

w0)

o(O

57450

57400

57350

57300


2100 2200 2300 2400

Easting2500 2600 2700

Base Station Values along OOON Base Line2100E 57404

2200E 57413

2300E 574192400E 574412500E 57432

2600E 57417


2100E 2200E 2300E 2400E 2500E 2600E

2100E 2200E 2300E 2400E 2500E 2600E

(mctera)

Contour Interval: S nT

Malamute Property, Dokis Twp GridMagnetic Total Field Strength

nanoTeslasSCINTREX ENVIUAP plot by Doualas Robinson. Doua Robinson Consulting Ovdiflation: 12 0*ir*n

2100E 2200E 2300E 2400E 2500E 2600E

2100E 2200E 2300E 2400E 2500E 2600E

Contour Interval: 10 nT

Malamute Property, Dokis Twp GridMagnetic Total Field Strength

nanoTeslas

SCINTREX ENVIMAP plot by Douglas Robinson, Douq Robinson ConsultingDeclination: 12 Oqren West

s x2100E 2200E 2300E 2400E * 2500E 2600E

o

Ko o

8eg

V

l

V

iu

i/Oot

1 , ———————————————————————————————————— , ———————————————————————————————————— , ———————————————————————————————————— r

-j.............. i i , 1 .

-

t.

-

— i— -"

-

L

r

.

r

L

. r

J- .-T-...........................................T..................^.......................r ......................................f.

L.

s'/

"1 134

\

* P

t

\

\ ^

-^ \V

X- -,\

x? H——— ̂ ——————————————— -,

1 ~~~

\^J — --^--^

335

-

L^"x^

^-1.^

485 "~ ~~ - —r

*1 565

Jt

""ose

-

0^ ^f** "^~" *"^"— a. — ̂

/?x

"? 255

s.p—— ̂ S ——— --t!

p _ ̂'?~ — "~"

. \

\CM \ T \L L

: "^-^S-

T ~ — ~- —437 ~ ~~ —

e———r- ——-r

^--"

X

S

035 i

-f f -h -

(O :

* i=== ^ -"*^H- 4

^^ i 215 -, — L

— -

^^^ iJ-- -^i^, '~

-*^ '

h 3io -\- ^ — — s .1 -s

^/^frx

•o . .- w

^n 446 S."- 3

U

E

^ — :—

578T ~ ~~ ~ ~ ~^~

? 1. ^.......................................^.......................................-t^................ i......-............-

S ?/

21 COE 22

' —— t —— Magnet!

x- ^ ' i1 32! ;1 x" ^

in U

7 171 —— *J

^ rIS: * 7il 7i /' Cii — h Hi

i ,/ T9 Ji/ 1 9 ^- L

(MID

4

^^ /?.

278 ? ^ ^

1 /'' 4

7 *™/' .

387"'g 372

m IT'•••••••••••••••••••••••••••••-•-T40

•**

n

J

b

458

475 ^ ~- ~ ~ ~ *-

-

530^

^ ^ 9 ~~~

555 '

i *mm* i i

J

m O —" S S

o

o3

o

1

jf

i

l/l8CO

0

CO

OOE 2300E 2400E 2500E 2600E

c High

qi

— i i - Magneth; Low

— J — Magnetic Break '

25 o 25 so Malamute Property, Dokis Twp Grid ^(nrwUrl)

SCINTREX ENV7MAP p/at by Douglas Robinson, Doug Robinson Consulting

;OKlination: 12 D*^r*M WMt

Property: MalamuteTownship: Dokis Tp.Claim: 1221835Northing (Lat): 349m SouthEasting (Long): 2050 m EastFrom (ft)

0.0

6.7

To (ft)

6.7

80.0

Hole Number: 99-01Azimuth: 180"Dip: -SO0Drilled by: Eric MarionDates Drilled: August 29-October 07, 1999

DescriptionAcid Tests: 100 -SO 0 , 300 -SO0 , 550 -50" , 700 -50".

CASING (Left in Hole)

ANDESITE FLOW

6.7-71.3

6.7-29.0

13.1-13.6

17.5-18.6

31.7

29.0-70.3

70.3-73.3

73.3-80.0

Uniform and massive, Fine grained light greenish grey.Moderately hard (-cnail) to hard (xiail).Below 45.0 hard ^nail).

Purpose: To establish base metal mineralizationCore Size: ^fc /^ " /^Core Stored: 126 Duncan Ave.Logged By: Douglas Robinson (Swastika, Ontario)Sampled by: Eric Marion (Kirkland Lake)Sample #

Weak to moderate calcite alteration with r/o Ga fracture fillingat 40-50", 600 .45". 5% calcite fracture filling to 1 mm.40". 5"M) calcite fracture filling to 2 mm.600 . 1 .0 cm calcite vein with irregular, tight walls.Uniform and massive, fine grained, light greenish grey.Hard (xiail). No Calcite alteration.1-2^, calcite fracture filling to 0.6 cm at 30", 800 8. 65".Alteration. Medium greenish grey with reddish tint.Moderately soft ^copper, ^nail).Fine grained, and slightly coarser grained than above.2Vo dark green chloritic fracture filling at 40" and 70".Minor white dolomite fracture filling sub-parallel chloriticfracture filling.Similar to 29.0-70.3.

From To Length PPBAu

Hole #99-01 1 of 11

From (tt)

80.0

134.5

To (ft)

134.5

176.2

Description

ANDESITE, Vesicular. Massive A Flow Textured.Aphanitic to very fine grained.Q-2% 1-4 mm Ca filled vesicles.Locally uniform and massive, light greenish grey withminor primary breccia.Possible pillow structures.^•ft calcite fracture filling at 0-10", 60", 4 25".From 90.0-94.0, 97.0-109.7, 114.5-124.4 mottled (blocky) appearance asyellow grey, medium green and pale gray.

94.0-97.0109.7-114.5

128.1-134.5

128.2-129.2

129.2-130.8

129.2-130.8

130.8-131.3

133.1-134.5

Uniform and massive with a few vesicles.Uniform and massive light greenish gray with a few vesicles.Weak alteration as bleaching.Aphanitic to very fine grained, pale gray.Calcite alteration along upper edge of bleaching

207o rusty specks to 3 mm oxidized since hole was drilled.200 . Four 0.1-0.3 cm quartz-calcite fracture filling with calcitein part weathered out.80". Calcite-quartz vein.25'ti opaque white calcite with dark green chlorite bands.750/0 transparent white translucent fine grained quartz-calcite.Vein banding sub-parallel vein walls.*\Vo fine grained disseminated pyrite in vein.Calcite Alteration.Calcite chlorite fracture filling to 133.1 .

Mixed DIKE and Vesicular ANDESITE.

Sample # From To Length PPBAu

Hole #99-01 2 of 11

From (tt)

176.2

189.0

To (ft)

189.0

374.1

DescriptionFlow textured andesite with up to 5Vo l mm calcite filled vesicles.Moderately hard O^nail), variable colour; pale gray to greenish gray.

134.5

135.0-135.2

135.5-139.7

155.9-161.7

.

161.7-176.2

45". 2.0 cm dike. Pale gray aphanitic chilled.Very hard ^nail, < file).40*. 4.0 cm dike similar to and parallel dike at 134.5.Dike similar to above.Contact at 135.5 40' parallel contacts above.Contact at 139.7 17".Dike similar to above.

Sample #

Contact at 155.9 sharp at 450 along 1 mm calcite fracture filling.Contact at 161 .7 sharp and irregular averaging 40".Dike.This dike cut by dike above.Uniform and massive, greenish gray vein hard (:-nail, < file).1-30A calcite fracture filling to 1 .5 cm at 20".Minor disseminated pyrite in calcite fracture filling.

ANDESITE, Vesicular and Flow Brecciated.Possibly flow breccia with fragments to 3.0 cm.Up to 40"fc 1-2 mm quartz filled vesicles in fragments.Moderately hard (-^nail), highly variable colour, pale gray fragments anddark greenish gray groundmass.

189.0 700 sharp contact. Unit below is chilled against this contact.

ANDESITE, Massive Vesicular Flow.Uniform and massive, aphanitic, pale gray.Moderately hard ^nail) to very hard (s-nail, ^ile).


Hole #99-01 3 of 11

From (ft) To (ft) DescriptionD-3% 3-5 mm quartz filled vesicles throughout.Two generations of quartz filling.Early transparent quartz filling andlate opaque weak quartz filling.Many vesicles have transparent edges with opaque centers.Both early and late quartz fillings are very hard ^file).Unit has many breccia-sulfide zones with white opaque and transparent

Sample #

to translucent quartz and large (to 3.0 cm) fine grained pyrite^/- pyrrhotite)masses cementing angular breccia fragments to 2.0 cm.Transparent to translucent quartz rims the breccia and opaque quartzfills the centers of the breccia voids.Pyrite occurs as fine grained masses to 1 .5 cm thick within the quartz filling.The quartz breccia zones are typically bounded by closely spaced palegray quartz fracture fillings.

189.5189.0-192.7

191.8

192.0

192.7

194.8

194.0-196.7

195.8-196.6

203.9-207.0

208.0-211.3

213.0-217.0

65". 2.0 cm 750Xo massive pyrite, 25"Xo gray calcite.Fine parallel quartz fracture fillings 30-50".75". 1 .5 cm fine grained white calcite fracture filling.80". 4.0 cm quartz-calcite vein.0.5X2.0 cm patch of pyrite.90". 1 .5X4.0 cm pyrite mass crosses core.Fine parallel quartz fracture fillings 65".20". Pyrite masses to 1 .0X3.0 cm.70". Fine quartz fracture filling set withbreccia zone from 205.3-205.9 (150Xo pyrite).Fine quartz fracture filling set at 400 and random orientationwith breccia from 210.0-211.3 (1007o pyrite).Fine quartz fracture filling set at 50" and random.


Hole #99-01 4 of 11

From (ft) To (ft) Description

231 .6-235.2

231.6-235.2

284.6-286.3

291.0-299.8

306.8-309.3

314.0-316.0

319.0-330.4

329.6-330.0

345.7-349.0

360.0-360.9i

363.8-364.0

365.2-365.8

374.1-374.4

Also widely spaced set at 06".Also with breccia from 213.0-215.8 (5"7o pyrite).Fine quartz fracture filling set at 40" withbreccia from 231.6-232.0 (10"}*) pyrite).Fine quartz fracture filling set at 75" withbreccia from 236.6-237.2 (W& pyrite) andbreccia from 237.6-238.6 (50A pyrite).Weakly developed breccia with 50Xo pyrite.30". Fine quartz fracture filling withbreccia from 292.0-295.2 (5-1 OVo pyrite-pyrrhotite) magetic.breccia from 297.0-298.1 (S1?*) pyrite-pyrrhotite) magetic.40". Fine quartz fracture filling withbreccia with 5-1 QVo mixed pyrite-pyrrhotite andProminent opaque white quartz.45". Fine quartz fracture filling.Minor breccia and pyrite masses to 0.5 cm.Fine quartz fracture filling.Fine quartz fracture filling withminor breccia at 332.0-332.3Minor fine quartz fracture filling.Clean geochemical sample.

Sample #

DO-99-09

D99-04

From

306.8

360

To

308.7

360.95

Length

1.9

0.95

PPBAu

15

nilSiO2 53.45, AI2O3 16.54, Fe2O3 7.79, CaO 8.32, MgO 4.65, Na2O, 2.74 K2O 1.36, LOI 2.61, Total 99.50.

507o pyrite in quartz fracture filling.Weakly developed breccia zone.Mixed zone (breccia?). 200Xo pyrite-pyrrhotite, magnetic.Tuff breccia?

Hole #99-01 5 of 11

From (ft)374.1

416.3

To (ft)

416.3

460.2

DescriptionANDESITE, Vesicular Tuff Breccia.374.1-387.4

387.4-416.3

379.1-380.0

384.4-421.3

395.0-411.0

Pale gray aphanitic, moderately hard ^nail) to hard ^nail).Fine tuff to 0.5X2.0 cm vesicular fragments.Flow breccia with 0.3-15.0 cm rounded pale gray aphaniticvesicular fragments in medium geenish groundmass.Has appearance of pillows.Moderately hard ^nail) to hard ^nail).Clean tuff geochemical sample.

Sample #

DO-99-03

From

379.1

To

380

Length

0.9

PPBAu

NilSiO2 52.34, AI2O3 16.28, Fe2O3 8.32, CaO 1 1 .65, MgO 4.20, Na2O, 0.49 K2O 0.40, LOI 4.30, Total 99.70.

0.5-1 "/o Patches pyrrhotite and pyrite to 0.5-1 .0 cm.In part associated with random weak opaque quartz fracturefilling. Magnetic (pyrrhotite dominant).Minor calcite fracture filling.

ANDESITE, Massive Flow.

Uniform and massive, very fine grained, light greenish gray.Moderately soft (-^nail) to soft ^copper coin). Above 418.9 moderately soft (^nail)Vesicles generally absent except as noted.426.0-437.5

418.9-460.2

418.9-419.7

2"7o 2-5 mm quartz filled vesicles and 507o 1 mm quartz filled vesicles.Foliation break intensity increasing down the hole.420 80", 425 75", 428 85", 441 45", 445 45", 451 55", 455 40".

S 1?*) irregular calcite-quartz veining to 0.5 cm in partsub-parallel foliation break.Locally minor disseminated pyrite in wall rock.1-2"fc 1 mm dark green chloritic fracture filling sub-parallelfoliation break.8.0 cm quartz-calcite vein, fine grained white with trace DO-99-08 418.9 419.7 0.8 19

Hole #99-01 6 of 11

From (ft)

460.2

To (ft)

546.8

Description

420.2-425.0

430.3-430.6

431.5-432.0

441 .3-442.5

442.5-444.4

453.6

456.4

pyrite cubes.Moderately soft (^nail).

Sample #

DO-99-02

From

420.2

To

425

Length

4.8

PPBAu

7

SJO2 41 .87, AI2O3 15.60, Fe2O3 9.44, CaO 7.59, MgO 5.75, Na2O, 0.74 K2O 2.89, LOI 8.79, Total 99.96.

421.0 30". 0.5 cm pyrite band.424.0 60". 3.0 cm quartz vein, very fine grained white.Fault gouge cored in natural position at ~85".3.0 cm pale gray mud gouge.6.0 white gouge and flaky chips to 0.5 cm.SO 0 . 10.0 cm chloritic banded calcite-quartz vein with1 07o disseminated pyrite.Schistose at low angle to core axis.Pale gray soft ^copper coin) with 5Vo calcite veining.At 442.5 500 2.0 cm quartz vein.Schistose, pale gray to dark green soft.100Xo quartz-calcite veining.30". 1.0-3.0 cm m coarse calcite-quartz vein.350 . 6.0 cm calcite-quartz vein with swirled ghost of chlorite.Strongly gouged walls and irregular fracture in vein.

BASALT, Flow

DO-99-07

DO-99-05

DO-99-06

Uniform and massive, and soft with relict medium grained crystalline textureoverprinted by pervasive chloritic alteration.Dark green soft ^ to > copper coin).Degree of shearing and alteration decrease down the hole.Shearing focused from 441 .0-466.7 andalteration focused from 419.0-470.4.

460.2 Contact not defined.

431.5

441.3

442.5

432

442.5

444.4

0.5

1.2

1.9

5

12

3

Hole #99-01 7 of 11

From (ft) To (ft) Description

462.6-463.9

460.8-461 .6

461.6-461.8

462.5-462.7

462.7-463.0

463.6-463.9

464.4-464.5

464.5-464.6

466.0-466.5

466.4-466.5

466.5-469.5

469.5-470.3

471.0-472.0

485.2

487.6

Shear zone.

40"7o calcite-quartz veining with 20"Xo thin chloritic wall rock

fragments floating parallel vein walls.~80". 4.0 cm fault with 1 .5 cm fault gouge.

800 . 5.0 cm calcite-quartz vein with 100Xo thin chlorite bands

parallel vein walls.

Fault gouge of very thin chloritic flakes. Core Angle?

1 .5 cm piece quartz vein at 25" floating in gouge.

6.5 cm calcite-quartz vein, banded white very fine grained.

Contorted chloritic bands in vein.

Strong slip within vein.

600 . Weakly healed fault with 2007o calcite-quartz.

80". Fault gouge.

70". Fault as strong slips spaced at 0.5-2.0 cm and

0.5 cm fine gouge at 466.4.

Calcite-quartz vein chloritic, banded, healing fault.

00-30". lO'fc calcite-quartz veining, chloritic.

28.0 cm quartz.

Coarse quartz with coarse calcite in quartz voids.

469.5-469.6 Fine grained shear banded chlorite-calcite at 90".

469.0 sheared vein wall 90".

470.3 frozen vein wall 55".

Clean geochemical sample of intense chlorite alteration.

Sample #

DO-99-01

From

471.0

To

472.0

Length

3.0

PPBAu

3

SiO2 41.09, AI2O3 10.71, Fe2O3 13.87, CaO 4.70, MgO 20.89, Na2O 0.06, K2O 0.01, LOI 7.33, Total 99.85.

Moderately soft (-^nail) uniform and massive break.

600 . 2.5 cm calcite-quartz vein.55". 2.5 cm calcite vein, fine grained, white.

Hole #99-01 8 of 11

From (ft)

546.8

To (ft)

556.5

DescriptionIntense Chlorite alteration to 495.0.495.0-500.0

500.0-534.0

525.2

526.3

526.6

534.0-546.8

546.5-546.8

526.6

546

546.8

Decrease in intensity of chloritic alteration marked bypreservation of primary crystalline texture.Soft ^copper coin). Dark green.Hardness increasing from soft ^copper coin) to.moderately hard ^nail).

Dark green.55". 7.0 cm calcite-quartz vein, coarse with chlorite bands.Strong slip walls.55". 1 .5 cm quartz vein, white with chlorite bands.550 . 2.5 cm chloritic quartz-calcite vein with strong chloriticslip walls.Well preserved primary 0.5 mm crystalline texture.Grain size decreases downwards to pale green aphanitic chillagainst unit below.Pale green aphanitic chill.

Sample #

55". 2.5 cm chloritic quartz-calcite vein with strong chloritic walls.55". 5.0 cm quartz vein with 3007o pale yellowish greenplaty (sericitic) wall rock fragments.60". Sharp lower contact with pale green aphanitic flowin contact with fine grained flow below.

ANDESITE, Flow

Uniform and massive, no vesicles, moderately hard (-snail),Light greenish gray, very fine grained from upper contact and decreasinggrain size down the hole towards lower contact.^Vo hairline pale greenish yellow fracture filling at variable angles,


Hole #99-01 9 of 11

From (ft)

556.5

562.0

To (ft)

562.0

586.6

Descriptioncommonly 60".

556.5548.3-549.0

548.0-554.0

60". Pale green aphanitic chill.

Sample #

350 . 14.0 cm quartz vein, coarse with 15"7o pale yellow epidote(epodote is mixed with calcite).Strong slip walls.00-35". Strong slips.

ANDESITE, Vesicular Flow.Light gray, Moderately hard ^nail), very fine grained to aphanitic.50Xo 1-2 mm quartz filled vesicles throughout.Lower contact frozen at 550 .

557.5

560.0-562.0

450 . 4.0 cm quartz vein with calcite-epidote ribs perpendicularvein walls.00". Strong slips.

ANDESITE, Vesicular Flow.

Light greenish gray, hard ^nail).562.0-565.0

562.0

562.0-585.0

585.0-586.4

586.4-586.6

586.6

571.1-571.4

Scattered quartz filled vesicles to 4 mm.Grades from aphanitic to fine grained.Fine grained crystalline, uniform and massive, vesicles absent.Grades to aphanitic below.*\ 0h 1 mm white quartz filled vesicles.Pale green aphanitic chill. Vesicles smaller than above.70". Contact sharp, frozen.550 . 9.0 cm calcite-axinite-quartz vein.2570 pale mauve axinite crystals to 1 .0 cm in coarse whitecalcite and quartz.


Hole #99-01 10 of 11

From (ft)

586.6

To (ft)

727.0

727.0

DescriptionSharp frozen walls.

ANDESITE Vesicular Breccia and Flow.Highly variable vesicle content. Bimodal distribution of vesicle size.D-7% 3-4 mm quartz filled vesides mixed with Q-10% 0.5-2 mm quartzfilled vesicles.Larger vesides tend to be filled by white quartz and smaller vesides bytransparent quartz.Moderately hard ^nail) to hard ^nail), medium greenish gray, aphanitic.586.6-645.0

645.0-727.0

670.5

670.9

691.8

715.0-715.7

715.7-716.3

716.3-727.0

Clearly defined rounded vesicular fragments to 10.0 cm.(Flow Textured?) andesite.

Sample #

Highly variable vesicle content (consistent over 1-3 foot sections).Possibly 1-3 foot fragments or thin flows.Medium greenish gray and aphanitic throughout.No internal flow contacts defined.Moderately hard (•cnail) to hard ^nail)40". 1 .5 cm quartz vein with calcite-epidote ribs.40". 0.5 cm quartz vein with calcite-epidote ribs.Possible flow contact 30".5Q7o 5 mm white quartz filled vesicles flattened 3:1^5:1 at 55".30". Tightly spaced pale green hairline fracture fillingcut by 3007o white quartz and epidote fracture filling.Trace disseminated pyrite in wall rock.Somewhat similar to quartz-breccia zones from 189.0-374.6.Flow texturing increased and vesicles content decreased.

END OF HOLE.

Dominant mineral of veins listed last in vein descriptions.


Hole #99-01 11 of 11

Property: MalamuteTownship: Dokis Tp.Claim: 1221835Northing (Lat): 372m SouthEasting (Long): 2095 m EastFrom (ft)

0.0

60.0

To (ft)

60.0

162.0

Hole Number: 99-02Azimuth: 3550Dip: -450Drilled by: Eric MarionDates Drilled: October 11-31, 1999

DescriptionAcid Tests: 100 -45", 300 -45", 450 -45".CASING (Left in hole)Cased boulders at 28.0 and 77.0

ANDESITE FLOW, MassiveUniform and massive, fine grained 0.1 mm crystalline, pale gray.No vesicles, no flow texturing.Moderately hard ^nail) to hard ^nail).Generally •cO.S'ft quartz-calcite fracture filling to 0.3 mm at 30-55".

60.0-70.0

121.2-121.8

130.4

130.5-130.8

131.6

Purpose: To test magnetic low.Core Size: flk ; '3.' - ^- '-JCore Stored: 126 Duncan Ave.Logged By: Douglas Robinson (Swastika, Ontario)Sampled by: Eric Marion (Kirkland Lake)Sample #

2-30Xo quartz-calcite fracture filling, fine grained white to 0.3 cm.Irregular 00-400 , 300 dominant.45". 8.0 cm quartz vein with sub-parallel walls.25^0 soft dark green chlorite patches and bands.Frozen walls.Weak wall rock alteration as less distinct crystalline texture.155". 0.5 cm quartz band with slip silicates, pale green.42". 0.3 cm chlorite filled gash fracture set, dark green.38". 4.3 cm calcite-quartz-clinozoisite(epidote) vein.9507o coarse white quartz.507o white clinozoisite, slender crystals.Minor chalcopyrite to 2 mm.Frozen walls.


Hole #99-02 1 of 8

From (ft)

162.0

171.6

To (ft)

171.6

196.2

Description132.0

140.0-140.6

145.4

151.5-152.8

162.0

135". 1 .5 cm quartz vein, pale green.40". 11.0 cm quartz vein,95*96 coarse white quartz,207o pale yellowish white clinozoisite as slender crystals.35'. 6.0 cm quartz vein similar to 121 .2.Composite set of gash fractures with65"7o white quartz, 20*36 wall rock inclusions,10*96 dark green chlorite masses, 50Xo pale gray clinozoisite00-1 00 . Opaque white quartz veining to 1 .5 cm.Lower (contact?) 25" along 0.5 cm green quartz slip vein.Dark green chloritic slip walls.No chill zone above or below contact.

ANDESITE FLOW, MassiveSimilar to 70. 0-162.0.Slight change in crystalline texture.Trace calcite-quartz fracture filling.

171.6 Lower contact sharp frozen at 62".No chill in flow above.

Sample #

Minor chlorite fracture filling perpendicular contact above contact.Prominent pale green chill in unit below.

ANDESITE FLOW, Massive171.6-172.6

172.6-180.0

180.0-196.2

Pale greenish gray aphanitic chill.Gradual coarsening of crystalline texture.Similar to 70.0-1 71 .6.Uniform and massive, fine grained 0.1 mm crystalline,


Hole #99-02 2 of 8

From (ft)

196.2

231.5

240.3

To (ft)

231.5

240.3

315.0

Description

187.8

196.2

hard ^nail < file).No vesicles, no flow texturing.30". 0.5 cm quartz slip vein, greenish.60". Lower contact(?) along 0.2 cm quartz stringer.

ANDESITE FLOW, MassiveSimilar to 70. 0-1 96.2.Uniform and massive, fine grained, pale gray,moderately hard (-snail) to hard ^nail).No vesicles, no flow texturing. Trace quartz-calcite fracture filling.

201.3

231.5

DIKE

Sample #

45". 5.0 calcite-quartz vein, coarse with minor very fine grainedpale green silicate. Minor pyrite to 3 mm.400 . Lower contact broken core.No chill above contact.

Similar to dike in hole 99-01 .231.5-233.0

233.0-240.0

240.0-240.3

240.3

Pale greenish gray aphanitic chill in broken ground.Very fine grained, uniform and massive, hard (sfile).Medium greenish gray.Pale green aphanitic chill.35". Sharp lower contact along 0.1 cm quartz seamUnit below not chilled.

ANDESITE FLOW, Massive

Similar to 70.0-231 .5.Uniform and massive, very fine grained crystalline (0.2 mm crystalline),


Hole #99-02 3 of 8

From (tt)

315.0

To (ft)

382.0

Descriptionpale gray. No vesicles. Noflowtexuring.Trace quartz-calcite fracture filling.249.0-258.0

249.0-252.0

252.0-258,0

252.4

254.8-255.0

291.0-293.0

Healed gash fracture set.30". 507o quartz-chlorite fracture filling to 0.3 cm.Dark green.5-1 OVo calcite-quartz-clinozoisfte gash fracture filling

Sample #

00-25". 1 .5 cm quartz filled gash fracture along 0.6 foot of core.50". 4.0 cm calcite-clinozoisite vein.70"Xo calcite with cleavages to 1 .0 cm,^5% clinozoisite, 15*^ wall rock.Typical of unit, minor quartz-calcite fracture filling. 992-04

From

291.0

To

293.0

Length

2.00

PPBAu

NilSiO2 50.29, AI2O3 17.13, Fe2O3 8.23, CaO 10.66, MgO 6.89, Na2O, 1.65 K2O 0.02, LOI 3.65, Total 99.53.

ANDESITE FLOW, Massive, VesicularUniform and massive, very fine grained crystalline, pale gray.O-D.5% vesicles, calcite filled, no flow texturing.Moderately hard O^nail).Trace quartz-calcite fracture filling.316.0-341.0

321.0-327.0

322.5

331.2

Calcite alteration, weak to moderate.Moderately soft ^penny, ^nail)Pale hairline fracture fillings.60". 6.0 cm fault vein.5007o fractured gray, fine grained quartz bands,4507o opaque grain reduced calcite,50Xo light green chlorite bands.3 strong slips with white powdery gouge.50". 4.0 cm quartz-calcite vein with pitted grainy appearance.

Hole #99-02 4 of 8

From (ft)

382.0

To (ft)

427.8

382.0-396.0

388.6-389.6

Description330.8-332.0

336.3

334.0-337.2

368.0-379.0

376.6-377.6

377.8-378.4

377.8-377.8

379.6-382.0

382.0

Calcite alteration, pervasive with thin calcite fracture filling.Soft ^copper coin).

Sample #

70". 3.0 cm quartz vein, banded with 2007o calcite-clinozoisite bands.Strong slip wall. Trace pyrite.Minor rusting that appears to post date drilling.Pervasive calcite alteration, soft ^copper coin) .1 0Xo calcite filled vesicles.Typical massive vesicler andesite flow. 992-03

From

376.6

To

377.6

Length

1.0

SiO2 48.50, AI2O3 17.93, Fe2O3 8.44, CaO 9.1 1 , MgO 7.02, Na2O, 1 .93 K2O 0.09 LOI 5.82, Total 99.90.

30". 100Xo chlorite-calcite veining withseveral parallel strong slips.

Calcite alteration, strong pervasive.Minor slips.507o opaque white calcite filled vesiclesand weak calcite alteration.Moderately soft (^nail) to moderately hard (/cnail).Gradational contact.

ANDESITE, Flow Textured, Vesicular, AlteredProminent flow texturing, aphanitic, very hard ^nail to ^le).Mottled appearance, pale green to light greenish gray.Prominent microfracturing, very hard ^file).2-50Xo quartz filled vesicles to 2 mm,Locally a few quartz filled vesicles to 4 mm.Calcite alteration, weak, moderately soft ^penny, -^nail) .Patchy hard ^nail) alteration and calcite alteration.50Xo calcite fracture filling.

992-02 388.6 389.6 1.0

PPBAu

2

Nil

Hole #99-02 5 of 8

From (tt)

427.8

TO (ft)

440.7

Description Sample # From To

SiO2 50.07, AI2O3 19.75, Fe203 6.63, CaO 7.12, MgO 3.52, Na2O, 3.82 K2O 1 .63 LOI 5.81, Total 99.52.

389.6

399.0-399.4

406.9-409.4

422.3-424.5

411.1-401.3

427.8

1 .0 cm calcite vein with 1 Q06 quartz, trace pyrite.Wall rock Moderately hard ^nail) to hard (xiail).25^0 vague white quartz patches.30-350 . lO'ft calcite-quartz fracture filling to 0.5 cm. Minor clinozoisite?Uniform and massive very fine grained section with no distinct contacts.Medium gray, moderately hard (-snail).15^0 opaque weak quartz patches.65". Lower contact sharp, frozen.

ANDESITE FLOW, VesicularChilled upper contact.Contact defined by hardness contrast and colour and vesicles in unit below..Unit above very hard ^file) and mottled.Unit below moderately hard (-snail) and uniform, medium greenish gray colour.427.8-430.5

430.5-439.0

438.0-439.0

439.0-440.7

5"7o 2-5 mm white quartz filled vesicles.Grades from almost aphanitic to very fine grained.Medium greenish gray, uniform and massive andmoderately hard ^nail).Fine grained crystalline with 0.5 mm feldspar in groundmass.Pale gray, uniform and massive.Typical massive flow. 992-01 438.0 439.0

Length

1.0

PPBAu

2

SiO2 49.00, AI2O3 16.40, Fe2O3 8.17, CaO 10.98, MgO 6.24, Na2O, 1.30 K2O 0.08 LOI 6.65, Total 99.84.

Grades to very fine grained at lower contact.2"ft vesicles to 4 mm.

Hole #99-02 6 of 8

From (ft)440.7

442.0

444.0

445.2

447.8

To (ft)

442.0

444.0

445.2

447.8

460.8

Description

ANDESITE, Flow Textured, Vesicular, AlteredAphanitic, pale gray mottled, very hard ^file),207o quartz fine vesicles.Microfracturing and alteration.442.0 Gradation contact.

ANDESITE FLOW, Vesicular

Uniform and massive, fine grained crystalline, medium greenish gray.

ANDESITE FLOW, Vesicular, AlteredAphanitic, pale greenish gray, with 207o 1 calcite filled vesicles.Microfracturing and alteration.Very hard ^file).

445.2 Sharp irregular lower contact at 60-90".

ANDESITE FLOW

Uniform and massive very fine grained crystallinecoarsens down the hole reaching maximum 0.5 mm grain size at 447.6.Pale gray, hard (xiail, ^ile).Weak chilling at 447.8.

447.8 25'. Sharp lower contact.Minor fragments of unit below within 1 .0 cm of contact.

ANDESITE Flow Textured, AlteredAphanitic to very fine grained with flow textured sections,generally massive (not uniform)Rare quartz filled vesicles


Hole #99-02 7 of 8

From (ft)

460.8

To (ft)

480.0

480

DescriptionVery hard ^nail to ^ile).Variable colour, pale green to pale gray.Microfracturing and alteration.

460.8 Sharp lower contact.Unit below appears to intrude into unit above as a 0.5 cmwide dike, however alrered volcanics on opposite sides differin appearance, indicating a fragment from the altered unitabove is floating in the coarse flow below.

ANDESITE FLOW, MassiveUniform and massive, fine grained crystalline with feldspar to 0.2X1.0 mm.Pale greenish gray, hard ^nail, < file).Occasional 1 .0-2.5 cm volcanic fragments floating in groundmass.^Va quartz filled vesicles to 4 mm.

END OF HOLE


Hole #99-02 8 of 8

ONTMIO MINISTRY OF NORTHERN DEVELOPMENT AND MINES

Transaction No: Recording Date: Approval Date:

W0180.00047

2001-FEB-06

2001-MAY-07

Work Report Summary

Status: APPROVED (D)

Work Done from: 1999-MAY-01

to: 2000-MAR-31

Client(s):

116181

164694

CARREAU, ALAIN RENE

MARION, ERIC JOSEPH

Survey Type(s):

ASSAY

PSTRIP

LC

PTRNCH

MAG PDRILL

Work Report Details:

Claim*

L

L

L

L

L

L

L

L

1221835

1221837

1221838

1221839

1225451

1225871

1225872

1 225892

Perform

544,141

SO

SO

sosoSO

soso

S44.141

External Credits:

Perform Approve

S44.141

SO

SO

sososososo

S44.141

SO

Applied

S1,868

S2,400

S6,000

S4.000

S 1,600

S2.400

53,600

53,600

S25.468

Applied Approve

51,868

52,400

56,000

S4.000

S1,600

52,400

53,600

S3.600

525,468

Assign

S23.600

SO

SO

SO

SO

SO

soso

523,600

Assign Approve

23,600

0

0

0

0

0

0

0

523,600

Reserve

518,673

SO

5050

sososo50

518,673

Reserve Approve

S1 8,673

soso505050soso

518,673

Due Date2001 -MAR-10

2002-APR-07

2002-APR-18

2002-APR-24

2002-MAR-04

2002-APR-15

2002-APR-23

2002-MAR-25

Reserve:318,673 Reserve of Work Report*: W01 80.00047

S1 8,673 Total Remaining

Status of claim is based on information currently on record.

32D05NE2019 2.20896 DOKIS 900

2001-Jun-12 11:09 Armstrongjj Page 1 of 1

Ministry ofNorthern Developmentand Mines

Date: 2001-JUN-07

Ministers du Developpement du Nord et des Mines

ERIC JOSEPH MARION 126 DUNCAN AVENUE KIRKLAND LAKE, ONTARIO P2N1Y5 CANADA

OntarioGEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E 6B5

Tel: (888)415-9845 Fax:(877)670-1555

Dear Sir or Madam

Submission Number: 2.20896 Transaction Number(s): W0180.00047

Subject: Deemed Approval of Assessment Work

We have approved your Assessment Work Submission with the above noted Transaction Number(s) as per6(7) of the Assessment Work Regulation. Only eligible assessment work is deemed approved for assessment workcredit. The attached Work Report Summary indicates the results of the approval.

NOTE: The report has not been reviewed for technical deficiencies and reported expenses were not evaluated based on the Industry Standard.

At the discretion of the Ministry, the assessment work performed on the mining lands noted in this work report may be subject to inspection and/or investigation at any time.

If you have any question regarding this correspondence, please contact BRUCE GATES by email at [email protected] or by phone at (705) 670-5856.

Yours Sincerely,

Ron GashinskiSupervisor, Geoscience Assessment Office

Cc: Resident Geologist

Alain Rene Carreau (Claim Holder)

Eric Joseph Marion (Assessment Office)

Assessment File Library

Eric Joseph Marion (Claim Holder)

Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:16020

MINING LAMB TEWURE

MAP

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General Information and Limitations

Date y Time of Issue Jun122001

TOWNSHIP r AREA

DOKIS

15:2Bh Eastern

PLAN

M-0342

ADMINISTRATIVE DISTRICTS i DIVISIONSMining Division Larder LakeLand Titles/Registry Division COCHRANE

Ministry of Nttural Resources District KIRKLAND LAKE

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TOPOGRAPHIC

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LAND TENURE

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LAND TENURE WITHDRAWALS

IMPORTANT NOTICES

LAND TENURE WITHDRAWAL DESCRIPTIONS

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THF SHOftES Of flLLUJHE**HDRn*R9

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