· Detour Lake project 1 Summary. The Detour Lake property is located on the northern most, relatively under-explored, Abitibi Greenstone Belt in northeastern Ontario. The property

Detour Lake project

January 11th, 2010

2009 REPORT OF ACTIVITIES ON THE DETOUR

LAKE PROPERTY (ON):

Filing of three delineation drilling holes:

DG-09-701 (claim P421382, P421383 and P421388),

DG-09-717 (claim P421282 and P421283) and

DG-09-779 (claim P421384 and P421389)

Presented by Roger Aubertin, P. Eng. Detour Gold Corp

Detour Lake project

1

Summary

The Detour Lake property is located on the northern most, relatively under-explored, Abitibi Greenstone Belt in northeastern Ontario. The property encompasses 265 square kilometers, including the Detour Lake deposit. The Detour Lake deposit is situated in the area of the former Detour Lake mine which was operated by Placer Dome from 1983 to 1999.

The Detour Lake project is approximately 12 kilometers west of the Ontario-Quebec border and 190 kilometers by road northeast of Cochrane. Access to the property is available via the Detour Lake mine road, an extension of Highway 652 from Cochrane, as well as by air to the site's 1.6 kilometer gravel airstrip.

The property is underlain by supracrustal rocks of the Abitibi Greenstone Belt. It is at the structural contact of the volcanic assemblage of the Deloro Group and the sediments of the Porcupine Group, defined as the Sunday Lake Deformation Zone. The gold mineralization is mainly concentrated within a 200m corridor, sub-parallel to the structural break.

The three diamond drill holes filed in this report totaled 2,190 meters; they were drilled between July 01st, 2009 and October 05th, 2009. These exploration holes tested principally the hangingwall mineralization associated to the known mineralized corridor. Landdrill International drilled these holes. Between July 01st 2009 and October 05th 2009, total expenditures of $303,777 were incurred in claims listed in the following table:

Claim # Hole Length (m) Claim

expenditure

P421382 DG-09-701 397 $55,068 P421383 DG-09-701 74 $10,265 P421388 DG-09-701 305 $42,307 P421282 DG-09-717 493 $68,385 P421283 DG-09-717 168 $23,303 P421384 DG-09-779 455 $63,113 P421389 DG-09-779 298 $41,336

Total 2,190 $303,777

Detour Lake project

2

1. Introduction The Detour Lake property is located in the northern part of Ontario, approximately 190 km by road northeast of Cochrane. Until the end of December 2009, the following activities were carried out on the property: Lidar elevation mapping survey, reconnaissance geological mapping and geophysics, 38 holes of reconnaissance diamond drilling (12,054 m) and 863 holes of delineation drilling (332,178 m). The majority of the activities were concentrated in the Mining Lease, except for some of the exploratory activities. This report summarises the drilling of three exploration holes totalling 2,190metres drilled in 2009. These are DG-09-701 (claims P421382, P421383 and P421388), DG-09-717 (claims P421282 and P421283) and DG-09-779 (claims P421384 and P421389).

2. Property

2.1 Location, access and resources

The Mine Option Property is easily accessible by the old Placer Dome Mine road, an extension of Highway 652 north. The first 151 km on Highway 652 is paved surface road followed by 34 km of well maintained gravel surfaced road to the project site. The site is also accessible via a 1,600 m gravel airstrip that is in excellent condition. Placer Dome Inc. used this airstrip prior to 1991 to fly-in and fly-out its employees (See location map in Appendix A) The Mine Option Property is relatively flat, with maximum relief of about 30 m, and is located close to the Hudson Bay Lowlands. There is very little bedrock outcrop and large areas of the property are overlain by thick accumulations of glacial material that includes till and glacio-fluvial material (poorly sorted sand with lenses of gravel). Approximately 30% of the property is covered by muskeg swamp, which can be up to 1.5 m in thickness. Drainage in the area is generally very poor.

2.2 Limits and ownership

The 265 km2 property forms contiguous claims and/or CLMs in the District of Cochrane. The Detour Lake property includes the Mine Option Property (focus of DGC’s exploration activities) and the surrounding lands known as the Detour Exploration Lands (Blocks A, B, C, D and E), as well as claims that were staked and purchased by the previous owner, Pelangio Mines Limited.

Detour Lake project

3

More recently, in June and August of 2008, a group of 16 claims (3,808 hectares) was staked by DGC north of the Mine Option Property.

3. Historical exploration and mining at Detour

Lake The Detour Lake mine was discovered by Amoco Canada Petroleum Company Limited in 1974. Most of the past exploration and mine development has been carried out by four main operators, including Amoco, Campbell Red Lake Mines, Placer Dome and Pelangio Mines Limited.

Amoco conducted the initial work between 1974 and 1979, followed by Campbell between 1979 and 1987, Placer Dome between 1987 and 1999 and Pelangio between 1999 and 2006. A minor amount of work was also completed by a number of small companies, such as Global Energy Limited, Gowest Amalgamated and Destor Resources Exploration.

The first mining activity at the property was by Campbell between 1983 and 1986, utilizing open pit methods. Campbell and then Placer Dome mined the deposit by underground methods until July 1999. Details regarding the original open pit are limited, but indications are that small-scale equipment and a selective mining approach were used. The open pit extended to a depth of approximately 120 metres with an estimated strip ratio of 4.5:1 (excluding low grade ore). Underground mining was conducted from the 120 metre level to approximately 785 metres below surface. Access for mining was provided by a 600 metre shaft located approximately 150 metre west of the open pit, as well as a series of ramps extending to the 785 metre level.

Past production totaled approximately 1,764,986 ounces of gold from the milling of just over 14.3 million tonnes of ore at an average recovered grade of 3.82 g/t including 5.2 million tonnes grading 2.57 g/t (430,516 ounces) from the open pit and 9.1 million tonnes grading 4.98 g/t (1,464,431 ounces) from underground. Average mill recoveries were 93.2 %.

From 2004 to 2006 Pelangio drilled 127 holes totaling 29,780 metres. Results from this recent work outlined a near-surface gold resource (0 to 250 metres) of 160,000 ounces in the indicated category and 850,000 ounces in the inferred category.

Detour Lake project

4

4. Geological environment

4.1 Reconnaissance geology The Detour Lake project is located within the northwestern portion of the Abitibi Greenstone Belt in the Superior Province of the Canadian Shield. The supracrustal rocks in the project area consist of mafic and ultramafic volcanic rocks of the Deloro Group in thrust contact to the south with the younger Porcupine sedimentary sequence. This regional east-west thrust zone is referred to as the Sunday Lake Deformation Zone ("SLDZ") and can be traced over a distance of more than 20 kilometers on the property. It is defined by a deeply mylonitized and mineralized siliceous alteration zone, referred as the Chert Marker Horizon ("CMH"), which marks the contact between the basaltic and ultramafic terranes.

4.2 Mineralization The bulk of the gold mineralization at Detour Lake is found in the hanging wall of the CMH, in the Upper Detour Lake Formation, which is composed of a thick assemblage of iron-rich tholeiitic mafic flows that are predominantly massive to pillowed, with minor rhyolitic flows and tuffs.

The mineralized east-west corridor forms a 200 m wide (locally up to 350 m) zone that is characterized by swarms of steeply dipping, folded and faulted mineralized quartz veining splaying off the CMH in the Upper Detour Lake Formation. The richest gold mineralized zones are commonly associated with increased biotite alteration, shearing, narrow quartz veining and pyrite or pyrrhotite. Local zones of strong brecciation with sulphide infilling have also been recognized along with chalcopyrite, telluride minerals and visible gold. Visible gold is usually found as specks, clusters or fracture coatings, and its abundance may be associated with the chlorite and chalcopyrite content of the vein. Pillowed flows or hyaloclastites are the preferred hosts to mineralized zones. In the area of the Calcite Zone, the gold mineralization is closely associated with weak potassic and strong carbonate alteration and often contains carbonate in veinlets and quartz veins.

Mineralized zones

The mineralization is located within three main zones: 1) Main zone or CMH, 2) Hangingwall zone and, 3) Footwall zone.

1) Main Zone: The Main Zone or Chert marker Horizon (CMH) was the

largest gold bearing mineralized zone at the former Detour Lake Mine and consisted of gold mineralization occurring in the CMH or in vein systems splaying from it. The former Campbell Pit is at the shallowest portion of the

Detour Lake project

5

surface expression of this west plunging mineralized zone developed along the contact between mafic (tholeiitic) volcanics and ultramafic (komatiitic) rocks. Gold occurs intimately with sulphides, mainly pyrite and pyrrhotite with minor chalcopyrite as rims to these sulphides.

2) Hangingwall zone: The mineralization forms a 200 m wide (locally up to

350 m) corridor within a broad assemblage of mafic volcanics with an overall east-west trend. The bulk of the mineralization within this corridor is concentrated along a highly strained zone showing a strong potassic alteration envelope at the contact between the lower massive and pillowed flows. To date, Detour Gold has tested this Zone and extended the mineralization for a distance of 3.0 km west of the former Campbell pit.

3) Footwall mineralization: The Talc Zone is principally located between 19,700E and 20,540E in a dilatational jog along the CMH. It is hosted in highly altered ultramafic flows with mineralization concentrated at the contact with the CMH and at its lower contact (Footwall mineralization) with barren volcaniclastics and mafic volcanics. The gold mineralization at the lower contact of the Talc Zone shows an increase in sulphide content.

5. Work by Detour Gold Corp

5.1 Recent work (2007-2009)

Year

Covered area

Work

Unity

2007-2009 Mining lease Delineation drilling. 863 holes for 332,178m 2007 Detour Lake

property Lidar elevation

mapping

2007 Detour Lake property

Reconnaissance mapping

2008 Mining lease and block D

Reconnaissance drilling

38 holes for 12,054m

2008 Detour Lake property

Ground magnetometer

compilation and re-interpretation

40 km2 (13kmEW by 3.2kmNS)

Table 1: Detour Gold’s field activities

Detour Lake project

6

5.1.1 2008 regional exploration drilling

The exploration program was designed largely to test 1) for the eastern extension of mineralized Sunday Lake Deformation Zone and, 2) for potential of a North Walter Lake type mineralized zone as it continues to the east. A total of 12,054 meters were drilled in 38 holes.

5.1.2 2007-2009 Delineation Program

In 2009, Detour Gold has drilled 101,074 metres in 241 holes, nearly completing its infill drilling program at Detour Lake with the 40 metre by 40 metre drill spacing up to section 18,000E (west end of Calcite Zone). Since the acquisition of the project, Detour Gold has completed 332,178 metres of drilling to define the Detour Lake gold deposit.

The gold mineralization is found along a known east-west 200 metre wide corridor extending from the West Pit to the Calcite Zone (a distance of 2.5 kilometres). In some areas of the West Pit and Gap Zone, the width of the mineralized corridor extends to near 400 metres. The mineralized corridor remains open west of the Calcite Zone for several kilometres. Gold mineralization within the corridor typically consists of multiple, subvertical, five to 25 metre wide zones grading between 1.0 to 3.0 g/t gold. High gold values are generally characterized by clusters of visible gold in quartz veins and pillow selvages within potassically altered mafic flows that contain a higher percentage of sulphide minerals.

.

6.0 Work filed in this report

6.1 Drillholes (Appendices C and D)

Three (3) drill holes totalling 2,190m are filed in this report. The holes, DG-09-701-, 717 and 779 are described in detail in the logs in Appendix B. These three holes targeted the extension at depth of the hangingwall mineralization, as well as the northern extension of the Sunday Lake Deformation Zone. These holes were drilled in 2009 and are part of the detailed delineation drilling program commenced in January of 2009.

Detour Lake project

7

Claim Hole ID Easting Northing Elv Depth Azi Dip Drill start Drill end P421382, P421383, P421388

DG-09-701 18460.01 20479.51 6287.10 776.0 175.0 -50.0 01/07/2009 11/07/2009

P421282, P421283 DG-09-717 19540.20 20477.88 6280.00 661.0 175.0

-50.0 14/07/2009 21/07/2009

P421384, P421389 DG-09-779 19120.04 20458.11 6278.12 753.0 175.0

-50.0 24/09/2009 05/10/2009

Total 2190.0

Table 2: Drilling summary

5.1.1 Hole DG-09-701: This hole was collared on section 18460E, in the west part of the deposit. It reached a final depth of 776m, targeting the north sector of the mineralized corridor into the hanging wall. The hole intersected mainly the Upper Detour Lake Sequence, mainly pillowed and massive flows. Gold mineralization is mainly associated to the altered pillow flows.

5.1.2 Hole DG-09-717: This hole was collared on section 19540E, NE of the former Campbell pit. It reached a final depth of 661m. This hole intersected the upper pillowed and massive flows. Weak mineralization is observed in the Pillow flow. 5.1.3 Hole DG-09-779: This hole was collared on section 19120E to confirm mineralization in the Gap zone. It reached a final depth of 753m and intersected only the Upper Detour Lake Sequence of massive and pillowed flows. Scattered mineralization is observed mainly in the pillowed flow units.

6.2 Assay results (Appendices E and F)

The three holes were entirely sampled and the samples were sent to the SGS Garson laboratory for preparation and then to SGS Don Mills lab for analysis. A total of 2,301 samples were sent to the lab:

Hole DG-09-701: 813 samples Hole DG-09-717: 682 samples Hole DG-09-779: 806 samples

6.3 Expenditures

Detour Gold Corporation

Detour Lake project

8

Property Detour Lake ON Activity Diamond Drilling Program

Period July. 01st, 2009

October 05th, 2009

Description Cost

Senior geologist (management)

$3,500

Contract geologist $12,000 Technicians + core cutter $10,950

Core Drilling $211,107 Assaying $41,400

Exploration supplies $2,500 Core shack rental $2,400

Office support $2,500 Transport $1,800

Truck rental $2,500 Room and board $10,320

Fuel $1,000 Report writing and map drafting $1,800

Total $303,777

Table 3 Certificate of expenditures

Claim # Hole Length (m) Claim

expenditure

P421382 DG-09-701 397 $55,068 P421383 DG-09-701 74 $10,265 P421388 DG-09-701 305 $42,307 P421282 DG-09-717 493 $68,385 P421283 DG-09-717 168 $23,303 P421384 DG-09-779 455 $63,113 P421389 DG-09-779 298 $41,336

Total 2,190 $303,777

Table 4 Distribution of expenditures

Detour Lake project

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LIST OF APPENDICES

APPENDIX A: Location map APPENDIX B: Claim map

APPENDIX C: Geological logs

APPENDIX D: Cross-sections

APPENDIX E: Assay results

APPENDIX F: Assay certificates

Hwy 6

52 (m

ain ac

cess

road

)

On

tario

Qu

ebec

Lower Detour Area

Sunday Lake Area

Hopper Lake Area

West of Sunday Lake Area

0 2,500 5,000

meters

Assesment Drilling

Existing Detour Lake Pit

Detour Property Outline

Sunday Lake

Hopper Lake

Sagimeo Lake

Detour Gold CorporationDetour Gold CorporationDetour Gold CorporationDetour Gold CorporationDetour Gold CorporationDetour Gold CorporationDetour Gold CorporationDetour Gold CorporationDetour Gold Corporation

Key Map - Assessment Work (4 Dec 2009)

%

P400975

RW306

P421282

P421389P400976

P421283

CLM 231

P400974

P400977

P421388

P421387

P421383P421382

P421384

0 125

meters

250

DG-09-701 DG-09-779

DG-09-717

20 000 N

20 500 N

21 000 N

20

00

0 E

19

50

0 E

19

00

0 E

20

50

0 E

Existing Open Pit

Rock Pile

Shaft

Detour Gold Corporation

Drill Plan - DG-09-701/779/717

1: 5000 (Detour Mine Grid Co-ords)

#

#

DDH

DDH used in

assesment

Azi: 175 degDip: -50 degDepth: 776m



18

50

0 E

Drill Hole LogDatabaseDetour Lake Project

Grid-X: 18,460.01

Grud-Y: 20,479.51

Grid-Z: 6,287.10

Ovb: 24.00

Casing: 24.00

Recover Casing: no

Drill Dates: 01-Jul-09 to 11-Jul-09

Drill: Landdrill International

Purpose: Calcite Zone

Geologist: Eldon Phillips

Hole Number: DG-09-701

Area: MINE

Brg: 174.40

Dip: -50.70

Depth: 776.00 Core Size: NQ

Surveyor: Talbot Surveys

Survey Date: 31-Jul-09

Log Dates: 03-Jul-09 to 11-Jul-09NTS: 32L/4 Claim:

Comments:

From To Length RockType Description From To Code Degree From To Code Percent Comments From ToCode CA Comments

Alteration Mineralization StructureLithology

Comments

0.00 24.00 24.00 OVB OVERBURDEN

24.00 32.10 8.10 PF PILLOW FLOW. Medium to dark green in color with moderately well developed pillow structures with albite alteration being very dominant. Very little carbonate infilling present. Most of the amigdules are chlorite infilled with very little sulphides present.

24.00 32.10 8.10 24.00 32.10 Alb M

24.00 32.10 8.10 24.00 32.10 Po-Py 0.2

32.10 65.60 33.50 MF MAFIC FLOW. Light grey green and fine grained with a massive fairly uniform texture. Numerous carbonate infilled veinlets visible over the unit. Only trace sulphides are visible over the length of the unit.

32.10 65.60 33.50 32.10 65.60 Cal W

32.10 65.60 33.50 32.10 65.60 Po-Py 0.2

32.10 32.11 0.01 32.10 32.11 CN 55

33.10 33.11 0.01 33.10 33.11 FOL 60

34.20 34.21 0.01 34.20 34.21 FOL 45

48.50 48.51 0.01 48.50 48.51 FOL 30

63.70 63.71 0.01 63.70 63.71 FOL 50

January 20, 2010 Page 1 of 20Hole Number: DG-09-701



Comments

65.60 66.60 1.00 II INTERMEDIATE INTRUSIVE. Light grey color with a light pinkish tint. Very fine grained with a mottled uniform texture. Very silicous in composition with few quartz veins or veinlets visible and very weak Kspar alteration with weak sulphides present.

65.60 66.60 1.00 65.60 66.60 Kspar W

65.60 66.60 1.00 65.60 66.60 Si M

65.60 66.60 1.00 65.60 66.60 Alb M

65.60 66.60 1.00 65.60 66.60 Po-Py 0.2

65.60 65.61 0.01 65.60 65.61 CN 80

66.60 84.70 18.10 MF MAFIC FLOW. Similar to the MF unit seen above.

66.60 84.70 18.10 66.60 84.70 Cal W

66.60 84.70 18.10 66.60 84.70 Po-Py 0.2

66.60 66.61 0.01 66.60 66.61 CN 50

78.10 78.11 0.01 78.10 78.11 FOL 30

84.70 87.70 3.00 PF PILLOW FLOW. Light grey green in color with more carbonate alteration and no albite alteration present. Pillow structures are much less well developed than that seen above and there is very weak hyloclastic textures also present.

84.70 87.70 3.00 84.70 87.70 Cal M

84.70 87.70 3.00 84.70 87.70 Po-Py 0.2

84.70 84.71 0.01 84.70 84.71 CN 55

87.70 97.50 9.80 MF MAFIC FLOW. Similar to the other Mafic Flow units seen above.

87.70 97.50 9.80 87.70 97.50 Cal W

87.70 97.50 9.80 87.70 97.50 Po-Py 0.2

87.70 87.71 0.01 87.70 87.71 CN 25

95.40 95.41 0.01 95.40 95.41 FOL 60




Comments

97.50 112.60 15.10 II INTERMEDIATE INTRUSIVE. Similar to the Intermediate Intrusive dykes seen above but shows some brecciated intervals as well as some weak epidote and Kspar alteration. Weak to moderate foliated with Plagioclase phenocrysts visible at the upper contact to about 101 then fade to none after that.

97.50 101.00 3.50 97.50 101.00 Si M

97.50 101.00 3.50 97.50 101.00 Alb M

97.50 102.00 4.50 97.50 102.00 Po-Py 0.2

97.50 97.51 0.01 97.50 97.51 CN 60

101.00 112.60 11.60 101.00 112.60 Si M

101.00 112.60 11.60 101.00 112.60 Alb M

101.00 112.60 11.60 101.00 112.60 Kspar W

101.00 112.60 11.60 101.00 112.60 Epidote

W Epidote alter

102.00 108.00 6.00 102.00 108.00 Po-Py 0.6

108.00 112.60 4.60 108.00 112.60 Po-Py 0.2


112.60 118.70 6.10 112.60 118.70 Cal W

112.60 118.70 6.10 112.60 118.70 Po-Py 0.2

112.60 112.61 0.01 112.60 112.61 CN 60

116.10 116.11 0.01 116.10 116.11 FOL 55

118.70 128.40 9.70 II INTERMEDIATE INTRUSIVE. Similar to the Intermediate Intrusive dyke seen directly above.

118.70 128.40 9.70 118.70 128.40 Alb M

118.70 128.40 9.70 118.70 128.40 Epidote.

W

118.70 128.40 9.70 118.70 128.40 Kspar W

118.70 128.40 9.70 118.70 128.40 Si M

118.70 128.40 9.70 118.70 128.40 Po-Py 0.2

118.70 118.71 0.01 118.70 118.71 CN 25

128.10 128.11 0.01 128.10 128.11 FOL 60




Comments

128.40 133.40 5.00 MF MAFIC FLOW. Similar to the other MF units seen above.

128.40 133.40 5.00 128.40 133.40 Cal W

128.40 133.40 5.00 128.40 133.40 Po-Py 0.2

128.40 128.41 0.01 128.40 128.41 CN 50

133.40 135.20 1.80 GTII GARNETIFEROUS INTERMEDIATE INTRUSIVE. Similar to the other Intermediate Intrusive dykes seen above but this one has about 2 to 5% garnets visible that are evenly disstributed over the unit. There are a few quartz veins visible and there is also a lack of sulphides visible.

133.40 135.20 1.80 133.40 135.20 Garnet

M

133.40 135.20 1.80 133.40 135.20 Si M

133.40 135.20 1.80 133.40 135.20 Po-Py 0.2

133.40 133.41 0.01 133.40 133.41 CN 60

135.20 138.60 3.40 PF PILLOW FLOW. Light greenish grey in color and fine grained with poorly developed pillow structures and no hyloclastic textures visible. Numerous carbonate veinlets visible over the length of the units.

135.20 138.60 3.40 135.20 138.60 Cal W

135.20 138.60 3.40 135.20 138.60 Po-Py 0.2

135.20 135.21 0.01 135.20 135.21 CN 70




Comments

138.60 144.30 5.70 GTII GARNETIFEROUS INTERMEDIATE INTRUSIVE. Similar to the other GTII dyke seen above but contains a couple small felsic intrusive dykes located at 138.6 to 139 and at 140.1 to 140. 4 meters. The Garnets are less evenly disstributed over the unit but with some sections showing more and larger garnets and other areas showing some finer grained garnets. There is also a similar lack of sulphides visible.

138.60 144.30 5.70 138.60 144.30 Si M

138.60 144.30 5.70 138.60 144.30 Garnet

M

138.60 144.30 5.70 138.60 144.30 Alb W

138.60 138.61 0.01 138.60 138.61 CN 60

143.50 143.51 0.01 143.50 143.51 FOL 50

144.30 187.10 42.80 PF PILLOW FLOW. Light greyish green in color with slightly better will developed pillow structures with a more hyloclastic textures present over most of the unit. Most of the pillow rinds show weak potassic alteration.

144.30 187.10 42.80 144.30 187.10 Cal M

144.30 148.00 3.70 144.30 148.00 Po-Py 0.6

144.30 144.31 0.01 144.30 144.31 CN 50

148.00 151.00 3.00 148.00 151.00 Po-Py 0.2

151.00 152.00 1.00 151.00 152.00 Po-Py 1.1

152.00 156.00 4.00 152.00 156.00 Po-Py 0.2

156.00 163.00 7.00 156.00 163.00 Po-Py 0.6

163.00 187.10 24.10 163.00 187.10 Po-Py 0.2

164.70 164.71 0.01 164.70 164.71 FOL 40

180.40 180.41 0.01 180.40 180.41 FOL 45




Comments

187.10 188.20 1.10 FI FELSIC INTRUSIVE. Light pinkish white and fine grained and very hard. No sulphides or quartz veins visible.

187.10 188.20 1.10 187.10 188.20 Alb S

187.10 188.20 1.10 187.10 188.20 Si S

187.10 188.20 1.10 187.10 188.20 Po-Py 0.2

187.10 187.11 0.01 187.10 187.11 CN 70

188.20 212.30 24.10 PF PILLOW FLOW. Similar to the other Pillow Flow units seen above.

188.20 212.30 24.10 188.20 212.30 Cal M

188.20 212.30 24.10 188.20 212.30 Po-Py 0.2

188.20 188.21 0.01 188.20 188.21 CN 45

197.50 197.51 0.01 197.50 197.51 FOL 30

210.30 210.31 0.01 210.30 210.31 FOL 30

212.30 217.20 4.90 PPFI PLAGIOCLASE PORPHYRITIC FELSIC INTRUSIVE. Similar to the Felsic Intrusive dyke seen above but contains about 5% fine grained plagioclase phenocrysts. Most of the plagioclase are about .5 to 1.5 mm in size.

212.30 217.20 4.90 212.30 217.20 Alb S

212.30 217.20 4.90 212.30 217.20 Si M

212.30 217.20 4.90 212.30 217.20 Po-Py 0.2

212.30 212.31 0.01 212.30 212.31 CN 30


217.20 220.80 3.60 217.20 220.80 Cal W

217.20 220.80 3.60 217.20 220.80 Po-Py 0.2

217.20 217.21 0.01 217.20 217.21 CN 45

220.80 221.90 1.10 PPFI PLAGIOCLASE PORPHYRITIC FELSIC INTRUSIVE. Similar to the PPFI dyke seen above.

220.80 221.90 1.10 220.80 221.90 Alb S

220.80 221.90 1.10 220.80 221.90 Si M

220.80 221.90 1.10 220.80 221.90 Po-Py 0.2




Comments

220.80 220.81 0.01 220.80 220.81 CN 70

221.90 228.90 7.00 PF PILLOW FLOW. Similar to the other Pillow Flow units seen above. There are a couple of Felsic Intrusive dykes present. One is a PPFI and the other is a FI dyke. The PPFI is located at 222.2 to 222.8 and the FI is located at 225.3 to 226.1 meters.

221.90 222.00 0.10 221.90 222.00 Cal W

221.90 228.90 7.00 221.90 228.90 Po-Py 0.2

221.90 221.91 0.01 221.90 221.91 CN 70

222.00 223.00 1.00 222.00 223.00 Alb M

222.00 223.00 1.00 222.00 223.00 Si M

223.00 225.00 2.00 223.00 225.00 Cal W

225.00 226.00 1.00 225.00 226.00 Alb S

225.00 226.00 1.00 225.00 226.00 Si M

226.00 228.90 2.90 226.00 228.90 Cal W

228.90 232.60 3.70 PPMI PLAGIOCLASE PORPHYRY MAFIC INTRUSIVE. Dark greenish in color with 5 to 8% plagioclase phenocrysts present.

228.90 232.60 3.70 228.90 232.60 Alb M

228.90 232.60 3.70 228.90 232.60 Po-Py 0.2

228.90 228.91 0.01 228.90 228.91 CN 25

232.60 253.80 21.20 PF PILLOW FLOW. Similar to the Pillow Flow unit seen above. There is a small Intermediate Intrusive dyke located at 251.7 to 252.1 meters.

232.60 244.00 11.40 232.60 244.00 Po-Py 0.2

232.60 232.61 0.01 232.60 232.61 CN 60

244.00 252.00 8.00 244.00 252.00 Po-Py 0.6

247.20 247.21 0.01 247.20 247.21 FOL 40

252.00 253.80 1.80 252.00 253.80 Po-Py 0.2




Comments

253.80 258.10 4.30 II INTERMEDIATE INTRUSIVE. Light grey in color with a light pinkish tint to the rock. Medium to fine grained with a moderate magnetic signiture that decreases towards the lower contact.There is a small pillow Flow unit located at 256.8 to 257.1 meters.

253.80 258.10 4.30 253.80 258.10 Alb W

253.80 258.10 4.30 253.80 258.10 Si M

253.80 258.10 4.30 253.80 258.10 Kspar W

253.80 257.00 3.20 253.80 257.00 Po-Py 2.1

253.80 253.81 0.01 253.80 253.81 CN 70

257.00 258.10 1.10 257.00 258.10 Po-Py 0.6

258.10 259.60 1.50 PF PILLOW FLOW. Light greenish grey in color and medium grained with no pillow structres evident. Numerous carbonate veinlets visible and few to no quartz veins present.

258.10 259.60 1.50 258.10 259.60 Cal W

258.10 259.60 1.50 258.10 259.60 Po-Py 0.2

258.10 258.11 0.01 258.10 258.11 CN 70

259.60 262.10 2.50 II INTERMEDIATE INTRUSIVE. Similar to the Intermediate Intrusive dyke seen directly above.

259.60 262.10 2.50 259.60 262.10 Si M

259.60 262.10 2.50 259.60 262.10 Alb M

259.60 261.00 1.40 259.60 261.00 Po-Py 0.2

259.60 259.61 0.01 259.60 259.61 CN 40

261.00 262.10 1.10 261.00 262.10 Po-Py 2.1




Comments

262.10 279.10 17.00 PF PILLOW FLOW. Light gray green in color with an increase in the amount of pillow structures visible with a moderate amount of hyloclastic textures present. Sulphide content is very low with only trace amounts of pyrite present but there is a slight increase in the amount of pyrrhotite present after 275 meters.

262.10 279.10 17.00 262.10 279.10 Cal M

262.10 273.00 10.90 262.10 273.00 Po-Py 0.2

262.10 262.11 0.01 262.10 262.11 CN 80

264.20 264.21 0.01 264.20 264.21 FOL 40

273.00 279.10 6.10 273.00 279.10 Po-Py 0.6

279.10 281.30 2.20 II INTERMEDIATE INTRUSIVE. Similar to the other Intermediate Intrusive dyke seen above but lacks the magnetic signiture.

279.10 281.30 2.20 279.10 281.30 Si M

279.10 281.30 2.20 279.10 281.30 Alb W

279.10 281.30 2.20 279.10 281.30 Po-Py 0.2

279.10 279.11 0.01 279.10 279.11 CN 45

281.30 319.40 38.10 PF PILLOW FLOW. Similar to the other Pillow Flow units seen above. This unit show very weak potassic alteration around the pillow margins as well as over the unit but only as small localized aggregates of biotite. Alteration is sporatic and not consistant with the KPF unit seen elsewhere.

281.30 319.40 38.10 281.30 319.40 Cal M

281.30 319.40 38.10 281.30 319.40 Po-Py 0.2

281.30 281.31 0.01 281.30 281.31 CN 40

283.20 283.21 0.01 283.20 283.21 FOL 40

300.30 300.31 0.01 300.30 300.31 FOL 40

316.50 316.51 0.01 316.50 316.51 FOL 40




Comments

319.40 322.20 2.80 II INTERMEDIATE INTRUSIVE. Similar to the other Intermediate Intrusive dykes seen above.

319.40 322.20 2.80 319.40 322.20 Si M

319.40 322.20 2.80 319.40 322.20 Alb M

319.40 322.20 2.80 319.40 322.20 Po-Py 0.2

319.40 319.41 0.01 319.40 319.41 CN 50

322.20 324.10 1.90 PF PILLOW FLOW. Similar to the Pillow Flow unit seen above.

322.20 324.10 1.90 322.20 324.10 Cal M

322.20 324.10 1.90 322.20 324.10 Po-Py 0.2

322.20 322.21 0.01 322.20 322.21 CN 60

324.10 333.00 8.90 PPII PLAGIOCLASE PORPHYRITIC INTERMEDIATE INTRUSIVE. Similar to the other II dykes seen above but contains about 5 to 10% plagioclase phenocrysts that are fine grained measuring in the .5 to 1mm in size and are more sporatic at the upper contact but becoming more numerous towards the lower contact. There is a small Pillow Flow unit located at 327 to 327.2 meters.

324.10 333.00 8.90 324.10 333.00 Si M

324.10 333.00 8.90 324.10 333.00 Alb M

324.10 333.00 8.90 324.10 333.00 Po-Py 0.2

324.10 324.11 0.01 324.10 324.11 CN 70

333.00 335.90 2.90 PF PILLOW FLOW. Similar to the other Pillow Flow unit seen above.

333.00 335.90 2.90 333.00 335.90 Cal W

333.00 335.90 2.90 333.00 335.90 Po-Py 0.6

333.00 333.01 0.01 333.00 333.01 CN 50

333.20 333.21 0.01 333.20 333.21 FOL 50




Comments


335.90 342.70 6.80 335.90 342.70 Po-Py 0.2

342.70 349.10 6.40 PF PILLOW FLOW

342.70 342.71 0.01 342.70 342.71 CN 50

349.10 352.20 3.10 MI MAFIC INTRUSIVE

349.10 349.11 0.01 349.10 349.11 CN 80

352.20 391.10 38.90 PF PILLOW FLOW

352.20 352.21 0.01 352.20 352.21 CN 60

354.10 354.11 0.01 354.10 354.11 FOL 45

369.60 369.61 0.01 369.60 369.61 FOL 45

384.10 384.11 0.01 384.10 384.11 FOL 45

391.10 393.40 2.30 II INTERMEDIATE INTRUSIVE. Similar to the other Intermediate Intrusive dykes seen above.

391.10 393.40 2.30 391.10 393.40 Alb M

391.10 393.40 2.30 391.10 393.40 Si M

391.10 393.40 2.30 391.10 393.40 Ser W

391.10 393.40 2.30 391.10 393.40 Po-Py 2.1

391.10 391.11 0.01 391.10 391.11 CN 60

393.40 399.10 5.70 PF PILLOW FLOW. Similar to the other Pillow Flow units seen above.

393.40 399.10 5.70 393.40 399.10 Cal W

393.40 396.00 2.60 393.40 396.00 Po-Py 2

393.40 393.41 0.01 393.40 393.41 CN 35

396.00 399.10 3.10 396.00 399.10 Po-Py 1.5


399.10 415.40 16.30 399.10 415.40 Cal W

399.10 415.40 16.30 399.10 415.40 Po-Py 0.6

399.10 399.11 0.01 399.10 399.11 CN 25

402.60 402.61 0.01 402.60 402.61 FOL 30




Comments

415.40 422.90 7.50 PF PILLOW FLOW. Dark to medium grey in color with several quartz veins containing a large amount of pyrrhotite with smaller amounts of chalcopyrite present. The veins appear to be moderately fractures with weak to moderate carbonate alteration visible.

415.40 422.90 7.50 415.40 422.90 Cal W

415.40 420.00 4.60 415.40 420.00 Po-Py 1.5

415.40 415.41 0.01 415.40 415.41 CN 55

416.90 416.91 0.01 416.90 416.91 VG 3 specks

419.60 419.61 0.01 419.60 419.61 FOL 50

420.00 422.90 2.90 420.00 422.90 Po-Py 1.1

422.90 514.80 91.90 MF MAFIC FLOW. Similar to the Mafic Flow unit seen above. There are several small intrusive units visible over the length of the unit. There is a small Gabbroic looking unit located at 424.2 to 424.7 meters and there are a couple of Intermediate Intrusive units located at 433.4 to 434.1 meters and 437.7 to 438.4 meters. There is a small brecciated zone located at 492.8 to 493.2 meters and consists of abite quartz, and Kspar.

422.90 514.80 91.90 422.90 514.80 Cal W

422.90 425.00 2.10 422.90 425.00 Po-Py 2

422.90 422.91 0.01 422.90 422.91 CN 50

425.00 429.00 4.00 425.00 429.00 Po-Py 1.1

429.00 435.00 6.00 429.00 435.00 Po-Py 0.2

435.00 441.00 6.00 435.00 441.00 Po-Py 0.6

436.70 436.71 0.01 436.70 436.71 FOL 60

441.00 447.00 6.00 441.00 447.00 Po-Py 1.1

447.00 476.00 29.00 447.00 476.00 Po-Py 0.6

452.70 452.71 0.01 452.70 452.71 FOL 60

465.60 465.61 0.01 465.60 465.61 FOL 50

472.80 472.81 0.01 472.80 472.81 FOL 30




Comments

476.00 483.00 7.00 476.00 483.00 Po-Py 0.2

483.00 486.00 3.00 483.00 486.00 Po-Py 0.6

486.00 514.80 28.80 486.00 514.80 Po-Py 0.2

486.20 486.21 0.01 486.20 486.21 FOL 45

505.10 505.11 0.01 505.10 505.11 FOL 35

514.80 523.30 8.50 KPF POTASSICALLY ALTERED PILLOW FLOW. Light pinkish green in color and medium grained with abandant pyrite and pyrrhotite which give the unit a moderate to strong magnetic signiture. Pillow structures are poorly developed but there is a moderate amount of hyloclastic textures visible. The pyrite shows up as both stringer veins as well as medium to large granular aggragets of pyrite. The pyrrhotite is more disseminated throughout the unit with only small aggragets of the magnetic mineral.

514.80 523.30 8.50 514.80 523.30 Cal M

514.80 523.30 8.50 514.80 523.30 K M

514.80 516.00 1.20 514.80 516.00 Po-Py 2.5

514.80 514.81 0.01 514.80 514.81 CN 55

516.00 523.30 7.30 516.00 523.30 Po-Py 7

520.80 520.81 0.01 520.80 520.81 FOL 30

523.30 524.70 1.40 MI MAFIC INTRUSIVE. Similar to the Mafic Intrusive dyke seen above but is less foliated and slightly finer graned.

523.30 524.70 1.40 523.30 524.70 Po-Py 0.2

523.30 523.31 0.01 523.30 523.31 CN 65

524.70 528.20 3.50 KPF POTASSICALLY ALTERED PILLOW FLOW. Similar to the other Potassically Altered Pillow Flow unit seen above.

524.70 528.20 3.50 524.70 528.20 K M




Comments

524.70 528.20 3.50 524.70 528.20 Cal M

524.70 528.20 3.50 524.70 528.20 Po-Py 7

524.70 524.71 0.01 524.70 524.71 CN 65

528.20 529.40 1.20 II INTERMEDIATE INTRUSIVE. Similar to the other Intermediate Intrusive dyke seen above.

528.20 529.40 1.20 528.20 529.40 Si M

528.20 529.40 1.20 528.20 529.40 Alb M

528.20 529.40 1.20 528.20 529.40 Po-Py 2.1

528.20 528.21 0.01 528.20 528.21 CN 80

529.40 537.80 8.40 KPF POTASSICALLY ALTERED PILLOW FLOW. Similar to the other KPF unit seen above.

529.40 537.80 8.40 529.40 537.80 K M

529.40 537.80 8.40 529.40 537.80 Cal M

529.40 533.00 3.60 529.40 533.00 Po-Py 7

529.40 529.41 0.01 529.40 529.41 CN 60

533.00 537.80 4.80 533.00 537.80 Po-Py 6

536.60 536.61 0.01 536.60 536.61 FOL 50

537.80 543.00 5.20 MI MAFIC INTRUSIVE. Similar to the other Mafic Intrusive dyke seen above.

537.80 543.00 5.20 537.80 543.00 Cal W

537.80 538.00 0.20 537.80 538.00 Po-Py 1.1

537.80 537.81 0.01 537.80 537.81 CN 35

538.00 542.00 4.00 538.00 542.00 Po-Py 0.2

542.00 543.00 1.00 542.00 543.00 Po-Py 1.1

542.00 542.01 0.01 542.00 542.01 FOL 30

543.00 548.80 5.80 KPF POTASSICALLY ALTERED PILLOW FLOW. Similar to the other KPF unit seen above but with less pyrite visible than that sen above.

543.00 548.80 5.80 543.00 548.80 Cal M

543.00 548.80 5.80 543.00 548.80 K M

543.00 548.80 5.80 543.00 548.80 Po-Py 5.1

543.00 543.01 0.01 543.00 543.01 CN 90




Comments

548.80 551.90 3.10 PPII PLAGIOCLASE PORPHYRITIC INTERMEDIATE INTRUSIVE. Similar to the PPII dyke seen at 324.1 to 333 meters but the plagioclase phenocrysts are much larger than that seen above. The phenocrysts here are 1 to 2 mm in size. The phenocrysts are more uniformly disstributed over the length of the unit. There are also a ew albite rich veins over the unit as well.

548.80 551.90 3.10 548.80 551.90 Si M

548.80 551.90 3.10 548.80 551.90 Alb S

548.80 551.90 3.10 548.80 551.90 Kspar W

548.80 551.90 3.10 548.80 551.90 Po-Py 0.2

548.80 548.81 0.01 548.80 548.81 CN 35




Comments

551.90 589.70 37.80 KPF POTASSICALLY ALTERED PILLOW FLOW. This KPF unit has much better developed pillow structures that that seen above and there is a much stronger hyloclastic texture to the unit. The fragments are stretched or oriented parallel to the pillow margins. There is also strong carbonate flooding around the fragments. Pillow margins are far apart in the order of 1 to 1.2 meters on average. The pillow margins are very distinct and are fairly broad lasting 10 to 15 cm wide. There is mostly finely disseminated pyrrhotite present with only minor to trace amount of pyrite present. Most of the pyrrhotite however is seen outside of the pillow margins and seen as small to moderate sized blotches of pyrrhotite.

551.90 589.70 37.80 551.90 589.70 K W

551.90 589.70 37.80 551.90 589.70 Cal M

551.90 589.70 37.80 551.90 589.70 Po-Py 2.1

551.90 551.91 0.01 551.90 551.91 CN 55

553.60 553.61 0.01 553.60 553.61 FOL 40

559.10 559.11 0.01 559.10 559.11 FOL 40

560.70 560.71 0.01 560.70 560.71 FOL 55

570.90 570.91 0.01 570.90 570.91 FOL 50




Comments

589.70 612.80 23.10 CBPF CARBONATED BRECCIATED PILLOW FLOW. Light grey green in color with a moderately brecciated appearance to the unit. It is very distinctive compared to the KPF unit seen above. There is a dramatic drop in the presence of hyloclastic textures with no well developed pillow margins visible. The unit is strongly brecciated as well as foliated at approx 20 degrees to the CA. The brecciation is very visible but is undefined in nature. There is a moderate amount of carbonate infilling around the fragments. There is also a strong presence of pyrrhotite over the length of the unit. There are few quartz veins visible in this unit with most containing mostly pyrrotite with minor to trace amount of either pyrite or pyrrotite.

589.70 612.80 23.10 589.70 612.80 Cal M

589.70 612.80 23.10 589.70 612.80 K W

589.70 612.80 23.10 589.70 612.80 Po-Py 5.1

589.70 589.71 0.01 589.70 589.71 CN 50

592.50 592.51 0.01 592.50 592.51 FOL 20

609.40 609.41 0.01 609.40 609.41 FOL 30




Comments

612.80 664.20 51.40 KPF POTASSICALLY ALTERED PILLOW FLOW. This KPF unit is moderately different that the KPF unit seen above. In this KPF unit there is some pillow structure development but is weak in nature. There is also very little hyloclastic textures visible in the upper portion of the unit but become moderately better 640 meters with the pillow margins being farther apart than that seen above. There is also a weak to moderate increase in the number of quartz veins present. However only a few of the quartz veins are strongly mineralized and the rest or only weakly mineralized. Only when the quartz vein contains abundant amount of carbonate does the amount of mostly pyrrhotite become visible.

612.80 664.20 51.40 612.80 664.20 K W

612.80 664.20 51.40 612.80 664.20 Cal M

612.80 631.00 18.20 612.80 631.00 Po-Py 2.1

612.80 612.81 0.01 612.80 612.81 CN 40

625.00 625.01 0.01 625.00 625.01 FOL 25

631.00 633.00 2.00 631.00 633.00 Po-Py 10.1

633.00 639.00 6.00 633.00 639.00 Po-Py 5.1

639.00 642.00 3.00 639.00 642.00 Po-Py 7

642.00 644.00 2.00 642.00 644.00 Po-Py 2.5

644.00 664.20 20.20 644.00 664.20 Po-Py 2.1

664.20 665.90 1.70 MI MAFIC INTRUSIVE. Lighter grey than the other Mafic Intrusive dykes seen above but is still fine grained and contains one quartz vein.

664.20 665.90 1.70 664.20 665.90 Po-Py 0.2




Comments

664.20 664.21 0.01 664.20 664.21 CN 50

665.90 711.90 46.00 KPF POTASSICALLY ALTERED PILLOW FLOW. Similar to the KPF unit seen above but there is an increase in the amount of potassic alteration visible after 670 meters.

665.90 711.90 46.00 665.90 711.90 K M

665.90 711.90 46.00 665.90 711.90 Cal M

665.90 671.00 5.10 665.90 671.00 Po-Py 2.1

665.90 665.91 0.01 665.90 665.91 CN 30

671.00 682.00 11.00 671.00 682.00 Po-Py 3

674.70 674.71 0.01 674.70 674.71 FOL 55

682.00 689.00 7.00 682.00 689.00 Po-Py 2

689.00 711.90 22.90 689.00 711.90 Po-Py 3

694.40 694.41 0.01 694.40 694.41 FOL 50

706.30 706.31 0.01 706.30 706.31 VG 1 specks

708.70 708.71 0.01 708.70 708.71 FOL 40

711.90 718.20 6.30 MF MAFIC FLOW. Similar to the other Mafic Flow unit seen above.

711.90 718.20 6.30 711.90 718.20 Cal W

711.90 718.20 6.30 711.90 718.20 Po-Py 0.2

711.90 711.91 0.01 711.90 711.91 CN 80

718.20 729.00 10.80 KPF POTASSICALLY ALTERED PILLOW FLOW. Similar to the other KPF unit seen above. There is a small PPMI dyke located at 725.5 to 726.2 meters.

718.20 729.00 10.80 718.20 729.00 K M

718.20 729.00 10.80 718.20 729.00 Cal M

718.20 719.00 0.80 718.20 719.00 Po-Py 3

718.20 718.21 0.01 718.20 718.21 CN 80

719.00 729.00 10.00 719.00 729.00 Po-Py 4

725.00 725.01 0.01 725.00 725.01 Other 3 Te

725.00 725.01 0.01 725.00 725.01 VG 2 specks

728.70 728.71 0.01 728.70 728.71 FOL 60




Comments

729.00 730.50 1.50 II INTERMEDIATE INTRUSIVE. Similar to the other Intermediate Intrusive dykes located above.

729.00 730.50 1.50 729.00 730.50 Alb W

729.00 730.50 1.50 729.00 730.50 Si M

729.00 730.50 1.50 729.00 730.50 Po-Py 0.2

729.00 729.01 0.01 729.00 729.01 CN 80

730.50 756.60 26.10 KPF POTASSICALLY ALTERED PILLOW FLOW. Similar to the other Potassically Altered Pillow Flow units seen above.

730.50 756.60 26.10 730.50 756.60 K M

730.50 756.60 26.10 730.50 756.60 Cal M

730.50 756.60 26.10 730.50 756.60 Po-Py 4

730.50 730.51 0.01 730.50 730.51 CN 85

747.50 747.51 0.01 747.50 747.51 FOL 60

756.60 776.00 19.40 MF MAFIC FLOW. Similar to the other Mafic Flow units seen above. There is a moderate increase in the number of quartz veins that are present.

756.60 776.00 19.40 756.60 776.00 Cal W

756.60 765.00 8.40 756.60 765.00 Po-Py 1.1

756.60 756.61 0.01 756.60 756.61 CN 70

762.20 762.21 0.01 762.20 762.21 FOL 65

765.00 767.00 2.00 765.00 767.00 Po-Py 0.6

767.00 771.00 4.00 767.00 771.00 Po-Py 0.2

771.00 773.00 2.00 771.00 773.00 Po-Py 1.1

773.00 774.00 1.00 773.00 774.00 Po-Py 0.6

774.00 776.00 2.00 774.00 776.00 Po-Py 0.2



Grid-X: 19,540.20

Grud-Y: 20,477.88

Grid-Z: 6,280.00

Ovb: 29.80

Casing: 29.80

Recover Casing: no

Drill Dates: 14-Jul-09 to 21-Jul-09


Purpose: West Pit

Geologist: Joseph Fars


Area: MINE

Brg: 174.90

Dip: -51.10



Survey Date: 31-Jul-09

Log Dates: 18-Jul-09 to 19-Jul-09NTS: 32L/4 Claim:

Comments:



Comments


29.80 142.60 112.80 MF MAFIC FLOW Fine grained, massive mafic mafic flow. Localized porphyritic texture and gradational changes in grain size. Strongly chloritized. Calcite stringers pervasive in fractures. Few qt veins with localized carbonate (calcite alteration). Very massive rock with seldom foliation. Albitic alteration in frequent intervals showing a lighter grey rock. Minor specks of pyrrhotite, with traces of pyrite. Frequent felsic intrusions at beginning of hole, and PPMI unit at 63.2 with gradational contacts at upper and lower boundry. Po band at 76.8m hosting 15% po and 4% py. Parasitic folds at 130.2 hosting weak potassic alteration. Calcite and postassic alteration moderately associated with quartz veinlets.

29.80 142.60 112.80 29.80 142.60 K W

29.80 142.60 112.80 29.80 142.60 Alb W

29.80 142.60 112.80 29.80 142.60 Po-Py 0.13




Comments

39.80 39.81 0.01 39.80 39.81 CN 80

47.30 47.31 0.01 47.30 47.31 CN 80

142.60 196.40 53.80 PF PILLOW FLOWLight to medium greyish green, moderately developd pillow structures present. Pillow rinds present showing weak hyoclastic textures, marked by strong albite alteration. Localized ones of sulfides (predominantly pyrrhotite) overprinting albite amygdales. Few albite amygdales hosting calcitic alteration. Congestion of qt veinlets and quartz stockworks at beginning transition of unit hosting up to 12% pyrrhotite and 7% pyrite. Sharp interval of over pervassive pyrrhotite banding seen at 167.4m to 168m within a Siliceous zone showing brecciated qt veinlets oriented parallel to shear at 45 degrees. Localied zones of pervasive pyrrhotite bands. Sulphide mineralization varies from weak to moderate; mainly fine disseminated blebs and patches of po and py.

142.60 159.40 16.80 142.60 159.40 K W

142.60 159.40 16.80 142.60 159.40 Si W

142.60 159.40 16.80 142.60 159.40 Kspar W

142.60 159.40 16.80 142.60 159.40 Alb W

142.60 196.40 53.80 142.60 196.40 Po-Py 12

142.60 196.40 53.80 142.60 196.40 Cpy 0.02

163.00 163.01 0.01 163.00 163.01 CN 60

167.40 168.00 0.60 167.40 168.00 Po-Py 42 Pervasive pyrrhotite banding parallel to brecciated QV and foliation.




Comments

167.40 168.00 0.60 167.40 168.00 Cpy 2

196.40 200.80 4.40 II INTERMEDIATE INTRUSIVEDark grey, very fine grained, moderately siliceous rock. Massive, homogeneous with slight foliation at 45 degrees. Few quartz veins hosting trace to little py mineralization. Localized plagioclase phenocrysts, with weak albitic alteration towards bottom margin.

196.40 200.80 4.40 196.40 200.80 Si W

196.40 200.80 4.40 196.40 200.80 Alb W

196.40 200.80 4.40 196.40 200.80 K W

196.40 200.80 4.40 196.40 200.80 Po-Py 0.02

196.40 196.41 0.01 196.40 196.41 CN 70

200.80 285.30 84.50 PF PILLOW FLOW Very similar to previous PF unit. Grey to dark grey, with moderately developed pillow structures. Pillow rinds showing prominent hyoclastic textures, typically associated with albite alteration. Few albite amygdales hosting calcitic alteration. Finely disseminated py and po found close to qt veinlets. Also, po veinlets infilling propogating fractures. Siliceous ones hosting biotite alteration. Few po bands. Localized shear showing parasitic folds, typically associated with Kspar. Intermediate intrusive 250.1m to 252.5m

200.80 285.30 84.50 200.80 285.30 Alb M

200.80 285.30 84.50 200.80 285.30 K W

200.80 285.30 84.50 200.80 285.30 Po-Py 13

200.80 200.81 0.01 200.80 200.81 CN 80

250.10 250.11 0.01 250.10 250.11 CN 60




Comments

252.50 252.51 0.01 252.50 252.51 CN 70

285.30 293.70 8.40 MF MAFIC FLOW Small mafic flow unit with gradual contacts. Fine grained, massive with few qt veins showing carbonate (calcite alteration). Minor specks of pyrrhotite, with traces of pyrite. Calcite and postassic alteration moderately associated with quartz veinlets.PPMI interval at 292.2m to 293.7m

285.30 293.70 8.40 285.30 293.70 K W

285.30 293.70 8.40 285.30 293.70 Alb W

285.30 293.70 8.40 285.30 293.70 Po-Py 5

293.70 352.10 58.40 PF PILLOW FLOW Very similar to pillow flow seen in above units. A fine grained, greenish grey in color with well developed pillow structures. Vascular pillow rinds embedded with strong albite alteration is present throughout the interval. Pillow margins are mark by albite amygdale which is overprinted with pyrrhotite sulphides. Several quartz veins occurs with trace to moderate sulphides. Weakly altered pottasic pillow unit from 343m to 343.8m and 350.2m to 352.1m.

293.70 352.10 58.40 293.70 352.10 K W

293.70 352.10 58.40 293.70 352.10 Alb W

293.70 352.10 58.40 293.70 352.10 Po-Py 16

293.70 293.71 0.01 293.70 293.71 FOL 30

343.00 343.01 0.01 343.00 343.01 FOL 45

343.80 343.81 0.01 343.80 343.81 FOL 50




Comments

352.10 417.40 65.30 MF MAFIC FLOW Similar to mafic flow seen above. Fine grained, massive with few qt veins showing carbonate (calcite alteration). Weakly potassic zones. Well compacted unit. Very massive rock with seldom foliation. Localized albitic alteration showing a lighter grey rock. Slight porprytic texture from 387.4m to 393m (posibbly gabbro, however not enough plag). BPF unit from 406m to 407m. Decrease in mineralization with localized pyrrhotite stringers.

352.10 417.40 65.30 352.10 417.40 Alb M

352.10 417.40 65.30 352.10 417.40 K W

352.10 417.40 65.30 352.10 417.40 Po-Py 7

406.00 406.01 0.01 406.00 406.01 FOL 70

407.00 407.01 0.01 407.00 407.01 FOL 70

417.40 469.40 52.00 PF PILLOW FLOW Similar to above unit with more prominent pillow structures. Hyloclastic structures showing slight brecciation. Calcitic amygdales pervasive in weakly potassic zones and moderately siliceous zone. Pillow margins are mark by albite amygdale which is overprinted with pyrrhotite sulphides. Few chloritic stringers. Mineralization decrease showing minor specks of pyrrhotite along quartz veinlets.

417.40 469.40 52.00 417.40 469.40 Alb W

417.40 469.40 52.00 417.40 469.40 K W

417.40 469.40 52.00 417.40 469.40 Po-Py 3

417.40 417.41 0.01 417.40 417.41 FOL 50




Comments

469.40 600.30 130.90 MF MAFIC FLOW Dark greyish colour, fine grained with localied porhphyritic texture showing slight foliation typically at 45 degrees. Gradational changes towards porphyritic texture and change in grain size in common. Possible amgydales seen, however no hyaloclastite structures present. Porphyritic texture from 474.4m tto 475.3m, as well as 520m to 521m with slight foliation at 55 degrees. PPMI unit at 496.3m to 498.3m showing slight foliation at 70 degrees. Possible PF at 565 to 566m indicated by calcitic amygdales. General decrease in overall mineralization

469.40 600.30 130.90 469.40 600.30 Alb W

469.40 600.30 130.90 469.40 600.30 K W

469.40 600.30 130.90 469.40 600.30 Po-Py 0.15

600.30 661.00 60.70 PF PILLOW FLOW Typical pillow flow as seen in previous units. Well formed hyaloclastite structures and calcititc amygdales. Strong chlorite alteration within hyaloclastic structures with localized strain causing slight foliation. Weakly potassicly altered unit and overall decrease in sulphides. Intermediate intrusive interval from 621.5m to 622.8 with a slight foliation at 60 degrees.

600.30 621.50 21.20 600.30 621.50 Alb W

600.30 621.50 21.20 600.30 621.50 K W

600.30 661.00 60.70 600.30 661.00 Po-Py 3



Grid-X: 19,120.04

Grud-Y: 20,458.11

Grid-Z: 6,278.12

Ovb: 11.99

Casing: 12.00

Recover Casing: no

Drill Dates: 24-Sep-09 to 06-Oct-09


Purpose: Gap Zone

Geologist: Annor Addae


Area: MINE

Brg: 175.20

Dip: -51.30



Survey Date: 15-Oct-09

Log Dates: 26-Sep-09 to 06-Oct-09NTS: 32L/4 Claim:

Comments: Wedge emplaced at bottom of hole (330m) to correct deviation



Comments





Comments

11.99 203.80 191.81 MF MAFIC FLOW A grey to green in color, massive, fine to medium grained Mafic Flow. Gradational changes of grain size is very common. Weak to moderate foliated; Well competent rock with weak to strong random broken rock. Broken rock is a result of man hole within the drill area. Sporadic quartz veining, mostly barren with odd once containing traces of pyrite and no visible gold are developed. Sulphide mineralization occurs from trace to weak amount; mostly fine trace of py, po and mild cpy respectively. Odd section of albite pillow selvages are developed in some areas. A well foliated section characterized by albite infill is present from 162-176.4m. Weak to moderate defined pillow flow unit is present from 626.8-628.2m. Numerous intrusion are present from the following sections:18-18.9 II25.5-25.9 II27.7-30.2 II47.8-48.2 FI52.1-52.8 FI66.7-67.1 FI89.7-91.1 FI203.7-203.8 PF

11.99 162.00 150.01 11.99 162.00 Cal W

11.99 162.00 150.01 11.99 162.00 K W

11.99 162.00 150.01 11.99 162.00 Alb W

11.99 203.80 191.81 11.99 203.80 Po-Py 0.4

12.00 203.80 191.80 12.00 203.80 CN 50

162.00 176.40 14.40 162.00 176.40 Cal W

162.00 176.40 14.40 162.00 176.40 K W

162.00 176.40 14.40 162.00 176.40 Alb M




Comments

162.00 176.40 14.40 162.00 176.40 Po-Py 1

162.00 176.40 14.40 162.00 176.40 Cpy 0.1

176.40 203.80 27.40 176.40 203.80 Cal W

176.40 203.80 27.40 176.40 203.80 K W

176.40 203.80 27.40 176.40 203.80 Po-Py 0.4

203.80 359.70 155.90 PF PILLOW FLOW A grey to green and odd cast brown color pillow flow unit. Poor to well defined pillow strcutures are developed throughout the interval. Moderately foliated, however foliation plane has a variable angles. Hyaloclastite are in-filled with calcite fragements as well as calcite amygadales. Sulfide concentration is fairly low; several sporadic quartz veins are present with little to no sulfides. A moderately siliceous plagioclase porphyritic felsic intrusive is present from 227.6-230.2m.

203.80 359.70 155.90 203.80 359.70 Kspar W

203.80 359.70 155.90 203.80 359.70 K W

203.80 359.70 155.90 203.80 359.70 Po-Py 1.1

203.80 359.70 155.90 203.80 359.70 Cpy 0.2

203.80 230.50 26.70 203.80 230.50 CN 89

203.80 359.70 155.90 203.80 359.70 CN 89




Comments

359.70 365.50 5.80 MF MAFIC FLOW A grayish green in color, fine to medium grained and fairly uniform composition mafic flow. Foliation is defined by a preferred orientation of amphibole and pyroxene minerals. There is a weak pervasive biotite alteration and strong chlorite alteration throughout this interval. The primary minerals composed mainly of pyroxene, amphibole, and interstitial plagioclase. Sulphide occurs in trace amount; mostly fine specks of pyrite and pyrrhotite. Quartz veining are rarely developed, the occurred once have variable angles.

359.70 365.50 5.80 359.70 365.50 K W

359.70 365.50 5.80 359.70 365.50 Cpy 0.1

359.70 365.50 5.80 359.70 365.50 Po-Py 0.3

359.70 365.50 5.80 359.70 365.50 CN 20

365.50 369.50 4.00 II INTERMEDIATE INTRUSIVE A fine grained, light grey to brown in color Intermediate intrusive. Several barren quartz veins are present. Slightly silicify and well competent rock overall.

365.50 369.50 4.00 365.50 369.50 Si W

365.50 369.50 4.00 365.50 369.50 Po-Py 0.1

365.50 369.50 4.00 365.50 369.50 CN 85




Comments

369.50 386.30 16.80 MF MAFIC FLOW Same as above MF unit; A grayish green in color, fine to medium grained and fairly uniform composition mafic flow. Foliation is defined by a preferred orientation of amphibole pyroxene minerals. There is a weak pervasive biotite alteration and strong chlorite alteration throughout this interval. The primary minerals composed mainly of pyroxene, amphibole, and interstitial plagioclase. Sulphide occurs in trace amount; mostly fine specks of pyrite and pyrrhotite. Quartz veining are rarely developed, the occurred once have variable angles.

369.50 386.30 16.80 369.50 386.30 K W

369.50 386.30 16.80 369.50 386.30 Po-Py 0.2

369.50 386.30 16.80 369.50 386.30 FOL 45

369.50 386.30 16.80 369.50 386.30 CN 45

386.30 392.90 6.60 PF PILLOW FLOW A fine grained, light brown to green in color weak to strongly developed pillow flow. A well defined pillow rims as well as hyaloclastite infilled with calcite / amygdales which is cast by light tan color is developed in localized area. Quartz veining is rare and minor cluster and blebs of po and py are present in localized area within hyaloclastite.

386.30 392.90 6.60 386.30 392.90 K W

386.30 392.90 6.60 386.30 392.90 Cb M

386.30 392.90 6.60 386.30 392.90 Alb W

386.30 392.90 6.60 386.30 392.90 CN 40




Comments

392.90 461.90 69.00 MF MAFIC FLOW Typical grayish green in color, fine to medium grained and fairly uniform composition mafic flow. Foliation is defined by a preferred orientation of amphibole pyroxene minerals. There is a weak pervasive biotitic alteration and strong chlorite alteration throughout this interval. The primary minerals composed mainly of pyroxene, amphibole, and interstitial plagioclase. Sporadic wispy bands / veinlets of calcite is developed throughout. Sulphide occurs in trace amount; mostly fine specks of pyrite and pyrrhotite. Quartz veining are rarely developed, the occurred once have variable angles. An intrusion is present from the following sections:398.4-401 MF403.2-404.8 MF

392.90 461.90 69.00 392.90 461.90 K W

392.90 461.90 69.00 392.90 461.90 Cb W

392.90 461.90 69.00 392.90 461.90 Alb W

392.90 461.90 69.00 392.90 461.90 Po-Py 0.2

392.90 461.50 68.60 392.90 461.50 CN 40

422.40 422.41 0.01 422.40 422.41 Po-Py 1.5 2 VG at 422.4m

422.40 422.41 0.01 422.40 422.41 VG 2 specks

422.40 422.41 0.01 422.40 422.41 Cpy 0.5

461.50 464.80 3.30 461.50 464.80 CN 20

461.90 475.90 14.00 MI MAFIC INTRUSIVE A fine to medium grained and grey colored mafic intrusive.

461.90 475.90 14.00 461.90 475.90 Alb W

461.90 475.90 14.00 461.90 475.90 Po-Py 0.3

464.80 475.90 11.10 464.80 475.90 FOL 40




Comments

464.80 475.90 11.10 464.80 475.90 CN 80

475.90 493.10 17.20 PF PILLOW FLOW A fine grained, green - grey in color with well defined pillow structures pillow flow unit. Well defined pillow selvages as well as hyaloclastite infilled with moderate calcite and amygdales are locally developed. Fine disseminated clusters and blebs of po, py and cpy are developed along hyaloclastite fragments and also within the groundmass. Quartz veining containing some sulfides are present in localized area. Alteration assemblages is characterized by chlorite, calcite, biotite and some k-feldspar.

475.90 493.10 17.20 475.90 493.10 Cb S

475.90 493.10 17.20 475.90 493.10 K W

475.90 493.10 17.20 475.90 493.10 Kspar W

475.90 493.10 17.20 475.90 493.10 Alb W

475.90 493.10 17.20 475.90 493.10 Cpy 0.3

475.90 493.10 17.20 475.90 493.10 Po-Py 1.5

475.90 493.10 17.20 475.90 493.10 CN 60

493.10 498.00 4.90 PPMI PLAGIOCLASE PORPHYRY MAFIC INTRUSIVE A fine to medium grained and grey colored mafic intrusive. A phenocrysts of plagioclase is set within the matrix. Dark bands of mafic aggregate is spotted within the groundmass. Odd specks of pyrite sulfides developed in localized area.

493.10 498.00 4.90 493.10 498.00 Alb W

493.10 498.00 4.90 493.10 498.00 Po-Py 0.2

493.10 498.00 4.90 493.10 498.00 CN 60




Comments

498.00 525.80 27.80 PF PILLOW FLOW Similar to PF unit above; A fine grained, green - grey in color with well defined pillow structures pillow flow unit. Well defined pillow selvages as well as hyaloclastite infilled with moderate calcite and amygdales are locally developed. Fine disseminated clusters and blebs of po, py and cpy are developed along hyaloclastite fragments and also within the groundmass. Quartz veining containing some sulfides are present in localized area. Alteration assemblages is characterized by chlorite, calcite, biotite and some k-feldspar.

498.00 525.80 27.80 498.00 525.80 Cal S

498.00 525.80 27.80 498.00 525.80 K W

498.00 525.80 27.80 498.00 525.80 Cpy 0.1

498.00 525.80 27.80 498.00 525.80 Po-Py 1.2

498.00 525.80 27.80 498.00 525.80 CN 40




Comments

525.80 541.50 15.70 KPF POTASSICALLY ALTERED PILLOW FLOW A fine grained, brown to pink in color with well defined pillow structures pillow flow unit. Well defined pillow selvages as well as hyaloclastite infilled with moderate calcite and amygdales are locally developed. Fine disseminated clusters and blebs of po, py and cpy are developed along hyaloclastite fragments and also within the groundmass. Quartz veining containing some sulfides are present in localized area. Alteration assemblages is characterized by strong potassic.

525.80 541.50 15.70 525.80 541.50 Cal S

525.80 541.50 15.70 525.80 541.50 K S

525.80 541.50 15.70 525.80 541.50 Cpy 0.1

525.80 541.50 15.70 525.80 541.50 Po-Py 1.5

525.80 541.50 15.70 525.80 541.50 CN 55

541.50 549.50 8.00 PPII PLAGIOCLASE PORPHYRITIC INTERMEDIATE INTRUSIVE A grayish in color and slightly siliceous PPII. Phenocrysts of plagioclase are set in fine grained matrix. A greenish with odd tan white color PPMI crosscut the from 546.5-548.8m. A broken rock with no evidence of fault is present from 542.5-543.2m

541.50 549.50 8.00 541.50 549.50 CN 80




Comments

549.50 559.00 9.50 MF MAFIC FLOW A green in color, massive, fine to medium grained Mafic Flow. Gradational changes of grain size is very common. Weak to moderate foliated; well competent rock with weak to strong random broken rock. Broken rock is a result of man hole within the drill area. Sporadic quartz veining, mostly barren with odd once containing traces of pyrite and no visible gold are developed. Sulphide mineralization occurs from trace to weak amount; mostly fine trace of py, po and mild cpy respectively. Odd section of albite pillow selvages are developed in some areas

549.50 559.00 9.50 549.50 559.00 Cpy 0.1

549.50 559.00 9.50 549.50 559.00 Po-Py 0.3




Comments

559.00 617.50 58.50 KPF POTASSICALLY ALTERED PILLOW FLOW A fine grained, pinkish to light green in color with well defined pillow structures pillow flow unit. Well defined pillow selvages as well as hyaloclastite infilled with moderate calcite and amygdales are locally developed. Fine disseminated clusters and blebs of po, py and cpy are developed along hyaloclastite fragments and also within the groundmass. Section with abundant potassic alteration lacks pillow development, Quartz veining containing some sulfides are present in localized area. Alteration assemblages is characterized by biotite, chlorite and calcite.

559.00 598.00 39.00 559.00 598.00 Cb W

559.00 598.00 39.00 559.00 598.00 K S

559.00 598.00 39.00 559.00 598.00 Po-Py 1.5

559.00 598.00 39.00 559.00 598.00 Cpy 0.2

597.40 597.41 0.01 597.40 597.41 Cpy 0.5

597.40 597.41 0.01 597.40 597.41 Po-Py 1.7 3 specks of VG

597.40 597.41 0.01 597.40 597.41 VG 3 specks

598.00 617.50 19.50 598.00 617.50 Cb M

598.00 617.50 19.50 598.00 617.50 K M

598.00 617.50 19.50 598.00 617.50 Po-Py 1

598.00 617.50 19.50 598.00 617.50 Cpy 0.1




Comments

617.50 753.00 135.50 MF MAFIC FLOW A green in color, massive, fine to medium grained Mafic Flow. Gradational changes of grain size is very common. Weak to moderate foliated; well competent rock with weak to strong random broken rock. Sporadic quartz veining, mostly barren with odd once containing traces of pyrite and no visible gold are developed. Sulphide mineralization occurs from trace to weak amount; mostly fine trace of py, po and mild cpy respectively. Sporadic quartz veining is present; the veins varies from boudinaged veins with chlorite alteration as with as veins which is barren. Two of the veins are found to composed of sulfides and visible gold. Numerous intrusion cross cut the unit from the following sections:611.1-611.6 PPII620.9-620.9 MI620.9-621.9 II621.9-623.1 MI623.1-625 II693.3-695.1 II

617.50 753.00 135.50 617.50 753.00 K W

617.50 753.00 135.50 617.50 753.00 Alb W

617.50 753.00 135.50 617.50 753.00 Po-Py 0.3

715.20 715.21 0.01 715.20 715.21 VG 1 specks

715.60 715.61 0.01 715.60 715.61 VG 6 specks

715.60 715.61 0.01 715.60 715.61 Po-Py 1.2 6 VG at 715.6m boudinaged vein with chlorite alteration


DG

C-0

9-01

3

DG

-07-

069

DG

-07-

073

DG

-07-

077

DG

-07-

138

DG

-07-

142

DG

-07-

145

DG

-07-

265

DG

-07-

266

DG

-07-

271

DG

-07-

274

DG

-07-

282

DG

-08-

425

DG

-08-

449

DG

-08-

455

DG

-08-

462

DG

-08-

471

DG

-08-

477

DG

-08-

547

DG

-08-

551

DG

-09-

677

DG

-09-

679

DG

-09-

687

DG

-09-

701

DG

-09-

761

Ph2

-06

PM

DDH-1

14

00-0

052

00-0

053

00-0

106

00-0

107

07-0818

07-081907

-0820

11-0265

11-026611-

0267

11-0268

11-0331

11-0416

11-0417

11-041911

-0420

11-043311

-043

7

11-0447

11-0448

11-0

449

11-0450

11-045111-0547

11-054811-054911-0

55011-05

51

11-0

552

13-052413-052513-052613-0

527

13-052813-05

29

15-0015

15-001615-001715-001815-001915

-0020

15-0

021

15-021515-021615-02

17

15-0

218

15-021915

-0220

15-0

221

15-024615-02

47

0.00.40.10.90.10.30.30.10.10.70.70.00.01.50.10.10.10.10.10.30.30.00.00.10.10.30.30.00.10.10.30.00.00.20.00.11.01.00.00.20.10.40.20.30.30.40.10.10.00.00.00.10.00.00.20.30.10.00.10.12.41.91.91.90.00.10.10.10.10.00.20.20.00.00.00.10.00.00.60.01.00.00.00.00.00.00.00.00.00.60.20.30.20.30.00.30.00.00.10.00.00.03.10.10.10.00.00.00.00.1

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1.10.10.00.00.20.10.40.00.10.20.10.00.00.00.00.50.00.01.20.00.00.00.10.40.10.10.50.30.00.00.00.00.00.00.10.00.00.00.00.60.30.30.30.00.10.10.10.30.00.00.00.00.00.00.46.00.80.20.00.10.20.21.70.20.40.10.40.40.60.50.10.10.20.10.10.20.00.10.10.00.00.00.21.50.31.50.40.40.92.43.91.60.30.20.20.10.00.00.1

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0.10.10.10.10.10.00.00.10.10.00.00.20.52.17.538.10.30.30.40.10.20.20.00.00.10.10.20.00.00.00.10.10.10.2

0.20.20.10.10.00.00.10.20.10.11.90.40.50.00.10.10.20.10.00.00.10.20.00.00.00.10.00.10.10.00.00.00.00.00.70.10.2

0.00.00.00.20.00.00.20.20.20.60.10.10.30.00.10.10.30.10.10.10.10.00.00.00.00.10.10.00.00.00.10.10.00.00.00.00.00.00.00.00.00.00.10.00.10.00.00.00.00.00.00.00.00.00.00.06.16.10.60.60.01.00.40.00.00.00.00.00.00.00.00.00.00.00.00.10.20.00.00.10.10.00.00.00.00.20.00.00.00.00.00.00.10.00.00.00.00.00.00.40.50.10.40.00.11.03.41.00.10.10.10.00.20.10.00.10.10.00.10.40.10.30.10.00.10.00.00.10.00.20.10.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.00.01.30.10.20.10.20.10.20.40.30.00.00.10.10.10.70.10.30.10.20.30.00.00.00.00.20.00.00.00.30.10.30.30.10.50.50.51.50.10.30.60.10.11.50.40.21.20.40.60.81.60.60.60.80.61.412.61.02.84.43.90.90.80.10.23.70.50.21.00.25.24.31.14.10.21.30.71.41.30.51.60.60.10.20.40.50.10.10.00.00.00.00.10.00.00.10.30.10.10.00.00.00.00.00.10.10.10.10.10.10.10.10.10.10.41.10.10.00.00.10.10.10.00.10.10.30.31.01.11.10.10.20.40.10.90.13.90.10.00.02.90.10.10.10.50.10.30.10.60.11.70.20.10.10.10.00.00.10.10.00.00.00.11.40.12.00.23.10.10.10.20.10.00.00.00.00.00.00.00.00.01.30.10.00.00.10.13.00.10.10.10.00.10.00.00.00.00.00.00.00.00.00.00.00.30.00.00.30.00.00.00.00.00.00.10.00.00.00.00.00.11.41.10.10.10.00.11.10.10.00.00.10.015.00.00.00.10.00.02.60.00.00.20.00.10.10.00.11.40.60.20.00.00.00.00.20.20.10.10.00.01.10.00.00.10.10.20.10.10.00.00.00.00.42.20.20.40.10.20.00.00.00.00.00.00.06.7

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51.90.21.00.20.00.00.10.00.20.11.00.20.61.20.4

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Documents

· Detour Lake project 1 Summary. The Detour Lake property is located on the northern most, relatively under-explored, Abitibi Greenstone Belt in northeastern Ontario. The property