Drill Report Pillar Lake Area Thunder Bay Mining … · This drill program was planned using knowledge gained from the 2007 mapping ... this 2008 program have been planned in order

Drill Report Armstrong (Red Granite) Property

Pillar Lake Area Thunder Bay Mining Division

Ontario

01 1 -1 2iJ GEO elENC P E~Srr.ENT

C FleE

By R.S. Middleton, P .Eng.

Neal Bennett, HB.Sc

Noverrlber, 2008

TABLE OF CONTENTS

Introduction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 2

Location and Access .............................................. , ................................ 3

Property ............................................................................................. 3

PreviousWork ..................................................................................... 3

Survey Dates and Personnel ..................................................................... 4

Regional Geology ......................... , .. .. . . . . . . . . . . .. . . . . .. .. . .. . . .. .. . .. . . . . . . . .. . . . . .. .... 5

Property Geology . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. . . . . . . . . . . . . . . . . . . .. . . . . . . . . . . . . . . . . . . . . . . . .. 8

Litho chemistry ................................................. , .................... " . . . . . . . . .... 9

Drill Hole Summary ............................................................................... 10

Conclusion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. . . . . . . . . .. . . . . . . . . . .. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 11

Recommendations ................................................................................ 12

References ... '" . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 13

Statement of Qualifications .................................................................. '" 17

APPENDIX

A) Claims Location Map, Continuity Map and Claims Info B) Vancouver Petrographic Thin Section Report (RG-08-03) C) Drill Logs & Magnetometer Data D) Drill Plan Maps (l:] 0,000) & Drill Cross Sections (1 :200 & 1 :250 for RG-04) E) Drill Core Assay Certificates (Chemex) F) Vancouver Petrographic Thin Section Report (RG-08-04)

INTRODUCTION

A drill program was carried out in beginning in February, 2008 to October of 2008. This drill program was planned using knowledge gained from the 2007 mapping program combined with magnetics data. The program consisted of 4 holes and totaled 619.52m of drilling. The purpose of the drill program is to test the copper-nickel-PGE potential of the gabbro that exists on the claims.

Basement rock consist of Archean gneiss and Proterozoic layered 1600 my mafic intrusion (olivine gabbro, tractolite, anorthosite) which is cut by a 1590 my alkali porphyry all of whom are part of Wawaig Intrusive complex. These rocks are age dated as part of the Lake Nipigon Geological Initiative Project that commenced in 2003. The age dates are tabulated by Heaman, L.M. (2005). The Proterozoic rocks were discovered in April 2000 and September 2003 while prospecting. A horizontal 20m-30m thick layer of pillowed andesite-basalt lava that may be 1242 my covers the older Proterozoic layered complex and porphyry and is in turn capped by horizontal gabbroic sills (Inspiration Sills) that are equivalent to the Nipigon Sills. These sills are reversely polarized magnetically similar to the Nipigon Sills and therefore are probably 1108 my in age (Middleton, R.S. and Borradaille, G., 2006).

The drill holes within this 2008 program have been planned in order to achieve a cross section of the gabbro body. Drilling that was carried out in 2004 intersected both the Java layer and basement gabbro-troctolite complex. Holes RG04-03, RG04-06, RG04-07, RG04-08, RG04-09, RG04-10 and RG04-11 were sampled as part of this study for whole rock analysis starting in April 2007 as well as rcp analysis for Cu, Ni, REE and PGE analysis with fire assay extraction and Iep finish. Holes RG04-03, RG04-06, RG04-07. RG04-08, RG04-09, and RG05-12 cut the olivine gabbro troctolite layered complex and RG05-1 0 and RG05-11 cut the outer margin which contained syenitic rocks. The outer syenite is considered to be part of the olivine gabbro complex and forms an outer ring to the 12 kilometer circular magnetic high feature that is associated with the gabbro. The syenite phase is associated with a magnetic low. A porphyry cuts the gabbro complex and numerous dikes are observed in the core and in outcrop cutting the gabbro. Pegmatitic phases are found within the porphyry and in dikes cross-cutting the gabbro. Aplite (fine-grained) phases of the porphyry also cut the syenite thereby suggesting that the syenite is older and possibly the same age as the gabbro.

Dikes of fine grained basalt cut the gabbro which are possible feeders to the overlying lava flows. Vv'hole rock analysis was done on the core to determine if the chemistry of these dikes matched that of the lavas.

Remnant Magnetism studies of the lavas and gabbro-troctolite complex have been carried out by Borradaile, G. and Middleton, R.S., which give Proterozoic ages of 1500-1600 my for the gabbro and 2500 my for the lavas. It is possible that the remnance has been altered by the 1108 my diabase sills (Inspiration and Nipigon) and that an older date is more likely since the sills cut the lavas. An age of 1242 my was suggested by Heaman, L (2005) for the lavas but was not considered accurate.

Glacial moraine on the west part of the property contains a preponderance of radio active debris cobbles and small boulders which resemble rocks from the west margin of the gabbro-syenite complex cut by the hole RG05-1 O. Clay alteration supports these boulders and is derived from a weathered horizon at the base of the lava series. The

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high rare earth content of these boulders provides a tool to matching the source rocks using these pathfinder elements, and also assists in studying the origin of these rocks and geological processes associated with the formation of the mineralization.

Exploration of the gabbro complex will be directed at Copper-Nickel-PGE (Platinum Group Elements) targets within layered phases and altered porphyry phases will be explored for rare earth uranium-thorium mineralization.

LOCATION AND ACCESS

The Armstrong property is located 230 km north of Thunder Bay, and covers approximately a 10 km by 10 km area, with the north boundary being 5 km south of the CNR rail line at Armstrong, Ontario. Hwy 527 passes through the property in a northsouth direction (which links Hwy 11-17 in Thunder Bay with Armstrong). The property falls within sheet 521/3 of the NTS map system. The area west of the Highway is largely clear cut and gravel roads installed by the lumber companies traverse the property to the west boundary. Logging roads have provided access into both the east side of the property towards McLauren Lake. The road which accesses the west side of the property west of highway 527 is called the Matice Rd.

PROPERTY

The Armstrong Property (Red Granite) consists of 36 claims or 545 units located in the Pillar Lake area of the Thunder Bay Mining Division in Northwestern Ontario, Canada.

PREVIOUS WORK

2000 Ontario Geological Survey. Garden-Obonga Lake Area Lake Sediment Survey; Au and PGE data. Operation Treasure Hunt, Open File Report 6028, July.10, 2000, 76 p (MRD 57).

2000 Ontario Geological Survey. Armstrong-Lake Nipigon area lake sediment survey: Operation Treasure Hunt- Area C; Ontario Geological Survey, Open File Report 6027.

2001 Inco Tech Services Ltd for Ninety-Nine Rescourc<;:s Ltd. Trenching and Prospecting.

2002 East West Resource Corporation. Airborne magnetic and radiometric survey

2002 East West Resource Corporation. Soil and Geochemical survey.

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2003 Ontario Geological Survey. Summary offield work and other activities, 2003: Nipigon Geoscience Initiative; Ontario Geological Survey, Open File Report 6120.

2004 East West Resource Corporation. Diamond Drilling and Thin Section analysis.

2004 Ontario Geological Survey. Ontario Airborne geophysical surveys, magnetic and gamma-ray spectrometer data, grid and vector data, Lake Nipigon Embayment area, OGS Geophysical Data Set 1047, Maps 81-812,813,836 & 837.

2004 Ontario Geological Survey. Ontario Geophysical Surveys, gravity data, Lake Nipigon Embayment OGS Geophysical Data Set 1047, Maps 81-931, 933 & 935, scale 1: 100,000

2005 Ontario Prospectors Association (OPA) with Geospec. Lake Nipigon Region Geoscience Initiative. U-Pb Age Dating. Interim Report No.5.

2005 East West Resource Corporation. Induced Polarization on the Red Granite Property, Pillar Lake area, Thunder Bay Mining Division 521103, Geosig.

2007 East West Resource Corporation. Field Mapping & Prospecting Program.

2008 East West Resource Corporation. Line Cutting and IP Geophysical Survey.

2008 East West Reource Corporation. Diamond Drilling Program & Thin Section analysis.

SURVEY DATES AND PERSONNEL

Drilling commenced in February of 2008 but was then delayed and began again on April 22nd

, 2008 and continued until October 16th of2008. Drilling was conducted by Custom Diamond Drilling. Supervising geologists were N. Bennett, N. Forslund, M. Lavigne, M. Husslage, P. Neilsen and R.S. Middleton. Geotechnicians on the project were G. Dunphy, B. King, M. King and Administration work was completed by L. Rajnovich.

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REGIONAL GEOLOGY

GENERAL GEOLOGY OF THE LAKE SUPERIOR NIPIGON AREA

Table of Lithologies

PROTEROZOIC

Nipigon Sills - Inspiration Sills (1108 my) - Olivine diabase, alkaline gabbro

Sibley Group (1450 - 1540 my)

Kama Hill Formation - Silt-clay-shale-grit sandstone, red to purple colour, hematized ripple

marks, general lack of carbonate.

Rossport Formation

- Brick red, stromatolites, high dolomite content - upper dolomite + anhydrite - central chert carbonate member + barite - lower dolomite member + anhydrite

Pass Lake Formation

Cross bedding, soft sediment deformation increasing upwards with micro fossils

Unconformity

local Chert quartz rich arenites buff-pink colour basal conglomerate with fragments of underlying rocks locally derived pebbles of Archean basement rocks or underlying Rove formation or Osler volcanics

Animikie Group (1868 my)

- Rove Formation - Gunflint Formation

Note: Barite - BaS04 Barium SUlphate Gypsum - Anhydrite CaS04 Calcium sulphate occur in Sibley rocks

Unconformity

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Pillar volcanics (1240 my?) Andesite-basalt pillow lava

Unconformity

English Bay Porphyry (1540 my)

Pillar porphyry (15 90 my) Alkali feldspar- quartz eye porphyry

Wawaig Layered Intrusive Complex (1599 my) Olivine Gabbro, anorthosite layers, troctolite, Syenite

Unconformity

Archean (basement) Gneiss, volcanics,

[Sibley units After Franklin (1982), Tanton (1931), and Cheadle (1986).]

SIBLEY SEDIMENTS

The Sibley Group of sediments occur on the north shore of Lake Superior and extend north-ward as far as Armstrong, Ontario, and form the base for the Nipigon Plate. This would be roughly a 200 km by 150 km area that has subsequently been intruded and capped by the Logan or Nipigon diabase sills. Age dating by RblSr methods have suggested an age of 1339 +1- 33 Ma, Franklin (1970), however, mapping by Sutcliffe (1987) suggests that an older date is possible for the base of the Sibley. Recent work carried out by the Nipigon Geological Initiative program in 2003-2004 suggests the Sibley to be 1450-1500 my in age, Heaman, L.M. et al (2005). In the vicinity of English Bay on Lake Nipigon, fragments of Sibley have been observed by Sutcliffe to be mixed with felsic volcanic fragments that are related to a high level alkali intrusion (English Bay) that yields an age of 1537-1540 Ma. Fragments of a quartzite and grit - shale units were observed in the alkaline porphyry intrusive by the writer (Middleton), suggesting the Sibley or lower sections existed when the alkali body was intruded. Therefore this suggests that an older rift system existed, as old as 1537 Ma. Tanton (1931), Franklin (1970, 1980, 1982), Cheadle (1986), McIlwaine and Wallace (1976), Wallace (1981), and Sutcliffe (1991) have described the stratigraphy and geological setting of the Sibley in detail.

The importance of the Sibley to the search for uranium unconformity deposits in the Nipigon Plate area is that the Sibley sediments are the same age as the Athabaska sediments. Franklin (1970, 1982) notes that barite occurs in the lower and middle

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formations (Pass Lake and Rossport) and that gypsum and anhydrite occur in the middle and upper formations (Rossport and Kama Hill). Stromatolite horizons occur in the Rossport and Kama Hill formations. Sandstone units have been observed at the basement contact at Havoc, along with 20-80 metre thick conglomerate units.

MID PROTEROZOIC MAFIC INTRUSIONS

The mid Proterozoic mafic intrusions in the vicinity of the Nipigon Plate consist of two knm.vn suites of rocks, an early stage ultramafic - picrite event, the full extent of which is unkno\vl1, and the diabase dolerite Nipigon Sills which are very extensive, 200 km x 120 to 250 X 200 km. The geology of the picrites and Logan sills in the Thunder Bay region has been described by Pye (1953), Blackadar (1954), Geul (1970, ] 973).

a) Early Picrite - Ultramafic Intrusives Picrite rocks have been mapped by Sutcliffe (1987a) near English Bay on the northwest shore of Lake Nipigon where dykes are found cutting an alkali granite - syenite porphyry dated at 1537 my. Drilling carried out by Corona Gold Corporation on the syenite intersected picrite dykes as well.

Evidence for these rocks to be older than the diabase is judged from the fact that the Fox Mountain dyke, which is made of diabase, cuts the ultramafic rocks. This dyke is reversely polarized magnetically, which makes it the same age as the diabase sills and likely is a feeder to the sills. This dyke is oriented N25° W and is parallel to the Black Sturgeon Fault.

b) Diabase - Logan - Nipigon Sills

The diabase sills in the Nipigon Plate area cover a minimum of 1 ] 0 km by 200 km area (22,000 km2

) with other extensions to the northwest called the Kopka Cone Sheet. These diabase sills over all cover a 200 x 250 km area and extend to the southwest of the Nipigon area past Thunder Bay and to the US border where they occur in the vicinity of the Great Lakes Nickel deposit. The diabase is subalkali - tholeiitic in composition with some olivine rich phases, Sutcliffe (1987b). It is. possible that the Keweenawan volcanics to the south once overlaid the diabase. The diabase projects below the Osler volcanics, Sutcliffe (1987), Wallace (1981).

The diabase sills intrude the Rove Formation southwest of Thunder Bay and the Sibley series north and northwest of Thunder Bay. The sills are in the order of 200 m in thickness with thinner 30 m sills below. Another 150 m thick sill is sometimes found above the main 200 m sill. Dips are in the order of 10°, but steeper dips occur along the Black Sturgeon Fault. The Sibley and Logan sill combination is up to 800 m thick and forms the Nipigon Plate, Stockwell et al (1972). Zircon dating of the diabase gives an age of 1109 +/- 2 Ma, Davis and Sutcliffe (1985), and the sill intrusion is interpreted to be contemporaneous with the Keweenawan basaltic magmatism (Osler volcanics) etc, Green (1983), that is associated with the Mid-continent Rift (the Keweenawan Event).

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At the same time as sill intrusion a controlling fault (Black Sturgeon Fault). which is a failed arm of the Mid-continent Rift reactivated along an older rift in the Nipigon Plate area. Graben development along the Black Sturgeon Fault took place as well as block movement and mafic intrusions on other parallel faults.

The Logan sills have reverse magnetic polarity, Dubois (1962), which corresponds to the Keweenawan lavas at the early stage ofvo1canism, Halls, H (1974), however, the polarity returns to normal toward the end of volcanism. Other bodies within the Nipigon Plate that are interpreted to be earlier or later intrusives below the Logan sills have positive polarity. Geological reconnaissance mapping by the writer has noted that some diabase areas are more fractured and altered (hematized) in the vicinity of deeper positive magnetic anomalies suggesting the presence of a post diabase heat source below the sills.

ALKALI - FELSIC INTRUSIVES (PROTEROZOIC)

The English Bay porphyry occurs on the east margin of the Havoc Lake property and contains elevated rare earth elements. This body has been recently age dated at 1540 my seen on Heaman, L.M. et al (2005) and is associated with high uranium thorium potassium values seen on an airborne radiometric survey flown in 2003 as part of the Lake Nipigon Geological Initiative program, O.G.S. (2004 a). The age of this intrusive is the same as Olympic Dam and with extensive hematization of the basement rocks, one should also be observant for IOCG type deposits (iron oxide eopper-gold) that contain uranium values. The alkali intrusion would also be a direct source rock for uranium that would be transported by fluids beneath the Sibley sediments. At Pillar Lake a quartz-feldspar porphyry occurs which is identical in appearance to the English Bay Porphyry but has been dated to be 1590 my. This porphyry cuts the gabbrotroctolite layered rocks.

PROPERTY GEOLOGY

The west margin of the property is underlain by gneissic rocks of Archean Age and are cut by fine grained pink aplite containing magnetite. The aplite phases are possibly derived from a alkali porphyry complex that occurs in Pillar Lake since similar rocks have been seen cutting syenite that occurs on the west margin of the Waweig mafic intrusive complex (see hole RG 04-10). Pegmatites and aplites also cut the Waweig mafic intrusive rocks and have been observed in drill core as well as in outcrop.

The Waweig mafic intrusive complex is a layered intrusion consisting of olivine gabbro, amorthositic layers, troctolite, glomerophyritie layers, and occasional layers of magnetite with sulphide.

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The feldspars are fresh and the only alteration occurs along the margin the pegmatite. Fine grained grey, brownish mafic dikes cut the gabbro and are thought to be feeders to the overlying mafic pillow lavas (see holes RG04-6. RG04-7, RG04-8).

The layering in the mafic intrusive dips south east at -45,-55 degrees and is best observed in the valley west of Badwater Creek.

An extensive horizontal layer of mafic volcanics called the Pillar volcanics extends from beneath the sills on the east side of the map area on claim 3016737 and 3016738 to claim 3000998 on the west side. These rocks are 20-30 m in thickness and consist of pillow lava haloclastite, flow top breccia and massive layers. One occurrence of inter flow sediment has been observed on the clifflike exposure east ofHwy 527 on claim 3016737.

Sibley rocks occur beneath the Inspiration Sills on the south east part ofthe property but have not been observed in the northwest quadrant of the property.

The remnance of olivine gabbro Waweig Complex contains a number of weak reversed remnance magnetism values suggesting that these rocks are Proterozoic (1599my) (Heaman & Easton, 2006) (Borradaile & Middleton, 2006).

LITHO CHEMISTRY

The sampling has shown that the Pillar Porphyry and related felsic (aplite, pegmatite) are elevated in Uranium, Thorium and REEs. This suggests that the altered porphyry rocks in the debris pile are related to this porphyry event.

There is elevated Uranium and Thorium in the trap dikes (basalt) but these particular rocks are highly altered (orange colour, hematized) and therefore may be contaminated because they have intruded the older porphyry rocks.

Alteration in the gabbro suggests that the porphyry has been driving fluids through gabbro carrying elevated U, Th and REE values which has been altering the gabbro.

Thin section work and litho chemistry on the gabbro has shown that the troctolite and olivine gabbro layers occur and are favourable for copper PGE mineralization. There are occcaisional elevated CulZr ratios supporting this.

The high Zr values seen in the porphyry and related rocks suggest a per-alkali intrusive event (Alaskite type).

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Sample Depth in I # Rock Type Hole # Hole Ce La • Nb Sn I Ta Th U

I UIT Zr • h

pp pp pp pp pp pp pp Pp I m m m m m m m m

C36539 RG05-173 I

0.1 6 Basalt Dike DB 4B.Om 360 161 3 7.3 26.2 3.67 500 4 C36540 I Reddish Basalt RG05- 126. 0.1 3 I Dike 08 210.1m 232 106 5 2_ 6.3 17 274 542 ._.

C36540 Serpentinized RG05- 174. 10. 7 Gabbro 08 272.5m 399 189 5 4 3 23.6 2.9 . 260 C36541 RG05- I 166. ~.67 I 867

0.2 9 Gabbro 09 229.2m 5 85 53.9 1 1.7 3.32 0 C36535 RG05- 44. 12.9 0.1 2 I Syenite 10 7B.5m 89 7 23.6 1 • 0.8 5 1.31 90 0 C36535 RG05- 0.1 4 Gabbro 10 141.0m 75.8 38 20 1 i 0.7 9.32 1.47 75 6 C36535 RG05- 171. 82. I I

177. 201 1.6

~.c- Syenite 10 163.9m 5 2 3.~0.2 109 5 0 3 C36536 RG05- 45. 0.2 9 ! Gabbro 11 77.3m 113 7 15.3 3. 0.8 4.06 1.15 165 8 C36537 1- RG05-

-99. 15

1

15.3 0gO !

5 • Porphyry 11 106.5m 201 3 585 I 2 6 165 5 ! 576

DRILL HOLE SUMMARY

RG-OS-Ol

Hole RG-08-01 was drilled at an azimuth of 110 degrees and a plunge of 50 degrees. It had to be abandoned due to troubles getting through thick overburden consisting of sand, gravel and boulders. The hole was then moved to location RG-08-02 to test the same gabbro target but from a setup on exposed bedrock.

RG-OS-02

Hole RG-08-02 was driJled at an azimuth of 110 degrees and a plunge of 50 degrees. This hole intersected 62.67m of diabase which overlies the pillowed lava flows which was drilled for 40.95m. The hole did not intersect the targeted gabbro body as it then hit a syenite unit at ] 08.62m. The hole was then shut down at 124.36m and did not intersect any significant zones of sulphide mineralization.

RG-OS-03

Hole RG-08-03 was drilled at an azimuth of 340 degrees and a plunge of 65 degrees. This hole was designed to test a magnetic high sitting under the pond just to the east of HWY #527. This hole intersected the mafic pillow lava flow to a depth of 47.1 Om. The hole then hit the Gabbro/Troctolite bodies that underlie the lava flow. Mineralization did not exceed trace to 1 % and consisted of pyrrhotite and pyrite and

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exists as very fine disseminations and small blebs up to 2mm. No chalcopyrite or was noted in this hole. Thin sections for this hole have been analyzed and results found in Appendix B.

RG-08-04

Hole RG-08-04 was drilled at an azimuth of 0 degrees and a plunge of 50 degrees. The hole was planned to drill through a mag high and into a mag low, The mag susceptibility data (Appendix C) does not show a distinct change to mag low values. Further follow up on magnetic reversals is recommended. The hole intersected the lava flows until a depth of 45. 12m. The hole then intersected the Gabbro unit. This unit appears to be layered with sharp contacts between fine-medium-coarse grained layers. Thin section work is recommended as well as follow up to determine if the fine grained units are geochemically similar to the overlying diabase unit not intersected in the hole. Boulders intersected at the top of the hole are similar to the REE-TH-U bearing boulders found further to the southwest on the property. This indicates that the source of these boulders is further up ice and follow up is warranted to determine the source location. No significant sulphide intercepts were encountered in this drill hole. Sulphides (pyrrhotite, pyrite) exist in trace to 1 % disseminations and small blebs up to 2mm in width.

CONCLUSION

The Waweig layered mafic intrusive complex has potential for layered (sulphide oxide hosted) PGE-copper deposits. These were tested were tested in this drill program.

Chalcopyrite was observed with pyrrhotite in the drill holes from earlier drill programs in holes RG04-2, RG04-3, RG04-6, and RG04-7. Layers of Magnetite and pyrrhotite occur in hole RG04-7. Copper-Zirconium ratios suggest a favourable environment for sulphide zones. This most recent program produced results that did not display any Cpy or Ni mineralization. The gabbro/troctolite body was intersected but sulfides do not reach values of higher than trace to 1 % and only consist of barren pyrrhotite and pyrite disseminated mineralization.

Boulders of rocks similar to those which have produced REE-U-Th values in the past were intersected in the overburden of hole RG-08-04 suggesting that the source of these boulders is still further in the up ice direction of glacial retreat.

Thin sections were analyzed to determine precisely the lithology of the units. These results are attached in appendix B.

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RECOMMENDATIONS

Magnetic susceptibility inversion processing of the aeromagnetic data suggests increased magnetite concentrations at depth within the layered gabbro. The western contact of the gabbro represents the lowest layers and should be followed up with further IP surveys.

The south east part of the complex should be drilled where lake sediment nickel copper platinum anomalies occur OGS (2000).

The source of the REE-Th-U bearing boulders appears to be further up ice direction due to their presence in the overburden ofRG-08-04. The source for these boulders should be further investigated.

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REFERENCES

Blackadar, RG. (1954) Differentiation and assimilation in the Logan Sills. Ph D thesis, University of Toronto.

Borradaile, G.J & Middleton, RS., (2006) Proterozoic paleomagnetism in the Nipigon Embayment of northern Ontario: Pillar Lake Lava, Waweig Troctolite and Gunflint Formation tuffs; in Precambrian Research, 144.

Caven, R. (2002) A report on airborne geophysical survey on the Nipigon Plate Property of East West Resource Corporation, Red Granite Claim Group, Thunder Bay Mining Division, (magnetic and gamma ray spectrometer).-Terraquest Surveys

Caven, R (2002) A report on airborne geophysical survey on the Nipigon Plate Property of East West Resource Corporation, Norwood and Pillar claim groups, Pillar Township, Thunder Bay Mining Division, Ontario.

Cheadle, Bums A. (1986) Alluvial - playa sedimentation in the lower Keweenawan Sibley Group, Thunder Bay District, Ontario. Canadian Journal of Earth Sciences, Vol 23, No 4, P 527-542.

Davis, D.W., and Sutcliff, RH. (1995) U-PB Zircon ages from the Nipigon Plate and Northern Lake Superior, Bull.Geol. Soc. Am. 96 p.1572 .. 1579

Dawson, J.M., (2002) Report on the Vale Lake Property, Thunder Bay Mining Division, Ontario; for Inco Technical Services Ltd.

Dubois, P.M. (1962) Paleomagnetism and Correlation of Keweenawan Rocks, GSC Bulletin 71.

East West Resource Corporation 2006 Annual Report to Shareholders.

Franklin, J.M. (1970) Metallogeny of the Proterozoic rocks of the Thunder Bay district, unpublished Ph D thesis, University of Western Ontario, London, 317 p.

Franklin, J.M.,McIlwaine, W.H., Poulsen, K.H. and Wanless, R.K. (1980). Stratigraphy and depositional setting ofthe Sibley Group, Thunder Bay district, Ontario, Canada, Canadian Journal of Earth Sciences, Vol. 17, No.5, p.633-651

Franklin, J.M. (ed. 1982) Proterozoic geology of the northern Lake Superior area, Geol Assoc of Canada Field Trip Guide Book 4, 71 pages.

Geotech Ltd. (2004) Report on Helicopter-borne Time Domain Electromagnetic Geophysical Survey, Armstrong Property, Pillar Lake Area. For East West Resource Corporation March 2004 (flown February 2004).

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Good, D.J., and Crockett, J.H. (1994) Genesis of the Marathon Cu - platinum group element deposit, Port Coldwell alkalic complex, Ontario: A mid-continent rift related magmatic sulphide deposit. Economic Geology, Vol 89, p 131-149.

Heaman, L.M., Easton, RM., (2006) Preliminary U/Pb Geochronology Results: Lake Nipigon Region Geoscience Initiative. Ontario Geological Survey, Miscellaneous Release, Data 191.

Hart, T.R. (2005) Lake Nipigon Synthesis, Project 05-002. in Summary ofField Work-2005 Open File Report G 172 p.12-1 to 12-6

Heggie, G., Middleton, RS., 2005. Diamond drill report for drill holes RG04-07, RG04-08, RG05-1 0, RG005-11 and RG05-12, Red Granite-Armstrong Property, Pillar Lake area, Thunder Bay Mining Division, Ontario, Province of Ontario; for East West Resource Corporation.

Jackson, 1.£., Dyer RD. (2000) Garden - Obonga Lake Area high Density Lake Sediment and Water Geochemical Survey, Northwestern Ontario, Ontario Geological Survey, Open File Report 6009.

Mason, J.K., Seim, G., White G.D., Bath, C (1998). English Bay Property Olympic Dam type target. Report of Activities 1997, Resident Geologists Program, OGS Open File 5970, pp 15-16

MacDonald, C.A. (2004) Precambrian Geology of the South Armstrong-Gull Bay Area, Nipigon Embayment, northwestern Ontario, OGS, OpenFile 6136,

Middleton, R.S., (2004) Diamond drilling on the Red Granite Property, Pillar Lake sheet, Armstrong, Ontario; for East West Resource Corporation.

Middleton. R.S., Borradaile G.J., Baker D., & Lucas K., 2004. Proterozoic diabase sills of northern Ontario: Magnetic properties and istory, J. Geophys. Res., 109, B02103, doi: 10.1029/2003JB002581

Miller, J.D. Jr, Smyk, M.C., Sage, R P, and Green, J.C. (1995) Geology, petrology and metanogeny of intrusive igneous rocks of the Mid-continent rift in the Lake Superior region, 1995 International Geologic Correlation Program, Project 336 Field Conference and Symposium, Duluth, Minnesota, p 121-216.

Naldrett, AJ., and Lightfoot, P.C. (1993) Society of Economic Geologists, Special Publication No 2, Giant Ore Deposits. Ed: Whiting, B H, Hodgson, C J, and Mason, R

14

Ontario Geological Survey (2000) Garden-Obonga Lake Area Lake Sediment Survey; Au and PGE data. Operation Treasure Hunt, Open File Report 6028, July. 10, 2000, 76 p (MRD 57).

Ontario Geological Survey (2000) Armstrong-Lake Nipigon area lake sediment survey: Operation Treasure Hunt- Area C; Ontario Geological Survey, Open File Report 6027.

Ontario Geological Survey (2003) Summary offield work and other activities, 2003: Nipigon Geoscience Initiative; Ontario Geological Surv{)y, Open File Report 6120.

Ontario Geological Survey (2004a) Ontario Airborne geophysical surveys, magnetic and gamma-ray spectrometer data, grid and vector data, Lake Nipigon Embayment area, OGS Geophysical Data Set 1047, Maps 81-812,813,836 & 837.

Ontario Geological Survey (2004b) Ontario Geophysical Surveys, gravity data, Lake Nipigon Embayment OGS Geophysical Data Set 1047, Maps 81-931, 933 & 935, scale 1 :100,000

Simoneau, Pierre, (2005) Induced Polarization on the Red Granite Property, Pillar Lake area, Thunder Bay Mining Division 521103, Geosig , 2005

Smith, A.R., and Sutcliffe, R.H. (1987) Keweenawan Intrusive Rocks of the Thunder Bay Area, in Summary ofField Work and Other Activities, OGS Misc Paper 137, pp 248-255.

Stockwell et al (l972)Geology of the Canadian Shield. Geological Survey of Canada Economic Geology Report I, P 830.

Sutcliffe, R.H., and Greenwood, R.C. (1982) Geology of the Lake Nipigon Area, in Summary ofField Work, OGS MP 106, pp 19-23.

Sutclift~ R.H., (1987) Ph D Thesis, University of Western Ontario, London, Ontario

Sutcliffe, R.H. (1991) Proterozoic Geology of the Lake Superior Area in Geology of Ontario, OGS Special Volume 4 pt 1, P 627-660.

Tanton, T.L. (1931) Fort William, Port Arthur, and Thunder Cape map areas, Thunder Bay District, Geological Survey of Canada, Memoir 167,222 p.

Vancouver Petrographics Ltd. 2004. Thin section study of II samples from Red Granite project for East West Resource Corporation.

Vancouver Petrographics Ltd. 2005. Thin section study of 13 san1ples from Red Granite project for East West Resource Corporation.

15

Vancouver Petrographics Ltd. 2005. Thin section study of3 samples from Red Granite project for East West Resource Corporation. Walker, E.C., Sutcliff, R.H. , Shaw, CSJ. and Shore, G.T. 91993) Preliminary Report on the Petrology and Chemistry of the Rare Earth Metal occurrences hosted by the Coldwell Alkaline Complex, Ontario Geological Survey, Open File Report 5840, 20p.

Wilson, A.W.G. (1910) Geology of the Nipigon Basin, Ontario. GSC Memoir 1.

Aeromagnetic Maps

7121G Armstrong, Scale: 1 "=4 miles

Gupta, V K (1991) Shaded image of total magnetic field of Ontario, east-central sheet, Ontario Geological Survey, Map 2586, scale 1: 1 ,000,000

Geological Maps

OGS Geological Map. 2169 Sioux Lookout -Amlstrong Sheet 1 "=4 mile.

Sage, R.P., Breaks, F.W., Stott, G.M., McWilliams G.M., Robertson, D. (1994): Obonga Lake-Lac des nes Sheet, Ontario Division of Mines, Map P. 963, 1 "=2 mile.

16

STATEMENT OF QUALIFICATIONS

I, Neal A. Bennett, of 320 Fitzgerald St., Thunder Bay, Ontario, Canada, hereby certify that:

I graduated from Lakehead University with an H.B.Sc.Geology in 2007.

Employed during the summers of:

2005 - North American Palladium as a geological assistant. 2006 - To present, East West Resource Corporation and Mega Uranium Ltd., Trillium North Minerals. And Cascadia International Resources Inc.

I am a geologist and have been employed as a project geologist by East West Resource Corporation since May 2007.

I wrote this report and completed it in November of2008.

I am not aware of any material fact or material changes with respect to the subject matter of this report, the omission of which would make this report misleading.

Dated at Thunder Bay, Ontario on :

17

APPENI>IXA

Claim Continuity Map, Location Map and Claim Status List

Geology of Thunder Bay Region

13 ree grid

Red Granite Property Claims Info - Thuner Bay Mining Division

Claim # Units Township/Area Recorded Holder Due Date

3000998 15 PILLAR LAKE EAST WEST RESOURCE CORPORATION (100.00 % 2008-DEC-03 3000999 15 PILLAR LAKE EAST WEST RESOURCE CORPORATION ( 100.00 % 2008-DEC-03

.PILLAR LAKE EAST WEST RESOURCE CORPORATION ( 100.00 % 2008-DEC-03 PILLAR LAKE EAST WEST RESOURCE CORPORATION ( 100.00 %) 2008-DEC-03 PILLAR LAKE EAST WEST RESOURCE CORPORATION ( 100.00 % 2008-DEC-03

4766 16 PILLAR LAKE EAST WEST RESOURCE CORPORATION (100.00 % 200B-NOV-10 4776 16 PILLAR LAKE EAST WEST RESOURCE CORPORATION (100.00 %) 2007 -JAN-'18

3014778 16 PILLAR LAKE EAST WEST RESOURCE CORPORATION (100.00 % 2007 -JAN-'18 3016733 16 ! PILLAR LAKE EAST WEST RESOURCE CORPORATION ( 100,00 %) 2008-NOV -10

10 PILLAR LAKE EAST WEST RESOURCE CORPORATION (100.00 % 200S-NOV-10 3016735 16 PILLAR LAKE EAST WEST RESOURCE CORPORATION ( 100,00 %) 200S-NOV -10 3016736 16 PILLAR LAKE EAST WEST RESOURCE CORPORATION ( 100.00 %) 200S-NOV-'10 3016737 16 PILLAR LAKE EAST WEST RESOURCE CORPORATION ( 100.00 % 2008-NOV-10 3016738 16 PILLAR LAKE EAST WEST RESOURCE CORPORATION (100.00 %) 200S-NOV-10 3016740 16 PILLAR LAKE EAST WEST RESOURCE CORPORATION (100.00 % 2008-NOV-'10 4225944 16 PILLAR LAKE EAST WEST RESOURCE CORPORATION (100.00 %) 2010-FEB-27 4225945 15 PILLAR LAKE EAST WEST RESOURCE CORPORATION (100.00 %) 2010-FEB-27 4225946 15 PILLAR LAKE EAST WEST RESOURCE CORPORATION (100,00 %) 2010-FEB-27 4225947 16 PILLAR LAKE EAST WEST RESOURCE CO~O-FEB-27 4229471 16 PILLAR LAKE EAST WEST RESOURCE COR 0-JUN-06 4229472 16 PILLAR LAKE EAST WEST RESOURCE CORPORATION 100.00 %) 0-JUN-06 4229473 16 PILLAR LAKE EAST WEST RESOURCE CORPORATION ( 100.00 % 2010-JUN-06 4229474 15 PILLAR LAKE EAST WEST RESOURCE CORPORATION ( 100.00 % 2010-JUN-06 4229475 16 PILLAR LAKE EAST WEST RESOURCE CORPORATION ( 100.00 % 2010-JUN-06 4229483 16 PILLAR LAKE EAST WEST RESOURCE CORP tt 2010-JUL-10 4229484 16 PILLAR LAKE EAST WEST RESOURCE CORPORATION (100.00 % 2010-JUL-10 4229485 16 ~LLAR LAKE EAST WEST RESOURCE CORPORATION ( 100.00 %) 2010-JUL-10 4229486 15 LLAR LAKE EAST WEST RESOURCE CORPORATION (100,00 % 2010-JUL-28

~LLARLAKE EAST WEST RESOURCE CORPORATION (100.00 %) 2010-JUL-2B 4229488 LLAR LAKE EAST WEST RESOURCE CORPORATION (100,00 % 2010-JUL-28 4229489 15 PILLAR LAKE EAST WEST RESOURCE CORPORATION ( 100.00 % 2010-JUL-2H

~15 PILLAR LAKE EAST WEST RESOURCE CORPORATION (100.00 %) 2010-JUL-2B 16 PILLAR LAKE EAST WEST RESOURCE CORPORATION (100.00 % 2010-AUG-2:5

4229492 12 PILLAR LAKE EAST WEST RESOURCE CORPORATION ( 100,00 % 2010-AUG-05 4229493 12 PILLAR LAKE EAST WEST RESOURCE CORPORATION ( 100.00 %) 2010-AUG-05 4229494 12 PILLAR LAKE EAST WEST RESOURCE CORPORATION ( 100.00 %) 2010-AUG-0!5

Total: 545

APPENDIXB

Petrographic Report (Thin Section Analysis Vancouver Petrographic)

PETROGRAPHIC REPORT ON 3 SAMPLES FROM ARMSTRONG PROJECT

Report for:

SUMMARY:

Bob Middleton East West Resources Corporation 1158 Russell Street Thunder Bay, Ont. P7B 5N2 (807 622 9734)

Invoice 080650

July 23, 2008.

Capsule descriptions are as follows:

RG08-3 96.33: olivine-biotite gabbro with accessory opaques (magnetite and pyrrhotite?) and only slight alteration to talc/sericite, actinolitic amphibole, and clay? Isericite.

RG08-3 155.48: olivine-biotite gabbro with accessory opaques (magnetite and ilmenite?) and locally significant alteration to actinolitic amphibole, talc/sericite, iddingsite and traces of clay?/sericite.

RG08-3 193: felsic porphyritic hypabyssal intrusive rock that may be loosely termed (quartz) trachyte if the alkali feldspar is plagioclase with An<5 (i.e. Ab95), which seems possible. If not, it would be' more correctly classified as (quartz) andesite, partly altered to carbonate and pyrite, with accessory apatite and rutile.

Detailed petrographic descriptions and photomicrographs are appended (as email attachment). If you have any questions regarding the petrography, please do not hesitate to contact me.

Craig H.B. Leitch, Ph.D., P. Eng. (250) 653-9158 craig.leitch@gmaiLcom 492 Isabella Point Road, Salt Spring Island, B.C. Canada V8K 1 V 4

2

RG08-3 96.33: OLIVINE-B[OTITE GABBRO (ACCESSORY MAGNETITE-PYRRHOTITE?), SLIGHT ALTERATION TO TALC/SERICITE-ACTINOLITIC AMPHIBOLE-CLA Y?/SERICITE)

Described as olivine gabbro/troctolite; hand specimen shows relatively coarse-grained, dark grey mafic plutonic rock with disseminated magnetite and pyrrhotite. The rock is strongly magnetic, but shows no reaction to cold dilute HCI, and no stain for K-feldspar in the etched offcut. Modal mineralogy in thin section is approximately:

Plagioclase (labradorite/bytownite?) 55% Clinopyroxene (augite?) 25% Biotite 10% Olivine (partly relict) 3% Talc/sericite, minor iddingsite (after olivine) 2% Amphibole (secondary, actinolitic) 2% Opaque (magnetite?) 2%

(pyrrhotite?) 1 % Clay? /s eric ite (after plagioclase) trace

This gabbroic sample consists mainly of plagioclase and lesser mafic minerals (pyroxene, biotite, relict olivine) plus accessory opaque oxides and sulfides.

Plagioclase forms mainly euhedral crystals up to about 4 mm long, with random orientations, partly enclosing the mafic minerals. Twining is regular but slightly bent; no zoning is apparent. Composition appears to be calcic, approximately on the labradorite-bytO\vnite boundary (An70) based on extinction yl\OlO up to 36 degrees. The crystals are essentially unaltered apart from traces of clay?/sericite along microfractures.

Clinopyroxene forms somewhat irregular, mainly subhedral crystals up to 4.5 mm long although locally somewhat glomeratic. They locally include plagioclase or olivine, and are locally mantled by biotite. The pyroxene has pale brownish green colour and extinction angle about 45 degrees, suggestive of augite. Some crystals are partly altered" mainly around the rims, to minor secondary amphibole as ragged subhedra mostly <1 mm in diameter, with dark olive- to sea-green pleochroism and extinction angle around 19 degrees (possibly actinolitic hornblende?).

Biotite forms ragged, irregular subhedral crystals mostly <2.5 mm in diameter (although locally aggregating to 3.5 mm), with dark red-brown pleochroism and commonly wrapped around pyroxene, or interstitial to pyroxene and plagioclase.

Olivine (or olivine relics) have somewhat rounded or subhedral outlines up to almost 3 mm in diameter, commonly contained within pyroxene crystals or aggregates. The olivine is generally strongly fractured, with traces of minute secondary magnetite (?) along the fractures. In places the olivine is partly to locally completely replaced or pseudomorphed by very fine-grained talc/sericite (randomly oriented flakes <0.1 mm in diameter) or minor red-brown to greenish-brown iddingsite (?) as ragged anhedra <0.35 mm in diameter.

Accessory opaques appear to be mostly magnetite (?) forming skeletal to irregular subhedral crystals up to 2 mm in diameter, interstitial to plagioclase, or associated with biotite and olivine or relict olivine (fine-grained magnetite in the latter case is likely mostly secondary). Sulfides forming irregular subhedra to 0.5 mm long (likely mostly pyrrhotite?) are also commonly interstitial to plagioclase and pyroxene, and associated with biotite.

In summary, this represents olivine-biotite gabbro with accessory opaques (magnetite and pyrrhotite?) and only slight alteration to talc/sericite, actinolitic amphibole, and clay?/sericite.

3

RG08-3 155.48: OLIVINE-BIOTITE GABBRO (ACCESSORY MAGNETITE-ILMENITE?), SIGNIFICANT ALTERA nON TO ACTINOLITIC AMPHIBOLE-TALC/SERICITE-TRACE CLA Y?/SERICITE)

Described as coarse gabbro-pyroxenite; hand sample shows dark blackish green, coarsegrained mafic to ultramafic rock with dotty, mottled texture. The rock is magnetic, but shows no reaction to cold dilute HCl, and no stain for K-feldspar in the etched offcut. Modal mineralogy in thin section is approximately:

Plagioclase (labradorite/bytownite?) 50% Clinopyroxene (augite?) 20% Amphibole (secondary, actinolitic) 13% Biotite 5% Olivine (partly relict) 5% Talc/sericite, minor iddingsite (after olivine) 3% Opaque (magnetite?) 2%

(ilmenite?) 2% Clay?/sericite (after plagioclase) trace

This gabbroic sample consists mainly of plagioclase and lesser mafic minerals (pyroxene or amphibole after pyroxene, biotite, relict olivine) plus accessory opaque oxides. It is similar in composition to the sample from 96.33m, but contains more relict olivine and is somewhat more altered. Relict olivine is erratically distributed in zones alternating with pyroxene-rich zones.

Plagioclase forms mainly euhedral crystals up to about 5 mm long, with random orientations, partly enclosing the mafic minerals in a sub-ophitic texture. Twining is regular but slightly bent, and no zoning is apparent. Composition appears to be calcic, around labradorite (An60) based on extinction yl\OlO up to 30 degrees. The crystals are essentially unaltered apart from traces of clay?/sericite along microfractures.

Clinopyroxene forms somewhat irregular to skeletal, mainly subhedral crystals up to 1 cm across although locally somewhat glomeratic. They locally include plagioclase or rarely altered relict olivine, and are locally associated with biotite. The pyroxene has pale brownish colour (salite?) and extinction angle about 45 degrees, suggestive of augite or salitic augite. In places, most crystals are partly altered, starting around the rims, to significant secondary amphibole as ragged fibrous subhedra mostly <0.5 mm long. In general, core areas have sea-green pleochroism and rims have olive-green pleochroism; extinction angle around 18 degrees in both suggests possibly actinolite andlor actinolitic hornblende (?).

Biotite forms ragged, irregular subhedral crystals mostly <1.5 mm in diameter (although locally aggregating to 6.5 mm), with dark red-brown pleochroism and commonly wrapped around pyroxene or amphibole altered pyroxene, or interstitial to pyroxene and plagioclase.

Olivine (or olivine relics) have somewhat rounded or ragged irregular to subhedral outlines mostly <1 mm long (glomeratic to 2.5 mm), most commonly interstitial to plagioclase or contained within amphibole altered pyroxene crystals or aggregates. The olivine is generally strongly fractured, with traces of minute secondary magnetite (?) along the fractures. In places the olivine is partly to locally completely replaced or pseudomorphed by very fine-grained talc/sericite (randomly oriented flakes <50 microns in diameter) or lesser bright red-brown to greenish-brown iddingsite (?) as ragged anhedra <0.25 mm in diameter.

Accessory opaques appear to be mostly magnetite and ilmenite (?) forming skeletal to irregular subhedral crystals up to 2 mm in diameter, interstitial to plagioclase, or associated with biotite and olivine or relict olivine (fine-grained magnetite in the latter case is likely partly to mostly secondary). No sulfides are visible.

In summary, this represents o1ivine-biotite gabbro with accessory opaques (magnetite and ilmenite?) and locally significant alteration to actinolitic amphibole, talc/sericite, iddingsite and traces of clay?/sericite.

4

RG08-3 193: PLAGIOCLASE PHYRIC, (QUARTZ) TRACHYTE OR ANDESITE (ACCESSORY APATITE. RUTILE) ALTERED TO CARBONATE AND PYRITE

Described as syenite/trachyte porphyry that cuts the gabbro and occurs in ring around the gabbro; hand specimen shows pale buff-grey, fine-grained rock with scattered white relict plagioclase phenocrysts. The rock is not magnetic, and shows significant reaction to cold dilute HCl, but no stain for K-feldspar in the etched offcut. Modal mineralogy in thin section is approximately:

Plagioclase (mainly albite?) 80% Carbonate (mainly calcite?) 10% Quartz (mainly primary, minor secondary) 7% Opaque (mainly pyrite?) 2% Apatite <1% Rutile <1% Clay? /sericite (after plagioclase) <1 %

This sample consists almost entirely of plagioclase (likely sodic), both as scattered phenocrysts and groundmass crystals, both partly altered to carbonate. There is only minor, interstitial, quartz (likely primary) and accessory opaques, apatite and rutile.

Plagioclase phenocrysts have somewhat rounded, sub/euhedral outlines up to about 3 mm in diameter, and are partly altered to carbonate as irregular sub/anhedra mostly <0.1 mm in diameter plus lesser opaque (mainly pyrite?) as euhedral cubic crystals of similar size. The phenocrysts make up about 15-20% of the sample, and lack twinning or zoning, suggesting they may have been recrystallized. Similarity in relief to groundmass plagioclase (which shows negative relief compared to quartz) and the altered character strongly suggest that both phenocryst and groundmass feldspar is albitic or possibly albitized. Traces of clay?/sericite forming minute flakes <15 microns in size occur in both phenocryst and groundmass feldspar.

In the groundmass, which makes up about 80% of the sample, small weakly aligned feldspar crystals are mostly subhedral and <0.25 mm long. They are generally weakly to vaguely twinned, with observed extinction angle on 010 up to about 12 degrees, but strongly negative relief compared to quartz, indicative of albitic composition. Carbonate occurs as irregular-shaped aggregates up toO.5 mm across composed of interlocking sub/anhedral crystals mostly <0.2 mm in size, likely mostly calcite to judge by the strong reaction to cold dilute HCI in hand specimen. Quartz forms small subhedral crystals mostly <0.1 mm in diameter, interstitial to the teldspar, and is likely mostly primary (except where present along narrow, <0.1 mm thick veinlets, where it is clearly secondary, with minor carbonate as subhedra up to 0.5 mm long).

Accessory opaques appear upon hand lens examination to be likely mostly pyrite, forming sub/euhedra to 0.25 mm but locally in aggregates to 0.75 mm. The aggregates are locally partly controlled along fractures or discontinuous veinlets. Apatite forms slender euhedral prisms up to 0.1 mm long. Traces of rutile form aggregates to 0.1 mm of rounded dark brown to opaque subhedra mostly <20 microns in size.

In summary, this is a felsic porphyritic hypabyssal intrusive rock that may be loosely termed (quartz) trachyte if the alkali feldspar is plagioclase with An<5 (i.e. Ab95), which seems possible. If not, it would be more correctly classified as (quartz) andesite, partly altered to carbonate and pyrite, with accessory apatite and rutile.

5

RG08-3 96.33: Gabbro composed of plagioclase (PL) and clinopyroxene (CPX, partly replaced by amphibole, am), with minor olivine (OL) partly replaced along fractures by magnetite, or pseudomorphed by talc/sericite (tls)-minor iddingsite? (id?) associated with biotite (Bl) and opaque oxides . Transmitted plane light, field of view 3.0 mm wide.

RG08-3 155.48: Gabbro composed of plagioclase (PL) and clinopyroxene (CPX, partly replaced by amphibole, am), with lesser olivine partly replaced along fractures by magnetite, or pseudomorphed by talc/sericite (tis) and associated with biotite (bi) and opaque oxides. Transmitted plane light, field of view 3.0 mm wide.

6

RG08-3 193: Ragged phenocrysts of recrystallized, possibly albitized plagioclase (also partly altered to calcite and minor opaques, likely pyrite) in trachytic textured groundmass of small plagioclase (albite?) laths, also partly carbonate altered, minor interstitial quartz, and traces of pyrite (opaque). Carbonate (cb) also occurs in veinlets. Transmitted light, crossed polars, field of view 3.0 mm wide.

Overview of thin sections and offcuts (green semi-circles mark photomicrograph locations).

APPENDIXC

Drill Hole Logs & Magnetometer Data

Rock Type Code

Primary Age Root Description Additional Notes

Code Quaternary

14 Overburden (Unsubdivided)

Proterozoic

13 Diabase (Unsubdivided)

Archean 12 lamprophyre (Unsubdivided)

11 late Structural Zones (Unsubdivided) l1a Shear zone (unsubdivided) l1b Breccia zone (unsubdivided) 11ba Tectonic breccia (late fault zones containing angular clasts)

11 c Fault zone (gouge, lost core)

lld Vein (unsubdivided) l1da Quartz vein

l1db Carbonate vein 11dc Quartz-carbonate vein

10 Late Felsic To Intermediate intrusions (Unsubdivided)

lOa Granite rocks Granite, tonalite, granodiorite, trondjemite, quartz diorite, quartz monzonite

lOb Syenitie rocks Syenite, monzonite, monzodiorite, quartz syenite

10e Quartz porphyry 10d Quartz-feldspar porphyry 10e Feldspar porphyry 10f Pegmatite

109 Aplite

9 Late Mafic-Ultramafic intrusions (unsubdivided)

9a Late Mafic intrusions (Unsubdivided) 9aa Diorite 9ab Anorthosite 9ac Gabbro (unsubdivided) 9aca Leueogabbro loeally grading to granite in No. 34 zone

9aeb Mefanogabbro 9ad Norita 9ae Granophyre

9b Late Ultramafic intrusions (Unsubdivided) 9ba Hornbfendite 9bb Pyroxenite (unsubdivided) 9bba Clinopyroxenite

9bbb Orthopyroxenite 9be Peridotite (unsubdivided)

9bea Wehrfite

Page 1 of 5

Rock Type Code


Code 9bcb Websterite 9bcc Dunite 9bed Lherzolite 9bce Serpentinite

r---

~ Hybrid zone complex mixing/assimilation zone of wall rock and chilled mafic-ultramafic units I---

Massive magmatic sulphide pyrrhotite, chalcopyrite, pentlandite I---

8 Early Felsic to Intermediate Meta-Intrusions (Unsubdivided) 8a Granitc rocks Granite, tonalite, granodiorite, trondjemite, quartz diorite, quartz monzonite

8b Syenitic rocks Syenite, monzonite, monzodiorite, quartz syenite 8c Quartz porphyry includes some amygdaloidal intrusions ad Quartz-feldspar porphyry 8e Quartz-feldspar porphyritic Georgeson Porphyry 8f Feldspar porphyry

8g Aphyric intrusions very fine grained and lacking phenocrysts 8h Pegmatite

7 Early Mafic-Ultramafic intrusions (unsubdivided) 7a Early Mafic intrusions (Unsubdivided) 7aa Diorite 7ab Anorthosite 7ac Gabbro (unsubdivided) 7aca Feldspar glomeritic gabbor 7acb Clinopyroxene oikiocrystic gabbro 7ad Norite 7ae Granophyre 7b Early Ultramafic intrusions (Unsubdivided) 7ba Hornblendite 7bb Pyroxenite (unsubdivided)

~ Peridotite (unsubdivided)

panlinite

6 Chemical Metasedimentary Rocks (Unsubdivided) 6a Graphitic sediments (unsubdivided) 6aa Graphitic Argillite 6b Chert (unsubdivided) 6c Iron formation (unsubdivided) 6ea Oxide facies iron formation 6cb Carbonate facies iron formation 6ec Silicate facies iron formation Sed Sulphide facies iron formation 6ed Argillitic iron formation (unsubdivided) 6c.e ~ clastic iiOn formation (unsubdividedj 6d xhalative sulphide, graphite, carbonate and/or argillite

Page 2 of 5

Rock Type Code


Code

5 Clastic Metasedimentary Rocks (Unsubdivided)

5a Argillite (unsubdivided)

5b Siltstone (unsubdivided)

5c Sandstone (unsubdivided)

5ca Wacke

5cb Arkose/Arenite

5cc Felsic volcanic, lithic sandstone

5cd Felsic volcanic, sandstone to siltstone

5ee Felsic volcanic, Pebbly Sandstone

5d Conglomerate (unsubdivided)

5da Polymictic, felsic volcanic conglomerate (unsudivided) rounded clasts identified

5dap Possible polymictic, felsic volcanic conglomerate (unsudivided)

5daa Boulder conglomerate

5daap Possible boulder conglomerate

5dab Cobble conglomerate

5dabp Possible cobble conglomerate

5dac Pebble conglomerate

5dacp Possible pebble conglomerate

5dad Cobble To boulder conglomerate

5dadp Possible cobble to boulder conglomerate

5dae Pebble To boulder conglomerate

5daep Possible pebble to boulder conglomerate

5daf Pebble To cobble conglomerate

5dafp Possible pebble to cobble conglomerate

5db Polymitic, felsic volcanic conglomerate and interbedded sandstone

5dbp Possible polymitic, Felsic volcanic conglomerate and interbedded sandstone

5dc Oligomictic, felsic volcanic conglomerate (unsudivided) rounded clasts identified

5dcp Possible oligomictic, felsic volcanic conglomerate (unsudivided)

5dd Polymictic, felsic to intermediate volcanic, pebble to boulder conglomerate

5ddp Possible polymictic, felsic to intermediate volcanic, pebble to boulder conglomerate

5de Polymictic, intermediate volcanic, pebble to boulder conglomerate

5dep Possible, polymictic, intermediate volcanic, pebble to boulder conglomerate

5f Siliceous sedimentary breccia possibly intraformational breccia

4 Felsic Metavolcanic Rocks (Unsubdivided)

4a Massive lava flows (unsubdivided)

4aa Quartz porphyritic, fractured to autobrecciated massive, locally amygdaloidallava flows

4ab Quartz-feldspar porphyritic massive lava flows

4ac Feldspar porphyritic massive lava flows

4ad Amygdaloidal massive lava flows

4b Pyroclastic flows (unsubdivided) Quartz crystal bearing with feldspar crystals which mayor may not be visible

4c Tuff (unsubdivided) fragments are <2mm in size

4ca Quartz crystal tuff

Page 3 of 5

Rock Type Code


Code 4cb Quartz-feldspar crystal tuff Nuinsco's QID unit 4cc Feldspar crystal tuff 4cd Lithic tuff 4ce Vitric tuff 4cf Monolithic fragmental units (unsubdivided) probably a component of lava flows 4cfa Monolithic lapilli-tuff fragments are >2mm to 64 mm in size 4cfb Monolithic lapilli-tuff to tuff breccia 4cfc Monolithic tuff-breccia or possibly breccia fragments are >64 mm in size 4cg Heterolithic fragmental units (unsubdivided) angular clasts observed 4cga Heterolithic lapilli-tuff fragments are >2mm to 64 mm in size 4cgb Heterolithic felsic lapilli-tuff to tuff-breccia 4cgc Heterolithic felsic tuff-breccia or possibly breccia fragments are >64 mm in size 4d Felsic unit of uncertain genesis (volcanic or sedimentary)

3 Intermediate Metavolcanic Rocks (Unsubdivided) 3a Massive lava flows (unsubdivided) 3aa Amygdaloidal lava flows 3ab Feldspar porphyritic lava flows 3b Tuff (unsubdivided) fragments are <2mm in size 3ba Crystal tuff 3bb Lithic tuff 3bc Vitric tuff 3bd Lapilli tuff fragments are >2mm to 64 mm in size 3be Tuff breccia fragments are >64 mm in size

2 Mafic Metavolcanic Rocks (Unsubdivided) 2a Massive lava flows (unsubdivided) 2aa Fine-grained massive lava flows 2ab Medium-grained massive lava flows 2ac Variolitic lava flows 2ad Amygdaloidal massive lava flows 2ae Porphyritic massive lava flows 2b Pillowed lava flows (unsubdivided) 2ba Pillow breccia/hyalociastite 2bb Amygdaloidal pillowed lava flows 2c Tuff (unsubdivided) fragments are <2mm in size 2ca Crystal tuff 2cb Lithic tuff 2cc Vitric tuff 2cd Lapilli tuff fragments are >2mm to 64 mm in size 2ce Tuff breccia fragments are >64 mm in size

1 Ultramafic MetavolcCtnic Rocks (Unsubdivided) 1a Massive lava flows

Page 4 of 5

Rock Type Code


Code 1b Pillowed lava flows 1c Polysutured lava flows 1d Spinifex·textured lava flows

Page 5 of 5

Hole 10: RG-08-01 Grid X: Grid Y:

Drill Start: Drll Finish:

ONT. P7B5N2 Surveyed

From

0.00

To

10.00

Project: Red Granite

Easting: 350270.00 Northing: 5560288.00

22/04/2008 Log Start: 22/04/2008 Log Finish:

RG-08-01

Year 2008 UTM Zone: 16 Grid Azimuth: Datum: NAD83 True Azimuth: 110

Claim: 4225947 Dip -50 Length: Elev (m): 0.00 Core Size:

10.00 BQ

TWP: Pillar Lake Casing: left in Casing (m): 10

Drill Company: Custom DiamondDrilling Drilled for: East West Resource Corp.

Cemented Target:

27/05/2008 28/11/2008 Foreman: Wally Magnusson Storage: East West Reource Corporation - 1158a Russell SI. Thunder Bay,

Logged by: Neal Bennett Checked by: R.S. Middleton Comments:

Lithology

Overburden

Code

14

Page 1 of 2

From

0.00

To

10.00

Lithology

Overburden

Overburden.

Consists of sand, gravel and boulders.

Code

14

RG-08-01

Boulders consist of medium to coarse grained reddish pink syenite, white/black to pink granite, mafic pillow lavas (med green fine granied with hematitic alt at selveges).

Hole had to be abandoned due to complications drilling through overburden. Hole was relocated to RG-08-02 location where the drill was set up on bedrock. The targeted magnetic high still remained the same as did the azimuth and dip of the planned hole. Hole RG-08-02 which was the substitute is northeast of the planned location for hole RG-08-01.

Page 2 of 2

Sample From To Width

Hole rD; RG-08-02 Project: Red Granite Grid X: Easting: 350313.00 Grid Y: Northing; 5560554.00

Drill Start: 22/04/2008 Log Start: Drll Finish: 21/05/2008 Log Finish:

P7B 5N2

UTM Zone: 16 Datum: NAD83

14/05/2008 16/05/2008

RG-08-02

Year 2008 Grid Azimuth: True Azimuth: 110

Claim: 4225947

Dip -50

Elev (m): 0.00

Drill Company: Custom Diamond Drilling Foreman: Wally Magnusson

TWP: Pillar Lake Length: 124.36 Casing: left in Cemented Core Size: Ba Casing (m): 3.23 Target:

Drilled for: EAST WEST RESOURCES CORPORATION Storage: East West Resource office-1158 Russell Street Thunder Bay, ON

Surveyed Logged by: Matt Husslage Checked by: EAST WEST RESOURCES Comments:

From To

0.00 3.23

3.23 6767

67.67 108.62

108.62 124.36

Lithology

Overburden

Diabase

Mafic Lava

Syenite

Code

14

13

2b

10b

Page 1 of2

From

0.00

3.23

67.67

To

323

67.67

Lithology

Overburden

Diabase

Code

14

13

RG-08-02

A fine texture of euhedrallath shaped plagioclase crystals set in a finer matrix of pyroxene (diabasic texture).

10862 Mafic Lava 2b

Some sections contain pillowed lava structures and flow top breccia massive layers. Really brecciated, large clasts (2.5cm->1mm) in a fine grained matrix.

Mineralogy- plagioclase, pyroxene, and olivine. Mineral grain size makes it difficult to determine percantages to whole rock.

Textures- Phenocrysts of plagioclase in a finer grained, almost glassy matrix.

Mi neralization 108.00 11918 Min % Style

Py o Disseminated

108.62 124.36 Syenite 10b

Light baige to pink coloruing, with medium to coarse grained (-Zmm) minerals with a uniform homogeneous equigranular texture. Colour variation (beige/pink to pink/red) appears as a function of alteration close to fractures and appears gradational. Very little quartz «5%) and very little plagioclase «10%). Abundant feldspar present

Page 2 of 2


MAG DATA - RG-OB-02

Depth IMag (1U Depth IMag (10 Depth IMag (10 Depth iMag (10 Depth IMag (1U

(tt) 6CGS) (tt) 6CGS) (tt) 6CGS) (tt) 6 CGS) (tt) 6CGS)

12 1010 131 900 258 0 15 1060 135 1060 261 0 18 1000 138 1050 EOH EOH

21 870 141 1220 24 1000 144 780 27 1010 147 500 30 1000 l150 1260 33 700 152 1100 36 850 155 [ 1055 39 970 158 540 42 980 162 430 45 700 165 700 49 940 168 800 52 930 171 500 55 790 175 900 58 990 178 1080 62 1030 181 1040 64 1180 185 400 67 1020 188 540 70 900 192 620 73 1000 195 710

950 198 700 79 900 201 1020 82 930 205 530 85 1030 208 490 87 840 211 800 89 950 214 720 92 1000 217 1610 95 1000 220 870

d9D 960 223 10 10 1000 226 10 103 730 229 20 106 1010 232 900 109 800 235 100 112 900 239 50 115 900 242 a 118 1000 245 0 121 1200 248 0 125 1000 252 0 128 1050 255 0

Hole 10: RG-08-03 Grid X:

GridY:

Drill Start: Drll Finish:

P7B 5N2 Surveyed

From

0.00

3.00

47.10

10500

106.00

126.22

12700

172.56

17315

To

300

47.10

105.00

106.00

126.22

127.00

172.56

173.15

202.61

Project: Red Granite Easting; 349198.00 Northing: 5564980.00

21/05/2008 Log Start: 18/06/2008 Log Finish:

UTMZone: 16 Datum: NAD 83

14/0712008

17/07/2008

RG-08-03

Year 2008 Grid Azimuth; True Azimuth: 340

Claim: Dip Elev (m):

3016737 -65

Drill Company: Custon Diamond Drilling Foreman: Wally Magnussen

Logged by: Matt Husslage Checked by: Paul Nielsen

Lithology

Overburden

Mafic Lava

Gabbro

Troctolite

Gabbro

Troctolite

Gabbro

Troctolite

Gabbro

Code

14

2b

7ac

7b

7ac

7b

7ac

7b

7ac

Page 1 of 5

TWP: Pillar Lake Length: 202.61 Casing: left in Cemented Core Size: SO Casing (m): 3 Target:

Drilled for: EAST WEST RESOURCES CORPORATION Storage: East West Resource office- 1158 Russell Street Thunder Say, ON

Comments:

From

0.00

3.00

47.10

To

3.00

47.10

Lithology

Overburden

Mafic Lava

Code

14

2b

RG-08-03

The core itself is really broken up. Some sections contain pillowed lava structures and flow top breccia massive layers. Really brecciated. large clasts (2.5cm->lmm) in a fine grained matrix. An abundance of hematitization occuring in the upper section.

Mineralogy- plagioclase, pyroxene, and olivine. Mineral grain size makes it difficult to determine percantages to whole rock.

Textures- Phenocrysts of plagioclase in a finer grained, almost glassy matrix.

105.00 Gabbro 7ac

Mineralogy- Feldspar, pyroxene, olivine, and magnetite (fine grained) Overall the the mineral composition is dominately mafic at arounbd 60% mafic to the whole rock. An unknown mineral occurs from 5230m-52.S0m. It occurs sporadically at 20% to the whole rock. It has a brownish red colour and has a equigranualar texture.

Texture- uniform equigranular. Black to dark grey in colour, medium grained (-2-3 mm) with fine grained magnetite.

Alteration occurs from the contact at 47.10m to ~54m. Hematite staining occurs pervasively as does chlorite and serpentization, occuring locafly to tiny (1-2mm) veintlets. Also serpentine veins occur sporadicafly throughout this unit.

At 90m, at 30 deg to CA At 94m, at 60 deg to CA. At 94.64m-94.70m- very fractured, occurres with chlorite At 95m, occurs with a calcite vein at 75 deg to CA.

Below is a list of the location where pegmatites cut the gabbro unit, along with theif thickness and COfe angle at which they cut

Location (m)fThickness (cm)/Angle to CA

59.40/5/50 66.77/15/25 68,50/20/35 75.40/6145 88.4011155 89.5011/65 90.57f87/NA- hard to distingush, assimilates parts of the gabbro 93.77/3/60- heavily fractured section. 97.32/28/75- this pegmatite has amphibole margin contacts! coarse grained hornblende devleoping around contacts. 101.41/4/65

Aplite dikes cut the gabbro at various locations, Mineral composition is quartz and feldspar and is fine grained.

Location (m)lThickness (cm)iAngle to CA

75.51/5/0- some xenoliths of gabbro present 98.05/11/75· sharp contacts


115.48/10/0 131.12/10/70 173.96/17/0- chill margins visible.

Page 2 of 5

Throughout the gabbro units grain size changes. See grain size changes throughout the log for description.

Mineralization 53.20 54.08 Min % Style

Py Disseminated Trave amount of fine grained pyrite, occuring disseminated.

61.00 62.00 Min % Style Py ° Disseminated Trace amount present

81.00 98.04 Min % Style Py o disseminated Trace amount present.

98.35 111.00 Min % Style Py ° disseminated Py:Po (4:1) trave amounts.

Po 0 disseminated

From 106.00

RG-08-03 To Lithology Code Troctolite7b

Mineralogy- Variable amount of olivine. plagioclase and minor amount of pyroxenes.

106.00 126.22 Gabbro 7ac

Same as gabbro unit above.

Grain size changes:

106. 15m-112.72m- gradual change from coarse to fine, from 112.72 till 119.23m the grain size is coarse.

Pegmatites cut at;

106.10m-106.15m at an angle of 0 deg. 108.62m-108.67m at an angle of 45 deg.

Mineralization 112.00 123.51 Min % Style

Py o disseminated Trace amount

Sample From To Width 105.00

From To Lithology Code

126.22 127.00 Troctolite 7b

Same composition as previous Troctolite.

127.00 172.56 Gabbro 7ae

Same as previous gabbro unit.

Grain size changes:

127m-134.41m- medium grained, gradual change to next unit. 134.41m-137m- fine grained, gradual change to next unit. 137m-138.33- coarse grained, sharp contact to next unit. 138.33m-141.12m- gradually becomes fine grained. 141.12m-145m- becomes coarse for this section. 145m-153.76m- becomes medium grained. 153.76m-159m- becomes coarse grained. 159m-161m- becomes fine grained 161m-167m- becomes medium grained. 167m-169m- becomes fine grained.

Pegmatites cut this unit at Location (m)fThickness (cm)/Angle to CA

129.54/1/40 149.54/10/30 153.14/7/70 151.35170/NA 172.38/10/70

Mineralization 130.20 134.63 Min

Py

138.10 147.17 Min Py

150.00 173.92 Min Py

% Style o Disseminated

% Style o disseminated

% Style o disseminated

Page 3 of 5

RG-08-03 Sample From To Width

Hole From To Lithology 172.56 173.15 Troctolite

Same composition as previous Troctolite.

173.15 202.61 Gabbro

Same as the other gabbro units.

Code 7b

7ac

Page 4 of 5

RG-08-03

An aplite cuts this unit at 190m for .75m. This section cuts the gabbro at 70 deg to CA.

173.15m-176.1Sm- medium grained. 176.1Sm-177.55m- fine grained. 177 .55m-181 .45m- Coarse grained.

All grain size changes are gradual.

sample From To Width

MAG DATA - RG-OB-03

Depth Mag (1U Depth iMag (1U Depth IMag (1U Depth Mag (1U Depth IMag (10

(m) 6CGS) (m) 6CGS) (m) 6CGS) (m) 6CGS) (m) 6CGS)

1 0 41 420 81 3200 121 2473 161 2310 2 0 42 218 82 8580 122 3600 162 2380 3 658 43 321 83 8054 123 5876 163 2050 4 1410 44 10 84 4160 124 5981 164 1535 5 2527 45 38 85 8701 125 7072 165 3200 6 1167 46 10 86 12820 126 9583 166 2322 7 862 47 1770 87 2927 127 8475 167 613 8 963 48 3269 88 1000 128 6522 168 4437 9 690 49 3093 89 1600 129 6063 169 608 10 310 50 2240 90 6939 130 4425 170 1640 11 450 51 67 91 3 131 10780 171 3390 12 322 52 109 92 5596 132 5155 172 7179 13 289 53 3063 93 3708 133 2601 173 7502 14 50 54 7485 94 12430 134 5650 174 312 15 21 55 1200 95 6931 135 7770 175 3867 16 190 56 12750 96 3780 136 3290 176 2780 17 93 57 4321 97 13660 137 3890 177 1080 18 348 58 6200 98 7100 138 4710 178 868 19 278 59 5242 99 7555 139 1640 179 2010 20 168 60 2920 100 6167 140 3510 180 2067 21 120 61 11000 101 9330 141 2320 181 4500 22 124 62 8900 102 5950 142 4180 182 295 23 35 63 14560 103 2140 143 6560 183 1102 24 648 64 8545 104 8462 144 8770 184 35 25 359 65 13600 105 9188 145 1980 185 60 26 545 66 15500 106 8600 146 3300 186 51 27 550 67 8700 107 7500 147 900 187 26 28 83 68 12000 108 1000 148 4320 188 28 29 322 69 11000 109 9783 149 2940 189 29 30 286 70 13440 110 3470 160 190 11 31 480 71 11500 111 11190 151 2210 191 15 32 151 72

~ 112 9200 152 4720 192 15

33 11 73 113 3108 153 7980 193 10 34 3 74 14690 114 5069 154 340 194 71 35 4 75 9800 115 5755 155 44 195 86 36 97 76 12400 116 8373 156 4040 196 62 37 11 77 6400 117 4130 157 290 197 15 38 1 78 6110 118 3390 158 4040 1981 15 39 280 79 3440 119 13200 159 1050 199 117 40 23 80 4746 120 6833 160 2490 200 160

Hole 10: RG-08-04 Grid X: GridY:

Drill Start: Dnl Finish:

P7B 5N2 Surveyed

Survey

From

0.00

22.86

45.72

60.66

64.01

70.56

8260

92.35

97.38

101.35

102.75

104.24

106.22

110.64

114.91

125.58

125.88

127.10

128.78

13305

134.72

To

22.86

45.72

60.66

64.01

70.56

82.60

92.35

97.38

101.35

102.75

104.24

106.22

110.64

114.91

125.58

125.88

127.10

128.78

133.05

134.72

139.06

Project: Red Granite Easting: 349242.00 Northing: 5565182.00

18/0612008 Log Start: 16/10/2008 Log Finish:

UTM Zone: 16 Datum: NAD83

20/10/2008 25/10/2008

Logged by: Matt Husslage/Bob

RG-08-04

Year 2008 Grid Azimuth: True Azimuth: 0

Claim: 3016736 Dip -50 Elev(m):

Drill Company: Custom Diamond Drilling Foreman: Wally Magnussen

Checked by: Paul Nielsen

Depth

207.00 477.00

Test

ACID ACID

Azimuth Dip Mag Field Mag Units Comments

Lithology

Overburden

Lava

Olivine Gabbro (Wawaig Complex)

Coarse Grained Gabbro

Medium Grained Gabbro




Fine Grained Gabbro

Coarse Grained phases




Fine Grained (Diabase?)


Pegmatite

Medium to coarse grained Gabbro

Fine grained, grey Diabase?

Medium to coarse grained gabbro

Fine grained gabbro


52

Code

14

2b

7ac

7ac

7ac

7ae

7ae

7ae

7ac

7ae

7ac

7ac

7ac

13

7ae

1Qf

7ac

13

7ae

7ae

7ae

139.06 139.29 Fine Grained grey-black diabase? Gabbro 13

139.29 140.21 Medium Grained Gabbro 7ae

Page 1 of 10

TWP: Pillar Lake Length: 282.55 Casing: feft in Cemented Core Size: BO Casing (m): 22.7 Target:

Drilled for: EAST WEST RESOURCES CORPORATION

Storage: East West Resource office- 1158 Russell Street Thunder Bay, ON

Comments:

RG-OS-04 From To Lithology Code 140.21 140.36 Fine Grained Gabbro 7ac

140.36 144.17 Medium Grained Gabbro 7ac

144.17 144.48 Fine Grained Gabbro 7ac

144.48 151.10 Coarse Grained Gabbro 7ac

151.10 153.92 Medium Grained Olivine Gabbro 7ac

153.92 15408 Apalite or Porphyry dike 8d


154.49 154.73 Apalite or Porphyry 8d


173.43 176.88 Medium Grianed Gabbro 7ae

176.88 179.68 Coarse grained gabbro 7ae

179.68 198.42 Fine to Medium grained gabbro 7ac

198.42 213.42 Coarse grained leucocratie gabbro 7ae

213.42 244.75 Fine grained gabbro 7ae


245.58 282.55 Fine grained gabbro 7ac

Page 2 of 10

From

0.00

22.86

45.72

To

22.86

45.72

60.66

53.10

53.34

53.37

53.64

53.83

57.42

57.97

58.46

58.85

59.44

5962

Lithology

Overburden

Code

14

RG-08-04

Sand and boulders (gneiss, lava, and altered porphyryr). Casing is to 16.76m, and cement is to 22.86m.

Lava 2b

Lava, grey with pink hematized patches, Haloclastite zone, flow top breccia.

Olivine Gabbro (Wawaig Complex) 7ac

Olivine Gabbro (wawiag complex) cut by dikes and veins of red altered porphyry and pegmatites. Hornblende developed along contacts. Starts as a medium to fine grained gabbro, minor chlorite veining at 50° to core axis. Red hematite spots to 170' in gabbro surface at 50' to 155' may be weathered. Becomes coarse grained at 99' in contact with pegmatite.

53.10 Felsic Intrusive 10

Pink coloured veinlet 1 cm wide.


Pinkish red vein let with fine grained chill margins.





58.59 Felsic Intrusive 10 Whitish cream coloured vein.


Light reddish/pink colour.


59.44 Felsic Intrusive 10 Light pink colour.


Light pink/red with gabbro blebs within interval.

59.71 59.89 Felsic Intrusive 10

Series of veins 1-4cm in width. Veins are whitish pink with contacts @ 45 degrees to core axis.


From 64.01

64.01

70.56

Page 3 of 10 59.92 59.98 Felsic Intrusive 10

Veinlets 05-1.0cm in width and are whitish pink in colour.

60.38 6075 Felsic Intrusive 10 Gabbro sections in between veins of felsic intrusive. Whitish pink/red in colour.

RG-08-04 To lithology Code

7ac Coarse Grained Gabbro

Coarse grained gabbro with biotite mica developed (wet phase}.


Vein lets 0.5-3.0cm with contacts ranging from 45-90 degrees to core axis and are pinkish red in colour.


6364

70.56

6404

68.21

82.60

Contacts @ 25 degrees to core axis. Large mica grains (1 cm) within pinkish felsic intrusive.

63.67 Felsic Intrusive 10 Whitish pink in colour.

Medium Grained Gabbro 7ac

Medium grained olivine gabbro, sharp upper contact at 85° to core axis. Becomes coarser downhole with mica appearing.

64.05 Felsic Intrusive 10 Vein lets O.5cm to 1cm wide.

68.24 Felsic Intrusive 10 Pinkish white in colour.

Coarse Grained Gabbro 7ac

Coarse grained gabbro, large mica flakes becomes greenish on dry surfaces. Lower contact 85" to core axis. Occasional pegmatite dikes.

73.40 73.43 Felsic Intrusive 10 Whitish grey veinlets 0.5-1.0cm in width. Contacts about 45 degrees to core axis.


Whitish grey with coarse mica grains.

77.91 78.00 Felsic Intrusive 10 Whitish colour with large micas up to 0.5cm at the vein margins.

79.89 80.19 Felsic Intrusive 10 Whitish colour with large micas up to 0.5cm at the vein margins.

80.83 81.26 Felsic Intrusive 10 Whitish colour with large micas and gabbro sections in between veinlets.


Drill Hole From

82.60

To

92.35

Lithology


Code

7ac

Page 4 of 10

RG-08-04

Medium grained gabbro becoming coarser to depth. Almost gradational into coarser gabbro below 303'.

85.95 85.98 Felsic Intrusive 10 Whitish colour with large mica grainsat margins.

86.90 87.17 Felsic Intrusive 10 Whitish colour with large mica grains at margins.

88.21 88.57 Felsic Intrusive 10 Whitish colour with large mica grains at margins.

88.91 89.03 Felsic Intrusive 10 3-5cm wide veinlets with contacts at 30 degrees to core axis.

90.07 90.08 Felsic Intrusive 10 Whitish grey intersecting core axis at 55 degrees.


93.54 93.67 Felsic Intrusive 10 Whitish fine grained with micas present at lower contact.


Fine grained gabbro, contact 90° to core axis, grades to medium grained gabbro.

101.35 102.75 Coarse Grained phases 7ac

Coarse grained phase or patches.

102.75 10424 Medium Grained Gabbro 7ac

Medium grained gabbro, contact 85° to core axis.

104.24 106.22 Coarse Grained Gabbro 7ae

Sharp contact 85° to core axis with coarse grained.


White with micas present at vein margins.


Drill Holf:' From To 106.22 110.64

Lithology Medium Grained Gabbro

Medium grained with 6" finer grained margin.

Code 7ac


Whitish grey 2cm vein.

110.64 114.91 Fine Grained (Diabase?) 13

Page 5 of 10

RG-08-04

Fine grained (diabase?) l' wide margin, 70 0 to core axis, grades into medium grained.

376 to 377 Fine grained grey, contact 88-90 0 to core axis, may be a dike, diabase? Cut by 3mm chlorite vein at 20 0 to core axis.

112.47 112.50 Felsic Intrusive

Whitish grey 2cm vein.

10

114.12 114.54 Felsiclntrusive 10

White with coarse mica grains and coarse grained gabbro blebs.

114.91 125.58 Medium Grained Gabbro

Starts as medium to coarse grained gabbro.


10% White Felsic Intrusive veins over interval.


7ac

10

10 Coarse white patchy veins with minor to moderate epidote alteration.


118.66

119.18

119.42

120.46

120.79

121.31

3 White coarse and 3 reddish very fine grained 1-2cm veins in this interval intersecting core axis at 75-90 degrees.


Whitish grey felsic intrusive vein.




Greyish felsic intrusive vein.


Greyish felsic intrusive vein.


Whitish grey felsic intrusive.


Whitish grey coarse grained felsic intrusive vein,

123.41 123,57 Felsic Intrusive 10 2 veins within interval ranging from 2-5cm in width,

123,75 123.76 Felsic Intrusive 10 Whitish grey coarse grained felsic intrusive vein,

124,15 124.42 Felsic Intrusive 10f Pegmalitic vein; whitish grey with minor pink k-spars present

From 125.88

To Lithology Pegmatite

RG-OS-04 Code 10f

Fine grained grey, 1 em pegmatite cuts at lower contact, 90· to core axis,

125,88 127,10 Medium to coarse grained Gabbro 7ac

Medium 10 coarse grained, minor sulphides.

127.10 128.78 Fine grained, grey Diabase? 13

Fine grained, grey.

128.78 133.05 Medium to coarse grained gabbro 7ac

Medium to coarse grained.

128.99 129,39 Felsic Intrusive 10 Mottled black and whitish grey with pink k-spars

131,37 131,67 Felsic Intrusive 10 White coarse grained felsic intrusive with biotite.

133.05 134.72 Fine grained gabbro 7ac

Fine grained, 88° to core axis, grey,

134,72 139.06 Coarse Grained Gabbro 7ac

Page 6 of 10

122.56 122,83 Felsic Intrusive 10


Page 7 of 10

DrW Hole RG-08-04 From To Lithology Code Sample From To Width 139.06 139.29 Fine Grained grey-black diabase? Gabbro 13



Fine grained gabbro, 90° to core axis, upper contact




Fine grained, 90° to core axis, contacts.


144.48 144.54 Felsic Intrusive 10 White coarse grained felsic intrusive

144.63 144.66 Felsic Intrusive 10 Grey fine grained with coarse biotite grains at vein margins.

147.55 147.58 Felsic Intrusive 10 Whitish grey felsic intrusive

148.47 148.77 Felsic Intrusive 10 Whitish with orange rusting stains along fractures.

148.93 148.78 Felsic Intrusive 10 Whitish Grey.

149.50 149.53 Felsic Intrusive 10 Whitish Grey

150.11 150.27 Felsic Intrusive 10f White to grey feldspathic pegmatite.

Drill Hole From 153.92

To Lithology Medium Grained Olivine Gabbro

153.92 154.08 Apalite or Porphyry dike

154.08 154.49 Medium Grained Gabbro

Code 7ac

ad

7ac


Grey fine grained felsic intrusive with black/brown biotite and mottled texture.

154.49 154.73 Apalite or Porphyry ad

Aplite or porphyry, fine grained, white pink, contact 80° to core axis.


Page 8 of 10


RG-08-04

Mineralization- At 567'10"- 1 coarse size grain (1.5cm across) of pyrite occurs. At 569' a whispy coarse grain of pyrite occurs. At 541'11" a coarse size grain of pyrite occurs.

Pegmatite with possible carbonate material and cavities occurs at 534'2"-534'9", cuts the core axis at 50 deg.

173.43 176.88 Medium Grianed Gabbro 7ac

Medium grained gabbro with agmatite texture.

Below is a list of location of several pegmatites cutting the gabbro. Location(feet)/thickness(cm)/angle to core axis 570'1 "/6/40 571 '11 "/2.5/40 573'2"/8/15 576'/2/20

176.88 179.68 Coarse grained gabbro 7ac

Coarse grained gabbro with agmatite.

Below is a list of location of several pegmatites cutting the gabbro. Location(feet)/thickness(cm)/angle to core axis

581 '7"/20/1 0 589' 1 "/1511 0

10

Sample From To Width151.10

Drill From To

591'15/40 608'15/45 642"/15/65

Lithology RG-08-04

Code

179.68 19S.42 Fine to Medium grained gabbro 7ae

Below is a list of location of several pegmatites cutting the gabbro. Location(feet)lthickness(cm)/angle to core axis

597'15/40 60S'/5/45 642"/15/65

Page 9 of 10

Mineralization- Fine grain of Po at 594'7". From 643'-660' disseminated pyrite occurs, trace amount.

198.42 213.42 Coarse grained leueoeratie gabbro 7ae

This Unit is different from all the other gabbro units as it contains more quartz and feldspar, giving it a light grey colour.

At 677' a cave In occurred with pebbles falling into the hole.

There is a chill margin at the contact with the unit below.

213.42 244.75 Fine grained gabbro 7ae


245.5S 282.55 Fine grained gabbro 7ae

A large vein of magnetite occurs at SOT. It is 1.5c thick and cuts the core at 0 deg to CA.


Depth (tt)

63 68 72 76 79 82 85 88 91 92 95 98 101 102 114 117 120 123 124 127 130 133 136 137 140 141 144 147 148 151 154 157 160 163 166 167 170 173 176 177

o o o

437 644 o

320 o

369 8 2

349 280

2 2

o 561 o 5

1050 o o o

631 724

859 o o o o o 3

649 701 1508 3680 120 700

2941 2821 427 o o

210 356 213 3905 216 4341 217 6645 220 9014 223 9491 226 11940 227 13420 230 11780 233 3744 236 242 237 4577

247 250 253 256 257 260 263

276 277 280

MAG DATA - RG-08-04

283 1562 380 5771 480 1708 286 60 383 9066 483 2177 287 3 386 1071 486 2025 290 o 387 4957 487 2263 293 3 390 1306 490 1983

393 7461 493 o 396 2524 496 1302 397 2287 497 83 400 2009 500 7487

37 403 o 503 3699 948 406 1268 506 7272

307 o 407 1865 507 348

310 1300 410 2118 510 1636 313 1800 413 1835 513 11120 316 3842 416 105 516 8810 317 1750 417 1487 519 11700 320 791 420 2109 522 5821 323 2125 423 11 525 11410 326 4583 426 1610 528 1410 327 3363 427 1594 531 12710 330 1154 430 2217 534 228 333 4263 433 2337 537 9382 336 765 436 4106 540 6450 337 548 437 1670 543 6180

440 3007 546 7632 443 4362 549 1664 446 4904 552 203 447 3969 555 2875 450 1156 558 233

9415 453 1480 561 1957 4206 456 2469 564 8564 4565 457 3150 567 4055 3588 460 4430 570 7913 5592 463 7547 573 5559 7452 466 7745 576 3796 8570 467 5191 579 4424

370 7910 470 2402 373 9202 473 8793 376 5170 476 942

277 9492 477 1610

MAG DATA - RG-08-04

Depth Mag (10 Depth Mag (10· Depth Mag (10 Depth Mag (10 Depth Mag (10 (ft) 6 CGS) (ft) 6 CGS) (ft) 6 CGS) (ft) 6 CGS) (ft) 6 CGS)

1---'-5...:..94--+--.;;2;;.,;;0...;,.14 __ +-7_1_2-+_1;;.,;;3...;,.27_+--8-,-29 10120

597 1411 715 8950 m8097

_9...;,.1...:..7_9-+_71...:..8-+_6...:..2...:..34~+- ~2...:..0~~-~ ____ -;----+-----~ 10280 721 8795 9466 5013 724 9165 841

727 8660 844 613 3100 730 11970 847 6777

....§.!ti 4636 733 12100 850 9145

~ 2460 736 6349 853 8810 622 10640 739 9286 856 1926 625 10640 742 10750 859 4425

628 I 106;;";;6~_~-+ __ ;~"':";--+ __ :_:~"':"9~"':":~~:"':"~~~ __ 1"':":;;;";;O~"':"~~~ __ +-____ -+ ____ +-____ -;

637 9637 754 8530 871 7963 640 1081-5 757 10600 874 6696 643 11000 760 4064 877 12470 646 8520 763 8872 880 6 649 766 9965 883 9049 652 53 769 5369 886 5946

---;----~--~--655 1486 772 12 5449

658 1578 775 8720 3550_f--_-I-___ -+ __ ~---I 661 3594 778 11250 8 664 286 781 4609 836 667 2620 784 11020 901 2466 670 3550 787 11050 904 2896 673 1531 790 7500 907 2616 676 1272 793 1133 910 6074 679 974 796 3196 913 3067 682 582 799 1310 916 997 685 1790 802 2070 919 1680 688 1684 805 809 922 534 7 691 1663 808 9199 925 5090 694 ==-3;;";;7"':"67"':"-+-"':"81;;";;1-~-7"':"7;;";;7"':"7~~9~27~--2~5~5"':"0~~--+-----~----~-----1

697 217 814 7763 EOH EOH 700 791 817 6604 703 8008 820 4964 706 6468 823 11900 709 3086 826 11050

APPENDIXD

Drill Hole Plan Map (1: 10,000)

Drill Hole Cross Sections:

RG-08-01 (1:200) RG-08-02 (1 :200) RG-08-03 (1 :200) RG-08-04 (1 :250)

APPENDIXE

Drill Core Assay Certificates & Sample Intervals

ALS Chemex To EAST WEST RESOURCE CORPORATION 1158 RUSSELL STREET

Page: 1 Finalized Date: 1B-JUN-200B

Account: NMZ EXCELLENCE IN ANAL YTICAL CHEMISTRY AlS Canada Lltt

THUNDER BAY ON P7B 5N2

Project RG-08-02

P.O. No.:

212 Brooksbank Avenue North Vancouver BC V7 J 2C 1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com

CERTIFICATE TB08074711

This report is for 11 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 6-JUN-200S.

The following have access to data associated with this certificate:

TWEST - GENERAL WEB ACCO NEAL BENNETT I BOB MIDDLETON I PAUL NIELSON

To: EAST WEST RESOURCE CORPORATION ATTN: NEAL BENNEIT 1158 RUSSELL STREET THUNDER BAY aN P7B 5N2

ALSCODE

WEI-21

CRU-QC PUL-QC

LOG-22

CRU-31

SPL·21

PUL·31

ALS CODE

ME·MS81

ME·XRF06

OA·GRA06

This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release.

SAMPLE PREPARATION DESCRIPTION

Received Sample Weight Crushing QC Test

Pulverizing QC Test

Sample login Red wlo BarCode

Fine crushing 70% <2mm

Split sample riffle splitter

Pulverize split to 85% <75 um

ANAL YTICAL PROCEDURES DESCRIPTION INSTRUMENT

38 element fusion ICP-MS ICP·MS

Whole Rock Package - XRF XRF LOI for ME-XRF06 WST·SIM

Signature: ~-------------Colin Ramshaw, Vancouver Laboratory Manager

Method Analyle

Units Sample Description LOR

Gl34751 G134752 G134753 G134754 G134755

G134756 G134757 G134758 G134759 G134760

G134761

ALS Chemex EXCELLENCE IN ANAL YTICAL CHEMISTRY ALS Canada Ltd,

212 Brooksbank Avenue North Vancouver Be V7 J 2Cl Phone: 604 984 0221 Fax: 604 984 0218 www,alschemex.Com

WEI-21 ME-MGBl ME-MS81 ME-MS81 ME-MS81 ME-MSB1

RecvdWt. Ag Ba Ce Co Cr

kg ppm ppm ppm ppm ppm

0,02 1 O,S 0.5 0.5 10

1,74 <1 16.1 46.2 4.5 <10 1,61 <1 10,5 68,4 5,3 <10 1,90 <1 221 143.0 4.4 <10 2,44 <1 130,0 54.4 2.9 <10 1.79 <1 223 184.5 1,6 <10

1.82 <1 282 73.5 2,3 <10 1,61 <1 111,5 152.0 3.1 <10 2,00 <1 239 53.2 2,0 <10 1,78 <1 164,5 63,1 2.2 <10 1.83 <1 202 191,5 1.4 <10

1,57 <1 114.0 55,7 1,0 <10

To: EAST WEST RESOURCE CORPORATION 1158 RUSSELL STREET THUNDER SAY ON P7S 5N2

Project: RG-08-02

I CERTIFICATE OF ANALYSIS

ME-MSB1 ME-MSBl ME-MS81 ME-MS81 ME-MS81 ME-MSB1

Cs Cu Dy Er Eu Gil

ppm ppm ppm ppm ppm ppm

0.01 5 0.05 0.03 0.03 0.1

0,09 47 6,94 4.95 0.49 22,5 0,35 29 7,90 5,22 0,51 27.1 1,24 22 915 6,07 0.69 29,9 1,27 8 6,51 4,72 0,51 30.0 1.24 <5 8.74 5,93 0.76 34.5

1,13 <5 7.16 5.16 0,56 31,0 1.44 13 9,87 6,76 0,74 29,3 1,21 9 11,65 8.08 0.58 26.5 1.30 <5 11,85 8.39 0,52 32.8 2.40 <5 14.40 9.85 0,71 30.9

1.67 <5 11,65 8,09 0.47 33.2

Page: 2-A Total # Pages: 2 (A - D)

Finalized Date; 18·JUN-2008 Account: NMZ

T808074711

ME-MS81 ME-MS81 ME-MSB1

Go HI Ho ppm ppm ppm

0.05 0.2 0.01

5.74 24.7 1.59 7,43 23,3 1,73 9,63 25.5 2,00 5,64 24.4 1.51 10,15 26.2 196

6,46 25.4 1.62 10.80 27,3 2.20 8,85 27,8 2,66 8,38 28.8 2,74 13,35 25,6 3,28

8.58 27,6 2,67

Method An.lyte


G134751 Gl34752 G134753 G134754 G134755

G134756 G134757 Gl34758 G134759 G134760

GI34761



ME-MS61 ME-MS81 ME·MS81 ME·MS81 ME-MS81 ME-MS81

La Lu MO Nb Nd Ni


0,5 0,01 2 0.2 0.1 5

17.7 0.91 <2 269 19.0 <5 32.9 0.93 <2 256 29.9 <5 68.7 1.10 <2 295 50.5 <5 26.2 0.92 <2 268 21.7 <5

92.1 1.07 <2 290 60.4 <5

32.6 1.00 <2 289 27.8 <5 77.6 1.23 <2 308 55.9 <5 24.1 1.41 <2 307 26.0 <5 28.2 1.55 <2 310 27,2 <5 87.2 1.61 <2 276 68.2 <5

23.5 1.44 <2 309 24.1 <5

To: EAST WEST RESOURCE CORPORATION 1158 RUSSELL STREET THUNDER SAY ON P7S 5N2

Project: RG-08-02

I CERTIFICA TE OF ANALYSIS

ME-MS81 ME-MS81 ME·MS81 ME-MS81 ME·MS81 ME-MS81

Pb Pr Rb Sm Sn Sr


5 0.03 0.2 0.03 1 0.1

<5 4.95 5.5 5.57 5 25.6 <5 7.75 20.2 7.82 5 26,2 <5 15.10 191.0 10,00 7 41,3 <5 6.07 140.5 5.34 8 37.9 <5 18.50 268 10.75 8 27.9

<5 7.98 216 6.47 8 39.2 <5 16.20 111.5 11.25 8 40,3 <5 6.60 158.0 8.50 7 45.4 <5 7.32 170.5 7.75 9 37.4 <5 19.75 187.5 13,95 11 43.8

<5 6.19 111.5 B.Q6 9 33.1

Page: 2 - S Total # Pages: 2 (A - D)

Finalized Date: 18-JUN-2008 Account: NMZ

TB08074711

ME-MS81 ME-MS81 ME-MS81

Ta Tb Th

ppm ppm ppm 0.1 0.01 0,05

13.3 1.10 56.7 13.3 1.33 57.0 14.4 1.58 66.4 14.4 1.02 63,3 14.7 1.54 68.2

14.3 1.14 60.7 15.3 1.68 66.3 16.1 1.83 70.8 16.9 1,76 69.2 15.6 2.28 58.2

17.1 1.80 67.9

Metflod Analyte


G134751 G134752 G134753 G134754 G134755

G134756 G134757 G134758 G134759 G134760

G134761

ALS Chemex EXCELLENCE IN ANAL YTICAL CHEMISTRY ALS Canada Ltd.

212 Brooksbank Avenue North Vancouver Be V7 J 2C 1 Phone: 604 984 0221 Fax 6049840218 www.alschemex,com

ME-MSBl ME-MS81 ME-MS81 ME-MSBl ME-MS81 ME-MS81

TI Tm U V W Y ppm ppm ppm ppm ppm ppm

0,5 0.01 0.05 5 1 0.5

1.0 0.83 3.64 20 5 37,2 0.6 0.88 4.01 14 4 40.4 <0.5 1.02 3.98 9 6 45.9 <0,5 0.81 4,04 7 7 40,6 <0,5 0,96 3,98 <5 8 48,0

<0,5 0.90 3,88 <5 7 40.8 <0,5 1,15 5.06 8 10 56.7 <0.5 1.37 4.65 5 9 60.2 <0,5 1.41 4.00 6 11 61.1 <0.5 1.64 4.60 <5 10 73.9

<0.5 1.41 5.52 <5 8 58.7

To: EAST WEST RESOURCE CORPORATION 1158 RUSSELL STREET THUNDER BAY ON P7B 5N2

Project RG-08-02


ME-MS81 ME-MS81 ME-MS81 ME-XRF06 ME-XRF06 ME-XRF06

Yb Zn Zr 8i02 AI203 Fe203 ppm ppm Pl'm % % %

0.03 5 2 0,01 0.01 0.01

5.44 16 935 5.77 24 875 6,66 21 939 5.32 22 884 6,39 26 967 67.85 15.71 1.58

5,81 36 931 7,50 58 986 8.75 41 1050 9.45 43 1060 10.60 30 959

9,10 23 1040

Page:2-C Total # Pages: 2 (A - D)

Finalized Date: 18·JUN-2008 Account: NMZ

T808074711

ME-XRF06 ME-XRF06 ME-)(RF06

CaO MgO Na20

% % %

0.01 0.01 0.01

0.18 1,96 2,84

Method Analym


G134751 Gl34752 G134753 G134754 G134755

G134756 G134757 Gl34758 G134759 G134760

G134761


212 Brooksbank Avenue North Vancouver Be V7 J 2C 1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com

ME·XRF06 ME-XRF06 ME-XRF06 ME-XRF06 ME-XRF06 ME-XRF06

K20 Cr203 TI02 MnO P205 srO

% % % % % %

0.01 0.01 0.01 0.D1 0.001 0.D1

6.65 0.02 0.25 0.01 0.017 <0.01


Project: RG-08-02


ME-XRF06 ME-XRF06 ME-XRF06

BaD LOI Total % % %

0.01 0.Q1 0.01

0.02 1.93 99.02

Page: 2 - D Total # Pages: 2 (A· D)

Finalized Date: 18·JUN·2008 Account: NMZ

TB08074711

Ticket #

G134762

G13~ G134

G134765

G134766

G134767

G134768

G134769

G134770

G134771

G134772

G134773

G134774

G134775

G134776

G134777

G134778

G134779

G134780

G134781

G134782

G134783

I G134784

G13

G134786

G134787

G134788

G134789

G134790

G134791

G134792

G134793

G134794

G134795

G134796

G134797

G134798

G134799

G134800

H421001

H421002

H4210

Red Granite Assay Data

Hole: RG-08-03

Meterage Length Assay Code

From To

61.00 62.00 1.00 XRF06, MS81, PGM 23

81.00 82.00 1.00 XRF06, MS81, PGM 23

83.51 84.54 I 1.03 PGM 23, ICP 41

85.34 8t:: C::'"l 1.18 XRF06, MS81, PGM 23

86.52 87.53 1.01 PGM 23, ICP 41

87.53 88.65 1.12 PGM 23, ICP 41

88.65 89.61 0.96 PGM 23, ICP 41

89.61 90.57 0.96 PGM 23, ICP 41

91.53 92.78 1.25 PGM 23, ICP 41

92.78 94.30 1.52 PGM 23, ICP 41

94.30 94.84 0.54 PGM 23, ICP 41

94.84 95.52 0.68 XRF06, MS81, PGM 23

95.52 96.33 0.81 PGM 23, ICP 41

96.33 96.85 0.52 PGM 23, ICP 41

96.85 97.32 0.47 XRF06, MS81, PGM 23

97.60 98.04 0.44 PGM 23, ICP 41

98.35 99.00 0.65 PGM 23, ICP 41

99.00 100.00 1.00 PGM 23, ICP 41

100.00 101.00 1.00 PGM 23, ICP 41

101.00 101.94 0.94 PGM 23, ICP 41

101.94 102.75 0.81 XRF06, MS81, PGM 23

102.75 103.73 0.98 PGM 23, ICP 41

103.73 104.80 1.07 PGM 23, ICP 41

04.80 105.75

t--%%! PGM 23, ICP 41

105.75 106.09 XRF06, MS81, PGM 23

106.15 107.15 1.00 PGM 23, ICP 41

107.15 108.07 0.92 PGM 23, ICP 41

108.07 109.09 1.02 PGM 23, ICP 41

109.09 109.40 0.31 PGM 23, ICP 41

109.40 110.05 0.65 XRF06, MS81, PGM 23

110.05 111.00 0.95 PGM 23, ICP 41

112.00 112.71 0.71 PGM 23, ICP 41

112.71 113.71 1.00 XRF06, MS81, PGM 23

113.71 114.71 1.00 PGM 23, ICP 41

114.71 115.48 0.77 PGM 23, ICP 41

115.58 116.55 0.97 PGM 23, ICP 41 116.55 117.06 0.51 PGM 23, ICP 41

117.06 118.24 1.18= PGM 23, ICP 41 118.24 119.24 1.00 XRF06, MS81, PGM 23

119.24 120.12 0.88 PGM 23, ICP 41 120.12 121.10 0.98 PGM 23, ICP 41

122.72 123.51 0.79 XRF06, MS81, PGM 23

I

H421004 130.20 131.12 0.92 PGM 23, lep 41 H421005 131.22 132.20 0.98 PGM 23, lep 41 H421006 133.17 134.17 1.00 XRF06, MS81, PGM 23 H421007 134.17 134.63 0.46 PGM 23, lep 41

138.10 139.10 1.00 PGM 23, lep 41 H421009 140.11 141.11 1.00 PGM 23, lep 41 H421010 141.11 142.18 1.07 PGM 23, lep 41 H421011 142.18 143.22 1.04 PGM 23, lep 41 H421012 1~44.19 0.97 PGM 23, lep 41 H421013 14 45.17 0.98 PGM 23, lep 41 H421014 145.17 146.17 1.00 PGM 23, lep 41

I H421015 146.17 147.17 1.00 PGM 23, lep 41 H421016 150.00 150.41 0.41 PGM 23, lep 41 H421017 150.41 151.33 0.92 PGM 23, lep 41 H421018 152.00 I 153.14 1.14 PGM 23, lep 41 H421019 153.24 153.56 0.32 PGM 23, lep 41

H421020 153.56 153.74 0.18 PGM 23, lep 41 H421021 155.48 156.60 1.12 XRF06, MS81, PGM 23 H421022 156.60 157.56 0.96 PGM 23, lep 41 H421023 157.56 1~R.58 1.02 PGM 23, lep 41 H421024 158.58 159.24 0.66 PGM 23, lep 41 H421025 159.24 160.24 1.00 PGM 23, lep 41 H421026 160.24 161.24 1.00 XRF06, MS81, PGM 23 H421027 161.24 162.24 1.00 PGM 23, lep 41 H421028 162.24 163.20 0.96 PGM 23, lep 41 H421029 163.20 164.20 1.00 PGM 23, lep 41

H421030 164.20 165.20 1.00 PGM 23, lep 41

H421031 165.20 166.20 1.00 PGM 23, lep 41

~032 168.31 169.31 1.00 PGM 23, lep 41

H421033 169.31 170.31 1.00 PGM 23, lep 41

H421034 172.92 173.92 1.00 PGM 23, lep 41

H421035 176.54 177.54 1.00 PGM 23, lep 41 H421036 180.00 181.00 1.00 PGM 23, lep 41 H421037 181.00 182.10 1.10 PGM 23, lep 41 H4210 3.00 1"'~ 0.20 PGM 23, MS81, XRF06, TS 193 H421039 201.26 201.90 0.64 PGM 23, lep 41 H421040 137.75 138.10 0.35 XRF06, MS81, PGM 23 H421041 139.10 140.11 1.01 PGM 23, lep 41 H421042 147.17 148.20 1.03 PGM 23, lep 41

TS 155.48 155.63 0.15 Thin Section

ALS Chemex To: EAST WEST RESOURCE CORPORATION 1158 RUSSELL STREET

Page: 1 Finalized Date: 8·JUL-2008

Account: NMZ EXCELLENCE IN ANAL YT/CAL CHEMISTRY THUNDER BAY ON P7B 5N2 ALS Canada Ltd

Project RG-08-3

P.O. No.:


CERTIFICATE T808084163

This report is for 18 Drill Core samples submitted to our lab in Thunder Bay, ON. Canada on 25-JUN-2008.

The following have access to data associated with this certificate: BOB MIDDLETON I PAUL NIELSON I TWEST - GENERAL WEB ACCO

To: EAST WEST RESOURCE CORPORATION ATTN: PAUL NIELSON 1158 RUSSELL STREET THUNDER BAY ON P7B 5N2

ALS CODE

WEI-21 LOG-22

CRU-31

CRU-QC

PUL-QC

SPL-21

PUL-31

ALSCODE

PGM-MS23

ME-ICP41

ME-XRF06

OA-GRA06

ME-MS81



Received Sample Weight

Sample login - Red wlo BarCode Fine crushing 70% <2mm

Crushing QC Test

Pulverizing QC Test




Pt, Pd. Au 30g FA ICP-MS ICP-MS

35 Element Aqua Regia ICP-AES ICP-AES Whole Rock Package - XRF XRF

LOI for ME-XRF06 WST-SIM

38 element fusion ICP-MS ICP-MS

Signature: ~---Colin Ramshaw, Vancouver Laboratory Manager

Method Analyle


G134782 G134783 G134784 G134785 G134786

G134787 Gl34788 G134789 G134790 G134791

8134792 G134793 8134794 G134795 Gl34796

G134797 G134798 G134799

ALS Chemex EXCELLENCE IN ANAL YT/CAL CHEMISTRY ALS Canada LId,


WEI-21 ME-XRF06 ME-XRF06 ME-XRF06 ME-XRF06 ME-XRF06

RecvdWt Si02 AI203 Fe203 CaO MgO

kg % % % % %

0,02 0,01 0,01 0,01 0,01 0,01

L58 43.47 17,29 13.62 10.44 8.59 1.97 1.95 1.96 0.69 42.01 16.40 15.61 11.11 6.54

2.07 1.87 1,93 0.71 1.31 46.03 17.74 11.33 11.03 8.84

3.94 1.58 2.21 44.00 14.74 13.73 12.65 7.51 2,16 1.76

2.09 1.09 2.45


Project: RG-08-3


ME-XRF06 ME-XRF06 ME-XRF06 ME-XRF06 ME-XRF06 ME-XRF06

Na20 K20 Cr203 Ti02 MnO P205

% % % % % %

0,01 0,01 001 0,01 0,01 0,001

2.36 0.37 0.02 1.35 0.17 1.137

2.31 0.41 0.03 2.67 0.16 0.727

2.38 0.35 0.03 1.00 0.15 0,225

2.12 0.47 0.02 2.12 0.16 1.266

Page: 2-A Total # Pages: 2 (A - G)

Finalized Date: 8-JUL-2008 Account: NMZ

TB08084163


srO BaO WI

% % %.

0,01 M1 om

0.10 0.07 0,82

0,10 0.08 0.37

0.10 0.07 0.57

0,08 0.08 0.62

Method Analyte


Gl34782 G134783 G134784 G134785 G134786

G134787 G134788 G134789 G134790 G134791

Gl34792 Gl34793 G134794 G134795 G134796

G134797 Gl34798 G134799


212 Brooksbank Avenue North Vancouver BC V7 J 2C 1 Phone: 6049840221 Fax: 604 984 0218 www.alschemex,com

ME-XRF06 ME-MSS1 ME-MSS1 ME-MSS1 ME-MSSl ME-MSSl

Total Ag Ba Ce Co Cr

% ppm ppm ppm ppm ppm

0.D1 1 0,5 0.5 0.5 10

99,81 <1 548 45.2 70,3 30

98,72 <1 572 33,4 71,7 30

99.85 <1 602 19.1 62.6 130

99,57 <1 597 63,5 61.3 SO


Project: RG-08-3


ME-MSS1 ME-MSS1 ME·MSS1 ME-MSS1 ME-MSS1 ME-MSSl

Cs Cu Dy Er Eu Ga


0,01 5 0,05 0,03 0,03 0,1

0.60 45 2,42 115 2,57 16,8

0.75 64 2.12 0.99 2.17 20.6

0,30 33 1,43 0,75 1,79 16,7

0,39 56 3.90 1.93 3,00 17,8

Page: 2 - B Total # Pages: 2 (A· G)

Finalized Date: 8·JUL-2008 Account: NMZ

"[808084163

ME·MS81 ME-MSS1 ME-MSB1

Gd HI Ho ppm ppm ppm

0,05 0,2 0,01

4,59 0,5 0.44

3.61 0.7 038

2.26 0,6 0,26

6,90 1.2 0,72

Method Anaiybo


G134782 G134783 G134784 G134785 G134786

G134787 G134788 Gl34789 G134790 G134791

G134792 G134793 G134794 Gl34795 G134796

G134797 G134798 G134799

ALS ~hemex EXCELLENCE IN ANAL YTICAL CHEMISTRY ALS Canada Ltd,

212 Brooksbank Avenue North Vancouver BC V7J 2C1 Phone: 6()4 984 0221 Fax 604 984 0218 www.alschemex.com

ME-MS81 ME·MS81 ME-MSa1 ME-MS61 ME-MS81 ME-MS81

La lu Mo Nb Nd Ni


0,5 0,01 2 0.2 0.1 5

20.0 0.10 2 3.3 27.7 13

14.3 0.10 <2 3.8 21.1 67

9.2 0.07 <2 2.8 11.9 38

27.8 0.19 <2 8.1 38.6 72


Project: RG-08-3


ME-Msa1 ME-MSal ME-MS81 ME-MS81 ME-MS81 ME-MSal

Pb Pr Rb Sm So Sr


5 0.03 0.2 om 1 0.1

7 6.23 6.4 4.84 <1 939

<5 4.73 11.2 3.99 1 924

<5 2,69 6.1 2.28 <1 990

<5 R94 9.8 7.17 1 758

Page: 2 - C Total # Pages: 2 (A - G)


TB08084163

ME-MSal ME-MS81 ME-MSBl

T. Tb Th

ppm ppm ppm

0.1 0.01 0,05

0.2 0.53 0.53

0.2 0.44 0.29

0.2 0.31 0.31

0.5 0.83 0.99

Method Analyte


G134782 G134783 G134784 G134785 G134786

G134787 G134788 G134789 G134790 G134791

G134792 G134793 G134794 G134795 G134796

G134797 G134798 G134799

ALS Chemex EXCELLENCE IN ANAL YTICAL CHEMISTRY ALS Canada Ltd

212 Brooks!)ank Avenue North Vancouver BC V7 J 2Cl Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com

ME·MS81 ME·MSal ME·MS81 ME·MS81 ME·MS81 ME·MS81

TI Tm U V W Y


0.5 0.01 0.05 5 1 0.5

<0.5 0.13 0.10 298 1 10.8

<0.5 0.11 0.06 568 2 10.0

<0.5 0.10 0.06 238 1 6.5

<0.5 0.22 0.19 453 15 18.0


Project: RG-08-3


ME·MS61 ME-MS81 ME·MS81 PGM·MS23 PGM·MS23 PGM·MS23

Yb Zn Zr Au PI Pd


003 5 2 0.001 0.0005 0.001

0.75 104 15 0.001 <0.0005 <0.001 0.001 <0.0005 <0.001 0.001 <0.0005 <0.001 0.001 <0.0005 <0.001

0.74 146 21 0.001 <0.0005 <0.001

0.001 <0.0005 <0.001 0.001 <0.0005 <0.001 0.001 <0.0005 <0.001 0.001 O.OOOS 0.001

0.59 84 19 0.001 <0.0005 <0.001

0.001 <0.0005 <0.001 0.001 <0.0005 <0.001

1.35 103 43 0.001 0.0005 <0.001 0.001 <0.0005 <0.001 0.001 0.0007 0.001

0.001 <0.0005 <0.001 0.001 "0.0005 <0.001 0.001 <0.0005 <0.001

Page: 2 - D Total # Pages: 2 (A - G)


T808084163

ME·ICP41 ME·ICP41 ME-ICP41

Ag AI As

ppm % ppm

0.2 0.01 2

<0.2 3.40 <2 <0.2 3.01 <2 <0.2 2.38 <2

<0.2 2.37 <2 <0.2 2.11 <2 <0.2 2.21 <2 <0.2 2.65 3

<0.2 2.93 2 <0.2 2.45 <2

<0.2 2.17 <2 <0.2 1.95 2

<0.2 2.03 <2 <0.2 2.51 <2 <0.2 2.36 <2

A Method Analyle

Un.its Sample Description LOR

G134782 GI34783 G134784 G134785 G134786

G134787 GI34788 GI34789 G134790 G134791

Gl34792 G134793 G134794 G134795 G134796

G134797 G134798 G134799

ALS Chemex EXCELLENCE IN ANAL YTICAL CHEMISTRY ALS Canada ltd.

212 Brooksbank Avenue North Vancouver BC V7 J 2C 1 Phone: 604 984 0221 Fax 6049840218 www.alschemex.com

ME·ICP41 ME·ICP41 ME·ICP41 ME-ICP41 ME·ICP41 ME·ICP41

a Ba Be Si Ca Cd

ppm ppm ppm ppm % ppm

10 10 0.5 2 0.01 0.5

<10 340 <0.5 <2 2.36 <0.5 <10 300 <0.5 <2 2.91 <0.5 <10 230 <0.5 <2 1.87 <0.5

<10 340 <0.5 <2 2.44 <0.5 <10 310 <0.5 <2 2.38 <0.5 <10 310 0.5 <2 2.75 <0.5 <10 330 <0.5 2 2.15 <0.6

<10 270 <0.5 <2 1.73 <0.5 <10 240 <0.5 <2 1.78 <0.5

<10 300 <0.5 <2 1.91 <0.5 <10 330 <0.5 <2 2.16 <0.5

<10 300 <0.5 <2 2.04 <0.5 <10 280 <0.5 <2 1.66 <0.5 <10 250 <0.5 <2 1.72 <0.5


Project: RG-08-3


ME·ICP41 ME·ICP41 ME·ICP41 ME·ICP41 ME·ICP41 ME·ICP41

Co Cr Cu Fe Ga Hg

ppm ppm ppm % ppm ppm

1 1 1 0.01 10 1

40 1 21 5.42 10 <1 39 3 41 6.35 10 <1 40 6 51 6.48 10 <1

36 H 49 5.76 10 <1 34 38 43 5.52 10 <1 30 66 45 5.05 10 <1 35 51 39 5.63 10 <1

39 22 38 5.69 10 1 48 21 71 7.87 10 1

27 42 39 4.55 10 <1 34 56 45 5.61 10 <1

44 38 51 6.75 10 <1 35 22 28 5.06 10 <1 41 23 39 6.Q8 10 <1

Page: 2 - E Total # Pages: 2 (A - G)


TB08084163

ME·ICP41 ME·ICP41 ME-lCP41

K La Mg

% ppm %

0.01 10 om

0.51 10 3.18 0.45 10 1.63 0.28 10 1.17

0.55 30 1.52 0.36 20 1.63 0.51 30 1.27 0,42 10 1.82

OAI 10 1.77 0.20 10 1.56

0.29 10 1.09 0.35 20 lA7

0.29 20 2.54 0.23 10 2A7 0.22 10 2.90

Method Analyte Units

Sample Description LOR

G134782 G134783 Gl34784 G134785 G134786

G134787 G134788 G134789 G134790 G134791

G134792 G134793 G134794 G134795 Gl34796

G134797 G134798 G134799

ALS Chemex EXCELLENCE IN ANAL YT/CAL CHEMISTRY ALB Canada Ltd

212 Brooksbank Avenue North Vancouver BC V7 J 2C 1 Phone: 604 984 0221 Fax: 6049840218 www.alschemex.com

ME·!CP41 ME·ICP41 ME-ICP41 ME-ICP41 ME·ICP41 ME-ICP41

Mn Mo Na NI P Pb

ppm ppm % ppm ppm ppm

5 1 0.01 1 10 2

612 2 0.51 18 3990 9 338 <1 0.53 28 6220 5 249 <1 0.41 41 2880 4

297 <1 0.37 46 5700 4 333 <1 0.34 48 5330 4 284 1 0.35 36 6540 5 328 <1 0.40 25 3980 2

296 <1 0.45 38 1320 3 280 <1 0.37 71 2520 2

218 <1 0.36 38 2920 <2 271 <1 0.30 50 5070 3

464 <1 0.29 75 5060 2 462 <1 D,39 53 1660 <2 524 <1 0.36 72 2430 <2

To: EAST WEST RESOURCE CORPORATION 1158 RUSSELL STREET THUNDER SAY ON P7B 5N2

Project: RG-08-3


ME·ICP41 ME·ICP41 ME·ICP41 ME·ICP41 ME·ICP41 ME-ICP41

S Sb Se Sf Th Ti

lIJo ppm ppm ppm ppm % 0.01 2 1 1 20 0.01

0.11 3 2 297 <20 0.12 0.22 <2 4 289 <20 0.16 0.27 2 3 213 <20 0.18

0.27 <2 5 194 <20 0.18 0.24 3 6 190 <20 0.16 0.24 <2 7 182 <20 0.18 0,22 <2 4 243 <20 0.15

0.20 3 3 240 <20 0.22 0.36 <2 4 220 <20 0.19

0.20 <2 4 185 <20 0.17 0.24 <2 4 172 <20 0.16

0.26 2 3 187 <20 0.15 0.14 <2 2 228 <20 0.13 0.18 <2 2 219 <20 0.13

Page: 2· F Total # Pages: 2 (A· G)


TB08084163

ME·ICP41 ME·ICP41 ME·ICP41

TI U V

ppm ppm ppm

10 10 1

<10 <10 152 <10 <10 389 <10 <10 432

<10 <10 315 <10 <10 282 <10 <10 304 <10 <10 281

<10 <10 328 <10 <10 557

<10 <10 260 <10 <10 325

<10 <10 345 <10 <10 195 <10 <10 251


Sample Description ~Olt

G134782 G134783 G134784 G134785 G134786

G134787 G134788 Gl34789 G134790 G134791

G134792 G134793 G134794 G134795 G134796

G134797 G134798 Gl34799

ALS Chemex EXCELLENCE IN ANAL ynCAL CHEMISTRY ALS Canada Ltd"

212 Brooksbank Avenue North Vancouver BC V7 J 2C 1 Phone 6049840221 Fax: 604 984 0218 www.alschemex.com

ME·[CP41 ME·ICP41

W Zn ppm ppm

10 2

1Q 75 <10 58 <10 39

10 49 <10 48 <10 47 <10 39

<10 36 <10 28

<10 32 <10 35

<10 46 <lQ 39 <10 43


Project: RG-Oa-3


Page: 2· G Total # Pages: 2 (A· G)


TB08084163


Page: 1 Finalized Date: 8-JUL-2008

Account: NMZ EXCELLENCE IN ANAL YTICAL CHEMISTRY THUNDER BAY ON P7B 6N2 ALS Canada ltd,

Project: RG-08-3 P.O. No.:

212 Brooksbank Avenue North Vancouver Be V7 J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com


This report is for 26 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 25-JUN-2008.

The following have access to data associated with this certificate: 80B MIDDLETON I PAUL NIELSON I TWEST GENERAL WEB AGGO

To: EAST WEST RESOURCE CORPORATION AnN: PAUL NIELSON 1158 RUSSELL STREET THUNDER BAY ON P7B 5N2

ALS CODE

WEI-21

LOG-22 CRU-31

CRU-QC

PUL-QC

SPL-21

PUL-31

ALSCODE

PGM-MS23

ME-JCP41

ME-XRF06

OA-GRA06 ME-MS81




Sample login - Red wlo BarCode Fine crushing - 70% <2mm

Crushing QC Test

Pulverizing QC Test

Split sample - riffle splitter Pulverize split to 85% <75 um


Pt, Pd, Au 30g FA ICP-MS ICP-MS

35 Element Aqua Regia ICP-AES ICP-AES

Whole Rock Package - XRF XRF


38 element fusion fCP-MS ICP-MS

~ Signature: <::::::: ------Colin Ramshaw, Vancouver Laboratory Manager

Method Analyte


G134800 H421001 H421002 H421003 H421004

H421005 H421006 H421007 H421008 H421009

H421010 H421011 H421012 H421013 H421014

H421015 H421016 H421017 H421018 H421019

H421020 H421021 H421022 H421023 H421024

H421025


212 Brooksbank Avenue North Vancouver BC V7 J 2Cl Phone: 604 984 0221 Fax: 6049840218 www.alschemex.com

WEI-21 ME-XRF06 ME-XRF06 ME-XRF06 ME-XRF06 ME-XRF06 Recvd wt. 5,02 AI203 Fe203 CaO MgO

kg % % % % %

0.02 0.01 0.01 0.01 0.01 0.01

2.14 44.09 15.35 12.89 12.30 8.74 1.75

2.05 1.60 44.51 17.85 13.02 1178 6.59 2.37

1.97 1.98 46.10 16.82 11.67 11.57 7.98 0.93

2.11 2.07

2.19 2.19 2.08 2.00 2.07

1.84 0.85 1.99 2.52 0.69

0.36 2.26 45.64 16.52 11.18 10.84 8.38 1.97 1.91 1.32

1.89


Project: RG-08-3


ME-XRF06 ME-XRF06 ME-XRF06 ME·XRF06 ME-XRF06 ME-XRF06 Na20 K20 Cr203 Ti02 MnO P205

% % % % % %

0.01 0.01 0.01 0.01 0.01 0.001

2.07 0.51 0.04 1.48 0.16 1.091

2.63 0.37 0.02 1.82 0.13 0.465

2.36 0.44 0.03 1.39 0.16 0.342

2.35 066 0.03 1.12 0.16 0.422



TB08084164

ME-XRF06 ME-XRF06 ME-XRF06 SrO BaO LOI % % %

0.01 0.01 0.01

0.08 0.07 0.67

0.10 0.08 0.23

0.09 0.09 0.42

0.08 0.09 0.61

Method A"alyte

Units Sample Description lOR

G134800 H421001 H421 002 H421 003 H421 004

H421005 H421 008 H421007 H42100B H421009

H421010 H421011 H421012 H421013 H421014

H421015 H421016 H421017 H421018 H421019

H421 020 H421021 H421022 H421023 H421024

H421 025

ALS Chemex EXCELLENCE IN ANAL YTICAL CHEMISTRY ALS Canada LId.

212 Brooksbank Avenue North Vancouver BC V7 J 2C 1 Phone: 604 984 0221 Fax 604 984 0218 www.alschemex.com

ME·XRF06 ME·MS81 ME·MS81 ME·MS81 ME·MS81 ME·MS81 Total Ag Sa C. Co Cr


0.01 1 0.5 0.5 0.5 10

9954 <1 505 54.8 62.7 130

99.60 <1 597 28.6 62.4 50

99.46 <1 728 36.4 56.4 130

98.08 <1 718 38.7 55.4 90


Project: RG..Q8-3


ME·MS81 ME·MS81 ME·MS81 ME·MS81 ME·MS81 ME·MS81

C. Cu Dy Er Eu G. ppm ppm ppm ppm ppm ppm

0.01 5 0.05 0.03 0.03 0.1

1.18 53 3.27 1.52 2.37 16.5

0.27 46 1.92 0.S7 1.S0 19.8

0.38 72 2.35 1.20 2.07 18.0

1.37 48 2.21 1 11 2.01 15.9

Page: 2 - B Total # Pages: 2 (A - G)


TB08084164

ME·MS81 ME·MS81 ME·MS81

Gd HI Ho

ppm ppm ppm

0.05 0.2 0.01

552 0.9 0.58

3.15 0.9 0.34

3.39 1.1 0.44

3.57 1.0 0.40

Method An"lyle


G134BOO H421001 H421 002 H421003 H421 004

H421005 H421 006 H421007 H421008 H42100S

H421010 H421011 H421012 H421013 H421014

H421015 H421016 H421017 H421018 H421019

H421020 H421021 H421022 H421 023 H421024

H421 025


212 Brooksbank Avenue North Vancouver BC V7 J 2Ci Phone: 604 984 0221 Fax 6049840218 www.alschemex.com

ME·MS8l ME·MS81 ME-MS8l ME·MS81 ME·MS8l ME-MS81

La lu Mo No Nd Ni ppm ppm ppm ppm ppm ppm

0.5 0.01 2. 0.2 0.1 5

23.6 0.14 <2 7.6 32.2 83

12.6 0.10 2 5.9 17.8 43

16.0 0.13 <2 11.7 21.2 66

16.6 0.11 <2 7.6 20.4 68


Project: RG-08-3


ME·MS8l ME-Msal ME·MS81 ME·MSal ME·MS81 ME·MS81

Pb Pr Rb Sm Sn Sr ppm ppm ppm ppm ppm ppm

5 0.03 0.2 0.03 1 0.1

<5 7.53 20.8 5.77 1 769

<5 3.97 8.4 3.32 1 946

5 4.99 11.5 3.86 1 875

8 4.90 238 3.67 1 785


Finalized Date: 8-JUL-200B Account: NMZ

T808084164

ME·MS8l ME·MS81 ME·MS81

Ta Tb Th

ppm ppm ppm

0.1 0.01 0.05

0.4 0.68 1.01

0.5 0.38 0.85

0.8 0.46 1.58

0.4 0.44 0.92

Method AIIa1yt ..

Units Sample Description 1.0R

Gl34BDO H421001 H42100Z H421003 H421 004

H421 005 H421006 H421007 H421 008 H421009

H421010 H421011 H421012 H421013 H421014

H421015 H421016 H421017 H421018 H421019

H421 020 H421D21 H421022 H421023 H421 024

H421025


212 BrooKsbanK Avenue North Vancouver Be V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com

ME-fCP41 ME-fCP41 ME-ICP41 ME-fCP41 ME-ICP41 ME-fCP41

8 Ba Be Bi Ca Cd


10 10 0.5 2 0.01 0.5

<10 220 <0.5 <2 1.98 <0.5 <lQ 180 <0.5 <2 1.61 <0.5

<10 270 0.6 2 1.56 <0.5

<10 280 <0.5 <2 1.47 <0.5

<10 380 <0.5 <2 1.45 <0.5 <10 360 <0.5 <2 1.21 <0.5 <10 410 <0.5 <2 1.54 <0.5

<10 410 <0.5 <2 1.16 <0.5 <10 540 <0.5 <2 1.76 <0.5 <10 480 <0.5 <2 1.B7 <0.5 <10 470 <0.5 <2 1.69 <0.5 <10 320 <0.5 <2 1.70 <0.5

<10 270 <0.5 <2 1.70 <0.5 <10 380 0.5 <2 1.87 <0.5 <10 390 <0.5 <2 170 <0.5 <10 250 <0.5 <2 1.43 <0.5 <10 400 0.5 <2 1.54 <0.5

<10 290 <0.5 <2 1.58 <0.5

<10 540 <0.5 <2 1.71 <0.5 <10 360 0.5 <2 1.84 <0.5 <10 350 <0.5 <2 1.80 <0.5

<10 350 <0.5 <2 1.48 <0.5

To: EAST WEST RESOURCE CORPORATION 1158 RUSSELL STREET THUNDER BAY ON PTB 5N2

Project: RG-OB-3


ME-fCP41 ME-fCP41 ME-ICP41 ME-fCP41 ME-fCP41 ME-fCP41

Co Cr Cu Fe Ga Hg


t 1 1 0.01 10 1

50 12 53 6.65 10 <:1 58 3 37 7.25 <10 <1

41 19 57 7.15 10 <1

40 53 53 6.64 10 <1

32 22 86 5.52 10 1 27 59 35 3.74 <10 <1 31 39 27 4.17 <10 1

37 49 28 4.67 <10 <1 28 138 34 4.40 10 <1 32 87 38 5.07 10 <1 36 6 25 4.94 <10 <1 43 2 20 5.48 <:10 <1

45 1 23 5.49 10 1 45 22 44 5.60 10 <1 40 16 30 5.15 10 <1 43 28 58 7.05 10 <1 33 32 26 5.14 10 <1

51 12 169 4.60 10 <1

29 27 36 3.91 10 1 36 30 45 4.93 10 <1 33 45 44 4.11 <10 <1

35 95 33 4.67 10 1



TB08084164

ME-fCP41 ME-ICP41 ME-ICP41

K La Mg

% ppm %

0.01 10 0.01

0.32 10 3.72 0.20 10 4.81

0.31 10 1.43

0.31 <10 1.64

0.44 10 1.68 0.27 10 1.52 0.34 10 1.98

0.27 10 2.38 0.35 10 1.21 0.33 10 1.55 0.35 10 2.53 0.26 10 3.72

0.23 10 4.03 0.78 10 2.93 0.52 10 2.86 0.31 <10 1.64 1.38 10 2.70

0.97 <10 2.17

0.68 10 2.00 0.45 20 2.74 0.51 10 2.41

0.40 <10 2.18

Method Analyte


G134800 H421001 H421 002 H421003 H421004

H42100S H421 006 H421007 H421008 H421 009

H421010 H421011 H421012 H421013 H421014

H421015 H421016 H421017 H421018 H421019

H421020 H421021 H421022 H421023 H421 024

H421025



ME-ICP41 ME-ICP41 ME~CP41 ME-ICP41 ME-ICP41 ME-ICP41 Mn Mo Na N, P Pb


5 1 0.01 1 10 2

620 <1 0.39 36 3350 5 790 <1 0.40 35 1710 <2

294 <1 0.44 43 780 <2

340 1 DAD 44 890 2

321 <1 0.40 49 1000 6 301 <1 0.32 36 1270 <2 391 <1 0.32 47 1800 <2

470 <1 0.23 55 2110 <2 240 <1 0.36 51 2810 2 323 <1 0.36 64 3270 3 482 <1 0.43 71 1910 <2 675 <1 0045 72 1380 <2

699 <1 0.44 35 1500 <2 452 <1 0.41 38 2790 2 519 <1 0045 25 1340 3 332 <1 0040 76 590 <2 413 2 0.37 55 820 9

329 <1 0044 74 260 11

332 <1 0.46 44 1100 6 506 24 0.42 59 1000 4 401 <1 0.47 55 1080 5

392 <1 0.44 60 650 6

To EAST WEST RESOURCE CORPORATION 1158 RUSSEll STREET THUNDER BAY ON P7B 5N2

Project: RG-08-3


ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME~CP41 ME-ICP41 S Sb Se Sr Th Ti

% ppm ppm ppm ppm %

0.01 2 1 1 20 0.01

0.23 <2 2 247 <20 0.11 0.17 <2 2 246 <20 0.10

0.26 <2 4 205 <20 0.25

0.22 3 4 199 <20 0.24

0.14 <2 3 193 <20 0.17 0.10 <2 2 166 <20 0.14 0.14 <2 3 175 <20 0.13

0.16 2 2 136 <20 0.13 0.18 <2 4 189 <20 0.20 0.20 <2 3 198 <20 0.18 0.13 <2 2 239 <20 0.15 0.09 <2 2 265 <20 0.10

0.09 2 2 257 <20 0.08 0.25 <2 2 217 <20 0.13 0.14 <2 3 244 <20 0.13 0.25 <2 3 213 <20 0.22 0.13 <2 4 164 <20 0.20

0.77 <2 4 202 <20 0.09

0.13 <2 4 225 <20 0.15 0.12 <2 3 218 <20 0.12 0.11 <2 3 269 <20 0.10

0.12 <2 2 227 <20 0.14

Page: 2 - F Total # Pages: 2 (A - G)

Finalized Date: 8·JUl·2008 Account: NMZ

TB08084164

ME-ICP41 ME-ICP41 ME~CP41

TI U V

ppm ppm ppm

10 10 1

<10 <10 213 <10 <10 182

<10 <10 498

<10 <10 406

<10 <10 290 <10 <10 132 <10 <10 108

<10 <10 117 <10 <10 215 <10 <10 234 <10 <10 129 <10 <10 86

<10 <10 68 <10 <10 116 <10 <10 109 <10 <10 453 <10 <10 163

<10 <10 40

<10 <10 112 <10 <10 126 <10 <10 102

<10 <10 155

Method An.lyle


G134800 H421001 H421002 H421003 H421004

H421005 H421006 H421007 H421008 H421009

H421010 H421011 H421012 H421013 H421014

H421015 H421016 H421017 H421018 H421019

H421020 H421021 H421 022 H421023 H421024

H421025


212 Brooksbank Avenue North Vancouver BC V7 J 2C 1 Phone: 604 984 0221 Fax 6049840218 www.alschemex.com

ME-ICP41 ME-ICP41

W Zn

ppm ppm

10 2

<10 115 <10 59

<10 45

<10 39

<10 50 <10 34 <10 35

<10 38 <10 31 <10 38 <10 42 <10 48

<10 49 <10 40 <10 47 <10 35 <10 75

<10 67

<10 52 <10 55 <10 53

<10 59


Project: RG-08-3


Page: 2 - G Total # Pages: 2 (A - G)


T808084164

A ALS Chemex To: EAST WEST RESOURCE CORPORATION

1158 RUSSELL STREET Page: 1

Finalized Date: 8-JUL-2008 Account: NMZ EXCELLENCE IN ANAL YTICAL CHEMISTRY THUNDER BAY ON P7B 5N2

ALS Canada Ltd.

Project: RG-08-3

P,O, No.:


CERTIFICATE T808084165

This report is for 17 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 25-JUN-200B.

The following have access to data associated with this certificate: BOB MIDDLETON I PAUL NIELSON I TWEST GENERAL WEB ACCO

To: EAST WEST RESOURCE CORPORATION ATTN: PAUL NIELSON 1158 RUSSELL STREET THUNDER BAY ON P7B 5N2

ALS CODE

WEI-21

LOG-22

CRU-31

CRU-QC

PUL-QC

SPL-21

PUL-31

ALSCODE

PGM-MS23

ME-ICP41

ME-MS81

ME-XRF06

OA-GRA06

This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release,



Sample login - Red wlo BarCode

Fine crushing - 70% <2mm

Crushing QC Test

Pulverizing QC Test

Split sample - riffle splitter Pulverize split to 85% <75 um





Whole Rock Package - XRF XRF


Signature: ~ --Colin Ramshaw, Vancouver Laboratory Manager

Method Analyte Unlb

Sample Description LOll,

H421026 H421027 H421028 H421 029 H421 030

H421031 H421032 H421033 H421034 H421035

H421 036 H421 037 H421038 H421039 H421 040

H421041 H421G42



WEI-21 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81

Recvd Wt. Ag Ba Ce Co Cr kg ppm ppm ppm ppm ppm

0.02 1 05 0.5 0.5 10

1.99 <1 764 25.7 50.1 70 2.25 1.98 2.19 2.05

2.16 2.22 2.27 2.30 2.14

2.18 2.36 0.49 1 38.1 221 7.7 10 1.22 0.78 <1 837 40.5 51.9 170

2.07 1.83


Project: RG-08-3


ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81 ME-MS81

Cs Cu Dy Er Eu Ga


001 5 0.05 0.03 0.03 0.1

1.24 31 1.67 0.B6 1.88 16.5

0.42 25 10.85 6.65 1.76 27.1

0.62 95 2.49 1.25 2.43 17.9


Finalized Date: 8..JUL-2008 Account: NMZ

TB08084165

ME-MSB1 ME-MS81 ME-MS81

Gd HI He

ppm ppm ppm

0.05 0.2 0.01

2.65 0.6 0.32

13.95 18.9 2.20

3.91 1.3 0.47

Method AnaIyte


H421 026 H421 027 H421 028 H421029 H421030

H421 031 H421032 H421033 H421034 H421035

H421036 H421037 H421038 H421039 H421040

H421041 H421 042


212 Brooksbank Avenue North Vancouver BC V7 J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com

ME-MS81 ME-MSBl ME-MS81 ME-MSBl ME-MSBl ME-MS81

La L~ Mo Nb No N, ppm ppm ppm ppm ppm ppm

0.5 0.01 2 0.2 0.1 5

12.5 0.10 <2 3A 15.1 71

116.5 1.06 12 195.0 87.4 <5

18.6 0.14 <2 115 230 60


Project: RG-08-3


ME-MS81 ME-MS81 ME-MS81 ME-MSB1 ME-MS81 ME-MSBl

Pb p, Rb Sm So Sr


5 0.03 0.2 0.03 1 0.1

9 3A9 20.2 2.80 1 948

5 25.2 45.8 14.35 24 143.0

5 5.47 13.4 4.38 1 874



TB08084165

ME-MSBl ME-MS81 ME-MS81

Ta Tb Th

ppm ppm ppm

0.1 0.01 0.05

0.2 0.34 0.42

10.7 1.92 42.7

0.6 0.48 1.09

Method AnaI¥te

Units Sample Description LOll

H421026 H421027 H421028 H421029 H421030

H421031 H421 032 H421 033 H421034 H421035

H421036 H421 037 H42103B H421039 H421040

H421041 H421 042



ME-MSSl ME-MSBl ME-MS81 ME-MS81 ME-MS81 ME-MSSl


0.5 0.Q1 0.05 5 1 0.5

<0.5 0.11 0.08 149 2 7.7

<0.5 1.07 7.41 6 6 58.6

<0.5 0.15 0.19 275 1 11.9


Project: RG-08-3


ME-MS81 ME-MS81 ME-MSSl ME-XRF06 ME-XRF06 ME-XRF06

Yb Zn Z:r S,02 AI203 Fe203

ppm ppm ppm % %

0.Q3 5 2 0.01 0.01 0.01

0.65 70 22 47.15 18.66 9.78

7.08 26 733 64.92 15.74 1.46

0.96 107 52 47.29 16.68 11.18

Page:2-C Total # Pages: 2 (A - G)


TB08084165


CaO MgO Na20

% % %

0.01 0.01 0.01

10.94 7.94 2.80

4.25 0.22 7.27

11.84 7.32 2.44

Melllod Analyle


H421026 H421027 H421028 H421029 H421030

H421031 H421 032 H421033 H421034 H421035

H421036 H421037 H421038 H421 039 H421040

H421041 H421042



ME·XRF06 ME·XRF06 ME·XRF06 ME·XRF06 ME'XRF06 ME·XRF06

1<20 Cr203 Ti02 MnO P205 srO % 0/0 % % % %

0.01 0.Q1 001 0.01 0.001 0.01

0.56 0.03 0.75 0.14 0.305 0.11

0.63 0.02 0.56 0.04 0.065 0.02

0.59 0.04 1.46 0.16 0.345 0.09


Project: RG-D8-3


ME·XRF06 ME·XRF06 ME·XRF06 PGM-MS23 PGM·MS23 PGM·MS23

BaO LOI TOlal Au PI Pd Il,.a % % ppm ppm ppm

0.01 0.01 0.01 0.001 0.0005 0.001

0.10 0.58 99.83 0.001 <0.0005 0.001 0.001 <0.0005 <0.001 0.001 <0.0005 <0.001 0.001 <0.0005 <0.001 0.001 <0.0005 <0.001

0.002 0.0016 0.001 0.001 <0.0005 <0.001 0.001 <0.0005 <0.001 0.001 <0.0005 <0.001 0.001 <0.0005 <0.001

0.001 <0.0005 <0.001 0.001 <0.0005 <0.001

<0.01 3.39 96.57 0.001 <0.0005 <0.001 0.002 <0.0005 <0.001

0.11 0.33 99.87 0.001 <0.0005 <0.001

0.001 <0.0005 <0.001 0.001 <0.0005 <0.001



TB08084165

ME·ICP41 ME·ICP41 ME·ICP41

Ag AI As ppm %:1 ppm

0.2 0.01 2

<0.2 2.13 4 <0.2 2.48 <2 <0.2 2.93 <2 <0.2 2.38 <2

<0.2 3.32 <2 <0.2 2.08 <2 <0.2 2.15 3 <0.2 2.54 <2 <0.2 2.70 2

<0.2 2.27 <2 <0.2 3.19 <2

<0.2 0.67 2

<0.2 2.00 <2 <0.2 1.86 <2

Method

A"alyte Units


H421D26 H421 027 H421028 H421029 H421030

H421031 H421D32 H421033 H421 034 H421035

H421 036 H421037 H421038 H421039 H421040

H421041 H421042


212 Brooksbank Avenue North Vancouver Be V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com

ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 8 B. Be 81 Ca Cd

ppm ppm ppm ppm % ppm 10 10 0.5 2 0.01 0.5

<10 460 <0.5 <2 1.77 <0.5 <10 320 <0.5 <2 1.44 <0.5 <10 330 <0.5 <2 1.85 <0.5 <10 290 <0.5 <2 1.37 <0.5

<10 330 0.7 <2 1.80 <0.5 <10 330 <0.5 <2 1.41 <0.5 <10 350 <0.5 <2 1.30 <0.5 <10 300 <0.5 <2 1.76 <0.5 <10 310 <0.5 <2 1.69 <0.5

<10 280 <0.5 <2 1.93 <0.5 <10 400 0.8 <2 2.25 <0.5

<10 <10 1.5 2 0.95 1.0

<10 500 <0.5 <2 1.33 <0.5 <10 300 <0.5 <2 114 <0.5


Project RG-08-3

I CER-riFICATE OF ANALYSIS

ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41

Co Cr Cu Fe Ga Hg


1 1 1 0.01 10 1

24 69 48 3.75 <10 1 35 33 37 4.58 <10 1 29 39 35 3.86 10 1 40 41 45 5.05 <10 1

34 33 42 4.24 <10 <1 30 26 46 3.79 <10 1 35 23 48 4.82 <10 1 30 76 55 4.22 <10 1 29 56 49 3.79 10 1

23 43 31 3.80 <10 1 20 61 20 4.00 10 1

64 1 352 2.44 <10 1

27 68 88 4.29 <10 1 29 27 25 3.79 <10 <1



T808084165

ME-ICP41 ME-ICP41 ME-ICP41

K L. Mg

% ppm %

0.01 10 0.01

0.54 10 1.31 0.34 <10 2.40 0.56 10 2.09 0.27 <10 2.81

0.60 <10 2.40 0.27 10 1.84 0.31 10 2.33

0.43 10 1.89 0.48 <10 2.04

0.44 10 1.66 0.98 10 1.83

0.Q1 130 0.43

0.36 10 1.27 0.24 <10 2.01

Method Analyte


H421026 H421027 H421028 H421029 H421030

H421031 H421032 H421033 H421034 H421035

H421036 H421037 H421038 H421039 H421040

H421041 H421 042


212 Brooksbank Avenue North Vancouver BC V7J 2C1 Phone: 6049840221 Fax 6049840218 www.alschemex.com


Mn Mo Na Ni P Pb


5 1 0.01 1 10 2

266 <1 0.30 47 2880 5 458 <1 0.34 64 1350 4 393 <1 0.38 44 1840 4 541 <1 0.34 44 860 6

388 <1 0.45 60 1160 5 349 <1 0.31 27 1520 2 442 <1 0.29 37 1470 <2 359 <1 0.38 55 2320 5 360 <1 0.37 52 1700 2

325 <1 0.29 32 3540 <2 392 <1 0.42 25 3450 2

86 <1 0.12 7 280 9

257 <1 0.32 42 1480 <2 388 <1 0.30 42 1140 <2


Project: RG-08-3



S Sb Sc Sr Th TI

% ppm ppm ppm ppm %

0.01 2 1 1 20 0.01

0.16 <2 5 146 <20 0.16 0.12 <2 2 215 <20 0.08 0.12 <2 4 203 <20 0.10 0.13 <2 2 203 <20 0.10

0.12 <2 3 266 <20 0.09 0.14 <2 2 178 <20 0.09 0.12 <2 2 171 <20 0.10 0.16 <2 4 212 <20 0.10 0.11 <2 3 217 <20 0.08

0.11 <2 5 149 <20 0.11 0.08 <2 6 202 <20 0.15

1.66 <2 5 23 30 0.09

0.20 <2 3 165 <20 0.18 0.09 <2 2 163 <20 0.09



T808084165


TI U V

ppm ppm ppm

10 10 1

<10 <10 151 <10 <10 88 <10 <10 98 <10 <10 113

<10 <10 99 <10 <10 89 <10 <10 129 <10 <10 123 <10 <10 84

<10 <10 118 <10 <10 110

<10 <10 1

<10 <10 169 <10 <10 79

ALS Chemex To EAST WEST RESOURCE CORPORATION 1158 RUSSELL STREET

Page: 1 Finalized Date: 7·JUL-2008

Account: NMZ EXCELLENCE IN ANAL YTICAL CHEMISTRY THUNDER SAY ON P7B 5N2 ALS Canada Ltd

Project: RG-08-3

P.O, No.:

212 Brooksbank Avenue North Vancouver Be V7 J 2C 1 Phone: 604 984 0221 Fax: 604 9840218 www.alschemex.com


This report is for 20 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 25-JUN-200B.

The following have access to data associated with this certificate: BOB MIDDLETON I PAUL NIELSON I TWEST - GENERAL WEB Aceo

To: EAST WEST RESOURCE CORPORATION AnN: PAUL NIELSON 1158 RUSSELL STREET THUNDER BAY ON P7B 5NZ

ALSCODE

WEI-21 LOG-22

CRU-31

CRU-QC

PUL-QC

SPL-21

PUL-31

AL5CODE

PGM·MS23

ME-ICP41

ME-XRF06

OA-GRA06

ME-MS81

This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release,



Sample login - Red wlo BarCode


Crushing QC Test

Pulverizing QC Test



ANAL Y"nCAl PROCEDURES DESCRIPTION INSTRUMENT



Whole Rock Package - XRF XRF LOI for ME-XRF06 WST-SIM 38 element fusion ICP-MS ICP·MS

~ Signature: ,,;,::=; ------Colin Ramshaw, Vanc.ouver Laboratory Manager

Method Analyle


G134762 G134763 G134764 G134765 G134766

G134767 G134768 G134769 G134770 G134771

G134772 G134773 G134774 G134775 G134776

G134777 G134778 G134779 G134780 G134781


212 Brooksbank Avenue North Vancouver BC V7 J 2Cl Phone: 604 9840221 Fax: 604 984 0218 www.alschemex.com

WEI·21 ME·XRF06 ME·XRF06 ME·XRF06 ME·XRF06 ME·XRF06

RecvdW!' S;02 AI203 Fe203 CaO MgO

kg % % % % %

0.02 0,01 0,01 0.D1 0,01 0,01

$,01 42.31 15,55 15,56 10,50 7.42 2.09 46.31 18.44 11,69 9.61 7.59 2.50 1.95 40,13 15,19 17,61 10,17 7,12 2.18

1.98 1,56 2,11 2,64 2,29

1.25 1.01 41,76 3.40 20,27 4,56 22,73 1.77 1.14 1,06 41,50 12,87 18,10 12.D2 8.37

0,88 2.12 2.06 2.08 1,85


Project RG-08-3


ME·XRF06 ME·XRF06 ME-XRF06 ME·XRF06 ME·XRF06 ME·XRF06

Na20 K20 Cr203 TI02 MnO P205

% % % '% % %

0,01 0,01 0,01 0.01 0,01 0,001

2,31 0,59 0,02 2.41 0,18 1.476 2,69 0,47 0.02 1.17 0,13 0,303

2,15 0.47 0.02 2,78 0,14 1.488

0.13 0,13 0.26 0,71 0,10 0,611

1.87 0.35 0.04 2,72 0,19 0.945



T808084162

ME-XRF06 ME·XRF06 ME·XRF06

SrO BaO LOI

% % %

0.01 0,01 0,01

0.10 0.13 0.96 0,12 0,10 1,32

0,08 0,09 1.37

0.01 0.01 479

0,07 0,07 0,69

Method Aftalyte

UnI ... Sample Description LOR

G134762 G134763 GI34764 G134765 G134766

G134767 G134768 G134769 G134770 G134771

G134772 G134773 Gl34774 G134775 G134776

G134777 G134778 G134779 G134780 G134781



ME-XRF06 ME-MS8l ME-MS81 ME-MS81 ME-MS81 ME-MS81

Total Ag Sa Ce Co Cr


0.01 1 0.5 0.5 0.5 10

99.52 <1 998 63.9 56.0 40 99.97 <1 816 26.5 46.7 50

98.70 <1 598 64.3 68.7 10

99.46 <1 453 64.0 111.5 1850

99.80 <1 421 39.6 75.9 150

To EAST WEST RESOURCE CORPORATION 1158 RUSSELL STREET THUNDER BAY ON P7B 5N2

Project: RG-08-3


ME-MS81 ME-MSal ME-MSal ME-MS8l ME-MSal ME-MS81

Cs Cu Dy Er Eu Ga ppm ppm ppm ppm ppm ppm

0.01 5 0.05 0.03 0.03 0.1

0.57 21 3,48 1.62 4.07 17.4 0.56 17 1.47 0.72 2.11 17.0

0.61 53 3.27 1.50 3.09 19.5

0.35 9 4.91 2.86 1.52 8.6

0.45 38 2.85 Ul 2.36 17.9

Page: 2· B Total # Pages: 2 (A - G)


T808084162

ME-MS81 ME-MBal ME-MBB1

Gd HI Ho ppm ppm ppm

0.05 0.2 om

6.47 0.8 0.61 2.39 0.5 0.27

6.14 0.7 0.59

6.07 4.0 0.98

4.69 0.7 0.51

Method Analyle


G134762 G134763 G134764 G134765 G134766

G134767 G134768 G134769 G134770 G134771

G134772 G134773 G134774 G134775 G134776

G134777 G134778 G134779 G134780 G134781


212 Brooksbank Avenue North Vancouver Be V7 J 2C1 Phone: 6049840221 Fax: 604 984 0218 www.alschemex.com

ME·MS81 ME·MS81 ME·MS81 ME·MS81 ME·MS81 ME·MS81

La Lu Mo Nb Nd Ni


0,5 0,01 2 0.2 0,1 5

28,3 0.14 :1 10.3 37,1 7 13.4 0,07 <2 4.7 13,9 29

28.2 0,13 <2 8.0 38,3 17

32.2 0,37 2 54,9 30.9 1390

17,0 0,13 <2 4,0 25.3 39


Project: RG-08-3


ME·MS81 ME·MSBl ME·MS81 ME·MS81 ME·MS81 ME-MS81

Pb p, Rb SOl Sn S, ppm ppm ppm ppm ppm ppm

5 0,03 0,2 0,03 1 0,1

<5 8.26 17.9 6.64 1 888 5 3.25 8.0 2.56 <1 1145

<5 8,52 11,1 6,83 <1 828

<5 7.47 6.1 6.25 1 46,3

10 5.43 8,9 5,02 <1 694



TB08084162

ME-MSBl ME·MS81 ME-MS81

Ta Tb Th

ppm ppm ppm

0.1 0.01 0.05

0.5 0.77 1.84 0,2 0.30 0.42

0,6 0.75 1.00

3.3 0.90 8.20

0.2 0.60 0.35

Method Analyle

Units Sample De5crlption LOR

G134762 G134763 G134764 G134765 G134766

G134767 G134768 G134769 G134770 Gl34771

G134772 G134773 G134774 G134775 G134776

G134777 G134778 G134779 G134780 G134781

ALS Chemex EXCELLENCE IN ANAL YTICAL CHEMISTRY AlS Canada ltd.


ME·MS81 ME-MS81 ME·MS81 ME·MS81 ME·MS81 ME·MS81

TI Tm U V W Y


0.5 0.01 0.05 5 1 0.5

<0.5 0.18 0.86 416 2 17.1 <0.5 0.08 0.07 210 1 7.0

<0.5 0.16 0.24 670 2 16.2

<0.5 0,39 1.61 37 3 26.0

<0.5 0.16 0,09 658 1 14.0


Project: RG-08-3


ME·MS81 ME·MS81 ME·MS81 PGM·MS23 PGM·MS23 PGM·MS23

Yb Zn Z, Au PI Pd


0.03 5 2 0.001 0.0005 0001

1.13 88 26 0.007 0.0005 0.001 0.51 75 18 0.002 0.0006 0.001

0.002 <0.0005 <0.001 0.98 99 21 0.002 <0.0005 <0.001

0.008 0.0009 0.001

Q.004 <0.0005 0.001 0.003 <0.0005 0.001 0.003 <0.0005 <0.001 0.002 <0.0005 <0.001 0.002 0.0011 0.001

0.003 0.0054 0.005 2.58 127 127 0.003 0.0057 0.006

0.002 0.0082 0.009 0.003 0.0038 0.004

0.94 135 20 0.002 0,0033 0.004

0.002 <0.0005 <0.001 0.002 <0.0005 <0.001 0,002 <0.0005 <0.001 0.002 <0.0005 <0.001 0.003 <0.0005 <0.001



TB08084162

ME·ICP41 ME-lCP41 ME·ICP41

Ag AI As

ppm % ppm

0.2 0.01 2

<0.2 2.30 <2

<0.2 3.11 <2

<0.2 3.46 <2 <0.2 3.29 2 <0.2 2.47 <2 <0.2 2.60 <2 <0,2 2.36 <2

0.2 1.54 <2

<0.2 2.12 <2 <0.2 1.83 <2

<0.2 1.90 <2 <0.2 1.96 <2 <0.2 2.13 <2 <0.2 1.62 2 <0.2 2.57 <2



G134762 G134763 G134764 Gl34765 G134766

G134767 G134768 G134769 G134770 G134771

G134772 G134773 G134774 G134775 G134776

G134777 G134778 G134779 G1347BO G134781


212 Brooksbank Avenue North Vancouver BC V7 J 2C1 Phone' 604 984 0221 Fax 604 9840218 www.alschemex,com

ME·ICP41 ME-ICP41 ME·ICP41 ME·ICP41 ME·ICP41 ME·ICP41

S Sa Be Bi Ca Cd


10 10 0,5 2 0,01 0,5

<10 240 <0,5 <2 0,98 <0,5

<10 290 <0.5 <2 2,23 <0,5

10 310 0.7 <2 1.72 <0.5 <10 300 0.9 <2 1.04 <0.5 <10 390 <0.5 <2 1.10 <0.5 <10 310 <0.5 <2 2,28 <0,5 <10 310 <0,5 <2 2.30 <0.5

<10 70 <0,5 <2 1.37 <0.5

<10 250 <0.5 <2 1.31 <0.5 <10 200 <0.5 <2 1,56 <0.5

<10 250 <0.5 <2 2.20 <0.5 <10 230 <0.5 <2 2.04 <05 <10 260 <0.5 <2 2.45 <0.5 <10 200 <0,5 <2 2.52 <0.5 <10 250 <0.5 <2 2,59 <0.5


Project: RG-08-3


ME·ICP41 ME-ICP41 ME·ICP41 ME-ICP41 ME-ICP41 ME-ICP41

Co Cr Cu Fe Ga Hg

ppm ppm ppm ',;' ppm ppm

1 1 1 Q,Ol 10 1

30 55 34 5,86 10 <1

38 3 159 5.84 10 <1

30 4 33 5.82 10 <1 41 15 21 6,11 10 <1 35 26 120 5,07 10 <1 30 31 23 5.00 10 <1 25 131 19 4.25 <10 <1

85 565 55 10.75 <10 <1

34 139 33 4.87 10 <1 48 238 65 7.18 10 <1

42 7 42 7.37 10 <1 42 28 51 6.97 10 <1 38 38 51 6.13 10 <1 45 44 61 7.06 <10 <1 41 31 47 6,25 10 <1

Page: 2 - E Total # Pages: 2 (A· G)

Finalized Date: 7 -JUL-2008 Account: NMZ

T808084162

ME-ICP41 ME-ICP41 ME·ICP41

K La Mg

% ppm % 0,01 10 0,01

0.18 <10 1.69

0.56 30 3.43

0.79 30 4,07 1.18 80 3.87 0,98 30 2.49 0.52 20 2.01 0,74 30 1.91

0.30 30 3,48

0.24 10 1.65 0.18 10 1,71

OAO 20 1.36 0.27 10 1.50 0.32 20 1.65 0.20 20 2.16 0.29 20 2.36

Method Analyle


G134762 G134763 8134764 Gl34765 G134766

G134767 G134768 G134769 G134770 G134771

G134772 G134773 G134774 G134775 G134776

G134777 G134778 G134779 Gl34780 G134781

ALS Chemex EXCELLENCE IN ANAL YTICAL CHEMISTRY ALS Canada LId.



Mn Mo Na NI P Pb


5 1 0.01 1 10 2

216 <1 0.30 5 750 <2

284 <1 0.19 21 7980 2

314 <1 0.17 31 6250 2 348 1 0.16 13 2620 3 284 <1 0.23 8 2070 <2 236 <1 0.31 81 6970 <2 287 <1 0.31 40 6960 <2

203 1 0.06 479 4640 4

241 <1 0.Z9 29 2050 <2 252 <1 0.20 30 3600 6

253 <1 0.27 46 6250 3 291 <1 0.27 49 5220 6 317 <1 0.30 54 6670 <2 459 <1 0.19 41 8560 <2 470 <1 0.37 11 6690 4


Project: RG-08-3


ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICNl ME-ICP41

S Sb Sc Sr Th Ti

% ppm ppm ppm ppm %

0.01 2 1 1 20 0.01

0.15 <2 3 163 <20 0.17

0.1S <2 3 124 <20 0.19

0.09 2 5 104 <20 0.16 0.18 2 5 81 20 0.25 0.17 <2 4 101 <20 0.24 0.14 <2 2 197 <20 0.12 0.10 <2 2 198 <20 0.12

0.28 <2 2 49 <20 0.10

0.21 <2 :3 170 <20 0.12 0.35 <2 4 132 <20 0.14

0.29 <2 4 177 <20 0.15 0.29 2 4 173 <20 0.15 0.23 <2 4 203 <20 0.13 0.29 <2 3 177 <20 0.12 0.22 <2 3 250 <20 0.12

Page: 2· F Total # Pages: 2 (A· G)

Finalized Date: 7..JUL·2008 Account: NMZ

T808084162


TI U V ppm ppm ppm

10 10 1

<10 <10 340

<10 <10 314

<10 <10 281 <10 <10 283 <10 ~10 226 <10 <10 247 <10 <10 110

<10 <10 139

<10 <10 209 <10 <10 397

<10 <10 486 <10 <10 454 <10 <10 364 <10 <10 348 <10 <10 278

MethOd Analyte

Units Sample Deseription LOR

8134762 G134763 G134764 G134765 G134766

G134767 G134768 G134769 G134770 G134771

G134772 G134773 G134774 G134775 G134776

G134777 G134778 G134779 G134780 G134781

ALS Chemex EXCELLENCE IN ANAL YTICAL CHEMISTRY ALS Canada Ltd"

212 Brooksbank Avenue North Vancouver Be V7 J 2C 1 Phone: 604 984 0221 Fax: 604 984 0218 www,alschemex,com

ME-ICP41 ME-ICP41

W Zn ppm ppm

10 2

<10 16

<10 19

<10 26 <10 39 <10 38 <10 29 <10 33

<10 29

<10 25 <10 33

<10 41 <1D 47 <10 38 <10 36 <10 46


Project: RG-08-3


Page: 2· G Total # Pages: 2 (A - G)

Finalized Date: 7·JUL·2008 Account: NMZ

TB08084162

Ticket #

B760951

B760952

B760953

B760954

B760955

B760956

B760957

B760958

B760959

B760960 B760961

B760962

B760963

B760964

B760965

B760966

B760967

B760968

B760971

B760972

B760973

B760975

B760980

B760982

B760983

B760984

B760986

B760988

B760989

B760991

B760992 B760993

B760994

TS

TS TS

Red Granite Assay Data

Hole: RG-08-04

Footage Assay Code

From To 63' 67'6" REE

68' 69'7" REE 175' 176'9" REE

188'3" 189'5" REE

250'2" 253'5" PGM 253'5" 256'7" PGM

329' 332'3" PGM

332'3" 335'7" PGM 342'11" 345'3" PGM

387'5" 342'4" PGM & REE

431' 432' REE 432' 437' PGM

440'4" 441'2" TS&WR 444' 444'10" TS&WR

452'6" 455'9" PGM

461'10" 465'2" PGM 477'5" 480'6" PGM 480'6" 483'10" PGM

559' 561'8" PGM 562' 565' PGM 567' 570' PGM

582'11" 584' PGM 650'3" 653'7" PGM 660' 663' PGM 683' 685'4" PGM 749' 751' PGM

914'10" 918'1" PGM 921'4" 927' PGM 834' 835' WR 631' 632' WR 707' 708' WR 555' 556' REE 608' 610' REE 835' 835'6" Thin Section

441'6" 442" Thin Section 446'6" 447" Thin Section


Page: 1 Finalized Date: 4-DEC-2008

This copy reported on 5-DEC-2008 Account: NMZ

EXCELLENCE IN ANALYTICAL CHEMISTRY THUNDER BAY ON P7B 5N2 ALS Canada Ltd,

Project: RG-08-04

P.O. No.:

212 Brooksbank A-renue North VanCOUlref Be V7 J 2C 1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com


This report is for 44 Drill Core samples submitted to our lab in Thunder Bay, ON, Canada on 7-NOV-2008,

The following have access to data associated with this certificate:

TWEST - GENERAL WEB Aceo 80B MIDDLETON I PAUL NIELSON I LUCY RAJNOVICH

To EAST WEST RESOURCE CORPORATION ATTN: BOB MIDDLETON 1158 RUSSELL STREET THUNDER BAY ON P7B 5N2

ALSCODE

WEI-21

PUL-31 SPL-21

DRY-21

CRU-QC

PUL-QC

CRU-31 LOG-22

AlSCODE

ME-ICP41

ME-XRF06

OA-GRA06 ME-MS81

PGM-ICP23



Received Sample Weight Pulverize split to 85% <75 um

Split sample - riffle splitter

High Temperature Drying

Crushing QC Test

Pulverizing QC Test


Sample login - Red WID BarCode



Whole Rock Package XRF XRF



Pt. Pd, Au 30g FA Ie? ICP-AES

Signature: ~ - -Colin Ramshaw, Vancouver Laboratory Manager

Method Analyte


8760951 8760952 B760953 8780954 8760955

8760956 8760957 8760958 8760959 8760960

8760961 8760962 8760963 8760964 8760965

8760966 8760967 8760968 8760969 8760970

8760971 8760972 8760973 B760974 8760975

8760976 B760977 8760978 8760979 8760980

8760981 8760982 8760983 8760984 8760985

8760986 B760987 8760988 8760989 8760990


212 Brooksbank Avenue North Vancouver Be V7 J 2C 1 Phone: 604 984 0221 Fax 604 984 0218 www,alschemex.com

WEI·21 ME·MS81 ME·MS81 ME·MS81 ME·MS81 ME·MS81

RecvdWI. Ag Sa Ce Co Cr


0.02 1 0.5 05 0.5 10

0.50 <1 410 31.0 3.6 20 0.56 <1 413 64.2 1.2 10 0.84 <1 69B 33.9 49.5 70 1.44 <1 727 124.0 37.3 20 1,19

1.16 1.16 1.41 1.22 2.05 <1 544 101.0 45.3 210

0.42 <1 1145 150.5 2B.1 40 1.98 0.32. <1 231 12.8 58.8 60 0.34 <1 406 242 55.7 160 1.79

1.25 1.25 1.24

Not Recvd Not Recvd

1.27 1,02 1.14

Not Recvd 1.02

Not Recvd Not Recvd Not Recvd No! Recvd

1.21

Not Recvd 1.07 0.86 0.79

Not Recvd

1,34 Not Recvd

2,08 0,36 <1 607 23.1 55,0 20

Not Recvd


Project RG-08-04


ME·MS81 ME·MS81 ME-MS81 ME·MS81 ME·MS81 ME·MS81

Cs Cu Dy Er Eu Ga


0.01 5 0.05 0.03 0.03 0.1

0.65 9 1.47 0.85 0.71 16.S 0.30 <5 1.52 0.60 0.48 15.3 5.71 <5 5.67 4.66 1.53 21.4 1.85 13 5.95 4.12 1.70 23.9

1.77 51 6.09 3.62 2.58 19.7

2.03 20 11,00 7.10 1.23 28.4

0.34 31 1.26 0.62 1.03 15.7 0.81 18 10.65 4.90 7.47 13.3

0.22 38 1.34 0,63 1.79 17.3


Finalized Date: 4-DEC-2008 Account: NMZ

TB08160023

ME·MS81 ME-MS81 ME·MS81

Cd HI Ho

ppm ppm ppm

0.05 0.2 0.01

2.12 2.0 0.29 3.66 4.0 0.23 3.94 45.0 1.27 7.03 10.1 1.26

8.54 4.1 1.19

11.85 7.7 2.22

1.66 0.7 0.23 21.2 0.9 1.97

2.36 0.4 0.25

Method Analyle


8760951 B760952 B760953 8760954 8760955

B760956 8760957 B760958 8760959 B760960

8760961 8760962 8760963 8760964 B760965

8760966 8760967 B760968 6760969 8760970

B760971 6760972 B760973 B760974 B760975

B760976 6760977 6760978 8760979 6760980

6760981 8780982 6760983 6760984 6760985

8760986 6760987 8760988 8760989 B760990

ALS Chemex EXCELLENCE IN ANAL YTICAL CHEMISTRY ALS Canada Lid.

212 Brooksbank Avenue North VancoUlier 8e V7 J 2C 1 Phone: 604 984 0221 Fax 6049840218 www.alschemex.com

ME-MS81 ME-MS81 ME·MS81 ME-MSBl ME-MSBl ME-MSB1

La Lu Mo Nb Nd Ni


0.5 0.01 2 02 0.1 5

15.0 0.11 <2 14.7 12.9 8 33.2 0.06 <2 5.5 23.5 <5 14,4 '.26 <2 281 17.3 21 67.0 0.59 <2 163.0 41.1 48

47.3 0,48 :2 96.2 50.2 63

77.0 0.92 3 337 62,4 31

5.6 0.07 <2 3.2 7.2 60 106.5 0.44 <2 13.2 129.5 37

10.1 0.Q6 <2 3.3 13.0 11


Project: RG-08-04


ME-MSB1 ME-MSBl ME-MSBl ME-MSBl ME-MSBl ME-MS81

Pb Pr Rb Sm So Sr


5 0.03 02 0.03 1 0.1

22 3.48 177.5 2.35 , 97.0 27 6.98 131.5 4.37 <1 118.0 8 4.22 226 3.71 17 624 5 12.95 94.6 7.05 7 725

8 12]0 99.2 9.01 3 576

21 17.50 184.0 12.25 5 591

<5 1.75 4.6 1.58 <1 726 <5 33.0 15.9 22.5 1 688

<5 3.16 3.6 2AO <1 1110



TB08160023

ME-MS81 ME-MS81 ME-MSBl

Ta Tb Th

ppm ppm ppm

0.1 0.01 0.05

0.8 0.28 7.22 0.2 0.40 29.2 19.9 0.79 143.0 5.9 '.00 42.5

5.0 1.12 16.85

10.8 1.Bl 73.3

0.2 0.24 OAO 0.8 2.54 2.73

0.2 0.30 0.27

Method Analy"


8760951 8760952 8760953 8760954 8760955

8760956 8760957 B760958 B760959 8760960

8760961 B760962 8760963 8760964 8760965

8760966 8760967 8760968 8760969 B760970

8760971 8760972 B760973 8760974 8760975

8760976 B760977 8760978 8760979 B760980

8760981 B760982 B760983 8760984 B760985

8760986 8760987 B760988 B760989 8760990


212 Brooksbank Avenue North Vancouver 8e V7 J 2C 1 Phone: 604 984 0221 Fax 6049840218 www,alschemex,com

ME-Msa1 ME-MS81 ME·MS81 ME·MS81 ME-MS81 ME·Msa1


0,5 0,01 0,05 5 1 0,5

<0,5 0,11 1.61 25 1 7,3 <0,5 0,08 4,08 <5 1 5,7 <0,5 0,95 2.34 183 4 24,5 <0,5 0,63 7,07 360 3 31.2

<0.5 O.SO 3.08 334 2 30,8

<0.5 1,02 6.42 104 6 55,7

<0,5 0.09 <0,05 245 1 6,1 <0,5 0.55 0,87 262 2 55,3

<0,5 0,08 <0.05 380 <1 6,5


Project: RG-Oa-04


ME·MS81 ME-Msa1 ME-Msal PGM-ICP23 PGM·ICP23 PGM·ICP23

Vb Zn Zr Au PI Pd ppm ppm ppm ppm ppm ppm

am 5 2 0,001 0,005 0,001

0,74 15 62 0.40 13 99 8,10 57 924 4,24 65 351

0,002 <0,005 0.001

0.002 <0.005 <0,001 0,002 <0.005 0.001 0,006 <0,005 <0,001 0,002 <0.005 0,001

3,37 107 108 0.001 <0,005 <0.001

6,45 197 197 0.002 <0.005 0.001

0,53 93 20 3,06 87 37

0,001 <0,005 <0,001

0.002 <0,005 <0,001 0,002 <0,005 <0,001 0.002 <0.005 0,001

0,002 <0,005 0.001 0,001 <0.005 0.001 0,002 <0,005 <0,001

0.002 <0,005 <0,001

0.002 <0,005 0,001

0,001 <0,005 <0,001 0,001 <0.005 0,001 0,001 <0,005 <0.001

0.001 <0.005 0,001

0,002 0.005 <0.001 0.43 89 15



TB08160023

ME·ICP41 ME·ICP41 ME-lCP4t

Ag AI As

ppm ppm

0.2 0,01 2

<0,2 1,89 <2

<0,2 2.45 <2 <0,2 1.87 <2 <0,2 1,96 <2 0,2 1.57 <2

<0,2 1,99 <2

0.3 2,37 <2

0,2 1,90 <2 <0,2 2,00 <2 <0,2 1,79 <2

<0,2 3.82 <2 <0.2 3.36 <2 0,3 3,60 <2

0,2 2,09 <2

<0.2 1,58 <2

<0,2 1,71 <2 <Q,2 1,51 <2 0.4 1.20 <2

0,4 2,25 <2

<0.2 1,84 <2

Method Analyte


B760951 8760952 8760953 B760954 8760955

B760956 8760957 B760958 8760959 8760960

B760961 8760962 8760963 8760964 8760965

B760966 8760967 8760968 8760969 8760970

8760971 8760972 8760973 8760974 8760975

8760976 8760977 8760976 8760979 8760960

8760981 8760982 8760983 8760984 8760985

8760986 8760987 8760988 8760989 8760990


212 Brooksbank Avenue North Vancouver BC V7J 2Cl Phone: 604 984 0221 Fax: 604 984 0218 www,alschemex.com


B Ba Be Bi Ca Cd


10 10 0,5 2 0,01 0.5

<10 530 <0.5 <2 1.85 <0.5

<10 680 <0.5 <2 1.60 <0.5 <10 340 <0.5 <2 1.09 <0.5 <10 400 <0.5 <2 1.27 <0.5 <10 440 <0.5 ,,2 1.03 <0.5

<10 210 <0.5 <2 1.34 <0.5

<10 340 <0.5 <2 1.45 <0.5

<10 300 <0.5 <2 1.21 <0.5 <10 440 <0.5 <2 1.46 <0.5 <10 280 <0.5 <2 1.02 <0.5

<10 320 1.0 <2 2.65 <0.5 <10 350 <0.5 <2 1.77 <0.5 <10 240 1.4 <2 2.05 <0.5

<10 410 0.7 <2 1.83 <0.5

<10 470 <0.5 <2 1.14 <0.5

<10 450 <0.5 <2 2.16 <0.5 <10 520 <0.5 <2 0.97 <0.5 <10 230 <0.5 <2 1.71 <0.5

<10 240 <0.5 <2 1.26 <0.5

<10 270 <0.5 <2 1.98 <0.5


Project: RG-08·04



Co Cr Cu Fe Ga Hg


1 1 1 0.Q1 10 1

25 66 40 4.05 <10 <1

28 50 34 4.05 10 1 35 69 26 5.24 <10 <1 33 32 50 4.72 <10 <1 34 52 63 4.79 <10 <1

34 47 36 5.00 <10 <1

37 41 46 5.15 <10 <1

33 23 63 5.90 <10 <1 25 91 57 4.15 <10 <1 25 63 33 2.60 <10 <1

45 95 6 5.46 10 <1 39 31 43 5.02 <10 <1 42 11 53 8.17 10 <1

24 86 47 3.55 <10 <1

28 147 51 5.11 <10 <1

24 123 40 4.28 <10 <1 32 39 25 4.70 <10 <1 52 19 93 8.18 <10 <1

32 39 29 4.50 <10 <1

35 114 47 5.44 <1Q <1

Page: 2· D Total # Pages: 3 (A· G)

Finalized Date: 4-DEC·2008 Account: NMZ

TB08160023


K La Mg

% ppm %

0.01 10 0.01

0.38 20 1.09

0.75 30 1.60 0.24 <10 2.36 0.25 10 2.28 0.26 10 2.09

0.24 10 2.06

0.30 10 2.59

0.21 <10 1.38 0.26 10 1.26 0.31 <10 1.09

0.29 10 3.47 0.24 <10 2.12 0.41 20 3.24

0.68 50 1.39

0.23 10 1.64

0.23 20 1.13 0.24 10 2.43 0.12 10 1.84

0.32 10 2.52

0.34 20 2.03

Method Analyte


B760951 8760952 8760953 8760954 8760955

8760956 8760957 8760958 8760959 8760960

B760961 B760962 B760963 B760964 B760965

8760966 8760967 8760966 B760969 B760970

B760971 8760972 B760973 8760974 B760975

8760976 B760977 B760978 B760979 B760980

B760981 8760982 B760983 B760984 8760985

B760986 B760987 8760988 8760989 8760990


212 Brooksbank Avenue North Vancouver Be V7 J 2C 1 Phone 6049840221 Fax 6049840218 www.alschemex.com


Mn MQ Na NI P Pb


5 1 0.01 1 10 2

208 <1 0.29 40 3740 2

254 <1 0.34 36 2560 5 436 <1 0.29 52 1010 2 448 <1 0.29 37 1760 2 408 <1 0.23 30 1390 4

462 <1 0.31 45 1410 3

510 <1 0.34 39 1580 4

286 <1 0.31 45 1090 2 258 <1 0.32 39 1870 2 217 <1 0.23 34 1090 2

417 <1 0.27 18 4300 <2 293 <1 0.44 17 930 :2 438 <1 0.12 21 280 4

376 <1 028 32 1680 7

354 <1 0.24 36 1500 3

257 <1 0.27 28 5300 3 515 <1 0.22 54 1490 2 365 <1 0.17 25 5410 20

501 <1 0.29 49 960 9

455 <1 0.25 36 4950 3


Project: RG-08-04


ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME·ICP41 ME-ICP41

S Sb So 5r Th TI

% ppm ppm ppm ppm %

0.01 2 1 1 20 0.01

0.20 <2 4 152 <20 0.15

0.14 <2 4 162 <20 0.19 0.08 <2 1 179 <20 0.14 0.14 <2 2 180 <20 0.12 0.16 <2 2 142 <20 0.15

0.18 <2 2 177 <20 0.10

0.12 <2 2 210 <20 0.12

0.19 <2 2 184 <20 0.16 0.17 <2 3 194 <20 0.14 0.07 <2 2 187 <20 0.11

0.28 <2 7 163 <20 0.16 0.16 <2 2 248 <20 0.12 0.65 <2 13 71 <20 0.37

0.17 <2 6 110 20 0.25

0.11 <2 3 148 <20 0.17

0.17 <2 4 175 <20 0.12 0.11 <2 2 142 <20 0.12 0.41 <2 2 149 <20 0.14

0.10 <2 2 182 <20 0.08

0.19 <2 3 193 <20 0.11

Page: 2- E Total # Pages: 3 (A - G)


T808160023


TI U V ppm ppm ppm

10 10 1

<10 <10 177

<10 <10 156 <10 <10 175 <10 <10 107 <10 <10 147

<10 <10 143

<10 <10 108

<10 <10 309 <10 <10 154 <10 <10 109

<10 <10 157 <10 <10 152 <10 <10 366

<10 <10 113

<10 <10 206

<10 <10 171 <10 <10 89 <10 <10 455

<10 <10 51

<10 <10 171

Method Anplyle


B760951 9760952 B760953 8760954 B760955

8760956 8760957 8760958 8760959 8760960

9760961 B760962 8760963 8760964 8760965

8760966 8760967 8760968 8760969 8760970

8760971 8760972 8760973 8760974 B760975

8760976 8760977 8760978 8760979 8760980

8760981 8760982 B760983 8760984 8760985

8760986 8760987 B760988 8760989 8760990


212 Brooksbank Avenue North Vancouver 8C V7 J 2C 1 Phone: 604 984 0221 Fax: 604 964 0218 www.alschemex.com

ME·ICP41 ME-ICP41 ME·XRF06 ME-XRF06 ME-XRF06 ME-XRF06

W Zn S.02 AI203 Fe203 CaO ppm ppm % % % % 10 2 0.01 0.Q1 0.D1 0.01

<10 27

<10 44 <10 34 <10 36 <10 36

<:10 44 46.36 17.54 12.54 10,49 37.81 11.28 13.70 17.11

<10 46

<10 28 <10 29 <10 33

<10 36 <10 22 <10 33

<10 68

<10 35

<10 35 <:10 37 <10 28

<10 62

<10 43 45.05 18.01 14.10 10.32


Project RG-08-04


ME-XRF06 ME-XRF06 ME-XRF06 ME-XRFOS ME-XRF06 ME-XRF06

MgO Na20 K20 Cr203 T.02 MnO

% % % % % %

0.01 0.01 0.01 Q.01 Q.01 0.01

8.33 2.42 0.28 0.01 0.96 0.17 8,25 1.61 0,49 0.02 1.38 0.14

6.30 2.73 0.34 <0.01 1.92 0.13



TB08160023

ME-XRF06 ME·XRF06 ME·XRF06

P205 SrO BaO

% Q/o %

0.001 0.01 0.Q1

0.035 0.08 0.03 6,492 0.07 0.05

0.377 0.12 0.08

A Method Analyte

Unit. Sample Description LOll

8760951 8760952 8760953 8760954 B760955

8760956 8760957 8760958 8760959 8760960

8760961 8760962 B760963 8760964 B760965

8760966 8760967 B760968 8760969 8760970

8760971 8760972 8760973 8760974 8760975

8760976 8760977 8760978 8760979 8760980

8760981 8760982 8760983 8760984 8760985

8760986 8760987 8760988 8760989 8760990


212 8rooksbank Avenue North Vancouver 8e V7 J 2C 1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com

ME-XRF06 ME-XRF06

LOI Total

% %

0.01 0.Q1

0.52 99.76 1.08 99.48

0.16 99.64


Project: RG-08-04


Page: 2-G Total # Pages: 3 (A - G)


TB08160023

Method Anal,-te

Unit. Sample Description LOR

8760991 8760992 8760993 8760994


212 8rooksbank Avenue North Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com

WEI·21 ME-MSa! ME-MS81 ME-MS81 ME-MSa1 ME-MSB1

Recvd WI. Ag Ba Ce Co Cr


0,02 1 0.5 0.5 0,5 10

0.39 <1 811 17.7 60.3 30 0.34 <1 908 16.5 58.2 150 0.57 <1 532 250 25.S 60 0.70 <1 498 416 13.9 20


Project: RG-08-04


ME·MS81 ME·MS81 ME-MSB1 ME-MSal ME-MSa1 ME·MS8!

Cs Cu Dy Er Eu Ga


0.Q1 5 005 0,03 0,03 0,1

0.16 56 1.30 0.62 1.71 17.2 0.04 23 0.98 0.46 1.62 15.2 2.51 14 9.83 6.51 1.40 27.9 1.41 9 12.80 8.61 1.28 30.0



TB08160023

ME·MSal ME-MS81 ME-MSBI

Gd Hf Ho

ppm ppm ppm

0.05 0.2 0,01

2.04 0.5 0.25 1.64 0.3 0.18

12.10 15.6 2,04 18.00 28.0 2.62

Method Anatyte


B760991 B760992 B760993 B760994


212 Brooksbank Avenue North Vancouver Be V7 J 2Cl Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com

ME-MS81 ME-MSB1 ME-MSBl ME-MSB1 ME-MSBl ME·MS81

La Lu Mo Nb Nd Ni


0.5 0.01 2 0.2 0.1 5

7.6 0.06 <2 3.4 10.1 33 7.5 0.04 <2 2.0 9.1 19

137.5 0.94 2 327 75.4 24 223 1.29 2 249 125.0 6


Project RG-08-04


ME·MS81 ME·MS81 ME·MS81 ME·MS81 ME-MSBl ME·MS81

Pb Pr Rb 8m Sn Sr


5 0.03 0.2 0.03 1 0.1

<5 2.41 3.1 2.03 <1 862 <5 2.21 1.8 1.72 <1 1045 11 24.3 137.5 11.90 3 556 17 40.7 159.0 17.85 6 451



T808160023

ME·MS81 ME·MSSl ME-MS81

Ta Tb Th

ppm ppm ppm

0.1 0.Q1 0.05

0.2 0.27 0.22 0.1 0.21 0.16 11.8 1.65 74.6 11.4 2.26 74.3

A . .

Method Analyte


B760991 B760992 B760993 8760994

ALS Chemex EXCELLENCE IN ANAL YTICAL CHEMISTRY ALS Caoada Ltd.

212 Brooksbank Avenue North Vancouver BC V7 J 2C 1 Phone: 604 984 0221 Fax: 604 9B4 0218 www.alschemex.com

ME-MS81 ME-MSSl ME-MSSl ME-MSSl ME-MSal ME-MSBl

TI Tm U V W Y


0.5 0.01 0.05 5 1 0.5

<0.5 0.08 <0.05 524 <1 6.4 <0.5 0.06 <0.05 300 <1 4.8 <0.5 0.96 9.53 67 3 48.7 <0.5 1.26 15.00 60 4 69.4


Project: RG-08-04


ME-MSSl ME-MS81 ME-MS81 PGM-ICP23 PGM-ICP23 PGM-ICP23

Yb Zn Zr Au PI Pd


0.03 5 2 0.001 0.005 0.001

0.44 109 18 0.31 84 12 6.33 64 483 8.70 76 1160



TB08160023


Ag AI As

ppm % ppm

0.2 0.01 2

Method Analyte


8760991 8760992 8760993 B760994


212 8rooksbank Avenue North Vancouver 8C V7 J 2C 1 Phone: 604 984 0221 Fax: 604 984 0218 www,alschemex,com

ME-ICP41 ME-ICP41 ME~CP41 ME-ICP41 ME:-ICP41 ME-ICP41

B Ba Be BI C. Cd


10 10 0,5 2 0,01 0,5

To EAST WEST RESOURCE CORPORATION 1158 RUSSELL STREET THUNDER BAY ON P7B 5N2

Project: RG-08-04



Co Cr Cu Fe Ga Hg

ppm ppm ppm %. ppm ppm

1 1 1 0,01 10 1



T808160023


K La Mg

% ppm %

0,01 10 0.01

Method Analyto Units


8760991 8760992 8760993 8760994

ALS Chemex EXCELLENCE IN ANAL YTICAL CHEMISTRY ilLS Canada Ltd.

212 Brooksbank Avenue North Vancouver Be V7J 2C1 Phone: 604 984 0221 Fax: 604 984 Q218 www.alschemex.com


Mn Mo Na NI P Pb


5 1 0.01 1 10 2


Project: RG-08-04


ME-ICP41 ME.fCP41 ME-ICP41 ME-ICP41 ME-ICP41 ME·ICP41

S Sb Sc Sf Th TI

% ppm ppm ppm ppm %

0.01 2 1 1 20 0.01



TB08160023


TI U V

ppm ppm ppm

10 10 j

Method An.'yte

Unite Sample Description LOR

8760991 8760992 8760993 8760994


212 Brooksbank Avenue North Vancouver BC V7J 2C1 Phone 6049640221 Fax: 604 984 0218 www.alschemex.com

ME-ICP41 ME-ICP41 ME-XRF06 ME-XRF06 ME-XRF06 ME-XRF06

W Zn 5i02 AI203 Fe203 CaO

ppm ppm % % % %

10 2 0,01 0,01 0,01 0,01

43A4 16,59 16.57 10.61 44,92 18,02 13.92 9,91


Project RG-08-04



CERTIFICATE OF ANALYSIS TB08160023

ME-XRF06 ME-XRF06 ME-XRF06 ME-XRF06 ME-XRF06 ME-XRF06 ME-XRF06 ME-XRF06 ME-XRF06

MgO Na20 K20 Cr203 Ti02 MnO P205 S!0 BaO

% % % % % % % % %

0,01 om om 0.01 0.01 0,01 0.001 0,01 0.01

6Al 2A2 0,32 0.01 2.89 0.15 0,132 0,09 0.10 7,86 2,64 0,33 0.03 1.57 0.15 0.227 0,12 0.12

Method Analyte


B760991 B760992 B760993 B760994


212 Brooksbank Avenue North Vancouver BC V7 J 2C1 Phone: 604 984 0221 Fax 6049840218 www.alschemex.com

ME-XRF06 ME-XRF06

LOI Total

% %

0.01 0.01

-0.07 99.66 -0.07 99.95


Project RG-08-04


Page: 3 - G Total # Pages: 3 (A - G)


TB08160023

APPENDIXF

Vancouver Petrographic Report (Thin Sections) RG-08-04

PETROGRAPHIC REPORT ON 4 SAMPLES FROM ARMSTRONG PROJECT

Report for:

SUMMARY:

Bob Middleton East West Resources Corporation 1158 Russell Street Thunder Bay, Ont. P7B 5N2 (807 622 9734)

Invoice 080957

Nov. 21,2008.

Capsule descriptions are as follows:

RG08-4 441.6: fine-grained biotite-olivine gabbro with accessory opaques (magnetite and ilmenite?) and locally significant alteration to actinolitic amphibole, talc/sericite, iddingsite and traces of clay?/sericite.

RG08-4 446.6: coarse biotite-olivine gabbro with significant accessory opaque oxides (magnetite and ilmenite), minor sulfides (pyrite after pyrrhotite) and local slight alteration to late-magmatic hornblende, actinolitic amphibole, talc/sericite, tremolitic amphibole and traces of clay?/sericite.

RG08-4 667: coarse biotite-olivine gabbro with minor accessory opaque oxides (likely magnetite and ilmenite), and local moderate alteration to tremolitic-actinolitic amphibole, taic/sericite, secondary magnetite and traces of green biotite and clay?/sericite.

RG08-4 835: fine, plagioclase-rich, biotite-olivine (troctolitic) gabbro with significant accessory opaque oxides (likely magnetite and ilmenite). and only minor alteration to tremolitic-actinolitic amphibole, talc/sericite, minor secondary magnetite and traces of clay?/sericite.

Detailed petrographic descriptions and photomicrographs are appended (on CD). If you have any questions regarding the petrography, please do not hesitate to contact me.

Craig H.B. Leitch, Ph.D., P. Eng. (250) 653-9158 craig.leitch@,gmail.com 492 Isabella Point Road, Salt Spring Island, B.C. Canada V8K 1 V4

2

RG08-4 441.6: FINE-GRAINED BIOTITE-OLIVINE GABBRO (ACCESSORY OPAQUE OXIDES) ALTERED TO ACTINOLITIC AMPHIBOLE, TALC-IDINGSITE?-CLA Y?/SERICITE

Described as fine-grained; hand specimen shows dark greenish grey, fine-grained gabbro with relatively massive texture, locally cut by narrow dark veinlets. The rock is strongly magnetic, but shows no reaction to cold dilute HCI, and no stain for K-feldspar in the etched offcut. Modal mineralogy in thin section is approximately:

Plagioclase (labradorite/bytownite?) 45% Clinopyroxene (augite?) 20% Amphibole (secondary, largely actinolitic?) 15% Olivine (partly relict) 10% Talc/sericite, minor iddingsite? (after olivine) 3% Opaque (magnetite?) 2%

(ilmenite?) 2% Biotite 1-2% Clay?/sericite (after plagioclase) 1-2%

This gabbroic sample consists mainly of plagioclase and lesser mafic minerals (clinopyroxene or amphibole after pyroxene, partly relict olivine, minor biotite) plus accessory opaque oxides. It is locally strongly amphibole altered along irregular fracture zones. Olivine and relict olivine is commonly closely associated with pyroxene aggregates, and opaques with biotite.

Plagioclase forms mainly euhedral crystals up to about 2 mm long, with slight preferred orientation, and partly enclosing the mafic minerals in a sub-ophitic texture. Twinning is regular but locally slightly bent, and no zoning is apparent. Composition appears to be calcic, around labradorite/bytownite (An70) based on extinction Y/'010 up to 36 degrees. The crystals are essentially unaltered apart from traces of clay?/sericite along microfractures, especially near the amphibole altered fracture zones.

Clinopyroxene forms somewhat irregular to skeletal, mainly subhedral crystals mostly <1 mm in size although locally somewhat glomeratic to about 2.5 mm long, elongated sub-parallel to a weak foliation. They aggregates generally enclose unaltered to partly altered relict olivine, and locally minor biotite and opaque oxides. The pyroxene has pale brownish colour (salite?) and extinction angle about 45 degrees, suggestive of augite or salitic augite. In places, most crystals are partly altered, starting around the rims, to significant secondary amphibole as ragged fibrous subhedra mostly <0.5 mm long. In general, core areas have brownish to olive-green pleochroism (latemagmatic hornblende?) and outer parts have pale sea-green pleochroism with extinction angle around 18 degrees, suggestive of actinolite and/or actinolitic hornblende (?).

Olivine (or olivine relics) have somewhat rounded or ragged irregular to subhedral outlines mostly <0.7 mm long (glomeratic to 1 mm), contained within pyroxene crystals or aggregates. The olivine is more strongly fractured than pyroxene, with traces of minute secondary magnetite (?) along the fractures. In places the olivine is partly to locally completely replaced or pseudomorphed by very fine-grained talc/sericite (randomly oriented flakes <35 microns in diameter locally mixed with actinolite) or lesser brown to greenish-brown iddingsite (?) as ragged anhedra <0.1 mm in diameter.

Biotite forms small ragged, irregular subhedral crystals mostly <0.5 mm in diameter, with dark red-brown pleochroism and commonly wrapped around pyroxene or amphibole altered pyroxene, or interstitial to pyroxene and plagioclase.

Accessory opaques appear to be mostly magnetite and ilmenite ('1) forming irregular subhedral crystals mainly <0.5 mm in diameter, associated with biotite and olivine or relict olivine (fine-grained magnetite in the latter case is likely partly to mostly secondary). No sulfides are visible.

In summary, this represents fine-grained biotite-olivine gabbro with accessory opaques (magnetite and ilmenite?) and locally significant alteration to actinolitic amphibole, talc/sericite, iddingsite and traces of clay?/sericite.

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RG08-4 446.6: COARSE BIOTITE-OLIVINE GABBRO WITH SIGNIFICANT ILMENITEMAGNETITE, ALTERED TO SECONDARY AMPHIBOLE-TALC/SERICITE

Described as coarse gabbro; hand sample shows dark blackish grey, coarse-grained mafic to ultramafic rock with clotty, mottled texture. The rock is magnetic, but shows no reaction to cold dilute HCI, and no stain for K-feldspar in the etched offcut. Modal mineralogy in thin section is approximately:

Plagioclase (labradorite/bytownite?) 40% Clinopyroxene (augite?) 35% Magnetite (partly secondary) 7% Amphibole (secondary, actinolitic) 7%

(late magmatic, hornblende?) 3% Olivine (partly relict) 3% Ilmenite 2% Biotite 1-2% Pyrite, pyrrhotite 1 % Talc/sericite (after olivine), clay? /sericite (after plagioclase) < 1 %

This gabbroic sample consists mainly of plagioclase and mafic minerals (pyroxene or amphibole after pyroxene, biotite, olivine partly altered to talc/sericite) plus significant accessory opaque oxides. It is similar in composition to the sample from 441.6m, but contains less olivine and is less altered. Relict olivine is erratically distributed as coarse crystals included within pyroxene-rich zones.

Plagioclase forms mainly euhedral crystals up to about 5 mm long, with random orientations, partly enclosing the mafic minerals in a sub-ophitic texture. Twinning is regular but locally slightly bent, and no zoning is apparent. Composition appears to be calcic, around labradorite-bytownite (An72) based on extinction YI\Ol 0 up to 37 degrees. The crystals are essentially unaltered apart from traces of clay?/sericite along microfractures.

Clinopyroxene forms somewhat irregular to skeletal, mainly subhedral crystals up to 7 mm long although locally glomeratic to almost 1 cm. They locally include plagioclase or rarely slightly altered olivine, and are locally associated with biotite and coarse, significant oxides. The pyroxene has pale brownish colour and extinction angle about 45 degrees, suggestive of augite or salitic augite. In places, most crystals are partly mantled by brown late-magmatic hornblende in parallel position as ragged subhedra to 1.5 mm, and then both are altered. starting around the rims, to secondary amphibole as ragged fibrous subhedra mostly <0.5 mm long, \\lith sea-green pleochroism and extinction angle around 18 degrees, suggesting actinolite or possibly actinolitic hornblende (?).

Biotite forms ragged, irregular subhedral crystals up to 3.5 mm in diameter (although mainly 1.5 mm), with dark red-brown pleochroism and commonly wrapped around pyroxene or amphibole altered pyroxene, or interstitial to pyroxene and plagioclase, and closely associated with oxides.

Olivine (partly relict) has somewhat rounded or ragged irregular to subhedral outlines up to 8 mm long, commonly mantled by a zone in which the olivine is altered along fractures to fine-grained talc/sericite and minor amphibole, with traces of minute secondary magnetite (?) along the fractures. Locally areas within these olivine crystals are pseudomorphed by fine-grained fibrous, almost colourless amphibole (tremolite-actinolite?).

Accessory opaques appear to be mostly ilmenite and minor magnetite, forming skeletal to irregular subhedral crystals up to 6 mm in diameter, interstitial to plagioclase/clinopyroxene, closely associated with biotite. Minor sulfides appear to be mostly pyrite (subhedra to 0.5 mm, mostly after pyrrhotite, some of which remains as subhedra <0.1 mm), aggregating in irregular blebs and subhedra up to about 2 mm long.

In summary, this is coarse biotite-olivine gabbro with significant accessory opaque oxides (magnetite and ilmenite), minor sulfides (pyrite after pyrrhotite) and local slight alteration to latemagmatic hornblende, actinolitic amphibole, talc/sericite, tremolitic amphibole and traces of clay?/sericite.

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RG08-4 687: COARSE BIOTITE-OLIVINE GABBRO WITH MINOR ILMENITE?-MAGNETITE, ALTERED TO SECONDARY AMPHIBOLE-TALC/SERICITE-MAGNETITE-GREEN BIOTITE

Described as coarse gabbro; hand sample shows dark blackish grey, coarse-grained mafic to ultramafic rock with very irregular clotty, mottled texture (highlighted in etched offcut). The rock is magnetic, but shows no reaction to cold dilute HCl, and no stain for K-feldspar in the etched offcut. Modal mineralogy in thin section is approximately:

Plagioclase (labradorite?) 50% Clinopyroxene (augite?) 30% Olivine (partly relict) 7% Biotite 3-5% Amphibole (secondary, actinolitic) 2-3% Talc/sericite (after olivine) 2-3% Ilmenite (?) 1-2% Magnetite (partly secondary) 1-2% Green biotite (after olivine), trace magmatic hornblende <1 % Clay?/sericite (after plagioclase) <1%

This gabbroic sample consists of coarse plagioclase and mafic minerals (pyroxene or amphibole after pyroxene, olivine partly altered to talc/sericite, biotite) plus minor accessory opaque oxides. It is similar in composition to the sample from 446.6m, but contains more olivine and less oxide. Olivine distribution is zoned, with distinct olivine-rich and pyroxene-rich zones at ~45 degrees to core axis.

Plagioclase forms mainly euhedral crystals up to about 3 mm long, with random orientations, but commonly glomeratic to 1 cm or so, partly enclosing the mafic minerals in a sub-ophitic texture. Twinning is regular but locally slightly bent; zoning is weak and slight. Composition appears to be calcic, around labradorite (An60) based on extinction yJ\O 1 0 up to 32 degrees. The crystals are essentially unaltered apart from traces of clay?/sericite along microfractures.

Clinopyroxene forms somewhat irregular to skeletal, mainly subhedral crystals up to 7 mm long although locally glomeratic to almost 1 cm. They locally include plagioclase or biotite, but olivine or altered olivine is mainly found around margins. The pyroxene has pale brownish colour and extinction angle about 45 degrees, suggestive of salitic augite. In places, some crystals are partly altered, starting around the rims or along fractures, to secondary amphibole as ragged fibrous subhedra mostly <0.5 mm long (but optically continuous up to 4 mm along veinlets), with variable pale coloured to bright sea-green pleochroism and extinction angle around 14 degrees, suggesting tremolite-actinolite or possibly actinolitic hornblende (?). Brown late-magmatic hornblende is rare.

Olivine (partly relict) crystals have somewhat rounded or ragged, corroded irregular to subhedral outlines up to 2 mm in diameter, commonly partly replaced or mantled by a zone in which the olivine is altered along fractures to fine-grained talc/sericite, very fine-grained «15 micron) secondary magnetite (7) along the fractures, and intimately intermixed amphibole, locally with traces of green biotite (aggregates to 0.4 mm of randomly oriented sub/euhedral flakes <65 microns in size). Locally the cores, or entire olivine crystals, are pseudomorphed by fine-grained talc/sericite and the fibrous, pale greenish to almost colourless amphibole (tremolite-actinolite?).

Biotite forms ragged, irregular subhedral crystals up to 3.5 mm in diameter (commonly glomeratic), with dark red-brown pleochroism, commonly surrounding or interstitial to pyroxene or amphibole altered pyroxene, or pyroxene and plagioclase, in places closely associated with oxides.

Accessory opaques are likely mostly ilmenite and magnetite, forming skeletal to irregular subhedral crystals up to 2.5 mm in diameter, interstitial to plagioclase/clinopyroxene and closely associated with biotite.

In summary, this is coarse biotite-olivine gabbro with minor accessory opaque oxides (likely magnetite and ilmenite), and local moderate alteration to tremolitic-actinolitic amphibole, talc/sericite, secondary magnetite and traces of green biotite and clay?/sericite.

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RG08-4 835: FINE PLAGIOCLASE-RICH BIOTITE-OLIVINE (TROCTOLITlC) GABBRO WITH ACCESSORY OPAQUE OXIDES, APATITE, SLIGHTLY ALTERED TO ACTlNOLITlC AMPHIBOLE, TALC/SERICITE

Described as troctolite (any olivine?) or feldspar-rich gabbro; hand specimen shows mediumdark grey, fine- to medium-grained, relatively massive, almost featureless gabbro with very faint foliation SUb-perpendicular to core axis. The rock is not magnetic, shows no reaction to cold dilute HCI, and no stain for K-feldspar in the etched offcut. Modal mineralogy in thin section is approximately;

Plagioclase (labradorite?) 60% Clinopyroxene (augite?) 20% Olivine (partly relict) 12% Opaque (ilmenite, magnetite (partly secondary) 3-5% Amphibole (secondary, tremolitic!actinolitic) 1-2% Talc/sericite (after olivine) 1-2% Biotite 1% Clay?/sericite (after plagioclase) <1 % Apatite <1%

This gabbroic sample consists of fine-grained plagioclase hosting lesser mafic minerals (clinopyroxene; olivine partly altered to talc/sericite or tremolite/actinolite; rare biotite) plus significant accessory opaque oxides, trace apatite. It is relatively rich in plagioclase and olivine, but poor in clinopyroxene and biotite. Olivine distribution is even, with no obvious concentrations apparent.

Plagioclase forms mainly euhedral crystals mm long, with random orientations, but commonly glomeratic to 7 mm or so, commonly enclosing the mafic minerals in an ophitic texture. Twinning is regular but locally spindle-shaped; zoning is essentially absent. Composition appears to be calcic, around labradorite (An60) based on extinction YAOIO up to 31 degrees. The crystals are essentially unaltered apart from traces of clay?/sericite along microfractures.

Clinopyroxene forms somewhat irregular to skeletal, mainly subhedral crystals up to 2.5 mm long, rarely glomeratic to 3 mm. They locally include biotite or rare apatite (euhedra <0.4 mm long), but olivine/altered olivine and opaque oxides are mainly found around margins of pyroxene. The pyroxene has pale brownish colour and extinction angle about 45 degrees, suggestive of salitic augite. Alteration to almost colourless, secondary tremolitic-actinolitic amphibole is only rarely noted around the rims of some pyroxene (mainly adjacent to talc/sericite altered olivine).

Olivine occurs as (mainly only slightly altered) crystals with somewhat rounded/corroded, irregular sub/euhedral outlines up to almost 2 mm in diameter, locally partly replaced or rimmed by a zone in which the olivine is altered along fractures to fine-grained talc/sericite, intimately intermixed amphibole, and very fine-grained «20 micron) secondary magnetite (?) along the fractures. Th finegrained talc/sericite is difficult to distinguish from the fibrous, pale greenish to almost colourless amphibole (tremolite-actino1ite?), both mostly 50 microns in size.

Biotite occurs as small, sub/euhedral crystals mostly <0.75 mm in diameter (locally glomeratic, or mantling opaque oxides), with dark red-brown pleochroism, generally interstitial to pyroxene and plagioclase, and closely associated with oxides.

Accessory opaques are likely mostly ilmenite and magnetite, forming skeletal to irregular subhedral crystals up to 0.75 mm in diameter, interstitial to plagioclase/clinopyroxene/olivine and closely associated with the biotite.

In summary, this is fine, plagioclase-rich, biotite-olivine (troctolitic) gabbro with significant accessory opaque oxides (likely magnetite and ilmenite), and only minor alteration to tremoliticactinolitic amphibole, talc/sericite, minor secondary magnetite and traces of clay?/sericite.

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Drill Report Pillar Lake Area Thunder Bay Mining … · This drill program was planned using knowledge gained from the 2007 mapping ... this 2008 program have been planned in order