GM 63746 PROSPECTING AND MAPPING RESULTS AND INTERPRETATIONS, GOLDBROOK RAGLAN PROJECT
GOLDBROOK ventures
Goldbrook Ventures 1550-200 Burrard Street Vancouver, B.C. V6C 3L6
Tel: 604-683-8083 Fax: 604-683-8087
GOLDBROOK RAGLAN PROJECT: 2007 PROSPECTING AND MAPPING RESULTS AND INTERPRETATIONS
Assessment Report for Goldbrook Ventures Inc.
By: S. Jonnes, B.Sc. (Hons) Supervised & Approved by: B. Grant, PGeo
NTS 35G/06, 35G/07, 35G/08, 35G/10, 35G/09 Belanger Camp: 498032mE, 6802503mN NAD 83, UTM Time Zone 18N
May 29, 2008 essources naturelles et faune, Québec evitiâNo~ 20C~8 2 2 AOUT 2008 REÇU 2 1 ; C ~s I~ I 41IERS DIR. INFORM. GÉOL. ~ 0 Y01 2008 DIRECTIO~
DIRECTION DES TITRES PAINTERS GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
TABLE OF CONTENTS
1. INTRODUCTION 5 2. LOCATION AND ACCESS 6 3. REGIONAL GEOLOGY 10 4. MINERAL DEPOSIT TYPES 11 5. GBK PROSPECTING AND MAPPING PROGRAM 2007 13 5.1. Relevant Claims 14 6. PROPERTY GEOLOGY 23 6.1. Bravo 23 6.2. Delta East 25 6.3. Delta South 27 6.4. Echo 28 6.5. Hellcat 30 6.6. Kozmo 30 6.7. PAD, East Pillow, R2 30 6.8. Pillow Lake 31 6.9. SuperFortress 31 6.10. Timtu 33 7. ASSAY RESULTS 33 8. RECOMMENDATIONS AND CONCLUSIONS 38 9. COST STATEMENT 40 10. REFERENCES 41 11. STATEMENT OF QUALIFICATIONS 43 12. APPENDIX 1: 2007 Field Report on the GBK Raglan Area: Investigations and Conclusions by M. Liard 44 13. APPENDIX 2: Raw Grab Sample Geological Data 58 14. APPENDIX 3: Raw Geochemical Data 72 15. APPENDIX 4: Grab Sample Assay Certificates 76 16. APPENDIX 5: September 14, 2007 News Release 88
2 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
TABLE OF FIGURES
Figure 1. Location map of the Goldbrook Raglan Properties in Nunavik, northern Québec. 7
Figure 2. Geological setting and distribution of major NiS deposits and showings about the Goldbrook Raglan Project properties. 8
Figure 3a. Claims map showing individual cells with prospecting and sampling locations (green circles), near to the Mystery showing. 15
Figure 3b. Claims map showing individual cells with prospecting and sampling locations (green circles), near to the Sylvie, Getty and Allard showings. 16
Figure 3c. Claims map showing individual cells with prospecting and sampling locations (green circles), near to the Timtu showing. 17
Figure 3d. Claims map showing individual cells with prospecting and sampling locations (green circles), near to the Echo South and Liberator showings 18
Figure 3e. Claims map showing individual cells with prospecting and sampling locations (green circles), near to the Echo East showing 19
Figure 3f. Claims map showing individual cells with prospecting and sampling locations (green circles), on the Bravo property. 20
Figure 3g. Claims map showing individual cells with prospecting and sampling locations (green circles), on the Thunder claim block. 21
Figure 4. Mapping and prospecting stations (solid black circles), superimposed on the regional GSC geology on the Ungava peninsula. 22
Figure 5. Mapping and prospecting traverses (overlapping blue circles) and samples sites (triangles) at Bravo East and Bravo West, overlying a property wide VTEM survey base map. Map author unknown. 24
Photo 1. A blasted trench at Bravo East, showing_ mineralized ultramafic rocks at surface. 25
Figure 6. Delta East and Hellcat traverses (solid blue circles) and station locations (triangles) on VTEM overlay. Map author unknown. 26
Photo 2. Peter's showing; a heavily malachite stained gabbroic boulder 27
Photo 3. Echo looking south, rubbly gossan in gabbro. Ultramafic outcrop in background. 28
Figure 7. Traverses (solid blue circles) and station locations (triangles) near the Echo showing on VTEM overlay. Map author unknown 29
3 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
Figure 8. Traverses (solid blue circles) and station locations (triangles) near the Timtu, Jabba and Echo West showings on VTEM overlay. Map author unknown. 32 Figure 9. Anomalous grab sample Ni occurrences (>0.2%) highlighted in red, on the Goldbrook Ventures Raglan Property, Nunavik, Québec. 35 Figure 10. Anomalous grab sample Cu occurrences (>0.3%) highlighted in orange, on the Goldbrook Ventures Raglan Property, Nunavik, Québec 36 Figure 11. Anomalous grab sample combined PGE+Au occurrences (>1.00 g/t) highlighted in grey, on the Goldbrook Ventures Raglan property, Nunavik, Québec. 37 Figure 12. Prospecting and mapping traverses (solid white lines) on the Belanger property on VTEM overlay. Map author: M. Liard. 47 Figure 13. Prospecting and mapping traverses (solid white lines) on the Bravo property on VTEM overlay. Map author: M. Liard. 51
TABLES
Table 1. Individual claim cells that were worked on in 2007 during the mapping and prospecting program. 14 Table 2. 95th percentiles based on 93 grab samples collected on the Raglan property in 2007. 34 Table 3. Anomalous grab sample results with Ni results > 0.15% highlighted in red, Cu results > 0.3% highlighted in yellow, and PGE+Au results >1.00 g/t highlighted in green 34 Table 4. Raw station data including UTM coordinates, sample ID, and geological descriptions for 361 mapping and prospecting locations. 59 Table 5. Geochemical data for 93 grab samples collected during the Goldbrook Raglan summer exploration 2007. 73
4 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
1. INTRODUCTION
Goldbrook Ventures Inc. (GBK) conducted prospecting, geological mapping and sampling work on its Belanger and Bravo properties, in Nunavik Québec, from July to September in 2007. The two properties are part of six claim blocks owned 100% by GBK, namely Wakeham, Ungava, Masuparia, Nuvilik , Bravo and Belanger. The purpose of the summer 2007 prospecting and geological mapping program was to continue to explore for magmatic nickel sulfide deposits, in conjunction with airborne geophysical surveys, ground geophysical surveys, and diamond drilling that were also conducted in the summer of 2007.
Prospecting and mapping was conducted in 13 areas on the GBK property, including Bravo West, Bravo East, Delta South, Delta East, Echo, Hellcat, Kozmo, Pillow Lake, East Pillow, PAD, R2, SuperFortress and Timtu. The following compilation report is a summary of the geology encountered in these areas together with assay results for select samples. At the end of the 2007 exploration season, 361 geological stations had been made and 93 grab samples had been collected for assay analysis. Appendix 2 and 3 contain all the raw geological and geochemical data, respectively. All grab samples were sent to ACCURASSAY Laboratories in Thunder Bay, Ontario and the samples were analysed for base and precious metals. Assay certificates have been included in Appendix 4 of this report.
Several areas showed favourable geology and encouraging assay results, and maps with the best nickel, copper and PGE+Au grades have been included in this report. Several geologists were responsible for mapping and prospecting in the summer of 2007, and Appendix 1 is a stand alone report compiled by M. Liard, one of the six geologists. The property geology section in this report is a compilation and summary of the notes made by the above mentioned geologists. Recommendations and suggestions for further exploration in 2008 are primarily based on their comments.
5 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 2. LOCATION AND ACCESS
The Wakeham, Ungava, Masuparia, Nuvilik, Belanger and Bravo properties are located within National Topographic System (NTS) sheets 25E/05, 35F/01, 35F/02, 35F/08, 35G/04, 35G/05, 35G/06, 35G/07, 35G/09, 35G/10, 35G/11, 35H/12, 35H/05, 35H/09, 35H/11, 35H/02, 35H/06, 35H/07, 35H/08, 35H/10, and 35H/11 (Fig. 1) in northern Quebec (Nunavik). The centre of the project area is located approximately 10 km south of Xstrata's (Katinniq) mine. From the centre, the project area extends 70 km to the east and 100 km to the west and southwest (Fig. 2).
The hamlet of Salluit located on the arctic coast approximately 93 km north of the properties, serves as the primary access point to the project area, with daily scheduled commercial flights (First Air, Air Inuit) from Montreal, Ottawa and Igaluit. Heavy equipment, fuel and freight can be shipped to Kangiqsujuaq by ocean barge, with arrivals in July, August and September, and transported to the field area by ski-equipped aircraft before the spring ice-breakup or by large helicopter (e.g., B214ST or Sikorsky S61).
The base of field operations for the Goldbrook Raglan Project was the Guindeau camp, located on the south shore of Lac Guindeau (572282 mE, 6828269 mN; NAD 83 Zone 18). During the summer, the properties are best accessed by helicopter. Float planes can land at the Esker Lake airstrip and supplies transported by helicopter 30 km east to Guindeau camp. There are at least three other airstrips in the region: Katinniq (Raglan mine), Purtuniq (Asbestos Hill), and Deception Bay. The Katinniq airstrip is a private airfield controlled by Xstrata Nickel (formerly Falconbridge Ltd). The remaining airstrips are listed in the 1995 VFR Aeronautic Navigational Map as abandoned and in uncertain condition.
6 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
500000 550000 600000 650000 Â C w en So cD
Legend — Goldbrook Claims Pingualuit Park X Raglan_mine
Figure 1. Location map of the Goldbrook Raglan Properties in Nunavik, northern Québec.
7 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
450000 500000 550000 600000 650000 o 8 /111rAmillIMINIIIIPP•11Q• -- 10"- 8 NiS Deposit or Major Occurrence 1111 Peridotite
Parent, Watts, Spartan Groups 62°ri
Chukotat Group
Povungnituk Group Q
o Gneisses 8
Nuvilik Property Kangiq- sujuac
~ ig .c
1:1,000,000 Km 0 15 30 60
75M/,, 74°W 7.-,",., r,.
Figure 2. Geological setting and distribution of major NiS deposits and showings about the Goldbrook Raglan Project properties. The old NovaWest Claim block in the centre of the map area was acquired by Goldbrook Ventures in 2007.
8 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
The project area is located north of the tree line. Topography ranges from rolling hills at -300 metres above sea level on the Belanger property in the west to >600 metres above sea level on the Wakeham property in the east. Outcrop exposure ranges from very poor to excellent. In some areas, exposed rock has been affected by frost action, reducing many outcrops to heaved rubble and angular blocks. Lowland areas are typically covered by till and boggy tundra to swamps, with scattered boulder fields of frost-heaved blocks and cobbles. The entire region is subject to permafrost to depths of up to 540 metres. Vegetation consists mostly of grass and moss.
Typical fauna in the region include caribou, wolf, fox, hare, snowy owl, Peregrine Falcon, Canada geese, and rodents. There are no black bears this far north, but Polar Bears have been sighted sporadically on the properties since 2004. Local rivers and lakes contain char and trout.
Summers are short, with temperatures ranging from 0°C to 20°C during late June to early September. Lake and river ice breaks-up in early July and lakes and rivers freeze in late September to early October. Weather becomes increasingly unpredictable in late summer and early autumn with fog, freezing rain, snow squalls and high gusty winds. The unpredictable weather increases stand-by time for helicopters and diamond drill rigs, and therefore affects exploration costs adversely, particularly in June and September. Ground work during the winter months is possible, but is largely restricted to ground geophysical surveys as insufficient daylight, extreme cold weather and lack of water hamper other kinds of work.
The properties are located immediately adjacent to claims currently held by Xstrata Nickel (formerly Falconbridge Limited), Canadian Royalties, Knight Resources/Anglo American, and Resolve Ventures (among others).
9 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
3. REGIONAL GEOLOGY
Regionally the GBK Raglan Project is underlain by rocks of the Cape Smith Belt, which extends for 375 km across the Ungava Peninsula of northwestern Quebec. The Cape Smith Belt is a thin-skinned foreland thrust belt that constitutes the northeast extension of the Trans-Hudson Orogen (known locally as the Ungava Orogen), an early Proterozoic collisional zone between the Archean Superior Craton and the Archean-Proterozoic Churchill Craton (Hynes and Francis, 1982; Hoffman, 1990). The Trans-Hudson Orogen also includes the Thompson Belt of Manitoba, which contains the productive Thompson Nickel Belt, and the Labrador Trough to the southeast of the Cape Smith Belt.
In the Goldbrook Raglan Project area, the Cape Smith Belt consists of two major Proterozoic units, the Povungnituk Group and the Chukotat Group (Bergeron, 1959). The Povungnituk Group consists of a lower sedimentary sequence (Lamarche and Dumas sub-groups; PPoi and PPosd), a middle volcanic sequence (Beauparlant sub-group; PPob and PPoga), and an upper sedimentary sequence (Nuvilik sub-group; PPos). The lower sequence consists of conglomerate, sandstone, iron formation, semipelite and dolomite in the base and sandstone, semipelite, pelite, minor basalt and mafic volcaniclastic sedimentary rocks in the top. The middle sequence of the Povungnituk Group consists of basalt, rhyolite and mafic volcaniclastic sedimentary rocks. The basalt is tholeiitic with continental affinity (Hynes and Francis, 1982). The upper sequence of the Povungnituk consists of sandstone and shale with minor basalt. The Povungnituk Group represents a continental rifting sequence.
The Chukotat Group (Bergeron, 1959) consists of massive and pillowed basalt, hypabyssal ultramafic and mafic intrusions, and discrete and interflow sedimentary rock units. The basalt ranges in composition from Mg-rich olivine-phyric komatiitic basalt at the base through pyroxene-phyric to plagioclase-phyic tholeiitic n-MORB equivalents at the top. The basalts are of oceanic affinity (Hynes and Francis,
10 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
1982) and record the change from continental rift volcanism to oceanic crust volcanism (Francis et al., 1983; Picard et al., 1990).
Pre-tectonic mafic and ultramafic sills of gabbro, pyroxenite and peridotite intrude the Povungnituk and Chukotat sequences along and adjacent to major structures and fed the overlying basalts. The intrusions within the upper Povungnituk and lower Chukotat host nickel-copper-PGE sulfide deposits, as described in the following section. Regional structure is dominated by east-west oriented fabric. The oldest structures are south verging, east-west striking D1 and D2 thrust faults, which splay off a basal décollement at the Archean basement—Proterozoic cover interface (St-Onge and Lucas, 1990, 1993). All the rock sequences and stratigraphic groups are bound by thrust faults. The Cape Smith Belt was subsequently deformed by east-west trending D3 folds and north-northwest trending D4 folds during the Hudsonian Orogeny.
4. MINERAL DEPOSIT TYPES
The ultramafic bodies of the Cape Smith Belt host many Ni-Cu-PGE (nickel- copper-platinum group element) sulfide deposits (Avramtchev, 1982; Naldrett, 1989; Barnes et al., 1992). These deposits are of three types (Lamothe, 1986; Giovenazzo et al., 1989; Giovenazzo, 1991): 1) magmatic segregation deposits of massive to disseminated sulfides located at the base of ultramafic units; 2) stratiform, disseminated sulfide deposits ("reefs") located within layered, differentiated mafic-ultramafic sills; and 3) remobilized sulfides in shear zones. The Ni-Cu-PGE mineralization occurs mainly within two currently defined geologic horizons (Giovenazzo et al., 1989; St-Onge and Lucas, 1993). The first is the Raglan (or north) horizon, located at the base of the Chukotat Group (Fig. 2) and host of many of the known economic nickel deposits in the Cape Smith Belt. The second defined favourable horizon is the Delta (or south) horizon, located within the Povungnituk Group. Ultramafic intrusions hosting nickel sulfide showings also
11 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 occur elsewhere within the Povungnituk (Avramtchev, 1982). A third horizon, the Rinfret horizon, is located to the north of the Raglan horizon, and is underexplored.
The Raglan horizon consists of a series of mafic-ultramafic bodies traceable along a strike length of 85 km. These units have been variously interpreted to be subvolcanic sills (Barnes et al., 1982) or channelized komatiitic basalt flows with peridotite (olivine cumulate) zones up to 150 metres thick (Barnes and Barnes, 1990; Lesher and Charland, 1999) within the upper sequence of the Povungnituk Group. Nine major magmatic segregation deposits have been discovered along the Raglan horizon, located at the base of host ultramafic units. These deposits from east to west are: Donaldson, Boundary, Zone 13-14, Zone 5-8, Katinniq, Zone 2, Zone 3, East Lake and Cross Lake (Fig. 2). The ultramafic units hosting mineralization contain pervasive sulfides, mainly 1%-3% finely disseminated to blebby pyrrhotite and pentlandite. The ore lenses vary considerably in size and shape, and are generally situated in footwall embayments at the base of the peridotite zones. Individual ore lenses consist of narrow zones of massive sulfide (up to a tens of metres thick with strike lengths of up to 200 metres), located along the footwall contact. Massive sulfides are overlain by net-textured and disseminated sulfides. Cobalt and platinum-group elements (PGE) are associated with the Fe-Ni sulfides.
The Katinniq deposit, currently mined by Xstrata Nickel (formerly Falconbridge Ltd. New Quebec Raglan Mines Inc.), consists of >20 discrete mineralized lenses (Chisholm et al., 1999). The lenses vary in size from 10,000 tonnes to 1.4 million tonnes, with diluted nickel grades of 2.5% to 5.0% Ni (Falconbridge Ltd., 2002). Altogether, the deposits along the Raglan horizon form an aggregate Reserve (proven and probable) of 18.1 million tonnes of 2.9% Ni and 0.8% Cu, in addition to an aggregate Resource (measured and indicated) of 2.88 million tonnes grading 2.0% Ni and 0.7% Cu.
12 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
The Delta horizon occurs within the central part of the Povungnituk Group and consists of a series of mafic-ultramafic sills and dikes (Fig. 2). The Delta horizon hosts numerous nickel sulfide deposits, such as Delta (Xstrata Nickel) and Expo- Ungava, Mesamax, Ivakkak and Allammaq (Canadian Royalties). The Delta deposit is hosted by a gabbro-peridotite sill and includes all three types of mineralization noted above (Giovenazzo, 1991). The Expo-Ungava and Mesamax deposits are hosted by discordant gabbro-peridotite bodies and could be magmatic segregation deposits.
5. GBK PROSPECTING AND MAPPING PROGRAM 2007
The 2007 field program strategy was to revisit the entire Belanger Horizon from Kozmo to Delta, as well as to reassess NovaWest's interpretations and conclusions of the Bravo claim block. Geologists Michal Russer, David Clark, Matt Liard, Dominic Lussier and prospector Sebastien Allard shared the task of mapping and prospecting the Delta-Belanger properties in the summer of 2007. Thirteen areas were the focus for geological mapping and sampling, including Bravo West, Bravo East, Delta South, Delta East, Echo, Hellcat, Kozmo, Pillow Lake, East Pillow, PAD, R2, SuperFortress and Timtu. The target areas were variably mapped and sampled (Appendix 1 and 2). Geological stations were made at 361 separate locations, and 93 grab samples were sent in for geochemical analyses to ACCURASSAY Laboratories in Thunder Bay, Ontario for base and precious metal analysis. A news release was submitted on the 14th September 2004 describing the assay results for 21 of these samples (Appendix 4).
13 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
5.1. Relevant Claims
The 2007 prospecting and mapping program took place in 3 specific claim blocks within Gold brook's property; Belanger, Bravo and Thunder. A complete list of all the claim cell numbers has been tabulated below (Table 1). All the claims are 100% owned by GBK, and registered at the Québec Ministry of Natural Resources, Wildlife and Parks. All prospecting and mapping station locations with respect to individual claim cells have been presented below (Figures 3a, b, c, d, e, f, and g).
Table 1. Individual claim cells that were worked on in 2007 during the mapping and prospecting program.
Property Cells Cells Cells Cells
Belanger 1047272 1047304 1130090 1108975 1047278 1130075 1130092 1108976 1047279 1130076 1109867 1108896 1047294 1130077 1109888 1108897 1047297 1130079 1108970 1108924 1047290 1130078 1108972 Property Bravo 1007761 1113660 1113476 2088232 2088259 18356 1113661 1113477 2088233 2088260 18357 1113662 1007681 2088234 2088261 18334 1113642 1007682 2088235 2088262 18335 1113644 1007683 2088236 2088263 18336 1113627 1007675 2088237 2088264 18337 1113601 1007670 2088238 2088265 18338 1113705 1007673 2088239 2088266 18341 1107797 1007668 2088240 2088267 18343 1006192 2088214 2088241 2088268 18344 1007726 2088215 2088242 2088269 18345 1007727 2088216 2088243 2088270 18346 1006048 2088217 2088244 2088271 18347 1007731 2088218 2088245 2088272 18348 1007733 2088219 2088246 2088273 18349 1113555 2088220 2088247 2088274 18350 1113535 2088221 2088248 1008057 1113536 2088222 2088249 1106975 1113538 2088223 2088250 18322 1113512 2088224 2088251 18323 1113513 2088225 2088252 18324 1113487 2088226 2088253 18325 1113488 2088227 2088254 18326 1113465 2088228 2088255 18327 1113466 2088229 2088256 18328 1113467 2088230 2088257 18318 1113474 2088231 2088258 Thunder 1120303 1120304 1120305 1120300
14
GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
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Figure 3a. Claims map showing individual cells with prospecting and sampling locations (green circles), near to the Mystery showing.
15 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
498000 f00000
GOLDBROOK BELANGER PROPERTY
ICI 10 ,
ea • f
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Figure 3b. Claims map showing individual cells with prospecting and sampling locations (green circles), near to the Sylvie, Getty and Allard showings.
16
GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
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Figure 3c. Claims map showing individual cells with prospecting and sampling locations (green circles), near to the Timtu showing.
17
GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
514000 51 518 522000 ----In— GOLDBROOK B O ii~i iid0°e~6tx ~ !* ~;`'~ i1' ~p¢i ~_i'/mûi :17"244 i~rov~zse ~Wig r~~ llôrrii~o° ',la q~ PROPERTY — . I i.. 1.1F A ~ ~ I ,' - ~ - ~ ` ~ t 11.1,- rimg,„Impta ~ d1IfŸQ 11111+ 1111111 111A4 _111114 11w776 IIIW7! 01X4/ ~ ~ lame Itwpl Illi,$ - all I1M11M7J4 IIISItd~, t Itl1174 ~ " ~ 1M111 e 1 111 . . . ` ~7~ ~~1 ~. . . ~ ~~ ,-.~ ~ •- • 11 ~ ~mitigoti 1111111 ~ 1NwN' ~ .. 'N111tl , J ~ I11gg ~ 111X130 116011 1 111 1111111 11111N; W. 110444110x1{ 1Uk0 11g111 ~ ti ~~ b .. ~%~ - ' ~ : (rMfi ti I ,; ~! ~►~,` f (t ~ 1y .p r"«] . 114143- { I~„yj!.~;~~~ ~ 1~1 ii. 1141104 .,11111M.' ,+, II . .. MAI? ~ IIIx J ~ j . I e did ~~ ®~~~~ ~ ~ é . `~ . . . -i~ ,_, .. . , _ -+, 1 .~ prolinlib._._ . . ~ ~ IIIX11g 11171W Î117U 11sXW 111411 . r1 .,.:. ~ ._ • 't wig 1117l11 M4- 1. 1pIM0' ~1~ ~ ~ _ ~~iirel~d~l~ II 1 ~ _ , J ~-~ ' 1ân c 1 . _ , l Ld1 e .~ ~•:::74, ,,i'm_. g, ~ / - 'i.' , _ ,. , J ,,'. fl':. J 1`,, ;I ~ ^ ~..~ l -_ , -' ~ p ~ / KC7XII p41111' ` pi 1IWX :al 110 .44s.1 ~ • 'tatil 117r41 X047111 `~, 11»1 11610 t140 ~ : m1~ 1p(t ~ 11111 11»1 - ~ , ~ I e .._. ~' - — l ~ - 310.., It{p1~1{ F ~~ ' ~ 1gsW. : ~i~Xin~ OtlM ~ d _ __ if■~ii~ ~ :.,gill ~wa_
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Figure 3d. Claims map showing individual cells with prospecting and sampling locations (green circles), near to the Echo South and Liberator showings.
18
GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
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Figure 3e. Claims map showing individual cells with prospecting and sampling locations (green circles), near to the Echo East showing.
19
GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
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20 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
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Figure 3g. Claims map showing individual cells with prospecting and sampling locations (green circles), on the Thunder claim block.
21 NUMÉRIQUE
PAGE(S) DE DIMENSION HORS STANDARD NUMÉRISÉE ET POSITIONNÉE À LA SUITE DES PRÉSENTES PAGES STANDARDS. GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
6. PROPERTY GEOLOGY
6.1. Bravo
Bravo West and Bravo East are separated by approximately 3 km in plan view. According to the regional geology mapped by the GSC, each area appears to occupy a limb of an anticlinal fold (Fig 4). The Bravo area is defined by several magnetic highs, which are coincident with rocks that have been mapped by the GSC as ultramafics (Fig 5). The geology that was encountered at Bravo West by GBK geologists is coarse grained pyroxenites in contact with variably mineralized basalts and sediments. Here, intermittent pyrrhotite and chalcopyrite mineralization was traced over 600 m in strike length. In the west, the magnetic anomaly maps clearly delineate one thick sill, although there appear to be local complications. The aeromagnetic results, surficial geology, and old NovaWest drill results all support a sub-vertical sill orientation. Another two EM conductor anomalies in the western half of Bravo were found not to be located in ultramafic rock. Rather, they appear coincident with a strange meta-quartzite.
According to notes made by geologists Russer and Clark, the eastern half of Bravo appears to be structurally more complex than the western half. At Bravo East a 5 to 10m wide 200 metre long in strike length, coarse-grained pyroxenite hosting approximately 2 to 3% pyrrhotite and chalcopyrite mineralization was encountered. NovaWest previously trenched and drilled this target (in drill hole NW05-19) and net textured mineralization of up to 10% pyrrhotite and chalcopyrite was found, as well as a wide zone of semi-massive sulphides at surface (Photo 1). The ultramafics and sediments were found to be in fault contact, which may explain the lack of mineralization at depth in follow-up drilling (NW04-20 and NW04-18).
23 NUMÉRIQUE
PAGE(S) DE DIMENSION HORS STANDARD NUMÉRISÉE ET POSITIONNÉE A LA SUITE DES PRÉSENTES PAGES STANDARDS. GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
Photo 1. A blasted trench at Bravo East, showing mineralized ultramafic rocks at surface.
6.2. Delta East
Mineralized and strongly magnetic basalts were encountered at Delta East (Fig. 4 and 6). Disseminated blebs and fracture controlled pyrrhotite mineralization (up to 7-8%) constituted the bulk of the mineralized rock. Siliceous sediments also hosted minor mineralization.
25 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
O 4 O O O O O O O O O O O O O O O O O O O $`s a s `a YS ~ R i~i R7i R R R R R ., ., N ., n R p Fi FS A R A u R R X X X X X AA I~ 6819400 19400 6815200 19200
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Figure 6. Delta East and Hellcat traverses (solid blue circles) and station locations (triangles) on VTEM overlay. Map author unknown.
26 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
6.3. Delta South
Two linear magnetic features at Delta South were prospected and identified as barren to very weakly mineralized, fine grained, rubbly magnetic peridotites (Fig. 4 and 6). Further to the west, directly south of the Delta block, targets for two NovaWest drill holes were examined. Numerous angular boulders with up to 3% disseminated and blebby chalcopyrite+pyrrhotite in fine to medium grained altered pyroxenite were located approximately 500 m to the west of drill hole NW04-26. The mineralized trend disappears under a large swamp (400 x 600m) with mineralized basalt boulders located on the opposite (western) edge of the swamp. NovaWest's other drill target, south of the Delta showing, consists of up to 4% of blebby and disseminated chalcopyrite+pyrrhotite hosted in altered, medium grained pyroxenites? Peter's showing, also in the Delta South area, consists of one large elongated altered gabbro boulder, which is heavily malachite stained, and contains up to 30% chalcopyrite (Photo 2). The outcrop surrounding it appears to be a feldspathic pyroxenite, although this is not in accord with the NovaWest map.
Photo 2. Peter's showing; a heavily malachite stained gabbroic boulder.
27 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 6.4. Echo
Echo is similar to Bravo in terms of its morphology and mineralization (Fig. 4 and Photo 3). The ultramafic rocks appear sandwiched between formational conductors (Fig. 7). Like Bravo, it is a large unit and has not been comprehensively prospected or mapped. Several distinct units make up the Echo complex.
Photo 3. Echo looking south, rubbly gossan in gabbro. Ultramafic outcrop in background.
28
GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
. o 0 0 0 0 0 0 0 0 0 0 0 0 o O ! 1i 8 k $ 6 ii 8 S 8 âd ~ A S $ 8 fd9o p P R ~ a u ~ x s x x >1 ~ %1 SQ P ~
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Figure 7. Traverses (solid blue circles) and station locations (triangles) near the Echo showing on VTEM overlay. Map author unknown.
29 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
6.5. Hellcat
The Hellcat area overlies a small EM anomaly (Fig. 4 and 6), which appears to be in the swamp next to the lake. North of the lake is a ridge of basalt, which contains sediments and/or flow textures indicating a possible north-dipping flow. There is generally a lack of exposure in the Hellcat area, although a very small outcrop of fine grained pyroxenite, with 1% finely disseminated and patchy chalcopyrite was found. There appears to be a close association between the EM conductor and the outcrop of mineralized ultramafic.
A second ultramafic body exists to the SW of Hellcat, which also has a coincident EM and magnetic anomaly. NovaWest drilled several holes here and discovered graphitic shale in the first hole. The south side of this ultramafic body is moderately mineralized with up to 2 to 3% pyrrhotite as patchy disseminated sulphides, and trace >1% disseminated chalcopyrite. This is another puzzling occurrence of a mineralized ultramafic at surface coinciding with an EM anomaly, which upon further exploration is found to be graphitic sediments.
6.6. Kozmo
The Kozmo portion of the Belanger trend was traversed and found to be composed of mainly ultramafic rock (Fig 4). While there is considerable ultramafic rock it appears to be largely unmineralized.
6.7. PAD, East Pillow, R2
This area is defined by an east-west 2 km trending body of ultramafic rocks (Fig. 4). The eastern portion of this ultramafic unit is moderately to well mineralized, which overlies a coincident EM anomaly. In 2006 AngloAmerican drilled this target and found the EM anomaly to be defining graphitic sediments.
30 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 6.8. Pillow Lake
The Pillow Lake ultramafic is a thin <20 m unit, which is variably mineralized (Fig. 4). The Magnetic anomaly map makes it appear to dip to the south, although this observation is not corroborated with any field evidence. The mafic volcanic units to the south of the ultramafic rocks are highly sulphur-rich, and ubiquitously mineralized with remobilised sulphides along fractures.
The Pillow Lake ultramafic, akin to the Sylvie ultramafic, appears to weather negatively with respect to its encasing units. The Pillow Lake ultramafic consists of an altered oikocrystic peridotite, which is moderately to highly magnetic. The entire exposure along Pillow Lake has been well prospected.
6.9. SuperFortress
SuperFortress is completely surrounded by water and appears to be the easternmost extent of the Echo ultramafic complex (Fig. 4). The majority of the exposed topographic high is a medium-grained massive gabbro. The contact between the gabbro and a heavily-mineralized pyroxenite occurs at the steep cliff on the north side of the body. Very little of the ultramafic rock is exposed, as it appears to have mostly been eroded away. A 150 m strike length limited gossan horizon is observed parallel to, and at the base of, the cliff. The pyroxenite is variably mineralized, with up to 20-25% sulphides as large magmatic patchy disseminates, locally net-textured, with generally a chalcopyrite:pyrite ratio of 3:2. There is clearly a relationship between the SuperFortress ultramafic and Echo ultramafic to the west, however, there appear to be more than one ultramafic body in this area.
31 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
812200
812000
-6811800
44- 681180 -0811600
081140 -ê811400
481120 -6811200
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0810000- -6810000
480500 -6805000
480500 805000
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G805000- -4805000
Figure 8. Traverses (solid blue circles) and station locations (triangles) near the Timtu, Jabba and Echo West showings on VTEM overlay. Map author unknown.
32 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
6.10. Timtu
A mineralized, coarse grained pyroxenite with up to 20% pyrrhotite and chalcopyrite, subcrops/outcrops in an area approx 80 m by 50 m in the Timtu area (Fig. 4 and 8). Sulphides are net textured, blebby and fracture controlled, and have a pyrite:chalcopyrite ratio of >3:1.
7. ASSAY RESULTS
Ninety-three grab samples were sent to ACCURASSAY Laboratories in Thunder Bay, Ontario for base metal ICPMS analysis and precious metal fire assay analysis. A news release was submitted on the 14th September 2007 summarizing results for 21 of these grab samples (Appendix 5). All the raw geochemical results and associated assay certificates have been included in Appendix 3 and 4, respectively. Table 2 summarizes the 95th percentiles of the 93 grab samples collected during the 2007 prospecting and mapping program. Table 3 lists the best assay results observed.
Three maps were constructed to show how the grades varied over the entire property. Figure 9 shows all the nickel results >0.15%, Figure 10 shows all the copper assay results >0.3%, and Figure 11 shows the combined Pt, Pd and Au assay results >1 g/t. Bravo East, Bravo West, Pad, Echo are 4 areas that yielded the best assay results, with one grab sample assaying 2.405% Ni from Bravo East (Fig. 9, Table 3). Copper results were encouraging with the best results from the Mystery, Timtu, Pillow Lake, Pad-1, Echo, Bravo West, Bravo East and Delta East (Fig. 10). The best copper result was from Delta East and averaged 15.528% Cu (Figure 10, Table 3). PGE+Au occurrences were encouraging at Timtu, Bravo East, Bravo West, and Delta East (Fig. 11, Table 3). The best combined Pt, Pd and Au assay result was 39.184 g/t from the Delta East (Fig. 11, Table 3).
33 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
Table 2. 95th percentiles based on 93 grab samples collected on the Raglan property in 2007. PtPdAu Ni % Cu % Co % Pt g/t Pd g/t Au g/t g/t 1.1269 1.1016 0.0798 7.5 5 2.5 4.5406
Table 3. Anomalous grab sample results with Ni results > 0.15% highlighted in red, Cu results > 0.3% highlighted in yellow, and PGE+Au results >1.00 g/t highlighted in green.
Sample PtPdAu Ni % Cu % Co % Pt (g/t) Pd (g/t) Au (g/t) (g/t) 280001 0.803 0.261 0.049 0.268 1.989 0.007 2.264 280002 0.023 0.363 0.066 <0.015 <0.01 <0.005 n/a 280005 0.361 0.299 0.061 0.113 0.249 0.025 0.387 280006 0.192 0.020 0.021 0.058 0.075 0.015 0.148 280007 0.112 0.743 0.012 0.421 1.361 0.026 1.808 280008 0.179 2.276 0.036 0.188 1.072 0.068 1.328 280009 0.959 0.129 0.105 2.938 1.832 0.077 4.847 280010 1.800 0.205 0.126 0.413 0.419 0.12 0.952 280011 0.223 0.024 0.356 1.276 0.030 1.662 280013 0.173 0.111 0.011 0.091 0.322 0.006 0.419 280024 0.169 0.001 0.012 0.045 0.083 0.047 0.175 280027 0.233 0.220 0.013 0.101 0.285 0.011 0.397 280028 0.253 0.211 0.017 0.1115 0.3500 0.0155 0.477 280501 0.976 0.331 0.037 0.027 0.01 <0.005 n/a 280502 0.945 0.320 0.035 0.564 2.772 0.062 3.398 280504 0.886 0.522 0.037 0.583 3.814 0.067 4.464 280505 0.414 1.479 0.050 0.112 0.163 0.01 0.285 280506 0.491 1.706 0.057 0.026 0.093 <0.005 n/a 280508 0.079 15.528 0.003 0.789 26.722 11.673 39.184 280510 0.207 0.307 0.006 0.324 0.574 0.053 0.951 280511 0.209 0.157 0.015 0.042 0.089 0.025 0.156 280513 0.532 0.515 0.016 0.165 0.775 0.071 280519 0.178 0.268 0.009 0.2195 0.482 0.0195 0.721 280520 0.472 0.262 0.024 0.204 0.394 0.007 0.605 280521 0.583 0.398 0.026 0.354 0.547 0.013 0.914 280522 0.505 0.432 0.022 0.229 0.403 0.026 0.658 280523 0.314 0.068 0.026 0.03 0.09 <0.005 nia 280534 0.211 0.008 0.015 0.057 0.067 0.017 0.141 285507 0.852 0.188 0.048 0.987 0.458 <0.005 n/a 285508 3.006 0.890 0.210 1.754 2.34 0.021 4.115 285509 1.311 0.647 0.097 0.6105 1.01 0.029 1.650 285510 2.405 1.360 0.123 1.092 3.027 0.344 4.463 285511 0.323 0.374 0.022 0.78 0.828 0.013 1.621 285512 1.508 0.806 0.066 0.177 0.748 0.019 0.944 285514 0.174 0.204 0.012 0.217 0.374 <0.005 nia 285515 0.282 0.540 0.023 0.241 1.103 0.015 1.359 285516 0.180 0.228 0.016 0.143 0.563 <0.005 n/a 285517 0.345 0.563 0.021 0.34 0.978 0.035 1.353 285518 0.180 0.223 0.055 <0.015 <0.01 0.018 n/a 285264 0.253 0.649 0.021 n/a n/a n/a n/a 285265 0.346 0.266 0.023 n/a n/a n/a n/a 285266 0.394 0.850 0.027 n/a n/a n/a n/a
34 NUMÉRIQUE
PAGE(S) DE DIMENSION HORS STANDARD NUMÉRISÉE ET POSITIONNÉE À LA SUITE DES PRÉSENTES PAGES STANDARDS. GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
8. RECOMMENDATIONS AND CONCLUSIONS
The 2007 field program strategy was to revisit the entire Belanger Horizon from Kozmo to Delta, and reassess NovaWest's interpretations and conclusions.
Along the Echo-SuperFortress-Bravo horizon, the ultramafics are generally well- mineralized, but there is little correlation with either the AeroTEM or the VTEM survey data. NovaWest performed a variety of geophysical surveys along this horizon; data which will need to be reanalyzed before proposing drill targets and future geophysical surveys in 2008. The map provided by NovaWest appears to contain numerous errors, and as such, detailed surface mapping of the ultramafic, including a description on mineralization style and texture, is crucial for the summer of 2008. For example, several separate units make up the Echo complex, however, the NovaWest map does not make these distinctions. The Echo complex will require remapping by GBK geologists. Future drill targets at Bravo and Echo will need to be proposed based on a reassessment of the AeroTEM and VTEM surveys conducted in this area.
The SuperFortress target was found to contain more than one ultramafic body, several of which contain sulphides, therefore, the entire complex would benefit from careful mapping in 2008. This area was not found to be anomalous in the AeroTEM survey data, which is puzzling. However a walking magnetic survey, which would take less than a day to complete, would be useful in delineating the ultramafic at SuperFortress and may highlight magnetic subtleties missed in the AeroTEM survey.
Delta South, in the vicinity of Peter's rock, requires further prospecting and may benefit from a walking magnetic survey. Similarly, a walking magnetic survey may be useful in the Hellcat area, since a large portion of the area is covered in swamp lands that may be overlying magnetic ultramafics. Based on a successful ground magnetic survey at Hellcat several Max-Min lines would be beneficial.
38 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
PAD was mapped and prospected at a time when snow still covered the ground, therefore the area will need to be revisited later stage in the summer of 2008. Before continuing with further exploration work at PAD, East Pillow and R2 it would be useful to assess the VTEM survey results so that more specific areas can be targeted. A walking magnetic survey and a Max-Min survey would be useful at Timtu, so that the horizontal extent and dip of the elongated pipe-like mineralized body can be determined. No further work is recommended at Kozmo at this stage.
During the summer of 2007 GBK geologists found that while the ultramafics of the Belanger trend are generally well-mineralized, the AeroTEM and VTEM are not helpful in targeting potential drill targets. A combination of ground geophysics and a different approach to exploration, such as expanding the search to include not well-connected lower-grade magmatic sulphide deposits, are recommended. Nova West's sampling procedures, as well as many of their drill hole locations and targets are not always in agreement with our own interpretations of the geology; there is thus significant room for re-interpretation of existing geological data and determination of a new suite of drill targets.
39 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
10. REFERENCES Avramtchev, L. 1982. Cartes des gites mineraux du Quebec, Region de la Fosse de l'Ungava. Ministere de l'Energie et des Ressources du Quebec, DPV- 897, Maps M327 to M336, scale 1:250 000.
Barnes, S.J. and Barnes, S.-J. 1990. A new interpretation of the Katiniq nickel deposit, Ungava, northern Quebec. Economic Geology 85, 1269-1272.
Barnes, S.J., Coats, C.J.A. and Naldrett, A.J. 1982. Petrogenesis of a Proterozoic nickel sulfide-komatiite association: The Katiniq sill, Ungava, Quebec. Economic Geology 77, 413-429.
Barnes, S.-J., Picard, C., Giovenazzo, D. and Tremblay, C. 1992. The composition of nickel-copper sulphide deposits and their host rocks from the Cape Smith Fold Belt, northern Quebec. Australian Journal of Earth Sciences 39, 335-347.
Bergeron, R. 1959. Povungnituk Range Area, New Quebec, Quebec Department of Mines. Preliminary Report 392 and Preliminary Map 1279.
Chisholm, K.M., Welch, M.J., Nemcsok, G. and Lemery, R.G. 1999. Mine geology of the Katinniq and Zone 2 Ni-Cu-(PGE) deposit. In: Lesher, C.M. and Green, A.H. (Editors), Komatiitic Peridotite-Hosted Fe-Ni-Cu-(PGE) Sulphide Deposits in the Raglan Area, Cape Smith Belt, New Quebec. Guidebook Series, v. 2, Mineral Exploration Research Centre, Paurentian University, Sudbury, p. 146-155.
Francis, D.M., Hynes, A.J. and Ludden, J.N. 1983. Crystal fractionation and partial melting in the petrogenesis of a Proterozoic high-MgO volcanic suite, Ungava, Quebec. Contributions to Mineralogy and Petrology 78, 27-36.
Giovenazzo, D. 1991. Geologie et caracteristiques geochimiques des mineralisations Ni-Cu-EPG de la region de Delta ceiture de Cape-Smith, Nouveau Quebec. In : Ph.D. thesis, University Quebec.
Giovenazzo, D., Picard, C. and Guha, J. 1989. Tectonic setting of Ni-Cu-PGE deposits in the central part of the Cape Smith Belt. Geoscience Canada 16, p. 134-136.
Hoffman, P.F. 1990. Subdivision of the Churchill Province and extent of the Trans- Hudson Orogen. In : J.F. Lewry and M.R. Stauffer (Editors), The Early Proterozoic Trans-Hudsonian Orogen of North America. Geological Association of Canada Special paper 37, 15-39.
41 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
Hynes, A., Francis, D.M., 1982. A transect of the Early Proterozoic Cape Smith foldbelt, New Quebec. Tectonophysics 88, 23-59.
Lamothe, D. 1986. Developpements recents dans la Fosse de l'Ungava. In Lamothe, D., Gagnon, R. and Clark, T. (Editors), Exploration en Ungava: donnees recentes sur la geologie et la gitologie, Minist. Engerg. Res. Quebec DV, pp. 1-6.
Lesher, C.M. and Charland, A. 1999. Geology of the Katinniq peridotite complex and associated Fe-Ni-Cu-(PGE) mineralization, Cape Smith Belt, New Quebec. In: Lesher, C.M. and Green, A.H. (Editors), Komatiitic Peridotite- Hosted Fe-Ni-Cu-(PGE) Sulphide Deposits in the Raglan Area, Cape Smith Belt, New Quebec. Guidebook Series, v. 2, Mineral Exploration Research Centre, Paurentian University, Sudbury, p. 88-104.
Picard, C., Lamothe, D., Piboule, M. and Olivier, R. 1990. Magmatic and geotectonic evolution of a Proterozoic oceanic basin system: the Cape Smith Thrust-Fold Belt (New-Quebec). Precambrian Research 47, 223- 249.
St-Onge, M.R. and Lucas, S.B. 1990. Evolution of the Cape Smith Belt: Early Proterozoic continental underthrusting , ophiolite obduction and thick- skinned folding. In: J.F. Lewry and M.R. Stauffer (Editors), The Early proterozoic Trans-Hudsonian Orogen of North America. Geological Association of Canada Special Paper 37, 313-351.
St-Onge, M.R. and Lucas, S.B., 1993. Geology of the eastern Cape Smith Belt: parts of the Kangiqsujuaq, Cratere du Nouveau-Quebec, and Lacs Nuvilik map areas, Quebec. Geological Survey of Canada Memoir 438, 110.
42 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 11. STATEMENT OF QUALIFICATIONS
I, Sheila Jonnes, hereby certify that:
1) I am a Geologist residing at 401-2033 Comox Street, Vancouver, BC, V6G 1S1
2) I am the Project Geologist for Goldbrook Ventures Inc. (Vancouver, BC), performing and supervising geological services on the Goldbrook Raglan Project for Goldbrook Ventures Inc. since February 2008.
3) I am a graduate of the University of Victoria, Victoria (British Columbia) in Geology (B.Sc. Honours 2007).
4) I have practiced my profession for more than 4 years
Signed :
Vancouver, BC May 2008
43 STATEMENT OF QUALIFICATION
I, Donald Brian Grant, P.Geo., do hereby certify that:
1. I am a practicing geologist employed by Goldbrook Ventures Inc, as President & COO, with an office located at 1550 — 200 Burrard St., Vancouver, British Columbia, V6C 3L6, and residing at 1331 Alberni Street, suite 2502, Vancouver. 2. I am a registered Professional Geologist of the Province of British Columbia, License number 20199; a registered Professional Geologist of the Province of Saskatchewan, Member number 04529; I have a Special Authorization number 99 to practice geology in the Province of Quebec from the Ordre des geologies du Quebec. 3. I am a graduate of Memorial University of Newfoundland and Labrador, St Johns, Newfoundland, in 1970 with a Bachelor of Science degree in geology. 4. Since graduation in 1970, I have been practicing my profession for 38 years. I have gained experience, managed and performed geological work in Canada, United States, Lesotho and Peru on a wide variety of mineral deposit types and geological environments. I have been employed as a Director in the British Columbia Geological Survey for 21 years managing government geoscience programs. 5. I have read the definition of "qualified person" as set out in National Instrument 43-101 ("N143-101") and certify that by reason of my education, affiliation with a professional association (as defined in NI43-101) and past relevant work experience, I fulfill the requirements to be a "qualified person" for the purposes of NI43-101. 6. I reviewed relevant data prepared by qualified persons and am responsible for the overall preparation and content of the technical report entitled "Goldbrook Raglan Project: 2007 Prospecting and Mapping Results and Interpretations", dated May 29, 2008. 7. To the best of my knowledge, information and belief, as of the date of the report, the Technical Report contains all scientific and technical information that is required to be disclosed to make the technical report not misleading.
Dated at Vancouver, 24th day of June, 2008
Q PR CV INC\.5' .,`
D.. B. GRANT D.B. Grant, PGeo eai r!s:1 ;COIUM£S;A~ 99â û c +, • _ 7 Special Authorization number§ '41 The Ordre des geolo•ies du Quebec REÇU AU S. Q L ' nu ~q 3t4` :3 2 8
DIRECTION DES TITRES GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
12. APPENDIX 1
2007 Field Report on the GBK Raglan Area: Investigations and Conclusions by M. Liard
44 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
NOTES ON 2007 FIELD INVESTIGATIONS CARRIED OUT BY M. LIARD ON THE GBK RAGLAN AREA PROPERTIES
The following notes will provide a subjective description and evaluation of the localities visited by myself during the 2007 field season. This documentation has been written to complement the information stored in the field database, which by its nature is largely restricted to the quantitative. In an attempt to commit these observations to paper while their memory remains fresh, the first copy (Sept. 23) is being written without the benefit of any assay results whatsoever. To preserve objectivity and to avoid hindsight, updates will be added to the complete first copy as assays become available. Allowing for weather conditions and a one week break, 26 days were available for fieldwork between 31 July and 20 September. Several of these were partial days owing to heavy demands on the Bell 206LR by the 15-man geophysics crew. The explicit mandate for the 2007 field program was the direct identification of drill targets. Owing to the amount of previous work on the most prospective areas, very little mapping was called for. A wide-ranging approach was taken in ranking the prospectivity of zones to be investigated. The parameters considered included any one of: • Current & historic surface sample assay results • The presence of sulphide mineralization in ultramafic rocks • Identified showing trends • The presence of favourable geology as identified on maps or interpreted from geophysics • Geophysical anomalies, especially combined mag & EM An absence of airborne EM response was not taken as definitively negative due to Goldbrook's experience with the Sylvie deposit, which singularly highlights the fickleness of EM methods. The new CZZ deposit east of Mesamax at > 100m depth, is also notable for a lack of Aerotem response. The traditional reliance on the infallibility of EM has certainly left many good prospects passed over. This situation could provide an exploration advantage for those willing to take the next steps, ie: to look more closely at areas with directly proven metal values.
A new sulphide occurrence was found at `Mystery' in the west-central Kozmo (Maverick) block, which has since been covered by a ground magnetic survey; there was no sign of previous human activity here. The most notable undrilled sulphide showings encountered were followed up from surface samples taken by Cominco in 1977-78 in the `Lightning' area at Delta East and at the far west end of the Delta complex (see "Delta West" section). UPDATE Oct 12:2 holes drilled into the Mystery showing encountered significant thicknesses of net-textured sulphides.
45 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
Belanger Property (Fig. 12)
Prior to program mobilization, several areas close to the Belanger camp were identified for prospecting in order to ensure that assays would be available for late season drill targeting. More distant parts of the Belanger property were not visited. Samples from the Belanger and Kozmo properties collected between July 31 and August 2 were ready for shipping on the August 3 backhaul, but were somehow held at camp until late August, and thus missed the lab change. UPDATE: As of October 7, assays are not yet available for drill targeting.
Allard Showing Area
The showing itself, identified by GBK in 2004, is a 70m strike length of frost-heaved sub-outcrop in a shallow till field approximately 75m south of the (unmineralized) associated linear ultramafic body; both ends disappear under lakes. It consists of well- mineralized pyroxenite which closely resembles rocks at other Getty & Echo trend showings, and carries encouraging metal values. Subcrop exposure along the shore of the lake immediately SE of the showing suggests that the Allard pxt is a narrow (30 to 50m thick) discrete dike or sill within sediments. This observed scenario is confirmed by the log of DDH BEL04-30, and can be seen on the subsequently completed ground mag. There is some evidence that the NE trending valley between the Getty and Allard areas is the expression of a property- scale sinistral fault. In this case it would follow that Allard is a faulted-off western extension of the Getty deposit (which is also spatially separated from the main sill). The 2004 DDH spotted under the showing was essentially barren, but taken in light of the Getty — Sylvie deposits, the Allard area remains interesting. It shares the characteristics of a detached position in the footwall of an elongate Getty -trend sill and a surface showing with good Ni — PGE tenor. The ground mag high is much larger than the area which contains the original surface showing and 2004 DDH; the mag high also strikes into an isolated Aerotem conductor which is under overburden on the W shore of Allard Lake, and remains untested by drilling. To the west of this conductor is a large outcrop of pxt and gabbro of the sill-related type.
Allard West
There are several points of interest along the Allard sill west of the showing: • Station 3016 in the database marks a limited (10 X 20m) area of generally fracture-controlled mineralization in pxt on the footwall margin of the main Allard sill. This area is on the E side of the pear-shaped lake. 3 samples were taken. • A weak, isolated, elongate Aerotem conductor under Pear Lake occurs on the f/w margin of the Allard sill coincident with an `embayment' or protrusion in the f/w of the mag response. • A small, isolated (perhaps) Aerotem conductor SW of Pear Lake lies near the f/w area of the main sill, it is covered by thick till. • The large isolated Aerotem conductor E of Pear Lake is unexplained by the somewhat cryptic outcrop in the area. The obvious W extension of the Allard
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u/m sill is nowhere to be seen. Sediments on the W side of the lake dip steeply N; above is a horizontal N-S striking contact with the overlying gabbro. Over the conductor is barren gabbro; there is some mineralization (sampled) 220m to the north.
Sylvie South
As of late July 2007, there were indications in the geophysics and drill sections that the lower (and richer) part of the Sylvie deposit may have a shallow N dip. This interpretation, along with the presence of sulphide mineralization noted in 2004 (from which samples had not been assayed) prompted interest in the area directly south of Sylvie. It appears that there are some narrow u/m dikes / sills approximately 350m south of the Sylvie area; some of these rocks carry weak (1 — 3%) mineralization. Outcrop exposure here is fair to poor. On the ground mag, the response of these dikes is very similar to the fragmented response of the Sylvie area u/m sill, as soon it becomes covered by overburden. If any of the samples taken in this area show interesting values, it deserves more investigation.
Getty North
Several samples were taken along the long (>250m), weakly mineralized gossan in melanogabbro and pxt north of Getty Lake. These lithologies show the characteristics of those related to ultramafic intrusives, though their relationship to the Getty sill is unknown. Assay results from the sampling should be examined before any work is allocated to this area.
Kozmo (Maverick) Property (Fia. 12)
Kozmo Main Sill
The persistent Getty ultramafic sill trend continues west of the Clark area onto the Kozmo claim block. For most of the eastern half, the sill is an outcropping, ridge-forming unit which continues the low-angle discordance of the Clark sill. This part of the sill has a very strong expression on the airborne mag. This section also appears to be barren, though the f/w contact is overburden covered along its whole length. The west half is very poorly exposed, trending along the footwall of a large basalt ridge, along which the u/m appears to be conformable. This part of the u/m unit has a weak, fragmented mag signature, excepting a short length at the far west end. The h/w contact is intermittently mineralized; much of this rock is a nebulous mixture of baked basalt and / or contaminated pxt. The lower (f/w) contact is not exposed on the property. The main Kozmo sill is notable for its lack of EM conductors. There is one coincident mag-EM anomaly at 491600E / 6805380N (not exposed) and another very small point conductor 200m to the east which lies over a small sulphide showing that was sampled. If Ni — PGE values occur in this area, the anomaly warrants drilling.
48 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
West of 490800E to 489460E, the picture is more complex; only the strong, ovoid mag high west of this area has extensive ultramafic exposure. With spotty mag and almost no u/m exposed, the persistence of the sill here is not known. The discordant feature WNW of this area may represent the continuing u/m trend, or it may continue to be confined south of the basalt through to the known outcrop, or both. Some of the mag responses and perhaps some conductors here are related to u/m rocks.
Mystery
Two prominent mag highs at the west end of the Kozmo block that were thought to lie on a western extension of the Timtu trend were found to be caused by u/m rocks. These discrete, high-weathering bodies occupy different stratigraphic levels in what may be isoclinally folded host rocks. The western unit (centered at 489600E / 6806000N) shows an assumed 30% exposure as more than half of the mag high is beneath or on the south side of the river. Although the basal contact with underlying basalt and metasediments is partially exposed, no mineralization at all was noted. Dips are steep north. The eastern unit, dubbed Mystery, has a complex mag response pattern which is similarly expressed on surface, with the most magnetic zones being pdt outcrop, whereas mag lows are mostly overburden covered. Some of the south (basal?) contact with underlying basalt and cherty metasediments is exposed; the sub-vertical contact is folded around a vertical axis. Two mineralized zones were noted: • Mineralized rubble is found along the cliff which marks the southern (probably basal) contact from 490680E to the best exposure at 490770E / 6806480. Coarse disseminated and blebby po + cpy up to 5% + 3% occur in typical grey granular pxt and gabbro as well as some altered fg rock with a ghost mg texture, which may be contaminated marginal gb - pxt or baked and altered basalt. The thin screen of metasediments on the contact is barren but the basalt below contains some disseminated po. Assays will be required to determine the prospectivity of this showing, due to the possibility of wallrock contamination. • Toward the unexposed north contact, an elongate gossan (from 490815E / 6806675N to -490980E) composed of mineralized pdt subcrop overlies a protrusion in a complex, formation-related Aerotem anomaly. The rock is fg to vfg, and locally contains phlogopite and magnetite, making it difficult to estimate the sulphide content with a hand lens, therefore assay results will be critical here as well. Update, Oct 12: Drilling on the north showing (2 DDH's on one section) has encountered significant widths of net-textured sulphide in peridotite. The undeformed mineralization in the 2nd hole shows good magmatic textures reminiscent of Raglan ore, with over 50m of 20% sulphide.
NVE Main Block: General (Fia. 13)
The greater Delta area (Delta) has some features otherwise uncommon in the eastern Cape Smith Belt.
49 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
• In contrast to the predominantly pillowed or massive basalt flows seen elsewhere, a large proportion of the mafic volcanics at Delta are tuffaceous or wholly v+olcaniclastic. These rocks are often calcareous, sulphide-bearing and very magnetic. Lithic clasts are common, including basalt breccia, bombs and rounded pebbles. Well-bedded tuffs have been seen with thin dolomite interbeds, and as interflows between pillowed strata. • Late-phase anorthositic gabbro and anorthosite dikes (sills?) up to 120m thick make up a significant proportion of the Delta West stratigraphy. These coarse grained, homogeneous rocks form resistant ridges which are generally conformable. In some cases they have been observed to cross-cut existing u/m rocks (e.g. @ station 3142) and carry pdt inclusions near contacts. This rock type is elsewhere seen only as rare isolated products of differentiation (usually thin late dikes) or locally in the most inhomogeneous gabbro units. • The Delta area can be seen to encompass some fold repetitions of u/m strata. Close folding on the east becomes isoclinal and semi-recumbent to the west as the whole structural package is shortened N-S. These structures are evident on surface, in geophysical plots and on satellite imagery. The River North intrusion is also an isoclinal structure. What is unique to the Delta area about this structural picture is likely not the intensity of deformation itself, but merely the ease of identifying it.
NVE Main Block: Far South Extension (Fig. 13)
Dragon's Eve
This small showing (5m X 15m) on the strike extent of the Expo trend occurs as disseminated sulphides on the basal contact of an isolated, thin (30 to 40m), otherwise barren dike or sill discordantly emplaced into mixed metasediments; its extent and orientation can be seen on the Aerotem CVG plot. On surface, the intrusion can be seen to pinch out to the west at 532422E / 6811893N. The mag suggests it thickens for a limited distance under the lake to the east. The larger mag trend, which continues west from the showing through the small pond, is not related to mafic / ultramafic rocks. The sill could pinch down dip as well: the fault suggested as the reason that DDH NW04-24 missed the sill may not exist. The values on surface and the intersection in NW04-23 (which includes 1 ore-grade sample of 0.5m - 50m down dip) are another indication that narrow features can host significant mineralization. In this case, the DDH spot which is universally agreed upon would only be accessible from lake ice.
East of D. Eye
The magnetically active area E of D's Eye is a sea of barren ultramafic rubble with outcrop along the north and south sills. There are indications of strong deformation on the rare outcrop in the central part, consistent with the FAP cleavage expected here on a major fold hinge. There is an impressive gossan near to the east on CZZ ground
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NVE Main: Delta South (Fig. 13)
Wackett Area and Wackett East Sill
The 7km long, curved ultramafic body running east of the Wackett area is weakly mineralized throughout. Though the western half is poorly exposed, the only real sulphide showing (which has not been drilled due to a lack of EM response) is on the ovoid, detached mag high at its far west end. The strong parallel mag feature to the north appears to be caused by basalt and sediments. Despite the ubiquitous sulphide, it would be difficult to justify a moving loop survey here. The formational airborne EM conductor along the south contact may be hiding a sulphide response, otherwise the most obvious EM targets have been exhausted by drilling.
Wellington and `1 a' Sill
The 1600m long, bow-shaped u/m body marked `1 a' by Picard lies almost entirely on XStrata claims, where it hosts the Delta 1 showing in gabbro on its north contact. The mag high south of its E end (Wellington) is caused by sulphidic tuffaceous - calcareous pillow breccia. The W end, which curves south onto GBK ground, carries a minor sulphide showing (@ 526260E / 6815850N, see station 3140 & associated samples), which is near a very weak Aerotem response and bulge in the mag, both overburden covered.
Halifax Area
The impressive surface showing and reasonable intersection at DDH NW04-27 show that this further extension of the Expo trend remains prospective. Here, the narrow ultramafic band hosting the showing lies on a north-facing ridge which grades into pxt then gabbro to the east, where there are 2 further sulphide occurrences (see stations 3161 & 3162). There are no airborne conductors here save the tiny point at the DDH, but if the samples taken are encouraging enough, it might be possible to justify a moving loop survey here. The mag high directly west of this area was not investigated due to an encroaching snowstorm. The bulk of the high ground to the south is gabbro; the southern mag high is sulphidic basalt. Halifax itself is south of the basalt contact in a flat swamp which suggests sediments.
52 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
NVE Main: Delta West / Cecilia Lake Area (Fiq. 13)
Delta West
The 2 distinctive Delta area synforms continue to the west through the XStrata Delta claims as semi-recumbent, Isoclinal structures, which form prominent ridges. Sulphides immediately encountered to the north of the Delta claims will be discussed below as Delta North. The southern synform comprises the `1 a' intrusion as its south limb and the u/m sill hosting the Delta 4 occurrence as its north limb. The local shallow E plunge at the nose of the structure can easily be seen from its north side as it surfaces -350m W of the claim boundary. There are 2 minor sulphide occurrences on the ridge associated with upper contact of the anorthositic gabbro (GbAn) sill (dike?), which is locally cross-cutting (see stations 3141 & 3142). It is not clear what DDH NW04-32 was targeting; also an extra, undocumented vertical casing remains at the drill site. The northern synform forms a large ridge distinguished by very complex but continuous stratigraphy, of which -3.5km of strike length lies on GBK ground. The centre of the ridge is occupied by a 150 to 180m exposure of coarse grained anorthositic and leuco-gabbro. The south slope is a continuous, N-dipping pdt - gabbro - pdt formation conformably overlying metasediments; here the pdt often features strong talc - carb alteration and weathers to gravel. North of the anorthositic gabbro is a complex, probably structurally repeated sequence of mafic - u/m horizons. From S to N it includes pdt (very friable talc-carb altered, 80 to 150m exposure, forms N-facing cliff) - metasediments- gabbro (20 to 40m) - pdt (20 to 30m, some very friable) - gabbro (10 to 20m) - pdt on N-facing cliff. The presence of metasediments is inferred from topography and frost boils; it does not outcrop and appears to be discontinuous. The 2 main Delta West sulphide occurrences (there is also a third subsidiary zone) on the north portion of the northern synform are among the most impressive surface showings in the region. Work includes pulse EM by NVE and 3 questionable DDH's, none of which properly tested the relevant mineralized horizon. The Aerotem response is flat here and through to Delta North and there is little excitement in the pulse EM as well, prompting the DDH's to be poorly located on any EM response in the general area. The D794 showing covers 275 of intermittently exposed, WNW striking pdt - GbAn contact west of station 3153 (525211 E / 6816400N). Mineralization includes NT Po up to 20% + lesser cpy in pdt and cpy veining up to 20% + lesser blebby po in GbAn. Cominco sample D-79-4 assayed 0.5% Ni; NVE samples were generally above 0.3%. DDH NW04-28 was collared in barren rocks 100m W of the W end of surface mineralization, likely on a pulse EM target, and returned 22m of 0.14% Ni, 0.25% Cu, 0.32g PGE. Careful prospecting in the area revealed a much larger generally mineralized zone of 440m X 100m (from stns 3153 to 3167 and north to stns 3165 & 3166), encompassing 2 pdt horizons and 2 gabbroic horizons. Up to 12% very fine- grained Po (average 5%) occurs intermittently in the northernmost pdt and south to the D794 contact. The D793 showing runs for 470m NNW along the presumed closure of the north Delta synform, 250m west of and perpendicular to the D794 showing. The structural complexity brought on by fold hinge-related thrust faulting and associated 2nd and 3`d order folding renders it impossible to follow the stratigraphy. The northernmost 250m of
53 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 this zone does appear to follow a generally bow-shaped gabbro - pxt contact with a postulated intermittent, very thin (2 to 5m) screen of sediments between. The upper gabbro hosts heavy disseminated and blebby Po + cpy up to 20%, whereas the lower pxt has fine disseminated to semi-massive Po > cpy and massive veins of either one. Cominco sample D-79-3, probably from the south pxt, assayed 1.8% Ni in 20% sulphur. SSE of the main zone, well-mineralized outcrops can be found in a perfectly straight line cutting across apparently unfolded stratigraphy until outcrop ends. DDH NW04-29 was drilled into very rusty metasediments above barren u/m, and that was what was intersected. The sediments are conductive. NW04-31 was drilled into the generally barren part of the southern stratigraphy, and still hit magmatic sulphides carrying highly anomalous values. The entire Delta West area (combined with Delta North) definitely merits more work, including a re-examination of NVE pulse EM data with in-fill coverage where necessary, small-scale mapping, and possibly a litho & soil geochem program.
Delta North
This area includes the north portion of the main ridge which carries east from the northern part of the Delta West area; it includes portions of the thick GbAN horizon and the same stratigraphy north of it. Much of the u/m here is gravelly-weathering though the northernmost cliff-forming u/m is whole, well-exposed, and very similar to the lithology which is mineralized north of showing D794. A new sulphide occurrence (no hammer marks) was found near the XStrata border at the east end of Delta North (see stns 3145, 3149, 3150). This zone, covering -125m to the claim line by 40m width, carries up to 10% Po as patchy NT and CG disseminated in pxt and of-pxt. The u/m rocks here are very red-weathering with oxide staining from relatively CG magnetite, making sulphide- mineralized rock difficult to distinguish. Found all over this area are variably rounded to angular boulders of strongly mineralized leuco-gabbro, beginning in the central GbAn horizon (stn 3144). Several samples of this were taken on Aug 23 and Sept 5; if they run, this till train should be chased down as it almost certainly originated on GBK ground.
NVE MAIN: Echo (Fig. 13)
The disappointing Ni and PGE tenors of the very impressive sulphide showings at Echo are in jarring contrast to the encouraging tenors at Bravo. This disparity comes despite the outward similarities in the mineralization and the spatial relations of the host rocks.
Echo 1
The largest (southern) u/m body in the Echo area shows complex igneous stratigraphy. As noted by NVE, more than one phase can be mineralized, in this case all toward the lower part of the sequence. Conductive sediments (evident on surface) were the target of the holes drilled northwards in 2003-4. Little can be added to existing descriptions of the the main Echo 1 showing:
54 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
• The most sulphide-rich samples found had a relatively high cpy: po ratio and remobilized textures. • A thin layer of gabbro which marks the first auto-intrusive contact above the showing is discontinuous. • Several narrow, mild zones of deformation parallel stratigraphy, this deformation has not been mapped. • Sediments south of the pond at the showing have highly variable dips.
Echo 2
The small main showing lies on a gb - gb intrusive contact; an intermittent, thin (<2m) screen of metasedimentary inclusions on the contact is generally absent toward the east, but thickens and coalesces westward. Though the main surface showing is limited to 60m X 4m, mineralization can be found along the whole 360m length of the Echo 2 hill. West of the showing the weak gossan follows the contact and ends in rusty metasediments. Eastward a narrow, mineralized deformation zone angles off into the south pdt and can be picked up again further north at the contact on the east cliff. Samples were taken from the whole length of the zone in hopes of a positive assay result.
Echo 3
The most disappointing of the Echo showings, it has a textbook coincident mag - EM signature, sulphide textures which run elsewhere, and one of the most impressive surface gossans in igneous rocks in the Raglan area. Drilling has shown a good sized deposit of sulphide with negligible Ni - PGE values. The most sulphide is contained in basal pxt and gabbro at an auto-intrusive contact. The primary showing covers -200m X 70m, but mineralization is present on the contact for over 1 km. This whole length was sampled, as at Echo2, in hopes of a change in the Ni - PGE tenors along strike
NVE Main: Delta East (Fia. 13)
Delta Sill and Peter's Rock
The `Delta' sill runs east from the D9 deposit of XStrata onto GBK ground. Here the pdt phase is only 10-12m thick, with a similar thickness of gabbro on the margins. Minor sulphide is observed in places in this sill for 700m until it the ultramafic phase slowly pinches out eastward into gabbro at 520590E / 6816450N, very close to Peter's Rock. The continuity of the Delta ultramafic through to this point is not difficult to establish between outcrops; existing maps do not show this feature however. The mag high marking the u/m sill appears to continue to the WSW, but this feature actually marks sulphide iron formation (which includes massive po) on the contact of mafic tuffs and flows.
55 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
The Peter's Rock showing itself consists of sugary qtz veins very rich in cpy within a brittle, coarse grained leucogabbro. Similar (less cpy-rich) veins are found up to 400m to the SE (stn 3102).
Liqhtninq
A long mafic — ultramafic sill which forms the north limit of the Delta complex proper was only partially prospected in 2007. An area from which 2 anomalous grab samples were taken by Cominco in 1978 was found to be an extensive, well mineralized sulphide showing in pdt & pxt. Over a width of 90m between stns 3105 & 3106, outcrop yields > 5% blebby & disseminated po + cpy, with >10% at the S contact to gabbro. This was not drilled by Cominco or NVE, likely due to an absolutely flat EM signature as seen on Aerotem plots. The evidence of unmarked, historic DDH setups suggests that this northern sill was the main focus of the PGE-oriented Phelps-Dodge drilling in 1980, which did encounter interesting sulphide mineralization in u/m rocks. If the assay results from 2007 grab samples show a high NI — PGE tenor, this showing in particular and the whole sill trend in general should be re-evaluated despite the lack of response by airborne EM methods. It is also recommended to procure the Phelps — Dodge exploration report (GM 49611, Lee, 1989) to be able to locate the DDH's in the area and possibly at River North as well.
Juliet East Area
The far E end of the Delta complex is a vast area of u/m rocks, much of which is due to fold repetition. Exposure here is 90%+ u/m rocks which form outcrop on high ridges separated by fields of locally derived pdt rubble. Some distal till fields likely mark metasedimentary rocks. In two half-days of prospecting here, coverage was marginal at best, and only one instance of minor sulphide was seen (stn 3129). It has been proven worthwhile to devote more than cursory effort to large ultramafic exposures such as this.
NVE Main: North Trends (Flo. 13)
River North
A series of ultramafic bodies appears to form a distinct 'sill trend' north of the Little Povungnituk River in the vicinity of the former NVE camp. Some minor showings found along this trend by Cominco and NVE were drilled in 2004 with poor results. The largest of the sills has one historic, unmarked DDH at its west end but no amount of research was able to locate any records or logs for it (The most likely program was Phelps-Dodge / Imperial Platinum 1989). The `River North' title was initially used to describe an AeroTem anomaly on the north side of this largest sill. Good exposure at its east end suggests that the Sill is a semi-recumbent, north-dipping, isoclinal synform cored by calcareous tuffs (including a sulphide-rich dolomite layer). Although elsewhere only the south limb is exposed, it is possible that the weak linear mag response on the north side
56 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 actually represents u/m rocks. In this case, the original till-covered EM conductor, which strikes onto an exposure of sporadically mineralized gabbro, has some merit. Later re-evaluation of existing EM data by R. Osmond of Cascadia Resources suggested that the basal contact of the south limb of the River North body was a primary target. Subsequent mapping at 1:5000 showed the ultramafic rocks to have a very thin (-1m) barren pxt margin conformably in contact with the underlying sediments, which though weakly sulphidic, are non-conductive at surface. One DDH returned no appreciable sulphide, though samples of remobilized and stringer mineralization were taken from the top of the hole.
Liberator
This area was investigated based on favourable Aerotem responses located by R. Osmond. The multiple complex of linear mag highs was found to represent all u/m rocks, and 2 sulphide showings were located -5.4 km apart despite very poor exposure due to strong talc-carbonate alteration of the pdt. At stn 3196 near the eastern fold closure, a zone of disseminated & stringer po + cpy in strongly altered pdt follows the basal contact for over 150m. The footwall basalt here is unmineralized. At stn 3203, mineralized pxt is found as angular boulders which appear to be sub-outcrop. A very thin pdt body outcrops slightly to the north; between is an horizon of strongly mineralized metasediments which unexpectedly features stringers of cpy (possible remobilized from u/m rocks?). One DDH (LIB07-001) was drilled into a blind conductor several hundred m west of stn 3196; no appreciable sulphide was found. There is exploration potential in this large volume of u/m rock, geological reconnaissance and thorough prospecting would be necessary as the existing geological maps are cursory.
57 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
13. APPENDIX 2
Raw Grab Sample Geological Data
58 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 Table 4. Raw station data including UTM coordinates, sample ID, and geological descriptions for 361 mapping and prospecting locations. Station Sample ID Sample Locality UTMUTM Mineralization Geologist Date Datum Description po% cp% py% Type Type Zone East North Type ePPI) (if Michal 24-Jun- gossan with large 'kill zone'; med to coarse pyroxenite with 10-15% cpy+po+py; gossanous material 280001 Assay Gossan n/a NAD83 18V 507996 6810677 n/a n/a n/a n/a Russer 07 subcropping over 40 m to E and to lakeshore Michal 25 Jun- 280002 Assay Subcrop n/a NAD83 18V 510048 6809629 subcrop and rubble in frost boils; mineralized basalt; 3% cpy+po+/-py n/a n/a n/a Russer 07 n/a Michal 25-Jun- 280003 Assay Subcrop n/a NAD83 18V 509215 6809517 subcrop; mod serpentinized of pxnite, 1% cpy+po+/-py; sulphides predominantly fracture controlled Russer 07 n/a n,/a n/a n/a Michal 26-Jun- 280004 AssaySubcropn/a NAD83 18V 516150 6813217 subcrop;p; gossan; unevenly (1-5%) mineralized (po+/ cpy+/ py), med grained?leucograbbro n/a n/a n/a Russer 07 n/a Michal 26-Jun- >10% S: rubbly gossan; gabbro with > 50% po + (cpy) +/- py; 20 m south of mafic outcrop; photo 280005 Assay Gossan n/a NAD83 18V 515960 6813206 Na n/a n/a n/a Russer 07 facing north Michal 26-Jun f.graind serpentinzed umafic with 1-2% v.fine grained disseminated cpy+?po; cluster in frost boils in 280006 Assay Float n/a NAD83 18V 515269 6813037 n/a n/a n/a n/a Russer 07 boulderfield with 80% orange-weathering fine grained ol pxnite. Michal 29-Jun- gossan in altered ?gabbro; 5-8% cpy+po (blebby & net texture with some fracture controlled); same 280007 Assay Gossan n/a NAD83 18V 511488 6811956 Blebby 4 3 n/a Russer 07 gossan as in 07-7046 but -20m E Michal 29-Jun- frost boil float (possibly subcrop); fine grained gabbro (?altered basalt?); nonmagnetic; 5-8% Fracture 280008 Assay Frostboil n/a NAD83 18V 511528 6812001 0.1 8 0.01 Russer 07 cpy+po+/-py; mineralization mostly fracture controlled controlled Michal 30-Jun- rubbly gossan; same mineralized trend as in trench (07-7052): <20% po+cpy in med to coarse 280009 Assay Gossan n/a NAD83 18V 521740 6814302 Net texture 14 4 n/a Russer 07 grained ol-pyroxenite? (?peridotite) Michal 30-Jun- >10% S: boulder (possibly from gossan in nearby flooded trench) with semi-massive po+(cpy) in med 280010 Assay Float n/a NAD83 18V 521639 6814270 Semi-massive 35 1 n/a Russer 07 to coarse grained ol-pyroxenite Michal 30-Jun- small (1x1.5m) blasted pit in rubbly. partially snow-covered gossan (40x10m); altered ?ultramafic; 10- 280011 Assay Gossan n/a NAD83 18V 520722 6813857 Blebby 10 5 n/a Russer 07 20% po+cpy: sulphides predominantly blebby but also net textured and fracture controlled Michal 01-Jul- 280012 AssayBoulder n/a NAD83 18V 519657 6813823 I boulder of siliceous seds with 3-5 /° po+cpy;p py; previously sampled (sample 3003) Disseminated 2 1 n/a Russer 07 9 Michal 01-Jul- 280013 AssaySubcropn/a NAD83 18V 519657 6813823 subcrop;coarsegrainedpyroxenite with 3-5% po+cpy;p pY; po»>cpy 4 Russer 07 Blebby 0.5 n/a Michal 01-Jul few, large (car size) angular boulders of coarse grained pyroxenite with <8% po+(cpy); behind and 280014 Assay Subcrop n/a NAD83 18V 519004 6813809 Net texture 7 0.5 n/a Russer 07 uphill from DDH NW04-14; (I think they f... up) Michal 05-Jul- 280024 Assay Subcrop n/a NAD83 18V 533016 6815031 8m wide; subcrop of rubbly; dark brown red, f grained ? Pyroxnite w/ <2% fracture controlled n/ a Russer 07 po n/a n/a n/a Michal 05-Jul- 280025 AssayGossan n/a NAD83 18V 532750 6815125 gossan rubble in frost boil; med grained gabbro with up to (dissem & blebby) 2% of po+py+cpy Na n/a n/a Russer 07 n/a Michal 07-Jul- 280026 Assay Subcrop n/a NAD83 18V 528740 6815231 subcrop; c grained ol pxnite with trace to minor po n/a n/a Russer 07 n/a n/a Michal 07-Jul- 280027 AssayFloat n/a NAD83 18V 528278 6815260 edge of I boulderfield; alteredpyroxenite (?gabbro) w/ 1-2% f.gr. Diss po+cpy n/a Russer 07 g 9 Na n/a n/a Michal 07-Jul- same bldr field as above; angular bldr of fine to med grained, magnetic, pyrxenite w/ 2-3% blebby and 280028 Assay Float n/a NAD83 18V 528282 6815259 Na n/a n/a n/a Russer 07 diss cpy+po (cpy:po = 2) Michal 09-Jul- 280029 AssayBoulder n/a NAD83 18V 516515 6812504 angular boulder of ggrungy, gy, med grained, magnetic ?pyroxenite; 3% diss po Na n/a n/a n/a Russer 07 g Michal 11 Aug 280030 Assay T.B.A. n/a NAD83 18V 524526 6815887 1. grained gabbro (or basalt) 10-15% blebby and dissem (w/ minor fract controlled) Russer 07 po + cpy n/a n/a n/a n/a Michal 12-Aug- 280031 Assay Frostheave n/a NAD83 18V 519450 6814490 couple of frost heaves w/ gossanous material;: blbby po (3-5%) in altered gabbro n/a n/a Russer 07 Na n/a Michal 19-Aug- cluster of gossanous gabbro bldrs; leucogabbro w/ 5-10% diss po+/-cpy; patchy gossanous frostboils 280033 Assay Boulder n/a NAD83 18V 517455 6814768 Na n/a n/a n/a Russer 07 continue 250m W Michal 23-Aug- 280034 Assay Boulder n/a NAD83 18V 507973 6809268 boulder; prey sampled; gabbro w/ 3-5% disseminated and blebby po+(cpy) n/a n/a n/a Russer 07 n/a Michal 23-Aug- 280035 Assay Subcrop n/a NAD83 18V 505843 6808666 blocky, med grained leucogabbro subcrop; 2-3% diss and blebby po+cpy n/a n/a n/a n/a Russer 07 Michal 23-Aug- med grained gabbro boulder in frost boil; proximal; 2-3% blebby and diss po; previously sampled 280036 Assay Boulder n/a NAD83 18V 505838 6808638 n/a n/a n/a n/a Russer 07 (BEL04-3056) 23 Jun- 280501 AssayFrostheave BEL07-5001 David Clark NAD83 18V 511366 6809728 AngularAn f/h. Mafic->um, m. g.,g., green, presumed +- in situ. F. patchy diss po +cp, 2%, 1 °/ Disseminated 2 1 Na
24-Jun- >10% S: Timtu. Sub-angular boulder ultramafic, v. rusty. Mod. Magnetic. F-diss -> almost net texture, 280502 Assay Boulder BEL07 5009 David Clark NAD83 18V 507989 6810733 Net texture 25 5 Na 07 v. fine. 20-30% sulphides. 90:10 po:cp. Boulder is +- 5 m from riverbank. Fairly altered, f.g. Jun- 280503 Assay Boulder BEL07-5009 David Clark NAD83 18V 507969 6810720 Sub-angular boulder, mg pxnite, less rusty than previous, patchy cp 5%, po tr->1% Patchy 1 5 Na 0 59
GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 Station ypelity Datum UTM UTM UTM Mineralization Sample ID Name (if Geologist Date Descrip Type le T Zone East North tion Type po% 4)% py% appl) 24-Jun- >10% S: Sub angular boulder, f.g. urn, mod magnetic. Leopard skin textured, with patchy -> net 280504 Assay Boulder BEL07-5009 David Clark NAD83 18V 507988 6810723 Net texture 30 8 n/a 07 textured framework surrounding 'blebs' of less mineralized um. 5:1 po:cp, -30-40% sulphides. 26-Jun- 280505 Assay Outcrop NOV07-5022 David Clark NAD83 18V 514672 6812629 >10% S: f.g. urn. Diss-> net textured po + cp. locally up to 50% po, 10-15% cp as blebs and stringers. Net texture 50 10 n/a 07 026 Jun- 280506 Assay Outcrop NOV07-5022 David Clark NAD83 18V 514672 6812629 >10% S: f.g. urn. Diss-> net textured po + cp. locally up to 50% po, 10-15% cp as belbs and stringers. Net texture 50 10 n/a 30-Jun- 280507 AssayOutcropNOV07-5042 David Clark 07 NAD83 18V 493825 6805987 Mafic volcanic, 3-4% po, 1-2% cp as patchy diss fr contr. occasional larger blebs. Patchy 3.5 1.5 n/a
02-Jul- From Peter's showing. Strange altered gabbro, heavily malachite stained.. v. soft, leeched to shit, +- 280508 Assay Boulder n/a David Clark NAD83 18V 530592 6816437 n/a 30 n/a 07 30% cp. From angular boulder. o/c here is rather a pyroxenite -> feldspathic pyroxenite. 03-Jul- 280509 Assay Outcrop NOV07-5055 David Clark NAD83 18V 532015 6818764 F.g. pyroxenite. V weakly magnetic. Disseminated nia 1 n/a -Jul- 280510 Assay Float n/a David Clark O~ NAD83 18V 526005 6815963 Float -> sic gabbro -> feld. Pyroxenite Patchy n/a 1.5 n/a
05-Jul- sic -> rubble, but < 10 m away from urn ridge; more or less in situ. Horzon of goassanous rubble. 280511 Assay Subcrop NOV07-5067 David Clark 07 NAD83 18V 526963 6816470 Disseminated 10 5 n/a Pyroxenite, 10%po as interstitial > almost locally net textured. cp 5% O05 ~lul 280512 Assay Subcrop NOV07-5067 David Clark NAD83 18V 526912 6816470 ->1% 7 Rubbly, as previous. C.g. pyroxenite -15% po, tr cp, as patchy aggregates. Patchy 15 0.5 n/a ~ul 280513 Assay Subcrop NOV07-5067 David Clark NAD83 18V 526951 6816584 ~~ Sic, f.g. peridotite. F diss patchy aggregates po. -10%, cp 2% Patchy 10 2 n/a 07 Jul Finely 280514 Assay Frostheave n/a David Clark NAD83 18V 535614 6818366 F/h rust looking f.g. mod. Magnetic peridotite, tr->1% po, f.diss, & small fracture smears. 0.5 n/a n/a 07 disseminated 07-Jul Finely 280515 Assay Float n/a David Clark NAD83 18V 535570 6818506 Float, to N of main sill. f.g. pyroxenite, rusty, -15% po as v. finely diss. 15 n/a n/a 07 disseminated 08-Jul- 0/c m.g.->c.g. pyroxenite massive. From N side of ridge. Not particularly rusty or gossanous, but Finely 280516 Assay Outcrop n/a David Clark 07 NAD83 18V 521858 6813983 2.5 n/a n!a mineralized throughoutg nonetheless. Mineralization is v. fine diss magmaticg sulphides,p 2-3%(?) disseminated 08 Jul Finely 280517 AssaySubcropn/a David Clark NAD83 18V 522063 6814010 Sic. Same horizon as previous. V. altered pervasivelyfractured. F. diss sulphides 1%. 1 nia n/a 07 p disseminated 09-Jul- Horizon of rusty mineralized mafic volcanics, N side of the unit. Rock is v. f.g., mineralized, w,' v.f. Fracture 280518 Assay Outcrop NOV07-5076 David Clark NAD83 18V 512608 6817932 5 n/a n/a 07 sulphides along fractures, -5% controlled
09-Jul o/c m.g. pyroxenite, patchy & blebs po + cp, 5:1, <1.5 cm, diss f cp. Total 6% po, 4% cp. Previously 280519 Assay Outcrop NOV07 5079 David Clark NAD83 18V 517660 6813175 Patchy 6 4 n/a 07 sampled by NW (?) sample #5102. 09-Jul- 280520 AssayOutcropNOV07-5079 David Clark NAD83 18V 517653 6813198 o c m.pyroxenite, diss f.g. po + cp. + patchy blebs cp < 1 cm. 15% total sulphides. n/a 07 / 9• Disseminated nia n/a 09-Jul- 280521 Assay Frostheave NOV07-5079 David Clark NAD83 18V 517635 6813219 f/h at base of hill. Mg. pyroxenite, 15-20% 60:40 po:cp as patchy blebs & diss. 12 07 Patchy 8 n/a 9 Jul 280522 Assay Frostheave NOV07-5079 David Clark p NAD83 18V 517632 6813228 >10% S: M.g. pyroxenite f/h. 20-25% sulphides, as large patches, locally net-textured, 60:40 po:cp Net texture 15 10 n/a
09-Jul- 280523 Assay Frostheave NOV07-5079 David Clark NAD83 18V 517655 6813283 fill -> float, c.g. pyroxenite. 10% po. 5% cp as patchy aggregates. Patchy 10 5 n/a
10-Jul- Assay of BRAVO-1-1; C.g. dark blue grey green pyroxenite, amphibolitized. F. diss cp tr. First o/c to 280524 Assay Outcrop n/a David Clark NAD83 18V 520165 6813847 n/a n/a nia n/a 07 the north of the lake. Assayed as 280524. Assay of BRAVO-1-2; C.g. dark blue grey oik peridotite. Characterisitc knobby tan weathered srfeace, 10-Jul- 280525 Assay Outcrop n/a David Clark 07 NAD83 18V 520171 6813865 whitish oikocrysts after pyroxene on fresh surface. Mod-> strongly magnetic. Barren. Assayed as n/a n/a n/a n/a 280525 10-Jul- Assay of BRAVO-1-3; c.g. dark grey-blue green peridotite. Losing poikilitic texture. although px oik. 280526 Assay Outcrop n/a David Clark 07 NAD83 18V 520164 6813883 n/a n/a n/a n/a Still present. Strongly magnetic. Rare tr diss sulphides. Assayed as 280526 10-Jul Assay of BRAVO-1-4; F.g. blue grey peridotite, poikilitic texture mostly gone, strongly magnetic. Tr f 280527 Assay Outcrop n/a David Clark NAD83 18V 520159 6813903 n/a nia n/a nia 07 diss sulphides. Assayed as 280527 Assay of BRAVO-1-5; F.g. blue grey peridotite, oikocrysts no longer present. Strongly magnetic, fairly 10-Jul- 280528 Assay Outcrop n/a David Clark 07 NAD83 18V 520153 6813935 pervasive fracturing. Eroded metre-scale columnar joints have trend & plunge 15@190. Assayed as n/a n/a n/a n/a 280528. 07 Jul- 280529 Assay Outcrop n/a David Clark NAD83 18V 520141 6813965 Assay of BRAVO-1-6; Ditto previous; joints have disappeared. n/a n/a n/a n/a
0~ Jul- 280530 Assay Outcrop n/a David Clark NAD83 18V 520110 6813990 Assay of BRAVO-1-7; Ditto previous. n/a n/a n/a n/a
10-Jul Assay of BRAVO-1-8; V. similar to previous, more ubiquitous magnetite veins, urn is fairly altered. 280531 Assay Outcrop n/a David Clark NAD83 18V 520136 6814015 n/a n/a n/a n/a 07 Assayed as 280531.
60
GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 Station Locality UTM UTM UTM Mineralization Sample ID Sample Name (if Geologist Date Datum Description po% Type Type Zone East North Type cp% py% apps) Jul 280532 Assay Outcrop n/a David Clark 07 NAD83 18V 520132 6814062 Assay of BRAVO-1-9; Ditto previous. n/a nia n/a n/a
10-Jul- 280533 Assay Outcrop n/a David Clark NAD83 18V tt 520134 6814106 Assay of BRAVO-1-10 & BRAVO-1-11; di o previous, 1-11 field dup of 1-10. nia nia n/a n/a 'Jul- 280534 Assay Outcrop n/a David Clark 07 NAD83 18V 520127 6814138 Assay of BRAVO-1-12; Ditto previous. nia n/a n/a n/a
10 Jul- Assay of BRAVO-1-13; NB: Lack of exposure bit this & previous sample. Was unable to take a 280535 Assay Outcrop n/a David Clark NAD83 18V 520092 6814230 n/a n/a n/a n/a 07 sample in that interval. 10-Jul 280536 Assay Outcrop n/a David Clark NAD83 18V 520126 6814266 Assay of BRAVO-1-14; Oik. Perido. Barren, strongly magnetic. n/a nia n/a n/a
10 Jul Assay of BRAVO-1-15; Pyroxenite. 280537 Assay Outcrop n/a David Clark NAD83 18V 520136 6814291 n/a n/a n/a n/a 07 Assayed as 280537. 16 Jul- f.g. v. magnetic peridotite subcrop. Finely 280551 Assay Subcrop n/a David Clark NAD83 18V 518656 6813513 7 3 n/a 07 7% po, 3% cp. as f. diss & small smears disseminated 16-Jul- 280552 AssaySubcropn/a David Clark NAD83 18V 518665 6813494 F. magneticperidotite subcrop.10% o, 3% cp,as interstitial sulphides (remob?) Interstitial 10 3 n/a 07 9• 9 P P 16-Jul F.g. serpentinized peridotite. V.f. diss po + cp, po + cp along serpentine smears, & int & odd patchy Finely 280553 Assay Subcrop n/a David Clark NAD83 18V 518640 6813666 7 3 n/a 07 blebs.. Remob? - where from? disseminated
16-Jul V rusty gossan rounded rock.. but v close to in situ. Leeched. Large patchy blebs po + cp, 5-10% 280554 Assay Subcrop n/a David Clark NAD83 18V 518642 6813662 Blebby 5 5 n/a 07 sulphides? Hard to tell - pretty leeched. ->10% S: Subcrop f.g. ultramafic. In slope/fault zone. 16-Jul 280555 Assay Subcrop n/a David Clark 07 NAD83 18V 518623 6813689 High-grading a particularly po-rich zone. Net texture 50 2 n/a Net-textured-> locally semi-massive po + minor cp. Po - 50% 16-Jul- >10% S: Subcrop f.g. urn. Net-textured to locally semi-massive sulphides. High-grading again, but this 280556 Assay Subcrop n/a David Clark NAD83 18V 518617 6813704 Semi-massive 60 10 n/a 07 rock is really impressive. 17-Jul- Float 0.3 m rounded boulder. Leeched f.g. massive sulphide. In grassy boulder train - not in situ, but 280557 Assay Float n/a David Clark NAD83 18V 518771 6813675 nia n/a n/a n/a 07 prob_ Pretty clsoe. Difficult to tell mineralogy as rock is fairly leeched. Non->v weakly magnetic. Jul 280558 Assay Float n/a David Clark 07 NAD83 18V 518771 6813675 Field duplicate of 280557. n/a n/a n/a n/a
17-Jul O/c f.g. sp pd. °Large o/c +l- gossanous /rusty horizon in urn. This sample fairly typical.F diss & Finely 280559 Assay Outcrop n/a David Clark NAD83 18V 518672 6813628 3 3 Na 07 interstitial po 3% cp% disseminated >10% S: 0/c oik perid, in fault zone. 17-Jul Finely 280560 Assay Outcrop n/a David Clark NAD83 18V 518598 6813622 Rusty portion of rock parallel to fracture patterns in rock, themselves parallel to the fault, dip steeply 30 n/a 07 disseminated N. Extremely magnetic. V.f. diss up to 30% po (??) 17-Jul float -> s/c. 1 mA3 angular rusty f.g.~.g > m . pd. Patchy interstitial sulphides, more magmatic-looking 280561 Assay Float n/a David Clark NAD83 18V 519104 6813848 Interstitial 3 2 nia 07 than the spitfire mineralization. 3-4% po, 2-3% cp. -Bravowest, south contact. Nice strike limited gossanous horizon in s/c. Previously sampled, but 20-Jul 280562 Assay Subcrop NOV07-5080 David Clark 07 NAD83 18V 519225 6813796 doesn't seem to be NW. Check their database. S/c -> float, f->m.g. urn, strongly magnetic, well- Smeared 5 5 nia mineralized w/ small patchy smears po+ cp, 5%po, 5%cp 20-Jul- 280563 Assay Subcrop NOV07-5080 David Clark NAD83 18V 519211 6813781 s/c oik pd. 5% po 5%cp as patchy interstitial sulphides. Moderately magnetic. Interstitial 5 5 nia 20-Jul- 280564 AssaySubcropNOV07-5080 David Clark NAD83 18V 519257 6813785 V. rustyrust pd s/c. smeared patchy po + cp, 5% po, 3%cp Smeared 5 3 Na 07 20 Jul Finely 280565 AssaySubcropNOV07-5080 David Clark NAD83 18V 519306 6813856 s/c oik+/-pd in situ. F. diss int-> locallyfinelynet-texturedpo, -15%, cp5% ? 15 5 n/a 07 () disseminated 20-Jul- 280566 AssayFloat NOV07-5080 David Clark 07 NAD83 18V 519299 6813848 angular9 float, f.9• pxnite -> olpxnite. Patchyinterstitial + patchyblebbysulphides. P Po 8% cp4% (?) Interstitial 8 4 n/a
20-Jul- Large s/c angular f.g. pd moderately -> strongly magnetic. Patchy interstitial po + large fracture 280567 Assay Subcrop NOV07-5080 David Clark NAD83 18V 519291 6813846 Interstitial 5 10 n/a 07 controlled surfaces of cp. This sample highgrades in cp. 5% po, -10% cp. >10% S: oic leeched & grungy semi-massive cp in f.g. grungy matrix. Corresponds exactly to gossan 20-Jul- 280568 Assay Outcrop n/a David Clark 07 NAD83 18V 519457 6813821 horizon in o/c. The area has been comprehensively sampled but unsure of the vintage of the Semi-massive n/a 50 n/a sampling. The flagging tape is old, faded to almost white and brit 20-Jul- 280569 AssayOutcropn/a David Clark NAD83 18V 519468 6813835 o/c f.g. pd. Int & diss patchy sulphides 5% po, 5% cp. Interstitial 5 5 n/a 07 20-Jul- 280570 AssaySubcropn/a David Clark NAD83 18V 519468 6813838 s/c f->m.g.g. pd, mod magnetic. 6% po 4% cp as int. patchy. Interstitial 6 4 n/a 07 20-Jul- 280571 AssayFloat n/a David Clark NAD83 18V 519477 6813829 float pxnite-> pd (bleached, hard to tell) mod -> str magnetic. Patchy diss & blebby 10-15% po, 5%cp. Patchy 12 5 n/a 07 o/c -> s/c m.g. pxnite -> ol. Pxnite mod->str. Magnetic well mineralized w/ patchy interstitial po 10- 20-Jul- 280572 Assay Outcrop n/a David Clark 07 NAD83 18V 519503 6813831 15% cp 5%. May have been sampled by us this year before this, but am not certain, so sampling n/a n/a n/a n/a again.
61 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 Station le Tocaypelity UTM UTM UTM Mineralization Sample ID Name (if Geologist Date Datum Description po% T; Zone East North Type oP% P" aPPl) 25-Jul- s/c -> float. Good gossan. Sampled previously by NW. px -> of px, c.g. well -mineralized. Stringers & 280573 Assay Subcrop n/a David Clark NAD83 18V 520736 6813854 Blebby 15 5 n/a 07 blebby po + cp. This sample 15% po 5% cp. >10% S: S/c -> float. This must be similar to what NW sampled in 2004 giving 1.9% Ni. Semi-massive 25-Jul- 280574 Assay Subcrop n/a David Clark NAD83 18V 520746 6813855 sulphides -> almost locally massive. V.f. po > 60%, cp > 10%. Proportions of each vary locally. NB: 60 07 Semi-massive 10 n/a Cut upon arrival at camp: not quite as massive as previo 280575 Assay Subcrop n/a David Clark 25-Jul- NAD83 18V 520746 6813855 >10% S: Field duplicate of same rock as 280574 Semi-massive 60 10 nia
280576 AssaySubcropn/a David Clark 25-Jul- NAD83 18V 520988 6813770 s/c -> float. C.g. pxnite. Well amphibolitized. Diss patchy po + cp. 10-12% po, 3-4% cp. 07 Disseminated 10 3 n/a 25-Jul- 280577 AssayOutcropn/a David Clark 07 NAD83 18V 521037 6813766 float. ofpx. 15-20% sulphides,p 50:50 po:cp,p p, patchy blebs. Patchy 10 10 nia float -> sic, valley bottom, from ridge immediatley N. semi-massive sedimentary sulphides. F.g. 19 Aug 280578 Assay Float n/a David Clark 07 NAD83 18V 542520 6830090 sulphides with angular fragments balck shale interspersed. Probably what NW was trying to hit with n/a n/a n/a nia NWT04-02 and 03. Pretty obviously not magmatic sulphide. 285151 Assay Subcrop BEL07-3001 Matt Liard 31-Jul- NAD83 18V 501167 6806704 FG pxt alt'd, appears to NOT be gbSp Disseminated 2 07 0.2 nia
285152 Assay Subcrop BEL07-3004 Matt Liard 31-Jul- NAD83 18V 501003 6806655 GbSp sampled for tenor (prob 0) 1 07 Disseminated n/a n/a
285153 Assay Boulder BEL07-3005 Matt Liard 31-Jul- NAD83 18V 501256 6806815 GbSp wkly min'd like all GbSp locally 1 07 Disseminated n/a n/a Fracture 285154 Assay Outcrop BEL07-3016 Matt Liard 01-Aug- NAD83 18V 498559 6806596 Dk grey fg pxt. some FF & diss min 3 0.5 n'a 07 controlled - 285155 Assay Outcrop BEL07-3021 Matt Liard Aug NAD83 18V 498118 6806857 Mildly defm'd Gb, some min 0~ Disseminated 3 1 n/a
285156 Assay Subcrop BEL07-3026 Matt Liard Aug- NAD83 18V 490772 6806482 0~ M-CG grey pxt, coarse blebs 5-15mm Blebby 2 2 n/a - 285157 Assay Subcrop BEL07-3026 Matt Liard Aug NAD83 18V 490772 0~ 6806482 FG pxt grey green defm'd, diss & sm blebs Disseminated 4 0.5 nia
285158 Assay Subcrop BEL07-3026 Matt Liard 07 Aug- NAD83 18V 490772 6806482 Green gbMs, eqgrnlr, CG diss & mnr blebs Disseminated 4 1 n/a
Finely 285159 Assay Subcrop BEL07-3026 Matt Liard 02-Aug- NAD83 18V 490772 6806482 bst (or maybe fg defm'd gbml), likely f/w contact bst w/ fg diss min 5 0.1 nia 07 disseminated - Finely 285160 Assay Subcrop BEL07-3026 Matt Liard 20-Aug NAD83 18V 490772 6806482 as 285159 5 n/a n/a disseminated
285161 Assay Outcrop BEL07-3030 Matt Liard 02-Aug- NAD83 18V 490895 6806724 pdt near centre of sill, alt'd to fg appearance. some mica, diss & blebs min, w/in Ig EM hi Disseminated 2 0.5 n/a Aug 285162 Assay Float BEL07-3033 Matt Liard NAD83 18V 0~ 490998 6806555 Alt'd, sil'd gb, poss ctct alt'n w/ contm'n min. Disseminated 5 0.2 n/a
285163 Assay Float BEL07-3033 Matt Liard Aug NAD83 18V 490998 0~ 6806555 as 285162 Disseminated 5 n/a n/a Finely 285164 Assay Outcrop n/a Matt Liard 02-Aug NAD83 18V 490887 6806690 fg mica bearing pdt w/ fg min 3 1 n/a 07 disseminated Finely 285165 Assay Outcrop n/a Matt Liard 02-Aug- NAD83 18V 490890 6806698 as 285164 3 1 nia 07 disseminated
285166 Assay Outcrop n/a Matt Liard ~~ Aug NAD83 18V 491001 6806688 Far east end of min'd pdt in kozmo N or "mystery N" area. Disseminated 4 1 n/a
285167 Assay Outcrop KOZ07-3034 Matt Liard -Aug- NAD83 18V 489161 6804706 Green (grey) pxt or MIGb, wk min 0 Disseminated 1 n/a n/a
285168 Assay Outcrop KOZ07-3043 Matt Liard ~~ Aug NAD83 18V 491795 6805447 alt'd pxt or amphblt'd bst on sill contact Bedded 1 1 nia
285169 Assay Outcrop KOZ07-3043 Matt Liard 07-Aug- NAD83 18V 491795 6805447 as 285168 Bedded 1 1 nia
285170 Assay Subcrop KOZ07-3044 Matt Liard 07Au g NAD83 18V 491986 6805468 green, grnlr fg gb or baked bst Disseminated 4 n/a n/a
285171 Assay Subcrop KOZ07-3045 Matt Liard -Aug- NAD83 18V 492476 6805680 n/a 0 Disseminated 2 n/a n/a
285172 Assay Subcrop NOV07-3048 Matt Liard 06-Aug- NAD83 18V 515742 6813205 MG Gb, mild fabric, strong frac's due to narrow mnr shear zn. 07 Blebby 3 2 n/a
285173 Assay Snow NOV07-3053 Matt Liard -Aug- NAD83 18V 515263 6813141 Weathered, mildly defm'd, alt'd gb now grey trem + Zo + qtz + min 0 Net texture 7 2 n/a Fracture 285174 Assay Subcrop NOV07-3054 Matt Liard 06-Aug- NAD83 18V 515206 6813148 dk grey frac'd pxt on cntct w/ min diss & ff. 2 2 n/a 07 controlled
62
GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 Station le ity UTM UTM UTM Mineralization po% cp% py% Sample ID Name (if Geologist Date Datum Description Type Tyype l Zone East North Type aPPi) 06-Aug- 285175 Assay Subcrop NOV07-3058 Matt Liard NAD83 18V 514612 6812921 >10% S: weathered MS from zn 351. Character indeterminate. 07 Massive 90 8 n/a 06-Aug- 285176 Assay Snow NOV07-3056 Matt Liard NAD83 18V 514784 6813017 frac'd & alt'd ol pxt. 1 07 Disseminated 2 n/a 06-Aug- 285177 Assay Outcrop NOV07-3060 Matt Liard NAD83 18V 514703 6812953 Wkly defm'd, wkly mind pdt in zone cont'd from 3056. 07 Disseminated 2 n/a nia
285178 Assay Outcrop NOV07-3071 Matt Liard -Aug- NAD83 18V 514637 6812509 cpy -rich of pxt w/ blebs & stringers 1 0 Blebby 8 n/a
285179 Assay Outcrop NOV07-3071 Matt Liard p7-Aug- NAD83 18V 514637 6812509 0l pxt w/ fg aggragates of Po & patchy net cpy Disseminated 5 5 nia
285180 Assay Outcrop n/a Matt Liard p7-Aug- NAD83 18V 514550 6812512 0l pxt w' weathered net txtr in strong patches intrstial to px grains Net texture 12 5 n/a
08-Aug- Finely 285181 Assay Outcrop NOV07-3081 Matt Liard NAD83 18V 511094 6811913 slight gossan in mild shr in gb 3 n/a n/a 07 disseminated 10-Aug Relatively undefm'd pdt in region of strong frac. Weak min in region of barren. FG appearance from Finely 285182 Assay Outcrop NOV07 3093 Matt Liard NAD83 18V 534269 6810644 0.5 0.2 Na 07 def & alt'n disseminated
285183 Assay Subcrop NOV07-3099 Matt Liard 11 Aug- NAD83 18V 530047 6816771 angular boulder at N margin of delta sill, minor min, in ol pxt 07 Disseminated 1 n/a n/a
285184 Assay Outcrop NOV07-3100 Matt Liard 11-Aug- NAD83 18V 530400 6816620 Alt'd gb lc weak min 1 07 Disseminated n/a n/a
285185 Assay Outcrop NOV07-3101 Matt Liard 11 Aug- NAD83 18V 530527 6816510 CG of pxt in narrow dike or poss delta sill pinch out. 07 Disseminated 2 n/a n/a
285186 Assay Boulder n/a Rob Gray Aug- NAD83 18V 530943 6816120 110 >10% S: boulder of MS. Likely related to MS exhalite @ stn 3103, but UP-ice ...? Massive 90 n/a n/a 11-Aug Boulders of sub-rounded to sub-angular 'Peter's Rock' type pegmatitic GbLc w! strong cpy + Po min, 285187 Assay Boulder NOV07 3102 Matt Liard NAD83 18V 531001 6816057 Blebby 3 5 n/a 07 coarse diss & blebs. 12-Aug- Lg u/m o/c, weak min throughout in pdt & ol pxt, esp in centre area. Strongly serp'alt'd pdt ol pxt w.% 285188 Assay Outcrop NOV07-3104 Matt Liard NAD83 18V 533601 6817255 Disseminated 2 n/a nia 07 strong serp vning , relatively soft chlor'd overall. Variable minor - 2% po. 12-Aug Finely 285189 Assay Boulder n/a Matt Liard NAD83 18V 533630 6817250 Rnded rusty boulder, greyish-white MG poss alt'd gb, w/ vfg po + cpy, weathered 10 2 Na 07 disseminated
285190 Assay Outcrop NOV07-3106 Matt Liard 12-Aug- NAD83 18V 533783 6816339 MG pdt. relatively fresh for delta east area, typical 4% diss sulphds. From o/c. 07 Disseminated 3 1 Na
285191 Assay Outcrop NOV07-3105 Matt Liard 12-Aug- NAD83 18V 533756 6816291 CG grey pxt w/ coarse diss min. Disseminated 6 2 Na 07
285192 Assay Outcrop NOV07-3105 Matt Liard ~~ Aug NAD83 18V 533759 6816290 alt'd grey cg pxt, fg nt aggregates of po intrst'l to cg pxt pheno's, also diss & cloudy po. Net texture 10 2 Na - 285193 Assay Outcrop NOV07-3108 Matt Liard 12-Aug NAD83 18V 534534 6816269 MG green ol pxt w! small patches of net txtr cpy & minor blebs. 2 07 Net texture 0.5 Na
285194 Assay Outcrop NOV07-3061 Matt Liard -Aug- NAD83 18V 514497 6812928 weak blebby min cpy>po on zn 351 horizon 0 Blebby 3 3 Na 06-Aug- 285195 Assay Outcrop NOV07-3062 Matt Liard NAD83 18V 514445 6812916 MG pxt (+/-ol) w/ cpy Disseminated n/a 2 nia 07
285196 Assay Snow NOV07-3097 Matt Liard ~~ Aug NAD83 18V 533179 6810734 From blasted trench in very rusty shear zone poss Gb strong alt'n, little visble min. Disseminated 3 n/a n/a >10% S: Massive Sulphides on bst - bst contact, probably exhalitive sed MS. Lower bst pillow & / or 11 Aug 285197 Assay Outcrop NOV07-3103 Matt Liard 07 NAD83 18V 531059 6816133 flow bx, upper bst massive tabular flows. MS pod 20m X 3m on extensive (>1 km) strike) min'd Massive 90 n/a n/a contact, strong gossan. strong linear mag feature. 285198 Assay Outcrop NOV07-3110 Matt Liard p5-Aug- NAD83 18V 534789 6809924 MG pdt, minor mg diss min poss from fracs Disseminated 2 n/a n/a
106-Aug- 285199 Assay Boulder n/a Matt Liard NAD83 18V 535038 6810147 angular boulder / prox 'I till. 01-pxt, 2-3% diss po in bldr field N of barren u/m ridge Disseminated 2 n/a n/a 106-Aug- 285200 Assay Boulder NOV07-3113 Matt Liard NAD83 18V 532115 6813480 Strained v. alt'd Gb w/ sil'n & chlort, diss po» cpy. Angular bldr poss prox till or s/c Disseminated 3 n/a n/a
106-Aug- 285201 Assay Float NOV07-3114 Matt Liard NAD83 18V 532014 6813451 Many gossanous gb bldrs in area, no o/c, just N of Ig u/m ridge Disseminated 3 3 n/a
106-Aug- 285202 Assay Subcrop NOV07-3116 Matt Liard NAD83 18V 532094 6813139 0l pxt, as 3115 & all of surrounding area. Wk min often as small patches of incip NT Disseminated 2 n/a Na
285203 Assay Subcrop NOV07-3117 Matt Liard Aug- NAD83 18V 532902 6812894 of-pxt mg modrt min in large wkly mind area on Ig o/c ridge. Exact loc 2903 / 2893 Disseminated 3 2 n/a 0716 106 Aug 285204 Assay Subcrop NOV07-3117 Matt Liard NAD83 18V 532902 6812894 as 285203. Exact loc = 29002894 Disseminated 2 1 n/a
63 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 Station Sample Locality UTM UTM UTM Mineralization Name (if Geologist Date Datum Description po% cp% py% Sample ID Zone East North Type aPPi) -Aug NOV07-3119 Matt Liard NAD83 18V 533089 6812794 PDT w/ small patches of incip NT min Disseminated 3 1 n/a 285205 Assay Subcrop 0 16-Aug- 285206 Assay Subcrop NOV07-3120 Matt Liard NAD83 18V 533360 6812835 as 285205 Disseminated 2 2 n/a 07 18-Aug- 285207 Assay Float NOV07-3122 Matt Liard NAD83 18V 534816 6812533 fg grnlr pxt + of from area of subanglr bldrs @ bottom of u/m scam. Disseminated 3 n/a n/a 07
NOV07-3123 Matt Liard 18-Aug NAD83 18V 534891 6812561 Strongly jntd pdt w/ oxide-type gossan bloom along jnts & fracs, minor to 2% po fg diss. Disseminated 2 n/a n/a 285208 Assay Outcrop 0 18-Aug- Assay Boulder NOV07-3124 Matt Liard NAD83 18V 535600 6813975 mg of pxt w/ vfg diss min Disseminated 1 1 n/a 285209 07 19-Aug- 285210 Assay Subcrop NOV07-3128 Matt Liard NAD83 18V 537121 6813466 of pxt from anglr bldr Disseminated 3 n/a nia 07
285211 Assay Outcrop NOV07-3129 Matt Liard 07 Aug NAD83 18V 536858 6813828 Pxt horizon w/ minor min. 20m wide in sea of barren pdt (attitude unknown). Exact loc 6855 / 3829 Disseminated 2 n/a nia
Matt Liard 19-Aug NAD83 18V 536812 6813850 alt'd gb w! blebs & frac cntrld po + cp. Appears similar to locally common rx, from subanglr bldr. Blebby 3 2 n/a 285212 Assay Boulder n/a 0 22-Aug- well mind, CG-VCG mlGb as bldrs over area 10m X 15m surrounded by of-pxt o/c. Would be Float NOV07-3132 Matt Liard NAD83 18V 531366 6814019 Bedded 3 3 n/a 285213 Assay 07 coincidence to have so much similar till over large area but rx somewhat incongruous.
285214 Assay Boulder NOV07-3132 Matt Liard Aug- NAD83 18V 531366 6814019 as 285213, actual loc 10m E Bedded 3 3 n/a 2207 well min'd, CG-VCG mlGb as bldrs over area 10m X 15m surrounded by ol-pxto/c. Would be 22-Aug- 285215 Assay Boulder NOV07-3132 Matt Liard 07 NAD83 18V 531366 6814019 coincidence to have so much similar till over large area but rx somewhat incongruous. Some Disseminated 2 1 n/a associated fg sub-oph mind gb as well makes up this sample well min'd, CG-VCG mlGb as bldrs over area 10m X 15m surrounded by of-pxt /c. Would be 22-Aug- 285216 Assay Boulder NOV07-3132 Matt Liard 07 NAD83 18V 531366 6814019 coincidence to have so much similar till over large area but rx somewhat incongruous. This sample Bedded 5 3 n/a similar but also remob min in fracs
285217 Assay Outcrop NOV07-3134 Matt Liard p~ Aug NAD83 18V 530945 6814384 mg of-pxt, looks like grey pxt but v magt'c Disseminated 2 n/a 22-Aug- 285218 Assay Outcrop NOV07-3135 Matt Liard NAD83 18V 529755 6815158 n/a Disseminated 2 2 n/a 07
NOV07-3136 Matt Liard -Aug NAD83 18V 528337 6815291 as 281218 Disseminated 2 1 n/a 285219 Assay Outcrop 0 Finely 285220 Assay Outcrop NOV07-3139 Matt Liard A ug NAD83 18V 527275 6815818 blue-green pdt, fg appearance from att'n. minor min 1 nia 0 disseminated Finely 2 1 n/a 285221 Assay Subcrop NOV07-3140 Matt Liard ~~ Aug NAD83 18V 526261 6815853 similar to 285220, from same intrusion disseminated
285222 Assay Subcrop NOV07-3140 Matt Liard -Aug NAD83 18V 526261 6815853 as 285222 Disseminated 2 1 n/a 0 - 285223 Assay Float NOV07-3144 Matt Liard p3-Au g NAD83 18V 525863 6816607 coarse diss po in alt'd mg gb from anglr bldr; rx common locally Disseminated 5 n/a Na
285224 Assay Boulder n/a Matt Liard -Aug- NAD83 18V 526972 6817422 roundish bldr chlor'd pdt w/ patchy net txtr po. Origin unknown... Net texture 5 1 n/a 0
285225 Assay Outcrop NOV07-3145 Matt Liard -Aug NAD83 18V 527488 6817622 cg to vcg pxt w/ coarse blebby po. Bedded 8 2 n/a 0
285226 Assay Outcrop n/a Matt Liard 07 Aug- NAD83 18V 527470 6817623 as 285225 but all mg. Bedded 8 1 n/a
285227 Assay Subcrop NOV07-3148 Matt Liard -Sep- NAD83 18V 534732 6818362 MG green / white GbMs, sharp gb'ic txtr (relatively fresh), cg diss & blebby po+cp. Disseminated 3 2 n/a 04
Subcrop NOV07-3148 Matt Liard -Sep NAD83 18V 534732 6818632 CG - MG grey Gb Peg w/ blades of grey trem 5 - 25 mm Disseminated 5 1 n/a 285228 Assay 04
Subcrop NOV07-3148 Matt Liard -Sep- NAD83 18V 534732 6818362 grey GbMs peg'ic w/ blades of dk grey hbl (trem?) 8 - 25 mm Bedded 2 4 n/a 285229 Assay 04
285230 Assay Outcrop NOV07-3151 Matt Liard -Sep NAD83 18V 527494 6817089 dk grey-green pdt, some min as fg diss & blebs Disseminated 3 n/a nia 05 Fracture Outcrop NOV07-3153 Matt Liard Sep NAD83 18V 525211 6816399 fg diss po & serp vein repl'nt in pdt @ GbLc contact. n/a n/a n/a 285231 Assay 0~ controlled Fracture 05-Sep- 1 5 n/a 285232 AssayOutcropNOV07-3153 Matt Liard 07 NAD83 18V 525211 6816399 CG GbLc w/ cpy veining controlled Fracture NOV07-3153 Matt Liard -Sep- NAD83 18V 525211 6816399 as 285232 but no cpy vns, has blebs of fg grnlr po 4 1 n/a 285233 Assay Outcrop 05 controlled
285234 Assay Outcrop NOV07-3154 Matt Liard 07-Sep NAD83 18V 525119 6816328 CG grey & wht GbLc w/ CG diss po-i-cp on contact gossan Disseminated 5 3 n/a 64 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 Namen Sample Locality UTM UTM UTM Mineralization Sample ID Type (if Geologist Date Datum Description po% cp% py% Type Zone East North Type P 09-Sep typical grey mg grnlr pxt w/ diss min. Almost certainly from stn 3160 area, sample taken before this Boulder NOV07-3158 Matt Liard NAD83 18V 527306 6814569 Disseminated 3 2 n/a 285235 Assay 07 was seen. 09-Sep- mg GbMs w/ 5%+ bt in mg books, likely from contamination, as commonly seen throughout this NOV07-3161 tt Liard NAD83 18V 527336 6814569 Disseminated 8 3 n/a 285236 Assay Outcrop Ma 07 horizon. Here is srongly mind w/ mg diss & large clots of Po 10%+.
NOV07-3162 Matt Liard 09-Sep NAD83 18V 527424 6814569 fg fresh gbms, evnly diss min - 5% Disseminated 3 2 nia 285237 Assay Outcrop 0 09-Sep- Typical min'd pxt, mg grey-green, from angular bldr on cntct at top of bst scarp, probably proximal Matt Liard NAD83 18V 527380 6814581 Blebby 4 4 n a 285238 Assay Boulder n/a 07 float. 07-Sep stn 3145 / 3150 area. Blue-green ol pxt / pdt. Weak MG granular txtr remains. some phlog. FG diss Finely Outcrop n/a Matt Liard NAD83 18V 527385 6817576 4 2 nia 285239 Assay 07 min. disseminated Blue-green ol pxt / pdt. FG appearance due to alt'n but mg txtr can be seen in small patches of NT 05-Sep- 18V 527372 6817620 Patchy 4 2 nia 285240 Assay Outcrop NOV07-3150 Matt Liard 07 NAD83 min. Also fg diss po.
NOV07-3150 Matt Liard -Sep- NAD83 18V 527372 6817620 MG ol pxt w/ cg diss min Disseminated 3 1 n/a 285241 Assay Outcrop 0
NOV07-3165 Matt Liard 12 Sep- NAD83 18V 525110 6816423 min'd fg pdt, mostly fg diss po Disseminated 7 1 n/a 285244 Assay Subcrop 07
Outcrop n/a Matt Liard 12 Sep- NAD83 18V 525088 6816376 fg pdt, min'd Net texture 6 1 n/a 285245 Assay 07 Finely 5 0.5 n/a 285246 Assay Outcrop NOV07-3166 Matt Liard p2- Sep- NAD83 18V 534727 6816325 as stn 3165 disseminated 12-Sep >10% S: MG of pxt, strong alt'n when strong min, apparently stringer / vein. Sample is semi-massive NOV07-3170 Matt Liard NAD83 18V 524718 6815950 Semi-massive 20 10 n/a 285247 Assay Outcrop 07 po w/ stringer cpy in v alt'd black pxt.
Outcrop NOV07-3172 Matt Liard Sep- NAD83 18V 524795 6815836 mg grnlr pxt, strongly min'd w/ heavy diss po>cp Net texture 8 3 n/a 285248 Assay 0712
NOV07-3174 Matt Liard Sep- NAD83 18V 524817 6815731 FG GbMI, 10% FG diss po Disseminated 10 1 n/a 285249 Assay Outcrop 0712
285250 Assay Outcrop NOV07-3174 Matt Liard p2-Sep- NAD83 18V 524817 6815731 fg GbMs, wi cg diss min Disseminated 5 3 n/a
Dominic 31-Jul- 285251 Assay Subcrop 1001 NAD83 18V 501115 6806665 CG gabbro, possibly SpGB with 2-3% Po. diss+ vein remob. suboutcrop n/a 3 n/a n/a Lussier 07 Dominic 31-Jul- 285252 Assay Subcrop 1002 NAD83 18V 501201 6806754 FG gabbro, gray colour, 2% Po 1% Cpy, diss, suboutcrop n/a 2 1 n/a Lussier 07 Dominic 31-Jul- 285253 Assay Subcrop 1003 NAD83 18V 499532 6806995 CG gabbro, possibly SpGB with 2-3% Po. diss+ vein remob, suboutcrop n/a 2 n/a n/a Lussier 07 Dominic 31-Jul- 285254 Assay Subcrop 1004 NAD83 18V 499433 6807001 CG gabbro, possibly SpGB with 1-2% Po, diss+ vein remob, suboutcrop n/a 2 n/a n/a Lussier 07 Dominic 31-Jul- Assay Subcrop 1005 NAD83 18V 499340 6806959 FG Pxt, gray colour, 1-2% diss sulphides, suboutcrop n/a 2 n/a n/a 285255 Lussier 07 Dominic 31-Jul- Subcrop 1006 NAD83 18V 499270 6806929 MG Pxt, green colour, 2% Po 1% Cpy FG diss, suboutcrop n/a 2 1 n/a 285256 Assay Lussier 07 Dominic 31-Jul- 285257 Assay Subcrop 1007 NAD83 18V 499290 6806730 MG Pxt, green colour, 4% Po 1% Cpy diss, suboutcrop n/a 4 1 n/a Lussier 07 Dominic 01-Aug- Assay Subcrop 1008 NAD83 18V 498923 6806401 MG Pxt, 1-2% Po, suboutcrop n/a 2 n/a n/a 285258 Lussier 07 Dominic 01-Aug- 285259 Assay Subcrop 1009 NAD83 18V 498564 6806606 MG to CG Pxt, 2% Po, suboutcrop n/a 2 n/a n/a Lussier 07 Dominic 01-Aug- 285260 Assay Subcrop 1010 NAD83 18V 498128 6806583 FG gabbro, 2% Po diss + FF, probably suboutcrop n/a 2 n/a n/a Lussier 07 Dominic 01-Aug- 285261 Assay Boulder 1011 NAD83 18V 498124 6806664 MG gabbro, visible Plag lath, 3-4% Po, from rounded boulder, none of the same around n/a 4 n/a n/a Lussier 07 Dominic 02-Aug- 285262 Assay Boulder 1012 NAD83 18V 490697 6806335 MG Pxt, euhedral Plag <10%, DK green lour, 4% Po 1% Cpy diss, from boulder n/a 4 1 n/a Lussier 07 Dominic 02-Aug- CG Pxt, possibly 01 Pxt. green colour, 5% Po 1% Cpy, from boulders at base of a slope, many other Boulder 1013 NAD83 18V 490780 6806479 n/a 5 1 n/a 285263 Assay Lussier 07 around Dominic 02-Aug- 285264 Assay Subcrop 1014 NAD83 18V 490816 6806679 FG Prt, rusty alt, presence of sulphide?? Is it mica?? Suboutcrop n/a n/a n/a n/a Lussier 07 Dominic 02-Aug- Assay Subcrop 1015 NAD83 18V 490815 6806679 same as 1014, presence of a 2mm sulphide vein n/a n/a n/a n/a 285265 Lussier 07 Dominic 02-Aug- 285266 Assay Subcrop 1016 NAD83 18V 490992 6806686 MG gabbro, light gray colour, 6% Po 2% Cpy interstitial, suboutcrop?? n/a 6 2 n/a Lussier 07 Dominic 22-Aug- 285270 Assay Gossan 1017 NAD83 18V 531360 6814008 MG 01 gabbro, light green colour, 12% Po 4% Cpy NT, part of a gossan n/a 12 4 n/a Lussier 07 65 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 Station Sample Locality UTM UTM UTM Mineralization Sample ID Name (if Geologist Date Datum Description po% cp% py% Type Type Zone East North Type aPPi) Dominic 22-Aug- 285271 Assay Boulder 1018 NAD83 18V 531244 6814290 MG-CG Pxt, green cour, Px up to 5mm, 7% Po 3% Cpy blebby,from boulders, 3-4 more around n/a 7 3 n/a Lussier 07 Dominic 22-Aug- 285272 Assay Subcrop 1019 NAD83 18V 528320 6815286 FG 01 Pxt, DK green colour, 3-4% Po diss, suboutcrop n/a 4 n/a n/a Lussier 07 Dominic 22-Aug- 285273 Assay Gossan 1020 NAD83 18V 527942 6815335 FG-MG gabbro, 60% Px-40% Plag, light gray colour, 8-10% Po diss + blebs, part of a small gossan n/a 10 n/a n/a Lussier 07 Dominic 23-Aug- MG leucogabbro, 60-70% Plag, light gray colour. 10% Po 1% Cpy interstitial, multiple same boulders 285274 Assay Gossan 1021 NAD83 18V 525835 6816598 n/a 10 1 n/a Lussier 07 in a area of 10m/10m Dominic 23-Aug- MG gabbro, 50% Plag 50% Px, gray colour, 8% Po diss + blebs, from angular boulders, 2-3 other 285275 Assay Boulder 1022 NAD83 18V 525830 6816914 n/a 8 n/a n/a Lussier 07 laying around, found same boulders at 526043 6817137 Dominic 23-Aug- 285276 Assay Outcrop 1023 NAD83 18V 525914 6816988 FG Pr, black colour, 2-3% Po 1% Cpy diss, outcrop n/a 3 1 n/a Lussier 07 Dominic 23-Aug- 285277 Assay Boulder 1024 NAD83 18V 526653 6817361 MG gabbro with long aciular amphibole 2-3% Po, from subangular boulders. 2-3 laying other around n/a 3 n/a n/a Lussier 07 Dominic 05-Sep- 285278 Assay Outcrop 1025 NAD83 18V 527475 6817618 MG Pr, dark black lour, 3-4% Po 1%py diss, outcrop n/a 4 1 n/a Lussier 07 Dominic 05-Sep- 285279 Assay Subcrop 1026 NAD83 18V 525030 6816325 FG Pr, Dk black colour, 8-10% Po diss to NT, probably suboutop n/a 10 n/a Na Lussier 07 Dominic 05-Sep- 285280 Assay Gossan 1027 NAD83 18V 524979 6816245 MG 01 Pxt, Dk green colour, 5% Po, from big 15m/50m gossan n/a 5 n/a n/a Lussier 07 Dominic 05-Sep- 285281 Assay Gossan 1028 NAD83 18V 525013 6816309 MG OIPxt, DK green colour, 6-7% Po from same gossan as 1027 n/a 7 n/a n/a Lussier 07 Dominic 05-Sep- 285282 Assay Boulder 1029 NAD83 18V 524835 6816190 CG gabbro, gray colour. 1-2% Po 6-8% Cpy, from rounded boulder n/a 2 7 n/a Lussier 07 Dominic 06-Sep- 285283 Assay Outcrop 1030 NAD83 18V 533653 6818060 FG Pr, dk black colour, from outcrop, 1-2% disseminated Po n/a 2 n/a n/a Lussier 07 Dominic 06-Sep- 285284 Assay Subcrop 1031 NAD83 18V 527167 6814916 MG Pxt, green colour, part of a 5 by 5m gossan, 5-8% disseminated PO 1% Cpy n/a 7 1 n/a Lussier 07 Dominic 06-Sep- 285285 Assay Subcrop 1032 NAD83 18V 527167 6814916 MG Pxt, green colour, part of a 5 by 5m gossan, 2-3% disseminated PO 4-5% Cpy n/a 3 4 n/a Lussier 07 Dominic 06-Sep- MG gabbro 50\50 Plag Px, dk gray colour, from small angular boulder possibly suboutcrop 2% 285286 Assay Subcrop 1033 NAD83 18V 527359 6814889 n/a 2 2 Na Lussier 07 disseminated Po 2% Cpy Dominic 06-Sep- 285287 Assay Boulder 1034 NAD83 18V 525008 6816451 MG pr, 50\50 OI\Px. black colour, from boulder at base of a slope, 6-8% blebby Po nia 7 n/a n/a Lussier 07 Dominic 08-Sep- 285290 Assay Boulder 1035 NAD83 18V 524824 6816281 FG gabbro, gray colour, from boulder at base of a slope, 5% blebby Po and 3% Cpy nia 5 3 n/a Lussier 07 Dominic 08-Sep- 285291 Assay Boulder 1036 NAD83 18V 524628 6816154 MG-CG gabbro, gray colour. from boulder, 7%diss Po 1%Cpy n/a 7 1 n/a Lussier 07 Dominic 08-Sep- 285292 Assay Outcrop 1037 NAD83 18V 524752 6816256 VFG gabbro? Basalt?, from outcrop, outcrop is and about 10m wide 3% diss Po n/a 3 n/a n/a Lussier 07 Dominic 08-Sep- 285293 Assay Subcrop 1038 NAD83 18V 524639 6816143 massive sulphide from 15cm large vein in gabbro, suboutcrop, 85% Po 10% Po n/a 85 10 n/a Lussier 07 Dominic 11-Sep- 285294 Assay Subcrop 1039 NAD83 18V 524639 6816143 MG gabbro. gray coulour, from suboutcrop, big blebs 20-30mm of Cpy and Po 5% Po 1% Cpy n/a 5 1 n/a Lussier 07 Dominic 11-Sep- 285295 Assay Subcrop 1040 NAD83 18V 531173 6817804 CG Pxt, dk green colour, from suboutcrop, 5-8% blebby Po n/a 7 n/a n/a Lussier 07 Dominic 12-Sep- 285296 Assay Subcrop 1041 NAD83 18V 530593 6817783 FG Pr, dk black colour, from suboutcrop, 3-5% disseminated Po 1% Cpy n/a 4 1 n/a Lussier 07 Dominic 12-Sep- 285297 Assay Subcrop 1042 NAD83 18V 519002 6816792 FG Pr, dk black colour, from boulder suboutcrop??, 1-2% disseminated Po n/a 2 n/a n/a Lussier 07 Dominic 15-Sep- 285298 Assay Float 1043 NAD83 18V 518735 6817006 MG Pxt, gray coulour, from rounded boulder, 4% Cpy diss 2-3% Po n/a 3 4 n/a Lussier 07 Dominic 15-Sep- 285299 Assay Subcrop 1044 NAD83 18V 518057 6817251 MG Pxt, dk green colour, from suboutcrop. 3-4% diss Po 2% Cpy n/a 4 2 n/a Lussier 07 Dominic 17-Sep- 285300 Assay Boulder 1045 NAD83 18V 517558 6827620 CG gabbro, dk gray colour, from big angular boulder (only one around), 2-3% diss Po n/a 3 n/a n/a Lussier 07
285301 Assay Outcrop NOV07-3184 Matt Liard 07-Sep- NAD83 18V 531166 6817813 mg, w/ well-preserved relict px oikos 3-8mm, 50% of rx, min'd w/ cg diss Disseminated 5 0.5 n/a
NOV07-3185 Matt Liard 13-Sep- NAD83 18V 530724 6817772 mg of pxt, w/ well-preserved relict px oikos 3-8mm, 50% of rx, min'd w/ diss po Disseminated 6 0.5 n/a 285302 Assay Outcrop 07
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GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 Station pelity UTM UTM UTM Mineralization Name (if Geologist Date Datum Description po% cp% py% Sample ID Type le Ty Zone East North Type apps) 285303 Assay Outcrop NOV07-3187 Matt Liard p4-Sep- NAD83 18V 519004 6816788 well mind, very serp'd black pdt, mostly blebs Blebby 5 2 Na
- 285304 Assay Outcrop NOV07-3187 Matt Liard p4-Sep NAD83 18V 519004 6816788 well mind, very serp'd black pdt. Blebs & stringers up to 2 cm. Blebby 15 2 n/a
NOV07-3176 Matt Liard Sep NAD83 18V 524467 6816064 grey mg gb w/ slightly vague texture due to alt'n Patchy 4 0.5 Na 285305 Assay Outcrop 0~ 020-Sep- 285306 Assay Outcrop NOV07-3196 Matt Liard NAD83 18V 518896 6816907 typical liberator area mind alt'd pdt Blebby 3 2 Na
200-Sep- NOV07-3196 Matt Liard NAD83 18V 518896 6816907 lalt'd pdt w/ diss min cp>po Disseminated 2 2 n/a 285307 Assay Outcrop 7 200-Sep NOV07-3196 Matt Liard NAD83 18V 518896 6816907 Ig blebs of cpy in black alt'd pdt Blebby 1 3 Na 285308 Assay Outcrop 7 20-Sep- Fracture 285309 AssayFloat NOV07-3203 Matt Liard NAD83 18V 513606 6817965 MG -fg pxt, partially black hbl, cloudymin o & c spreads out from fracs generallycp>po 2 2 n/a 07 controlled 20-Sep- Finely 285310 Assay Float NOV07-3203 Matt Liard NAD83 18V 513606 6817965 pxt, fg diss min likely from fracs or qtz vnlets though none in this sample 3 3 Na 07 disseminated Finely ô0-Aug- 2 2 Na 285311 Assay Float NOV07-3097 Matt Liard NAD83 18V 533197 6810734 fg gb It grey w/ diss min. **Not sure sample is from exactly this location** disseminated Fracture 4 285312 Assay Outcrop NOV07-3169 Matt Liard 12-Sep- NAD83 18V 524640 6816139 mg gbms, diss & stringers cpy>po 5 Na 07 controlled
Assay Outcrop n/a Matt Liard 12-Sep NAD83 18V 524640 6816139 mg gbms, heavy diss sulphide Disseminated 5 4 Na 285313 07 Sebastien 26-Jun- NAD83 gossan with large "kill zone"; med to coarse pyroxenite with 10-15% cpy+po(+py?); gossanous Fracture n/a 18V 515980 6813209 4 6 Na 285501 Assay Outcrop Allard 07 material subcropping over 40m to E and to lakeshore controlled Sebastien 26-Jun- 285502 Assay Subcrop n/a NAD83 18V 515529 6813205 gabbro Disseminated 5 1 Na Allard 07 Sebastien 26-Jun- 285503 Assay Outcrop n/a NAD83 18V 515863 6813219 gabbro Disseminated 5 3 n/a Allard 07 Sebastien 26-Jun- 285504 Assay Subcrop n/a NAD83 18V 515513 6812966 gabbro or peroxynite Disseminated 3 1 Na Allard 07 Sebastien 29-Jun- 285505 Assay Subcrop n/a NAD83 18V 511433 6811956 px Disseminated 3 1 Na Allard 07 Sebastien 29-Jun- 285506 Assay Boulder n/a NAD83 18V 511557 6812115 pd angular boulder Disseminated 1 1 n/a Allard 07 Sebastien 30 Jun- 285507 Assay Outcrop n/a NAD83 18V 521821 6814332 px Blebby 10 5 n/a Allard 07 Sebastien 30-Jun- 285508 Assay Outcrop n/a NAD83 18V 521820 6814330 px Semi-massive 10 10 n/a Allard 07 Sebastien 30-Jun- 285509 Assay Outcrop n/a NAD83 18V 521820 6814330 px Semi-massive 10 10 n/a Allard 07 Sebastien 30-Jun- 285510 Assay Outcrop n/a NAD83 18V 521640 6814283 > 10% S: px Massive 20 20 Na Allard 07 Sebastian 30-Jun- 285511 Assay Outcrop n/a NAD83 18V 521645 6814265 px Disseminated 10 5 n/a Allard 07 Sebastien 30 Jun- 285512 Assay Outcrop n/a NAD83 18V 520750 6813859 px Disseminated 2 5 Na Allard 07 Sebastien 01-Jul- 285513 Assay Outcrop n/a NAD83 18V 520025 6813856 px Disseminated 10 1 Na Allard 07 Sebastien 01-Jul- 285514 Assay Outcrop n/a NAD83 18V 519752 6813909 px Disseminated 5 1 n/a Allard 07 Sebastien 01-Jul- 285515 Assay Subcrop n/a NAD83 18V 519621 6813822 px Disseminated 3 3 Na Allard 07 Sebastien 01-Jul- 285516 Assay Outcrop n/a NAD83 18V 519598 6813834 px Disseminated 2 3 n/a Allard 07 Sebastien 01-Jul- 285517 Assay Outcrop n/a NAD83 18V 519505 6813832 px Disseminated 3 5 n/a Allard 07 Sebastien 02-Jul- Assay Outcrop n/a NAD83 18V 530790 6816239 >10% S: px? Ba? Disseminated 20 5 n/a 285518 Allard 07 Sebastien 02-Jul- 285519 Assay Outcrop n/a NAD83 18V 530795 6816254 >10% S: px? Ba? Disseminated 20 5 n/a Allard 07 Sebastien 02-Jul- 285520 Assay Outcrop Na NAD83 18V 530801 6816235 px? Ba? Disseminated 5 5 Na Allard 07 67 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 Station yypecelity UTM UTM UTM Mineralization Sample ID Name (if Geologist Date Datum Description po% cp% py% Type a T Zone East North Type aPPi) Sebastien 03-Jul- 285521 Assay Outcrop n/a NAD83 18V 531165 6817806 px Disseminated 10 10 n/a Allard 07 Sebastien 03-Jul- 285522 Assay Outcrop n/a NAD83 18V 531248 6817811 px 1 Allard 07 Disseminated 3 n/a Sebastien 03-Jul- 285523 Assay Subcrop n/a NAD83 18V 532814 6817853 px 1 Allard 07 Disseminated 3 nia Sebastien 07-Jul- 285524 Assay Outcrop n/a NAD83 18V 528347 6815313 px Allard 07 Disseminated 1 1 n/a Sebastien 07-Jul- 285525 Assay Subcrop n/a NAD83 18V 528284 6815268 px Disseminated 3 2 n/a Allard 07 Sebastien 07-Jul- 285526 Assay Subcrop n/a NAD83 18V 527874 6815349 px Allard 07 Disseminated 5 3 n/a Sebastien 07-Jul- 285527 Assay Subcrop n/a NAD83 18V 527336 6814927 gb? Ba? Allard 07 Disseminated 3 3 n/a Sebastien 07-Ju1- 285528 Assay Subcrop n/a NAD83 18V 527170 6814901 px?gb? Disseminated 5 5 Allard 07 n/a Sebastien 07-Jul- 285529 Assay Subcrop n/a NAD83 18V 527162 6814906 px? Gb? Disseminated 5 3 Allard 07 n/a Sebastien 10-Jul- 285530 Assay Subcrop n/a NAD83 18V 520831 6814254 gb Allard 07 Disseminated n/a 2 nia Sebastien 10-Jul- 285531 Assay Subcrop n/a NAD83 18V 520937 6814390 px Allard 07 Disseminated 3 3 n/a Sebastien 10-Jul- 285532 Assay Subcrop n/a NAD83 18V 520914 6814393 px Allard 07 Disseminated 1 5 n/a Sebastien 16-Jul- 285533 Assay Subcrop n/a NAD83 18V 518493 6813452 pd Disseminated n/a 10 n/a Allard 07 Sebastien 16-Jul- 285534 Assay Outcrop n/a NAD83 18V 518502 6813499 pd Disseminated 10 n/a n/a Allard 07 Sebastien 19-Jul- 285535 Assay Outcrop n/a NAD83 18V 519009 6813802 px Allard 07 Disseminated 10 2 nia Sebastien 19-Jul- 285536 Assay Subcrop n/a NAD83 18V 519012 6813811 px Disseminated 10 5 Allard 07 n/a Sebastien 19-Jul- 285537 Assay Outcrop n/a NAD83 18V 519910 6813848 px Allard 07 Disseminated 10 2 nia Sebastien 19-Jul- 285538 Assay Subcrop n/a NAD83 18V 519291 6814065 px 1 Allard 07 Disseminated 5 nia Sebastien 19-Jul- 285539 Assay Subcrop n/a NAD83 18V 519930 6814089 px Disseminated 5 1 n/a Allard 07 Sebastien 19-Jul- 285540 Assay Subcrop n/a NAD83 18V 519759 6814280 px Disseminated 5 Allard 07 1 n/a Sebastien 20-Jul- 285541 Assay Outcrop n/a NAD83 18V 519750 6814263 pd 1 Allard 07 Disseminated 1 n/a Sebastien 20-Jul- 285542 Assay Subcrop n/a NAD83 18V 520573 6814193 px Disseminated 3 n/a n/a Allard 07 Sebastien 20-Jul- 285543 Assay Subcrop n/a NAD83 18V 521044 6814390 px Disseminated 5 1 n/a Allard 07 Sebastien 21-Jul- 285544 Assay Subcrop n/a NAD83 18V 521103 6814361 px Disseminated 15 3 n/a Allard 07 Sebastien 21-Jul- 285545 Assay Outcrop n/a NAD83 18V 521240 6814371 pd Disseminated 5 n/a n/a Allard 07 Sebastien 21-Jul- 285546 Assay Float n/a NAD83 18V 521534 6814285 beside an ultramafic outcrop and a gossan. Disseminated 2 7 n/a Allard 07 Sebastien 21-Jul- 285547 Assay Outcrop n/a NAD83 18V 521517 6814278 px Disseminated 3 3 n/a Allard 07 Sebastien 24-Jul- 285548 Assay Subcrop n/a NAD83 18V 542767 6830094 pd n/a 3 n/a n/a Allard 07 Sebastien 24-Jul- 285549 Assay Subcrop n/a NAD83 18V 542722 6830059 pd n/a 5 2 n/a Allard 07 Sebastien 24-Jul- 285550 Assay Subcrop n/a NAD83 18V 543468 6830220 pd n/a 3 2 n/a Allard 07 Sebastien 25-Jul- 285551 Assay Outcrop n/a NAD83 18V 520770 6813840 px n/a 15 10 n/a Allard 07 68
GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 Station le Tyypecelity UTM UTM UTM Mineralization Sample ID Name (if Geologist Date Datum Description po% cp% py% T; Zone East North Type apps) Sebastien 25-Jul- 285552 Assay Subcrop n/a NAD83 18V 520981 6813757 px n/a 10 10 n/a Allard 07 Sebastien 25-Jul- 285553 Assay Subcrop n/a NAD83 18V 520980 6813755 px n/a 10 10 n/a Allard 07 Sebastien 25-Jul- 285554 Assay Subcrop n/a NAD83 18V 521032 6813767 px n/a 5 5 nia Allard 07 Sebastien 25 Jul- 285555 Assay Outcrop n/a NAD83 18V 521320 6813889 px n/a 4 10 n/a Allard 07 Sebastien 31-Jul- 285556 Assay Subcrop n/a NAD83 18V 511697 6809941 pxt n/a 5 5 nia Allard 07 No Sebastien 31 Jul 285557 Assay n/a NAD83 18V 511681 6809935 pxt, seb didn't specify locality type nia 10 5 nia exposure Allard 07 Sebastien 31-Jul- 285558 Assay Subcrop n/a NAD83 18V 511676 6809938 >10% S: semi-massive suphides Semi-massive 60 5 nia Allard 07 Sebastien 02-Aug- 285559 Assay Subcrop n/a NAD83 18V 530214 6817308 gb n/a 10 n/a n/a Allard 07 Sebastien 02-Aug- 285560 Assay Subcrop n/a NAD83 18V 530215 6817309 gb n/a 10 2 nia Allard 07 Sebastien 05-Aug- 285561 Assay Subcrop n/a NAD83 18V 491782 6805452 bst??pxt?? nia 1 0.1 nia Allard 07 Sebastien 06-Aug- 285562 Assay Outcrop n/a NAD83 18V 515961 6813203 >10% S: semi-msv sulphd Semi-massive 30 3 nia Allard 07 >10% S: semi-msv slphd. No cpy noted by seb but likely lots in sample. **NOTE** seb's field book Sebastien 06-Aug- n/a NAD83 18V 515959 6813208 says easting of 519959 for this sample. which is south of the lake at Bravo in a swamp; this could still Semi-massive 50 n/a nia 285563 Assay Outcrop Allard 07 be a laie entry. However ML was at Echo on aug 6 wh >10% S: semi-msv slphd. No cpy noted by seb but likely lots in sample. **NOTE** seb's field book Sebastien 06-Aug- 285564 Assay Subcrop n/a NAD83 18V 515933 6813213 says easting of 519933 for this sample. which is south of the lake at Bravo in a swamp; this could still Semi-massive 70 n/a nia Allard 07 be a late entry. However ML was at Echo on aug 6 whe Sebastien 06-Aug- 285565 Assay Outcrop n/a NAD83 18V 515845 6813210 >10% S: semi-msv slphd. Echo 3. No cpy noted by seb but likely lots in sample. Semi-massive 50 n/a n/a Allard 07 Sebastien 06-Aug- 285566 Assay Subcrop n/a NAD83 18V 514596 6812922 semi-msv slphd. No cpy noted by seb but likely lots in sample. Echo 2 area Semi-massive 20 n/a nia Allard 07 Sebastien 06-Aug- 285567 Assay Subcrop n/a NAD83 18V 514575 6812919 gb. Echo 2 area n/a 5 2 nia Allard 07 Sebastien 06-Aug- 285568 Assay Subcrop n/a NAD83 18V 514484 6812919 gb, echo 2 area nia 5 1 nia Allard 07 Sebastien 07-Aug- 285569 Assay Subcrop n/a NAD83 18V 515008 6812673 pdt, rubble @ bottom of echol hill n/a 2 2 nia Allard 07 Sebastian 07-Aug- 285570 Assay Subcrop n/a NAD83 18V 514881 6812614 pxt, rubble @ bottom of echol hill nia 3 3 nia Allard 07 Sebastien 07-Aug- 285571 Assay Subcrop n/a NAD83 18V 514876 6812617 pxt, rubble @ bottom of echol hill nia 10 2 nia Allard 07 Sebastien 07-Aug- 285572 Assay Subcrop n/a NAD83 18V 514853 6812613 pxt, rubble @ bottom of echol hill Blebby 10 3 nia Allard 07 Sebastien 07-Aug- 285573 Assay Subcrop n/a NAD83 18V 514819 6812601 pxt, rubble @ bottom of echol hill n/a 10 3 nia Allard 07 Sebastien 07-Aug- 285574 Assay Subcrop n/a NAD83 18V 514767 6812585 pxt, rubble @ bottom of echol hill n/a 5 3 nia Allard 07 Sebastien 07-Aug- 285576 Assay Subcrop n/a NAD83 18V 514515 6812504 pxt, rubble @ bottom of echol hill n/a 5 3 nia Allard 07 Sebastien 09-Aug- 285577 Assay Subcrop n/a NAD83 18V 532507 6811857 pdt from dragon's eye showing. Seb was asked to take several here but... nia 2 n/a nia Allard 07 Sebastien 07-Aug- 286575 Assay Outcrop n/a NAD83 18V 514623 6812539 pxt, echo 1 n/a 5 3 ria Allard 07 Dominic 17-Sep- FG Pr??, dk green colour from suboutcrop, presence of blue cristaline mineral?? (blue eye qtz??), 1- 285582 Assay Subcrop 1046 NAD83 18V 513637 6817897 n/a 2 n/a nia Lussier 07 2% diss Po Dominic 17-Sep- 285583 Assay Float 1047 NAD83 18V 513251 6817868 CG gabbro, gray colour from rounded boulder, 10% diss Po n/a nia n/a nia Lussier 07 fd pxnite -> pxnite. o/c. from direct & v. sharp (<1mm) contact w/ underlying sediments. o/c ends here BRAVO 2- Whole 21-Jul- Outcrop n/a David Clark NAD83 18V 519632 6813815 but good urn o/c <5m N. Assumption: this represents the 'chilled margin' of the sill system. See n/a nia n/a nia 1 rock 07 picture of contact (100-0155, 100-0156). F->mg light gre
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GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 Station Locality UTMI UTM UTM Mineralization Po% GM Py% Sample ID Sample Name (if Geologist Date Datum Description Type Type Zone East North Type aPPi) BRAVO-2- Whole 21-Jul Outcrop n/a David Clark NAD83 18V 519633 6813825 o/c minerlized of pxnite -> oik peridotite. Patchy & sm blebs po + cp, po 1%-2% cp tr -> 1%. Patchy 1 0.5 nia 2 rock 07 0/c oik pd. F.g. peridotite w/ med. Oikocrysts after pyroxene. Contains tr->1% po + tr cp as small diss BRAVO-2 Whole 21-Jul- Outcrop n/a David Clark 07 NAD83 18V 519605 6813859 patches. Unit contains numerous < 1 cm magnetite veins along fracture surfaces (although this was Disseminated 0.5 0.1 n/a 3 rock avoided for sample).
oik pd from BRAVO-2-3 grades into a talc-rich pxnite over < 3m. This is a sample from first convincing BRAVO -2 Whole 21-Jul- Outcrop n/a David Clark 07 NAD83 18V 519590 6813892 pxnite. Tr diss po + cp. NB: Possibility that fault runs through unit between 2-3 and 2-4. It may be that nia nia n/a nia 4 rock 2-4 is the marginal pxnite for the next urn uni
BRAVO -2- Whole 21-Jul Outcrop n/a David Clark NAD83 18V 519558 6813909 o/c m.g. -> c.g. pxnite, talcose & soft. Probably quite hydrated. Barren From same unite as 2-4. n/a n/a n/a n/a 5 rock 07 BRAVO-2- Whole 21-Jul- o/c knobby oik perid. F.g. perid w/ oik after px. Tr sulphides along fractures. Contiguous o/c with Outcrop n/a David Clark 07 NAD83 18V 519539 6813936 n/a n/a n/a nia 6 rock previous. Whole 03-Aug- CL-1-0 Outcrop n/a David Clark NAD83 18V 540599 6829647 n/a n/a n/a n/a nia rock 07 Whole 03-Aug- CL-1-1 Outcrop n/a David Clark NAD83 18V 540598 6829663 n/a n/a n/a n/a n/a rock 07 Whole 03-Aug- CL-1-2 Outcrop n/a David Clark NAD83 18V 540591 6829683 n/a n/a n/a n/a n/a rock 07 Whole 03-Aug- CL-2-0 Outcrop n/a David Clark NAD83 18V 540401 6829626 n/a n/a n/a n/a n/a rock 07
CL-2-1 Outcrop n/a David Clark -Aug- NAD83 18V 540411 6829623 n/a n/a n/a n/a n/a cockle 0 Whole 03-Aug- CL-3-0 Outcrop n/a David Clark NAD83 18V 539994 6829515 n/a n/a n/a n/a n/a rock 07 Whole 03-Aug- CL-3-1 Outcrop n/a David Clark NAD83 18V 539996 6829539 n/a n/a n/a n/a n/a rock 07 Whole 03-Aug- CL-4-1 Outcrop n/a David Clark NAD83 18V 537797 6829252 putative urn flow-top breccia. n/a n/a n/a n/a rock 07 Whole 02-Aug- pxnite. Sill margin. <3m from gradual magmatic contact w/ overlying urn. Grey-green m.g. massive DELTA-1-1 Outcrop n/a David Clark NAD83 18V 530334 6817003 nia n/a n/a n/a rock 07 pxnite. barren 02-Aug- oik pd. Large metre-scale columnar joints, lineation dipping shallowly (45 degrees) SE. dark blue- DELTA-1-2 Whole Outcrop n/a David Clark NAD83 18V 530322 6817012 n/a n/a n/a n/a rock 07 green f.g. perid w/ pseudomorphs of px oik. Intensely fractured. DELTA-1-3 Outcrop n/a David Clark Aug NAD83 18V 530310 6817035 f.g. blue green pd, well fractured. n/a n/a n/a n/a rock le 0 02-Aug DELTA-1-4 Whole Outcrop n/a David Clark NAD83 18V 530286 6817038 blue grey green f.g. knobby oik pd. n/a n/a n/a n/a rock 07 Whole 02-Aug- s/c urn sill that appears on strike with the D8 deposit, and is partially on GBK ground. F.g. blue green DELTA-2-1 Subcrop n/a David Clark NAD83 18V 529968 6816739 n/a n/a n/a n/a rock 07 pd, fractured. 02-Aug- DELTA-2-2 Whole Subcrop n/a David Clark NAD83 18V 529960 6816737 identical to previous, along strike a few metres n/a n/a n/a n/a rock 07 02-Aug- DELTA-2-3 Whole Subcrop n/a David Clark NAD83 18V 529960 6816737 field duplicate of DELTA-2-2 n/a n/a n/a n/a rock 07 Whole 02-Aug- DELTA-3-1 Outcrop n/a David Clark NAD83 18V 529971 6816975 same sill as DELTA-1 series? F.g. blue grey green pd, some oik of pseudomorphed px. n/a n/a n/a n/a rock 07 Whole 01-Aug- NW-RAG-1 Outcrop n/a David Clark NAD83 18V 522982 6820902 Rock from sill. Rubbly. many fractures. Do not expect great analysis n/a n/a n/a n/a rock 07 Whole 31-Jul- PAD-1-1 Outcrop n/a David Clark NAD83 18V 511590 6809829 Base of the PAD um. Tremolite-rich pxnite, largely barren, quite altered. n/a nia n/a n/a rock 07 Whole 31-Jul- PAD-1-2 Outcrop n/a David Clark NAD83 18V 511571 6809874 Oik pd. Blue green grey. barren. Knobby brown weathered surface. Serpentine veins fairly common. n/a n/a n/a n/a rock 07 Whole 31-Jul- PAD-1-3 Outcrop n/a David Clark NAD83 18V 511527 6809886 oik pd. Identical to previous. Slightly higher in sill stratigraphy n/a n/a n/a n/a rock 07 Whole 31-Jul- PAD-1-4 Outcrop n/a David Clark NAD83 18V 511484 6809889 oik pd. similar to previous, maybe slightly more altered n/a n/a n/a n/a rock 07 Han stn3020 men Outcrop BEL07-3020 Matt Liard 07 Aug- NAD83 18V 498214 6806764 Spec of Mseds taken for cond testing n/a n/a n/a n/a spea light grey green f->mg pyroxenite (I think). Barren. From o/c ridge. Well-developed columna joints, THUNDER Whole 24-Jul- Outcrop n/a David Clark 07 NAD83 18V 542566 6830127 metre-scale. Below this unit, base of small u-shaped valley, chips of graphitic slate in the till. Another n/a n/a n/a n/a 1-1 rock ridge begins to the S. We are just west of NWT-0 THUNDER- Whole 24-Jul From frist good o/c at next ridge s of THUNDER-1-1. F.g. peridotite. R. tr. Cp. Mod-> strongly Outcrop n/a David Clark NAD83 18V 542608 6830013 n/a n/a n/a n/a 1-2 rock 07 magnetic. 70
GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 Station Locality UTM UTM UTM Mineralization Po% cp% Py% Sample ID Sample Name (If Geologist Date Datum Description Type Type Zone East North Type appl) THUNDER- Whole 07Jul-- Outcrop n/a David Clark 1-3 rock NAD83 18V 542611 6829997 F.g. perid, o/c. top of small ridge. Tr cp. Mod-> str magnetic. n/a n/a n/a n/a THUNDER- Whole 24-Jul F.g. perid o/c well-developed. Columnar joints. metre-scale. Last convincing o/c on transect. Mod- Outcrop n/a David Clark NAD83 18V 542625 6829971 n/a nia n/a n/a 1-4 rock 07 >strongly magnetic. Appears to be the eastwards extension of the same sill sampled in the THUNDER-1 series. No o/c THUNDER- Whole 24-Jul- Outcrop n/a 07 2-1 rock David Clark NAD83 18V 543048 6830145 here, but good amount of urn in float, angular. This sample is slightly rusty - sampled in the hope it will n/a n/a n/a n/a contain higher S. and maybe yield valuable Ni/S data. THUNDER- Whole 24-Jul- Small but v. prominent ridge o/c f.g. -> m.g. grey green um pxnite? Under the lens seems quite Outcrop n/a David Clark NAD83 18V 543434 6830319 n/a n/a n/a n/a 3-1 rock 07 amphibolitized. Mod-> strongly magnetic. THUNDER- Whole 19-Aug- Outcrop n/a David Clark NAD83 18V 542521 6829979 4-1 rock 07 Angular float, atop ridge. Blue green f.g. perdotite, rusty-tan colour, 5-6% interstitial f.g. po + cp. n/a n/a n/a nia
71 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
14. APPENDIX 3
Raw Geochemical Data
72 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 Table 5. Geochemical data for 93 grab samples collected during the Goldbrook Raglan summer exploration 2007.
Sample Station Sample Batch # Locality Easting Northing MineralizationType Ni,pct Cu_pct Co_pct Pt_gpt Pd_gpt Au_gpt PtPdAu_gpt Ni_Cu Pt_Pd Description Type Category
gossan with large 'kill zone': med to coard pyxenite with 10-15% cpy+po+py; gossanous material 200720006 280001 n/a gossan 507996 6810677 n/a grab 0.803 0.261 0.049 0.268 1.989 0.007 2.264 3.1 7.4 subcro PPin 9 over 40 m to E and to Lakeshore 200720006 280002 n/a subcrop 510048 6809629 n/a grab 0.023 0.363 0.066 <0.015 <0.01 <0.005 n/a 0.1 nia subcrop and rubble in frost boils; mineralized basalt; 3% cpy+po+/-py 200720006 280003 n/a subcrop 509215 6809517 n/a grab 0.082 0.012 0.008 <0.015 0.015 <0.005 n/a 7.0 n/a subcrop; mod serpentinized of pxnite, 1% cpy+po+/-py; sulphides predominantly fracture controlled 200720006 280004 n/a subcrop 516150 6813217 n/a grab 0.004 0.060 0.005 0.028 <0.01 <0.005 n/a 0.1 n/a subcrop; gossan: unevenly (1-5%) mineralized (po+/-cpy+i-py), med grained?leucograbbro 200720006 280005 n/a gossan 515960 6813206 n/a grab 0.361 0.299 0.061 0.113 0.249 0.025 0.387 1.2 2.2 rubbly gossan; gabbro with > 50% po + (cpy) +/- py; 20 m south of umafic outcrop; photo facing north f.graind serpentinzed umafic with 1-2% v.fine grained disseminated cpy+?po; cluster in frost boils in 200720006 280006 n/a float 515269 6813037 n/a grab 0.192 0.020 0.021 0.058 0.075 0.015 0.148 9.7 1.3 boudlerfield with 80% orange-weathering fine grained oI pxnite. gossan in altered ?gabbro; 5-8% cpy+po (blebby & net texture with some fracture controlled); same 200720006 280007 n/a Gossan 511488 6811956 Blebby grab 0.112 0.743 0.012 0.421 1.361 0.026 1.808 0.2 3.2 gossan as in 07-7046 but -20m E frost boil float (possibly subcrop); fine grained gabbro (?altered basalt?): nonmagnetic; 5-8% cpy+po+/- 200720006 280008 nia Frostboil 511528 6812001 Fracture controlled grab 0.179 2.276 0.036 0.188 1.072 0.068 1.328 0.1 5.7 py: mineralization mostly fracture controlled rubbly gossan; same mineralized trend as in trench (07-7052); <20% po+cpy in med to coarse grained 200720006 280009 n/a Gossan 521740 6814302 Net texture grab 0.959 0.129 0.105 2.938 1.832 0.077 4.847 7.5 0.6 ol-pyroxenite? (?peridotite) boulder (possibly from gossan in nearby flooded trench) with semi-massive po+(cpy) in med to coarse 200720006 280010 n/a Float 521639 6814270 Semi-massive grab 1.800 0.205 0.126 0.413 0.419 0.12 0.952 8.8 1.0 grained ol-pyroxenite small (1x1.5m) blasted pit in rubbly, partially snow-covered gossan (40x10m); altered ?ultramafic; 10 200720006 280011 n/a Gossan 520722 6813857 Blebby grab 0.223 0.561 0.024 0.356 1.276 0.030 1.662 0.4 3.6 20 /° po+cpy; sulphides predominantly blebby but also net textured and fracture controlled 200720006 280012 n/a Boulder 519657 6813823 Disseminated grab 0.009 0.018 0.001 <0.015 <0.01 <0.005 n/a 0.5 Ig boulder of siliceous seds with 3-5% po+cpy; previously sampled (sample 3003) 200720006 280013 n/a Subcrop 519657 6813823 Blebby grab 0.173 0.111 0.011 0.091 0.322 0.006 0.419 1.6 3.5 subcrop; coarse grained pyroxenite with 3-5% po+cpy; po»>cpy few, large (car size) angular boulders of coarse grained pyroxenite with <8% po+(cpy): behind and uphill 200720006 280014 n/a Subcrop519004 6813809 Net texture grab 0.045 0.036 0.008 0.024 0.031 <0.005 nia 1.3 1.3 from DDH NW04 14; (I think they f... up) 200720006 280024 n/a subcrop 533016 6815031 n/a grab 0.169 0.001 0.012 0.045 0.083 0.047 0.175 153.2 1.8 8m wide; subcrop of rubbly; dark brown red, f grained ? Pyroxnite w/ <2% fracture controlled po 200720006 280025 n/a gossan 532750 6815125 n/a grab 0.009 0.039 0.002 0.02 0.014 0.012 0.046 0.2 0.7 gossan rubble in frost boi: med grained gabbro with up to (dissem & blebby) 2% of po+py+cpy 200720006 280026 n/a subcrop 528740 6815231 n/a grab 0.102 0.004 0.009 0.016 <0.01 <0.005 n/a 28.4 n/a subcrop; c grained of pxnite with trace to minor po 200720006 280027 n/a float 528278 6815260 n/a grab 0.233 0.220 0.013 0.101 0.285 0.011 0.397 1.1 2.8 edge of Ig boulderfield; altered pyroxenite (?gabbro) w/ 1-2% f.gr. Diss po+cpy same bldr field as above; angular bldr of fine to med grained, magnetic, pyrxenite w/ 2-3% blebby and 200720006 280028 n/a float 528282 6815259 n/a grab 0.253 0.211 0.017 0.1115 0.3500 0.0155 0.477 1.2 3.1 diss cpy+po (cpy:po = 2) 200720006 280029 n/a boulder 516515 6812504 n/a grab 0.008 0.035 0.005 0.017 <0.01 0.036 nia 0.2 nia angular boulder of grungy. med grained, magnetic ?pyroxenite; 3% diss po 200720006 280501 BEL07-5001 Frostheave 511366 6809728 Disseminated grab 0.976 0.331 0.037 0.027 0.01 <0.005 nia 2.9 0.4 Angular f/h. Mafic->um, m.g., green, presumed +- in situ. F. patchy diss po + cp, 2%, 1% Timtu. Sub angular boulder ultramafic. v. rusty. Mod. Magnetic. F-diss > almost net texture, v. fine. 20 200720006 280502 BEL07-5009 Boulder 507989 6810733 Net texture grab 0.945 0.320 0.035 0.564 2.772 0.062 3.398 2.9 4.9 30% sulphides. 90:10 po:cp. Boulder is +- 5 m from riverbank. Fairly altered, f.g. 200720006 280503 BEL07-5009 Boulder 507969 6810720 Patchy grab 0.155 0.793 0.011 0.601 2.436 0.061 3.098 0.2 4.1 Sub-angular boulder, mg pxnite, less rusty than previous, patchy cp 5%, po tr->1% Sub angular boulder, f.g. urn, mod magnetic. Leopard skin textured, with patchy -> net textured 200720006 280504 BEL07-5009 Boulder 507988 6810723 Net texture grab 0.886 0.522 0.037 0.583 3.814 0.067 4.464 1.7 6.5 framework surrounding 'blebs' of less mineralized urn. 5:1 po:cp, -30-40% sulphides. 200720006 280505 NOV07-5022 Outcrop 514672 6812629 Net texture grab 0.414 1.479 0.050 0.112 0.163 0.01 0.285 0.3 1.5 f.g. urn. Diss-> net textured po + cp. locally up to 50% po, 10-15% cp as blebs and stringers. 200720006 280506 NOV07-5022 Outcrop 514672 6812629 Net texture grab 0.491 1.706 0.057 0.026 0.093 <0.005 nia 0.3 3.6 f.g. urn. Diss-> net textured po + cp. locally up to 50% po, 10-15% cp as belbs and stringers. 200720006 280507 NOV07-5042 Outcrop 493825 6805987 Patchy grab 0.023 0.057 0.006 <0.015 <0.01 <0.005 nia 0.4 nia Mafic volcanic. 3-4% po, 1-2% cp as patchy diss fr contr, occasional larger blebs. From Peter's showing. Strange altered gabbro, heavily malachite stained, v. soft. leeched to shit. +- 200720006 280508 n/a Boulder 530592 6816437 n/a grab 0.079 15.528 0.003 0.789 26.722 11.673 39.184 0.0 33.9 30% cp. From angular boulder. o/c here is rather a pyroxenite -> feldspathic pyroxenite. No 200720006 280509 NOV07-5055 Outcrop 532015 6818764 Disseminated grab n/a nia n/a nia n/a Sample n/a n/a n/a F.g. pyroxenite. V weakly magnetic. Received 200720006 280510 n/a Float 526005 6815963 Patchy grab 0.207 0.307 0.006 0.324 0.574 0.053 0.951 0.7 1.8 Float -> s/c gabbro -> feld. Pyroxenite sic > rubble, but < 10 m away from um ridge; more or less in situ. Horzon of goassanous rubble. 200720006 280511 NOV07-5067 Subcrop 526963 6816470 Disseminated grab 0.209 0.157 0.015 0.042 0.089 0.025 0.156 1.3 2.1 Pyroxenite, -10%po as interstitial -> almost locally net-textured, cp 5% 200720006 280512 NOV07-5067 Subcrop 526912 6816470 Patchy grab 0.143 0.091 0.011 0.043 0.132 <0.005 nia 1.6 3.1 Rubbly, as previous. C.g. pyroxenite -15% po, tr ->1% cp. as patchy aggregates. 200720006 280513 NOV07-5067 Subcrop 526951 6816584 Patchy grab 0.532 0.515 0.016 0.165 0.775 0.071 1.011 1.0 4.7 S/c, f.g. peridotite. F diss patchy aggregates po, -10%. cp 2%
200720006 280514 n/a Frostheave 535614 6818366 Finely disseminated grab 0.118 0.005 0.009 <0.015 <0.01 <0.005 nia 24.6 n/a F/h rust looking f.g. mod. Magnetic peridotite, tr->1% po, f.diss, & small fracture smears.
200720006 280515 n/a Float 535570 6818506 Finely disseminated grab 0.009 0.022 0.003 <0.015 <0.01 <0.005 n/a 0.4 n/a Float, to N of main sill. f.g. pyroxenite, rusty, -15% po as v. finely diss.
O/c m.g.->c.g. pyroxenite massive. From N side of ridge. Not particularly rusty or gossanous, but 200720006 280516 n/a Outcrop 521858 6813983 Finely disseminated grab 0.060 0.009 0.008 <0.015 <0.01 <0.005 nia 6.9 n/a mineralized throughout nonetheless. Mineralization is v. fine diss magmatic sulphides, 2-3% (?)
200720006 280517 n/a Subcrop 522063 6814010 Finely disseminated grab 0.086 0.009 0.008 <0.015 <0.01 <0.005 n/a 9.6 n/a S/c. Same horizon as previous. V. altered pervasively fractured. F. diss sulphides 1%.
73 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 Sample Station Sample Batch # Locality Easting Northing MineralizationType Ni_pct Cu_pct Co_pct Pt_gpt Pdypt Au_gpt PtPdAu_gpt Ni_Cu Pt Pd Description ID Type Category Horizon of rusty mineralized mafic volcanics, N side of the unit. Rock is v. f.g., mineralized. w/ v.f. 200720006 280518 NOV07-5076 Outcrop 512608 6817932 Fracture controlled grab 0.020 0.018 0.006 0.02 <0.01 <0.005 n/a 1.1 nia sulphides along fractures, -5% o/c m.g. pyroxenite, patchy &blebs po + cp. 5:1, <1.5 cm, diss f cp. Total 6% po, 4% cp. Previously 200720006 280519 NOV07-5079 Outcrop 517660 6813175 Patchy grab 0.178 0.268 0.009 0.2195 0.482 0.0195 0.721 0.7 2.2 sampled by NW (?) sample #5102. 200720006 280520 NOV07-5079 Outcrop 517653 6813198 Disseminated grab 0.472 0.262 0.024 0.204 0.394 0.007 0.605 1.8 1.9 o/c m.g. pyroxenite, diss f.g. po + cp, + patchy blebs cp < 1 cm. 15% total sulphides. 200720006 280521 NOV07-5079 Frostheave 517635 6813219 Patchy grab 0.583 0.398 0.026 0.354 0.547 0.013 0.914 1.5 1.5 f/h at base of hill. Mg. pyroxenite. 15-20% 60:40 po:cp as patchy blebs & diss. 200720006 280522 NOV07-5079 Frostheave 517632 6813228 Net texture grab 0.505 0.432 0.022 0.229 0.403 0.026 0.658 1.2 1.8 M.g. pyroxenite f/h, 20-25% sulphides, as large patches, locally net-textured, 60:40 po:cp 200720006 280523 NOV07-5079 Frostheave 517655 6813283 Patchy grab 0.314 0.068 0.026 0.03 0.09 <0.005 n/a 4.6 3.0 f/h -> float, c.g. pyroxenite. 10% po, 5% cp as patchy aggregates. 200720006 280524 n/a Outcrop 520165 6813847 n/a grab 0.074 0.014 0.009 <0.015 <0.01 <0.005 n/a 5.3 nia Assay of BRAVO-1-1 200720006 280525 n/a Outcrop 520171 6813865 n/a grab 0.083 0.003 0.009 <0.015 <0.01 <0.005 n/a 24.3 nia Assay of BRAVO-1-2 200720006 280526 n/a Outcrop 520164 6813883 n/a grab 0.091 0.003 0.010 <0.015 <0.01 <0.005 n/a 33.5 nia Assay of BRAVO-1-3 200720006 280527 n/a Outcrop 520159 6813903 n/a grab 0.098 0.005 0.010 <0.015 <0.01 <0.005 n/a 20.9 n/a Assay of BRAVO-1-4 200720006 280528 n/a Outcrop 520153 6813935 n/a grab 0.128 0.023 0.011 0.041 0.046 n/a n/a 5.6 1.1 Assay of BRAVO-1-5 200720006 280529 n/a Outcrop 520141 6813965 n/a grab 0.135 0.006 0.012 0.023 0.033 0.005 0.061 22.8 1.4 Assay of BRAVO-1-6 200720006 280530 n/a Outcrop 520110 6813990 n/a grab 0.139 0.002 0.011 0.027 0.041 <0.005 n/a 73.1 1.5 Assay of BRAVO-1-7 200720006 280531 n/a Outcrop 520136 6814015 n/a grab 0.144 0.007 0.012 0.026 0.023 <0.005 n/a 21.5 0.9 Assay of BRAVO-1-8 200720006 280532 n/a Outcrop 520132 6814062 n/a grab 0.148 0.001 0.008 0.033 0.011 <0.005 n/a 295.4 0.3 Assay of BRAVO-1-9 200720006 280533 n/a Outcrop 520134 6814106 n/a grab 0.120 0.008 0.012 0.03 0.018 <0.005 n/a 15.8 0.6 Assay of BRAVO-1-10 & BRAVO-1-11 200720006 280534 n/a Outcrop 520127 6814138 n/a grab 0.211 0.008 0.015 0.057 0.067 0.017 0.141 27.0 1.2 Assay of BRAVO-1-12 200720006 280535 n/a Outcrop 520092 6814230 n/a grab 0.122 0.014 0.012 0.041 0.038 <0.005 n/a 9.0 0.9 Assay of BRAVO-1-13 200720006 280536 n/a Outcrop 520126 6814266 n/a grab 0.097 0.006 0.011 0.03 0.015 <0.005 n/a 15.9 0.5 Assay of BRAVO-1-14 200720006 280537 n/a Outcrop 520136 6814291 n/a grab 0.052 0.002 0.007 0.032 <0.01 <0.005 nia 26.2 nia Assay of BRAVO-1-15. gossan with large "kill zone"; med to coarse pyroxenite with 10-15% cpy+po(+py?): gossanous material 200720006 285501 n/a outcrop 515980 6813209 fracture grab 0.054 0.068 0.009 <0.015 0.028 <0.005 n/a 0.8 nia subcropping over 40m to E and to lakeshore 200720006 285502 nia subcrop 515529 6813205 disseminated grab 0.137 0.163 0.022 0.199 0.133 0.026 0.358 0.8 0.7 gabbro 200720006 285503 nia outcrop 515863 6813219 disseminated grab 0.058 0.062 0.012 0.126 0.136 0.01 0.272 0.9 1.1 gabbro 200720006 285504 nia subcrop 515513 6812966 disseminated grab 0.148 0.107 0.015 0.024 0.113 <0.005 n/a 1.4 4.7 gabbro or peroxynite 200720006 285505 n/a subcrop 511433 6811956 disseminated grab 0.050 0.002 0.009 <0.015 <0.01 <0.005 n/a 22.5 nia px 200720006 285506 n/a boulder 511557 6812115 disseminated grab 0.114 0.044 0.014 0.062 0.2 <0.005 n'a 2.6 3.2 pd angular boulder 200720006 285507 n/a outcrop 521821 6814332 blebby grab 0.852 0.188 0.048 0.987 0.458 <0.005 n/a 4.5 0.5 px 200720006 285508 n/a outcrop 521820 6814330 semi-massive grab 3.006 0.890 0.210 1.754 2.34 0.021 4.115 3.4 1.3 px 200720006 285509 n/a outcrop 521820 6814330 semi-massive grab 1.311 0.647 0.097 0.6105 1.01 0.029 1.650 2.0 1.7 px 200720006 285510 n/a outcrop 521640 6814283 massive grab 2.405 1.360 0.123 1.092 3.027 0.344 4.463 1.8 2.8 px 200720006 285511 n/a outcrop 521645 6814265 disseminated grab 0.323 0.374 0.022 0.78 0.828 0.013 1.621 0.9 1.1 px 200720006 285512 n/a outcrop 520750 6813859 disseminated grab 1.508 0.806 0.066 0.177 0.748 0.019 0.944 1.9 4.2 px 200720006 285513 n/a outcrop 520025 6813856 disseminated grab 0.034 0.018 0.009 <0.015 <0.01 0.012 n/a 1.9 nia px 200720006 285514 n/a outcrop 519752 6813909 disseminated grab 0.174 0.204 0.012 0.217 0.374 <0.005 n/a 0.8 1.7 px 200720006 285515 n/a subcrop 519621 6813822 disseminated grab 0.282 0.540 0.023 0.241 1.103 0.015 1.359 0.5 4.6 px 200720006 285516 n/a outcrop 519598 6813834 disseminated grab 0.180 0.228 0.016 0.143 0.563 <0.005 nia 0.8 3.9 px 200720006 285517 n/a outcrop 519505 6813832 disseminated grab 0.345 0.563 0.021 0.34 0.978 0.035 1.353 0.6 2.9 px 200720006 285518 n/a outcrop 530790 6816239 disseminated grab 0.180 0.223 0.055 <0.015 <0.01 0.018 n/a 0.8 n/a px? Ba? 200720006 285519 n/a outcrop 530795 6816254 disseminated grab 0.137 0.135 0.046 0.021 0.014 n/a 1.0 n/a px? Ba? 200720006 285520 n/a outcrop 530801 6816235 disseminated grab 0.131 0.147 0.047 0.223 0.177 0.038 0.438 0.9 0.8 px? Ba? 200720008 285251 1001 Subcrop 501115 6806665 n/a GRAB 0.010 0.017 0.005 <15 <10 <5 n/a n/a n/a CG gabbro, possibly SpGB with 2-3% Po, diss+ vein remob. subcrop 200720008 285252 1002 Subcrop 501201 6806754 n/a GRAB 0.009 0.010 0.006 <15 <10 <5 nia n/a nia FG gabbro, gray colour, 2% Po 1% Cpy, diss, subcrop 200720008 285253 1003 Subcrop 499532 6806995 n/a GRAB 0.009 0.013 0.006 <15 <10 <5 nia n/a n/a CG gabbro, possibly SpGB with 2-3% Po, diss+ vein remob, subcrop 200720008 285254 1004 Subcrop 499433 6807001 n/a GRAB 0.007 0.011 0.006 <15 <10 <5 n/a n/a nia CG gabbro, possibly SpGB with 1-2% Po, diss+ vein remob, subcrop 200720008 285255 1005 Subcrop 499340 6806959 n/a GRAB 0.004 0.053 0.006 <15 <10 <5 nia n/a nia FG Pxt, gray colour, 1-2% diss sulphides, subcrop 200720008 285256 1006 Subcrop 499270 6806929 n/a GRAB 0.003 0.045 0.006 <15 0.013 <5 n/a n/a nia MG Pxt, green colour, 2% Po 1% Cpy FG diss, subcrop 200720008 285257 1007 Subcrop 499290 6806730 n/a GRAB 0.002 0.026 0.005 <15 <10 <5 n/a n/a nia MG Pxt, green colour, 4% Po 1% Cpy diss. subcrop 200720008 285258 1008 Subcrop 498923 6806401 n/a GRAB 0.002 0.015 0.004 <15 <10 <5 n/a n/a nia MG Pxt, 1-2% Po, subcrop 200720008 285259 1009 Subcrop 498564 6806606 n/a GRAB 0.004 0.011 0.004 <15 <10 <5 n/a n/a nia MG to CG Pxt, 2% Po, subcrop 200720008 285260 1010 Subcrop 498128 6806583 n/a GRAB 0.007 0.003 0.005 <15 <10 <5 nia n/a nia FG gabbro, 2% Po diss + FF, probably subcrop 200720008 285261 1012 Boulder 498124 6806664 n/a GRAB 0.006 0.003 0.005 <15 <10 <5 n/a n/a n/a MG gabbro, visible plag lath. 3-4% Po, from rounded boulder 200720008 285262 1013 Boulder 490697 6806335 n/a GRAB 0.005 0.016 0.006 <15 0.012 <5 n/a n/a nia MG Pxt, plag <10%, dk green, 4% Po 1% Cpy diss 200720008 285263 1014 Boulder 490780 6806479 n/a GRAB 0.003 0.046 0.006 <15 <10 0.008 n/a n/a nia CG Pxt, possibly 01 Pxt, green, 5% Po 1% Cpy, base of a slope, many other around 200720008 285264 1015 Subcrop 490816 6806679 n/a GRAB 0.253 0.649 0.021 41,3-141 4648 9928 n/a n/a nia FG Prt, rusty alt, presence of sulphide?? Is it mica?? Subrop
74
GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007 SampleI Station Sample Batch # Locality a E sting Northing MlnerallzationTeyp Ni_pct Cu_pct Co_pct Pt_gpt Pd_gpt Au_gpt PtPdAu_gpt Ni_Cu Pt_Pd Description Category 9 y 200720008 285265 1016 Subcrop 490815 6806679 n/a GRAB 0.346 0.266 0.023 A.A70 047-5 13,00.7 n/a n/a n/a same as 1014. presence of a 2mm sulphide vein 200720008 285266 n/a Subcrop 490992 6806686 n/a GRAB 0.394 0.850 0.027 4:444 4446 Q044 n/a n/a n/a MG gabbro, light gray colour, 6% Po 2% Cpy interstitial, subcrop??
75 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
15. APPENDIX 4
Grab Sample Assay Certificates
Job number: 200720006_AL912_2007-08-24 see assay tag numbers: 280001-280014; 280024-280029; 280501-280537; 285501-285520
Job number: 200720008_AL917_2007-10-03 see assay tag numbers: 285251-285259; 285260-285266
76 1 of 7
Goldbrook Ventures Inc. Date Created: 07-08-24 03:20:57 PM Job Number: 200720006 Date Received: Jul 19, 2007 Number of Samples: 457 Type of Sample: Rock Date Completed: Aug 24, 2007 Project ID:
Acc # Client ID Au ppm Pt ppm Pd ppm Rh ppm Ag ppm Co / Cu % Fe % Ni % Pb % Zn % 0.005 DL 0.015 DL 0.01 DL 0.005 DL 284 280001 0.007 0.268 1.989 0.0491 0.2613 0.8031 285 280002 <0.005 <0.015 <0.01 0.066 0.3632 0.0226 286 280003 <0.005 <0.015 0.015 0.0081 0.0118 0.0823 287 280004 <0.005 0.028 <0.01 0.0049 0.0602 0.0044 288 280005 0.025 0.113 0.249 0.0612 0.2994 0.3609 289 280006 0.029 0.057 0.054 0.0184 0.0231 0.1691 290 280007 0.026 0.421 1.361 0.0115 0.7425 0.1117 291 280008 0.068 0.188 1.072 0.0361 2.2759 0.1785 292 280009 0.077 2.938 1.832 0.1052 0.1287 0.959 293 280010 0.12 0.413 0.419 0.1257 0.2048 1.8003 294 280010 0.093 0.493 0.404 0.1173 0.1872 1.9925 295 280011 0.023 0.414 1.337 0.0284 0.4348 0.2732 296 280012 <0.005 <0.015 <0.01 0.0013 0.0179 0.0087 297 280013 0.007 0.088 0.355 0.0104 0.1141 0.1716 298 280014 <0.005 0.024 0.031 0.0082 0.0358 0.045 299 280015 0.005 0.095 0.312 0.0107 0.1072 0.1737 300 280016 <0.005 0.056 0.096 0.0237 0.0163 0.2147 301 280017 0.036 0.298 1.215 0.0187 0.6878 0.1727 302 280018 0.071 0.233 0.317 0.0877 0.9046 1.8952 303 280019 0.133 0.354 0.43 0.0874 0.8939 1.8652 304 280020 0.108 0.197 0.204 0.0858 0.8804 1.8615 305 280020 0.056 0.152 0.222 0.086 0.9742 2.0707 306 280021 0.043 0.048 0.085 0.001 0.0055 0.0135 307 280022 0.02 <0.015 <0.01 0.0007 0.0022 0.007 308 280023 0.009 0.028 <0.01 0.0007 0.0019 0.0049 309 280024 0.047 0.045 0.083 0.0115 0.0011 0.1685 310 280025 0.012 0.02 0.014 0.0022 0.0394 0.0091 311 280026 <0.005 0.016 <0.01 0.0089 0.0036 0.1024 312 280027 0.011 0.101 0.285 0.0131 0.2195 0.2331 313 280028 0.017 0.113 0.342 0.0169 0.2107 0.2539 314 280028 0.014 0.11 0.358 0.0168 0.2111 0.2526 315 280029 0.036 0.017 <0.01 0.0045 0.0353 0.0081 316 280030 Received 317 280031 Received 318 280032 Received 319 280033 Received 320 280034 Received 321 280035 Received 322 280036 Received 323 280037 Received 324 280038 Received 325 280038 Received 326 280039 Received 327 280040 Received 328 280041 Received 329 280042 Received 330 280043 Received 331 280044 Received 332 280045 Received 333 280046 Received 334 280047 Received 335 280048 Received 336 280048 Received 337 280049 Received 338 280050 Received 339 280051 <0.005 0.051 0.108 0.0097 0.0273 0.0911 340 280052 0.007 0.063 0.15 0.0092 0.068 0.0865 341 280053 0.013 0.047 0.205 0.0087 0.0692 0.0946 342 280054 0.013 0.048 0.148 0.0092 0.0711 0.1158 343 280055 0.011 0.132 0.458 0.014 0.1287 0.2083 344 280056 0.008 0.106 0.512 0.0138 0.1508 0.22 345 280057 0.009 0.082 0.247 0.0076 0.0522 0.0898 346 280058 0.005 0.148 0.475 0.0143 0.146 0.1926 347 280058 0.006 0.139 0.514 0.0147 0.192 0.1945 348 280059 0.01 0.088 0.278 0.0078 0.082 0.1003 349 280060 0.007 0.078 0.223 0.0077 0.0371 0.0934 350 280061 0.014 0.07 0.329 0.0078 0.0879 0.1133 351 280062 0.009 0.092 0.443 0.0142 0.1984 0.2352 352 280063 0.009 0.058 0.351 0.0102 0.2778 0.1565 353 280064 <0.005 0.031 0.236 0.0127 0.1736 0.1952 354 280065 0.026 0.19 0.706 0.0176 0.2867 0.2765 2 of 7
355 280066 0.021 0.341 0.89 0.0165 0.3797 0.2933 356 280067 0.015 0.29 0.802 0.0201 0.2647 0.4441 357 280068 0.044 0.496 5.746 0.0743 3.1293 1.7292 358 280068 0.095 0.3184 5.904 0.0728 2.9048 1.6616 359 280069 0.006 0.023 9.08 0.0071 0.0319 0.0574 360 280070 0.007 <0.015 0.037 0.0056 0.0128 0.0295 361 280071 0.017 0.125 0.715 0.0448 0.5432 1.0544 362 280072 0.014 0.114 0.628 0.0306 0.2565 0.6753 363 280073 0.012 0.1.8 115 0.0392 0.3758 0.903 364 280074 0.065 0.057 0242 0.0037 0.1809 0.0571 365 280075 0.11 0.883 5.33 0.0688 0.599 1.4565 366 280076 0.126 0.64 5.677 0.0419 1.2573 0.9874 367 280077 <0.005 <0.015 0.108 0.0015 0.0297 0.0147 368 280078 0.006 <0.0115 0.013 0.0005 0.0012 0.0019 369 280078 <0.005 0.034 0.018 0.0004 0.0011 0.0018 370 280079 0.023 0. ^c 0.463 0.011 0.1152 0.1068 371 280080 0.021 0.067 0.41 0.011 0.1288 0.1149 372 280081 0.029 0.075 0.402 0.0148 0.1982 0.1546 373 280082 0.014 0137 0.416 0.0119 0.1437 0.1213 374 280083 0.012 0.044 0243 0.01 0.0735 0.0942 375 280084 0.007 0.0119 0.186 0.0119 0.0741 0.104 376 280085 0.007 0.017 0153 0.0096 0.0337 0.079 377 280086 0.012 <0.015 0.069 0.009 0.0149 0.0664 378 280087 0.012 <0.015 0.069 0.0096 0.0183 0.0723 379 280088 0.019 <0.0115 0.047 0.0092 0.0138 0.0655 380 280088 <0.005 0.027 0.046 0.0089 0.0133 0.0636 381 280089 0.027 <0.0115 0175 0.0091 0.0205 0.0678 382 280090 0.01.4 <0.0115 9.061 0.0092 0.0151 0.0664 383 280091 0.043 0.063 0.993 0.0088 0.0141 0.0632 384 280092 0.012 <0.0115 9.038 0.0097 0.0142 0.0736 385 280093 0.011 <0.0115 0.154 0.011 0.0227 0.0859 386 280094 0.03 0_162 0.068 0.0108 0.0216 0.0805 387 280095 0.037 <0.015 0.052 0.0094 0.0175 0.072 388 280096 0.0144 <0.0115 0.054 0.0078 0.0177 0.0522 389 280097 0.009 <0.045 0.081 0.0102 0.0101 0.0785 390 280098 0.019 0.023 0.078 0.0111 0.0192 0.0849 391 280098 0.009 0.036 9.082 0.012 0.02 0.0902 392 280099 0.009 0.016 0.071 0.0102 0.0105 0.0788 393 280100 0.008 0.039 0.05 0.0101 0.0169 0.0812 394 280101 <0.005 0.028 0199 0.0101 0.0252 0.0761 395 280102 0.013 0.048 0162 0.011 0.0095 0.088 396 280103 0.02 0.043 0.075 0.0098 0.0158 0.0766 397 280104 0.087 0.022 9.013 0.0113 0.0181 0.0927 398 280105 0.005 0.025 0.082 0.0099 0.0276 0.0855 399 280106 0.032 0.055 0.144 0.0098 0.0263 0.0882 400 280107 0.012 0.062 1.179 0.0096 0.0335 0.0856 401 280108 <0.005 0.046 0.054 0.009 0.0185 0.0709 402 280108 <0.005 0.044 0.00.5 0.009 0.019 0.0738 403 280109 <0.005 0.025 0.037 0.0106 0.0178 0.0852 404 280110 <0.005 <0.0115 G0.01 0.003 0.0045 0.0176 405 280111 0.011 0.025 0.051 0.01 0.0184 0.0776 406 280112 <0.005 0134 13.167 0.0091 0.028 0.0742 407 280113 0.006 0.039 10242 0.0095 0.016 0.0705 408 280114 <0.005 0.025 0.051 0.0099 0.0209 0.0735 409 280115 0.15 0.063 0.114 0.0109 0.0363 0.0887 410 280116 0.006 0.034 0.039 0.0089 0.0181 0.0699 411 280117 0.005 0.0211 0.028 0.0102 0.0192 0.081 412 280118 0.076 0.043 0.105 0.009 0.0535 0.0896 413 280118 0.083 0.032 0.092 0.01 0.052 0.0884 414 280119 0.037 0.075 0219 0.0079 0.0278 0.0672 415 280120 <0.005 0.046 0.118 0.0043 0.0348 0.0215 416 280501 <0.005 0.027 0.01 0.0372 0.3312 0.9759 417 280502 0.062 0.564 2.772 0.0352 0.3203 0.9447 418 280503 0.061 0_6011 2.436 0.0107 0.7928 0.1546 419 280504 0.067 0.563 3.814 0.0366 0.5216 0.8858 420 280505 0.01 0.112 0.163 0.0501 1.4788 0.4143 421 280506 <0.005 0.026 0.093 0.0567 1.7064 0.4909 422 280507 <0.005 <0.0115 <001 0.0056 0.0566 0.0231 423 280508 12.061 0.668 28258 0.0027 14.5995 0.0796 424 280508 11.285 0.91 25.186 0.0024 16.4574 0.0777 425 280509 Received 426 280510 0.053 0.324 0574 0.0058 0.3071 0.207 427 280511 0.025 0.042 0089 0.0145 0.1571 0.2092 428 280512 <0.005 0.043 0.132 0.0109 0.0911 0.1427 429 280513 0.0711 0.165 0.775 0.0156 0.5149 0.5315 430 280514 <0.005 <0.015 <911 0.0092 0.0048 0.1179 431 280515 <0.005 <0.0115 <0.01 0.0033 0.0216 0.0093 432 280516 <0.005 <0.045 <1101 0.0075 0.0087 0.0602 433 280517 <0.006 <0.0115 40.01 0.0083 0.009 0.0861 434 280518 <0.005 0122 4061 0.0064 0.0176 0.0202 435 280519 0.022 0.13e 0.431 0.0095 0.2625 0.1727 436 280519 0.017 024177 0.483 0.0094 0.2734 0.1835 3of7
437 280520 0.007 0.204 0.394 0.0243 0.2621 0.4715 438 280521 0.013 0.354 0.547 0.0262 0.3984 0.5828 439 280522 0.026 0.229 0.403 0.0223 0.4324 0.5048 440 280523 <0.005 0.0.3 0.09 0.0255 0.0683 0.3144 441 280524 <0.005 <0.015 <0.01 0.0086 0.014 0.0743 442 280525 <0.005 <0.015 <0.01 0.0094 0.0034 0.0827 443 280526 <0.005 <0.015 <0.01 0.0103 0.0027 0.0905 444 280527 <0.005 <0.015 <0.01 0.0101 0.0047 0.0981 445 280528 <0.005 0.04E 0.042 0.0112 0.0226 0.1257 446 280528 <0.005 0.035 0.05 0.0116 0.0231 0.1303 447 280529 0.005 0.023 0.033 0.0116 0.0059 0.1346 448 280530 <0.005 0.023 D.041 0.0112 0.0019 0.1388 449 280531 <0.005 0.026 0_023 0.0122 0.0067 0.1443 450 280532 <0.005 0.038 1.011 0.0083 0.0005 0.1477 451 280533 <0.005 0.03 13.018 0.0122 0.0076 0.1203 452 280534 0.017 0.057 0.067 0.015 0.0078 0.2107 453 280535 <0.005 0.041 9.038 0.0121 0.0135 0.1215 454 280536 <0.005 0.03 0.015 0.0107 0.0061 0.0969 455 280537 <0.005 0.032 <0.01 0.0069 0.002 0.0523 456 280538 <0.005 0.031 0.018 0.0091 0.0097 0.0658 457 280538 <0.005 0.01:6 0.021 0.0085 0.0094 0.0638 458 280539 0.009 0.015 0.016 0.0076 0.0087 0.0593 459 280540 <0.005 0.031 0.02 0.0088 0.014 0.0683 460 280541 <0.005 0.032 0.026 0.0084 0.0147 0.0688 461 280542 <0.005 0133 0.035 0.0072 0.0033 0.0461 462 280543 <0.005 <0.015 0.017 0.0077 0.0056 0.0547 463 280544 <0.005 0.052 0.194 0.0095 0.0067 0.06 464 280545 <0.005 <0.01.5 0.015 0.0084 0.0047 0.0536 465 280546 <0.005 0.021 0.044 0.0075 0.0064 0.0458 466 280547 0.007 <0.015 0.025 0.0076 0.0028 0.0436 467 280548 0.014 0.021 0.051 0.0077 0.002 0.0505 468 280549 <0.005 0215 0.572 0.0206 0.4193 0.4154 469 280549 0.012 0.212 0.619 0.0202 0.4184 0.4021 470 280550 0.021 0.245 0.606 0.0107 0.2183 0.1874 471 281360 0.022 0.115 0.403 0.0148 0.2381 0.2397 472 281361 0.013 0.153 0.436 0.0175 0.2429 0.2889 473 281362 0.074 0.153 0.494 0.0164 0.2984 0.2537 474 281363 0.018 0.185 0.506 0.017 0.2925 O.iARS 475 281364 0.031 0.275 79978 0.0251 0.659 0.5272 476 281365 0.03 0.294 1.35 0.0178 0.3874 0.3471 477 281366 0.029 0.252 0.626 0.0296 0.7411 0.5853 478 281367 0.007 0.053 D.161 0.0088 0.0729 0.0902 479 281368 0.022 0.057 0286 0.0114 0.3326 0.1811 480 281369 0.009 0.132 0.297 0.0146 0.1917 0.2884 481 281369 0.014 0.139 0.315 0.0142 0.1851 0.284 482 281370 0.012 0.12a1 0,343 0.0188 0.3211 0.3405 483 281371 0.022 0.09E 031 0.012 0.2331 0.1802 484 281372 0.006 0.054 0.177 0.0145 0.2821 0.254 485 281373 0.031 024 0.742 0.0212 0.5207 0.3977 486 281374 0.026 0.189 0.68 0.019 0.4046 0.3609 487 281375 0.006 0_08,7 11261 0.0139 0.2447 0.2458 488 281376 0.045 0.17 0.615 0.0185 0.4588 0.3247 489 281377 0.017 0.173 0.696 0.0168 0.4583 0.3066 490 281378 0.107 0_75 0378 0.0191 - 0.5913 0.2694 491 281379 <0.005 <0.015 <0.01 <0.0001 <0.0001 <0.0001 492 281380 0.012 0.113B 0.623 0.0187 0.4074 0.3552 493 281380 0.028 0.175 0.618 0.0178 0.3895 0.3476 494 281381 0.035 0.204 0.655 0.0152 0.3518 0.2897 495 281382 0.011 0.097 0.399 0.0154 0.3892 0.3087 496 281383 0.019 0.199 0.634 0.0178 0.3496 0.3744 497 281384 0.017 0.191 1169 0.0157 0.3593 0.311 498 281385 0.042 0.153 0.653 0.0155 0.3262 0.3135 499 281386 0.036 0.159 0.572 0.0118 0.2423 0.2185 500 281387 0.012 0.11-4 0.454 0.013 0.1912 0.272 501 281388 0.011 0.029 1.864 0.0613 0.0784 1.4118 502 281389 0.011 0.127 0.358 0.1315 0.2094 4.6798 503 281389 0.006 0.145 0.406 0.1217 0.2021 4.1136 504 281390 0.015 0.486 1.294 0.0197 4.1115 0.4233 505 281391 0.019 0.095 0.913 0.0108 0.169 0.2135 506 281392 0.053 0.053 0.422 0.0108 0.2161 0.2129 507 281393 0.021 0.139 0 IRS 0.019 0.3741 0.3274 508 281394 0.015 0.31 1.361 0.0196 0.1703 0.3493 509 281395 0.027 0.2d'w7 1.178 0.0291 0.1134 0.5419 510 281396 0.019 0212 1.717 0.0287 0.1822 0.5306 511 281397 0.011 0.178 1.509 0.0109 0.3764 0.1526 512 281398 0.044 0.057 0.149 0.0725 1.0065 2.0913 513 281399 <0.005 <0.0115 <0.01 <0.0001 <0.0001 <0.0001 514 281400 0.017 032 1326 0.0288 0.2845 0.5376 515 281400 0.015 0.3117 1.261 0.0268 0.2746 0.4991 516 281401 0.029 0.7411 +3.863 0.0539 8.408 0.8992 517 281402 0.008 0.863 0.349 0.1715 0.3098 3.2244 518 281403 <0.005 0242 0203 0.1693 0.6311 3.6407 4 of 7
519 281404 0.021 0.3 0.534 0.0296 2.1845 0.532 520 281405 0.01 0.198 0.294 0.1454 0.4146 1.5369 521 281406 0.036 0.194 0.546 0.0153 0.6226 0.2608 522 281407 0.019 0.107 0.436 0.019 0.3507 0.3537 523 281406 0.021 0.302 0.706 0.0467 0.212 0.8671 524 281409 0.018 0.052 0.189 0.0059 0.139 0.074 525 281409 0.017 0.066 0.213 0.0061 0.136 0.0725 526 281410 0.014 0.235 5.124 0.0411 0.1785 0.7973 527 281411 0.015 0.214 0.403 0.169 1.1367 3.3147 528 281412 0.007 0.266 0.243 0.1589 0.5453 3.5753 529 281413 0.009 0.229 0.289 0.1509 0.4257 3.272 530 281414 <0.005 0.253 0.854 0.1333 0.6886 3.427 531 281415 0.013 0.235 1.011 0.0472 0.3973 0.876 532 281416 0.229 0.176 0.79 0.0456 0.1635 0.8779 533 281417 0.017 0.094 0.181 0.012 0.1455 0.1758 534 281418 0.38 1.977 1.181 0.1758 1.2508 3.9756 535 281419 <0.005 <0.015 <0.01 <0.0001 <0.0001 <0.0001 536 281420 0.06 0.981 1.39 0.1807 1.1923 2.9903 537 281420 0.037 0.84 1.257 0.1814 1.2681 3.3529 538 284141 0.023 0.079 0.11 0.008 0.0243 0.0864 539 284142 0.024 0.111 0.209 0.0123 0.1619 0.1834 540 284143 0.034 0.084 0.125 0.0086 0.1194 0.099 541 284144 0.009 0.077 0.115 0.0094 0.0824 0.11 542 284145 0.01 0.085 0.142 0.0105 0.0529 0.1147 543 284146 0.041 0.087 0.175 0.008 0.0593 0.1108 544 284147 0.012 0.102 0.18 0.0118 0.0787 0.1757 545 284148 0.033 0.124 0.218 0.0119 0.1177 0.1846 546 284149 0.014 0.111 0.175 0.0105 0.084 0.1431 547 284149 0.017 0.101 0.172 0.0105 0.0835 0.144 548 284150 0.017 0.11 0.204 0.0125 0.1159 0.1745 549 284151 0.015 0.124 0.226 0.0133 0.1398 0.1831 550 284152 0.02 0.139 0.295 0.013 0.1335 0.1955 551 284153 0.025 0.131 0.317 0.0156 0.219 0.2467 552 284154 0.02 0.167 0.381 0.0169 0.2105 0.2786 553 284155 0.016 0.167 0.386 0.0171 0.2317 0.2807 554 284156 0.013 0.161 0.389 0.0175 0.1984 0.2869 555 284157 0.031 0.077 0.168 0.0123 0.2937 0.188 556 284158 0.113 0.746 0.362 0.019 0.5989 0.2699 557 284159 <0.005 <0.015 <0.01 <0.0001 <0.0001 <0.0001 558 284160 0.006 0.083 0.185 0.017 0.2443 0.2869 559 284160 <0.005 0.074 0.211 0.0161 0.2319 0.2691 560 284161 <0.005 0.015 0.043 0.0176 0.2553 0.283 561 284162 <0.005 <0.015 0.046 0.0129 0.1233 0.1965 562 284163 <0.005 0.02 0.055 0.0126 0.17 0.1973 563 284164 <0.005 0.104 0.286 0.0176 0.3346 0.3282 564 284165 <0.005 0.053 0.085 0.0165 0.3102 0.3267 565 284166 <0.005 0.08 0.214 0.0218 0.4789 0.3798 566 284167 <0.005 0.065 0.1 0.0188 0.374 0.3236 567 284168 0.009 0.167 0.517 0.0211 0.2721 0.3791 568 284169 <0.005 0.131 0.41 0.0226 0.1915 0.4337 569 284169 0.006 0.124 0.413 0.0237 0.1996 0.4608 570 284170 <0.005 0.057 0.126 0.0064 0.0216 0.0893 571 284171 <0.005 0.04 0.073 0.0064 0.0378 0.0762 572 284172 <0.005 0.019 0.032 0.009 0.0966 0.1174 573 284173 <0.005 0.059 0.157 0.013 0.2129 0.2152 574 284174 <0.005 0.118 0.322 0.0153 0.2877 0.2491 575 284175 <0.005 0.074 0.122 0.0078 0.0796 0.0966 576 284176 <0.005 0.036 0.079 0.008 0.0379 0.0792 577 284177 <0.005 0.037 0.053 0.0061 0.032 0.0616 578 284178 0.112 0.73 0.362 0.0175 0.5856 0.2695 579 284179 <0.005 <0.015 <0.01 0.0003 <0.0001 <0.0001 580 284180 <0.005 0.052 0.151 0.0128 0.2113 0.2388 581 284180 <0.005 0.053 0.144 0.0131 0.2108 0.2335 582 284181 <0.005 0.045 0.085 0.0064 0.0598 0.0751 583 284182 <0.005 0.071 0.11 0.0083 0.093 0.0991 584 284183 0.006 0.095 0.208 0.0098 0.1379 0.1603 585 284184 <0.005 0.056 0.109 0.0061 0.0486 0.0782 586 284185 0.009 0.046 0.144 0.0046 0.0086 0.0262 587 284186 <0.005 0.029 0.087 0.0061 0.0328 0.0471 588 284187 <0.005 0.033 0.069 0.0096 0.0661 0.1036 589 284188 <0.005 0.046 0.076 0.0088 0.0408 0.0826 590 284189 <0.005 0.079 0.181 0.0126 0.1242 0.1597 591 284189 0.005 0.082 0.157 0.0123 0.1171 0.1474 592 284190 0.007 0.07 0.157 0.0098 0.0994 0.1214 593 284191 0.01 0.058 0.113 0.0094 0.096 0.108 594 284192 0.012 0.082 0.174 0.0125 0.1412 0.1638 595 284193 0.01 0.113 0.437 0.0151 0.1901 0.2246 596 284194 0.015 0.131 0.247 0.0141 0.1584 0.2128 597 284195 0.011 0.106 0.308 0.0133 0.1845 0.2088 598 284196 0.006 0.07 0.221 0.0124 0.1489 0.1772 599 284197 <0.005 0.086 0.244 0.0108 0.1475 0.1604 600 284198 0.119 0.788 0.358 0.0173 0.5838 0.2672 5 of 7
601 284199 <0.005 <0.015 <0.01 <0.0001 <0.0001 <0.0001 602 284200 0.013 0.109 0.371 0.01 0.1305 0.153 603 284200 0.009 0.113 0.4 0.01 0.1327 0.153 604 284201 0.033 0.089 0.313 0.0061 0.0971 0.08 605 284202 0.009 0.05 0.123 0.0045 0.0341 0.0467 606 284203 0.025 0.149 0.369 0.0117 0.2443 0.1992 607 284204 0.015 0.138 0.439 0.0123 0.2731 0.2135 608 284205 0.014 0.18 0.547 0.0237 0.4648 0.4449 609 284206 0.018 0.262 0.822 0.0317 0.5487 0.5933 610 284207 0.011 0.188 0.738 0.0208 0.4092 0.3703 611 284208 0.015 0.171 0.503 0.0139 0.2492 0.2303 612 284209 0.006 0.174 0.627 0.0144 0.2545 0.2632 613 284209 0.005 0.149 0.658 0.014 0.2509 0.2619 614 284210 <0.005 0.044 0.118 0.0091 0.1289 0.1376 615 284211 0.038 0.062 0.166 0.0198 0.2664 0.2908 616 284212 0.005 0.049 0.172 0.0101 0.1923 0.1457 617 284213 0.012 0.137 0.523 0.0172 0.325 0.2962 618 284214 0.054 0.15 0.494 0.0142 0.3592 0.2875 619 284215 0.013 0.077 0.321 0.0107 0.2749 0.1911 620 284216 <0.005 0.057 0.132 0.0135 0.1167 0.1272 621 284217 0.009 0.023 0.05 0.0063 0.0494 0.0676 622 284218 0.054 0.111 0.146 0.0742 0.9959 2.076 623 284219 <0.005 <0.015 <0.01 <0.0001 <0.0001 <0.0001 624 284220 0.006 0.041 0.088 0.012 0.2345 0.202 625 284220 0.006 0.04 0.093 0.0119 0.2358 0.1996 626 284221 0.015 0.129 0.417 0.007 0.0475 0.0807 627 284222 0.012 0.048 0.162 0.008 0.0753 0.1112 628 284223 0.023 0.102 0.798 0.0113 0.0651 0.2085 629 284224 0.008 0.04 0.11 0.0093 0.0893 0.0755 630 284225 <0.005 0.027 0.055 0.0088 0.0606 0.0657 631 284226 0.009 0.06 0.193 0.0187 0.1889 0.1728 632 284227 0.011 0.069 0.189 0.0191 0.1607 0.1594 633 284228 0.009 <0.015 0.037 0.0044 0.0127 0.0295 634 284229 0.023 0.233 0.595 0.0092 0.1124 0.1503 635 284229 0.042 0.252 0.555 0.0089 0.113 0.1516 636 284230 0.023 0.113 0.364 0.0147 0.1827 0.2666 637 284231 0.03 0.123 0.448 0.0134 0.2367 0.2722 638 284232 0.025 0.169 0.577 0.018 0.2978 0.3761 639 284233 0.011 0.017 0.113 0.007 0.0188 0.1044 640 284234 0.013 0.069 0.152 0.0114 0.0562 0.1873 641 284235 0.01 0.057 0.151 0.0113 0.0301 0.1803 642 284236 0.018 0.131 0.383 0.015 0.1749 0.2637 643 284237 0.028 0.212 0.606 0.0186 0.3175 0.3675 644 284238 0.109 0.716 0.379 0.0184 0.5912 0.2718 645 284239 <0.005 <0.015 <0.01 <0.0001 <0.0001 <0.0001 646 284240 0.02 0.167 0.541 0.0187 0.3286 0.3836 647 284240 0.017 0.165 0.518 0.0194 0.3392 0.4017 648 284241 0.091 0.271 0.798 0.0285 0.4951 0.6186 649 284242 0.027 0.113 0.343 0.0386 0.2805 0.8602 650 284243 0.017 0.191 0.47 0.0214 0.4142 0.4567 651 284244 0.019 0.073 0.257 0.0158 0.3528 0.3003 652 284245 0.023 0.193 0.733 0.0245 0.3894 0.4932 653 284246 0.011 0.028 0.249 0.0322 0.335 0.6448 654 264247 0.022 0.21 0.591 0.0399 0.4437 0.8069 655 284248 0.011 0.063 0.199 0.0201 0.414 0.384 656 284249 0.02 0.118 0.651 0.0498 0.6784 0.9502 657 284249 0.021 0.142 0.589 0.0461 0.6553 0.9187 658 284250 0.008 0.161 0.535 0.0291 0.3363 0.5554 659 284251 0.007 0.162 0.531 0.0295 0.2613 0.5647 660 284252 0.021 0.166 0.774 0.0306 0.424 0.5924 661 284253 0.037 0.21 0.731 0.0282 0.4732 0.5362 662 284254 0.024 0.271 0.582 0.0471 0.6486 0.8232 663 284255 0.018 0.064 0.169 0.0078 0.0729 0.111 664 284256 0.014 0.025 0.079 0.0091 0.2923 0.1174 665 284257 0.006 0.059 0.142 0.0094 0.1229 0.1332 666 284258 0.045 0.098 0.137 0.0732 0.9953 2.094.4 667 284259 <0.005 <0.015 <0.01 <0.0001 <0.0001 <0.0001 668 284260 0.01 0.193 0.399 0.0516 0.7454 0.8923 669 284260 0.012 0.206 0.413 0.0505 0.7558 0.8599 670 285001 <0.005 <0.015 0.02 0.0039 0.0086 0.0248 671 285002 0.007 0.058 0.122 0.006 0.0828 0.0561 672 285003 0.011 0.151 0.376 0.013 0.1815 0.2022 673 285004 0.016 0.091 0.285 0.0114 0.2173 0.1741 674 285005 0.019 0.153 0.553 0.0219 0.5815 0.3962 675 285006 0.015 0.147 0.478 0.0182 0.9802 0.3655 676 285007 0.014 0.18 0.493 0.0166 0.3444 0.3237 677 285008 0.02 0.286 1.237 0.0199 0.4758 0.3993 678 285009 0.039 0.152 1.363 0.0384 0.2793 0.7652 679 285009 0.036 0.176 1.364 0.038 0.2717 0.7591 680 285010 0.031 0.27 2.639 0.0643 0.6997 1.2226 681 285011 0.031 0.043 2.851 0.0951 0.4261 1.6564 682 285012 0.018 0.233 1.574 0.0336 0.4828 0.6795 6 of 7
683 285013 0.015 0.081 0.309 0.0096 0.1668 0.1786 684 285014 0.058 0.058 0.153 0.0251 0.1427 0.4426 685 285015 0.018 0.187 0.353 0.0369 0.2929 0.7043 686 285016 Received 687 285017 0.054 0.091 0.15 0.0751 1.0038 2.0989 688 285018 <0.005 <0.015 <0.01 <0.0001 <0.0001 <0.0001 689 285019 Received 690 285019 Received 691 285020 0.019 0.027 0.041 0.0202 0.4065 0.3662 692 285021 2.303 0.146 1.501 0.018 0.1791 0.3197 693 285022 0.01 0.062 0.526 0.0423 0.3604 0.7239 694 285023 0.066 0.091 1.314 0.0268 0.1519 0.4755 695 285024 0.388 0.307 0.747 0.0348 0.3412 0.6186 696 285025 0.316 0.766 1.101 0.0467 0.4981 0.8838 697 285026 1.974 0.204 0.519 0.0285 0.2219 0.5408 698 285027 0.188 0.192 0.826 0.0312 0.4351 0.5882 699 285028 0.139 0.113 0.794 0.0207 0.2729 0.3953 700 285029 0.039 0.121 0.77 0.0297 0.2554 0.5445 701 285029 0.076 0.087 0.711 0.027 0.2445 0.5197 702 285030 0.084 0.618 1.262 0.0379 0.2723 0.7133 703 285031 0.022 0.212 1.139 0.0255 0.2301 0.443 704 265032 0.01 0.1 0.295 0.0147 0.1648 0.2477 705 285033 0.017 0.145 0.535 0.0158 0.242 0.2632 706 285034 0.016 0.143 1.714 0.0211 0.7858 0.3709 707 285035 0.011 0.087 0.221 0.0176 0.218 0.2855 708 285036 0.006 0.062 0.279 0.0219 0.246 0.3608 709 285037 0.046 0.08 0.15 0.0252 0.3297 0.4172 710 285038 <0.005 <0.015 <0.01 <0.0001 <0.0001 <0.0001 711 285039 0.016 0.226 0.823 0.0268 0.3519 0.4361 712 285039 0.041 0.241 0.797 0.0262 0.3433 0.4248 713 285040 0.013 0.157 0.994 0.0228 0.3088 0.3844 714 285041 0.017 0.192 0.75 0.027 0.4484 0.4435 715 285042 0.037 0.132 0.47 0.0308 0.469 0.4928 716 285043 0.01 0.057 0.459 0.0417 1.7407 0.6634 717 265044 0.013 0.029 0.096 0.0148 1.3379 0.1703 718 285045 0.015 0.061 0.086 0.0102 0.4966 0.1208 719 285046 0.009 0.103 0.272 0.0219 0.7344 0.3764 720 285047 0.007 0.048 0.214 0.0224 2.9227 0.3888 721 285048 0.041 0.028 <0.01 0.0117 0.0139 0.1234 722 285049 <0.005 0.054 0.034 0.0116 0.0278 0.1164 723 285049 <0.005 0.04 0.024 0.0117 0.0271 0.1168 724 285050 <0.005 0.021 <0.01 0.0106 0.0037 0.11 725 285051 <0.005 0.022 <0.01 0.0057 0.0281 0.0075 726 285052 <0.005 0.04 0.09 0.0213 0.1391 0.1436 727 285053 0.006 0.053 0.112 0.0147 0.0665 0.2121 728 285054 Received 729 285055 Received 730 285056 <0.005 0.02 0.015 0.0018 0.0033 0.0082 731 285057 0.054 0.107 0.141 0.0674 1.0032 2.1017 732 285058 <0.005 <0.015 <0.01 <0.0001 <0.0001 <0.0001 733 285059 <0.005 0.034 0.076 0.012 0.1976 0.0973 734 285059 <0.005 0.037 0.082 0.0137 0.2227 0.1093 735 285501 <0.005 <0.015 0.028 0.0088 0.0684 0.0535 736 285502 0.026 0.199 0.133 0.0224 0.1627 0.1365 737 285503 0.01 0.126 0.136 0.0115 0.0623 0.0583 738 285504 <0.005 0.024 0.113 0.0145 0.1068 0.1475 739 285505 <0.005 <0.015 <0.01 0.009 0.0022 0.0496 740 285506 <0.005 0.062 0.2 0.0137 0.0437 0.1136 741 285507 <0.005 0.987 0.458 0.0478 0.1878 0.8523 742 285508 0.021 1.754 2.34 0.2102 0.8898 3.0056 743 285509 0.029 0.606 0.985 0.094 0.6247 1.2891 744 285509 <0.005 0.615 1.035 0.0993 0.6699 1.3338 745 285510 0.344 1.092 3.027 0.1229 1.3604 2.405 746 285511 0.013 0.78 0.828 0.0219 0.3743 0.3228 747 285512 0.019 0.177 0.748 0.0655 0.8063 1.5081 748 285513 0.012 <0.015 <0.01 0.0091 0.0183 0.0343 749 285514 <0.005 0.217 0,374 0.0123 0.2042 0.1735 750 285515 0.015 0.241 1.103 0.0233 0.5395 0.2818 751 285516 <0.005 0.143 0.563 0.0161 0.2276 0.1804 752 285517 0.035 0.34 0.978 0.0205 0.5633 0.3452 753 285518 0.018 <0.015 <0.01 0.0548 0.2229 0.1795 754 285519 0.014 <0.015 <0.01 0.045 0.134 0.1365 755 285519 0.014 <0.015 0.021 0.0468 0.1357 0.1382 756 285520 0.038 0.223 0.177 0.047 0.1469 0.131 757 289003 <0.005 0.046 0.155 0.0101 0.0649 0.1098 758 289004 <0.005 <0.015 <0.01 <0.0001 <0.0001 <0.0001 759 289005 0.103 0.741 0.386 0.0205 0.591 0.2736 760 289006 <0.005 0.084 0.042 0.0075 0.0029 0.0405 761 289007 0.112 0.752 0.37 0.0209 0.5868 0.2732 762 289008 <0.005 <0.015 <0.01 <0.0001 <0.0001 <0.0001 763 289009 <0.005 0.029 0.041 0.0103 0.0124 0.0772 764 289010 0.109 0.775 0.388 0.0203 0.604 0.2749 7 of 7
765 289011 Sample 766 289012 <0.005 0.04 0.063 0.0115 0.0178 0.0854 767 289012 <0.005 0.049 0.064 0.0116 0.0176 0.0848 768 289013 0.094 0.724 0.353 0.0234 0.5909 0.2704 769 289014 <0.005 <0.015 <0.01 <0.0001 <0.0001 <0.0001 770 289015 0.014 0.099 0.342 0.0129 0.063 0.1227 771 289016 0.113 0.731 0.39 0.0227 0.5853 0.2666 772 289017 <0.005 <0.015 <0.01 <0.0001 <0.0001 <0.0001 773 289018 0.088 0.73 0.369 0.0222 0.5895 0.2737 774 289019 <0.005 <0.015 <0.01 <0.0001 <0.0001 <0.0001 775 289020 0.106 0.688 0.389 0.0219 0.5926 0.266 776 289021 <0.005 <0.015 <0.01 <0.0001 <0.0001 <0.0001 777 289021 Sample 1 of 4
Galdbrook Ventures Inc. Date Created: 07-10-03 11:43:32 AM Job Number: 200720008 Date Received: Aug 10, 2007 Number of Samples: 260 Type of Sample: Core Date Completed: Oct 3, 2007 Project ID:
Acc fJ Client ID Au ppb Pt ppb Pd ppb Rh ppb Ag ppm Co ppm Cu ppm Fe ppm Ni ppm Pb ppm Zn ppm 5DL 15DL 10 DL 5DL 1449 284531 7 62 114 94 654 1587 1450 284532 10 72 328 95 1474 1643 1451 284533 5 54 80 112 1841 1968 1452 284534 157 153 284 113 3156 1903 1453 284535 9 130 196 101 1283 1383 1454 284536 18 186 386 124 2190 2178 1455 284537 9 102 175 108 1735 1887 1456 284538 7 184 347 125 2425 1963 1457 284539 9 62 314 77 1152 1265 1458 284540 8 65 307 224 1604 4523 1459 284540 6 62 327 230 1625 4715 1460 284541 <5 37 19 35 201 88 1461 284542 6 49 22 34 62 23 1462 284543 <5 61 46 73 321 763 1463 284544 <5 52 54 74 264 729 1464 284545 <5 58 51 69 276 661 1465 284546 <5 68 82 78 584 800 1466 284547 <5 54 83 73 530 861 1467 284548 109 729 382 199 5876 2715 1468 284549 <5 <15 <10 <1 <1 <1 1469 284550 8 136 123 84 599 1010 1470 284550 <5 108 113 78 583 923 1471 284551 <5 88 114 96 926 1113 1472 284552 10 119 159 96 1083 1252 1473 284553 6 129 231 112 1408 1529 1474 284554 9 113 232 103 1441 1405 1475 284555 11 156 311 106 1910 1734 1476 284556 14 134 246 84 1587 1780 1477 284557 9 87 171 104 1941 2306 1478 284558 9 90 180 77 376 1270 1479 284559 8 77 130 103 885 1697 1480 284560 20 87 183 96 1162 1407 1481 284560 6 41 82 100 1333 1468 1482 284561 15 281 519 174 4234 3310 1483 284562 25 312 843 229 5721 4637 1484 284563 43 249 479 260 1768 5024 1485 284564 5 23 <10 60 543 634 1486 284565 31 157 450 93 1157 2225 1487 284566 30 213 512 140 3399 3217 1488 284567 17 134 371 132 2773 2932 1489 284568 26 219 788 245 807 14683 1490 284569 <5 <15 <10 <1 <1 <1 1491 284570 38 224 545 154 3682 3604 1492 284570 16 197 580 156 3744 3748 1493 284571 16 57 140 141 3158 3173 1494 284572 23 95 173 193 4348 4704 1495 284573 259 52 78 224 4622 5573 1496 284574 36 342 898 41 290 460 1497 284575 <5 108 261 63 1176 1019 1498 284576 13 75 218 57 681 880 1499 284577 69 310 131 94 1413 2147 1500 284578 <5 24 <10 121 2495 1871 1501 284579 16 115 264 117 2368 2334 1502 284580 14 80 137 76 1371 1325 1503 284580 24 76 105 83 1530 1499 1504 284581 23 70 129 58 743 829 1505 284582 51 112 258 76 1328 1525 1506 284583 23 91 181 72 1060 1352 1507 284584 13 81 112 76 516 868 1508 284585 26 104 173 96 1437 1603 1509 284586 38 175 414 150 2210 1388 1510 284587 8 119 270 146 2564 2955 1511 284588 199 5876 2716 1512 284589 <5 <15 <10 <1 <1 <1 1513 284590 28 159 251 147 1156 2902 1514 284590 16 163 248 139 1238 2776 1515 284591 16 219 392 161 2917 3457 1516 284592 26 255 591 164 3186 3553 1517 284593 22 287 692 207 4670 1917 1518 284594 20 480 1423 222 4609 5376 1519 284595 20 364 882 215 1993 5090 2 of 4
1520 284596 13 197 449 167 2813 4021 1521 284597 9 277 634 213 3975 5621 1522 284598 172 214 660 152 <1 3520 1523 284599 25 267 687 195 4246 4659 1524 284600 99 155 794 164 4559 4116 1525 284600 148 180 781 195 4317 3749 1526 284601 18 210 507 217 8031 5408 1527 284602 24 179 798 252 4952 6392 1528 284603 30 317 630 456 6225 12235 1529 284604 40 440 831 668 15527 16744 1530 284605 17 205 818 323 3998 8097 1531 284606 9 159 358 513 2338 12174 1532 284607 15 256 547 472 2489 12898 1533 284608 314 1903 1090 1714 12560 36522 1534 284609 <5 <15 <10 <1 <1 <1 1535 284610 21 296 407 535 2405 8275 1536 284610 11 130 188 563 2571 8311 1537 284611 31 377 630 286 5844 6745 1538 284612 15 235 1788 245 1991 5312 1539 284613 <5 65 308 153 862 2731 1540 284614 <5 26 <10 91 95 954 1541 284615 9 16 <10 94 51 997 1542 284616 6 22 <10 93 26 887 1543 284617 <5 34 <10 85 27 856 1544 284618 8 41 <10 98 38 982 1545 284619 <5 49 <10 98 88 966 1546 284620 10 30 136 79 387 968 1547 284620 6 27 134 81 403 1026 1548 284621 49 133 546 157 1679 2409 1549 284622 12 104 384 194 2088 3569 1550 284623 12 179 684 175 1414 2948 1551 284624 14 773 580 295 3258 5478 1552 284625 6 69 71 84 534 1208 1553 284626 <5 <15 <10 103 908 1532 1554 284627 25 282 119 125 885 1870 1555 284628 111 739 377 195 5893 2701 1556 284629 <5 <15 <10 <1 <1 <1 1557 284630 <5 <15 43 57 427 1178 1558 284630 <5 <15 54 84 417 1155 1559 285120 12 91 272 140 3027 2053 1560 285121 <5 26 31 98 1451 1298 1561 285122 5 56 35 62 545 646 1562 285123 13 129 283 150 1264 2416 1563 285124 8 158 321 73 404 963 1564 285125 <5 26 60 79 257 901 1565 285126 5 70 117 81 441 1036 1566 285127 6 39 139 BO 1012 1209 1567 285128 <5 <15 61 108 1786 2015 1568 285129 <5 15 106 77 784 846 1569 285129 <5 24 135 72 755 809 1570 285130 <5 <15 125 62 219 599 1571 285131 <5 <15 41 118 1200 2409 1572 285132 6 41 103 109 1408 2086 1573 285133 <5 125 609 139 2615 2681 1574 285134 7 117 574 177 2631 3398 1575 285135 9 155 538 227 4221 4533 1576 285136 <5 68 306 183 1958 3582 1577 285137 12 120 453 216 2697 4254 1578 285138 120 721 378 193 5876 2698 1579 285139 <5 <15 <10 <1 <1 <1 1580 285140 9 120 362 275 2972 5434 1581 285140 <5 92 347 279 2993 5505 1582 285251 <5 <15 <10 49 170 104 1583 285252 <5 <15 <10 55 103 94 1584 285253 <5 <15 <10 60 125 91 1585 285254 <5 <15 <10 56 112 67 1586 285255 <5 <15 <10 57 529 38 1587 285256 <5 <15 13 62 449 26 1588 285257 <5 <15 <10 54 257 19 1589 285258 <5 <15 <10 43 152 22 1590 285259 <5 <15 <10 37 112 38 1591 285260 <5 <15 <10 48 34 66 1592 285260 <5 <15 <10 45 32 61 1593 285261 <5 <15 12 55 164 51 1594 285262 8 <15 <10 55 464 34 1595 285263 28 318 1648 207 6487 2529 1596 285264 7 70 375 225 2662 3461 1597 285265 14 144 606 266 8496 3941 1598 285266 <5 41 328 104 2075 1080 1599 285267 <5 125 186 269 902 14390 1600 285268 <5 <15 <10 <1 <1 <1 1601 285269 19 60 255 118 1776 1454 3 of 4
1602 285741 15 45 37 54 133 414 1603 285742 <5 135 499 169 3962 3619 1604 285743 15 184 417 147 2633 3630 1605 285744 22 202 639 189 3402 4281 1606 285745 15 135 444 136 2762 2457 1607 285746 24 352 1035 188 4410 4851 1608 285747 12 127 431 144 2810 3069 1609 285748 7 70 251 90 1418 1417 1610 285749 15 103 173 96 1150 1416 1611 285750 8 69 114 106 1187 1312 1612 285750 12 43 101 94 1095 1199 1613 285751 10 100 203 118 1126 1506 1614 285752 13 106 230 108 1380 1550 1615 285753 8 62 146 84 1011 1315 1616 285754 14 102 139 59 712 791 1617 285755 10 104 127 78 733 1009 1618 285756 19 160 329 102 1756 1874 1619 285757 73 537 278 83 955 1263 1620 285758 106 735 390 195 5862 2692 1621 285759 <5 <15 <10 <1 <1 <1 1622 285760 31 298 177 76 734 1120 1623 285760 14 127 185 80 762 1164 1624 285761 <5 124 243 78 935 1317 1625 285762 9 170 460 114 2223 2532 1626 285763 15 142 247 89 1322 1753 1627 285764 10 98 202 114 1094 1675 1628 285765 <5 <15 15 126 1185 2204 1629 285766 31 139 361 170 3500 2837 1630 285767 24 126 330 104 1730 1701 1631 285768 35 216 545 181 7649 3205 1632 285769 38 138 417 187 4491 3734 1633 285770 23 93 198 105 1418 1645 1634 285770 69 57 181 97 1334 1565 1635 285771 26 377 574 140 1957 2861 1636 285772 <5 <15 94 78 630 1381 1637 285773 51 318 1724 128 3514 3028 1638 285774 <5 57 269 150 3063 3071 1639 285775 8 86 267 106 1394 1779 1640 285776 <5 <15 57 42 282 340 1641 285777 9 39 106 46 667 480 1642 285778 115 732 381 194 5879 2717 1643 285779 <5 <15 <10 <1 <1 <1 1644 285780 9 69 72 37 187 270 1645 285780 15 52 66 40 203 308 1646 287001 17 26 115 83 466 699 1647 287002 15 <15 123 77 66 655 1648 287003 <5 58 193 85 1003 1293 1649 287004 10 101 266 109 1780 1387 1650 287005 14 143 315 115 1626 2000 1651 287006 22 150 269 111 1472 1763 1652 287007 19 83 337 113 1328 2180 1653 287008 18 185 501 120 2440 2558 1654 287009 15 124 378 155 3860 3918 1655 287010 14 233 731 180 3816 3850 1656 287010 22 286 661 167 3590 3631 1657 287011 8 27 116 59 701 1027 1658 287012 29 176 672 113 2361 3666 1659 287013 12 236 813 144 3143 3951 1660 287014 6 66 310 115 1786 2525 1661 287015 5 67 355 101 1489 2116 1662 287016 7 151 504 167 3883 4058 1663 287017 6 160 623 181 3869 4368 1664 287018 124 206 299 229 783 14318 1665 287019 <5 <15 <10 <1 <1 <1 1666 287020 <5 162 603 173 3860 3973 1667 287020 12 159 667 182 4072 4232 1668 287021 <5 174 563 181 3380 4377 1669 287022 18 163 386 131 1470 3008 1670 287023 6 212 456 136 3106 2919 1671 287024 21 269 912 194 4988 5070 1672 287025 17 231 751 155 3840 4060 1673 287026 29 91 313 193 1649 5360 1674 287027 11 120 413 175 4360 4467 1675 287028 22 130 525 179 3153 4430 1676 287029 10 225 788 158 2640 3422 1677 287030 30 203 820 141 2884 2718 1678 287030 11 236 714 149 2932 3082 1679 287031 15 25 41 43 297 250 1680 287032 <5 91 79 106 1534 1723 1681 287033 <5 104 149 113 1909 2121 1682 287034 <5 83 122 130 2650 2674 1683 287035 11 167 380 146 2985 2937 4 of 4
1684 287036 8 210 577 149 3187 3335 1685 287037 14 275 561 159 3516 3627 1686 287038 245 816 14081 1687 287039 <5 <15 <10 <1 <1 <1 1688 287040 21 248 555 143 3239 3205 1689 287041 <5 57 72 51 430 544 1690 287041 <5 60 86 50 415 519 1691 287042 <5 51 77 48 1104 786 1692 287043 19 153 288 63 6800 1402 1693 287044 <5 68 49 39 2750 627 1694 287045 8 154 1122 138 2581 2443 1695 287046 10 299 531 319 7875 7722 1696 287047 <5 267 899 203 1465 5468 1697 287048 6 271 665 206 3875 4914 1698 287049 33 272 701 202 3636 3534 1699 287050 30 274 1080 227 3402 5485 1700 287051 <5 181 548 191 2998 3963 1701 287051 <5 211 483 202 3167 4130 1702 287052 11 180 537 177 2984 3646 1703 287053 8 210 600 219 3946 4861 1704 287054 <5 171 516 194 2170 3950 1705 287055 270 859 13976 1706 287056 <5 <15 <10 <1 <1 <1 1707 287057 6 128 668 207 2242 4232 1708 287058 14 65 233 130 2231 2143 1709 287059 76 42 145 42 151 833 1710 287060 13 102 503 172 2036 3278 1711 288001 <5 19 165 80 884 1185 1712 288002 19 72 249 101 1440 1659 1713 288003 59 34 108 93 1137 1405 1714 288004 6 99 303 113 1737 2062 1715 288005 21 116 297 96 1625 1692 1716 288006 18 87 291 93 1746 1710 1717 288007 9 101 305 113 1656 2003 1718 288008 12 77 263 109 1249 1718 1719 288009 23 68 300 121 1607 1575 1720 288010 16 112 313 123 1617 1956 1721 288010 23 132 317 123 1643 1954 1722 288011 10 76 190 81 1032 1247 1723 288012 16 138 311 114 1479 1952 1724 288013 19 130 400 137 2043 2787 1725 288014 24 131 392 142 2294 2749 1726 288015 51 242 811 113 1734 1933 1727 288016 98 446 248 134 2307 2338 1728 288017 <5 34 12 142 4284 2233 1729 288018 Sample 1730 288019 <5 <15 <10 <1 <1 <1 1731 288020 31 146 313 121 1982 2159 1732 288020 40 43 107 119 1913 1741 GOLDBROOK VENTURES INC. Geological Mapping & Prospecting 2007
16. APPENDIX 5
September 14, 2007 News Release
88 GOLDBROOK ventures Explore • Discover • Prosper Nickel, copper and platinum group metals unearthed
Not for Distribution to U.S. Newswire Services or for Dissemination in the United States For Immediate Release September 14, 2007 Trading Symbol: GBK - TSX-V
NEWS RELEASE
Goldbrook Reports Massive Nickel Sulfides on Surface
Vancouver, British Columbia - Goldbrook Ventures Inc ("Goldbrook") is pleased to release partial assay results for grab samples from its nickel sulfide exploration project in the Raglan District, Northern Quebec. The samples were collected as part of Goldbrook's 2007 exploration program on 100% owned Belanger and Bravo claim blocks in the south-central part of Raglan. The $15 million exploration program is discovering new nickel sulfide zones and developing nickel-copper PGE sulfide resources for future mining along the highly mineralized Belanger-Delta Horizon.
The assay results for mineralized grab samples from ten surface showings are presented in Table 1 and described below. The locations of the showings are represented in Figure 1, available for viewing on the Goldbrook website www.goldbrookventures.com/en/tables and diagrams
Table 1. Best assay results for grab samples from the Belanger-Delta Horizon
Sample Target Ni % Cu % Co % Pt (gpt) Pd (gpt) Au (gpt) PtPdAu 285515 Bravo B4 0.28 0.54 0.02 0.241 1.103 0.015 1.359 285517 Bravo B4 0.35 0.56 0.02 0.340 0.978 0.035 1.353 280011 Bravo B6 0.22 0.56 0.02 0.356 1.276 0.030 1.662 280010 Bravo B8 1.80 0.21 0.13 0.413 0.419 0.120 0.952 280009 Bravo B9 0.96 0.13 0.11 2.938 1.832 0.077 4.847 285507 Bravo B9 0.85 0.19 0.05 0.987 0.458 <0.005 1.445 285508 Bravo B9 3.01 0.89 0.21 1.754 2.340 0.021 4.115 285509 Bravo B9 1.31 0.65 0.10 0.611 1.010 0.029 1.650 285510 Bravo B9 2.41 1.36 0.12 1.092 3.027 0.344 4.463 280506 Echo 0.49 1.71 0.06 0.026 0.093 <0.005 0.119 280505 Echo 0.41 1.48 0.05 0.112 0.163 0.010 0.285 280007 Echo 0.11 0.74 0.01 0.421 1.361 0.026 1.808 280008 Echo 0.18 2.28 0.04 0.188 1.072 0.068 1.328 280521 McCart Island 0.58 0.40 0.03 0.354 0.547 0.013 0.914 280522 McCart Island 0.50 0.43 0.02 0.229 0.403 0.026 0.658 280508 Peter's Rock 0.08 15.53 0.00 0.789 26.722 11.673 39.184 280501 R2 0.98 0.33 0.04 0.027 0.010 <0.005 0.037 280502 Timtu 0.95 0.32 0.04 0.564 2.772 0.062 3.398 280504 Timtu 0.89 0.52 0.04 0.583 3.814 0.067 4.464 280001 Timtu 0.80 0.26 0.05 0.268 1.989 0.007 2.264 280503 Timtu 0.15 0.79 0.01 0.601 2.436 0.061 3.098 Page 2
BRAVO CLAIM BLOCK
The best nickel assay results were returned by samples from the area of the Bravo complex, in the west-central part of Bravo claim block, which was acquired recently from Novawest and Cascadia (see press releases dated June 20, 2007 and August 17, 2007). The highest copper assays reported are for samples from the Echo complex, located 5 km west of Bravo. Bravo and Echo are two large mafic-ultramafic complexes with many geophysical anomalies and nickel sulfide showings. The highest platinum- palladium and gold assay results were determined for a sample from Peter's Rock, located 9 km northeast of the historic Delta deposit. The assay results are described below.
Bravo-B9. The B9 showings are located in the east part of the Bravo complex, 8 km west of the historic Delta nickel-copper PGE deposit. Assays of massive, semi-massive, net-textured and blebby sulfide bearing pyroxenite returned results of up to 3.01% nickel, 0.89% copper, 0.21% cobalt, 1.75 grams per tonne platinum, and 2.34 grams per tonne palladium (Table 1). Results of a 15 line-km deep-penetrating ground electromagnetic (SQUID) survey are pending.
Bravo-B8. The B8 showing is located 200 metres southwest of B9. Assays of massive and semi- massive sulfide bearing olivine pyroxenite returned results of up to 1.80% nickel, 0.21% copper, 0.13% cobalt, and 0.95 grams per tonne PGE. Results of a 15 line-km deep- penetrating ground electromagnetic (SQUID) survey are pending.
Bravo-B6. The B6 showing is located 1 km southwest of B8. Assays of a sample of ultramafic gossan with disseminated sulfides returned results of 0.56% copper, 0.36 grams per tonne platinum and 1.28 grams per tonne palladium.
Bravo-B4. The B4 showings are located 1 km west of B6, in an area of a very strong airborne electromagnetic (VTEM) anomaly. Assays of samples of pyroxenite with disseminated sulfides returned results of up to 0.35% nickel, 0.56% copper, and 1.35 grams per tonne PGE.
McCart Island. The McCart Island showing is located 2 km southwest along strike of B4 on the Bravo claim block. The McCart ultramafics are part of the Bravo complex. Prospecting found frost heaved ultramafic rocks hosting weak disseminated and patchy nickel sulfide mineralization. Assays of a single sample returned results of 0.58% nickel, 0.40% copper, and 0.91 grams per tonne PGE.
Echo-El. The E-1 showing is located 3 km west of McCart Island, along the highly mineralized south contact of the Echo complex. The highest assays for two samples of net-textured sulfide bearing ultramafic rocks are 0.49% nickel, 1.71% copper and 0.06% cobalt. Page 3
Peter's Rock. Peter's Rock is located 9 km along strike to the east of the B9 showing (described above), east along strike of the Delta deposit. A sample of copper-stained pegmatitic gabbro boulder returned assay results of 15.5% copper, 0.789 grams per tonne platinum, 26.7 grams per tonne palladium, and 11.7 grams per tonne gold. These assays of greater than an ounce per tonne precious metals are the highest recorded to date for samples from the extensive Goldbrook's claim holdings in the Raglan District. Their significance for drill testing is currently under investigation.
BELANGER CLAIM BLOCK
The Belanger claim block includes the Getty and Sylvie mineralized zones, which are currently being drilled to NI43-101 compliant resource categories. Assay results are reported below for the Echo West, Timtu and R2 showings.
Echo West. The Echo west showing is located 3.2 km southwest along strike of Echo E 1. Assays of gabbro samples with net-textured, blebby and fracture controlled mineralization returned results of up to 2.28% copper and 1.33 grams per tonne PGE.
Timtu. The Timtu showing is located 3.7 km southwest along strike of Echo West. Timtu consists of a 150 metre by 80 metre size area of boulders of ultramafic rock with net-textured and disseminated mineralization. Assays for four samples of ultramafic rock with net-textured mineralization (Table 1) returned results of up to 0.95% nickel, 0.32% copper, 0.56 grams per tonne platinum, and 2.77 grams per tonne palladium. Assays of another sample returned results of 4.46 grams per tonne PGE. A third sample returned assay results of 0.79% copper and 3.10 grams per tonne PGE. Previous drilling (see Press Release February 27, 2007) below the Timtu showing intersected distinctive breccia style nickel-copper-PGE sulfide mineralization.
R2. The R2 showing is located 4.4 km southeast of Timtu, on the Belanger claim block Prospecting revealed a large amount of boulders of mineralized ultramafic rock. A sample of frost heaved mafic-ultramafic rock with disseminated sulfide mineralization returned assays of 0.98% nickel, 0.33% copper, and 0.04% cobalt (Table 1). Assay results for additional samples are pending.
SIGNIFICANCE
The assay results for the ten showings confirm that the Belanger-Delta Horizon is mineralized on surface along a strike length of at least 30 km from Peter's Rock in the east to the Getty and Sylvie mineralized zones in the west. The high Ni/Cu ratios at Bravo-B8 and Bravo-B9 could reflect proximity to a major magmatic conduit system at depth. The very strong electromagnetic VTEM anomaly at Bravo-B4 indicates the presence of strong conductors, under cover at depth. Additional assay results for surface grab samples and for core samples are pending. Goldbrook intends to drill many of the showings in 2007 as part of an ongoing 25,000 metre drill program with five diamond drill rigs. Drilling is expected to continue during the 2008 drill program. Page 4
ANALYSES
The grab samples were assayed by Accurassay Laboratories, Thunder Bay (Ontario). Accurassay is accredited by the Standards Council of Canada to ISO-IEC 17025 standards for the analyses of base metals, platinum and palladium. Assay results for nickel, copper and cobalt are determined by aqua regia digest followed by Atomic absorption analysis. Assay results for platinum, palladium and gold are determined by lead fire assay followed by Atomic absorption analysis. In addition to quality control by Accurassay, Goldbrook regularly inserts blind Certified Reference Materials (standards), blanks and sample duplicates into sample batches for independent verification.
Dr Bill Stone, P.Geo., Senior Vice President of Exploration and Development for Goldbrook Ventures is the qualified person responsible for the technical content of this press release.
ON BEHALF OF THE BOARD:
(signed) "David Baker," President
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