Embed Size (px)
Citation preview
GITENNES EXPLORATION INC.
ASSESSMENT WORK REPORTon the
SEPTEMBER 2002 EXPLORATION PROGRAMMEfor the
BADGER PROPERTY
GARDEN-OBONGA AREA
District of Thunder Bay, Ontario NTS 52H/5, 52H6, 52H11, 52H/12
James R. Foster, H.B.Se., P.Geo.
April 9, 2003
52H11SW2004 2.25432 KITCHEN LAKE 010
SUMMARY C?* T .&J -
Gitennes Exploration Inc. acquired the Badger Property in the Garden-Obonga area of northwestern Ontario
for its potential to host platinum-group element mineralization and diamondiferous kimberlites. The property
consists of 19 contiguous unpatented mining claims totalling 241 units, located 150 road-kilometres north of
Thunder Bay, Ontario. The claims are held in the name of Gitennes Exploration Inc., pursuant to the terms of an
option agreement between Gitennes and Mr. Robert Fairservice. Access is by a logging road originating at Highway 811.
The Badger Property and its immediate surroundings are covered by extensive glaciofluvial deposits of the
Kaiashk Interlobate Moraine' Bedrock exposures are diabase, and foliated to gneissic felsic intrusives. No
mineralization is known to occur on or nearby the property.
Geochemical data released under the Operation Treasure Hunt programme of the Ontario Geological
Survey led to the staking of the Badger Property, to cover a lake sediment sample of 73.3 ppb Pd. The OGS also
identified diamond targets in the Garden - Obonga survey area by Keating Correlation Coefficient modelling of
airborne magnetic data. Gitennes evaluated a number of these on the Badger Property, the most significant being
the Black Hole target.
In June 2002, Gitennes carried out exploration comprising geological mapping and geochemical (MMI-B
and MMI-D) sampling. Linecutting and geophysical surveying on the Badger Grid followed in July, with till/stream
sediment sampling and grid-based MMI-D sampling in September. This work was initially designed to search for
a source for the 73.3 ppb Pd anomaly; however the MMI-B sampling did not outline a Pd anomaly in soil that could
point to a bedrock source. Magnetic surveying on the Badger Grid covered a large positive magnetic signature
which hosts a small strongly negative Keating anomaly. The positive feature thought to be related to the
anomalous lake sediment sample. Ground magnetics showed the Keating anomaly was related to a very strong
negative anomaly, the Black Hole, which has a magnetic signature similar to that of known kimberlites elsewhere
in Canada.
This report describes an exploration programme comprising MMI-D soil sampling, till and stream sediment
sampling and magnetometer surveying undertaken by Gitennes in September 2002. MMI-D results suggest a
geochemical signature comprising depletion of Mg and Rb and weak enrichment in Ti and Nb is directly
associated with the Black Hole. Although there is no outcrop in the area, the geochemical anomalies are believed
to be the result of significant change in bedrock, such that the Black Hole may represent the result of intrusion of a
small discrete igneous body which may be kimberlite. Based on this supposition, Gitennes evaluated other
negative Keating anomalies on the property for magnetic and geochemical characteristics similar to the Black
Hole. Their geochemical signatures are less easily characterized, as a result of complex magnetic signatures or
incomplete magnetic and geochemical coverage. However, they bear some similarities to the geochemical
response of the Black Hole.
Till and stream sediment samples did not detect any unequivocal indicator mineral trains. This could be due
to the complex glacial history of the area, and the lack of suitable sampling medium for this kind of work.
A drill programme comprising two core holes is recommended for testing the Black Hole target.
TABLE of CONTENTS
Page SUMMARY...................................................................................................................................................................!INTRODUCTION AND TERMS OF REFERENCE................................................................................................. 1 -PROPERTY DESCRIPTION AND LOCATION .....................................................................................................- 1 .ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND PHYSIOGRAPHY ................... - 2 -HISTORY...............................................................................................................................................................^-REGIONAL GEOLOGY..........................................................................................................................................3-LOCAL GEOLOGY.................................................................................................................................................4-PROPERTY GEOLOGY.........................................................................................................................................5-DEPOSITTYPES..................................................................................................................................................-6-MINERALIZATION............................................................................................................................................EXPLORATION.....................................................................................................................................................-?-RESULTS OF SURVEYS.......................................................................................................................................8-
Black Hole MMI Sampling ........................................................................,..... r ,.,.....,a .....^:-...:-:J.....................-9 -Anomaly 13470B .....................................................................^....... ...:.,.:..........-..l......^....:::...................- 11 -Anomaly 13500A ......................................................................^............^.....V............................................. 12-Till and Stream Sediment Sampling.............................................................................................................- 13 -.
SAMPLING METHODS AND APPROACH.......................................................................................................... 13-SAMPLE PREPARATION, ANALYSES AND SECURITY.................................................................................... 14-DATA VERIFICATION.......................................................................................................................................... 15-INTERPRETATION AND CONCLUSIONS .........................................................................................................- 15 -REFERENCES..................................................................................................................................................... 17-CERTIFICATE of QUALIFIED PERSON.............................................................................................................. 18 -
LIST of FIGURESFigure 1: Badger Property Location Map Following Page 18Figure 2: Badger Property Claim Map Following Page 18Figure 3: Operation Treasure Hunt Total Field Magnetics Following Page 18Figure 4: Regional Geology - Thunder Bay South Mining Division Following Page 18Figure 5: Badger Property Geology Following Page 18Figure 6: Badger Grid Contoured Ground Magnetics Following Page 18Figure 7: Black Hole Anomaly Contoured MMI Mg (ppb) + Contoured Ground Magnetics Following Page 18Figure 8: Black Hole Anomaly: Contoured MMI Rb (ppb) + Contoured Ground Magnetics Following Page 18Figure 9: Black Hole Anomaly: MMI Ti (ppb) + Contoured Ground Magnetics Following Page 18Figure 10: Black Hole Anomaly: MMI Ni (ppb) + Contoured Ground Magnetics Following Page 18Figure 11: Black Hole Anomaly: MMI Cr (ppb) * Contoured Ground Magnetics Following Page 18Figure 12: Black Hole Anomaly: MMI Nb (ppb) + Contoured Ground Magnetics Following Page 18Figure 13: Anomaly 13320D Contoured Corrected Ground Magnetics Following Page 18Figure 14: Anomaly 13320D Contoured MMI Mg (ppb) + Contoured Ground Magnetics Following Page 18Figure 15: Anomaly 13320D Contoured MMI Rb (ppb) * Contoured Ground Magnetics Following Page 18Figure 16: Anomaly 13320D MMI Ti (ppb) + Contoured Ground Magnetics Following Page 18Figure 17: Anomaly 13320D MMI Co (ppb) + Contoured Ground Magnetics Following Page 18Figure 18: Anomaly 13320D MMI Ni (ppb) + Contoured Ground Magnetics Following Page 18Figure 19: Anomaly 13320D MMI Nb (ppb) * Contoured Ground Magnetics Following Page 18 Figure 20: Anomaly 13470B Contoured Corrected Ground Magnetics + Keating Anomalies Following Page 18Figure 21: Anomaly 13470B Contoured MMI Mg (ppb) + Contoured Ground Magnetics Following Page 18Figure 22: Anomaly 13470B Contoured MMI Rb (ppb) + Contoured Ground Magnetics Following Page 18Figure 23: Anomaly 13470B MMI Ti (ppb) + Contoured Ground Magnetics Following Page 18Figure 24: Anomaly 13470B MMI Ni (ppb) + Contoured Ground Magnetics Following Page 18Figure 25: Anomaly 13470B MMI Y (ppb) * Contoured Ground Magnetics Following Page 18Figure 26: Till and Stream Sediment Sample Sites Following Page 18Figure 27: Anomaly 13500A Contoured Corrected Ground Magnetics Following Page 18Figure 28: Anomaly 13500A Contoured MMI Mg (ppb) + Contoured Ground Magnetics Following Page 18Figure 29: Anomaly 13500A Contoured MMI Rb (ppb) + Contoured Ground Magnetics Following Page 18Figure 30: Anomaly 13500A Contoured MMI Ti (ppb) * Contoured Ground Magnetics Following Page 18Figure 31: Anomaly 13500A MMI Ni (ppb) + Contoured Ground Magnetics Following Page 18
LIST of TABLESPage
Table 1. Badger Property- Land Status................................................................................................................ 2 -Table 2: Badger Property Geological Units............................................................................................................ 6 -Table 3: Basic Statistics for MMI-D Samples, Black Hole Sampling ....................................................................- 9 -Table 4: Badger Property Keating Anomaly Evaluation....................................................................................... 10 -Table 5: Basic Statistics for MMI-D Samples, Anomaly 13320D Sampling.........................................................11 -Table 6: Basic Statistics for MMI-D Samples, Anomaly 13470B Sampling......................................................... 11 -Table 7: Basic Statistics for MMI-D Samples, Anomaly 13500A Sampling......................................................... 12 -Table 8. Proposed Budget for the Badger Property............................................................................................. 16 -
LIST of APPENDICES APPENDIX l............................................................................................................................... Analytical CertificatesAPPENDIX II................................................................................................... MMI Anomaly Sampling Spreadsheets
Table 11-1: Badger Grid MMI-D SamplingTable II-2: Anomaly 13320D MMI-D SamplingTable II-3: Anomaly 13470B MMI-D SamplingTable II-4: Anomaly 13500A MMI-D Sampling
APPENDIX III.................................................................................Geophysical Instruments Specifications and DataAPPENDIX IV ........................................................................................................................... KIM Dynamics Report
Table IV-1: Badger Property Till and Stream Sediment Sampling
INTRODUCTION AND TERMS OF REFERENCE GITENNES EXPLORATION INC. acquired an option on the Badger Property in 2002. It lies within the
Garden-Obonga Area of Operation Treasure Hunt (OTH), a geochemical and geophysical initiative of the Ontario
Geological Survey (OGS) of the Ministry of Northern Development and Mines (MNDM). Based on a palladium
value of 73.3 ppb from lake sediment sampling done during OTH, the property was optioned from Robert
Fairservice early in 2002. In June 2002, Gitennes began exploring its potential to host platinum-group element
(PGE) mineralization. Gitennes also evaluated a number of possible kimberlite targets on the property. One
target, informally called the "Black Hole", is a discrete strongly negative magnetic anomaly with a geochemical
signature characterized by Mg, Rb and Ti anomalies.
Because of extensive overburden of the Kaiashk Interlobate Moraine and poor access, the Badger
Property area is considered by Gitennes to be underexplored. New logging roads from the highway are opening
the. area to exploration. However, no economically interesting bedrock mineralization is known to occur on or
close to the property.
This report was prepared for filing assessment work credits for geochemical and geophysical work
undertaken in September 2002 on the Badger Property, using standards set out in National Policy Instrument 43-
101 and in the MNDM requirements for geochemical submissions for assessment credit. Sources of information
include maps and reports from OTH surveys, Ontario Base Maps of 1:20,000 topography, geological maps and
reports from the OGS, two assessment work reports done on behalf of Gitennes for the Badger Property, and on
the list of references provided in the References section of this report. Other than those filed by Gitennes, there
are no reports of work for the immediate area of the Badger Property at the Mining Recorder's Office in Thunder
Bay.
Field work was carried out from September 9 to October 1, 2002 under direct supervision of the writer.
PROPERTY DESCRIPTION AND LOCATION The Badger Property is located in the Thunder Bay Mining Division, Ontario (NTS 52H/5, 52H/11), about
150 road-kilometres north of Thunder Bay (Figure 1). It lies in a rectangle bounded by UTM coordinates 320000E
5489000N, 320000E 5481000N, 311000E, 5481000N, and 311000E 5489000N (all UTM coordinates and map
projections in this report are for Zone 16, NAD27 datum, to conform with Ontario Base Maps for this area. OTH
data is available in either NAD27 datum or WGS83 datum.) Approximate centre of the property is at 49" 29'
Latitude, 890 32' Longitude. It comprises 19 contiguous unpatented and unsurveyed mining claims (Claims
1241563-1241566, 1245613-1245618, 1221169, 1221171, 1221172, 1221191-1221195, 1221206) totalling 241
units (3,856 hectares; see Table 1 and Figure 2). The claims are located in the Kaiashk Lake, Cheeseman Lake,
Kitchen Lake, and Ruffo Lake Areas (Mining Plans G-0735, G-0709, G-0738, and G-0756). Gitennes has
entered into an option agreement with Mr. Robert Fairservice of the City of Kenora, Ontario, effective February 7,
2002, whereby Gitennes can earn a 10007o interest in the claims comprising the Badger Property. Gitennes will
earn this interest by making cash payments totalling CdnS67,500, issuing a total of 100,000 common shares of its
capital to Fairservice, and committing exploration expenditures totalling CdnSl80,000 by January 22, 2005.
When vested, the property will be subject to a 2 07o Net Smelter Return royalty with respect to any mineral
production (Gitennes news release, January 25, 2002). Gitennes can elect to purchase one-half of the NSR for a
-1 -
single payment of CdnSSOO.OOO. All staking and transfer documents are registered with the Mining Recorder,
District of Thunder Bay, Ontario.
Table 1 lists the claims comprising the Badger Property and their expiry dates. All information regarding
claims is on file at the Resident Geologist's Office in Thunder Bay, and can be viewed at the MNDM website at
http://www.mndm.gov.on.ca/mndm/mines.
No permits were required to undertake the exploration work described herein. Permits would be required
for any significant road-building.
Table 1. Badger Property - Land StatusCLAIM1241563124156412415651241566124561312456141245615124561612456171245618122116912211711221172122119112211921221193122119412211951221206
TOTAL
UNITS16161616612151616162168161688616
241
RECORD DATEAug/21/2000Aug/2 1/2000Aug/21/2000Aug/21/2000Aug/30/2000Aug/30/2000Aug/30/2000Aug/30/2000Sep/1 3/2000Sep/1 3/2000Aug/1 0/2001Aug/1 0/2001Aug/1 0/2001Aug/1 0/2001Aug/1 0/2001Aug/1 0/2001Aug/1 0/2001Aug/1 0/2001Aug/1 0/2001
EXPIRY DATEAug/21/2003Aug/2 1/2003Aug/21/2003Aug/21/2003Aug/30/2003Aug/30/2003Aug/30/2003Aug/30/2003Sep/1 3/2003See/1 3/2003Aug/1 0/2004Aug/1 0/2003Aug/1 0/2003Aug/1 0/2003Aug/1 0/2003Aug/1 0/2004Aug/1 0/2003Aug/1 0/2003Aug/1 0/2003
OWNERGitennes Expl. Inc.Gitennes Expl. Inc.Gitennes Expl. Inc.Gitennes Expl. Inc.Gitennes Expl. Inc.Gitennes Expl. Inc.Gitennes Expl. Inc.Gitennes Expl. Inc.Gitennes Expl. Inc.Gitennes Expl. Inc.Gitennes Expl. Inc.Gitennes Expl. Inc.Gitennes Expl. Inc.Gitennes Expl. Inc.Gitennes Expl. Inc.Gitennes Expl. Inc.Gitennes Expl. Inc.Gitennes Expl. Inc.Gitennes Expl. Inc.
AREAKaiashk LakeKaiashk Lake
Ruffo LakeRuffo Lake
Kaiashk LakeKaiashk LakeKaiashk Lake
Ruffo LakeCheeseman Lake
Kitchen LakeRuffo Lake
Cheeseman LakeKaiashk LakeKaiashk LakeKaiashk LakeKaiashk LakeKaiashk Lake
Ruffo LakeRuffo Lake
CLAIM MAPG-0735G-0735G-0756G-0756G-0735G-0735G-0735G-0756G-0709G0738G-0756G-0709G-0735G-0735G-0735G-0735G-0735G-0756G-0756
ACCESSIBILITY, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND PHYSIOGRAPHY Access to the Badger Property is by vehicle. Thunder Bay, population 117,000, is on the north shore of
Lake Superior. It is the nearest population and service centre. From Thunder Bay airport, it is 19 kilometres east
on Highways 11 and 17 East to the Highway 527 North exit; 108.3 kilometres north along paved Highway 527 to
gravel-surfaced Highway 811; 20 kilometres west along the latter to Kennah Road; and 5 kilometres east to the
western boundary of the Badger Property. Kennah Road is gated at Kilometre 3 before Abitibi Consolidated's
Camp 231. Secondary logging roads give vehicular access to much of western and southern portions of the
Badger Property. Ongoing logging by Abitibi Consolidated Inc. is continuing to improve vehicle access on the
property, and is expected to continue through 2003.
Climate is typical of northwestern Ontario, with cool to hot summers and cold winters.
Ontario Hydro transmission lines and a Trans-Canada natural gas pipeline cross Highway 527 a few
kilometres north of Highway 17. A 95-kilometre transmission line from here provides power to the Lac des Isle
mine site. The mine is located 20 kilometres southwest of the junction of Highway 527 and Highway 811. It has
an ore processing plant capable of milling 15,000 tonnes per day of platinum-palladium ores. Other than roads,
there is no other infrastructure in the immediate area of the Badger Property.
-2-
Topography is dominated by low rolling hills comprising glaciofluvial sedimentary deposits and hummocky
end moraine of the Kaiashk Interlobate Moraine (Zoltai, 1965; Mollard, 1981). Drainage is to the northeast by
Gull River, and thereafter north to Lake Nipigon.
Elevations on the property vary from 350 to 500 metres a.s.l. Vegetation is typical of a northern boreal
forest, consisting of mature stands of white spruce, jackpine, balsam fir, birch and poplar, with an understory of
willow, alder, maple and mountain ash.
HISTORY The Badger Property is part of the Garden - Obonga Lake Area of OTH (Figure 3). OTH is an initiative of
the Ontario Ministry of Northern Affairs and Mines to gather and distribute geoscience information. The Garden -
Obonga Area was covered by detailed lake sediment sampling for precious, base and PGE elements (see
Jackson and Dyer, 2000 and OGS OFR 6028, 2000), and flown with magnetometer and frequency-domain EM
survey equipment. The Badger Property was staked based on a 73.3 ppb Pd result from lake sediment sample
2044 from Badger Lake, at UTM coordinates 316991E 5485525N.
There has been no exploration work by non-government companies or individuals recorded for the Badger
Property in the Assessment Files Research Office of the Thunder Bay Mining Recorder. The writer did not
observe indications of previous ground exploration during the field programme reported herein.
REGIONAL GEOLOGYThe Badger Property lies within the Central Wabigoon Subprovince of the Superior Province of the
Canadian Shield. The Central Wabigoon is an assemblage of Archean granitic and tonalitic intrusions, gneisses
and greenstone belts lying west of the Proterozoic (Southern Province) intrusive and sedimentary rocks of the
Nipigon Embayment (Figure 4). Old supracrustal rocks (~3 Ga) are confined to the southern and northern
margins of the subprovince (Tomlinson et al, 1998). In its middle, supracrustal rocks of the Heaven Lake
greenstone belt, the Garden Lake greenstone belt, and the southern portion of the Obonga Lake greenstone belt
have variable ages ranging from 2732 Ma to 2710 Ma (Tomlinson et al, 1998). Foliated to gneissic granitoid
rocks lie between the Garden Lake belt to the north and the Heaven Lake belt to the south. As described by Hart
(2000), these are medium to very coarse-grained granodiorite to tonalite, white to light grey in colour, with mafic
contents less than 1007o.
Proterozoic rocks in the report area are related to the Paleoproterozoic Penokean Orogeny and to
Mesoproterozoic rifting centred under Lake Superior. Paleoproterozoic dyke swarms are present in northwestern
Ontario (Osmani, 1991), some or all of which may be present in the Garden - Obonga area. These include the
Matachewan dyke swarm (2446 to 2473Ma), the Marathon dyke swarm (2101 and 2121 Ma), and the Fort
Frances dyke swarm (2076 Ma). Mesoproterozoic rocks are well represented in the map area, which lies along
the western flank of the Nipigon Embayment. The embayment is a sequence of pre-Keweenawan clastic
sedimentary rocks (sandstones, shales, conglomerates) of the Sibley Group deposited during opening of the
Midcontinent Rift in Lake Superior (Sutcliffe, 1991). These are intruded by Keweenawan Nipigon diabase sills. In
the Garden - Obonga area north of Highway 811, Sibley rocks are exposed as small isolated outcrops of
sandstone and shale in a few road cuts along the Gull River valley. Diabase intrusions observed during field work
are typically massive, medium to coarse-grained and fresh-looking when broken. Mineralogy consists primarily of
-3-
Topography is dominated by low rolling hills comprising glaciofluvial sedimentary deposits and hummocky
end moraine of the Kaiashk Interlobate Moraine (Zoltai, 1965; Mollard, 1981). Drainage is to the northeast by
Gull River, and thereafter north to Lake Nipigon.
Elevations on the property vary from 350 to 500 metres a.s.l. Vegetation is typical of a northern boreal
forest, consisting of mature stands of white spruce, jackpine, balsam fir, birch and poplar, with an understory of
willow, alder, maple and mountain ash.
HISTORY The Badger Property is part of the Garden - Obonga Area of OTH (Figure 3). OTH is an initiative of the
MNDM to gather and distribute geoscience information. The Garden - Obonga Area was covered by detailed
lake sediment sampling for precious, base and PGE elements (see Jackson and Dyer, 2000 and OGS OFR
6028, 2000), and flown with magnetometer and frequency-domain EM survey equipment. The Badger Property
was staked based on a 73.3 ppb Pd result from lake sediment sample 2044 from Badger Lake, at UTM
coordinates 316991E 5485525N.
There has been no exploration work by non-government companies or individuals recorded for the Badger
Property in the Assessment Files Research Office of the Thunder Bay Mining Recorder. The writer did not
observe indications of previous ground exploration during the field programme reported herein.
REGIONAL GEOLOGYThe Badger Property lies within the Central Wabigoon Subprovince of the Superior Province of the
Canadian Shield. The Central Wabigoon is an assemblage of Archean granitic and tonalitic intrusions, gneisses
and greenstone belts lying west of the Proterozoic (Southern Province) intrusive and sedimentary rocks of the
Nipigon Embayment (Figure 4). Old supracrustal rocks (~3 Ga) are confined to the southern and northern
margins of the subprovince (Tomlinson et al, 1998). In its middle, supracrustal rocks of the Heaven Lake
greenstone belt, the Garden Lake greenstone belt, and the southern portion of the Obonga Lake greenstone belt
have variable ages ranging from 2732 Ma to 2710 Ma (Tomlinson et al, 1998). Foliated to gneissic granitoid
rocks lie between the Garden Lake belt to the north and the Heaven Lake belt to the south. As described by Hart
(2000), these are medium to very coarse-grained granodiorite to tonalite, white to light grey in colour, with mafic
contents less than 1007o.
Proterozoic rocks in the report area are related to the Paleoproterozoic Penokean Orogeny and to
Mesoproterozoic rifting centred under Lake Superior. Paleoproterozoic dyke swarms are present in northwestern
Ontario (Osmani, 1991), some or all of which may be present in the Garden - Obonga area. These include the
Matachewan dyke swarm (2446 to 2473Ma), the Marathon dyke swarm (2101 and 2121 Ma), and the Fort
Frances dyke swarm (2076 Ma). Mesoproterozoic rocks are well represented in the map area, which lies along
the western flank of the Nipigon Embayment. The embayment is a sequence of pre-Keweenawan clastic
sedimentary rocks (sandstones, shales, conglomerates) of the Sibley Group deposited during opening of the
Midcontinent Rift in Lake Superior (Sutcliffe, 1991). These are intruded by Keweenawan Nipigon diabase sills. In
the Garden - Obonga area north of Highway 811, Sibley rocks are exposed as small isolated outcrops of
sandstone and shale in a few road cuts along the Gull River valley. Diabase intrusions observed during field work
are typically massive, medium to coarse-grained and fresh-looking when broken. Mineralogy consists primarily of
-3-
pyroxenes and feldspar - olivine was identified in hand specimen but is not abundant. Sills usually stand out as
positive relief features, and can form steep cliff faces along the edges of drift-covered hills. Relative ages of the
diabase intrusions encountered during mapping were not established by Gitennes, although all are believed to be
of Keweenawan age.
Zoltai (1965) and Mollard (1981) reported on the Quaternary surficial deposits, ice movements and glacial
lakes in the area west of Lake Nipigon. Overburden comprises glacial deposits (ground moraine, drumlins),
glaciofluvial deposits (interlobate moraines, eskers, kames, outwash deposits), glaciolacustrine deposits (varved
clay, deltaic deposits, and littoral features of Glacial Lake Agassiz), and aeolian deposits (dunes, loess). Ice
direction north of the Badger Property was from north-northwest to south-southeast (see Zoltai, 1965, and GSC
Map 1702A, scale 1:5,000,000 by Dyke and Prest, 1987). To the south, a separate lobe of the Laurentide ice
sheet moved from east-northeast to west-southwest. The Kaiashk Interlobate Moraine was deposited where the
two ice sheets came together. Zoltai (1965) also indicates that this moraine may in part be a terminal moraine,
as suggested by the presence of kettles on its north side. The distribution of glacial deposits and subsequent
drainage patterns appears to have been strongly influenced by bedrock topography. Diabase usually underlies
topographic highs - locally, abrupt cliff faces of diabase rise several tens of metres above the surrounding
terrane. It appears likely that thicker glacial deposits were ramped against or channelled along diabase dykes or
sills.
Recent deposits are peat bogs, and fluvial sands and gravels of no great extent.
LOCAL GEOLOGY Sage et al (1974) carried out and compiled reconnaissance-scale mapping (one inch to two miles) for the
Obonga Lake - Lac des Isles Sheet (ODM Preliminary Map P. 963, Scale 1 inch to 2 miles). Detailed government
mapping in the vicinity of the Badger Property is restricted to the Garden Lake greenstone belt (Milne, 1964, and
Hart, 2000) and the Heaven Lake greenstone belt west of Highway 811 (Hart, 1999).
Because of scarce outcrop, local geology must be inferred from OTH geophysical data. Based on their
distinctive magnetic signatures, the writer proposes a four-fold division of lithologies suitable for reconnaissance
mapping: 1) diabase dykes and sills; 2) foliated to gneissic intermediate to felsic intrusive lithologies; 3) mafic to
ultramafic intrusives (i.e. Lac des Isles Complex, Tib Lake Complex); and 4) supracrustal rocks (Heaven Lake
greenstone and Garden Lake greenstone belts).
1. Diabase Dykes and Sills. The most obvious features on OTH magnetic maps are round to oblate rings and
polygonal areas. These are associated with diabase, and show up particularly well on 1:50,000 scale maps of the
shaded image of the second vertical derivative of the magnetic field (see OGS Maps 82 133 and 82 135, which
cover the area from the Badger Property to the Lac des Isles Mine). A cross-section across a ring segment usually
consists of a central intense linear magnetic low flanked by intense magnetic highs. Within the rings are domains of
more subdued magnetic response that are windows into the Archean basement. The rings themselves may be
vertical dykes, although where observed by the writer in the field, they have subhorizontal jointing suggesting sill
intrusion. It is possible the rings are the upward-stepping leading edges from larger sills or sill complexes at depth
(T. Hart, pers. comm.). Polygonal areas of diabase with no central domains have a choppy strongly contrasting
magnetic signature. The writer believes these are sills rather than fault-bounded vertically-emplaced plutons.
-4-
2. Foliated to Gneissic Intermediate to Felsic Rocks. These probably underlie most of the Garden-Obonga area.
Based on magnetic signature, the writer recognizes three types of gneiss terrane. "GNEISS 2" has a noisy magnetic
signature. It is thought to be terrane that is underlain at shallow depth by diabase sills which are influencing its
magnetic response. GNEISS 2 was observed in outcrop west of Highway 811. There, it has a more mafic
composition and better-developed foliation than GNEISS or GNEISS 1. Its internal inhomogenieties may also be
responsible for its choppy magnetic signature. "GNEISS 1" has a more subdued but still noisy magnetic signature.
It is thought to be underlain at greater depth by diabase. However, this terrane may also in part be underlain by
metavolcanic rocks or gneissic metasedimentary rocks which contribute contrast to its overall magnetic signature.
"GNEISS" is a terrane with a subdued broadly even magnetic response. No diabase is likely to be present at depth.
The writer saw no significant differences in mineralogy between GNEISS and GNEISS 1.
3. Mafic to Ultramafic Intrusives. Near the Badger Property these include the Lac des Isles Complex, the Tib
Lake Complex, the Legris Lake Intrusion, and the Dog River Intrusion. Their overall magnetic signature is a strong
low, with pronounced internal magnetic contrasts, significantly different from the surrounding country rocks (see
OGS Map 82 135, Scale 1:50,000 for the magnetic signature of the Lac des Isles complex). This type of signature
does not appear on OTH maps for the immediate environs of the Badger Property.
4. Supracrustal Rocks. Greenstone belts in the area of the Badger Property consist of mafic to felsic volcanic
and volcaniclastic rocks, with intercalated clastic and chemical metasedimentary rocks. One occurrence of spinifex-
textured ultramafic volcanic was reported by Sage et al (1974) and Tom Hart (pers. comm.) in the Heaven Lake
greenstone belt. Magnetic signature of the greenstones is marked by linear magnetic highs related to iron-rich
sedimentary rocks. Otherwise, the magnetic signature can be rather subdued, and contacts between greenstone
and gneissic or felsic intrusive rocks are difficult to interpret from OTH geophysical maps.
PROPERTY GEOLOGYFigure 5 shows the geology of the Badger Property based on mapping by the writer, by his interpretation of
OTH magnetic maps, and by mapping by Sage et al (1974). Lithological units (Table 2) described herein and
coded on Figure 5 conform to those described by Hart (2000). In the absence of whole rock geochemical
analyses, granitoid rocks have been designated as either intermediate to felsic or felsic.
The writer interprets a simple picture of gneissic intermediate to felsic and felsic rocks intruded by diabase
dykes. Diabase forms a teardrop-shaped ring dyke lying east of Highway 811, the eastern portion of which crops
out on the property. Within and without the ring are foliated felsic intrusives (GNEISS and GNEISS 2). Near-
vertical contacts striking 230" and 2350 were mapped between diabase dykes and gneissic felsic intrusives on
Claim 1245616. Distinctive cooling cracks on horizontal diabase surfaces were observed here as well. Diabase
Hill on Claim 1221191 coincides with an isolated circular magnetic high and a cluster of negative Keating
anomalies (see OGS Map 82 133, Scale 1:50,000 - the feature is centred at 315560E 5482380N). Its discrete
magnetic response suggests that the intrusion does not have any extent beyond the observed outcrop.
No exposures of Archean supracrustal metavolcanic and metasedimentary rocks or Sibley sedimentary
rocks occur on the Badger Property.
-5-
Table 2: Badger Property Geological Units
PHANEROZOIC CENOZOIC
QUATERNARYPLEISTOCENE Glacial, glaciofluvial and glaciolacustrine deposits; sand, gravel, till
Unconformity PRECAMBRIAN
PROTEROZOICNipigon and Logan Sill Complexes Diabase dykes and sills
Intrusive Contact (not observed) Diabase dykes
Intrusive Contact ARCHEAN
Intermediate to Felsic Intrusive(s) Massive felsic intrusive, ^"/o ferromagnesian mineralsIntrusive Contact (not observed)
Mafic to Ultramafic Intrusive(s) Inferred from Geophysical Data Gneissic Intermediate to Felsic Intrusives Gneissic felsic intrusive, ^"/0 ferromagnesian minerals
(GNEISS, GNEISS 1)Gneissic intermediate to felsic intrusive, S-20% ferromagnesian minerals
(GNEISS 2)
Pleistocene geology of the property is complex. Glacial deposits shown on the Gull River and Heaven
Lake Data Base Maps (see Maps 5049 and 5051, Mollard, 1981) have an overall ENE-WSW trend. Ground
moraine till on Claims 1254616 and 1221192 is thin and clay-rich, with boulders of various intrusive lithologies.
Almost all of the boulders checked during traverses on the Badger Property are intermediate to felsic and felsic
gneisses, felsic intrusives, or diabase - very few Sibley sedimentary rock boulders or cobbles were seen. The
remainder of the property is covered by deposits of the Kaiashk Interlobate Moraine that are related to a
readvance of the Laurentide ice sheet (Zoltai, 1965). Thicknesses range from a metre or less on Claim 1245616
to nearly 75 metres at the water well of Abitibi's Camp 231 (Tom Katz, Abitibi Consolidated, pers. comm.) Kettle
lakes, including Tarrison Lakes and Badger Lake, and several dry kettles are distributed along the north side of
the Kaiashk Interlobate Moraine. On the south side, much of the moraine is mantled by fine sands believed to be
of glaciofluvial or glaciolacustrine origin. Cross-stratification and coarsening-upward sequences in several 1-2-
metre high road-side exposures on the property suggest that sands and gravels were deposited in a fluvial
environment. An exposure of coarsely varved sand and silt on Claim 1245616 (UTM coordinates 314305 E
5485760 N) is thought to be evidence of overbank deposition during flood conditions. This exposure lies
immediately north of an ENE-trending esker on Claims 124616 and 1245615, and is likely related to it. The esker
is part of an intermittent trend that extends northeast to Lake Nipigon.
No glacial striae were observed during mapping, nor were any oriented current structures in the
glaciofluvial sediments measured.
DEPOSIT TYPES
Gitennes is exploring the Badger Property for intrusive-hosted PGE mineralization and for diamondiferous
kimberlite.
The area west of Lake Nipigon is known for a diversity of PGE occurrences. Its geology has been
compared to the Noril'sk region of Russia (Schneiders et al, 2001). Better-known PGE mineralization includes
the Lac des Isles Mine, the Legris Lake Intrusion, Great Lakes Nickel deposit, and the Wolf Mountain property.
-6-
Host rocks for PGE occurrences range in age from Neoarchean (Lac des Isles) to Mesoproterozoic (Great Lakes
Nickel). Deposit types of PGE mineralization are also diverse. At Lac des Iles, PGE mineralization is found in
several environments, including a zone between pyroxenite and a gabbro-breccia contact, an erratically
mineralized coarse-grained leucogabbro, and a breccia ore zone (www.napalladium.com website). The
Neoarchean Legris Lake intrusion features three styles of mineralization: a magmatic Cu-Pd-rich style, and
hydrothermal Pd-rich, Cu-Ni-poor and Rh-Pd-rich, Cu-Ni-poor styles (www.avalonventures.com website). At Wolf
Mountain, the Mesoproterozoic Seagull Intrusion has a layer of cumulate-textured disseminated copper-nickel-
PGE sulphide mineralization near its base (www.avalonventures.com website).
Kimberlites can occur as steep-sided cone-shaped diatremes from less than 2 up to 146 hectares in area
(Pell, 2002). They may have a distinct circular magnetic high or low signature, which can be several tens to
hundred metres in diameter. If capped by a significant thickness of weathered clay minerals, there may be a
positive EM anomaly or resistivity low. Kimberlites have a distinctive mineralogy of high Gr, low Ca pyrope
garnets, chrome diopside, picroilmenite and olivine. Dispersion trains of these indicator minerals in ground
moraine are commonly used in Canada for diamond exploration. The MMI-D element suite has been used to
explore the Delta 1 Kimberlite in the Attawapiskat area of Ontario and the Nabberu Kimberlite in Australia (case
studies for these can be obtained from SGS Canada Inc.). The Delta 1 kimberlite Is covered by several metres of
peat and complex Quaternary sediments. Its MMI response is particularly enriched in Ni, Gr, Nb and Y, and to a
lesser extent in Mg, although the element enrichments are variable from line to line on the test data. The
Nabberu Kimberlite is a shallowly-dipping dyke-like body buried under 10 to 45 metres of aeolian sands, hardpan,
and saprolite. Its response is enriched in Cr, Nb, and Rb, and there is some indication of a halo enriched in Mg.
The diamond potential of the Badger Property was initially based on OGS modelling of OTH airborne
magnetics. Keating (1995) devised a computer-automated pattern recognition technique that identifies roughly
circular magnetic anomalies by computing a first-order regression between a vertical cylinder model and gridded
magnetic data. The technique has been used to model kimberlite targets in Australia and Canada. On OTH
maps, these are depicted as one or more overlapping circles (red for positive, blue for negative) which are scaled
to reflect the correlation value. Each target can consist of a cluster of Keating anomalies of varying intensity. The
technique does not identify dyke-like kimberlites, and will have difficulty in discriminating circular features lacking
strong magnetic contrast with surrounding bedrock. Thick overburden may also mask bedrock magnetic
features.
MINERALIZATION No mineralization is known to occur on the Badger Property. Other than traces of pyrrhotite in diabase and
pyrite in foliated felsic intrusive rocks, no sulphides were observed.
EXPLORATIONGitennes began exploring the PGE potential of the Badger Property in June, 2002 (Foster, 2002). MMI
sampling was selected as being the geochemical method most likely to detect anomalous bedrock mineralization
beneath the extensive glacial deposits. Upon receipt of results from this work, the Badger Grid was cut for
ground magnetic and VLF-EM surveys (Milani, 2002), covering a broad magnetic high south of Badger Lake
thought to be a source for the lake sediment Pd anomaly. The diamond potential of the property was enhanced
-7-
after ground magnetics showed that a Keating anomaly included within the grid was a very high contrast steep- sided magnetic low (Figure 6). Named the Black Hole, it is a mag low with strong magnetic susceptibility and likely reversely polarized. If reversely polarized, it is likely of different age, and is presumed to be younger than the surrounding bedrock. It is interpreted as a small, 150m x 200m elliptical to circular mafic or ultramafic intrusion, possibly a kimberlite diatreme. Subsequently, several orientation lines of MAXMIN EM surveying and a number of MMI-D (diamond indicator) soil sampling lines were done over the target. Till and stream sediment samples were collected for diamond indicator mineral picking.
Discovery of the Black Hole suggests that as a first pass, the evaluation of the Keating anomalies has merit. Four other Keating anomaly clusters on the property were evaluated in September 2002 by ground magnetic surveys, MMI-D (diamond indicator) soil sampling and till or stream sediment sampling where possible. The work on these targets was reconnaissance in nature. Anomalies were explored by establishing chain-and- compass evaluation grids comprising E-W and N-S survey lines. Magnetic surveying was done using an OMNI- IV tie-line magnetometer (Serial #255225) manufactured by EDA Instruments Ltd. The magnetometer was used in its tie-line mode, which does not require the use of a base station to correct for diurnal magnetic variations. Instead, a tie-line was established (usually an E-W baseline) and readings taken on this at the start and finish of the survey. The magnetometer automatically calculates corrected readings based on tie-line data. Lines were usually spaced 50 metres apart; readings were taken every 12.5 metres. Data were levelled using a magnetic datum of -57,500nT for all surveyed grids, conforming to that used for the Badger Grid magnetic survey. Both uncorrected and corrected magnetics were downloaded as ASCII files to laptop computers for text editing and plotting.
The MMI geochemical analytical technique uses a weak partial extraction to enhance geochemical responses over buried ore deposits. Sampling media and methods are discussed in the section entitled "Sampling Method and Approach".
Data reliability for the Badger Grid is reckoned to be good, due to the detail of the surveys carried out. However, interpretation of the results is hampered by complex glacial-derived overburden and lack of bedrock. Reconnaissance work on the other Keating anomalies is much less reliable, primarily because of the minimal coverage of the evaluation grids. Any follow-up work will need to address this lack of detail.
RESULTS OF SURVEYSA total of 239 samples were analyzed for MMI-D elements. No blind or duplicate samples were inserted by
Gitennes for quality control. MMI-D samples were usually moderate to well sorted fine- to medium-grained medium brown sands with variable amounts of pebbles or cobbles, an essentially homogenous sampling medium. MMI-D sampling was done on three other negative Keating anomalies (13320D, 13470B, 13500A). These have some geochemical similarities to the Black Hole, but none is considered to be a priority at this time. A fourth cluster of negative Keating anomalies, informally known as Diabase Hill, was not sampled.
MAXMIN surveying was done on Lines 4 East, 5 East and 6 East using 100-metre and 150-metre cable spacing, and 7111Hz and 14080Hz frequencies (Figures 32 and 33). No conductor was detected, however the 150-metre cable data and to a lesser extent the 100-metre cable data for 14080Hz indicate a rise in quadrature response over the Black Hole. In-phase response rises on all lines for the 150-metre cable spacing for 14080Hz
-8-
as well. The relatively flat responses for the 100-metre cable spacing suggests that bedrock lies at a depth
greater than 45-50 metres (ie Yt of the cable spacing).
Black Hole MMI SamplingA total of 157 MMI-D samples were collected on Lines 1E, 3E, 4E, 450E, 5E, 550E, 6E, 7E and 8E on the
Badger Grid (see Table 11-1 in Appendix II for sample locations and analytical results). Basic statistics are given
in Table 3 (for statistical calculations, sample analyses less than detection limit were given a value of Yt of the
detection limit for that element). Because so few samples had detectable Y or Pd, these elements are excluded
from further discussion.
Table 3: Basic Statistics for MMI-D Samples, Black Hole Sampling
Detection Limit
MeanStandard Error
Median
Mode
Standard Deviation
Sample Variance
Kurtosis
Skewness
Range
Minimum
Maximum
Count
CountlF^etection
Mg
100
9171
3038450
8100
3796
14411591
-0.318
0.641
17041
2110
19151
157
157
Ti
1
3.096
0.506
1
0.5
6.346
40.273
48.886
6.035
61.5 !1
62
157
81
Cr
1
0.768
0.0430.5
0.5
0.539
0.290
4.028
2.167
2.5 si
3
157
42
Co
1
0.602
0.031
0.5
0.5
0.391
0.153
21.252
4.506
2.5 :1
3
157
14
Ni
3
1.860
0.132
1.5
1.5
1.650
2.724
52.228
6.709
15.5
0
17
157
13
Rb
1
35.070
0.672
34
27
8.423
70.950
0.690
0.202
53
5
58
157
157
Y
0.1
0.057
0.004
0.05
0.05
0.045
0.002
69.420
7.880
0.45
O.1
0.5
157
7
Nb
0.1
0.065
0.004
0.05
0.05
0.044
0.002
12.329
3.448
0.25
O.1
0.3
157
24
Pd
0.1
0.054
0.002
0.05
0.05
0.022
0.000
39.369
6.232
0.15
O.1
0.2
157
6
When it became apparent that the Black Hole target had a geochemical signature related to the depletion
of certain elements, background and anomaly threshold values were not calculated. Instead, contoured maps
were produced for Mg and Rb using Surfer 6.0 to see how the MMI-D results plotted with respect to ground
magnetics contours that defined the extent of the target. Ti, Cr, Co, Ni, and Nb were plotted as classed plots to
determine the location of higher values relative to magnetic contours.
Figure 7 shows contoured Mg values in ppb with superimposed ground magnetics contours that define the
Black Hole (the Keating anomaly is shown as a white doughnut). There is a distinct depletion in Mg over the area
of the target, highlighted by an ill-defined ring of low Mg around its perimeter. Within this ring, coincident with the
edge of the steep magnetic gradient, is a second intermittent ring or horseshoe of higher Mg values. Rb is
depleted over the Black Hole (Figure 8), showing higher values on its north and south flanks. Figure 9 shows
posted values for Ti. Five of the eight highest values (M 5 ppb Ti) show a correlation with the target. Figure 10
shows the two highest Ni values of 10 ppb are directly coincident with the Black Hole. A weak but definite
increase in detectable values of Cr (Figure 11) is shown immediately east of the target, suggesting that bedrock
associated with the broad magnetic anomaly may be elevated in this metal. Finally, Nb (Figure 12) shows no real
trends or correlations with the Black Hole magnetics.
-9-
Figure 5 shows the location of other Keating anomalies on the Badger Property with respect to the Black
Hole - Table 4 summarizes their characteristics based on work done by Gitennes.
Anomaly 13320DThis target consists of a cluster of four Keating anomalies on Claim 1241564, some 760 metres west of the
Black Hole. It is in a topographic depression; the terrane slopes to west and defines a NNE-trending valley
parallel to a segment of a major diabase dyke (see Figure 5). Glaciofluvial or glaciolacustrine deposits obscure
bedrock which is interpreted to be massive to foliated felsic intrusives.
Table 4: Badger Property Keating Anomaly EvaluationANOMALY13320D
13470B
13500A
"Diabase Hill"
MAGNETICSWeak double mag low from ground mag - anomaly not completely covered by ground surveyWeak triple mag low at edge of beaver pondPoorly defined and subdued mag low in dry kettle depressionAirborne only; similar to Black Hole
GEOCHEMISTRYCoincident Mg depletion, Rb high
Nearly coincident Mg depletion; somewhat coincident Rb high over mag lowsPossible Mg depletion
No MMI sampling
INTERPRETATIONUncertain. Requires expanded mag and MMI sampling
Uncertain. Requires expanded mag and MMI samplingRequires expanded ground mag survey
Diabase outlier; no kimberlite potential
A chain-and-compass grid was established with its baseline going due west from Line O Station 0+00 on
the Badger Grid. The raw magnetics data (Figure 13) shows two weak mag lows on Line 450W, the
southernmost coinciding in part with the Keating anomalies of the 13320D target. Neither mag low is of the
magnitude of the Black Hole. Anomaly 13320D could be due to a north-south dyke-like feature that remains open
to the south.
Forty-two MMI-D samples were spaced 50 metres apart on six 50-metre spaced lines (see Table II-2 in
Appendix II for sample locations and analytical results). Basic statistics for Anomaly 13320D are given in Table 5
(for statistical calculations, sample analyses less than detection limit were given a value of V-i of the detection limit
for that element).
Differences between Anomaly 13320D sample set and the Black Hole sample set are the lack of Gr, lesser
range between minimum and maximum values for Ti and Ni, and the increase in detectable Pd in the former. As
the bulk of the MMI-D coverage of Anomaly 13320D lies east of the magnetic lows, these differences may be a
function of changes in bedrock lithology. The range of Pd is essentially 1 ppb, which is not considered to be
significant. Because of low detected values, Cr, Y and Pd are excluded from further discussion.
As for the Black Hole, Mg lows (Figure 14) are roughly coincident with the mag lows on Line 450W. On
Line 200W, Mg and magnetic responses are significantly higher. This may be responding to a geological
boundary, perhaps the edge of the broad magnetic high covered by the Badger Grid. An Rb high (Figure 15) is
partly coincident with the northern mag low, but extends well beyond it to the east. Rb lows along Line 250 West
may be indicating a contact with the broad magnetic high on the Badger Grid. Elevated Ti values occur on Line
450 West and to a lesser extent on Line 350 West (Figure 16). There is some suggestion that Ti is depleted over
the magnetic lows; however, similar depletion is also apparent along Line 250 West. Although not detected over
-10-
the mag lows, Co (Figure 17) is slightly anomalous on Lines 300 West and 250West. Figure 18 and Figure 19
show that Ni and Nb, which have limited ranges between minimum and maximum values, are not anomalous
over the mag lows.
Table 5: Basic Statistics for MMI-D Samples, Anomaly 13320D Sampling
Detection Limit
Mean
Standard Error
Median
Mode
Standard Deviation
Sample Variance
Kurtosis
Skewness
Range
Minimum
Maximum
Count
COUNTIF^etection
Mg
100
8442
534
. 7525
#N;A3461
11977497
0.6424
0.5781
16280
1740
18020
42
42
Ti
1
5.93
1.017
4
4
6.59
43.46
13.31
3.16
37.5 d
38
42
38
Gr
1
0.536
0.036
0.5
0.5
0.23
0.05
42
6.48
1.5 :1
2
42
1
Co
1
0.77
0.0889
0.5
0.5
0.576
0.332
5.438
2.391
2.5
^
3
42
11
Ni
3
2.19
0.183
1.5
1.5
1.184
1.402
5.812
2.181
5.5
O
7
42
14
Rb
1
40.24
1.573
39.5
46
10.193
103.893
0.226
0.396
49
17
66
42
42
Y
0.1
0.053
0.0036
0.05
0.05
0.0231
0.0005
42
6.4807
0.15o.TI
0.2
42
1
Nb
0.1
0.0869
0.0101
0.05
0.05
0.0654
0.00427
1 .8046
1.6815
0.25
O.01
0.3
42
13
Pd
0.1
0.0738
0.006
0.05
0.05
0.0417
0.0017
4.025
2.07
0.15
O.1
0.2
42
14
Anomaly 13470B
Located on Claim 1245618 three kilometres northeast of the Black Hole, Anomaly 13470B is a cluster of
moderate to strong Keating anomalies. These are at the margin of a dried beaver pond. Steep glaciofluvial sand
ridges bound the west, south and east sides of the pond. A spring originates at the base of the south sand ridge.
Bedrock is probably massive to foliated gneissic felsic intrusives. Ground magnetics (Figure 20) detected a weak
linear magnetic low underlying the south sand ridge and correlating with the position of the Keating anomalies.
Table 6: Basic Statistics for MMI-D Samples, Anomaly 13470B Sampling
Detection LimitMean
Standard Error
MedianMode
Standard DeviationSample Variance
KurtosisSkewness
RangeMinimum
Maximum
CountCountlF^etection
Mg
100
12674.21
1275.09
10932SN/A
5557.98630891212
-1.1739
0.3374168885180
2206819
19
Ti
1
7.7105
3.4661
10.5
15.1082
228.25889.0110
2.924860.5
0.5
6119
10
Cr
10.7895
0.2895
0.5
0.51.2618
1.592119
4.35895.50.5
619
1
Co
1
0.6842
0.0872
0.50.5
0.38040.1447
7.7389
2.61211.50.5
219
5
Ni
32.157895
0.259477
1.51.5
1.131035
1 .27924-0.71849
1.1701932.5
1.54
19
5
Rb
117.6315
3.025218
40
13.1865
173.885-0.8581
0.537039.5
0.540
1917
Y
0.10.1026
0.0266
0.05
0.05
0.1160
0.01357.8308
2.76040.45
0.050.5
19
6
Nb
0.1
0.0605
0.0082
0.05
0.050.0357
0.0013
14.7075
3.77080.15
0.050.2
19
2
-11 -
Nineteen MMI-D samples were collected on several north-south lines over Anomaly 13470B (see Table II-3 in Appendix II for sample locations and analytical results). Basic statistics for the anomaly are given in Table 6
(for statistical calculations, sample analyses less than detection limit were given a value of V* of the detection limit
for that element. Pd was not included, as all samples had less than detection limit value). Cr had only one detectable value and Co had a range of 2 ppb - both are excluded from further discussion.
Figure 21 shows high Mg overlying the area of beaver pond, defining a southeast-trending anomaly that remains open in that direction. Mg is depleted over the mag low, and to the west. Rb (Figure 22) has a very
distinct low coincident with the beaver pond, but and is higher over the magnetic low. Mg (high) and Rb (low)
appear to be mapping a bedrock contact that flanks the northeast margin of the magnetic low. Figure 23 plots Ti
values, which show no significantly anomalous results over the Keating anomalies. Ni (Figure 24) and Y (Figure
25) show some tendency to have elevated values related to the target.
A stream sediment sample (17529 on Figure 26) collected on Line O about 25 metres south of the baseline
had 1 chromite, 20 picroilmenite, 4 chrome diopside and 7 olivine grains (Kiridzija, 2002). The presence of these indicator grains makes Anomaly 13470B a priority for detailed follow-up work.
Anomaly 13500A
The anomaly consists of two Keating anomalies three kilometres east of the Black Hole, coincident with a
dry kettle lake. Overburden is glaciofluvial or glaciolacustrine sands, likely mantling terminal moraine deposits.
No outcrop is present, but is thought to be foliated to gneissic felsic intrusives.
Analytical results for MMI sampling on Anomaly 13500A are given in Table II-3 in Appendix II. Table 7
gives basic statistics.
Table 7: Basic Statistics for MMI-D Samples, Anomaly 13500A Sampling
Detection Limit
Mean
Standard Error
Median
Mode
Standard Deviation
Sample Variance
Kurtosis
Skewness
Range
Minimum
Maximum
Count
CountlF^etection
Mg
100
8422.381
1250.588
6280
#N7A
5730.914
32843379
0.341
1.152
19250
2150
21400
21
21
Ti
1
4.310
1.270
2
2
5.821
33.887
8.122
2.744
24.5
el
25
21
18
Cr
1
0.524
0.024
0.5
0.5
0.109
0.012
21.00
4.583
0.5
el
1
21
1
Co
1
0.905
0.168
0.5
0.5
0.768
0.590
1.423
1.631
2.5
*:1
3
21
5
Ni
3
3.048
0.404
3
1.5
1.850
3.423
-0.103
0.964
5.5
^
7
21
11
Rb
1
32.381
2.540
33
33
11.638
135.45
2.865
0.355
55
10
65
21
21
Y
0.1
0.060
0.004
0.05
0.05
0.020
0.000
0.975
1.700
0.05
O.1
0.1
21
4
Nb
0.1
0.064
0.008
0.05
0.05
0.036
0.001
10.581
3.101
0.15
O.1
0.2
21
4
Pd
0.062
0.008
0.05
0.05
0.035
0.001
13.034
3.493
0.15
O.1
0.2
21
3
Figure 27 shows the position of Anomaly 13500A plotted on ground magnetics. Although not quite
coincident with ground magnetic lows, the Keating anomalies are based on airborne lines flown at 200-metre
spacing, such that they may be plotted offset from their position on the ground. Likely, the two anomalies are
-12-
related to magnetic lows on Line 50 East, which themselves appear to be related to a much larger, possibly dyke- like magnetic low feature.
Like Anomalies 13320D and 13470B, Anomaly 13500A had no Cr, and only a few samples with detectable Co, Y, Nb, and Pd. Mg (Figure 28) is generally depleted in the centre of the grid, but can be enriched or depleted with respect to ground magnetic lows. It is strongly anomalous over a magnetic high at the south end of Line O, and immediately north of the northern magnetic low on Line 50 East. Rb (Figure 29) is broadly anomalous over the entire central portion of the grid. Ti (Figure 30) is strongly anomalous immediately north of the Keating anomalies, coincident with a ground magnetic high. Ni (Figure 31) is not obviously coincident with any ground magnetic feature.
Till and Stream Sediment Sampling
Till sampling was attempted on the Badger Property to see if any indicator mineral dispersion trains were present. Unfortunately, there are only two areas of undoubted ground moraine till on the property (samples 17558 and 17560 on Figure 26). To compensate for the lack of coverage, eight stream sediment samples were collected from an active creek and at the site of Anomaly 13470B.
Because of the large sample weights after heavy mineral separation, only Vi of the concentrates were observed for indicator mineralogy (Kiridzija, 2002 - see Appendix IV). All samples consist predominantly of orthopyroxene and lesser amounts of olivine. Most of the olivine grains are characterized as being from a non- kimberlite source. This is consistent with the amount of diabase intrusions in the Garden - Obonga area. Four samples (17529, 17552, 17553, 17557) had a different morphologically-distinct type of olivine. This type could also be from non-kimberlitic sources. Four samples (17529, 17553, 17554, 17560) had one or more grains of picroilmenite and chrome diopside present. No kimberlitic garnets were observed. Splits of the heavy mineral concentrates were sent to ALS Chemex, an ISO 9001:2000 registered laboratory in North Vancouver for analyses. No unusual analytical results were returned (see Table IV-1 in Appendix IV).
SAMPLING METHODS AND APPROACHUnlike conventional soil sampling of specific soil layers, MMI (mobile metal ion) sampling requires samples
to be taken at a consistent depth, no matter what the soil medium may be (Birrell and Mann, 1995). Samples were collected from holes hand-dug with a long-handled stainless steel gardening trowel, at a consistent depth of 15-25 centimetres below the Ao horizon. When necessary, samples were sieved with a 1/4-inch mesh stainless steel riddle to remove pebbles and coarse organic matter. During the sampling programme in June, black organic muck in wet areas was usually collected by hand from depths of 20-35 centimetres. At that depth; these samples were generally still within or at the bottom of the Ao horizon, but standing water or ice prevented any deeper digging. Subsequent analytical results indicated this sample medium gave a subdued or less than detection geochemical response. For this reason, MMI sampling was not done in swampy terrane during the September sampling programme.
On the Badger Property, Gitennes collected samples at 25-metre or 50-metre intervals on magnetometer survey lines. All samples were placed in plastic ziploc bags. They were not weighed, but would have been about 300-600 grams. None was dried prior to shipment. No duplicates were inserted into the sample stream. All were
-13-
shipped or delivered to SGS Canada Inc. (formerly XRAL Laboratories) in Don Mills, Ontario. SGS is an ISO- 9002 certified facility.
Two till samples and eight stream sediment samples were collected on the Badger Property for heavy
mineral separation and indicator grain picking. All were washed and screened to -1/4-inch mesh in the field. The
samples were then shipped to Vancouver Indicator Processors Inc. of Burnaby, British Columbia for sample
preparation and heavy mineral separation. After this procedure, the concentrates were sent to KIM Dynamics of
North Vancouver, British Columbia for indicator mineral picking and identification.
SAMPLE PREPARATION, ANALYSES AND SECURITYNo sample preparation was required in the field for MMI samples. No quality control measures beyond
those implemented by SGS for the MMI samples were deemed necessary. As well, no extraordinary security
measures were put in place for any of the sample shipments. Samples were either shipped via Manitoulin
Transport Inc. in Thunder Bay to SGS in Don Mills, Ontario, or delivered directly to the lab.
Upon receipt at the lab, fifty grams of as-received material is weighed into a plastic container with screw
cap. Fifty millilitres of MMI extractant ("B" for precious metals suite or "D" for diamond suite) is added and the
container is capped. Extraction takes place at room temperature on a shaker for 20 minutes and allowed to settle
overnight. The resulting extractant is decanted and if required is centrifuged. The sample then undergoes the
following procedure for analyses:
1. Pipette 1 ml sample into centrifuge test tube.2. Add 9 ml (to the mark 10 ml) solution B, containing 50 ppb Re internal standard, internal standard's final concentration being 45 ppb.3. Cover sample with parafilm and shake.4. Load samples into racks and set it into the auto/sampler station.
The samples are analysed for the various elements of interest using ICP-MS. All extraction apparatus and
test tubes from the instrument are disposed after analysis.
Till and stream sediment samples were deslimed, disaggregated and screened in the field under the
supervision of the writer using continuous water supply and a stainless steel mesh screen (1/4-inch;
approximately -6mm mesh). Coarse rejects were saved for percentage estimates in the field of pebble
lithologies. At Vancouver Indicator Processors Inc. (VIPI), the deslimed samples were wet screened at 0.5 mm
and 0.25 mm and a heavy mineral concentrate made from the -0.5+0.25 mm fraction by magnet and heavy
liquids. Wet screening was carried out on two 30 inch Vibroscreens manufactured by Kason Corporation and
operated in a cascade fashion. Samples were centre-fed onto a 0.5 mm screen and the underflow directed onto a
0.25 mm screen. The -0.25 mm material was trapped in a settling pan. All samples were dried. The magnet
used is a permanent type magnetic separator operating at about 2.1 Tesla, and manufactured by Outukumpu
Technology Inc. The weak and strong magnetic fractions were combined and passed on for heavy liquid processing. Heavy liquid processing was carried out at the Exploration Laboratory of Teck Cominco Limited in
Vancouver, using a two-stage process in which the sink from tetrabromoethane is further separated in methylene
iodide. No fractions were discarded, and remain in storage at VIPI. Heavy concentrates were taken by VIPI to
KIM Dynamics for microscopic examination. Samples were received at VIPI on October 8 and 16 and the
-14-
concentrates sent on for observation on November 4, 2002. A report by VIPI which includes the foregoing
procedure and results and a report by KIM Dynamics (Kiridzija, 2002) are on file with Gitennes Exploration Inc. in
Vancouver.
DATA VERIFICATION
No data verification procedures were applied to the geochemical sampling. The writer received all
analytical data directly in electronic files submitted by the labs to Gitennes, and is responsible for compiling and
interpreting this data. The writer does not believe that rigorous data verification is required for the work done to
date, but that this situation will change should any drilling be undertaken.
INTERPRETATION AND CONCLUSIONS The writer's interpretation of bedrock geology is shown on Figure 5. The main bedrock features are a
diabase ring dyke complex which in part underlies the Badger Property, and a diabase sill that crops out on the
southern portion of the property. Other diabase sills and dykes of apparently limited extent are present within the
ring dyke. Otherwise, Archean bedrock consists of foliated to gneissic felsic rocks. The diabase intrusions are
positive topographic features affecting the distribution of Pleistocene glacial deposits.
Although PGE mineralization was not discovered on the Badger Property, the writer believes the MMI
results indicate the presence of discrete geochemically-distinct bedrock intrusions directly associated with the
Keating anomalies. Including the Black Hole, all anomalies sampled have Mg-depletion closely associated with
the magnetic target. Rb and to a lesser extent Ti are also anomalous, but may be elevated or depressed when
compared to Mg. The writer believes that MMI-D sampling is indicating fundamental changes in bedrock
lithology, as would be expected when small geochemically distinct bodies intrude an essentially homogenous
granitoid country rock. No unequivocal indicator minerals were observed in the till and stream sediment samples.
This suggests the possibility that such intrusions are not kimberlites. However, the complex Pleistocene
geological environment hampers the suitability of surficial material for finding indicator mineral dispersion trains.
RECOMMENDATIONS The writer recommends drilling the Black Hole anomaly with at least two core holes. One should be
vertical in the centre of its magnetic response. The second should be an inclined hole at no less than a -450 dip to
traverse from north to south the entire width of the magnetic anomaly. Total meterage for these holes should be
250 metres. A budget for this work is given in Table 6. In the writer's opinion, additional geophysical surveys will
not serve to better discriminate or identify the source of the target, and that a programme of core drilling is
warranted.
Additional work on the Badger Property will be contingent on this drilling. Assuming positive results, the
other Keating anomalies need to be covered by cut grid lines spaced no greater than 50 metres and surveyed
with magnetometer and detailed (25-metre-spaced) MMI-D sampling. In the case of Anomaly 13470B, this work
should take place in winter to ensure proper coverage over the wet lands immediately north of the Keating target.
-15-
Table 8. Proposed Budget for the Badger PropertyCATEGORY
AssayingAssaying
Camp (room b board)CommunicationsContract geology
DrillingFuel
Mob/DemobVehicle
SubtotalGST
SubtotalContingency
Total
RATE200 samples @ S15 (Au/Pt/Pd fire assay)10 samples @S1500 (diamond extraction)
14 days @ /diem
12.5 days @ SSOO/diem500m @ SSO/metre
SISOO/month
/"/o
1007o
COSTS3,000
815,000S4,000
520010000
25,000S500
S8,00051,500
567,200S4.704
S71,904S7.190
S79,094
Signed and sealed this 9 day of April, 2003.ia Vancouver, British Columbia, Canada:
and Sealed by)
James R. Foster, H.B.Sc., P.Geo.
Registration Number 27413
-16-
REFERENCES
Avalon Ventures Ltd., 2002: Legris Lake Palladium-Platinum Project, Thunder Bay, Ontario; Avalon Ventures website http://www.avalonventures.com/legrislake01.html.
Avalon Ventures Ltd., 2002: Wolf Mountain Platinum-Palladium Project, Leckie Lake Area, Ontario; Avalon Ventures website http://www.avalonventures.com/wolf01 .html.
Birrell, R. D. and Mann, A. W., 1998: Mobile Ions in Weathering Environments; Geochemistry Research Centre Workshop Course Notes Version 98-01.
Hart, T. R., 2000: Precambrian Geology, Garden Lake Area; Ontario Geological Survey Open File Rept. 6037, 82 p.
Jackson, J. E. and Dyer, R. D., 2000: Garden - Obonga Lake Area High Density Lake Sediment and Water Geochemical Survey, Northwestern Ontario; Ontario Geological Survey Open File Rept. 6009, 107 p.
Keating, P.; 1995: A simple technique to identify magnetic anomalies due to kimberlite pipes; Explor. Mining Geol., Vol. 4, No. 2, pp 121-125.
Kiridzija, M., 2002: Notes on procedures and results of the observations of the samples; private report prepared for Gitennes Exploration Inc.
Milne, V. G., 1964: Garden Lake Area; Ontario Dept. Mines Geol. Rept. No. 25, 21 p. Accompanied by Map No. 2058 (coloured) - Garden Lake area, Thunder Bay District. Scale 1 inch to 1 mile (East half, and west half).
Mollard, D. G., 1981: Gull River Area (NTS 52H/NW), District of Thunder Bay; Ontario Geological Survey, Northern Ontario Engineering Terrain Study 25, 26 p. Accompanied by Data Base Map 5049, Scale 1:100,000.
Mollard, D. G., 1981: Heaven Lake Area (NTS 52H/SW), District of Thunder Bay; Ontario Geological Survey, Northern Ontario Engineering Terrain Study 41, 34 p. Accompanied by Data Base Map 5051, Scale 1:100,000.
Ontario Geological Survey, 2000: Garden - Obonga Lake Area Lake Sediment Survey: Gold and PGE Data; Ontario Geological Survey Open File Rept. 6028, 76 p.
Ontario Geological Survey, 2000: Airborne magnetic and electromagnetic surveys, Garden - Obonga area; Ontario Geol. Survey Map 82 106, scale 1:20,000.
Ontario Geological Survey, 2000: Airborne magnetic and electromagnetic surveys, Garden - Obonga area; Ontario Geol. Survey Map 82 110, scale 1:20,000.
Ontario Geological Survey, 2000: Airborne magnetic and electromagnetic surveys, total magnetic field and electromagnetic anomalies, Garden - Obonga area; Ontario Geol. Survey Map 82 125, scale 1:50,000.
Ontario Geological Survey, 2000: Airborne magnetic and electromagnetic surveys, shaded image of the second vertical derivative of the magnetic field and Keating coefficients, Garden - Obonga area; Ontario Geol. Survey Map 82 133, scale 1:50,000.
Osmani, L. A., 1991: Proterozoic mafic dike swarms in the Superior Province of Ontario; in Geology of Ontario, Ontario Geological Survey Special Volume 4, Part 1, pp. 661-681.
Pell, J., 1998: Kimberlite-hosted diamonds; in Geological Fieldwork 1997, British Columbia Ministry of Employment and Investment, Paper 1998-1, pp24L-1 - 24L-4.
Schneiders, B. R., Scott, J. F., Smyk, M. C., Parker, D. P. and O'Brien, M.S., 2002: Report of Activities, 2001, Resident Geologist Program, Thunder Bay South Regional Resident Geologist Report: Thunder Bay South District; Ontario Geological Survey Open File Report 6081, 44p.
Sutcliffe, R. H., 1991: Proterozoic geology of the Lake Superior area; in Geology of Ontario, Ontario Geological Survey Special Volume 4, Part 1, pp. 627-658.
Tomlinson, K. Y., Hughes, D. J., Thurston, P. C., Davis, D. W. and Keays, R. R., 1997: The greenstone belts of the central Wabigoon Subprovince: geochemistry, petrogenesis and tectonic setting; 1997 Western Superior Transect Workshop Volume, pp. 83-88.
Zoltai, S. C., 1965: Glacial features of the Quetico - Nipigon area, Ontario; Can. J. Earth Sci. Vol. 2, pp. 247-269.-17-
CERTIFICATE of QUALIFIED PERSQN ,-. r; A '.] 'g v i.; J- : ;. --
l, James Rutherford Foster, P. Geol., do hereby certify that:
1. l am a geologist residing at 301-7300 Moffatt Road, Richmond, British Columbia, Canada, V6Y 1X8;
2. l graduated from the University of Waterloo with an Honours Bachelor of Sciences degree in Earth Sciences and Geography in 1979;
3. l have practised my profession 26 years since 1976;
4. l have read the definition of "qualified person" as set out in National Instrument 43-101 and certify that by reason of my education, affiliation with the Association of Professional Engineers and Geoscientists of British Columbia (Registration Number 27413) and past relevant work experience, l fulfil the requirements to be a qualified person;
5. . l am responsible for the preparation of this Technical Report titled "Assessment Work Report on the September 2002 Exploration Programme for the Badger Property, Garden-Obonga Area, District of Thunder Bay, Ontario, NTS 52H/5, 52H/11" and dated March 31, 2003. l visited the property for a total of 24 days in 2002.
6. l have not had prior involvement with the property that is the subject of this Technical Report;
7. As of the date of this certificate, l am not aware of any material fact or material change with regard to the Badger Property that would make this Technical Report misleading;
8. l am Vice President and an Officer of Gitennes Exploration Inc. l own 2,000 shares in the capital stock of Gitennes Exploration Inc. and have been granted options to acquire shares in Gitennes Exploration Inc.;
9. l have read National Instrument 43-101 and Form 43-101F1, and the Technical Report has been prepared in compliance with that instrument and that form;
10. l consent to the filing of the Technical Report with any stock exchange and other regulatory authority and any publication by them for regulatory purposes, including electronic publication of the Technical Report in the public company files on their websites accessible by the public.
Dated the 9th day of April 2003, in the City of Vancouver, British Columbia.,'. ' ' ; ", '*'
*,' 'i. ' - '
(Sicjned arad Sealed bty)\ - . .' James R. Foster, P. Geo. Registration Number 2741
-18-
sb
3.
N
WffN
- < approx 375 knO -
GITENNES EXPLORATION INC.Badger Property
Location MapScale as shown Marl 8 2003 Figure 1
"orner post positions for most claims have been located with Garmin 12 GPS. Those claims not verified are shown as depicted on the relevant claim sheets.
.GITC'NNES EXPLORATION INC. ; ' Badger Property
Claim Map-June 2002
Scale: As shown | NTS: 52H/11,12 | FIGURE 2
GITENNES EXPLORATION INC.Badger Property
Operation Treasure Hunt - Garden - Obonga Area Total Field Magnetics
i "X. f fI'oVl'lJCWlNt'LX*y ri—"-— -^ ii- .1 H tOSItR J
Lake Superior
After Ontario Geological Survey http://www.mndm.gov.on.caAnndmAnines^esgeo^northwestAbsA3eo-e.asp
Legend
Proterozoic (Southern Province)) Rocks
^^^H Alkaline intrusive rocks
Mafic intrusive (diabase) dikes tilffPPM ancj s j|| s
Keewenawan mafic volcanic and associated sedimentary rocks
l j Sibley Group sedimentary rocks
Ultramafic to mafic intrusive rocks
Archean (Superior Province) Rocks
^^^H Sedimentary racks, some ^^^ highly metamorphosed
imH Intermediate to felsic volcanic rocks
^^^| Mafic to intermediate volcanic rocks
l l Felsic intrusive rocks and gneisses
GITENNES EXPLORATION INC. Garden - Obonga Properties
Regional Geology - Thunder Bay South Mining DivisionFigure 4
f
GNEISS
Kennah Lake .
GNEISS 2\
13470B 7GNEI3S2/
Badger Lakevarvedysilts ,
' o
^— ™ —: -t.'— — — - .
-54825pg -j__, __3___; ___f—(y s- ti .-.F /
13320D r-
- GNEISS 123120A GNEISS
l8a Massive felsic intrusive8c Foliated to gneissic felsic intrusive12 Diabase, unsubdivided12a Diabase, cooling cracks
13161A Positive Keating Anomaly'3270A Negative Keating Anomaly
G1TENNES EXPLORATION INC.
Badger Property Geological Interpretation
Scale 1:12,500 Mar 18 2003 Figure 5
5485500-
54B500&
54B4500-
Keating Anomaly
' l GITENNES EXPLORATION INC, J -" ,^ lj: "' 1"' : Badger Property
~-,~Badger Grid Contoured Ground Magnetics '^^ Scale 1:10,000 Feb 2003 Figure 6 PSCIEN'"
)
5435200-
5485100-
5485000-
5484900-
5484800-
5484700-
-5485200Mg (ppb)
18000
16000
14000
12000
10000
8QOQ
6000
4000
onnn
G1TENNES EXPLORATION INC. Badger Property - Black Hole Anomaly
Contoured MMI Mg (ppb) -f- Contoured Ground Magnetics Scale 1:6,000 February 2003 Figure 7
)548530CT
5435200
5485100 X
5485000-
GITEI^NES EXPLORATION INC. Badger Property - Black Hole Anomaly
Contoured MMI Rb (ppb) + Contoured Ground Magnetics Scale 1:5,000 February 2003 Figures
5485200 x
5485100 X
5485000
5484900-
5484800
5484700
GfTENNES EXPLORATION INC.Badger Property - Black Hole Anomaly
M Ml Ti (ppb) + Contoured Ground MagneticsScale 1:5,000 February 2003 Figured
)
5485300-
5465200)
5485100
5485000-
5484900-
5484800
54847DO
X*1
lX
o3
o o(D
o O (Qto
o oto
o oCOto
o oOJw
1w4)C
LU
.
S UJS
x#— ##
oCD*—c-i
o fe
o
ima o
•5485300
5485200
5485100
•5485000
5484900
5484800
5484700
GITENNES EXPLORATION INC.Badger Property - Black Hole Anomaly
MMI Ni (ppb) * Contoured Ground MagneticsScale 1:5,000 February 2003 Figure 10
)
548530W
548520W
548510m
S4850QN
548490CH
548480CH
54S470W
^5485300
GITENNES EXPLORATION INC.Badger Property - Black Hole Anomaly
MMI Cr (ppb) + Contoured Ground MagneticsScale 1:5,000 February 2003 Figure 11
)
548530
548520CW
548510CH
548500W
5484900
548480CH
548470N
^5485300
GfTENNES EXPLORATION INC. Badger Property - Black Hole Anomaly
MMI Nb (ppb) -f Contoured Ground Magnetics Scale 1:6,000 February 2003 Figure 12
5485050
5485000
5484950
5484900
484850
5484801
5484750
m to
ED
E oID
E o in
Ground magnetics data is superimposed on Keating anomlies
GITENNES EXPLORXlON INC.Badger Property - Anomaly 13320D
Contoured Corrected Ground Magnetics Scale 1:2,000 February 2003 Figure 13
o w o in to
os-
-505
-100 S
-1505
-200 S
-250 5
-300
SmV
S(N
-os
owT
Mg (ppb)
-SOS H•100 S
•150 S
-2005
-2505
17000
15000
i 13000
11000
9000
7000
5000
3000
1000
-300 S
dto ro
MM! data is superimposed on ground magnetics contoursGITENNES EXPLORATION INC.
Badger Property -Anomaly 1332DDContoured MMI Mg (ppb) + Contoured Ground Magnetics
Scale 1:2,000 February 2003 Figure 14
osj
-so a
-100 S|
-150 a
-200
-250 ffl
-300
Rb (ppb)
.•yv.'iNwui.i. A \f (——--2-——-" i \ .1 n. FOSTER
O Oing 27.113
GITENNES EXPLORATION INC. Badger Property -Anomaly 13320D
Contoured MMI Rb (ppi)) * Contoured Ground Magnetics Scale 1:2,000 February 2003 Figure 16
os
-60S
-100 S-
-150 S-
-200 S
-250 S
-300 S
O Iftm
35o to
ES
MMI data is superimposed on magnetic contours
o a
1.
-OS
-SOS
-100 S
-150 S
^2003
-250 S
-3005
c'ti f* 1
GITENNES EXPLORATION INC.Badger Property - Anomaly 13320D
MMI-D TJ (ppb) * Contoured Ground MagneticsScale 1:2,000 February 2003 Figure 16
-SOS
-100 S
-150 S
-200 S
-250 S-
-300 S-
MMI data is superimposed on magnetic contours
t ., H FOS1U1 5
GITENNES EXPLORATION INC.Badger Property -Anomaly 13320D
MMI-D Co (ppb) * Contoured Ground MagneticsScale 1:2,000 February 2003 Figure 17
-50 ST
-100 S
-150 S-
-200 S
-250 S-
-300 S-
GITENNES EXPLORATION INC.Badger Property -Anomaly 13320D
MMI-D Nr (ppb) + Contoured Ground MagneticsScale 1:2,000 February 2003 Figure 18
-50S1
-100:
-150S
-200&
-250S
-300&
I
-50S
A
-100S
150S
200S
250S
300S
irf V^s' (tjs,'^Xi t" wiw ixV "^
MMI data is superimposed on magnetic contours
GITENNES EXPLORATION INC.Badger Property -Anomaly 13320D
MMt-D Nb (ppb) * Contoured Ground MagneticsScale 1:2,000 February 2003 Figure 19
5486950-
5486900-
54868501
5486800-
5486750-
O m
Keating anomlies are superimposed on ground magnetics data
r548695C
-548690C
-5486850
-6486800
5486750
6ITENNES EXPLORATION INC. Badger Property -Anomaly 13470B
Contoured Corrected Ground Magnetics + Keating Anomlies Scale 1:2000 February 2003 Figure 20
nT
- 1000
-950
-900
-850
-800
-750
-700
-650
-600
-550
-500
5487000
5486950
5486900-
5486850
5486800
5486750
MMI data is superimposed on Keating anomalies and ground magnet
GITENNES EXPLORATION INC.Badger Property -Anomaly 13470B
Contoured MMI Mg Data * Contoured Ground MagneticsScale 1:2.000 February 2003 Fiaure 21
5487000
548695
5486900
5486850
5486800
5486750
Om
MMI data is superimposed on Keating anomalies and ground magnet!
5487000
Rb {ppb)
5486950
5486900
5486850
5486800
36
32
28
24
20
16
12
5486750
GITENNES EXPLORATION INC. Badger Property -Anomaly 13470B
Contoured MMI Rb (ppb) + Contoured Ground Magnetics Scale 1:2,000 February 2003 Figure 22
5487000-
5486950-
5486900-
5486850-
5486800-
5486750-
f o o o o o 0 S s CO CO CO CO CD
C) 0 5 O CI S
XXX*"
u
ss
^X
X
x J
x*
lv•p m, ^•^x
-S ———— 5^-Tffi X
L ^l x\^^
feA
feX
^* 'y.
^ ^^ ^i*vf^\i'\ ^ift*^*•^ r^x 0 x ^
.*^a^. ^x~~-^
c^\ V --—"- ('C ri. v:^
x "
x^X
X
x K^
\xlV\1^1 x^f
e^yr^x© iX-x *
^\ ———
\
\
-5487000
-5486950
-5486900
-5486850
-5486800
-5486750
i i 0 i 0 i m o m o LO o S m m tt (0 f*,
co oo 35 co eoco to m rt m m
E E E E E0 s s s aT™ (^| CO "ij1
MM! data is superimposed on Keating anomalies and ground magne
Ti (ppb)
C 50 to 228 B 30 to 50 T 20 to 30 A 5 to 2D X 1 to 5
^-^
GITENNES EBadger Property
MMI Ti (ppb) * Contoured Scale 1:2,000 Ma
,- i^s'suiS.fi AM lV*\ L i—— ———— K 1 —— *LIG5 *i'/" i"^"\ "-v
'^1?^S^. )^^srXPLORATION INC. -Anomaly 13470A Ground Magnetics
re h 2003 Figure 23
a O O O O O o 55 a to p•tf 1Q in ffi OJ f~ Go co CO GO co coo o o o o o
5487000-
5486950-
5486900-
5486850-
5486800-
5486750-
XXX— : — |-
/
/
#X
Xy
\'
x^
7
fyk '
^x
#x
V
^ X* ^^^* ^k.T|
. — . x :^^rfP ** - xca|
,*xx
t^m \
1 /' "- - ^ \
* ** "l Jx ^ -^— ^ V^iyPJ
' x "N ,
V xS,^
^ ^ jr y
) ^^ V^"
®^ -X--X*
P*v
s\
l-
-5487000
-5486950
tt-5486900
-5486850
-5486800
-5486750
^ 0 ^ ^ ^ i in o 55 5 in o•* m in (p to r^-00 CO OD 00 00 COTT- 1— V" T" T— -1—CO co CO tO ro cO
E E E E EO 0 o o o
O O O O
MMI data is superimposed on Keating anomalies and ground magnetics /,A* x
^Ti (ppb)
5 to 10 4 to S
X 3to4
*/* J /I Jf sl
^Sp^1-,
jx-fosTrR*?7413
s^LF\ k^ix/i,*
GITENNES EXPLORATION INC. Badger Property - Anomaly 13470A
MMI Ni (ppb) + Contoured Ground Magnetics Scale 1:2,000 March 2003 Figure 24
5487000-
5486950-
5486900-
5486850-
5486800-
5486750-
5487000
5486950
•5486900
-5486850
-5486800
5486750
EO
EO.o
EOo 01
EQo m
MMI data is superimposed on Keating anomalies and ground magnetics /'
GITENNES EXPLORATION INC.Badger Property-Anomaly 13470A
MMI Y (ppb) + Contoured Ground MagneticsScale 1:2,000 March 2003 Figure 25
5460000
Kennafr
1221206
5485000
Lake
1221195m
T—
CM CM
-h
1245616
17558-1
124561
1241565 l?A
Badger Lake1241564 7
1241566
1241 562
Tarrison
Vi 24561817529
1245617 x
Nt
w
TIM or Stream Sediment
GITENNES EXPLORATION INC.
^ ^. Badger Property 3 Vill:and Stream Sediment Sample Sites
^aV 1:12,500*S^——-—— Feb102003 Figure 26
319200 319250 319300 31935D 319400
5486050
5486000
548595O
5485900
5485850
5485800- -
5485750
Ground magnetics data is superimposed on Keating anomliesGITENNES EXPLORATION INC.
Badger Property -Anomaly 13500AContoured Corrected Ground Magnetics
Scale 1:2,000 March 2003 Figure 27
5486050
5486000-
5485950*
548590O
548565O
5485800-
5485750
E o E o in o o o m
-5486050
5486000
5485950 Mfl (ppb)
-5485900
5485850
-5485800
-5485750
5485700
21000
19000
17000
15000
13000
11000
9000
7000
5000
3000
1000
MMI data is superimposed on Keating anomlies and magnetic contours
GITENNES EXPLORATION INC. Badger Property - Anomaly 13500A
Contoured MMI-D Mg (ppb) + Contoured Ground Magnetics Scale 1:2,000 March 2003 Figure 28
5486050
5486000
5485950-
548590O
548585O
5485800
5485750
Rb{ppb)
MMI data is superimposed on Keating anomlies and magnetic contours
GITENNES EXPLORATION INC. Badger Property -Anomaly 13 600 A
Contoured MMI-D Rb (ppb) + Contoured Ground Magnetics Scale 1:2,000 March 2003 Figure 29
5486050-
548600O
5485950-
5485900
5485850
5485800-
5485750-
-5486050
16
MM1 data is superimposed on Keating anomlies and magnetic contours
GITENNES EXPLORATION INC. Badger Property - Anomaly 13500A
Contoured MMI-D Ti (ppb} + Contoured Ground Magnetics Scale 1:2,000 March 2003 Figure 30
5486050-
5486000-
5485950
5485900
5485850-
5485800-
5485750-
MMI data is superimposed on Keating anomlies and magnetic contours
GITENNES EXPLORATION INC.Badger Property - Anomaly 13500A
MMI-D Ni (ppb) + Contoured Ground MagneticsScale 1:2,000 March 2003 Figure 31
Badger Grid Line 400E MAXMIN 100-m cable12(-T
14080HZ quadrature 14080Hzirvphase 71 11 Hz quadrature 71 11 Hz in-phase
-350 -300 -250 -2DO -150
.-C:k3fa rtGoWysia\OaaiaManWHbaag1Q04db inefavup: L4OO 200&04/10
Badger Grid Line 500E MAXMIN 100-m cable
14080H?quadralure 14080HZ in-phase
-- — - 7111 Hz quadrature
-350 -.300 -250 -200 -150 -100 -50
2003M/10
Badger Grid Line 600E MAXMIN 100-m cable
-350 -300 -250 -200 -150 -100
C&tormMtSai^Qt^^ tint/group-- L6OO
-50
- 14080HZ quadrature- 14080HZ in-phase- 7111 Hz quadrature- 7111Hz in-phase
20Q3W1Q
GITENNES EXPLORATION INC.Badger Property
Black Hole MAXMIN Profiles (100-m cable)Figure 32
Badger Grid Line 400E MAXMIN 150-m cable
14080HZ quadrature 14O80Hz in-phase 71 11 Hz quadrature 71 11 Hz in-phase
-375 -350 -300 -250 -200 -150 -100 -50
database: C:\GOannoliiataillitBoopftyvlcalOasiaMontafWbadg150.ydti 9netgmup:LMD
50 75
20C&04/10
Badger Grid Line 500E MAXMIN 150-m cable
UOSOHz quadrature 14080H? in-phase 71 11 Hz quadrature 71 1 1 Hz in-phase
-300 -250 -200 -150 -100 50 75
Oat^)aae:C:\Qt^nnga\BatisB^Geoptysic^OaslaMorit^\Htiat)g15O.gdb too/group: LBOO
Badger Grid Line 600E MAXMIN 150-m cable
14080HZ quadrature 14080Hz in-phase 7111 Hz quadrature 7111 Hz in-phase
-300 -250 -200 -150 -100 50 75
databMe:C^l^nnes\Badg^VSeoptytfcs\OeafeMotit^\Hbadg150.yib too/group;LOGO 2OO3/04/10
GITENNES EXPLORATION INC.Badger Property
•So Black Hole MAXMIN Profiles (150-m cable)Figure 33
APPENDIX l
Analytical Certificates
EXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 CanadaPhone: 604 984 0221 Fax: 6049840218
y. GITENNES EXPLORATION INC. 2390 -1055 W. HASTINGS ST. VANCOUVER BC V6E 2E9
Page#: 1 Date : 25-Nov-2002
Account: LCY
CERTIFICATE VA02006006
Project: VI PI Screened Fines P.O. No:This report is for 26 samples submitted to our lab in North Vancouver, BC, Canada on 16-NOV-2002.The following have access to data associated with this certificate:
JERRY BLACKWELL
SAMPLE PREPARATIONALS CODE
WEI-21 LOG-22 SPL-21 PUL-31
DESCRIPTION
Received Sample Weight Sample login - Red w/o BarCode Split sample - riffle splitter Pulverize split to 85"7o <75 um
ANALYTICAL PROCEDURESALS CODE
Au-AA23 ME-ICP41
DESCRIPTIONAu 30g FA-AA finish 34 element aqua regia ICP-AES
INSTRUMENT
AAS ICP-AES
To: GITENNES EXPLORATION INC. ATTN: JERRY BLACKWELL 2390 -1055 W. HASTINGS ST. VANCOUVER BC V6E 2E9 This is the Final Report and supersedes any preliminary report with this
certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release.
Signature:
ALS CliemexEXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 CanadaPhone: 604 984 0221 Fax: 6049840218
):GITENNES EXPLORATION INC. 2390 -1055 W. HASTINGS ST. VANCOUVER BC V6E 2E9
Project: VIPI Screened Fines
Page # : 2 - ATotal # of pages : 2 (A-C)
Date : 25-Nov-2002Account: LCY
MethodAnolyteUnits
Sample Description LOR
429-17527430-17530431-17559432-17529433-17551
434-17552435-17553436-17554437-17555438-17556
439-17557440-17558441-17560442-16581443-16582
444-16923445-16924446-16925447-16926448-16927
449-16928450-17531451-17545452-17546453-17547
454-17548
WEI-21RecvdWt
kg0.02
0.120.140.160.460.10
1.380.800.601.261.34
1.500.801.420.480.40
0.260.260.320.280.70
0.200.420.240.240.30
0.16
AU-AA23Au
ppm0.005
O.005O.005O.005O.0050.005
O.005O.005O.005O.005O.005
O.0050.005O.0050.005O.005
0.005O.005O.005O.005O.005
O.005O.005O.005O.005O.005
O.005 ,
ME-ICP41Ag
ppm0.2
O.20.2O.2O.2O.2
O.2O.2O.2O.2O.2
O.20.2O.2O.2O.2
O.20.2O.2O.2O.2
O.2O.2O.20.2O.2
O.2
ME-ICP41Al
CERTIFICATE OF
ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41 ME-ICP41
As B Ba Be Bl Ca•X. ppm ppm ppm ppm ppm %
0.01
1.681.901.530.531.22
0.790.680.710.720.97
0.831.531.011.762.37
1.170.990.920.490.71
0.510.790.850.920.77
1.12
2 10 10 0.5 2
^ ":10 70 O.5 ^^ *:10 50 O.5 ^^ ^0 30 0. 5 ^^ *^10 70 0. 5 ^40 •elO 110 0. 5 ^
^ t10 80 O.5 ^^ *^10 100 0. 5 ^^ "^10 70 0. 5 ^^ ^0 50 0. 5 ^^ ^0 80 O 5 ^
^ -510 70 0. 5 ^^ •s10 40 0. 5 ^^ ^0 70 0. 5 ^^ *10 40 0. 5 <2^ <10 40 0. 5 <2
^ <10 30 <0.5 <2^ <10 30 0. 5 <2*2 <10 20 0. 5 <2^ <10 20 0. 5 <2^ <10 40 0. 5 <2
^ <10 20 0. 5 <2^ <10 30 0. 5 <2^ <10 30 0. 5 <2^ <10 30 0. 5 <2^ <10 30 0. 5 <2
^ <10 30 O.5 <2
0.01
1.060.860.920.281.01
0.480.380.440.430.49
0.510.600.570.730.95
0.400.240.520.290.38
0.280.290.270.300.35
0.42
ANALYSIS
ME-ICP41 ME-ICP41Cd Co
ppm ppm0.5 1
O.5 24O.5 210. 5 180.5 290. 5 19
O.5 7O.5 160.5 12OS 6O.5 12
0. 5 80.5 16O.5 130. 5 18O.5 28
0. 5 220.5 15O.5 19O.5 17O.5 20
0. 5 90.5 17O.5 13O.5 180. 5 22
0. 5 20
VA02006006
ME-ICP41Cr
ppm1
109997992116
7883857785
9763714543
5532403229
2630283231
37
ME-ICP41Cu
ppm1
438256735460
3319191232
1249385483
4032221953
730262642
38
ME-ICP41Fs'X.
0.01
4.755.955.2711.458.06
2.075.723.921.713.30
2.253.963494.395.13
5.333.483.733.554.49
1.544.033.224.484.74
5.15
A L S ChemexEXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 CanadaPhone: 604 984 0221 Fax: 604 984 0218
o: GITENNES EXPLORATION INC. 2390 -1055 W. HASTINGS ST. VANCOUVER BC V6E 2E9
Project: VIPI Screened Fines
Page#: 2-BTotal # of pages : 2 (A - C)
Date : 25-Nov-2002Account: LCY
CERTIFICATE OF ANALYSIS VA02006006
KUthodAnal/teUnit.
Sample Description LOR
429-17527430-17530431-17559432-17529433-17551
434-17552435-17553436-17554437-17555438-17556
439-17557440-17558441-17560442-16581443-16582
444-16923445-16924446-16925447-16926448-16927
449-16928450-17531451-17545452-17546453-17547
454-17548
ME-ICP41
Gappm10
1010102010
101010
•c10
10
1010101010
1010101010
^010101010
10
ME-ICP41 ME-ICP41
Hg Kppm %
1 0.01
•el 0.04^ 0.05•:1 0.05^ 0.05•0 0.08
^ 0.05^ 0.04•O 0.04^ 0.03^ 0.05
•d 0.04•si 0.13<1 0.04<1 0.05
1 0.06
^ 0.05<1 0.05<1 0.03*:1 0.03<1 0.11
<1 0.02<1 0.06<1 0.03^ 0.06<1 0.05
^ , 0.04
ME-ICP41La
ppm10
•:10<10<10^0<10
<101010
*:10•C10
<101010
•c10t10
<1010
<101010
*:10<10<10<1010
ME-ICP41
Mg%
0.01
0.300.610.320.360.84
0.360.340220.270.51
0.270.710.470.750.98
0.680.640.520.560.76
0.200.620.450.640.70
0.63
ME-ICP41 ME-ICP41
Mn Mo
ppm ppm5 1
657 -d473 ^442 ^560 ci1035 3
197 -:1383 t1245 *M155 *:1280 -:1
260 ^362 -O340 *:1317 <1380 1
395 -:1286 <1340 ^393 <1388 <1
223 "d307 <1220 -M306 <1408 <1
381 <1
ME-ICP41Na14
0.01
0.260.220.230.030.12
0.100.070.090.090.10
0.110.120.120.170.26
0.080030.110.040.04
0.050.040.050.040.05
0.08
ME-ICP41
Nl
ppm
1
4063367248
2143281734
1940344978
6346504549
1352415563
56
ME-ICP41P
ppm10
420260390100340
200180200210260
200520320360190
160280270300550
230290240390360
330
ME-ICP41Pb
ppm2
54336
33^24
33^2^
34^32
2^44^
2
ME-ICP41S
140.01
^.010.01O.010.012.12
0.010.01^.010.01O.01
0.01O.01O.01O.01O.01
O.01O.010. 01*^0.01*:0.01
O.01•:0.01O.01O.01^.01
ME-ICP41Sb
ppm2
35362
^44^^
224^^
2^2^2
^^222
3
ME-ICP41
Seppm
1
22222
22212
12222
22112
11122
2
ME-ICP41
Srppm
1
322728419
1510131314
1520172626
1271679
797710
12
ALS ChiemexEXCELLENCE IN ANALYTICAL CHEMISTRYALS Canada Ltd.212 Brooksbank AvenueNorth Vancouver BC V7J 2C1 CanadaPhone: 604 984 0221 Fax: 604 984 0218
xGITENNES EXPLORATION INC. 2390 -1055 W. HASTINGS ST. VANCOUVER BC V6E 2E9
Project: VI PI Screened Fines
?age#: 2-CTotal # of pages : 2 (A - C)
Date : 25-Nov-2002Account: LCY
CERTIFICATE OF ANALYSIS VA02006006
MethodAnalyte
UniteSample Description LOR
429-17527430-17530431-17559432-17529433-17551
434-17552435-17553436-17554437-17555438-17556
439-17557440-17558441-17560442-16581443-16582
444-16923445-16924446-16925447-16926448-16927
449-16928450-17531451-17545452-17546453-17547
454-17548
ME-ICP41Tl•)4
0.01
0.470.480.490.970.32
0.170.550.450.170.25
0.210.250.260.260.31
0.360200.290.180.23
0.120.230.220.250.27
0.31
ME-ICP41 ME-ICP41Tl U
ppm ppm10 10
*10 10t10 10^0 10^0 20*10 10
•;10 ^0^0 10^10 10•clO ^0•C10 ^0
^0 ^0*10 10<10 10•:10 10<10 10
^0 10<10 <10<10 10^0 <10<10 10
^0 <10<10 10<10 10^0 10<10 10
^0 , 10
ME-ICP41V
ppm1
3764834491225335
125549365110223
151209233307309
382207240231274
98287224323338
393
ME-ICP41 ME-ICP41W Zn
ppm ppm10 2
^0 6110 82
•:10 7010 14610 82
^0 32^0 82^0 67^0 31^0 46
•:10 41^0 52•^0 39^0 5320 72
^0 69^0 52^0 46<10 43<10 62
^0 19<10 54^0 40<10 59<10 62
^0 64
XRAL XRAL LaboratoriesA Division of SGS Canada Inc.
1885 Leslie Street Don Mills, Ontario Canada MSB 3J4 Telephone (416) 445-5755 Fax (416) 445-4152 CERTIFICATE OF ANALYSIS
Work Order: 069888
To: Gitennes Exploration Inc Attn: Jim Foster.1055 West Hastings Street Suite 2390 VANCOUVER B.C. V6E 2E9
Date 30/09/02
Copy 1 to
P.O. No. Project No. No. of Samples Date Submitted Report Comprises
80 Soil(MMI) 16/09/02 Cover Sheet plus Pages 1 to 4
Distribution of unused material: Pulps: Store Rejects: Store
Certified By
e Souza, General Manager laboratories
ISO 9002 REGISTERED
ISO 17025 Accredited for Specific Tests. S.C.C. No. 456
Report Footer:
Subject to SGS General Terms and Conditions
L.M.R. = Listed not received l.S. = Insufficient Sample n.a. = Not applicable - = No result *INF = Composition of this sample makes detection impossible by this method M after a result denotes ppb to ppm conversion, "/o denotes ppm to 'fo conversion
Member of the SGS Group (Societe Generate de Surveillance)
XRAL XRAL LaboratoriesA Division of SGS Canada Inc.
Work Order: 069888 Date: 30/09/02 FINAL Page l of 4
Element. Method. Det.Lim.Units.
LIE-000L1E-025NL1E-050NL1E-075NL1E-100N
L1E-125N L1E-150N L1E-175N L1E-200N L1E-225N
L1E-250N L1E-275N L1E-300N L3E-075S L3E-050S
L3E-025SL3E-000L3E-025NL3E-050NL3E-075N
L3E-100N L4E-400S L4E-375S L4E-350S L4E-325S
L4E-300S L4E-275S L4E-250S L4E-225S L4E-200S
MgMMI-D
100ppb
132405380
131701218010460
8100710096608340
15300
1701019150106001561015730
13040126609690
1000011450
65704750
1600096708100
8450156101474057008300
TiMMI-D
1ppb
0CiCI
3CI
451
ci7
024
•Ci•Ci•CI
•CI2
CiO
5
2cici
32
ci1
1027
CrMMI-D
1ppb
CiCICICI<i
•ciCICI<l<l
1<].•ci<l*:i•ciCICI* l41CICI•ci<1<lCIci•ci
1
Co NiMMI-D MMI-D
1 3ppb ppb
ci C3ci <3ci C3ci 4CI C3
ci C3Ci C3Ci C3CI C3ci c3
2 C31 4
C 1 4Ci C3ci C3
CI C3ci c3CI C3ci C3ci c3
ci C3<l C3ci C3ci C3CI C3
Ci C3ci 4ci c3ci C3ci C3
RbMMI-D
1ppb
4527502832
4022354045
245
283935
4435262941
2935514250
5838465232
YMMI-D
0.1ppb
CO.lCO.lCO.lCO.lCO.l
CO.lCO.l
0.2CO.lCO.l
CO.l0.5
CO.lCO.lCO.l
CO.lCO.lCO.lCO.lCO.l
CO.lCO.lCO.lCO.lCO.l
CO.lCO.lCO.lCO.lCO.l
NbMMI-D
0.1ppb
CO.l0.10.10.2
CO.l
CO.lCO.lCO.lCO.lCO.l
CO.l0.2
CO.lCO.lCO.l
0.1CO.lCO.lCO.lCO.l
CO.lCO.lCO.lCO.lCO.l
CO.lCO.lco.iCO.l•co.i
PdMMI-D
0.1ppb
CO.lCO.lCO.lCO.lCO.l
CO.lCO.lCO.lCO.lCO.l
CO.lCO.lCO.lco.CO.
co.CO.CO.CO.CO.l
CO.lCO.lCO.lCO.lCO.l
CO.lCO.lCO.lCO.lCO.l
Member of the SGS Group (Societe Generate de Surveillance)
XRAL XRAL LaboratoriesA Division of SGS Canada Inc.
Work Order: 069888 Date: 30/09/02 FINAL Page 2 of 4
Element. Method. Det.Lim. Units.
L4E-175S L4E-150S L4E-125S L4E-100S L4E-075S
L4E-050SL4E-025SL4E-000L4E-025NL4E-050N
L4E-075NL4E-100NL450E-300SL450E-275SL450E-250S
L450E-225S*Blk BLANK*Std MMISRM12L450E-200SL450E-175S
L450E-150S L450E-125S L450E-100S L450E-075S L450E-050S
L450E-025SL450E-000L450E-025NL450E-050NL450E-075N
MgMMI-D
100ppb
46106300860081305840
97408880
170709030
10430
7730118109680
167605570
1118000018700127509360
7750571078809860
12820
84006750779065208270
TiMMI-D
1ppb
22
O94
O•Ci-Ci
21
5O
112
1•Ci•ci
33
22
•ci3
•Ci
O8612
CrMMI-D
1ppb
O•ci•CI•ci•ci
o•cio•ci
1•CI
1o
2•CI•ci0•cio•ci
o•ci•CI
o•CI
1oo•CI•ci
CoMMI-D
1ppb
O•CI•CI•CIoo•CIo•CI•ci
<l<l•ci<l<l<l<l20o•CI
<l<lo•CI<l<l<l•ci<l<l
NiMMI-D
3ppb
•C3<3<3•C3•C3
O<3<3O•C3
<3<3<3OO
•c 3o45O<3
O<3O•C 3O
<30<3O0
RbMMI-D
1ppb
3028373552
4845333432
3221363350
34•CI634329
3740362834
5121383038
YMMI-D
0.1ppb
•cO.l•CO.l•cO.l•CO.l•CO.l
•CO.l•CO.l•CO.l•CO.l•CO.l
•CO.l•CO.l*:0.l•co.l•CO.l
•CO.l•CO.l
0.5•cO.l•CO.l
•CO.l•cO.l*c0.1•CO.l•cO.l
•CO.l•cO.l•CO.l•cO.l<0.1
NbMMI-D
0.1ppb
0.1^.1•CO.l<0.1<0.1
<0.1•CO.l<0.1<0.1<0.1
<0.1•CO.l•CO.l•CO.l•CO.l
0.1•CO.l•CO.l^.1•CO.l
•CO.l•CO.l•CO.l•CO.l•CO.l
^.1•CO.l•CO.l^.1•CO.l
PdMMI-D
0.1ppb
•CO.l•CO.l•CO.l<0.1<0.1
<0.1<0.1•co.l<0.1<0.1
<0.1<0.1•CO.l•CO.l<0.1
<0.1<0.1
0.1•CO.l•cO.l
•CO.l0.2
•CO.l•CO.l•CO.l
•CO.l^.1•CO.l•CO.l•CO.l
Member of the SGS Group (Societe Generate de Surveillance)
XRAL XRAL LaboratoriesA Division of SGS Canada Inc.
Work Order: 069888 Date: 30/09/02 FINAL Page 3 of 4
Element. Method. Det.Lini. Units.
L450E-100NL5E-400SL5E-375SL5E-350SL5E-325S
L5E-300S L5E-275S L5E-250S L5E-225S L5E-200S
L5E-175S L5E-150S L5E-125S L5E-100S L5E-075S
L5E-050SL5E-025SL5E-000L5E-025NL5E-050N
L5E-075N L5E-100N*Dup LIE-000*Dup L1E-300N*Dup L4E-325S
*Dup L4E-025S*Dup L450E-150S*Dup L5E-375S*Dup L5E-075S*Blk BLANK
MgMMI-D
100ppb
654080005740
143907510
10020469078005410
11390
715013330860084306730
431011590103505470
12450
50908460
12540101207290
8280740058507100000
TiMMI-D
1ppb
•a•ci•CI
23
2•Ci
6•CI
8
4•Ci
41818
10152
<l4
34
•ciO
2
14
•CI16
•CI
CrMMI-D
1ppb
•CIO•Ci<lO
1O•Ci•ci•ci
•ci1
•ci<l<l
1•CI<l<l<l<l<l<l<l<l
<l•CI<l<l<l
CoMMI-D
1ppb
•Ci<lo•ci<l<l<l•CI<l<l<l<l•CI<l<l
3<l•ci<l<l
<l<l•ci<l<l<l<lo•ci<l
NiMMI-D
3ppb
•C3<3O•C3<3
<30•C3•C3<3
<3<3<3
3O
10•C3O0o
o•C3O•C3<3
•C3<3<3•C3<3
RbMMI-D
1ppb
2736301736
3332374248
3143263132
2722303138
3935422751
44353331
•CI
YMMI-D
0.1ppb
•CO.l•CO.l•CO.l•CO.l•CO.l
•CO.l•CO.l•CO.l•CO.l•CO.l
^.1•CO.l•CO.l•cO.l•CO.l
0.2•CO.l•CO.l•cO.l•CO.l
•CO.l•CO.l•CO.l•CO.l•CO.l
^.1•CO.l<0.1<0.1<0.1
NbMMI-D
0.1ppb
0.1•CO.l•CO.l•CO.l•CO.l
•CO.l•CO.l•CO.l•CO.l•CO.l
•CO.l•CO.l•cO.l•co.i•CO.l
0.2•CO.l•CO.l•co.i•CO.l
•CO.l•CO.l•CO.l-C 0.1•CO.l
•CO.l•cO.l•CO.l•CO.l•CO.l
PdMMI-D
0.1ppb
0.20.1
•CO.l•CO.l•CO.l
•CO.l•CO.l•CO.l•cO.l•cO.l
•CO.l•CO.l
0.1•CO.l•CO.l
0.2•CO.l•CO.l
0.1•CO.l
•CO.l•CO.l•CO.l•CO.l•CO.l
•CO.l•cO.l•CO.l•CO.l•CO.l
@ SGS Member of the SGS Group (Societe Generate de Surveillance)
XRAL XRAL LaboratoriesA Division of SGS Canada Inc.
1885 Leslie Street Don Mills, Ontario Canada M38 3J4 Telephone (4161 445-5755 Fax (4161 445-4152 CERTIFICATE OF ANALYSIS
Work Order: 069889To: Gitennes Exploration Inc
Attn: Jim Foster- 1055 West Hastings Street Suite 2390 VANCOUVER B.C. V6E 2E9
Date 30/09/02
Copy 1 to
P.O. No. Project No. No. of Samples Date Submitted Report Comprises
49 Soil(MMI) 16/09/02 Cover Sheet plus Pages 1 to 2
Distribution of unused material: Pulps: Store Rejects: Store
Certified By
e Souza, General Manager oratories
ISO 9002 REGISTERED
ISO 17025 Accredited for Specific Tests. S.C.C. No. 456
Report Footer:
Subject to SGS General Terms and Conditions
L.N.R. s Listed not received l.S. = Insufficient Sample n.a. = Not applicable - = No result *INF = Composition of this sample makes detection impossible by this method M after a result denotes ppb to ppm conversion, "ft denotes ppm to 07o conversion
@ SGS Member of the SGS Group (Societe Generate de Surveillance)
XRAL XRAL LaboratoriesA Division of SGS Canada Inc.
Work Order: 069889 Date: 30/09/02 FINAL Page l of 2
Element. Method. Del. Lira. Units.
L550E-300S L550E-275S L550E-250S L550E-200S L550E-175S
L550E-150S L550E-125S L550E-100S L550E-050S L550E-025S
L550E-000L550E-025NL550E-050NL550E-075NL550E-100N
L6E-300S L6E-275S L6E-250S L6E-225S L6E-200S
L6E-175S L6E-150S L6E-125S L6E-100S L6E-075S
L6E-050SL6E-025SL6E-000L6E-025NL6E-050N
MgMMI-D
100ppb
135304330505046905410
7130152801095059607910
110409370409064609210
78402110355038703720
94108100
17190101707640
99408780455067108490
TiMMI-D
1ppb
3•Ci
2•Ci
2
3O
2•Ci<l
36
<lO16
4<l-CiO•Ci
•CI<[o62<i
•CI•Ci•CI•ci
1
CrMMI-D
1ppb
•CI<l•ci•ci<l
•cio
l•ci
2
•CI2113
2•CIO
1•Ci
<l<l
23
O
11
•ci•Ci
2
CoMMI-D
1ppb
'CI<l
2•ci<l
<l<l<l•ci<l
<l<l<l•CI
1<l<l<l•CI<l<l<l<l
21
•CI<l<l•CI<l
NiMMI-D
3ppb
O•C3
4<3O
•C3O<3<3•C3
<3<3O<3O
<3<3<3<3•C3
<3<30
30
10•C3<300
RbMMI-D
1ppb
4028294439
3427333025
4034263740
3138443733
5617262526
3535373143
YMMI-D
0.1ppb
•CO.•CO.O.•CO.•CO.
0.1O.IO.IO.I<0.1
0.1•CO.lO.I<0.1
0.3
<0.1•CO.l•CO.l•CO.l•CO.l
•CO.l•CO.lO.I
0.1O.I
0.1•cO.l•CO.l•CO.l•CO.l
NbMMI-D
0.1ppb
•cO.lO.I•cO.l•CO.lO.I
O.IO.IO.IO.I0.1
O.IO.IO.I0.1O.I
O.IO.IO.IO.IO.I
0.1O.IO.IO.I0.1
0.1O.IO.I0.10.1
PdMMI-D
0.1ppb
O.IO.IO.I0.1O.I
O.I0.1O.IO.IO.I
O.IO.IO.IO.IO.I
0.1O.IO.I0.1O.I
O.I0.1O.IO.IO.I
O.I0.1O.IO.I0.1
Member of the SGS Group (Societe Generate de Surveillance)
XRAL XRAL LaboratoriesA Division of SGS Canada Inc.
Work Order: 069889 Date: 30/09/02 FINAL Page 2 of 2
Element. Method. Det.Lim. Units.
L6E-075N L6E-100N L8E-300S L8E-275S L8E-250S
L8E-225S L8E-200S L8E-175S L8E-150S L8E-125S
L8E-100S L8E-075S L8E-050S L8E-025S L8E-000
L8E-025N*Blk BLANK*Std MMISRM12L8E-050NL8E-075N
L8E-100N*Dup L550E-300S*Dup L550E-050N*Dup L6E-075S*Dup L8E-200S
*Dup L8E-100N*Blk BLANK*Std MMIXRAL01
MgMMI-D
100ppb
806010960452062409050
127505070
1800091809120
1500012580103801348014110
17660^00196301730017280
1572013100443076705490
15820^0014080
TiMMI-D
1ppb
•CIO•Ci
4•CI
•ci•ci•ci•ci•ci
1•CI•ci<l•ci
<l<l<l<l•ci
<l5
<l<l
1<l<l
1
CrMMI-D
1ppb
22221
1•Ci
122
12211
1•CI•CI
12
22112
2-Ci•Ci
CoMMI-D
1ppb
•ci•CI•ci<l
2
•CI1
<l<l<l<l<l<l<l
1
3•CI19
1<l
<l<l<l
13
•ci<l<l
NiMMI-D
3ppb
•C 3<3O•C3<3
17<3O•C3<3
<3<3O•C3<3
4<354
4•C 3
O•C 3•C30O
4O
8
RbMMI-D
1ppb
2735474150
2930362743
2727393432
32<l643640
2737242633
25•CI39
YMMI-D
0.1ppb
•cO.l•CO.l•cO.l•CO.l•cO.l
•cO.l•CO.l•CO.l^.1•cO.l
•CO.l•co.i•CO.l<0.1•cO.l
•CO.l•CO.l
0.5•CO.l<0.1
<0.1<0.1<0.1<0.1•CO.l
•CO.l<0.1
0.6
NbMMI-D
0.1ppb
•CO.l•CO.l•CO.l•CO.l•CO.l
*:0.i<0.1•cO.l<0.1<0.1
<0.1<0.1•CO.l<0.1<0.1
<0.1<0.1•CO.l•CO.l•cO.l
•CO.l•CO.l•co.i•CO.l<0.1
<0.1<0.1•CO.l
PdMMI-D
0.1ppb
•CO.l•CO.l•CO.l•CO.l•CO.l
•CO.l^.1•CO.l•CO.l•CO.l
•CO.l•CO.l•CO.l•CO.l<0.1
•CO.l•CO.l•CO.l•CO.l•CO.l
•CO.l•CO.l•CO.l•cO.l•co.i•cO.l•CO.l
0.2
©SGS Member of the SGS Group (Societe Generate de Surveillance)
XRAL XRAL LaboratoriesA Division of SGS Canada Inc.
1885 Leslie Street Don Mills, Ontario Canada M3B 3J4 Telephone (4161 445-5755 Fax (416) 445-4152 CERTIFICATE OF ANALYSIS
Work Order: 069977To: Gitennes Exploration Inc
Attn: Jim Foster.1055 West Hastings Street Suite 2390 VANCOUVER B.C. V6E 2E9
Date 08/10/02
Copy 1 to
P.O. No. Project No. No. of Samples Date Submitted Report Comprises
63 Soil(MMI) 23/09/02 Cover Sheet plus Pages 1 to 3
Distribution of unused material: Pulps: Store Rejects: Store
Certified By
Souza, General Manager oratories
ISO 9002 REGISTERED
ISO 17025 Accredited for Specific Tests. S.C.C. No. 456
Report Footer:
Subject to SGS General Terms and Conditions
L.N.R. = Listed not received l.S. = Insufficient Sample n.a. = Not applicable -- s No result *INF = Composition of this sample makes detection impossible by this method M after a result denotes ppb to ppm conversion, "/o denotes ppm to "/o conversion
© 5B5 Member of the SGS Group (Societe Generate de Surveillance)
XRAL XRAL LaboratoriesA Division of SGS Canada Inc.
Work Order: 069977 Date: 08/10/02 FINAL Page l of 3
Element. Method. Det.Lim. Units.
L450W-300S L450W-250S L450W-200S L450W-150S L450W-100S
L450W-050S L450W-OOOS L400W-300S L400W-250S L400W-200S
L400W-150S L400W-100S L400W-050S L400W-OOOS L350W-300S
L350W-250S L350W-200S L350W-150S L350W-100S L350W-050S
L350W-OOOSL3W-300SL3W-250SL3W-200SL3W-150S
L3W-100SL3W-050SL3W-OOOSL250W-300SL250W-250S
MgMMI-D
100ppb
86806170756056606590
534012600749063201740
649017604710
111809840
4340544058806430
10710
5990740072306780
12320
47606280932092707390
TiMMI-D
1ppb
911748
27
•CI
41
345
142
718
•Ci36
•ci•ci
494
32382
CrMMI-D
1ppb
<l<l<l•ci•ci
•CI•a<\•0*:i
•CI•CI<l•ci<l
o•ci-ciO•ci
<l<l<l<l<l
*:l<l<l<l<l
CoMMI-D
1ppb
<l•CI<l<l<l
<l1
O•ci<l<l•CI<l<l<l
1•ci
1<l<l
<l2
<l2
<l
<l•CI
2<l
3
NiMMI-D
3ppb
O•C3
3•C3•C3
<3353
O
3•C30•C3O
OO0o•C3
•C3733
•C3
O<3
4•C3
3
RbMMI-D
1ppb
3152464547
4629403741
4857414233
3531306640
3633514056
4752363526
YMMI-D
0.1ppb
O.IO.I0.1•CO.l•CO.l
O.I0.10.1O.IO.I
O.I0.10.1O.IO.I
O.I0.1O.IO.I0.1
0.2O.I0.1O.I0.1
0.1O.IO.I0.10.1
NbMMI-D
0.1ppb
0.30.10.20.20.2
O.I0.1
O.IO.IO.I
O.IO.I0.1
0.1O.I
0.20.2
O.IO.I0.1
0.1O.I0.1O.I0.1
0.1O.IO.IO.I0.1
PdMMI-D
0.1ppb
0.1O.I0.1
0.10.1
O.I0.1O.IO.IO.I
O.IO.IO.I
0.10.1
O.I0.1O.IO.I
0.1
O.I0.1
0.2O.I
0.2
0.1O.IO.IO.I
0.1
Member of the SGS Group (Societe Generate de Surveillance)
XRAL XRAL LaboratoriesA Division of SGS Canada Inc.
Work Order: 069977 Date: 08/10/02 FINAL Page 2 of 3
Element. Method. Det.Lim. Units.
L250W-200S L250W-150S L250W-100S L250W-050S L250W-OOOS
L200W-300S L200W-250S L200W-200S L200W-150S L200W-100S
L200W-050S L200W-OOOS L050W-200S L050W-150S L050W-100S
L050W-050S*Blk BLANK*Std MMIXRAL01L050W-OOONL050W-050N
L050W-100NLO-200SLO-150SLO-100SLO-050S
LO-OOONLO-050NLO-100NL050E-200SL050E-150S
MgMMI-D
100ppb
1060089109660
1802010250
123608850
164401096014060
11420113501034042402150
5490•c 1001487029808980
3820197501840040302520
53308040
12320144707970
TiMMI-D
lppb
6145
38
717
1102
24315
2•Ci
1o
3
3528
•ci
11525
21
CrMMI-D
1ppb
•si•CI<l•CI•ci
•ci•ci•ci•ci•ci
2•CI
1^1•ci
<l•CI<l<l•CI
<l<l<l<l•ci
<l<l<l<l•ci
CoMMI-D
1ppb
1O
12
•CI
o<l<l<l<l•ci
l<l<l
3
0<l<l<l
2
2•Ci<l
2<l
•CI2
<l<l<l
MiMMI-D
3ppb
0O
33
O
•C3•C3
3O<3
<34
•C3O
5
5<3
6<3
3
3374
O
O0
5O•C3
RbMMI-D
1ppb
3837331762
3935264829
3146104216
65•CI462933
3126333637
4330303232
YMMI-D
0.1ppb
•cO.l•CO.l•CO.l•CO.l•CO.I
•CO.l•cO.l•CO.l•CO.l•CO.l
•cO.l•CO.l•CO.l•CO.l•CO.l
•CO.l•CO.l
0.4^.1
0.1
•CO.l•CO.l•CO.l
0.1•CO.l
•CO.l•CO.l•co.i•CO.l•CO.l
NbMMI-D
0.1ppb
0.1*;o.i•cO.l^.i
0.2
•CO.l0.2
•CO.l0.1
•CO.l
^.1•CO.l•CO.l•CO.l•CO.l
0.1•CO.l•CO.l•CO.l•CO.l
*:o.i•CO.l•CO.l•CO.l•CO.l
•CO.l0.10.2
•CO.l•CO.l
PdMMI-D
0.1ppb
0.10.20.10.1
•CO.l
*:0.10.10.1
•CO.l•CO.l
0.1•CO.l•cO.l•CO.l•CO.l
•CO.l•CO.l
0.1•CO.l•CO.l
•CO.l0.2
•CO.l•cO.l•CO.l
•co.i•CO.l•CO.l^.1
0.1
@ SGS Member of the SGS Group (Societe Generate de Surveillance)
XRAL XRAL LaboratoriesA Division of SGS Canada Inc.
Work Order:
Element.Method.Det.Lim.Units.
L050E-100SL050E-050SL050E-OOONL050E-050NL050E-100N
*Dup L450W-300S*Dup L400W-050S*Dup L3W-150S*Dup L200W-250S*Dup L050W-100N
*Dup L050E-OOON*Blk BLANK*StdMMISRM12
069977
MgMMI-D
100ppb
6280582048707670
21400
98704760
1267082803530
4840•C 10020500
Date: 08/10/02
TiMMI-D
1ppb
22
*C172
756
162
•CIO
1
CrMMI-D
1ppb
0•Ci•ci<l<l
1o
2•CI<1<l<l<l
CoMMI-D
1ppb
•Ci•ci<l<l<1<l•CI
1<l
2
<l•C 124
NiMMI-D
3ppb
3•C3<3
74
OO<3O0
<3<364
FINAL
RbMMI-D
1ppb
3834363710
3039513131
32•ci74
YMMI-D
0.1ppb
0.10.1
•CO.l•CO.l^.1
•CO.l•CO.l'CO.l'CO.l•CO.l
•CO.l•cO.l
0.5
NbMMI-D
0.1ppb
0.1•CO.l•CO.l•cO.l•cO.l
•CO.l•cO.l'CO.l
0.1'CO.l
•CO.l•CO.l•CO.l
PdMMI-D
0.1ppb
0.1•CO.l•CO.l'CO.l•CO.l
•cO.l•cO.l
0.20.1
•cO.l
•cO.l•CO.l
0.2
Page 3 of 3
Member of the SGS Group (Societe Generate de Surveillance)
XRAL XRAL LaboratoriesA Division of SGS Canada Inc.
1885 Leslie Street Don Mills, Ontario Canada M3B 3J4 Telephone (416) 445-5755 Fax (416) 445-4152 CERTIFICATE OF ANALYSIS
Work Order: 070164
To: Gitennes Exploration Inc Attn: Jerry Blackwell1055 West Hastings Street Suite 2390 VANCOUVER B.C. V6E 2E9
Date 10/10/02
Copy 1 to
P.O. No. Project No. No. of Samples Date Submitted Report Comprises
Badger Property 19 Soil(MMI) 02/10/02 Cover Sheet plus Pages 1 to 1
Distribution of unused material: Pulps: Store Rejects: Store
Certified By
ouza, General Manager atories
ISO 9002 REGISTERED
ISO 17025 Accredited for Specific Tests. S.C.C. No. 456
Report Footer:
Subject to SGS General Terms and Conditions
L.N.R. = Listed not received l. S. = Insufficient Sample n.a. = Not applicable - = No result *INF = Composition of this sample makes detection impossible by this method M after a result denotes ppb to ppm conversion, Vo denotes ppm to Vo conversion
Member of the SGS Group (Societe Generate de Surveillance)
XRAL XRAL LaboratoriesA Division of SGS Canada Inc.
Work Order: 070164 Date: 10/10/02 FINAL Paae l of l
Element. Method. Det.Lim.Units.
1666616667166681666916670
1667116672166731667416675
1667616677166781667916680
16681166821668316684*Dup 16666
*Dup 16678*Blk BLANK*Std MM1SRM12
MgMMI-D
100ppb
1711010510191702185012980
568060605180
1036014500
15150220701093083807600
9640198607200
1658017390
10950•c 10017990
TiMMI-D
1ppb
t;!
32•Ci•Ci•CI
0•ci
3•CI•CI
106
1761
•ci
4126
•ci
160
1
O CoMMI-D MMI-D
1 1ppb ppb
•Ci -CiO 1"Ci -CI•CI <l'CI <l
<l <l<l -CI•CI <l<l <l'CI <l
<l <l6 *C1
<l 1<l 1•CI <l
<l 1<l <i<l 2<l <l0 <l<l 2<l -CI'Ci 22
NiMMI-D
3ppb
444
OO
O<3<3O•C3
<3<3
44
•C3
<3<3OO
3
OO49
RbMMI-D
1ppb
^10
'CI99
2931404020
56
214020
201118
5< l
23'CI73
YMMI-D
0.1ppb
•CO.l0.5
•CO.l•CO.l•C0.1
•CO.l•co.i
0.1•CO.l•CO.l
0.20.1
•CO.l0.3
'CO.l
-CO.l•CO.l'CO.l
0.1-CO.l
•CO.l•CO.l
0.5
NbMMI-D
0.1ppb
'CO.l0.1
*:0.1•CO.l•CO.l
•CO.l<0.1•CO.l<0.1<0.1
<0.1<0.1'CO.l
0.2•CO.l
<0.1<0.1'CO.l<0.1<0.1
<0.1<0.1'CO.l
PdMMI-D
0.1ppb
•CO.l•CO.l•CO.l•CO.l•CO.l
•CO.!•cO.l•CO.l<0.1<0.1
•CO.l<o.l<0.1<0.1<0.1
•CO.l'CO.l•CO.l'CO.l<0.1
•cO.l•CO.l•CO.l
Member of the SGS Group (Societe Generate de Surveillance)
XRAL XRAL LaboratoriesA Division of SGS Canada Inc.
1885 Leslie Street Don Mills, Ontario Canada M3B 3J4 Telephone (416) 445-5755 Fax (4161 445-4152 CERTIFICATE OF ANALYSIS
Work Order: 070267To: Gitennes Exploration Inc
Attn: Jerry Blackwell1055 West Hastings Street Suite 2390 VANCOUVER B.C. V6E 2E9
Date 23/10/02
Copy 1 to
P.O. No. Project No. No. of Samples Date Submitted Report Comprises
BADGER PROJECT 28 Soil 09/10/02 Cover Sheet plus Pages 1 to 2
Distribution of unused material: Pulps: STORE Rejects: STORE
Certified By
Souza, General Manager ^boratories
ISO 9002 REGISTERED
ISO 17025 Accredited for Specific Tests. S.C.C. No. 456
Report Footer:
Subject to SGS General Terms and Conditions
L.N.R.n.a.*INF
s Listed not received l.S. = Insufficient Sample= Not applicable ~ = No result= Composition of this sample makes detection impossible by this method
M after a result denotes ppb to ppm conversion, "/o denotes ppm to "/o conversion
© SGS Member of the SGS Group (Societe Generate de Surveillance)
XRAL XRAL LaboratoriesA Division of SGS Canada Inc.
Work Order: 070267 Date: 23/10/02 FINAL Page l of 2
Element. Method. Det.Lim. Units.
1655316554165551655616557
1655816559165601656116562
1656316564165651656616567
1656816569165701657116572
1657316574165751657616577
165781657916580*Dup 16553*Dup 16565
MgMMI-D
100ppb
80804250887090306510
64805840722038005850
46109780
168608090
10390
934014330502046307600
523046303850
115905880
6160415083907210
17480
TiMMI-D
1ppb
2•a•ci
64:1
0•Ci1945
21
•Ci5
<l
12123
•CI24
13
•ci
11•CI
61
O
Cr CoMMI-D MMI-D
1 1ppb ppb
<l •CI•ci O•CI •CI
2 2<l .CI
<l <l<l <l
1 <l<l <l<l •CI<l <l<l <l<l <l<l <l<l •ci
<l <l<l 1•CI <l<l <l<l o
<l <l<l <lO "CI<l <l<l •CI
<l <l1 <l
•CI <l<l <l<l "CI
NiMMI-D
3ppb
•C3<3O<30
•C3•C 3<3•C3<3
0•C3
5<3•C3
O•C30Oo•C3<3<3<3<3
•C3<3<3<3<3
RbMMI-D
1ppb
3654234241
3029403329
2629253628
3731454346
3029343256
4338313426
YMMI-D
0.1ppb
^.1•CO.l•CO.l•co.i•CO.l•co.•CO.•co.•CO.•co.•co.•CO.•CO.l•CO.l•CO.l
*:0.1<0.1<0.1<0.1<0.1
<0.10.1
•co.l<0.1<0.1
<0.1<0.1•CO.l<0.1<0.1
NbMMI-D
0.1ppb
0.10.2
•CO.l0.2
•CO.l
•CO.l<0.1
0.30.1
<0.1
<0.1<0.1<0.1
0.1^.1<0.1
0.20.20.10.1
0.10.30.1
•CO.l0.1
0.2•CO.l•CO.l•CO.l•CO.l
PdMMI-D
0.1ppb
•co.i•CO.l•CO.l•CO.l-C0.1
•CO.l•CO.l^.1<0.1•CO.l
•CO.l•CO.l•CO.l•CO.l•CO.l
•CO.l•CO.l•CO.l•CO.l•CO.l
•CO.l•CO.l^.1•CO.l•CO.l
•CO.l^.1•co.i•cO.l•CO.l
Member of the SGS Group (Societe Generate de Surveillance)
XRAL XRAL LaboratoriesA Division of SGS Canada Inc.
Work Order: 070267 Date: 23/10/02 FINAL Page 2 of 2
Element. Method. Det.Lim. Units.
*Dup 16577*Blk BLANK*Std MMISRM12
MgMMI-D
100ppb
5770•C 10017950
TiMMI-D
1ppb
1<l<l
CrMMI-D
1ppb
•CI•CI<l
CoMMI-D
1ppb
•CI*C122
NiMMI-D
3ppb
O051
RbMMI-D
1ppb
64•Ci76
YMMI-D
0.1ppb
•CO.l•cO.l
0.4
NbMMI-D
0.1ppb
•co.i^.i
0.1
PdMMI-D
0.1ppb
-co.i^.i
0.2
©SGS Member of the SGS Group (Societe Generate de Surveillance)
APPENDIX II
MMI Anomaly Sampling Spreadsheets
BlackholeMMI 030331 .xls Black Hole
GITENNES EXPLORATION INC.Badger Property
Table 11-1: Black Hole Anomaly MMI-D SamplingC:\Gitennes\Badger\Assessment\030331filing\BlackholeMMI_030331.xls
08/04/2003 2:59 PM
Black HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack Hole tBlack Hole i
ilSll/IBllliL1E-000
L1E-025NL1E-050NL1E-075NL1E-100NL1E-125NL1E-150NL1E-175NL1E-200NL1E-225NL1E-250NL1E-275NL1E-300N
165801657916578165771657616575165741657316572
L3E-075SL3E-050SL3E-025SL3E-000
L3E-025NL3E-050NL3E-075NL3E-100NL4E-400SL4E-375SL4E-350SL4E-325SL4E-300SL4E-275SL4E-250SL4E-225S
100100100100100100100100100100100100100300300300300300300300300300300300300300300300300300400400400400400400400400
0255075100125150175200225250275300-300-275-250-225-200-175-150-125-100-75-50-250
255075100-400-375-350-325-300-275-250-225
lIEASIliNCil316309316309316309316309316309316309316309316309316309316309316309316309316309316506316506316506316506316506316506316506316506316506316506316506316506316506316506316506316506316506316605316605316605316605316605316605316605316605
54850065485031548505654850815485106548513154851565485181548520654852315485256548528154853065484696548472154847465484771548479654848215484846548487154848965484921548494654849715484996548502154850465485071548509654846015484626548465154846765484701548472654847515484776
132415380
1317012183104608100710096608340
153001701019151106008390415061605880
115923850463052307600
156101573413040126609690
100001145065704750
16000967081008450
15610147405700
^^*:1
3^
451
•d7
•:124•d
6^11^
31
24•C1
3•C1
•d•d
2^•C1
52
*:1•d
32
^1
10l2
^•d^*:1
^^•ci•ci
^^•:1
1•d•ci•C1
^•ci^•:1*:1^•d•si^•C1
^•si•C1
*:1•d•d^^^^^•d-^
Se:::::±!-;;pra^vSi'JSJ^sssfci^Q
^^^^^^•ci•:1•:1*:1
21
•d•ci•?1•d*:1•d•:1<1<1<1<1*:1<1<1<1<1^<1<1<1<1•d<1<1—— -^
~*Tl
0oo
400OO0oo44
OO0O0OO00OO0O0000O0O0O
4O"
O
4527502832402235404524
52831384356323429304639354435262941293551425058384652
O.10.1O.1O.1O.1O.10.1
0.2O.1O.10.1
0.5O.10.1O.1O.10.1O.1O.10.1O.1O.10.1O.1O.10.10.1O.1O.10.1O.1O.1O.1O.1O.1O.1O.1O.1
i|S~fi|jS!O.1
0.10.10.2
0.1O.10.1*cOJj0.10.1O.1
0.20.1O.1O.1
0.20.1
0.10.10.30.10.1
O.1O.1
0.1O.1O.1O.1O.10.1O.10.1O.1O.1O.1O.1O.1O.1
•3?s? v f^^jj^g;"' K;Si':. , 1^Q,™S;:
O.10.1<0.1<0.1O.1O.10.1O.1O.1O.1O.10.1O.10.1O.1O.1O.10.1O.1O.10.1O.10.1O.1O.10.10.10.1O.1O.1O.1O.1O.1O.1O.10.1O.10.1
Page 1 of 5
BlackholeMMI 030331 .xls Black Hole
GITENNES EXPLORATION INC.Badger Property
Table 11-1: Black Hole Anomaly MMI-D SamplingC:\Gitennes\Badger\Assessment\030331filing\BlackholeMMI_030331.xls
08/04/2003 2:59 PM
?iii^ft'"Kfi^\ Hill-A'1'^^/^'li^sii^lJl:Si^I'"**li'*:?IsS;
Black HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack Hole
fiPSAMRllHL4E-200SL4E-175SL4E-150SL4E-125SL4E-100SL4E-075SL4E-050SL4E-025SL4E-000
L4E-025NL4E-050NL4E-075NL4E-100N
L450E-300SL450E-275SL450E-250SL450E-225SL450E-200SL450E-175SL450E-150SL450E-125SL450E-100SL450E-075SL450E-050SL450E-025SL450E-000
L450E-025NL450E-050NL450E-075NL450E-100N
L5E-400SL5E-375SL5E-350SL5E-325SL5E-300SL5E-275SL5E-250SL5E-225S
400400400400400400400400400400400400400450450450450450450450450450450450450450450450450450500500500500500500500 t500
-200-175-150-125-100-75-50-250
255075100-300-275-250-225-200-175-150-125-100-75-50-250
255075100-400-375-350-325-300-275-250-225
s^jti^StCifc":^riii^"i^5^^.•CiiHlWsl:-:*! -1 SJm
316605316605316605316605316605316605316605316605316605316605316605316605316605316656316656316656316656316656316656316656316656316656316656316656316656316656316656316656316656316656316706316706316706316706316706316706316706316706
5484801548482654848515484876548490154849265484951548497654850015485026548505154850765485101548469954847245484749548477454847995484824548484954848745484899548492454849495484974548499954850245485049548507454850995484596548462154846465484671548469654847215484746 15484771
83004610630086008130584097408880
170709030
104307730
118109680
167605570
111801275093607750571078809860
1282084006750779065208270654080005740
143907510
10020469078005410
722
^94
•d•ci•d
215
•C1
11213322
*:13
•?1•d
8612
•d•C1
•C1
232
^6
•d
1^*:1
^^•:1
^•d•C1
*:1
1•d
1•d
2•ci
^^^^*:1
^•ci•d
1•:1
^*:1•d•d•C1
•S1^•ci
1•ci•ci•ci
'iiisallfey
"C1
*:1•:1^^*:1•:1•ci•^1
^*:1•ci•ci•ci•ci-C1
*:1•ci•^*:1•:1*:1•C1
•si•ci•C1^•:1•ci-ci•d
^^-ci
^^^^
OOO0Oooo0oo00o^0o0oo0oo00o000^o0o0o0oo
3230283735524845333432322136335034432937403628345121383038273630173633323742
O.10.1O.1O.1O.1O.10.1O.1O.10.10.1O.1O.10.1O.10.10.1O.1O.10.1O.1O.10.1O.10.10.1O.1O.1O.10.1O.1O.1O.1O.1O.1O.1O.1O.1
O.10.1
O.1O.1O.1O.10.1O.1O.10.10.1O.1O.10.1O.1O.1
0.1O.1O.10.1O.1O.10.1O.1O.10.1O.1O.1O.1
0.1O.1O.1O.1O.1O.1O.1O.10.1
•millO.1O.1O.10.10.10.1O.10.10.1O.1O.1O.10.1O.10.1O.1O.1O.10.1O.1
0.20.1O.10.1O.1O.1O.1O.10.1
0.20.1
0.1O.1O.1O.1O.1O.1O.1
Page 2 of 5
BlackholeMMI030331 .xls Black Hole
GITENNES EXPLORATION INC.Badger Property
Table 11-1: Black Hole Anomaly MMI-D SamplingC:\Gitennes\Badger\Assessment\030331filing\BlackholeMMI_030331.xls
08/04/2003 2:59 PM
P'JI'fci^V^ji^k^os™ AN U m Au T
Black HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack Hole
llSAJiiHigllL5E-200SL5E-175SL5E-150SL5E-125SL5E-100SL5E-075SL5E-050SL5E-025SL5E-000
L5E-025NL5E-050NL5E-075NL5E-100N
L550E-300SL550E-275SL550E-250S
16571L550E-200SL550E-175SL550E-150SL550E-125SL550E-100S
16570L550E-050SL550E-025SL550E-000
L550E-025NL550E-050NL550E-075NL550E-100N
L6E-300SL6E-275SL6E-250SL6E-225SL6E-200SL6E-175SL6E-150SL6E-125S
llllllN'Eii
500500500500500500500500500500500500500550550550550550550550550550550550550550550550550550600600600600600600600600 j
-200-175-150-125-100-75-50-250
255075100-300-275-250-225-200-175-150-125-100-75-50-250
255075100-300-275-250-225-200-175-150-125
:;M*C;: ' A^O'Tl Ki'f*--~fi*•ll|!l2iftOJlll PI \3ll
316706316706316706316706316706316706^316706316706316706316706316706316706316706316760316760316760316760316760316760316760316760316760316760316760316760316760316760316760316760316760316813316813316813316813316813316813316813316813
54847965484821548484654848715484896548492154849465484971548499654850215485046548507154850965484698548472354847485484773548479854848235484848548487354848985484923548494854849735484998548502354850485485073548509854847015484726548475154847765484801548482654848515484876
113907150
133278600843067304310
11590103505470
1245050908460
13528433050504630469054107130
1528210950502059607910
1104293704090646092107840211035503870372094108100
171861
84
*:1
4181810152
•d
4343
*:1
22
•d23
•d21
^^
36
•C1
^164^^^^•S1*:1•d
•;1^
1*:1•:1
^1
•d*:1•d•^1
^^^*:1
^•d•d•ci
^*:1
1*:1•:1
2^
21132
*:1
^1
•:1
^^
2
•ci
^•d•C1
•ci*:1
3•si*C1
•d•ci
^•ci
^*:1
2•C1
•d•C1
*:1•^1•d
^*:1*:1
^•ci*:1
^1
•d
^^^-d•ci•;1•si
O000
3O10OOO00O0O4
00OO0O0OOO00O
0OOOOO0O^
lliil^Jriiiillllfi^iiiflll4831432631322722303138393540282943443934273345302540342637403138443733561726
0.10.1O.1O.1O.10.1
0.20.1O.1O.10.1O.1O.10.1O.1O.10.10.1O.10.1O.10.10.1O.1O.1
0.10.1O.1O.1
0.30.1O.1O.1O.1O.1O.1O.10.1
O.1O.10.10.1O.1O.1
0.20.10.1O.10.1O.1O.1O.10.1O.1
0.10.1O.10.1O.1O.1
0.20.1O.1O.10.1O.1O.1
O.1O.1O.1O.10.1O.1O.1O.1O.1
O.1O.1O.1
0.1O.1O.1
0.2O.10.1
0.1O.10.1O.1O.1O.10.1O.10.1O.1O.10.1O.1O.10.10.1O.10.10.10.1
O.1O.10.1O.10.1O.10.1O.1O.1
Page 3 of 5
BlackholeMMIJ)30331 .xls Black Hole
GITENNES EXPLORATION INC.Badger Property
Table 11-1: Black Hole Anomaly MMI-D SamplingC:\Gitennes\Badger\Assessment\030331filing\BlackholeMMI_030331.xls
08/04/2003 2:59 PM
Black HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack HoleBlack Hole
L6E-100SL6E-075SL6E-050SL6E-025SL6E-000
L6E-025NL6E-050NL6E-075NL6E-100NL8E-300SL8E-275SL8E-250SL8E-225SL8E-200SL8E-175SL8E-150SL8E-125SL8E-100SL8E-075SL8E-050SL8E-025SL8E-000
L8E-025NL8E-050NL8E-075NL8E-100N
165531655416555165561655716558165591656016561165621656316564
600600600600600600600600600800800800800800800800800800800800800800800800800800700700700700700700700700700700700700
-100-75-50-250
255075100-300-275-250-225-200-175-150-125-100-75-50-250
255075100-300-275-250-225-200-175-150-125-100-75-50 ^-25
316813316813316813316813316813316813316813316813316813317006317006317006317006317006317006317006317006317006317006317006317006317006317006317006317006317006316910316910316910316910316910316910316910316910316910316910316910316910
548490154849265484951548497654850015485026548505154850765485101548470954847305484754548477954848045484828548485354848785484902548492754849525484976548500154850265485051548507654851015484700548472554847505484775548480054848255484850548487554849005484925 ,54849505484975 l
101737640994087804550671084908060
10963452062409050
127485070
1799791809120
149971257910375134801410817655172971727915718808042508870903065106480584072203800585046109780
62-:1*c1
^•d•ci
1•d
^^
4•d*:1-:1•d*:1•ci
1•ci•ci•C1^^-M•M•C1
2•d•ci
6•:1•:1
^194521
3^
11
^^
2222211
^122122111122
•d•d•:1
2-:1*:1•:1
1^^*C1
^
21
^•d*:1•ci
^•:1•d
^•C1
2*:1
1^^^•d•si•d•ci
131
•:1•d•C1
•ci*:1
2^^^^^<1<1<1
3010^<3^<3<3<3O0^17<3<3^0<3<30^<3
44
00OO^<3^O<3<3<3^O<3
25263535373143273547415029303627432727393432323640273654234241302940332926 129
0.1O.1
0.1O.1O.1O.1O.1O.1O.1O.1O.1O.1O.10.10.1O.10.10.1O.1O.10.10.10.10.1O.1O.10.10.1O.1O.10.1O.1O.1O.1O.1O.1O.1O.1
0.1O.1O.1O.1O.10.10.1O.1O.10.10.1O.10.10.1O.1O.10.10.1O.10.1O.10.10.1O.1O.10.1
0.10.2
O.10.2
O.1O.10.1
0.30.1
O.1O.10.1
0.1O.1O.1O.1O.1O.10.1O.1O.1O.10.1O.1O.10.1O.1O.1O.10.1O.10.1O.10.1O.1O.1O.10.10.1O.1O.10.1O.1O.10.1O.1O.10.10.10.1
Page 4 of 5
BlackholeMMI J330331 .xls Black Hole
GITENNES EXPLORATION INC.Badger Property
Table 11-1: Black Hole Anomaly M M l-D SamplingC:\Gitennes\Badger\Assessment\030331filing\BlackholeMMI_030331.xls
08/04/2003 2:59 PM
JORTHI IB:.
Black Hole 16565 700 316910 5485000 16861 <1 25 O.1 O.1Black Hole 16566 700 25 316910 5485025 8090 36 O.1 0.1
O.1O.1
Black Hole 16567 700 50 316910 5485050 10386 <1 <3 28 0.1Black Hole 16568 700 75 316910 5485075 9340 37 O.1Black Hole 16569 700 100 316910 5485100 14332 31 O.1 0.2 O.1
Page 5 of 5
13320D_030331.xls 13320D
GITENNES EXPLORATION INC.Badger Property
Table II-2: Anomaly 13320D MMI-D SamplingC:\Gitennes\Badger\Assessment\030331filing\13320D_030331.xls
08/04/2003 3:00 PM
ANOMAljy13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D13320D
L2W-000L2W-050SL2W-100SL2W-150SL2W-200SL2W-250SL2W-300SL250W-000
L250W-050SL250W-100SL250W-150SL250W-200SL250W-250SL250W-300S
L3W-000L3W-050SL3W-100SL3W-150SL3W-200SL3W-250SL3W-300SL350W-000
L350W-050SL350W-100SL350W-150SL350W-200SL350W-250SL350W-300S
L4W-000L4W-050SL4W-100SL4W-150SL4W-200SL4W-250SL4W-300SL450W-000
L450W-050SL450W-100SL450W-150SL450W-200SL450W-250SL450W-300S
-200-200-200-200-200-200-200-250-250-250-250-250-250-250-300-300-300-300-300-300-300-350-350-350-350-350-350-350-400-400-400-400-400-400-400-450-450-450-450-450-450-450
18TJVTION0
-50-100-150-200-250-300
0-50
-100-150-200-250-300
0-50
-100-150-200-250-300
0-50
-100-150-200-250-300
0-50
-100-150-200-250-300
0-50-100-150-200-250-300
SSHffi316085316085316085316085316085316085316085316035316035316035316035316035316035316035315985315985315985315985315985315985315985315935315935315935315935315935315935315935315885315885315885315885315885315885315885315835315835315835315835315835315835^315835
IMBITO*!548506354850135484963548491354848635484813548476354850635485013548496354849135484863548481354847635485063548501354849635484913548486354848135484763548506354850135484963548491354848635484813548476354850635485013548496354849135484863548481354847635485063548201354820645482014548206554820155482066
'^Sss;^;:i:; v^Sfln Q
11350114201406010960164408850
12360102501802096608910
1060073909270932062804760
123206780723074005990
1071064305880544043409840
11180471017606490174063207490
12600534065905660756061708680
422
101
177
38541628323494
0.50.5
63
0.51872
1454314
0.572847
119
'fSiS^SSSSSi-fffffSi-t.-'f^JI1.
^2
•d^•d•d^^•C1
"d^*:1^•d•el
^•ci*:1^*M•M^^^•d^^^•d•M•:1*C1
^•^1•:1•:1^^^^•^1^
1•el^-:1•d*:1•d•ci
21
•ci13
•:12
"M^*:1
2•d
2•d•C1
^1
^1
^^^*:1•:1
^•d•d
1•:1•:1•:1
^^•; 1,
s|i!tllWpH^
4OOO
3OOO
33
OO
3O
4OOO
337
0OOOOOOOOO
3O
353
OOO
3O^
.'.•ssscciK.^O lii-i;. 1 .?; . l : 1 . 1 : 1 :;liisMSk—i
463129482635396217333738263536524756405133364066303135334241574841374029464745465231
O.1O.1O.1O.10.1O.1O.1O.1O.1O.1O.1O.1O.1O.1O.10.1O.10.1O.1O.1O.1
0.2O.1O.1O.1O.1O.1O.1O.1O.1O.1O.1O.1O.1O.1O.1O.1O.1O.10.1O.1O.1
O.1O.1O.1
0.1O.1
0.2O.1
0.2O.1O.1O.1
0.1O.1O.1O.1O.1O.10.1O.1O.1O.10.10.10.1O.1
0.20.2
O.10.1
O.1O.1O.1O.1O.1O.1
0.1O.1
0.20.20.2ti.r0.3
0.10.1
O.10.1
0.10.1
0.10.1
0.10.10.20.10.1
O.10.10.1O.1
0.2O.1
0.2O.1O.1
0.10.10.10.10.1O.1
0.10.1O.10.10.1O.1O.10.1O.10.1
0.1O.1O.1
0.1
Page 1 of 1
13470B_030331.xls 13470B
GITENNES EXPLORATION INC.Badger Property
Table II-3: Anomaly 13470B MMI-D SamplingC:\Gitennes\Badger\Assessment\030331filing\13470B_030331.xls
08/04/2003 3:04 PM
13470B13470B13470B13470B13470B13470B13470B13470B13470B13470B13470B13470B13470B13470B13470B13470B13470B13470B13470B
ISSMRiH16666166691667116675166741667016673166721667916678166671667616677166801668116668166821668316684
liiffiHSEiB!125-100-50-50-50-50-5000000
7575757575
00
-100-500
50100-100-500
50100-100-500
50100
ilBSSTJNS!318669318705318480318530318530318530318530318530318593318576318580318576318572318668318662318655318655318655318561
aORWINBi5486872548686054868605486760548681054868605486910548696054867475486820548686054869155486961548676054868105486860548691054869605486987
iieilBlwfi!1710821852
5680144991036012981518060608380
10932105101515022068
76009640
19168198627200
16580
•el•el
^^•d•el
3-:1611732106
•el4
•:1126
^K.-y-yif^fy^^'iy.-f^f ^^•••ffW^'f^'.^f^-i
•el-:1<1<1<1<1<1<1<1<1<1•el
6<1<1<1<1<1<1
•el<1^<1<1<1<1<1
111
<1•el<1
1<1<1
2<1
4O<3OO<3<3<3
444
OO0O
4Ooo
;^^!Ri3lilll<1
9292040
94031402110
56
2020•el1118
5
O.10.1O.1O.1O.1O.1
0.1O.1
0.3O.10.50.20.1
O.10.1O.1O.1O.1
0.1
IlilUftSllsO.1O.1O.1O.1O.1O.10.1O.1
0.20.1
0.1O.1O.1O.1O.1O.1O.1O.1O.1
O.1O.1O.1O.1O.1O.1O.1O.10.1O.1O.10.1O.1O.1O.1O.1O.1O.1O.1
Page 1 of 1
13500A_030331.xls 13500A
GITENNES EXPLORATION INC.Badger Property
Table II-4: Anomaly 13500A MMI-D SamplingC:\Gitennes\Badger\Assessment\030331filing\13500A_030331.xls
08/04/2003 3:08 PM
ANOMALY13500A13500A13500A13500A13500A13500A13500A13500A13500A13500A13500A13500A13500A13500A13500A13500A13500A13500A13500A13500A13500A
I'^ft'O^A'itiDl^IS^^ l-sl*;:O^\flfl:I^^E;ffsi:
L050W-100NL050W-050N
L050W-ONL050W-050SL050W-100SL050W-150SL050W-200S
LO-100NLO-050N
LO-ONLO-050SLO- 1 DOSLO- 1 SOSLO-200S
L050E-100NL050E-050N
L050E-ONL050E-050SL050E-100SL050E-150SL050E-200S
-50-50-50-50-50-50-500000000
50505050505050
KiWIfe100500
-50-100-150-200100500
-50-100-150-200100500
-50-100-150-200
iilsflK319240319240319240319243319246319249319252319290319290319290319290319290319290319290319340319340319340319340319340319340319340
NORTHING548605054860005485950548589854858455485793548574054860505486000548595054859005485850548580054857505486050548600054859505485900548585054858005485750
382089802980549021504240
10340123208040533025204030
184001975021400
76704870582062807970
14470
33
•;12513
2515
1*:1
82527
•el2212
t1•el
^^•d
^1
t1•:1•si•O"O•el•:1•d
^•M•el•si
^-:1
22
•:1•el
3<1*:1<1
2•:1<1
2<1<1•M<1<1<1<1•si<1
33
<355
OO
5^<3O
47347
OO
3OO
cSS5KjS^btU;':v:vrt s^^^fV lP"v2 Sim
313329651642103030433736332610373634383232
O.10.1
0.10.1O.1O.1O.1O.1O.1O.1O.1
0.1O.10.1O.1O.1O.1
0.10.1
O.1O.1
; ;^|?ss^li3^^^"ip';!
O.1O.1O.1
0.1O.10.10.1
0.20.1
O.1O.1O.1O.1O.1O.1O.1O.1O.1
0.1O.1O.1
O.1O.10.1O.1O.1O.10.1O.1O.1O.1O.1O.1O.1
0.20.1O.1O.1O.1
0.10.1
0.1
Page 1 of 1
APPENDIX III
Geophysical Instruments Specifications and Data
y
dj
l
OMNI IV
EDA
j j j ljy yu U
Four Magnetometers in One, yself correcting for Diuf-ftai VariationsReduced instrumentation Requirements253/6 weight ReductionUser Friendly Keypad Operationuniversal Computer interfaceComprehensive Software Packages
20 SOISAHdCGD D31W
i. As a Self Correcting.7iTletine'r ; Magnetometer...
"" Any survey can now be run and corrected automatically with only one OMNI IV,
j The OMNI iv Is able to store "looping" or "tie/line" data. This data Is stored in
, a separate memory at the beginning of each survey. Total field readings
^ are then subsequently stored In a second memory along with the field readings of the tle-polnt(s). At the end of each survey day, these two
^ memories are merged to auto matically correct the total field data for diurnal variations.FeaturesThe OMNI iv In the "tie-line" mode can:- Store "looping" or "tie-line" data
sways:• - using one "looping" base point,
- using one "tie-line" comprised of a number of tie-points, or
- using multiple "tie-lines".- store up to 100 tie-points in one
survey area or divide these points into extensions of survey areas as needed.
™ * Store tie-points or tie-lines for the duration of the survey.
- calculate the drift between established tie-points, to readily
• see variations In the earth's magnetic field.
' Key Benefits~ Eliminates Manual
Correction of DataDiurnal corrections, using the tie-line
•— method, can be done automatically by the OMM rv, eliminating hours of manual and tedious calculations, cor rected data can then be directly
•* transferred to a computer for further data processing.Flexibility of Tie-Line"f—tThe OMNI iv "tie-tine" system offers
, the operator the flexibility of j choosing the most appropriate tle- M line method best suited for the
survey, depending upon the size and character of the grid. The operator
1 ^n choose from:•d a single base point.
- a single tie-line,- multiple tie-lines, or
l - a random scattering of tie-points.
"Looping" Method
1+OON I-f~
0 + 50N |-
rLO H
0 + 50S
1-t-OOS
(^) Base Point
i rK \ : t"
I J - 5il/f
rOO fi^ "i"t!d
P. - —— **-
r ^r —— -1 ——- ^- —— -
I ' —— *LH-OOE
""i
:3- ~~i— — —r — Base Line~"~}
~~\"J
- .JL2+OOE
-*- Tielng back to base point•~* Direction of Travel
"Tie-Line" Method
1+OON I-
0 + SON I-
f(?
LO 4 0-t-SOS
1-t-OOS
(^) Base Point
I - —— I
- ^^^ ~
W — J^"^ —— —— H
oo -
Fi-j^^*?•B P
J - —————— *
L1*OOE
::^—}
^ J- Tie-Line
I J
II)- -J
L2+OOE
® -*. Setting up Tie-Line and tielng back to base pointTie- Point -* Direction of travel
Reduced Instrumentation RequirementsThe self-correcting "tie-line" feature of the OMNI IV can remove base station requirements from some, surveys.
Tie-Line Capability In Gradient ModeThe "tie line" capability Is also applic able when used as a gradiometer. The operator can therefore obtain corrected total field data without re quiring a base station magneto meter.
Programmable DatumThe OMNI rv can be programmed to automatically remove a designated datum from field data. Removal of this coarse, background value facilitates plotting and interpretation of data.
Automatic Drift CalculationsThe OMNI iv can automatically calculate the desired diurnal drift measured between consecutive tie- point readings.
Data Recall"Tie-line" data can be recalled, even if stored on different days.
ea SOISAHdCOD 031W 6002SE6Z.08 E00Z/0Z/Z0
From: Paul E Nielsen To: Mik* Dale: 10/23/88 Time: 2:13:02 PM Page 4 of 5
SpaMtffeatlon*oyrwnlc Dang* .. . ,.. ... . . ... .,, .. , ... . le.OOCco 1io,OOD gammas. Roil-over dUBlav ***Eura
SuooraSta* f imilonlftenc digit upnnaKCMdlnB 100,000
Turma Metnae .. .,,. .. . ........... ,. . ..Tuningvaiu*licaeuiamdstcuriralv uniuing aipoclnlTyaavrtapM TiinlnB algorithm
AuccrrtaOcnne Tuning . . .. ... .,..,., .. x 15*4 ralaova to amotantflald (Iranst* of la*t Korea, valu*
Display Mnduttdrt. . .. .. .. . . -,...... . . .. . O.1 Bamma*roc**Uf*fl SepslQv'ty . .. .... . .,., ... r, . -. x 0.03 gami'TOMjuiuun error Kesolutlpn. - ....,..... . ... 0.01 aammaAbcoHjta Accuracy - - -. -. .............2-1 aamrDaac 3O,ooogamma4at 23*C
e 2 aanma ovar total ewmsarwura r*rv;a sandaro Mamorv caoiKicy
i .'.'.'., '.'.'.','.'.', ! ibodaOD*ockSora8CK7rr*aalno)i
ottoiav " . .. , ,., , - ....!..... - - - - - djccom-dmdgrnd. ruimdEEea liquid crynal dliplay witfi anaporadn0 tvmoaratura rana* from -9O*C to * SS^C. Th* dltpiay oamalm rix nunnrte digits, dacimal ortrre, biRery •sCBtiH monitor, sibnal decay rate and alonal amplltuiM menltsrand function dasenpcon.
ra 232 Serui I/O mterfage. - .......,.... . 2*00 baud, t o*ta Din, 2 stop bio. no oarley
TMt Mod* ., .... .... ..,... - -.. - .... .. . A. Dteanasdc te*flng (dscaand croararrunabl* rnamory)a. t*fTtit (ha rovrara)
sensor ,. .. ...... .... .., ,, ., .. .. ,. . oocJmlxvd mlnlatur* d**lgn, Yl*oneclc cwannrm li-. j- ' cpnsirotrn with me ipacmeo sosotute accuracy.
' " ' " ' ' ftammas/mecar, Oallond 1.0 mac*rsBmor tapjratlon awallabla. Kortzonm samsws optional.
Cycling tune (Base Sation MadM ..., .,., . Piui)rai-.imabla from S oeondB UP te to mlrmm In 1
ronrrmncM "*noe.. - - -. .... ... . j^^^-^^|^j^^^^^-|ijijjj(j-^-r pj1p0^jJ|j-ajreefv
carblOD* or Celt or 12V DC po*er source opden ror base rtathan operation.
dwnndlfia uoon ainaiinc twnDomturc ana rate ofraaaingi
wefghoand CKmwnliom innrumerrt contcne OWV.. . . .. . . . ., .., .. z* w, TSB a isoii aBOmmNicad or Ajicallne Bacta^carerMa* .... ... 1.3 ka, 315 x 105* 9QmmWO.d or Alkaline BattHryBWt..,.. .. .. .. -1.2 W. saoxiooxaomm
uaaOAOO Battery MR .... --'' '' '' '' '- '' llakaleMax-lBOxaommaansor ............ - - - -..... - - . - - -1.2 no. "8111111 oiamccw x aoommDradlanc lon*or ^
^ ^ ~" ii.,-. ' 2,1 kJ9, Bflf^Tl QlJtl ICC^r X 79UIt".1 f^rt^tth ^4H~iH*j~Sfii?oraW?ia*ros
.....,... 2.2 kg, Mmm diameter i* 13PBmm oratijriinMOwntt Tgronto,. ....... Imtrurnvnc corwole; aarnori S-met**- ea OIC. aluminum
laetlanal Krtsor stair, pOMV*r KiDDly. hane™ nomtjly. op*rat)ons manual,
l sanan option .. . ... .. ,.. . tunaard Jvspem plus X) rn 66m-cable•rODdon . . , . . . . . . , . . . . . . . .. Stanoarfl ivietm OHJjO,SrTwtar**nsor
Attachment l
170 SOISAHd039 031W E002/02/20
FREQUENCIES: 110,220.440.880.1760.3520.70401 140BOHZ.
COIL SEPARATIONS:
SETNO. 1: 12-5. 25. 50. 75. 100. 125. ISO. 200. 250. 300 and 400 metaac (the staadardsef). SETNO 2 10. 20. 40. 80. 80.100.120. 180. 200. 248 aad 320 metres (selected aa'ta grid tank* ia rocewer)SET NO. J: SO. 100. 200. 300. 400, 500. 500. 800. 1000. 1200 and 1800 feet (selected vritta grid natch ia receiver).
TRANSMITTERDIPOLE MOMENTS
MOOESOFOPERATION:
1760 Hz: taOAbn' 3520Hr 80A**5 7640 He 40ABH2
14080 Hz: 20Abr'
110 Hz: 220Atnr 270 Hz 21 S Aon1 440Hz: 210Aajr' 880 Hz: 200 Atm3
MAX 1 HerizOTtBt loop or iXngraai aad receiver cal planes horizontal aad coatasar MAX f. Vertical cooiaaar loop mod* friwmltter aad receiver coil planes vertical and coptaaar. MM 1: Punjoaefculei mode 1 - traiamittar to* plea* horizontal and receiver coil ptaae vertical. MID 2: Perpeadkator mod* 2 - traRsmrtter coil plaMvartfcal and receiver co j plane bortmntal
la-pnase and quadratare compoaeb of the secondary magaelk field, ia * of primary field.
Analog direct edgeejise meter raadeat* for m- p*aso, aaadratare and at AddWonal (igrtat LCD readouts provide m the optional MMC caaipatar. Irtertauig aad contrals are provided tar ready pajg-i* ofthaMUC.
Saitch activated analog ia-phase aad quiiatare scales: 0±4%, 0:t20H andO± 100X, aadalgnal
8tO±75H
PARAMETERS MEASURED:
READOUTS:
RANGES OF' READOUTS:
RESOLUTION
REPEATABILITY: 0.01 to 1 % of pmnary fjeld, typkal.depeadmgea beqeaaqr. coil separate* aad condttnns.
SIGNAL Power*** comb fitter, conbaaoas apeertc noise FILTERING: cfppiag, aatoedjasting nmo constant and more.
WARNING Receiver signal Md reference avniaf iolits a) LIGHT S: mdkate potential error coadffioiis.
Analog m-pkaM and aoodratar* 0.1 to 1 H o* priaiatf field. dapeKfeg on scale nad. dgftsl
SURVEY DEPTH PENETRATION
REFERENCE CABLE
INTERCOM:
TEMP. RANGE:
RECEIVER BATTERIES
TRANSMITTER BATTERIES
TRANSMITTERBATTERYCHARGERS:
RECEIVER WEIGHT:
From surface doam to 1.S Bines ceil separatioa for large horizontal target and 0.7S Bme* con ••ponton for tare* mace) tat***, ntoa* trpical.
14/2 ewfor majdnum oparatiag temperature mage aad for mamma oafiag friction
Vok* coonaaaicalion iak provided for operators via rte reference cable.
Winn 40 to pie* M degree* Cotton, opefeflag.
Foar staadard t V - 0.8 Aa akatiae battarias. Lfle 25 hours caathanas dety. hns in cold wu stair Optional 1J Ah extamtad life iBwrn battarias avatable (recemanaded for very cold enatJter)
Standard lacbaraaabta 9eMyp* laed-acid 12V- 14AD batteries (4 x 8 V - 12 AU) ia nylon be* pack. Opnenefy racaargeeMe loea He 12 V - 14 Aa mckal-cadamm batteries (20 x 1 .2 V - 7 Aa) aath al-cad diargan - best caoica for coM cmnatss.
Lead acid battery charger 14.4V Q12S A. Mi-cad bartary charger. 1.4 A S IS V. aoaaaal oaknt Operation Iron 110-120 and 220-240 VAC. SO- 80 Hz. and 12 - IS VDC nppin
8 Kg carrying anigat 0advdmg dw an lanN* cored aatanaa cois). 9 Kg arith MMC comparer.
TRANSMITTER WT 16 Kg carry M g meiofct
SHIPPING WEIGHT:
STANDARD SPARES:
60 Kg pies waigkt of rafaranca cable. alUKf per 100 moire, plea optional itean VHf. aaa]kM
nHailaaejiiiadtetd/ 1 ||aa) r linn.mtaanH
~|nii niiiiiiim*rMinii) (lin anM (faajaiiitir battety dtaroar. tan spare tnmsmoEer laliacHe conaectiag cords, spare set of receinr battarie* .
OPTIONS AND e MMC. MaxMia Campater apboa ACCESSORIES, * Data ialm pi ataBua aad preseataaea program s PLEASE SPECIFY: e- Rafereace cables, wagtta as raojafctad
e Reference cable eiteeiina adaytar , * Handheld wcfaanntaT for roegk tetraia
* RBcenaraxiaadad We ttHmm battarias* TraasmiUar af-cad battery ( charger opte* e Minanal. regalar or extended spare parts kit
SpocJVCslions subfod* to ctwiocs witttoul nutrfiLxtaun
93-10 -15
APPENDIX IV
KIM Dynamics Report
KIM Dynamics Exploration Mineral Services
#6-230 West 14th StreetNorth Vancouver, B.C., V7M 1P3
Tel. (604) 985 7542
NOTES ON PROCEDURES AND RESULTS
OF THE OBSERVATION OF THE SAMPLES
There are few following notes about the procedure of the work and the observation results:
PROCEDURE
* Due to enormously large sample weights and as it was agreed with Gitennes Exploration, only 1A of each sample was observed. In order to split samples on four
v equal parts the simple "splitter" that divides on two equal parts was used. Each sample was firstly divided into two halves and then one of the half was split again into two halves producing two 1A . The three of these portions were combined making 3A of each sample that was collected but ignored for the observation at this point of time. The one of these split portions, that made 1A, was placed in the separate bag, weighted and observed.
* Before the observation, each of those 1A samples was sieved through four mesh sizes that included 0.5mm, 0.4mm, 0.3mm and 0.25mm. The magnetic portion was removed by hand magnetite and combined with ^.25mm in the same plastic bag. This procedure produced five size fractions placed in the five separate bags, labeled: +0.5mm, -t-0.4mm, -H).3mm, H-0.25mm and "handmag * •tc0.25". All bags were weighted and weights were recorded. The size fractions, -+0.5, +0.4, +0.3 and +0.25mm were observed under the binocular microscope in order to pick any indicator mineral. The "handmag + ^.25mm" fraction was not observed.
* In order to keep detailed information about the observation for each sample, sample sheets were used.
RESULTS
* All samples have very similar background mineralogy. All of them consists predominantly of orthopyroxene (70*54 - 95Vo) and olivine (l"/o - 1007o). The ratio of those two minerals varies slightly among the samples. The other minor minerals are epidote, amfibole, rock fragments, clinopyroxene, ilmenite, sphene and staurolite.
Most of the olivine in the background is from the non-kimberlitic source. Based on their morphologies ("wavy" and "grooves" surfaces) and optical features (R.I. n^.69) they might be originated from komatite. These grains were not recorded as indicators but few of them from each sample were collected for the reference and kept in cards labeled "REJECTED".
The olivines that were recorded as indicators are morphologically (absence of "grooves" and pale green colors) and optically (R.I. n ^.69) different then above "background" olivines suggesting possible kimberlitic origin. Be aware that all these recorded olivines hardly show any resorption features characteristic for typical kimberlitic indicators suggesting that they also might be from non-kimberlitic source.
All recorded picroilmenite were marked as "possible" since they do not have typical kimberliic features. All of them would need checking (SEM or probing) before they are recorded as definitely kimberlitic.
The single occurrence of the beautiful, emerald green chrome diopside is recorded in samples 17547,17545 and 17554. Although tiny (4-25mm) these grains might be the only true kimberlitic indicators!
Based on the absence of pyrope garnet as the only certain kimberlitic indicator mineral and the vague kimberlitic features of the recorded indicators the kimberlitic signature of the examined samples has to be taken cautiously.
KIM Dynamics Exploration Mineral Services
#6-230 West 14th Street North Vancouver, B.C., V7M 1P3
Tel. (604) 985 7542
.KIM Lr
The Results o. uie Observation Dece;,..^-r, 2002
No
1
23456789
1011121314151617181920212223242526
Gitennes Samples
1752717530175591752917551175521755317554175551755617557175581756016581165821692316924169251692616927169281753117545175461754717548
Lab Samples
19491950195119521953195419551956195719581959196019612210221122122213221422152216221722182219222022212222
WEIGHTS
Total HMC
weights(g)
98.3
115.4
107.8
561.9
100.3
111.5
336.9
266.1
184.7
251.3
214.8
171.9
161.4
264.9
197.8
201.7
82.4
209.3
102.8
371.2
47.5
305.6
143.4
157.1
300.0169.5
1/4 of the HMC
weights(g)
22.0*
28.9
26.7
140.5
25.0
27.8
84.2
66.5
46.2
62.8
53.7
43.0
40.4
66.2
74.5
50.4
20.6
52.3
25.7
92.8
11.8
76.4
35.9
39.3
75.0
42.4
Observing
weights(g)
22.0*20.020.684.418.820.658.343.635.648.444.232.829.648.350.638.316.843.120.175.710.561.729.331.459.932.5
Handmag and
O.25mm weights
(g)0*
8.96.1
56.16.27.2
25.922.910.614.49.5
10.210.817.923.912.14.19.25.6
17.11.3
14.76.67.9
15.19.9
INDICATORS
Peridotite garnet
Eclogitic garnet
Chromite
1
Picroilm enite
20**
9**•i**
5**
Chrome Diopside
4
31
1
1
1
Olivine
2
7
15
2
Background minerals
opx, ol, epopx, ol, epopx, ol, epopx, ol, eppyrite!opx, ol, epopx, ol, epopx, ol, epopx, ol, epopx, ol, epopx, ol, epopx, ol, epopx, ol, epopx, ol, epopx, ol, epopx, ol, epopx, ol, epopx, ol, epopx, ol, epopx, ol, epopx, ol, epopx, ol, epopx, ol, epopx, ol, epopx, ol, epopx, ol, ep
Observing time
(hours)
7.2
7.0
10.5
18.0
6.3
7.0
16.0
13.2
10.2
14.3
12.5
10.010.012.512.09.05.5
12.05.8
16.52.0
14.07.27.5
10.012.7
Notes:
KIM Dynamics
* see sample sheet for details possible, need testing
The Results of the Observation Invoice N 0 1
KIM Dynamics Exploration Mineral Services
#6-230 West 14th Street North Vancouver, B.C., V7M 1P3
Tel. (604) 985 7542
SAMPLE DATA SHEET
Sample Number
t? 62?Observed by KIM Dynamics
Date of Observation
Observing time 07
S.CD
Size fraction (mm)
Weight (g)
Peridotitic garnet
Eclogitic garnet
Picroilmenite
Chromite
Chrome diopside
Olivine
TOTAL INDICATORS
+0.5
f.2
+0.4
8 J.*
g*1l2/Z,
+0.3
30 J
T
a,
1
+0.25
/23
^A
7f/l
Total Observed
x W
^0lt7-
3L
HandMag
4-
^.25^.y
NOT OBSERVED
\
TOTAL 1/4 of the
HMC
/4^. 5"
Comment
c/,•-G/' rx de.
KIM Dynamics Exploration Mineral Services
#6-230 West 14* Street North Vancouver, B.C., V7M 1P3
Tel. (604) 985 7542
SAMPLE DATA SHEET
Sample Number
Observed by KIM Dynamics
Date of Observation
Observing time
SCO
Size fraction (mm)
Weight (g)
Peridotite garnet
Eclogitic garnet
Picroilmenite
Chromite
Chrome diopside
Olivine
TOTAL INDICATORS
+0.5
Z. Z
+0.4
9*9
+0.3
4.9-+0.25
2.0
Total Observed
/#. ^
^
Hand Mag
4-
O.256.2,
NOT OBSERVED
i
TOTAL 1/4 of the
HMC
2S.0
Comment
KIM Dynamics Exploration Mineral Services
#6-230 West 14th Street North Vancouver, B.C., V7M 1P3
Tel. (604) 985 7542
SAMPLE DATA SHEET
Sample Number
Observed by KIM Dynamics
Date of Observation
Observing time v O
Se D
Size fraction (mm)
Weight (g)
Peridotitic garnet
Eclogitic garnet
Picroilmenite
Chromite
Chrome diopside
Olivine
TOTAL INDICATORS
+0.5
o.e+0.4
'•1+0.3
?.5
+0.25
f^
1
1
Total Observed
Zo.6
1
1
Hand Mag
+O.25^,2~
NOT OBSERVED
TOTAL 1/4 of the
HMC
J7.^
Comment
KIM Dynamics Exploration Mineral Services
#6-230 West 14th Street North Vancouver, B.C., V7M IPS
Tel. (604) 985 7542
SAMPLE DATA SHEET
Sample Number
Observed by KIM Dynamics
Date of Observation
Observing time
Size fraction (mm)
Weight (g)
Peridotitic garnet
Eclogitic garnet
Picroilmenite
Chromite
Chrome diopside
Olivine
TOTAL INDICATORS
+0.5
^.6
+0.4
2 Z. X
^
.z.6
+0.3
* /.S
3*
12
T
+0.25
ft * JG?
rt ^.
2/
H
Total Observed
53. 3
9
3rx?-
HandMag
O.25tt- J
NOT OBSERVED
i
TOTAL 1/4 of the
HMC
f 4. Z,
Comment
KIM Dynamics Exploration Mineral Services
#6-230 West 14th Street North Vancouver, B.C., V7M 1P3
Tel. (604) 985 7542
SAMPLE DATA SHEET
Sample Number
Observed by KIM Dynamics
Date of Observation
Observing time
Se O
Size fraction (mm)
Weight (g)
Peridotite garnet
Eclogitic garnet
Picroilmenite
Chromite
Chrome diopside
Olivine
TOTAL INDICATORS
+0.5
3 J
+0.4
ff-if
+0.3
/&Z.
t1*
1
+0.25
^
i
1
Total Observed
43.6
l
l
JL
HandMag
O.25^.?
NOT OBSERVED
i
TOTAL 1/4 ofthe
HMC
^K S~
Comment
KIM Dynamics Exploration Mineral Services
#6-230 West 14* Street North Vancouver, B.C., V7M 1P3
Tel. (604) 985 7542
SAMPLE DATA SHEET
Sample Number
Observed by KIM Dynamics
Date of Observation
Observing time f O.
Size fraction (mm)
Weight (g)
Peridotitic garnet
Eclogitic garnet
Picroilmenite
Chromite
Chrome diopside
Olivine
TOTAL INDICATORS
+0.5
0*6
+0.4
W
+0.3
/3.^
+0.25
//.J
Total Observed
3G.6
^
HandMag
+O.25W. 6
NOT OBSERVED
TOTAL 1/4 ofthe
HMC
^.J2.
Comment
KIM Dynamics Exploration Mineral Services
#6-230 West 14* Street North Vancouver, B.C., V7M IPS
Tel. (604) 985 7542
SAMPLE DATA SHEET
Sample Number
Observed by KIM Dynamics
Date of Observation
Observing time f 4.
Size fraction (mm)
Weight (g)
Peridotitic garnet
Eclogitic garnet
Picroilmenite
CJbromite
Chrome diopside
Olivine
TOTAL INDICATORS
+0.5
/7
+0.4
ft. Z
+0.3
P. Z
+0.25
/#r
Total Observed
4Z4
^^
Hand Mag
-t- O.25ft.*1
NOT OBSERVED
TOTAL1/4 of the
HMC
6X.^
Comment
KIM Dynamics Exploration Mineral Services
#6-230 West 14* Street North Vancouver, B.C., V7M 1P3
Tel. (604) 985 7542
SAMPLE DATA SHEET
Sample Number
Observed by KIM Dynamics
Date of Observation
Observing time
SG. O
Size fraction (mm)
Weight (g)
Peridotite garnet
Eclogitic garnet
Picroilmenite
Chromite
Chrome diopside
Olivine
TOTAL INDICATORS
+0.5
/.*
+0.4
/^.*f
;;
+0.3
/^
;y
+0.25
/0JL
Total Observed
^.z
^2-.
HandMag
+ O.2525"
NOT OBSERVED
i
TOTAL 1/4 of the
HMC
S3. 7-
Comment
KIM Dynamics Exploration Mineral Services
#6-230 West 14th Street North Vancouver, B.C., V7M IPS
Tel. (604) 985 7542
SAMPLE DATA SHEET
Sample Number
Observed by KIM Dynamics
Date of Observation
Observing time
TILL.
Size fraction (mm)
Weight (g)
Peridotitic garnet
Eclogitic garnet
Picroilmenite
Chromite
Chrome diopside
Olivine
TOTAL INDICATORS
+0.5
/.T
+0.4
/?.7-
+0.3
//.f
+0.25
^rTotal
Observed
3A.8
^
HandMag
+O.25/O.Zs
NOT OBSERVED
\
TOTAL 1/4 ofthe
HMC
43.0
Comment
KIM Dynamics Exploration Mineral Services
#6-230 West 14th Street North Vancouver, B.C., V7M 1P3
Tel. (604) 985 7542
SAMPLE DATA SHEET
Sample Number
Observed by KIM Dynamics
Date of Observation
Observing time
Tr
/O.
Size fraction (mm)
Weight (g)
Peridotite garnet
Eclogitic garnet
Picroilmenite
Chromite
Chrome diopside
Olivine
TOTAL INDICATORS
+0.5
/•B
+0.4
//.f
+0.3
(0.4
^
3
+0.25
^
2*
1
3
Total Observed
a?, t
JT
1z
HandMag
-t- O.25
/O. X
NOT OBSERVED
TOTAL 1/4 of the
HMC
fa f
Comment
02badgertill_020922.xls SAMPLES
GITENNES EXPLORATION INC.Badger Property
Table IV-1: September 2002 Till and Stream Sediment SamplingC:\Gitennes\Badger\Assessment\030331filing\02badgertill_020922.xls
10/04/2003 10:08 AM
SAMPLE17529175511755217553175541755517556175571755817560
PROJECTBadgerBadgerBadgerBadgerBadgerBadgerBadgerBadgerBadgerBadger
ZONE16161616161616161616
NAD27E318653316535319447319361319026318186317528318370314744317448
NAD27N5486840548206354855075485393548520354838745482931548422154865485483186
SAMPLERJRFJRFJRFJRF
CL/KJRCL/KJRCL/KJRCL/KJR
KJRJRF
DATE27-Sep-200218-Sep-200221-Sep-200221-Sep-200221-Sep-200221-Sep-200221-Sep-200221-Sep-200222-Sep-200221-Sep-2002
DESCRIPTIONslream sed, screened lo -1/4 meshcamp creek 2 m upstream of culvertfine sand sill, no pebblesslream sed, screened to -1/4 meshstream sed, screened to -1/4 meshfine sand silt, no pebblesfine sand silt, no pebblesfine sand silt, no pebblesgy bn till above granitoid o/cboulder till, silt/clay mx
Au ppm
0. 005O.OOS0.005O.OOS0.005O.OOS0.005O.OOS0.0050.005
Ag ppm0.20.20.20. 20. 20.20. 20.2O.20.2
AlV,
0.531.220.790.680.710.720.970.831.531.01
As ppm
*240^•:2*2*2^^^*2
B ppm
•MO"MO•CIO"10•MO•c10*10•*10•MO•MO
Ba ppm
7011080
100705080704070
Be ppm0.5O.50.5O.50.5O.50.5O.50.50.5
Bi ppm
^^•:2^•:2^^^^^
Ca V.
0.281.010.480.380.440.430.490.51
0.60.57
Cd ppm0.5O.50.5O.50.5O.5O.50.5O.5O.5
Co ppm
2919
71612
6128
1613
Cr ppm
921167883857785976371
Cu ppm
54603319191232124938
Fe•A
11.458.062.075.723.921.713.3
2.253.963.49
Gappm
2010101010
•MO10101010
Hg ppm
C1
•C1•M•M•M•M•M•C1
<1•M
K•f.
0.050.080.050.040.040.030.050.040.130.04
Page 1 of 2 C:\Gitennes\Badger\Assessment\030331filing\02badger1ilL020922.xls
02badgertill_020922.xls SAMPLES
GITENNES EXPLORATION INC.Badger Property
Table IV-1: September 2002 Till and Stream Sediment SamplingC:\Gitennes\Badger\Assessment\030331filing\02badgertill_020922.xls
10/04/2003 10:08 AM
SAMPLE17529175511755217553175541755517556175571755817560
PROJECTBadgerBadgerBadgerBadgerBadgerBadgerBadgerBadgerBadgerBadger
ZONE16161616161616161616
NAD27E318653316535319447319361319026318186317528318370314744317448
NAD27N5486840548206354855075485393548520354838745482931548422154865485483186
SAMPLERJRFJRFJRFJRF
CL/KJRCL/KJRCL/KJRCL/KJR
KJRJRF
DATE27-Sep-200218-Sep-200221-Sep-200221-Sep-200221-Sep-200221-Sep-200221-Sep-200221-Sep-200222-Sep-200221-Sep-2002
DESCRIPTIONstream sed, screened to -1/4 meshcamp creek 2 m upstream of culvertfine sand silt, no pebblesstream sed, screened to -1/4 meshstream sed, screened to -1/4 meshfine sand silt, no pebblesfine sand silt, no pebblesfine sand silt, no pebblesgy bn till above granitoid o/cboulder till, silt/clay mx
La ppm
•MO•C10^0
1010
•MO^0•MO
1010
Mg 14
0.360.840.360.340.220.270.510.270.710.47
Mn ppm
5601035
197383245155280260362340
Mo ppm
•M311111111
Nay.
0.030.12
0.10.070.090.09
0.10.110.120.12
Nl ppm
72482143281734194034
P ppm
100340200180200210260200520320
Pb ppm
3633
*22433
*2
S1.
•:0.012.120.010.01
O.010.01
O.010.01
•:0.01O.01
Sb Ppm
62^
44^^
224
Se ppm
2222212122
Sr ppm
4191510131314152017
Tl•h
0.970.320.170.650.450.170.250.210.250.26
Tl ppm
•MO•MO^0•MO^0^0^0^0•MO^0
uPPm
2010
•MO1010
•MO^0^0
1010
V ppm1225335125549365110223151209233
W ppm
1010
"MO•MO^0^0^0^0•MO•MO
Zn ppm
146823282673146415239
Page 2 of 2 C:\Gitennes\Badger\Assessment\030331filing\02badgertill_020922.xls
MINISTRY OF NORTHERN DEVELOPMENT AND MINES
Transaction No: Recording Date: Approval Date:
Client(s):400504
Survey Type(s):
W0340.00646
2003-APR-14
2003-MAY-01
Work Report Summary
Status: APPROVED
Work Done from: 2002-SEP-09
to: 2002-OCT-01
GITENNES EXPLORATION INC.
ASSAY
MAG
BENEF EM GCHEM
Work Report Details:
Claim*
TB
TB
TB
TB
TB
TB
TB
TB
TB
TB
1221171
1221192
1221194
1241563
1241564
1241565
1241566
1245616
1245617
1245618
Perform
31,612
31,612
S1.100
33,015
312,604
SO
30
31,100
33,470
31,810
326,323
External Credits:
Perform Approve
31,612
31,612
31,100
33,015
312,604
SO
SO
S1.100
33,470
31,810
326,323
SO
Applied
SO
SO
SO
S6.400
S6.400
36,400
36,400
SO
SO
SO
325,600
Applied Approve
303030
36,400
36,400
56,400
S6.400
30
SO
SO
S25.600
Assign
31,612
31,612
31,100
SO
S5.481
30
30
31,100
33,470
31,810
316,185
Assign Approve
1
1
1
,612
,612
.100
0
5,481
1
3
1
516
0
0
.100
,470
.810
.185
Reserve
SO
5050SO
S723
SO
SO
soSO
SO
5723
Reserve Approve
SO
SO
SO
SO
S723
SO
sosososo
3723
Due Date
2003-AUG-10
2003-AUG-10
2003-AUG-10
2004-AUG-21
2004-AUG-21
2004-AUG-21
2004-AUG-21
2003-AUG-30
2003-SEP-13
2003-SEP-13
Reserve:S723 Reserve of Work Report*: W0340.00646
S723 Total Remaining
Status of claim is based on information currently on record.
52H11SW2004 2.25432 KITCHEN LAKE 900
2003-May-06 14:34 ArmstrongjJ Page 1 of 1
(Viiiiistry ofNorthern Developmentand Mines
Date: 2003-MAY-01
Ministers du Developpement du Nord et des Mines Ontario
GEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E 6B5
GITENNES EXPLORATION INC. 36 TORONTO STREET, SUITE 1000 TORONTO, ONTARIO M5C 2C5 CANADA
Tel: (888) 415-9845 Fax:(877)670-1555
Dear Sir or Madam
Submission Number: 2.25432 Transaction Number(s): W0340.00646
Subject: Approval of Assessment Work
We have approved your Assessment Work Submission with the above noted Transaction Number(s). The attached Work Report Summary indicates the results of the approval.
At the discretion of the Ministry, the assessment work performed on the mining lands noted in this work report may be subject to inspection and/or investigation at any time.
If you have any question regarding this correspondence, please contact BRUCE GATES by email at [email protected] or by phone at (705) 670-5856.
Yours Sincerely,
Ron GashinskiSenior Manager, Mining Lands Section
Cc: Resident Geologist
Gitennes Exploration Inc. (Claim Holder)
Assessment File Library
Gitennes Exploration Inc. (Assessment Office)
James R. Foster (Agent)
Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:18237
ONIMUOCANADAMining Land Tenure
MaP
o oM
O H
m inN
3210006 322000E
MMOOON
6486000N W
•R vvf " Vi54MOOONC-™,*
54B2000N
547BOOON
MrSOOON
847TOOON
5476000N -r-
309000E 310000E 312000E 316000E 322000E
UTM Zone 16 1000m grid
rre*w *nntna*5M"lw rrtnOM cl*lmilvMiia tomuK wtthlht Pmrtcttl MWno Rocoia*(i" Dftlwol thaMntttiyot Northom DwBbpnvm *rM Mlnw tw *1dHten*l rtatrmiton an Irt
n iwy *l** b* obUinn) IhwugH Hw tac*| Land T*)** or togteln W!)w, ei it* MtiAtty ot Noturtl A
General Information and Limitations
Date /Time of Issue: Thu May 01 09:43:19 EOT 2003
TOWNSHIP l AREA PLAN KAIASHK LAKE AREA O-0735
ADMINISTRATIVE DISTRICTS l DIVISIONSMining Division Thunder BayLand Titles/Registry Division THUNDER BAYMinistry of Natural Resources District THUNDER BAY
TOPOGRAPHIC Land Tenurefnwhnta Paumt
jjj iLrta-
|;jjjj;'j 8u
ra M
MtoWto
m U
Tjkl Surtau AM Mtr*xj IBi
g]
i"""""""'".':L..1!?!:LAND TENURE WITHDRAWALS
Ordv hi Qwrx*! Mol upwn tof kd
WMft4 *t* WIW-BWWi Tnm
Wl IUMri N#liianfr WMnm
i IMPORTANT NOTICESl
LAND TENURE WITHDRAWAL DESCRIPTIONSld*rrtHI*r Typa Daw D*W*WbH
W-LL-C2410 ..Worn Aw IS, 2CCQ ** twef*" Mlti:.Vww#.mndmoov.Dn.W.ir/U W* *n 1,309! M.T.C. SEC.ddlMi.ir/r4 !W4iT4t,tl.O. 111103W-LL-Pece-l :Wam Aus S* ( tOCC in I
2.25432ASSAYGCHEMBENEFMAGEM
Mip txkim MAO B ri tctww Bid !**4 MM4Itui nttitt w tKttMInv antry batata nMni BMW nvr iral
Ul nmllE*- UntlMnnwnti.KC^M'^
