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DEB EERSDe Beers Canada Exploration Inc.

SUMMARY OF EXPLORATION WORK ON ANOMALIES SP3-0011 CLAIM P1242319

AND

029 CLAIM P1242329 SpiDER-3 JOINT VENTURE

SUBMITTED TO:PROVINCIAL RECORDING OFFICE

MINISTRY OF NORTHERN DEVELOPMENT AND MINESFOR ASSESSMENT WORK PURPOSES

HOLDER:DE BEERS CANADA EXPLORATION INC.

UNIT4, 2555 MALEY DRIVESUDBURY, ONTARIO

P3A 4R7

AUTHOR: DEIRDRE O'DONOHOE ANTONY FRENCH

ASSESSMENT DATE: MARCH 09, 200 DOCUMENT DATE: MARCH 06, 200:

RECEIVEDMAR O 7 2003

GEOSCIENCE ASSESSMENTOFFICE

Distribution: Provincial Recording (2)Copies: DBCE - Toronto, Sudbury, Field and Spider Resources

KEYWORDS: Assessment Report, James Bay Lowlands, MMI, Geophysics, Ground Magnetic Survey, Helicopter Magnetic/Electromagnetic Survey, Environmental Water Monitoring, Drilling, Assays, PIMA

Classification Code: L010 ICD#: M/7086 Project Number: 1043

43D16SE2001 2.25123 BMA 527 861 010

EXECUTIVE SUMMARY

De Beers Canada Exploration Inc. (DBCEI) carried out a diamond exploration program in the James Bay Lowlands area of Ontario as part of a joint venture partnership with Spider Resources Ltd. Two mineral claims were staked to the north of McFaulds Lake, 300kms north of Nakina, Ontario and are the subject of this work assessment report which satisfies the requirements of the Ontario Mining Act. Work has been carried out in the area over the past two years in an effort to locate kimberlites, which are one of the primary source rocks for diamonds. Work conducted within the claims included, Mobile Metal Ion (MMI) geochemical surveying, helicopter-borne Magnetic and Electromagnetic geophysical surveying, ground magnetic surveying and Reverse Circulation Drilling. Although no kimberlite type rocks were intersected during drilling the analyses of the geochemical samples submitted for assay showed copper values averaging J.69% over a 7.3 metre drilled intersection on anomaly SP3-0029. Total exploration expenditure for this program was S200,443.54. Further work is recommended as follow-up to the anomalous geochemical response.

CONTENTS

1.0 INTRODUCTION

1.1 Location and Access 7

1.2 Property Description and Ownership 8

1.3 Physiography and Vegetation 9

1.4 Geology 91.4.1 Precambrian Geology 101.4.2 Palaeozoic Geology 101.4.3 Quaternary Geology 11

2.0 WORK PROGRAMS_________________________________12

2.1 Mobile Metal Ion Geochemical Survey 132.1.1 Sampling Procedures 132.1.2 MMIl Sample Treatment and Analysis 142.1.3 MMI Geochemical Survey Results 14

2.2 Helicopter-borne Magnetic and Electromagnetic Survey 15 2.2.1 Helicopter Survey Results 15

2.3 Ground Magnetics 16 2.3.1 Ground Magnetic Survey Results 16

2.4 Exploration Drilling 162.4.1 Assay Results and Discussion 172.4.2 PIMA Spectral Response 182.4.3 Water Quality Monitoring 18

3.0 EXPLORATION EXPENDITURES________________________19

4.0 CONCLUSIONS AND RECOMMENDATIONS_________________19

5.0 REFERENCES_____________________________________21

6. 0 STATEMENT OF QUALIFICATIONS_______________________2J

FIGURES

Figure 1: .... Project Location Map 7

Figure 2:.... Property Location Map 8

TABLES

Table 1: Mineral Claims ................................................. 9

Table 2: Stratigraphy - James Bay Lowlands .............................. 10

Table 3: Work Summary................................................ 12

Table 4: Drillhole Summary............................................. 17

Table 5: Personnel ..................................................... 19

APPENDIX

Appendix 1: MMI Geochemical Survey.

Appendix 2: Helicopter Magnetic Survey

Appendix 3: Ground Magnetic Survey

Appendix 4: Reverse Circulation Exploration Drilling

Appendix 5: Assays

Appendix 6: PIMA Geochemistry

Appendix 7: Environmental H2O Monitoring.

Appendix 8: Statements of Exploration Expenditure .

1.0 INTRODUCTION

De Beers Canada Exploration Inc. (DBCEI) entered into a joint venture partnership with Spider Resources Ltd in 2000 as part of a regional diamond exploration programme in thejames Bay lowlands area of Northern Ontario. An interpretation of a reconnaissance fixed-wing aeromagnetic survey carried out by Spider Resources provided magnetic anomalies that were possibly related to deep-seated kimberlitic type intrusives. This information was therefore used as the rationale to stake mineral claims over a number of selected anomalies. Exploration work as follow-up to the fixed-wing anomalies included helicopter-borne geophysical surveying, geochemical sampling, environmental water monitoring and exploration drilling. This work was conducted over a period of two years between March 2001 and December 2002. This report summarizes the exploration work conducted over two of the mineral claims (P1242319 and P1232329) which covered two magnetic anomalies that were deemed to be related to deep-seated intrusives and is therefore submitted in accordance with the assessment work requirements of the Ontario Mining Act.

1.1 Location and Access

The surveyed mineral claims are located within the James Bay Lowlands area of Northeastern Ontario, approximately SOOkms north of the township of Nakina (Figure: 1).

Spider3 Joint Venture

ik Lake Camp

ON

Figure 1: Project Location Map

The operational base for fieldwork was located near Highbank Lake while the DBCEI office in Sudbury, Ontario, provided logistical and managerial support. The Highbank Lake camp was situated on First Nations traditional lands, 75 kilometres north of the Marten Falls community. The joint venture project also impacted on other First Nations communities of Webequie 105 kilometers to the north-northwest and Neskantaga (Landsdown House), 115 kilometers to the west- southwest. (Figure: 2)

Location Map of Mineral Claim Blocks P1242319, P1242329

n

UTM Nad 27. Zone 16 NTS.43C, 430 January 7. 2003 Author Deirdre Odonohoe Drawn by: An Ik Boucher

LEGEND

l j DBCEI Claims

Figure 2: Property Location Map

rr

1.2 Property Description and Ownership

The two mineral claims forming the subject of this report were staked on March 9, 2001 in the Porcupine Mining Division of Ontario. Claim P1242319 occupies nine units each of 16 hectares while the second claim P1232329 occupies six units. The claims were staked to cover anomalous magnetic targets selected from a fixed- wing total intensity aeromagnetic survey. De Beers Canada Exploration Inc currently holds a 100*56 interest in both of these claims on behalf of the Spider

8

Resources Ltd Joint Venture in which it has earned a SI'% interest. By agreement additional interest can be earned if so required. Information on the claims is listed in Table 1 below.

Table 1: MINERAL CLAIMS

Claim Number

P1242319

P1232329

Recording Date

March 09,2001

March 09,2001

NTS Map Sheet

43 D/16

43 D/16

OBM

527 861

527861

Mining Division

Porcupine

Porcupine

G-Plan

G-4306

G-4306

Claim Size 16 Ha units

09

06

1.3 Physiography and Vegetation

The topography of the James Bay Lowlands area consists of gently rolling plains of low relief with an average decrease in elevation of roughly 100 metres from southwest to northeast towards James Bay.

Drainage throughout the work area is poor, with vast areas of muskeg, string bogs, shallow ponds and drunken forests. Streams and rivers are generally incised five to ten metres below the surrounding terrain, and drain in an easterly direction towards James Bay. Four main rivers transect the area; they are the Attawapiskat, Muketei and Ekwan Rivers and the Winiskis Channel. Smaller tributaries tend to have poorly defined channels and marshy type borderlands. Lakes in the area are generally constrained to the southern portion of the project area and are typically small and shallow.

Ground cover across the area is variable, spanning the subarctic forest and tundra transition zone. In the southern part of the project area, large black and white spruce and tamarack are fairly common which become smaller further to the north where larger trees are restricted to narrow bands along rivers and creeks and on well-drained raised beaches. In the southern portion of the area, trembling aspen, balsam poplar and white birch are present locally, but occur only on the driest sites in the northern part of the work area. North of the Attawapiskat River tundra terrain characterized by stunted vegetation is prevalent.

Organic deposits ranging up to 4.5 metres in thickness are common and no topsoil horizons have developed. The thick peat layer is seen to lie directly over the top of glacial and post-glacial marine deposits. Raised beach ridges forming one to two metre local topographic highs are only slightly better drained than the surrounding terrain and often support a local ecosystem of mixed white spruce and birch.

1.4 Geology

The project area lies along the western margin of the Superior craton on the contact between the Archaean and Palaeozoic rocks. The work area however contains very little rock outcrop except for scattered exposures along some of the

9

riverbanks. Table 2 below highlights the general geological formations for the project area.

Quiiicnaoc/ Rejceot Alluvium, glaciolacustrine deposits, multiple tills (Wisconsinian and Sangamonian)

Major Unconformity --P-

; A: - lE Q ZO1 - C

Silurian Severn River Formation: fossiliferous limestone

Disconformity: 438 Ma

Ordovician

Churchill River Group: stacked transgressive/regressive sequences: sandstone, limestone, mudstone, evaporite

Disconformity

Bad Cache Rapids Group: sub tidal to intertidal marine sediments: quartz sandstone, dolostone, minor shale

Major UnconformityPRICAMBRAIN

(Archaean)Metavolcanics, porphyritic granite, gabbro, diorite, minor

iron formation

Table 2: STRATIGRAPHY, JAMES BAY LOWLANDS

1.4.1 Precambrian Geology

Regional aeromagnetic data suggests that the older Archaean basement rocks consist of magnetically complex intervals of volcanic and sedimentary rocks within large blocks of granite and high-grade gneissic rocks of likely sedimentary derivation. Highly sheared mafic metavolcanics, coarse-grained porphyritic granite, mafic volcanics and porphyritic granite with local intrusions of diorite and gabbro are all thought to be represented in the area.

Structurally the area is also quite complex. The region lies within the Trans- Hudson Orogen of the Superior Craton which follows an east-southeast trend from the Nelson River in Manitoba to north of the Ekwan River at which point it turns sharply northward towards the Cape Smith Fold Belt on Ungava Peninsula. The Winisk Fault Zone trends in an east-southeasterly direction across the northwest portion of the area with prominent linears parallel to this trend apparent in aeromagnetic coverage further to the south. Other fault and dyke directions are also evident on the aeromagnetic maps, the most prominent of which generally have a north-south orientation.

1.4.2 Palaeozoic Geology

Formation of the Hudson Bay and Foxe basins during the Palaeozoic was a result of continental uplift along various arches and basement structures. The project area is bordered to the east by two large Phanerozoic sedimentary basins which are divided by the northeast trending Transcontinental Arch, with the Hudson Bay Basin found to the north of the arch, and the Moose River Basin to the south. With the inundation of the continental craton by the Tyrell Sea,

10

these intracratonic basins became depositional environments for sedimentary sequences overlying the exposed Archaean basement.

The lowermost Palaeozoic unit present in the work area represents the initial marine transgression over the Superior Craton during Middle to Upper Ordovician time, and is called the Bad Cache Rapids Group (BCRG). This unit which is comprised of poorly cemented basal calcareous sandstone grading upwards into siltstone and cherty limestone consists of two distinct formations deposited in intertidal to subtidal marine environments within the Moose River Basin.

Disconformably overlying the BCRG are mixed sediments of a second major marine transgression, the Churchill River Group (CHRG). This group of allochemical rocks is comprised of a stacked series of transgressive/regressive sequences containing alternating beds of well-sorted sandstone and limestone at the base of the unit. Where the transgression experienced a slight dissipation during Upper Ordovician time, some areas experienced a minor regression wherein sediments were deposited in a restricted marine environment resulting in localized deposition of finely bedded light grey mudstone and evaporite.

Marking the 438 Ma Ordovician/Silurian boundary is a sharp disconformable contact between mudstone of the Red Head Rapids Formation and fossiliferous limestone of the overlying Severn River Formation.

1.4.3 Quaternary Geology

The Quaternary geology of the Joint Venture project area is not well recorded and is further complicated by several different glacial advances and re-advances across the area. The region is also the focus of debate as to the location of centers of glacier buildup and ice dispersal. The stratigraphic record of the Hudson Bay Lowlands is known to consist of three or more old (Sangamonian) tills, interglacial formations, several younger (Wisconsin) tills separated by sand and silt beds of uncertain age, and a post glaciolacustrine and marine sequence (Fulton, 1995).

In his study of the Hudson Bay Lowlands, Thorleifson (1989) recognized up to five tills and ice flow trends based on lithofacies sequences, till composition, bedrock striations and pebble fabric analyses. The oldest and most rarely exposed till at the base of the sequence (till E) is the product of southward flow, whereas till D, enriched in Paleozoic erratics from the east, yields a southeast to northwest flow vector. Till C, which yields sparse pebble fabric data and boulder pavement striae, according to Thorleifson indicates an east- west orientation and probably westerly glacier flow. The most extensive till in the area, till B, is associated with southwesterly ice flow indicated by striated boulder pavements and surface fluting. The uppermost till, till A, which occurs only under the pattern of converging but generally north to south glacier flow in the work area, is best preserved in landform/lake lineations throughout the low land area. Much of the glacial deposits from the various

11

episodes have also undergone subsequent redistribution by alluvial action. The possibility of encountering pre-Wisconsin till in some buried valleys in the area is believed to be high.

Surficial geological mapping undertaken by Prest (1963) indicates. Till and glaciofluvial sediments comprising eskers and kames, and possible marine beaches occur at surface. Prest demarcates the marine limit at approximately 86" 05' W but indicates that terrain further to the west was likely covered in part by a proglacial lake. In fact, the vast majority of the work area is poorly drained and is underlain by up to 4.5 metres of peat forming bogs and fens. South of latitude 52 0 N, up to lO'JG of the area is underlain by permafrost, whereas north of this latitude, ID-50% permafrost is present. The effects of permafrost are evident in the shape of round, shallow lakes throughout the area as well as by two to three metre high palsas covered by dense stands of black spruce which are characteristic of periglacial processes elsewhere in the sub arctic.

2.0 WORK PROGRAMS

Exploration work on the two mineral claims was conducted during the summer of 2001. Soil or organic samples were collected for mobile metal ion (MMI) geochemical analyses and a helicopter-borne geophysical survey was completed as follow-up to the two anomalies selected from a fixed-wing airborne geophysical survey. See Table 3 below for details on the work completed on each anomaly.

Claim NumberDBCEI NumberMMI

Ground MAG Survey

Helicopter MAG/EM Survey

Environmental Water Monitoring

Exploration Drilling

Assay

PIMA

Number of SamplesYear of SurveySurvey NameYear of SurveySurvey Name

Year of Survey

Survey Completed

Year of SurveyDrill Hole NameYear of DrillingSurvey CompletedYear of AssaySurvey CompletedYear of Assay

P 1242319SP3 00117

2001SP3 0192001Yes

2001

Yes

2002SP3-02-006R2002No2002Yes2002

P1242329SP3 00298

2001SP3 0292001Yes

2001

Yes

2002SP3-02-007R2002Yes2002Yes2002

Table 3: WORK SUMMARY

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Exploratory drilling was then carried out over both anomalies during the summer of 2002. Clay material encountered during this drilling underwent spectral analyses using a PIMA instrument to determine any relationship to clays typically derived from a kimberlite source rock. Drillhole samples were also submitted for analyses to indicate any anomalous intersections. The water quality in the vicinity of each drill site was also monitored as part of the drill program.

2.1 Mobile Metal Ion Geochemical Survey

Mobile metal ions (MMI) are ions that are loosely attached or interstitial within the near surface soil particles. Most metallic ions are produced during the oxidation of an ore body and go into solution and are absorbed into the overlying soil, often attaching to larger particles. They are generally present in low concentrations and are transported through the soil column by evaporation and capillary rise. Mobile metallic ions are detected by using a weak partial extraction method and may reflect the underlying chemistry of their parent source, which in turn may indicate geochemical signatures undetectable by more conventional methods. Due to higher resolution, MMI anomalies are usually sharply bounded, and are directly related to the boundaries of the geological phenomena that they distinguish.

2.1.1 Sampling Procedures

Sample traverses covering both the geophysically anomalous area and the anomaly background were conducted at various intervals depending upon the size and shape of each anomaly. A traverse was planned to collect seven or eight samples along a line from outside the target body, across its center to the opposite side of the body. Two samples were collected at either end of the traverse to provide a background response. The sample locations were recorded in the field using a Garmin 12XL hand held GPS that has an accuracy of +I- 30m.

An extendible steel auger made up of 13 individual one-foot sections with a stainless steal enclosed cylindrical headpiece was used on both surveys. Other equipment often utilized during the sampling procedure was a hoe-pick and shovel that allowed for deeper penetration of the peat layer. For some sites however these methods were not sufficient to reach the mineral soil and a sample could not be obtained.

The auger was pushed into the ground through the overlying peat layer until the sediment contact surface was met. The auger was then brought to the surface and the sediment was cleaned as best as possible of organics and placed in a plastic "Zip-lock" bag. The sample was then labeled using sample tickets supplied by XRAL Laboratories.

In almost all sample locations, the water table was near surface. Duplicate samples were collected randomly as a method of testing lab quality control.

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2.1.2 MMI Sample Treatment and Analysis

For kimberlitic exploration a specific set of elements indicative of kimberlite chemistry are chosen for MMI analyses. These include a suite of elements native to kimberlite as well as the rare earth elements. Samples were subjected to a weak leaching solution that contains ligands that complex with the selected suite of mobile metal ions to bring them into solution. This solution was then analyzed by standard solution ICP-MS. Detailed sample treatment and laboratory procedures as well as the complete analyses can be found in Appendix l. The MMI-D suite of elements used for the detection and discrimination of kimberlite-type MMI anomalies is as follows:

XRAL Laboratories - Kimberlitic MMI Element SuiteNi, Co, Pd, Cr, Nb, Mg MMI-D base packageRb, Ti, Ba, La.TaCe, Pr, Nd, Sm, Gd, Tb, Er, Yb Full rare earth spectrum

Standard SampleThe De Beers Standard Sample known as V6219 accompanies each set of samples run through XRAL laboratories. This sample is composed of 4.31 kg of dry, clean, minus 0.3 mm quartz-dominated concentrator table tailings with 0.72 kg of minus 0.3 mm weathered kimberlite included. The standard is run to aid in determining the analytical efficiency of the above elemental package.

MMI Data ManipulationThe raw data was formulated to determine a response ratio for each element ofeach individual sample. Response ratios are determined by calculating the meanof the lowest quartile of a data set and then using this value divided against theppb of the element. The result is a quick means of determining anomaloussamples.

Response ratios for MMIs with concentrations below that of the lower limit of detection were set to nil, thus excluding them from further analysis. MMI results are displayed in Appendix l as stacked bar charts, where each stacked bar represents the total response of all mobile metal ions.

2.1.3 MMI Geochemical Survey Results

Anomaly SP3J)011 Claim P1242319A sampling traverse was conducted from the southeast to northwest across the P1242319 claim area (anomaly SPS^OII). Seven samples in total were collected across the anomaly. See Appendix l for details

MMI data interpretation does not show a well-defined geochemical anomaly. There is however a slight increase in the concentration of elements beginning at sample 19061 and ending at 19065. These sample locations are coincident with the geophysical anomaly. Sample 19065 has the most anomalous response but is located to the northwest of the magnetic high. These results are not indicative of any kimberlitic response.

14

Anomaly SP3.0029 Claim P1242329The sampling traverse over anomaly SP3-0029 (P 1242329) was conducted from the southeast to the northwest crossing both the high and low sections of the dipolar anomaly. Eight samples were collected in total. Vegetation in the area is dense with undulating topography that increases slightly to the north- northwest. The depth to the sediment below the peat cover decreases towards the northwest and the type of sediment changes from a till to a gravel in the same direction.

Directly below the glacial and marine sediments of this anomaly location are the Paleozoic sediments of the Churchill River Group of the Hudson and Foxe Basins. West of these sediments and possibly below the Paleozoic sediments are a unit of foliated to massive tonalite to granodiorite as well as basaltic and andesitic flows, tuffs and breccias of a mafic to intermediate metavolcanic suite.

MMI results were unable to produce an anomaly indicative of a kimberlitic response. The two anomalous samples collected over the target occur at what looks to be the edge of the inferred body. See Appendix l for details.

2.2 Helicopter-borne Magnetic and Electromagnetic Survey

The Ministiko Lake Survey covering the two claim areas was flown using a high- resolution helicopter magnetic and frequency domain electromagnetic system (DIGHEMv-DSP). This survey allowed for better definition and discrimination of the two anomalies selected from the reconnaissance fixed-wing aeromagnetic survey.

The survey was undertaken by Fugro Airborne Surveys Inc. and commenced on July 13 th , 2001. The Highbank Lake camp was used as base for operations. The survey specifications are described in Appendix M.

2.2.1 Helicopter Survey Results

Anomaly SP3J)011 Claim P1242319A strong dipolar magnetic anomaly with a magnetic intensity of 5,000 nT was delineated from this survey. The anomaly lies at the end of a long north- northeast linear magnetic structure that reflects the basement geology. The target anomaly is centered at 563280 mE l 5850320 mN (WGS 84). No EM response is associated with this anomaly. See Appendix II

Anomaly SP3J)029 Claim P1242329A strong dipolar magnetic anomaly with a magnetic intensity also of 5,000 nT was defined from this survey. The anomaly is ellipsoidal with its long axis trending northeast-southwest and is approximately 200 meters long. The target is centered at 566490 mE l 5855200 mN (WGS 84). Some weaker responses were also defined in the southwest corner of the claim area but survey would need to be extended to better delineate them. See Appendix II.

15

2.3 Ground Magnetics

Ground magnetic surveys using GPS local positioning were carried out by a two- man crew supplied by Abitibi Geophysics of Val-d'Or, Quebec during the spring of 2001. The purpose of the ground magnetic work was to delineate more accurately the kimberlite-type intrusive targets previously identified from fixed wing magnetic and helicopter borne magnetic and electromagnetic surveys.

A GEM GSM-19W (ver. 6) magnetometer (precision: 0.01 nT) with an integrated Canadian Marconi GPS resolution of 1m and staff mounted sealed Overhauser sensor was used in the survey. Observations of the total magnetic field during the survey were made every two seconds with corresponding GPS positions made for each reading. Plotted values were corrected for diurnal variations using post processing software in conjunction with a synchronized magnetic base station positioned near the Highbank Lake camp. The base station magnetometer was setup at 554399.552 E l 5796842.567 N (WGS84 Zone 16N) and was inspected daily for magnetic storms. Although some active periods were encountered, the diurnal corrections were judged to be satisfactory.

The survey was carried out with a post processing Differential Global Positioning System (DGPS) support and no survey lines were cut in the field. However, some lines were flagged. All positioning data were collected in UTM WGS84 Zone 16N projection. For further details on the ground surveys see Appendix III.

2.3.1 Ground Magnetic Survey Results

Anomaly SP3J)011 Claim P1242319The magnetic anomaly selected from the airborne surveys was clearly delineated on the ground survey. The magnetic intensity as defined increased a further 300 nT above background. This very high magnetic intensity and dike like characteristics extending to the south from this anomaly downgrades this target. However kimberlitic indicator grains were found in the area and based on this it was recommended that the anomaly be tested with one drill hole located at 563280 E l 5850320 N (WGS84 Zone 16N).

Anomaly SP3.0029 Claim P1242329A very strong magnetic response was outlined on this grid with values of more than 5,000 nT above background. Some poorly leveled lines occur to the west and east of this anomaly. It is unusually strong for a kimberlite response however it is discrete and has features similar to kimberlitic magnetic signatures. A drill hole is recommended at 566490 mE l 5855200 mN to determine the nature of this anomaly.

2.4 Exploration Drilling

Reverse circulation drilling was undertaken in search of kimberlite-type intrusives during March and April 2002. The drilling was contracted to Heath and Sherwood Drilling Inc., of Kirkland Lake, Ontario. A Fly-Aker reverse circulation air assist

16

drill was used. It was transported on site by a Bell 205 helicopter. A total of 58.0m were drilled in two holes.

The drill was operated by a two-person drill crew assisted by a local labourer from Marten Falls First Nation, on a 12-hour (day-shift) basis. A geologist was also on site during the drilling to collect samples and complete preliminary logging of the drill cuttings.

Although no kimberlite-type rocks were discovered during the campaign, two of the claims will be maintained based on the copper showing from one of the drill holes. Detailed drill hole logs and magnetic susceptibility readings were recorded and are presented in Appendix IV.

Table 4 below is a summary of the drill hole data.

Claim Tag ID

P1242319

P1242329

Drill Hole

SP3-02- 006RSP3-02- 007R

Drill Hole Collar (Nad 27, Zn 16)

Easting

563284

566476

Northing

5850105

5854975

Drilling Period

Start Date08/04/0 110/04/01

End Date

04/08/0 111/04/01

EOH Dept h (m)

26.0

32.0

EOH material

Sheared mafic volcanicsMassive sulphides in an altered schist

Table 4 : DRILLHOLE SUMMARY

2.4.1 Assay Results and Discussion

Representative samples collected on site during the drilling of hole SP3-02- 007R (claim P1242329), were submitted to Chimitec Bondar Clegg for pre- concentration by fire assay fusion and analyzed by inductively coupled plasma (ICP) spectrometry.

Initial observations of the samples did not show any sulphide of interest because of the nature of the sample recovered during the RC drilling technique. Two samples were first sent to the laboratory for assay covering the sulfide zone (26.0m-29m and 29. Om-32. Om).

As the detail of this assay was not adequately suited to interpretation, a second sample was taken from each representative downhole drill sample and re-filed. As a result, twenty-two sulfide rich samples showed a high sulfide content in the Archaean basement rock from the 24.2m to 32.0m interval in drill hole SP3-02-007R (claim P1242329). Copper vales of 1.69 07o C^7.3m at a depth of 24.2m to 31.5m were found as a result of this assay. The laboratory assay results can be found in Appendix V.

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2.4.2 PIMA Spectral Response

Clay material encountered in the drill holes near the base of the Palaeozoic during the 2002 exploration drilling campaign was subjected to spectral analyses to determine the likely parent rock for the clays. A PIMA instrument was used in an effort to identify clays that may be associated with the alteration of an ultramafic or kimberlitic source.

The PIMA is a field portable infrared spectrometer that measures the reflectance spectra of rocks, minerals, drill core, cuttings and pulps in the 1300nm to 2500nm range of the electromagnetic spectrum. Minerals that contain hydroxyl radicals (such as clays, amphiboles, some sulfates) and carbonate radicals absorb incident radiation at specific wavelengths in this wavelength region and in relative amounts that are diagnostic of such mineral species. The PIMA provides a fast means of identifying these minerals, their crystallinity and compositional variations and plotting these variations down drillhole or along a traverse.

De Beers geologists at the De Beers Canada Exploration eastern office in Sudbury, Ontario, completed the PIMA work. It was concluded that the clays were not derived from a kimberlitic source rock. See Appendix VI for further details.

2.4.3 Water Quality Monitoring

Prior to drilling, Trow Consulting Engineers of Thunder Bay, Ontario was contracted to undertake water quality monitoring of surface waters in streams, lakes and rivers downslope from drill targets. The initial set of samples collected in March 2002 was used to provide an environmental baseline for the second round of sampling undertaken after drilling was completed. Post- drilling water sampling was undertaken on April 2002. Sample sites were accessed by helicopter from the field camp at Highbank Lake, Ontario.

Trow collected the water samples in accordance with Ontario Ministry of Environment Provincial Water Quality Objectives (Ontario Ministry of the Environment, 1994). Samples were analyzed for the following parameters: pH, hardness, alkalinity, carbonate, bicarbonate, conductivity, total dissolved solids, dissolved organic carbon, ammonia, turbidity, silica, color, nitrate, nitrite, sulfate, phosphate, chloride, total petroleum hydrocarbons (heavy oils) and metals/metalloids including: sodium, calcium, potassium, mercury, magnesium, aluminum, cadmium, phosphorus, titanium, arsenic, boron, copper, strontium, barium, chromium, phosphorous, titanium, arsenic, selenium, iron, zinc, manganese, beryllium, cobalt, silver, vanadium, molybdenum, uranium and thallium. The collected samples were submitted to a CAEAL certified laboratory (Philip Analytical Services Corp.) in Mississauga, Ontario for analysis, with blind duplicate samples inserted into each sample batch for quality assurance/quality control purposes.

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The results of the sampling program do not indicate a deleterious effect on overall water quality attributable to the drilling activities. In many cases, reported levels of potential contaminants decreased between the pre and post drilling samples. It is our opinion that apparent increases observed for some parameters (primary metals) between the pre-drilling and post-drilling sampling results at some locations reflect water sampling limitations and natural (seasonal) water chemistry changes and are not related to the drilling activity by De Beers. No follow-up work is considered to be necessary at this time. See Appendix VII.

3.0 EXPLORATION EXPENDITURE

The personnel listed below in Table 5 worked on the project during the 2001 and 2002 work programmes and have been considered in calculating the work programme expenditure. Further information on the expenditure allocated to each claim is shown in Appendix VIII as statements of expenditure and an expenditure distribution chart.

4.0 CONCLUSIONS AND RECOMMENDATIONS

An indication of volcanogenic massive sulphide mineralization was found during this exploration program. The assay results over a 7.3 metre interval returned copper values averaging J.69% copper with a short interval suggesting other elevated anomalous base metal values. It is difficult to interpret the assay results as only drill chip samples were recovered from the reverse circulation drill hole. Further work is therefore required to further define the anomalous results and provide more definitive assay results.

19

DE BEERS CANADA EXPLORATION INC. Company and PersonnelDonald Boucher

Deirdre O'Donohoe

Jason BerenyiJustin WardDoug WinzarRafael MunozRon Avery (contractor)Charlotte Boyce

Table 5: PERSONNEL

Project PositionEastern DivisionalManager l ProjectManagerContract field geologist lproject supervisor

GeologistProject geophysicistGeologistField geologist (contract)Geologist (contract)Field cook

MARTEN FALLS FIRST NATION Company and PersonnelAdam Achneepineskum

Carol Achneepineskum Tony Achneepineskum

Gordon Baxter

Lance Baxter

Norman Baxter

Donald Coaster Scott Loon David Rody Dan Wesley

GEOPHYSICS CONTRACTORS Company and Personnel Abitibi GeophysicsMichelle Guimont

Marcel Naud

Fugro Airborne Surveys

Project Work PeriodPermanently Attached to Project

April 13 to May 04.2001

July 10 to July 30, 2001 March 11 to April 26, 2002 March 11 to April 26, 2002 April 10 to April 19,2002 May 20 to May 23, 2002 April 13 to May 04, 2001 Sept. 01 to Oct. 28, 2002 April 22 to May 04, 2001 March 10 to April 26, 2002

Project PositionGeophysical fieldassistantField cookGeological field assistantDrill handGeological field assistantDrill handGeophysical fieldassistantField cookCamp attendantCamp attendantGeological field assistantGeological field assistantGeological field assistantGeological field assistant

Project Work PeriodApril 13 to May 02, 2001

July 10 to July 30, 2001 April 12 to April 19,2002 April 20 to April 26, 2002 April 13 to May 02, 2001 March 11 to April 19,2002 April 13 to May 02, 2001

April 13 to May 03, 2001 July 10 to July 30, 2001 March 11 to April 26, 2002 March 11 to April 26, 2002 March 11 to April 26, 2002 July 10 to July 30, 2001 April 13 to May 02, 2001

Project Position

Geophysics Field Technician Geophysics Field Technician

Project Work Period

April 13 to May 02, 2001

April 13 to May 02, 2001

19

Patrick Dickenson Chris Sawyer Bill Hofstead

Electronics Technician Geophysicist Helicopter Pilot

July 10 to July 30, 2001 July 10 to July 30, 2001 July 10 to July 30, 2001

HELICOPTER CONTRACTORS Company and Personnel Abitibi HelicoptersRejean Dulong

Johan Gravel

Richard Berube

Kevin Riese

Bill Moore

Daniel Jaeger Paul Berguon Erik Desilt

Heli-max Helicopters Ltd.Nick Greenfield

DRILLING CONTRACTOR Company and Personnel Heath S Sherwood Drilling Inc.Henry Durette Wayne Goodyear Joe Doonan

ENVIRONMENTAL CONSULTANT Company and Personnel Trow Engineering Ltd.John Lobbezoo

Project Position

Helicopter Pilot (Bell206)Helicopter Pilot (Bell206)Helicopter Pilot (Bell205)Helicopter Pilot (Bell205)Helicopter Pilot (Bell205)Helicopter EngineerHelicopter EngineerHelicopter Engineer

Project Work Period

March 14 to April 08, 2002

April 08 to April 26, 2002

March 15 to April 14, 2002



March 15 to April 14, 2002 April 14 to April 26, 2002 April 14 to April 26, 2002

Helicopter Pilot (Notar) April 13 to May 02, 2001

Project Position

Driller/ ForemanDrillerMechanic

Project Position

Geotechnical Engineer

Project Work Period

March 11 to April 26, 2002 March 11 to April 26, 2002 March 11 to March 21, 2002

Project Work Period

March 14 to March 15,2002April 23 to April 24, 2002

20

5.0 REFERENCES

Fulton, R.J., 1995:Surficial Material of Canada. Geologic Survey of Canada Map 1880A1:5 000000 scale.

Prest, V.K., 1963:Surficial Geology of the Red Lake-Lansdowne House Area, NorthwesternOntario. Geological Survey of Canada Paper 63-6.

Thorleifson, H. L, 1989:Quaternary Stratigraphy of the Central Hudson Bay Lowland, NorthernOntario, Canada, Unpupl. Ph.D. thesis, University of Colorado, 363p.

6.0 STATEMENT OF QUALIFICATIONS

l, Antony Claver French, reside at 383 Winchester Ave. Sudbury, Ontario, P3E 3T4 and hold a M.Sc.(Hons.) degree in Geology from Auckland University in New Zealand, l have practiced geology on a continuous basis since 1981 and l have over 21 years of experience in conducting diamond exploration programmes worldwide. l have reviewed the foregoing report and have reviewed the expenditure data and consider it to be satisfactory for the purposes of assessment reporting.

Antony C. French M. Se. (Hons)

March 6, 2003

21

Appendix l

Sample Location Map MMI Geochemistry Assay Results

Response Ratio TaijleResponse Ratio Stacked Bar Graph

XRAL Laboratory Work InstructionsCertificate of Analysis

22

Location Map of Mineral Claim Block P 1242319 Helicopter Total Magnetic Intensity Survey

5850000-

IIUTM Nad 27, Zone 16 NTS:43D January 7, 2003 Author: Deirdre Odonohoe Drawn by: Anik Boucher

Claim P 1242319

Q Corner Post

9 Line Post

A MM! Samples

^ Dhll Hole

^ Traverse Line

1: 10,000

564000

MMI FIELD DATA Magnetic Anomaly: Mineral Claim: Total Samples: Total Metres Traversed:

SP3J)011 P1242319 7 800

Sample #EastingNorthingAnomaly #DateMap (NTS)Tools Used

Material Type

Depth (ft)Depth (m)Comments

Sampled by

19059563588

5849764

SP3J)011

20/04/01

043D16

Encased end auger, axe

sandy, clay with some granules (light grey)

10.03.040cm of ice (frozen vegetation), followed by veg/water; hummocky terrain with abundant low trees and labrador tea bush

RM/GB

19060

563537

5849832

SP3J)011

20/04/01

043D16


light grey predominantly sand with visible granules, some clay and silt8.02.4hummocky terrain with abundant short coniferous; 60cm thick frozen vegetation

RM/GB

19061

563373

5849993

SP3J)011

20/04/01

043D16


light grey sand , silt and clay with some granules

8.02.4swampish terrain, 30m E of the creek; dead trees, only coniferous around, labrador tea underbrush; 30cm thick frozen vegetation cover

RM/GB

19062

563274

5850109

SP3JD011

20/04/01

043D16


light grey sandy silty clayey with some granules

9.02.7swampish terrain, approx. 30m W of creek; abundant dead trees (coniferous), and young thin coniferous; slight moss growth, some labrador tea underbrush; 30cm thick frozen surface organics

RM/GB

19063

563206

5850182

SP3J)011

20/04/01

043D16


light grey sandy silty clayey material with no granules

9.02.7swampish with heavy underbrush and coniferous trees, more mature forest; 30cm thick frozen surface organics

RM/GB

19064

563120

5850246

SP3J)01 1

20/04/01

043D16


light grey sandy clayey silty with some small granules

10.03.0heavily treed area with heavy underbrush; mostly flat terrain, no apparent rises in the area; 30cm thick frozen surface organics

RM/GB

19065

563025

5850317

SP3J)011

20/04/01

043D16

Encased end auger, axe, shovel

light grey sandy material with small visible granules

11.03.4heavy labrador tea underbrush and well treed area, coniferous of all sizes; 30cm thick frozen vegetation cover; struck rock at bottom of hole

RM/GB

Depth to Sediment PI 242319 (SP3.0011)

w o

lO)5o

ODSL •*-"a o

-2

-8

-10

^ Samples located over the geophysical magnetic anomaly

mnm *±4 fc -12

19059 1UUOU 19061 19062 19063Samples (Southeast to Northwest)

~795m

19064 19065

Table of Raw Results for SP3-02-006R (SP3 0011). from XRAL

Sample IdentityMgTiCrCoNiRbYNbPdBaLaTaCePrNdSmGdTbErYbCaSr

Analysis Unitppbppbppbppbppbppbppbppbppbppbppbppbppbppbppbppbppbppbppbppbppbppm

Detection Limit10011131

0.10.10.10.10.10.50.10.10.10.10.10.10.10.10.010.1

*STD V621934600

-1-1-111160.40.8-0.188.40.3-0.5-0.1-0.10.4-0.1-0.1-0.1-0.1-0.113470110

MMI SAMPLES190592010

1-1-1-315

-0.10.2-0.1227-0.1-0.50.1-0.10.1-0.1-0.1-0.1-0.1-0.136470135

190602450-1-1-1-38

-0.10.2-0.1172-0.1-0.5-0.1-0.1-0.1-0.1-0.1-0.1-0.1-0.12796097

1906145002-1-1-335-0.10.2-0.1149-0.1-0.5-0.1-0.10.1-0.1-0.1-0.1-0.1-0.130650102

19062458028-1-13190.30.4-0.12000.9-0.51.30.20.60.20.2-0.1-0.1-0.134260139

190637400-1-1-1-322-0.10.1-0.1206-0.1-0.5-0.1-0.1-0.1-0.1-0.1-0.1-0.1-0.128030205

190646680

1-1-1-311

-0.10.2-0.1306-0.1-0.5-0.1-0.1-0.1-0.1-0.1-0.1-0.1-0.13381088

19065664045-126120.50.40.61570.9-0.51.70.20.70.20.1-0.1-0.1-0.14062091.7

Table of Element Response Ratios

Sample ^Identity

Mg..-,. J! - .;.

CrCotlj ^ f .

:..-,: Wb: Y /: '

NbPdBaLaTaCePrNdSmGdTbErYb

..-,:-::.-- -:. ; -. - . - MMISAMPLES : .--,. .^,:,,ty ̂ .'.:-, : ^ .,^\^^;':,;::':^-.^:-^-'^190590.582.000.000.000.001.300.001.000.001.380.000.000.000.000.000.000.000.000.000.00

190600.710.000.000.000.000.700.001.000.001.050.000.000.000.000.000.000.000.000.000.00

190611.294.000.000.000.003.040.001.000.000.910.000.000.000.000.000.000.000.000.000.00

190621.32

56.000.000.000.001.650.002.000.001.220.000.000.000.000.000.000.000.000.000.00

190632.130.000.000.000.001.910.000.500.001.250.000.000.000.000.000.000.000.000.000.00

190641.922.000.000.000.000.960.001.000.001.860.000.000.000.000.000.000.000.000.000.00

190651.91

90.000.000.000.001.040.002.000.000.950.000.000.000.000.000.000.000.000.000.00

Response Ratio PI 2423 l 9 (SP3.0011)

100.00

90.00

80.00

70.00

60.00

o, 50.00VIC O O.

O)cc

40.00

30.00

0.0019059

Anomaly Extent

19060 19061 19062 19063

Samples (SE-NW)

19064 19065

Mg BTi DCr DCo BNiBRbBYBNb BPd BBa DLa BTa BCe BPr BNd BSm BGdBTbBErDYb

Location Map of Mineral Claim Block P 1242329 Helicopter Total Magnetic Intensity Survey

5855000-

li

UTM Nad 27, Zone 16 NTS: 43D January 7. 2003 Author: Deirdre Odonohoe Drawn by: Anik Boucher

Cfaim P 1242329

Corner Post

Line Post

MMI Samples

Drill Hole

Traverse Line

O 1 Q 2km

1: 10,000

566000 567000

MMI FIELD DATA Magnetic Anomaly: Mineral Claim: Total Samples: Total Metres Traversed:

SP3J)029 P1242329 8 1020

Sample IdentitySample #Easting (Nad 27)Northing (Nad 27)Anomaly #DateMap (NTS)Tools Used

Material Type

Depth (ft)Depth (m)Comments

Sampled by

19044

19044-29

566223

5855355

SP3J)029

29/04/01

043D16

Encased end auger, shovel

yellow-brown till, clay size to small pebbles

3.00.91material at 90cm; scraping rock in hole; area is a forest of spruce, undulating; slightly raised topography

DO/DW/GB

19043

19043-29

566321

5855254

SP3J)029

29/04/01

043D16


brown till (good till) has all grain sizes up to small pebbles (subangular to subrounded)1.50.46material at 45cm depth; roughly 1 5cm of ice; spruce forest, undulating floor, mod. to dense underbrush, lots of cariboo moss

DO/DW/GB

19042

19042-29

566420

5855126

SP3J)029

29/04/01

043D16

Encased end auger

rich brown colour, very sandy but does contain minor clay, silt and granules.

1.00.3010cm of ice; hit material at 30cm; area has a bumpy floor, abundant underbrush and tall spruce

DO/DW/GB

19041

19041-29

566505

5855025

SP3J)029

29/04/01

043D16


brown sandy material with minor granules and pebble sized clasts

3.00.91^Ocm of frozen ground, hit material at 0.9m; sample in a bog full of willows and labrador tea and other brush. Very wet ground

DO/DW/GB

19040

19040-29

566577

5854942

SP3J)029

29/04/01

043D16


brown gravel ^ silt to small pebbles subrounded to subangular clasts.

7.02.13small hill of dense spruce, thick underbrush (thick permafrost) moved off hill side (low wet swamp), hit material at 2.2m, approx 35cm of frozen organics above

DO/DW/GB

19039

19039-29

566645

5854844

SP3J)029

29/04/01

043D16

Encased end auger, axe, shovel

brown-grey coarse gravel, many lithologies carbs also rich, domantly subangular4.51.37dense spruce forest, rich underbrush and undulating forest floor; deep frozen ground (1-1 .3m) , ground sounds hollow (stream beneath?)

DO/DW/GB

19038

19038-29566781

5854718

SP3J)02929/04/01043D16Encased end auger

brown sand changing into small pebble gravel

9.02.74frozen oganics for ^Ocm; material at 2.8m (went to 3.0m); at edge of dense forest and tamarack bog; scraping a rock at 3.0m?

DO/DW/GB

19037

19037-29

566927

5854620

SP3J)029

29/04/01

043D16

Encased end auger

fairly uniform grey sand

10.03.05Less than 35cm of frozen veg. Cover; hit material at 3.0m; in a flat, bog area with stunted knarty tamarack trees and some spruce

DO/DW/GB

Depth to Sediment Layer SP3-0029

Samples located over the geophysical magnetic anomaly

19043 19042 19041 19040 19039 19038 19037

Samples (Southeast to Northwest) -1020m

Table of Raw results for SP3-02-007R (SP3 0029). from XRAL

Sample Identity

MgTiCrCoNiRbYNbPdBaLaTaCePrNdSmGdTbErYbCaSr

Analysis Unit

ppbppbppbppbppbppbppbppbppbppbppbppbppbppbppbppbppbppbppbppbppbppm

Detection Limit

10011131

0.10.10.10.10.10.50.10.10.10.10.10.10.10.1

0.010.1

*STD V6219

34600-1-1-1

11160.40.8-0.1

88.40.3-0.5-0.1-0.1

0.4-0.1-0.1-0.1-0.1-0.1

13470110

' /V MMl -' v , : .^ . - :.^;'- ;^-:!'^:"-. " - ' Samples -.-' : - -^^ Hl p''' r -;.:,j':... -

190374860

13-1-1-3

11-0.1

0.2-0.1

2140.3-0.5

0.4-0.1

0.2-0.1-0.1-0.1-0.1-0.1

2195081.9

190384440

4-1-1-3

9-0.1-0.1-0.1

1690.1-0.5

0.2-0.1-0.1-0.1-0.1-0.1-0.1-0.1

19720114

190395620199426

251.71.30.298.72.6-0.5

4.70.62

0.40.3-0.1

0.10.2

2632083.4

190403250

12-1-1-3

10-0.1-0.1-0.1

1450.3-0.5

0.5-0.1

0.2-0.1-0.1-0.1-0.1-0.1

1635063.1

1904113900

2-1-1-3

150.2-0.1-0.1

66.90.2-0.5

0.3-0.1

0.3-0.1-0.1-0.1-0.1-0.1

50950114

190426480

1-1-1-3

8-0.1-0.1-0.1

42.7-0.1-0.5-0.1-0.1-0.1-0.1-0.1-0.1-0.1-0.1

3253061.9

1904311700

29-1-1-3

150.90.2-0.1

33.91

-0.5

1.80.20.90.20.2-0.1-0.1-0.1

3129046.6

190449380

1-1-1-3

120.1-0.1-0.1

38.6-0.1-0.5

0.2-0.1

0.2-0.1-0.1-0.1-0.1-0.1

4005064.5

Table Element Response Ratios (Those marked in red are over the anomaly)

Sample Identity

MgTiCrCoWRbYNbPdBa

4-aTaCePrNdSmGd

- . :-:;ii);.":- :.".••I'&r: '' Yb ' -

Ca: :;' :'TSr' -. . ,

MMI SAMPLES190441.970.570.000.000.001.230.000.000.000.930.000.001.000.001.330.000.000.000.001.871.039.93

190432.4616.570.000.000.001.540.000.000.000.8113.330.009.000.006.000.000.000.000.001.460.7451.92

190421.360.570.000.000.000.820.000.000.001.030.000.000.000.000.000.000.000.000.001.520.996.29

190412.921.140.000.000.001.540.000.000.001.612.670.001.500.002.000.000.000.000.002.381.82

17.57

190400.686.860.000.000.001.030.000.000.003.484.000.002.500.001.330.000.000.000.000.761.00

21.65

190391.18

113.710.000.000.002.560.000.000.002.3734.670.00

23.500.0013.330.000.000.000.001.231.33

193.89

190380.932.290.000.000.000.920.000.000.004.061.330.001.000.000.000.000.000.000.000.921.82

13.27

190371.027.430.000.000.001.130.000.000.005.144.000.002.000.001.330.000.000.000.001.031.30

24.38

250.00 i —————

200.00

0 150.00-ura aeVMCOS- 100.00V

of

50.00

0.00

Response Ratio

^

f

VM k

1904

P1242329(SP3.0029)

A nomaly Extent

i

H

i

\

—

.^

4 19043 19042 19041 19040 19039 19038 19037

Samples (SE-NW)

B Mg BTi D Gr B Co BNi BRb BY BNb BPd BBa DU BTa 1 Ce BPr BNd BSm BGd BTb BEr DYb

XRAL LABORATORIES WORK INSTRUCTION

TITLE: MMID CD#-TO-WI-SD-16 DATE: February 27, 2001 REV: 00 WRITTEN BY: Adel Mina APPROVED BY: H. DeSouza PROCESS: Wet Laboratory

1. PURPOSE

To dissolve the mobile metal ions (Ni, Co, Pd, Cr, Nb, Mg).

2. SCOPE

This work instruction describes how to dissolve MMI that is in the samples, prior to ICP-MS analysis.

3. GENERAL INSTRUCTIONS

REAGENTS INSTRUCTION FOR MMI D SOLUTION

3.1 Weigh out 50 grams of the sample into a plastic vial fitted with a screw cap. NOTE: Due to the non-homogeneity of the sample, it should be scooped from different areas. If the sample consists of large lumps, the sample may be gently broken down into smaller lumps.

3.2 Dilute MMI D solution 1:100 (10 ml MMI D + 990 ml distilled water).3.3 Add 50 ml of the diluted MMI D solution to the sample.3.4 Place the samples tray in a shaker and shake for 20 minutes. Allow to stay

overnight.3.5 Centrifuge the samples for 10 minutes if needed.3.6 Decant the liquid into 15 ml plastic test tube,3.7 Transfer the test tube rack to the ICP-MS area.

QUALITY CONTROL

MMI D certified reference material is weighed and digested every 46 sample.

4. SAFETY

See MSDS for precautions.

XRAL LABORATORIES WORK INSTRUCTION

TITLE ICPMS Analysis - MMI - D (Mobile Metal Ions) CD#TO-WI-MS-16

Date: February 27, 2001 Rev: 01Written by: Dana Mills Approved by: H. DeSouzaProcess: ICPMS Relates to Procedure:MMLD

1. PURPOSE:

To measure (analyze) the mobile metal ions of Mg, Ti, Co, Ni, Rb, Cr, Y, Nb, Pd, Ba, La, Ta, Ce, Pr, Nd, Sm, Gd, Tb, Er and Yb in MMI samples

2. SCOPE:Involves a process that sample goes through from the introduction via the autosampler through PQ2 or PQ3 to the final interpretation of data obtained from the printer

3. INSTRUCTIONS:

3.1 Standard solutions used for preparing Calibration Standards:

STOCK #1 All individual element standards at lOOOppm

STOCK #2 All elements at 10ppm except Pd at 1 ppm

3.2 Matrix Solution:

MOBILE METAL ION CONCENTRATE (1/10) from Wet Lab, additionally diluted 10 times (total dilution is 100 times).

3.3 CALIBRATION STANDARDS:

#1 O.OPPB All elements at Oppb#2 I.Oppb 1ppb Pd * 100ppb Mg * 10ppb all other elements#3 5.0ppb 5ppb Pd * 500ppb Mg * 100ppb all other elements

All standards and samples contain 45 ppb Re Internal Standard.

INTERNAL STANDARD SOLUTIONS (SO.Oppb Re) used to dilute samples 1/10, added are 2 pellets NaOH plus 0.1g NaCN.

4.0 SAMPLES PREPARATION

4.1 Pipette 1 ml sample into centrifuge test tube4.2 Add 9ml (to the mark 10m) solution B, containing

50ppb Re internal standard, internal standard's final concentration being 45ppb.

4.3 Cover it with parafilm and shake4.4 Load the samples into racks and set it into the auto/sampler

station.4.5 Standard #2 is run after every 11 samples as QC check.

5.0 Reporting Results

The results of the analysis are transfered by a flopy to main computer, processed, checked and reported to the data centre for reporting to the client.

6.0 SAFETY PRECAUTIONS:

Follow standard safety laboratory procedure (gloves, glasses) while handling samples.

XRAL XRAL LaboratoriesA Division of SGS Canada Inc.

1885 Leslie Street Don Mills, Ontario Canada M3B 3J4

To:

CERTIFICATE OF ANALYSIS

Work Order: 063501

De Beers Canada Exploration Inc. Attn: Herman Grutter

One William Morgan Drive TORONTO ON/CANADA/M4H 1N6

Date 13/06/01

Copy 1 to

P.O. No. Project No. No. of Samples Date Submitted Report Comprises

CHAPADA DIAMANTINA 106 Soil 08/05/01 Cover Sheet plus Pages 1 to 10

Distribution of unused material:Pujps: Discarded After 90 Days Unless Instructed!!!Rejects: Discarded After 90 Days Unless Instructed!!!

Certified By

Dr. Hugh de Souza, General Manager XRAL Laboratories

ISO 9002 REGISTERED

Subject to SGS General Terms and Conditions

Report Footer: L. M. R. = Listed not received l. S. = Insufficient Sample n.a. = Not applicable - = No result *INF s Composition of this sample makes detection impossible by this method M after a result denotes ppb to ppm conversion, 0A denotes ppm to % conversion

SGS Member of the SGS Group (Societe Generate de Surveillance)


Work Order: 063501 Date: 13/06/01 FINAL Page l of 10

Element. Method. Det.Lim. Units.

*Std V621919001190021900319004

1900519006190071900819009

1901019011190121901319014

1901519016190171901819019

1902019021190221902319024

1902519026190271902819029

MgMMI-D

100ppb

346007030765060708420

4770102001110030704030

56507330415045205210

880197019306690

11600

15104530734033201660

10503330255011902030

TiMMI-D

1ppb

•CI65

•CI39

107

•CI227519

748859436392331

93

•CI147

1100

3226

133

•CI

1022

•CI•Ci

CaMMI-D

0.01ppb

^9.9^9,9^9.9^9.9^9.9

^9.9^9.9^9.9^9.9^9.9

^9.9^9.9^9.9^9.9^9.9

^9.9^9.9^9.9>99.9>99.9

>99.9>99.9^9.9>99.9>99.9

>99.9>99.9^9.9>99.9>99.9

GrMMI-D

1ppb

•Ci<l<l•CI<l<l<l<l

616

30341710

8

•CI•Ci<l

340

•CI7

<l•CI<l

<l<l<l•Ci<l

CoMMI-D

1ppb

•a<l<l<l•ci

<l<l<l

24

77333

•CI•Ci<l

29

•a3

<l<l•CI

<l<l<l<l<l

NiMMI-D

3ppb

11O•C30•C3

•C30o

510

1718987

•C3OO

624

•C31017O•C3

O•C3OO•C3

RbMMI-D

1ppb

1623119

32

1820

62448

4651273621

1314162660

1137

967

1314202029

SrMMI-D

0.1ppm

110110201137

92.2

133144295

59.569.0

65.970.684.573.455.8

83.2162127

65.779.2

60.162.7150

92.081.2

78.260.752.389.4115

YMMI-D

0.1ppb

0.40.30.1

O.I0.5

0.20.3

O.I2.24.5

6.38.44.13.73.0

0.20.1o.i

1.613.0

0.11.80.2

•CO.lO.I

0.2O.I•CO.l•CO.l•CO.l

NbMMI-D

0.1ppb

0.80.70.30.40.5

0.30.20.21.43.1

4.75.51.92.52.0

0.20.1

0.10.97.2

•co.i1.40.1

•CO.l0.2

0.2•CO.l•CO.l•CO.l0.1

PdMMI-D

0.1ppb

0.10.10.1O.IO.I

O.I0.1O.I

0.20.4

0.50.70.30.40.5

0.10.10.1

0.20.9

0.10.3

O.IO.IO.I

0.1O.IO.IO.IO.I

BaMMI-D

0.1ppb

88.4145171226159

12496.9117182121

211212154152151

165173167139186

164204181123161

133147159167160

LaMMI-D

0.1ppb

0.30.30.2

O.I1.4

0.30.4

0.14.78.8

14.318.67.87.16.7

0.4O.I0.1

2.827.3

0.13.70.3

O.IO.I

0.8O.I

0.30.1O.I

TaMMI-D

0.5ppb

O.50.50.5O.50.5

O.5O.50.50.50.5

O.5O.50.50.5O.5

O.50. 5O.50.5

0.5

0.5O.50. 5O.5O.5

O.5O.5O.5O.50.5

CeMMI-D

0.1ppb

O.I0.60.3

O.I2.5

0.50.9

O.I9.1

17.4

28.334.712.313.612.7

0.60.2

O.I5.2

52.0

0.47.10.60.1

0.1

0.80.10.40.2

O.I

PrMMI-D

0.1ppb

0.10.1O.IO.I

0.3

O.I0.1

0.11.12.1

3.34.01.51.61.5

0.1O.IO.I

0.66.3

O.I0.7

O.IO.IO.I

0.1O.IO.IO.IO.I

©5G5 Member of the SGS Group (Socie"te Generate de Surveillance)


Work Order: 063501 Date: 13/06/01 FINAL Page 2 of 10


1903019031190321903319034

1903519036190371903819039

1904019041190421904319044

19045*Blk BLANK*Std STANDARD1904619047

1904819049190501905119052

*Std V621919053190541905519056

MgMMI-D

100ppb

45103020604023102520

55801230486044405620

3250139006480

117009380

3290C 100182042607650

45404110

12500136006900

3350037307930

104002150

TiMMI-D

1ppb

5•Ci•ci•ci<l•19530134

199

1221

291

134•ci•CI294

43204

119025

Ci91

181

CaMMI-D

0.01ppb

^9.9^9.9^9.9^9.9^9.9

^9.9^9.9^9.9^9.9^9.9

^9.9^9.9>99.9^9.9>99.9

^9.9<0.01^9.9^9.9>99.9

>99.9>99.9>99.9^9.9>99.9

>99.9>99.9>99.9^9.9>99.9

Cr CoMMI-D MMI-D

1 1ppb ppb

•CI CI•CI <l<l CI<l <l<1 <1

3 2Ci CICi CICI Ci

4 2

CI CICi CICI CICI CICI CI

ci ciCi CICi CICi CICI CI

CI CiCI CI40 8

CI CICI CI

CI CICI 1CI CICI 1CI CI

NlMMI-D

3ppb

C3C3C3C3C3

4C3C3C3

6

C3C3C3C3C3

3cs

5C3C3

C33

21C3C3

124

C3C3C3

RbMMI-D

1ppb

101510147

328

119

25

1015

81512

32CI391618

2439781310

17114

2542

STMMI-D

0.1ppm

17780.4181118

99.5

13645.681.9114

83.4

63.1114

61.946.664.5

63.2CO.l54.8119

92.6

69.776.884.4169173

107129218

85.996.3

YMMI-D

0.1ppb

0.2CO.lCO.lCO.lCO.l

1.80.4

CO.lCO.l

1.7

CO.l0.2

CO.l0.90.1

1.7CO.lCO.l

0.2CO.l

0.51.9

16.7CO.l

0.2

0.30.8

CO.l0.40.1

NbMMI-D

0.1ppb

CO.lCO.lco.ico.ico.i

1.00.30.2

CO.l1.3

CO.lCO.lCO.l

0.2CO.l

0.8CO.lCO.l

1.10.8

0.22.09.20.60.5

0.30.80.20.30.2

PdMMI-D

0.1ppb

co.ico.ico.ico.i

0.1

0.2CO.lco.ico.i

0.2

co.ico.iCO.lCO.lCO.l

0.1CO.lCO.lCO.lCO.l

CO.lco.i

1.0CO.lCO.l

CO.lCO.lCO.lCO.lCO.l

BaMMI-D

0.1ppb

207141230142162

274119214169

98.7

14566.942.733.938.6

121CO.l11.8178

66.6

72.4107247

69.2174

88.7109111

97.3134

LaMMI-D

0.1ppb

0.2CO.lCO.lCO.lCO.l

3.50.70.30.12.6

0.30.2

CO.l1.0

CO.l

2.7CO.lCO.l

0.2CO.l

0.94.5

39.60.10.1

0.21.4

CO.l0.6

CO.l

TaMMI-D

0.5ppb

C0.5C0.5C0.5C0.5C0.5

C0.5C0.5C0.5C0.5C0.5

C0.5C0.5C0.5C0.5C0.5

CO. 5CO. 5CO. 5C0.5•C0.5

C0.5C0.5

0.6C0.5C0.5

C0.5C0.5C0.5CO. 5C0.5

CeMMI-D

0.1ppb

0.3CO.lco.iCO.l

0.1

6.41.30.40.24.7

0.50.3

CO.l1.80.2

5.2CO.lCO.l

0.4CO.l

1.58.0

76.40.20.3

CO.l2.6

CO.l1.30.2

PrMMI-D

0.1ppb

CO.lco.ico.iCO.lCO.l

0.80.2

CO.lCO.l

0.6

CO.lco.iCO.l

0.2CO.l

0.6CO.lCO.lCO.lCO.l

0.20.98.8

CO.lCO.l

CO.l0.3

CO.l0.1

CO.l

Member of the SGS Group (Societe Generate de Surveillance)




1905719058190591906019061

1906219063190641906519066

1906719068190691907019071

1907219073190741907519076

1907719078190791908019081

1908219083190841908519086

MgMMI-D

100ppb

27902740201024504500

4580740066806640

11300

8180134001110074707180

63808790393058609060

98503720

1020017704650

6980141008070

137003370

TiMMI-D

1ppb

541

O2

28<l

145

1120

320917155

105

10•Ci121314

74075

67582

•CI•Ci10

31

CaMMI-D

0.01ppb

^9.9^9.9^9.9^9.9^9.9

^9.9^9.9^9.9^9.9^9.9

^9.9^9.9^9.9^9.9^9.9

>99.9>99.9>99.9^9.9>99.9

>99.9>99.9>99.9^9.9>99.9

>99.9>99.9>99.9^9.9>99.9

CrMMI-D

1ppb

•O<l<l<l•a<l<l<l<l41

230

•CI<l•CI

O•Ci<l<l•n

19<l<l<l•a<l<l<l<l•ci

CoMMI-D

1ppb

•CI<l<l<l<l•CI<l<l

28

16

•Ci<l<l

0O.<l<l<l

5•CI<l162

•CI<l

1<l<l

NiMMI-D

3ppb

0•C30oo

3OO

628

5194

03

0O00•C3

144

•C3103

•C3OO•C3O

RbMMI-D

1ppb

1824158

35

1922111294

4171232624

399

191919

6630106927

25143620

8

SrMMI-D

0.1ppm

49.269.8135

97.0102

139205

88.091.799.8

71.384.595.655.373.1

116124

97.883.587.7

127124126

15.039.2

48.090.6118117

91.3

YMMI-D

0.1ppb

0.10.1

O.IO.IO.I

0.3•CO.l•CO.l

0.57.7

4.36.82.30.10.8

0.50.10.30.30.6

7.11.00.60.42.0

•CO.lO.I

0.21.9

•CO.l

NbMMI-D

0.1ppb

0.50.40.20.20.2

0.40.10.20.47.1

2.75.81.60.30.2

0.30.10.20.20.2

5.10.70.10.50.9

0.2O.I

0.20.1

O.I

PdMMI-D

0.1ppb

•CO.l•CO.l•CO.lO.I•CO.l

•CO.lO.I•CO.l

0.60.7

0.20.50.1

0.1•CO.l

•CO.l•CO.l•CO.l•CO.l•CO.l

0.6•CO.l•CO.lO.I•CO.l

•CO.l•CO.l•CO.l*co.i•CO.l

BaMMI-D

0.1ppb

136155227172149

200206306157424

186300125151141

15159.7151159172

382171

76.2306

21.2

49.448.4170

52.4149

LaMMI-D

0.1ppb

0.10.2

•CO.l•CO.lO.I

0.9•CO.l•CO.l

0.920.0

7.717.75.00.11.2

0.50.10.50.41.0

18.42.01.00.43.2

•CO.l•CO.l

0.53.7

•CO.l

TaMMI-D

0.5ppb

O.5O.5O.5O.5O.5

O.50.50.5O.50.5

0.5•C0.50.5•C0.5O.5

•C0.5^.5•C0.5•c:0.5•CO.S

^.5•C0.5•C0.5^.5•C0.5

0.5•C0.5•CO.S•C0.5•C0.5

CeMMI-D

0.1ppb

0.50.20.1

•CO.l•CO.l

1.3^.1^.1

1.737.2

15.034.6

9.30.52.1

1.20.11.20.91.8

36.33.71.90.76.4

•CO.l•CO.l

0.80.6

^.1

PrMMI-D

0.1ppb

•CO.l•CO.lO.IO.I•CO.l

0.2•CO.lO.I

0.24.2

1.73.91.1

O.I0.3

0.2O.l

0.1O.I

0.2

4.00.40.2

O.I0.7

O.IO.IO.I

0.7O.I

@5G5 Member of the SGS Group (Societe Generate de Surveillance)




19087190881908919090*Blk BLANK

*Std STANDARD19091190921909319094

1909519096190971909819099

19100191011910219103*Std V6219

*Dup 19002*Dup 19012*Dup 19024*Dup 19036*Dup 19048

*Dup 19059*Dup 19071*Dup 19083*Dup 19095*Blk BLANK

MgMMI-D

100ppb

2300172029102530

•C 100

19308390865029104600

13001430523049506140

51201120048702820

34400

66803380200013904640

21607160

120001180

•c 100

TiMMI-D

1ppb

310

12

•CI

•ci2122

22

165

86

712

1071

4413•ci3240

25

•Ci3

•ci

Ca Cr CoMMI-D MMI-D MMI-D

0.01 1 1ppb ppb ppb

^9.9 -Ci -CI^9.9 -Ci -CI^9.9 "Ci -Ci^9.9 O *C1•C0.01 -Ci <l

^9.9 <l <l>99.9 <l •Ci>99.9 <l <l>99.9 -Ci <l>99.9 <l <l

^9.9 <l <l>99.9 <l -CI>99.9 <l <l>99.9 O <l>99.9 <l <l

^9.9 <l <l>99.9 <l *C1^9.9 <l <l>99.9 -Ci <l>99.9 <l <l

^9.9 <l <l>99.9 20 3^9.9 <l <l>99.9 O <l>99.9 <l <l

^9.9 <l <l>99.9 <l -Ci>99.9 <l <l>99.9 "Ci O<0.01 <l <l

NiMMI-D

3ppb

•C34

O<3<3

300OO

0•C300<3

•C 34

•C 3<312

O6

<3•C 3•C3

064

•C 30

RbMMI-D

1ppb

12141415

< l

399

101115

2220161917

2116233017

1326

88

23

14261720

•CI

SrMMI-D

0.1ppm

201114184166

•CO.l

54.7275338227246

99.0132

49.151.841.4

35.5111

82.498.1104

17982.484.651.570.2

15380.280.090.6

•CO.l

YMMI-D

0.1ppb

0.10.3

•CO.l•CO.l•CO.l

•CO.l•CO.l•CO.l•co.i•CO.l

•CO.l•CO.l

0.3•CO.l

1.3

0.1•CO.l•CO.l

1.50.4

•CO.l3.7

•CO.l0.50.4

•CO.l0.7


NbMMI-D

0.1ppb

0.10.20.2

•CO.l•CO.l

•CO.l0.30.30.20.1

0.10.10.2

•CO.l0.6

0.1•CO.l•CO.l

0.70.3

0.21.60.10.30.3

•CO.l0.1


PdMMI-D

0.1ppb

•CO.l•co.i•CO.l^.1•CO.l

•CO.l•co.i•CO.l•co.i•CO.l

•CO.l•co.i•CO.l

0.30.2

•CO.l•CO.l•co.i•CO.l•CO.l

•CO.l0.2


•CO.l0.1


BaMMI-D

0.1ppb

166167150182

•CO.l

12.4157182171148

184161138151118

93.072.4192188

91.0

143140167135

72.2

253146

52.9182

•CO.l

LaMMI-D

0.1ppb

0.10.4



0.1•co.i•CO.l•CO.l

0.60.22.8

0.1•CO.l•CO.l

5.00.2

0.19.4

•CO.l0.81.0

•CO.l1.0


TaMMI-D

0.5ppb

•CO. 5•C0.5•C 0.5•C0.5*C0.5

•C0.5•C0.5•C0.5•C0.5•CO.S

•C0.5•C0.5•C0.5•C0.5•CO. 5

•CO. 5•C0.3•CO.S•C0.5•C0.5

•C0.5•C0.5•C0.5•C0.5•C0.5

•c 0.5•c 0.5•CO.S•C0.5•C0.5

CeMMI-D

0.1ppb

0.20.7


•CO.l•CO.l

0.10.20.6

•CO.l0.11.30.45.2

0.3^.1•CO.l

5.0•CO.l

0.210.1

•CO.l1.51.4

0.11.7

•CO.l0.1

•CO.l

PrMMI-D

0.1ppb

^.1•CO.l•CO.l•CO.l•CO.l


•CO.l•CO.l

0.1•CO.l

0.6


0.7•CO.l

•CO.l1.2

•CO.l0.20.2

•CO.l0.2

^.1^.1•CO.l

© SGS Member of the SGS Group (Societe Generate de Surveillance)




MgMMI-D

100ppb

TiMMI-D

1ppb

CaMMI-D

0.01ppb

CrMMI-D

1ppb

CoMMI-D

1ppb

NiMMI-D

3ppb

RbMMI-D

1ppb

SrMMI-D

0.1ppm

YMMI-D

0.1ppb

NbMMI-D

0.1ppb

PdMMI-D

0.1ppb

BaMMI-D

0.1ppb

LaMMI-D

0.1ppb

TaMMI-D

0.5ppb

CeMMI-D

0.1ppb

PrMMI-D

0.1ppb

*Std STANDARD 1910 <l •Ci 38 51.6 •CO.l •CO.l 12.9

©SGS Member of the SGS Group (Societe Generate de Surveillance)


Work Order: 063501 Date: 13/06/01 FINAL Page 6 of l O


*Std V621919001190021900319004

1900519006190071900819009

1901019011190121901319014

1901519016190171901819019

1902019021190221902319024

1902519026190271902819029

NdMMI-D

0.1ppb

0.40.30.2

O.I1.1

0.20.6

O.I4.07.2

11.814.25.45.55.3

0.30.1

O.I2.2

21.8

0.13.00.2

0.10.1

0.40.10.30.2

O.I

SmMMI-D

0.1ppb

o.i0.1O.Io.i

0.2

0.1O.IO.I

0.71.3

2.12.60.91.00.9

O.IO.IO.I

0.33.9

0.10.4

<0.1<0.1<0.1

O.I<0.1<0.1<0.1<0.1

GdMMI-D

0.1ppb

O.I0.1<0.1<0.1

0.2

<0.1O.I<0.1

0.51.1

1.72.20.90.80.8

O.IO.I<0.1

0.33.2

<0.10.5

O.I<0.1<0.1

<0.1O.I<0.1<0.1<0.1

TbMMI-D

0.1ppb

0.1<0.1o.i<0.1<0.1

<0.1<0.1^.i<0.1

0.1

0.20.30.20.1

-CO.l

<0.1<0.1*:o.i<0.1

0.4

<0.1<0.1^.1<0.1<0.1

<0.1<0.1^.1<0.1<0.1

ErMMI-D

0.1ppb

^.1<0.1<0.1*:o.i<0.1

<0.1<0.1<0.1

0.20.4

0.60.90.30.30.3

*:o.i^.1<0.1

0.21.3

*:0.0.

<0.•iO.<0.

<0.<0.<0.•:o.i<0.1

YbMMI-D

0.1ppb

•;o.i<0.1<0.1<0.1•CO.l

•CO.l•co.i^.i

0.20.5

0.60.80.50.40.3

O.I•CO.l*C0.1

0.21,3

*C0.10.2

•CO.l0.10.1

O.IO.IO.IO.ICO.l

@ SGS Member of the SOS Group (Societe Generate de Surveillance)



Element. Method. Det.Lim.Units.

1903019031190321903319034

1903519036190371903819039

1904019041190421904319044

19045*Blk BLANK*Std STANDARD1904619047

1904819049190501905119052

*Std V621919053190541905519056

NdMMI-D

0.1ppb

0.20.1

O.IO.lO.I

2.90.60.2

O.I2.0

0.20.3

O.I0.90.2

2.2O.IO.I

0.20.1

0.83.6

31.20.20.3

0.21.3

O.I0.70.1

SmMMI-D

0.1ppb

O.IO.l<0.1o.i<0.1

0.40.1

<0.1O.l

0.4

<0.1<0.1<0.1

0.2o.i

0.5<0.1<0.1o.i<0.1

0.20.65.0

•CO.l••CO.l

0.10.3

<0.10.1

<0.1

GdMMI-D

0.1ppb

•CO.lO.l<0.1<0.1•CO.l

0.40.1<0.1<0.1

0.3

•CO.l0.1<0.1

0.20.1

0.4<0.1<0.1<0.1O.l

0.10.54.2

<0.1O.l

<0.10.2

<0.10.1

0.1

TbMMI-D

0.1ppb

•CO.l<0.1<0.1<0.1<0.1

•CO.l0.1<0.1<0.1<0.1

•CO.l•CO.lO.l<0.1<0.1

0.1<0.1<0.1<0.1<0.1

•co.iO.l

0.7<0.1<0.1

O.l<0.1<0.1<0.1<0.1

ErMMI-D

0.1ppb

•CO.l•co.i^.i•co.i^.i

0.1•CO.l^.1<0.1

0.1

<0.1•co.i•co.i•CO.l^.i

0.2•CO.l•CO.l<0.1<0.1

<0.10.21.7

•CO.l•CO.l

•CO.l•co.i0.10.1•CO.l

YbMMI-D

0.1ppb

•CO.l•co.i•CO.lO.I•CO.l

0.2•CO.l•CO.l•CO.l

0.2


0.2•CO.lO.IO.IO.I

0.10.21.5

O.I0.1

O.I0.1O.IO.IO.I





1905719058190591906019061

1906219063190641906519066

1906719068190691907019071

1907219073190741907519076

1907719078190791908019081

1908219083190841908519086

NdMMI-D

0.1ppb

0.30.20.1

O.I0.1

0.6O.IO.I

0.714.3

5.813.24.00.21.0

0.50.10.60.40.8

13.81.80.90.43.1

0.10.10.42.6

0.1

SmMMI-D

0.1ppb

O.IO.IO.I0.1O.I

0.2O.IO.I

0.22.2

1.02.50.80.20.2

0.20.1

0.1O.I

0.1

2.20.30.20.10.6

0.1O.IO.I

0.50.1

Gd TbMMI-D MMI-D

0.1 0.1ppb ppb

O.I O.IO.I O.IO.I O.IO.I O.IO.I O.I

0.2 O.IO.I O.IO.I O.I

0.1 O.I2.0 0.3

0.9 0.11.9 0.30.6 O.I

O.I O.I0.2 0.1

0.1 O.IO.I O.IO.I O.IO.I O.I

0.2 O.I

1.9 0.30.3 O.I0.2 O.I

O.I O.I0.5 O.I

O.I O.IO.I O.IO.I O.I

0.4 O.IO.I O.I

ErMMI-D

0.1ppb

O.IO.IO.I0.1O.I

O.IO.IO.IO.I

0.8

0.50.70.3

O.I0.1

O.I0.10.1O.I0.1

0.80.1

O.IO.I

0.2

O.IO.IO.I

0.1O.I

YbMMI-D

0.1ppb

0.1O.I0.1O.IO.I

O.IO.IO.IO.I

0.8

0.40.60.3

O.I0.1

0.10.1O.IO.I

0.1

0.70.1

O.I0.1

0.2

O.IO.IO.I

0.2O.I

Member of the SGS Group (Socie"te~ Generals de Surveillance)




19087190881908919090*Blk BLANK

*Std STANDARD19091190921909319094

1909519096190971909819099

19100191011910219103*Std V6219

*Dup 19002*Dup 19012*Dup 19024*Dup 19036*Dup 19048

*Dup 19059*Dup 19071*Dup 19083*Dup 19095*Blk BLANK

NdMMI-D

0.1ppb

0.10.3

O.IO.IO.I

O.I0.1

O.I0.20.1

0.1O.I

0.60.22.3

0.10.1

O.I4.00.4

0.24.3

O.I0.70.7

0.10.80.10.1

O.I

SmMMI-D

0.1ppb

0.10.2

O.IO.IO.I

O.IO.IO.IO.IO.I

O.IO.I

0.1O.I

0.4

O.IO.I0.1

0.4O.I

O.I0.8

O.I0.10.2

O.I0.1

O.IO.IO.I

GdMMI-D

0.1ppb

O.I0.1

O.IO.IO.I

O.IO.I0.1O.IO.I

0.1O.I

0.1O.I

0.4

O.IO.IO.I

0.50.1

0.11.0

O.I0.10.1

0.10.1

O.IO.IO.I

TbMMI-D

0.1ppb

0.10.10.1O.IO.I

0.10.1O.IO.IO.I

O.I0.10.1O.IO.I

O.IO.I0.1O.IO.I

O.IO.I0.10.1O.I

O.IO.IO.IO.IO.I

ErMMI-D

0.1ppb

O.I0.10.1O.IO.I

O.IO.I0.1O.I0.1

O.IO.IO.IO.I

0.1

O.I0.1O.I

0.10.1

O.I0.3

O.I0.1O.I

O.IO.IO.IO.I0.1

YbMMI-D

0.1ppb

O.I0.10.1O.IO.I

O.I0.10.1O.IO.I

0.1O.IO.IO.I

0.1

O.IO.IO.I

0.1O.I

0.10.4

0.10.1

O.I

O.IO.IO.IO.IO.I





NdMMI-D

0.1ppb

SmMMI-D

0.1ppb

GdMMI-D

0.1ppb

TbMMI-D

0.1ppb

ErMMI-D

0.1ppb

YbMMI-D

0.1ppb

*Std STANDARD 'CO.l •CO.l •CO.l

Member of the SGS Group (Societe Centrale de Surveillance)

Appendix M

Survey Specifications

Helicopter Magnetic and Electromagnetic SurveyTotal Intensity Contour Map

And Resistivity Contour Map

SURVEY SPECIFICATIONS

Anomaly SPS.OOH Claim P1242319

Period: April 19, 2001Coverage (km): 24.2 line kmsSurvey Lines: 23 survey linesGrids: East/West: LO+OOE to L11+50E

North/South: Baseline 0+OON to 10+OON Survey Corners: NW corner: 562 650E ; 5 850 725N

SE corner: 563 800E l 5 849 725N

Anomaly SP3J)029 Claim P1242329

Period: April 28, 2001Coverage (km): 23.8 line kms (2 times)Survey Lines: 22 survey linesGrids: East/West: L1+OOE to L11+50ENorth/South: Baseline 2+OOS to 9+OON (small block on SW cornerextending to 5+OOSSurvey Corners: NW corner: 566 050E l 5 855 SOON

SE corner: 567 OOOE l 5 854 750NSW corner: 565 900E l 5 854 450N

*Differential GPS: May 1 st and 2 nd

*A Differential GPS test was conducted over claim P 1242329 to ensure the magnetometers accuracy.

5650000-

Helicopter Magnetic Surveyof Mineral Claim Block P 1242319

IIUTM Nad 27, Zone 16 NTS:43D January 7. 2003 Author: Deirdre Odonohoe Drawn by: Anik Boucher

| | Claim P 1242319

D Corner Post

9 Line Post

A MMI Samples

-fy Drill Hole

———— 10nT Contour

1: 10,000

563000 564000

5855000-

Helicopter Magnetic Survey of Mineral Claim Block P 1242329

fjUTM Nad 27, Zone 16 NTS:43D January 7, 2003 Author: Deirdre Odonohoe Drawn by: Anik Boucher

D

Claim P 1242329

Corner Post

Line Post

MMI Samples

Drill Hole

10nT Contour

1: 10,000

566000 567000

5850000-

Helicopter Electromagnetic Surveyof Mineral Claim Block P 1242319

IIUTM Nad 27, Zone 16 NTS: 43D January 7, 2003 Author: Deirdre Odonohoe Drawn by: Anik Boucher

Claim P 1242319

D Comer Post

* Line Post

A MMI Samples

-ty Drill Hole

——— 2ohm-m Contour

1: 10,000

563000

5855000-

Helicopter Electromagnetic Surveyof Mineral Claim Block P 1242329


Claim P 1242329

Comer Post

t Line Post

A MMI Samples

-fy Drill Hole

2ohm-m Contour

01 0.2 km

1: 10.000

566000l

567000

APPENDIX E

ARCHIVE DESCRIPTION

Survey Information:

Name of Survey Survey ID Contractor Contractor Job # NTS Sheets Province

Ministiko LakeMINFugro Airborne Surveys206243D,43eONT

Total Line km (delivered)Total number lines (flight and control;Dates flown (from, to)Aircraft wing type (fixed/ rotary)Aircraft Model EurocopterPilot: Bill HofstedeSurvey mode (drape/constant baro)Nominal bird terrain clearanceNominal sample intervalNominal traverse line spacingTraverse line directionNominal tie line spacingTie line direction

1086651 traverse; 63 control; -21 test13 July 01 - 27 July 01RotaryAS350D, Reg. C^FPOOFlights: allDrape20 mO.ls50 m0-180 degrees500m90-270 degrees

Projection Description:

Datum NAD27Spheroid Clarke 1866Projection UTMCentral meridian -87False Easting 500000False Northing OScale factor 0.9996WGS84 to NAD27 conversion method MolodenskyDelta x shift +10Delta y shift -158Delta z shift -187

Processing Information:

Total field Magnetics

EM inphase and quadrature data

Resistivity data

GPS data

DTM data

Barometric altimeter data

manual spike identification and removaldiurnal correction (diurnal data is first filteredusing a 31 pt. median followed by a 31 pt. banningalong line filter)lag correctionmanual and micro-levellingModified Akima spline gridding (Akima across line,linear interpolation along line)

drift correction using base level dataspheric removallag correctionmanual and mircro-levelling in areas of low signal

calculated from inphase and quadrature data for 2 coaxial and 3 coplanar coil pairs based on a pseudo- layer half-space modelmicro-levelling applied in areas of low signal modified Akima spline gridding (Akima across line, linear interpolation along line)

differential correction of the raw X, Y and Z data (postprocessing) using the base station data,convert X, Y and Z data to local system

manual removal of spikes from the GPS-Z datadigital terrain model was calculated from the despiked GPS-Z minusthe radar altimeter.tie line levelled of the above DTMthe radar altimeter was added back to the tie line levelled DTM toget a new corrected GPS-Zdigital terrain model was calculated from the correctedbaroaltimeter minus the radar altimeterresulting DTM was microlevelledmodified Akima spline gridding (Akima across line,linear interpolation along line)

convert pressure (kilopascals) to barometric altimeter (m) (Dighem software)

Radar altimeter data

manual removal of spikesmanual and microlevelling adjustments

manual indentification and removal of noise spikes

Sensor and Instrumentation Description:

Sensor typeSensor mountingNominal sensor terrain clearanceSample rate

DIGHEM V FREQ EM30 m below helicopter20 m10 per second

Nominal Frequency

1000900

55007200

56000

HzHzHzHzHz

Actual Frequency

1055880

57727272

55662

HzHzHzHzHz

Coil Orientation Separation

vertical coaxialhorizontal coplanarvertical coaxialhorizontal coplanarhorizontal coplanar

88886

.0

.0

.0

.0

.3

mmmmm

Channels

I,I,I,I,I,

QQQQQ

Sensitivity

0.0.0.0.0.

06 ppm12 ppm12 ppm24 ppm60 ppm

Sensor type

Sensor modelSensor mountingSensor Coordinates (dec. degress)Nominal sensor terrain clearanceSample rateResolutionAccuracy/ Absolute accuracy

Digital recording cesium vapourmagnetometerGeometrics G823In EM bird 30 m below helicopterN/A20 m10 per second0.01 nTmanufacturer's stated accuracy: 0.1 nT

Sensor type

Sensor modelSensor mounting

Base station cesium vapourmagnetometerGSM-19n/a

Sensor Coordinates (dec. degrees)Nominal sensor terrain clearanceSample rateResolutionAccuracy/ Absolute accuracy

554397.0 E, 5796638.0 W (Nad27 zone 16)N/A5 per second0.2 nTmanufacturer's stated accuracy: l nT

Sensor type

Sensor modelSensor mountingSensor Coordinates (dec. degrees)Nominal sensor terrain clearanceSample rateResolutionAccuracy/ Absolute accuracy

Base station cesium vapourmagnetometerFugro CF1n/a554397.0 E, 5796638.0 W (Nad27 zone 16)N/A5 per second0.01 nTmanufacturer's stated accuracy: l nT

Sensor typeSensor modelSensor mountingSensor Coordinates (dec. degress)Nominal sensor terrain clearanceSample rateResolutionAccuracy/ Absolute accuracy

Radar altimeterHoneywell/Sperry AA300In helicopterN/A50 m10 per second0.3 m3.0 m

Sensor typeSensor modelSensor mountingSensor Coordinates (dec. degress)Nominal sensor terrain clearanceSample RateResolutionAccuracy/ Absolute accuracy

Analog recorderRMS Instruments, DGR33Inside helicopterN/AN/AN/AN/AN/A

Sensor typeSensor modelSensor mounting

Digital data acquisition system RMS Instruments, DGR33 Inside helicopter

Sensor Coordinates (dec. degress)Nominal sensor terrain clearanceSpeedResolutionAccuracy/ Absolute accuracy

N/AN/A1.5 mm/sec4x4 dots/mmN/A

Sensor type Sensor model

Sensor mountingSensor Coordinates (dec. degress)Nominal sensor terrain clearanceSpeedResolutionAccuracy/ Absolute accuracy

Digital recorderRMS TCR-12, 6400 bpi type cartridgerecorderInside helicopterN/AN/AN/AN/AN/A


Tracking cameraPanasonic AG2400/WVCD132Under helicopterN/A50 mN/AN/AN/A


GPS Navigation systemAshtech GG24 real-time differential GPS positioningInside helicopterN/A50 m2 per second<5 metresManufacturer's stated accuracy is better than 10 metresreal-time


GPS Base station Marconi Allstar

Sensor mountingSensor Coordinates (dec. degress)

Nominal sensor terrain clearanceSample rateResolutionAccuracy/ Absolute accuracy

N/A52 0 19.13773'N, 86 0 12.11759'W (WGS84)elevation 149.3 mO metres3 per second<l metremanufacturer's stated accuracy for differential GPS is2 metres


Navigation systemPNAV-2001 navigation consoleInside helicopterN/A50 m2 per secondlOOxlOOm non-differentiall'y correctedN/A


Sensor mountingSensor Coordinates (dec. degress)Nominal sensor terrain clearanceSample rateResolution

Accuracy/ Absolute accuracy

Barometric pressure and temperature sensorsMotorola MPX4115AP analog pressure sensorAD592AN high-impedance remote temperature sensorInside helicopterN/A50 m10 per secondPressure:150 mV/kPaTemperature: 100 mV/'^C or 10 mV/'C (selectable)Pressure: Accuracy over the temperature range

(O degrees C to 85 degrees C) is maximum 1.5?;, in the temperature range from -40 to O degrees C the error increases linearly to a maximum of approximately 3.5 to 4% @-40 degrees C. Its the same with the temperature range from +8S to +125 degrees C with 3.5 to 41 error at +125 degrees C.

Temperature: Accuracy over the entire temp range of -25 to +105 degrees C is a maximum of */- 3.5 degrees with a typical value of +/-2 degrees

Appendix Mi

Ground Magnetic Survey Maps

Ground Magnetic Surveyof Mineral Claim Block P 1242319

5850000-


| | Claim P 1242319

Q Corner Post

0 Line Post

A MMI Samples

-^- Drill Hole


1: 10,000

563000 564000

5855000-

Ground Magnetic Survey of Mineral Claim Block P 1242329

UUTM Nad 27, Zone 16 NTS: 43D January 7, 2003 Author: Deirdre Odonohoe Drawn by: Anik Boucher

| | Claim P 1242329

D Comer Post

9 Line Post

A MMI Samples

•^ Drill Hole


Q2km

1; 10,000

566000 567000

Appendix IV

Reverse Circulation Exploration Drilling

Drill Hole Summary TableDrill Hole Location Map

Drill Logs and Magnetic Susceptibility Logs

Drill Hole Location Map of Mineral Claim BlockP 1242319

5850000-


Claim P 1242319

Corner Post

Line Post

Drill Hole

02km

1: 10,000

563000 564000


DRILL HOLE LOG

Hole ID:

Anomaly: Drill Type:

SP3-02-006R

SP3J)011Reverse Circulation

Total Depth: 26.0 m

Date Drilled: 08/04/02 to 08/04/02

Orientation: 0 0 I90 0

Drilled By: Heath S Sherwood Drilling Inc.

Logged By: Deirdre O'Donohoe, Jason Berenyi

Province: Mining Division:

Township:

Claim Number:

Ontario Porcupine

527861

P1242319

UTM Coordinates: 563284E l 5850105N(Nad 27, Zone 16)

NTS Mapsheet: 43 D/16

DEPTH INTERVAL

From (m)

02.5

7.17.8

10

13.9

16.9

18

18.5

22.8

To (m)

2.57.1

7.810

13.9

16.9

18

18.5

22.8

26

MATERIAL

OverburdenTill#1

BoulderTill#1

Lacustrine Clay

Till #2

UnconformityArenitic sandstone

Mudstone

Arenitic sandstone

UnconformityMafic Volcanic

DESCRIPTION

ice, water, organics.tan-brown sandy-clayey silty diamicton, uniform and relatively homogenous with granule-pebble sized clasts of biomicritic limestone, mafic volcanics and dolostone.dull grey carbonatized mafic volcanics.till as above, homogenous and relatively uniform with a decrease in pebble content with depth.dull brown sandy clay (10. 0-10. 8m) to tan/grey/brown clay; dense, massive, well compacted and featureless; free mica absent, occasional limestone granule dropstones.silty sandy diamicton, relatively uniform and dense with subangular to rounded granules and pebbles of arenitic sandstone, micritic limestone and dolostone.Quaternary sediments 1 Paleozoic Rocksunconsolidated, homogenous, mature, well sorted quartz sand, fine to coarse grained, very minor lithic component, predominantly clear, angular to subrounded quartz grains; Portage Chute Formation.unconsolidated marine clay, pale greenish-grey, dense, massive and structureless; non magnetic; Portage Chute Formation.unconsolidated sandstone as above, homogenous, well sorted with minor increase in lithic dolostone fragments with depth; Portage Chute Formation.Paleozoic Rocks 1 Archaean Basement Rocksdull greenish-grey, foliated to sheared, moderate to strongly chloritized, fine grained mafic volcanics; laser foliation and sub-schistose texture well developed in sheared cuttings.

MAGNETIC SUSCEPTIBILITY LOG

CLAIM ID: P1242319 DRILLHOLE: SP3-02-006R

Depth (m)

2.55.07.17.88.08.28.310.010.811.013.914.016.516.816.918.018.519.019.520.022.823.025.025.726.0

Sample Material

till/diamictonsandy tillsandy tillboulder 1 tillsandy tillsandy tillsandy tillsandy tilllacustrine claylacustrine claylacustrine claytill/diamictontill/diamictontill/diamictontill/diamictonarenitic sandstonemudstonearenitic sandstonearenitic sandstonearenitic sandstonearenitic sandstonemafic volcanicsmafic volcanicsmafic volcanicsmafic volcanics

Mag Susceptibility Value (xlO-3 SI units)

0.890.990.500.400.930.410.180.460.350.140.180.090.080.110.090.130.290.050.050.070.100.120.110.390.11

DRILL HOLE SECTION

SP3-02-006RProject. Spider3JV-1043Drill Hole- SP3-G2-Q06RAnomaiy: SP3J3Q11Location; 563283.88mE /.585Q10.5.26mNNAD27

NTS:043D716Claim Tag: 1242319Drilled: 08/04/02 to 08/04/02Geologist: Jason Berenyi l Deirdre O'Donohpe

LEGEND:

No Recovery

Boulders

Depth -3Mag Susceptx 10 Si

0.99

Sandy Clay

10m

15m —

20m-

25m -

Om - 2.5m: Overburden, ice, water, organics2.5m - 7.1m: Till, tan-brown sandy-clayey-silty diamicton, uniform and relatively homogenous with granule to pebble oversize of biomicrite limestone, mafic volcanics and dolostone 7.1m - 7.8m: Boulders, dull grey, carbonatized mafic volcanics

7.8m - 10m: Till, as above, homogenous and relatively uniform with a decrease in pebble content with depth

10m -13.9m: Lacustrine clay, dull brown sandy clay (10.Om-iO.8m) to tan-grey-brown clay; dense, massive, well compacted and featureless; free mica absent, occasional limestone granule dropstones

13.9m - 16.9m: Till, silty sandy diamicton, relatively uniform and dense with subangular to rounded granules and pebbles of arenitic sandstone, micritic limestone and dolostone

16.9m - 18m: Sandstone, unconsolidated, homogenous, mature, well sorted quartz sand, fine to coarse grained, very minor lithic component, predominantly clear angular to subrounded grain shapes18m - 18.5m: Marine clay (mudstone), unconsolidated, pale greenish grey, dense massive and structureless, non magnetic

18.5m - 22.8m: Sandstone, unconsolidated sand as above, homogenous, well sorted with minor increase in lithic dolostone fragments with depth

22.8m - 26m: Mafic volcanics, dull greenish-grey, foliated to sheared, moderate to strongly chloritized. fine grained: flaser foliation and sub- schistose texture well developed in sheared cuttings

Drill Hole Location Map of Mineral Claim BlockP 1242329

5855000-SP3-02-007R

fjUTM Nad 27. Zone 16 NTS: 43D January 7, 2003 Author: Deirdre Odonohoe Drawn by: Anik Boucher

Claim P 1242329

Corner Post

Line Post

Drill Hole

Marsh

a2 km

1: 10,000

566000 567000


DRILL HOLE LOG

Hole ID:

Anomaly: Drill Type:

SP3-02-007R

SP3J)029 Reverse Circulation

Total Depth: 32.0 m

Date Drilled: 10/04/02 to 11/04/02

Orientation: 0"V90 0

Drilled By: Heath S. Sherwood Drilling Inc.

Logged By: Jason Berenyi, Deirdre O'Donohoe

Province: Mining Division:

Township:

Claim Number:

Ontario Porcupine

527861

P1242329

UTM Coordinates: 566476E l 5854975N(Nad 27, Zone 16)

NTS Mapsheet: 43 D/16

DEPTH INTERVALFrom im)

05

511

19

22.7

23.5

24

24.2

24.5

To (m)

55

1119

22.7

23.5

24

24.2

24.5

25

MATERIAL

No sample recoveryGlaciofluvial outwash

No sample recoveryLimestone

Arenitic grainstone

Marine mudstone

Mudstone

UnconformityClayey regolith?

Brecciated micro-diorite?

DESCRIPTION

minor material recovered; clean moderately well sorted, subangular to subrounded, coarse granules and gravels of biomicritic limestone, mafic volcanics and lesser quartz/intrusive fragments.Unconformity: Quaternary sediments and Paleozoic Rocks.homogenous, pale whitish-tan, weakly dolomitized, interbedded biomicritic limestone (wackestone), very fine to fine grained (vfl-fu) quartz arenite grainstone, micritic limestone ^90*36 microcrystalline calcite), tight rock, vuggy porosity exceedingly rare, bitumen absent. Portage Chute Fm.tan-grey, weakly dolomitized poorly sorted, fine-minor medium grained (ml-mu) lithic arenite grainstone; limey carbonate matrix supported, interbedded with minor fine grained arenitic grainstone (vfu-fu), tight rock, porosity T-2%, mafic lithic fragments 2-7%; intensity of dolomitization increases to moderate at depth. Portage Chute Fm.dull olive-grey, unconsolidated carbonaceous mudstone, highly plastic, greasy texture, unit becomes increasingly grittier at depth. Portage Chute Fm.unconsolidated, olive-green gritty mudstone, grit component: very fine-medium grained (uvf-lm) quartz and lithic fragments. Portage Chute Fm.Paleozoic Rocks 1 Archaean Basement Rocksintense bright red hematite and chlorite altered, friable, vuggy, clayey gouge zone. No discernable rock fragments but occasional coarse vuggy pore fillings with py-cpy-carb (1. 76*56 Cu^]'fc Pb); interval is strongly carbonatized.friable, dull greenish-grey clay gouge, strongly carbonatized and chloritized, vuggy carb-py-cpy-po fillings, (1.58"fcCu, >^%Pb).intense brick red hematite altered, intensely carbonatized and brecciated; quartz and carbonate veining, vuggy py-cpy-qtz-carb mineralization, host rock type undefined due to pervasive alteration and brecciation.

25 31.5 Diorite submetallic, dull greenish-blue, strongly chloritized, intense to strongly carbonatized, massive to fine-grained biotite micro-diorite? common zones of quartz flooding and matrix carbonitization; three styles of sulphide mineralization noted: 1) Cu mineralization hosted in 2-4 mm wide qtz-carb-py- cpy-po veinlets (stockwork fractures?), 2) finely disseminated py-cpy-po in quartz flooded zones adjacent to fractures (wall rock alteration), 3) as massive replacement mineralization (py-cpy-po) in carbonate filled vugs; common Cu bloom on cuttings: 25.5-28. Om; pervasive py-cpy-po replacement mineralization: 25.0-31. 5m with carbonate alteration waning at depth; assay range in interval: 0. ]8"A Cu/O.Sm to T.09% Cu/O.Sm; average assay: T.75% Cu/6.8 m.

31.5 32 Schist olive green-tan, welt foliated; chlorite and limonite altered biotite- quartzofeldspathic schist; footwall to Cu mineralized zone; schistose texture well developed, non-magnetic and no carbonate alteration. Assays of 0.84 and 0.51*fcCu70.5m; average: Q.68% Cu/I.Om.______________________

MAGNETIC SUSCEPTIBILITY LOG

DRILLHOLE: SP3-02-007R CLAIM ID: P1242329

DEPTH (m)

5.011.015.016.017.018.019.020.021.021.522.022.522.723.023.523.823.924.024.224.324.424.525.025.526.026.527.028.028.529.029.229.530.030.531.031.532.0

SAMPLE MATERIAL

gravellimestonelimestonelimestonelimestonelimestonelimestonearenitic sandstonearenitic sandstonearenitic sandstonearenitic sandstonearenitic sandstonemarine claymarine claymarine claymarine claymarine clayclayey regolithclayey regolithclayey regolithclayey regolithclayey regolithmicro-dioritemicro-dioritemicro-dioritemicro-dioritemicro-dioritemicro-dioritemicro-dioritemicro-dioritemicro-dioritemicro-dioritemicro-dioritemicro-dioritemicro-dioritemicro-dioriteschist

MAG SUSCEPTIBILITY VALUE (xlO'3 SI UNITS)

0.700.020.020.000.000.000.010.000.030.050.020.010.120.060.010.0712.5025.5011.100.100.091.140.360.610.870.730.801.571.241.411.262.801.171.020.570.226.29

Project- Spider3JV-1043Drill Hoie SP3-02-007RAnomaly SP3-0029Localion 566475.34mE t 5854975.07mNNAD27 ' , T ,- Tnmbie Proxrs

SP3-02-007RNTS:Q43D;16Claim Tag: 1242329 (staked 26/02/2001}Drilled 10/04/0210 11/04/02Geologist: Jason Berenyi ' Deirdre O'Donohoe

LEGEND:

No Recovery

Limestone

Arenite

Mudstone

Gouge Zone

Bedrock(diorite)Bedrocki schist}

10m-

15m-

r

Average ,3 MagSusceptx 10 SI

20m-

25m

30m —

Om -11 m: No sample recovery

070 5m-5.1m: Glaciofluvial outwash: coarse granules and gravels of limestone, mafic volcanics and lesser quartz/intrusive fragments

11m - 19m: Limestone: weakly dolomitizedInterbedded limestone and quartz arenite grainstone

19m - 22.7m: Lithic arenite grainstone: weakly dolomitized, poorly sorted, fine-medium grained, Limey carbonate clast supported, interbedded with minor fine grained arenitic sandstone; mafic lithic fragments 2-7 0Xo. Intensity of dolomitization increases to moderate at depth. 22.7m - 24m: Mudstone, unconsolidated carbonaceous mudstone becomes increasingly grittier, with depth

24m -25m: Regolith l Breccia zone, intensely hematite altered, vuggy, clay zone. Strongly carbonatized and chloritized with coarse vuggy pore fillings of py-cpy-carb; some quartz and carbonate veiningI25m - 31.5m: Diorite: strongly chloritized. intense to strongly carbonatized, massive to fine grained biotite micro diorite? Cu mineralization hosted in cpy-py-po-qtz carbonate veinlets. Assay results range D.18% Cu ' 0.5m to 7.090Xo Cu /0.5m

31.5m - 32m: Schist: chlorite and limonite altered biotite-quartzo-feldspathic schist; Assays of 0.84and51 07oCu70.5m.

DETAILED DRILL HOLE SECTION

rr

Blow up of sulphide mineralized zoneProjeci 5pider3JV- iC43 Drill Hole: SP3-02-OQ7R Anomaly SP3-0029 Location 566476. 34mE ' 5854975. 07mN

EJ - "^ftp?? Real Time Trimble Proxrs

LEGEND: Depth24m-

Regolith

Gouge Zone

BrecciaD rf t 25m- Bedrock(di on le JBedrock(schist)

26m-

27m-

28m-

29m-

30m -

31m -

^j&MMM^

'\ \ "l 'i \ 'i y

tt f f t f 1 1 1 S t S/ f 'S tft/S/ftfff/S/S/ tSS 'S/S/fSt /'SSS

32m \ettt'fftftt"(tfl

CL PC T

2.34 Nl.58

0^60

\1.58

2.02

1 63

1 46

1.18

0.78

025

0.18 0.33

0.23

0.87

3.10

7.09

0.51

between 24 - 32 m in SP3-02-007RNTS. 0430/16 Claim Tag: 1242329 (staked 26/02/2001) Drilled: 10/04/0210 11/04/02 Geologist: Jason Berenyr'/'DeirdreQ'Donohoe

24m - 24.2m: Regolith: intense bright red hematite altered, chloritic; friable, vuggy, clay gouge zone. No discernable rock fragments but occasional coarse vuggy pore fillings with py-cpy- carb {1 .760ACu^1 0APb). interval is well carbonatized

24.2m - 24.5m: Clay gouge zone: friable, dull greenish grey, strongly carbonatized and chloritized, vuggy py-cpy-carb fillings, (1 .58V* Cu, "T'/oPb). 24.5m - 25m: Brecciated undefined rock: intense brick red hematite altered, intensely carbonatized and brecciated with quartz and carbonate veining and vuggy py-cpy-qtz-carb mineralization, host rock type undefined due to pervasive alteration and brecciation

25m - 31.5m: Diorite: submetallic, dull greenish- blue, strongly chloritized. intense to strongly carbonatized, massive to fine grained biotite micro-diorite?, common zones of quartz flooding and matrix carbonization; three styles of sulphide mineralization noted: 1} Cu mineralization hosted in 2-4 mm wide qtz-carb- py-cpy-po veinlets (stockwork fractures?). 2) finely disseminated py-cpy-po m quartz flooded zones adjacent to fractures (wall rock alteration), 3) as massive replacement mineralization {py- cpy-po) in carbonate filled vugs; common Cu bloom on cuttings: 25.5-28-Om. pervasive py-cpy- po replacement mineralization: 25.0-31 .5m with carbonate alteration waning at depth; assay range in interval Q.18% Cu/O.Sm to 7.090Xo Cu/O.Sm. average assay: 1 .75Va Cu/6.8 m.

31.5m - 32m: Schist: olive green-tan, well foliated; chlonte and limonite altered biotite- quartzo feldspathic schist, footwall to Cu mineralized zone; schistose texture well developed, non magnetic and no carbonate alteration. Assays of 0.84 and 0.51 "/o Cu/O.Sm; average: Q.68% Cu/1 ,0m.

Appendix V

Massive Sulphide Assay Certificates

ASSAY CERTIFICATE-1 (07/07/2002)

Sample DepthFrom

26.0

29.0

To29.0

32.0

Material

Regolith, Clay gouge zone, Massive Chlorite Schist

Sulphide and minor

Massive Sulphide, Chlorite Schist

ASSAY CERTIFICATE-2 (11/06/2002)

Sample Depth24.224.324.424.525.025.526.026.527.027.528.028.529.029.229.530.030.531.031.5

32.0

MaterialHematite altered RegolithHematite altered RegolithHematite altered RegolithClay gouge materialMassive Sulphide, PyrrhotiteMassive Sulphide, PyrrhotiteMassive Sulphide, PyrrhotiteMassive Sulphide, PyrrhotiteMassive Sulphide, PyrrhotiteMassive Sulphide, PyrrhotiteMassive Sulphide, PyrrhotiteMassive Sulphide, PyrrhotiteMassive Sulphide, PyrrhotiteMassive Sulphide, PyrrhotiteMassive Sulphide, PyrrhotiteMassive Sulphide, PyrrhotiteMassive Sulphide, PyrrhotiteMassive Sulphide, PyrrhotiteChlorite altered biotite-quartzo- feld. Schist, minor sulphideChlorite altered biotite-quartzo- feld. Schist, minor sulphide

ASSAY CERTIFICATE-3 (23/07/2002)The third assay completed by Chimitec Bondar-Clegg, was carried out to re-assay those samples that had elements with responses :*10 000 ppm (ie. Pb and Zn) to obtain a percentage of base metal contained in the interval.

BOIMDAR CLEGG

Rapport Lab Geociiimie Geochemical Lab Report

REPORT: C02-61579.0 ( COMPLETE ) EFERENCE: P.O.: 2233

CLIENT: DE BEERS CANADA EXPLORATION INC. PROJECT: 1043

SUBMITTED BY: DEIRDRE O'DONOHOE DATE RECEIVED: 11-JUN-02 DATE PRINTED: 27-JUI-02

1 DATEj APPROVED ELEMENT

i-020617 1 Au30i 020617 2 Agi 020617 3 Cui 020617 4 Cui 020617 5 Pbj 020617 6 Zn

l 020617 7 Moi 020617 8 Nil 020617 9 Co i 020617 10 Cd1020617 11 Bij 020617 12 As

: 020617 13 Sbi 020617 14 Fe i 020617 15 Mni 020617 16 Tei 020617 17 Baj 020617 18 Cr

l 020617 19 Vi 020617 20 Sni 020617 21 Wi 020617 22 Lai 020617 23 Al| 020617 24 Mg

i 020617 25 Cai 020617 26 Nai 020617 27 K'- 020617 28 Sr020617 29 Y020617 30 Ga

020617 31 Li020617 32 Nb020617 33 Se020617 34 Ta020617 35 TiC20617 36 Zr

GoldAg - IC01Cu - IC01Cu - GA50Pb - IC01Zn - IC01

Mo - IC01Ni - IC01Co - I C01Cd - IC01 Bi - IC01As - IC01

Sb - IC01Fe - IC01 Mn - IC01Te - IC01Ba - IC01Cr - IC01

V - IC01Sn - IC01W - IC01La - IC01Al - IC01Mg - IC01

Ca - IC01Na - IC01K - IC01Sr - IC01Y - IC01Ga - IC01

Li - IC01Nb - IC01Se - IC01Ta - IC01Ti - IC01Zr - IC01

NUMBER OFANALYSES

222222

2222 22

22 2222

222222

222222

222222

LOWERDETECTION EXTRACTION

5 PPB Fire Assay of 30g0.2 PPM HCL:HN03 (3:1)

1 PPM HCL:HN03 (3:1)0.01 PQ HF-HN03-HCL04-HCL

2 PPM HCL:HN03 (3:1) 1 PPM HCL:HN03 (3:1)

1 PPM HCL.-HN03 (3:1)1 PPM HCL:HN03 (3:1)1 PPM HCL:HN03 (3:1)

09 )DM un 'Uurft /7*1\ tC rn nLL*nNUv \Ji \J

5 W HCL:HN03 (3:1)5 'PM HCL.-HN03 (3:1)

5 PPM HCL:HN03 (3:1)0.01 PCT HCL:HN03 (3:1)

1 PPM HCL:HN03 (3:1)10 PPM HCL:HN03 (3:1)1 PPM HCL:HN03 (3:1)1 PPM HCL:HN03 (3:1)


0.01 PCT HCL:HN03 (3:1)0.01 PCT HCL:HN03 (3:1)

0.01 Pa HCL:HN03 (3:1)0.01 Pa HCL:HN03 (3:1)0.01 PCT HCL:HN03 (3:1)

1 PPM HCL.-HN03 (3:1)1 PPM HCL:HN03 (3:1)2 PPM HCL:HN03 (3:1)


0.010 PCT HCL:HN03 (3:1)1 PPM HCL:HN03 (3:1)

j ; i DATE NUMBER OF LOWER ;METHOD j APPROVED ELEMENT ANALYSES DETECTION EXTRACTION METHOD j

l , i l i 30g Fire ASsay - AA 020617 37 S S - IC01 2 0.01 PCT HCL:HN03 (3:1) INDUC. COUP. PLASMINDUC. COUP. PLASMAINDUC. COUP. PLASMAAAS LOW LEVEL ASSAY SAMPLE TYPESINDUC. COUP. PLASMA - -~INDUC. COUP. PLASMA OTHER DRILL T

NUMBER SIZE FRACTIONS NUMBER SAMPLE PREPARATIONS NUMBER!

'PES 2 -150 2 CRUSH/SPLIT i PULV. 2 ;

INDUC. COUP. PLASMA !INDUC. COUP;. PLASMA REPORT COPIES TO: DEIRDRE O'DONOHOE INVOICE TO: DEIRDRE O'DONOHOE :INDUC. COUP. PLASMA

INDUC. COUP. PLASMA This riport must not be reproduced except fn full. The data presented in this lINDUC. COUP. PLASMA report is specific to those sanples identified under "Sample Winter" ard is l

i applicable only to the sanples as received expressed on a dry basis unless : INDUC. COUP:. PLASMA otherwise indicated iINDUC. COUP. PLASMA *******i-"" ' ' - - ' " - ' - * - - - - - - - - - " - ' - - - - . - - - - - - - - - - - - - ' .^^^^- . . . . . . . ^^^^^^^^^-^^^^ :

INbUC. COUP. PLASMAINDUC. COUP, PLASMAINbUC. COUP. PLASMAINDUC. COUP. PLASMA

INbUC. COUP. PLASMAINDUC. COUP. PLASMAINDUC. COUP. PLASMAINbUC. COUP. PLASMAINDUC. COUP. PLASMA :INDUC. COUP. PLASMA :

INDUC. COUP. PLASMAINbUC. COUP. PLASMA iINDUC. COUP. PLASMAINDUC. COUP. PLASMAINDUC. COUP. PLASMAINDUC. COUP. PLASMA

INDUC. COUP. PLASMA ! iINDUC. COUP. PLASMA i iINDUC. COUP. PLASMAINDUC. COUP. PLASMA iINDUC. COUP. PLASMAINDUC. COUP. PLASMA J^

Chimitec - Bondar Clegg, 1322-B Harrican*. Val-d'Or, Quebec, J9P 3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

BOISIDXVFt CLEGG

j CLIENT: DE BEERS CANADA EXPLORATION INC. i REPORT: C02-61579.0 ( COMPLETE )

Rapport Lab Geudiimie Geochemical Lab Report.

DATE RECEIVED: 11-JUN-02

SAMPLE NUMBER

ELEMENT AuJO Ip

UNITS PPB pillCu

PPMmi pb im MO lil o, lip BI ip sb f tl|pjjjjj** Illf™ IffN lif-pM fifppM mmm

'Mn sitellfippM fifiippM itffppM iifm

SP3-02-007RC26-2SN) SP3

Ba lcl; V S W

1820

DATE PRINTED: 27-JUI-02

III Al |||iPiPCT IHl

11||| K liftlHi! PCT HII

PROJECT: 1043 PAGE 1 OF 1

Y ffff Li Illi Se f|||PPM |i|ppM iilppM liil

;||^2q ||l.37 ^iliO.43 111.01 11

Chimitec . Bondar a.W. 1322-B H.rric.n., V.WOr, Quebec, ,9P 3X6, Td: (8,9) 825-0178, F.x: (819) 825-0256

sPCT

16 ^5Illl 20 111 <5 I

l-c.01 1^10.00

r

s o

BONDAR CLEGG

Rapport Lab Geochimie Geochemical Lab Report

CLIENT: DE BEERS CANADA EXPLORATION INC. REPORT: C02-62246.0 { COMPLETE ) DATE RECEIVED: 07-AUG-02 DATE PRINTED: 23-AUO-02

PROJECT: NONE PAGE 1A( l/ 2)

SAMPLENUMBER

ELEMENT Au30 UNITS PPB

Wm cu :; :;\cof: PPM liffi

pb |:|| PPM 111

i Mo Ip Co IH

uEHHKh-1

O

o

SP3-02-007R/24.2M SP3-02-007R/24.3M SP3-02-007R/24.4M SP3-02-007R/24.5M SP3-02-007R/25M

SP3-02-007R/25.5MSP3-02-007R/26MSP3-OZ-007R/26.5MSP3-02-007R/27MSP3-02-007R/27.5M

J SP3-OZ-007R/28M SP3-02-007R/28.5M SP3-02-007R/29M SP3-02-007R/29.2M SP3-02-007R/29.5M

ea ino1O

00 Oi

05 1/5

00O

CMo

00o

SP3-02-007R/30M

SP3-02-007R/30.5H

SP3-02-007R/31H

SP3-02-007R/31.5M

SP3-02-007R/32M

296 If P496 l|ijt 634 , :^||i*10000 111 : |8si3;: 6029 761 :6;i ^10000 \

695565

Ip 9 sag? 52 lip? lljil: 30 ||f 58 : ;|;1 fill 25 gg;. 31 Iplit: 10 :!|il; 6l*(

76 l;74 :.i 68 ;88 |; ;| 86 1:2

isB ^ 10000 111*10000 ||? .710000 l/ 'V 10000

78 ;-: ::;2i!iS:: 84 î|I78 |;|jsf l72 111:; 88 ?I1P-

7769 |';:';|::; 2534 111:1;: 1804 Hill 3308 |:l:|l 2292 HI

2658 : !;';;:45j?;; 9 " ;:;:|;484 ..|.i;

76 Illlllfl <1 llbl:687 ';M

121 Ilill *i ;|li:262 |:|r|.

91 ilf||: <1 !:|i5i6 lil

91 Illjifl <1 |I|:i721 ji|^|103 111!!! 1 1111624 'ip!97 !I|lp <1 :||i642 l^''^

B i :î|? Sb ififJPPM i

75 11 728 1031 623 HI 10 i

6 -l|^; *5 l

*5 ;Bf?: 7 ;

*5 l|2 6 ;

*5 1^: 13 \

6;||; 7^

*5 ii|S:.: 6 ? <5 :j|i|l <5 l<5 lp:: •i

Mn la*;:, Ba 4S^: : v ;?sn;: w AlPCTîfPPM ||||PPM iflPPM J!! PCT

li|:|25111145 ;:|fN2o Ifpi .60 ipiHo.oo p ||sl-: is lif'' '""'^132; 15 Sp! 73 :::||^litit.' s 26; n i|ff;^2o I|||o.o9 ll^sll

;|i|S K l|j-| Y ^ Li |p| Se lip T iPCT

{(31x20 lp;0.88 lilllHo.OO ||^ 1S l|l 15IH? 10 Ibl: 12

x. 01

PUpPH

p!69 i 95 f 62 ; t 13J:- 6 i

|;PPM PfiM;;: PCT

l? *5 ill.013

168 |2tJ:': 7 157' :4 |:?||^20 i'^.O 86 .'-a| 7 213:: ' 4 ::|i;i^20 1||('X.O

i^J; : 49 ;:;:i:^::: 6 |^; : 7 :|^:';*20

iS;: 44 Ip': 6 |||l: 7 If ii:Ho; : 57 :;||| 6 |t||:' 5 l||^2o; 65 îf;' 7 2|j:;;: [16 *i?0fx20

M 51 |j|:: 6 H| ' 6 ;||:x20

8673 Hi 162 ll|i 2 |^|730 |||1iruinn *::::i:ifi-:: *ne i'ift^Sî*1^: * iynlwJ^-to t'.X&'&t

84 ;|p|74 IffUNoOOO p^ 195 || 86 mflÔOOO iH 165 f" 13 HIP 18 Hill

Ii||7i8 liiii:!:;:i:-:|::ix:

|||il Kl !||472 III 8462 Il|: 401 |||||: 75 l||^99 l|tli 5119 111 162 Iiif 10 ||f|l1 ||1|

^ |||: 9 ||;||; 49 li! 7 HI 7 |||*2013 iip; 7 Ililiil 52 III;' 7 |i|: ! 4 fl|^027 |||| <5 ||ii||:s 65 |ft 7 ij||| 6 i||p 25

IHI; <5 Ifillil BS Hi; 5 i|i| 12 lliiô""""""""l 88 111; 6 lil; 11 11*20

Hi0 - 12;|||o.i4|i|o.l1 : 1||0.86 ; Hi". 51 \

1 Illl

4.99 *iOji 2.24 fifJI 1.02 |||2.48 i:bl:

0.18 si 0.20 l 0.04 H 1.02 II 0.05 n

i : :;||: *i .sp: ^ îpjx.oi

61

0.10 l 0.04 l 0.07 l 0.13 l 0.12 l

pl*-01

HN.01

lipIIIII

o Ml

-i 111

d l|l 1 IP

o I®

6 ^189 :s|p

S :i||

7 \SSjij.8 ::^J:S

7 Isi;:: 22 ill

8 lill

<5 ilKoi

*tf^.01Hi*- 01

Oo

Chimiuc - Bondar Clegg. 1322-B H mcsDS, V.I-d'Or, Quebec, J9P3X6, Tel: (819) 825-0178, Fax: (819) 825-0256

CO 0og

o

O

to<

co ino in0001

X

o oo: oZ

esioCO^ x

CHIJVirTEC BONDAR CLEGG

Rapport Lab Geochimie Geochemical Lab Report

\ CLIENT: DE BEERS CANADA EXPLORATION INC. 1 REPORT: C02-62246.0 C COJfLETE )

PROJECT: NONE DATE RECEIVED: 07-AUG-D2 DATE PRINTED: 23-AUO-02 PAGE 1BC Z/ 2)

SAWLE ELEMENT Ir liiijjj.

NUMBER UNITS PPM |||ii|f:

SP3-02-007R/24.2M SP3-02-007R/24.3M SP3-02-007R/24.4M SP3-02-007R/24.5M SP3-02-007R/25M

SP3-02-007R/25.5MSP3-02-007R/26MSP3-02-007R('26.5HSP3-02-007R/27M

SP3-02-007R/27.5M

SP3-02-007R/28HSP3-02-007R/2B.5MSP3-02-007R/29M

SP3-02-007R/29.2MSP3-02-007R/29.5M

SP3-02-007R/30MSP3-02-007R/30.5MSP3-02-007R/31M

SP3-02-007R/31.5HSP3-02-007R/32H

825 : """""

aa*

Chimitec - Bondar Clegg, 1322-B H iniciiM, Vi!-d'0r, Quebec, J9P 3X6, Tel: (819) 825-0178, Fix: (819) 825-0256

CHIIVIITEC BONDAR CLEGG

Certificat D' Analyse Assay Lab Report

REPORT: C02-62246.1 ( COMPLETE ) REFERENCE: P.O.: 7725

CLIENT: DE BEERS CANADA EXPLORATION INC. SUBMITTED BY:

PROJECT: NONE DATE RECEIVED: 08-OCT-02 DATE PRINTED: 9-OCT-02

DATE NUMBER OF LOWER APPROVED ORDER ELEMENT ANALYSES DETECTION LIMIT EXTRACTION METHOD

021009 1 Pb Pb - GA50 3 0.01 PCT HF-HN03-HCL04-HCL AAS LOW LEVEL ASSAY 021009 2 Zn Zn - GA50 1 0.01 PCT HF-HN03-HCL04-HCL AAS LOU LEVEL ASSAY

SAMPLE TYPES NUMBER SIZE FRACTIONS NUMBER SAMPLE PREPARATIONS NUMBER

ROCK 4 -150 4 SAMPLES FROM STORAGE 4

REPORT COPIES TO: 2555 MALEY DRIVE, UNIT 4 INVOICE TO: 2555 MALEY DRIVE, UNIT 4 FAX:

********************************************************************************

This report must not be reproduced except in full. The data presented in this report is specific to those samples identified under "Sample Number" and is

.................................l......V..*p]jiiT(c'^^^otherwise indicated

********************************************************************************

Chimitec - Bondar Clegg1322-B rue Harricana, Val d'Or, Quebec, J9P 3X6

Tel: (819) 825-0178, Fax: (819) 825-0256

cmivirrccBONDAR CLEGG

Certificat D'Analyse Assay Lab Report

CLIENT: DE BEERS CANADA EXPLORATION INC. REPORT: C02-62246.1 ( COMPLETE ) DATE RECEIVED: 08-OCT-02

PROJECT: NONE DATE PRINTED: 9-OCT-02 PAGE 1 DE 1

SAMPLE NUMBER

ELEMENT

UNITSPb

PCTZn

PCT

SP3-02-007R/24.2M 1.83 SP3-02-007R/24.3M 2.68 SP3-02-007R/24.4M 1.20 SP3-02-007R/31H

Chimitec - Bondar CleggI322-B me Harricana, Val d'Or, Quebec, J9P 3X6

Tel: (819) 825-0178, Fax: (819) 825-0256

CHIIVIITEC BOIMDAR CLEGG

Certificat D 'Analyse Assay Lab Report

REPORT: C02-62246.2 ( COMPLETE )

CLIENT: DE BEERS CANADA EXPLORATION INC.

PROJECT: NONE

REFERENCE: P.O.: 7725

SUBMITTED BY:

DATE RECEIVED: 10-OCT-02 DATE PRINTED: 22-OCT-02

DATEAPPROVED

021022021022

ORDER

1 Au2 Pt

ELEMENT

Gold - Fire AssayPlatinum

NUMBER OFANALYSES

2020

LOWERDETECTION

1 PPB5 PPB

LIMIT EXTRACTION

FIREFIRE

ASSAYASSAY

METHOD

FIREFIRE

ASSAY-DCP

ASSAY-DCP

021022 3 Pd Palladium 20 1 PPB

SAMPLE TYPES NUMBER SIZE FRACTIONS

FIRE ASSAY

NUMBER

FIRE ASSAY-DCP

SAMPLE PREPARATIONS NUMBER

.VsA*iPlEJs":fRb*Vs'fMA(3EZZ'.Mr

INVOICE TO: 2555 MALEY DRIVE, UNIT 4REPORT COPIES TO: 2555 MALEY DRIVE, UNIT 4

FAX:t*******************************************************************************

^report is specific to those samples identified under "Sample Number" and is applicable only to the samples as received expressed on a dry basis unless otherwise indicated

**************************************************************

Chimilcc - Bondar Clegg1322-B rue Harricana, Val d'Or, Quebec, J9P 3X6

Tel: (819) 825-0178, Fax: (819) 825-0256

CHIIVIITEC BOIMDAR CLEGG

Certificat D'Analyse Assay Lab Report

CLIENT: DE BEERS CANADA EXPLORATION INC.i REPORT: C02-62246.2 ( COMPLETE )

i SAMPLE ELEMENTi NUMBER UNITS

Au PtPPB PPB

PROJECT: NONE :DATE RECEIVED: 10-OCT-02 DATE PRINTED: 22-OCT-02 PAGE 1 DE 1 ;

Pd lPPB i

i SP3-02-007R/24.2Mj SP3-02-007R/24.3M

; SP3-02-007R/24.4MSP3-02-007R/24.5M

: SP3-02-007R/25M

285 ^460 6624 *5101 ^712 x5

9 j9 i

3 i1 i2 ;

SP3-02-007R/25.5MSP3-02-007R/26MSP3-02-007R/26.5M

; SP3-02-007R/27Mi SP3-02-007R/27.5M

65 <567 562 1095 ^90 5

ei i1 j2 i^ i

i i

: SP3-02-007R/28M; SP3-02-007R/28.5Mi SP3-02-007R/29M; SP3-02-007R/29.2Mi SP3-02-007R/29.5M

66 879 871 559 587 5

1 ;1 i

<1 i1 i^ ;

i SP3-02-007R/30MSP3-02-007R/30.5M

SP3-02-007R/31M

: SP3-02-007R/31.5Mi SP3-02-007R/32M

74 562 ^

88 ^

4 ^6 ^

<1 i<1 i d ;<1 i

* 1 i

Chimitec - Bondar CleggI322-B rue Harricana, Val d'Or, Quebec, J9P 3X6

Tel: (819) 825-0178, Fax: (819) 825-0256

Appendix VI

PIMA Geochemistry

Spectral Response Table Spectral Response Graphs

1400 1600 1800 Wavelength

2000 2200 2400

P 1242329 (SP3-0029)

Table of PIMA response elements

n^sy&^tom^--'---:--^.'-'-22.723.023.523.823.924.024.224.324.5

Major MineralSaponite?

IlliteSaponite?

Illite?Talc

BiotiteBiotite

Fe-BiotiteBiotite

1 ,. ; Z* M InojrJMin e ral± i^FMg-Fe Chlorite

Opaques, SaponiteOpaques

Opaques, SaponiteSerpentine, Opaques

Talc, OpaquesTalc, Opaques

Opaques, Illite

These samples also contained weak spectral absorbance features associated with high amounts of opaques. The Mg-OH absorbance was the main diagnostic feature in these samples and this suggests they are of interest.

S020722

s0207(a)23

s0207(b)23

s0207(c)23

s0207(d)23

s0207(a)24

s0207(b)24

s0207(c)24

s0207(d)24

1400

SP3-02-07R

22-7,•vi

-8*

13

1600 18002000 Wavelength

2200 2400

Appendix VII

Environmental Water Monitoring

Map of drill holes and water sample locations

5850000-

Drill Hole and Water Sample Location Map of Mineral Claim BlocksP1242319, P1242329

IJ

MBQC

UTM Nad 27, Zone 16 NTS: 43C, 43D January 7. 2003 Author: Deirdre Odonohoe Drawn by: Anik Boucher

LEGEND

DBCEI Claims

Water Samples

Drill Holes

560000 570000

CLAIM NUMBER

P 1242319

P 1242329

DRILL HOLE NUMBER

SP3-02-006R

SP3-02-007R

DRILL HOLE COLLAR LOCATION

563283

566476

5850105

5854975

WATERDRAWPOINT/ SAMPLING LOCATION

563388

568851

5849460

5855907

DESCRIPTION OF WATER SOURCE

North side of McFaulds Lake, ~650m south of drill siteUnnamed stream, outflow to Attawapiskat River, ~2500m northeast of drill site

Appendix VIII

Statements of Exploration Expenditures Expenditure Distribution Chart

Statement of Expenditures P12423 19

2001 spring campaign MMI Ground Geophysics

2001 summer campaign Helicopter Geophysics

2002 winter campaign DRILLING PIMA ASSAYS

Salary and WagesGeologistsField AssistantsDrill AssistantCookCamp PersonDraftingReport Preparation

TotalsField CostsTent Camp Accom. And Meals(3135/day)Field SuppliesFuel (Diesel,propane, Jet fuel)Field TelephoneFreightTravel Costs

TotalsRental EquipmentTrimble Real time GPSRadios

TotalsContractor ServicesAbitibi Helicopters(2001:bell 206)(2002: 206,205)Nakina AirserviceAbitibi GeophysicsFugroHeath S Sherwood DrillingTrow Engineering

TotalsLaborartory ChargesXRALChimitec Bondar CleggDBCE

Totals

3Ss5ss5ss

s3sss

3ss

3

ss353s

s3ss

250.00350.00

-500.00350.00200.00

1,000.002,650.00

2,722.00

605.26

439.8653.63

111.893,932.64

-19.7919.79

1,508.33

2,234.47----

3,742.80

101.67--

101.67

3s5ss53s5

3ssss331s5s553s

39SS

250.00350.00

-500.00350.00

-1,000.002,450.00

2,722.00

605.26

439.8653.63

1 1 1 .893,932.64

-19.7919.79

1,508.33

2,234.472,733.00

---

6,475.80

----

Sss33SSS

3ssss3s

3sss

sssssssss

500.00--

500.00350.00

--

1,350.00

3,780.00

200.002,034.57

251.356.30

64.696,336.91

---

-

-8,238.39

--

8,238.39

----

Sssssssssssssss

ss

s3sssssssss

1,500.00350.00600.00750.00525.00

-2,000.005,725.00

6,480.00

2,000.003,703.79

461.3099.00

238.8212,982.91

--

20,510.03

13,128.26--

6,722.81866.49

41,227.59

----

S 75.0033SS3S 20.00S 95.00

S

3S

Ss3S

ssssssss3S

ss

S 25.00S 25.00

S53SS35S

5

53

535S

35S

3

S

S3S

353S

--------

-

--

----

---

.

-

---

----

Assessment Activity Totals:ASSESSMENT TOTAL:

ss

10,446.9099,305.93

s 12,878.23 s 15,925.30 s 59,935.50 S 120.00 S -

Stay .lent of Expenditures P1242329

2001 spring campaign MMI Ground Geophysics

2001 summer campaign Helicopter Geophysics

2002 winter campaign DRILLING RIMA ASSAYS

Salary and WagesGeologistsField AssistantsDrill AssistantCookCamp PersonDraftingReport Preparation

TotalsField CostsTent Camp Accom. And Meals(S1357day)Field SuppliesFuel (Diesel,propane, Jet fuel)Field TelephoneFreightTravel Costs

TotalsRental EquipmentTrimble Real time GPSRadios

TotalsContractor ServicesAbitibi Helicopters(2001:bell 206)(2002: 206,205)Nakina AirserviceAbitibi GeophysicsFugroHeath S Sherwood DrillingTrow Engineering

TotalsLaboratory ChargesXRALChimitec Bondar CleggDBCE

Totals

SSsssssss

sssssssssssssss

ssss

250.00350.00

-500.00350.00200.00

1,000.002,650.00

2,722.00

605.26

439.8653.63

111.893,932.64

-19.7919.79

1,508.33

2,234.47----

3,742.80

101.67--

101.67

Ssssss3S

s

sssssssssssssssssss

250.00350.00

-500.00350.00

-1,000.002,450.00

2,722.00

605.26

439.8653.63

111.893,932.64

-19.7919.79

1,508.33

2,234.472,733.00

---

6,475.80

----

Sssss$ss

ss3

Sssssss3

S33SS

3SSS

500.00--

500.00350.00

--

1,350.00

3,780.00

200.002,034.57

251.356.30

64.696,336.91

---

-

-8,238.39

--

8,238.39

----

S3SS3SSS

ssssssssss

sssssss

ssss

1,500.00350.00600.00750.00525.00

-2,000.005,725.00

6,480.00

2,000.003,703.79

461.3099.00

238.8212,982.91

365.62-

365.62

20,510.03

13,128.26--

6,722.81866.49

41,227.59

----

S 75.00SSss3

S 20.00S 95.00

S

sssssss3S

sssssssss

S 25.00S 25.00

sS3SSs3S

ssss3SS

sssssssssssss

250.00------

250.00

-

--

-174.06

-174.06

---

-

-

----

-1,042.00

-1,042.00

Assessment Activity Totals:ASSESSMENT TOTAL:

ss

10,446.90101,137.61

s 12,878.23 s 15,925.30 s 60,301.12 S 120.00 s 1,466.06

Expenditure Allocation Chart

Claim Number: P1242319Record Date: Aniversary Date: Claim Units: Work Required: Total Monies Spent: Work Monies to Applied: Work Period Applied for: Excess Monies (to be banked): Next Assessment:

09/03/200109/03/20039S 3,600.00S 99,305.93S 18,000.005 yearsS 81,305.9309/05/2005

Claim Number: P1242329Record Date: Aniversary Date: Claim Units: Work Required: Total Monies Spent: Work Monies to Applied: Work Period Applied for: Excess Monies (to be banked): Next Assessment:

09/03/200109/03/20036S 2,400.00S 101,137.61S 12,000.005 yearsS89,137.6109/05/2005

ONTMJO MINISTRY OF NORTHERN DEVELOPMENT AND MINES

Transaction No: Recording Date: Approval Date:

W0360.00362

2003-MAR-07

2003-MAR-11

Work Report Summary

Status: APPROVED

Work Done from: 2001-APR-13

to: 2002-OCT-08

Client(s):

171748 DE BEERS CANADA EXPLORATION INC.

Survey Type(s):

AEM AMAG ASSAY

MAG PBORE

GCHEM

Work Report Details:

Claim*

P 1242319

P 1242329

External Credits:

Reserve:

Perform Applied Assign Perform Approve Applied Approve Assign Approve Reserve

399,306 399,306 S1 8,000 318,000 30 0 381,306

3101,138 3101,138 312,000 312,000 SO 0 389,138

3200,444 3200,444 330,000 330,000 SO 30 3170,444

SO

S1 70,444 Reserve of Work Report#: W0360.00362

S1 70,444 Total Remaining

Status of claim is based on information currently on record.

Reserve Approve Due Date

381,306 2008-MAR-09

389,138 2008-MAR-09

3170,444

43D16SE2001 2.25123 BMA 527 861 900

2003-Mar-17 13:10 Armstrong_d Page 1 of 1

Ministry ofNorthern Developmentand Mines

Date:2003-MAR-12

Ministere du Developpement du Nord et des Mines Ontario

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

DE BEERS CANADA EXPLORATION INC.2555 MALEY DRIVEUNIT4SUDBURY, ONTARIOP3A 4R7 CANADA

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

Dear Sir or Madam

Submission Number: 2.25123 Transaction Number(s): W0360.00362

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 STEVEN BENETEAU by email at [email protected] or by phone at (705) 670-5855.

Yours Sincerely,

Ron GashinskiSenior Manager, Mining Lands Section

Gc: Resident Geologist

De Beers Canada Exploration Inc. (Claim Holder)

Assessment File Library

De Beers Canada Exploration Inc. (Assessment Office)

Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:18068

43D16SE2001 2.25123 BMA 527 861 200

ONTARIOCANADA

MINISTRY OF NORTHERN DEVELOPMENT AMD MINES

PROVINCIAL MINING RECORDER'S OFHCE

Mining Land Tenure Map

E65POOE

Sfei^L;.-'^ '^'"I"*"-';; 1 ''iL..V^feii^^ '^'""•i"~:""L:,-,, ;'^fc:" J !L;. ^rfc'" '-'V;"'- rftk ,;;-,-.. -" ."j:;":: r' -fti!,',, jf,. - :^^..':' -!"j!;";" adfc".":l:iI' : .-iAfc",;...-,V ,~j-;"; :"-J.k '3.^'':Al,5~l';:"'V ..'"j : ,-;.:" *k ,rr. ;* ., .-"3^. .:::" :*ljl; ,;^-. '*-., .:~r :-Jij.fc p::: ;"iJ.fc ,;.. -*^ ., .:::r ::^ .;:;::::' ^ ,--. -*•;^;j;j, .;:;,:.y-^ '.::I:;;'^™^^ ;:™' :*| '^"rSk E':[|"Si.fc•i)"".,^; ^'ii'^ ;:3"î# -i™" j^; ̂

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UTM Zone 18 SOOOcnerm

Those wishing to ateke mining duima should consult with the Provincial Mining Recorders' Office of the Ministry of Northern Development end Mines for additional General Information and Limitations information on the statue of the lands chown haraon. This map is not intended for navigational, survey, or land title determination purposes as the information Contact Information: shown on this map It compiled from various source*. Cornpletenew and accuracy are not guaranteed. Additional information rn*y also be obtained through the local Land Titles or ReglBtry Office, or the Ministry of Natural Resources.

The information shown is derived from digital data available in the Provincial Mining Recorders' Office at the time of downloading from the Ministry of Northern Development and Mines web situ,

This map me/ not ohow unregistered lund tenure and interests inToll Free Map Datum: NAD 63 '"nc* including certain patents, laasos, easemante, right of ways,

Provincial Mining Recorder^ Office Tol: 1 (688)415-6848 ea S/ttojection: UTM (8 degree) flooding rights, licences, or other forms of disposition of rights and WJHet Green Miller Centre 933 Ramsey Lake Road Fax: 1 (677) 670-1444 Topographic Data Source: Land Information Ontario interest from ths Crown. Also curtain land tenure and land uses Sudbury ON PSE BBS Mining Lsnit Tenure Source: Provincial Mining Hecordera' office lhat restrict or prohibit free entry to stake mining claims may not be Home Page: www.nmdm.gcw.on.ca/MNDM/MINES/LANDS/mlBmnpga.htrn illustrated.

Date l Time of Issue: Tue Mar 11 14:24:51 EST 2003

TOWNSHIP l AREA PLAN BMA 527 861 AREA G-4306

ADMINISTRATIVE DISTRICTS ; DIVISIONSMining Division PorcupineLand Titles/Registry Division UnavailableMinistry of Natural Resources District Unavailable

TOPOGRAPHIC

Administrative Boundaries

:f w ] Township

~""" "l Corioession, Let

'S"S* Provincial Park

i î Indian Rasatvt

!"": cm, pit s Pi*

____ Contour

P Mine ShaHl

a Mine HeadFrflme

Railway

Trail

Natural Gat Pi|Mllng

IJIIIItkM

Land Tenure

Freehold Patent

Cpl Surface And Mining Rtghto

[jiT Surface Kijhti Only

fa"} Minna Rinht. Only

Leasehold Patent

( Sunset And Mining Right*

OH BurMM Right* Only

("Jjl Mmlno Rlohti Only

Licence of Occupation

Surface And Mining HigirU

Surtto* Kanw only

Mining Rightl Only

Land Una PtmSt

Orddr In Council {Not open For staking)

Water Power Uaa9 AgrMnwnt

Mining Claim

FiM Only Mining Clalmi

LAND TENURE WITHDRAWALS

ArftHK Withr]rawn

Mining ATM wiMrawal Typtt Ws-n KurtKi *na Mnlnj wgMsiMMmn Ws SiiHmRl9tilsC!nlymihdrawn Wm MMriH RlgrrB Orty Wirrtrawn

Order in Council withdrawal Types Wm Surtece And Mining Rlshto tMMmm V/ft SurffiuiRiBhlsOnlyWiihcirawr W'm Minln(Hisl*OrilyWilWTavin

IMPORTANT NOTICES

(call 1:41010

LAND TENURE WITHDRAWAL DESCRIPTIONSIdcntlftar Type Deis D*iorlpflon

Jan 1, 2001 OTOSKWIN - ATTAWAPISKAT RIVER PROVINCIAL PARK

43D16SE2001 2.25123 BMA 527 861 210

ONTMIIOCANADA

MINISTRY OF NORTHERN DEVELOPMENT AMD MINES

PROVINCIAL MINING RECORDER'S OFFICE

Mining Land Tenure Map

SB5000E

SOOOin arid

Those wishing lo slake mining daimi shouW consult with the Provincial Mining Rncordors' Office of the Ministry of Northern Development and Mines for additional Gene ral Information and Limitations information on the ttrttus of the lands shown hanton. This map is not Intended for navigational, survey, or (tind title determination purpoiMS ae the information Contact Information: shown onthl&map l* compiled from varlou* sourca*. Completeness and accuracy are not guaranteed. Additional information may alio be obtained through the local Land Titles or Registry Office, or the Ministry of Natural Resources.

hd Information shown id derived from digits] date available in the Provincial Mining Reccrders' Office at the time of downloading from tnc Ministry of Northern Development and Mines web site.

Toll Free Map Datum; NAD 33Provincial Mining Recorders' Office Tel: 1 (888)416-6845 ext 67t8ijection: UTM (B degree)Willet Green Miller Centre 933 Ramsey Lake Road FaK 1 (877) 670-1444 Topographic Data Source: Land Information Ontario Sudbury ON P3E BBS H Home Page: www.rnndm.gav.on.ca/MNDMWINES/LANDSfrnlsmnpg6.hlm

This map may not ahow unregistered lend tenure and interests in land Including certain patents, laasas, easements, right of ways, flooding rights, licences, or other forms of disposition of rights and interest from the Crown. Also certain land tenure and land uses

and Tanura Source: Provincial Mining Recorders' Offlco lhat restrict or prohibit free entry to stake mining claims may not beillustrated.

Data l Time of Issue: Tue Mar 11 14:29:31 EST 2003

TOWNSHIP ; AREA PLAN BMA 527 861 AREA G-4306

ADMINISTRATIVE DISTRICTS l DIVISIONSMining DivisionLand Titles/Registry DivisionMinistry of Natural Resources District

PorcupineUnavailableUnavailable

TOPOGRAPHIC

: Administrative

f"""! Township li_.j

\'"""l 'Concession, Lol

iSifi Provincial ParhLwS*

["H" Indian Reserve

: " ": an, pit * put

Land Tenure

Freehold Patent

ra

FJ]

fill

Surtscs And Mining Rights

SurlK* Wahls Only

E

A

Contour

Mine Statto

Mine Hoadfrome

Railway

Road

TraS

Nalural Gai Pipeline

S surfKft AnU Mining Rights

[gl SurfoMi RlahW Only

fjjjl Minlno Nghtt Only

Lloencfi ofOccutiflltori

*

SurliKO And Mining R'gnts

3urMot Riani* only

Mining Right) Only

IwdUMi Permit

Ordflf In Council (Not open For making)

Mining Ci*m

f" " " " ~7,' ~ ," FiW Only Mining Claims:-.'; 'ts"

LAND TENURE WITHDRAWALS

: t;84: : 1 AraSB WUhdravm from DWntwlllnn

Mining Ads withdrawal Types Wsm Surtaw And Minlnfi RighttWIUKfiewn Wb Surteos Rlghis Only Vflthowwp

Onttr in Council withdrawal Types W'srn Birtxt *nd Mining RiahtoWlhdrmin W"s Sufftc* Rlghss Only Wfcfxlrawrf W'rfl Mining Rlfllils Only WHlKJtHwrt

IMPORTANT NOTICES

Soul. 1:41(10

LAND TENURE WITHDRAWAL DESCRIPTIONSld*ntlH*r Typ* DM* D*terlpllon

S2 Jan 1. 2001 OTOSKWIN . ATTAWAPISKAT RIVER PROVINCIAL PARK

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