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ASSESSMENT REPORT ON

WILSON LAKE MOBILE METAL ION REGIONAL SAMPLING PROGRAM

HANSON LAKE CLAIM GROUP CHAMBERS TWP.

G-3416

Prepared For:

TEMEX RESOURCES CORP.4307 Kerry Road, Unit 100

Burlington, OntarioL7L 1V8

Distribution:

2 Copies - Ministry of Northern Development 8c Mines3 Copies - Temex Resources Corp.

January, 2002

"RECEIVEDj AN 2 b 2CD2

GEOSCIENCE ASSESSMENT OFFICE_____

Wilson Lake Project -2- Chambers Township Mobile Metal Ion Sampling Program_______________________________January. 2002

TABLE OF CONTENTS

1.0 INTRODUCTION.............................................................................................................................^2.0 CLAIM GROUP.................................................................................................................................43.0 LOCATION AND ACCESS ..............................................................................................................44.0 GEOLOGY........................................................................................................................................^

4.1 Regional Geology ...........................................................................................................................45.0 MMI SAMPLING RESULTS ............................................................................................................ 56.0 CONCLUSIONS...............................................................................................................................^7.0 RECOMMENDATIONS....................................................................................................................68.0 STATEMENT OF QUALIFICATIONS ............................................................................................ 7

LIST OF FIGURES

Figure l: Claim Location Map Figure 2: MMI Sample Location Map

LIST OF APPENDICIES

Appendix A: Sampling MethodologyAppendix B: MMI Sampling ResultsAppendix C: MMI Sample Descriptions

TEMEX RESOURCES CORP.

Wilson Lake ProjectMobile Metal Ion Sampling Program

-3- Chambers Township ____January. 2002

LO INTRODUCTION

From November l, 2001 to November 3, 2001 a regional mobile metal ion leach (MMI) sampling program was completed by Temex Resources Corp. (Temex) on the Hanson Lake Claim Group of the Wilson Lake Diamond project (Figure 1). All claims are held in good standing by Temex, of 4307 Kerry Road, Burlington, Ontario, L7L 1V8 (MNDM Client No. 303055). Geological staff on contract to Temex completed the work including Mr. Jim Laidlaw, Mr. Graham Stone, Mr. Gordon Hume and Mr. Angus MacDonnell completed the field work with Mr. Jim Laidlaw participating and supervising the field crews. Mr. Dan Bunner. Senior Geologist for Temex provided overall project supervision.

A total of 74 MMI soil samples, with 9 duplicate analyses were collected from 7 sampling lines (Figure 2). Samples were collected at 50 m intervals over known airborne and ground geophysical targets suspected to be potential buried kimberlitic intrusives. Samples were collected over top of the geophysical anomalies and off of the anomalies.

The objectives of the MMI sampling program were

* to obtain information that could be used as a lithological discriminator of potential 'blind' kimberlitic intrusions; and

* obtain additional information that could subsequently be used to assist in prioritizing potential drilling targets using the MMI, previous geophysical and kimberlitic indicator mineral till sampling and geological mapping data that Temex previously obtained.

The MMI soil samples were submitted to XRAL Laboratories in Don Mills, Ontario. All samples were analyzed for MMI-DD elements, which include:

MgCrTiCoNiRbSrYNb

PdBaLaTaCePrNdSmGd

TbErYb

The sampling methodology followed is described in the technical bulletins provided within Appendix A.


Wilson Lake Project -4- Chambers Township Mobile Metal Ion Sampling Program___________________________ January. 2002

2.0 CLAIM GROUP

The MMI sampling work was completed on a contiguous block of claims owned by Temex within Chambers Township. In total this contiguous claim block comprises 24 claim units or 384 hectares. Sampling was completed on both of the claims within the claim group. These claims were:

Claim Group Claim Number MMI Sampling Lines

Hanson Lake 1203044 72, 73, 74, 75 and 76 Hanson Lake 1203045 70 and 71

3.0 LOCATION AND ACCESS

The Hanson Lake Claim Group of the Wilson Lake diamond Project is west-north-west of the town of Temagami by about 12 km. Temagami is located about 100 km north of the City of North Bay which in turn is about 450 km north of the City of Toronto. A logging road running west off of Highway 11 may be used to reach the claims.

4.0 GEOLOGY

The following sections provide a brief description of regional and local lithology present within the MMI sampling area.

4.1 Regional Geology

The following description of the regional geology was obtained from a Report on Airborne Geophysical Target Field Evaluation prepared for Temex by Interbon Mineral Exploration and Services. The Report is entitled:

* Report of Airborne Target field Evaluation, Wilson Lake Property, NTS 31 M, Interbon Mineral Exploration C& Services, September l, 2000, Rick G. Bonner (A uthor)

"The Wilson Lake Project is heated approximately thirty kilometers to the west of the southern end of Lake Timiskaming. It is positioned on the boundary of the Superior and the Grenville Provinces. More locally the northern portion of the project is within the Cobalt Embayment; a Paleoproterozoic sedimentary basin developed as a continuation of the Archean initiated techtonic events. The southern portion of the project is within the Grenville Tectonic Zone (GTZ), a broad zone characterized by variable fabric development, metamorphism and faulting.


Wilson Lake Project -5- Chambers Township Mobile Metal Ion Sampling Program_________________________________January. 2002

Lithologically the property is underlain by a bi-modal sequence of metamorphosed ultramafic to felsic volcanics, metasediments and granitic intrusions of Archean age. These are in turn are unconformably overlain by coarse to fine sediments of the Huronian Supergroup; itself subsequently intruded by the Nipissing Diabase event. Several smaller mafic to intermediate intrusive events resulted in dyke arrays trending north/south and northwest. Rocks exposed to the south of the GTZ comprise gneiss, schist, marble and granites with fabric development ranging from intense to moderate.

A major crustal feature, the Lake Timiskaming Structural Zone (TSZ), is known to host kimberlites in the Kirkland Lake and Cobalt areas. Sage (2000) observes that northern Ontario kimberlites occur on a trend of 325", a trend approximately parallel to the TSZ. It is also observed that kimberlites occur in close proximity to the intersections of property scale features, such as contacts and lineaments, and the major northwest trending TSZ structures. Several major northwest trending TSZ structures are observed in magnetic data from the Wilson Lake Project. These structures are oblique to the northwest trending Grenville Front Tectonic Zone crossing the southern portion of the project area. "

5.0 MMI SAMPLING RESULTS

The following report section summarizes the MMI sampling results. Sample analyses are provided in Appendix B. Sample descriptions are provided in Appendix C. Figure 2 shows the location of all samples. Within this report the results of individual lines have not been subject to a statistical analysis to produce sacked bar graph representations of the data since element groupings determined by Temex are considered proprietary.

A review of the duplicate analysis suggests that the sample methodology was sound since in general the analytical results can be reproduced, taking in to consideration the heterogeneous nature of most soil samples. Similarly, a review of the analytical Standard results suggests that the laboratory has been able to reproduce the analytical data.

It is apparent from the data that potential kimberlitic anomalies are showing increasing trends in Mg. Cr and Ni content. Similarly, the lathanide series elements are elevated. Along individual lines favourable anomalies appear to be showing higher ratios of these elements near the centre of the body relative to the margins of the body where samples are not expected to be over top of a kimberlite.


Wilson Lake Project -6- Chambers Township Mobile Metal Ion Sampling Program_________________________ January, 2002

6.0 CONCLUSIONS

Based on a preliminary review of the data indicates that one line may be considered highly anomalous. That line is Line 75. Line 77 is known to be associated with an isolated, ovoid airborne magnetometer geophysical anomaly and a favourable topographic feature (an oval swamp).

Moderately anomalous lines or lines that have geochemistry indicators with a frequency response that would represented by a skewed profile include Line 73 and Line 74. Both of these MMI lines are associated with negative response Keating anomalies as outlined on Ontario Geological Survey Map 60 092 -Airborne Magnetic and Electromagnetic Surveys, first Vertical derivative of the Magnetic Field and Keating Coefficients, Temagami South Area, Scale 1:50,000, 2001.

7.0 RECOMMENDATIONS

Further compilation work in preparation for drilling of potential kimberlite targets is warranted on the Wilson Lake Project - Hanson Lake Claim Group. Prior to selecting targets the following is recommended:

* The MMI data should be subject to statistical analysis. The analytical results for individual lines sampled should be plotted on stacked bar chart diagrams and the data reevaluated to rank the potential MMI anaomalies;

* The statistical analysis data should be reviewed in-conjunction with data Temex already has in its possession including; airborne and ground geophysics, geological mapping and kimberlitic indicator mineral till sampling data;

* The MMI and geophysical anomalies should be prioritized for potential drill targets;

* Those potential drilling targets which have not been subject to ground geophysical screening using a magnetometer and a Max Min II EM should be surveyed with a small reconnaissance grid; and

* Following the ground geophysics the high priority targets should be drilled

Respectfully Submitted,


(f.Dan P. Bunner. M.Sc., C.E.T. Geologist


Wilson Lake Project -7- Chambers Township Mobile Metal Ion Sampling Program_______________________________January. 2002

8.0 STATEMENT OF QUALIFICATIONS

I Dan P. Bunner of Oakville, Ontario hereby certify that:

1. I hold a Master of Science Degree in Geology from Carelton University, Ottawa, Ontario, obtained in February 1989.

2. I have been practicing my profession since 1979 in Newfoundland, Nova Scotia, Quebec, Ontario, Manitoba and the Northwest Territories.

3. I am currently employed as a Geologist/Project Manager for Golder Associates Ltd. and am also currently Senior Geologist of Exploration for Temex Resources Ltd. and as of the date of preparing this report held shares in the company.

4. I am a Registered Professional Geoscientist (P. Geo.) in the Association of Professional Engineers and Geoscientists of the Province of British Columbia.

5. I am a Certified Engineering Technologist (C.E.T.) in the Ontario Association of Certified Engineering Technicians and Technologists.

6.1 have based conclusions and recommendations contained in this report on knowledge of the area, my previous experience and on the results of the drilling conducted on the property during 2001.

7) I currently reside at 501 Orchard Drive, Oakville, Ontario, L6K 1N9.

Dated thisJanuary 21, 2002in Mississauua, Ontario

Dan P. Bunner


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APPENDIX A

MMI SAMPLING METHODOLGY

A PO BOX l 132

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The application of MMI Geochemistry

For

DIAMOND Exploration.

May, 2001

INTRODUCTIONA number of companies approached MMI Technology enquiring whether MMI geochemistry would be applicable for diamond exploration. Several companies had reported success in using the existing MMI-B element suite to target kimberlite units in Africa, South America, and Australia. Research and developmental work has been undertaken by MMI Technology to assess the applicability of the MMI technique for diamond exploration, and to develop a new MMI leachant, specifically for elements associated with kimberlitic hosts. Initial results are presented below.

RESEARCH AND DEVELOPMENTThe existing MMI Leachants, MMI-A (Cu, Pb, Zn, Cd), and MMI-B (Au, Ag, Ni, Co, Pd) were developed to target commodity based elements, namely for gold, base metals, and nickel exploration. The success of the MMI technique in its application to these mineral commodities can largely be attributed to the extensive research and case studies undertaken.

From the existing suite of elements available to the MMI process, only Ni, Co, and Pd were considered useful for diamond exploration, and these had been used successfully to identify diamondiferous kimberlite pipes. Other elements considered as 'core elements' of kimberlite exploration include Nb, Cr, and Mg. During the research program Y and Rb were added. To be able to include these elements into the MMI suite, a new leachant was developed; - MMI-D Mg, Nb, Cr, Ni, Co, Pd, Y, Rb.

The testing of MMI-D has been undertaken on soil samples collected by various participating companies. Samples have been collected across known kimberlite units in a number of geological settings and climatic regimes in Australia, Africa, Canada, and Brazil. The studies have included dykes covered by colluvial scree and till between 5 to 20 metres deep, through to dykes buried beneath sand colluvium and up to 50 m of sandstone and granite. Some samples submitted test magnetic or geophysical anomalies and are yet to be confirmed by drilling. Three such case studies applying the new leachant are presented below as Case Study 1,2, and 3.

SAMPLE COLLECTIONAll case study sampling was undertaken in accordance with published standard MMI Geochemical sampling instructions.

l Sampling PositionDo not vary depth, or target a specific layer/feature of a soil profile when sampling. - Extensive research has shown that element concentrations can vary markedly with a change in sampling depth. Any significant variation in sampling depth and technique can cause severe problems for interpretation. It is imperative that all samples are collected in a consistent manner.

In undisturbed environments samples should be collected approximately 50 to 200 mm below the surface at a consistent depth. - The initial step in taking an MMI soil sample requires the surface soil layer to be scraped away eliminating loose organic matter, debris, and any possible contamination. In cases where there is an extensive organic horizon (O or Ao) at the surface, (e.g. Canada), the sample should be taken 50 to 200mm below the lower interface, i.e. into the A horizon where there is some mineral content in the soil rather than all organic material. Before actually taking the soil sample material, equipment should be brushed to eliminate residue from previous samples and preferably flushed with the soil from the new sample site.During sample collection and handling, no jewellery (watches, rings, bracelets, and chains) should be worn, as this can be a major source of contamination.

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Moist Samples. - Damp samples should be collected in a similar manner to soils in dry environments. Samples should not be dried in ovens or pulverised in crushers or mills. In the case of dry plastic clays, sample material can be desegregated by crushing with a mallet between disposable plastic sheets. Sieving should be avoided if there is any possibility of serious cross-contamination during sample collection via the sieve. In this case, larger rocks and twigs/leaves etc can be removed by hand.

Organic Material. - Organic material in the form of fine roots and hairs, decomposing leaf material and other fine organic debris WILL NOT adversely affect MMI analyses. Experimental work has shown that variability in sampling depth has a more significant impact on element responses.

Contaminated Sites. - Where there is a potential contamination problem, samples should be collected at a depth so as to avoid any contaminated material and the sampler's judgment must be relied upon. Another option available to the sampler if there is possible site contamination is to sample in the lee of a tree and/or under a thick layer of organic litter.

2 Equipment* A 30-cm diameter plastic garden sieve or kitchen colander with minus 5-mm apertures, available

from hardware and super markets, is ideal for sample collection;* Plastic collection dish with similar diameter and a kitchen floor brush used for cleaning the sieve

and dish between samples;* A bare steel (no paint) garden spade; and* Plastic snap seal bags, do not use calico.Where samples are wet, large rocks should be picked out and material placed directly into a plastic snap seal bag. Double bagging can be useful if there is concern that the bags may be split or punctured by angular rock fragments.

3 Sample SpecificationA 300-gram sample is collected and stored in a plastic bag (a 90 x 150-mm plastic snap seal sample bag is recommended). Once sealed in the snap seal plastic bags, samples should be placed in polyweave sample dispatch bags (maximum 40 per bag). Stored in this manner, samples can be carried on tray-back vehicles during summer without problems and be stored for long periods.

4 Sample SiteSample sites should be undisturbed and preferably away from any major contamination: creek beds, drainage, drilling lines, pads, roads, etc. Wind borne contamination should also be eliminated during sample collection by sampling just below the surface.

MMI SOIL SAMPLING - IN SUMMARY* Use one laboratory wherever possible.* For a particular survey, avoid submitting samples in small batches (if possible). If this

cannot be avoided, calculate Response Ratios for each batch, BEFORE combining the data.* ALWAYS sample consistently 50 - 200mm below surface or interface between organic

layers and mineral soil horizon.

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CASE STUDIES

Case Study l - North Kimberley Kimberlite Province, Western AustraliaThe project area is located in the North Kimberley Kimberlite Province. Previous exploration included an extensive EM/magnetic airborne programme that had identified a number of anomalies that required prioritizing in order to establish an effective drilling programme. Conventional geochemical techniques in the area were not effective because of the depth of overburden.

A trial of the MMI-D leachant was completed across a known diamondiferous kimberlite. The kimberlite is beneath approximately 10-15 m of cover. Samples were collected at the surface according to standard MMI sampling practice. The soil samples were treated using the MMI-D leachant, and analysed by Australian Laboratory Services (ALS) in Perth for Mg, Nb, Cr, Ni, Co, and Pd by ICPMS. Duplicate samples of the soils were also sent to ALS for conventional analysis of the above elements. The results for MMI and conventional geochemistry are shown in Figures l and 2 respectively.

Case Study l - Review of ResultsThe MMI-D leachant shows a strong multi-element anomaly across the middle of the traverse corresponding to the kimberlitic pipe. The most responsive elements appear to be Cr, Nb, Ni, Co, and Pd. The MMI response across this traverse is most promising due to the multi-element nature and magnitude of the anomaly. The conventional geochemistry only shows a significant response in the Cr for three samples. The conventional responses are offset from the MMI anomaly and primary source. The single element Cr response is somewhat erratic, occurring over 3 discrete samples, and is thought to represent surficial dispersion away from the original position.

Case Study 2 - Nabberu Kimberlite, Western AustraliaThe project area is located 250 km NE of Meekatharra. The field survey collected samples on a 50 m x 50-m grid covering an area of 200 m N-S and 350 m E-W. The sample material consisted mainly of sandy loam soil collected 5-15 cm from the surface. Care was taken to avoid contamination from previous exploration activities, especially drilling. The soil samples were treated using the MMI-D leachant, and analysed by Australian Laboratory Services (ALS) in Perth for Mg, Nb, Cr, Ni, Co, and Pd by ICPMS. Duplicate samples of the soils were also sent to ALS for conventional analysis of the above elements. Results comparing MMI and conventional geochemistry are shown in Figures 3 and 4.

Case Study 2 - Review of ResultsThe drill section logs clearly show an erratic sub-surface occurrence of the Nabberu 08 Kimberlite. Generally, the body is tabular in nature and dips to the NW. In addition, there appears to be a number of apotheoses and kimberlitic stringers recognised in the drill holes. A relatively distinctive boundary striking NE-SW provides a trace of the nearest projection of the body to surface with between 7-10 m of aeolian sand cover. The stacked bar charts clearly identify the known near surface edge of the body with elevated responses in Cr, Nb, and Y. There is also a weaker Mg and Pd association with these elements with responses up to eighteen and eight times background respectively. These elements also respond to the deeper sections of kimberlite to the NW where samples have elevated response ratios up to 84 for Cr, 36 for Nb, and 23 for Y above kimberlite at 65 m depth including 10 m of sand overburden (holes 105 and 106), see Figure 3.

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Conventional geochemistry has shown no significant responses across the kimberlite (Figure 4).

Kimberlite Pipe - 10m Cover\;:-:':^-' :Kimberley, Kimberlite

Response Ratios 60 H

TJC

50

40D)

l 30 mS 20E

10

o

MMI

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Figure l

Kimberlite Pipe - 10mKimberley, Kimberlite

Response Ratios

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Figure 2

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Nabberu 08, Western AustraliaLine 7220350 N

Response Ratio

226750 226800 226850 226900 226950 227000 227050 227100

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Granite

Kimberiite

Figure 3

A Division of Wamtech Pty. Ltd. A.C.N. 009 315 404 Sniic 2. HniL-rprise 1,'nit 2. l l Brodit-llall Drv. Bentley. 6102

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Conventional Response Ratios

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Figure 4

Case Study 3 - James Bay, Ontario, CanadaThe study area is located in Northern Ontario. Canada. Sampling was undertaken to evaluate the effectiveness and suitability of near surface geochemical techniques as a practical exploration tool. The prime aim of the study was to determine the suitability of the MMI leachants/techniques, and to highlight any modifications or adjustments required for adapting this technology for Canadian field situations. The study area had a number of known kimberlite occurrences with good control available from previous exploration activities.

The kimberlites in the study area have intruded Ordovician-Silurian carbonates, at an approximate date of 155 to 180 Ma. Overburden in the study area is typified by several metres of peat, from l to •2 m as shown by trenching and pitting. The peat is underlain by a highly variable quaternary

stratigraphy comprising beach sand layers (up to l rn thick), a transgressive marine clay layer (up to l m thick), sandy clay till (up to 2 m thick), and finally locally derived till up to 0.5 m thick. The region is subject to discontinuous permafrost; however, the orientation has been completed on a sub- area free of permafrost.

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Case Study 3 - Review of ResultsBackgrounds for each element, using the mean of the lowest quartile of data for each element, were used to calculate response ratios (anomaly to background) for the element suite. Response ratios for samples collected at the peat/mineral soil layer, were then plotted as stacked bar charts along sample lines. Response ratios for Ni, Co, Pd, Cr, Nb, Mg, and Y are plotted for the MMI-D extractant (upper) and for Ni. Cr, Nb, and Mg after total digestion (lower), see Figure 5.

110 100 90 80 70 60 50 40 30 20 10 O

James Bay, OntarioLine OE

MM l Response Ratios

9.1 10 1 11.1 12.1

Sample No

13.1 14.1

INt HCo EPd mCr EDNb E

Line OE3nventional Response Ratios

"kimberlite

9.1 101 11.1 12.1 13.1

Sample No

JBNiCon MCrCon BNbCon BMgCon j

14.1

Figure 5

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Implications for ExplorationThe studies above present some initial results from the MMI-D digestion. Further work from other case study sites is continuing to confirm the applicability of MMI-D to diamond exploration. Based on the findings above, it would appear that MMI may prove to be a very effective tool for diamond exploration.

Until a larger number of studies have been completed, the MMI-D leachant should be applied with appropriate diligence. Companies interested in using the MMI process for diamond exploration should endeavour to complete orientation studies where possible. It is important to realise that in this application, MMI is being used as a lithological discriminator. As such, the concentrations of diagnostic elements in the source are expected to be significantly lower than normally expected from base or precious metal mineralisation. Therefore, interpretation of data may require careful examination of what would normally be classified as subtle geochemical trends or patterns. In some cases, the total element suite may not respond and effective discrimination may rely on one or two elements depending on depth to source and surficial regolith conditions. For example where dykes intrude basaltic hosts elements such as Nb, Y, Rb have been diagnostic of buried diamondiferous dykes in Africa.

New DirectionsIn geological settings where the contrast between host and source is less definitive, e.g. kimberlitic intrusions in mafic/ultramafic (Brazil, Africa), the element suite for MMI-D may not be as effective. In this environment Nb, Y and Rb may be the only effective elements. Currently research is underway assessing new leachants for rare earth elements for both kimberlitic and pegmatitic dykes. Clients exploring in these terrains should contact MMI Technology for more current information on the applicability of new leachants.

AcknowledgementsThis document contains information generated from the M323 MERIWA research project.

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Samplingm

Boreal Climatic Zones

Technical Bulletin TB14 July 1999.

Sampling in Boreal Climatic Zones

INTRODUCTION

Clients from North America and Europe have requested information on the optimum sampling position in Boreal climatic zones. This Technical Bulletin has been prepared in an effort to clarify the most appropriate sampling positions within soil profiles in these areas.

PROCEDURE

MMI sampling in boreal climates, particularly with overlying peat blankets, should be completed asfollows;

Penetrate the leaf litter and organic material that still has structure i.e. decomposing leaves, bark, twigs etc, (includes peat). Once through to a true A-horizon i.e. where the sou resembles a decomposed mass without any obvious leaf or vegetation visible, discard the top 10cm of this horizon, then collect the sampfe between 10 and 25 cm within the unit.As sampling moves along a grid line, where topographic influences cause variartion in the profile and the material available for collection, (moving onto a dominantly mineral soil with or without organics), collect the sample at 10-25 cm below me interface with surface leaf/twig matter.

Experience with sampling programs in Europe and North America has demonstrated that the Mobile Ion geochemical technique works best with samples collected at a constant depth (10-25 cm) BELOW the interface between leaf and twig litter on surface, and completely decomposed material beneath that can vary from A to B horizon material Case study information for these environments from Night Hawk Lake, Timmins, Ontario, Canada and Puolalaki, Sweden, is available. The technique is now being applied successfully at other sites in Canada, Alaska and Europe using this protocol.

Idem J .f

10cm

I twiji -

Orfmicii(hful

Errferred Sample

Witcr

Section 6.0 - SAMPLE COLLECTION of the MMI Operations Manual provides furtherinformation (see extract below,), www.mmigeochem.com

In undisturbed environments samples should be collected approximately 10 to 20 cm below the surface at a consistent depth. - The initial step in taking an MMI soil sample requires the surface soil layer to be scraped away eliminating loose organic matter, debris, and any possible contamination. In cases where there is an extensive organic horizon (O or Ao) at the surface, (e.g. Canada), the sample should be taken 5 to 20 cm below the lower interface, i.e. into die A horizon. Before actually taking die soil sample material, equipment should be brushed to eliminate residue from previous samples and preferably flushed with the soil from the new sample site. During sample collection and handling, no jewellery (watches, rings, bracelets, and chains) should be worn, as this can be a major source of contamination.

APPENDIX B

MMI ANALYTICAL RESULTS

XRAL XRAL LaboratoriesA Division of SGS Canada Inc.

1885 Leslie Street Don Mills, Ontario Canada M3B 3J4 Telephone (416) 445-5755 Fax (416) 445-4152 CERTIFICATE OF ANALYSIS

Work Order: 066209To: Temex Resources Corp.

Attn: Duane ParnhamTemagami Exploration Company 4307 Kerry Drive, Unit 100 BURLINGTON ON/CANADA/L7L 1V8

Date 22/11/01

Copy 1 to

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

86 SOIL(MMI)12/11/01Cover Sheet plusPages 1 to 8

Distribution of unused material: Pulps: Store Rejects: Store

Certified By

ISO 9002 REGISTERED

ouza, General Manager ratories

Subject to SGS General Terms and Conditions

Report Footer: L.N.R. ~ Listed not received l.S. = Insufficient Sample n.a. = Not applicable — — No result "INF = Composition of this sample makes detection impossible by this method M after a result denotes ppb to ppm conversion, % denotes ppm to "/o conversion

Member of the SGS Group (Scciete Generate de Surveillance)


Work Order: 066209 Date: 22/11/01 FINAL Page l of 8

Element. Method. Det.Lim. Units.

L680+OOE L680 + 50E L68 l +OOE L68 1+50E L682 + OOE

L682 + 50E L683 + OOE L68 3 + 50E L684 + OOE L684 + 50E

L685 + OOE L685 + 50E L68 6 + OOE L690 + OOE L690 + 50E

L69 l +OOE L69 1+50E L692+OOE L692 + 50E L693+OOE

L693 + 50E L694 + OOE L694 + 50E L695+OOE L695 + 50E

L69 6 + OOE L696 + 50E L697+OOE L69 7 + 50E L698+OOE

MgMMI-D

100ppb

1040980

1120870630

281037103550

6001280

6103170296075004310

490290540960

7690

15501430870

11001070

299010301150580980

TiMMI-D

1ppb

•Cio•ci1625

<l214

415

37

1421211634

131

•ci3

273

282

•Ci7

•Ci

11•Ci

1331543

919

CrMMI-D

1ppb

•CI•ci•ciO•CI

•ci•CI0•CI•ci

o<l•CI<l<l<l<l•CI<l

1<l<lo•CI<l<l<l•ci<l<l

CoMMI-D

1ppb

42661

2438

17

24849

•Ci

26

98161

•ci426

17

21221

43

14

NiMMI-D

3ppb

86799

420171023

53241

929

•C36

101750

O26

89

18

27181475

RbMMI-D

1ppb

4366473769

3444723039

353036147

3054253420

3049362339

3959415050

SrMMI-D

0.1ppb

11.46.6

28.416.915.0

79.392.264.7

8.418.3

9.927.750.1108

51.4

45.87.2

14.923.670.8

74.227.825.051.427.7

55.714.110.617.118.0

YMMI-D

0.1ppb

•CO.l•CO.l•CO.l

0.30.2

•CO.l0.50.10.20.2

•CO.l0.40.40.10.3

•CO.l0.40.20.20.5

•CO.l^.1•CO.l

0.2•CO.l

0.40.60.20.30.4

NbMMI-D

0.1ppb

•CO.l•CO.l•CO.l•CO.l•CO.l

•CO.l0.70.1

•CO.l0.1

•CO.l0.40.5

•CO.l0.4

•CO.l•CO.l•CO.l•CO.l

0.9


0.4•CO.l•CO.l•CO.l•CO.l

PdMMI-D

0.1ppb


•CO.l•CO.l•CO.•CO.^.•CO.•CO.•CO.•CO.•co.



•cO.l•CO.l•CO.l•CO.l•CO.l

BaMMI-D

0.1ppb

198132194

89.6159

48281.4193

82.8146

212102185113204

270157123107189

369123169304318

10375.444.4144141

LaMMI-D

0.1ppb

•cO.l•cO.l•cO.l

0.40.2

•cO.l0.50.20.20.3

0.10.30.40.20.2

•cO.l0.40.20.30.7

•CO.l•CO.l•cO.l

0.3•cO.l

0.40.60.30.30.5

TaMMI-D

0.5ppb

^.5^.5^.5•C0.5^.5

•CO. 5•C0.5•CO. 5•CO. 5•CO. 5

•CO. 5^.5^.5^.5^.5

•CO. 5•CO. 5•C0.5^.5•C0.5

•CO. 5•CO. 5•CO. 5•CO. 5•CO. 5

•CO. 5•CO. 5•CO. 5^.5•CO. 5

CeMMI-D

0.1ppb

•CO.l•CO.l

0.10.80.7

0.10.80.40.50.6

0.20.71.00.40.4

0.20.90.40.61.3

•CO.l•CO.l

0.20.6

•CO.l

0.91.60.50.61.0

PrMMI-D

0.1ppb


•cO.l•cO.l•cO.l•CO.l•cO.l

•CO.lCO.l

0.1•CO.l•CO.l

•CO.l0.1

•CO.lCO.l

0.2


0.10.2

CO.l•CO.l

0.1

NdMMI-D

0.1ppb


0.40.2

•CO.l0.40.10.30.3

0.10.30.50.20.3

0.10.60.20.30.6


0.2•CO.l

0.50.70.30.30.7

Member of the SGS Group (Societe Generale de Surveillance)


Work Order: 066209 Date: 22/11/01 FINAL Page 2 of 8

Element. Method. Det.Lim.Units.

L698 + 50E L699 + OOE L699 + 50E L69 10 + OOE I.720 + OOE

L720 + 50E L72 l +OOE L72 1+50E L722+OOE L722 + 50E

L72 3+OOE L72 3 + 50E L724 + OOE L724 + 50E L72 5 + OOE

L760E*Blk BLANK*Std MMISRM11 L76 50E L76 100E

L76 150E L76 200E L76 250E L76 300E L76 350E

L76 400E L76 450E L76 500E L76 550E L76 600E

MgMMI-D

100ppb

360370

109025402670

800200650

1000420

650710

18801150610

280'C 10018500

660700

760820380530240

360920700

5220740

TiMMI-D

1ppb

392

433612

400'Ci21

352

2856

4691866

<lOO0<l

2•CI

227

•ci866

*ci

CrMMI-D

1ppb

<l<l•CI'Ci•ci

•ci•ci•ci'Ci•ci

•ci<l<l<l<l'Ci<l<l<l<l•CI<l<l<l<l•CI<l<l<l<l

CoMMI-D

1ppb

1017

143

3•CI

410

1

6<l

8180

1

•ciO

2•Ci

8

26422

•ci27

•CI3

MiMMI-D

3ppb

5O2546

8

14•C3

1885

105

1913

8

O•C3

6•C3

12

54444

015434

RbMMI-D

1ppb

312375413

1937294737

2279334652

60•CI764420

4649533222

482646

233

SrMMI-D

0.1ppb

9.04.8

24.916.951.3

18.44.6

27.411.55.7

11.116.030.516.128.2

7.1-CO.l

27622.516.4

8.09.2

14.313.29.6

6.727.123.885.58.9

YMMI-D

0.1ppb

0.30.10.60.80.7

1.00.30.20.20.2

0.5•CO.l

0.90.40.3


0.1

0.2^.1

0.2•CO.*:0.

•CO.0.0.1.3

•CO.l

NbMMI-D

0.1ppb

•CO.l'CO.l

0.20.2

•CO.l

1.9•CO.l'CO.l^.1

0.3

1.3'CO.l

1.7•CO.l

0.2

'CO.l•cO.l'CO.l•CO.l•CO.l

•C0.1*C0.1•CO.•CO.^.

'CO.'CO.•CO.•CO.!•CO.l

PdMMI-D

0.1ppb

'CO.•CO.l'CO.l^.1•CO.l

^.1•CO.'CO.l•CO.l'CO.l

•CO.•CO.•CO.•CO.'CO.

•CO.l•CO.l'CO.l•CO.lo.•CO.l'CO.l'CO.l•CO.'CO.l

•CO.l'CO.l•CO.l•CO.l•CO.l

BaMMI-D

0.1ppb

223109200

66.592.1

79.1181108157

48.1

62.5145238125185

209-CO.l92.3168255

160251167252221

200280151

36.976.6

LaMMI-D

0.1ppb

0.40.20.71.40.8

1.10.30.20.20.3

0.5'CO.l

1.40.60.5

•CO.l•CO.l•CO.l'CO.l

0.2

0.20.10.5

•CO.l0.2

•CO.l0.30.23.70.1

TaMMI-D

0.5ppb

•CO. 5'CO. 5•CO. 5•CO. 5•CO. 5

•C0.5'CO. 5•CO. 5•CO. 5•C0.5

•C0.5•CO. 5•CO. 5•CO.S•CO. 5

•CO. 5'CO. 5•CO. 5<0.5<0.5

•CO. 5<0.5<0.5<0.5<0.5

•CO. 5<0.5<0.5<0.5<0.5

CeMMI-D

0.1ppb

1.40.41.22.91.3

2.00.90.40.30.5

1.00.22.31.80.6

•CO.l•CO.l"CO.l

0.10.3

0.60.31.00.10.3

•CO 10.50.34.40.2

PrMMI-D

0.1ppb

0.1•co.i

0.20.30.2

0.30.1

-CO.!^.1•CO.l

0.1•CO.l

0.30.20.1

•CO.l<0.1•CO.l<0.1<0.1

<0.1<0.1

0.2^.1<0.1

<0.1<0.1•CO.l

0.9<0.1

NdMMI-D

0.1ppb

0.50.20.71.20.8

1.10.50.20.20.3

0.5^.1

1.10.60.5

•CO.l'CO.l"CO.l•CO.l

0.2

0.30.20.6

"CO.l0.2

•CO.l0.20.23.30.1





L76 650E L76 700E L740 + OOE L740 + 50E L74 1+OOE

L74 1+50E L742 + OOE L742 + 50E L743 + OOE L743 + 50E

L744 + OOE L744 + 50E L745+OOE L745 + 50E L74 6+OOE

L730+OOE L730 + 50E L73 l +OOE L73 1+50E L732+OOE

L732 + 50E L73 3 + OOE L73 3 + 50E L734+OOE L734 + 50E

L73 5 H-GOE L73 5 + 50E L73 6+OOE*Dup L68 0 + OOE*DupL68 6 + OOE

MgMMI-D

100ppb

360450830330

1540

620250970900

2980

2630770320

2750510

2030730870

1090710

3960•C 1001650540

1950

1510590

5870920

2850

TiMMI-D

1ppb

1•ci34

25532

5923

4320169

352

•ci115

9

6969

964261

185

216834

84•a139*C1105

CrMMI-D

1ppb

OOOO•CI

•CI•ci•ci•cio•ci•ci•CI•ci•ci

•ci•ci<l<l<l•CI

2<l<\<l•CI<l<l<l<l

CoMMI-D

1ppb

1O

2'Ci

2

2124

•ci

9•CI•ci

44

21532

2•Ci

3•ci

7

4•Ci

6038

NiMMI-D

3ppb

4•C3•C3

313

14•C3

410

O

o•C30

6O

165

1264

10O15

•C323

16015

641

RbMMI-D

1ppb

2431552644

3244473630

2552333446

3356215743

2729341937

7456574236

SrMMI-D

0.1ppb

5.68.9

18.37.5

50.4

22.16.29.2

17.647.1

22268.237.463.910.0

73.625.817.118.618.2

77. 10.8

41.625.949.6

46.114.199.910.349.5

YMMI-D

0.1ppb

0.4^.1

0.30.40.2

0.20.40.21.31.7

0.7•CO.l•CO.l

1.20.2

0.4•CO.l

1.30.20.9

1.30.60.20.20.1

0.3•CO.l

1.3"CO.l

0.4

NbMMI-D

0.1ppb


0.90.1

0.3*C0.1•CO.l

1.20.6

0.1•CO.l•CO.l

0.4•CO.l

2.8•CO.l

0.40.10.2


0.20.1

0.3•CO.l

0.5•CO.l

0.4

PdMMI-D

0.1ppb

•CO.l•CO.l•CO.l•CO.l^.1


•CO.l*C0.1•CO.l•CO.l•CO.l

^.1•CO.l•CO.l•CO.l•CO.l


•CO.l•CO.l•CO.l*:0.l^.l

BaMMI-D

0.1ppb

101291216

60.2163

151182221

82.890.4

111221202224108

175148151

99.794.2

15212.1222

56.3218

195366

87.7218187

LaMMI-D

0.1ppb

0:6•CO.l

0.50.60.2

0.20.90.23.82.4

1.5•CO.l•CO.l

1.60.2

0.4•CO.l

2.10.21.1

3.32.00.20.30.2

0.5•CO.l

2.5•CO.l

0.4

TaMMI-D

O.Sppb

^.5•CO. 5•CO. 5•C0.5•CO. 5

•CO. 5•CO. 5•CO. 5•CO. 5•CO. 5

•CO.S•CO. 5^.5*C0.5^.5

^.5•CO. 5•C0.5•CO. 5•CO. 5

•CO. 5•CO. 5•CO. 5•CO. 5•CO. 5

•CO. 5•CO. 5•CO. 5•CO. 5•CO.S

CeMMI-D

0.1ppb

1.50.11.51.40.5

0.31.30.64.96.7

4.10.2

•CO.l2.70.4

0.70.24.00.62.5

2.54.00.40.70.4

0.80.14.4

•CO.l0.8

PTMMI-D

0.1ppb

0.3^.1

0.10.2

*C0.1

•CO.l0.3

^.10.70.8

0.5•CO.l*C0.1

0.5•CO.l

^.1•CO.l

0.5•CO.l

0.3

0.80.6


•CO.l•CO.l

0.7•CO.l

0.1

NdMMI-D

0.1ppb

0.9•CO.l

0.50.50.2

0.21.00.22.43.0

1.9•CO.l•CO.l

1.90.2

0.3•CO.l

2.00.21.3

2.92.20.20.30.2

0.3•CO.l

2.7•CO.l

0.4

® SGS Member of the SGS Group (Societe Generale de Surveillance)




*Dup L695 + 50E*Dup L72 l +OOE*Dup L76 150E*DupL740H-OOE*Blk BLANK

*Std MMISRM11*DupL746*OOE*DupL73 5 + 50E*Blk BLANK*StdMMISRMll

MgMMI-D

100ppb

1040240850950

000

20000560730

•C 10018700

TiMMI-D

1ppb

O0

132

•ci

•ci10

•ci<l<l

CrMMI-D

1ppb

•CI<l•CI<l<l<l<l<l<l•ci

CoMMI-D

1ppb

16O

23

<l

23

•CI•ci

2

NiMMI-D

3ppb

17•C3

5<3•C3

6<3

3•C3

6

RbMMI-D

1ppb

40394162

•ci

824259•n78

SrMMI-D

0.1ppb

28.85.38.5

19.9*:0.1

29310.415.6

•CO.l275

YMMI-D

0.1ppb

•CO.l0.20.10.3

•CO.l

•CO.l0.2

'CO.l'CO.l•CO.l

NbMMI-D

0.1ppb

*c0.1•CO.l^.1•CO.l'CO.l

*C0.1<0.1<0.1•CO.l•CO.l

PdMMI-D

0.1ppb

•CO.l•CO.l•CO.l•CO.l'CO.l


BaMMI-D

0.1ppb

327192154230

•CO.l

99.8103395

•CO.l94.6

LaMMI-D

0.1ppb

•CO.l0.30.20.4

•CO.l

•CO.l0.2


TaMMI-D

0.5ppb

•C0.5•CO. 5•CO. 5•CO. 5^.5

•:0.5<0.5^.5•CO. 5<0.5

CeMMI-D

0.1ppb

•CO.l0.80.61.6

^.1

•CO.l0.40.1

•CO.l•CO.l

PTMMI-D

0.1ppb

*C0.1•CO.l•CO.l

0.1*C0.1

<0.1<0.1<0.1<0.1•CO.I

NdMMI-D

0.1ppb

^.10.30.20.4

<0.1

^.10.2

<0.1<0.1<0.1

Member of the SGS Group (Societe Generate de Surveillance)




L680 + OOE L680 + 50E L68 1+OOE L68 1+50E L682 + OOE

L682 + 50E L68 3 + OOE L68 3 + 50E L68 4 + OOE L684 + 50E

L685 + OOE L685 + 50E L68 6+OOE L69 0+OOE L690 + 50E

L69 1+OOE L691+50E L692 + OOE L692 + 50E L69 3 + OOE

L693 + 50E L69 4+OOE L69 4 + 50E L695+OOE L695 + 50E

L69 6+OOE L696 + 50E L697+OOE L697 + 50E L698+OOE

SmMMI-D

0.1ppb


0.1•CO.l

0.20.1

•cO.l•cO.l•CO.l

^.1

0.2•CO.l•CO.l

0.10.2

•CO.l0.10.2

0.1•CO.l•CO.l

0.20.1

0.10.2

•CO.l0.10.2

Gd TlMMI-D MMI-I

0.1 0.ppb pp

•CO. •CO.•CO. "CO.•CO. •CO.•co. -CO.•CO. •CO.

<0. <0.<0. <0.•co. <o.<0. <0.<0. •CO.

<0. <0.

^o. ^o'.<0. <0.<0. <0.

<0.1 -CO.<0.1 <0.<0.1 <0.•CO.l •CO.

0.1 <0.

<0.1 •CO.<0.1 <0.<0.1 <0.•CO.l -CO.<0.1 <0.

<0.1 <0.0.1 <0.

<0.1 <0.•CO.l •CO.

0.1 <0.

j Er Yb) MMI-D MMI-D

0.1 0.1t) ppb ppb

•cO.l -co.l<0.1 -CO 1<0.1 *C0.1<0.1 <0.1<0.1 <0.1

•CO.l •CO.l<0.1 <0.1<0.1 •CO.l•CO 1 <0.1<0.1 "C 0.1

<0.1 <0.1 <0.1 <0.1•CO.l •CO.l•CO.l -CO.!

<0. -C0.1<0. <0.1<0. <0.1•CO. <0.1<0. <0.1

<0. •CO.l•CO. <0.1<0. <0.1•CO. <0.1<0.1 <0.1

<0.1 -CO.l<0.1 <0.1<0.1 <0.1•CO.l "CO.l<0.1 <0.1





L698 + 50E L699 + OOE L699 + 50E L69 10 + OOE L720 + OOE

L720 + 50E L72 1+OOE L72 1+50E L722 + OOE L722 + 50E

L72 3 + OOE L723 + 50E L724+OOE L72 4 + 50E L725 + OOE

L760E*Blk BLANK*StdMMISRMll L76 50E L76 100E

L76 150E L76 200E L76 250E L76 300E L76 350E

L76 400E L76 450E L76 500E L76 550E L76 600E

Sm MMI-D

0.1ppb

0.1"CO.l

0.20.30.2

0.20.2


0.1•CO.l

0.30.20.1


0.1

0.10.10.1

•CO.l•CO.l

•CO.l0.1

•CO.l0.6

•CO.l

Gd MMI-D

0.1ppb


0.20.2

0.2•CO 1•CO.l•CO.l•CO.l

•CO.l•CO.l

0.20.1

•CO.l




0.4•CO.l

Tb Er Yb MMI-D MMI-D MMI-D

0.1 0.1 0.1ppb ppb ppb

•CO.<0.•CO.•cO.•CO.

•CO.•cO.•cO.<0.•CO.

•CO.•cO.

<0.1 "CO.l<0.1 •COI<0.1 "CO<0.1 <0.•CO.l <0,

<0.1 0.<0. -CO.<0. <0.<0. <0.•CO. -CO.

•CO. •CO 1<0. -cO.l

•cO.l ^cO. -:0.1•cO.l <0. <0.1<0.1 ^. <0.1

<0.1 <0.1 <0.1•cO.l <0.1 <0.1<0.1 <0.1 -CO.l<0.1 <0.1 <0.1<0.1 •CO.l -CO.l

<0. <0.1 <0.1•CO. <0.1 <0.1<0. <0.1 "CO.l•CO. <0.1 <0.1<0. "CO.l -SO.I

<0.1 <0.1 <0.1•CO.l -CO.I <0.1<0.1 <0.1 -CO.l<0.1 <0.1 <0.1<0.1 •CO.l <0.1





L76 650E L76 700E L740+OOE L74 0 + 50E L74 l +OOE

L74 1+50E L742 + OOE L742 + 50E L743+OOE L743 + 50E

L744 + OOE L744 + 50E L745 + OOE L745 + 50E L746+OOE

L73 0+OOE L730 + 50E L73 l +OOE L73 1+50E L732 + OOE

L732 + 50E L73 3 + OOE L73 3 + 50E L734+OOE L734 + 50E

L73 5 + OOE L73 5 + 50E L73 6 4-GOE*Dup L68 0 + OOE*Dup L68 6 + OOE

SmMMI-D

0.1ppb

0.30.10.10.1

^.1

0.20.10.40.6

0.4•CO.l-CO.l

0.5

^.1<0.1

0.4•iO.l

0.3

0.50.40.1

S!0.10.10.5

*:0.l0.1

GdMMI-D

0.1ppb

0.2•cO.l^.1<0.1'COJ

0.1'CO.l

0.30.5

0.2*C0.1<0.1

0.3

.-0!<0.1

0.3•CO.l

0.2

0.40.3

•CO.l*S:1<0.1<0.1

0.4-CO.l<0.1

Tb ErMMI-D MMI-D

0.1 0.1ppb ppb

•CO. cCO.l<0. <0.1<0. 'CO.l<0. <0.1<0. <0.1

^S; H'l<0. <0.1<0. 0.1-CO. 0.2

^.1 <0.1^.1 <0.1<0.1 <0.1<0.1 0.1

^.1 <0.1<0.1 <0.1•CO.l 0.1<0.1 <0.1<0.1 0.1

^.1 0.<0.1 <0.^.1 <0.

<0.1 <0.

<0.1 -CO.*;o.i <o.<0.1 0.^.1 <0.<0.1 <0.

YbMMI-D

0.1ppb

•c 0.1<0.1<0.1<0.1<0.1

^J;|<0.1

0.10.2

•CO.<0.<0.

0.

•CO.<0.

0.<0.1•CO.l

<0.1<0.1<0.1

^S:!•C0.1<0.1

0.1<0.1<0.1





*DupL695H-50E*DupL72 1+OOE*DupL76 150E*DupL740-(-OOK*Blk BLANK

*Std MMISRM11*Dup L74 6+OOE*DupL73 5 + 50E*Blk BLANK*StdMMISRMll

Sm GdMMI-D MMI-D

0.1 0.1ppb ppb

TbMMI-D

0.1 ppb

Er YbMMI-D MMI-D

0.1 0.1ppb ppb

CO.l CO.0.2 CO.

CO. co.0. CO.

CO. CO.

CO. CO.CO. CO.

0. CO.CO.l CO.CO.l CO.

cO.l cO.lCO.l cO.lcO.l cO.lcO.l CO.lCO.l CO.l

CO 1 CO.lCO.l CO.lCO.l CO.lCO.l CO.l

CO.lCO.lCO.lcO.lCO.l

CO.lcO.lCO.lcO.l



1885 Leslie Street Don Mills, Ontario Canada M3B 3J4

To:

CERTIFICATE OF ANALYSIS Work Order: 066210

Temex Resources Corp. Attn: Duane ParnhamTemagami Exploration Company 4307 Kerry Drive, Unit 100 BURLINGTON ON/CANADA/L7L 1V8

Date 23/11/01

Copy 1 to

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

SOIL(MMI)11512/11/01Cover Sheet plusPages 1 to 10

Distribution of unused material: Pulps: Store Rejects: Store

Certified By

ISO 9002 REGISTERED

rGeneral Manager'C/

Subject to SGS General Terms and Conditions

Report Footer: L.N.R.n.a.*INF

= Listed not received l. S. = Insufficient Sample= Not applicable - = No result= Composition of this sample makes detection impossible by this method

M after a result denotes ppb to ppm conversion, 'fo denotes ppm to % conversion



Work Order: 066210 Date: 23/11/01 FINAL Page l of 10


L710E L71 50E L71 l GOE L71 150E L71 200E

L71 250E L71300E L71 350E L71 400E L71 450E

L71500E L700N L70 SON L70 100N L70 150N

L70 200N L70 250N L70 300N L70 350N L70 400N

L70 450N L70 SOON L70 550N L70600N L750E

L75 50E L75 100E L75 150E L75 200E L75 250E

MgMMI-D

100ppb

3330990

14101560350

26015903050

600410

480340550360220

340810

1990310350

1850520910

1060250

370610

7060510360

TiMMI-D

1ppb

75264

1134

275955582

-cio

3•ci•ci

•ci22

2•ci

5

116

70135

•CI6

7357

6

CrMMI-D

1ppb

43111

13433

222

•ci-ci

28227

1327

262

1-ci

7-ci

2

CoMMI-D

1ppb

42

•CI41

•CI6

1033

122

•Ci3

-ci2111

61971

•CI•ci

238

-ci

NiMMI-D

3ppb

843

04

O7765

516

584

84258

39

1966

125435

4

521271614

RbMMI-D

1ppb

1730242025

3223172838

4015121742

4133

•CI2330

1821384735

4446123730

SrMMI-D

0.1ppb

41.127.3135

36.419.9

17.452.147.1

8.18.1

11.69.9

12.63.41.5

5.210.751.0

5.614.0

38.711.830.028.5

7.6

4.839.932.618.512.7

YMMI-D

0.1ppb

1.00.3

-CO.l0.1

-CO.l

-cO.l0.20.20.50.4

^.1•CO.l"CO.l•CO.l•CO.l

•CO.l0.50.30.20.2

0.50.20.20.30.2

•CO.I•CO.l

0.90.40.2

NbMMI-D

0.1ppb

•CO.l0.6

-CO.l-CO.l•CO.l

"CO.l•CO.l•CO.l•CO.l•cO.l

•CO.l•CO.l•cO.l-CO.l^.1

•CO.l•CO.l-CO.l-CO.l^.1

•CO.l*co.l"CO.l•CO.l-CO.l

^.1-CO.l

0.2•CO.l^.1

PdMMI-D

0.1ppb

•CO.l-CO.l•CO.l•co.-CO.

•CO.•CO.•CO."CO.l•CO.l

•cO.l•CO.l•CO.l"CO.l•CO.l

-CO.l•CO.l•CO.•CO.l-cO.l

"CO.l-CO.l•CO.l•cO.l-CO.l

-CO."CO.^.•CO.-CO.

BaMMI-D

0.1ppb

132173405293339

232187184105

91.5

219116

64.2109

71.3

163109

65.8120227

412271328

90.3357

192328

49.895.0211

LaMMI-D

0.1ppb

2.60.6

•CO.l0.3

"CO.l

0.20.30.50.90.8

-CO.l-CO.l-CO.l•CO.I

0.4

-CO.l0.50.40.30.2

1.00.30.30.50.4

•CO.l•CO.l

3.21.60.6

TaMMI-D

0.5ppb

•C0.5•CO. 5•CO. 5^.5•C0.5

"C0.5•C0.5-C0.5^.5^.5

•C0.5•CO. 5-C0.5•CO. 5-CO. 5

-C0.5-CO. 5-CO. 5•C0.5•CO. 5

"CO. 5•C0.5•CO. 5•C0.5-CO. 5

•CO. 5•CO. 5-C0.5-C0.5-CO. 5

CeMMI-D

0.1ppb

5.81.2

"CO.l0.70.1

0.63.11.01.51.7

"CO.l-CO.l

0.20.10.5

•CO.l0.70.40.60.4

1.70.40.51.30.6

-CO.l0.2

10.82.00.8

PTMMI-D

0.1ppb

0.80.1

-CO.l*C0.1-co.i"CO.l-CO.l

0.10.20.2

-CO.l-CO.l•CO.l•CO.l•CO.l

^.10.2

•CO.l^.1•CO.l

0.2-CO.l•CO.l

0.1•CO.l

"CO.l•CO.l

0.80.40.1

NdMMI-D

0.1ppb

3.20.5

^.10.3

•CO.l

0.20.30.40.80.7

"CO.l•CO.l

0.1-CO.l

0.2

•CO.l0.60.40.30.2

1.00.30.20.60.4

•CO.l-CO.l

2.71.30.5





L75 300E L75 350E L75 400E L75 450E L75 500E

L75 550E L75 600E O 15 O 16 O 17

018 O 19 020 O 21022

023*Blk BLANK*StdMMISRMllO 24025

L800 + OOE L800 + 50E L80 1+OOE L80 1 + 50E L802 + OOE

L802 + 50E L803 + OOE L803 + 50E L804+OOE L804 + 50E

MgMMI-D

100ppb

3701100200300

14600

1120900

165001760014600

2000011500237002260013000

8730•c 1001400012100

870

1010880440620290

270380770320320

TiMMI-D

1ppb

3605

1320

3

1659

2•CI

2

226

•CI013

70•Ci•Ci•ci

2

8131

5•CI21

132

5452

CrMMI-D

1ppb

111

125

44244

95885

7•Ci

434

64434

33433

CoMMI-D

1ppb

•Ci6

•Ci2

O

2•ci

4•Ci•Ci

•ci•ci•ci•ci•a

4O

144

75

<l•Ci

2

•ci12

•ai

NiMMI-D

3ppb

481

71221

100

4OO

•C33

O0O

7•C3

558

1663

O4

074

O4

RbMMI-D

Ippb

464

2831

5

3235241118

35

•ci4

22

20•Ci671837

4327454517

3635213811

SrMMI-D

0.1ppb

26.67.87.97.8110

28.097.6

170177197

298114259278214

128•CO.l

230138

13.3

21.010.67.3

15.94.2

5.76.3

20.88.2

21.0

YMMI-D

0.1ppb

•CO.l1.30.10.30.1

0.20.20.1

•CO.l•CO.l

0.20.4

•CO.l*:0.1

0.1

0.3•CO.l•CO.l

0.20.1

0.70.40.20.10.2

0.20.10.20.10.1

NbMMI-D

0.1ppb

•co.l2.5



•CO.l•CO.l•CO.l•co.l•co.l•co.l•co.l•CO.l•CO.l•CO.l

•co.l•co.l•CO.l•co.l•CO.l

•CO.l•CO.l•CO.l•CO.l•co.l

PdMMI-D

0.1ppb


•CO.l•:o.i•CO.l•CO.l•co.l

•CO.l•co.l•co.l^.1•co.l

•co.l•co.l•CO.l•CO.l•CO.l


•:0.1•CO.l•CO.l•CO.l•CO.l

BaMMI-D

0.1ppb

12976.898.0322

93.4

176193115

91.3113

14061.986.0115162

109•CO.l98.591.6164

181101

87.2207144

127121

77.9157

77.6

LaMMI-D

0.1ppb

•CO.l4.50.20.40.2

0.30.30.20.20.2

0.31.0

•CO.l•CO.l

0.3

0.7•CO.l•CO.l

0.20.3

2.10.60.30.30.4

0.40.10.3

•CO.l0.2

TaMMI-D

0.5ppb

•CO. 5^.5^.5^.5•CO. 5

^.5•CO. 5•CO. 5•CO. 5•CO. 5

^.5^.5^.5•CO. 5•CO. 5

•CO. 5•C0.5•CO. 5•CO. 5^.5

•CO. 5•CO. 5•CO. 5•CO. 5•CO. 5

•C0.5•CO. 5•CO. 5•C0.5^.5

CeMMI-D

0.1ppb

0.29.30.40.80.3

0.50.90.40.40.3

0.51.7

•CO.l0.10.8

1.9*C0.1•CO.l

0.40.4

7.11.40.80.60.9

0.80.30.70.30.5

PrMMI-D

0.1PPb

•CO.l1.0

^.10.1

•CO.l

^.1•CO.l•co.l•CO.l•CO.l

•co.l0.2

•co.l•CO.l•co.l

0.2•CO.l•CO.l•CO.l^.1

0.50.2

•co.l•CO.l•co.l•CO.l^.1*:0.1•CO.l•CO.l

NdMMI-D

0.1ppb

•CO.l3.70.20.40.2

0.30.20.20.20.1

0.30.9

•CO.l•CO.l

0.3

0.7•CO.l•CO.l

0.30.2

1.70.60.40.30.3

0.30.20.30.10.2





L805 + OOE L780+OOE L780 + 50E L78 1+OOE L78 1+50E

L782 + OOE L782 + 50E L78 3+OOE L78 3 + 50E L784 + OOE

L78 4 + 50E L785 + OOE L785 + 50E L78 6+OOE L78 6 + 50E

L787 + OOE L790E L79 50E L79 l GOE L79 150E

L79 200E L79 250E L79 300E L79 350E L79 400E

L79 450E L79 500E L79 550E L79 600E L770E

MgMMI-D

100ppb

2503350

350370790

10200380

492044204350

361044605070

540340

540520

1100280

1430

190230330180220

280260690370

6260

TiMMI-D

1ppb

•ci13

•ci<\24

3643

631

12

•ci3

15

389

174O54

62

315

0

•ci7

1012

<l

CrMMI-D

1ppb

33245

87533

33235

44825

44432

34342

CoMMI-D

1ppb

14

•ci22

•ci2

•ci•ci•ci•ci•ci•ci

41

54316

2•Ci

6•Ci•Ci

1•ci

1•ci•ci

NiMMI-D

3ppb

15104

144

44

•C3•C30

Ooo

65

14734

19

O673

•C3

O3

OO

6

RbMMI-D

1ppb

283111

g24

3127

241

113

2753

28372041

7

1943283179

40472556

1

SrMMI-D

0.1ppb

7.756.65.9

11.127.9

75.98.2

51.764.669.3

60.248.953.214.312.2

15.911.723.09.4

91.0

4.65.19.05.16.6

7.55.3

16.413.538.7

YMMI-D

0.1ppb

•CO.l0.2

•CO.l•CO.l

0.2

0.30.20.3

^.1•CO.l


0.3

0.20.20.8

•CO.l0.3

0.10.20.30.2

•CO.l

•CO.l0.10.30.2

CO.l

NbMMI-D

0.1ppb


•CO.l^.1•CO.l•CO.l•CO.l

•CO.l•CO.l•cO.l•CO.l•CO.l

•CO.l•CO.l

0.2•CO.l^.1

•CO.lCO.l•CO.l•CO.l•CO.l

•CO.l•CO.lCO.l•CO.l•CO.l

PdMMI-D

0.1ppb

•CO.l•CO.l•CO.l•CO.l*c0.1


•CO.l•CO.l•CO.lCO.lCO.l



•CO.l•CO.lCO.lCO.l•CO.l

BaMMI-D

0.1ppb

202183155

67.299.3

56.9198

23.422.717.6

14.012.614.189.790.1

149105

78.6301

72.7

86.6148113

73.187.5

122176

94.0182

12.0

LaMMI-D

0.1ppb

CO.l0.2

•CO.l•CO.l

0.4

0.70.30.60.2

•CO.l


0.4

0.20.32.1

•CO.l0.4

0.20.20.40.2

•CO.l

CO.l0.20.60.3

•CO.l

TaMMI-D

0.5ppb

•CO. 5CO. 5CO. 5•CO. 5•CO. 5

•CO. 5•CO. 5•CO. 5•CO. 5•CO. 5

•CO. 5•CO. 5•CO. 5C0.5CO. 5

•CO. 5•CO. 5•CO. 5C0.5•CO. 5

•CO. 5CO. 5•CO. 5•CO. 5CO. 5

•CO. 5•CO. 5•CO. 5•CO. 5•C0.5

CeMMI-D

0.1ppb

^.10.7

•CO.l0.11.0

1.42.40.70.1

•CO.l

CO.l•CO.l•CO.lCO.l

1.0

0.60.96.1

•CO.l0.6

0.60.61.10.5

•CO.l

•CO.l0.50.81.9

•CO.l

PTMMI-D

0.1ppb

^.1•CO.l^.1•CO.I

0.1

0.2•CO.l

0.2^.1•CO.l

^.1^.1^.1•CO.l

0.1

•CO.l•CO.l

0.6^.1*C0.1

^.1•CO.l

0.1•CO.l^.1

•CO.l•co.i

0.2^.1•CO.l

NdMMI-D

0.1ppb

•CO.l0.2

•CO.l•CO.l

0.4

0.70.30.70.1

"CO.l


0.4

0.20.32.1

•CO.l0.4

0.20.30.50.3

•CO.l

•CO.l0.30.70.3

•CO.l





L77 50E L77 l GOE L77 150E L77 200E*Blk BLANK

*Std MMISRM11 L77 250E L77 300E L77 350E L77 400E

L820 + OOE L820 + 50E L82 1+OOE L82 1+50E L822+OOE

L822 + 50E L82 3+OOE L823 + 50E L824 + OOE L81 0 + OOE

LSI 0 + 50E L81 1+OOE LSI 1 + 50E LSI 2+OOE L81 2 + 50E

LSI 3+OOE LSI 3 + 50E L81 4+OOE LSI 4 + 50E*Dup L71 OE

MgMMI-D

100ppb

9130853064909170c loo

15400660

1750570

5460

2301540750200470

95016104900

810240

100190230190180

430290

1170260

3460

TiMMI-D

1ppb

3427

O

-Ci103969

388

ci457•CI

3215

4018

32382

415

368496O4570

99711

826

85

CrMMI-D

1ppb

2333

<l

4557

30

39434

44

1363

46135

74335

CoMMI-D

1ppb

•cicici•cici

1442

10

ci2

CI•ci•ci

1111

•CI

•ci•CIci•cioCI

13

ci4

MiMMI-D

3ppb

4c3c3C3C3

5853

29

O42

5C3

7

6C3

47

C3

c3C3O0

4

47

11C3

9

RbMMI-D

1ppb

2342

•ci

7218154910

4661492315

29303370

9

927326362

435

746216

SrMMI-D

0.1ppb

56.265.160.890.3

•CO.l

24819.330.013.842.3

17.345.315.86.6

29.2

56.290.370.616.67.1

3.23.23.85.18.6

5.317.718.35.0

39.6

YMMI-D

0.1ppb

•CO.lCO.l•CO.l•CO.lCO.l

•CO.l0.50.20.62.0

•CO.l0.4

CO.l0.20.2

0.1•CO.l

0.40.20.2

0.40.4

CO.l0.20.3

0.10.20.2

CO.l1.1

NbMMI-D

0.1ppb

•CO.•CO.•CO.•CO.•CO.

•CO.•co.•CO.•CO.

1.8

co.l1.7

CO.lCO.l

0.8

•CO.l•CO.l

0.90.20.9

0.61.4


0.11.9

•CO.l•CO.lCO.l

PdMMI-D

0.1ppb



•CO.lCO.l•CO.l•CO.lCO.l



•CO.l•CO.l•CO.lCO.l•CO.l

BaMMI-D

0.1ppb

12.817.522.612.6

•CO.l

97.8167263167159

100361139

83.595.0

182102

54.0149

24.9

11.215.1161

66.974.1

30.666.977.242.4119

LaMMI-D

0.1ppb

•CO.•CO.•cO.

0.•CO.

•CO.l1.40.31.27.8

0.20.7

CO.l0.70.3

0.2CO.l

0.60.50.2

0.80.6

•CO.l0.41.0

0.30.30.5

CO.l2.6

TaMMI-D

0.5ppb

•CO. 5•CO. 5•CO. 5•CO. 5•CO. 5

•CO. 5•CO. 5•CO. 5•CO. 5•CO. 5

•CO. 5CO. 5C0.5C0.5•CO. 5

C0.5•CO. 5•CO. 5•CO. 5•CO. 5

•CO. 5•CO. 5•CO. 5•CO. 5CO. 5

CO. 5•CO. 5C0.5<0.5<0.5

CeMMI-D

0.1ppb


0.2CO.l

•CO.l3.01.0

10.117.3

0.31.2

•CO.l1.70.7

0.40.11.20.50.6

1.11.10.10.82.1

0.70.61.20.16.2

PrMMI-D

0.1ppb

•CO.l•CO.lCO.lCO.lCO.l

CO.l0.4

CO.l0.31.9

CO.l0.2

CO.l0.2

CO.l

CO.lCO.l

0.2CO.lCO.l

0.20.1

CO.l0.10.2

CO.lCO.l

0.2CO.l

0.9

NdMMI-D

0.1ppb

CO.lCO.lCO.lCO.lCO.l

CO.l1.50.31.37.3

0.20.5

CO.l0.90.2

0.1CO.l

0.60.30.2

0.60.5

CO.l0.51.0

0.40.30.5

CO.l3.5

Member of the SGS Group (SocietS Generate de Surveillance)




*Dup L70 SON*Dup L75 OE*Dup L75 600E*DupL800 + OOE*DupL78

*DupL78 6 + 50E*Dup L79 500E*DupL82(HOOE*DupL81 1+50E*Blk BLANK

*StdMMISRMll

Mg Ti Cr Co Ni RbMMI-D MMI-D MMI-D MMI-D MMI-D MMI-D

100ppb

610260970830260

380280290210

C 100

14700

1ppb

46

7194

Ci

189

CIC 1<l

Ci

1ppb

33472

6432

CI

5

1ppb

21

< l6

ci

1CIci

1ci

1

3ppb

4c3c3

13C3

5c3C3C3C3

5

1ppb

1337364010

58484632

C 1

71

SrMMI-D

0.1ppb

12.87.8105

19.57.1

12.45.4

17.43.3

CO.l

241

YMMI-D

0.1ppb

CO.l0.20.20.8

CO.l

0.30.1

cO.lCO.lCO.l

CO.l

NbMMI-D

0.1ppb

CO.lCO.lCO.lco.lCO.l


CO.l

Pd BaMMI-D MMI-D

0.1 0.1ppb ppb

CO.l 59.1CO.CO.COCO.

CO.co.CO.

326188171166

96.0175

92.8CO.l 156CO.l CO.l

CO.l 94.5

LaMMI-D

0.1ppb

CO.l0.30.32.3

CO.l

0.40.20.1

CO.lCO.l

CO.l

TaMMI-D

0.5ppb

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

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

CO. 5

CeMMI-D

0.1ppb

0.20.61.07.5

CO.l

1.20.50.3

CO.lCO.l

CO.l

PTMMI-D

0.1ppb

CO.lCO.lCO.l

0.5CO.l

0.1CO.lCO.lCO.lCO.l

CO.l

NdMMI-D

0.1ppb

CO.l0.40.32.1

CO.l

0.50.30.1

CO.lCO.l

CO.l





L71 OE L71 50E L71 100E Lil 150E L71 200E

L71 250E L71 300E L71 350E L71 400E L71 450E

L71500E L700N L70 SON L70 l DON L70 150N

L70 200N L70 250N L70 300N L70 350N L70 400N

L70 450N L70 500N L70 550N L70 600N L750E

L75 50E L75 100E L75 150E L75 200E L75 250E

Sin CdMMI-D MMI-D

0.1 0.1ppb ppb

0.6 0.1

0.2•CO. l

0.1 0.1 0.1 0.2 0.2

•CO.l

0.2

•CO. l

0.3

0.1 0.2 0.2

•CO.l

0.5 0.2 0.1

0.5

•co.i

0.2 0.1

•CO. l

0.1

0.1

0.1 •iO.l

0.40.2

•CO.l

TbMMI-D

0.1 ppb

Er YbMMI-D MMI-D

0.1 0.1ppb ppb

0.1•CO.l•CO.l

•CO.l

•CO.l

-CO.l

•CO.l

•CO.l•CO.l

•CO.l





L75 300E L75 350E L75 400E L75 450E L75 500E

L75 550E L75 600E O 15 O 16 017

O 18 O 19 O 20021022

023*Blk BLANK*StdMMISRMll O 24 O 25

L800+OOE L800 + 50E L80 1+OOE L80 1+50E L802 + OOE

L802 + 50E L803+OOE L803 + 50E L804+OOE L804 + 50E

Sm GMMI-D MMI-I

0.1 0.ppb pp

•CO.l •CO.0.6 0.'

•CO.l -CO.0.2 •CO.

•CO.l -CO.

•CO.l <0.0.1 -CO.

•CO.l -CO.•CO.l •CO.•CO.l -CO.

•CO.l •CO.0.2 0.

•CO.l *CO.<0.1 -CO.<0.1 <0.

0.2 <0.•CO.l -CO.<0.1 <0.<0.1 -CO.<0.1 <0.

0.4 o.:0.1 -CO.

•CO.l -CO.<0.1 -CO.

0.1 <0.

<0.1 <0.

^.1 <0.<0.1 <0.<0.1 *CO.

J Tb) MMI-D1 0.1) ppb

<0.1l <0.1

<0.1<0.1<0.1

•C0.1<0.1<0.1<0.1* 0 - 1•CO.l•CO.l•CO.l•CO.l•co.l•CO.l•CO.l•CO.l

l •CO.ll .CO.l

! -CO.I[ ^.1L <0.1

<0.11 .CO.l

•co.l1 <0.11 .CO.l1 <0.1

ErMMI-D

0.1ppb

.CO.l0.2




•CO.l•CO.l•CO.l•CO.l10.1

•CO.l•CO.l•CO.l.CO.l.CO.l

•CO.l

.CO.l•CO.l•CO.l

YbMMI-D

0.1ppb

•CO.l0.2

•CO.l•CO 1.CO.l


•CO.l•CO.l•CO.<0.•CO.

<0.<0.<0.<0.•CO.

<0.1<0.1<0.1<0.1•CO.l

•CO.l

^o!i<0.1<0.1





L805 + OOE L780 + OOE L780 + 50E L78 l +OOE L78 1+50E

L782+OOE L782 + 50E L78 3 4-GOE L783 + 50E L784+OOE

L784 + 50E L785+OOE L785 + 50E L78 6+OOE L78 6 + 50E

L78 7+OOE L790E L79 50E L79 l GOE L79 150E

L79 200E L79 250E L79 300E L79 350E L79 400E

L79 450E L79 500E L79 550E L79600E L770E

SmMMI-D

0.1ppb

CO.lCO.lCO.lCO.l

0.1

0.1CO.l

0.1CO.lCO.l

CO.lCO.lCO.lCO.l

0.1

CO.lCO.l

0.4CO.lCO.l

CO.l0.10.1

CO.lCO.l

CO.lCO.l

0.20.1

CO.l

Gd TbMMI-D MMI-D

0.1 0.1ppb ppb

cO.l CO.lCO.l CO.lcO.l cO.lCO.l CO.lCO.l CO.l

CO.l cO.lCO.l CO.lCO.l CO.lco.i •cO.lCO.l CO.l

CO.l CO.lcO.l CO.lcO.l cO.lCO.l CO.lCO.l CO.l

CO.l CO.lCO.l cO.l

0.2 cO.lCO.l CO.lCO.l CO.l

CO.l CO.lcO.l cO.lCO.l CO.lCO.l CO.lCO.l CO.l

CO.l CO.lcO.l CO.lco.i co.iCO.l CO.lcO.l CO.l

ErMMI-D

0.1ppb

cO.lCO.lcO.lCO.lCO.l

CO.lCO.lcO.l•CO.lCO.l

CO.lCO.lcO.lcO.lCO.l

CO.lcO.l

0.1CO.lCO.l

CO.lCO.lcO.lcO.lCO.l

CO.lCO.lCO.lCO.lco.i

YbMMI-D

0.1ppb




cO.lCO.lCO.lCO.lCO.l

CO.lCO.lcO.lCO.lCO.l

CO.lCO.lco.iCO.lCO.l





L77 50E L77 100E L77 150E L77 200E*Blk BLANK

*Std MMISRM11 L77 250E L77 300E L77 350E L77 400E

L82 O H-GOE L820 + 50E L82 1+OOE L82 1+50E L822 + OOE

L822 + 50E L823+OOE L823 + 50E L824 + OOE L81 0+OOE

LSI 0 + 50E L81 1+OOE L81 1 + 50E LSI 2+OOE L81 2 + 50E

LSI 3 + OOE LSI 3+50E LSI 4+OOE LSI 4 + 50E*Dup L71 OE

SmMMI-D

0.1ppb

•CO.l•CO.l•CO.lCO.l•CO.l

CO.l0.30.10.31.3

•CO.l0.2

cO.l0.2

•CO.l

•cO.l•CO.l

0.1•CO.l•CO.l

0.1•CO.lCO.l

0.10.2

CO.l•CO.l

0.1•cO.l

0.7

GdMMI-D

0.1ppb

•CO.l•cO.l•CO.l•CO.I•CO.l

•CO.l0.2

•cO.l0.20.9

•CO.l0.1

•CO.l0.1

•CO.l

•CO.lCO.l

0.1•CO.l•cO.l

0.1•CO.l•CO.l•CO.l

0.2

CO.lCO.lCO.l•CO.l

0.5

Tb ErMMI-D MMI-D

0.1 0.1ppb ppb

cO.l •CO.cO.l •CO.cO.l -CO.CO.l •CO.•CO.l CO.

•CO.l cO.l•CO.l CO.l•CO.l CO.lCO.l CO.l

0.1 0.3

CO.l cO.lcO.l cO.lCO.l cO.lCO.l cO.lCO.l CO.l

CO.l CO.lcO.l cO.lCO.l CO.lCO.l cO.lCO.l CO.l

cO.l cO.lCO.l CO.lCO.l CO.lCO.l cO.lCO.l CO.l

CO.l cO.lCO.l •CO.lco.i co.iCO.l CO.lco.i o.i

YbMMI-D

0.1ppb

CO.lCO.lCO.lcO.lCO.l

cO.lco.iCO.lCO.l

0.2




CO.lCO.lCO.lCO.l

0.1





*Dup L70 SON*Dup L75 OE*Dup L75 600E*Dup L80 0 + OOE*DupL7804-50E

*DupL786 + 50E*Dup L79 500E*DupL82 0+OOE*DupL81 1+50E*Blk BLANK

*StdMMISRMll

Sin CdMMI-D MMI-D

0.1 0.1ppb ppb

0.2 0.1 0.5

0.20.1

•CO. l

TbMMI-D

0.1 ppb

•CO. l•CO. l <0.

0.3

0.1

•CO. l

Er YbMMI-D MMI-D

0.1 0.1ppb ppb

•CO. l

0.1

•CO. l

•CO.l


APPENDIX C

MMI SOIL SAMPLE DESCRIPTIONS

Mobile Metal loo Soil Survey, Keating Anomaly Follow-up

L70. 0+OON to 6+OON. Chambers Tp.. Claim 1203045Station

0+OON

0+50N1+OON

1+50N

2+OON

2+50E

3+OOE

3+50E

4+OOE4+50E5+OOE

5+50E

6+OOE

Easting

582413

582399582387

582336

582338

582312

582287

582270

582253582235582204

582180

582167

Northing

5218261

52182975218323

5218392

5218420

5218470

5218524

5218588

5218617521B6625218712

5218749

5218801

Surface slope 0Expression

undulatingflatflatundulating

ridged north 20

apronundulatingapron north 4undulatingundulatingflatundulatingflatundulating north 2undulating south 1undulating south 1

undulating west 5

ridged

Drainage

well

wellwell

well

well

well

poor

moderate

wellwellwell

well

well

Vegetation

mixed conifer

conifermixed conifer

conifer

conifer

conifer

bog, spruce

conifer

coniferconifermixed conifer

mixed conifer

conifer

Horizon

B

BB

B

B

B

Ao

B

BBB

B

B

MaterialThickness

3

33

1A

1A

3

3

3

331A

3

1A

Colour

medium-brown

orange-brownmedium-brown

orange-brown

medium-brown

dark-brown

black

medium-brown

medium-brownmedium-brownmedium-brown

pale-brown

pale-brown

Texture

sand

sandsand

sand

sand

sand

organic

sand

sandsandsand

sand

sand

Clast

few pebblesfew cobblesfew pebblesfew pebblesfew cobblesfew pebblesfew cobblesfew pebblesfew cobblesfew pebblesfew cobbles

few cobbles

few pebblescommon cobblesfew pebblesfew cobblesfew pebblesfew cobblesfew pebblesfew cobbles

Remarks

till, top of broad hill

till, top of broad hilltill, top of broad hill

till, top of ridge

till

till.

forest litter

till

tilltilltill

till

till, sedimentary outcrop

L71. 0+OOE to 5+OOE. Chambers Tp.. Claim 1203045Station

0+OOE0+50E

1+OOE

Easting

582550582579

Northing

52186485218656

Surface slope 'Expression

undulating west 3undulatingflatundulatingflat

Drainage

wellwell

well

Vegetation

coniferconifer

conifer

Horizon

BB/A

B/A

MaterialThickness

33

3

Colour

medium-browngray-brown

medium-brown

Texture

sandsand

sand

Clast

common pebblesfew pebbles

common pebblesfew cobbles

Remarks

till, start of linetill, reforested, disturbed.off-line stationtill, reforested, disturbed

Temex Resources Corporation, Wilson Lake Diamond Project

Mobile Metal ton Soil Survey, Keating Anomaly Follow-up

L71. 0+OOE to 5+OOE. Chambers Tp.. Claim 1203045 continuedStation

1+50E

2+OOE

2+50E3-t-OOE

3+50E4+OOE

4+50E

5+OOE

Easting Northing SurfaceExpressionundulatingflatundulatingflatundulatingundulatingflatundulating

582956 5218633 undulating

undulating

583045 5218649 undulatingflat

L72. 0+OOE to 5+OOE. Chambers Tp.. ClaimStation

0+OOE

0+50E

1+OOE

1+50E

2+OOE

2+50E

Easting Northing SurfaceExpression

580040 5219409 levelridged

steepridgedveneerinclinedblanketridgedinclinedblanketridgedinclinedblanketridgedsteeptread

slope "

east 2

east 2north

north 2

1203044slope "

west 40

west 35

wests

west 25

north 45

Drainage

poor

well

wellwell

wellmoderate

moderate

well

Drainage

poor

well

well

well

well

well

Vegetation

conifer

conifer

coniferconifer

mixed conifermixed conifer

conifer

mixed deciduous

Vegetation

scrub

conifer

mixed conifer

scrub, mix

coniferscrub deciduous

conifer

Horizon

B/A

B/A

B/AB/A

BB

B

B

Horizon

Ao

B

B

B

B

B

MaterialThickness

3

3

33

1A1A

3

3

MaterialThickness

3

1

2

2

2

1A

Colour

pale-brown

orange-brown

pale-browngrayish-brown

pale-brownmedium-brown

medium-brown

orange-brown

Colour

black

gray-brown

orange-brown

gray-brown

dark brown

orange- brown

Texture

sand

sand

sandsand

sandsand

silly-sand

sand

Texture

organic

silly-sand

silly-sand

sitty-sand

silty-sand

silly-sand

Clast

few pebblesfew cobblesfew pebbles

common pebblefew pebble

few pebblefew pebblesfew cobblesfew pebblesfew cobblesfew pebblesfew cobbles

Clast

few pebbles

common pebblefew cobblesfew bouldersrare pebble

few pebbles

common pebblecommon cobble

Remarks

till, reforested, disturbed

till, reforested, disturbed

till, reforested, disturbedtill, reforested, disturbed

tilltill, off-line

till

till

Remarks

forest litter, N-S linear depressiontalus filledgranite-sedimentary contact.colluvium from weatheredgranite outcrop, talus blocks

till, granite outcropupland

till, granite outcrop uplandboulder erratic on surfacetill, talus blocks, adjacent toN-S granite outcrop ridge

till pocket, granite outcropupland, pink coarse-grained


Mobile Metal Ion Soil Survey, Kenting Anomaly Follow-up

L72. 0+OOE to 5+OOE. Chambers Tp.. Claim 1203044 continued3+OOE

3+50E

4+OOE

4+50E

5+OOE

ridgedsteepveneerridgeinclinedblanketapronridgeinclinedblanketinclinedblanket

580500 5219399 inclinedblanket

L73. 0+OOE to 6+OOE. Chambers TD.. ClaimStation

0+OOE

0+50E

1+OOE

1+50E

2+OOE


580347 5219444 apronblanketinclinedinclinedblanketapronveneerridgedtreadtreadinclinedblanketridgedaproninclinedblanket

north 45

west 15

west 25

north-west15

north 20

1203044slope "

north-west15

north-west10

north-east6

north 20

north 15

well mix conifer

well scrub deciduous

well mix conifer

poor scrub deciduous

well scrub mix

Drainage Vegetation

well scrub mix

well scrub deciduous

moderate scrub mixdeciduous

well scrub conifer

moderate scrub coniferrunoff

B 1A gray-brown

B 2 orange-brown

B 2 yellow-brown

A 1A dark-brown toblack

B 2 orange-brown

Horizon Material ColourThickness

B 2 gray-brown

B 2 orange-brown

B 1A gray-brownto black

B 2 orange-brown

B 3 orange-brown

clayey-silty-sand

silly-sand

silty-sand

sand withorganicsilty-sand

Texture

silty-sand

silty-sand

silty-sand

silty-sand

silty-sand

few pebble

common pebblecommon cobblecommon boulder

few pebblefew cobble

few pebblefew cobble

Clast

few pebble

abundant pebbleabundant cobbleabundant boulder

abundant pebbleabundant cobbleabundant boulder

till in pocket in talus blocks.at base of granite outcrop upland

till, talus blocks, granite outcrop ridge east of station

till, boulder lag

organic layer in old logging road, disturbed, boulder in hole till, erratic sedimentary boulder on surface, whalesback granite outcrop knob

Remarks

till, nearby granite outcrop knob

glacial deposits, nearby graniteoutcroptill, overlying talus blocksfrom nearby granite outcropupland

till, granite upland

glacial deposit, boulder erratic, base of granite upland


Mobile Metal Ion Soil Survey, Keating Anomaly Follow-up

L73. 0+OOE to 6+OOE. Chambers Tp.. Claim 1203044 continued2+50E

3+OOE

3+50E

4+OOE

4+50E

5+OOE

5+50E

6+OOE

aproninclinedblanketaproninclinedblanketlevel

580749 5219458 inclinedsteepridged



580910 5219473 inclinedblankethummocky


L74. 0+OOE to 6+OOE. Chambers TD.. ClaimStation

0+OOE

0+50E

HOOE

1+50E


580949 4219525 inclinedblanketinclinedveneertreadridged

581049 5219517 inclinedblanketinclinedblankethummocky

north-west8

wests

north 45

north-west15

south 15

south 15

south 15

1203044slope "

south-east15

easts

west 20

north-west15

poorrunoff

poorrunoff

well

well

well

well

well

moderaterunoff

Drainage

well

moderaterunoff

well

well

scrub mudeciduous

scrub mixdeciduous

scrub mixdeciduous

scrub mixdeciduous

conifer

scrub mixdeciduousscrub mixdeciduous

scrub mixconifers

Vegetation

scrub mixdeciduousconifer

scrub decidi

scrub mixdeciduous

A-B 3 orange-brown silty-sand to brown-black with

organic B 2/1A yellow-brown silty-sand

B 3/2/01 orange-brown silty-sand

B 3 orange-brown silty-sand

B 2 orange-brown sitty-sand


B 2 yellow-brown silty-sand

B 2 gray-brown silty-sand

Horizon Material Colour Texture Thickness

B 2 yellow-brown silty-sand

B 1A gray-brown sand

B 2/3/01 orange-brown silty-sand


abundant pebble abundant cobble abundant boulder abundant pebble abundant cobble abundant boulder abundant pebble abundant cobble abundant boulder abundant pebble abundant cobble abundant boulder few pebble

few pebble

few pebble

few pebble

Clast

few pebble

few pebble

few pebble few cobble few pebble few cobble few boulder

glacial deposit, gravel pit area, disturbed

glacial deposit, gravel pit area, disturbed

glacial deposit, undisturbed, granite outcrop

glacial deposit, disturbed

till, granite erratic, granite outcrop to north, gravel pit area till, logged area

till, logged area, granite outcrop knobs

till, granite erratic

Remarks

till, granite erratic, granite outcrop to north glacial deposit, granite outcrop lowest

till. 10 m outcrop granite ridge

till, logged area


Mntfil Inn Soil Survey, Knntmg Anomaly Follow-up

L74. 0+OOE to 6+OOE. Chambers Tp.. Claim 1203044 continued2+OOE

2+50E3+OOE

3+50E

4+OOE4+50E5+OOE

5+50E

6+OOE

581197581252

52195135219523

inclinedblankethummockyinclinedinclinedsteepridgedundulating

undulatingundulatingundulatinglevelundulating

undulatingblanket

L75. 0+OOE to 6+OOE. Chambers Tp.. Claim

Station

0+OOE0+50E

1+OOE1+50E

2+OOE2+50E3+OOE3+50E4+OOE4+50E

5+OOE

Easting

581200581217

581241581279

581356581386581413581479581514581554

581582

Northing

52201775220184

52202045220235

522028552203135220334522037652204215220435

5220472

SurfaceExpression

undulatingundulating

undulatingundulatingflatundulatingundulatingundulatingundulatingundulatingundulatingflatflat

L75. 0+OOE to 6+OOE. Chambers TD.. Claim5+50E

6+OOE

581604

581655

5220487

5220524

undulating

undulating

north 15

north 20north-east

35

west 3

west3east 2

south-east2

east3

1203044

slope "

southeast

west

south-westwestsoutheasteast

moderate scrub mnrunoff deciduous

well coniferwell scrub mix

deciduous

moderate scrub mixdeciduous

moderate coniferwell coniferwell conifer

well mix deciduous

moderate mix conifer

Drainage Vegetation

well mixed coniferwell conifer

well mixed coniferpoor bog. alder

poor deciduouswell scrub-deciduouswell scrub-deciduous

moderate mixed deciduouswell mixed deciduouswell mixed deciduous

poor bogmixed conifer

B

BB

B

BA/BA/B

A/B

B

Horizon

BB

BB

BBBBBB

B

2

22

3

333

3

3

MaterialThickness

31A

1A3

333

1A33

3

orange-brown

orange-browngray-brown

medium-brown

gray-brownmedium-brownpale-brown

medium-brown

medium-brown

Colour

orange-brownpale-brown

medium-brownbrown

brownyellow-brownmedium-browngray-brownorange-brownpale-brown

gray

silty-sand

silty-sandsilty-sand

silty-sahd

silty-sandsandsand

sand

sand

Texture

sandsand

sandsandgravelclayey-sandsandsandsilty-sandsandsand

clayey-sand

few pebble

few pebblecommon pebblecommon cobblecommon boulderrare pebblecommon cobblecommon pebblecommon pebblecommon pebble

common pebble

common pebble

Clast

few pebblefew pebblesfew cobblesfew pebblefew pebblefew pebblesfew cobblesfew pebblesfew pebblesfew pebblesfew pebblesfew pebbles

few pebbles

till, granite erratic

till, granite uplandtill, slope creep

till, adjacent to old loggingroadtilltill, reforestedtill, reforested

till

till

Remarks

till, ridge toptill pocket, ridge top

tilltilltill

tilltilltilltilltill, claim line

till

1203044 continuedsouth

east

well mixed conifer

well mixed deciduous

B

B

1A

3

dark-brown

medium-brown

sand

sand

few pebblesfew cobblescommon pebbles

till

till


ONTARIO MINISTRY OF NORTHERN DEVELOPMENT AND MINES

Transaction No:

Recording Date:

Approval Date:

Client(s):303055

Survey Type(s):

W0270.00147

2002-JAN-25

2002-JAN-29

Work Report Summary

Status: APPROVED

Work Done from: 2001-NOV-01

to: 2001-NOV-03

TEMEX RESOURCES LTD.

BENEF

Work Report Details:

Claim*

S 1203044

S 1203045

Perform

34,325

31,766

36,091

Perform Approve

34,325

31,766

36,091

Applied

34,800

31,291

36,091

Applied Approve

34,800

31,291

36,091

Assign

303475

3475

Assign Reserve Approve Reserve Approve Due Date

0

475

3475

SO

SO

SO

SO 2004-OCT-05

SO 2003-OCT-05

SO

Status of claim is based on information currently on record.

31M04NW2020 2.22840 CHAMBERS 900

2002-Feb-22 14:01 Armstrong_d Page 1 of 1

Ministry ofNorthern Developmentand Mines

Date: 2002-FEB-21

Ministere du Developpement du Nord et des Mines Ontario

GEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E6B5

TEMEX RESOURCES LTD. 4307 KERRY DRIVE, SUITE 100 BURLINGTON, ONTARIO L7L 1V8 CANADA

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

Dear Sir or Madam

Submission Number: 2.22840 Transaction Number(s): W0270.00147

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

Cc: Resident Geologist

Dan Peter Bunner (Agent)

Temex Resources Ltd. (Assessment Office)

Assessment File Library

Temex Resources Ltd. (Claim Holder)

Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:16901

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Dato y Timo of Issue Jan 3D 2002

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PLAN

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ADMINISTRATIVE DISTRICTS l DIVISIONSMining Division Sudbury

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Ministry of Natural Resources District NORTH BAY

TOPOGRAPHIC LAND TENURE

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MAP

Date y Time of Issue Jan 30 2002

TOWNSHIP l AREA

CHAMBERS

08:18h Eastern

PLAN

Q-3416

ADMINISTRATIVE DISTRICTS l DIVISIONSMining Division Sudbury Land Titles/Ragistry Division NIPISSING

Ministry of Natural Resources District NORTH BAY

TOPOGRAPHIC LAND TENURE

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