Jet Aurora ~~ Fieldex Exploration -Ai Piatinum Corp

GM 62648 ASSESSMENT REPORT BASED ON THE 2006 LAFORCE GEOLOGICAL MAPPING & PROSPECTING PROGRAM, LAFORCE PROJECT jet Aurora ~~ Fieldex Exploration -Ai PIatinum Corp.

ASSESSMENT REPORT

BASED ON THE

2006 LAFORCE GEOLOGICAL MAPPING & PROSPECTING PROGRAM

Laforce Project, Brodeur and Devlin Townships Claims: 1119531 1119530 1019423 1019424 5243412 5256056 1131342 1131343 1131339 3ESSOUI !,' E • 3 MINES H Ressources naturelles et Faune, Québec 2 ùEC. 206 NTS 31M/10 1 1 JAN, 2007 BUR5.I: Ari:..,( AL it .4 ?. Service de la Géoinformation

GM 6 2648

Roger Poulin, BSc., PGeo. (Ont, Que) Shastri Ramnath, M.Sc., PGeo. (Ont, Que) November 25th, 2006

LAFORCE ASSTStiNiFA I' REPORT No\eniher 2006

64gmp Aurora Fieldex ~ r ~ Exploration ,41 Platinum Corp.

SUMMARY Between October 9th and October 27`h, 2006, Aurora Platinum Corp. ("Aurora"), a wholly-owned subsidiary of FNX Mining Company Inc. and Fieldex Exploration Inc. ("Fieldex") carried out a Geological Mapping and Prospecting Program on the Aurora- Fieldex Laforce joint venture claims 1119531, 1119530, 1019423, 1019424, 5243412, 5256056, 1131342, 1131343, and 1131339 located in Brodeur and Devlin Townships (the "Laforce Property"). The Laforce Geological Mapping and Prospecting Program targeted Cu-Ni-PGE mineralization known as the Laforce prospect as well as areas outside the known mineralization. The objectives of the 2006 Geological Mapping and Prospecting Program were to: 1) Identify the extension of the gabbro intrusion; and 2) To use the knowledge acquired during the drill campaign to identify new and untested target areas east and west of the Laforce prospect. The mapping area covered an area approximately 1800m long by 350m wide. A total of 152 outcrop stations were identified and mapped, 87 rock samples were taken for hand specimens, and 16 rock samples were taken for assay analysis. The total expenditures for the summer 2006 Laforce Geological Mapping and Prospecting Program were $18,665.89.

LAFt. )RCI✓ :ASSE.SSN1E. N1 RF,PO R1 No\ ernher 2006 Aurora l~ Platinum Corp.

TABLE OF CONTENTS

SUMMARY 2 INTRODUCTION 5 PROPERTY LOCATION AND ACCESS 5 PROPERTY STATUS 6 PHYSIOGRAPHY AND CLIMATE 7 PREVIOUS WORK 7 REGIONAL GEOLOGY 8 PROPERTY GEOLOGY 10 2006 GEOLOGICAL MAPPING AND PROSPECTING PROGRAM 10 FIELD PROGRAM 10 LITHOLOGY 1 1 MINERALIZATION 1 1 ALTERATION 1 1 STRUCTURE 11 SAMPLING PROCEDURES 13 PERSONNEL AND CONTRACTORS 13 EXPENDITURES 14 CONCLUSIONS 15 RECOMMENDATIONS 15 STATEMENT OF QUALIFICATIONS 16 REFERENCES 18

LAEORCL: ,1SSESSN1EN1 I:EPOR1 November 2006 Aurora

Fieldex lif a Exploration ,vk Platinum Corp.

LIST OF FIGURES Figure 1: Laforce Property — Location Map 5 Figure 2: Laforce Property — Claims 6 Figure 3: Laforce Property — Regional Geology 9 Figure 4: Laforce Property — Geological Mapping Area 10

LIST OF TABLES Table 1: Laforce Property — Claim Status 7 Table 2: Laforce Property — Previous Work 8 Table 3: Laforce Property — Detailed descriptions of the mafic, ultramafic and brecciated rock types identified on the property during the 2006 program. 12 Table 4: Laforce Property — Personnel 13 Table 5: Laforce Property — Contractors 13 Table 6: Laforce Property — 2006 Expenditures 14

LIST OF APPENDICES

Appendix I: Geological Mapping and Prospecting Field Stations Appendix 11: Sample Location List and Sulphide Mineralization Appendix (I1: ALS Chemex Lab Certificates and Sample Locations

LIST OF MAPS

Map 1: Topographic map showing the field station locations Back Pocket Map 2: Geological map showing the geological interpretation Back Pocket

LAFOR('F \SSLSSNIENF RI-:POfZ I tio\ ember 2.UU6 lifit Aurora F ex Exploration ► Platinum Corp.

INTRODUCTION In 2004, Aurora acquired a 50% interest in certain claims located in the District of Temiscamingue, Quebec from Fieldex under a Joint Venture Agreement dated March 25, 2004. The JV Agreement includes three of the nine claims worked on during the 2006 Laforce Geological Mapping and Prospecting Program which is the subject of this report. In 2006, Aurora acquired a 50% interest in the remaining six claims described in this report from Fieldex under a second Joint Venture Agreement dated June 12, 2006. Although Aurora and Fieldex own a 50% interest in each of the nine claims, two of the claims are registered in Aurora's name as to a 100% ownership and the remaining seven claims are registered in Fieldex's name as to a 100% ownership (Table 1).

PROPERTY LOCATION AND ACCESS The Laforce Property is located 50 km northeast of the town of Ville Marie, Quebec and 2.2 km southwest of Laforce, Quebec in Brodeur Township (Figure 1). The property is centered approximately at 670600mE and 5264800mN (NAD 83, Zone 17).

Access to the property is by Highway 382 east from Ville Marie to the town of Fugereville and then north to the town of Moffet. Approximately 20 km east along the road Chemin de Moffet-Laforce, there is a turn off to a 3-km long, snowmobile/ATV trail heading south that leads directly to the property.

~~ O Kilometers r '0) ")).-;"-c~~ '

Figure 1: Laforce Property — Location Map

LAFORCE ASSESSMENT REPORT — November 2006

F ;4 M W ail Aurora Fieldex m4 i ExploraBon i Platinum Corp.

PROPERTY STATUS The Laforce Property consists of nine contiguous claims covering an area of 356.79 hectares located in Brodeur and Devlin Townships, District of Temiscamingue, P.Q. and is subject to two agreements between Aurora and Fieldex dated March 25, 2004 and June 12, 2006 respectively. Aurora and Fieldex each own a 50% interest in the Devlin Property (Figure 2) by virtue of the aforesaid two agreements. Two of the claims are registered on the Ministere des Resourcesses Naturelles et de la Faune mining titles system in the name of Aurora as to a 100% ownership and the remaining seven claims are registered in the name of Fieldex as to a 100% ownership. The current status of the Laforce Property is described in Table 1.

a' a Town of Laforce 1":. Ir lc /~ = j I / m ô 10- Is 0 ~ ~' ~ 07 Y 10 CO O ~ N 0~ ~ N. f0 _ Ô O O N', n ~ , ~OV . N N 11aaa1 ~ N N Mui h N pN! 01 ' T ~: O~ m rn rn m 01 ~ 01 N 01 W CO Ôl ( Ô/ O 0 0 ÔI T W _._ N W ~~ CO ~ 00~ ~- D. CO CO CO CO CO CO CO OD CO CO. CO ' ~ .- e- ~ ~ T. e- ~ ~ y s-N N ~N 0 ~ ~ ' ~ . ,. Q1 . .. . ' . - ~ wo0 00 '- ~ . . ~~~ . O~ r• cr• ‘— I

1 1 583x-,1119548 1119549 1119550 } /3 31q1131343 1131344 1131345

vi• N 1r CO 01 N N ~ %!N N N N N rc co Or al 01 en as ~01 ' O~i OS M N V Q Nmm m O0 10 a1 01 V ~ M c7 .~ 0! {+! CO ~- e~ ~ r• r Ô Ô Ô Ô ô N N 0 G p ~ rf c'1 . M N ~ 'PJ ; r T . ~ 7 2 1 ~Ze 77 3 N ~' 0 {; t co C.3 18 13 750 0 4

475 13 11 1 6 4 \ 32 33 27 2 25 2 22 J

.. ... 95

195 ~' 195 4 195 195 1195 5 1 11 00 11 1 1 N

11 e- 34 11195 11

1 - 87 1 of PJ 43 CO 4 13

1101872 01 3 47 ô 47 .- ~ 1 11

u~ 6 9 1 0 30 Aurora-Fieldex Claims co 2 m • 4 1866 13 7431

1101864 3

M. 4 47

ô 474 1

1 Claims with 2006 Geological Mapping - • 110

Kilometers 0 1

Figure 2: Laforce Property — Claims

LAFORCE ASSESSMENT REPORT — November 2006 6 Aurora "TM/~ Fieldex Platinum Corp. aExploration '+

Table 1: Laforce Property — Claim Status

Claim No. Hectares Registration Date Expiry Date Titleholder 1019423 42.39 26-May-01 25-May-07 Fieldex 100% 1019424 42.35 26-May-01 25-May-07 Fieldex 100% 1119530 42.89 11-Mar-03 10-Mar-07 Aurora 100% 1119531 42.92 11-Mar-03 10-Mar-07 Aurora 100% 1131339 58.15 14-Dec-04 19-Feb-08 Fieldex 100% 1131342 13.77 14-Dec-04 19-Feb-08 Fieldex 100% 1131343 34.32 14-Dec-04 19-Feb-08 Fieldex 100% 5243412 40.00 18-Sep-00 * 17-Sep-06 Fieldex 100% 5256056 40.00 18-Sep-00 * 17-Sep-06 Fieldex 100% * Renewal application is currently being processed by Ministere de Ressources Naturelles et de la Faune. Quebec.

PHYSIOGRAPHY AND CLIMATE The property has a moderate relief that varies from 250 to 325 meters above sea level. Overburden is relatively thin, varying from zero to one metre in the reported drilling area. Most of the property is forested by spruce, birch and poplar. No major water body or rivers occur near the current drilling area however, there are a few seasonal streams and ponds in the low lying areas. The district has typical boreal climate.

PREVIOUS WORK Copper-nickel mineralization was discovered in the Laforce area in 1957. The original showing was stripped, trenched and sampled revealing disseminated to semi-massive pyrrhotite, pentlandite, and chalcopyrite in amphibolite (Table 2). Kerr Addison optioned the property and in 1958 and 1959, drilled 29 holes on the property, 15 of which intersected a pod of mineralization. Further drilling included 11 holes drilled by Lynwatin Nickel Copper Ltd. in 1961, 19 holes by Texmont Mines Ltd. in 1967 and 8 holes by Vista Exploration in 1976. Alotta Resources completed a ground IP survey in 1988 and followed up with four drillholes to the east of the main showing. Between 2001 and 2004 several geophysical surveys were completed by Aurora including a Terraquest airborne magnetic survey and a Geotech VTEM survey. In 2005, Aurora and Fieldex completed a regional reconnaissance mapping and prospecting program to follow up the airborne conductors identified in the 2004 VTEM survey.

L.11 ORCE .\SSESSNlE\ l REYOR I No \. ember 2.006 Aurora Fieldex ~ AA ~Exploration é Platinum Corp,

Table 2: Laforce Property — Previous Work Laforce Resource Kerr Addison 1958 geological mapping Geological Laforce Grab Samples ARP/FLX* 2001 prospecting Mapping Boudrias Ni-Cu Tom Exploration 2002 geological compilation Showing IP Survey Alotta Resources 1988 Ground IP Survey Belanger IP Survey 2001 Ground IP & Mag Geophysics Geophysics Magnetic Survey Meeguish 2001 Magnetic Survey JVX IP Survey JVX 2002 Ground IP Magnetic Survey Terraquest 2004 Airborne Magnetic VTEM Survey Geotech 2004 Airborne EM & Mag Laforce Rock Geochemistry ARP/FLX 2004 rock sampling Sampling 1958- Assessment DDH 6 companies 84 drillholes ** Diamond 1988 Drilling Boudrias DDH Brominco 1975 ? drillholes Interpretation Laforce Compilation ARP/FNX/FLX 2006 GIS & 3D Compilation * ARP=Aurora Platinum Corp; FLX=Fieldex Exploration Inc. ** 7 drill logs not found in assessment records

REGIONAL GEOLOGY The project area is located in the Belleterre-Angliers greenstone belt, part of the Pontiac Subprovince in eastern Superior Province of the Canadian Shield. Belletere-Angliers is the most southerly greenstone belt in the Superior Province, situated south of the Abitibi greenstone belt and north of the Grenville Front in the Temiscamingue area (D'Amours, 2004). The generalized stratigraphy of this belt is one of komatiites and komatiitic basalts, tholeiitic basalts, calc-alkaline intermediate to felsic volcanic rocks, volcanic sedimentary rocks and minor iron formation (Barnes et al, 1993). Gabbro intrusions that are rich in metals have intruded the supracrustal stratigraphy and are interpreted by Barnes et al. (1993) to have been produced by a mantle plume that intersected and rifted an island arc. The Belletere-Angliers greenstone belt is physically separated into three distinct groups; the Baby Group in the west, the Belletere Group in the east, and Lac des Bois Group in the center (D'Amours, 2004; Figure 3). Contacts with younger Pontiac Group metasedimentary rocks and older tonalite-trondhjemites intrusion suites are sheared. The Pontiac metasedimentary rocks dip beneath the Belletere-Angliers greenstone belt and are tectonically interleaved with the intrusive rocks. Gabbros, that intrude the tholeiites, are compositionally similar to the volcanic suite (D'Amours, 2004). Both rock types have undergone a similar degree of deformation and metamorphism. The gabbros have been interpreted as the products of the interaction as a mantle plume with an island arc and may have been generated in a rift arc setting.

LAFORCL ASSESSMENI RLPORI November 2.006 AA Aurora Fieldex +s Exploration 's Platinum Corp,

The Belletere-Angliers greenstone belt is host to numerous nickel-copper and gold occurrences/prospects and two past producing mines, the Belleterre gold Mine and the Lorraine Cu-Ni Mine (Osmani, 2005). The Ni-Cu+/-PGE deposits are mafic intrusion-hosted and gold mineralization occurs in quartz veins commonly along or adjacent to sheared volcanic-gabbro or granitoid-volcanic contacts. The Midrim Deposit and its satellite Ni-Cu- PGE prospects occur in roughly a 2.5x5.0 km area in the Baby greenstone belt. The Lorraine Cu-Ni mine (594,000 tonnes of ore grading 1.07% Cu and 0.45% Ni) and Lac Kelly deposits are hosted in the Lac des Bois greenstone belt (Mineral Bulletin MR198). The Belleterre gold Mine and LaForce Ni-Cu prospect occur within the Belleterre greenstone belt. The Belleterre Mine, as of 1958, produced $27.72 million worth of gold from 2.397 million tons of ore (Beecham and Ng-See-Quan, 1978). Sill-like bodies of mafic to ultramafic composition (gabbros and pyroxenites) of various sizes have intruded the volcano-sedimentary sequences of the Belletere-Angliers greenstone belt (Osmani, 2005). Some of these bodies, as mentioned above, are host to magmatic Ni-Cu+/- PGE deposits (e.g., Midrim, Lorraine and LaForce deposits). Two geochemically distinct suites of gabbroic intrusions, fertile and barren, have been reported (Imreh, 1978). The fertile gabbros, hosting the known Ni-Cu+/-PGE mineralization (e.g., Midrim and Satellite deposits), are geochemically evolved (i.e., enriched in light and intermediate REEs) relative to the barren gabbros, which display flat REE patterns. However, both types of intrusions are of tholeiitic affinity and have undergone a similar degree of deformation and metamorphism as their volcanic host rocks. The Lorraine Mine is the only past producer (Ni-Cu) occurring in the eastern part of the Lac des Bois greenstone belt.

Quaternary Cover ,.amprophyre . Granttoids Greenstoné Belts Gabbro i Ultrarric Diorite

Temiscamingue Area 0 15km

Figure 3: Laforce Property — Regional Geology

LAFORCE ASSESSMENT REPORT — November 2006 9 M7111111111 1 iht,-1 Aurora Fieldex ~ ~ Exploration All Platinum Corp.

PROPERTY GEOLOGY The Laforce Property contains part of an elongate, east-west trending gabbroic intrusion approximately 4.6 km long and 0.20 km wide. The gabbro body occurs near the northern margin of a 4.2 km wide dioritic plug (Figure 3). The northern margin of the dioritic plug is cut by several northeast-southwest trending faults.

The main Laforce mineralization occurs within the central segment of the gabbro. The mineralization is hosted within an amphibolitic body which is enveloped by porphyritic gabbro and gabbro that are in contact with porphyritic diorite. The area is cut by lamprophyre and quartz-feldspar dykes.

2006 GEOLOGICAL MAPPING AND PROSPECTING PROGRAM

Field Program A regional geological mapping and prospecting program was completed on the Laforce Property between October 9th and 27th, 2006. The mapping was completed at a scale of 1:2500 and covered an area approximately 1800m long by 350m wide (Figure 4). A total of 152 outcrop stations were identified and mapped, 87 rock samples were taken for hand specimen, and 16 rock samples were taken for assay analysis (Appendix II and III). A Garmin GPS was used to locate outcrop edges and the data was transferred on paper at 1cm =10m scale. The hand drawn map was then scanned and digitized using Autocad. The final map was edited and interpreted using ArcMap (Maps I and II).

INE Diabas ~ Gabbr Tonali Porph

Figure 4: Laforce Property — Geological Mapping Area

LAFORCE ASSESSMENT REPORT -- November 2006 10 Aurora Fieldex a Exploration A Platinum Corp.

Lithology The mapping was confined to the main gabbroic intrusion interpreted as being near the edge of a hornblende diorite batholith. The gabbro dyke is arcuate in shape, steeply dipping, averaging 200 meters in width and mapped over a distance of approximately 2700 meters.

A variety of mafic and ultramafic intrusive rocks were identified within the main gabbro dyke including gabbro, melagabbro, amphibolite, pyroxenite, hornblende gabbro, diabase, gabbro breccia, gabbro porphyry and metagabbro (Table 3). The contacts between mafic and ultramafic rocks were generally sharp. The contacts between the mafic rocks were not always observable and cannot be commented on. Both the mafic and ultramafic rocks were crosscut by younger, mafic diabase dykes.

Mineralization At the Laforce showing, Ni-Cu-PGE-bearing sulphides occur within brecciated and non- brecciated amphibolite. Sulphides comprise up to 15% of the unit and occur as 1-3 mm, blebs and veinlets of pyrrhotite, pentlandite, chalcopyrite, pyrite and trace millerite. Sulphide mineralization identified in other parts of the property generally occur as trace, cubic pyrite in gabbro and pyroxenite (Appendix II).

Alteration The gabbro units are generally unaltered except for occasional epidote and late quartz and feldspar veins, which sometimes give a brecciated appearance. The most prominent alteration is closely associated with the main Laforce showing as the pyroxenite is altered to amphibolite and the gabbroic units contain significant identifiable biotite and chlorite.

Structure Five strong lineaments, interpreted from air photos, appear to crosscut the main gabbro body. These lineaments strike north-south and are truncated by a major south-west trending regional fault. Only one major north-south striking fault was identified in outcrop. The structure was 4 to 5 meters wide and did not displace the gabbro unit.

L,IEORC E :'\SSESSi\1EN1 REP( MI No\ cruller 2006 1 I

01A Aurora

Fieldex 1' r II Exploration s Platinum Corp.

Table 3: Laforce Property — Detailed descriptions of the mafic, ultramafic and brecciated rock types identified on the property during the 2006 program. Rock Type Code Mineralogy Detailed Description Dark grey-green rock with 40-60% anhedral to subhedral feldspar. The rock has a hypidiomorphic texture and is medium mafic content 40- gabbro GAB grained. Finer grained gabbros occur in small dikes and in 60% + plagioclase breccia matrix along intrusion contacts. Black hornblende and green amphibole are the major visible mafic minerals present.

Dark black-green rock with 10-30% feldspar. The feldspars are usually interstitial to the hornblende and smaller in size. They mafic content 70- melagabbro MLGB are also unevenly distributed. Poikilitic textures are occasionally 90% present. Black hornblende is the major visible mafic mineral present. mafic content >90 % Dark green rock made of long green feathery amphibole grains. It is associated with the Laforce showing gabbro/amphibolite amphibolite AMPH green blocky or breccia and is sheared. It is the host rock of the Ni-Cu-PGE feathery amphiboles bearing sulphides. Dark grey-black rock with 2-20% feldspar. The pyroxenititic mafic content >90 % rocks are coarse grained and consist of equant uralitized pyroxenite PYRT hornblende or other hornblende and amphibole grains. Feldspar content is 0 to 10% blocky amphiboles and the distribution is patchy. Black hornblende and green amphibole are the major visible mafic minerals present.

hornblende Dark grey-black rock with 40-60% anhedral to subhedral hornblende (unaltered) is the feldspar. The feldspars are usually interstitial to the hornblende HBGB gabbro primary amphibole and smaller in size. Black hornblende is the major visible mafic present mineral present. One 2m east-west oriented dike was mapped. The rock is dark diabase DIA mafic diabase dyke grey-green, fine grained, massive and strongly magnetic. Light to dark grey rock composed of fine to medium grained amphibole or gabbro matrix supporting up to 30cm, medium any brecciated grained, subrounded, gabbro and pyroxenite fragments. Breccia gabbro occurring along the edge of the intrusion is typically composed GBBX gabbro (ultramafic breccia of 50%, tonalitic and porphyritic hornblende diorite fragments included) (footwall rocks). Ni-Cu-PGE bearing sulphides sometimes occur in the matrix of the gabbro breccia as disseminations and semi massive sulphides. define Dark grey-green rock with 40-60% anhedral to subhedral gabbro porphyroblasts, feldspar. The matrix of the gabbro GBPY has a hypidiomorphic texture porphyry feldspar or mafic and is medium grained. Black hornblende and green amphibole mineral are the major visible mafic minerals present. metagabbro MTGB Sheared gabbro (as described above).

L.kFOIZC'E :'\SSFSSNII:NT REI'OIZ I No\ ember 2(.)06 12 44 Aurora ~Fdielex Exploration ~ Platinum Corp,

Sampling Procedures

Samples were submitted for preparation to ALS Chemex in Sudbury and for assay to ALS Chemex in Vancouver where they were analyzed for Au, Pt, Pd, Ag, Cu, Pb, Ni, and Co. Precious metals were analyzed using an inductively-coupled plasma mass spectrometer (ICP-MS). Base metals were analyzed using an atomic absorption spectrometer (AA). Lab certificates are provided in Appendix III.

PERSONNEL AND CONTRACTORS

All work was supervised and implemented by Aurora Platinum Corp., 1300 Kelly Lake Road, Sudbury Ontario, P3E 5P4 (Tables 4 & 5).

Table 4: Laforce Property — Personnel Name Position Location Catharine Farrow Chief Geologist 1300 Kelly Lake Rd, Sudbury, P3E 5P4 Shastri Ramnath Senior Project Geologist 1300 Kelly Lake Rd, Sudbury, P3E 5P4 Roger Poulin Project Geologist 1300 Kelly Lake Rd, Sudbury, P3E 5P4 Steve Dunlop Project Geologist (covered for RP) 1300 Kelly Lake Rd, Sudbury, P3E 5P4 Ahmed D'jour CAD Technician 1300 Kelly Lake Rd, Sudbury, P3E 5P4 1010 Chemin du Golf, Hugo Girard Core Technician Duhamel-Ouest, Que, J9V 1 M6

Table 5: Laforce Property — Contractors Name Position Location ALS Chemex Assay Lab 212 Brooksbank Ave, Vancouver, V7J 2C1

1 AFORCL ASSF.SSMf;NT Novmnei- 2006 1;

oil Aurora ~~ III Fieldex 7r~' ~ Exploration Platinum Corp.

CONCLUSIONS

The following conclusions are based on the summer 2006 Geological Mapping and Prospecting Program at the Laforce Property: 1) The main Laforce mineralization is hosted within a locally brecciated amphibolite pod hosted by porphyritic gabbro which is in contact with the porphyritic diorite; 2) The mineralized showing was composed of up to 15% sulphides, made up of disseminated to wispy pentlandite, pyrite and chalcopyrite; and 3) The gabbro extends towards the southwest and is locally associated with pyroxenite.

RECOMMENDATIONS

The following recommendation is based on the results of the summer 2006 Laforce Geological Mapping and Prospecting Program:

1) To complete a mapping, and sampling program of the Laforce property and conduct stripping where necessary, to locate and delineate other zones of brecciated amphibolite within the much larger host gabbro.

i_:-11 ORCE ASSI:SSMTN"1 REPORT -- No\ember 2006 Aurora ~ Fieldex ~ l~1i Platinum Corp. IIMMIIIIIIIMMIlaExploration s l

STATEMENT OF QUALIFICATIONS I, Roger Y. Poulin, of the Town of Val Caron, Province of Ontario, do hereby certify that:

1) I am an Exploration Geologist, residing at 3171 Romeo St., Val Caron, Ontario, P3N 1G5, employee of Aurora Platinum Corp., 1300 Kelly Lake Road, Sudbury, Ontario, P3E 5P4;

2) 7) I completed a 3 year Geological Engineering Diploma from Cambrian College, Sudbury, Ontario in 1979 and graduated from Laurentian University, Sudbury, Ontario, (Bachelor of Science in 1990)I have been practicing in my profession as an Exploration Geologist continuously since 1979;

3) I am a Professional Member of the Association of Professional Geoscientists of Ontario (APGO) and a temporary member of the Ordre des géologues du Québec(OGQ);

4) This report is based on personal examination of the properties between October 9th to 27`", 2006; and

5) I have no personal interest in the property covered by this report.

/\ V • , Roger Y. Poulin, B.Sc., PGeo.

OGQ #: 1095

Dated in Sudbury, Ontario this 25th day of November, 2006

L OIZCL ASSESSNtLN 1 1:L1'c.)Il I No\emhcr 1(106 E Aurora Ill Fieldex - F Expl oration ~ Piatinum Corp.

STATEMENT OF QUALIFICATIONS

I, Shastri M. Ramnath, of the Greater City of Sudbury, Province of Ontario, do hereby certify that:

1) I am an Exploration Geologist, residing at 455 Tedman Avenue, Sudbury, Ontario, P3C 5A8, employee of Aurora Platinum Corp., 1300 Kelly Lake Road, Sudbury, Ontario, P3E 5P4;

2) I graduated from the University of Manitoba, Manitoba (Bachelor of Science — Honours) in 1999 and from Rhodes University, South Africa (MSc. Exploration Geology) in 2001 and have been practicing in my profession as an Exploration Geologist continuously since;

3) I am a Professional Member of the Association of Professional Geoscientists of Ontario (APGO) and a temporary member of the Ordre des géologues du Québec(OGQ);

4) This report is based on personal examination of the properties between July 1st and October 31st, 2006; and

5) I have no personal interest in the property covered by this report.

. e' •.~i ~ ;~ ti «

I ~ 6iF ASTRI M. RAMNATH PRACTISING MEMBER y 1174 • NTAft f Shastri M. R. nath, M.Sc., PGeo.

OGQ #: 1093

Dated in Sudbury, Ontario this 25th day of November, 2006

L.UORCL :ISSESStiIEN C REPC)R [ November 2006 of Aurora Fieldex a Exploration Platinum Corp.

REFERENCES

Barnes, S.-J., Couture, J.-F., Sawyer, E. W., and Bouchaib, C., 1993, Nickel-copper Occurrences in the Belletere-Angliers Belt of the Pontiac Subprovince and the Use of Cu-Pd Ratios in Interpreting Platinum-Group Element Distributions. Economic Geology, v. 88, p. 1402-1418.

Beecham, A.W. and Ng-See-Quan, W., 1978, Report on Geophysical and Geological Surveys and Diamond Drilling Results, Harding Lake East and West Properties; St. Joseph Explorations Limited, Unpublished Report, 20 p.

D'Amours, C., 2004, Technical Report NI43-101 Fl for Aurora Platinum Corp. on the Temiskaming Joint Venture Project, Belletere-Angliers, Quebec, 29 p.

Imreh. L., 1978, Baby Township: Quebec Ministere Richnesses Naturelles. Geol. Rept. 185. 87 p.

Mineral Bulletin MR198

Osmani, I.A., 2005, Aurora Platinum Corp. Fieldex Exploration Inc. 2004-2005 Exploration Programs, Petosa Property, Gaboury-Laverlochere Townships, Quebec, NTS Map Sheet 31 M/6, 18 p.

i..1Ft)RCF: _1SSESSN1ENT REPORT November ->Of)fi 18 Aurora vw a Fieldex `A' l-1 Exploration ' Platinum Corp.

APPENDIX I: GEOLOGICAL MAPPING AND PROSPECTING STATIONS

L:\1 t)RC'E ;\SSFSS:bIEN f IZI:POR I tio\ cmhcr 2006 i

r`e a` ,y g~ a~ 8 a' as as 6~ D` Number Rock Type Colour Texture Strike Dip Phenocrysts Alteration k4. 4f e 4 Ur Comments L001 tonalite _ pink _ mg. 1 gneissic auartz-feldspar schist L002 tongue pink m.g. gneissic quartz-feldspar schist L003 pyroxenite _ green c.g. massive 100% all hornblende? L004 porphyrine diome pink _ mg. equigranular 10% feldspar 5% 80% 5% hornblende diorite L005 porphyritic gabbro grey m.g. massive 45% feldspar 20% 45% 20% feldspar 3mm phenol L006 pyroxenite green c.g massive 70% hornblende _ 100% 10% all homblentle? L007 porphyritic gabbro grey m.g. massive 103 -70 40% 60% sheared az 103 705 weak _ L008 tonalite pink f.g. gneissic 320 -80 60% 55% 5% gneissic az 320 80 dip, gtz-feldspar schist L009 pyroxenite green c.g. massive 100% 10% all hornblende? L010 porphyritic diorite grey m.g. porphyritic 10% feldspar 30% 25% 45% 3mm feldspar phenocrysts, weak foliation L011 porphynlic diorite gyqy _ m.g. porphyritic 10% feldspar 5% 65% 30% weak foliation L012 porphyrilic diorite grey m.g porphyritic 185 -85 10% feldspar 10% 60% 30% weak foliation az 185 85w L013 porphyritic diorite grey _ m.g. porphyrhic 181 _-85 15% feldspar 10% 65% 25% _ weak foliation az 181 85 dip _ L014porphyritic gabbro grey m equi ranular 20% feldspar 50% 50% green hornblende _ L015 diabase green f.g massive 90 -90 100% 2m e-w dyke Oedipal L016 porphyoticgabbro - green m.g. porphyrine 5% feldspar 50% 50% L017 porphyritic diorite prey m.g. porphyritic 20% feldspar 10% 65% 25% weak foliation, magnetic _ L018 po phyritic diorite g rey m g. porphyrilic 20% feldspar 15% 50% 35% magnetic L019 porphyritic diorite grey m g. porphyrilic 328 -90 30% feldspar 10% 60% 30% weak foliation az 328. 3mm feldspar L020 porphyritic diorite grey m g. porphyritic 15% feldspar 5% 65% 30% weak foliation L021 porphyritic diorite grey m g. , porphyritic 10% feldspar 5% 65% 30% weak foliation 1_022 porphyritic diorite grey m~ porphyritic 269 -70 10% feldspar 5% 65% 30% strong foliation az 269 70w dip L023 porphyritic dole _ grey m.g. porphyrine 30% feldspar 2% 68% 30% weak foliation L024 porphyritic gabbro grey _ porphyritic 15% feldspar 50% 50% massive 3mm feldspar L025 gabbro grey mg. massive 65% 35% banded. oink-grey, breccia boulders nearby L026 melagabbro green c_9: massive 80% hornblende 2% 98% 2% hornblende 101 cm interlocking crystals L027 gabbro grey fg. massive 20% 80% 5% 1cm matit xenoliths in fg. gabbro. contact with gabbro L026 porphyritic gabbro _ grey m.g, porphyritic__ 20% feldspar 55% 45% - __ 1_029 melagabbro grey m.g. massive 10% 90% hornblende m.g. to c.g.

_ L030 melagabbro grey m g_4 massive 10% 90% hornblende m.g. to c.q. L031 _ gabbro grey mg. , massive _ _ 20% BO% variable hornblende content 20-60% L032 melagabbro grey reg. - massive 10% 90% homblentle to lcmn 1_033 . 9aDhro grey mg. i massive 30% 70% hornblende L034 melagabbro _ _ y r massive 10% 90% m.o.-c.o. hornblende L035 melagabbrog grey ~. massive 5% 95% 1 cm homblentle, pink feldspar veins L036 melagabbro grey cg. i massive _ 5% 95% boulders. subcrop, hornblende to 1cm L037 gabbro breccia - grey mg i brecciated _ - gabbro (rags 1-30cm in oYn matrix, poop-Dv tliss to 30% L038 gabbro breccia grey my. brecciated ~ gabbro (rags 1-30cm in Ovn matrix, po-cp-pv dins to 50% L039 gabbro grey m.g. massive 30% 70% L040 gabbro grey cg. massive ihornblende 20% 80% hornblende to 1cm L041 gabbro grey e.g. massive 4ornblende 20% 80% hornblende to 1cm. contorted folialion 1_042 gabbro grey f.g. massive _ 25% 75% foliation ris L043 melagabbro grey_ co. massive thornblende 20% 80% _ hornblende to 1cm _ L044 melagabbro grey co. massive hornblende 20% 80% hornblende to smm 1_045 hornblende gabbro ___.. grey cg. massive I hornblende 20% 80% hornblende to 4mm 1_046 hornblende gabbro grey m.g. massive hornblende 20% 80% hornblende to 2mm _ L047 gabbro _ _-_ grey m.g. 1 massive 90 • -90 20% 80% _ weak foliation e-w dip 90 L048 porphyrine diorite grey in g massive 20% epidote 5% 30% 2mm feldspar L049 gabbro _ grey m. g equigranular epidote 50% 50% vanabie hornblende 1-2mm 30-50% L050 gabbro grey m.g. ] equigranular 60% 40% 2% hornblende 1,051ag bbro grey m g equigranular 60% 40% 2% hornblende L052 gabbro grey m.g. equigranular 40% 60% 3% variable hornblende 1-2mm 20-60% L053 gabbro breccia _ grey m.g. brecciated ' 5% 95% hx with torrents, gabbro, dip/ frogs to 30cm in green amptlibolitic matrix L054 gabbro _grey m.g. equigranular _ 60% 40% 1% 30-40% hornblende mod shearing az 316 dip 80, layered\sheared 10-20% hornblende alers to L055 porphyritic diorite light grey m.g. 316 -80 5% 80% 15% sheared 30% homblentle 50cm 1_056 gabbro - grey mg. equigranular 60% 40% 30-40% hornblende L057 pyroxenue 9 reen f.g. equigranular 5% 95% green amphiboliteibole laths 1_058 gabbro grey mg. - equigranular epidote 60% 40% 30-40% hornblende L059 porphyrilic diorite light grey m.g. sheared 322 -60 95% 5% sheared az 322 dip 60 L060 pyroxenite grey f.g. sheared 189 -80 100% 2% mylonitic major shear az 189 dip 80w, may be sheared gabbro L061 porphyritic diorite pink fg. sheared 10% epidote veins 5% • 90% 5% mixed with some m 9. gabbro? L062 gabbro grey m.g. equigranular - 55% 45% 25-55% hornblende. variable L063 gabbro grey m.g. equigranular 55% 45% 45-50% 2mm hornblende L064 gabbro grey_ m.g. equigranular 50% 50% 10% 35-50% hornblende 2mm L065 gabbro breccia grey m.g. brecciated 55% 45% gabbro mal. 30% elongate granitic, dipv frogs, hornblende 2mm L066 gabbro grey m.g. equigranular 55% 45% 30-45% hornblende, subcrop _ L067 gabbro grey m.g. equigranular 55% 45% 1% 35-45% hornblende, pv 1mm cubes L068 gabbro grey m.g. equgranular 50% 50% 30-50% hornblende _ L069 gabbro grey m.g. equigranular 50% 50% _ 30-50% hornblende L070 gabbro grey m.g. equigranular _ 60% 40% 2% hornblende, some felsic lavers DIPS? Within gabbro L071 porphyritic diorite pink fg porphymic 289 -75 20% feldspar 80% 20% stir/layering az 289 dip 75 _ 1_072 gabbro grey mg. eqm renular _ I 60% 40% 30-40% hornblende L073 gabbro grey mg equigranular 50% 50% 40-50% hornblende L074 gabbro _ _ grey mg. equigranular 60% 40% 30-40% hornblende -_ L075 gabbro grey mg_ eq uigranular epitlote 35% 65% 65% hornblende _ L076 gabbro grey m g ~I euigranularq` _ 30% 70% hornblende gabbro 1cm Drains. 25-30% feldspar L077 hornblende gabbro grey cg -m g. equigranular _ 25% 75% 2% 4mm-1 cm hornblende L075 gabbro grey m. g. equigranular 30% 70% 1% hornblende to 2mm L079 gabbro grey m. q. equigranular epidote 30% 70% weak foliation, hornblende to 2mm

vig. = very fine grained: m.g. = medium grained c . = coarse-grained

f ~

0s 'l 43°r~ 0 0 ca Number Rock TeColour Texture Strike ~ Dip Phenocrysts Alteration ~+ Comments L080 gabbro grey m.g. equigranular : 0I 30% 70% hornblende 2mm L081 gabbro grey mg equigranular 20% 80% hornblende 4mm. hornblende gabbro L082 hornblende gabbro grey _—_m.g. equigranular - 20% 80% hornblende 4mm, hornblende gabbro L083 feldspar porphyry pink f.g ', porphyrilic 10% 90% dyke with 20cm pegmatite east side of dyke 1004 _gabbro grey cg. leguigranular 25% 75% 25% 30cm feldspar dykes, irregular, hornblende gabbro 1 3mm-icm hornblende, s-w 5cm felsic dykes, hornblende gabbro, 10% L085 melagabbro grey c.g equigranular 20% 80% 1% muscovite alteration L086 porphyntic diorite light grey mg. ' porphyritic epidote 80% 20% 2mm feldspar L087 gabbro grey c.g. equigranular 20% 80% 2% 10-20% feldspar, hornblende gabbro L088 gabbro grey m.g. .equigranular ~ 20% 80% 2% pvroxenke xenos to 5cm, hornblende gabbro L089 gabbro grey m.g equigranular -~— 30% 70% 4mm hornblende 25-30%, hornblende gabbro L090 gabbro grey f.g-mg_ equigranular 30% 70% 3% hornblende 2mm _1091 gabbro __ _ __ mg equigranular 30% 70% 3mm hornblende, hornblende gabbro L092 gabbro grey equigranular 30% 70% 3mm hornblende, hornblende gabbro _ L093 gabbro_ grey equigranular 10% 90% 1% 10-20% feldspar, hornblende gabbro 1094 pnrph diorite rigor grey _ f sheared 8 -80 20% 60% 20% strong shear az 08 dip 80.5%cart veins. siliciron formation 1095 melagabbro - y cg. equigranular 30% 70% 10-30% feldspar variable c g. to m.g. going west to outer contact. L096 gabbro grey c.g. equigranular I 60% 40% 30-40% feldspar. 2mm-icm hornblende, hornblende gabbro L097 gabbro grey mg. 1 equigranular 60% 40% 3-4mm hornblende 1098 hornblende gabbro _ grey m.g. equigranular _ 50% 50% 40-50% feldspar. hornblende gabbro, same as o/c 100 L099 pyroxenile green c.g. equigranular 25% 75% icm hornblende. 20% feldspar veins forming angular breccia 20-30% feldspar, and veins, occ PYRT xenos to 10cm, hornblende 1100 hornblende gabbro grey m g.-y g. equigranular 30% 70% _ ___ _ gabbro 7 20-30% feldspar, and veins, occ PYRT xenon to 10cm, hornblende 1101 gabbrog grey m.g. equigranular 30% 70% gabbro L102 gabbro -__ grey mg. equigranular 30% 70% hornblende gabbro. occ feldspar veins L103 pyroxenite green c g. equigranular 36-91:1 , ' 100% m.g -c .g. green amphibole, shearing n-s vertical L104 pyxenite _ green cg. equigranular 360 -90 Î 100% m.g-cg green amphibole, shearing n-s vertical Li35 porphyritic d o te pink g_ i equigranular 90% 10% 5-10% hornblende, var mafics. in layers, occ 5cm diontic oblong xenos —i-- L106_ porphyritic diorite pink m. g. porphymic 2?feldspa_r 5% 90% 5% L107 porp h y rtic diorite kpin m. g equigranular i 10% 70% 20% 5-20% hornblende, subcrop 1108 gabbro grey m.g. egranular _ 30% 70% hornblende. subcrop L109 melagabbroag green cge ul anular__ _ 10% 90% 1-10% feldspar. 10% feldspar veins, subcmp Lt 10 e a abbrd orne perk m g. porphyrul 20%feldspar 85% 15% 5-15% hornblende, eubcrop L111 pyroxenite green 44_co. j equigranular 5% 95% 1cm hornblende. 10% feldspar veins, green amphibole. subcmp L112 melagabbro _ grey m.g-c.g equigranular 15% 85% hornblende gabbro, 10% 1-5mm feldspar veins 1113 porphyritic diorite pink (.g_-mg. 4 peThynuc ' 5%ifeltlspar 95% 5% L114 porphyr lit diorite pink m g poPrhyrc 20%lteltl5par 80% 20% 15-20% hornblende L115 ___pbbro grey m.g. equigranular _ _ epidote 70% 30% pyroxenile xenos lo 5cm, subcrop L116 hornblend _abbro green m.g. I equigranular epidote veins 30% 70% strong epidote alteration. 20% feldspar veins L117 gabbro gam rig. equigranular 1 40% 60% 30-40% feldspar L118 melagabbro_ grey m.g. oikiocrysls _ 25% 75% 5-25% feldspar, some feldspar clots oikocrystic L119 gabbro _ _ gré mg equigranular r - 60% 40% hornblende L120 gabbro grey m.g. I equigranular _ _ _ _ 40% 60% hornblende L121 gabbro _-_ grey mg. equigranular 50% 50% 40-50% hornblende L122 gabbro _-_ grr m.g. I equigranular _ 60% 40% -40% feldspar L123 amphiboltebbro __.. dark g f.g.-m.g. massive ~ 1% _ chlorite 50% bl 2% 1% L124porphyntic gabbro s&p, dark grey m.g. massive ~ 6% chlorite 40% bl trace G . L125 gabbro dark grey f9. foliated % : chlorite 60% lot trace weakly foliated, disseminated pyrite L126 porphyntic diorite light to medgrey m.g. massive 30% chlorite 20% bt L127 chlorite 40% bt weakly porph gabbro L128 _ Ilechlorite 40% lot trace weakly porph gabbro, disseminated pyrite L129 gabbro s&p. dark grey m.g massive 10 ' sericite, chlorite 40% bt trace weakly pariah gabbro: disseminated pyrite L130 gabbro s&p, dark grey m massive 15% sericite, chlorite 40% bt trace weakly to moderalely porch gabbro: disseminatedpvme brecciated with fragments 1-10 cm subangular, unsure iron formation L131 amphibolite greenish black f g.-m.g. breccia 1 % biotite trace amphibolite is fragmented or is the matrix? Disseminated pyrite 1132 porphyntic gabbro s&p, dark grey m.g. massive ~ 35% chlorite 40% lot .25% 1% increase in pheMcrysis from previous stations, matit clots up to 2cm amphibolite matrix surrounding 2J0 cm subrounded, blocks and L133 amphibolle breccia greenish black and pink m.g. breccia % chlorite g fragments of diorite and granite 1734 porphyritic gabbro s8p, dark rey mg massive 15% sericite. chlorite 40% bl L135 porphyntic gabbro s&p, darkr~ey m.g. massive 15% quartz-carbonate, chlorite 45% lot trace trace trace sulphides pvicp in mafic clot L136 porphyntic diorite s&p, light to med grey m.g. • massive 20% sericite, chlorite 20% 1% 3% 1%small trench along contacontact of amphibolite and diorite L137 amphibolile greenish black mg 1 massive % biotite 2% 2% small Trench along contacontact of amphibolite and diorite L138 porphyritic gabbro s&p, dark grey 1 m g. I massive 15% 40% bt same outcrop as SRSO14a.b L139 amphibolite greenish black mg. breccia % btottte 25% 1% % brecciated with 1-15 cm dioritic fragments in places L140 amphibolite dark greenish black v.c.g. l massive % 1% up to 2.5 cm amphibole surrounded Dy c.0. amphibole/chlorite L141 amphibolite dark greenish black mg. massive % 10% 2% 3% well mineralized L192 porphyritlo gabbro s&p, dark grey m.g. massive 20% chlorite 40% kt L14porphyritic gabbro s&p, dark grey _.-m.g. massive 10% epidote, chlorite 45% bt Trace disseminated pynle L144 gabbro dark grey m.g. massive — 3% sericite, chlorite 40% bt 1% L145 porphyrit.ic gabbro s&p, med lo dark grey m.g. massive 10% chlorite 40% bl trace L146 40% bl trace contact runs through outcrop. Possibly gradational gabbro -__ medium grey m.g. massive • , _5%i _ chlorite L147 gabbro dark grey fg.-mg. massive 1% chlorite 50% bl amphibolite matrix with 2-10 cm dioritic to granitic fragments, similar to L148 amphibolite-breccia greenish black mg. breccia %35% _ SRSD11 • L149 ~phyritic gabbro sop, dark grey fg.-m.g.: massive 10%' chlorite 35% bt L150 porphyritic gabbro sop, dark grey f,gm.g. massive 10% chlorite 35% bt same as SRSD26 L151 porphyritic gabbro s&p, med to dark grey m.g. massive 8% chlorite 40% bt L152 gabbro dark grey f a. • foliated • % chlorite I 60% bt weakdv foliated

v f.g. = very fine grained: mg. = medium grained: cg. = coarse-grained Aurora 44 Platinum Corp.

APPENDIX II: SAMPLE LOCATION LIST & SULPHIDE MINERALIZATION

LAFORCE ASSESS4IEN~I~ REPORI. No\ember 2(106 i I 1 I I i I I

Aurora Ay low Fieldex ar Exploration Platinum Corp.

Appendix II: Laforce Sample Location List and Sulphide Mineralization

*UTM *UTM Station Samples Sulphide (%) Mineralization Easting Northing L123 C073464 670384 5265203 2 1-2% pyrrhotite, chalcopyrite L125 C073465 670372 5265191 0.25 trace disseminated pyrite L126 C073466 670370 5265190 0 no visible sulphides L127 C073451 670380 5265151 0 no visible sulphides L128 C073452 670371 5265157 0.25 trace disseminated chalcopyrite L131 C073453 670340 5265150 0.5 trace -0.5% disseminated and fracture filled pyrite L132 C073454 670347 5265148 1 up to 1% pyrrhotite / pyrite L135 C073455 670339 5265212 0.25 trace pyrite / chalcopyrite L136 C073456 670347 5265219 5 3 pyrrhotite, 1% pyrite, 1% chalcopyrite L137 C073457 670347 5265219 5 up to 5% pyrrhotite / pyrite L139 C073458 670355 5265211 1 0.5% pyrrhotite, 0.25% chalcopyrite, 0.25% pyrite L140 C073459 670385 5265217 1 1% pyrite L141 C073460 670366 5265211 15 disseminated 10% pyrite, 3% chalcopyrite, 2% pyrrhotite L143 C073461 670400 5265195 0.25 trace disseminated pyrite L147 C073462 670355 5265198 0 no visible sulphides L152 C073463 670407 5265162 0 no visible sul hides

* UTM Nad83, Zone 17

1 1.01Z `iSi...•;S\1PvH' IZI:I'(il~'l N,,\ cmht2r 12006 Aurora ~ Fieldex ~ ~Exploration A Platinum Corp.

APPENDIX III: ALS CHEMEX LAB CERTIFICATES

I. A1~(_)RCE SSESSMEVf- REPORlF November 2006 Ill I I I I I I I I I I

To: FNX MINING COMPANY INC. Page: 1 ALS Chemex 1300 KELLY LAKE ROAD Finalized Date: 10-SEP-2006 EXCELLENCE IN ANAL YTICAL CHEMISTRY Account: TMD ALS Canada Ltd. SUDBURY ON P3E 5P4 212 Brooksbank Avenue North Vancouver BC V7J 2C1 ALS Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com

CERTIFICATE SD06082764 SAMPLE PREPARATION ALS CODE DESCRIPTION

Project: LAFORCE WEI-21 Received Sample Weight Sample login - Rcd w/o BarCode P.O. No.: 68 LOG-22 CRU-31 Fine crushing - 70% <2mm This report is for 17 Rock samples submitted to our lab in Sudbury, ON, Canada on CRU-QC Crushing QC Test 24-AUG-2006. SPL-21 Split sample - riffle splitter The following have access to data associated with this certificate: PUL-31 Pulverize split to 85% <75 urn FNX ASSAYS SEBASTIEN BERNIER JOHN EVEREST SPL-21d Split sample - duplicate CATHARINE E.G. FARROW JOHN FEDOROWICH JUDD FEE KAESY GLADWIN STEVE GREGORY CHANTAL JOLETTE PUL-31d Pulverize Split - duplicate DAVE KING GORDON MORRISON JIM PATTERSON ROGER POULIN SHASTRI RAMNATH LUC VALADE JO-ELLE WICKE CHRISTINA WOOD JIAN XIONG ANALYTICAL PROCEDURES ALS CODE DESCRIPTION INSTRUMENT PGM-ICP27 Ore grade Pt, Pd and Au by ICP ICP-AES As-AA45 Trace As-Aqua regia digestion AAS Ag-AA45 Trace Ag - aqua regia/AAS AAS ME-ICP81 ICP Fusion - Ore Grade ICP-AES

To: FNX MINING COMPANY INC. ATTN: CHANTAL JOLETTE 1300 KELLY LAKE ROAD SUDBURY ON P3E 5P4

This is the Final Report and supersedes any preliminary report with this certificate number. Results apply to samples as submitted. All pages of this report have been checked and approved for release. Signature: Keith Rogers, Executive Manager Vancouver Laboratory

To: FNX MINING COMPANY INC. Page: 2 - A ALS Chemex 1300 KELLY LAKE ROAD Total # Pages: 2 (A) EXCELLENCE IN ANALYTICAL CHEMISTRY SUDBURY ON P3E 5P4 Finalized Date: 10-SEP-2006 ALS Canada Ltd. Account: TMD 212 Brooksbank Avenue ALS North Vancouver BC V7J 2C1 Phone: 604 984 0221 Fax: 604 984 0218 www.alschemex.com Project: LAFORCE CERTIFICATE OF ANALYSIS SD06082764

Method WEI-21 ME-ICP81 ME-ICP81 ME-ICP81 ME-ICP81 ME-ICP81 ME-ICP81 ME-ICP81 ME-ICP81 PGM-ICP27 PGM-ICP27 PGM-ICP27 As-AA45 Ag-AA45 Aealyte Recvd wt. Cu Ni Co Fe As Pb Zn S Au Pt Pd As Ag Units kg % % % % % % % % g/tonne g/tonne g/tonne ppm ppm Sample Description LOR 0.02 0.005 0.005 0.002 0.05 0.01 0.01 0.01 0.01 0.03 0.03 0.03 5 0.2

C073451 0.84 0.006 0.017 0.003 8.44 <0.01 <0.01 0.01 0.14 <0.03 <0.03 <0.03 8 <0.2 C073452 1.23 0.008 0.011 0.006 8.43 0.01 <0.01 0.01 0.21 <0.03 <0.03 <0.03 14 <0.2 C073453 1.00 <0.005 0.054 0.007 8.77 <0.01 <0.01 0.01 0.11 <0.03 <0.03 <0.03 5 0.4 C073454 1.71 0.012 0.023 0.006 7.05 <0.01 <0.01 0.01 0.07 <0.03 <0.03 <0.03 <5 0.2 C073455 1.23 0.012 0.027 0.007 8.15 0.01 <0.01 0.01 0.16 <0.03 <0.03 <0.03 <5 <0.2 C073456 0.80 0.142 0.183 0.008 7.72 <0.01 <0.01 0.01 0.85 <0.03 0.03 <0.03 10 0.3 C073457 0.64 0.030 0.224 0.008 9.91 <0.01 <0.01 0.02 0.36 <0.03 <0.03 <0.03 9 1.2 C073458 0.58 0.108 0.112 0.008 10.00 <0.01 <0.01 0.01 0.18 <0.03 <0.03 <0.03 9 0.5 C073459 1.23 0.008 0.056 0.010 10.30 <0.01 <0.01 0.01 0.11 <0.03 <0.03 <0.03 5 <0.2 C073460 1.40 0.152 0.569 0.026 12.55 <0.01 <0.01 0.01 3.39 <0.03 0.03 0.03 11 0.9 C073461 1.57 0.007 0.023 0.005 8.51 0.01 <0.01 0.01 0.09 <0.03 <0.03 0.03 <5 0.5 C073462 0.26 0.010 0.020 0.005 6.56 <0.01 <0.01 0.01 <0.01 0.15 0.19 0.22 6 0.2 C073463 0.86 0.007 0.021 0.003 5.06 <0.01 <0.01 0.01 <0.01 <0.03 <0.03 <0.03 5 <0.2 C073464 3.35 0.013 0.025 0.007 8.53 0.01 <0.01 0.01 0.12 <0.03 0.04 0.05 7 <0.2 C073465 2.44 0.014 0.025 0.007 8.58 0.01 <0.01 0.01 0.15 <0.03 <0.03 <0.03 5 <0.2 C073466 0.41 0.007 0.011 0.006 4.31 <0.01 <0.01 0.01 <0.01 <0.03 <0.03 <0.03 6 <0.2 C073466 DUP <0.02 0.008 0.012 0.003 4.36 <0.01 <0.01 0.01 0.08 <0.03 <0.03 <0.03 5 <0.2