Geological Mapping Report on the River Valley Property ... · PREVIOUS WORK Information on previous...

41I09NE2008 2.20092 MCWILLIAMS 010

Geological Mapping Reporton the

River Valley Property - North Grid,November to December, 1999

Dana and Mcwilliams townships, Ontario (NTS 411/09)for

L Geodigital K Mapping l \ Systems LA Inc.

Timmins, Ontario (705)267-7128

2 .2009 2

Peter C.Wood February, 2000

SUMMARY

Mustang Minerals Corp. (Mustang) acquired the River Valley property in early 1999 in order to explore the River Valley gabbro-anorthosite intrusion for economic concentrations of contact-type platinum group metal mineralization. First phase exploration on the North Grid was initiated in early November and geological mapping commenced on November 12, 1999 and was completed by December 1, 1999. During this time a total of approximately 48 line kilometres of grid were systematically mapped (1:5000), sampled, prospected and also covered by a ground magnetic survey. A total of 83 locations were sampled and submitted for assay.

The mapping, sampling and prospecting program confirmed that the intrusive contact on the North Grid hosts anomalous to highly anomalous concentrations of Au+Pt+Pd (PGM) with a best assay of 2503ppb PGM. A program of IP followed by trenching and stripping over selected anomalies in areas with thin overburden cover is recommended. Diamond drilling should subsequently test the continuity of the best targets at depth.

TABLE OF CONTENTSSUMMARY......................................................................................................................................^

TABLE OF CONTENTS ..................................................................................................................3

LIST OF FIGURES ..........................................................................................................................4

LIST OF TABLES............................................................................................................................4

LIST OF APPENDICES...................................................................................................................4

INTRODUCTION................................................................^^

LOCATION AND ACCESS.............................................................................................................. 5

TOPOGRAPHY AND VEGETATION .............................................................................................. 5

PROPERTY......................................................................................................................^

REGIONAL GEOLOGY................................................................................................................. 12

PROPERTY GEOLOGY................................................................................................................12

PREVIOUS WORK........................................................................................................................12

GEOLOGICAL MAPPING PROGRAM ......................................................................................... 16

ROCK UNITS................................................................................................................................. 18ANALYSES....................................................................................................................................^RESULTS OF GEOLOGICAL MAPPING PROGRAM.............................................................................. 19ASSAYS........................................................................................................................................20LITHOGEOCHEMISTRY................................................................................................................... 21

CONCLUSIONS AND RECOMMENDATIONS ............................................................................. 24

CERTIFICATE OF QUALIFICATION ............................................................................................ 25

REFERENCES...............................................................................................................................26

41I09NE2008 2.20092 MCWILLIAMS 010C

3

LIST OF FIGURES

Figure 1: Location Map....................................................................................................... 7

Figure 2: Grid Location Map............................................................................................... 8

Figure 3: Claim Location Map............................................................................................ 11

Figure 4: Location of Early Proterozoic Layered Complexes in the

Huronian-Nipissing Magmatic Belt, Ontario........................................................ 13

Figure 5: Property Geology............................................................................................... 14

Figure 6: Summary of Previous Work................................................................................17

Figure 7: Alkalies-Silica Plot for River Valley Intrusive Rocks, North Grid.......................... 22

Figure 8: Jensen Cation Plot for River Valley Intrusive Rocks, North Grid......................... 23

LIST OF TABLES

Table 1: River Valley PGM Property - Claim List................................................................. 9

LIST OF APPENDICES

Appendix l: Summary of Assay and Whole Rock Data

Appendix 2: Assay and Whole Rock Certificates

Pocket 1: North Grid Bedrock Geology (1:5000)

Pocket 2: North Grid Sample Locations and PGM Assay Data (1:5000)

INTRODUCTION

Mustang Minerals Corp. (Mustang) acquired the River Valley property in early 1999 in order to explore the River Valley gabbro-anorthosite intrusion for economic concentrations of contact-type platinum group metal (Au+Pt+Pd) mineralization. The first phase 1999 exploration program was initiated in early November with linecutting. Between November 12 and December 1, 1999, approximately 48km of 200m grid were systematically mapped at 1:5000, sampled, prospected and also covered by a ground magnetic survey (Patrie, 1999). Analytical results are presented in Appendices 1 and 2, respectively. The North Grid Bedrock Geology map (1:5000 scale), and the Sample Location and PGM Assay Data map (1:5000 scale) are located in Pockets 1 and 2, respectively, at the back of this report.

LOCATION AND ACCESS

The River Valley property is located approximately 50km east of Sudbury and covers roughly 8200 hectares (see Figure 1). The claims occur within NTS 411/09 and are centred on latitude 490 36' N and longitude 800 17' W (554892mE, 5160746mN, UTM Zone 17, NAD 27) as shown in Figures 1 and 2.

Excellent year round access to the property can be gained from Sudbury by travelling east on Highway 17 to Warren, and then northwards on Highway 539 to the town of River Valley. Access to the North Grid is via two gravel roads that extend to the northeast from Highway 539a just north of the town of River Valley. Additionally, several logging and hunting trails provide access to both the western and eastern portions of the grid. Supplies and accommodations are available at the town of River Valley (see Figure 2).

TOPOGRAPHY AND VEGETATION

The terrain in the vicinity of the North Grid is generally flat and swampy with overburden (predominantly sand) covered areas exhibiting flat to rolling topography. Overall relief is in the order of 55m and ranges from 260m up to approximately 315m above sea level. The area is poorly to moderately well drained and forested by black spruce, pine, birch and poplar. In lower wet areas the cover is typically spruce, cedar, tamarack, labrador tea and sphagnum-covered muskeg.

Overburden is typically composed of glaciofluvial (gravel and sand) and glaciolacustrine (sand, gravelly sand and gravel) deposits (Barnett et al., 1991). Locally, glacial striae on exposed bedrock indicate an approximate north-south ice flow direction. Newman (1996) reports that the overburden covering the western and northern portions of the intrusion is characterized by a relatively thin veneer of till over intermittent bedrock knobs.

Water suitable for drilling is readily available from rivers, creeks, streams and numerous beaver ponds

PROPERTY

The River Valley PGM property (see Figure 3) consists of 54 contiguous, unpatented mining claims, totalling 511 units covering approximately 8176 hectares. The claims are located in Crerar (G-2903), Dana (G-2094), Gibbons (G-2905), Henry (G-2913) and McWillams (G-2910) townships, Sudbury Mining Division, Ontario. Mustang acquired the property in early 1999 through staking and several option agreements. Subsequently, during early August 1999, Mustang signed a letter of intent to jointly explore its River Valley property with Impala Platinum Holdings Limited (Implats), the world's second largest primary producer of platinum group metals. In order to earn a 600Xo interest in the property, Implats must incur work expenditures totalling C$6 million over five years, and make cash payments totalling C$255,000 over four years. A number of the claims are subject to various Net Smelter Returns back to the original vendors which are documented in the underlying agreements. All claims are currently in good standing and are listed in Table 1.

Hudson Bay

James Bay

Geraldton

Manitouwadge

Marathon

SUPERIOR

River Valley PGM Property Figure 1: Location Map

100 200 Kilometres

00

River Valley PGM Property Figure 2: Grid Location Map

(RVAL.Grids.P9.d*g; Jan. 25. 2000)

Table 1: River Valley PGM Property - Claim List

Township

CrerarCrerarCrerarCrerarCrerarCrerarCrerarCrerarCrerarCrerarCrerarCrerarCrerarCrerarCrerarCrerarCrerarCrerarCrerarCrerarCrerarCrerarCrerarDana*DanaDanaDanaDana*DanaDanaDanaDanaDanaDanaDanaGibbonsHenryHenryHenryHenryHenry

Claim Number

12108171214609121461012146371214771121477212147731229523122952612295271230534123056412311181231119123112012312531231262123126312312641231267123590112359021235903121463812288001229367123118112312651235836123583712359041236443123644412375071237521123126012291601230060123006112300621230063

Number of Units

1644161246416814624481016164488151312

1421674314615816165

Area Hectares

2566464

256192649664256128224963264641281602562566464128128240208192166432

2561126448166496

24012825625680

Table 1 (cont): River Valley PGM Property - Claim List

Township

HenryHenryHenryHenryHenryHenryHenryHenryMcwilliams *Mcwilliams *Mcwilliams *McwilliamsMcwilliams

TOTALS

Claim Number

1230064123006512300661230067123125812300161230019123002112291521229153122915412291551237522

54

Numberof Units

8616161616161612151516

1

511

AreaHectares

12896

25625625625625625619224024025616

8176

indicates claims covered by the North Grid

10

River Valley PGM Property Figure 3: Claim Location Map

w Dana Mcwilliams i

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vara***

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1236444s

. 1210817

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Henry

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1235902

1214771. (formttly

12305313) Tomrose,11214772! ffonrnrV 9231254;

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1229527 f-Mustang-lmpala JV Property Boundary

Crerar

HHJ-, 539

4km

(MustJmp-JV-Clms.dwg; Jan. 11. 2000)

REGIONAL GEOLOGY

The River Valley property is underlain by the early Proterozoic-aged (2475+2/-1 Ma) River Valley Intrusion, a layered gabbro-anorthosite pluton. The intrusion is approximately 30km long and up to 15km wide, and is part of the Huronian Nipissing Magmatic Belt, which includes the East Bull Lake and Shakespeare-Dunlop intrusions which are located in the Southern Province to the west of Sudbury (see Figure 4). The River Valley Intrusion occurs close to the juxtaposition of the Superior, Southern and Grenville provinces. The intrusion is situated in the Grenville province and is cut, but not displaced, by the Grenville Front tectonic zone along the northwest margin. Regionally, the River Valley pluton is associated with a large, positive gravity anomaly that suggests a possible associated denser, more mafic phase at depth.

PROPERTY GEOLOGY

The River Valley area was mapped by Lumbers (1973) during a regional reconnaissance mapping program, which broadly outlined the geology of the River Valley Intrusion, the surrounding host rocks and the location of the Grenville Front (see Figure 5). More recently, Easton and Hrominchuk (1999) and Hrominchuk (1999) have examined and documented the geology, stratigraphy and copper-platinum group element potential of Dana and Crerar townships.

Mustang's River Valley PGM property is underlain by the River Valley gabbro-anorthosite intrusion and high-grade metasedimentary gneisses of the Grenville Province. Ashwal and Wooden (1989) report that the intrusion is comprised mostly of leuconorite and leucogabbro with lesser anorthosite, mafic and ultramafic phases. More recently however, Easton and Hrominchuk (1999) indicate that the intrusion is dominated (~6007o of the surface area) by gabbro, norite, gabbronorite, leucogabbronorite, and leuconorite compositions. True anorthosite forms only 1007o of the surface exposures of the intrusion. Minor Cu-Ni-PGM mineralization occurs in the southeast portion of the intrusion (Tomrose Occurrence).

PREVIOUS WORK

Information on previous exploration activities on the River Valley Intrusion is available from the Ministry of Northern Development and Mines in Sudbury, or through the ERLIS database.

The River Valley Intrusion has been the focus of relatively limited exploration activity over the past 45 years, and the bulk of this work has attempted to locate marginal-type massive copper-nickel sulphide mineralization similar to the Sudbury deposits. However, the intrusion has never been systematically explored for Platinum Group Metals (PGM) associated with disseminated sulphides (e.g. Stillwater and Lac des Iles deposits). Interestingly, it should also be noted that the Sudbury mines have collectively produced in excess of 20 million ounces of PGM as by-product from the nickel-copper ores.

12

Figure 4: Location of Early Proterozoic Layered Complexes in the Huronian-Nipissing Magmatic Belt, Ontario

l ONTARIO

k THUNDER BAY. QUEBEC

TIMMINS \* ' AREA OF

SUDBURYX INTEREST

tf

. r

***~*

Wisner Township Intrusion ^—.

Tee Lk--Splake Lk.- Barrow Lk. Intrusions

/'

East Bull Lake Intrusion ,-'}

( \ .-x

Drury Township

460 15, Intrusion ...—:*. Dunlop

Intrusion C

y

/

\

Y, : Falconbridge r Township

.- ,/, y V ^H. Xs Z**-s

20L

40km

81 0 l After Peck et al (1995)

K ^'--•'^ '

A--{^ -"'#5*River Valley Intrusion

| | Grenville Province

j | Sudbury Complex

j | Southern Province

[ | Huronian Volcanics

^| HNMB Mafic Plutons

l l Superior Province

River Valley PGM Property Figure 5: Property Geology

Crerar

(MusUmp.JV.Geol.dwg; Jan. 11. 2000)

A ._-

Between 1973 and 1996 much of Dana Township was included in the Temagami Land Caution, and was not available for staking. Additionally, historic building stone quarries are present in better preserved portions of the River Valley Intrusion north of the Sturgeon River in Dana Township. These quarries exploited a black anorthosite that is locally known as "Black Granite". Coarse garnet was also extracted from the gneisses in east-central Dana Township just north of the intrusive contact.

Historically, previous exploration work has focused on the southeastern contact of the intrusion in Crerar Township and is summarized below:

1956: Mcintyre Porcupine Mines, Limited completed two diamond drill holes on the Ferguson claims to test quartz veins with associated semi-massive chalcopyrite-pyrite mineralization. The holes totalled 32.6m (107 feet) on historic claim 90348. The best intersection was reported at 2507o Cu and 0.01 7o Ni over 0.61m (2.0 feet).

1960-1962: Tomrose Prospecting Syndicate completed prospecting, rock trenching, character sampling and 113.7m (373 feet) of pack sack drilling. Additionally, a total of 20 pits and trenches were excavated. The best assays from this work included 25 07o Cu and 8.9 g/t Au (0.26 opt).

1963-1964: Tomrose Mines Limited completed prospecting and 13 diamond drill holes (1 to 9 and 64-10 to 13, inclusive) totalling 1233.83m (4,408 feet). Although no significant assays were reported the drill logs indicated that several drill holes had intersected significant concentrations of sulphides (pyrite, pyrrhotite and chalcopyrite) associated with blue quartz eyes within the intrusion. The holes were drilled on historic claims 52410 and 51682.

1965: Falconbridge Nickel Mines optioned the Tomrose property and completed ground magnetometer and electromagnetic surveys and six diamond drill holes (CRE-1 to 6, inclusive) totalling 331.01m (1086 feet). No significant assays were reported and Falconbridge subsequently dropped the option.

1965: Tomrose Mines Limited, drilled two holes (NE-1 8.. 2) for a total of 114.00m (374 feet). No assays were reported.

1966: Tomrose Mines Limited, completed one 134.72m (442 feet) diamond drill hole (T66-1). Minor sporadic pyrrhotite, pyrite and chalcopyrite were reported but no assays were submitted.

1966: Azen Mines Limited, staked 10 claim units to the west of the Tomrose claim group and conducted a ground magnetic survey only. No drilling was reported.

1983-1986: Albert Leblanc drilled three holes (1-83, 1-84 and 1-86) for a total of 104.85m (344 feet) on two claim units in the northwest corner of Henry Township. No assay results are available.

1990: Albert Leblanc drilled three holes (90-1 to 90-3) for a total of 403.56m (1324 feet). Only 14 samples were submitted for assay and up to 338ppb PGM was reported. It also appears that Teck Explorations Limited logged the core from at least one hole

15

(DDL-0143; 153.01m). Interestingly, the drill log indicated a 34.78m (114.1 feet) sulphide mineralized section with sulphides ranging from trace up to 47o disseminated pyrrhotite, chalcopyrite and pyrite; however, no assay results were reported.

1994: Albert Leblanc conducted power stripping on three areas under an OPAP Grant. The claims were subsequently optioned by WMC International and formed part of a larger land package that was being assembled at that time.

1994-1996: WMC International Limited, staked and optioned a total of 1541 units covering a large portion of the River Valley Intrusion in an attempt to explore for marginal type Ni-Cu-PGM mineralization. An integrated program of airborne magnetic and electromagnetic geophysical (DIGHEM) surveys, soil and till geochemical surveys, and reconnaissance mapping and sampling was conducted. Several areas of interest were identified within the intrusion; however, no follow up work was performed. The report also confirmed the high PGM potential of the intrusion.

1998-1999: R. Bailey, L. Luhta and R. Orchard discovered two significant PGM prospects (Dana North and Azen Creek zones) associated with the northern contact of the River Valley Intrusion in Dana Township. Interestingly, these claims are situated within the area that was previously included in the Temagami Land Caution. This property was optioned by Pacific Northwest Capital Corporation (PFN) in 1998, and is currently being explored under an option-joint venture agreement (August, 1999) between PFN and Anglo American Platinum Corporation Limited (Amplats). Preliminary results from the 1999 outcrop stripping and detailed sampling programs in the Dana Lake Area have indicated five mineralized zones, which extend over a distance of 780m and are anomalous to highly anomalous (0.25 to IG.Og/t PGM). An average assay value of 376 samples that were collected from the mineralized zones average 2.4g7t PGM, Q.16% Cu and Q.04% Ni. Rhodium averages 0.05g7t, with individual assays ranging up to O.Sg/t.

1999: Mustang Minerals Corp. performed a geological prospecting survey on the Tomrose Zone (Albert Leblanc claims) in Crerar Township and several claims in Dana and Mcwilliams townships. Mustang verified the that the Cu-Ni showings are enriched with platinum group metals with assays up to 0.69gft PGM.

For convenience, the previous exploration activities are also summarized in Figure 6.

GEOLOGICAL MAPPING PROGRAM

Geological mapping commenced on Mustang's River Valley North Grid on November 12, 1999, and was completed by December 1, 1999. During this time a total of 48 line kilometres of 200m grid were systematically mapped at 1:5000, sampled, prospected and also covered by a ground magnetic survey (Patrie, 1999). A total of 83 locations were sampled (one sample for assay and one representative hand sample from each location). The current magnetic declination for the area (11 0 west) was obtained from the Natural Resources Canada, Geomagnetics Laboratory in Ottawa.

16

f-'"h—.,.-~.

River Valley PGM PropertyFigure 6: Summary of

Previous Work

::::7 ~

\ \ill,1-

X ll

Mcwilliams

Gibbons

Mustang-lmpala JV ' Property BoundaryRiver Valley

Intrusion

11l 11

\ \1 ti'*11 ix

\ }\ \ ' t'\ ' S

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S S

/X'

Henry

(RVAUPrev.DDH.dwg; Jan. 11. 2000)

Geological mapping was conducted by T. Keast with the assistance of G. Wright, and this work was supervised by P. Wood. It should be noted that as the mapping program was commenced so late in the field season it was decided that traverses would be restricted to outcrop exposures that were close to the grid lines. This would ensure that the task was completed before the outcrops were covered with snow.

Daily travel to the North Grid was via two gravel roads that extend to the northeast from Highway 539a just north of the town of River Valley. Additionally, several logging and hunting trails provide access to both the western and eastern portions of the grid (see Figure 2).

Rock UnitsMapping was carried out using the WMC geological legend (Newman, 1996) as listed below:

UNIT1110987654321

ROCK TYPELate Mafic DikesGraniteDioriteAnorthositeGabbroic-AnorthositeLeucogabbro, Anorthositic-GabbroGabbroGabbronoriteNoritePyroxeniteMetasedimentary Gneiss

Anorthosite was identified on the basis of ^"/o mafic component. The anorthosite is typically medium- to coarse-grained and composed of plagioclase with minor ^50Xo), interstitial black amphibole after clinopyroxene. Minor zones of black anorthosite were also observed with up to 707o magnetite. The anorthosite phase is the most dominant rock type on the north grid.

Gabbroic Anorthosite contains between 5 07o and 1507o mafic minerals. These rocks are typically medium- to coarse-grained and composed of plagioclase laths with interstitial black amphibole after clinopyroxene. Textures vary from massive to gneissic.

Leucogabbro, or anorthositic gabbro, is characterized as having between 15 and 4007o mafic minerals. The rock is composed of cumulate, medium-grained plagioclase with intercumulate black amphibole after clinopyroxene. Texturally this unit varies from massive to gneissic. Gneissic leucogabbro was common on the northern portion of the grid and consists of alternating plagioclase bands and amphibole-garnet-biotite bands..

18

Gabbro is defined as having greater than 4007o mafic component, with less than 100Xo of the mafic component being cumulate. The gabbros observed on the property typically consist of fine- to medium-grained cumulate plagioclase in a dark green amphibole- chlorite matrix. The gabbros generally occur along the margins of the intrusion and as an east-west trending unit across the north of the grid.

Gabbronorite is defined when good cumulate mafic mineral textures are observed. The rock is composed of greater than 4007o mafic cumulates with subhedral plagioclase and minor interstitial magnetite.

Norite is defined when cumulate orthopyroxene can be identified.

Late Mafic Dikes which crosscut the River Valley Intrusion are magnetite-rich, relatively unaltered and unmetamorphosed.

Well-preserved, primary, igneous layering consisting of alternating anorthosite and leucogabbro layers up to 25m thick was observed on one outcrop the west end of the grid at L2+OOE/4+OON.

Granite to Granitic Gneiss occurs to the north of the intrusive contact and is the predominant lithology on the east half of the North Grid. This unit is medium-grained granodiorite to monzogranitic gneiss.

AnalysesThe samples were shipped via courier to XRAL Laboratories, Rouyn-Noranda, Quebec, for analyses. All samples were assayed for Au, Pt, Pd, Cu and Ni. All precious metal concentrations were determined using fire assay (30g charge) followed by a direct coupled plasma/mass spectormeter (DCP) finish. The detection limits for a one assay ton (30g) sample are 1ppb for Au and Pd, and 10ppb for Pt. Base metal concentrations were determined by atomic absorption spectrometry after 0.25 to 0.3g of the pulp was subjected to an nitric aqua regia digestion. Six samples were also submitted for whole rock analyses (major element oxides, LOI and several other trace elements) using x-ray fluorescence spectrometry (XRF) on a fused disc prepared from a 2g sample. The detection limits for all of the major oxides are 0.01 07o except for TiO2 at 0.001 0Xo.

All of the samples that contain anomalous to highly anomalous PGM will also be submitted for Rh (rhodium) assays. Additionally, a selected number of samples of the reject material remaining from the samples that were processed at XRAL will be submitted to another laboratory for check analyses.

Results of Geological Mapping ProgramA program of geological mapping, sampling and prospecting was initiated over the North Grid to locate and test any sulphide occurrences for PGM enrichment and explore for the possible extension of PFN's Azen Creek Zone (samples up to 4.2g7t PGM and D.84%

19

Cu+Ni). This mineralization is located approximately 3km to the northwest of the North Grid and close to the intrusive contact. The assay results and whole rock data are summarized in Appendix 1, and assay certificates are given in Appendix 2. Included in these results are the major element oxides, LOI and several other trace elements. The North Grid Bedrock Geology Map (1:5000 scale), and the Sample Location and PGM Assay Data map in "bubble plot" format (1:5000 scale) are located in Pockets 1 and 2, respectively, at the back of this report.

The following observations and generalities are made based on the 1999 mapping program:

* The River Valley Intrusion in the vicinity of the North Grid is composed ofpredominantly anorthosite to gabbroic anorthosite and lesser leucogabbro. Gabbroic and noritic phases are absent in this area. Metamorphic grade appears to attain at least amphibolite grade. Petrography will assist in rock identification and metamorphic grade determination.

* The location of the intrusive contact in this area is not where previous mapping had indicated. In fact the contact was oriented at a steeper angle and located approximately 500-600m further south than anticipated.

* The intrusion exhibits variable degrees of recrystallization and primary clinopyroxene has been commonly replaced by black amphibole. Minor deformed, gneissic domains are also present.

* Alternating anorthosite and leucogabbro layers up to 25m thick were observed on one outcrop the west end of the grid at L2+OOE/4+OON.

* The rocks contained nil to trace amounts of pyrite, pyrrhotite and chalcopyrite and only weak rust staining.

* The best mineralization, in terms of PGM concentration (2503ppb), occurs adjacent to the intrusive contact within a coarse-grained, relatively unmineralized, slightly rusty anorthosite approximately 250m from the intrusive contact.

* No evidence of any previous exploration activity was observed.

AssaysOf the 83 samples that were submitted for assay, on sample contained greater than 1000ppb PGM (57157 - 2503ppb PGM). Additionally, approximately 607o of the samples contained greater than 100ppb PGM. Interestingly, Easton and Hrominchuk (1999) report that, based on their more regional sampling of mineralized and unmineralized rocks from the area, samples containing between 70 to 140ppb PGM and 70 to 140ppm Cu are anomalous. Samples containing higher concentrations (i.e. greater than 140ppb PGM and 140ppm Cu) are described as highly anomalous. Statistical data for the South Grid samples are summarized below:

Average PGMStandard DeviationRangeNumber

69ppb275ppb0 to 2503ppb83

20

It should be noted that the samples show a strong negative skew towards lower PGM concentrations and this will consequently result in a relatively large standard deviation.

Platinum/palladium (Pt/Pd) rations show considerable variation for the North Grid sample population. Ratios range from 0.19 up to 11.0, but generally fall around 1.0 to 3.0 in lower concentrations and anomalous levels. In the single highly anomalous sample the ratio is 0.3. The significance of this observation is currently unclear, but is likely related to the processes that resulted in the concentration of PGM in the well-mineralized zones. Another interesting point to note is that highly anomalous copper values do not necessarily correspond with highly anomalous PGM concentrations, and vice versa. This suggests that systematic sampling of rock units may be a safer strategy, rather than simply focusing on rocks with rust-stains or visible sulphides.

LithogeochemistrySix representative samples of the River Valley Intrusion in the North Grid area were selected for whole rock and trace element analyses by XRF. These results are presented in Appendix 1. Plots derived by Irvine and Baragar (1971: Alkalies-Silica) and Jensen (1976: Jensen Cation) are used to characterize the intrusive rocks of the River Valley property.

As the Alkalies-Silica plot (Figure 7) illustrates, all of the intrusive rocks of the River Valley Pluton have a subalkalic affinity. On the Jensen Cation plot (see Figure 8), the River Valley intrusive rocks from the North Grid plot in the calc-alkalic, tholeiitic and komatiitic fields and define a rhyolitic to komatiitic trend. Interestingly, three samples that were identified in the field as anorthosite (2) and leucogabbro (1) plot in the basaltic komatiite field. This suggests that these rocks are probably more gabbroic in composition.

21

Figure 7: Alkalies-Silica Plot for River Valley Intrusive Rocks, North Grid Rocks

M M

20

18

~ 16

14

O 12CM

10

Irvine 8t Baragar, 1971

CO ft8

4

2

O

Alkaline

oo o

SubAlkaline

35 40 45 50 55 Si02

60 65(wt 'X)

70 75 80 85

Figure 8: Jensen Cation Plot for River Valley Intrusive Rocks, North Grid

FeO TIO2

AI2O3 Cation 7o Jensen, 1976

MgO

LEGEND

* Anorthosite (8)o Gabbroic Anorthosite (7)" Leucogabbro (6)A Gabbro (5)* Diabase Dike (11)

23

CONCLUSIONS AND RECOMMENDATIONS

The results of the 1999 mapping, sampling and prospecting program, designed to test the River Valley Intrusion in the North Grid area for PGM potential were encouraging. Up until most recently, the River Valley Intrusion has received very little systematic exploration for Cu-PGM mineralization. Anomalous to highly anomalous PGM concentrations were detected in several areas that should be investigated further. Other interesting and/or significant results include:

1. The North Grid is underlain by predominantly anorthosite, gabbroic-anorthosite to leucogabbro. Granite to granitic gneiss is the predominant rock type on the east end of the grid.

2. The northern contact was examined at one location on the grid and appeared to be primary.

3. No evidence of any previous exploration (prior to Mustang) was observed.

4. The mapping and sampling program has verified that the anorthositic rocks adjacent to the north intrusive contact yielded highly anomalous PGM concentrations.

Following are a series of recommendations for the next phase of exploration on the River Valley PGM Property:

1. In light of the results of the 1999 mapping program and the recent exploration results from the PFN property to the northwest, exploration should be mainly focussed along the primary contacts of the intrusion. The contacts should be covered with an IP survey (~1000m per line; 500m of intrusion to contact and 250m additional coverage to the north and south) in order to delineate sulphide concentrations.

2. Follow-up to the IP should include trenching and stripping over selected anomalies in areas with thin overburden cover.

3. Wherever possible, detailed geologic mapping should also be conducted over the contact zone mineralization in order to document the width and characteristics of the marginal and inclusion-bearing rocks in these areas.

4. Diamond drilling should then test the continuity of the best targets at depth.

24

Certificate of Qualification

l, Peter C. Wood, of the city of Timmins, Province of Ontario, Canada, do hereby certify that:

1. l am a practising consulting geologist with Geodigital Mapping Systems Inc., with an office at 637 Algonquin Blvd. East, Timmins, Ontario, and a mailing address of P.O. Box 983, Timmins, Ontario, P4N7H6;

2. l am a graduate of the University of Toronto, Ontario with an Honours Bachelor of Applied Science Degree (1983) in Geological Engineering and Applied Earth Sciences (Exploration Option), and a Master of Science Degree (1987) in Economic Geology;

3. l have been practising my profession as a geologist in Ontario, Quebec, and the Northwest Territories since 1987;

4. The information contained in this report and accompanying maps is based on personal observations and direct supervision of the field work; and,

5. l hold no interest, directly or indirectly in the properties of Mustang Minerals Corp. nor do l expect to receive any interest or considerations from Mustang Minerals Corp. except for regular fees for work completed.

Dated this 14th day of February, 2000, Timmins, Ontario

Peter C. Wood, B.A.Sc., M.Sc.

25

REFERENCES

Assessment Files: Dana Township Files; Ministry of Northern Development and Mines, Sudbury Ontario

Ashwal, L.D. and Wooden, J.L.1989: River Valley Pluton, Ontario: a late-Archean/early proterozoic anorthositic intrusion in the Grenville Province; Geochimica et Cosmochimica acta, v. 53, p.633-641.

Barnett, P.J., Henry, A.P. and Baubin, D.1991: Quaternary geology of Ontario, west-central sheet; Ontario Geological Survey, Map 2554, scale 1:1 000 000.

Easton, R.M. and Hrominchuk, J.1999: Geology and Copper-Platinum Group Element Mineral Potential of Dana and Crerar Townships, River Valley Area, Grenville Province, Project Unit 99-07; in Summary of Field Work and Other Activities 1999, Ontario Geological Survey, Open File Report 6000, p. 30-1 to 30-35.

Hrominchuk, J.1999: Geology, Stratigraphy, and Copper-Platinum Group Element Mineralization of the River Valley Intrusion, Dana Township, Project Unit 99-07, in Summary of Field Work and Other Activities 1999, Ontario Geological Survey, Open File Report 6000, p. 31-1 to 31-9.

Jensen, L.S.1976: A New Cation Plot for Classifying Subalkalic Volcanic Rocks; Ontario Division of Mines, Miscellaneous Paper 66, 22p.

Lumbers, S.B.1973: River Valley Area, Districts of Nipissing and Sudbury; Ontario Division of Mines Prelim. Map P.844.

Newman, C.R.1996: Report on the 1995 Geological and Geochemical Exploration on the River Valley Project, Sudbury Mining District, Ontario (Project 3011), 30p.

Patrie, D.1999: Geophysics Report on the River Valley PGE Property, North Grid, District of Nippissing, Sudbury Mining Division for Mustang Minerals Corp., 10pp.2 maps.

26

APPENDIX lSummary Tables of Assay and Whole Rock Data

River Valley Property, North Grid - Sample Descriptions and Assay Data

Sample #570765707757078570795708057081570825708357084570855708657087570885708957090570915709257093570945709557096570975709857099571005710157102571035710457105571065710757108571095711057111571125711357114571155711657117571185711957120

LocationEasting

218205205205195326412395400402410405400

1000985

100512151190118011901195810820602590600800800

14031400160516051610181018001805162514451398200020102008221022352210

Northing35

125175405705

1010955800575400

45290328

136014051406885300155120

95525280109600810

1075845720900675565345540708980980998

13001000900600325600656

Rock TypeAnorthositeLeucogabbroAnorthositeLeucogabbroLeucogabbroAnorthositeAnorthositeLeucogabbroAnorthositeAnorthositeLeucogabbroAnorthositeLeucogabbroAnorthositeGabbroic AnorthositeLeucogabbroLeucogabbroAnorthositeAnorthositeAnorthositeAnorthositeGabbroic AnorthositeGabbroic AnorthositeAnorthositeLeucogabbroLeucogabbroAnorthositeAnorthositeLeucogabbroLeucogabbroAnorthositeAnorthositeAnorthositeAnorthositeLeucogabbroGabbroic AnorthositeLeucogabbroLeucogabbroLeucogabbroAnorthositeAnorthositeGabbroic AnorthositeLeucogabbroLeucogabbroAnorthosite

Grain SizeM.G.M.G.C.G.M.G.C.G.C.G.C.G.C.G.F.G.C.G.C.G.M.G.F.G.C.G.M.G.M.G.M.G.M.G.M.G.M.G.M.G.M.G.C.G.M.G.M.G.M.G.C.G.C.G.C.G.M.G.M.G.C.G.M.G.M.G.M.G.C.G.C.G.M.G.M.G.C.G.M.G.C.G.M.G.C.G.M.G.

SulphidesNilNilNilNilNilNilNilRustyNilNilNilRustyNilNilTr py.po.cpyNilNilNilNilNilNilRustyNilNilNilRustyRustyRustyRustyNilNilRustyRustyNilNilRustyRustyNilRustyNilRustyNilNilNilRusty

Mag Sus.8.050.15

30.250.15

2.51.2

0.351.85

1.20.17

3.50.25

30.450.450.15

7.55

121.2

0.130.25

20.130.15

5.50.6

0.150.2

1.351.510

3.50.170.150.150.150.354.53.5

0.150.1

0.221.35

AssaysAu ppb

12396633746334

111742443

132

118545

1136437834

1646645473

Pt ppb48

^028

•:10•:10

14*:10

14•:10

15*:10^0*:10

157511

^02222172123

^0^0•:10^0•dO

39•^10

13^0

12262212

^0151613

^01016

^01513

Pd ppb52

623

68

404122

71312

75

224845

52764

118

166

149

25101221

94537

72217

3122024187

2267

Pt+Pd+Au ppb

1129

60121457444311341510

948

14060

728332638361924111814751331252478672226482331263839114483

Pt/Pd

0.92

1.22

0.35

0.64

1.15

0.681.560.24

11.003.142.835.252.09

1.56

1.08

1.330.580.591.71

0.885.331.08

0.420.89

0.680.19

Cu ppm

3713

10354122718

171614145322238

32137213830396742494724165365

92

48333373213071

376544822

81313

Ni ppm216

6292213191636225013521638

1363452302794182141

160352098211310245262

4101922171580

1122311191620

Ni/Cu

0.22.23.62.50.91.41.14.82.80.83.50.61.41.02.41.10.41.31.10.43.72.01.20.30.70.80.53.10.70.22.00.60.50.21.11.44.20.21.00.52.10.52.41.21.5

River Valley Property, North Grid - Sample Descriptions and Assay Data

Sample #5712157122571235712457125571265712757128571295713057131571325713357134571355713657137571495715057151571525715357154571555715657157571585715957160571615716257163571645716557166571675716857169

LocationEasting

22002390240024052170219019802612299529953001298528002795280031985025498048104610420041504580380037953800381537953807380536103590360032003195320034003400

Northing985985700450

1240122010751450630318280220

30185255150

-135-575

-1025-510-750-655-675-7651-710-615-518-500-395j-185-385-430-575-640-510-410-428-538

Rock TypeAnorthositeGabbroic AnorthositeLeucogabbroLeucogabbroGraniteAnorthositeAnorthositeGraniteGraniteAnorthositeAnorthositeAnorthositeAnorthositeAnorthositeAnorthositeGraniteGranite Gneiss/sedimentsGabbroLeucogabbro (diorite?)AnorthositeAnorthositeAnorthositeAnorthositeAnorthositeAnorthositeAnorthositeAnorthosite (diorite?)AnorthositeGraniteGraniteAnorthositeAnorthositeAnorthositeAnorthositeAnorthositeAnorthositeAnorthositeAnorthosite

Grain SizeM.G.M.G.M.G.M.G.M.G.M.G.M.G.F.G.F.G.M.G.M.G.M.G.M.G.M.G.M.G.F.G.F.G.F.G.M.G.F.G.F.G.F.G.F.G.C.G.M.G.C.G.F.G.F.G.F.G.F.G.F.G.F.G.C.G.C.G.C.G.C.G.M.G.C.G.

SulphidesRustyRustyNilNilNilRustyRustyNilNilNilRustyRustyNilRustyNilRustyNilNilNilNilNilNilNilRustyNilRustyTrpyRustyRusty1-307opyNilTrpyNilNilNilNilNilNil

Mag Sus.25

7.50.420.180.13

55

0.350.852.55

95.54.67.55.8

1.059.510

0.258.58.5

913.32.62

258.75

AssaysAu ppb

332

111

•ei

3134233721361

•:13

•:11

•si4

5832

46•:1*:171431222

Pt ppb•:10•:10

3020

*:10^0^0•:10•:10

10291617

104^0":10

12•:10

13^0•:10•C10^0•:10

11535

20^0

11•:10

111704665

•^10

581820

Pd ppb67

3640

4•el

3334

3618384531

94593

10*:1•:12010

191032•M•elt1

717744241525

713

Pt+Pd+Au ppb

9106871

50646

18673758

1563310191123

313

01

2025

250355

257

018

418949216852735

Pt/Pd

0.830.50

2.500.810.890.452.31

3.00

1.44

1.100.280.63

1.570.961.052.71

2.322.571.54

Cu Ppm

294550

11526

848

5703131481236305019401826

1413528

935669537465879

1090441614522840

Ni ppm786736

24502015

19015

12636303121

255306933462347794952242155

1403015

13552

20024222126

44425

Ni/Cu

27.116.40.50.40.81.94.03.01.81.21.00.61.87.11.01.41.71.21.31.80.61.41.92.70.60.81.50.80.32.30.70.20.51.41.50.5

15.90.6

Statistical DataAverage PGMStandard DeviationRangeNumber

69 ppb275 ppb

0 to 2503 ppb83

River Valley Property, North Grid - Whole Rock Data Summary

Sample Ident Analysis Unit Detection Limit

570835711057127571355715057157

Easting

39518001980280048103800

Northing

800708

1075255

-1025-615

Rock Type

LeucogabbroLeucogabbroAnorthositeAnorthositeDioriteT/LeucogabbroAnorthosite

SIO2%

0.0151.749.550.451.551.352.5

AI203%

0.015.7427.38.9714.621.711.5

CaO"X,

0.017.5914.36.1712.611.57.61

MgO"k

0.0116.82.5219.19.845.0315.2

Na20'k

0.010.532.090.921.652.721.33

K20V,

0.010.11

0.20.140.130.540.14

Fe203%

0.0114.73.3713.38.845.51

11

MnO"X.

0.010.280.050.220.18

0.10.21

Ti02"h

0.0010.8040.126

0.250.22

0.1720.182

P205Ve

0.010.110.010.020.020.020.02

Cr203"h

0.010.080.030.170.080.030.09

LOI%

0.000.650.650.450.35

1.40.25

Sum%

0.0199.1

100.1100.1100.1100.1100.1

Mg No.

69.459.774.068.864.473.2

RbPPM

2346784

SrPPM

212

305104156278154

YPPM

211-255

-2-2

ZrPPM

244

713101113

NbPPM

22

-2-2-2-2-2

BaPPM

2023876686

11376

APPENDIX 2Assay and Whole Rock Certificates

XRAL LES LABORATOIRES XRAL LABORATORIESUNE DIVISION DE l A DIVISION OF SGS CANADA INC.

129 AVE. MARCEL BARIL - ROUYN-NORANDA * QUEBEC J9X 7B9TEL: (819) 764-9108 FAX: (819) 764-4673

CERTIFICAT D'ANALYSE/CERTIFICATE OF ANALYSIS

Nom de la Compagnie/Company: Mustang Minerals CorporationBon de Commanda No/ P.O. No:ProjetX Project No : RVALDate Sounds/ Submitted : Nov 19, 1999Attention : Ken Lapierre

R17259

Dec 02, 1999

No. D' Echantillon Sample No.

5683156832568335683456835568365c3375683856839568405684156842568435684456845568465684756848568495685056851568525685356854568555685656857568585685956860568615686256863568645686556866568675686856869

AU PPB

10567754455434955512610134449526914213135443432•ci

PT PPB

80222079•clOtlO2221*:10392515-clO39233411471116183724•clO12163512001534010201927•clO•clO•clO•clO1914

PD PPB

^2 ^yo-^-'r^~^ C*i^c\.

201073321292281684141117^31•ci21512915525301196113681040311119261^ /7^ ^7^/

Certifie par ,/ Certified by

Merribre du Groupe SGS (Societe Generate de Surveillance)

LES LABORATOIRES XRAL LABORATORIESUNE DIVISION DE l A DIVISION OF SGS CANADA INC.

129 AVE. MARCEL BARIL * ROUYN-NORANDA - QUEBEC J9X 7B9TEL: (819) 764-9108 FAX: (819) 764-4673


Norn de la Compagnie/Company: Mustang Minerals CorporationBon de Corranande No/ P.O. No:Pro jet X Project No :' RVALDate Sounds/ Submitted : NOV 19, 1999Attention : Ken Lapierre

R17259

Dec 02, 1999

No. D' Sample

568705687156872568735687456875568765687756878568795688056881568825688356884568855688656887568885688956890568915704157042570435704457045570465704757048570495705057051570535705457055570565705757058

Echantillon AU No . PPB

^4413692173•ci•ci^l453242236193220951265511556755

PT PPB

*:10-clO•clO•clO1815231265635•clO•clO^02611121210•clO12102513176142803011261717143539132017^027

PD PPB

e ^5cJ^A.^V^ C-i f~i cA.

524145281^1710

oj^t3<l46646-ci1750151441558320164265411158131198

Membre du Groups SGS (Society Generate de Surveillance)


129 AVE. MARCEL BARIL - ROUYN-NORANDA ' QUEBEC J9X 7B9TEL: (819) 764-9108 FAX: (819) 764-4673


Nom de la Compagnie/Company: Mustang Minerals CorporationBon de Commande No/ P.O. No:Projet X Project No : RVALDate Sounds/ Submitted : Nov 19, 1999Attention : Ken Lapierre

R17259

Dec 02, 1999

No. D'Echantillon Sample No.

57059570615706257063570645706557066570675706857069570705707157072570735707457093570945709557096

AU PPB

84868564498644944313

PT PPB

54174417451524132128152718221622221721

PD PPB

20 ^c^W, C,^3113188853214•ci98532 NJ o- -V^ C^ f^.-.^-

1 i4 V

Membre du Groupe SGS (Societe Generate de Surveillance)

Page l


129 AVE. MARCEL BARIL - ROUYN-NORANDA - QUEBEC J9X 7B9TEL: (819) 764-9108 FAX: (819) 764-4673


Norn de la Compagnie/Company: Mustang Minerals CorporationBon de Commande No/ P.O. No:Projet/ Project No : RVALDate Sounds/ Submitted : Dec 06, 1999Attention : Ken Lapierre

R17378

Dec 10, 1999

No. D'Echantillon AU Sample No. PPB

569075690856909569105691156912569135691456915569165691756918569195692056921570915709257097570985709957100571015710257103571185711957120571215712257123571245712557126571275712857129571305713157132

Certifie par

4355121337301743222542211854511473332111•ci313423

/ Certified

PT PPB

•clO10141213316772912717•clO•clO171611•clO23•clO•clO•clO•clO•clO39•clO1513•clO•CIO3020•clO•clO<10<10•clO102916

bv :

PD AG CU NI CO PPB PPM PPM PPM PPM

11 JSo-xV-w Ci^c-v.13 b33 y169284258675145821744184 5 ^ o ' "^ ^ •^'A..5 j11 ^816614925722676736404•ci33343618 .^f^/

/t@SMembre du Groupe SGS (Societe Generate de Surveillance)




Norn de la Compagnie/Company: Mustang Minerals CorporationBon de Coinmande No/ P.O. No -Projet7 Project No \ RVALDate Soumis/ Submitted : Dec 06, 1999Attention : Ken Lapierre

R17378

Dec 10, 1999


5713357134571355693756938569395694056941569425694356944569455694656947 56948 569495695056951569525695356954569555707657077570785707957080570815708257083570845708557086570875708857089570905710457105

AU PPB

37251525433393157 11 85161053512396633746334111736

PT PPB

17104•clO282012152215•clO1110•clO•clO •clO 19•clO221325301348•clO28•clO•clO14•clO14•clO15•clO•clO•clO1575•clO13

PD AG PPB PPM

38 isj o ,' i-^45 J31 ^23 Sv~*r^

1? 14 *1114102193067 5.5 2 1.1 174461936272252 KJo.-f^6 ,23 ^68404122713127522481012

CU NI CO PPM PPM PPM

C,^

C^\ f \.*A

24920 142 53 392 32 13

CA ri f{

Membre du Groupe SGS (Soctete G6n6rale de Surveillance)

fage


129 AVE. MARCEL BARIL - ROUYN-NORANDA * QUEBEC J9X 789TEL: (819) 764-9108 FAX: (819) 764-4673


Norn de la Compagnie/Company: Mustang Minerals CorporationBon de Connnande No/ P.O. No:Projet l Project No : RVALDate Soumis/ Submitted : Dec 06, 1999Attention . Ken Lapierre

R17378

Dec 10, 1999


571065710757108571095711057111571125711357114571155711657117569225692356924569255692656927569285692956930569315693256933569345693556936568925689356894568955689656897568985689956900569015690256903

AUPPB

43783416466456942424941042243383455343228441247

PT PPB

•clO12262212•clO151613•clO101654361815•clO234812772816•clO1522•clO20•clO-clO1014•clO16•clO4017100466

PD AG CU NI CO PPB PPM PPM PPM PPM

21 ^ ' *"*~ C- f -945377??4* 4*

17312?0tt \J

74 ^ 1 Qlo47 ,^'O^V-V-N d/i^A30 |56 J/7429AJ J

9S6* -J

535"5 Q JO

4

937

2045

41515c; QJO

14105392

Membre du Groupe SGS (Society Generate de Surveillance)

Page l


129 AVE. MARCEL BARIL - ROUYN-NORANDA - QUEBEC J9X 7B9TEL.: (819) 764-9108 FAX: (819) 764-4673


Norn de la Compagnie/Company: Mustang Minerals CorporationBon de Commands No/ P.O. No:Projet/ Project No \ RVALDate Soumis/ Submitted : Dec 06, 1999Attention . Ken Lapierre

R17377

Dec 10, 1999

No. D'Sample

571365713757138571395714057141571425714357144571455714657147571485697656977569785697956980569815698256983569845698556986569875698856989569905695656957569585695956960569615696256963569645696556966

Echantillon AU No . PPB

13411•ci*cl11113442313•ci•ci<l<l<l3112<l4•ci11<l17<l<l<l2<l•ci5N/S<l

Certifie par / Certified^

PT PPB

<101224•clO•clO<1013•clO101741713•clO<101524•clO<102132<1011214217•clO<102918262323<10381422•clON/S35

-Sfc-i -

PD PPB

9 Ni o ' V"V C* ruA.4 i37 jSo~^ (Strxi-Ao n6 U i

6 V9956109237?7^t 1

16?lfj J-

51719111451120321 Q J.O

1971?.J ^

36TO /. O

19?3^t ~J

1039162630N/S

/l^Mejjjbr&j&rGroupe SGS (Societe Generate de Surveillance)




Norn de la Compagnie/Company: Mustang Minerals CorporationBon de Commanda No/ P.O. No:Projet7 Project No : RVALDate Soumis/ Submitted : Dec 10, 1999Attention . Ken Lapierre

R17452

Dec 15, 1999

No. D'Echantillon AU Sample No. PPB

571495715057151571525715357154571555715657157571585715957160571615716257163571645716557166571675716857169574115741257413574145741557416574175741857419574205742157422574235742457425574265742757428

Certifie par

61•ci3•ci1•ci4583246•ci•el71431222•ci3•ci247828134432773

7 Certified ^ —

PT PPB

•clO13•clO•clO•clO•clO•clO1153520•clO11<10111704665•clO581820131320•clO<10<10•clO<1014<103913•clO<10<10<10<10<10

by :

PD PPB

5 Nj o f t^ d < i ck~9 1l ^10<l•ci2D/j \J

10191032<l<l<l71774424 ^ ±1525t* -~)

71311 E?^-^- c^f^c*O C25 i11 v297213025b — '1

22o ZJ15

9617!x^/^rX^

(Societe Generate de Surveillance)

LES LABORATOIRES XRAL LABORATORIESUNE DIVISION DE l A DIVISION OF SGS CANADA INC

129 AVE. MARCEL BARIL - ROUYN-NORANDA - QUEBEC J9X 789TEL: (819) 764-9108 FAX: (819) 764-4673

CERTIFICAT D' ANALYSE/CERTIFICATE OF ANALYSIS

BonProiet/ Project NoDate Soumis/ SubmittedAttention

RVALjan 20, 2000 Ken Lapierre

R17259A

Jan 27, 2000

No. D' Sample

56831568325683356834568355683656837568385683956843c,r q t i•~i v- O -Z -L

5634256843568445634556346563475684856349563505635156852568535635456 8555635G56857568535635?563605686156362563635636456365568665636~5 6 B 6 ft5686?

Echantillon CU No . PPM

148546859144638810113343238621874681117138196103222951223616844552916981915161613132720

NI PPM

49 .Sc-t^ CrwA-19202049295423241799ft t*

17331530?4 t* i c. t. b403333171 7-L fi

2731274?^x t*

166•5 onA o y16355671?47^i^l

0 P ^ o3699f* ft

1 S -Lo172015 ^

C s rt i fie par 7 Certified bMembre du Groups SGS (Societe Generate de Surveillance)

t^age


129 AVE. MARCEL BARIL' ROUYN-NORANDA - QUEBEC J9X 7B9TEL.: (819) 764-9108 FAX: (819) 764-4673


Ncm de la Compagnie/Company: Ben de Commands No/ P.O. No: Projet/ Project No : Date Soumis/ Submitted :Attention :

Mustang Minerals Corporation

RVALJan 20, 2000Ken Lapierre

R17259A

Jan 27, 2000


56870563715637256873563745637556876568775637856879568805688156862563835638456885568865638756383563895639056391570415704257043570445704557046570475704857049570505705157 35357354570555~05b5735757053

CU PPM

314760623771581516453174106013325734292728221811181072706225495630297821184143321219

NI PPM

^ g ^*c? -^ *~^ d f v*^"

25272514739182471821002229211615191343151626132023611045131218162015141119211213919



129 AVE. MARCEL BARIL - ROUYN-NORANDA - QUEBEC J9X 789TEL: (819) 764-9108 FAX: (819) 764-4673


Nom de la Compagnie/Company: Mustang Minerals CorporationBon de Commanda No/ P.O. No:Frojet/ Project No : RVALDate Sounds/ Submitted : Jan 20, 2000Attention : Ken Lapierre

R17259A

Jan 27, 2000

Ne. D'Echantillon CU NI Sample No. PPM PPM

57059570615706257063570645706557066570675706857069570705707157072570735707457093570945709557096

416191221274026302618313119029633838303967

13111437101025186625914132030279418


fage .

XRAL LES LABORATOIRES XRAL LABORATORIESUNE DMSION DE t A DIVISION OF SGS CANADA INC.



Nom de la Compagnie/Company: Mustang Minerals CorporationBon de Commande No/ P.O. No:Projet/ Project No : RVALDate Soumis/ Submitted : Jan 20, 2000Attention : Ken Lapierre

R17378A

Jan 24, 2000


569075690856909569105691156912569135691456915569165691756918569195692056921570915709257097570985709957100571015710257103571185711957120571215712257123571245712557126571275712857129571305713157132

CU PPM

4819152033616135410747067262234414293721424947241653658131329455011526848570313148

NI PPM

17 s~~^ c.,^-14 L16 *212713424217716038251016281334 Kjo.-rv-v C,^A.5221 141160352098211916207867362450201519015126363031

Certifie par / Cert iMembra du Groupe SGS (Societe Generate de Surveillance)

ray c ^

XRAL LES LABORATOIRES XRAL LABORATORIESUNE DIVISION DE /A DIVISION OF SGS CANADA INC.



Norn de la Compagnie/Company: Mustang Minerals CorporationBon de Commanda No/ P.O. No:Projet l Project No : RVALDate Soumis/ Submitted : Jan 20, 2000Attention : Ken Lapierre

R17378A

Jan 24, 2000


571335713457135569375693856939569405694156942569435694456945569465694756948569495695056951569525695356954569555707657077 570785707957080570815708257083570845708557086570875708857089570905710457105

CU PPM

123630448645523171021226--1683084707787263713 1035412271817161414532223832192

NI PPM

21 Kj D ,ev, C,^

255 i3013 S^~^ C,,^13 |15 f14161418123018--96910111620 s-216 Njo.-n~ 0~*A

6 \ 29 V22131916362250135216381361310

Membre du Groupe SGS (Societ6 Generate de Surveillance)

ray fei


129 AVE. MARCEL BARIL - ROUYN-NORANDA. QUEBEC J9X 789TEL: (819) 764-9108 FAX: (819) 764-4673


Nom de la Compagnie/Company: Mustang Minerals CorporationBon de Commande No/ P.O. No:Projet/ Project No : RVALDate Sounds/ Submitted : Jan 20, 2000Attention : Ken Lapierre

R17378A

Jan 24, 2000


571065710757108571095711057111571125711357114571155711657117569225692356924569255692656927569285692956930569315693256933569345693556936568925689356894568955689656897568985689956900569015690256903

CU PPM

4833337321307137654482245121063313824880212782812457322514144010921904788552400

NI PPM

24 Nlo.'t"^ c^i^'A52 i.62 V410192217158011223118 S* *~ V-v^ C~ ^10 .7 V1518172326201115151733173222221426131811221588028

Membre du Groupe SGS (Sotiete Generale de Surveillance)

Fac . .

XRALLES LABORATOIRES XRAL LABORATORIES

UNE DIVISION DE y A DIVISION OF SGS CANADA INC.129 AVE. MARCEL BARIL - ROUYN-NORANDA - QUEBEC J9X 7B9

TEL: (819) 764-9108 FAX: (819) 764-4673


Norn de la Compagnie/Company: Mustang Minerals CorporationBon de Commande No/ P.O. No:Projet/ Project No : RVALDate Sounds/ Submitted : Jan 20, 2000Attention : Ken Lapierre

R17377A

Jan 25, 2000


571365713757138571395714057141571425714357144571455714657147571485697656977569785697956980569815698256983569845698556986569875698856989569905695656957569585695956960569615696256963569645696556966

CU PPM

50194632382662430352138406455508149202581878641777775233746976801025370330N/S38

NI PPM

g (J Kjc^-r-^ C\ r^e*-

33 ^22 ^o^.'r^ (^c^c^26 .182 V20171217161715190291623141215181930261816181417882019161619171818N/S15

Certifie par / CertifiMembre du Groupe SGS (Sotiete Centrale de Surveillance)

raye x


129 AVE. MARCEL BARIL ' ROUYN-NORANDA - QUEBEC J9X 7B9TEL: (819) 764-9108 FAX: (819) 764-4673


Nom de la Compagnie/Company: Mustang Minerals CorporationBon de Commands No/ P.O. No:ProjetX Project No : RVALDate Soumis/ Submitted : Jan 20, 2000Attention : Ken Lapierre

R17452A

Jan 25, 2000

No. D' Sample

571495715057151571525715357154571555715657157571585715957160571615716257163571645716557166571675716857169574115741257413574145741557416574175741857419574205742157422574235742457425574265742757428

Echantillon CU No . PPM

40182614135289356695374658791090441614522840959217519177277111099028513163391133849

NI PPM

4 g ^-Jov'"^ C^f^^.21 i * J47 v7949522421551403015135^2J A*20074^t *±

72 ft ft21 ft j.o c.z o44425 ft j _ ~ .•50 ^CS-^-^V-N C-i .rvcX.ft LA

27 l *^ i17 *1 2A, fi

124223f* —J

113120303727 ^ 161047 *± i1513

Certifie par f Certified b© Membre du Groups SGS (Soci6t6 G6n6rale de Surveillance)

.nd winesDeclaration of Assessment Work Performed on Mining LandMining Act, Subsection 65(2) and 66(3), R.S.0.1990

Transaction Number (office UM)

VJOQIQ.Assessment Files Research Imaging

lubsection 65(2) and 66(3) of the Mining Act. Under section 8 of the Mining Act isesnent work and correspond with the mining land holder. Questions about this rthem Development and Mines, 3rd Floor, 933 Ramsey Lake Road, Sudbury.

41I09NE2008

Instructions:

2.20092 MCWILLIAMS 900

For work performed on Crown Lands before recording a claim, use form 0240. Please type or print in ink,

1. Recorded holder(s) (Attach a list if necessary)Name C** Numb*

Telephone Number

7MO -1A3T-FaxNumber

Name

RECORDS;Client Number

Address Telephone Numberfte-Fax Number

2. Type of work performed: Check K) and report on only ONE of the following groups for this declaration.Geotechnical: prospecting, surveys, assays and work under section 18 (regs)

Physical: drilling stripping, trenching and associated assays

Rehabilitation

Work Type ^e0^ca\

yData* Work From PvrfofiNod K: , \ \ , qQ TO H , 07- , OD

l Month | Ye*r D*y | Month | YdrGlobal Positioning System Data (if available)

A-'t^-OQ j AA.CvO\\M C^^V'b 1^0M or G-Plan Number

Office UseCommodityTotal S Value ofWork Claimed 3 1. ^/BNTS Reference

Mining Division (SvtirltY Lt^JxResident Geologist., J District rtAJidfoK-UJ

Please remember to: - obtain a work permit from the Ministry of Natural Resources as required;- provide proper notice to surface rights holders before starting work;- complete and attach a Statement of Costs, form 0212;- provide a map showing contiguous mining lands that are linked for assigning work;- include two copies of your technical report.

3. Person or companies who prepared the technical report (Attach a list if necessary)

Certification by Recorded Holder or Agent 2 . 2 0 0 9, do hereby certify that l have personal knowledge of the facts set

2forth in(PhnlNamc)

this Dedaration of Assessment Work having caused the work to be performed or witnessed the same during or after its completion and, to the best of my knowledge, the^annexed report is true.Signature of Recorded Holder or Agent Date

FaxNumber

0241(0*97)

5. Wock to be recorded and distributed. Work can only be assigned to claims that are contiguous (adjoining) to the mining land whore work was performed, at the time work was performed. A map showing the contiguous link must accompany this form. - . DOC *J-8Mining Claim Number. Or If work was dona on other eligible mining land, show In this

column the location number indicated on the claim map.

eg

eg

eg

1

2

3

4

5

6

7

8

g10

1112

13

14

15

TB7827

1234567

1234568

\na \ST^m^^nQA\5^i'33^55

\2_ZJ3\UOpmio'M*\7L1 \74oCSP^ !;1^1

irV?5o-7tem SZ \t^VJSZT.I2/M7UO

Column Totals

Number of Claim Units. For other mining land, list hectares.

16 ha

12

2

\1.\ C)

\5\ i?\S\64-* .t

H\(j

Value of work performed on this dalm or other mining land.

S26,825

0

S 8,892

^yoT.DDOSoooyy\o^-73-0\s*^^-^"*^~^

MDfc

Value of work applied to this dalm.

N/A

524,000

54,000

?®ID

5ODO5~i o

koco^~boo x^tDO :

MUDl bo D^00\MV

\^1 Ift

Value of work assigned to other mining claims.

524.000

0

0

kooo

V^C?S^tf

l D^ 2..?r

Bank. Value of work to be distributed at a future date

52,825

0

54.892

Z-OOO

Zoo Dl. , do hereby certify that the above work credits are eligible under

(FHnt Full Name)subsection 7 (1) of the Assessment Work Regulation 6/96 for assignment to contiguous claims or for application to the claimwhere the work was done.

Agent Authorized in Writing

6. Instruction for cutting back credits that are not approved.

Some of the credits claimed in this declaration may be cut back. Please check (S) in the boxes below to show how you wish to prioritize the deletion of credits:

Js( 1. Credits are to be cut back from the Bank first, followed by option 2 or 3 or 4 as indicated. D 2. Credits are to be cut back starting with the claims listed last, working backwards; or D 3. Credits are to be cut back equally over ill rhjQTi IlitncJjpJft'un1rfO"ltinrr or O 4. Credits are to be cut back as prioritized on tiptpni&J&epperiairor fs follows (describe):

Note: If you have not indicated how your credits are to be deletj followed by option number 2 if necessary.

om the Bank first,

For Office Use OnlyReceived Stamp

0241 (03/97)

Deemed Approved Date

Date Approved

Date Notification Sent

Total Value of Credit Approved

Approved for Recording by Mining Recorder (Signature)

2

Ontario Ministry olNorthern Developmentand Mines

Statement of Costs for Assessment Credit

Transaction Number (-ilia use)

rsonal Information collected on this form Is obtained under the authority of subsection 6(1) of the Assessment Work Regulation 6/96. Under ;llon 8 of the Mining Act. the Information Is a public record. This Information will be used lo review the assessment work and correspond with i mining land holder. Questions about this collection should be directed lo the Chief Mining Recorder. Ministry of Northern Development and las. 6th Floor, 933 Ramsay Lake Road. Sudbury, Ontario. P3E 6BS.

Work TypeUnits of Work

Depending on the type of work, list the number of hours/days worked, metres of drilling, kilo metres of grid line, number of samples, etc.

Cost Per Unit of work

Total Cost

Geo\ QC\\. cal ?-\

2.

L,soclated Costs (e.g. supplies, mobilization and demobilization).

ip Tfi Ov\ 1 DU . 2.6,

Transportation Costs 3200*1T 50-008tM .

rotations of Filing Discounts:

rVork filed within two years of performance Is claimed at KXP/b of the above Total Value of Assessment Work, f work Is filed after two years and up to five years after performance, It can only be claimed at SOW of the Total /alue of Assessment Work. If this situation applies to your claims, use the calculation below:•OTAL VALUE OF ASSESSMENT WORK x 0.50 - Total $ value of worked claimed.

irk older than 5 years Is not eligible for credit.ecorded holder may be required to verify expenditures claimed In this statement of costs within 45 days of a est for verification and/or correction/clarification. If verification and/or correction/clarification Is not made, the iter may reject all or part of the assessment work submitted.

Iflcallon verifying cost*: o 20092(ptotie print turtfcame) ———~ ' do nerebv certlfy. 'hat the amounts shown are as accurate as may

wiably be determined and the costs were Incurred while conducting assessment work on the lands Indicated on

ccompanyfng Declaration of Work form as

ike this certification.

l am authorized

Ministry of Ministere duNorthern Development Developpement du Nordand Mines et des Mines Ontario

Geoscience Assessment Office 933 Ramsey Lake Road

March 21, 2000 6th FloorSudbury, Ontario

Ken Lapierre P3E 6B5MUSTANG MINERALS CORP.P.O. Box 1433 Telephone: (888) 415-9845Timmins, Ontario Fax: (877)670-1555P4N 7N2

Visit our website at: www.gov.on.ca/MNDM/MINES/LANDS/mlsmnpge.htm

Dear Sir or Madam: Submission Number: 2.20092

Status Subject: Transaction Number(s): W0070.00048 Approval

We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.

If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day Notice. Allowable changes to your credit distribution can be made by contacting the Geoscience Assessment Office within this 45 Day period, otherwise assessment credit will be cut back and distributed as outlined in Section #6 of the Declaration of Assessment work form.

Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the response date on the summary.

If you have any questions regarding this correspondence, please contact STEVE BENETEAU by e-mail at [email protected] or by telephone at (705) 670-5855.

Yours sincerely,

ORIGINAL SIGNED BYBlair KiteSupervisor, Geoscience Assessment OfficeMining Lands Section

Correspondence ID: 14693

Copy for: Assessment Library

Work Report Assessment Results

Submission Number: 2.20092

Date Correspondence Sent: March 21, 2000 Assessor:STEVE BENETEAU

Transaction First Claim Number NumberW0070.00048 1229152

Section:12 Geological GEOL

Township(s) l Area(s)DANA

StatusApproval

Approval Date

March 20, 2000

Correspondence to:Resident Geologist Sudbury, ON

Assessment Files Library Sudbury, ON

Recorded Holder(s) and/or Agent(s):Ken LapierreMUSTANG MINERALS CORP.Timmins, Ontario

Page: 1Correspondence ID: 14693

41I09NE2008

2.20092

MCWILLIAMS

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ae 10

Ministry ofNaturalResources

Ministry ofNorthern Developmentand Mines

Ontario

INDEX TO LAND DISPOSITION

PUN

G-2904 'TOWNSHIP

DANA

M.N.A. ADMIHISTRffnVE DISTRICT

NORTH BAYMIWNG DIVISION

SUDBURYLAND TITLES/REGISTRY DIVISION

NIPISSING

Seal* 1-20 000

two

(NO CM ri H rt

moo 2000--1 M*lfM

10M 3000 3000 4000 5000 .ODM 7000 WO 6 0000 10MO

Contour Interval 10

SYMBOLSBoundary

Township, Meridian, Baseline

Road allowance; surveyed shoreline

Lot/Concession; surveyedunsurveyed

Pare*!; surveyed .,..,.,.....,.,..,..,......unsurveyed ........................

Right-of-way; road - - - - - - - - - - - - - - - - - -railway utility

Reservation ..,..,.... .....,.............

Cliff, Ph, Pile................................

ContourInterpolatedApproximate ...... .. ....,..,..........

Depression - - - - - - - - - - - - - - - - - -

Control point {horizontal}..

Flooded land . .... .. . . .. .. ... .. ...Mine head frame

Pipeline (above ground}- - - - - - - - - - - -

Railway; single trackdouble track.,...........,.........abandoned

Road; highway, county, townshipaccess ....,.,..,.....................trail, bush .. .................... ....

Shoreline (original) - - - - - - - - - - - - - - - -

Transmission line..........................

Wooded area ..............................

20'

A

..., Q

-H—————H————H-

DISPOSITION OF CROWN LANDSPatent

Surface S Mining Rights .. .. . .. .. . .. .. .... ..... . ^Surface Rights Only-..............................,........ ^Mining Rights Only..,.,..,..,....,....,..,.......,..,....,. ^

LeaseSurface S Mining Rights - - - - - - - - - ^Surface Rights Only-........... ..................,....,... pMining Rights Only .........................................^

Licence of Occupation - - - - - - - - - - - - - - - - - - - - - - - - - - - ^

Order-in-Couticil............,.............,................... OC

Cancelled--- -...-.. ...............,...............,.......

Reservation - - - - - - - - - - - - - - - - - . . - . ..

Sand & Gravel....... ............... .. ....................

LAND USE PERMIT

AREAS WITHDRAWN FROM DISPOSTIQN

M.R.O. - MINING RIGHTS ONLY S.R.O. - SURFACE RIGHTS ONLY M.+S. - MINING AND SURFACE RIGHTS

Description Order No. Date Disposition File

*f **r W IJM 041. WytO MM (ffMHiit Aprt IJMB it TflO UI KIT.

) Sec. 35 W-LL-C182/99 ONT 11/05/99 M

A.P.-MQBO JUNE Mt* TO HAY

f. - ' - f ". . - *- ,

NOTES

SUBDIVISION OF THIS TOWNSHIP IMTQ LOTS AMD CONCMaiQNM WAS

THE INFORMATION THAT APPEARS OH THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCES, AND ACCURACY IS NOT GUARANTEED, THOSE WISHING TO STAKE MINING CLAIMS SHOULD CONSULT WITH THE MINING RECORDER MINISTRY OF NORTHERN DEVELOPMENT AND MINES. FOR ADDITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEREON.

Map base and land disposition drafting by Surveys and Mapping Branch, Ministry of Natural Resournes

The disposition of land, location of Jot fabric and parcel bourn d anas an this index was com p l led f or ad m in ist ra t i ve purposes only.

Spruce Ridge

10 10 1 9 .v. -.V.V.- x :: - : 10

A

Tag AlderThick Spruce*/; Bog '

Spruce \Bog

Poplar, Birch, \5pruce

(Az. 110')

.....10;10 LOW

Rolling i . ,..-'* BirchBirch, Spruce

HatBirch, -1Q

Spruce Poplar^~-~i.. - 1 "^ — '' 8 SpruceFlat

•.'••;SSon rf Ridge '-..10 \ \\

LOW-.A 8 Spruce r

\ *. - * ft*.--- ; ^ [57110 A S/oVs ... Spruce

Cedar'/Bog ,/

\ Open\Alder

Spruce ^ Bfrchf .. 'Poplar

BirchPoplar Spruce .. *-..

7 \ Spruce,

Pine .. Alder, Spruce

Spruce,Birch Poplar, --

Birch

Poplar, Birch

Poplar Spruce

Rolling Sahd

'.'•8 Spruce BirchLEGEND ABBREVIATIONS

/I/o'er, • ;g Poplarboulders

dark colouredfine-grainedgeophysically inferredgneissiclayered

: massive , standard iron barPyroxeniteGabbroic Anorthosite

chalcopyrite magnetite pyrrhotite pyrite

Leucogabbro Metasedimentary Gneiss

SYMBOLSMartin Creek •--1——-J— *r

.-I —— "^

;. x Outcrop, outcrop area; small outcrop

a60 Magnetic susceptibility

Gneissosity

Contact (defined, inferred)

Fault (geophysically inferred)

McwilliamsRiver Valley PGM Property Claim Location Map

A57164 Sample Location and number

Sulphide/Mineral ocurrence

Positive topographic feature

a Claim post (located, inferred)

- ' """ Claim lineGibbonsSwamp

Pond with Beaver damRIVER VALLEY PGM PROPERTYMAPI:

NORTH GRID BEDROCK GEOLOGY

Mustang-lmpala JV Property BoundaryRiver Valley

Intrusion^23TO63-- _____ ^__ f

l f ^

L Geodigital K Mapping l\ Systems LA Inc.Timmins, Ontario, Canada 705) 267-7128

LU O oH- CM

LU OO

LU O O4-CO

15+OON

14+OON

13+OON

12+OON

LU O O ± 00

LU O O4- o

LU O OH-CM

LU O O

LU Oo* CO

LU Oo4-00

LU O O•fo

Ld Q O

LU O O4- ^h CM

LU O O4- toCM

140toO

8

BL 10+OON (Az. 110e )

9+OON

8 + OON

7 + OON

6+OON

5 + OON

4 + QON

3+OON

2+OON

1+OON

0+00

1+OOS

57

43

14

60

1 1 12

44

••18

1111

34

10

14

28

33i

26

-- \

31

23

X

\

\

\

\

Y\

\\

48*26

\

22

24 •67

38

\\

26

\

-•^\

\

\

\

\

\

LU O O±COCM

LU Oo4 o

LU 0 \

?\LU OOH-

\

LU O O-f(OK)

Ld O OH-GO

Ld O O4- o

UJ Oo-f CM

LU O O

UJ O O * co

LJ O O-h o in

\\

\\

68

\

\\

\

11

\\\\

\

\

\\

\

\\\

33|

156

t58

\\\

\V^

y

,x

x

\

p

41I09NE2008 2.20092 MCWILLIAMS 230

(formarty Tf-imrr~Jnn --\2xeut) l OmrOQe,.^-L—^,. — ~ *-l- j---— — h214772r ' '

Mustang-lmpala Jv Property Boundary

PGM ASSAYS

Combined Pt+Pd+Au (ppb)

2" 1500 ppb ,

iMOOO-1500 ppb

l>500-1000 ppb

^00-500 ppb

l ^0-100 ppb

0-50 ppb

"

\

\\\

\\

\-

\

-

\\

\\\\\

\

\\\

\\

.* \\\

418 \55

XX

y

s

S

11

19

15+OON

14+OON

13+OON

12+OON

11+OON

BL 10+OON (Az. 110')

9+OON

8 + OON

7 + OON

6+OON

5+OON

4+OON

3+OON

2 + OON

1+OON

TL 0+00

1+OOS

2+OOS

3+OOS

4+OOS

5+OOS

6+OOS

2009 -KOQS

8+OOS

9+OOS

10+OOS23

Stotistico! Data Average PGM Standard Deviation Range Number

69 ppb 275 ppb

j O to 2503 ppb i 83

L Geodigital K Mapping IX Systems LA Inc.Timmins, Ontario, Canada (705) 267-7128

mRIVER VALLEY PGM PROPERTYMAP 2: NORTH GRID

SAMPLE LOCATIONS AND PGM ASSAY DATA

Drawn:GMSI

Date:Jan., 2000

Sampled:Todd Keost

Revised:

Province:Ontario

Scale:1:5,000

NTS:41-1/09

Drawing:North —Assays

O 100 200 300 400m

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