diamond drilling rpt chabanel twp - ontario...inc's facility in thunder bay. the 298 tonnes of...

ASSESSMENT REPORT ON

2005 – 2006 DIAMOND DRILLING ON THE

LEADBETTER DIAMOND PROJECT NTS 42C/2, Chabanel Township, Ontario

Centered at Latitude: 48o 03’ 57”N, Longitude: 84o 42’ 15”E or 671,030E; 5,326,160N (UTM, NAD83, zone 16)

For

3814793 CANADA INC.

AND

DIANOR RESOURCES INC. 649 – 3rd Avenue, 2nd Floor

Val-d’Or, Quebec J9P 1S7

Tel: 819-825-7090

By

Carl G. Verley, PGeo Amerlin Exploration Services Ltd.

2150 – 1851 Savage Road Richmond, B.C. V6V 1R1

Tel: 604-821-1088

May 26, 2008

ii

TABLE OF CONTENTS

1.0 Summary .................................................................................................................................. 1

2.0 Property, Location and Access ................................................................................................ 3

3.0 Accessibility Climate, Local Resources, Infrastructure and Physiography........................... 6

4.0 Geological Setting.................................................................................................................... 7

4.1 Regional Geology ................................................................................................................ 7

4.2 Property Geology............................................................................................................... 12

5.0 Drilling................................................................................................................................... 17

5.1 Exploration Work Summary ............................................................................................... 17

5.2 Phase 1 Diamond Drilling................................................................................................... 18

5.3 Phase 2 Diamond Drilling................................................................................................... 18

6.0 Sample Preparation, Analyses and Security .......................................................................... 22

7.0 Interpretation and Conclusions .............................................................................................. 23

8.0 Recommendations.................................................................................................................. 24

8.1 - Phase 1: Drilling and sampling......................................................................................... 24

8.2 - Phase 2: Sampling Program.............................................................................................. 24

9.0 References.............................................................................................................................. 25

10.0 Certificate of Qualification .................................................................................................. 28

LIST OF FIGURES

Figure 1. Location of Leadbetter project. ....................................................................................... 1

Figure 2. Claim Location Map........................................................................................................ 5

Figure 3. Regional stratigraphic setting of the Leadbetter Project ................................................. 8

Figure 4. Regional structural model for the Leadbetter Project area.............................................. 9

Figure 5. Regional geological setting of the Leadbetter Project (from McGill, 1992)................. 10

Figure 6. Local geological setting Leadbetter Diamond Project (from McGill, op.cit.) .............. 11

Figure 7. Stratigraphy – Leadbetter Project (from Miller & Associates, 2007) ........................... 12

Figure 8. Leadbetter Project - Property Geology.......................................................................... 14

Figure 9. Phase 1 – Drill Hole Location Plan ............................................................................... 20

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LIST OF TABLES

Table 1. Unpatented mining claims constituting the Leadbetter Property...................................... 3

Table 2. Patented mining claims constituting the Leadbetter Extension Property ......................... 4

Table 3. Summary of NQ Diamond Drill Holes ........................................................................... 19

Table 4. Summary of Diamond Recovery by Caustic Fusion ...................................................... 21

APPENDICES

Appendix A: Diamond Drill Hole Logs

Appendix B: Diamond Drill Hole Sections

Appendix C: Diamond Data & Laboratory Certificates

1

1.0 Summary

The Leadbetter Diamond Project is comprised of 2 contiguous properties (Leadbetter and Leadbetter Extension), 1590 hectares in total area, located 12 kilometres northeast of the town of Wawa, Ontario. A separate 3-claim block forms another part of the original Leadbetter property at Arliss Lake.

Figure 1. Location of Leadbetter project.

(Some of the more significant diamond-bearing kimberlites, such as Ekati, Diavik and Victor are denoted by yellow diamonds)

Dianor Resources Inc has an option agreement with the property owner – 3814793

Canada Inc – under which Dianor can earn a 90% and 80% interest in the respective properties. The Leadbetter diamond project is underlain by Archean age metavolcanics and

metasediments that have been intruded by Paleoproterozoic mafic dykes and pyroxenite intrusions. Diamonds were discovered in an outcropping conglomeratic unit within the volcano-sedimentary succession by a prospector – Mr. Joe Leadbetter – in 2004. Reconnaissance diamond drilling of the entire Leadbetter conglomerate has enabled the preliminary subdivision of it into 3 units: a basal, mixed volcanic, volcaniclastic, unit, the main Leadbetter diamond-bearing conglomerate (CONGLO) and an overlying fine clastic sediment succession.

2

Exploration, by Dianor, has consisted of two phases of diamond drilling in 146 holes totalling 45,723.51 metres (l08 NQ holes totalling 42,684.68 metres and 38 BQ holes totalling 3,038.83 metres) and test pitting of representative areas across the width and breadth of the conglomerate outcrop. The test pitting of 105 sites was completed and the samples, weighing on average 5 tonnes, were processed to recover diamonds through a dense media separation ("DMS") plant at SOS Lakefield Research in Lakefield Ontario. Of the 94 pits in the conglomerate a total of 349 tonnes was processed, yielding 3,603 diamonds weighing 82.7 carats. An additional 23 test pits were sampled in 2006, but have not yet been processed by DMS. Also in 2006, four of the original test pits were resampled, but with 70 to 80 tonnes collected at each site. These samples were processed by DMS at Kennecott Exploration Canada Inc's facility in Thunder Bay. The 298 tonnes of material processed in Thunder Bay yielded 2911 diamonds weighting in total 82.82 carats. The largest diamonds recovered were 1.522 and 1.011 carats in size. In conjunction, with the dlilling and test pitting, preliminary geological mapping of the property was undertaken. Airborne geophysical surveys (magnetic, electromagnetic and radiometric) were also conducted.

Drill core was routinely split and samples sent out for recovery of diamonds by caustic fusion techniques. To date complete results have been received from 20 holes. Microdiamond processing at various laboratories continues on an ongoing basis.

This report discloses, for assessment work purposes, detailed information for 23 of the holes drilled and caustic fusion data for 10 of those drill holes for which results have been received.

A staged program is recommended in order to continue the evaluation of the conglomerates. The first phase is infill core drilling to better define diamond variations in the conglomerates in the North Sector. A series of four 1000 tonne bulk samples are proposed to be collected in the North and Central Sectors of the property. Contingent upon, but not dependent on, the success of this work a second phase consisting of a series of additional bulk samples is recommended.

The estimated cost of the first phase program is $5,000,000; second phase work is estimated to cost $13,400,000, for a total program cost 0[$18,400,000.

Respectfully submitted,

Amerlin Exploration Services Ltd.

signed "Carl G. Verlev" Carl G. Verley, POeo

Dated: May 26, 2008

3

2.0 Property, Location and Access Diamond drilling that is reported on, was conducted on 2 claims – 1,243,332 and 1,243,335 - as well as a patented claim: number SSM 21166. These claims are apart of the larger land holdings constituting the Leadbetter Diamond Project.

The Leadbetter Diamond Project area consists of two contiguous land packages: the Leadbetter Property and Leadbetter Extension Property. In addition, a group of 3 contiguous claims, located at Arliss Lake, comprises another part of the project area, and are part of the original Leadbetter property. All of the blocks are located in the central and southeast area of Chabanel Township which is within the Mining District of Algoma; Sault Ste. Marie area of Northwestern Ontario (Figure 2). The combined Leadbetter and Leadbetter Extension properties consist of unpatented (mining rights) and patented (surface and mining rights) claims, totaling 1590 hectares or 16.0 square kilometers.

The property is situated 12 kilometers northeast of the Town of Wawa and 6 kilometers

west of the Town of Hawk Junction (from other major centers, approximately: 1,100 kilometers northwest of Toronto, 220 kilometers north of Sault Ste. Marie, and 520 kilometers east of Thunder Bay). Wawa is located on the Trans Canada Highway #17. The diamond-bearing discovery outcrops on the Leadbetter Property are centered at 671,030E, 5,326,160N (UTM, NAD83, zone 16). The Leadbetter Property consists of unsurveyed mining claims (19 in number), whereas the Leadbetter Extension Property is comprised of surveyed patented mining claims (49 in number).

Table 1. Unpatented mining claims constituting the Leadbetter Property

Claim No. Township

Record Date

Expiry Date

Claim units

Area (ha) Owner

1243332 Chabanel 16-Sep-03 16-Sep-10 4 50.27 3814793 Canada Inc1235754 Chabanel 27-Nov-02 27-Nov-11 3 47.52 3814793 Canada Inc1243335 Chabanel 16-Sep-03 16-Sep-11 4 19.3 3814793 Canada Inc1235757 Chabanel 22-Nov-02 22-Nov-10 2 31.15 3814793 Canada Inc1243325 Chabanel 02-Oct-02 02-Oct-11 1 8.237 3814793 Canada Inc1243510 Chabanel 16-Sep-03 16-Sep-11 5 66.75 3814793 Canada Inc1243373 Chabanel 12-May-03 12-May-11 2 44.02 3814793 Canada Inc1243369 Chabanel 27-May-03 27-May-11 1 21.5 3814793 Canada Inc1243365 Chabanel 27-May-03 27-May-11 4 58.17 3814793 Canada Inc1243319 Chabanel 16-Sep-03 16-Sep-11 3 49.22 3814793 Canada Inc1243509 Chabanel 16-Sep-03 16-Sep-11 4 42.01 3814793 Canada Inc1243318 Chabanel 16-Sep-03 16-Sep-11 8 103.9 3814793 Canada Inc1243363 Chabanel 27-May-03 27-May-11 3 37.95 3814793 Canada Inc1243377 Chabanel 27-May-03 27-May-11 1 11.52 3814793 Canada Inc1243336 Chabanel 16-Sep-03 16-Sep-11 1 7.004 3814793 Canada Inc1235747 Chabanel 22-Nov-02 22-Nov-07 6 91.08 3814793 Canada Inc

52 689.6

4

Table 2. Patented mining claims constituting the Leadbetter Extension Property

SSM No. Township Area SSM No. Township Area 13683 Chabanel 26.80 18639 Chabanel 13.75 13686 Chabanel 15.66 18640 Chabanel 10.49 13687 Chabanel 11.23 18641* Chabanel 13.60 15445 Chabanel 11.71 18642 Chabanel 8.38 17333 Chabanel 10.02 18643 Chabanel 10.65 17334 Chabanel 10.18 18644 Chabanel 15.46 17335 Chabanel 11.01 18645 Chabanel 17.76 17336 Chabanel 11.08 21166 Chabanel 15.97 17337 Chabanel 11.80 21167 Chabanel 17.56 17338 Chabanel 12.77 21168 Chabanel 6.42 17339 Chabanel 11.07 21169 Chabanel 20.30 17340 Chabanel 15.38 21171 Chabanel 15.39 17341 Chabanel 16.93 22714 Chabanel 17.54 17342 Chabanel 19.95 22718 Chabanel 14.55 17343 Chabanel 21.74 22719 Chabanel 6.52 17358 Chabanel 15.03 22721 Chabanel 22.44 17359 Chabanel 16.73 22722 Chabanel 29.85 17360 Chabanel 9.26 22726 Chabanel 11.32 17361 Chabanel 11.98 22874 Chabanel 9.00 17362 Chabanel 10.79 22945 Chabanel 16.44 17363 Chabanel 9.19 22946 Chabanel 14.87 17650 Chabanel 5.55 23011 Chabanel 9.60 18637 Chabanel 8.66 23012 Chabanel 6.41 18638 Chabanel 7.37 23543 Chabanel 17.73

23544 Chabanel 15.48 311.89 357.48

* A 0.48 hectare claim held by others lies within SSM 18641

The Leadbetter diamond project area is situated in a vegetation fume kill zone that resulted from toxic fume release during sintering operations at Algoma Steel’s iron sintering plant in Wawa. Vegetation was killed in an area, locally known as the “barren lands”, forming a belt 20 kilometres long and 5 kilometres wide extending to the northeast from Wawa. Vegetation in the fume kill zone is recovering. Grasses make up the predominant species in the vegetative cover at present, because of this, during dry summers, there can be extreme fire hazard conditions in the area, resulting in access closures. Consequently, operation of heavy equipment may be limited during closures. This is the only environmental liability that the project area is subject to as far as the writer knows.

l()

,:; :::;:~

_,1,235,747.;;--

- f

.1 ;i4~,J1~' ,;:.: . ~. ."

. ".: _r '.~ \ ; ." ,

Explanation

D Claims on Crown Land

D P:n.nted claims

Claim5 on whieh work waS' done and is reported on (1.243 .332: 1.243.33~ and p:ttomed claim: S SM21166)

D Claim5 tor whloh assessmel'll work oredit is bel nQ applied for

~ $yriace trace ot Leadbetter cooglomer:ne

Note: map grid is in map d:num NAD 83. lOM lG

topogr:lphic base is fnom 1 :20.000 scale maps 4:l C02_D2 S. 03.

Dianor Resources Inc.

CLAIM LOCATION PLAN

Leadbetter Diamond Project

Chabanel Township Wawa Area, Ontario

NTS 42002

Figure 2.

6

3.0 Accessibility Climate, Local Resources, Infrastructure and Physiography

The Leadbetter diamond project area is situated in an area of gentle rolling hills. The maximum topographic relief is 110 metres with the lowest point being, Mildred Lake at approximately 325 metres above sea level. Three-fifths of the property is void of vegetation as it lies within the “fume-kill” area caused by sulphur emissions from the Algoma Steel sintering plant in Wawa. A majority of the diamondiferous zones are also void of vegetation and much of the higher elevation areas are void of organics and till cover due to wind erosion and glacial scouring respectively. Access is by car or truck from the Town of Wawa, either by driving some 7 kilometers from Wawa east along Highway #101 and taking the Loonskin Lake Forest Access Road for some 5 kilometers north around the east side of Wawa Lake to the southeast side of the property, or by taking Trans Canada Highway #17 north from Wawa for some 9 kilometers to the Steephill Falls Road and for another eight kilometers east to the west side of the property. The property can be accessed from Hawk Junction along the old Algoma Central Railway bed west for some 17 kilometers to the north side of the property; Hawk Junction is 8 kilometers due east of the property. The northeast side of the property is accessible by the Loonskin Lake Forest Access Road to the Loonskin-Lucy Mine Road fork (at the south side of Lena Lake) a distance of 4.5 kilometers. Access can also be made by floatplane to Lena or Mildred Lake from either Wawa or from Hawk Lake. These lakes are in the southeast and central parts of the property respectively. The property has abundant water supply from lakes and creeks within the property boundaries. Power is available from Steephill Falls hydroelectric plant operated by Brascan and located approximately 3 kilometres west of the property. Skilled and experienced mining workforce is available from Hawk Junction and Wawa. Housing and supplies are available in Wawa. Exploration can be conducted on a year-round basis. The extent of the property provides a large land base for a future production facility, associated tailings facility, and potential waste dumps. Screened gravel and waste can be used for roadbed material.

7

4.0 Geological Setting

4.1 Regional Geology

From a regional perspective the Leadbetter Project area is located in the southern part of the Superior craton. The Craton is one of the largest Archean age blocks and forms the old stable continental nucleus around which younger terranes have been accreted. The Superior is made up of a series of volcano-sedimentary terranes that amalgamated in early Proterozoic times and were then deformed and intruded during the Proterozoic by granitic batholiths.

The Leadbetter Project is situated in the Michipicoten Greenstone Belt – one of the Archean volcano-sedimentary belts within the Superior Craton. This greenstone belt is considered a western extension of the Southern Volcanic Zone of the Abitibi greenstone belt (Ludden et al., 1986), but differs from it in that the mafic and felsic volcanic rocks record three cycles of igneous activity (at approximately 2.89, 2.75 and 2.70 billion years ago- Turek et al., 1982, 1992 and also named the Hawk, Wawa and Catfish assemblages respectively – Williams et al. 1991), compared with one (at approximately 2.75–2.7 billion years ago) in the Abitibi. All of the Michipicoten cycles are bimodal basalt–rhyolite suites with the oldest (2.89 billion years) containing komatiites (Sage and Lightfoot, 1996).

The first cycle of volcanism consists of mafic flow of the Gros Cap greenstone, estimated to range from 600 to 6,000 metres in thickness. The mafic volcanics are overlain by intermediate to felsic volcanics. The volcanics are capped by iron formation conjectured to have formed in a hotspring environment during the later stages of volcanic activity (Goodwin and Shklanka, 1967).

The second cycle of volcanism (Figure 3) is characterized by massive and pillowed, intermediate to mafic, tholeiitic lava flows, that are conformably overlain by intermediate to felsic tuff, breccia and minor clastic sedimentary rocks (Williams et al., 1991; Sage, 1994). Intrusive rocks generated by this cycle of magmatism include gabbro to quartz–diorite sills and dykes (Sage, 1994) and syenites (Stott et al., 2002). Termination of the second cycle is also marked by the deposition of iron formation.

A third cycle of volcanism is documented by renewed mafic to felsic volcanism which is succeeded by sediments consisting of greywackes, siltstone and conglomerates. The volcanic component of cycle three consists primarily of pillowed mafic flows with intermediate and felsic pyroclastics prevailing in the upper section of the sequence below the sediments. The sediments are interpreted to have been derived from the cycle two intermediate and felsic volcanics by rapid erosion into relatively shallow water basins (Sage, 1993).

U-Pb dating of zircons by the Ontario Geological Survey (Wyman et al., 2007) have

shown that volcanic material (felsic tuff) in the Leadbetter conglomerate is 2.697 billion years old. The age date clearly places the Leadbetter conglomerate in the third cycle of volcanism and suggests that it is 20 million years older that the diamond-bearing “Wawa volcaniclastic” succession located to the north of the Leadbetter project area.

Syn-and post-Kenoran magmatism in the Michipicoten is represented by four events: lamprophyre dyke intrusions at 2.7–2.67 billion years ago (Stott et al., 2002), granite intrusions at 2629–2650 million years ago (Percival and West, 1994), the northwesterly striking Matachewan diabase dyke swarm at 2454 million years ago (Osmani, 2001) and the northeasterly striking Keewenawan dyke swarm at 1142 million years ago (Vallancourt et al.,

8

2003). Lamprophyre dyke emplacement occurred in the Abitibi Greenstone Belt at 2687–2675 million years ago (Wyman and Kerrich, 1993; Wyman and Kerrich, 2002; Ayer et al., 2003), and over a wider range within the Superior Craton between 2.7 and 2.67 billion years ago (Barrie, 1990; Stern and Hanson, 1992). The age of the Sunrise carbonatite intrusion has been dated at 1097 million years (ref Sage, 1993). Pyroxenite intrusions at Lena and Mildred Lake are likely either the same age or younger.

Figure 3. Regional stratigraphic setting of the Leadbetter Project

within the Michipicoten Greenstone Belt, Chabanel Township (from Sage, 1993 with modifications after Arias and Helmstaedt, 1990)

Deformation during the Wawan phase of the Kenoran orogeny (approximately 2.67

billion years ago - Stott, 1997) resulted in large-scale recumbent folding and thrusting of the Michipicoten Greenstone Belt. Upright folding and high-angle reverse faulting (Arias and Helmstaedt, 1990; McGill, 1992) followed this deformation, resulting in local stacking of stratigraphy (Figure 4). A four-stage deformational history for the Michipicoten Greenstone Belt has been recognized by Arias (1996).

9

Figure 4. Regional structural model for the Leadbetter Project area

(Based on Arias & Helmstaedt, 1991: the structural section is derived from work conducted in the central part of the Michipicoten greenstone belt; the sketch in the lower left illustrates the present configuration of the belt as a regional nappe fold (F1) refolded about F2; imbricate thrust are considered related to F2)

At present, two tectonic models have been set forth as possible histories for the Early to

Middle Archean rocks of the Superior province. The first suggests the Superior province may have formed by repeated accretion of terranes as a result of subduction in a compressional margin (Hoffman, 1989; Williams et al., 1991). This model is supported by seismic, structural and geological data (Calvert et al., 1995; Calvert and Ludden, 1999; Thurston, 2002). Under this model, deformation within the Michipicoten Greenstone Belt resulted from subsequent accretion of volcanic arcs during formation of the belt, and by accretion of the Wawa subprovince to the Superior Craton nucleus (Arias, 1996). The volcanic rocks of Wawa are interpreted to be allochthonous assemblages of island and continental arcs (Sylvester et al., 1987), tectonically transported to their present position (Thurston, 2002).

An alternative model calls for an autochthonous origin for the Michipicoten Greenstone

10

Belt, with greenstones being accumulated in place, erupting through and being deposited upon older units (Thurston, 2002; Ayer et al., 2003). Under this model, the Superior Province would have experienced orderly, autochthonous progression from platforms through rifting of continental fragments, and late assembly during the Kenoran orogeny. This interpretation of all cycles of Michipicoten volcanics as intra-cratonic magmatism is supported by geochemical evidence, which records crustal geochemical signatures and significant contributions from continental passive margin sources (Sage and Lightfoot, 1996).

Figure 5. Regional geological setting of the Leadbetter Project (from McGill, 1992) Note: the non-stippled area containing iron formation and within which the Leadbetter project is

situated represents the supracrustal rocks, i.e. metasediments and metavolcanics.

11

Figure 6. Local geological setting Leadbetter Diamond Project (from McGill, op.cit.) Note: the diamondiferous conglomerate of the Leadbetter Project area is McGill’s

“conglomerate of the SHF (Steep Hill Fault) contact zone”

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4.2 Property Geology

Preliminary mapping and stratigraphic correlation by Allan R. Miller, PhD, PGeo, (2005a, 2005b and 2006) in conjunction with the work of the late Winfried Brach, PhD, PGeo, Ed Van Hees, PhD, PGeo and MSc candidate Dawn Niedermiller has documented the distribution of lithologies outcropping on the Leadbetter project area. Detailed logging of drill core by and under the supervision of Bernard-Olivier Martel PGeo has enabled the subdivision of the conglomerate and other lithologies into the units tabulated and described below. It is believed that this sequence correlates to Cycle 3 volcanics of Sage (1993). The degree of metamorphism has been determined to be sub-biotite zone greenschist facies based on the mineral assemblage: Mg-chlorite with epidote+actinolite (Miller, 2005a). The lithologies are distributed across the property in a manner illustrated in Figure 7 and 8.

Figure 7. Stratigraphy – Leadbetter Project (from Miller & Associates, 2007)

13

Basal Volcanic Sequence (V, V3A, V3B, V3R, VC): The oldest unit on the property consists of a sequence of grey-green to pale greenish,

metavolcanics exhibiting distinct pillow structures, massive flow units, minor interflow argillite-siltstone-fine-grained sandstone and volcaniclastic members as well as rare felsic tuff. The metavolcanics range in composition from basalt to dacite with rare rhyolitic intervals.

The Basal Volcanic sequence crops out in a northwesterly striking band that dips to the northeast across the northern part of the project area. A complete section of the unit is not exposed in the project area, therefore the thickness of it is not known, but is estimated to be in excess of 1000 metres by Sage (op cit). The top of the sequence is capped by a relatively thin (2 to 20 metres) sequence of pale tan to pinkish weathering, fine to medium-grained, thick to medium bedded metapsammite of probable greywacke composition. Cross bedding is preserved in some areas. Rare, thin silty layers and felsic tuff occur within this unit, which is locally called the Old Sandstone Formation.

Overlying the pillow lavas is a clastic sedimentary succession, locally called the Brilliant Cut Formation and also referred to as the Leadbetter conglomerate sequence, consisting of the following lithologies. Brillant Cut Formation - Conglomerate (CONGL)

This unit, referred to as the Leadbetter Conglomerate, is the main diamond-bearing unit on the property; it is comprised of clast supported polymictic conglomerate that is poorly sorted. Predominantly massive, the unit is rarely stratified and when it is the bedding varies in thickness from 10-30 centimetres to over 1metre with no obvious graded bedding. The sediments range in clast size from mud-sized particles to boulder-sized clasts, which are sub-rounded to rounded, flattened and highly stretched. The matrix is very fine grained and chlorite rich with a minor amount of quartzofeldspathic material. The clasts predominantly consist of volcanics (mafic dominant with lesser felsic clasts) with a minor amount of non-volcanics (siltstone, chert). Pentlandite, pyrrhotite, chalcopyrite and pyrite are minor sulphide phases occurring predominantly in the matrix. Alternating volcanic and sedimentary units are intercalated at the base of the conglomerate succession. A polymictic conglomerate occurs at thetop of the succession and is either matrix or clast supported depending on the location within the property. The unit is poor to weakly stratified and displays an unequal layering that varies in thickness from very thin (1-3 centimetre) to very thick (>1 metre) and locally displays reverse graded bedding.

The conglomerate appears to pinch out to the northwest in the project area, but thickens dramatically in the central and eastern parts of the project area where surface exposures give an indicated thickness of up to 300 metres. However, the average true thickness is estimated to be in the order of 110 metres. Deformation of this unit has resulted in stretched or elongated clasts. The degree of stretching is variable suggesting that there are local zones of intense deformation. Deformation appears to have imbricated the unit resulting in an increased thickness due to staking of panels of conglomerate.

.-

// /

14 .

LEGEND

Quaternary

Glacio-fluvial and lacustrine deposits

Paleoproterozoic

~ Mafic dykes. post deformation

Archean: Wawa Group Magpie Creek Formation

Sitlstone with interbedded sandstone

Brilliant Cut Formation

Debris flow/conglomerate unit - Diamond-bearing

Basal Volcanic sequence

sandstone with minor siltstone

Volcanics

y Attitude of bedding

7 Attitude of foliation

/15 Trend and plunge of lineation

_ - Normal fault ---

DIANOR RESOURCES INC.

Geology Leadbetter Property

Chabanel Township Wawa Area, Ontario, NTS 42CI02

Figure 8

15

Magpie Creek Formation: Meta-Argillite/Sandstone (SS, S2A, ARG, S5C and V/S?)

Overlying the Leadbetter conglomerate is a succession of thin-bedded and interbedded metapelites and metapsammites with bedding ranging from 1centimetre to greater than 1 metre thick. The bedding may occur as normal graded or it may occur as reverse graded bedding depending on the location on the property. Along with bedding a number of other sedimentary features such as rip-up-clasts, lode casts and flame structures can be identified in the unit. The sediments range in size from mud to sand sized particles. Pentlandite, pyrrhotite and chalcopyrite are minor sulphide phases in the sediments. The top of this unit is not exposed on the property, consequently the thickness is unknown, but work by Sage (op cit.) would indicate that the siltstone – sandstone unit is in the order of 100 + metres in thickness. This unit is typical of distal classical turbidites (d-e bouma series) and therefore represents deposition into a relatively quiet basin. This period of quiescence in sedimentation clearly helped preserve the Leadbetter conglomerate.

Intrusive Rocks (I2D, I3G, I3L and I5G)

The volcano-sedimentary sequence is cut by several dyke sets. The older set is a lamprophyre based on the melanocratic colour index and abundant fine-grained black mica. This dyke set is metamorphosed and deformed along with the metasediments into which it has intruded. These dykes are typically less than 1 metre in width. The second dyke set contains rare euhedral feldspar phenocrysts up to 3 centimetres in diameter. The dykes can be up to 20 wide on the property. These dykes strike to the northwest and believed to be part of the 2.5 billion year old Matachewan diabase dyke swarm. A third set of dykes consists of relatively unaltered northeasterly striking gabbroic apophyses that are probably part of the 1.1 billion year old Keewenawan dyke swarm. On the property, Keewenawan dykes are up to 15 metres wide. Alluvium (OB)

The central part of the project area is covered by Pleistocene and Recent glaciofluvial sand, gravel and lacustrine deposits to a thickness exceeding over thirty metres in some locations. Sampling of this material by backhoe indicates that the glaciofluvial material to be made of rounded cobbles (5 to 20 centimetres in diameter) generally consisting of granitic rock, mafic volcanics, felsic volcanics, and carbonatite. In areas where bedrock was encountered, a clay layer (light brown to light grey) was observed for a few meters, mixed with coarse boulders, lying immediately above the bedrock. The glaciofluvial material was a product of Late Wisconsinian glacial advance that had an ice direction of 165 degrees to 263 degrees (T. Morris, 2001). Studies conducted by T.F. Morris of the Ontario Geological Survey in 1993 and 1994 have demonstrated that there is a heavy mineral dispersion anomaly (chromite, garnet and ilmenite) that emanates from the area of the Leadbetter project (Morris, 1999). The original discovery of alluvial diamonds in Lena Creek draining westward from the Leadbetter project area was from the glaciofluvial outwash material that is exposed in the banks of Lena Creek where it enters the Magpie River. There is clearly potential in the Leadbetter Project area for the discovery of a resource of alluvial diamonds in the glaciofluvial material that underlies parts of the property. Structure

Structurally, the lithologies underlying the Leadbetter project area have been folded several times, in addition brittle failure has produced a series of prominent fault directions on the property some of which have been intruded by northwesterly and northeasterly striking mafic

16

dykes. Based on small-scale structures in the siltstone-sandstone unit overlying the conglomerate and the regional stratigraphy, it appears that the volcano-sedimentary succession underlying the Leadbetter project area has been isoclinally folded and overtuned. Later deformation has warped the conglomerate sequence into a gentle synform-antiform pair that plunges approximately 30o to the northeast. In addition, slip within high strain zones has imbricated the sequence into a series of panels, that are not well defined at the present time, but which may have resulted in an apparent thickening of the conglomerate in the central part of the project area.

17

5.0 Drilling

5.1 Exploration Work Summary Dianor Resources has conducted exploration on the Leadbetter property since November

2004. During this period, the initial thrust of the exploration work was to verify the diamondiferous nature of the host rock and determine if a suite of diamond indicator minerals exists in the diamond host that can be utilized to shed light on the nature of the source of the diamonds (“Due Diligence Diamond Sampling Phase”). The results of this work were successful in verifying the diamondiferous nature of the Leadbetter conglomerate. In addition, microprobe data of diamond indicator minerals recovered, taken as a whole, were indicative of mineral grains that have been sourced from diamond-bearing mantle regions and have both eclogitic and peridotitic parageneses. The exact nature of the transporting magma has yet to be determined. A detailed presentation and discussion of the results can be found in a SEDAR filed report by C.G. Verley, PGeo (2006).

Since that time Dianor has continued exploration of the Leadbetter properties, starting in April 2005 with a Phase 1 diamond drilling program designed to test the lateral and down-dip continuity and diamond content of the conglomerate. In the Fall of 2005 a program of surface test pit sampling was undertaken and 105 test pits were sampled primarily in the north sector, with some in the central sector. In addition, permitted bulk sampling of an area of alluvial material was undertaken at that time. McPhar Geosurveys Ltd undertook an airborne magnetic and radiometric survey of the Leadbetter Project area on October 22, 2005. In the late Fall of 2005 a Phase 2 diamond drilling program was initiated and completed in December 2006. Additional test pit sampling was also conducted during 2006. In conjunction with this work low-level aerial surveys (3,000 and 4,500 metres) were flown under the supervision of Eagle Mapping Ltd. Orthophoto maps and detailed topographic maps to 1 metre contour intervals were produced. Summary disclosure of these programs and their results are presented below.

Down-hole surveys of NQ drill holes were conducted on completion of each hole using the “FLEXIT Smart Tool” down-hole surveying system, which read inclination and azimuth at 3 metre intervals. Data from the surveys was down loaded into a computer and merged with the drill log database. Drill hole locations have been surveyed by Descarreaux & Dubé, licenced surveyors from Val-d’Or, Québec

Drill core samples that are to be processed for diamonds are chosen in relation to the contacts of differing units to differentiate the diamond contents within each unit. Samples are given a number in a sequence and the intervals are measured and entered in the logging program.

The sample interval is generally 3.5m in length for split NQ core. This length has been established on the basis of maximum sample weight accepted at the caustic fusion facilities (8 kg per sample).

All fragmental rocks, sedimentary (e.g.: conglomerate, sandstone, argillite) and volcaniclastic rocks (e.g.: pyroclastics, lahars, tuffs) are sampled.

In the sediments stratigraphically above the diamond-bearing conglomerates and in the volcanics below, 3 to 5 samples are taken. Otherwise, samples from the volcanic rocks underlying the diamondiferous conglomerate are chosen at the geologist’s discretion, usually at every 12.5 metres. Again, at the geologist’s discretion, any unusual rock or unit are also sampled for diamond recovery by caustic fusion.

A numbered sample tag is stapled in the core box at the end of every sample as proof of sampling.

18

5.2 Phase 1 Diamond Drilling Dianor initiated its first stage of diamond drilling on the Leadbetter property on April 24,

2005. The object of this work was to drill a fence of holes across the Leadbetter conglomerate in order to get a preliminary idea of the thickness and attitude of that unit. Colbert Drilling of Timmins, Ontario and Foramex Drilling of Val d’Or, Quebec undertook the work.

A total of 16 NQ- and 38 BQ-sized core holes were drilled during this phase, which was completed November 16, 2005. The NQ drill holes were laid out along an east-west line and drilled at an inclination of –60o to the west (azimuth: 270o). Three holes (Q1 to Q3 series) were drilled through a diabase dyke in order to obtain material that would be suitable for use as blanks for quality control purposes during diamond recovery.

5.3 Phase 2 Diamond Drilling

A second phase of diamond drilling commenced in August 2005 and was completed in December 2006. The object of this program was to further define the lateral and down dip extension of the Leadbetter conglomerate and to provide preliminary data on the diamond content of the unit. Foramex Drilling and Forage Benoit of Val d’Dor, Québec undertook the work. A total of 92 NQ-sized drill holes were completed during this phase. Four holes (Q4 to Q7 series) were drilled through a diabase dyke in order to obtain additional material that would be suitable for use as blanks for quality control purposes during diamond recovery.

The object of the Phase 2 drilling was to delineate, on a reconnaissance basis, the lateral extent and down-dip continuity of the Leadbetter conglomerate. The program was successful in reaching this objective as the conglomerate succession was found to be continuous over a strike length of 1.7 kilometres and was tested down-dip to a depth of 742 metres (hole Chab 06-101). The conglomerate is still open beyond that depth. To the east the succession is truncated by the Mildred Lake fault. To the west the conglomerates appear to pinch out, but exposures of diamondiferous conglomerate across the lake and west of the area drilled in the North Sector suggest that the sequence has not been completely closed off to the west. Further details on work and results conducted on the Leadbetter Diamond Project can be found in the SEDAR filed report by C.G. Verley, C. D’Amours and B.O. Martel (2007).

Summary information concerning the drill holes described in this report is tabulated

below (Table 3). Drill hole locations are illustrated on Figure 9. Logs for each of the drill holes are found in Appendix A. Drill holes sections are found in Appendix B. Conglomerate intercepts from the NQ-sized core of drill holes were split and shipped to Saskatchewan Research Council (“SRC”) in Saskatoon, Saskatchewan where they were processed to recover diamonds by caustic fusion techniques. Check, duplicate and quality control samples were sent to SGS Minerals Research in Lakefield, Ontario also for processing to recover diamonds by caustic fusion methods. Results of diamond recovery by caustic fusion are summarized in Table 4, below. At present, complete diamond results from 7 holes and partial results from 3 holes have been received. The diamond recovery results along with copies of original laboratory reports are found in Appendix C.

19

Table 3. Summary of NQ Diamond Drill Holes

Hole Claim Elevation No Start Date Completion Easting* Northing (mASL) Incl'n Azimuth Length (m)

05-08 1243332 24-Apr-05 29-Apr-05 670793 5326201 335 _600 270 0 199.50 05-09 1243332 30-Apr-05 01-May-05 671002 5326201 337 _60 0 270 0 87.00 05-10 1243332 02-May-05 05-May-05 671198 5326198 341 _60 0 270° 174.00 05-11 1243335 06-May-05 18-May-05 671401 5326202 327 _60 0 270 0 285.00 05-20 1243335 18-Aug-05 27-Aug-05 671302 5326295 331 _60 0 270 0 271.00 05-21 1243332 29-Aug-05 09-Sep-05 671137 5326296 355 -60 270 303.00 05-22 1243332 10-Sep-05 13-Sep-05 670897 5326299 345 -60 270 169.50 05-23 1243332 14-Sep-05 19-5ep-05 670749 5326311 337 -60 270 136.00 05-25 1243332 21-Sep-05 25-Sep-05 670898 5326349 347 -60 270 217.50 05-27 1243332 26-Sep-05 30-Sep-05 670897 5326311 346 -60 180 192.00 06-35 1243335 22-Apr-06 29-Apr-06 671456 5326300 330 -87 270 474.00 06-45 1243332 08-Jun-06 02-Jul-06 670817 5326404 336 -87 270 768.00 06-46 1243332 03-Jul-06 05-Aug··06 671000 5326404 350 -87 270 924.00 06-47 1243332 06-Aug-06 17-Sep-06 671200 5326400 350 -87 270 1020.00 06-50 1243335 28-Sep-06 21-Nov-06 671450 5326398 325 -87 270 1238.00 06-58 SSM21166 26-May-06 07-Jun-06 672100 5325297 344 -87 180 333.00 06-61 SSM21166 II-Jun-06 13-Jun-06 672198 5325401 331 -87 180 303.00 06-62 SSM21166 13-Jul-06 15-Jul-06 672313 5325488 336 -87 180 309.00 06-63 SSM21166 15-Jun-06 18-Jun-06 672398 5325404 340 -87 180 312.00 06-65 SSM21166 29-Jun-06 o I-Jul-06 672302 5325302 343 -87 180 324.00 06-99 1243335 21-Nov-06 07-Dec-06· 671387 5326590 330 -87 225 612.00

06-101 1243335 07-Dec-06 I1-Dec-06 671301 5326490 340 -87 225 453.00 07-104 1243335 05-Feb-07 24-Feb-07 671506 5326501 327 -87 225 612.00

Total: 4,11a-:78 * All Location data datum: NAD 83, zone 16

r ,.' ~.

~ , ,-... ~

1 ,235,757 ~"j

/

1,235,747 .. ;. .....

Explanation

D D m D

Diamond drill hole number and coil or location

Cia ims on Crown La nd

P:nerrt~d claim<

Claims on which work was dOM and is "'poned on (1.2~.332: 1.2~.335 and patem~d claim: SSMl1166)

Claims for which ass~ssmeM wol\( oJlldit IS being applied for

N",~' map grid ... in map datum N AD S3. ,one 16

topographic base is from 1 :20,000 scale maps 4J C02_02 Ii 03.

Dianor Resources Inc.

DIAMOND DRILL HOLE LOCATION PLAN

Leadbetter Diamond Project

Chabanel Township Wawa Area, Ontario

NTS 42002

Figure 9 .

21

Table 4. Summary of Diamond Recovery by Caustic Fusion Results for Diamond Drill Holes

Drill Hole/ Length Weight Bottom Sieve Aperture in Microns Total Rock Type From To metres Kgs +75 +106 +150 +212 +300 +425 +600 +850 +1180 +1700 DiamondsChab 05-08 CONGLO 0.30 22.90 22.4 66.09 82 56 41 21 12 5 5 2 0 0 226 Chab 05-09 CONGLO 3.00 57.10 54.1 118.99 217 135 117 66 52 14 6 2 1 0 610 Chab 05-10 CONGLO 0.70 138.00 137.30 320.59 701 358 205 146 84 37 23 4 1 1 1560 Chab 05-11 CONGLO 30.80 44.96 13.16 32.25 71 41 40 16 6 7 1 1 0 0 183 CONGLO 77.54 241.90 164.36 363.67 808 480 230 156 85 48 19 3 2 0 1831

Total 177.52 395.92 879 521 270 172 91 55 20 4 2 0 2014 Chab 05-20 V 36.40 169.60 55.10 120.65 N/R 8 7 5 2 3 1 0 0 0 26 CONGLO 169.60 237.20 67.60 139.90 N/R 156 95 59 35 15 9 3 2 1 385 SS/ARG 237.20 271.00 33.80 75.90 N/R 0 0 0 0 0 0 0 0 0 0

Total 156.50 336.45 164 102 64 37 18 10 3 2 1 411 Chab 05-21 CONGLO 1.50 263.90 262.40 623.89 N/R 539 320 225 125 58 30 10 4 0 1327 Chab 05-22 Partial rslts 41.22 100.70 4 2 2 0 0 0 0 0 0 0 8 Chab 05-25 V 153.27 199.50 46.23 95.94 N/R 5 0 0 1 0 0 0 0 0 6 Chab 05-27 Partial rslts 22.20 51.65 13 20 14 14 11 5 1 1 0 0 79 Chab 06-45 Partial rslts 152.17 352.64 6 1 1 0 0 0 0 0 0 0 8

22

6.0 Sample Preparation, Analyses and Security On site there was no sample preparation work undertaken, other than the splitting of drill core by diamond saw and bagging of resultant samples. Handling of drill core was documented in terms of who was involved in the splitting and bagging operations on a sample-by-sample basis. The sampling records are maintained on site. Numbered, tamper-proof plastic seals are used to secure and identify samples. The samples are held in a fenced and gated compound under 24 hour security prior to shipping by bonded commercial transport to laboratories for diamond recovery. No aspect of sample preparation was conducted by an employee, officer, director or associate of Dianor Resources Inc.

Diamond recovery from samples was undertaken by caustic fusion, a process that dissolves the diamond host in molten caustic soda. The process is a total recovery, down to the limit of the size of the bottom screen used, for diamond. The majority of core samples were processed at Saskatchewan Research Council’s facility in Saskatoon. Duplicate samples of drill core were send to SGS Lakefield Research Ltd in Lakefield, Ontario, were they were also processed by the caustic fusion technique. Both Saskatchewan Research Council and SGS Lakefield are ISO 17025 accredited laboratories for caustic fusion processing. The use of these laboratories as opposed to a single laboratory was in part an aspect of the quality control/quality assurance program to insure reliability of results. In terms of quality control practices, approximately every fifteenth sample was sent to SGS Lakefield Research as a check against work preformed by SRC. In addition, a duplicate (or double) sample was cut from approximately every fifth sample. Seventy-five percent of the duplicates were sent to SGS Lakefield and the remaining samples were sent to SRC. Furthermore, “blanks”, that is, samples of sterile rock, were inserted into sample runs for approximately every fifteenth sample with one blank going to SGS Lakefield and one to SRC. During the later part of Phase 2 drilling a program was implemented to insert synthetic diamonds into the drill core samples in order to test the recovery rates of both SRC and SGS Lakefield.

23

7.0 Interpretation and Conclusions

The Leadbetter Diamond Project is located 12 kilometres northeast ofthe town of Wawa in an area where there is excellent infrastructure, good access and a well-trained, competent work force. Mine development in this environment will be low cost.

The Project is focused on testing an Archean age (2.67 billion year old) diamondiferous debris flow. Diamonds are hosted in a conglomeratic sequence interpreted to have formed from a subaqueous marine, proximal debris flow fan complex that has been folded and metamorphosed under sub-biotite greenschist conditions. The diamondiferous conglomerates have an exposed strike length of 1.7 kilometres on the property. The sequence dips moderately to the northeast True thickness of the sequence averages 236 metres.

Diamond core drilling in 23 holes on claims 1,243,332, 1,243,335 and patented claim: SSM 21166 are reported on. The results of diamond recovery by caustic fusion are reported on for 7 holes and partial results are provided for another 3 holes.

Further work is recommended in order to test the: potential for higher-grade portions containing larger diamonds internal to the conglomerate horizons. Once these zones have been defined bulk sampling should be undertaken in order to accumulate sufficient sized parcels of diamonds to initiate valuation studies.

24

8.0 Recommendations A program of further exploration is recommended to continue the evaluation of the Leadbetter project. The next phase of exploration work should focus on several aspect of this deposit, namely;

- in-fill diamond drilling in order to better understand the diamond distribution within the conglomerate units. This work should include down-hole geophysical surveys

- sampling of the surface exposures of the diamond-bearing unit in order to get a better understanding of the diamond distribution within the conglomerate.

- Expanded testing of alluvial deposits that flank the conglomerate to the south in order to test the diamond potential of this material.

- in conjunction with this work geological studies must attempt to subdivide the conglomerate into differing facies and an attempt to determine the relationships between the different facies and diamond content must be pursued.

The estimated cost for these components is:

8.1 - Phase 1: Drilling and sampling

− Diamond drilling 10,000 metres HQ, all-in at $120/metre......................$1,200,000 − Attrition milling of drill core for diamonds ..............................................3,200,000 − Diamond indicator mineral studies & microprobing ....................................200,000 − Down-hole geophysical surveys .....................................................................50,000 − Geological mapping, detailed drill core

and petrographic studies ...............................................................................100,000 − Expansion of secure on-site office, core-logging,

storage and sampling facility ........................................................................150,000 − Engineering and technical support............................................................... 100,000

Total ....................$5,000,000 Contingent upon the success of this work underground bulk sampling will be required in order to increase confidence levels in resource estimates.

8.2 - Phase 2: Sampling Program - Dense Media Separation (DMS) Plant........................................................$700,000 - Installation of DMS Plant .............................................................................800,000 - DMS operation costs annually ...................................................................1,000,000 - Underground bulk sampling, 2000 metres.................................................8,000,000 − Testing of alluvial deposits for diamonds, including - DMS processing of concentrates ..................................................................600,000 - Security costs ................................................................................................500,000 - Third party processing of DMS concentrates ............................................1.500,000 - Modelling of diamonds grades and values.................................................. 300,000 Total ..................$13,400,000

Grand Total Phases 1 & 2 .......$18,400,000

25

9.0 References Archibald, F.T., 2004a: Summary Report #4: VLF Electromagnetics-Magnetometer-Geology-

Bulk Sampling-Diamond Drilling, report for 3814783 Canada Inc. and P. Mousseau-Leadbetter

Archibald, F.T., 2004b: Bulk Sampling & Chemical Composition Summary Report for 3814793 Canada Inc. & Paulette Mousseau-Leadbetter

Arias, Z.G., 1996: Structural Evolution of the Central Michipicoten Greenstone Belt, Superior Province, Wawa Ontario, Canada, M.Sc. thesis, Queen’s University, Kingston, Ontario, Canada.

Arias, Z.G., Helmstaedt, H., 1990. Structural evolution of the Michipicoten (Wawa) greenstone belt. In: Superior Province: Evidence for an Archean Fold and Thrust Belt. Geoscience Research Program, Summary of Research, 1989–1990. Ontario Geological Survey, pp. 107–114 (miscellaneous paper 15).

Ayer, J.A., Conceicao, R.V., Ketchum, J.W.F., Sage, R.P., Semenyna, L., Wyman, D.A., 2003. The timing and petrogenesis of diamondiferous lamprophyres in the Michipicoten and Abitibi Greenstone belts. In: Summary of Field Work and Other Activities 2003. Ontario Geological Survey, Open File Report 6120, 10-1-10-9.

Barrie, C.T., 1990. U–Pb garnet and titanite age for the Bristol Township lamprophyre suite, western Abitibi Subprovince, Canada. Can. J. Earth Sci. 27, 1451–1456.

Calvert, A.J., Sawer, E.W., Davis, W.J., Ludden, J.N., 1995. Archean subduction inferred from seismic images of a mantle suture in the Superior Province. Nature 375, 670–674.

Calvert, A.J., Ludden, J.N., 1999. Archean continental assembly in the southeastern Superior Province of Canada. Tectonics 18, 412–429.

Goodwin, A.M. and R. Shklanka, 1967: Archean Volcano-Tectonic Basins: form and Pattern, Canadian Journal of Earth Sciences, Vol. 4, p.777 – 795.

Hoffman, P.F., 1989. Precambrian geology and tectonic history of North America. In: Bally, A.W., Palmer, A.R. (Eds.), The geology of North America—An Overview. GSA, Boulder, VA, pp. 447–512.

Hourican, P.G., 2006: Preliminary Report on Initial Test (Test Pit-2) for Diamond Content in Unconsolidated Sediments (“Alluvials”) Leadbetter Diamond Project, private report prepared for Dianor Resources Inc.

Konstantinovskii, A.A., 2003: Epochs of Diamond Placer Formation in the Precambrian and Phanerozoic, Lithology and Mineral Resources, Vol 38, No. 6, pp. 530-546.

Lefebvre, N., Maya Kopylova and Kevin Kivi, 2005: Archean calc-alkaline lamprophyres of Wawa, Ontario, Canada: Unconventional diamondiferous volcaniclastic rocks, Precambrian Research, vol. 138, p. 57-87

Ludden, J., Hubert, C., Gapiery, C., 1986. The tectonic evolution of the Abitibi Greenstone Belt of Canada. Geol. Mag. 123, 153– 166.

McGill, G.E., 1992. Structure and kinematics of a major tectonic contact, Michipicoten greenstone belt, Ontario. Can. J. Earth Sci. 29, 2118–2132.

26

McPhar Geosurveys Ltd, 2006: Final Report on a Geophysical Survey, Leadbetter Project, Wawa, Ontario, McPhar Report #0521 for Dianor Resources Inc.

Miller, A.R., 2005a: A contribution to the geology of the diamondiferous metasedimentary rocks: sedimentology, stratigraphy, detrital mineralogy and conceptual model, Leadbetter property Chabanel township, Michipicoten greenstone belt, Superior province, Ontario using petrography – ore microscopy – scanning electron microscopy. Report dated April 6, 2005 for Dianor Resources Inc.

Miller, A.R., 2005b: A Contribution: interpretation of the Stratigraphy and Structure of the Leadbetter Discovery Area, report dated June 3, 2005 for Dianor Resources Inc.

Miller, A.R., 2006: Geology of the Leadbetter Discovery Zone, Chabanel Township, Michipicoten greenstone belt, Ontario, report dated January 14, 2006 for Dianor Resources Inc.

Mitchell, R.H., 1986: Kimberlites: Mineralogy, Geochemistry and Petrology, Plenum Press, New York, 442 p.

Morris, T.F., 1999: Geochemical, Heavy Mineral Data of Sediment Sampling Program, Wawa Region, Ontario Geological Survey Open File Report 5981, 74 p.

Morris, T.F., 2001: Quaternary Geology of Wawa Area, Ontario Geological Survey Map 2574- Open File Report 6055.

Osmani, I.A., 2001. Proterozoic mafic dike swarms in the Superior Province of Ontario. In: Thurston, P.C., Williams, H., Sutcliffe, H.R., Stott, G. (Eds.), Geology of Ontario. Ontario Geological Survey, pp. 661–681.

Percival, J.A., West, G.F., 1994. The Kapuskasing uplift: a geological and geophysical synthesis. Can. J. Earth Sci. 31, 1256–1286.

Ramsay, R.R. and Linda A. Tompkins, 1994: The Geology, Heavy Mineral Concentrate Mineralogy, and Diamond Prospectivity of the Boa Esperanca and Cana Verde Pipes, Corrego D’Anta, Minas Gerais, Brazil, in Proceedings or the Fifth International Kimberlite Conference, Conpania de Pesquisa de Recursos Minerais – Printer, Vol. 2, pp. 329-345.

Sage, R.P., 1993: Geology of Chabanel, Esquega, Lastheels and McMurray Townships, District of Algoma, Ontario Geological Survey, Open File Report 5586, 462 pp.

Sage, R.P., 1994: Geology of the Michipicoten Greenstone Belt, Ontario Geological Survey

Sage, R.P., and D.W. Lightfoot, 1996: Geochemical characteristics of granitoids rocks from within the Archean Michipicoten Greenstone Belt, Wawa subprovince, Superior province, Canada: implications for source regions and tectonic evolution. Precambrian Research, vol. 76, p 155-190.

Stern, R.A., Hanson, G.N., 1992. Marathon dykes: Rb–Sr and K–Ar geochronology of ultrabasic lamprophyres from the vicinity of McKillar Harbour, northwestern Ontario, Canada. Can. J. Earth Sci. 20, 193–227.

Stott, G.M., Ayer, J.A., Wilson, A.C., Grabowski, G.P.B., 2002. Are the neoarchean diamond-bearing breccias in the Wawa area related to late-orogenic alkalic and “sanukitoid”intrusions? In: Summary of Field Work and Other Activities 2002. Ontario Geological Survey, Open File Report 6100, 9-1 to 9-10.

27

Stott, G.M., 1997. The Superior province, Canada. In: Greenstone Belts. Clarendon Press„ Oxford United States, pp. 480–507.

Sylvester, P.J., Attoh, K., Schulz, K.J., 1987. Tectonic setting of late Archean bimodal volcanism in the Michipicoten (Wawa) greenstone belt, Ontario. Can. J. Earth Sci. 24, 1120–1134.

Thurston, P.C., 2002. Autochthonous development of Superior Province greenstone belts? Precambrian Res. 115, 11–36.

Turek, A., R.P. Sage and W.R. Van Schmus, 1992: Advances in the U-Pb zircon geochronology of the Michipicoten greenstone belt, Superior province, Ontario; Canadian Journal Of Earth Sciences, vol. 29, p.1154-1165.

Turek, A., P.E. Smith and W.R. Van Schmus, 1982: Rb-Sr and U-Pb ages of volcanics and granite emplacement in the Michipicoten belt, Wawa, Ontario; Canadian Journal Of Earth Sciences, vol. 19, p.1608-1626.

Vallancourt, C., Wilson, A.C., Dessureau, G.R., 2003. Synthesis of Archean geology and diamondbearing rocks in the Michipicoten greenstone belt: geology of Menzies township. In: Summary of Field Work and Other Activities 2003. Ontario Geological Survey, Open File Report 6120, 9-1-9-11.

Verley, C.G., 2006: Technical Report on the Leadbetter Project Due Diligence Diamond Sampling Program. SEDAR filed report prepared for Dianor Resources Inc.

Verley, C.G., C. D’Amours and Bernard O. Martel, 2007: Preliminary Tonnage Estimate for the Diamondiferous Conglomerates of the Leadbetter Diamond Project. SEDAR filed report prepared for Dianor Resources Inc.

Williams, H.R., G.M. Stott, K.B. Heather, T.L. Muir and R.P. Sage, 1991: Wawa Subprovince, in Geology of Ontario, Ontario Geological Survey, Special Volume 4, Part1, p.485-539

Wyatt, Bruce A., M. Baumgartner, E. Anckar, H. Grutter, 2004: Compositional classification of “kimberlitic” and “non-kimberlitic” ilmenite, Lithos, vol. 77, p. 819-840.

Wyman, D.A., C.O’Neill and J.A. Ayer, 2007: Evidence for Modern-style Subduction to 3.1 GA: A Plateau – Adakite – Gold (Diamond) Association GAS Bulletin (pre-print).

Wyman, D.A., Kerrich, R., 2002. Formation of Archean continental lithospheric roots; the role of mantle plumes. Geology 30 (6), 543–546.

Wyman, D., Kerrich, R., 1993. Archean shoshonitic lamprophyres of the Abitibi Subprovince, Canada: Petrogenesis, age, and tectonic setting. J. Petrol. 34 (6), 1067–1109.

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10.0 Certificate of Qualification

Carl G. Verley BSc, PGeo.

C E R T I F I C A T E

I, Carl G. Verley, am the author of this report entitled; Assessment Report On 2005 – 2006 Diamond Drilling On The Leadbetter Diamond Project for 3814793 CANADA INC., do hereby certify that;

• I am a graduate of the University of Britich Columbia, B.Sc., 1974 in geology and have worked in mining industry since graduation.

• I am in good standing as a registered member of the Association of Professional

Geoscientists of Ontario (#1313) and the Association of Professional Engineers and Geoscientists of British Columbia (#18572)

• As of the date of this certificate I am not aware of any changes in fact or circumstances as

regards the subject matter of this report which materially affects the content of the report or the conclusions reached. I was onsite during much of the exploration work described in this report, and am involved with mineral exploration in Northwestern Ontario.

• I have neither received, nor do I expect to receive any interest, direct or indirect from

3814793 Canada Inc. regarding this property or any properties owned by this company. Dated at Richmond, B.C, this 26th day of May, 2008 ____”Carl G. Verley”_____ Carl G Verley, PGeo.

APGO Reg. No. 1313 2150 – 1851 Savage Road Richmond, B.C. V6V 1R1 Phone: (604) 821-1088

28

APPENDIX A

DIAMOND DRILL HOLE LOGS

Legend Rock Type Name/Texture/Structure Intrusive Rocks

Diorite (I2D) Angular Pyroclastic

Diabase (I5D) Argillite Clasts Quartz Eyes

Gabbro (I3G) Breccia Rounded

Lamprophyre (I3L) Chert Clasts Siliceous Zone

Quartz Vein (I1N) Clast Supported Stratified

Meta-Volcanic Rocks Contact Zone Sub-angular

Andesite-Dacite (V3A) Dark Grey Sub-rounded

Basalt (V3B) Dark Green Tuff/Ash

Rhyolite (V3R) Felsic Clast Tuff Breccia

Volcanic (V) Graded Bedding Yellow Green

Volcanic/Sediment? (V/S?) Grey Yellow Grey

Volcaniclastic (VC) Grey Green

Meta-Sedimentary Rocks Green

Conglomerate (CONGL) Laminate

Sandstone (SS) Mafic Green

Volcanic/Sediment? (V/S?) Massive

Chert (S5C) Matrix Supported

Arkose Wacke (S2A) Medium-Supported

Argillite (ARG) Monomictic Other Pillow

Core Not Recovered (CNR) Polymictic

Overburden (OB) Porphyritic

GY

YG

TBL

Ta

SRd

SAg

ST

SZ

Rnd

QE

Py Ang

POR

Po

Pw

Mo

MmS

MxS

Mas

MG

Lam

G

GaG

Ga

GB

C/F

DG

DGa

CZ

CtS

C/S5C

Bre

C/S4A

Ressources Dianor inc.

Project : Chab 2007-06-22

DDH : CHAB 05-08Claims title : 1243332Township : ChabanelRange :Lot :

Section :Level :Work place : Leadbetter initial

Drilled by : Colbert Drilling From : 2005-04-24 To : 2005-04-29Geologist : Bernard-Olivier Martel Description date : 2005-07-11

Collar

Core size : NQ Cemented : No Storage : Yes

Comments

Azimuth : 270.00°Plunge : -60.00°Length : 199.50m

Longitude (East)Latitude (North)Elevation

Casing Left. NAD 83 Zone 16

670793.1895326200.913334.814

Down hole surveyType Depth Azimuth Plunge

Flex-it 15.00m 278.65° -59.70°Flex-it 18.00m 276.19° -59.82°Flex-it 21.00m 276.70° -59.79°Flex-it 24.00m 278.28° -59.63°Flex-it 27.00m 278.32° -59.41°Flex-it 30.00m 278.64° -59.23°Flex-it 33.00m 278.60° -59.11°Flex-it 36.00m 278.53° -58.91°Flex-it 39.00m 278.65° -58.75°Flex-it 42.00m 278.75° -58.60°Flex-it 45.00m 278.38° -58.52°Flex-it 48.00m 278.46° -58.42°Flex-it 51.00m 278.38° -58.45°Flex-it 54.00m 278.24° -58.53°Flex-it 57.00m 277.93° -58.68°Flex-it 60.00m 277.61° -58.77°

Type Depth Azimuth Plunge



Project : Chab DDH : CHAB 05-08 Page : 2

Type Depth Azimuth PlungeFlex-it 111.00m 275.19° -58.15°Flex-it 114.00m 275.73° -58.11°Flex-it 117.00m 275.96° -58.16°Flex-it 120.00m 275.76° -58.35°Flex-it 123.00m 275.22° -58.46°Flex-it 126.00m 275.13° -58.64°Flex-it 129.00m 275.12° -58.73°Flex-it 132.00m 274.63° -58.85°Flex-it 135.00m 274.33° -58.90°Flex-it 138.00m 273.93° -58.88°Flex-it 141.00m 274.10° -58.83°Flex-it 144.00m 273.93° -58.78°Flex-it 147.00m 273.84° -58.78°Flex-it 150.00m 273.79° -58.75°Flex-it 153.00m 273.55° -58.56°Flex-it 156.00m 274.82° -58.30°Flex-it 159.00m 275.28° -58.27°Flex-it 162.00m 275.15° -58.32°Flex-it 165.00m 274.52° -58.67°Flex-it 168.00m 274.18° -58.87°Flex-it 171.00m 274.14° -58.92°Flex-it 174.00m 274.09° -58.95°Flex-it 177.00m 274.05° -58.92°Flex-it 180.00m 274.05° -58.97°Flex-it 183.00m 274.23° -58.99°Flex-it 186.00m 273.95° -59.01°Flex-it 189.00m 274.33° -58.97°Flex-it 192.00m 274.64° -58.89°Flex-it 195.00m 275.35° -58.64°




DESCRIPTION

0.00 0.30 OBOverburdenOverburn. Casing 1m.

0.30 9.10 CONGLO; YG; PoConglomerate; Yellow Green; PolymicticSparkling FMConglomérat polygénique "clast-supported". De couleur jaune-gris. La grosseur et le type de clast varient: les principaux clasts sont des clasts volcaniques felsiques, intrusifs métamorphisés et quelquesclasts de sanstone et argillite. Leurs grosseurs oscillent bcp, entre le 0.5mm à 13 cm (coarse sand to cobbles). La morphologie des clasts est arrondie à sub-arrondie et les clasts semblent êtresub-parallèles à la foliation. La foliation (CA), définie par la matrice, est à environ 75 degrés. La matrice confinée entre les clasts est peu visible, de granulométrie inférieure à 0.25 mm (Fine Sand) et estcomposée essentiellement de chlorite, d'épidote ? et par endroit de sulfure (pyrrhotite). Trois fragments de 0.5mm à 2mm de chrome-diopside sont observés à 5,75m, à 6.10m et à 8,50m.Cette section se distingue de la suivante par son altération à limonite? observée en surface des clasts (couleur beige-jaune) et dans la matrice (vert-jaune).De plus, plusieurs veinules millimétriques à demi-centimétriques blanc laiteux composées de Quartz et Calcite recoupent l'unitée. Les veinules ne semblent pas avoir produit d'altération aux épontes.

0.30 22.90 CtSClast-SupportedConglomérat clast-supported

0.30 9.10 LmLimoniteAltération à limonite. De couleur beige-jaune en surface des clasts et de la matrice.

9.10 22.90 CONGLO; GaConglomerate; GrayContact supérieur graduel.Conglomérat polygénique "clast supported". De couleur gris à vert pâle. La grosseur et le type de clast varient: les principaux clast sont des clasts volcaniques felsiques, volcaniques mafiques et desclasts d'argillite et de sanstone. Leurs grosseurs oscillent bcp, entre le 0.5mm to 100cm (coarse sand to cobbles). La morphologie des clasts est arrondie à sub-arrondie et les clasts semblent êtresub-parallèle à la foliation. La foliation (CA), définie par la matrice, est à environ 65 degrés. La matrice confinée entre les clasts est peu visible, de granulométrie inférieure à 0.25 mm (Fine Sand) et estcomposée essentiellement de chlorite, d'épidote ? et par endroit de sulfure (pyrrhotite).De plus, plusieurs veinules millimétriques à demi-centimétriques blanc laiteux composées de Quartz et Calcite recoupent l'unitée. Les veinules ne semblent pas avoir produit d'altération aux épontes.

22.90 199.50 ARG; SS; Lam; GBArgillite; Sandstone; Laminates; Graded BebbingContact supérieur net.Séquences turbiditaires. Bandes de couleur gris pâle composées de fragments de quartz-felspath de 0.5 mm à 2 mm compris dans une matrice gris foncé à chlorite et à ? , alternant avec des bandes decouleur gris foncé composées de pélite (Shale). La morphologie et la largeur des bandes varient: en bandes mince ( 1mm à 2cm), en bandes large (1cm à 10cm) et en bandes irrégulières (figures decharge, "load-coasts" ou slump ?). Certaines sections sont pauvres en bandes pélitiques et on observe parfois un granuloclassement inverse. La foliation est visible, en bandes, à environ 70 degrés. Dansles plans de fissilité des bandes pélitiques, on observe régulièrement la présence de sulfures (pyrhottite, chlaco, ...).De plus, plusieurs veinules millimétriques à demi-centimétriques blanc laiteux composées de Quartz et Calcite recoupent l'unitée. Les veinules ne semblent pas avoir produit d'altération aux épontes.Présence de sulfure observée dans les plans de fissilité du shale et dans les vénules de quartz et/ou carbonate.A 5.75 Fragment de chrome-diopside. De couleur vert-turquoise. De 2 mm de diamètre.A 6.1 Fragment de chrome-diopside. De couleur vert-turquoise. De 1 mm de diamètre.A 8.5 Fragment de chrome-diopside. De couleur vert-turquoise. De 2 mm de diamètre.

22.90 26.95 SS; ARG76Sandstone; Argillite76°Section de couleur gris pâle, pauvre en bandes pélitiques de couleur gris foncé. La grosseur des grains de quartz-felspath varie de 0.5mm à 2mm.

22.90 197.15 CbcarbonateAltération carbonatique. Pegmentation de couleur blanche qui réagie au HCl.

22.90 22.95 Con; SheContact; ShearingImposible de déterminer l'angle exact avec plastique rouge, le core est trop brisé dans le haut et le bas du trou. Le contact apparent est de 78 degré.

26.95 44.60 ARG; Lam; SS; GBArgillite72°; Laminates; Sandstone; Graded BebbingSection riche en bandes gris foncé pélitique alternant avec des bandes gris pâle à quartz-feltpah. Par endroit, on observe des granuloclassements inverses. CA à environ 72 degrés.



DESCRIPTION

44.60 49.70 SS; ARG82Sandstone; Argillite82°Section de couleur gris pâle, pauvre en bandes pélitiques de couleur gris foncé. La grosseur des grains de quartz-felspath varie de 0.5mm à 1.5mm.

49.70 107.30 ARG; Lam; SS; GBArgillite65°; Laminates; Sandstone; Graded BebbingArgillite. Section riche en bandes gris foncé pélitiques alternant avec des bandes gris pâle à quartz-feltpah. Par endroit, on observe des granuloclassements inverses. CA à environ 65 degrés.

107.30 110.70 SSSandstoneSanstone. Section de couleur gris pâle, pauvre en bandes pélitiques gris foncé. La grosseur des grains de quartz-felspath varie de 0.5mm à 1.5mm.

110.70 110.80 S5CChertChert

110.80 111.10 SS; ARG70Sandstone; Argillite70°Sanstone. Section de couleur gris pâle, pauvre en bandes pélitiques de couleur gris foncé. La grosseur des grains de quartz-felspath varie de 0.5mm à 2mm.

111.10 124.75 ARG; Lam; SS; GBArgillite75°; Laminates; Sandstone; Graded BebbingArgillite. Section riche en bandes gris foncé pélitiques alternant avec des bandes gris pâle à quartz-feltpah. Par endroit, on observe des granuloclassements inverses. CA à environ 75 degrés.

124.75 129.20 SSSandstoneSanstone. Section de couleur gris pâle, pauvre en bandes pélitiques de couleur gris foncé. La grosseur des grains de quartz-felspath varie de 0.5mm à 2mm.

129.20 151.60 ARG; Lam; SS; GBArgillite79°; Laminates; Sandstone; Graded BebbingArgillite. Section riche en bandes gris foncé pélitiques alternant avec des bandes gris pâle à quartz-feltpah. Par endroit, on observe des granuloclassements inverses. CA à environ 79 degré.

151.60 175.15 SSSandstoneSanstone. Section de couleur gris pâle, pauvre en bandes pélitiques de couleur gris foncé. La grosseur des grains de quartz-felspath varie de 0.5mm à 2mm.

175.15 180.10 ARG; Lam; SS; GBArgillite75°; Laminates; Sandstone; Graded BebbingArgillite. Section riche en bandes gris foncé pélitiquess alternant avec des bandes gris pâle à quartz-feltpah. Par endroit, on observe des granuloclassements inverses. CA à environ 75 degré.

180.10 182.50 Conglo; CtSConglomerate; Clast-SupportedComglomérat polygénique "clast-supported". De couleur gris pâle à gris foncé. La grosseur et le type de clast varient: les principaux clasts sont des clasts volcaniques felsiques, quelques clastsde sanstone (S2S), de silstone (S3S), d'argillite (S4A) et parfois des Qz eyes. Leurs grosseurs ossillent entre le 0.5mm à 1cm (coarse sand to pebbles). La morphologie des clasts est sub-arrondià sub-anguleux. La foliation (CA), définie par la matrice, est à environ 80 degré. La matrice confinée entre les clasts est peu visible, de granulométrie inférieur à 0.25 mm (Fine Sand) et estcomposée essentiellement de chlorite et de carbonate.

182.50 199.50 SS; GB; ARG74; LamSandstone; Graded Bebbing ; Argillite74°; LaminatesSanstone. Section de couleur gris pâle, pauvre en bandes pélitiques de couleur gris foncé. La grosseur des grains de quartz-felspath varie de 0.5mm à 1,5mm.

197.15 199.50 SrMvsericite/muscoviteAltération à Séricite ? Pegmentaions de couleur brun pâle jaune mélimétrique. Pas de réaction au HCl.

199.50 DDH endNumber of samples : 0Number of samples QA/QC : 0Total lenght sampled : 0.00




Section :Level :Work place : Leadbetter

Drilled by : Colbert Drilling From : 2005-04-30 To : 2005-05-01Geologist : Bernard-Olivier Martel et Christian D'Amours Description date : 2005-07-04

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Comments




671001.8585326201.300336.601




Flex-it 58.00m 275.29° -59.43°Flex-it 61.00m 275.92° -59.30°Flex-it 64.00m 276.01° -59.20°Flex-it 67.00m 276.37° -59.10°Flex-it 70.00m 276.62° -59.00°Flex-it 73.00m 276.54° -58.99°Flex-it 76.00m 276.70° -59.04°Flex-it 79.00m 276.53° -59.08°Flex-it 82.00m 276.23° -59.18°



DESCRIPTION

0.00 3.00 OBOverburden

Overburden3.00 57.10 CONGLO; Ga; Po

Conglomerate; Gray; PolymicticConglomérat polygénique généralement "clast supported". De couleur gris. La grosseur et le type de clasts varient: les principaux clast sont des clasts d'origine volcaniques (felsiques et quelquesmafiques)et des clasts d'origine sédimentaires (argillite , sanstone et microconglomérat. Leurs grosseurs oscillent entre le 0.5mm et 18cm (coarse sand to cobbles). La morphologie des clasts est arrondieà sub-arrondie et les clasts semblent être sub-parallèle à la foliation. La foliation (CA), définie par la matrice, est à environ 65 degrés. La matrice confinée entre les clasts est peu visible, de granulométrieinférieure à 0.25 mm (Fine Sand), composée essentiellement de chlorite, d'épidote ?, et par endroit de sulfures disséminés (pyrite-pyrrhotite-chlaco 1 à 2%). Trois fragments de 1mm à 2mm dechrome-diopside sont observés à 15.45m et à 21.92m.De plus, plusieurs veinules millimétriques à demi-centimétriques blanc laiteux composées de Quartz et Calcite recoupent l'unitée. Les veinules ne semblent pas avoir produit d'altération aux épontes.

3.00 24.00 MmSMedium-SupportedLes clasts varient de 0.1 à 3 cm avec quelques exceptions à plus de 15 cm.

3.70 3.80 FrcFractureFracture avec évidence de circulation d'eau.






22.17 22.27 VEI;10;Cl;T;70°;;Vein 10 Chlorite Tension 70°Veine de Quartz Blanc à légèrement vitreux non carbonaté, faiblement chloritisé surtout près de l'éponte. Pas de trace de minéraux métalliques.


24.00 57.10 CtSClast-SupportedLes clasts varient de 0.2 a 5 cm. Les clasts les plus gros ont 5 à 8 cm et sont plus abondant qu'au début du trou.

27.90 28.10 FrcFractureZone avec plusieurs fractures. Pas d'évidence de circulation d'eau.

28.70 28.72 VEI;2;Cl;T;70°;;Vein 2 Chlorite Tension 70°Veine de quartz blanc vitreux avec 1% chlorite distribué dans la veine. Épontes altèrée (plus foncée) sur 0.2 cm.

36.85 37.10 SchSchistosity45°Schistosité de foliation non pénétrative avec élongation des fragments. 45 degrés de core axe. Rubanement noir semi-centimétrique de chlorite.



DESCRIPTION

44.10 44.20 VEI;1;ClTo;T;70°;;Vein 1 Chlorite Tourmaline Tension 70°Veine de quartz blanc vitreux avec 4% chlorite en amas et des traces de carbonates en fractures. Présence d'un Mx noir : tourmaline ?

46.95 47.15 VEI;3;Cl;S;40°;Po01;Vein 3 Chlorite Sheeted 40° Pyrrhotine01Veine de quartz gris pale à blanc assez diffus. 3-5% Chlorite concentré dans les plans de cisaillement. Trace à 1% Pyrrhotine surtout près de l'éponte mais aussi dissiminée dans la veine.

54.94 54.97 VEI;3;Cl;T;70°;;Vein 3 Chlorite Tension 70°Veine de quartz légèrement vitreux avec 3-5%chlorite en amas. épontes légèrement altèré (plus foncé) avec présence de Pyrrhotite (tr-1%) finement dissiminée dans les épontes sur 1 cm

57.10 61.38 SSSandstoneContact supérieur net.Sandstone massive de couleur gris pâle composés de felspath et de quartz recoupé ou laminé par quelques bandes minces (0.5mm à 1mm) de couleur gris foncé noir de shale. La grosseur des fragmentsvarie de 0.5mm à 2mm (coarse sand to very coarse sand). La foliation, en bande mince, est peu visible, à 53 degrés. Quelques sulfures disséminés (pyrite-pyrrhotite-chlaco 1%). sont visibles entre lesgrains de Qz-felspath.Certains grains de quartz ressemble à des "QZ-eyes" bleu?De plus, plusieurs veinules millimétriques à demi-centimétriques blanc laiteux composées de Quartz et Calcite recoupent l'unitée. Les veinules ne semblent pas avoir produit d'altération aux épontes.

57.13 57.14 ConContactAngle en plan 66 degrès.Angle en section 73 degrés.Core angle 60 degrés.

61.38 87.00 ARG; SS; STArgillite; Sandstone; Stratified/LaminatedLe contact supérieur est graduel.Séquences turbiditaires. Bandes de couleur gris pâle composées de fragments de quartz-felspath de 0.5 mm à 1.5 mm compris dans une matrice peut visible gris pâle verdâtre à chlorite et ? et alternantavec des bandes de couleur gris foncé noir pélitique (Shale) 10 à 20% distribué régulièrement. La morphologie et la largeur des bandes pélitique varient: bande mince (1mm à 2cm) et en bandeirréguliaire (figures de charge, "load-coasts" ou slump ?). La foliation est visible, principalement en bandes et à environ 55 degrés. Dans les plans de fissilité des bandes pélitiques, on observerégulièrement la présence de sulfure dissiminés (pyrrhotite-chlaco 1 à 2%).De plus, plusieurs veinules millimétriques à demi-centimétriques blanc laiteux composées de Quartz et Calcite recoupent l'unitée. Les veinules ne semblent pas avoir produit d'altération aux épontes.







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Comments




671198.2815326198.368340.716







Type Depth Azimuth PlungeFlex-it 106.00m 272.95° -56.90°Flex-it 109.00m 272.51° -56.92°Flex-it 112.00m 270.08° -56.92°Flex-it 115.00m 270.95° -56.89°Flex-it 118.00m 272.40° -56.87°Flex-it 121.00m 271.99° -56.77°Flex-it 124.00m 271.73° -56.68°Flex-it 127.00m 272.30° -56.65°Flex-it 130.00m 272.55° -56.59°Flex-it 133.00m 273.16° -56.44°Flex-it 136.00m 273.09° -56.43°Flex-it 139.00m 272.83° -56.42°Flex-it 142.00m 273.32° -56.41°Flex-it 145.00m 273.44° -56.39°Flex-it 148.00m 273.25° -56.39°Flex-it 151.00m 273.13° -56.36°Flex-it 154.00m 273.34° -56.28°Flex-it 157.00m 273.32° -56.22°Flex-it 160.00m 273.42° -56.16°Flex-it 163.00m 273.50° -56.11°Flex-it 166.00m 273.57° -56.04°Flex-it 169.00m 273.49° -56.01°




DESCRIPTION


Overburden. 1.5m de casing.0.70 81.75 CONGLO; Ga; Po

Conglomerate; Gray; PolymicticConglomerat polygénique varie de "matrix supported" à "medium suported". De couleur gris. Le type et la grosseur de clast varient: les principaux clast sont des clasts volcaniques mafiques, volcaniquesfelsiques, quelques clasts intrusifs et sédimentaires (sanstone et d'argillite. Leurs grosseurs oscillent entre le 0.5mm to 30cm (coarse sand to cobbles) Le nombre et la grosseur des clasts semblentaugmenter en profondeur. La morphologie des clasts est arrondie à sub-arrondie. La foliation (Core Angle), définie par la matrice, est à environ 60 degrés. La matrice (gray matrix) entre les clasts estbien visible, de granulométrie inférieure à 0.25 mm (Fine Sand), composée essentiellement de chlorite, d'épidote ? et par endroit de sulfures disséminés (pyrrhotite-chlaco 1 à 2%). De plus, plusieursveinules millimétriques à demi-centimétriques blanc laiteux composées de Quartz et Calcite recoupent l'unitée. Les veinules ne semblent pas avoir produit d'altération aux épontes.

0.70 81.75 MxSMatrix-SupportedLes clasts varient de 1 à 3 cm avec quelques rares occurrences près de 20 cm. Ils sont arrondis et de composition variés.

0.70 1.80 FrcFractureZone fracturée avec évidence de circulation d'eau (hydroxydation)



4.63 4.77 VEI;8;Cc;X;55°;;Vein 8 Calcite Brecciated 55°Veine de quartz et calcite avec fragment d"éponte à l'intérieur.


6.00 9.00 FrcFractureZone avec plusieurs fractures et évidence de circulation d'eau (hydroxydation).



18.75 18.82 VEI;5;;;45°;;Vein 5 45°Veine de quartz et calcite avec fragment d'éponte



23.10 23.44 VEI;20;Cc;;25°;;Vein 20 Calcite 25°Veine de quartz et calcite diffuse avec plus 40% de fragments d'éponte inclus.

23.30 23.90 Frc



DESCRIPTION

FractureZone avec plusieurs fractures et évidence de circulation d'eau (hydroxydation).



34.56 36.40 VEI;20;FuCc;X;;Po01;Vein 20 Fuchsite Calcite Brecciated Pyrrhotine01Veine de quartz et calcite odulante presque parrallèle à l'axe du core avec plus de 60% d'éponte inclus. Trace de pyrrhotite surtout au éponte supérieur. Trace de circulation d'eau avec lessivagedes carbonate au centre de la veine. Pour terminer, présence de fuchsite localisée.


39.50 39.59 VEI;8;;T;60°;Po01;Vein 8 Tension 60° Pyrrhotine01Veine de quartz légèrement en fumé avec carbonate dans les fracture. Trace de pyrrhotite.



49.90 49.95 VEI;4;;T;;Po01;Vein 4 Tension Pyrrhotine01Veine de quartz légèrement en fumé avec carbonate dans les fracture. Trace de pyrrhotite. Contact très irrègulier.

58.90 79.60 Po; CbPyrrhoyite; carbonatePrésence de pyrrhotite en amas de 0.1 à 3cm associés à des carbonates. La pyrrhotite semble parfois être remplacé par la pyrite.

70.36 70.42 VEI;3;CcCl;S;80°;To01;Vein 3 Calcite Chlorite Sheeted 80° Tourmaline01Veine de quartz et carbonate. Trace de tourmaline noir concentrée dans les plan chloriteux parallèle aux épontes.

81.75 102.80 CONGLO; GY; PoConglomerate; Yellow Grey; PolymicticContact supérieur et inférieur passe graduellement du gris au jaune-gris et du Jaune-gris au gris.Conglomérat polygénique "clast supported". De couleur gris pâle à Jaune-gris. La grosseur et le type de clasts varient. On observe une forte prédominance de clasts de couleur beige jaune oranged'origine felsiques (ryholite-dacite), accompagnés de clasts mafiques et de clasts sédimentaires de sanstone. Leurs grosseurs oscillent entre le 0.5mm et 18cm (coarse sand to cobbles) mais une forteconcentration de pebbles et cobbles. La morphologie des clasts est arrondie à sub-arrondie. La foliation (Core Angle), définie par la matrice, est à environ 58 degrés. La matrice (Gray-yellow matrix)confinée entre les clasts est peu visible, de granulométrie inférieure à 0.25 mm (Fine Sand), composée essentiellement de chlorite, d'épidote ?, Les veinules de Quartz-carbonates notées dans l'unitéeprécédente sont absente, les veinules beaucoup moins nombreuses sont constituées de Quartz plus vitreux souvent enfumé et ptymatitic

81.75 138.00 CtSClast-SupportedLe conglomérat généralement clast supported mais parfois medium supported. Les clasts de volcanites felsiques prédomine nettement. Ils sont plus nombreux et aussi plus gros (de 3 à 8 cm).les clasts des autres composition sont généralement de 1 à 3 cm avec quelques occurrences à près de 8 cm.

84.70 84.75 VEI;2;;S;;Po01;Vein 2 Sheeted Pyrrhotine01Veine de quartz légèrement carbonaté. Trace de pyrrhotite aux éponte.

87.70 109.00 VNL;12%;Fu;P;;To03;Veinule 12% Fuchsite Ptygmatic Tourmaline03



DESCRIPTION

Veine de quartz en fumé. Trace de fuchsite, de pyrrhotite et de pyrite dans les épontes.Les veines ont une largeur de 0.5 à 3 cm, de direction très variable et ondulantes.Trace de tourmaline noir et brune.

102.80 138.00 CONGLO; Ga; PoConglomerate50°; Gray; PolymicticContact supérieur passe graduellement du Jaune-gris au gris.Conglomérat polygénique "clast supported". De couleur gris pâle à Jaune-gris. La grosseur et le type de clast varient. Les types de clasts sont des clats volcaniques mafiques, volcaniques felsiques et desclasts d'origine sédimentaire d'argillite et de sandstone. À proximité du contact avec l'unité sous-jacente, on observe une forte concentration de clasts d'argillites. Leurs grosseurs oscillent entre le 0.5mmet 32cm (coarse sand to cobbles) mais une forte concentration de pebbles et cobbles. La morphologie des clasts est arrondie à sub-arrondie. La foliation (Core Angle), définie par la matrice, est à environ50 degrés. La matrice (Gray matrix) confinée entre les clasts est peu visible, de granulométrie inférieure à 0.25 mm (Fine Sand), composée essentiellement de chlorite, d'épidote ? Les veinules de Quartzblanc vitreux non carbonates, parfois enfumé, pygmatic et rare.

111.90 119.90 PoPyrrhoyitePrésence d'amas de pyrrhotite et de silicates de 0.1 à 3cm. Les carbonates sont beaucoup moins abondant, semblent lissivés.

137.00 138.00 FaiFaultingZone de transition faillée entre conglomérat et argillite-sandstone. Les clasts sont étirés et de diamètre plus petit.Angle en plan 62 degrésAngle en section 72 degrésCore angle 65 degrès

138.00 174.00 ARG; SSArgillite; SandstoneContact supérieur net.Séquences turbiditaires. Bandes de couleur gris pâle composées de fragments de quartz-felspath de 0.5 mm à 2 mm compris dans une matrice gris foncé à chlorite et à ? , alternant avec des bandes decouleur gris foncé composées de pélite (Shale). La morphologie et la largeur des bandes varient: en bandes mince ( 1mm à 2cm), en bandes larges (1cm à 10cm) et en bandes irrégulières (figures decharge, "load-coasts" ou slump ?). Certaines sections sont pauvres en bandes pélitiques et on observe parfois un granuloclassement inverse. La foliation est visible, en bande, à environ 45 degrés. Onobserve plusieurs petites veinules de quartz et/ou de calcite parfois plissées, qui recoupent la structure et souvent accompagnées de sulfures (pyrhottite, chlaco, ...) . Dans les plans de fissilité des bandespélitiques, on observe régulièrement la présence de sulfures (pyrhottite, chlaco à 2%).De plus, plusieurs veinules millimétriques à demi-centimétriques blanc laiteux composées de Quartz et Calcite recoupent l'unité. Les veinules ne semblent pas avoir produit d'altération aux épontes.

138.00 138.10 ConContactContact entre S1C et S4A/S2SAngle en plan 66 degrésAngle en section 33 degrésCore angle 35 degrésMesure imprécis core très fracturé.

157.70 165.70 SSSandstoneContact supérieur et inférieur graduel.Sandstone plus ou moins massive. Composé de quartz-felspath de 0.5mm à 2mm. Présence de 1 à 2% de bandes minces (1à3mm) pélitique. Trace-1% de sulfures (pyrrhotite) disséminés. Deplus, quelques veinules (1%) millimétriques à demi-centimétriques blanc laiteux composées de Quartz et Calcite recoupent l'unité. Les veinules ne semblent pas avoir produit d'altération auxépontes.







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Comments




671400.6005326201.679326.515







Type Depth Azimuth PlungeFlex-it 118.00m 269.58° -58.03°Flex-it 121.00m 269.86° -58.03°Flex-it 124.00m 269.62° -58.05°Flex-it 127.00m 270.03° -58.04°Flex-it 130.00m 269.66° -58.05°Flex-it 133.00m 269.70° -58.04°Flex-it 136.00m 270.13° -58.05°Flex-it 139.00m 270.16° -58.05°Flex-it 142.00m 270.64° -58.03°Flex-it 145.00m 270.10° -58.02°Flex-it 148.00m 270.23° -58.00°Flex-it 151.00m 270.10° -58.00°Flex-it 154.00m 269.83° -57.97°Flex-it 157.00m 270.56° -57.92°Flex-it 160.00m 269.76° -57.90°Flex-it 163.00m 271.11° -57.83°Flex-it 166.00m 269.68° -57.81°Flex-it 169.00m 270.98° -57.78°Flex-it 172.00m 271.37° -57.69°Flex-it 175.00m 271.77° -57.64°Flex-it 178.00m 271.02° -57.61°Flex-it 181.00m 270.41° -57.58°Flex-it 184.00m 271.77° -57.54°Flex-it 187.00m 272.09° -57.48°Flex-it 190.00m 272.04° -57.39°Flex-it 193.00m 272.00° -57.35°Flex-it 196.00m 272.68° -57.30°Flex-it 199.00m 272.45° -57.17°Flex-it 202.00m 271.58° -57.08°Flex-it 205.00m 272.27° -57.04°Flex-it 208.00m 272.40° -56.96°Flex-it 211.00m 272.56° -56.89°Flex-it 214.00m 272.29° -56.84°Flex-it 217.00m 272.22° -56.78°Flex-it 220.00m 273.06° -56.73°Flex-it 223.00m 272.97° -56.68°Flex-it 226.00m 273.14° -56.62°Flex-it 229.00m 273.02° -56.58°Flex-it 232.00m 273.26° -56.52°Flex-it 235.00m 273.26° -56.47°Flex-it 238.00m 273.20° -56.44°Flex-it 241.00m 272.61° -56.38°Flex-it 244.00m 268.77° -56.31°Flex-it 247.00m 270.63° -56.28°Flex-it 253.00m 270.40° -56.23°Flex-it 256.00m 270.00° -56.15°Flex-it 259.00m 271.19° -56.14°Flex-it 262.00m 272.19° -56.06°Flex-it 265.00m 274.25° -56.01°Flex-it 268.00m 274.70° -55.92°

Type Depth Azimuth PlungeFlex-it 271.00m 274.67° -55.84°Flex-it 274.00m 274.61° -55.76°Flex-it 277.00m 274.67° -55.64°Flex-it 280.00m 274.71° -55.53°



DESCRIPTION

0.00 15.40 OBOverburdenCaising 16.6 m.

15.40 30.80 VC; G; MoVolcaniclastic; Green; MonomicticVolcaniclastite-Conglomérat? "matrix-supported"Les clastes sont peut abondant généralement composés de volcaniques mafiques et felsiques. ( les clastes sédimentaires n'ont pas été observés.)Les clastes varient de 1 à 3 cm allongé dans la foliation orienté 64 deg CA.La matrice chloriteuse n'est pas carbonnatée mais les clastes sont souvent carbonatés.L'ensemble est traversé par de nombreuses veinules millimétriques de Quarts-Carbonates blanc laiteux.

15.40 30.80 MxSMatrix-SupportedLes clasts sont relativement rares "Matrix-Supported". Les clasts sont allongés, (trois fois plus long que large) dans la foliation à 60 deg to CA. Quelques sections de 5 à 10 cm ou, laconcentration de clats augmente (clast-supported).

30.80 44.96 CONGLO; G; PoConglomerate; Green; PolymicticLe contact supérieur est graduel. Les fragments sont généralement arrondis à sub-arrondis mais ne sont pas allongé. Certains clasts sont traversés par des veinules de Qz-Cb les quelles ne traversent pasdans la matrice.La roche est traversée par des veinules de Qz-Cb millimétriques.Un amas de Pyrrhotite de 3 cm a été noté.

30.80 44.96 MmSMedium-SupportedLes clasts composés majoritairements de volcanites mafiques (foncé) et de volcanites felsiques (pâles) et plus rarement de granitoides et de sandstone-argillite. La grosseur varie de 0.1 à 4 cmavec une moyenne de 1 cm. La matrice est verte et chloriteuse.

44.96 77.54 SSSandstoneSandstone de couleur gris à grain fin (<0.5mm) composé de Qz et feldspath. La roche est uniforme et massive. L'unité ne présente pas de banc de shale ni de stratification évidente.moins de 1% de veinules de Qz-Cb millimétrique recoupe l'unité.Un deuxième réseau de veinules très irrégulière, composée essentiellement de Qz parfois légèrement enfumé recoupe la roche à intervalle de 50 cm à 1.5 m. Ces veines créent une altération enplagioclase? Albite? , chlorite et pyrrhotite en traces sur 5 à 10 cm de part et d'autre de le veine.

60.20 93.00 PoPyrrhoyiteTraces de Pyrrhotite en amas de 0.5 cm plus ou moins cubique et framboidale. Il n'y a pas de carbonates associés. Le centre des amas est parfois occupé par de la pyrite.

77.54 93.00 CONGLO; G; PoConglomerate; Green; PolymicticConglomérat polymictique "clast à medium supported" à matrice verte. Les fragments composés majoritairement de volcanites mafiques et dans une plus faible proportion des fragments de volcanitesfelsique et sédimentaire (grès) varient de 0.5 cm à 2 cm. Quelques gros fragments vont jusqu'a 6 cm arrondis composées majoritairement de volcanites felsiques avec des yeux de Qz bleu.L'unitée est traversée d'un réseau de veinules deQz-Cb millimétrique ne présentant pas d'altération évidente des épontes.

77.54 83.44 CtSClast-SupportedLa matrice est composée de fragments de 0.3 à 0.5 cm.

83.44 93.00 MmSMedium-SupportedLa matrice est vraiement plus fine les grains ne sont plus identifiable.

83.93 84.15 VEI;5;;T;00°;;Vein 5 Tension 00°La veine est probablement sub parallele à la carotte. Les épontes sont noircies sur 0.5 cm (altération en chlorite). aucune minéralisation n'est apparente.

93.00 107.75 CONGLO; Ga; PoConglomerate; Gray; PolymicticConglomérat gris polymictique "medium-suported". les clasts sont composés principalement de volcanites felsiques suivis par les volcanites mafiques. Quelques fragments sédimentaires son aussi



DESCRIPTION

présent.Le réseau de veinules de Qz-Cb est présent mais moins développé.Présence d'un fragment de Chrome -Diopside de 1mm a 94.65

93.00 102.40 MmSMedium-SupportedLa matrice gris légèrement chloriteuse. Les clasts varient de 0.5 à 2 cm sub-arrondis avec quelques exceptions de 2 à 12 cm arrondis.

101.10 101.45 VEI;;Cc;T;55°;Py01;Vein Calcite Tension 55° Pyrite01Veine de Qz blanc laiteux avec carbonates et chlorite. les épontes sont minéralisées en Pyrite 1-3%

102.40 103.58 I3L; PORLamprophyre52°; PorphyriticDyke noir à grains fin contenant 1% de porphyres de 0.5 cm blanc à blanc-verdâtre.Les épontes ne présentent pas d'évidence de métamorphisme.

103.58 107.75 MmSMedium-SupportedLa matrice gris légèrement chloriteuse. Les clasts varient de 0.5 à 2 cm sub-arrondis avec quelques exceptions de 2 à 12 cm arrondis.

107.75 146.80 CONGLO; DGa; PoConglomerate; Dark Gray; PolymicticConglomérat polymictique "matrix à Medium-supported". La matrice est foncée chloriteuse à grain fin. Les clasts dominant sont de composition felsique suivis de clastes mafiques et quelques sédiment.Ils varient de 1 à 3 cm et sont arrondis à sub-arrondis. Les plus gros fragments sont bien arrondis et de composition felsiques.Les contactes supérieur et inférieur sont graduelles.Le réseau de veinules millimétriques de Qz-Cb est présent mais pas très bien développé.Traces de pyrrhotite finement disséminés.Chrome diopside de 0.5 mm a 139.85

107.75 120.00 CtSClast-SupportedLes clastes assez bien arrondis. La majorité varie de 0.5 à 2 cm.

120.00 123.60 I3LLamprophyre54°Le Dyke est foncé à grain très fin avec quelques traces de porphyres blanc-verdâtre.

123.60 125.90 MxSMatrix-SupportedLes contactes sont nets (sup 55 deg.CA et inférieur 45 deg CA) et altérés noir sur 1 cm. Les fragments sont plus flous. Les plus gros fragments (5 cm) sont composés de volcanites felsiques àyeux de Qz.

125.90 126.80 I3LLamprophyreLe Dyke est foncé à grain très fin avec quelques traces de porphyres blanc-verdâtre.Le contact sup est à 45 deg Ac et le contact inf est à 25 deg AC

126.80 130.30 MxSMatrix-SupportedLes contacts sont nets et altérés noir sur 1 cm. Les fragments sont plus flous. Les plus gros fragments (12 cm) sont composés de volcanites felsiques. Aussi la présence d'un fragment d'originemetamorphique de 5 cm.

130.30 132.70 I3L; PORLamprophyre30°; PorphyriticLe Dyke est foncé à grain très fin avec quelques traces de porphyres blanc-verdâtre (0.3 à 1 cm)Le contacte sup est à 30 deg Ac et le contact inf est à 34 deg AC

132.70 146.80 MmSMedium-SupportedLes fragments sont sub-arrondis à rond en générale de 1 à 3 cm. Les plus gros fragments sont composés de volcanites felsiques.

146.80 174.12 CONGLO; GY; Po



DESCRIPTION

Conglomerate; Yellow Grey; PolymicticConglomérat jaune grisâtre polymictique "medium supported". La matrice est fine légèrement jaunâtre. La majorité des fragments varient de 1 à 4 cm (sub-arrondi à arrondi) et sont composés devolcanite de sédiments et de quelques roches intrusives.Les fragments les plus grossier comptent pour moins de 1% des fragments mais pour plus de 10% de la roche. Ils varient de 5 à 12 cm (arrondis) et sont composés majoritairement de volcanites felsiquesmais aussi de volcanite mafique et de roche métamorphiques.Le réseau de veinules millimétriques de Qz-Cb est absent de la séquence.3 chrome diopside 0.5mm et 1 grenat de 0.5mm? a 151.4Deux chromes diopsides de 0.3mm à 0.7mm. a 160.1

146.80 174.12 MmSMedium-SupportedLes fragments sont arrondis à sub arrondis. Les plus gros fragments sont composés de volcanites felsiques et de roches metamorphiques.

174.12 191.40 CONGLO; Ga; PoConglomerate; Gray; PolymicticConglomérat "médium à clast supported" polymictic. Les principaux clasts sont des clasts volcaniques felsiques, volcaniques mafiques et quelques que clasts sédimentaires.Le réseau de veinules Qz-Cb de couleur blanc laiteux millimétrique est présent (1%).

174.12 191.00 MmSMedium-SupportedConglomérat généralement medium-supported. La morphologie principal des frgaments est sud-arrondis, de 0.5 à 3cm. Cependant, 5% des fragments sont plus gros, de 3 à 10cm, arrondis etd'origine felsique.La matrice est de couleur grise, chloritisée et à grin fin (moin de 0.25mm).

175.12 175.22 VEI;10;Cc;X;80°;Py02Po02;Vein 10 Calcite Brecciated 80° Pyrite02 Pyrrhotine02Veine de quartz blanc laiteux lègèrement en fumée par endoit. La veine est stéril mais les fragments d'épontes et les épontes sont ménéraliées Py, Po et chloritisées.

179.77 203.60 Po; CbPyrrhoyite; carbonatePyrrhotite en amas de 1 à 3 cm associé à des plages de carbonates blanc.

189.70 192.25 VNL;40;CcCl;P;;;Veinule 40 Calcite Chlorite PtygmaticVénule de quartz avec amas de chlorite d'épaisseur variable de 3 à 5 cm et de direction variable. Les épontes sont carbonatées et chloritisées. Aucune minéralisation n'est observée.

191.00 203.60 MxSMatrix-SupportedConglomérat matrix supported. Les principaux clasts sont des clasts d'origine felsiques, quelques mafiques et rarement des clasts sédimentaires. Les clasts sont flou et varient de 0.5 à 3cmsub-arrondis. Les clasts les plus gros sont rare (2%) et arrondis.

191.40 203.60 CONGLO; MG; PoConglomerate; Mafic Green; PolymicticContact supérieur graduel et occupé par des veines de quartz légèrement en fumée et ptygmatic.Conglomérat "matix supported" polymictic. La roche a une texture mouchetée, ce présent comme des moucheture blanche sur un fond vert foncé. Texture soyeuse qui fait penser à la présence de talc.Les clats sont flou et difficile à distinguer. Le réseau de veinule de Qz-Cb est bien développé (5%) et la matrice est carbonatée.

203.60 229.35 CONGLO; Ga; PoConglomerate; Gray; PolymicticLe contact supérieur est net 57 AC.Conglomérat medium-supported polymictic. La matrice est de couleur gris chloritisée.Les clasts sont bien visible.La présence de filonets noir dispersés dans la matrice, donne une teinte plus foncé à la matrice. Elle peut donc être confondue avec le conglomérat Drak Gray.La roche est recoupée par le réseau de veinules de Qz-Cb mais elles sont plus larges qu'habituellement. Les veinules sont stériles, n'ont pas produit d'altération des épontes et mesure 1 cm.Le contact supérieur avec le dyke (à 213.16) est cisaillé sur 60cm, à 35 degrés et marqué par la chlorite et tourmaline?On note aussi la présence de Pyrrhotite framboidale (1 à 2%) de 0.2 à 0.8cm dispersées dans la roche.

203.60 213.13 MmSMedium-SupportedConglomérat "Medium-supported". Les principaux clasts sont des clasts volcaniques felsiques, volcaniques mafiques et quelques clasts d'origine sédimentaires. La grosseur des clasts est



DESCRIPTION

majoritairement de 1cm. Quelques fragments felsiques arrondis de 3 à 10 cm.213.13 215.38 I3L; POR

Lamprophyre; PorphyriticIntrusif tres foncé noirâtre à grain fin avec 2% de porphyres blanc (plagio) de 0.1 à 0.7 cm. Le contact inférieur est orienté 28 deg to CA.La roche est traversée par un réseau de veinules millimétriques de Cb.

215.38 229.35 MmSMedium-SupportedConglomérat "Medium-supported". Les principaux clast sont des clasts volcaniques felsiques, volcaniques mafiques et quelques clasts d'origine sédimentaires. La grosseur des clasts estmajoritairement de 1cm. Quelques fragments felsiques arrondis de 3 à 10 cm.

229.35 241.90 CONGLO; DGa; PoConglomerate; Dark Gray; PolymicticConglomérat polymictic à matrice gris foncé et silicifiée. Les principaux clasts sont des clats felsiques, mafiques et quelques clasts d'origine métamorphiques. Le réseau de veinules de Qz-Cb est absent.Plusieurs fragments prennent une teinte rougeâtre et présente un pourtour (rim) noir millimétrique.

229.35 241.90 MxSMatrix-SupportedConglomérat.Matrix-Supported.Les clast correspondent à 60% de la roche. Ils ont généralement 1 à 3 cm et sub-arrondis. Les plus gros fragment, d'origine felsiques et quelques ignées, sont arrondis et peuvent mesurerjusqu'à 13 cm.La matrice fine, très foncée, sillicifiée et corresponds à environs 40% de la roche.

240.40 241.90 BobiotiteAltération ou métamorphisme de contact à tourmaline brune ou à biotite brune ???La matrice est totalement envahi par un Mx brun rougâtre fin.Présence de pyrhotite (3 à 5 %) désiminé.

241.90 260.95 I5DDiabase33°Dyke mafique. Diabase ? Très massif, non déformé, à grain moyen et de couleur gris foncé. Très magnétique. Réseau de veinules de Cb est présent 1%. Par endroit très fracturé et présence de chloritedans les fractures.

260.95 285.00 ARG; SS65; STArgillite65°; Sandstone65°; Stratified/LaminatedMagpie Creek FMArgillite-Sandstone. Alternance de bandes grises foncées à grain très fin et de bandes gris pâle à grain fin. On observe des bandes minces (moins de 1cm), des bandes larges (1 à 10 cm) et des bandesirrégulières (figure de charges :slumping)En plus des slumpings, on peut observer des granuloclassements à plusieurs endroits. Lesquels conduisent à une interprétation tantôt normale et tantôt inverse.

270.32 271.97 I3L; PORLamprophyre65°; PorphyriticDyke mafique porphyrique. De couleur vert foncé, à grain fin, avec 1% des porphyres de plagioclase variant de 0,2 à 1 cm.

277.20 278.40 VEI;2;ClCc;P;00°;Po01;Vein 2 Chlorite Calcite Ptygmatic 00° Pyrrhotine01Veine de quartz-carbonate de couleur blanc laiteux. Les épontes sont noircies. On observe de la chlorite dans la gangue et de la pyrhotite dans les épontes.






Drilled by : Colbert Drilling From : 2005-08-18 To : 2005-08-27Geologist : Antoine Cloutier Description date : 2005-10-24

Collar


Comments




671302.3055326295.383330.750


Flex-it 11.00m 267.14° -57.83°Flex-Dip 14.00m -57.75°Flex-Dip 17.00m -57.82°Flex-Dip 20.00m -57.76°Flex-it 23.00m 265.33° -57.76°Flex-it 26.00m 265.98° -57.75°Flex-it 29.00m 265.25° -57.80°Flex-Dip 32.00m -57.85°Flex-it 35.00m 265.34° -57.88°Flex-Dip 38.00m -57.91°Flex-it 41.00m 266.09° -57.91°Flex-it 44.00m 266.44° -57.85°Flex-it 47.00m 266.33° -57.84°Flex-it 50.00m 266.15° -57.78°Flex-it 53.00m 266.34° -57.66°Flex-it 56.00m 266.47° -57.53°





Type Depth Azimuth PlungeFlex-it 107.00m 264.96° -56.24°Flex-it 110.00m 265.00° -56.04°Flex-it 113.00m 264.91° -55.91°Flex-it 116.00m 265.11° -55.79°Flex-it 119.00m 264.56° -55.79°Flex-it 122.00m 264.56° -55.69°Flex-it 125.00m 264.29° -55.59°Flex-Dip 128.00m -55.62°Flex-Dip 131.00m -55.44°Flex-Dip 134.00m -55.29°Flex-it 137.00m 263.00° -55.31°Flex-it 140.00m 262.86° -55.22°Flex-it 143.00m 263.33° -55.13°Flex-it 146.00m 262.72° -55.08°Flex-it 149.00m 262.51° -54.96°Flex-it 152.00m 262.66° -54.84°Flex-it 155.00m 262.91° -54.82°Flex-it 158.00m 262.37° -54.75°Flex-Dip 161.00m -54.70°Flex-Dip 164.00m -54.64°Flex-Dip 167.00m -54.61°Flex-Dip 170.00m -54.60°Flex-Dip 173.00m -54.57°Flex-Dip 176.00m -54.47°Flex-Dip 179.00m -54.43°Flex-it 182.00m 263.77° -54.29°Flex-it 185.00m 264.70° -54.17°Flex-it 188.00m 265.06° -54.10°Flex-it 191.00m 264.83° -54.03°Flex-it 194.00m 264.45° -53.96°Flex-it 197.00m 265.32° -53.99°Flex-it 200.00m 265.71° -53.95°Flex-it 203.00m 265.21° -53.92°Flex-it 206.00m 264.14° -54.03°Flex-it 209.00m 266.08° -53.99°Flex-it 212.00m 264.71° -53.98°Flex-it 215.00m 264.91° -54.06°Flex-it 218.00m 264.76° -54.15°Flex-it 221.00m 265.74° -54.16°Flex-it 224.00m 265.10° -54.21°Flex-it 227.00m 264.92° -54.20°Flex-it 230.00m 265.32° -54.20°Flex-it 233.00m 265.21° -54.21°Flex-Dip 236.00m -54.20°Flex-it 239.00m 264.75° -54.18°Flex-it 242.00m 264.54° -54.18°Flex-it 245.00m 264.59° -54.18°Flex-it 248.00m 264.47° -54.11°Flex-it 251.00m 264.87° -54.08°Flex-it 254.00m 264.79° -54.08°

Type Depth Azimuth PlungeFlex-it 257.00m 264.63° -54.12°Flex-it 260.00m 264.26° -54.07°Flex-it 263.00m 263.78° -54.03°Flex-it 266.00m 264.31° -54.01°Flex-it 269.00m 263.68° -53.84°



DESCRIPTION


7.00 14.75 CZContact ZoneZone de contact gris foncé - noir à déformation intense. Il est impossible de déterminer le matériel d'origine dû à la déformation et à la coloration foncée produite par l'intrusion d'un dyke. Il semble yavoir des clasts cependant ce pourrait une zone bréchique produite durant l'emplacement d'un dyke. Le réseau de veinules milimétrique à centimétrique de Qz-Cb compose 1-5 % de l'intervalle parendroits. Seul les veinules réagissent au HCL. Les veinules démontrent des plissement et déformation.

14.75 36.40 I5D; MasDiabase; MassiveDiabase, massiveDyke de diabase massive, melanocrate, grains de -0.3 mm à 2 mm. Pas de structures visibles. Traces de veinule millimétrique de Qz-Cb. Seul les veinules réagissent au HCL. Le dyke est magnétique.

36.40 51.60 CZContact ZoneZone de contact gris foncé - noir à déformation intense. Il est impossible de déterminer le matériel d'origine dû à la déformation et à la coloration foncée produite par l'intrusion d'un dyke. Le matériel estprobablement le même que l'intervalle 51.6 m à 84 m car la déformation et la coloration diminuent demanière graduel. Il semble y avoir des clasts cependant ils sont flous et pourrait une zone bréchiqueproduite durant l'emplacement d'un dyke. Le réseau de veinules milimétrique à centimétrique de Qz-Cb compose 1-5 % de l'intervalle par endroits. Seul les veinules réagissent au HCL. Les veinulesdémontrent des plissement et déformation.

36.40 56.50 She; FolShearing; FoldingZone de déformation avec plissement et foliation intense, probablement dû à l'intrusion du dyke de diabase (14.75m-36.4m).

51.60 84.00 S2AArkose WakeRoche détritique à grains relativement grossier (plus de 2 mm) composé majoritairement de plagioclases avec dans une plus faible proportion du quartz et des minéraux mafiques. La matrice chloriteuseet séricitisée compte pour 10 à 15% et elle est légèrement carbonatée. On observe des clasts flous et arrondis dans quelques zones décimétriques de manière sporadique dans l'intervalle.La roche est très massive non trié et de couleur gris jaune avec une teinte verdâtre. L'absence de litage visible sur toute la longueur de l'unité est une caractéristique qui laisse supposer que cette rochepourrait être volcanique. Voir lame mince pour confirmer le type de roche.Le réseau de veinules millimétriques à centimétrique de Qz-Cb compose 2-5% de l'unité. Certaines veines sont composées de Qz fumé. La roche est généralement moyennement déformé, parfoisfortement déformé. La foliation varie de 35 degrés à 70 degré CA. Les veines démontrent des plissements et déformation disharmonique par endroits.1%de sulfures disséminés dans l'intervalle.Minéral vert chromifère, altération de spinnel? a 64.24

80.80 80.95 S5CChert45°Chert

82.30 83.10 S5CChert60°Chert

84.00 146.00 S2AArkose WakeRoche détritique à grains relativement grossier (1mm à plus de 2 mm) composé majoritairement de plagioclases avec dans une plus faible proportion du quartz et des minéraux mafiques. La matricechloriteuse compte pour 10 à 15% et elle est légèrement carbonatée. On observe des clasts flous et arrondis dans quelques zones décimétriques de même que des zones à grains plus fins, parfois de chert,de manière sporadique dans l'intervalle.Quelques Qz eyes visibles dans l'intervalle.La roche est très massive non trié et de couleur gris parfois avec une teinte verdâtre et jaunâtre. L'absence de litage visible sur toute la longueur de l'unité est une caractéristique qui laisse supposer quecette roche pourrait être volcanique. Voir lame mince pour confirmer le type de roche.Le réseau de veinules millimétriques à centimétrique de Qz-Cb compose 1% de l'unité. Certaines veines sont composées de Qz fumé. La roche est généralement non déformé.1% de sulfure disséminés dans l'intervalle.

99.05 102.95 S2A; ARGArkose Wake; ArgilliteZone de coulée de débris. le wacky contient environs 15% d'argille. La texture et l'apparence des amas d'argillite suggère une coulée de débris.



DESCRIPTION

Le contact supérieur est à 45 degrés CA.Le contact inférieur est à 65 degrés CA.

115.05 120.05 SheShearingZone de déformation, la foliation est forte et mesure 45 degrés CA.La zone semble être clastique mais ceci peu être du à la déformation.

146.00 151.65 VVolcanicRoche Volcanic, possiblement sédimentaireRoche gris foncé, mésocrate, à grains de -0.3 mm à 1 mm, assez massive mais qui pourrait être fragmentaire. La roche est très homogène ce qui laisse croire que c'est une roche volcanique. Possiblementun wacky ou sandstone. Voir lame mince pour confirmer.Le réseau de veinules millimétriques à centimétriques de Qz-Cb est présent et compose 1% de la roche. Les sulfures disséminés composent 1% de l'intervalle.

151.65 160.50 V; PwVolcanic; PillowRoche volcanique (Dacite ?)Contact supérieur flouÀ grain fin, de couleur gris pâle à verdâtre, de leucocrate à mésocrate et avec évidence de coussin (trempes noirâtres). La longueur des coussins varie de 15 à 50 cm. Par endroits, à proximité des trempes,la roche à un aspect brèchique.La foliation semble être entre 50 et 60 degrés (CA), elle est défini par les sulfures, disséminés et l'allongement de la chlorite. Dureté moyenne. Le réseau de veinules millimétrique à demi- centimétriquede Qz-Cb est présent (1-2 %) avec rarement des altérations aux épontes. Seulement les veinules réagissent aux HCl.Contact inférieur flou

160.50 163.70 V; TaVolcanic; Tuff /AshRoche volcanique possiblement fragmentaire (tuff).De couleur grise et phanéritique avec quelques zone à lapillistones et/ou brèche difficiles à distinguer due à leurs apparences floues. La grosseur des grains varie de <0.3mm à 2 mm dans une matricegrisâtre, beige à vertâtre chloritique. Aspect plus ou moins granulaire. L'observation des lames minces permettrait l'identification positive du type de roche composant cet intervalle. Aucune foliationclaire n'est apparente.On observe 2-4% de sulfures déssiminés de dimension de 0.5mm à 2 mm. Quelques amas de 1cm sont aussi présents. Une bande de sulfures est observée entre 161.7m et 161.8 m. Des veinules dequartz, quartz fumé et carbonate, millimétrique à centimétrique, sont observées. La pluspart réagissent au HCl.Contact inférieur graduel.Zone riche en sulfures (pyrrhotine et pyrite). Une bande composée de 50% sulfures est présente entre 161.7m et 161.8m.

163.70 167.50 SSSandstoneRoche fragmentaire.Contact supérieur graduel sur 10 cmDe couleur gris foncé, à grain moyen (0.5mm-2mm) avec quelques granules et clasts dispersées aléatoirement ( 5-10%). Les clasts sont arrondis à sub-angulaire et ils sont parfois étiré Environ 15% degrains de Qz transparents de 1-2 mm (Qz eyes, cristal tuff ?)Pourrait être un lahar, volcaniclastique ou micro-conglomérat.Le réseaux de veinules millimétriques à demi-centimétriques de Qz-Cd compose moins de 1% de l'unité. Seul les veinules réagissent à l'HCL. On observe des traces de sulfures disséminé.Il semble avoir un granoclassement inverse de cet unité.

167.50 169.60 ARG; SSArgillite; SandstoneAlternance de Sandstone et conglomératContact supérieur graduelIntervalle mixte de roche détritique de grains fins (argilite) à grossier (conglomérat). L'argilite est noir et compose environ 35% de l'intervalle, le sandstone est gris et compose 50% de l'unité et leconglomérat 15%. La roche est très folié ce qui ne permet pas une distinction clair des différentes unités. La foliation est à 70 degrés CA. Les clasts du conglomérat sont flou et il est impossible dedistinguer les différentes lithologies.Le réseau de veinules millimétriques à demi-centimétriques de Qz-Cb compose moins de 1% de l'unité. Seul les veinules réagissent au HCL. Des traces de sulfures disséminé sont observées dansl'intervalle.Pourrait être une roche volcaniclastique.Contact inférieur graduel.



DESCRIPTION

Flysch?167.50 175.00 Fol; She

Folding; ShearingZone de déformation moyenne, la foliation est très développé et quelques plis sont définit par des veines. On observe aussi des crénulations localement et des évidences de micro-failles.

169.60 175.00 CONGLO; PoConglomerate; PolymicticConglomérat polygénique gris foncé medium supportedLa roche est gris foncé et clastique. L'intense foliation masque les clasts, il est difficile de distinguer entre clasts et matrice. La matrice est aphanitique, on observe du Shear Banding de la matrice entrecertains clasts au microscope. La foliation est mesuré à 75 degrés CA.Le réseau de veinule millimétrique à centimétrique Qz-Cb est présent et compose 1% de l'intervalle. Seul les veinules réagissent au HCL. Environ 1-2% de sulfures disséminés compose l'intervalle.

175.00 205.80 CONGLO; Po; GYConglomerate; Polymictic; Yellow GreyConglomérat polygénique gris-jaune clast supportedContact supérieur graduelMatrice: Gris foncé à gris, -0.3mm à 1mm compose environ 35%de l'unité.Clast: Plutôt blanc, gris pâle à gris foncé et vert pâle avec petite teinte jaune (séricite?) sur la majoritée des clasts, subangulaire à arrondis de 0.5 cm à 15cm (la majoritée entre 1cm-5cm) composent 65%de l'unité.Composition: majoritairement felsic, intermédiaire et sandstone avec quelques mafiques et intrusifs foliésStructure: Foliation faible à médium, variation de 70-80 degrés CA, shear banding visible locallement dans la matrice.Réseau de veinules millimétriques à demi-centimétriques Qz-Cb compose 1% de l'unité, jusqu'à 5% locallement. Quelques veines entre 1cm à 10 cm avec quelques unes composées de Qz en fumé sontobservé dans l'intervalle.Quelques amas d'un minéral vert (spinnel altéré?) observé dans l'intervalle.Les veinules et quelques clasts réagissent au HCL.Traces de sulfures (pyrite et pyrrhotine).Contact inférieur graduel.

175.00 205.80 Conglo; CtSConglomerate; Clast-SupportedConglomérat Clast-supported

205.80 237.20 CONGLO; Ga; PoConglomerate; Gray; PolymicticConglomérat polygénique gris clast supportedContact supérieur graduelMatrice: Gris foncé à gris, parfois verdâtre, -0.3mm à 1mm compose environ 35%de l'unité.Clast: Plutôt blanc, gris pâle à gris foncé et vert pâle, subangulaire à arrondis de 0.5 cm à 15cm (la majoritée entre 1cm-5cm) composent 65% de l'unité.Composition: majoritairement felsic, intermédiaire et sandstone avec quelques mafiques et intrusifs foliés. Quelques fragments d'argillites sont visiblent vers la fin del'intervalle.Structure: Foliation faible à médium, variation de 50 à 70 degrés CA, shear banding et crénulation visiblent locallement dans la matrice. Les veinules démontrent parfois des plissementsQuelques amas d'un minéral vert (spinnel altéré?) observés dans l'intervalle.Réseau de veinules millimétriques à demi-centimétriques Qz-Cb compose 1% de l'unité.Quelques veines centimétrique à décimétrique, parfois de Qz en fumé sont observés dans l'intervalles.Les veinules et quelques clasts réagissent au HCL.Traces de sulfures (pyrite et pyrrhotine).Il y a une petite teinte verdâtre donc possiblement conglomérat gris-vert.Contact inférieur graduel.

205.80 237.20 Conglo; CtSConglomerate; Clast-SupportedConglomérat Clast supported.

213.15 213.60 FaiFaultingPetite zone de failles de quelques mm d'épaisseur. La roche est faillé et un déplacement à eu lieu de part et autre des failles. On retrouve un peu de mylonite dans les failles.

237.20 239.05 SS



DESCRIPTION

SandstoneSandstone gris avec quelques bandes d'argilliteSandstone de couleur gris pâle à grain fin (0.3mm à 1.5 mm, parfois avec des granules) en alternance avec quelques petites (0.3cm-5cm) bandes d'argillite. Le sandstone compose plus de 92% del'intervalle.Foliation, S0 généralement à environs 75-65 degrés.Des plissements et crénulations sont aussi observés dans l'intervalle.Le réseau de veinules Qz-Cb est présent 2 % avec régulièrement une altération aux épontes (chlorite et calcite). La structure des veinules est parfois plissée ptygmatique. Des traces de sulfures disséminéssont aussi observées.

239.05 241.60 ARG; SSArgillite; SandstoneRoche sédimentaire grise à gris-foncé avec alternance d'argilite à sandstone.Argillite-Sandstone. Alternance de bandes d'argillite de couleur grise foncée à grain très fin avec des bandes de sandstone de couleur gris pâle à grain fin (0.3mm à 1.5 mm, parfois avec des granules). Onobserve des bandes minces (moins de 1 cm), des bandes larges (1 à 10 cm) et des bandes irrégulières (figure de charges :slumping et structure de flame). L'argillite compose plus de 65% de l'intervalle.Foliation, S0, en bandes minces, larges et irrégulières, généralement à environs 75-65 degrés. De plus, plusieurs granuloclassement normale et inverse sont observés.Des plissements et ce qui semble êtrecharnières de plis sont aussi observés dans l'intervalle.Le réseau de veinules Qz-Cb est présent 2 % avec régulièrement une altération aux épontes (chlorite et calcite). La structure des veinules est parfois plissée ptygmatique. Des traces de sulfures disséminéssont aussi observées.

241.60 271.00 SS; ARGSandstone; ArgilliteRoche sédimentaire grise à gris-foncé avec alternance d'argilite à sandstone.Argillite-Sandstone. Alternance de bandes d'argillite de couleur grise foncée à grain très fin avec des bandes de sandstone de couleur gris pâle à grain fin (0.3mm à 1.5 mm, parfois avec des granules). Onobserve des bandes minces (moins de 1 cm), des bandes larges (1 à 60 cm) et des bandes irrégulières (figure de charges :slumping et structure de flame). Le sandstone compose plus de 85% de l'intervalle.Foliation, S0, en bandes minces, larges et irrégulières, généralement à environs 75-65 degrés. De plus, plusieurs granuloclassement normale et inverse sont observés.Des plissements et ce qui semble êtrecharnières de plis sont aussi observés dans l'intervalle.Le réseau de veinules Qz-Cb est présent 2 % avec régulièrement une altération aux épontes (chlorite et calcite). La structure des veinules est parfois plissée ptygmatique. Des traces de sulfures disséminéssont aussi observées.






Drilled by : Colbert Drilling From : 2005-08-28 To : 2005-09-09Geologist : Antoine Cloutier Description date : 2005-10-24

Collar

Core size : NQ Cemented : No Storage : No

Comments




671137.1195326295.503354.569


Flex-Dip 10.00m -58.78°Flex-it 13.00m 270.73° -59.05°Flex-it 16.00m 270.43° -59.05°Flex-it 19.00m 270.59° -59.05°Flex-it 22.00m 270.71° -59.04°Flex-it 25.00m 270.48° -59.02°Flex-it 28.00m 271.23° -58.73°Flex-it 31.00m 271.31° -58.67°Flex-it 34.00m 271.23° -58.63°Flex-it 37.00m 271.40° -58.56°Flex-it 40.00m 271.29° -58.47°Flex-it 43.00m 271.35° -58.45°Flex-it 46.00m 271.80° -58.41°Flex-Dip 49.00m -58.79°Flex-it 52.00m 269.80° -58.76°Flex-it 55.00m 269.99° -58.79°


Flex-it 58.00m 269.46° -58.73°Flex-it 61.00m 269.22° -58.70°Flex-it 64.00m 269.05° -58.54°Flex-Dip 67.00m -58.25°Flex-Dip 70.00m -58.60°Flex-Dip 73.00m -58.55°Flex-Dip 76.00m -58.51°Flex-Dip 79.00m -58.49°Flex-it 82.00m 269.13° -58.47°Flex-it 85.00m 270.31° -58.34°Flex-it 88.00m 269.77° -58.27°Flex-it 91.00m 270.16° -58.26°Flex-it 94.00m 271.05° -57.98°Flex-it 97.00m 270.29° -58.33°Flex-Dip 100.00m -58.26°Flex-Dip 103.00m -58.20°



Type Depth Azimuth PlungeFlex-it 106.00m 268.69° -58.15°Flex-it 109.00m 269.00° -58.10°Flex-it 112.00m 270.14° -58.09°Flex-it 115.00m 270.75° -57.63°Flex-it 118.00m 270.95° -57.61°Flex-it 121.00m 270.41° -57.89°Flex-Dip 124.00m -57.84°Flex-it 127.00m 271.42° -57.76°Flex-Dip 130.00m -57.67°Flex-Dip 133.00m -57.52°Flex-it 136.00m 271.63° -57.46°Flex-it 139.00m 271.32° -57.42°Flex-it 142.00m 272.32° -57.41°Flex-it 145.00m 271.38° -57.50°Flex-it 148.00m 271.39° -57.42°Flex-it 151.00m 272.07° -57.36°Flex-it 154.00m 272.18° -57.39°Flex-it 157.00m 271.04° -57.73°Flex-it 160.00m 270.96° -57.69°Flex-it 163.00m 271.07° -57.58°Flex-it 166.00m 271.27° -57.46°Flex-it 169.00m 271.87° -57.30°Flex-it 172.00m 272.53° -57.14°Flex-it 175.00m 272.21° -57.07°Flex-it 178.00m 270.73° -57.48°Flex-it 181.00m 271.65° -57.41°Flex-it 184.00m 269.74° -57.43°Flex-Dip 187.00m -57.35°Flex-it 190.00m 270.99° -57.28°Flex-Dip 193.00m -56.81°Flex-it 196.00m 269.23° -57.18°Flex-it 199.00m 271.90° -57.12°Flex-it 202.00m 271.75° -56.64°Flex-it 205.00m 272.21° -56.66°Flex-it 208.00m 271.89° -56.57°Flex-it 211.00m 271.83° -56.50°Flex-it 214.00m 272.82° -56.45°Flex-it 217.00m 272.03° -56.30°Flex-it 220.00m 271.97° -56.78°Flex-it 223.00m 271.09° -56.75°Flex-it 226.00m 270.64° -56.77°Flex-it 229.00m 271.37° -56.55°Flex-it 232.00m 271.53° -56.53°Flex-it 235.00m 270.82° -56.47°Flex-it 238.00m 271.49° -56.43°Flex-it 241.00m 270.83° -56.42°Flex-it 244.00m 270.97° -56.39°Flex-it 247.00m 271.72° -56.37°Flex-it 250.00m 271.63° -56.37°Flex-it 253.00m 271.60° -56.32°

Type Depth Azimuth PlungeFlex-it 256.00m 271.77° -56.33°Flex-it 259.00m 271.06° -56.31°Flex-it 262.00m 271.33° -56.25°Flex-it 265.00m 271.90° -56.26°Flex-it 268.00m 272.08° -56.19°Flex-it 271.00m 272.45° -56.08°Flex-it 274.00m 272.13° -55.95°Flex-it 277.00m 272.44° -55.96°Flex-it 280.00m 272.59° -55.94°Flex-it 283.00m 272.44° -55.95°Flex-it 286.00m 272.41° -55.99°Flex-it 289.00m 272.31° -56.00°Flex-it 292.00m 272.28° -56.00°Flex-Dip 295.00m -56.35°Flex-Dip 298.00m -56.37°Flex-Dip 301.00m -56.32°



DESCRIPTION


1.50 4.70 SSSandstoneSandstoneSandstone à grains moyen (0.3 mm - 1.5 mm) de couleur gris pâle. La carotte est très fracturée donc impossible de déterminer si il y a granoclassement ou litage. Le sandstone est composé de Qz,Feldspath et chlorite donnant un aspect verdâtre. Une faible foliation à 75 degrés CA est mesurée. La roche semble homogène à l'exception d'une bandes de chert d'environ 5cm au début de l'intervalle.Des traces du réseau de veinules demi-centimétriques Qz-Cb sont visiblent et plissé. Des traces de sulfures disséminé sont observé au microscope.Cette roche pourrais aussi être un tuff, voir lame mince pour confirmer.

4.70 5.50 S5CChertContact supérieur netteIntervalle de chert déformé avec des bandes plus foncés. Cet unité pourrait être le résultat de remplissage de faille causé par un chevauchement. La roche est très fracturé.Contact inférieur nette

5.50 19.80 V; MasVolcanic; MassiveRoche Volcanique massive (Dacite ?)De grain fin à grossier, de couleur vert à gris vert et de mésocrate à leucocrate. Présence de pigmentation beige jaune (2 %) par section interprété comme altération à séricite. Foliation généralementvisible, discontinue (alignement de mx mafique: chlorite), à environs 70 degrés. Dureté moyenne. Quelques amygdules remplis de Qz-Cb sont visibles dans l'intervalle.Le réseau de veinules millimétrique à demi- centimétrique de Qz-Cb est présent (2-3%). Seul les amygdules et veinules semblent réagir au HCL.La roche semble parfois bréchique cependant ceci pourrait être due au réseau de veinules.

19.80 23.10 S5C; SSChert; SandstoneChert SandstoneContact supérieur nette à 70 degrés (CA)Alternance graduel de bandes de chert-sandstone, le tous est gris avec quelques bandes plus foncées. Le sandstone à presque la même apparence que le chert (sillicifié?). Le sandstone est homogène etcomposé de grains de - 1mm.Le réseau de veinules millimétriques à demi-centimétriques Qz-Cb est présent et compose 1-2 % de l'unité. Les veinules démontrent parfois un plissement.

23.10 40.30 V; MasVolcanic; MassiveRoche Volcanique massive (Dacite ?)Contact supérieur netteDe grain fin à grossier, de couleur vert à gris vert et de mésocrate à leucocrate mais devient plus foncé vers la fin de l'intervalle. Présence de pigmentation beige jaune (2 %) par section interprété commealtération à séricite. Foliation généralement visible, discontinue (alignement de mx mafique: chlorite), à environs 70 degrés. Dureté moyenne.Le réseau de veinules millimétrique à demi- centimétrique de Qz-Cb est présent (2-3%). Quelques amygdules remplis de Qz-Cb sont visibles dans l'intervalle.Seul les amygdules et veinules semblentréagir au HCL.La roche semble parfois bréchique cependant ceci pourrait être due au réseau de veinules.Une zone de déformation est présente de 37 m à 51.2 m ce qui masque le contact avec le conglomérat. La foliation est plus prononcée dans cette zone mais elle reste à 70 degrés CA.Contact inférieur flou

29.20 30.10 S5CChert70°Chert 100%

37.00 51.20 FolFoldingZone de déformation moyenne à intense, foliation varie de 55-70 degrés CA. Pourrait-être le résultats de plissement ou chevauchement.

40.30 51.20 CONGLO; DGa; PoConglomerate; Dark Gray; PolymicticConglomérat gris foncé polygénique déformé.L'intervalle se situe dans une zone de déformation. La roche un conglomérat car il est possible d'y distinguer des clasts cependant il est impossible de déterminer la lithologie ou le pourcentage de clastsdue à la déformation. La roche est gris foncé et fortement folié, la foliation varie de 55-70 degrés CA dans l'intervalle. Le réseau de veinules millimétriques à demi-centimétrique Qz-Cb compose 1% de



DESCRIPTION

l'unité. Certaines veinules démontrent un plissement. On observe 1% de sulfures disséminés dans l'unité. Seul les veinules réagissent au HCL.51.20 131.70 CONGLO; GY; Po

Conglomerate; Yellow Grey; PolymicticConglomérat polygénique gris-jaune clast supportedContact supérieur graduelMatrice: Gris foncé à gris, -0.3mm à 1mm compose environ 35%de l'unité.Clast: Plutôt blanc, gris pâle à gris foncé et vert pâle avec petite teinte jaune (séricite?) sur la majoritée des clasts, subangulaire à arrondis de 0.5 cm à 15cm (la majoritée entre 1cm-5cm) composent 65%de l'unité.Composition: majoritairement felsic, intermédiaire avec quelques sandstones, mafiques et intrusifs foliésStructure: Foliation très faible à médium, variation de 45-70 degrés CA.Réseau de veinules millimétriques à demi-centimétriques Qz-Cb compose 1% de l'unité, jusqu'à 3% locallement. Quelques veines entre 1cm à 10 cm avec quelques unes composées de Qz en fumé etaltération à tourmaline sont observées dans l'intervalle.Quelques amas d'un minéral vert (spinnel altéré?) observé dans l'intervalle.Les veinules et quelques clasts réagissent au HCL.Traces de sulfures (pyrite et pyrrhotine). Quelques amas de sulfures sont aussi observés dans l'intervalle.Quelques zones sont plus grisâtre par endroits, surtout au milieu de l'intervalle et vers la fin.Contact inférieur graduel.

51.20 263.90 Conglo; CtSConglomerate; Clast-SupportedConglomérat, clast-supported

131.70 167.80 CONGLO; G; PoConglomerate; Green; PolymicticConglomérat polygénique vert clast supportedContact supérieur graduelMatrice: verte, -0.3mm à 1mm compose environ 40%de l'unité.Clast: Plutôt verdâtre avec quelques blancs, gris pâle à gris foncé, subangulaire à arrondis de 0.5 cm à 15cm (la majoritée entre 1cm-5cm) composent 60% de l'unité.Composition: majoritairement, intermédiaire, beaucoup de felsic (rhyolite), mafique avec quelques sandstones et intrusifs foliésStructure: Foliation très faible à médium, variation de 60-70 degrés CA.Réseau de veinules millimétriques à demi-centimétriques Qz-Cb compose 1% de l'unité, jusqu'à 3% locallement. Quelques veines entre 1cm à 10 cm avec quelques unes composées de Qz en fumé etaltération à tourmaline sont observées dans l'intervalle.Quelques amas d'un minéral vert (spinnel altéré?) observé dans l'intervalle.Les veinules et quelques clasts réagissent au HCL.Traces de sulfures (pyrite et pyrrhotine). Quelques amas de sulfures sont aussi observés dans l'intervalle.Contact inférieur graduel.

167.80 210.90 CONGLO; Ga; PoConglomerate; Gray; PolymicticConglomérat polygénique gris, clast supportedContact supérieur graduelMatrice: Gris foncé à gris, -0.3mm à 1mm compose environ 35%de l'unité.Clast: Plutôt blanc, gris pâle à gris foncé et vert pâle subangulaire à arrondis de 0.5 cm à 15cm (la majoritée entre 1cm-5cm) composent 65% de l'unité.Composition: majoritairement felsic, intermédiaire avec quelques sandstones, mafiques et intrusifs foliésStructure: Foliation très faible à médium, variation de 55-70 degrés CA.Réseau de veinules millimétriques à demi-centimétriques Qz-Cb compose 1% de l'unité, jusqu'à 3% locallement. Quelques veines entre 1cm à 3cm sont observées dans l'intervalle.Quelques amas d'un minéral vert (spinnel altéré?) observés dans l'intervalle.Les veinules et quelques clasts réagissent au HCL.Traces de sulfures (pyrite et pyrrhotine).Quelques zones sont plus foncés par endroits.Contact inférieur graduel.

210.90 213.20 CONGLO; G; PoConglomerate; Green; Polymictic



DESCRIPTION

Conglomérat polygénique vert clast supportedContact supérieur graduelMatrice: verte, -0.3mm à 1mm compose environ 30%de l'unité.Clast: Plutôt verdâtre, blancs, gris pâle à gris foncé, subangulaire à arrondis de 0.5 cm à 15cm (la majoritée entre 1cm-5cm) composent 70% de l'unité.Composition: majoritairement intermédiaire, beaucoup de felsic (rhyolite).Structure: Foliation faible à médium, variation de 65-80 degrés CA.Réseau de veinules millimétriques à demi-centimétriques Qz-Cb compose 3% de l'unité, jusqu'à 5% locallement. Quelques veines entre 1cm à 5 cm sont observées dans l'intervalle.Les veinules et quelques clasts réagissent au HCL.Traces de sulfures (pyrite et pyrrhotine).Contact inférieur graduel.

213.20 263.90 CONGLO; Ga; PoConglomerate; Gray; PolymicticConglomérat polygénique gris, clast supportedContact supérieur graduelMatrice: Gris foncé à gris, -0.3mm à 1mm compose environ 35%de l'unité.Clast: Plutôt blanc, gris pâle à gris foncé et vert pâle subangulaire à arrondis de 0.5 cm à 15cm (la majoritée entre 1cm-5cm) composent 65% de l'unité.Composition: majoritairement felsic, intermédiaire avec quelques sandstones, mafiques et intrusifs foliésStructure: Foliation très faible à médium, variation de 60-80 degrés CA.Réseau de veinules millimétriques à demi-centimétriques Qz-Cb compose 1% de l'unité, jusqu'à 3% locallement. Quelques veines entre 1cm à 10cm sont observées dans l'intervalle.Entre 215 m et 218 m, les veines de Qz composent jusqu'à 30% de l'intervalle.Quelques amas d'un minéral vert (spinnel altéré?) observés dans l'intervalle.Les veinules et quelques clasts réagissent au HCL.Traces de sulfures disséminé (pyrite et pyrrhotine).Quelques zones sont plus foncés par endroits.Contact inférieur nette

215.00 218.00 VEI;;;;;;VeinVeines de Qz variant en épaisseur de 1cm à 20 cm composant 30% de l'intervalle, aucune altération aux épontes. Pas de structure évidente.

263.90 266.50 SSSandstoneSandstone gris avec quelques bandes d'argilliteSandstone de couleur gris pâle à grain fin (0.3mm à 1.5 mm, parfois avec des granules) en alternance avec quelques petites (0.3cm-5cm) bandes d'argillite. Le sandstone compose plus de 97% del'intervalle.Foliation, S0 généralement à environs 80 degrés.Des plissements et crénulations sont aussi observés dans l'intervalle.Le réseau de veinules Qz-Cb est présent (trace). Des traces de sulfures disséminés sont aussi observées.

266.50 303.00 ARG; SSArgillite; SandstoneRoche sédimentaire grise à gris-foncé avec alternance d'argilite à sandstone.Argillite-Sandstone. Alternance de bandes d'argillite de couleur grise foncée à grain très fin avec des bandes de sandstone de couleur gris pâle à grain fin (0.3mm à 1.5 mm, parfois avec des granules). Onobserve des bandes minces (moins de 1 cm), des bandes larges (1 à 60 cm) et des bandes irrégulières (figure de charges :slumping et structure de flame). Le sandstone compose plus de 70% de l'intervalle.Foliation, S0, en bandes minces, larges et irrégulières, généralement à environs 55-85 degrés. De plus, plusieurs granuloclassement normale et inverse sont observés.Des plissements et ce qui semble êtrecharnières de plis sont aussi observés dans l'intervalle.Le réseau de veinules Qz-Cb est présent 1 % . La structure des veinules est parfois plissée ptygmatique. Des traces de sulfures disséminés sont aussi observées.






Drilled by : Colbert Drilling From : 2005-09-10 To : 2005-10-13Geologist : BERNARD-OLIVIER MARTEL Description date : 2005-10-05

Collar


Comments




670896.7745326298.513345.259


Flex-Dip 11.00m -59.44°Flex-it 14.00m 277.78° -59.46°Flex-Dip 17.00m -59.39°Flex-it 20.00m 277.79° -59.23°Flex-it 23.00m 277.71° -59.16°Flex-it 26.00m 277.89° -59.11°Flex-it 29.00m 277.85° -59.03°Flex-it 32.00m 277.99° -58.98°Flex-it 35.00m 278.23° -58.94°Flex-it 38.00m 278.28° -58.91°Flex-it 41.00m 278.40° -58.87°Flex-it 44.00m 278.49° -58.85°Flex-it 47.00m 278.41° -58.85°Flex-Dip 50.00m -58.88°Flex-Dip 53.00m -58.84°Flex-Dip 56.00m -58.80°


Flex-it 59.00m 278.54° -58.73°Flex-Dip 62.00m -58.64°Flex-it 65.00m 277.61° -58.58°Flex-it 68.00m 279.71° -58.50°Flex-it 71.00m 279.48° -58.50°Flex-it 74.00m 279.55° -58.47°Flex-it 77.00m 279.74° -58.41°Flex-Dip 80.00m -58.32°Flex-it 83.00m 279.21° -58.26°Flex-it 86.00m 279.13° -58.27°Flex-it 89.00m 278.90° -58.24°Flex-it 92.00m 278.46° -58.20°Flex-it 95.00m 278.36° -58.16°Flex-it 98.00m 278.53° -58.13°Flex-it 101.00m 278.24° -58.21°Flex-it 104.00m 277.94° -58.27°



Type Depth Azimuth PlungeFlex-it 107.00m 277.87° -58.25°Flex-it 110.00m 277.70° -58.15°Flex-it 113.00m 277.74° -58.14°Flex-it 116.00m 277.74° -58.09°Flex-it 119.00m 277.59° -58.15°Flex-it 122.00m 277.38° -58.15°Flex-it 125.00m 277.34° -58.13°Flex-it 128.00m 277.18° -58.12°Flex-it 131.00m 277.48° -58.06°Flex-it 134.00m 277.00° -58.07°Flex-it 137.00m 277.27° -58.09°Flex-it 140.00m 276.22° -58.12°Flex-it 143.00m 276.90° -58.19°Flex-it 146.00m 276.87° -58.18°Flex-it 149.00m 276.76° -58.16°Flex-it 152.00m 276.98° -58.09°Flex-it 155.00m 277.14° -58.01°Flex-Dip 158.00m -58.03°Flex-it 161.00m 277.21° -57.96°Flex-it 164.00m 277.29° -57.89°Flex-it 167.00m 277.79° -57.76°




DESCRIPTION


1.00 9.80 V; PwVolcanic; PillowRoche volcanique (Basalt?)De grain fin à moyen, de couleur gris vert avec teinte jaune, mésocrate et avec évidence de coussin (trempes noirâtres). La longueur des coussins varie de 30 à 90 cm. Par endroits, à proximité destrempes, la roche à un aspect brèchique.Foliation visible, discontinue, à environs 65-70 degrés, définie par chlorite possiblement secondaire.Le réseau de veinules millimétrique à demi- centimétrique de Qz-Cb est présent (1-2 %) avec rarement des altérations aux épontes. La roche et les veinules réagissent aux HCl.

9.80 19.50 CONGLO; GY; PoConglomerate; Yellow Grey; PolymicticConglomerate, polymictic et fortement déformé.Contact sup. avec veine de quartz laiteux sur 25 cm.La matrice est de couleur gris avec teinte jaune (yellow gray matrix), à grain très fin et difficile à distinguer avec les clasts dû à la déformation.Les clast sont généralement fortement étirés, de couleur et de grosseur variée et difficilement perceptible (flou). Les gros clasts sont sub-arrondis, plus perceptible et en petite quantité. L'origine des clastsest difficilement identifiable, mais semble être volcanique et sédimentaire.La foliation est odulante, up and down, de 10 à 40 degrés. Peut-être zone mylonitique?Injecté de cinq veines de quartz décimétrique de couleur blanc laiteux au centre et gris en bordure avec altération aux épontes en chlorites, carbonates et sulfures.Le réseau de veinule Qz-Cb est visible (1%) et déformé.Contact inf. gradule sur 1.5 m avec clast flou et chlorite discontinue secondaire (volcanique pillow)

9.80 22.60 She; FaiShearing20°; FaultingZone de déformation important. Foliation ondulante, up and down, 10-40 degrés donc peut-être charnière de plis?

19.50 42.80 V; PwVolcanic; PillowRoche volcanique (Basalt?)De grain fin à moyen, de couleur gris vert avec teinte jaune, mésocrate et avec évidence de coussin (trempes noirâtres). La longueur des coussins varie de 30 à 90 cm. Par endroits, à proximité destrempes, la roche à un aspect brèchique.Foliation visible, discontinue, à environs 65-70 degrés, définie par chlorite possiblement secondaire.Le réseau de veinules millimétrique à demi- centimétrique de Qz-Cb est fortement présent (3-5 %) avec rarement des altérations aux épontes. La roche et les veinules réagissent aux HCl.Idem que 9.8 à 19.5 mais avec bcp plus de veinules et avec le début de l'unité déformé.

42.80 60.40 CONGLO; GY; PoConglomerate; Yellow Grey; PolymicticConglomerate polymictic clast-supported. Semblable à l'unitée 9.8 à 19.15 mais avec pyrhoritite.Contact sup. graduel de déformé (mylonite ?) à non déforme sur 5 m.La matrice est de couleur gris avec teinte jaune (yellow gray matrix), à grain très fin et avec une forte présence de sulfures (pyrrhotite). Cette pyrrhotite résulte un fort magnétisme de l'unité (voir GDD)Les clasts sont généralement visible, sub-arrondis, parfois étirée, de couleur et de grosseur variée et difficilement perceptible (flou) sur le début de l'uniftée. Les gros clasts sont sub-arrondis, perceptibleet en petite quantité. L'origine des clasts est difficilement identifiable (dû à altération jaune), mais semble être volcanique (++felsique et - mafique) et sédimentaire.Injecté de 7 veines de quartz décimétrique de couleur blanc laiteux au centre et gris en bordure avec altération aux épontes en chlorites, carbonates et sulfures.Le réseau de veinule Qz-Cb est visible (2-3%) et déformé.

42.80 60.40 CtSClast-Supported

43.30 47.80 She; FaiShearing; FaultingZone de déformation important.Mylonite ?. Foliation ondulante, up and down, 10-40 degrés donc peut-être charnière de plis ?

47.50 64.00 Po; CbPyrrhotite; carbonate



DESCRIPTION

Altération en pyrrhotite et carbonate en groupe d'amas ondulante et aléatoire.60.40 77.60 V; Py

Volcanic; PyroclasticRoche fragmentaire ( Sédimentaire ou volcanique ? )Contact sup. graduel de clasts ou fragment grossier à pebbles.De couleur grise, de grain fin à moyen, composée de Qz-Fp et ?. Présence de fragments (pebbles ou amygdules (roche volcanique ?) de Qz et Qz-Cb, de 1 mm à 2 cm et dispersés aléatoirement. J'observeaussi des passages ou lamine noirâtre, dispersé aléatoirement, parfois ondulante, à grain très fin qui me semblent être de l'argillite mais ?. Réclame une pétro. voir lames minces LG15774, LG15775 etLG15776.Sandstone avec figure sédimentaire? ou volcaniclastic?Fortement injecté ( 5% ) du réseau de veinules millimétrique à demi-centimétrique de Qz-Cb à structure plissée. De plus, 3 veines de quartz demi-décimétrique de couleur blanc laiteux au centre et grisen bordure avec altération aux épontes en chlorites, carbonates et sulfures.Logger dans le short log comme une roche pyroclastique.Contact inf. graduel absence de lamine (strate) à lamine sur 50 cm.

77.60 84.24 SS; STSandstone; Stratified/LaminatedRoche sédimentaire.De couleur grise et de grain très fin (silt) à grain fin (sand). Stratifier avec granuloclassement inverse : sand à silt. S0à 70 degré et semble plissée. 5 à 8% de sulfure disséminé de phyrrhotite-chalco-pyrite. Magnétique (voir GDD). Composée de Qz-Fp et ? Composition semblable aux unitées supérieur et inférieur.Le réseau de veinules Qz-Cb est présent (2%) et à structure plissées.

77.60 83.65 Po; CbPyrrhotite; carbonateAltération en pyrhotite et carbonate en bandes minces à aspect disséminée et ondulante. Voir lame mince LG15778.

81.00 81.10 S5CChert

81.50 81.62 S5CChert

82.68 82.90 S5CChert

83.65 84.30 S5CChertCette sucession de chert ou roche QZ-FP est peut-être le résultat d'un plissement ( S0 est plissé et le réseau de veinules aussi ).

84.24 115.50 V; PyVolcanic; PyroclasticIdem à 60.4 à 77.6Voir lames minces LG15780, LG15781, LG15784 et LG15785.Fortement injecté du réseau de veinules Qz-Cb à structure plissées.

115.50 120.50 VC; MoVolcaniclastic; MonomicticRoche fragmentaire de couleur grise.La matrice est silteux-argileuse, de couleur gris plus foncé et correspond à 10 % de la roche.Les fragments sont sub-arrondis avec un aspect étiré, de composition semblable à l'intervalle supérieur (monomictic) et correspondent à 85 % de la roche. Peu faire penser à une roche pyroclastique(structure de flamme).

120.50 123.00 V; PyVolcanic; PyroclasticIdem que 84.24 à 115.5.

120.50 123.00 SheShearing



DESCRIPTION

Zone déformée.123.00 127.46 VC; Mo

Volcaniclastic; MonomicticIdem que 115.5 à 120.5 mais fortement déformé. Fragments monomictic étirés.

127.46 130.90 SS; ARGSandstone; ArgilliteRoche sédimentaire.De couleur grise, à grain fin (0.5 à 2 mm), granuloclassement inverse et avec 2% de bandes minces d'argillite à 75 degrés de CA.

127.46 161.70 GbGraded BeddingGranuloclassement semble inverse.

130.90 169.00 ARG; SSArgillite; SandstoneRoche sédimentaire.Alternance de bandes d'argillite de couleur grise foncée à grain très fin avec des bandes de sandstone de couleur gris pâle à grain fin. On observe des bandes minces (moins de 1 cm), des bandes larges (1à 10 cm) et des bandes irrégulières (figure de charges :slumping et structure de flame)Foliation, S0, en bandes minces, larges et irrégulières à environs 75-65 degrés. De plus, des granuloclassements normale et inverse sont observés.Le réseau de veinules Qz-Cb est présent 2 % à structure plissé et même parfois boudinée.

161.70 169.00 GbGraded BeddingGranuloclassement semble normal.







Collar


Comments




670749.4535326311.432337.109


Flex-Dip 14.00m -57.85°Flex-it 17.00m 276.51° -57.85°Flex-it 20.00m 276.41° -57.81°Flex-it 23.00m 276.17° -57.82°Flex-it 26.00m 276.01° -57.87°Flex-it 29.00m 275.97° -57.87°Flex-it 32.00m 275.06° -57.90°Flex-it 35.00m 275.99° -57.89°Flex-it 38.00m 275.21° -57.92°Flex-it 41.00m 275.81° -57.91°Flex-Dip 44.00m -57.91°Flex-Dip 47.00m -57.99°Flex-it 50.00m 275.59° -57.98°Flex-it 53.00m 275.32° -57.92°Flex-it 56.00m 275.78° -57.86°Flex-Dip 59.00m -57.87°





Type Depth Azimuth PlungeFlex-it 110.00m 275.90° -57.40°Flex-it 113.00m 275.52° -57.44°Flex-it 116.00m 275.95° -57.46°Flex-it 119.00m 276.12° -57.41°Flex-it 122.00m 275.39° -57.43°Flex-it 125.00m 276.32° -57.38°Flex-it 128.00m 275.90° -57.38°Flex-it 131.00m 275.31° -57.42°Flex-it 134.00m 275.72° -57.41°




DESCRIPTION

0.00 1.80 OBOverburdenOverburden

1.80 5.55 V; MasVolcanic; MassiveRoche volcanique ( Dacite ?)À grain fin, de couleur gris à gris foncé et composée de FP-Qz et mica?À aspect massif (pas de structure particulaire). 2-4% de sulfure (pyrrhotite) déssiminé. Voir lame mince 05-23-5.45 pour comfirmer le type de roche.

5.55 19.85 V; PyVolcanic; PyroclasticRoche volcanique à aspect fragmentaire.Les fragments sont composés de qz-fp, mica et 2-4% de pyrrhotite déssiminé le tout à grain fin et de couleur gris foncé beige. Petite réaction aux HCl.Forte présence de petites veinules millimétrique de qz vitreux entre les fragments qui donne l'aspect fragmentaire à la roche. Cet aspect fragmentaire est-il le résultat d'une silicification de la roche oubien une structure primaire volcanique (pyroclastite)? Voir lames minces 05-23-12.85 et 05-23-17.3.Le réseau de millimétrique à demi-centimétrique est présent (1%) avec rarement une altération aux épontes.5.55 à 8 m: tuff ?8 à 19.85 m: lapillistone?

19.85 27.05 SS; CONGLO; Mo; GBSandstone; Conglomerate; Monomictic; Graded BeddingRoche fragmentaire monomictic avec graded bedding.La couleur de la matrice est gris, peu à très présente, à grain fin et composée de qz-fp et ? La morphologie des fragments est sub-arrondis, un peu étirée par endroit mais pas en structure flamme.Deux séquences de granuloclassement inverse sont observés: de 19.85 à 22.85 m et 22.85 à 24.0 m. Ces granuloclassement relèvent des fragments grossier (2 à 4cm) avec peu de matrice suivi de petitsfragments (0.5 à 1 cm) avec beaucoup de matrice (matrice silt-argile)De 24.0 à 27.85 début d'un granuloclassement inverse: les fragments sont grossier, peu de matrice, sub-arrondis et la fin est tronquée1% de veinules Qz-Cb.Contact inf. net 80 degrés.Séquence turbiditaire grossière?

27.05 35.90 SSSandstoneRoche sédimentaire. Aspect massif. Associée à l'intervalle précédant: sa composition ressemble beaucoup à la matrice de l'unitée supérieur.De couleur gris à gris foncé. De grain fin à très fin. Composée de qz-fp et arilige. 2-3% de pyhrrotite déssiminé. 2-3% de veinules millimétrique à demi-centimétrique de Qz-Cb.Contact inf graduel sur 20 cm: de peu argile à beaucoup d'argile.

35.90 136.00 ARG; SSArgillite; SandstoneContact supérieur graduelSéquences turbiditaires. Bandes de couleur gris pâle composées de fragments de quartz-felspath de 0.5 mm à 2 mm compris dans une matrice gris foncé à chlorite et ? , alternant avec des bandes decouleur gris foncé composées de pélite (Shale). La morphologie et la largeur des bandes varient: en bandes mince ( 1mm à 1cm), en bandes large (1cm à 10cm) et en bandes irrégulières (figures decharge, "load-coasts" et/ou slump et/ou déformation). Certaines sections sont pauvres en bandes pélitiques et on observe des granuloclassements inverses. La foliation est visible, en bandes, à environ70-75 degrés. Dans les plans de fissilité des bandes pélitiques, on observe régulièrement la présence de sulfures (pyrhottite, chlaco, ...).De plus, plusieurs veinules millimétriques à demi-centimétriques blanc laiteux composées de Quartz et Calcite à structure ptygmatique et en tension recoupent l'unitée. Les veinules ne semblent pas avoirproduit d'altération aux épontes.

35.90 44.20 SheShearingZone riche en veinules ptygmatique et/ou plissées.Zone de déformation?

47.30 49.30 SSSandstoneDebris flow sanstone with fragmenst of argillite.

60.35 63.90 SSSandstone



DESCRIPTION

Debris flow sanstone with fragmenst of argillite.Zone pauvre en bande d'argillite.

85.32 86.28 BreBrecciaBrecciated vein calcite + Qtz.Contact sup. et inf net à 40 degrés.Composée de fragments subanguleux à anguleux de sandstone et argillite, 0.5 à 3 cm dans une matrice de calcite, quartz et sulfure.

87.60 89.50 SheShearingzone de déformation.

94.90 98.30 SSSandstoneZone pauvre en bande d'argillite.Debris flow sanstone with fragmenst of argillite.

105.90 107.50 SSSandstoneDebris flow sandstone with fragment of argillite.

117.60 121.40 SheShearingZone de déformation ?

134.67 136.00 SSSandstoneDebris flow sandstone with fragment of argillite. Avec veine de qz-cb à structure brèchique.







Collar


Comments




670898.3015326348.636346.653


Flex-Dip 12.00m -59.33°Flex-it 15.00m 277.43° -59.34°Flex-it 18.00m 277.36° -59.30°Flex-it 21.00m 277.54° -59.30°Flex-it 24.00m 277.69° -59.26°Flex-it 27.00m 277.59° -59.34°Flex-it 30.00m 277.59° -59.32°Flex-it 33.00m 277.81° -59.26°Flex-it 36.00m 277.71° -59.30°Flex-it 39.00m 277.65° -59.34°Flex-it 42.00m 277.49° -59.43°Flex-it 45.00m 277.45° -59.44°Flex-it 48.00m 277.54° -59.46°Flex-it 51.00m 277.59° -59.36°Flex-it 54.00m 277.50° -59.40°Flex-it 57.00m 277.59° -59.41°


Flex-it 60.00m 277.41° -59.45°Flex-it 63.00m 277.39° -59.48°Flex-it 66.00m 277.33° -59.51°Flex-it 69.00m 277.49° -59.45°Flex-it 72.00m 277.42° -59.48°Flex-it 75.00m 277.46° -59.52°Flex-it 78.00m 277.68° -59.48°Flex-it 81.00m 277.65° -59.41°Flex-it 84.00m 277.90° -59.33°Flex-it 87.00m 277.95° -59.33°Flex-it 90.00m 278.04° -59.31°Flex-it 93.00m 278.03° -59.29°Flex-it 96.00m 277.99° -59.20°Flex-it 99.00m 278.14° -59.28°Flex-it 102.00m 278.13° -59.31°



DESCRIPTION


1.50 69.90 V; PwVolcanic; PillowRoche volcanique (Dacite?)À grain fin, de couleur gris, leucocrate, composée de Qz-Fp et chlorite et avec évidence de coussins (trempes noirâtres). La longueur des coussins varie de 30 à 100 cm. Par endroits, à proximité destrempes, la roche a un aspect brèchique et peut faire penser à des petite zone de pyroclastic. La roche réagit au HCl. Le réseau de veinules millimétrique à demi-centimétrique est présent (2 %). Présencede sulfure, pyrrhotite-pyrite, cubique (donc remplacement de la pyrite en pyrrhotite), tr-1 % et de 1 à 3mm de grosseur.Foliation visible, définie par alignement de mx de chlorite, discontinue et à environs 65 degrés.

69.90 70.30 V; TBLVolcanic; Tuff Breccia/LapillistoneRoche fragmentaire monomictic :probablement volcanique pyroclastiqueLes fragment sont de couleur gris, à grain fin, 85% de la roche, de 1 mm à 3 cm , sub-arrondis, flou et composée de Qz-Fp et ? . Présence de fragments (pebbles ou amygdules de Qz et Qz-Cb, de 1 mm à1 cm et dispersés aléatoirement 1%.La matrice est à grain très fin, de couleur noir, ondulante (contour des fragments) qui semblent être de l'argillite mais ?.Foliation visible, définie par la matrice, à environs 75 degrésRéclame une pétro. voir lames mincesSandstone avec figure sédimentaire? ou volcaniclastic?

70.30 104.60 V; PwVolcanic; PillowRoche volcaniqueÀ grain fin, de couleur gris, leucocrate, composée de Qz-Fp et chlorite et avec évidence de coussins (trempes noirâtres). La longueur des coussins varie de 30 à 100 cm. Par endroits, à proximité destrempes, la roche a un aspect brèchique, souvent de couleur beige et peut faire penser à des petite zone de pyroclastic. La roche réagit au HCl. Le réseau de veinules millimétrique à demi-centimétriqueest présent (5 %).




119.90 129.37 V; Pw



DESCRIPTION

Volcanic; PillowRoche volcaniqueÀ grain fin, de couleur gris, leucocrate, composée de Qz-Fp et chlorite et avec évidence de coussins (trempes noirâtres). La longueur des coussins varie de 30 à 100 cm. Par endroits, à proximité destrempes, la roche a un aspect brèchique, souvent de couleur beige et peut faire penser à des petite zone de pyroclastic. La roche réagit au HCl. Le réseau de veinules millimétrique à demi-centimétriqueest présent (5 %).Foliation visible, définie par alignement de mx de chlorite, discontinue et à environs 65 degrés.



138.60 156.77 V; TBLVolcanic; Tuff Breccia/LapillistoneRoche fragmentaire monomictic :probablement volcanique pyroclastiqueLes fragment sont de couleur gris, à grain fin, 75% de la roche, de 1 mm à 3 cm , sub-arrondis, flou et composée de Qz-Fp et ? . Présence de fragments (pebbles ou amygdules de Qz et Qz-Cb, de 1 mm à1 cm et dispersés aléatoirement 1%.La matrice est à grain très fin, de couleur noir, ondulante (contour des fragments) qui semblent être de l'argillite mais ?.Foliation visible, définie par la matrice, à environs 75 degrésRéclame une pétro. voir lames mincesSandstone avec figure sédimentaire? ou volcaniclastic?Contact inf. graduel: présence de chlorite dans la matrice sur le dernier mètre.

156.77 214.50 ARG; SSArgillite; SandstoneRoche sédimentaire.Contact supérieur net 65 degrésAlternance de bandes d'argillite de couleur grise foncée à grain très fin avec des bandes de sandstone de couleur gris pâle à grain fin. On observe des bandes minces (moins de 1 cm), des bandes larges (1à 10 cm) et des bandes irrégulières (figure de charges ou zone de déformation : charnière de plis)Foliation, S0, en bandes minces, larges et irrégulières à environs 45 à 75 degrés:de 156.77 à 165.27 la foliation est entre 60 et 75 degrés et avec un granuloclassement qui me semble inversede 165.27 à 181.0 la foliation est up and dwon: charnière de plis ou zone de faille.de 181.0 à 188.43 la foliation est à environs 50 degrés avec crénulations et avec granuloclasse inversede 188.43 à 214.5 la foliation commence vers 50 degrés, augmente à 70 degré avec crénulations et avec un granuloclassement qui me semble inverse.

156.77 161.40 SSSandstoneZone pauvre en bandes pélitiques (noirâtre d'argillite)

165.27 181.00 She; FolShearing; FoldingZone fortement déformée, de couleur gris-noir avec teinte verte. La roche primaire me semble entre argillite/sandstone mais maintenant avec chlorite secondaire et recoupée avec plusieursinjection de veinules de quartz-carbonate déformées (plissées et boudinées)Charnière de plis ou zone de faille?



DESCRIPTION




Ressources Dianor inc

Projet : Chab 2005-11-09

Forage : CHAB 05-27Titre minier : Canton : ChabanelRang : Lot :

Section : 670900Niveau : Place de travail : Wawa Dome

Foré par : Colbert Drilling Du : 2005-09-26 Au : 2005-09-30 Décrit par : Bernard-Olivier Martel Date description : 2005-10-20

Collet

Dimension de la carotte : NQ Cimenté : Non Entreposage : OuiRemarques : Le log préliminaire a été décrit par Bernard-Olivier et Al Miller.

Azimut : 180.00°Plongée : -60.00°Longueur : 192.00m

Longitude (Est)Latitude (Nord)Élévation

UTM

670899.00532615.00345.00

Déviation Type Profondeur Azimut Plongée


Projet : Chab Forage : CHAB 05-27 Page : 2

DESCRIPTION


1.50 11.25 V; Pw; GYVolcanic; Pillow; Yellow GreyRoche volcanique (Andésite ?)À grain fin, de couleur gris foncé à gris jaunâtre, leucocrate et avec évidence de coussins (trempes noirâtres). Composée de Fp-Qz et chlorite (2-4%). La longueur des coussinsvarie de 20 à 70 cm. Par endroits, à proximité des trempes, la roche a un aspect brèchique. Foliation visible, discontinue (alignement de chlorite) et à environs 45-50 degrés.Dureté moyenne. La roche réagit au HCl. Le réseau de veinules millimétrique à demi-centimétrique est fortement présent (3 %), à une teinte jaunâtre et les veinules ont desstructures en tension et ptygmatic.Contact inférieur fortement déformé sur 2m.

1.50 62.60 SrMvsericite/muscoviteZone à altération à séricite. teinte jaunâtre.

9.17 21.15 SheShearingZone de déformation intense. Foliation étrange.Les clasts sont fortement étirées, plissées et parfois boudinéesLa foliation est up and down (10 à 70 degrés) donc charnière de plis?Présence de 4 veines de Qz : deux enfumées et deux blanc laiteux.Zone de chevauchement???

11.25 50.00 S1C; GY; PoConglomerate; Yellow Grey; PolymicticConglomerat clast-supported polymictic.Contact supérieur déformé sur 10 m.Matrice de couleur grise avec teinte jaune (altération à séricite?), à grain très fin, avec 2 % de pyrrhotite et correspond à 15 % de la roche.Clasts : sub-arrondis à arrondis, souvent étirés et correspond à 85 % de la roche.Clasts Felsique, de couleur gris pâle, gris foncé et jaune gris (altération séricite) (75 %)Clasts Mafique? de couleur gris foncé, gris vert foncé et avec altération à leucoxene. (20 %)Clasts Sédimentaire? gris pâle à gris foncé mais incertain. (5 %)Le réseau de veinules millimétriques à demi- centimétriques est présent, 2 %, mais seulement en structure en tension et avec très peu altération aux épontes.

11.25 50.00 CtSClast-SupportedConglomerat clast-supported.

50.00 62.60 V; Pw; Bre; GYVolcanic; Pillow; Breccia; Yellow GreyRoche volcanique ? Fragmentaire et monomictic.Contact supérieur irrégulier (début de la matrice à séricite)De couleur gris pâle jaunâtre à gris foncé.Aspect brèchique, clasts floux, sub-arrondis, étirés et de composition felsique ?Matrice jaunâtre, composée de séricite et pyrrhotite (5-10%).



DESCRIPTION

50.3 à 53.2 : Peu de matrice mais fragments grossier (2 à 4 cm)53.2 à 62.6 : Beaucoup de matrice mais petit fragments (0.5 à 2 cm)Contact inférieur net à 70 degré.Voir pétro des lames minces.

50.30 62.60 SheShearingZone de déformation. Foliation très étrange.

62.60 100.26 VVolcanicRoche possiblement volcanique. Aspect massif.De couleur gris foncé. À grain fin et avec 2% de granule (fragment? vésicule? ou agmyldule?)80.6 à 84.9: zone riche en chlorite (au moins 40%)Fortement injecté de veinules millimétriques à demi-centimétriques de Qz-Cb à structure ptygmatic et tension.Pas de couleur jaune donc arrêt de altération à séricite ?Pas de lamination et/ou stratification donc pas sédimentaire ?Contact inférieur net à 45 degrés.Important de voir pétro des lames minces pour le nom de la roche.

100.26 141.50 S1C; GaG; PoConglomerate; Gray Green; PolymicticConglomerat clast-supported polymictic Gray Green matrix.Matrice (15-20% de la roche) de couleur grise verte, à grain très fin et avec peu de sulfures.Les Clast correspondent à 80-85% de la roche,Clasts felsiques de couleur gris pâle, gris foncé, blanc jaune, à morphologie sub-arrondis à arrondis et généralement plus gros.Clasts mafiques de couleur vert pâle, vert foncé, gris foncé, avec souvent altération à leucoxene et à morphologie sub-arrondie et allongée.Clasts sédimentaires peu présent, plus vers la fin de l'intervalle, au contact de l'argillite. De couleur gris pâle à gris foncé et de petite taille.Les 10 derniers mètre plus grisâtre, matrice plus argileuse donc mélange de dépôt argileux avec conglomérat donc interdigitation( syn-sédimentaire?)Le réseau de veinules Qz-Cb est présent (2%) et à structure en tension et ptygmatic.100.26 à 129.0: Les Clasts sont peux étirés, avec CA 35-45 degrés.129.0 à 141.5: Les clasts sont plus étirés, avec CA 55-65 degrés et injecté de Veines de quartz blanc laiteux donc zone de déformation ?


141.50 192.00 S4A; S2S; GBArgillite; Sandstone; Graded Bedding Roche sédimentaire.Alternance de bandes d'argillite de couleur grise foncée à grain très fin avec des bandes de sandstone de couleur gris pâle à grain fin. On observe des bandes minces (moins de 1cm), des bandes larges (1 à 10 cm) et des bandes irrégulières (figure de charges :slumping et structure de flame ou déformation dans charnière de plis associé avecgranuloclassement normal et inverse ?)Foliation en bandes minces, larges et irrégulières à environs 60-65 degrés. De plus, des granuloclassements normale et inverse sont observés.Le réseau de veinules Qz-Cb est présent 2 % à structure ptgymatic et en tension.

185.50 192.00 S2S; S4A



DESCRIPTION

Sandstone; ArgilliteZone pauvre en bandes d'argillite.

192.00 Fin du sondage

Nombre d'échantillons : 50 Longueur totale échantillonnée : 165.25





Drilled by : Foramex From : 2006-06-08 To : 2006-07-02Geologist : Laura Mancini Description date : 2006-07-24

Collar


Comments




670817.0005326404.000336.000


Flex-it 12.00m 262.26° -87.06°Flex-it 15.00m 264.66° -86.96°Flex-it 18.00m 261.54° -87.26°Flex-it 21.00m 255.04° -87.15°Flex-it 24.00m 254.97° -86.59°Flex-it 27.00m 256.48° -87.13°Flex-it 30.00m 262.00° -86.85°Flex-Dip 33.00m -86.71°Flex-Dip 36.00m -86.20°Flex-it 39.00m 260.05° -86.31°Flex-it 42.00m 256.87° -86.05°Flex-it 45.00m 257.50° -86.03°Flex-it 48.00m 257.27° -86.47°Flex-it 51.00m 248.63° -86.36°Flex-Dip 54.00m -85.74°Flex-Dip 57.00m -86.02°





Type Depth Azimuth PlungeFlex-it 708.00m 256.79° -74.73°Flex-it 711.00m 257.13° -74.70°Flex-it 714.00m 257.50° -74.55°Flex-it 717.00m 258.06° -74.41°Flex-it 720.00m 258.30° -74.42°Flex-it 723.00m 258.92° -74.29°Flex-it 726.00m 259.20° -74.26°Flex-it 729.00m 258.79° -74.30°Flex-it 732.00m 258.36° -74.35°Flex-it 735.00m 258.05° -74.35°Flex-it 738.00m 258.58° -74.27°Flex-it 741.00m 259.56° -74.00°Flex-it 744.00m 258.52° -74.15°Flex-it 747.00m 259.97° -73.92°Flex-it 750.00m 260.11° -73.89°Flex-it 753.00m 259.80° -74.01°Flex-it 756.00m 260.23° -73.90°Flex-it 759.00m 260.54° -73.76°Flex-it 762.00m 259.26° -73.95°Flex-it 765.00m 259.98° -73.85°




DESCRIPTION

0.00 1.50 OBOverburdenoverburden

1.50 12.62 V; V3A; PwVolcanic; Andesite/Dacite; PillowThe rock is a coarse-grained grey pillowed andesite or possibly a basalt. There are dark-grey fine-grained areas that appear to be pillow rinds. These areas are ~30 .00 cm - 82.00 cm apart. The pillowsare coarse-grained and are large (up to 82.00 cm). There is chlorite replacement of primary minerals, as well as quite a bit of carbonate in the pillows. This could be indicative of spilitization. There isvery little disseminated pyrite in the unit. There is a bit of sericite and chlorite alteration throughout the unit. There is a hint of foliations from 11.00 m - 12.00 m at 55º TCA.The rock contains ~3% quartz veins (mm - cm), and tiny little spider veins. Most of the veins have carbonate alterations. Several of the veins are deformed with a sigmoidal form. Some of the veinshave a bit of chlorite and sericite alteration.The contact at 12.62 m is approximate. There is veining and the rock is broken at this point making it difficult to see any real contact.

12.62 27.10 V; V3A; MasVolcanic; Andesite/Dacite; MassiveThe rock is a fine-grained grey massive andesite or possibly basalt. There are a lot of subhedral to euhedral carbonate crystals and small piles of pyrite from ~13.00 m - 15.50 m. There are four largepiles (mm), at 17.40 m. There is very little disseminated pyrite in the rest of the unit. There is some sericite alterations and amygduls filled with carbonate throughout the unit. basalt. There is a slightlycoarser-grained section from ~21.50 m - 24.00 m (there is sericite alteration in this section which may only be giving the appearance of coarse-grain). There is a hint of foliations, between 50º - 60ºTCA, throughout the unit.The rock contains ~5% quartz veins (mm - cm) and tiny spider veins. A lot of the veins are deformed with sigmoidal forms and carbonate alterations. Some of the veins have a bit of sericite and/orchlorite alterations.The contact at 27.10 m is approximate. The rock is altered at this location making it difficult to see clearly, but it looks like the rock grades into the more coarse-grained unit.

12.62 27.10 V; V3A; MasVolcanic; Andesite/Dacite; MassiveMassive fine-grained andesite or basalt flow

27.00 51.00 SrMvsericite/muscoviteSericite alterations in volcanic unit

27.10 72.40 V; V3A; PwVolcanic; Andesite/Dacite; PillowThe rock is a coarse-grained grey pillowed andesite or possibly a basalt. There are dark-grey fine-grained areas that appear to be pillow rinds. These areas are ~10 .00 cm - 25.00 cm apart. There ischlorite replacement of primary minerals, as well as quite a bit of carbonate in the pillows. This could be indicative of spilitization. There are a lot of sericite alterations throughout the unit, particularlyfrom ~27.00 m - 51.00 m, giving that section a yellow color. The pillows are coarse-grained and are smaller than the previous unit (up to 25.00 cm with a couple up to 60.00 cm), and, particularly from54.70 m - 58.15 m, the pillows appear brecciated. There is very little disseminated pyrite in the unit. There appears to be foliations, at ~55º TCA, throughout the unit. This is seen by the way the chloritereplacement is elongated and aligned along with the sericite. This is particularly evident from 43.84 m - 45.00 m.There is <1% quartz veins (mm - cm) and tiny spider veins in the unit. Some of the veins are deformed with a sigmoidal form. The veins have carbonate alterations and a few have a bit of chlorite andsericite alterations.The contact at 72.40 m is approximate. The rock appears to grade from coarse-grained to fine-grained pillowed volcanic rock.

72.40 81.30 V; V3A; PwVolcanic; Andesite/Dacite; PillowThe rock is a fine-grained grey pillowed andesite or possibly basalt. There are dark-grey finer-grained areas that appear to be pillow rinds. These areas are ~10 .00 cm - 28.00 cm apart. The pillows arefine-grained and are medium sized (up to 28.00 cm). There is some chlorite replacement of primary minerals, as well as some carbonate in the pillows. This could be indicative of spilitization. There isa bit of disseminated pyrite, sericite and chlorite alteration in the unit. There is a shear zone from ~80.50 m - 81.30 m. The rock is foliated, with the foliations at ~50º TCA.There is ~5% quartz veins (mm - cm), with carbonate alterations. A lot of the veins are deformed with sigmoidal and brecciated forms.The contact at 81.30 m is approximate. There is a lot of quartz veining and the rock is broken at this point making it difficult to see an actual contact.

80.50 81.30 SheShearingShear zone in volcanic unit

81.30 87.92 V; V3A; TBLVolcanic; Andesite/Dacite; Tuff Breccia/LapillistoneThe rock is a fine-grained grey lapillistone. There are finer-grained dark-grey areas, ~4.00 cm - 20.00 cm apart, that appear to be pillow rinds. The pillows are fine-grained and are small sized (up to20.00 cm), also their small size and random orientations indicate they could be brecciated pillows. There is some chlorite replacement of primary minerals, as well as some carbonate in the pillows. This



DESCRIPTION

could be indicative of spilitization. There is a hint of foliations at ~60º TCA. There is a small amount of disseminated pyrite in the unit.there is ~3% quartz veins (mm - cm), and tiny little spider veins. The veins have carbonate alterations and a few have a bit of sericite and chlorite alterations. Some of the veins are deformed withsigmoidal forms.The contact at 87.92 m is approximate. There is a quartz vein right at this point which might be obscuring the contact, otherwise the rock looks like it grades into the pyroclastic unit.

87.92 94.26 V; V3A; TBLVolcanic; Andesite/Dacite; Tuff Breccia/LapillistoneThe rock is a fine-grained grey volcanic rock, possibly a tuff/ash. There are fine-grained brownish colored layers throughout the unit that could be ash. There are foliations (or possibly layers), at ~65ºTCA throughou the unit. There is some carbonate, along with a little sericite and chlorite alteration and a tiny amount of disseminated pyrite in the unit.There is <1% quartz veins (mm - cm), with carbonate alterations. A few of the veins are deformed with sigmoidal and brecciated forms.The contact at 94.26 m is approximate. The rock is broken at this point making it difficult to see any real contact.

94.26 99.50 V; V3A; PwVolcanic; Andesite/Dacite; PillowThe rock is a fine-grained grey pillowed andesite or possibly basalt. There are dark-grey finer-grained areas that appear to be pillow rinds. These areas are ~10 .00 cm - 26.00 cm apart. The pillows arefine-grained and are medium sized (up to 26.00 cm, with one that is 33 cm). There is some chlorite replacement of primary minerals, as well as some carbonate in the pillows. This could be indicative ofspilitization. There is a tiny bit of disseminated pyrite, along with some sericite and chlorite alteration in the unit. The rock is foliated, with the foliations at ~65º TCA.There is <1% quartz veins (mm - cm), with carbonate alterations. A few of the veins are deformed with sigmoidal and brecciated forms.The contact at 99.50 m is approximate. There is a lot of quartz veining and the rock is broken at this point making it difficult to see an actual contact.

99.50 164.86 V; V3A; MasVolcanic; Andesite/Dacite; MassiveThe rock is a fine-grained massive andesite or possibly basalt. The whole unit is highly deformed, but there are small sections that are not and they appear massive (no obvious foliations, layers, pillows,etc.). The rock is greyish colored but looks splattered with very light grey to white and greyish-green (has a very non-uniform coloring). The light color is from carbonate alteration and the greyish-greenis from chlorite replacement of primary minerals (spilitization). The rock, including the carbonate and chlorite, is strongly foliated at 55º TCA. There are no obvious disseminated or piles of pyrite in theunit. It is very difficult to properly identify this section. It has the appearance of both a shear zone and/or possibly pyroclastic rock.There is ~8% quartz veins (mm - cm), and tiny spider veins in the rock. The percentage could be higher but it is difficult to tell with the amount of deformation. Almost all the veins have been orientedwith the foliation. Some of the veins are deformed and have a sigmoidal and brecciated form. There is a lot of carbonate alteration in the veins. A few of the veins have a tiny amount of disseminatedpyrite associated with them.The contact at 164.86 m is approximate. The strong deformation makes it difficult to see any real contact.

99.50 164.86 V; V3A; MasVolcanic; Andesite/Dacite; MassiveMassive fine-grained andesite or basalt flow

99.50 164.86 SheShearingShear zone(?), in volcanic unit. The rock is very deformed with strong foliations and the quartz veins are oriented to the foliation. The non-uniform color and coarse-grained texture makes therock look like it could also possibly be pyroclastic.

164.86 174.00 V; V3A; PyVolcanic; Andesite/Dacite; PyroclasticThe rock is a coarse-grained light grey-green to grey colored pyroclastic andesite or possibly basalt. There are a lot of small sub-angular to sub-rounded fragments and shards (1 mm - 2 cm), in the unit.Some of the fragment have a brownish color, possibly from alteration. Most of the fragments are different shades of grey and a few have a grey-green color. Most of the fragments appear stretched andthere is a strong foliation to the unit at ~60º TCA (shearing?). There is some sericite and a lot of chlorite and carbonate alteration in the unit. There is no obvious pyrite in the unit. There are what couldpossibly be light yellowish-brown ash layers (mm), throughout the unit. These layers could also be sericite alteration.The rock contains ~15% quartz veins (mm - cm), and tiny spider veins. The veins have a lot of carbonate alterations and are oriented to the foliation. Several of the veins are deformed and havesigmoidal and brecciated forms. The vein at 172.80 m appears to have smokey quartz.The contact at 174.00 m is approximate. The rock is broken and there are missing pieces at this point, but the rock becomes fine-grained right after 174.00 m

174.00 182.30 V; V3A; TaVolcanic; Andesite/Dacite; Tuff /AshThe rock is a fine-grained grey tuff with grey-green to brownish colored layers, possibly ash. No discernable contact can be seen between layers, the rock is foliated at ~55º - 60º TCA, which may beobscuring the contacts or the layers are actually sericite alterations within the foliation. There is a tiny bit of disseminated pyrite throughout the unit.There is ~10% quartz veins (mm - cm), and tiny spider veins in the unit. There are some piles of pyrrhotite, carbonate alterations and a bit of sericite and chlorite in the veins. The veins are oriented withthe foliation and a lot of the veins are deformed with sigmoidal forms.The contact at 182.30 m is approximate. The rock is broken and there are pieces missing at this point, but the rock becomes finer-grained right after 182.30 m.



DESCRIPTION

182.30 187.61 V; V3A; TBLVolcanic; Andesite/Dacite; Tuff Breccia/LapillistoneThe rock is a medium-grained grey lapillistone. There are sections that are finer-grained or coarser-grained. The medium and coarse-grained sections have what appear to be fragments that have beenstretched and imbricated at ~55º TCA. The fragments are similar to the ones in the unit from 164.86 m - 174.00 m. The rock is foliated at ~55º TCA. There is a tiny bit of sericite and disseminatedpyrite in the unit, along with chlorite and carbonate alterations.The rock contains ~4% quartz veins (mm - cm), and tiny spider veins. Most of the veins are deformed with sigmoidal forms, and have carbonate alterations. Some have a bit of chlorite alteration and acouple look like they contain a bit of smokey quartz.The contact at 187.61 m is approximate. The rock grades into the argillite.

187.61 308.57 SS; ARGSandstone; ArgilliteThe rock is a medium to coarse-grained grey sandstone with fine-grained medium-grey to black argillite layers. The rock is composed of ~65% sandstone (mm - m), 30% argillite (mm - cm) and 5%quartz veins (mm - cm).The contacts between the sandstone and argillite layers are irregular to gradational. There are sections from 204.00 m - 219.00 m and 287.96 m - 288.92 m, where the contacts are convoluted and thelayers are mixed together (shear zone? Mixing caused by supersaturation? Rip-up fragments?). This is most evident from 217.10 m - 218.00 m (217.10 m - 217.50 m, the argillite layers are sub-parallelTCA). From 247.50 m - 249.00 m there are sandstone clasts in an argillite matrix within a sandstone section. There are several small faults (cm) throughout the unit with a larger one from 229.68 -230.56 m. The rock is very fractured and ground up (rock flour), at these locations. There is a bit of sericite and chlorite alteration and disseminated pyrite and pyrrhotite throughout the unit. There is ashear zone from 268.88 m - 279.00 m. There are several very coarse-grained sandstone sections with very little argillite, wnere pebbles (2 mm - 4 mm), of quartz and argillite can be seen.Most of the quartz veins are deformed, with sigmoidal and brecciated forms, and have carbonate alterations. There are some pyrrhotite piles associated with a few veins.The contact at 308.57 m is irregular and ~ perpendicular TCA (~88º).

189.00 189.90 FaiFaultingfault in sandstone unit



204.00 208.60 SheShearingSheared (?) section in sandstone unit. Could also be caused by supersaturation or rip-up fragments


258.70 262.64 SSSandstoneVery coarse-grained sandstone with ~1% argillite within a sandstone-argillite unit

266.39 268.88 SSSandstoneVery coarse-grained sandstone with <1% argillite within a sandstone-argillite unit

268.88 279.00 SheShearingShear zone in sandstone unit

294.66 305.00 SSSandstoneCoarse-grained sandstone with ~15% argillite within a sandstone-argillite unit

308.57 374.74 SS; MasSandstone; MassiveThe rock is a grey coarse-grained massive sandstone. There are small areas throughout the unit that are finer-grained. There appears to be primary (bedding) structures in these areas at ~45º TCA,particularly in the fine-grained siltstone (52%)-sandstone(48%) section from 321.00 m - 328.20 m. This section also contains euhedral and subhedral carbonate crystals. There are blue quartz eyes and a



DESCRIPTION

bit of carbonate throughout the unit. There is a hint of foliation in the unit at ~55º TCA (there appears to be alternating light and dark bands in which the grains and pebbles seem to have a preferedorientation). There is a shear zone from 370.31 m - 374.74 m, with sericite and a bit of carbonate alteration. There is a little disseminated and piles of pyrite scattered throughout the unit.There is ~2% quartz veins (mm - cm), with carbonate alterations. Some of the veins have a bit of sericite and chlorite alteration. There are a couple of large veins from 345.80 m - 346.06 m and 353.30m - 353.45 m. A few of the veins are deformed with a sigmoidal form and a couple are sub-parallel TCA.The contact at 374.74 m is approximate. The rock is sheared and altered at this point but the color change from grey to a much darker grey is abrupt at 374.74 m.

321.00 328.20 S; SSSiltstone; SandstoneFine-grained siltstone-sandstone section with possible primary bedding in sandstone unit.

370.31 405.00 SheShearingShear zone in sandstone unit.

374.74 381.75 ARGArgilliteThe rock is a fine-grained dark-grey to black argillite. The shear zone that started in the previous unit continues all the way through this unit and has badly deformed the rock. The section from 375.00m - 381.00 m has the appearance of fault breccia. From 379.00 m - 380.20 m there is a lot of sericite alteration giving the rock a brownish color. There is some carbonate alteration and quite a bit ofpiles of pyrrhotite and pyrite throughout the unit. The rock is foliated at ~82º TCA.There appears to be <1% quartz veins (mm - cm), there could be more but it is difficult to tell. The veins have brecciated forms and carbonate alterations. Most of the veins are oriented to the foliation.The contact at 381.75 m is approximate. The deformation makes it difficult to see an actual contact.

381.75 389.52 V; V3A; TaVolcanic; Andesite/Dacite; Tuff /AshThe rock is possibly a fine-grained andesite/basalt tuff ( it could also be sedimentary). The shear zone that was in the previous two unit continues all the way through this unit and has badly deformed therock. There is heavy sericite alteration through the whole unit giving it a yellowish-brown color. Both the deformation and alteration make it very difficult to properly identify the rock. There is a bit ofdisseminated pyrite and carbonate alteration in the unit. The rock is foliated at ~55º TCA.The rock contains ~25% quartz veins (mm - cm), and tiny little spider veins. The veins contain a lot of carbonate and are a very dark color (dark-grey?). Most of the veins are deformed with a sigmoidalform. Some of the veins are oriented with the foliation.The contact at 389.52 m is approximate. The deformation makes it difficult to see an actual contact.

389.52 409.55 ARGArgilliteThe rock is a fine-grained dark-grey to black argillite with some siltstone and sandstone layers. The shear zone that was in the previous three unit continues all the way to ~405.00 m and has deformedthe rock obscuring contacts between layers and making it difficult to give percentages (the layers are often convoluted and mixed together). The rock is strongly foliated at 70º TCA. There isdisseminated pyrite throughout the unit.There appears to be <1% quartz veins (mm - cm) in the rock. There may be more but it is difficult to tell. The veins are deformed with sigmoidal, brecciated and ptygmatic forms. There are carbonatealterations and piles of pyrite associated with the veins. Some of the veins are oriented with the foliation.The contact at 409.55 m is irregular and at 65º TCA.

409.55 420.40 SS; MasSandstone; MassiveThe rock is a medium to fine-grained grey massive sandstone. The core is quite broken up and blocky making it difficult to see features clearly. There appears to be foliations at 55º TCA (the grainsseem to have a prefered orientation). The unit has some sericite and chlorite alteration and a bit of disseminated pyrite throughout. There are a couple of small faults from 417.6 m - 418.00 m and420.00 m - 420.40 m (brecciated and lots of rock flour).The rock contains ~4% quartz veins (mm - cm), and a lot of tiny little spider veins. Because the rock is so broken, it is difficult to give a proper percentage of veins. Most of the veins are deformed withsigmoidal and brecciated forms, and have quite a bit of carbonate alteration.The contact at 420.40 m is approximate. The rock is broken at this point and there are pieces missing.

417.60 418.00 FaiFaultingFault in sandstone unit.

420.00 420.40 FaiFaultingFault in sandstone unit

420.40 449.36 SS; CONGLO; G; STSandstone; Conglo; Green; Stratified/Laminated



DESCRIPTION

The rock is made up of repetitive sequences with alternating zones of grey fine to coarse-grained pebble sandstone (several cm - several m) and grey granular to pebble conglomerate (cm - several m).The sequences appear to be from the same sources deposited by different events. The rock is composed of 84% sandstone, 15% conglomerate and 1% quartz veins. The contacts between zones aregradational.The fine-grained sandstone zone from 434.00 m - 435.00 m appears to have possible primary bedding structures (alternating bands that are lighter or darker), at ~55º TCA. The pebble sandstone zonefrom 420.40 m - 421.74 m, has 1 fine-grained grey clast 2 cm in size, with the rest under 1 cm.The conglomerate zones are polymictic (limited), clast-supported and composed of ~70% felsic clasts and 30% matrix. The clasts range in shape from angular to sub-rounded and in size from 1 mm - 1cm. There is quite a bit of chert and some small dark-grey to black clasts that could be argillite. There are some fine-grained light-grey to creamy colored clasts that could be a felsic tuff. There is onelarge (9 cm) pinkish colored porphyritic clast that could be pyroclastic. A thin section (LG20332-1), was taken of the clast and surrounding matrix, to determine composition. Some of the clasts,particularly from 434.80 m - 435.86 m, appear to be stretched and imbricated at 50º TCA. The cherty clasts are very angular and sharp. The matrix is fine-grained grey colored with a hint of foliationsat 50º TCA. There is quite a bit of carbonate alteration and some disseminated pyrite throughout the matrix.There is a bit of sericite, chlorite and carbonate alteration (the coarser sections have more carbonate), and some disseminated pyrite throughout the unit. The rock is foliated at 50º TCA.The veins are mm - cmin size and some are deformed with brecciated form. Most of the veins contain carbonate alterations and some have a bit of sericite and chlorite alteration.The contact at 449.36 is approximate. The rock grades from a more green to a more grey color.

449.36 454.00 SS; CONGLO; Ga; STSandstone; Conglo; Gray; Stratified/LaminatedThe rock is a sequence with a zone of medium-grey medium-grained sandstone (m) and a zone of medium-grey conglomerate (m). The rock is composed of ~50% sandstone, 49% conglomerate and 1%quartz veins.The sandstone zone appears massive with a couple of argillite shards. There are no obvious foliations or other structural features. There is a small amount of carbonate alteration and disseminated pyritein the sandstone. The contact between the sandstone zone and the conglomerate zone is irregular and at ~33º TCA.The conglomerate zone is mostly monomictic, clast-supported and is composed of ~80% felsic clasts and 20% matrix. The clasts range in shape from sub-angular to sub-rounded and in size from 1 mm -2 cm. There are fine-grained grey and dark-grey clasts that are probably argillite. The clasts are imbricated at ~40º TCA. The matrix is fine-grained medium grey in color and is foliated at 40º TCA.There is a bit of carbonate alteration and disseminated pyrite throughout the matrix.The veins are mm - cm in size and have carbonate alterations. Most of the quartz is in one vein from 450.25 m - 450.36 m, which has a bit of chlorite alteration.The contact at 454.00 m is approximate. There is a quartz vein at this point obscuring the contact, but the rock is more green right after 454.00 m.

454.00 464.33 CONGLO; SS; C/ARG; C/F; STConglo; Sandstone; Argillite Clasts; Felsic Clast; Stratified/LaminatedThe rock is made up of repetitive sequences with alternating zones of grey-green polymictic (limited) conglomerate (several m), and grey-green coarse-grained sandstone (several m). The sequencesappear to be from the same sources deposited by different events. The rock is composed of 60% conglomerate, 40% sandstone and <1% quartz veins. The contacts between conglomerate and sandstonezones are gradational.The conglomerate zones are polymictic (limited), mainly clast-supported and are composed of ~80% felsic clasts and 20% matrix. The clasts range in shape from angular to sub-rounded and in size from1 mm - 2 cm. There are several fine-grained grey and dark-grey clasts that are probably argillite. There are some very fine-grained pinkish-grey clasts that could be chert (very hard). There are a few tinyfine-grained creamy colored clasts that could be felsic tuff. The clasts are imbricated at ~35º TCA. The matrix is fine-grained and grey-green in color and is foliated at ~40º TCA. There is quite a bit ofcarbonate and chlorite alteration, along with some disseminated pyrite throughout the matrix.The sandstone zones appear massive with a couple of argillite and several chert shards. There are foliations at ~40º TCA (the grains and fragments appear to have a prefered orientation). There is quite abit of carbonate and some chlorite alteration, and very little disseminated pyrite in the sandstone.The veins are mm - cm in size and have carbonate alterations.The contact at 464.33 m is approximate. There is no sharp contact, but there are mostly argillite clasts after this point.

464.33 468.53 SS; CONGLO; C/ARG; STSandstone; Conglo; Argillite Clasts; Stratified/LaminatedThe rock is made up of repetitive sequences with alternating zones of grey medium-grained sandstone (several cm - several m) and grey conglomerate (cm - several m). The sequences appear to be fromthe same sources deposited by different events. The rock is composed of ~69% sandstone, 29% conglomerate and 2% quartz veins. The contacts between sandstone and conglomerate zones are irregular(at 38º TCA), to gradational.The sandstone zones appear massive and contains a few argillite shards. There is a hint of foliations (seen in the orientation of the tiny fragments), at 45º TCA. There is quite a bit of carbonate alterationand some disseminated pyrite in the sandstone.The conglomerate zones are mostly monomictic, matrix-supported and are composed of ~80% matrix and 20% felsic clasts. The clasts range in shape from angular to sub-rounded and in size from 1 mm- 1 cm. There are several fine-grained grey to dark-grey clasts that are probably argillite and some small fine-grained light-grey to creamy colored clasts that could be a felsic tuff. The clasts areimbricated at ~38º - 35º TCA. The matrix is fine-grained and grey in color and is foliated at ~38º TCA. There is quite a bit of carbonate alteration and some disseminated pyrite and pyrrhotitethroughout the matrix.The veins are mm - cm in size and have carbonate alterations. Some of the veins are slightly deformed with sigmoidal form.The contact at 468.53 m is approximate. The rock grades from mostly argillite clasts, through sandstone, to mostly chert clasts.



DESCRIPTION

468.53 476.30 CONGLO; SS; C\S5C; STConglo; Sandstone; Chert Clasts; Stratified/LaminatedThe rock is made up of repetitive sequences with alternating zones of grey-green polymictic (limited) conglomerate (cm - m), and grey-green medium-grained sandstone (several cm - m). The sequencesappear to be from the same sources deposited by different events. The rock is composed of ~60% conglomerate, 40% sandstone and <1% quartz veins. The contacts between zones are gradational.The conglomerate zones are polymictic (limited) and are medium-supported (1/2 clast and 1/2 matrix-supported). The clasts range in shape from angular to sub-rounded and in size from 1 mm - 4 cm.The clasts are mostly chert along with some fine-grained grey and dark-grey clasts that are probably argillite. There are some small fine-grained pinkish-grey clasts that that appear to be porphyritic,possibly pyroclastic. There are a few tiny fine-grained creamy colored clasts that could be felsic tuff. The clasts are imbricated at ~40º - 45º TCA. The matrix is fine-grained and grey-green in color andis foliated at ~40º TCA. There is quite a bit of carbonate and chlorite alteration, along with a tiny bit of disseminated pyrite throughout the matrix.The sandstone zones appear massive with a few tiny argillite and felsic fragments scattered throughout. There is a hint of foliations (the grains seem to have a prefered orientation), at ~40º TCA. There iscarbonate and a bit of chlorite alteration, along with disseminated pyrite in the sandstone.The veins are mm - cm in size and have carbonate alterations. A few are slightly deformed with sigmoidal form.The contact at 476.30 m is approximate. There is no sharp contact, but there are more argillite than chert clasts after this point.

476.30 506.28 CONGLO; SS; C/ARG; C/F; STConglo; Sandstone; Argillite Clasts; Felsic Clast; Stratified/LaminatedThe rock is made up of repetitive sequences with alternating zones of grey-green polymictic (limited) conglomerate (several cm - several m), and grey-green coarse-grained sandstone (several cm -several m). The sequences appear to be from the same sources deposited by different events. The rock is composed of 65% conglomerate, 35% sandstone and <1% quartz veins. The contacts betweenzones are sharp to gradational. From 476.59 m - 477.00 m, there is a fine-grained grey clast or possibly siltstone layer. There appears to be possible primary bedding (alternating lighter and darkerlayers), at 33º TCA. The upper and lower contacts of the clast/layer (?) are irregular and at 35º TCA. There is another fine-grained grey clast/layer (?) from 489.28 m - 489.82 m, this one appearsmassive with irregular contacts. The upper contact is at 49º TCA and the lower at 45º TCA.The conglomerate zones are polymictic (limited), and are medium-supported (1/2 clast and 1/2 matrix-supported). The conglomerate zones are composed of ~70% felsic clasts and 30% matrix. Theclasts range in shape from angular to sub-rounded and in size from 1 mm - 5 cm. There are several fine-grained grey and dark-grey clasts that are probably argillite. There are some very fine-grainedpinkish-grey and yellowish-grey clasts that could be chert (very hard). There are a lot of tiny fine-grained light-grey and creamy colored clasts that could be felsic tuff (some of these clasts lookporhyritic and could be pyroclastic). The clasts are imbricated between 35º - 40º TCA (some of the clasts look stretched). The matrix is fine-grained and grey-green in color and is foliated at ~40º TCA.There is quite a bit of carbonate and chlorite alteration, along with some disseminated pyrite throughout the matrix.The sandstone zones appear massive with a few argillite and felsic clasts. Some areas in the sandstone zones appear foliated at ~40º TCA (the grains and fragments appear to have a prefered orientation).There is a bit of carbonate and chlorite alteration, and very little disseminated pyrite throughout the sandstone zones.The veins are mm - cm in size and have carbonate alterations.The contact at 506.28 m is irregular and at ~33º TCA.

506.28 530.23 CONGLO; SS; C/F; STConglo; Sandstone; Felsic Clast; Stratified/LaminatedThe rock is made up of repetitive sequences with alternating zones of grey-green polymictic (limited) conglomerate (several cm - several m), and grey-green medium to coarse-grained sandstone (severalcm - several m). The sequences appear to be from the same sources deposited by different events. The rock is composed of 85% conglomerate, 15% sandstone and <1% quartz veins. The contactsbetween zones are sharp to gradational. From 512.50 m - 516.50 m, the section has argillite clasts that are larger and more rounded than the clasts in previous units, possibly indicating a higher energydepositional environment. There are no contacts which suggests it is part of the unit (not a separate unit). This whole section has been selected for Caustic Fusion.The conglomerate zones are polymictic (limited), and are mainly clast-supported. The conglomerate zones are composed of ~75% felsic clasts and 25% matrix. The clasts range in shape fromsub-angular to sub-rounded (there are a few angular clasts), and in size from 1 mm - 8 cm. There are several fine-grained grey and dark-grey to black clasts that are probably argillite. There are somevery fine-grained pinkish-grey and yellowish-grey clasts that could be chert (very hard). There are a lot of tiny fine-grained light-grey and creamy colored clasts that could be felsic tuff (some of theseclasts look porhyritic and could be pyroclastic). The clasts are imbricated at ~40º TCA (some of the clasts look stretched). The matrix is fine-grained and grey-green in color and is foliated at ~40ºTCA. There is quite a bit of carbonate and chlorite alteration, along with some disseminated pyrite and a few blue quartz eyes throughout the matrix.The sandstone zones appear massive with a few argillite and felsic clasts. Some areas in the sandstone zones appear foliated at ~45º TCA (the grains and fragments appear to have a prefered orientation).There is carbonate and a little chlorite alteration, along with disseminated pyrite throughout the sandstone zones.The veins are mm - cm in size and have carbonate alterations.The contact at 530.23 m is approximate. The core is broken and there is a small vein at this point which may be obscuring the contact.

512.50 516.50 CONGLO; SS; C/ARGConglomerate other; Sandstone; Argillite ClastsThe conglomerate in this section has larger rounder argillite clasts than what has been seen in previous units.

530.23 532.47 SS; CONGLO; C/ARG; STSandstone; Conglo; Argillite Clasts; Stratified/LaminatedThe rock is a sequence with zones of grey medium-grained sandstone (several cm) and grey conglomerate (several cm). The rock is composed of ~50% sandstone, 49% conglomerate and 1% quartzveins. The contacts between zones are gradational.



DESCRIPTION

The sandstone zones appear to be mainly massive with quite a bit of quartz veins. From 531.16 m - 531.25 m there seems to be possible argillite layers with irregular contacts at ~45º TCA (there are alsosmall argillite shards in the same location, therefore the "layers" may only be clasts). The rock is foliated at ~40º TCA. There is some carbonate alteration and disseminated pyrite in the sandstone zones.The conglomerate zones are polymictic (very limited), matrix-supported and are composed of ~80% matrix and 20% felsic clasts. The clasts range in shape from angular to sub-rounded and in size from1 mm - 1 cm. There are several fine-grained grey to dark-grey clasts that are probably argillite and some small fine-grained light-grey to creamy colored clasts that could be a felsic tuff. There are a fewpinkish colored clasts that look porhyritic and could be pyroclastic. The clasts are imbricated at ~45º TCA. The matrix is fine-grained and grey in color and is foliated at ~45º TCA. There is somecarbonate alteration and disseminated pyrite throughout the matrix.The veins are mm - cm in size and have carbonate alterations. Some of the veins are slightly deformed with sigmoidal form.The contact at 532.47 m is approximate. The rock is broken at this point and there is quite a bit of chlorite alteration starting right after 342.47 m. This makes it difficult to see an actual contact.

532.47 581.17 CONGLO; SS; C/F; STConglo; Sandstone; Felsic Clast; Stratified/LaminatedThe rock is made up of repetitive sequences with alternating zones of grey-green polymictic (limited) conglomerate (several cm - several m), and grey-green medium to coarse-grained sandstone (severalcm - several m). The sequences appear to be from the same sources deposited by different events. The rock is composed of 74% conglomerate, 23% sandstone and 31% quartz veins. The contactsbetween zones are gradational. From 532.47 m - 546.00 m, there is quite a bit of chlorite and sericite(?) alteration making it difficult to see the clasts and matrix clearly.The conglomerate zones are polymictic (limited), and are medium-supported (has areas that are clast-supported or matrix-supported). The conglomerate zones are composed of ~70% felsic clasts and30% matrix. The clasts range in shape from sub-angular to sub-rounded (there are a few angular clasts), and in size from 1 mm - 6 cm. There are several fine-grained grey and dark-grey to black claststhat are probably argillite. There are some very fine-grained light-grey, pink to pinkish-grey and yellowish-grey clasts that could be chert (very hard). There are a lot of tiny fine-grained light tomedium-grey and creamy colored clasts that could be felsic tuff (some of these clasts look porhyritic and could be pyroclastic). There are several pinkish-grey porhyritic clasts that could also bepyroclastc. From 578.50 m - 578.60 m, there are a couple of small clasts that are very green in color and could possibly be mafic or very altered with chlorite. The clasts are imbricated at ~45º TCA(some of the clasts look stretched). The matrix is fine-grained and grey-green in color and is foliated at ~45º TCA. There is quite a bit of carbonate and chlorite alteration, along with some disseminatedpyrite and a few blue quartz eyes throughout the matrix. From ~561.80 m - 567.00 m, there is a pale-pink to medium pink mineral that could be leucoxene alteration (it is difficult to tell if the alterationis in a clast or the matrix).The sandstone zones appear massive with a few tiny argillite and felsic clasts. Some areas in the sandstone zones appear foliated at ~45º TCA (the grains and fragments appear to have a preferedorientation). There is carbonate and some chlorite alteration, also disseminated pyrite throughout the sandstone zones.The veins are mm - cm in size and have carbonate alterations. A few of the veins have some chlorite and sericite alterations and some disseminated pyrite associated with them. Some of the veins areslightly deformed with sigmoidal and brecciated forms.The contact at 581.17 m is slightly irregular and at ~35º TCA.

581.17 587.98 CONGLO; C/ARG; C/FConglo; Argillite Clasts; Felsic ClastThe rock is a grey colored polymictic conglomerate that grades from granual to pebble sized clasts. There is a small siltstone/sandstone section (cm), from ~583.70 m - 584.10 m. The upper and lowercontacts between the conglomerate and siltstone/sandstone are irregular and at ~45º TCA. The siltstone and sandstone layers within the section are cm in size and also have irregular contacts at ~45ºTCA.The conglomerate is composed of ~73% felsic clasts, 25% matrix and 2% quartz veins. The conglomerate is clast-supported with the clasts ranging in shape from angular to sub-rounded and in sizefrom 1 mm - 4 cm. There is a lot of argillite (dark-grey to black, soft), as well as a lot of fine-grained grey to light-grey clasts that could be a felsic tuff (a lot of these have quite a bit of chloritealteration). There are some fine-grained creamy colored clasts that are porphyritic, possibly pyroclastic. The clasts are imbricated at ~40º TCA.The matrix is fine-grained grey in color and is foliated at ~40º TCA. There is quite a bit of carbonate and a bit of chlorite alteration, along with some disseminated pyrite throughout the matrix.The quartz veins are mm - cm in size, with carbonate alterations. Some of the veins are deformed with sigmoidal and brecciated forms. There is a large vein from 586.40 m - 586.60 m (slightlybrecciated with a bit of chlorite).The contact at 587.98 m is approximate. There is a quartz vein obscuring the actual contact.

587.98 593.76 CONGLO; C/ARGConglo; Argillite ClastsThe rock is a medium-grey colored polymictic (limited), conglomerate. The rock is medium-supported (areas that are clast-supported or matrix-supported) and composed of 64% felsic clasts, 35%matrix and 1% quartz veins. The clasts range in shape from angular to sub-rounded and in size from 1mm - 5 cm There are a lot of argillite clasts (fine-grained, medium to dark-grey, soft), as well as afew fine-grained grey clasts that could be a felsic tuff. Also, there are a few fine-grained grey porphyritic clasts that could be pyroclastic. A lot of the argillite clasts look like rip-up fragments (elongatedwith sharp curled-up ends), others look stretched and have a slight sigmoidal shape. The clasts are imbricated at ~35º TCA.The matrix is fine-grained grey in color and is foliated at ~35º TCA. There is quite a bit of carbonate and a bit of chlorite alteration, along with disseminated pyrite throughout the matrix.The quartz veins are mm - cm in size, with carbonate alterations. Some of the veins are deformed with sigmoidal and brecciated forms.The contact at 593.76 m is approximate. The rock grades from mostly argillite clasts to more felsic clasts.

593.76 598.04 CONGLO; C/ARG; C/FConglo; Argillite Clasts; Felsic ClastThe rock is a grey colored polymictic conglomerate. The rock is clast-supported and is composed of ~80% felsic clasts, 20% matrix and <1% quartz veins. The clasts range in shape from angular to



DESCRIPTION

rounded and in size from 1 mm - 4 cm. There are several clasts that are much larger (up to 12 cm), than seen in previous units. There are several argillite clasts (dark-grey to black, soft), as well as a lotof fine-grained grey to light-grey clasts that could be a felsic tuff (a lot of these have quite a bit of chlorite alteration). There are some fine-grained pinkish to creamy colored clasts that are porphyritic,possibly pyroclastic. There is a large (9 cm) coarse-grained porphyritic clast that could also be pyroclastic. There is a large (12 cm) fine-grained grey clast that appears porphyritic, but could also befeldspar crystals. The clasts are imbricated at ~40º TCA.The matrix is fine-grained grey in color and is foliated at ~40º TCA. There is quite a bit of carbonate and a bit of chlorite alteration, along with some disseminated pyrite throughout the matrix.The quartz veins are mm in size (mostly tiny little spider veins), with carbonate alterations. Some of the veins are deformed with sigmoidal form.The contact at 598.04 m is approximate. It is where the argillite clasts start to become dominant.

598.04 609.59 SS; CONGLO; C/ARG; STSandstone; Conglo; Argillite Clasts; Stratified/LaminatedThe rock is made up of repetitive sequences with alternating zones of grey medium-grained sandstone (several cm - several m) and grey conglomerate (several cm). The sequences appear to be from thesame sources deposited by different events. The rock is composed of ~74% sandstone, 23% conglomerate and 3% quartz veins. The contacts between sandstone and conglomerate zones are irregularand at ~37º TCA.The sandstone zones appear mostly massive and contains a few argillite shards. From 607.16 m - 607.40, there appears to a sandstone layer within a sandstone section (the contacts are sharp and at ~35ºTCA). There is a hint of foliations (seen in the orientation of the grains and fragments), between 35º - 40º TCA. There is some carbonate alteration and a tiny bit of disseminated pyrite in the sandstone.The conglomerate zones are mostly monomictic, matrix-supported and are composed of ~80% matrix and 20% felsic clasts. The clasts range in shape from angular to sub-rounded and in size from 1 mm- 6 cm. There are several argillite clasts (very fine-grained, grey to dark-grey, soft), and some small fine-grained light-grey to grey and creamy colored clasts that could be a felsic tuff. The clasts areimbricated at ~35º - 38º TCA. The matrix is fine-grained and grey in color and is foliated at ~35º - 38º TCA. There is quite a bit of carbonate alteration and some disseminated pyrite throughout thematrix.The veins are mm - cm in size and have carbonate alterations. Some of the veins are deformed with sigmoidal and brecciated forms.The contact at 609.59 m is approximate. The rock grades from sandstone to argillite.

609.59 654.05 S; SS; ARGSiltstone; Sandstone; ArgilliteThe rock is a grey fine grained siltstone (mm - several m), with layers of fine to medium-grained light-grey to grey sandstone layers (cm - several m), and very fine-grained dark-grey argillite (mm -several m). The contacts between layers are sharp to irregular and at ~35º TCA. There is ~38% siltstone, 32% sandstone, 30% argillite and <1% quartz veins. The rock contains carbonate alterationsand a little disseminated pyrite. From ~618.30 m - 619.50 m and 650.50 m - 651.30 m, the sandstone contains some angular argillite fragments. The majority of the argillite is found between ~609.59 m- 623.50 m.The quartz veins are mm - cm in size and have carbonate alterations. Some of the veins are deformed with sigmoidal and brecciated forms.The contact at 654.05 m is approximate. The core is broken and there is a quartz vein at this point which is obscuring the actual contact.

654.05 663.13 SS; CONGLO; C/ARGSandstone; Conglo; Argillite ClastsThe rock is a sequence with zones of grey fine to medium-grained sandstone (several cm - m) and grey conglomerate (several cm - m). The rock is composed of ~55% sandstone, 45% conglomerate and<1% quartz veins. The contacts between zones are irregular and at 35º TCA.The sandstone zones appear to be mainly massive. From 659.75 m - 659.88 m, there is a siltstone layer. The upper contact is irregular and the lower is sharp, both contacts are at~45º TCA. From 662.10m - 662.86 m, the sandstone is very fine. The rock is foliated at ~45º TCA. There are carbonate alterations and disseminated pyrite throughout the sandstone zones. It is possible that these sandstonezones are actually matrix in the conglomerate.The conglomerate zones are mainly monomictic, matrix-supported and are composed of ~85% matrix and 15% felsic clasts. The clasts range in shape from angular to sub-rounded and in size from 1 mm- 1 cm. There are several fine-grained grey to dark-grey clasts that are probably argillite and some small fine-grained light-grey clasts that could be a felsic tuff. There are a few very fine-grained greyclasts that could be siltstone. The clasts are imbricated at ~45º TCA. The matrix is fine-grained and grey in color and is foliated at ~45º TCA. There is some carbonate alteration and disseminated pyritethroughout the matrix.The veins are mm - cm in size and have carbonate alterations. Some of the veins are slightly deformed with sigmoidal and brecciated forms.The contact at 663.13 m is irregular and at ~50º - sub-parallel TCA.

663.13 680.25 CONGLO; C/FConglo; Felsic ClastThe rock is a grey polymictic (limited), conglomerate. The conglomerate is medium-supported (has areas that are clast-supported or matrix-supported), and is composed of ~60% felsic clasts, 38%matrix and 2% quartz veins. The clasts range in shape from sub-angular to rounded (there are a few angular clasts), and in size from 1 mm - 3 cm. From ~669.25 m - 669.55 m, there is a very large (30cm) fine-grained medium-grey clast, with quartz eyes, feldspar and quartz crystals. There are some fine-grained grey and dark-grey to black clasts that are probably argillite. There are a lot offine-grained light-grey to grey (some have chlorite alterations), light brown, pinkish colored and creamy colored clasts that could be felsic tuff (some of these clasts look porhyritic and could bepyroclastic). The brown color of the clasts could be an alteration. There are a few very fine-grained grey clasts that are very hard and may be chert. The clasts are imbricated at ~45º TCA (some of theclasts look stretched). The matrix is fine-grained and grey in color and is foliated at ~45º TCA. There is quite a bit of carbonate and chlorite alteration, along with some disseminated pyrite and a fewblue quartz eyes throughout the matrix.



DESCRIPTION

The veins are mm - cm in size and have carbonate alterations, some have tourmaline crystals (elongated, black). There is a large vein from 671.64 m - 671.90 m with a lot of chlorite alteration. Severalof the veins are deformed with sigmoidal and brecciated forms.The contact at 680.25 m is approximate. The rock grades from having a bit of argillite to having much more argillite.

680.25 698.67 CONGLO; C/ARGConglo; Argillite ClastsThe rock is a grey polymictic (very limited), conglomerate. The conglomerate is medium-supported (has areas that are clast-supported or matrix-supported), and is composed of ~39% felsic clasts, 20%argillite and 40% matrix and 1% quartz-carbonate veins. The clasts range in shape from angular to sub-rounded and in size from 1 mm - 4 cm. There are a lot of fine-grained grey and dark-grey claststhat are probably argillite. There are a lot of fine-grained light-grey to grey (some have chlorite alterations), that could be felsic tuff. From 681.67 m - 687.00 m, the surface of the core is very rough andthere is a lot of carbonate and chlorite alteration making it difficult to properly identify clasts and matrix. The clasts are imbricated at ~45º TCA (some of the clasts look stretched).The matrix is fine-grained and grey in color and is foliated at ~45º TCA. There is quite a bit of carbonate and chlorite alteration, along with some disseminated pyrite.The veins are mm - cm in size and have carbonate alterations, some have tourmaline crystals (elongated, black). Most of the veins are deformed with sigmoidal and brecciated forms.The contact at 698.67 m is approximate. The core is broken and there is a quartz vein at this point obscuring the actual contact.

698.67 712.29 CONGLO; C/FConglo; Felsic ClastThe rock is a grey polymictic (limited), conglomerate. The conglomerate is medium-supported (has areas that are clast-supported or matrix-supported), and is composed of ~65% felsic clasts, 30%matrix, 5% argillite and <1% quartz veins. The clasts range in shape from sub-rounded to rounded (there are a few sub-angular clasts), and in size from 1 mm - 5 cm. From ~702.30 m - 702.50 m, thereis a very large (20 cm) fine-grained medium-grey clast, with quartz eyes, feldspar and quartz crystals. There are some fine-grained grey and dark-grey to black clasts that are probably argillite. There area lot of fine-grained light-grey to grey (some have chlorite alterations), and pinkish colored clasts that could be felsic tuff (some of these clasts look porhyritic and could be pyroclastic). There are a fewsmall very fine-grained grey clasts that are very hard and may be chert. The clasts are imbricated at ~35º TCA (some of the clasts look stretched).The matrix is fine-grained and grey in color and is foliated at ~35º TCA. There is quite a lot of carbonate and a bit of chlorite alteration, along with some disseminated pyrite throughout the matrix.The veins are mm - cm in size and have carbonate alterations. Some of the veins are deformed with sigmoidal and brecciated forms.The contact at 712.29 m is approximate. The rock grades from having a bit of argillite to having much more argillite.

712.29 717.70 CONGLO; C/ARG; C/FConglo; Argillite Clasts; Felsic ClastThe rock is a grey colored polymictic conglomerate. The rock is clast-supported and is composed of ~45% felsic clasts, 35% argillite, 20% matrix and <1% quartz veins. The clasts range in shape fromsub-angular to sub-rounded (there are a few angular clasts), and in size from 1 mm - 10 cm. From ~712.68 m - 713.61 m, there is a very large (93 cm) coarse-grained medium-grey clast, with bluequartz eyes, also possibly feldspar and quartz crystals (there are a few smaller clasts with the same composition). A this section (LG20448-1) has been taken to determine composition. There are severalargillite clasts (medium to dark-grey, soft), as well as a lot of fine-grained grey to light-grey clasts that could be a felsic tuff (a lot of these have quite a bit of chlorite alteration). There are somefine-grained pinkish-grey to creamy-grey colored clasts that look porphyritic, possibly pyroclastic. The clasts are imbricated at ~45º TCA.The matrix is fine-grained grey in color and is foliated at ~45º TCA. There is quite a bit of carbonate and a bit of chlorite alteration, along with some disseminated pyrite throughout the matrix.The quartz veins are mm - cm in size and have carbonate alterations. Some of the veins are deformed with sigmoidal form.The contact at 717.70 m is approximate. It is where the conglomerate becomes matrix-supported with mainly argillite clasts.

717.70 721.05 CONGLO; C/ARGConglo; Argillite ClastsThe rock is a grey polymictic (very limited), conglomerate. The conglomerate is matrix-supported and is composed of ~89% matrix, 10% argillite clasts and 1% quartz veins. The clasts are mainlyangular with a few that are sub-angular and a couple that are sub-rounded. The clasts range in size from 1 mm - 4 cm. The argillite clasts are fine-grained medium to dark-grey in color and soft. Theclasts are elongated and imbricated at ~35º TCA.The matrix is grey medium-grained (sandstone?), and is foliated at ~45º TCA. There is some carbonate and a little chlorite alteration, along with some disseminated pyrite.The veins are mm - cm in size and have carbonate and a little chlorite alteration.The contact at 721.05 m is approximate. There is a quartz vein at this point obscuring the actual contact.

721.05 728.05 CONGLO; C/ARG; C/FConglo; Argillite Clasts; Felsic ClastThe rock is a grey colored polymictic conglomerate. The rock is medium-supported (has areas that are clast-supported or matrix-supported), and is composed of ~35% felsic clasts, 24% argillite, 40%matrix and 1% quartz veins. The clasts range in shape from sub-angular to sub-rounded (there are a few angular clasts), and in size from 1 mm - 3 cm. There are a lot of argillite clasts (medium todark-grey, soft), as well as a lot of fine-grained grey to light-grey clasts that could be a felsic tuff (several have chlorite alteration). There are a couple of very fine-grained pinkish-grey clasts that are veryhard, possibly chert. The clasts are imbricated at ~45º TCA.The matrix is medium-grained grey (sandstone?) and is foliated at ~45º TCA. There is quite a bit of carbonate and a bit of chlorite alteration, along with some disseminated pyrite throughout the matrix.The quartz veins are mm - cm in size and have carbonate alterations (some have a bit of chlorite alteration). Some of the veins are deformed with sigmoidal and brecciated forms.The contact at 728.05 m is approximate. The rock grades into sandstone/argillite.

728.05 768.00 SS; S; ARG



DESCRIPTION

Sandstone; Siltstone; ArgilliteThe rock is a light to medium-grey fine to coarse-grained sandstone (cm - several m), with grey fine-grained siltstone layers (mm - several cm), and dark-grey fine-grained argillite layers (mm - cm). Thecontacts between the layers are irregular and at ~45º TCA. The rock is composed of ~60% sandstone, 34% siltstone, 5% argillite and 1% quartz vein. There is some sericite and carbonate alterations, aswell as some disseminated pyrite throughout the unit. Several of the sandstone sections have a few argillite clasts that are 1 mm - 2 cm in size and sub-angular to sub-rounded in shape. From ~758.50 m- 759.56 m and 764.20 m - 768.00 m, there is some deformation in the rock seen by the convoluted layers of sandstone, siltstone and argillite (the contacts of the layers have a sigmoidal shape and someare sub-parallel TCA).The quartz veins are mm - cm in size and most have some carbonate alteration (a few have a lot). Several of the veins are deformed with sigmoidal and brecciated forms






Drilled by : Foramex 2 From : 2006-07-03 To : 2006-08-05Geologist : Laura Mancini and Bernard Olivier Martel, géo Description date : 2006-08-06

Collar


Comments




671000.0005326400.000350.000








Type Depth Azimuth PlungeFlex-it 852.00m 281.44° -55.83°Flex-it 855.00m 280.36° -56.03°Flex-it 858.00m 280.79° -55.78°Flex-it 861.00m 280.63° -55.93°Flex-it 864.00m 280.26° -55.87°Flex-it 867.00m 281.17° -55.63°Flex-it 870.00m 282.09° -55.48°Flex-it 873.00m 280.56° -55.70°Flex-it 876.00m 280.99° -55.59°Flex-it 879.00m 282.40° -55.34°Flex-it 882.00m 282.60° -55.34°Flex-it 885.00m 282.47° -55.43°Flex-it 888.00m 281.21° -55.50°Flex-it 891.00m 281.11° -55.50°Flex-it 894.00m 281.34° -55.48°Flex-it 897.00m 281.68° -55.39°Flex-it 900.00m 282.45° -55.27°Flex-it 903.00m 283.40° -55.06°Flex-it 906.00m 281.86° -55.40°Flex-it 909.00m 281.65° -55.42°Flex-it 912.00m 282.28° -55.25°Flex-it 915.00m 282.70° -55.19°Flex-it 918.00m 284.01° -54.96°Flex-it 921.00m 283.31° -55.21°



DESCRIPTION

0.00 0.50 OBOverburdenoverburden. 1 m of casing

0.50 21.45 V; V3A; TBLVolcanic; Andesite/Dacite; Tuff Breccia/LapillistoneThe rock is a greenish grey fine to coarse-grained (up to 2 mm), dacite (?) lapillistone with possible volcanic bombs. The rock is very deformed and altered making proper identification difficult. Thereare fine-grained section that have what appear to be bombs (medium-grained pinkish colored with a dark grey boundary or rind, somewhat oval in shape). The bombs are ~ 2 cm - 7 cm in size and somehave a greenish color from chlorite alterations. There are areas of the lapillistone that appear to have a lot of sericite alteration (creamy-grey color). There is carbonate alteration and chlorite replacementof primary minerals (spilitization), and sericite alteration, throughout the lapillistone. The overall impression of the unit is of a very fragmental and/or brecciated rock. The rock is foliated at ~45º TCAThe rock contains ~1% quartz veins (mm - cm), with carbonate alterations. Most of the veins are deformed with sigmoidal, brecciated and ptygmatic forms. Several of the veins have a lot of tourmalineand pyrrhotite, as well as some chlorite and sericite associated with them.The contact at 21.45 m is approximate. There is a quartz vein and the core is broken with pieces missing at this point. The rock appears more massive after 21.45 m.

21.45 51.08 V; V3A; TBLVolcanic; Andesite/Dacite; Tuff Breccia/LapillistoneThe rock is a greenish-grey coarse-grained (up to 2 mm), dacite (?) lapillistone. The rock is very deformed and altered and in many places the surface of the core is very rough. This makes properidentification difficult. There are some finer-grained sections from 25.8 m - 26.48 m and 37.55 m - 44.50 m. These sections appear massive (no apparent bedding layers, pillows, etc.), with irregularcontacts at ~53º TCA. There are areas of the lapillistone that appear to have a lot of sericite alteration (creamy-grey color). There is carbonate alteration and chlorite replacement of primary minerals(spilitization), and sericite alteration, throughout the lapillistone. There is a small shear zone from ~31.56 m - 33.00 m and a larger one starting at ~43.00 m and continuing into the next unit. The rockis deformed and altered, and heavily foliated between ~45º - 50º TCA, particularly within the shear zone.The rock contains ~10% quartz veins (mm - cm), with carbonate alterations. Most of the veins are deformed with sigmoidal, brecciated and ptygmatic forms. Several of the veins have a lot oftourmaline and pyrrhotite, as well as some chlorite and sericite alteration. The majority of the veins have been transposed and are oriented to the foliation.The contact at 51.08 m is approximate. The core is broken with pieces missing at this point. The first evidence of pillows is seen right after 51.08 m.



51.08 145.35 V; V3A; PwVolcanic; Andesite/Dacite; PillowThe rock is a greenish-grey coarse to fine-grained pillowed dacite (?). There are dark-grey fine-grained areas that appear to be pillow rinds. These areas are 1 cm - 4 cm wide and ~10 .00 cm - 30.00 cmapart. There is carbonate alteration and chlorite replacement of primary minerals (spilitization), and sericite alteration, in the pillows and throughout the unit. The rock starts out coarse-grained andgrades into a more fine-grain starting around 78.00 m (has less sericite alteration as well). There is more sericite and chlorite alteration in the unit starting around 100.00 m. There is a tiny bit ofdisseminated pyrite and pyrrhotite in the unit. The rock is heavily foliated between ~45º - 50º TCA and the pillows are very deformed and altered by the shear zone that started in the previous unit andappears to continue to ~75.00 m.The rock contains ~20% quartz veins (mm - cm), with carbonate alterations. Most of the veins are deformed with sigmoidal, brecciated and ptygmatic forms. Many of the veins are oriented to thefoliation. Several of the veins have a lot of tourmaline, as well as some chlorite and sericite alteration.The contact at 145.35 m is approximate. There is no obvious contact but the rock appears to become more fragmental after this point.

145.35 158.38 V; V3A; TBLVolcanic; Andesite/Dacite; Tuff Breccia/LapillistoneThe rock is a greenish grey coarse-grained (up to 2 mm), dacite (?) lapillistone with possible volcanic bombs. The rock is very deformed and altered making proper identification difficult. The sectionfrom ~145.35 m - 153.90 m appears to have brecciated (and fragments of), pillows (can see dark bands around lighter centers). The section from ~153.90 m - 158.38 m has what appear to be bombs(coarse-grained light grey colored with a dark grey boundary or rind, somewhat oval in shape). The bombs are ~ 1 cm - 3 cm in size. There is a lot of sericite alteration giving the rock a creamy-greycolor. There is carbonate alteration and chlorite replacement of primary minerals (spilitization), throughout the lapillistone. The rock is foliated between ~45º - 55º TCA.The rock contains ~20% quartz veins (mm - cm), with carbonate alterations. Most of the veins are deformed with sigmoidal, brecciated and ptygmatic forms. Many of the veins are oriented to thefoliation. Several of the veins have some chlorite and sericite alteration.The contact at 158.38 m is approximate. The core is broken with pieces missing at this point but the rock becomes fine-grained and appears massive right after 158.38 m.

158.38 200.22 V; V3A; MasVolcanic; Andesite/Dacite; MassiveThe rock is a fine-grained grey massive volcanic (no obvious layers, pillows, etc.), possibly andesite or dacite. There is quite a bit of deformation and alteration in the rock making it difficult to see any



DESCRIPTION

real features. There is some carbonate alteration and small amounts of what appear to be chlorite replacement of primary minerals (spilitization), also a tiny bit of disseminated pyrite throughout theunit. The rock is foliated at ~45º TCA.The rock contains ~10% quartz veins (mm - cm), with carbonate alterations. Several of the veins are deformed with sigmoidal and brecciated forms. A few of the veins have chlorite and sericitealterations. The vein from 168.00 m - 168.70 m has brown tourmaline associate with it. Many of the veins are oriented to the foliation and a few veins are sub-parallel TCA.The contact at 200.22 m is approximate. The core is broken and there is quite a bit of deformation and alteration at this point which is obscuring the actual contact.

158.38 200.22 V; V3A; MasVolcanic; Andesite/Dacite; MassiveMassive fine-grained volcanic unit

200.22 219.38 V; V3A; TaVolcanic; Andesite/Dacite; Tuff /AshThe rock is a greenish-grey fine-grained volcanic tuff, possibly an andesite or basalt. The rock is very deformed and altered making proper identification difficult. There are foliations that wereinterpreted by Ed Van Hees (as stated in his short log), as ash layers. These layers are heavily foliated and crenulated. The layers are in a series of synclinal and anticlinal folding and some aresub-parallel TCA, the majority are at 40º TCA. It is unclear if these are really ash layers or sericite alterations within foliations that were caused by tectonic deformation (the unit may be in a shear zonecreated by folding). This uncertainty is due to the fact that the quartz veins in these sections are deformed in exactly the same manner. Also, there are several veins that have a boudinage form. There isa lot of chlorite and carbonate alteration, as well as some disseminated pyrite and pyrrhotite throughout the unit.The rock contains ~35% quartz veins (mm - cm), with carbonate alterations. As mentioned above, many of the veins are heavily deformed with with sigmoidal, brecciated and boudinage forms. Severalof the veins have some chlorite and sericite alterations.The contact at 219.38 m is approximate. The core is broken at this point and there is a lot of deformation and alteration obscuring any real contact.

219.38 223.25 V; V3A; TBLVolcanic; Andesite/Dacite; Tuff Breccia/LapillistoneThe rock is a greenish-grey medium to coarse-grained volcanic lapillistone, possibly an andesite or basalt. The rock is very deformed and altered making proper identification difficult. The section from~219.38 m - 223.00 m has what appear to be bombs (coarse-grained light grey colored with a dark grey boundary or rind, somewhat oval in shape). The bombs are ~ 1 cm - 3 cm in size. The rock isfoliated at ~40º TCA. There is chlorite, sericite and a bit of carbonate alteration throughout the unit.The rock contains ~35% quartz veins (mm - cm), with carbonate alterations. The veins are deformed with sigmoidal and brecciated forms and are oriented to the foliation.The contact at 223.25 m is approximate. There is a lot of deformation and alteration obscuring any real contact.

223.25 239.90 V; V3A; Ta; TBLVolcanic; Andesite/Dacite; Tuff /Ash; Tuff Breccia/LapillistoneThe rock is a greenish-grey to grey coarse to fine-grained volcanic tuff-lapillistone, possibly andesite or dacite. The rock grades from coarse to fine-grained (also more grey), starting from ~233.25 m -235.00 m. There are areas throughout the coarse-grained section that have carbonate alteration and chlorite replacement of primary minerals (spilitization). These areas tend to be slightly lighter in colorthan the rest of the section. Both sections are deformed and altered and are foliated at ~55º TCA. The fine-grained section is very deformed and altered making it difficult to see any features.The rock contains ~25% quartz veins (mm - cm), with carbonate alterations. Many of the veins are deformed with sigmoidal and brecciated forms. Most of the veins are oriented to the foliation.The contact at 239.9 m is approximate. The core is broken and there is a vein at this point obscuring the actual contact.

239.90 242.26 SS; MasSandstone; MassiveThe rock is a grey medium-grained sandstone (as interpreted by Ed Van Hees in his short log), possibly with a volcanic source (the unit is situated between two volcanic units). The unit appears massive(no obvious bedding, layers, etc) with faint foliations at ~55º TCA. There is carbonate, chlorite and some sericite alterations, alog with some disseminated pyrite throughout the unit.The rock contains ~1% quartz veins (mm - cm), many with carbonate and a bit of chlorite alteration. Most of the veins are deformed with sigmoidal and brecciated forms. Many of the veins are orientedto the foliation.The contact at 242.26 m is approximate. The core is broken and there is a vein at this point obscuring the actual contact.

242.26 252.66 VC; TBL; PoVolcaniclastic; Tuff Breccia/Lapillistone; PolymicticThe rock is a greenish-grey polymictic (limited) volcanoclastic with coarse-grained sections that look like lapillistone. The rock appears to be ~65% volcanoclastic and 35% lapillistone.The volcanoclastic is composed of 63% felsic clasts, 20% quartz veins, 15% matrix and 2% mafic clasts. The rock is very deformed and altered making it difficult to see clasts and matrix clearly and toproperly identify the clasts. Therefore, the percentages are a very rough estimation.The clasts are mainly sub-rounded (there are a few sub-angular clasts), and range in size generally from 1 mm - 5 cm, with a few ranging up to 10 cm, There are several coarse-grained light grey to greyand beigish-grey clasts that could possibly be pyroclastic (the beige color could be sericite alteration). There are a few light to dark grey fine-grained (hard) clasts that could be dacite tuff. There are afew green fine-grained clasts that could be a basalt tuff (these clasts could also be matrix, it is difficult to tell). The clasts are imbricated at ~55º TCA and many appear stretched.The matrix in the volcanoclastic sections is dark grey to green fine-grained and is foliated at ~55º TCA. There is chlorite, some carbonate and sericite alteration and disseminated pyrrhotite and pyritethroughout the matrix.The lapillistone section has a few grains up to 2 mm in size. There are areas that have what resemble flame structures (ex. around 249.00 m). There is chlorite, some carbonate alteration throughout the



DESCRIPTION

lapillistone sections. Some areas have what appears to be leucoxene alteration.The quartz veins are mm - cm in size and have carbonate alterations. Most of the veins are deformed with sigmoidal and brecciated forms. Many of the veins are oriented to the foliation.The contact at 252.66 m is approximate. There is no obvious contact but there are no clasts seen after this point.

242.26 252.66 VCVolcaniclasticVolcanoclastic medium-supported. Some sections are definitely clast-supported, other sections are to altered to say for sure.

252.66 273.98 V; V3A; Ta; TBLVolcanic; Andesite/Dacite; Tuff /Ash; Tuff Breccia/LapillistoneThe rock is a fine-grained light grey tuff (55%), with coarse-grained grey lapillistone sections (45%). The rock is very deformed and altered making it difficult to see any features. The lapillistonesections have a few grains up to 2 mm in size. There are areas that have what resemble flame structures throughout the sections. There is some carbonate alteration and small amounts of what appear tobe chlorite replacement of primary minerals (spilitization), also a tiny bit of disseminated pyrite throughout the unit, particularly from 263.75 m - 270.20 m. The tuff sections also have chlorite and a bitof carbonate alteration and some sericite as well (it is hard to see any features due to the amount of veining). The rock is heavily foliated between 45º - 65º TCA.The rock contains ~40% quartz-feldspar veins (mm - cm), with carbonate alterations. Most of the veins are oriented to the foliation. Many veins are deformed with sigmoidal and brecciated forms. Afew veins have quite a bit of piles of pyrrhotite associated with them.The contact at 273.98 is approximate. The rock grades into sandstone.

273.98 459.97 SS; ARG; SSandstone; Argillite; SiltstoneThe rock is a light-grey to grey fine to coarse-grained sandstone (cm -m), with dark-grey to black very fine-grained argillite layers (mm - several cm), and medium-grey fine-grained siltstone layers (mm -cm). The rock is composed of ~65% sandstone, 25% argillite, 10% siltstone and <1% quartz veins.The contacts between layers are sharp to irregular and at ~55º TCA. Some of the contacts are very convoluted and the layers are all mixed up, particularly in the shear zones from 289.72 m - 298.90 m,307.80 m - 315.30 m and 450.73 m - ~459.97 m (continues into next unit). The rock in the shear zones is brecciated and ground up. There is a massive sandstone sections from 408.00 m - 425.44 m,where the sandstone grades from coarse to very coarse to fine-grained. There is another massive section (with a little bit of argillite), from 430.23 m - 450.73 m, where the sandstone is coarse-grained.The rock is foliated between 50º - 60º TCA, and there are crenulations mainly in the argillite layers at ~40º TCA. There is some carbonate alteration and disseminated pyrite throughout the unit.The veins are mm - cm in size and have carbonate alterations. Most are deformed with sigmoidal and brecciated forms. Many of the veins are oriented to the foliation.The contact at 459.97 m is approximate. The contact is in the shear zone and has been ground up, therefore it cannot actually be seen.

289.72 298.90 SheShearingShear zone in sandstone-argillite unit.

307.80 315.30 SheShearingShear zone in sandstone-argillite unit.

408.00 425.44 SS; MasSandstone; MassiveMassive coarse to very coarse-grained sandstone in layered sandstone-argillite-siltstone unit.

430.23 450.73 SS; MasSandstone; MassiveMassive coarse-grained sandstone with a tiny bit of argillite in a layered sandstone-argillite-siltstone unit.

450.73 465.00 SheShearingShear zone in sandstone-argillite-siltstone unit.

459.97 473.24 V/S?; MasVolcanic/Sédiment?; MassiveThe rock is a brown-grey colored medium-grained volcanic or possibly sedimentary rock. The rock is heavily altered (sericite?), making proper identification very difficult. A thin section (LG20814),was taken to determine composition. The shear zone that started in the previous unit continues through this one to ~465.00 m. The rock in the shear zone is ground up and brecciated, and has a lot ofchlorite, sericite and carbonate alteration.The rock contains ~20% quartz veins (mm- cm), most are tiny little spider veins. There is some carbonate and chlorite alteration in the veins. Many of the veins are deformed with sigmoidal andbrecciated forms.The contact at 473.24 is approximate. The rock is deformed and altered making it difficult to see an actual contact. Argillite is obvious right after this point.

473.24 492.00 ARG; SS; SArgillite; Sandstone; Siltstone



DESCRIPTION

The rock is a grey to dark-grey very fine-grained argillite (mm - cm), with grey fine to medium-grained sandstone layers (mm - cm), and fine-grained medium-grey siltstone layers (mm - cm). The rock iscomposed of ~45% argillite, 35% sandstone, 19% siltstone and 1% quartz veins. The unit is in a shear zone starting at ~473.24 m and continuing into the next unit. The shearing has badly deformed therock, therefore the percentages are a very rough approximation. The contacts between layers are very irregular, convoluted and crenulated and range from sub-parallel to perpendicular TCA. The rock isfoliated at ~55º TCA. There is carbonate alteration and some disseminated pyrite throughout the unit.The veins are mm - cm in size and have carbonate alterations. The veins are deformed and oriented in the same manner as the layers. Several are oriented to the foliation.The contact at 491.00 m is approximate. The rock is deformed from the shear at this point and the core is broken with pieces missing which has obscured the actual contact.

473.24 496.00 SheShearingShear zone starting in an argillite-sandstone unit and appears to stop in the following massive sandstone unit.

492.00 518.75 SSSandstoneThe rock is a light-grey to grey medium to very coarse-grained sandstone. From 492.00 m - 511.20 m, the rock starts out massive with a few layers (mm - cm), and small fragments (1 mm - 2 cm), ofargillite here and there. From 511.20 m on the rock is much more layered (most are mm in size and a few are several cm), but still not with a lot of argillite . It is possible that the more massive section isthe bottom, or start, of the flow and the more layered sections is the top or end of the flow (lower velocity, settling of finer particles). The contacts between layers are sharp to irregular and at ~45º TCA.The rock appears to be foliated at ~40º TCA (grains have a preferred orientation). There is carbonate alteration and disseminated pyrite throughout the unit. There is a bit of chlorite alteration from~511,20 m - 516.00 m.The rock contains ~1% quartz veins (mm - cm), with carbonate alterations. Several of the veins are deformed with brecciated forms. Many are oriented with the foliation.The contact at 518.75 is approximate. The core is broken with pieces missing at this point.

518.75 534.14 SS; S; ARGSandstone; Siltstone; ArgilliteThe rock is a grey medium-grained sandstone (cm - m) with medium-grey fine-grained siltstone layers (mm - m), and a few very fine-grained dark-grey argillite layers (mm - cm). The rock is composedof ~ 50% sandstone, 45% siltstone, 5% argillite and <1% quartz veins. The contacts between layers range from gradational to sharp to irregular at ~45º TCA. The section from ~519.00 m - 525.00 m ismostly massive siltstone with a tiny bit of argillite fragments (5 mm - 1 cm), around 523.30 m. The section from 525.00 m - 534.14 m is mostly sandstone with a few argillite layers. There is a hint offoliation at ~40º TCA (grains appear to have a preferred orientation). There is carbonate alteration and disseminated pyrite throughout the unit.The quartz veins are mm - cm in size and have carbonate alterations. A few are deformed with a sigmoidal form.The contact at 534.14 m is irregular and at ~30º TCA.

534.14 561.75 SS; S2GSandstone; GreywackeThe rock is a grey fine to coarse-grained sandstone, possibly a greywacke (has grains of quartz, feldspar and angular argillite fragments, in a fine-grained matrix, matrix >15% of rock). The rock gradesback and forth from coarse to fine-grained and there are a few layers of argillite (cm - m), throughout the unit, particularly from ~558.62 m - 561.75 m. The contacts between layers are at ~50º TCA.The grains in the coarse sections are 1 mm - 3 mm and the fragments are 3 mm - 1 cm in size. There is quite a bit of blue quartz eyes throughout the coarse-grained sections. There is carbonatealteration and disseminated pyrite throughout the unit.The rock contains ~2% quartz veins (mm - cm), a lot are tiny spider veins. The veins have carbonate alteration and many are deformed with sigmoidal and brecciated forms. Some of the veins have a bitof chlorite alteration.The contact at 561.75 m is irregular and at ~45º TCA.

561.75 569.12 CONGLO; C/F; C/ARGConglo; Felsic Clast; Argillite ClastsThe rock is a grey-green polymictic (limited) conglomerate. The rock is medium-supported (has sections that are clast-supported or matrix-supported), and is composed of ~48% matrix, 47% felsicclasts and 5% quartz veins.The clasts range in shape from angular to sub-rounded and in size from 1 mm - 2 cm. The clasts are imbricated at ~45º TCA (some of the clasts look stretched). There are several fine-grained light-greyto grey clasts that could be a dacite tuff. There are a few fine-grained pinkish and creamy colored clasts that appear to be porphyritic, possibly pyroclastic. There are several fine-grained creamy tobrown colored clasts that could be a felsic tuff. There are a few very fine-grained dark-grey clasts that could possibly be argillite (they are hard). There are a lot of very fine-grained very light-grey towhite clasts that are most likely quartz (very hard). The section from ~567.00 m - 569.12 m has more of the fine-grained grey clasts.The matrix is fine-grained grey colored with a lot of carbonate, chlorite and sericite alterations and disseminated pyrite. The matrix in the clast-supported sections have more chlorite alteration than inthe matrix-supported sections. The matrix is foliated at ~45º TCA.The veins are mm - cm in size with carbonate alterations. A few of the veins are deformed with sigmoidal and brecciated forms. A couple of veins have a bit of chlorite alteration.The contact at 569.12 m is approximate. The surface of the core is very rough and the core is broken at this point with pieces missing, therefore the actual contact cannot be seen.

561.75 569.12 MmSMedium-Supportedconglomerate medium-supported (has areas that are clast-supported or matrix-supported).



DESCRIPTION

569.12 579.38 SS; CONGLO; C/ARG; STSandstone; Conglo; Argillite Clasts; Stratified/LaminatedThe rock is a sequence with a zone of light-grey to grey coarse-grained sandstone (several m) and a zone of light-grey conglomerate (m). The sequence appears to be from the same source deposited bydifferent events. The rock is composed of ~74% sandstone, 25% conglomerate and 1% quartz veins.The sandstone zone appears massive and starts out very coarse-grained grading to coarse-grained. There are no obvious foliations or other structural features. There is carbonate alteration and a smallamount of disseminated pyrite in the sandstone. The sandstone appears to be foliated at ~50º TCA (the grains have a prefered orientation). The contact between the sandstone zone and the conglomeratezone is gradationalThe conglomerate zone is mostly monomictic, matrix-supported and is composed of ~75% matrix and 25% argillite clasts (fine-grained dark-grey, soft). There are a couple of coarse-grained grey claststhat are probably sandstone. The clasts range in shape from sub-angular to sub-rounded and in size from 1 mm - 4 cm. The clasts are imbricated at ~50º TCA (some of the clasts look stretched). Thematrix is coarse-grained light-grey in color and is foliated at 50º TCA. There is carbonate alteration and a bit ofdisseminated pyrite and some blue quartz eyes throughout the matrix.The veins are mm - cm in size and have carbonate alterations. Some of the veins are deformed with a brecciated form.The contact at 579.38 m is approximate. The core is broken with pieces missing at this point, but the rock is much finer and darker right after 579.38 m

579.38 589.66 SSSandstoneThe rock is a dark-grey to grey fine-grained sandstone (several m), with granular to pebbly (2 mm - 5 mm), sandstone sections (cm - m). The rock is composed of ~65% sandstone, 15% pebblysandstone and 10% quartz veins. The contacts between layers are irregular and at ~45º TCA.The granules and pebbles appear to be mainly quartz (very light-grey to white, very hard), and argillite (dark-grey to black, soft), and have a prefered orientation at ~45º TCA.The rock is foliated at ~45º TCA and there is carbonate alteration and some disseminated pyrite throughout the unit.The quartz veins are mm - cm in size and have carbonate alteration. Several of the veins are deformed with sigmoidal and brecciated forms. A couple of veins have some chlorite alteration.The contact at 589.66 m is approximate. The core is broken and there is a quartz vein at this point, but the rock becomes lighter in color and coarser-grained right after 589.66 m

589.66 596.17 CONGLO; SS; C/F; STConglo; Sandstone; Felsic Clast; Stratified/LaminatedThe rock is a series of alternating sequences with zones of grey conglomerate (several m) and zones of grey coarse-grained sandstone (m) . The sequences appear to be from the same source depositedby different events. The rock is composed of ~75% conglomerate, 25% sandstone and <1% quartz veins. The rock has quite a lot of alteration making it difficult to see clasts and matrix clearly (and clasttypes), therefore the percentages are a rough estimation.The conglomerate zones are polymictic medium-supported (has areas that are clast-supported or matrix-supported), and is composed of ~75% felsic clasts and 25% matrix. The clasts range in shapefrom sub-angular to sub-rounded and in size from 1 mm - 1 cm. There are several fine-grained yellowish-brown clasts that could be a felsic tuff, the color may be from sericite alteration. There are a lotof quartz fragments (very light-grey to bluish-white, very fine-grained and very hard). There are several fine-grained grey to medium-grey clasts that could be a andesitic or dacitic tuff. There are a fewcoarse-grained grey clasts that are possibly sandstone. There are a few tiny very fine-grained dark-grey clasts that are probably argillite (soft). There are several fine-grained pinkish-grey clasts, some ofwhich appear to be porphyritic, that could be pyroclastic. The clasts are imbricated at ~50º TCA (some of the clasts look stretched). The matrix is fine-grained grey in color and is foliated at 50º TCA.There is carbonate, chlorite and sericite alteration and a bit of disseminated pyrite throughout the matrix. The contacts between the the conglomerate zones and the sandstone zones are gradational.The sandstone zones appear massive with no obvious foliations or other structural features. There are a few tiny felsic and argillite fragments scattered throughout the sandstone. There arecarbonate,chlorite and sericite alterations and a small amount of disseminated pyrite in the sandstone. The sandstone is foliated at ~50º TCA with sericite alterations in foliations.The veins are mm - cm in size and have carbonate alterations. Some of the veins are deformed with sigmoidal and brecciated forms.The contact at 596.17 m is approximate. The core is broken with pieces missing and there is a quartz vein with alterations at this point, but there are no more visible clasts starting right after 596.17 m.

596.17 600.75 SS; ARGSandstone; ArgilliteThe rock is a medium-grained grey sandstone ( cm - several m), with very fine-grained dark-grey to black argillite layers (cm). The rock is composed of 64% sandstone, 35% argillite and 1% quartzveins. The contacts between layers are irregular and at ~60º TCA. Some of the contacts and argillite layers are very convoluted and mixed up in the sandstone.There are some small areas (cm), where there is the impression of a more granular sandstone (ie. around 598.55 m). With the argillite and the more granular sections, it is possible the sandstone could bea greywacke.There is carbonate, some chlorite and sericite alterations and a bit of disseminated pyrite in the sandstone layers and a bit of disseminated pyrite in the argillite layers.The quartz veins are mm - cm in size and have carbonate alterations. Most of the veins are deformed with sigmoidal and brecciated forms.The contact at 600.75 m is approximate. The rock is very altered making it difficult to see an actual contact.

600.75 622.27 CONGLO; SS; C/F; STConglo; Sandstone; Felsic Clast; Stratified/LaminatedThe rock is made up of repetitive sequences with alternating zones of grey polymictic conglomerate (m - several m), and grey coarse-grained sandstone (m - several m). The sequences appear to be fromthe same source deposited by different events. The rock is composed of 55% conglomerate, 45% sandstone and <1% quartz veins. The contacts between zones are irregular at ~45º TCA and gradational.The conglomerate zones are medium-supported (has areas that are clast-supported or matrix-supported), and are composed of ~65% felsic clasts and 35% matrix. The clasts range in shape fromsub-angular to sub-rounded (there are a few angular clasts), and in size from 1 mm - 4 cm. There are several fine-grained light-grey to medium-grey clasts that could be an andesitic or dacitic tuff.



DESCRIPTION

Several of the grey clasts have quite a bit of chlorite alteration. There are several fine-grained pinkish-grey and creamy colored clasts that could be felsic tuff (some of these clasts look porhyritic andcould be pyroclastic). There are several fine-grained greyish-brown clasts that could be a felsic tuff, with alterations giving the color. There are a few small soft, very fine-grained dark-grey clasts thatare probably argillite. The clasts are imbricated at ~40º TCA (some of the clasts look stretched). The matrix is fine-grained and grey in color and is foliated at ~40º TCA. There is some carbonate andchlorite alteration, along with some disseminated pyrite and blue quartz eyes throughout the matrix. From ~605.00 m - 607.00 m, there are quite a few large piles of pyrrhotite in the matrix.The sandstone zones appear massive (no obvious bedding, layers, etc.), and are foliated at ~40º TCA (the grains have a prefered orientation). There is some carbonate and chlorite alteration, along withblue quartz eyes and a bit of disseminated pyrite throughout the sandstone zones.The veins are mm - cm in size and have carbonate alterations. A few veins are slightly deformed with a sigmoidal form.This unit is similar to the unit from 589.66 m - 596.17 m. This could be representative of an S-type fold.The contact at 622.23 m is approximate. There is a vein at this point which may be obscuring the contact.

622.27 640.68 CONGLO; SS; C/F; C/ARG; STConglo; Sandstone; Felsic Clast; Argillite Clasts; Stratified/LaminatedThe rock is made up of repetitive sequences with alternating zones of grey conglomerate (m - several m), and grey coarse-grained sandstone (cm - m). The sequences appear to be from the same sourcedeposited by different events. The rock is composed of 75% conglomerate, 25% sandstone and <1% quartz veins. The contacts between zones are irregular and between ~45º - 50º TCA.The conglomerate zones are polymictic, medium-supported (has areas that are clast or matrix-supported), and are composed of ~ 55% felsic clasts, 25% matrix and 20% argillite clasts. The clasts rangein shape from sub-angular to sub-rounded and in size from 1 mm - 5 cm ( a few are up to 10 cm). There are several fine-grained light-grey to medium-grey clasts that could be an andesitic or dacitictuff. There are several soft, very fine-grained dark-grey clasts that are probably argillite. There are a lot of quartz fragments (very light-grey to bluish-white, very fine-grained and very hard). There are afew light-grey to grey coarse-grained clasts that could be sandstone. There are two large (17 cm - 18 cm), coarse-grained medium bluish-grey (from blue quartz) clasts, possibly granitic. A thin section(LG20870), was taken to determine composition. There are a few light grey - medium-grey clasts with quartz eyes (feldspathic intrusives?). The light-grey clasts have pyrite and feldspar laths, they greyhave quartz eyes, muscovite and a mafic mineral (chlorite?). One of these clasts is altered yellow from sericite. The core surface is very rough making it difficult to properly identify the clasts. Theclasts are imbricated at ~50º TCA (some of the clasts look stretched). The matrix is coarse-grained grey in color and is foliated at 50º TCA. There is carbonate alteration and a bit of disseminated pyriteand some blue quartz eyes throughout the matrix.The sandstone zones appear massive with no obvious foliations or other structural features. There is carbonate and some chlorite alteration and a small amount of disseminated pyrite in the sandstone.The sandstone appears to be foliated at ~50º TCA (the grains have a prefered orientation).The veins are mm - cm in size and have carbonate alterations. Some of the veins are deformed with sigmoidal and brecciated forms.The contact at 640.68 m is approximate. The core is broken with pieces missing at this point, but the clasts are smaller and there is chert in the section right after 640.68 m.

640.68 678.00 CONGLO; SS; C/F; C\S5C; STConglo; Sandstone; Felsic Clast; Chert Clasts; Stratified/LaminatedThe rock is made up of repetitive sequences with alternating zones of grey polymictic conglomerate (m - several m), and grey coarse-grained sandstone (cm - m). The sequences appear to be from thesame source deposited by different events. The rock is composed of 80% conglomerate, 20% sandstone and <1% quartz veins. The contacts between zones are irregular at ~30º TCA.The conglomerate zones are medium-supported (has areas that are clast or matrix-supported), and are composed of ~40% felsic clasts, 25% chert and 35% matrix. The clasts range in shape fromsub-angular to sub-rounded (there are a few angular clasts), and in size from 1 mm - 4 cm. There are several fine-grained light-grey to medium-grey clasts that could be an andesitic or dacitic tuff.Several of the grey clasts have some chlorite alteration. There are several fine-grained pinkish-grey and creamy colored clasts that could be felsic tuff (some of these clasts look porhyritic and could bepyroclastic). There are several fine-grained light-brown clasts that could be a felsic tuff, with alterations giving the color. There are a few small soft, very fine-grained dark-grey to black clasts that areprobably argillite. There are a lot of very fine-grained very hard pinkish to yellowish-grey and grey clasts that are probably chert (the largest amount is seen from 640.68 m - 675.68 m). There areseveral very light-grey to dark-grey porphyritic clasts that contain blue quartz, and feldspar laths (the light ones contain muscovite and one of them is yellow from sericite (?) alteration). These clastscould possibly be feldspathic trachyte. There are several white coarse-grained intrusive clasts that are difficult to fracture with a hammer and are probably granitic. These clasts contain quartz, feldspar,pyrite and biotite. These clasts are not seen in hole CHAB 06-45. The clasts are imbricated at ~50º TCA (some of the clasts look stretched). The matrix is fine-grained and grey in color and is foliatedat ~50º TCA. There is carbonate, sericite and chlorite alteration, along with some disseminated pyrite and blue quartz eyes throughout the matrix.The sandstone zones appear massive (no obvious bedding, layers, etc.), and are foliated at ~50º TCA (the grains have a prefered orientation). There are a few tiny felsic and chert clasts scatteredthroughout the sandstone. There is some carbonate and chlorite alteration, along with a bit of disseminated pyrite throughout the sandstone zones.The veins are mm - cm in size and have carbonate alterations. A few veins are slightly deformed with sigmoidal and brecciated forms.The contact at 678.00 m is irregular and at ~50º TCA.

678.00 693.13 CONGLO; C/ARGConglo; Argillite ClastsThe rock is a grey polymictic (limited) conglomerate. The rock is matrix-supported and composed of ~ 55% matrix, 25% argillite clasts, 19% felsic clasts and 1% quartz veins.The clasts range in shape from sub-angular to rounded and in size from 1 mm - 5 cm (there are a few large clasts up to 12 cm). From 678.68 m - 679.24 m there is a very large (56 cm) greymedium-grained clast that could be sedimentary in origin. There are many soft very fine-grained, dark-grey to black clasts that are probably argillite. Also there are several soft very fine-grained greyclasts that could be siltstone. There are several fine-grained grey clasts, with chlorite alterations, that could be a dacitic tuff. There are a few light-grey to pinkish colored very fine-grained very hardclasts that may be chert. There are several very light-grey to dark-grey porphyritic clasts that contain blue quartz, and feldspar laths. These clasts could possibly be feldspathic trachyte. There are severalvery hard white coarse-grained intrusive clasts that are probably granitic. These clasts contain quartz, feldspar, pyrite and biotite. The clasts are imbricated at ~45º TCA (some appear stretched).



DESCRIPTION

The matrix is grey medium-grained and foliated at ~45º TCA (grains appear to have a prefered orientation). There is carbonate and chlorite alteration and some disseminated pyrite throughout the matrix.The veins are mm - cm in size and contain carbonate alterations. Some of the veins are deformed with sigmoidal and brecciated forms. A few veins have a bit of chlorite alteration.The contact at 693.13 m is approximate. There is quite a bit of chlorite alteration and quartz veining obscuring the actual contact.

693.13 729.17 CONGLO; C/FConglo; Felsic ClastThe rock is a grey polymictic conglomerate. The conglomerate is medium-supported (has areas that are clast-supported or matrix-supported), and is composed of ~60% felsic clasts, 35% matrix and 5%quartz veins. The clasts range in shape from sub-rounded to rounded (there are a few sub-angular clasts), and in size from 1 mm - 5 cm (there are a few clasts up to 10 cm). From ~694.54 - 694.92 m,there is a large (38 cm) fine-grained grey feldspathic clast, with feldspar and quartz crystals. There are some soft very fine-grained dark-grey to black clasts that are probably argillite. There are a lot offine-grained grey to medium-grey (some have chlorite alterations), that could be a dacitic tuff. There are a few pinkish colored and creamy colored clasts that could be felsic tuff (some of these clastslook porhyritic and could be pyroclastic). There are several very fine-grained light pinkish-grey to grey clasts that are very hard and may be chert. There are several very hard white coarse-grainedintrusive clasts that are probably granitic. These clasts contain quartz, feldspar, pyrite and biotite. There are several dark-grey porphyritic clasts that contain blue quartz, and feldspar laths. These clastscould possibly be feldspathic trachyte. There are a few medium-grained grey clasts that could be sandstone. The clasts are imbricated at ~45º TCA (some of the clasts look stretched).The matrix is fine-grained and grey in color and is foliated at ~45º TCA. There is quite a bit of carbonate and chlorite alteration, along with some disseminated pyrite and pyrrhotite and a few blue quartzeyes throughout the matrix. From ~725.50 m - 729.17 m, there is a bit of leucoxene alteration in the matrix. There is a large pile of pyrrohtite at 725.83 m.The veins are mm - cm in size and have carbonate alterations. Several of the veins are deformed with sigmoidal and brecciated forms. A few veins are sub-parallel TCA. Several of the veins have a bitof chlorite and a few piles of pyrrhotite associated with them.The contact at 729.17 m is approximate. There is a quartz vein and a bit of alteration at this point obscuring any actual contact.

729.17 743.51 CONGLO; SS; C/ARG; C/F; STConglo; Sandstone; Argillite Clasts; Felsic Clast; Stratified/LaminatedThe rock is a series of alternating sequences with zones of grey conglomerate ( cm - several m) and zones of grey medium-grained sandstone (cm - m) . The sequences appear to be from the same sourcedeposited by different events. The rock is composed of ~65% conglomerate, 33% sandstone and 2% quartz veins. The contacts between layers are irregular at ~40º TCA and gradational.The conglomerate zones are polymictic, matrix-supported and are composed of ~45% matrix, 35% argillite clasts and 20% felsic clasts. The clasts range in shape from sub-rounded to rounded and insize from 1 mm - 2 cm ( there are a few up to 5 cm). There are several fine-grained light-grey to medium-grey clasts that could be dacitic tuff. Several of the grey clasts have chlorite alterations. Thereare several fine-grained pinkish-grey and creamy colored clasts that could be felsic tuff (some of these clasts look porhyritic and could be pyroclastic). There are several soft, very fine-grained dark-greyto black clasts that are probably argillite. Also there are several soft very fine-grained grey clasts that could be siltstone. There are a few very hard white coarse-grained intrusive clasts that are probablygranitic. These clasts contain quartz, feldspar, pyrite and biotite. There are a few very fine-grained light pinkish-grey to light-grey clasts that are very hard and may be chert. The clasts are imbricated at~45º TCA (some of the clasts look stretched). The matrix is fine-grained and grey in color and is foliated at ~45º TCA. From 737.32 m - 738.34 m, the matrix is very coarse-grained. There is carbonateand some chlorite alteration, along with some disseminated pyrite and blue quartz eyes throughout the matrix.The sandstone zones appear massive (no obvious bedding, layers, etc.), and are foliated at ~45º TCA (the grains have a prefered orientation). There is some carbonate and chlorite alteration, along with abit of disseminated pyrite throughout the sandstone zones.The veins are mm - cm in size and have carbonate alterations. A few veins are slightly deformed with sigmoidal and brecciated forms.The contact at 743.51 m is approximate. The core is broken with a few pieces missing right along the contact. It appears to be at ~38º TCA.

743.51 781.32 SS; ARGSandstone; ArgilliteThe rock is a fine to coarse-grained grey sandstone (cm - several m), with very fine-grained dark-grey to black argillite layers (mm - m). The rock is composed of 60% sandstone, 40% argillite and <1%quartz veins. The contacts between layers are irregular and at ~50º TCA. Some of the contacts and argillite layers are very convoluted and mixed up in the sandstone. The sandstone grades back andforth from fine to coarse and some of the sandstone sections have small angular argillite fragments. The unit is foliated at ~55º TCA and there are crenulations between ~30º - sub-parallel TCA in someareas in the argillite layers.There is carbonate alterations and a bit of disseminated pyrite throughout the unit.The quartz veins are mm - cm in size and have carbonate alterations. Many of the veins are deformed with sigmoidal and brecciated forms. There are a few veins that are sub-parallel TCA.The contact at 781.32 m is irregular and at ~50º TCA.

781.32 815.12 CONGLO; SS; C/F; C\S5C; STConglo; Sandstone; Felsic Clast; Chert Clasts; Stratified/LaminatedThe rock is made up of repetitive sequences with alternating zones of grey polymictic conglomerate (m - several m), and grey coarse-grained sandstone (cm - m). The sequences appear to be from thesame source deposited by different events. The rock is composed of 85% conglomerate, 14% sandstone and 1% quartz veins. The contacts between zones are irregular at ~50º TCA and gradational.The conglomerate zones are medium-supported (has areas that are clast or matrix-supported), and are composed of ~60% felsic clasts, 35% matrix and 5% chert. The clasts range in shape fromsub-angular to sub-rounded (there are a few angular clasts), and in size from 1 mm - 4 cm (there are a few up to 7 cm). There are several fine-grained light-grey to medium-grey clasts that could be anandesitic or dacitic tuff. Several of the grey clasts have chlorite alteration. There are several fine-grained pinkish-grey and creamy colored clasts that could be felsic tuff (some of these clasts lookporhyritic and could be pyroclastic). There are several soft, very fine-grained dark-grey to black clasts that are probably argillite. There are a lot of very fine-grained very hard pinkish to yellowish-greyand grey clasts that are probably chert. There are a few dark-grey porphyritic clasts that contain blue quartz, and feldspar laths, that could possibly be feldspathic trachyte. There are a few white



DESCRIPTION

coarse-grained intrusive clasts that are probably granitic and contain quartz, feldspar, pyrite and biotite. The clasts are imbricated at ~45º TCA (some of the clasts look stretched). The matrix ismedium-grained and grey in color and is foliated at ~45º TCA. There is carbonate and chlorite alteration, along with a bit of disseminated pyrite and blue quartz eyes throughout the matrix.The sandstone zones appear massive (no obvious bedding, layers, etc.), and are foliated at ~45º TCA (the grains have a prefered orientation). From ~783.3 m - 784.33 m, there are a few felsic andargillite clasts in the sandstone section. There is some carbonate and chlorite alteration, along with a bit of disseminated pyrite throughout the sandstone zones.The veins are mm - cm in size and have carbonate alterations. Several veins are deformed with sigmoidal and brecciated forms and have some chlorite alteration.The contact at 815.12 m is irregular at ~50º TCA.

815.12 818.34 CONGLO; C/ARGConglo; Argillite ClastsThe rock is a grey mainly monomictic (there are a few felsic clasts) conglomerate. The rock is matrix-supported and composed of ~ 69% matrix, 25% argillite clasts, 5% felsic clasts and 1% quartz veins.The clasts range in shape from angular to sub-rounded and in size from 1 mm - 2 cm. There is one large (17 cm) grey porphyritic clast that contains blue quartz, and feldspar laths, possibly a feldspathictrachyte. There are many argillite clasts (soft very fine-grained, dark-grey to black). There are a few fine-grained grey clasts, with chlorite alterations, that could be a dacitic tuff. The clasts areimbricated at ~55º TCA (some appear stretched).The matrix is grey medium-grained and foliated at ~55º TCA (grains appear to have a prefered orientation). There is carbonate and chlorite alteration and some disseminated pyrite throughout the matrix.The veins are mm - cm in size and contain carbonate alterations. Some of the veins are deformed with sigmoidal and brecciated forms. A few veins have a bit of chlorite alteration.The contact at 818.34 m is approximate. There is a quartz vein obscuring the actual contact.

818.34 822.64 CONGLO; C/FConglo; Felsic ClastThe rock is a grey polymictic conglomerate. The conglomerate is polymictic medium-supported (has areas that are clast-supported or matrix-supported), and is composed of ~68% felsic clasts, 30%matrix and 2% quartz veins. The clasts range in shape from sub-angular to sub-rounded and in size from 1 mm - 3 cm (there are a few clasts up to 8 cm). There are some soft very fine-graineddark-grey to black clasts that are probably argillite. There are a lot of fine-grained grey to medium-grey (some have chlorite alterations), that could be a dacitic tuff. There are a few very fine-grainedlight pinkish-grey to grey clasts that are very hard and may be chert. There are several very hard white coarse-grained intrusive clasts that contain quartz, feldspar, pyrite and biotite and are probablygranitic. There are several dark-grey porphyritic clasts that contain blue quartz, and feldspar laths that could possibly be feldspathic trachyte. There are a few medium-grained grey clasts that could besandstone. The clasts are imbricated at ~40º TCA (some of the clasts look stretched).The matrix is fine-grained and grey in color and is foliated at ~40º TCA. There is quite a bit of carbonate and chlorite alteration, along with some disseminated pyrite and a few blue quartz eyesthroughout the matrix.The veins are mm - cm in size and have carbonate alterations. A few of the veins are deformed with sigmoidal and brecciated forms.The contact at 822.64 m is approximate. There is a quartz vein at this point obscuring the actual contact.

822.64 846.23 CONGLO; SS; C/ARG; STConglo; Sandstone; Argillite Clasts; Stratified/LaminatedThe rock is a series of alternating sequences with zones of grey conglomerate (cm - several m), and zones of grey medium-grained sandstone (cm - several m). The sequences appear to be from the samesource deposited by different events. The rock is composed of ~50% conglomerate, 46% sandstone and 4% quartz veins. The contacts between layers are gradational.The conglomerate zones are polymictic (limited), matrix-supported and are composed of ~65% matrix, 30% argillite clasts and 5% felsic clasts. The clasts range in shape from angular to sub-roundedand in size from 1 mm - 2 cm ( there are a few up to 4 cm). There are a few fine-grained light-grey to medium-grey clasts that could be dacitic tuff. Several of the grey clasts have chlorite alterations.There are a lot of argillite clasts (soft, very fine-grained dark-grey to black), many are quite angular like rip-up fragments. Also there are several soft very fine-grained grey clasts that could be siltstone.The clasts are imbricated at ~50º TCA (some of the clasts look stretched). The matrix is medium-grained and grey in color and is foliated at ~50º TCA. There is carbonate and some chlorite alteration,along with some disseminated pyrite and blue quartz eyes throughout the matrix.The sandstone zones appear massive (no obvious bedding, layers, etc.), and are foliated at ~50º TCA (the grains have a prefered orientation). There is some carbonate and chlorite alteration, along with abit of disseminated pyrite throughout the sandstone zones.The veins are mm - cm in size and have carbonate alterations. A few veins are slightly deformed with sigmoidal and brecciated forms.The contact at 846.23 m is irregular at ~40º TCA.

846.23 924.00 ARG; S; SSArgillite; Siltstone; SandstoneThe rock is a dark-grey to black very fine-grained argillite (mm - several m), with medium-grey fine-grained siltstone layers (mm - cm) and light-grey to grey medium to coarse-grained sandstone layers(cm -m). The rock is composed of ~% 50 argillite, 39% siltstone, 10% sandstone and 1% quartz veins.The contacts between layers are sharp to irregular and at ~50º TCA. Some of the contacts are very convoluted and the layers are all mixed up. There are a few small argillite fragments in some of thesandstone sections. The rock is foliated at ~45º TCA and there are crenulations in some areas in the argillite. There are some areas in the argillite where fluting can be seen, the direction of he flutingindicates a down hole polarity. There is carbonate alteration and disseminated pyrite throughout the unit (there is a bit of chlorite alteration in the siltstone and sandstone sections).The veins are mm - cm in size and have carbonate alterations. Several are deformed with sigmoidal and brecciated forms. There are a few veins that are oriented to the foliation.



DESCRIPTION






Drilled by : Foramex 1 From : 2006-08-06 To : 2006-08-06Geologist : Laura Mancini, Élise Bourgault et finalisé par Serge Massé Description date : 2006-08-06

Collar


Comments




671200.0005326400.000350.000




Flex-it 51.00m 268.48° -83.96°Flex-it 54.00m 268.62° -84.13°Flex-it 57.00m 269.75° -83.95°Flex-it 60.00m 272.55° -83.41°Flex-it 63.00m 272.29° -83.34°Flex-it 66.00m 277.17° -83.82°Flex-it 69.00m 268.96° -83.44°Flex-it 72.00m 278.17° -83.08°Flex-it 75.00m 278.20° -83.02°Flex-Dip 78.00m -82.65°Flex-it 81.00m 278.29° -82.78°Flex-it 84.00m 277.97° -82.99°Flex-it 87.00m 271.89° -82.50°Flex-it 90.00m 272.20° -82.35°Flex-it 93.00m 271.41° -82.40°Flex-it 96.00m 272.45° -82.20°




Type Depth Azimuth PlungeFlex-it 252.00m 267.28° -77.22°Flex-it 255.00m 268.49° -77.10°Flex-it 258.00m 268.17° -77.07°Flex-it 261.00m 270.83° -76.57°Flex-it 264.00m 272.13° -76.27°Flex-it 267.00m 271.79° -76.18°Flex-it 270.00m 268.91° -76.41°Flex-it 273.00m 268.16° -76.35°Flex-it 276.00m 269.62° -76.23°Flex-it 279.00m 268.42° -75.71°Flex-it 282.00m 271.19° -75.85°Flex-it 285.00m 271.39° -75.74°Flex-it 288.00m 271.11° -75.65°Flex-it 291.00m 269.86° -75.71°Flex-it 294.00m 268.41° -75.50°Flex-it 297.00m 267.72° -75.17°Flex-it 300.00m 271.43° -75.13°Flex-it 303.00m 269.80° -75.08°Flex-it 306.00m 270.77° -74.98°Flex-it 309.00m 271.80° -74.38°Flex-it 312.00m 271.52° -74.68°Flex-it 315.00m 271.59° -74.60°Flex-it 318.00m 268.96° -74.45°Flex-it 321.00m 269.83° -74.18°Flex-it 324.00m 268.92° -74.06°Flex-Dip 327.00m -73.97°Flex-it 330.00m 269.45° -73.89°Flex-it 333.00m 269.46° -73.93°Flex-it 336.00m 270.48° -74.09°Flex-it 339.00m 270.67° -73.60°Flex-it 342.00m 270.72° -73.45°Flex-it 345.00m 272.15° -73.80°Flex-it 348.00m 272.21° -73.54°Flex-it 351.00m 269.90° -73.35°Flex-it 354.00m 270.94° -73.05°Flex-it 357.00m 270.23° -73.07°Flex-it 360.00m 270.01° -73.00°Flex-it 363.00m 272.35° -73.08°Flex-it 366.00m 271.84° -73.01°Flex-it 369.00m 269.57° -72.62°Flex-it 372.00m 272.20° -72.43°Flex-it 375.00m 269.99° -72.20°Flex-it 378.00m 270.41° -72.10°Flex-it 381.00m 272.00° -72.04°Flex-it 384.00m 269.82° -71.99°Flex-it 387.00m 269.42° -72.06°Flex-it 390.00m 270.59° -71.77°Flex-it 393.00m 269.91° -72.27°Flex-it 396.00m 269.57° -72.27°Flex-it 399.00m 269.72° -72.14°



Type Depth Azimuth PlungeFlex-it 1002.00m 289.29° -63.59°Flex-it 1005.00m 288.19° -63.86°Flex-it 1008.00m 288.19° -63.71°Flex-it 1011.00m 288.81° -63.76°Flex-it 1014.00m 288.94° -63.72°Flex-it 1017.00m 288.37° -63.76°




DESCRIPTION


2.50 90.81 V; V3B; PwVolcanic; Basalt; PillowThe rock is a fine-grained green to beigish-green pillowed basalt. There are dark-green fine-grained areas that appear to be pillow rinds. These areas are 1 cm - 5 cm wide and ~7.00 cm - 32.00 cmapart. From ~19.60 m - 46.00 m, there is a lot of alteration giving the rock a much lighter (beigy) color. There are areas in this section that have a lot of rust. This section also appears to be moremassive up to ~35.00 m (cannot see any obvious pillows), but because of the alteration it is difficult to see any features clearly. The rock is more grey from ~79.20 m - 85.06 m. From 85.06 m - 90.81m, the rock is green again but slightly more coarse-grained than previously and there is more carbonate alteration in this section. There is some carbonate alteration a lot of piles of pyrite throughout theunit. The rock is foliated at ~45º TCA.The rock contains ~10% quartz veins (mm - cm), with a lot of carbonate alterations. Most of the veins are deformed with sigmoidal and brecciated forms. A few of the veins have some chloritealteration. Several of the veins are oriented to the foliation.The contact at 90.81 m is approximate. There is a quartz vein at this point obscuring the actual contact.

90.81 155.23 V; V3R; MasVolcanic; Rhyolite; MassiveThe rock is a grey fine-grained massive felsic volcanic, possibly a rhyolite. There are no obvious pillows, bedding, layers etc. From 92.50 m - 98.40 m there is a melanocratic gabbroic intrusion(dark-grey very coarse-grained). The rock is very silicified from ~99.00 m - 103.50 m. It is also much lighter and finer-grained in this section. There are three mesocratic gabbroic intrusions (lightcolored coarse-grained), from 112.59 m - 116.60 m, 120.20 m - 122.50 m and 126.64 m - 127.12 m. The pyroxene is from 1 mm - 3 mm in size and is much larger than the feldspar in all theintrusions. There is quite a bit of carbonate alteration and chlorite replacement of primary minerals (spilitization) in these sections. The section from 130.50 m - 138.00 m has a lot of what appear to beamygdules filled with carbonate. There is a shear zone that starts at ~141.00 m and continues into the next unit. The rock is foliated at ~50º TCA. There is a bit of carbonate and sericite alteration alongwith disseminated and piles of pyrite throughout the unit.The rock contains ~25% quartz veins (mm - cm), with carbonate alterations. Several of the veins are deformed with sigmoidal and brecciated forms. There are a couple of veins that are sub-parallelTCA and some are oriented to the foliation. Some of the veins have piles of pyrite associated with them.The contact at 155.23 m is approximate. There is a quartz vein and the core is broken at this point obscuring the actual contact.

92.50 98.40 I3GGabbroMelanocratic gabbro intrusion in fine-grained volcanic unit.

112.59 116.60 I3GGabbroMesocratic gabbro intrusion in fine-grained volcanic unit.



155.23 167.45 CONGLO; C/ARGConglo; Argillite ClastsThe rock is a dark-grey polymictic (limited) conglomerate. The rock is in the shear zone that started in the previous unit and is very deformed and altered. It is very difficult to tell what are clasts andmatrix and if the rock is clast or matrix-supported, therefore percentages are a rough approximation. The conglomerate appears to be composed of ~45% argillite clasts, 25% felsic clasts, 20%quartz-carbonate veins and 10% matrix.The clasts are very stretched and elongated and appear to be ~1 mm - 2 cm in size. Because of their deformity, it is difficult to say if the clasts are rounded, sub-rounded, etc. There are a lot of argilliteclasts (dark-grey to black very fine-grained and very soft). There are a few fine-grained grey clasts, some with chlorite alteration, that could be a volcanic tuff. There are several light-grey to white clasts(?) that are probably quartz-carbonate (very hard and fizzy). There are a few grey medium-grained clasts that could be sandstone. The clasts are imbricated at ~50º TCA.The matrix appears to be dark-grey, fine-grained and is heavily foliated at ~50º TCA. There are carbonate, sericite, chlorite alterations, some leucoxene alteration and some disseminated pyritethroughout the unit.The quartz-carbonate veins are mm - cm in size and tiny little spider veins. Many are deformed with sigmoidal form. Most of the veins have been transposed and are oriented to the foliation.The contact at 167.45 m is approximate. There is veining and the rock is broken at this point, but the clasts are more felsic and a little less deformed right after 167.45 m.

167.45 186.25 CONGLO; C/FConglo; Felsic Clast



DESCRIPTION

The rock is a grey polymictic conglomerate. The shear zone from the other two units continues through this one and has deformed and altered the rock. From ~168.70 m - 173.00 m, the rock is lessdeformed and appears to be clast-supported. The clasts are also less deformed in this section. The rest of the unit is so deformed it is difficult to see clasts or matrix clearly. Percentages are a very roughestimation. The rock appears to be composed of 60% felsic clasts, 25% quartz-carbonate veins and 15% matrix.The clasts range in shape from sub-angular to sub-rounded and in size from ~1 mm - 3 cm. There are a few creamy colored and grey fine-grained clasts that look porphyritic and could be pyroclastic.There are several fine-grained grey clasts, a lot with chlorite alteration, that could be a felsic tuff. There are several very fine-grained, very hard light-grey clasts that are probably quartz. there are a fewdark-grey to black very fine-grained soft clasts that are probably argillite. There are a few medium-grained grey clasts that could be sandstone. the clasts are imbricated at ~50º TCA. and many appearstretched.The matrix is fine-grained grey and heavily foliated at ~50º TCA. There are carbonate, sericite, chlorite alterations, some leucoxene alteration and some disseminated pyrite throughout the unit.The quartz-carbonate veins are mm - cm in size and tiny little spider veins. Many are deformed with sigmoidal form. Most of the veins have been transposed and are oriented to the foliation. Some ofthe veins have a few pyrite piles associated with them.The contact at 186.25 m is approximate. The rock is heavily veined and altered obscuring any actual contact.

186.25 213.86 CZContact ZoneShear zone with ~40% quartz veins which are very deformed with sigmoidal and brecciated forms. The veins contain a lot of carbonate and chlorite alterations. The rock appears to be a grey color andis very deformed (brecciated), and altered. There are no distinguishable clasts or other features to properly identify the rock. It is very difficult to tell what the protolith was. There is chlorite alterationand disseminated pyrite throughout the unit.

213.86 220.63 CONGLO; Ga; PoConglomerate; Gray; PolymicticThe rock is a grey polymictic conglomerate. The shear zone from the other units continues through this one and has deformed and altered the rock (less than the previous units). The conglomerate isclast-supported and the clasts are also less deformed in this section. The rock is composed of 75% felsic clasts, 20% matrix and 5% quartz-carbonate veins.The clasts range in shape from sub-angular to sub-rounded (there are a few rounded), and in size from ~1 mm - 5 cm (there are a couple at 7 cm). There are a few grey fine-grained clasts that lookporphyritic and could be pyroclastic. There are several fine-grained grey clasts, a lot with chlorite alteration, that could be a felsic tuff. There are several very fine-grained, very hard light-grey clasts thatare probably quartz. there are a few tiny dark-grey to black very fine-grained soft clasts that are probably argillite. There are a few coarse-grained dark-grey clasts with what appear to be feldpsarcrystals, could be feldspathic trachyte. There is a coarse-grained light colored intrusive clasts that could be a leucocratic gabbro. The clasts are imbricated at ~50º TCA. and many appear stretched.The matrix is fine-grained grey and foliated at ~50º TCA. There are carbonate, sericite and a lot of chlorite alterations and some disseminated pyrite throughout the unit.The quartz-carbonate veins are mm - cm in size and tiny little spider veins. Many are deformed with sigmoidal form. Most of the veins have been transposed and are oriented to the foliation. Some ofthe veins have a few pyrite piles associated with them.The contact at 220.63 m is approximate. The core is broken and the rock is heavily veined and altered obscuring any actual contact.

213.86 220.63 CtSClast-Supportedconglomerate clast-supported

220.63 246.09 S; V; V3RSiltstone; Volcanic; RhyoliteThe rock is a fine-grained dark-grey to grey siltstone (cm - m), with light-grey volcanic layers (cm - m), possibly rhyolite. The shear zone from the previous units continues through this one and hasdeformed and altered the rock. This makes it very difficult to see any real features. The rock is heavily foliated at ~50º TCA.There is no obvious primary bedding, layers, etc., in the siltstone sections. The silstone does have quite a bit of disseminate and small piles of pyrrhotite and some carbonate alteration in it. The contactsbetween the siltstone and volcanics are irregular at ~47º TCA. Most of the contacts are obscured by veining.The volcanic sections have the appearance of possibly being pillows. There are dark-grey bands cm wide that could be pillow rinds. These bands are ~10 cm - 30 cm apart. It is difficult to say for surethat they are rinds, they may just be alterations caused by the large number of quartz veins in the section. There is carbonate alteration and chlorite replacement of primary minerals (spilitization) seenthroughout the volcanic section.The rock contains ~30% quartz veins (mm - cm), and a lot of tiny little spider veins. The veins are deformed with sigmoidal and brecciated forms. The veins contain carbonate alterations and a few havepiles of pyrrhotite associated with them. Many of the veins appear to have been transposed and are oriented to the foliation. There is one large vein from ~222.03 m - 222.53 m that appears to containsmokey quartz.The contact at 246.09 m is approximate. The core is broken and there is a quartz vein at this point obscuring the actual contact. Clasts appear right after 246.09 m.

246.09 344.75 CONGLO; GaG; PoConglo; Gray Green; PolymicticThe rock is a grey polymictic conglomerate. The shear zone from the previous units seems to end at ~262.70 m (the rock is less deformed and there are a lot less quartz veins after this point). From~321.00 m - 334.00 m, the rock starts to grade back and forth from a pebble-cobble conglomerate to a more granule conglomerate. The clast types and matrix, however are identical to the rest of the unit.The conglomerate is clast-supported and is composed of ~65% felsic clasts, 20% quartz veins and 15% matrix . The clasts range in shape from sub-angular to rounded and in size from 1 mm - 5 cm(there are several clasts that range from 6 cm - 17 cm). There are a few fine-grained grey feldspathic clast, with quartz eyes and feldspar crystals. There are a lot of fine-grained brownish-grey and grey



DESCRIPTION

to medium-grey clasts (several of the grey clasts have chlorite alterations), that could be a felsic tuff. The brown color could be from alterations. There are several pinkish colored, creamy and light-greycolored porhyritic clasts that could be pyroclastic. There are several light colored coarse-grained intrusive clasts that are possibly leucocratic gabbro. There are a few medium-grained grey clasts thatcould be sandstone. There are several very fine-grained, very hard light-grey to white clasts that are probably quartz. There are a few dark-grey porphyritic clasts that contain blue quartz, and feldsparlaths. These clasts could possibly be feldspathic trachyte. There are a few very fine-grained light yellowish-grey to grey clasts that are very hard and may be chert. There are some small soft veryfine-grained dark-grey to black clasts that are probably argillite (mostly from 321.00m 334.00 m). The clasts are imbricated at ~50º TCA (most of the clasts look stretched).The matrix is fine-grained and grey in color and is foliated at ~50º TCA. There is quite a bit of carbonate, sericite and chlorite alteration, along with some disseminated and piles of pyrrhotite and pyrite,and a bit of leucoxene alteration throughout the matrix.The veins are mm - cm in size and there are a lot of tiny little spider veins. The veins are deformed with sigmoidal and brecciated forms. The veins contain carbonate alterations and a few have piles ofpyrrhotite associated with them. Many of the veins appear to have been transposed and are oriented to the foliation. A few veins have chlorite alteration. There is a large vein from 277.72 m - 277.89m, that has a lot of sericite and chlorite alteration giving it a pale yellowish-greenish-grey color.Contact net à 45 p/r à A/C.

246.09 334.00 CtSClast-Supportedconglomerate clast-supported

344.75 352.30 SS; ARG; STSandstone; Argillite; Stratified/LaminatedRoche sédimentaire : bandes de sandstone en alternance avec des laminations d'argilites.Unité composé de bancs (décimétriques à métriques) de sandstone (80%) en alternance avec des lits (0.1-1cm) d'argilites (20%).L'argilite est de couleur gris foncé et aphanitique.Le sandstone est de couleur gris moyen à pâle avec une granulométrie très fine à fine. Les lits sont généralement massifs, mais parfois littées. Très localement quelques grains sont plus grossiers (Qzeyes).Les lits (sandstone et argiles) ont une orientation de 70 degré A/C.De plus, environ 5 % de veinules de QZ et de CB sont présentes irrégulièrement à travers les lits et sont parfois déchirées.Des très fines traces de PY et PO sont disséminées irrégulièrement.Contact graduel

352.30 621.95 ARG; SS; STArgillite; Sandstone; Stratified/LaminatedRoche sédimentaire : Argilites en alternance avec des bandes de sandstone.Unité composé de bandes (0.5-30cm) de sandstone (40%) en alternance avec des lits (0.1-10cm) d'argilites (60%).L'argilite est de couleur gris foncé et aphanitique.Le sandstone est de couleur gris moyen à pâle avec une granulométrie très fine à fine. Les lits sont généralement massifs, mais parfois littées. Très localement quelques grains sont plus grossiers (Qzeyes et rip-up clasts)Les lits (sandstone et argiles) ont une orientation de 70 à 75degré A/C. Les lits sont en bandes minces, en bandes larges et en bandes irrégulières.De plus, environ 5 -10% de veinules de QZ et de CB sont présentes irrégulièrement à travers les lits et sont parfois déchirées.Des très fines traces de PY et PO sont disséminées irrégulièrement.Contact inférieur net à 40 degrés.

394.78 396.18 SS; TBL; MasSandstone; Tuff Breccia/Lapillistone; MassiveRoche sédimentaire : banc de sandstone et lapilli.Unité composé de deux bandes (65-70cm) de sandstone séparées par des lits (0.1-0.5cm) d'argilites (3%).L'argilite est de couleur gris foncé et aphanitique.Le sandstone est de couleur gris moyen à pâle avec une granulométrie de l'ordre des lapilli. Les bancs sont massifs. Orientation des lits d'argile à 75degré A/C.De plus, environ 5 à 10% de veinules de QZ et de CB sont présentes irrégulièrement et sont parfois déchirées.Rares traces de PY et PO sont disséminées irrégulièrement.Contact inférieur net

449.95 450.10 S5CChertchert

497.69 502.70 SS; ARG; STSandstone; Argillite; Stratified/Laminated



DESCRIPTION

Roche sédimentaire : bandes de sandstone en alternance avec des laminations d'argilites.Unité composé de bancs (décimétriques à métriques) de sandstone (90%) en alternance, dansl a 2ième moitié de l'unité, avec des lits (0.1-1cm) d'argilites (10%).L'argilite est de couleur gris foncé et aphanitique.Le sandstone est de couleur gris moyen à pâle avec une granulométrie fine à lapilli. Les lits sont généralement massifs, mais parfois littées.Les lits (sandstone et argiles) ont une orientation de 75 degré A/C.De plus, environ 2-3 % de veinules de QZ et de CB sont présentes irrégulièrement à travers les lits et sont parfois déchirées.Des très fines traces de PY et PO sont disséminées irrégulièrement.Contact graduel

507.10 510.28 SS; ARG; STSandstone; Argillite; Stratified/LaminatedRoche sédimentaire : bandes de sandstone en alternance avec des laminations ou petites bandes d'argilites.Unité composé de bancs (décimétriques à métriques) de sandstone (75%) en alternance, dansl a 2ième moitié de l'unité, avec des lits (0.1-4cm) d'argilites (10%).L'argilite est de couleur gris foncé et aphanitique.Le sandstone est de couleur gris moyen à pâle avec une granulométrie fine à lapilli. Les lits sont généralement massifs, mais parfois littées.Les lits (sandstone et argiles) ont une orientation de 75 degré de A/C.Un granoclassement normal constaté.De plus, environ 2-3 % de veinules de QZ et de CB sont présentes irrégulièrement à travers les lits et sont parfois déchirées.Des très fines traces de PY et PO sont disséminées irrégulièrement.Contact inférieur marqué par une bande de lapillistone de 27cm

518.07 554.60 SheShearingshear zone

560.40 563.00 SS; ARG; STSandstone; Argillite; Stratified/Laminatedc

621.95 643.15 SS; ARG; CONGLO; C/F; STSandstone; Argillite; Conglo; Felsic Clast; Stratified/LaminatedRoche fragmentaire : bandes de sandstone en alternance avec quelques bandes de conglomérats de la taille des granules (2-4mm).Quelques lamines d'argilite sont présentes.Passages ou bandes plus fin, à "granule sandstone" pluri-décimétrique à décimétrique alternant avec des passages ou bandes grossiers de "pebble to granule conglomerate monomictic and clast tomatrix-supported", pluri-métrique à décimétriquePassage plus fin à "granule sandstone" corresponds à 80% de l'intervalle.Passage conglomératique corresponds à 20% de l'intervalleLes contacts entre les passages sont parfois net et parfois graduel.Matrice est de couleur grise avec teinte jaunâtre, peu présente (20-30%), de grain très fin à fin (1/16 mm à 2 mm), composée de fp-qz et séricite. Ne semble pas avoir de chlorite.Les fragments sont sub-anguleux à sub-arrondis, souvent étirés, de couleur gris pâle, gris moyen et souvent avec teinte jaunâtre. Donc l'origine des fragments est probablement volcanique felsiquerhyolitique (tuff-Qz-Eyes et massif à cristaux porphyrique de Qz) et d'origine sédimentaire (sandstone et argillite)Foliation est visible, discontinue , en bandes et en environs 45-55 degrés.Granuloclassements indéterminé.Le réseau de veinule de Qz-Cb est présent (2%).Contact inf net avecpassage au S2S/S1C0/S4A à rip-up clasts

621.95 643.15 MxS; CtSMatrix-Supported; Clast-Supported

643.15 651.18 SS; ARG; CONGLO; C/ARG; C/F; STSandstone; Argillite; Conglo; Argillite Clasts; Felsic Clast; Stratified/LaminatedRoche fragmentaire : bandes de sandstone en alternance avec quelques bandes de conglomérats de la taille des granules (2-4mm).Quelques lamines et bandes d'argilite sont présentes.Passages ou bandes plus fin , à "granule sandstone" pluri-décimétrique à décimétrique alternant avec des passages ou bandes grossiers de "pebble to granule conglomerate monomictic and clast tomatrix-supported", pluri-métrique à décimétrique.L'unité se caractérise par la présence de petits (1mm) et gros (5cm) rip-up clasts .Passages plus fin à "granule sandstone" correspondant à 70% de l'intervalle. Passages conglomératique correspondant à 15% de l'intervalle et passages d'argilite correspondant à 15% de l'intervalleLes contacts entre les passages sont parfois net et parfois graduel.



DESCRIPTION

Matrice est de couleur grise avec peu de teinte jaunâtre, peu présente (20-30%), de grain très fin à fin (1/16 mm à 2 mm), composée de fp-qz et séricite. Ne semble pas avoir de chlorite.Les fragments sont sub-anguleux à sub-arrondis, souvent étirés, de couleur gris pâle, gris moyen et avec teinte jaunâtre. Donc l'origine des fragments est probablement volcanique felsique rhyolitique(tuff-Qz-Eyes et massif à cristaux porphyrique de Qz) et d'origine sédimentaire (sandstone et argillite)Foliation est visible, discontinue , en bandes et en environs 45 degrés a/c.Granuloclassement normal observé.Le réseau de veinule de Qz-Cb est présent (1-2%).Contact inf net avec passage au S2S/S1C0/S4A sans ou avec peu de rip-up

643.15 651.18 MxS; CtSMatrix-Supported; Clast-Supported

651.18 679.56 SS; CONGLO; C/FSandstone; Conglo; Felsic ClastRoche fragmentaire : bandes de sandstone en alternance avec des bandes de conglomérats de la taille des granules (2-4mm).Passages ou bandes plus fin, à sandstone massive pluri-décimétrique à décimétrique alternant avec des passages ou bandes grossièrs de "granule conglomerate monomictic medium to matrix-supported"décimétriqueDe 161.5 à 662.2 petite zone d'argillite.Passage plus fin à "granule sandstone" corresponds à 80% de l'intervalle.Passage conglomératique corresponds à 20% de l'intervalleLes contacts entre les passages sont parfois net et parfois graduel.Matrice est de couleur grise avec teinte jaunâtre, peu présente (20-%), de grain très fin à fin (1/16 mm à 2 mm), composée de fp-qz et séricite. Ne semble pas avoir de chlorite.Les fragments sont sub-anguleux à sub-arrondis, souvent étirés, de couleur gris pâle, gris moyen et souvent avec teinte jaunâtre. Donc l'origine des fragments est probablement volcanique felsiquerhyolitique (tuff-Qz-Eyes et massif à cristaux porphyrique de Qz).Foliation est visible, discontinue , en bandes et en environs 55 degrés.Granuloclassements peu visible et flouLe réseau de veinule de Qz-Cb est présent (2%).Contact inférieur net à 50 degrés A/C

651.18 679.56 MmS; MxSMedium-Supported; Matrix-Supported

679.56 862.70 SS; CONGLO; QE; C/ARGSandstone; Conglo; Quartz eyes; Argillite ClastsSérie de séquences sédimentaires : passage de faciès grossier (granules 2-4mm) conglomératique avec rip-up clast d'argillite (mm à cm) alternant avec des sandstones et silstones (massif) puis parfoisavec des bandes d'argilite (lamination).La majoritée des débuts de séquence du début de l'unité sont marquées par un faciès grossiers avec présence de rip-up clast d'argilite (granule to pebble). Par la suite, ces séquences présent ungranoclassement: Passages graduels de "granule conglomerate polymictic medium to matrix-supported" décimétrique à des bancs sandstone décimétriques à pluri-décimétriques puis d'argiliteLes rip-ups clast de la majorité des débuts de séquence implique selon moi la base du chenal. Donc nous avons une série de chenaux que ce mettent en place un par dessus l'autre et le tout est renversée.Une des séquences débutant à 703.83m présente une plus large bande contenant des rip-up (fin des rip up à 707.32).À partir de 748.96 et jusqu'à env. 807.5, il y a peu ou pas de bandes d'argilite, les rip-up clast d'argilite sont peu présent et de plus petite taille.à partir de 807.5,reprise argile et rip-up de même nature. La séquences débutant à 715.4m présente une plus large bande contenant bcp de rip-up (fin de l'abondance des rip up à 827.6).À 827.6, retour aux séries de séquence sans fin pélitique (mais avec peu de rip-up clast d'argilite jusqu'à environ 862.7.De 843.5 reprise rip-up d'argilite, mais avec nouveauté (entre 845.6 et 848.3), présence de rip-up de chert ? à texture aphanitique.Par la suite, la fin des séquence devient de plus en plus pélitique jusqu'à 892.15, puis retour à une séquence de conglomérat à rip-up d'argilite.En général :Passage plus fin à "granule sandstone" corresponds à 65% de l'intervalle.Passage conglomératique corresponds à 30% de l'intervallePassage pélitique corresponds à 5% de l'intervalleLes contacts entre les passages sont parfois net et parfois graduel.Les contacts entre les séquences sont plutôt net et tjs à 50 degrés A/C. Certaines fins de séquence sont marquées par des horizons d'argilite centimétrique.Matrice est de couleur grise avec teinte jaunâtre, peu présente (20-%), de grain très fin à fin (1/16 mm à 2 mm), composée de fp-qz et séricite. Ne semble pas avoir de chlorite.Les fragments de rip-un sont anguleux alors que les granules de conglomérat sont sub-anguleux à sub-arrondis, souvent étirés, de couleur gris pâle, gris moyen et souvent avec teinte jaunâtre. Donc



DESCRIPTION

l'origine des fragments est probablement volcanique felsique rhyolitique (tuff-Qz-Eyes et massif à cristaux porphyrique de Qz).Foliation est visible, discontinue , en bandes et à environ 40 degrés A/C.Le réseau de veinule de Qz-Cb est présent (2-3%).Contact inférieur de l'unité à degrés A/C.

679.56 862.70 MmS; MxSMedium-Supported; Matrix-Supported

748.96 753.82 Ak; SrMvankerite; sericite/muscoviteLe conglomérat, compris entre 748.96 et 753.82, du début de la séquence finisant à 760, présente une altération brune (à la limite de oxydation). Source altération non déterminée.

862.70 892.15 ARG; SS; STArgillite; Sandstone; Stratified/LaminatedRoche sédimentaire : Argilites en alternance avec des bandes de sandstone.Unité composé de lits d'argilites (60%) en alternance avec des bandes de sandstone (40%)L'argilite est de couleur gris foncé et aphanitique.Le sandstone est de couleur gris moyen à pâle avec une granulométrie très fine à granule. Les lits sont généralement massifs, mais parfois littées. Très localement à la base des sandstones (à 867.73 et à869.0m) quelques grains sont plus grossiers (Qz eyes et rip-up clasts).Les lits (sandstone et argiles) ont une orientation de 35 degré A/C. Les lits sont en bandes minces, en bandes larges et en bandes irrégulières.Plusieurs veines de QZ et de CB sont présentes irrégulièrement à travers les lits et sont déchirées (zone de déformation).Des très fines traces de PY et PO sont disséminées irrégulièrement.Contact inférieur plutôt net à 40 degrés.

872.00 886.70 SheShearingZone de charnière ou de shear

892.15 901.60 CONGLO; SS; SConglo; Sandstone; SiltstoneRetour à un séquences sédimentaires à matrix-supported : passage de faciès grossier (granules to pebble 2-10mm) conglomératique avec nombreux rip-up clast d'argillite (2mm à 60mm) alternant avecdes sandstones et silstones (massif) aussi à rip-up c/a.Aucune bande d'argilite n'est présente.La séquence débute par un petit horizon conglomératique c/a qui change rapidement par granoclassement progressif à un sandstone massif à rip-up clast jusqu'à 895.9.Par la suite, conglomérat à rip-up c/a abondant jusqu'à 901.2.Unité passant de matix-supported à médium-supportedPolymictique : c/a, QE, andésite/dacitePassage conglomératique corresponds à 65% de l'intervallePassage plus fin à "granule sandstone" corresponds à 35% de l'intervalle.Les contacts entre les passages sont graduel et tjs à 50 degrés A/C.Matrice est de couleur grise avec teinte jaunâtre, peu présente (20-%), de grain très fin à fin (1/16 mm à 2 mm), composée de fp-qz et séricite. Ne semble pas avoir de chlorite.Les fragments de rip-un sont anguleux alors que les granules de conglomérat sont sub-anguleux à sub-arrondis, souvent étirés, de couleur gris pâle, gris moyen et souvent avec teinte jaunâtre.Foliation est visible, discontinue , en bandes et à environ 60 degrés A/C.Le réseau de veinule de Qz-Cb très peu présentContact inférieur marqué par disparition des c/a.

892.15 901.60 MmS; MxSMedium-Supported; Matrix-Supportedmedium to matrix

901.60 938.50 CONGLO; SSConglo; SandstoneSérie de séquence de roche sédimentaires à medium matrix-supported : passage de faciès grossier (granules to pebble 2-150mm) conglomératique avec absence ou peu de rip-up c/a. Augmentation dufaciès sandstone en bande de 1-2cm jusqu'à 20-30cm) vers la fin de l'unité. Aucune bande d'argilite n'est présente.Unité marquée par la faible présence de c/a, mais augmentation de la taille des fragments conglomératiques.Unité à médium matrix -supported.



DESCRIPTION

Polymictique : c/a, QE, andésite/dacite + rhyolitePassage conglomératique corresponds à 80% de l'intervallePassage plus fin à "granule sandstone" corresponds à 20% de l'intervalle.Les contacts entre les passages sont graduel et tjs à 45-50 degrés A/C.Matrice est de couleur grise avec teinte jaunâtre, peu présente (20-%), de grain très fin à fin (1/16 mm à 2 mm), composée de fp-qz et séricite. Ne semble pas avoir de chlorite.Les fragments de rip-un sont anguleux alors que les granules de conglomérat sont sub-anguleux à sub-arrondis, souvent étirés, de couleur gris pâle, gris moyen et souvent avec teinte jaunâtre.Foliation est visible, discontinue , en bandes et à environ 55-60 degrés A/C.Le réseau de veinule de Qz-Cb peu présent.Contact inférieur marqué par la reprise de c/a dans l'unité suivante

901.60 938.50 MmSMedium-Supported

938.50 962.30 CONGLO; SS; C/ARGConglo; Sandstone; Argillite ClastsSérie de séquence de roche sédimentaires : passage de faciès grossier (granules to pebble 2-150mm) conglomératique avec augmentation graduelle des rip-up c/a au début de l'unité et alternant avec dessandstones et silstones (massif) aussi à rip-up c/a.Diminution du faciès sandstone en allant vers la fin de l'unité. Aucune bande d'argilite n'est présente.Unité marquée par la reprise graduelle de c/a au début et augmentation de la taille des fragments conglomératiques jusqu'à la fin de l'unité.Unité à médium- matrix supported.Polymictique : c/a, QE, andésite/dacite + rhyolitePassage conglomératique corresponds à 65% de l'intervallePassage plus fin à "granule sandstone" corresponds à 35% de l'intervalle.Les contacts entre les passages sont graduel et tjs à 50 degrés A/C.Matrice est de couleur grise avec teinte jaunâtre, peu présente (20-%), de grain très fin à fin (1/16 mm à 2 mm), composée de fp-qz et séricite. Ne semble pas avoir de chlorite.Les fragments de rip-un sont anguleux alors que les granules de conglomérat sont sub-anguleux à sub-arrondis, souvent étirés, de couleur gris pâle, gris moyen et souvent avec teinte jaunâtre.Foliation est visible, discontinue , en bandes et à environ 60 degrés A/C.Le réseau de veins de Qz-Cb plus abondant en fin d'unité du à la zone de déformation présente.Contact inférieur difus compte tenu de zone défo, mais relativement net puisque fin du conglo et reprise des argilite/sandstone


961.50 965.00 FrcFractureSheaing zone (?) plus ou moins évidente avec réseau de veins de quartz/ calcite

962.30 1020.00 ARG; SS; S; ST; C/ARGArgillite; Sandstone; Siltstone; Stratified/Laminated; Argillite ClastsRoche sédimentaire : Argilites en alternance avec des bandes de sandstone/silstone.Unité composé de bandes (0.2-60cm) de sandstone (40%) en alternance avec des lits (0.1-10cm) d'argilites (60%).L'argilite est de couleur gris foncé et aphanitique.Le sandstone/silstone est de couleur gris moyen à pâle avec une granulométrie très fine à fine. Les lits sont généralement massifs, mais parfois littées. Très localement quelques grains sont plus grossiers(rip-up clasts de 2 -10mm)Les lits (sandstone et argiles) ont une orientation de 60degré A/C. Les lits sont en bandes minces, en bandes larges et en bandes irrégulières.De plus, environ 5 -10% de veinules de QZ et de CB sont présentes irrégulièrement à travers les lits et sont parfois déchirées.Des très fines traces de PY et PO sont disséminées irrégulièrement.EOH à 1020m

993.00 1020.00 SheShearingZone déformation probable



DESCRIPTION






Drilled by : Foramex 2 From : 2006-09-28 To : 2006-11-21Geologist : Élise Bourgault Description date : 2006-11-23

Collar


Comments




671449.5155326398.912325.289


Flex-Dip 3.00m -85.83°Flex-Dip 6.00m -85.81°Flex-Dip 9.00m -85.82°Flex-Dip 12.00m -85.81°Flex-Dip 15.00m -85.43°Flex-it 18.00m 255.33° -84.95°Flex-it 21.00m 257.70° -84.84°Flex-it 24.00m 259.28° -84.69°Flex-it 27.00m 259.90° -84.60°Flex-it 30.00m 259.85° -84.52°Flex-it 33.00m 260.35° -84.40°Flex-it 36.00m 259.92° -84.31°Flex-it 39.00m 260.20° -84.25°Flex-it 42.00m 259.61° -84.09°Flex-it 45.00m 259.31° -83.97°Flex-it 48.00m 258.81° -83.74°






Type Depth Azimuth PlungeFlex-it 1149.00m 284.66° -63.65°Flex-it 1152.00m 285.65° -63.53°Flex-it 1155.00m 286.25° -63.36°Flex-it 1158.00m 286.67° -63.24°Flex-it 1161.00m 285.45° -63.52°Flex-it 1164.00m 285.90° -63.49°Flex-it 1167.00m 285.97° -63.47°Flex-it 1170.00m 285.89° -63.35°Flex-it 1173.00m 286.90° -63.32°Flex-it 1176.00m 286.22° -63.40°Flex-it 1179.00m 286.70° -63.27°Flex-it 1182.00m 286.47° -63.43°Flex-it 1185.00m 286.30° -63.36°Flex-it 1188.00m 286.22° -63.28°Flex-it 1191.00m 286.78° -63.15°Flex-it 1194.00m 286.27° -63.18°Flex-it 1197.00m 287.58° -62.79°Flex-it 1200.00m 286.70° -63.08°Flex-it 1203.00m 286.53° -62.95°Flex-it 1206.00m 287.24° -62.82°Flex-it 1209.00m 287.14° -62.80°Flex-it 1212.00m 287.29° -62.72°Flex-it 1215.00m 287.44° -62.68°Flex-it 1218.00m 287.19° -62.62°Flex-it 1221.00m 287.51° -62.59°Flex-it 1224.00m 286.96° -62.59°Flex-it 1227.00m 288.41° -62.28°Flex-it 1230.00m 287.26° -62.39°Flex-it 1233.00m 287.72° -62.37°Flex-it 1236.00m 288.45° -62.16°



DESCRIPTION


15.00 95.07 V; V3B; PwVolcanic; Basalt; PillowRoche volcanique : basalteRoche de couleur vert moyen avec une granulométrie aphanitique. Elle contient des pillows très bien visible à certains endroits, les rims sont biens visibles. Dans l'ensemble, la roche est chloritisée.Elle contient aussi une altération en carbonate, souvent sous forme de cristaux (parfois altéré), cette altération est plus abondante (5-10% de CB) entre 33.16-52.70m. Cette altération en CB, rendl'évaluation de la texture difficile. Des petits leucoxènes sont aussi présents à certains endroits. À certains endroits une foliation est présente, généralement à 60 degré A/C.Entre 62.21-79.82 : passage plus pâle, plus grossiers, lave grossière? gabbro?. Selon Ed Van, volcanoclastique. Voir LG22510.À partir de 79.82m jusqu'à la fin, les amygdules de CB sont présentes (1-4mm).Des traces de PY (souvent cubique) sont disséminées irrégulièrement.Environ 3% de veines (1-3cm) et veinules de CB-QZ blanc sont injectés irrégulièrement, souvent en tension et parfois déchirées.Contact diffus et graduel avec l'unité suivante.

73.70 74.40 VEI;;;;;;VeinVeine de QZ gris et blanc, déchiré, fragmenté, localement bréchique. Elle contient aussi des CB, de la séricite et semble composé de tourmaline (minéral noir dur). Des fines traces locales dePY sont présentes. Environ 10-15% d'encaissant est présent dans la veine.Épontes à 20 degré A/C.

95.07 105.00 V; PyVolcanic; PyroclasticRoche pyroclastique?? Tuff/Lapilli?Roche difficile à évaluer, elle possède une texture particulière.Elle semble contenir environ 60% de fragments plus felsique (mono) de couleur grisâtre dans une matrice verte aphanitique (semblable au basalte précédent). Le contour des fragments est souvent flou.Un littage? ou foliation? est présent a environ 50 degré A/C.Voir LG22512.

105.00 148.63 V; V3B; MasVolcanic; Basalt; MassiveRoche volcanique : basalteRoche de couleur vert moyen avec une granulométrie aphanitique à très fine. Elle est généralement massive et contient quelques pillows. Dans l'ensemble, la roche est chloritisée.Elle contient aussi une altération en carbonate, souvent sous forme de grains (<1-3mm), cette altération est plus abondante (5% de CB) entre 116-127m et 134.90-148.6m. Des petits leucoxènes sontaussi présents à certains endroits. Quelques passages sont localement bréchiques et des amygdules remplis de CB semblent présentes à certains endroits?Des traces-1% de PY et quelques traces de CP sont disséminées localement.Environ 3% de veines (1-3cm) et veinules de CB-QZ blanc sont injectés irrégulièrement, souvent en tension et parfois déchirées.Contact diffus et graduel avec l'unité suivante.

148.63 184.12 V; V3A; PwVolcanic; Andesite/Dacite; PillowRoche volcanique felsique : Dacite? ou andésite fortement altéré?Roche de couleur beige moyen avec des passages pâle et foncé. Plusieurs pillows sont présents (10-20cm). Des amygdules sont parfois présentes dans les pillows. La roche est siliceuse et séricitisé. Lespillows sont généralement orientés entre 45-60 degré A/C.Ed Van : Pillows and could also be pyroclastic bombs. Voir LG22514 et 06-50-183.30.Des traces de PY et PO sont disséminées irrégulièrement.Environ 3-5% de veinules de CB-QZ blanc sont injectés irrégulièrement, souvent déchirées.Contact diffus.

184.12 199.55 V; Ta; TBLVolcanic; Tuff /Ash; Tuff Breccia/LapillistoneRoche très déformée. Cette roche est très difficile à identifier.Pyroclastique??Semble une séquence de roche pyroclastique principalement composé de fine-coarse tuff et localement des lapillis. La roche est de couleur gris-vert moyen. La roche semble felsique et de la fuschite estprésente un peu partout à travers.



DESCRIPTION

La roche est très déformée et contient un littage très variable entre 0-45 degré A/C.La texture n'est pas facile à évaluer. Quelques plis sont présents.Environ 5% de veinules et quelques veines (1-10cm) de QZ-CB sont injectées irrégulièrement. Le QZ est parfois gris foncé.Des fines traces des sulfures (PY) sont disséminées irrégulièrement.Contact inférieur à environ 20 degré A/C.Voir 06-50-187.75 et LG22520

199.55 288.10 V; V3A; PwVolcanic; Andesite/Dacite; PillowRoche volcanique felsique : Dacite? ou andésite fortement altéré?Roche de couleur gris-beige moyen avec des passages pâle et foncé. Plusieurs pillows sont présents (10-20cm). Des amygdules (3-6mm) sont parfois présentes dans les pillows. La roche est siliceuse etséricitisé. Elle contient aussi une altération en carbonate, souvent sous forme de petits cristaux, cette altération est plus abondante (10% de CB) entre 231.90-236.05 et 242.30-247.70 et rend l'évaluationde la texture difficile. Parfois la roches est aussi carbonaté pervasivement.À certains endroits : vésicule rempli de CB ou cristaux de CB allotriomorphe?Localement des passages bréchiques sont présents autours des pillows.Les pillows sont généralement orientés entre 40-60 degré A/C.Avec la profondeur, le nombre de pillow semble diminuer.Entre 214.17-217.17 : Dyke beige de leuco-gabbro, altéré et folié? Semble de même compositon que certains fraqments rencontrés dans le conglomérat gris.Des traces de PY et de PO sont disséminées irrégulièrement.Environ 3-5% de veines (1-5cm) et veinules de CB-QZ blanc (parfois gris) sont injectés irrégulièrement, souvent déchirées.Contact inférieur diffus (fin des pillows).

288.10 321.00 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique : DaciteRoche de couleur gris-beige moyen avec une granulométrie aphanitique à très fine. La roche devient plus grisâtre avec la profondeur. Elle est généralement massive, mais semble parfois foliée (50 degréA/C). Dans l'ensemble, la roche est silicifiée et séricitisée. Elle contient aussi une altération en carbonate, localement pervasive et aussi sous forme de cristaux (<=1mm), cette altération estprincipalement présente entre 319-321m. Voir 06-50-314.20 pour cette unité.Des traces-1% de PO sont disséminées irrégulièrement.Environ 5% de veines (1-10cm) et veinules de CB-QZ blanc sont injectés irrégulièrement. Les veines de QZ sont parfois grise. L'échantillon no.22527 contient une veine de QZ blanc et gris dontl'éponte longe parallèlement la carotte.Contact approximatif.

321.00 343.10 SS; S; ARGSandstone; Siltstone; ArgilliteRoche sédimentaire : Sandstone en alternance avec des siltstone et quelques argilites.Séquence sédimentaire interdigitant sandstone fin, siltstone et quelques argilite. Les pourcentage sont difficile à déterminer, couleur et granulométrie semblable.La roche est de couleur gris moyen et contient un litage qui varie entre 45-60 degré A/C. Certains bancs sont massifs et ne contiennent aucun littage.342.50-343.10 : Argilite avec 2-3% de PO et PY.De plus, environ 3% de veines (1-1.5cm) et veinules de QZ et de CB sont injectées irrégulièrement, souvent en tensions.Quelques traces de PY est disséminée irrégulièrement.Contact inférieur à 60 degré A/C.Ed Van : Massive and dark grey dacite.Voir 06-50-333.20

343.10 360.10 V; V3RVolcanic; RhyoliteRoche volcanique : Dacite/Rhyolite?Roche de couleur gris moyen-foncé avec une granulométrie aphanitique à très fine. Elle est généralement massive, mais semble parfois foliée entre 40-60 degré A/C. La texture n'est pas toujours facile àévaluer, semble contenir parfois des pyroclastiques. Dans l'ensemble, la roche est silicifiée. Présence de quelques cristaux de CB, pourrait être parfois des amygdules??Des traces de PY et PO sont disséminées irrégulièrement.Environ 5% de veinules de CB-QZ blanc sont injectés irrégulièrement.Contact très approximatif avec l'unité suivante.

360.10 367.92 CONGLO; SZ



DESCRIPTION

Conglomerate; Silicified ZoneConglomérat fortement silicifié (en contact avec le diabase qui suit)Difficile de préciser de quel conglomérat il s'agit, ainsi que d'en faire l'évaluation.Conglomérat de couleur brun très foncé. La roche est très silicifiée.La matrice est de couleur gris foncé, aphanitique et représente environ 10%.Semble clast-supported (localement matrix-supported) et polymictic felsic (limited).Morphologie : semble sub-arrondi (pas toujours évident à identifier, roche déformée).Puissance des clasts : 0.5-4cm.Origine des clasts? Volcanic felsic?La roche est foliée à 50 degré A/C.Contient des traces-1% de sulfures (PO et PY) disséminés irrégulièrement dans la foliation et matrice.Environ 5% de veinules de QZ-CB, parfois avec du feldspath sont injectés dans la foliation, déchirées et aussi fragmentées. Ces veines sont parfois verdâtre.Contact inférieur net et légèrement irrégulier avec le diabase à environ 20 degré A/C.Ressemble à l'unité silicifié rencontré dans le 06-Q4 et 06-Q5.

367.92 420.33 I5DDiabaseIntrusif de couleur gris moyen à foncé avec quelques passages verdâtre. La granulométrie est généralement fine (parfois plus moyenne), avec des bordures à grains très fins. Le dyke est massif,équigranulaire et magnétique. Quelques veinules (<=1-2mm) de CB, souvent en tension, sont présentes.Des fines traces de PY et PO sont localement disséminées.Contatc inférieur net et irrégulier à environ 10 degré A/C.

420.33 459.00 CONGLOConglomerateConglomérat fortement silicifié (au contact inférieur du diabase)Même conglomérat que celui qui précède.Conglomérat gris?Difficile d'en faire l'évaluation.Conglomérat de couleur gris-brun très foncé. La roche est très silicifiée.La matrice semble de couleur gris foncé, aphanitique et représente environ 10%.Semble clast-supported et polymictic felsic.Morphologie : semble sub-arrondi (pas toujours évident à identifier, roche déformée).Puissance des clasts : 0.5-17cm (localement 50 cm).L'origine des clasts semblent principalement volcanique felsique avec quelques intrusif (gabbro, tonalite grise). Aucun clast mafique ne semblent présent.Entre 446.65-451.05m : diabase? (voir litho.secondaire)La roche est foliée à 50-55 degré A/C. Entre 451.05-453.55, la déformationest plus intense, fragments brisés.Contient des traces-1% de sulfures (PO et PY) disséminés irrégulièrement dans la matrice et parfois dans quelques clasts.Environ 5% de veinules de QZ-CB, parfois avec du feldspath sont injectés dans la foliation, déchirées et aussi fragmentées. Ces veines sont parfois verdâtre.Contact inférieur net à 60 degré A/C.

446.65 451.05 I5DDiabaseDiabase? Voir LG22548Intrusif de couleur gris moyen-foncé avec une très fine granulométrie. Le dyke est massif, non magnétique et contient quelques veinules (<=1-2mm) de CB. Des fines traces de PY sontlocalement disséminées. Localement, quelques minéraux plus grossiers sont présents (feldspath épidotisé?)Contatcs à 15 et 25 degré A/C.

459.00 636.75 SS; ARGSandstone; ArgilliteRoche sédimentaire : Sandstone en alternance avec des argilites.Unité composé de lits (1-300cm) de sandstone (55%) en alternanc avec des lits (0.1-10cm) d'argilites (45%).L'argilite est de couleur gris foncé. Des siltstones sont certainement interdigités à travers les argilite (couleur semblable, difficile à évaluer un poucentage)Le sandstone est de couleur gris moyen-foncé, localement plus pâle, avec une granulométrie très fine, localement grossière (1-2mm). Contient pasfois des fragments d'argilite (allongé et gris foncé).Tout ces lits ont une orientation variant entre 55-65 degré A/C, parfois 70-75 degré A/C.



DESCRIPTION

Localement, ceux-ci sont irréguliers, discontius et déchirée. La distribution des lits de sandstone et d'arglite est hétérogène, donc certains passages sont plus concentrés en sandstone et d'autre en argilite.Entre 1-5% de veinules et quelques veines (1-2cm) de QZ-CB sont distribuées irrégulièrement. Le sansdstone semble contenir plus de veines.Des très fines traces de PY et PO sont disséminées irrégulièrement.Entre 585.30-587.45 : zone de faille (voir structure).Entre 625.50-636.75 : Passage fortement cisaillé (voir structure).Contact inférieur irrégulier et diffus.

585.30 587.45 FaiFaultingZone de faille.Roche très fracturé contenant de la boue de faille à certains endroits.Contact supérieur à 25 degré A/C et contact inférieur approximatif.

625.60 636.75 SheShearingPassage fortement cisaillé.La déformation est très irrégulière. Le littage est parfois parallèle à la carotte et les lits sont souvent plissés et crénulés.La roche est plus pâle, volcanique à travers?

636.75 687.82 V/S?Volcanic/Sédiment?Roche très déformé de couleur gris-beige moyen.Semble des sédiments (argilite/sandstone) interlittés avec des pyroclastiques (fine-coarse tuff et quelques lapilli).La déformation est irrégulière, l'orientation des lits varient entre 0-65 degré A/C. Ceux-ci sont parfois plissés et sont localement fracturés.Dans l'ensemble la roche est silicifiée, séricitisée et parfois carbonaté.À partir de 666.25m, la roche est plus grisâtre (non séricitisé) et semble composée principalement de sédiments. Des petits fragments (<=1mm) anguleux de QZ gris foncé sont présents dans certainspassages.Environ 5% de veinules de QZ(blanc, parfois fumé)-CB sont injectés irrégulièrement et suivent la déformation. Quelques veines (1-15cm) de QZ fumé sont aussi présentes.Quelques fines traces de PY et PO sont disséminés dans la roche et sont aussi associée aux veines et veinules.Contact inférieur diffus.Voir LG22564 et LG22566.

636.75 687.82 SheShearingPassage fortement cisaillé.La déformation est très irrégulière. Le littage est parfois parallèle à la carotte parfois plissés et sont localement fracturés.Semble des sédiments interlittés avec des pyroclastiques.

687.82 942.20 SS; ARGSandstone; ArgilliteRoche sédimentaire : Sandstone en alternance avec des argilites.Unité composé de lits (1-300cm, parfois 3-5m) de sandstone (55%) en alternanc avec des lits (0.1-45cm) d'argilites (45%).L'argilite est de couleur gris foncé. Des siltstones sont certainement interdigités à travers les argilite (couleur semblable, difficile à évaluer un poucentage)Le sandstone est de couleur gris moyen-foncé, localement plus pâle, avec une granulométrie très fine, localement grossière (1-2mm). Contient pasfois des fragments d'argilite (allongé et gris foncé).Tout ces lits ont une orientation variant entre 30-50 degré A/C, parfois 25 degré A/C et 55-60 degré A/C.À certains endroits, ceux-ci sont irréguliers, discontius, déchirée et parfois plissés. La distribution des lits de sandstone et d'arglite est hétérogène, donc certains passages sont plus concentrés ensandstone et d'autre en argilite. Cerains passages semblent plus abondant en siltstone.À partir d'environ 880m, le sandstone est beaucoup moins présent, la roche est composée majoritairement d'argilite et de silstone.Entre 799.80-802.10 : présence de pyroclastique? à travers les sédiments. Présence de fines bandes beiges avec quelques fragments de QZ gris anguleux. Foliation entre 0-50 degré A/C.Entre 1-5% de veinules et quelques veines (1-10cm, parfois fumé) de QZ-CB sont distribuées irrégulièrement.Des très fines traces de PY et PO sont disséminées irrégulièrement.842.35-343m : Envrion 1-2% de PO suivent les lits.Contact inférieur est net à 40 degré A/C.Les passages échantillés sont dans les sandstone.Ed Van : entre 689.87-704.96m, massive tuff mafic volcanic. Voir 06-50-692.90.



DESCRIPTION

, parfois 70-75 degré A/C.sansdstone semble contenir plus de veines.Entre 585.30-587.45 : zone de faille (voir structure).Entre 625.50-636.75 : Passage fortement cisaillé (voir structure).

689.62 689.87 VEI;;;;;;VeinVeine de QZ blanc et fumé à certains endroits. Quelques feldspath sont présents ainsi que quelques CB. La veine est assez massive et ne semble pas contenir de sulfures.Les contacts sont irréguliers à environ 80 et 30 degré A/C.

771.50 771.67 FaiFaulting20°Zone de faille orientée à 20 degré A/C.Faille de deux cm de large contenant de la boue de faille et des fragment.

942.20 994.90 SSSandstoneRoche sédimentaire : sandstoneRoche de couleur gris moyen contentant des fragments principalement de puissance <=2mm. Quelques granules et pebbles sont présents, ceux-ci représentent environ 1-2% de la roche et ont unepuissance variant entre 2-4mm. Cependant, entre 951-965m, ceux-ci semblent plus nombreux (3%) et aussi plus grossiers (2-6mm). Leurs composition est felsique et argilitique (50%-50%). À partitrde 978m, il y a seulement quelques traces de granules et pebbles.Des yeux de QZ bleu sont présent (environ 2-3%, 1-2mm).La roche est assez massive, mais un léger littage semble présent à certains endroits à 45 degré A/C (pas très visible).Environ 3% de veinules et veines sont présentent. Les veines (1-40cm) sont principalement composées de QZ gris, avec quelques traces de PO et PY.Fine trace de PY aussi disséminées dans le sandstone.Contact inférieur diffus, graduel.Les passages contetant plusieurs granules et pebbles sont échantionnés.

994.90 1005.00 SS; CONGLO; C/FSandstone; Conglo; Felsic ClastRoche sédimentaire : sandstone ou conglomérat à support de matrice (de sandstone)?Roche de couleur gris moyen contentant des fragments principalement de puissance <=2mm (sandstone). Environ 5% de fragments ont une puissance qui varie de granule à pebble, plus précisémententre 2-40mm (mais généralement entre 2-5mm). Leur composition est felsique (80%) et argilitique (20%). Les fragments felsiques sont sub-arrondi et aphanitique (origine?). Du chert semble présent.Les fragments d'argilite sont sub-anguleux, souvent allongés et sont aussi souvent plus grossiers. Des yeux de QZ bleu sont présent (environ 5%, 1-2mm). Quelques yeux de QZ sont supérieur à 2mm.La roche est assez massive, mais un léger littage semble présent à certains endroits à 55 degré A/C (pas très bien visible).Environ 1% de veinules sont présentent. Une veine (20cm) est composées de QZ gris, avec quelques traces de PO et PY.Fine trace de PY et PO aussi disséminées dans la roche.Contact inférieur diffus, graduel.

1005.00 1035.82 SSSandstoneRoche sédimentaire : sandstoneRoche de couleur gris moyen contentant des fragments principalement de puissance <=2mm. Quelques granules et pebbles sont présents, ceux-ci représentent environ des traces-1% de la roche et ontune puissance variant entre 2-4mm (localement 10mm).Entre 1011-1017m et 1026.74-1032.15m, ceux-ci semblent plus nombreux (1-2%) et aussi plus grossiers. Leurs composition est felsique (75%) et argilitique (25%).Des yeux de QZ bleu sont présent (environ 2-3%, 1-2mm).La roche est généralement massive et un littage est localement visible à 60 degré A/C.Environ 3% de veinules de QZ-CB sont injectées irrégulièrement.Fine trace de PY aussi disséminées dans le sandstone.Contact inférieur est net à 45 degré A/C.Les passages contetant plus de granules et pebbles ont été échantionnés.

1035.82 1042.45 SS; CONGLO; C/ARGSandstone; Conglo; Argillite ClastsRoche sédimentaire : sandstone ou conglomérat à support de matrice (de sandstone)?Roche de couleur gris moyen contentant des fragments principalement de puissance <=2mm (sandstone). Environ 5-10% de fragments ont une puissance qui varie de granule à pebble, plus précisément



DESCRIPTION

entre 2-50mm (mais généralement entre 2-10mm). Leur composition est argilitique (75%) et felsique (25%). Les fragments d'argilite sont sub-anguleux, souvent allongés et sont aussi souvent plusgrossiers. Les fragments felsiques sont sub-arrondi et aphanitique (origine?). Du chert semble présent.Des yeux de QZ bleu sont présent (environ 3-4%, 1-2mm).La roche contient un littage à certains endroits entre 45-55 degré A/C.Environ 1-2% de veinules de QZ-CB sont présentent.Fine trace de PY et PO sont disséminées.Contact inférieur diffus, graduel.

1042.45 1067.00 SSSandstoneRoche sédimentaire : sandstoneRoche de couleur gris moyen contentant des fragments principalement de puissance <=2mm. Quelques granules et pebbles sont présents, ceux-ci représentent environ 2% de la roche et ont unepuissance variant principalement entre 2-10mm.Cependant, entre 1047-1050.10 et 1053-1056.55m, ceux-ci semblent plus nombreux (2-3%) et aussi plus grossiers (2-50mm). Leurs composition est argilitique (70%, sub-anguleux) et felsique (80%,sub-arrondi).Des yeux de QZ bleu sont présent (environ 1-2%, 1-2mm).La roche est assez massive, mais un léger littage semble présent à certains endroits à 55-60 degré A/C (pas très visible).Environ 2-3% de veinules de QZ-CB sont injectés irrégulièrement.Fine trace de PY aussi disséminées dans le sandstone.Contact inférieur est à 60 degré A/C.Les passages contetant plusieurs granules et pebbles sont échantionnés.

1067.00 1073.05 SS; ARGSandstone; ArgilliteRoche sédimentaire : Sandstone en alternance avec des argilites.Unité composé de lits (1-10cm) de sandstone (50%) en alternanc avec des lits (0.1-2cm) d'argilites (50%).L'argilite est de couleur gris foncé. Des siltstones sont certainement interdigités à travers les argilite (couleur semblable, difficile à évaluer un poucentage)Le sandstone est de couleur gris moyen-foncé avec une granulométrie très fine.Tout ces lits ont une orientation variant entre 50-60 degré A/C.Localement, ceux-ci sont irréguliers, discontius et déchirée.Quelques veinules de QZ-CB sont distribuées irrégulièrement.Contact inférieur à 50 degré A/C.

1073.05 1103.90 SSSandstoneRoche sédimentaire : sandstoneRoche de couleur gris moyen contentant des fragments principalement de puissance <=2mm. Quelques granules et pebbles sont présents, ceux-ci représentent environ des traces-1% de la roche et ontune puissance variant principalement entre 2-10mm, localement 10-30mm.Quelques yeux de QZ bleu sont présent.La roche est assez massive, mais contient très localement un littage à 55 degré A/C (pas très visible).Environ 2-3% de veinules de QZ-CB et quelques veines (1-2cm) sont injectés irrégulièrement.Fine trace de PY aussi disséminées dans le sandstone.À partir de 1100.45m, le sandstone est gris pâle.Contact inférieur diffus.

1103.90 1166.33 SS; CONGLO; ARGSandstone; Conglo; ArgilliteRoche sédimentaire : Sandstone contenant des passages pebbly-granule conglomerate avec aussi des lits d'argilite.Sandstone : Roche de couleur gris moyen contentant des fragments principalement de puissance <=2mm. Elle représente environ 75% de la roche. Quelques granules et pebbles sont présents, ceux-cireprésentent environ 2% de la roche et ont une puissance moyenne variant entre 2-15mm.Leurs composition est argilitique (50%, sub-anguleux) et felsique (50%, sub-arrondi).Quelques yeux de QZ bleu sont présent. La roche est assez massive, mais contient très localement un littage à 40 degré A/C (pas très visible).Pebbly-granule conglomerate (à support de matrice de sandstone, 85%) : Semble la même composition que le sandstone, mais les granules-pebbles (15%) sont majoritairement felsiques.Représente environ 10% de la roche et se situe principalement dans les premiers mètres de l'unité.



DESCRIPTION

Argilite : lit d'argilite représentant environ 15% de la roche. Semble interlitté avec des siltstone. Lits orientés à 45-55 degré A/C. Les lits sont parfois brisés (donne l'impression d'être des gros fragmentsd'argilite).Environ 3% de veinules de QZ-CB et quelques veines (1-2cm) de QZ fumé sont injectés irrégulièrement.Quelques traces de Fine trace de PY aussi disséminées.Contact inférieur irrégulier (veine au contact).

1166.33 1183.30 SSSandstoneRoche sédimentaire? : sandstone? Voir LG22611Roche de couleur brun qui semble un sandstone altéré (séricitisé?). Les fragments ont une puissance de <=2mm.Quelques yeux de QZ bleu sont présent.La roche est assez massive, mais les fragments sont orientés localement à 60 degré A/C.Environ 3% de veinules de QZ-CB et quelques veines (1-2cm) de QZ fumé sont injectés irrégulièrement.Fine trace de PY aussi disséminées.Contact inférieur diffus (Qz fumé injecté).

1183.30 1194.00 V/S?Volcanic/Sédiment?Siltstone? / fine tuff? Voir 06-50-1188Roche de couleur gris moyen avec une granulométrie très fine.Un littage est présent et est orienté entre 60-70 degré A/C. Les lits sont déchirés et parfois fragmentés.Environ 2% de veinules de QZ-CB et quelques veines (1-5cm) de QZ fumé sont injectés irrégulièrement.Fine trace de PY aussi disséminées dans le sandstone.Contact inférieur diffus.

1194.00 1237.80 ARG; SArgillite; SiltstoneRoche sédimentaire : Argilite en alternance avec des silstoneRoche de couleur gris foncé avec une très très fine granulométrie. Il est difficile d'évaluer un pourcentage pour l'argilite vs silstone, puisque les couleurs et granulométrie sont très similaires.Le littage varie entre 20-40 degré A/C et est localement parallèle. Les lits sont pas toujours très bien visibles.Entre 1-5% de veinules et quelques veines (1-2cm) de QZ-CB sont distribuées irrégulièrement.Des très fines traces de PY et PO sont disséminées irrégulièrement.EOH




DDH : CHAB 06-58Claims title : SSM 21166Township : ChabanelRange :Lot :

Section : 5325300Level :Work place : Leadbetter Extension

Drilled by : Benoit From : 2006-05-26 To : 2006-06-07Described by : Bernard-Olivier Martel Description date : 2006-06-08

Collar

Core size : NQ Cemented : No Stored : Yes

Remarks

Azimuth : 198.00°Plunge : -87.00°Length : 333.00 m



672100.0005325297.000344.000

Down hole surveyType Depth Azimuth Plunge Invalid

Flex-Dip 12.00 m -86.75° NoFlex-Dip 18.00 m -86.35° NoFlex-Dip 21.00 m -87.09° NoFlex-Dip 24.00 m -86.64° NoFlex-Dip 27.00 m -86.32° NoFlex-it 30.00 m 199.79° -86.13° NoFlex-it 33.00 m 204.14° -86.37° NoFlex-it 36.00 m 195.40° -85.64° NoFlex-it 39.00 m 205.06° -86.04° NoFlex-it 42.00 m 204.32° -86.17° NoFlex-it 45.00 m 190.54° -85.97° NoFlex-it 48.00 m 193.65° -86.04° NoFlex-it 51.00 m 204.23° -85.28° NoFlex-it 54.00 m 193.32° -84.91° NoFlex-it 57.00 m 203.69° -85.09° NoFlex-it 60.00 m 200.64° -85.45° No

Type Depth Azimuth Plunge Invalid

Flex-it 63.00 m 202.10° -85.29° NoFlex-it 66.00 m 197.74° -85.28° NoFlex-it 69.00 m 202.35° -84.60° NoFlex-it 72.00 m 198.97° -85.05° NoFlex-it 75.00 m 202.25° -84.52° NoFlex-it 78.00 m 202.78° -84.34° NoFlex-it 81.00 m 195.19° -84.03° NoFlex-it 84.00 m 190.29° -84.43° NoFlex-it 87.00 m 193.44° -84.63° NoFlex-it 90.00 m 194.75° -84.52° NoFlex-it 93.00 m 195.43° -84.39° NoFlex-it 96.00 m 200.25° -83.85° NoFlex-it 99.00 m 196.75° -83.50° NoFlex-it 102.00 m 193.34° -83.24° NoFlex-it 105.00 m 190.51° -83.10° NoFlex-it 108.00 m 189.40° -82.95° No



Type Depth Azimuth Plunge InvalidFlex-it 111.00 m 190.78° -83.73° NoFlex-it 114.00 m 193.48° -83.67° NoFlex-it 117.00 m 192.98° -83.58° NoFlex-it 120.00 m 195.13° -83.43° NoFlex-it 123.00 m 194.49° -83.43° NoFlex-it 126.00 m 195.55° -83.26° NoFlex-it 129.00 m 197.19° -82.94° NoFlex-it 132.00 m 194.20° -82.13° NoFlex-it 135.00 m 196.42° -82.15° NoFlex-it 138.00 m 192.31° -81.87° NoFlex-it 141.00 m 195.27° -82.44° NoFlex-it 144.00 m 193.79° -82.45° NoFlex-it 147.00 m 195.87° -82.35° NoFlex-it 150.00 m 193.35° -82.39° NoFlex-it 153.00 m 197.02° -81.64° NoFlex-it 156.00 m 195.62° -81.81° NoFlex-it 159.00 m 197.69° -81.77° NoFlex-it 162.00 m 195.10° -82.06° NoFlex-it 165.00 m 196.59° -81.87° NoFlex-it 168.00 m 197.74° -81.56° NoFlex-it 171.00 m 192.32° -80.92° NoFlex-it 174.00 m 189.84° -81.71° NoFlex-it 177.00 m 190.99° -81.70° NoFlex-it 180.00 m 195.91° -80.94° NoFlex-it 183.00 m 196.10° -80.85° NoFlex-it 186.00 m 194.93° -80.68° NoFlex-it 189.00 m 196.24° -80.96° NoFlex-it 192.00 m 194.53° -80.62° NoFlex-it 195.00 m 195.05° -80.37° NoFlex-it 198.00 m 195.01° -80.27° NoFlex-it 201.00 m 196.63° -80.34° NoFlex-it 204.00 m 195.20° -80.11° NoFlex-it 207.00 m 194.44° -79.80° NoFlex-it 210.00 m 192.61° -79.70° NoFlex-it 213.00 m 190.59° -79.54° NoFlex-it 216.00 m 189.00° -79.51° NoFlex-it 219.00 m 188.90° -79.29° NoFlex-it 222.00 m 190.04° -79.16° NoFlex-it 225.00 m 188.44° -79.31° NoFlex-it 228.00 m 187.53° -79.02° NoFlex-it 231.00 m 189.61° -78.81° NoFlex-it 234.00 m 192.06° -78.71° NoFlex-it 237.00 m 188.97° -78.79° NoFlex-it 240.00 m 189.77° -78.99° NoFlex-it 243.00 m 190.72° -78.90° NoFlex-it 246.00 m 189.24° -78.49° NoFlex-it 249.00 m 192.70° -78.08° NoFlex-it 252.00 m 196.42° -78.03° NoFlex-it 255.00 m 190.96° -77.81° NoFlex-it 258.00 m 190.99° -77.56° No

Type Depth Azimuth Plunge InvalidFlex-it 261.00 m 190.94° -77.43° NoFlex-it 264.00 m 189.48° -77.53° NoFlex-it 267.00 m 192.45° -77.18° NoFlex-it 270.00 m 191.67° -77.06° NoFlex-it 273.00 m 192.82° -77.01° NoFlex-it 276.00 m 192.65° -76.93° NoFlex-it 279.00 m 193.39° -76.83° NoFlex-it 282.00 m 192.80° -76.71° NoFlex-it 285.00 m 190.27° -76.69° NoFlex-it 288.00 m 191.09° -76.51° NoFlex-it 291.00 m 190.68° -76.58° NoFlex-it 294.00 m 190.62° -76.48° NoFlex-it 297.00 m 190.33° -76.62° NoFlex-it 300.00 m 191.06° -76.41° NoFlex-it 303.00 m 190.91° -76.49° NoFlex-it 306.00 m 191.09° -76.22° NoFlex-it 309.00 m 191.00° -76.27° NoFlex-it 312.00 m 191.77° -76.50° NoFlex-it 315.00 m 193.63° -76.51° NoFlex-it 318.00 m 194.22° -76.37° NoFlex-it 321.00 m 194.24° -76.27° NoFlex-it 324.00 m 193.23° -76.24° NoFlex-it 327.00 m 194.25° -76.17° NoFlex-it 330.00 m 193.25° -75.52° No



DESCRIPTION

0.00 25.00 OBOverburdenOverburden.

25.00 75.05 CONGLO; SS; Po; GBConglo; SS; Polymictic; Graded BeddingRoche fragmentaire : épiclastite rhyolitique?Passages grossiers de "pebble to granule conglomerate polymictic and clast to matrix-supported", pluri-métrique à décimétrique alternant avec passage plus fin, à "granule sandstone"et depluri-décimétrique à décimétrique.Passage conglomératique corresponds à 60% de l'intervallePassage plus fin à "granule sandstone" corresponds à 40% de l'intervalle.Les contacts entre les passages sont parfois net et parfois graduel.Matrice est de couleur grise avec teinte jaunâtre, peu présente (20-30%), de grain très fin à fin (1/16 mm à 2 mm), composée de fp-qz et séricite. Ne semble pas avoir de chlorite.Les fragments sont sub-anguleux à sub-arrondis, souvent étirés, de couleur gris pâle, gris moyen et souvent avec teinte jaunâtre. Donc l'origine des fragments est probablement volcanique felsiquerhyolitique (tuff-Qz-Eyes et massif à cristaux porphyrique de Qz) et d'origine sédimentaire (sandstone et argillite).Foliation est visible, discontinue , en bandes et en environs 45-55 degrés.J'observe ce qui me semble être des granuloclassements normales et inverses.Le réseau de veinule de Qz-Cb est présent (2-4%).Contact inf approximatif: fin de la présence de granule.

75.05 130.62 ARG; SS; STARG; SS; Stratified/LaminatedRoche sédimentaire : Argillite en alternance avec sandstone.Alternance de bandes (0.1-10cm) d'argillite (70%) avec environ 30% de bandes (1-50cm) de sandstone.L'argillite est de couleur gris très foncée à noir avec une granulométrie aphanitique et généralement en bandes minces et parfois en bandes larges.Le sandstone est de couleur gris moyen avec une fine granulométrie (2mm max), les lits sont massifs et parfoist littés. Certaines bandes semblent être composées de siltstone (grains très fins de couleurgris foncé).Le littage général de ces lithologies varie entre 35-45 degré A/C.Certains secteurs contiennent des lits très irréguliers. Ceux-ci sont plissés, éttirés et déchirés.Environ 2-3% de veinules de QZ-CB (1-10mm) sont injectées irrégulièrement, elles sont parfois déchirées et ptygmatiques. Quelques fines traces de PY sont disséminés.Le contact inférieur est net à 50 degrés.

130.62 150.53 SSSSSéquence sédimentaire composée principalement de sandstone en alternance avec des bandes décimétrique de conglomérat.Le conglomérat (granules-pebble) corresponds à 20% de l'intervalle, tandis que le sandstone représente environ 80%. Les contacts entre ces deux unités sont assez nets, mais parfois graduels.Le conglomérat (granules-pebbles) est à matrix-supported et est polymictic. La matrice est de couleur gris moyen à localement beige et est à grains très fins. Les clats sont principalement felsique decouleur variables : brun-beige et gris (pâle, moyen à foncé). Donc l'origine des fragments est probablement volcanique felsique et sédimentaire. Les fragments gris foncé, possiblement argillite, sontallongé et sub-anguleux. La morphologie des fragments est généralement sub-arrondis et leurs puissances varient généralement entre 2 et 15mm, parfois 20mm. Une foliation varie entre 45 et 60 degréA/C (pourrait aussi être un littage, puisque les clast ne semble pas toujours déformés et éttirés). Certains passages semblent être clast-supported.Le sandstone est de couleur gris moyen et contient une granulométrie variable (très fine à 4mm). Les lits qui contient plusieurs grains plus grossiers (granule sandstone). Le sandstone semble avoir lamême composition que le conglomérat (mais avec une granulométrie plus petite). De plus, des petits lits discontinue d'argilite sont aussi présents. Un littage à 35-40 degré A/C est présent (ou foliation,puisque certains grains semblent éttirés).Environ 1-2% de veinule de Qz-Cb sont présentes en structure en tension et suivent parfois la foliation et les lits.Le contact inférieur est net à 45 degrés.

150.53 271.60 ARG; SS; STARG; SS; Stratified/LaminatedRoche sédimentaire : Argillite en alternance avec sandstone.Alternance de bandes (0.1-10cm) d'argillite (80%) avec environ 20% de bandes (1-50cm) de sandstone.L'argillite est de couleur gris très foncée à noir avec une granulométrie aphanitique et généralement en bandes minces et parfois en bandes larges.Le sandstone est de couleur gris moyen avec une fine granulométrie (2mm max), les lits sont massifs et parfoist littés. Certaines bandes semblent être composées de siltstone (grains très fins de couleurgris foncé).Le littage général de ces lithologies varie entre 35-45 degré A/C.



DESCRIPTION

Certains secteurs contiennent des lits très irréguliers. Ceux-ci sont plissés, éttirés et déchirés.Environ 2-3% de veinules de QZ-CB (1-10mm) sont injectées irrégulièrement, elles sont parfois déchirées et ptygmatiques. Quelques fines traces de PY sont disséminés.LLe contact inférieur est légèrement approximatif (graduel avec volcanique) à 55 degré A/C.

271.60 297.00 V; V3A; TaVolcanic; Andesite/Dacite; Tuff /AshRoche possiblement volcanique (pyroclastique)? ou sédimentaire?Difficile à dire, déformé. Foliation ou littage??Roche de couleur gris moyen généralement felsique. La granulométrie est aphanitique à fine. La roche possède une foliation (ou littage?) qui varie entre 40-50 degré A/C.Certains secteurs (première moitié) semblent pyroclastic (fine and coarse tuff). Il y a présence de petite bande beige irrégulière (séricitisée).Le contact inférieur approximatif (de gris à vert moyen)

297.00 333.00 V; V3B; MasVolcanic; Basalt; MassiveRoche volcnique: Bsalt?De couleur vert moyen, à grain fin et mésocrate. Aspect massif.Foliation peu visible, discontinue et à environs 50 degrés.Au début de l'intervalle, j'observe des cubes de pyrite-pyrrhotite demi-centimétrique (1%) proche du contact avec le tuff.EOH.

303.00 318.75 SheShearing45°

Zone déformée. Riche en lamines de séricite et en veinesde Qz transposée et boudinées.

333.00 DDH endNumber of samples : 0Number of samples QAQC : 0Total sampled length : 0.00





Drilled by : Forage Benoît From : 2006-06-11 To : 2006-06-13Described by : Bernard-Olivier Martel Description date : 2006-06-15

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Remarks




672198.0005325401.000331.000


Flex-Dip 12.00 m -86.40° NoFlex-Dip 15.00 m -86.02° NoFlex-it 18.00 m 205.56° -86.43° NoFlex-it 21.00 m 205.59° -86.27° NoFlex-it 24.00 m 205.75° -86.13° NoFlex-it 27.00 m 204.54° -86.42° NoFlex-it 30.00 m 203.58° -86.24° NoFlex-it 33.00 m 204.08° -86.40° NoFlex-it 36.00 m 202.28° -86.22° NoFlex-it 39.00 m 202.35° -86.17° NoFlex-it 42.00 m 202.90° -86.29° NoFlex-it 45.00 m 205.17° -86.28° NoFlex-it 48.00 m 208.19° -86.15° NoFlex-it 51.00 m 207.94° -85.75° NoFlex-it 54.00 m 206.82° -85.73° NoFlex-it 57.00 m 203.16° -85.63° No






Type Depth Azimuth Plunge InvalidFlex-it 258.00 m 188.24° -80.23° NoFlex-it 261.00 m 187.86° -80.30° NoFlex-it 264.00 m 186.39° -80.23° NoFlex-it 267.00 m 187.55° -79.76° NoFlex-it 270.00 m 187.12° -79.94° NoFlex-it 273.00 m 186.02° -79.30° NoFlex-it 276.00 m 186.65° -79.26° NoFlex-it 279.00 m 186.83° -79.33° NoFlex-it 282.00 m 186.90° -79.07° NoFlex-it 285.00 m 186.56° -79.11° NoFlex-it 288.00 m 186.74° -79.09° NoFlex-it 291.00 m 184.60° -79.22° NoFlex-it 294.00 m 186.75° -78.98° NoFlex-it 297.00 m 183.32° -78.94° NoFlex-it 300.00 m 185.63° -78.71° No



DESCRIPTION


13.00 59.40 ARG; SS; STARG; SS; Stratified/LaminatedRoche sédimentaire : Argillite en alternance avec sandstone.Alternance de bandes (0.1-10cm) d'argillite (70%) avec environ 30% de bandes (1-50cm) de sandstone.L'argillite est de couleur gris très foncée à noir avec une granulométrie aphanitique et généralement en bandes minces ondulantes et parfois en bandes larges.Le sandstone est de couleur gris moyen avec une fine granulométrie (2mm max), les lits sont massifs et générallement très irréguliers. Ceux-ci sont plissés, éttirés et déchirés. Certaines bandes semblentêtre composées de siltstone (grains très fins de couleur gris foncé).Le littage général de ces lithologies varie entre 10 et 45 degré A/C.Environ 2-3% de veinules de QZ-CB (1-10mm) sont injectées irrégulièrement, elles sont parfois déchirées et ptygmatiques. Quelques fines traces de PY sont disséminés.Le contact inférieur approximatif (fortement fracturé)

59.40 78.80 SS; CONGLOSS; CongloRoche fragmentaire : épiclastite rhyolitique?Passages grossiers de "pebble to granule conglomerate polymictic and clast to matrix-supported", pluri-décimétrique à décimétrique alternant avec passage plus fin, à "granule sandstone"et depluri-métrique à décimétrique.Passage conglomératique corresponds à 40% de l'intervallePassage plus fin à "granule sandstone" corresponds à 60% de l'intervalle.Les contacts entre les passages sont parfois net et parfois graduel.Matrice est de couleur grise, peu présente (20-30%), de grain très fin à fin (1/16 mm à 2 mm), composée de fp-qz et séricite. Ne semble pas avoir de chlorite.Les fragments sont sub-anguleux à sub-arrondis, souvent étirés, de couleur gris pâle, gris moyen et souvent avec teinte jaunâtre. Donc l'origine des fragments est probablement volcanique felsiquerhyolitique (tuff-Qz-Eyes et massif à cristaux porphyrique de Qz) et d'origine sédimentaire (sandstone et argillite).Foliation est visible, discontinue , en bandes et en environs 45-55 degrés.J'observe ce qui me semble être des granuloclassements normales et inverses.Le réseau de veinule de Qz-Cb est présent (2-4%).Contact inf approximatif: fortement fracturé

78.80 303.00 ARG; SS; STARG; SS; Stratified/LaminatedRoche sédimentaire : Argillite en alternance avec sandstone.Alternance de bandes (0.1-10cm) d'argillite (70%) avec environ 30% de bandes (1-50cm) de sandstone.L'argillite est de couleur gris très foncée à noir avec une granulométrie aphanitique et généralement en bandes minces ondulantes et parfois en bandes irréguliaire et en bandes larges.Le sandstone est de couleur gris moyen avec une fine granulométrie (2mm max), les lits sont massifs et générallement très irréguliers. Ceux-ci sont plissés, étirés et déchirés.Certaines bandes semblent être composées de siltstone (grains très fins de couleur gris foncé).Le littage général de ces lithologies varie entre 10 et 65 degré A/C.S0=+ou- 45-60 degrés et S1= 30 degrés donc crénulation.Environ 4-5% de veinules de QZ-CB (1-10mm) sont injectées irrégulièrement, elles sont parfois déchirées et ptygmatiques. Quelques fines traces de PY sont disséminés.EOH





Section : 5325500Level :Work place : Leadbetter extension

Drilled by : Forage Benoît From : 2006-07-13 To : 2006-06-15Described by : Bernard-Olivier Martel Description date : 2006-06-20

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Remarks




672313.0005325488.000336.000








Type Depth Azimuth Plunge InvalidFlex-it 258.00 m 148.45° -81.68° NoFlex-it 261.00 m 150.14° -81.79° NoFlex-it 264.00 m 149.80° -81.77° NoFlex-it 267.00 m 150.47° -82.01° NoFlex-it 270.00 m 147.69° -81.47° NoFlex-it 273.00 m 150.34° -81.84° NoFlex-it 276.00 m 148.32° -81.41° NoFlex-it 279.00 m 148.41° -81.43° NoFlex-it 282.00 m 148.40° -81.15° NoFlex-it 285.00 m 148.57° -81.25° NoFlex-it 288.00 m 148.74° -81.17° NoFlex-it 291.00 m 148.35° -81.37° NoFlex-it 294.00 m 150.10° -81.63° NoFlex-it 297.00 m 151.79° -81.70° NoFlex-it 300.00 m 149.07° -81.52° NoFlex-it 303.00 m 150.44° -81.62° NoFlex-it 306.00 m 153.25° -81.79° No



DESCRIPTION


2.00 157.67 ARG; SS; STARG; SS; Stratified/LaminatedRoche sédimentaire : Argillite en alternance avec sandstone.Alternance de bandes (0.1-20cm) d'argillite (70%) avec environ 30% de bandes (1-30cm) de sandstone.L'argillite est de couleur gris très foncée à noir avec une granulométrie aphanitique et généralement en bandes minces ondulantes et parfois en bandes irréguliaire et en bandes larges.Le sandstone est de couleur gris moyen avec une fine granulométrie (2mm max), les lits sont massifs et générallement très irréguliers. Ceux-ci sont plissés, étirés et déchirés.Certaines bandes semblent être composées de siltstone (grains très fins de couleur gris foncé).Le littage général de ces lithologies varie entre 35 et 80 degré A/C et localement, par sections, sub-parallèle à l'axe de la carotte.Environ 4-5% de veinules de QZ-CB (1-10mm) sont injectées irrégulièrement, elles sont parfois déchirées et ptygmatiques. Quelques fines traces de PY sont disséminés.Contact inférieur net à 50 degrés

21.40 26.80 S2SSandstone

Zone pauvre en bandes d'argillite. Présence de veines de quartz en fumé avec lamines de sécirite.42.80 50.70 S2S

SandstoneZone pauvre en bandes d'argillite. Présence de veines de quartz en fumé avec lamines de sécirite.

152.40 157.67 S2SSandstone

Zone pauvre en bandes pélitique et avec présence de granule.157.67 251.50 V; V3A; Py

Volcanic; Andesite/Dacite; PyroclasticRoche fragmentaire volcanique "pyroclastique" (mixte de passages fin à tuff avec passages grossier à lapillistone)Roche de couleur gris moyen avec teinte jaune généralement felsique. La granulométrie est aphanitique à fine. Présence de bordure noirâtre, de zones centimétrique brèchique (espase entre deux lapillisou fragments) donc pillow breccia ou pyroclastique roche.Le milieu de l'unitée (de 183.37 à 193.93m) est à granulométrie plus fine, de couleur gris moyen, avec absence de lapillis et présence de graphite.Il y aussi présence et cela à plusieur endroit des zones avec de petite bande millimétrique beige irrégulière (séricitisée).Environ 2% de veinules de QZ-CB (1-10mm) sont injectées irrégulièrement, elles sont parfois déchirées et ptygmatiques. Quelques traces de pyrite et pyrrhotite sont disséminés.Contact inférieur graduel.

251.50 309.00 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique massive. Andésite ou basalte?De couleur vert gris moyen. Leucocrate. De grain aphanitique à moyen. Aspect massif.De 276 m à 282 m. présence de ce qui semble être des bordure de pillow mais incertain.EOH

251.50 305.95 V; V3A; MasVolcanic; Andesite/Dacite; Massive

Volcanique massive de grain aphanitique à fin.305.95 309.00 V; V3A; Mas

Volcanic; Andesite/Dacite; MassiveVolcanique massive à grian moyen.

305.95 309.00 Leuleucoxene

Roche avec pigmentation beige jaune (1%) donc altération à leucoxene.



DESCRIPTION






Drilled by : Forage Benoît From : 2006-06-15 To : 2006-06-18Described by : Laura Mancini Description date : 2006-06-22

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Remarks




672398.0005325404.000340.000








Type Depth Azimuth Plunge InvalidFlex-it 258.00 m 97.61° -79.74° NoFlex-it 261.00 m 96.51° -79.73° NoFlex-it 264.00 m 96.26° -79.70° NoFlex-it 267.00 m 97.39° -80.06° NoFlex-it 270.00 m 96.45° -79.44° NoFlex-it 273.00 m 95.61° -79.48° NoFlex-it 276.00 m 96.03° -79.35° NoFlex-it 279.00 m 97.17° -79.73° NoFlex-it 282.00 m 96.75° -79.34° NoFlex-it 285.00 m 97.85° -79.65° NoFlex-it 288.00 m 97.24° -79.29° NoFlex-it 291.00 m 96.26° -79.16° NoFlex-it 294.00 m 97.15° -79.03° NoFlex-it 297.00 m 96.45° -79.00° NoFlex-it 300.00 m 96.78° -78.97° NoFlex-it 303.00 m 97.98° -78.99° NoFlex-it 306.00 m 97.16° -78.60° NoFlex-it 309.00 m 96.56° -78.69° No



DESCRIPTION


2.44 86.73 V; V3AVolcanic; Andesite/DaciteThe rock is a mainly green andesite that grades back and forth into a greenish-grey, then grey dacite. The rock is very deformed by vein emplacement making it very difficult to tell if the rock is massive,has pillows, etc. There are areas where foliations can be seen at ~55º TCA.The unit has an argillite section from 42.09 m - 44.22 m. Both contacts are approximate, the changes from one rock type to the other are gradual. There are a couple of much coarser-grained sections,with pyroxene and feldspar crystals, from ~60.30 m - ~62.15 m and 73.16 m - 77.80 m. These sections could be intrusive rock or a xenolith or possibly just an area of slower cooling. Thin sections(06-63-60 and 06-63-77), were taken to determine composition and identity. The core is broken-up at both ends of the 60.30 m - 62.15 m section making it difficult to see any real contact. The secondsection grades back and forth from coarse to fine-grained. From ~83.50 m - 86.73 m the rock grades into a beigish-brown.The rock contains ~25% quartz-feldspar-carbonate veins. Most of the veins are deformed and have sigmoidal and ptygmatic forms. There are a few veins that are sub-parallel TCA. There is a large areafrom ~21.00 m - 26.50 m that has been brecciated by vein emplacement.There is a little bit of disseminated pyrite throughout the unit.The contact at 86.73 m is approximate. The rock grades into beigish-brown then into grey.

42.09 44.22 S4AArgillite

Argillite layer in andesite/dacite unit.60.30 62.15 V; V3A

Volcanic; Andesite/Dacitecoarse-grained section, with pyroxene and feldspar crystals within the finer-grained andesite/dacite unit, from ~60.30 m - ~62.15 m. This section could be an intrusive rock or a xenolith orpossibly just an area of slower cooling.

73.16 77.80 V; V3AVolcanic; Andesite/Dacite

The section grades back and forth from coarse to fine-grained within the fine-grained andesite unit.86.73 101.50 V; V3A

Volcanic; Andesite/DaciteThe rock is a fine-grained grey dacite. There are so many quartz-carbonate veins deforming the rock, it is difficult to tell if the rock is massive, pillowed, foliated, etc. From 96.00 m - 98.60 m there arewhat may be sericite alterations (or possibly ash layers), associated with the quartz-carbonate veins. There is a bit of disseminated pyrite throughout the section.There is ~20% quartz-carbonate veins (mm - cm), and tiny little spider veins. The veins are deformed and have sigmoidal and ptygmatic forms. There are a few veins that are sub-parallel TCA.The contact at 101.50 m is irregular and at ~20º TCA. The rock is fractured along the contact.

101.50 164.33 ARG; SSARG; SSThe rock is a fine-grained dark-grey to black graphitic argillite with ~25% medium to coarse-grained sandstone. The argillite layers range from 50 cm to several meters and the sandstone layers rangefrom 16 cm to several meters in length. The contacts between the two layers are irregular and at55º TCA. There is a lot of graphite throughout the argillite. There is what appears to be a fine-grained greyish-green volcanic (andesite?), section from 129.68 m - 132.95 m and a volcanoclastic sectionfrom 139.67 m - 140.50 m. Thin sections were taken (06-63-129 and 06-63-140), to determine compositions and identities. There is disseminated and piles of pyrite throughout the unit.The rock contains ~10% quartz veins (mm - cm), some with feldspar and most with carbonate alterations. Several of the veins are deformed with sigmoidal and ptygmatic forms. There are a lot of pilesof pyrite associated with the veins.The contact at 164.33 m is approximate. There is some veining at this point obscuring the actual contact.

129.68 132.95 V; V3AVolcanic; Andesite/Dacite

Andesite/dacite section within the graphitic argillite unit139.67 140.50 V2T

Volcaniclasticvolcanoclastic section in graphitic argillite unit.

164.33 175.80 CONGLO; SSConglo; SSThe rock is a grey colored polymictic (limited), conglomerate-sandstone. The rock is medium-supported (has areas that are clast-supported or matrix-supported)The clasts appear to be 100% felsic and range in shape from angular to sub-rounded (the majority of the clasts are angular to sub-angular). The clasts sizes range from 1mm - 3 cm. There are



DESCRIPTION

fine-grained light grey, medium grey and pinkish-grey clasts that could be a volcanic tuff. There are some very fine-grained black clasts that could be argillite. Some of the clasts appear stretched andimbricated at ~45º TCA. There is a lot of pyrite associated with clast boundaries.The matrix is fine-grained grey with disseminated and piles of pyrite throughout. There are sections that appear to be argillite (very fine-grained and black colored). There are hints of foliationsthroughout the matrix at ~50º TCA. There is a lot of carbonate in the matrix in the sections containing the clasts.The rock contains <1% quartz veins (mm - cm), most are deformed with carbonate alterations and a sigmoidal or ptygmatic form. There are a lot of piles of pyrite associated with the veins.The contact at 175.80 m is approximate. The rock grades into the argillite but there are no obvious clasts after this point.


Conglomerate medium-supported (some areas are clast-supported and some are matrix-supported)175.80 243.39 ARG; SS

ARG; SSThe rock is a fine-grained grey to black graphitic argillite with ~20% medium-grained sandstone. The argillite layers range from 1 mm to several meters and the sandstone layers range from 2 cm toseveral meters in length. The contacts between the two layers are either gradational or irregular and at 50º TCA. There is a lot of graphite throughout the argillite. There is what appears to be afine-grained greenish volcanic (tuff/ash?), mixed with the argillite from ~235.20 m - 238.20 m. A thin section (06-63-235), was taken to determine composition and identity. There is disseminated andpiles of pyrite throughout the unit. Some areas appear to have rip-up fragments of argillite in sandstone as seen from 188.5 m - 189.00 m.The rock contains ~2% quartz veins (mm - cm), and tiny spider veins. Some of the veins have feldspar and most have carbonate alterations. The majority of the veins are deformed with sigmoidal andptygmatic forms. Some of the veins are sub-parallel TCA. There are a lot of piles of pyrite associated with the veins. From 176.20 m - 177.60 m and 219.7 m - 220.70 m the rock is very brecciated byvein emplacement.The contact at 243.39 m is approximate. The rock grades from argillite to volcanic.

235.20 238.20 Ta; S4ATuff /Ash; Argillite

Tuff/ash mixed with argillite within graphitic argillite unit.243.39 250.14 V; V3A

Volcanic; Andesite/DaciteThe rock is a fine-grained grey colored volcanic (dacite?). There are a lot of carbonate alterations with euhedral to subhedral crystals along with sericite alterations from 245.60 m - 247.00 m. Foliationsor bedding layers are seen throughout the section at 40º TCA. There is a small amount of disseminated pyrite throughout the section.The rock contains ~10% quartz veins (mm - cm), most are deformed with carbonate alterations. The veins have sigmoidal and ptygmatic forms and a couple around 248.50 m, appear to have smokeyquartz.The contact at 250.14 m is approximate. The rock grades from volcanic to argillite.

250.14 256.17 ARG; S3SARG; SiltstoneThe rock is a fine-grained grey colored siltstone with a small amount of argillite (~3%). The rock has foliations at 60º TCA. No disseminated pyrite was found.There is ~1% quartz veins (mm - cm), and tiny little spider veins, with sigmoidal form, throughout the section. Some of the veins have a little bit of carbonate alterations. Some of the veins appear tocontain smokey quartz.The contact at 256.17 is approximate. The rock is broken at this point and there are a lot of alterations making it difficult to see an actual contact.

256.17 260.32 V; V3AVolcanic; Andesite/DaciteThe rock is a fine-grained grey volcanic (dacite?). The rock is highly altered with sericite and carbonate alterations making it very difficult to identify the rock. There is a small amount of disseminatedpyrite seen in the less altered areas. There is a hint of foliations around 258.00 m at 40º TCA.There is ~1% quartz veins (mm - cm), with some carbonate alterations. A few of the veins have sericite alterations and some piles of pyrite associated with them.The contact at 260.32 m is approximate. The rock has alterations at this point which may be obscuring the contact but the volcanic rock looks like it grades into sedimentary.

260.32 271.94 SS; ARGSS; ARGThe rock is a coarse to fine-grained grey to dark-grey sandstone-argillite. The rock is composed of ~73% sandstone 24% argillite and 3% quartz veins. Some of the contacts between layers aregradational and most are irregular and at ~45º TCA.The coarse-grained sections have what appear to be quartz pebbles, argillite fragments, piles of pyrite and some sericite and carbonate alterations. The fine-grained sections are mostly argillite, possiblywith a small amount of siltstone.The quartz veins are mm -cm in size and are deformed with sigmoidal and ptygmatic forms. Most of the veins have carbonate alterations and a lot of the veins have pyrite associated with them(particullarly in the argillite).The contact at 271.94 m is approximate. The rock is broken at this point and there are missing pieces.



DESCRIPTION

271.94 273.52 V; V3A; PyVolcanic; Andesite/Dacite; PyroclasticThe rock appears to be a fine-grained grey volcanic (dacite?). From 271.94 m - 272.70 m the rock has what appears to be tiny fragments indicating it could be pyroclastic, also it is highly altered,possibly with sericite, carbonate and chlorite. From 273.00 m - 273.52 m there is a hint of foliations at 50º TCA. No disseminate pyrite was found.There is ~1% quartz veins (mm - cm), and tiny little spider veins, with some carbonate alterations. Most of the veins are deformed with sigmoidal form or are brecciated.The contact at 273.52 is approximate. The rock is broken at this point and there are pieces missing.

273.52 281.13 ARG; S3S; SSARG; Siltstone; SSThe rock is a fine-grained grey to dark-grey argillite-siltstone-sandstone. The rock is composed of 35% argillite, 34% siltstone, 25% sandstone and 3% quartz veins. Some of the contacts between layersare irregular and at ~45º TCA, others are gradual. There is a small amount of disseminated pyrite in the unit.The quartz veins are mm - cm in size and most are deformed with carbonate alterations and sigmoidal or brecciated forms. There are a couple of veins that are sub-parallel TCA. There are some piles ofpyrite associated with the veins.The contact at 281.13 is irregular and from ~30º to sub-parallel TCA.

281.13 312.00 V; V3AVolcanic; Andesite/DaciteThe rock is a fine-grained grey volcanic (dacite?). From 281.13 m - 283.70 m and ~307.00 m - 312.00 m, the rock has what appears to be tiny fragments indicating it could be pyroclastic, also it ishighly altered, possibly with sericite, carbonate and chlorite. From 283.70 m - 288.00 m the rock looks like it could possibly be sedimentary (has similar appearance to the sandstone in the unit from273.52 m - 281.13 m), as well as from 294.00 m - 307.70 m. There are foliations in the unit at ~35º TCA. There is a shear zone from 298.00 m - ~300.00 m and 305.00 m - 305.50 m, with what appearsto be sericite alterations inthe foliations. There is disseminated and a few piles of pyrite throughout the unalterd sections.The rock contains ~10% quartz veins (mm - cm). The veins are deformed with sigmoidal, ptygmatic, brecciated and boudinage forms. Most of the veins contain carbonate alterations, some have a bit ofsericite alterations. Some of the veins appear to contain smokey quartz.


shear zone in volcanic unit.305.00 305.50 She

Shearingshear zone in volcanic unit.






Drilled by : Forage Benoît From : 2006-06-29 To : 2006-07-01Described by : Laura Mancini Description date : 2006-07-04

Collar


Remarks




672302.0005325302.000343.000


Flex-Dip 12.00 m -86.73° NoFlex-Dip 15.00 m -87.17° NoFlex-Dip 18.00 m -87.55° NoFlex-Dip 21.00 m -86.78° NoFlex-Dip 24.00 m -87.13° NoFlex-Dip 27.00 m -86.81° NoFlex-it 30.00 m 143.89° -86.54° NoFlex-it 33.00 m 143.85° -87.24° NoFlex-it 36.00 m 142.99° -86.90° NoFlex-it 39.00 m 158.86° -87.30° NoFlex-it 42.00 m 142.18° -86.95° NoFlex-it 45.00 m 151.49° -87.42° NoFlex-it 48.00 m 158.75° -87.06° NoFlex-it 51.00 m 159.69° -86.86° NoFlex-it 54.00 m 146.64° -86.32° NoFlex-Dip 57.00 m -86.61° No






Type Depth Azimuth Plunge InvalidFlex-it 258.00 m 164.48° -84.57° NoFlex-it 261.00 m 164.70° -84.47° NoFlex-it 264.00 m 173.12° -84.66° NoFlex-it 267.00 m 166.69° -84.14° NoFlex-it 270.00 m 163.35° -84.31° NoFlex-it 273.00 m 174.17° -84.21° NoFlex-it 276.00 m 166.39° -83.71° NoFlex-it 279.00 m 163.62° -84.03° NoFlex-it 282.00 m 163.71° -83.66° NoFlex-it 285.00 m 164.69° -83.75° NoFlex-it 288.00 m 165.54° -83.12° NoFlex-it 291.00 m 171.83° -83.25° NoFlex-it 294.00 m 167.11° -83.00° NoFlex-it 297.00 m 165.95° -83.05° NoFlex-it 300.00 m 169.99° -83.64° NoFlex-it 303.00 m 170.60° -83.53° NoFlex-it 306.00 m 166.44° -82.91° NoFlex-it 309.00 m 170.11° -83.46° NoFlex-it 312.00 m 167.22° -82.70° NoFlex-it 315.00 m 173.73° -82.82° NoFlex-it 318.00 m 167.15° -82.64° NoFlex-it 321.00 m 168.58° -83.27° No



DESCRIPTION


24.00 87.34 ARG; S3S; SSARG; Siltstone; SSThe rock is a fine-grained grey siltstone with fine-grained dark-grey argillite layers and medium to coarse-grained grey sandstone layers. The rock is composed of ~64% siltstone (2.0 mm to severalmeters in length), 20% argillite (1.0 mm - 35.0 cm), 15% sandstone (1.0 cm - several meters), 1% quartz veins.The contacts between the layers are irregular and at ~45º TCA. There are a lot of sericite alterations in the silstone and sandstone layers. There is disseminated pyrite throughout the unit. There is ashear zone from ~29.50 m - 34.50 m. There is a possible fault zone from ~44.50 m - 52.15 m. The rock appears brecciated (fault breccia), and sheared (has rock flour).The quartz veins are mm - cm in size, most are deformed with sigmoidal and ptygmatic forms. Most of the veins have carbonate alterations and some have sericite. The veins in the argillite sections,particullarly from 34.30 m - 39.00 m, have a lot of pyrite and chalcopyrite associated with them.The contact at 87.34 m is approximate. There is a lot of quartz-carbonate veining at this point making to see any real contact. Also the rock may grade from sedimentary to volcanic.


Shear zone in siltstone unit.87.34 116.51 V; V3A; Mas

Volcanic; Andesite/Dacite; MassiveThe rock is a fine-grained greyish-brown massive volcanic dacite or possibly rhyolite. There is a lot of sericite alterations throughout the unit. There is a hint of foliations throughout at ~52º TCA.There is a lot of carbonate and a small amount of disseminated pyrite scattered through the unit. There are no obvious pillows or layers.The rock contains ~30% quartz veins (mm - cm), and tiny little spider veins. Most of the veins are deformed and have sigmoidal, ptygmatic and brecciated forms (the veins have also heavily brecciatedthe rock). The majority of the veins have a lot of carbonate alterations.The contact at 116.51 m is approximate. There is a lot of veining deforming the rock making it difficult to see a contact, but the rock appears to grade from greyish-brown to grey.


Fine-grained massive felsic flow116.51 138.41 V; V3A; TBL

Volcanic; Andesite/Dacite; Tuff Breccia/LapillistoneThe rock is a fine-grained grey colored massive volcanic (dacite?). There are areas throughout the unit, particularly from 120.00 m - 122.20 m, that are coarse-grained and have the appearance of either apyroclastic (lapillistone?), or a sandstone. There is a lot of carbonate as well as a small amount of sericite alteration and disseminated pyrite and pyrrhotite, throughout the unit. There are no obviouspillows, layers, foliations, etc.The rock contains ~30% quartz veins (mm - cm), and tiny little spider veins. Most are deformed with sigmoidal and brecciated forms (the veins have also heavily brecciated the rock). The veins containa lot of carbonate alterations. There are piles of pyrrhotite associated with some of the veins.The contact at 138.41 m is irregular and at 25º TCA.

138.41 173.82 V; V3A; MasVolcanic; Andesite/Dacite; MassiveThe rock is a fine-grained light green colored massive volcanic, possibly andesite. There is some disseminated pyrite, sericite and a lot of carbonate throughout the unit. There are no obvious pillows,foliations, layers, etc. There is a shear zone from ~160.38 m - 166.60 m.The rock contains ~15% quartz veins (mm - cm), most are deformed with sigmoidal and brecciated forms. The veins have carbonate alterations and a few, particularly from 142.15 m - 142.28 m,contain what appear to be amphibole crystals. Several of the veins have epidote alterations.The contact at 173.82 m is approximate. There is a lot of alteration at this point making it difficult to see the actual contact.


Massive fine-grained felsic volcanic flow160.38 166.60 She

ShearingShear zone within volcanic unitn with some sericite layer.

173.82 188.35 V; V3A; PwVolcanic; Andesite/Dacite; PillowThe rock is a coarse-grained dark-green volcanic (andesite?). The rock appears to grade back and forth from really coarse-grained to medium-grained. There are dark bands several mm wide at 60º TCAthroughout the section that could possibly be pillow rinds. It is difficult to say for sure because they all contain quartz-carbonate veins, which might be the reason for the color difference. There is a lot



DESCRIPTION

of cabonate alterations, sericite and a tiny amount of disseminated pyrite throughout the section. There are no obvious foliations.The rock contains~5% quartz veins (mm - cm), with carbonate alterations. Some of the veins have sigmoidal or brecciated forms. Some of the veins contain a lot of very fine-grained dark-greenmineral, possibly chlorite. A thin section (06-65-179.7), was taken for proper identification.The contact at 188.35 m is approximate. The rock grades from coarse-grained dark-green to fine-grained light green.


Massive coarse-grained felsic volcanic flow.188.35 213.18 V; V3A; Pw

Volcanic; Andesite/Dacite; PillowThe rock is a fine-grained light green volcanic (andesite?). There are sections that are slightly darker green, possibly from more chlorite alterations. There are what appear to be possible pillows from198.00 m - 201.00 m (similar to what was seen in the section from 173.82 m - 188.35 m). There are vesicles filled with quartz, sericite or chlorite throughout the section. There is some carbonate andsericite in the unit.The rock contains ~10% quartz-carbonate veins (mm -cm), and tiny little spider veins with sericite alterations. Most of the veins are deformed with sigmoidal and brecciated forms. There are a coupleof veins that are sub-parallel TCA. There is a tiny amount of pyrite associated with some veins throughout the unit.The contact at 213.18 is approximate. The rock grades from light green to a light brown color.

213.18 221.78 V; V3A; TaVolcanic; Andesite/Dacite; Tuff /AshThe rock is a light brown (with grey sections), fine-grained volcanic, possibly a felsic tuff/ash. In the first ~2 meters, the rock appears massive then grades into argillite over several meters (the more greysections). There are no obvious pillows or foliations and there are no clear contacts between the volcanic and argillite layers (they are mixed together). There is disseminated pyrite in the mixed layersbut none in the volcanic section. There are a few amygdules filled with quartz at around 214.70 m.The rock contains ~10% quartz veins (mm - cm), and tiny little spider veins, most are deformed with a sigmoidal form and a lot of carbonate alterations. There are piles of pyrite associated with theveins particularly from 219.00 m - 221.78 m.The contact at 221.78 is very approximate since the rock grades over several meters.

221.78 324.00 ARG; S3SARG; SiltstoneThe rock is a fine-grained dark-grey to black graphitic argillite with fine-grained grey siltstone layers and coarse to medium grained medium-grey sandstone. The rock is composed of ~65% argillite(mm - m), 13% siltstone (mm - m), 12% sandstone (cm - m) and 10% quartz veins. There is disseminated and piles of pyrite throughout the section and the argillite sections contain a lot of graphite.The contacts between the layers are irregular ( at 55º TCA), to gradational. There are shear zones from ~227.00 m - 228.00 m and 259.00 m - 261.00 m. There is a very coarse-grained section ofsandstone from 231.90 m - 233.30 m, where quartz pebbles are easily seen. Some of the sandstone sections have what appear to be argillite rip-up fragments. There are euhedral carbonate crystals from~291.00 m - 295.00 m.The quartz veins are mm - cm in size and most are deformed with sigmoidal and brecciated forms. There are a lot of carbonate alterations and piles of pyrite associated with the veins, particularly from221.78 m - 227.30 m(at the contact with the volcanic unit). There is a lot of vening from ~226.00 m - 256.00 m and 258.00 m - 261.00 m, which is has deformed the rock. There is a large vein with sericite alterations from289.22 m - 289.45 m and 299.20 m - 299.65 m.


Shear zone in argillite unit259.00 261.00 She

Shearingshear zone in argillite unit






Drilled by : Foramex From : 2006-11-21 To : 2006-12-07Geologist : Bernard-Olivier Martel, géo Description date : 2007-06-06

Collar


Comments




671387.0005326590.000330.000


Flex-Dip 3.00m -85.36°Flex-Dip 6.00m -85.35°Flex-Dip 9.00m -85.06°Flex-Dip 12.00m -84.45°Flex-it 15.00m 256.10° -84.52°Flex-it 18.00m 259.69° -84.49°Flex-it 21.00m 266.09° -84.16°Flex-it 24.00m 259.83° -83.90°Flex-it 27.00m 266.62° -83.75°Flex-it 30.00m 260.26° -84.03°Flex-it 33.00m 266.22° -83.40°Flex-it 36.00m 265.93° -83.64°Flex-it 39.00m 261.26° -83.82°Flex-it 42.00m 261.82° -83.71°Flex-it 45.00m 267.16° -83.04°Flex-it 48.00m 265.57° -83.33°






Type Depth Azimuth PlungeFlex-it 549.00m 277.03° -55.16°Flex-it 552.00m 277.82° -54.85°Flex-it 555.00m 277.73° -55.04°Flex-it 558.00m 277.82° -54.95°Flex-it 561.00m 277.21° -55.14°Flex-it 564.00m 278.46° -54.77°Flex-it 567.00m 277.54° -54.96°Flex-it 570.00m 278.10° -54.83°Flex-it 573.00m 278.25° -54.66°Flex-it 576.00m 278.37° -54.62°Flex-it 579.00m 277.68° -54.98°Flex-it 582.00m 277.30° -54.96°Flex-it 585.00m 278.28° -54.59°Flex-it 588.00m 278.31° -54.73°Flex-it 591.00m 277.55° -54.96°Flex-it 594.00m 278.74° -54.60°Flex-it 597.00m 277.43° -54.93°Flex-it 600.00m 278.68° -54.53°Flex-it 603.00m 277.58° -54.95°Flex-it 606.00m 278.43° -54.63°Flex-it 609.00m 277.89° -54.58°



DESCRIPTION


9.30 48.40 V; V3B; TBLVolcanic; Basalt; Tuff Breccia/LapillistoneRoche volcanique fragmentaire.Basalt? Lapillestone.Green colorGrain size: mud to cobble.Components: lithic fragment (volcanic mafique, monomictic).Lithofacies: Matrix-supported, poorly sorted, and non-graded visibleVesicular (moderately to highly).Altteration: chlorite, sériciteContact inférieur approximatif

48.40 75.27 V; V3A; TBLVolcanic; Andesite/Dacite; Tuff Breccia/LapillistoneRoche volcanique fragmentaire. Andésite t? Lapillestone.Gray green color.Grain size: mud to cobble.Components: lithic fragment (volcanic intermèdiaire, monomictic).Lithofacies: Matrix-supported, poorly sorted, and non-graded visibleVesicular (highly).Altteration: chlorite, sériciteContact inférieur net à 65 degrés

75.27 96.80 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique. andésite?Composition: Plagioclase+ferromagnesian phase: amphibole, pyroxène and maybe some Qz?Lithofacies: massive .By section aphanitic to fine and by other fine to coarse.Vesicular (moderately)Foliation discontinuous at 45 to 55 degresAlteration: chlorite, séricite.2 % de veinule de Qz-Ca et Qz-Fp avec par section 3% déchiré.Contact inférieur approximatif et fracturé.

96.80 125.50 V; V3B; TBLVolcanic; Basalt; Tuff Breccia/LapillistoneRoche volcanique fragmentaire.Basalt? Lapillestone.Green colorGrain size: mud to cobble.Components: lithic fragment (volcanic mafique, monomictic).Lithofacies: Matrix-supported, poorly sorted, and non-graded visibleVesicular (sparsely).Altteration: chlorite, sériciteContact inférieur approximatif et fracturé.

125.50 214.65 V; V3A; TBLVolcanic; Andesite/Dacite; Tuff Breccia/LapillistoneRoche volcanique fragmentaire. Andésite t? Lapillestone or pseudo-pillows?Gray green color.Grain size: mud to cobble.Components: lithic fragment (volcanic intermèdiaire and mafic, polymict).



DESCRIPTION

Lithofacies: Matrix-supported, poorly sorted, and non-graded visibleVesicular (sparsely).Altteration: chlorite, sériciteContact inférieur net à 70 degrés

214.65 230.70 V; V3A; PwVolcanic; Andesite/Dacite; PillowRoche volcanique. Dacite?Composition: Plagioclase+ferromagnesian phase: amphibole, pyroxène and maybe some Qz? Gray colour.Lithofacies: pillows.Foliation discontinuous at 60 degresTexture: aphanitic, non-vesicular.Alteration: chlorite and séricite.2 à 5% de veinule de Qz-Ca et Qz-Fp.Contact inférieur approximatif.

230.70 254.75 V; V3A; Ta; TBLVolcanic; Andesite/Dacite; Tuff /Ash; Tuff Breccia/LapillistoneRoche volcanique fragmentaire. Andésite ? Lapillestone ?Gray green color.Grain size: mud to pebble.Components: crystals fragment of Qz and lithic fragment (volcanic intermèdiaire, monomict).Foliation discontinuous at 70 degres by sectionLithofacies: Matrix-supported, poorly sorted, and non-graded visibleVesicular (sparsely).Altteration: chlorite, séricite and ankérite.Contact inférieur net à 70 degrés


255.20 297.30 V; V3B; PwVolcanic; Basalt; PillowRoche volcanique. Basalt ou andésite?Composition: Plagioclase+ferromagnesian phase: amphibole, pyroxène and maybe some Qz? Green gray colour.Lithofacies: pillows.La foliation est peu visible, discontinue et à environs à 60 degrésTexture: aphanitic to fine, no-vesicular.Alteration: chlorite and séricite.2 à 5% de veinule de Qz-Ca et Qz-Fp.Contact inférieur net à 50 degrés

297.30 305.30 V; V3B; MasVolcanic; Basalt; MassiveRoche volcanique. Basalt ou andésite?Composition: Plagioclase+ferromagnesian phase: amphibole, pyroxène and maybe some Qz?Lithofacies: massive.By section aphanitic to fine and by other fine to mediumNo-vesicularLa foliation est peu visible, discontinue et à environs 60 degrésAlteration: chlorite, séricite.2 % de veinule de Qz-Ca et Qz-Fp avec par section 3% déchiré.Le contact inférieur à un aspect brèchique sur le dernier mètre et cependant le contact avec le chert sous-jacent est nette à environs 85 degrés.

305.30 306.49 S5C



DESCRIPTION

Chert306.49 326.00 V; V3A; TBL; Ta; ST

Volcanic; Andesite/Dacite; Tuff Breccia/Lapillistone; Tuff /Ash; Stratified/LaminatedRoche volcanique fragmentaire.andésite? Lapillistone to tuffGray color.Passage grossier au début de l'unitée (Lapillistone), passage moyen au milieu (tuff) et passage fin à très fin vers la fin de la l'unité (tuff argillitique).Grain size: mud to cobbleComponents: crystal fragment (quartz), lithic fragment (volcanic felsic, more monomictic). Fp-Qz, séricite et chlorite.Lithofacies: stratified (laminated to medium bedded) and non-graded visible. Vesicular (moderately)Altteration: chlorite, sériciteContact inférieur net à 45 degrés.

326.00 347.30 V; V3A; Ta; STVolcanic; Andesite/Dacite; Tuff /Ash; Stratified/LaminatedRoche volcanique fragmentaire.andésite? tuff à ash tuffGray color.Passage moyen au (tuff) et passage fin à très fin vers la fin de la l'unité (tuff argillitique ou ash tuff).Grain size: mud to sandComponents: crystal fragment (quartz), lithic fragment (volcanic felsic, more monomictic). Fp-Qz, séricite et chlorite.Lithofacies: stratified (laminated to medium bedded) and non-graded visible. vesicular (moderately)Altteration: chlorite, sériciteContact inférieur net à 65 degrés.

347.30 354.32 V; V3A; Ta; STVolcanic; Andesite/Dacite; Tuff /Ash; Stratified/LaminatedRoche volcanique fragmentaire.andésite? tuffGray green color.Passage moyen au (tuff) et passage fin à très fin vers la fin de la l'unité (tuff argillitique ou ash tuff).Grain size: mud to sandComponents: crystal fragment (quartz), lithic fragment (volcanic felsic, more monomictic). Fp-Qz, séricite et chlorite.Lithofacies: stratified (laminated to medium bedded) and non-graded visible. vesicular (moderately)Altteration: chlorite, sériciteContact inférieur net à 65 degrés.

354.32 380.80 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique. andésite?Composition: Plagioclase+ferromagnesian phase: amphibole, pyroxène and maybe some Qz?Lithofacies: massive.By section aphanitic to fine and by other fine to mediumNo-vesicularLa foliation visible, discontinue et à environs 60 degrésAlteration: chlorite, séricite.2 % de veinule de Qz-Ca et Qz-Fp avec par section.Le contact inférieur approximatif ( zone de déformation).

380.80 387.84 V; V3B; Ta; LamVolcanic; Basalt; Tuff /Ash; LaminatesRoche volcanique fragmentaire. Tuff basaltique? Nom de la roche incertain dû à la zone de déformation voir structure et Lame-mince #LG21929.Gray green color.Alternance de bandes minces, généralement irrégulières, de couleur vert et noirâte. Les bandes verdâtre interprétées comme étant des niveaux plus grossiers (sand) de tuff et les bandes noirâtresinterprétées comme étant des laminations plus fines (argillite)Grain size: mud to sandComponents: Fp-Qz, séricite et chlorite.



DESCRIPTION

Lithofacies: stratified (laminated to thinly beded) and non-graded visible. no-vesicular.La foliation est visible, discontinue et en bandes mince et à environs 60-70 degrés.Altteration: chlorite, sériciteContact inférieur graduel sur 50 cm, riche en pyrrothine et allant de couleur vertâdre à noirâtre.Environs 2% de veinules de QZ-CB

387.84 393.41 ARG; SS; STArgillite; Sandstone; Stratified/LaminatedRoche fragmentaire possiblement d'origine volcanique.Gray and black color.Alternance de bandes larges, minces parfois irrégulières, de couleur grise et noirâte. Les bandes gris interprétées comme étant des niveaux plus grossiers (sand) de tuff et les bandes noirâtres interprétéescomme étant des laminations plus fines (argillite)Grain size: mud to sandComponents: Fp-Qz, séricite et chlorite.Lithofacies: stratified (laminated to thinly beded) and non-graded visible. no-vesicular.La foliation est visible, irrégulière et en bandes et à environs 60-70 degrés.Altteration: chlorite, sériciteEnvirons 2% de veinules de QZ-CB, généralement mince, associées à de la pyrrothine et le tout transposées.Contact inférieur approximatif.

393.40 404.80 SheShearing75°Zone de déformation avec présence de gauge de faille sur 20 cm entre 404.0 à 404.2.Transposition importante avec plusieur veines de Quartz en fumé déformées et déchirées.Cette déformation nuit à l'interprétation.

393.41 410.77 V; V3A; TaVolcanic; Andesite/Dacite; Tuff /AshRoche volcanique fragmentaire. Andésite ? Tuff ?Gray color.Grain size: mud to sandComponents: crystal fragment (quartz), lithic fragment (volcanic felsic, more monomictic). Fp-Qz, séricite et chlorite.Lithofacies: stratified (laminated to medium bedded) and non-graded visible. vesicular (sparsely)Altteration: chlorite, sériciteDe 396.5 à 404.8: zone riche en veine de Qz en fumé (Plus de 50%) avec altération en chlrorite aux épontes. (Probablement associer à la zone de déformation)Contact inférieur approximatif

410.77 421.36 V; V3A; PwVolcanic; Andesite/Dacite; PillowRoche volcanique. andésite?Composition: Plagioclase+ferromagnesian phase: amphibole, pyroxène and maybe some Qz?Gray colour.Lithofacies: pillows.Foliation discontinuous at 65 degresTexture: aphanitic to fine and vesicular (sparely)Alteration: chlorite and séricite.2 à 5% de veinule de Qz-Ca et Qz-Fp.Contact inférieur approximatif.

421.36 426.55 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique. andésite?Composition: Plagioclase+ferromagnesian phase: amphibole, pyroxène and maybe some Qz?Lithofacies: massive.Aphanitic to fine



DESCRIPTION

No-vesicularLa foliation visible, discontinue et à environs 60 degrés ?Alteration: chlorite, séricite.2 % de veinule de QzLe contact inférieur net à 75 degrés


427.29 443.30 V; V3AVolcanic; Andesite/DaciteRoche volcanique fragmentaire. Andésite ? Tuff ?Gray color.Grain size: mud to sandComponents: crystal fragment (quartz), lithic fragment (volcanic felsic, more monomictic). Fp-Qz, séricite et chlorite.Lithofacies: stratified (laminated to medium bedded) and non-graded visible. vesicular (sparsely)Altteration: chlorite, sériciteContact inférieur approximatif

443.30 498.92 V; V3A; TBL; Ta; STVolcanic; Andesite/Dacite; Tuff Breccia/Lapillistone; Tuff /Ash; Stratified/LaminatedRoche volcanique fragmentaire.andésite? Lapillistone to tuffGray color.Passage grossier (Lapillistone) alternant avec passage plus fin (tuff). Le contact entre les passages sont parfois nette mais généralement graduel et peu visible.Grain size: mud to cobbleComponents: crystal fragment (quartz), lithic fragment (volcanic felsic, monomictic). Fp-Qz, séricite et chlorite.Lithofacies: stratified (laminated to medium bedded) and non-graded visible. Vesicular (moderately)Altteration: chlorite, sériciteContact inférieur net à 45 degrés.

498.92 513.52 V; V3A; TaVolcanic; Andesite/Dacite; Tuff /AshRoche volcanique fragmentaire. Andésite ? Tuff ?Gray color.Grain size: mud to sandComponents: crystal fragment (quartz), lithic fragment (volcanic felsic, more monomictic). Fp-Qz, séricite et chlorite.Lithofacies: stratified (laminated to medium bedded) and non-graded visible. vesicular (sparsely)Altteration: chlorite, séricitePrésence veine de Qz en fumé 5%) avec altération en chlrorite aux épontes. (Probablement associer à la zone de déformation)Contact inférieur plutôt net

512.00 513.80 SheShearingZone de déformationTransposition importante avec quelques veines de Quartz fumé déformées et déchirées.Cette déformation nuis à l'interprétation.

513.52 530.80 CONGLO; GaG; PoConglo; Gray Green; PolymicticConglomerat gris vert pâle, polymictic et généralement clast-supported.La matrice correspond à environs 20% de la roche, elle est aphanitique à fine, de couleur gris vert pâle et avec des traces de sulfure.Le conglomérat est princpalement composé de fragments felsiques et il ne semble pas avoir de fragment mafique.Fragments felsiques : couleur gris pâle, gris moyen et beige (alt séricite?) avec une granulométrie généralement aphanitique à fine mais avec quelques exeption à granulométrique moyen (Clast derhyolite). La morphologie est généralement arrondi à sub- anguleux. Leurs puissances varie entre 0.3-10cm, mais est généralement entre 1-5cm. L'origine de ces fragments semble principalementvolcaniques felsique (pyroclastique, massive et/ou pillow)



DESCRIPTION

Une foliation est visible, définie par l'alignement des clast et par la matrice et varie généralement entre 65-75 degré A/C.1 à 2% veinules de CB-QZ sont présente et injectées irrégulièrement.Le contact inférieur est net, avec veine de quartz laminé et à environs 55 degrés


530.80 612.00 ARG; SS; STArgillite; Sandstone; Stratified/LaminatedRoche sédimentaire : Argilites en alternance avec des bandes de sandstone.Unité composé de lits (0.5-30cm) de sandstone (40%) en alternance avec des lits (0.1-10cm) d'argilites (60%).L'argilite est de couleur gris foncé et aphanitique.Le sandstone est de couleur gris moyen à pâle avec une granulométrie très fine à fine. Les lits sont généralement massifs, mais parfois littées. Très localement quelques grains sont plus grossiers (Qzeyes et rip-up clasts)Les lits (sandstone et argiles) ont une orientation de 65degré A/C. Les lits sont en bandes minces, en bandes larges et en bandes irrégulières.De plus, environ 3 à 5 % de veinules de QZ et de CB sont présentes irrégulièrement à travers les lits et sont parfois déchirées.Des très fines traces de PY et PO sont disséminées irrégulièrement.EOH

578.80 589.47 SS; ARG; STSandstone; Argillite; Stratified/LaminatedZone pauvre en bande pélitique (moins de 10%)

594.00 603.50 SS; ARG; STSandstone; Argillite; Stratified/LaminatedZone pauvre en bande pélitique (10- 20%)






Drilled by : Foramex From : 2006-12-07 To : 2006-12-11Geologist : Serge Massé Description date : 2007-01-16

Collar


Comments




671301.0005326490.000340.000







Type Depth Azimuth PlungeFlex-it 399.00m 258.64° -79.72°Flex-it 402.00m 260.87° -79.84°Flex-it 405.00m 261.56° -79.87°Flex-it 408.00m 260.45° -79.36°Flex-it 411.00m 262.86° -79.55°Flex-it 414.00m 260.88° -79.20°Flex-it 417.00m 261.49° -79.16°Flex-it 420.00m 260.63° -79.09°Flex-it 423.00m 264.05° -79.04°Flex-it 426.00m 264.13° -79.30°Flex-it 429.00m 263.61° -78.97°Flex-it 432.00m 261.21° -79.45°Flex-it 435.00m 263.89° -79.41°Flex-it 438.00m 264.83° -78.96°Flex-it 441.00m 264.42° -78.72°Flex-it 444.00m 263.16° -78.57°Flex-it 447.00m 264.57° -78.51°Flex-it 450.00m 264.78° -78.68°




DESCRIPTION

0.00 2.10 OBOverburdenOverburden. 1.5m de casing.

2.10 17.70 V; V3A; Pw; BreVolcanic; Andesite/Dacite; Pillow; BrecciaRoche volcanique fragmentaire (andésite ou dacite ?) Pyroclastique: lapillistone à bloc. Flow breccia (brèche de coulée)Semble une roche pyroclastique composée principalement de fragment felsique dans une matrice aphanitique chloritisée et séricitisé ?).Apparence de marge de pillow à phénocristaux séricitisés.Les fragments sont felsique (dacite, rhyolite ?)La matrice est de couleur gris vert moyen et présente des amygdules.Foliation ou déformation très visible qui varient entre 45-55 degré A/C.Environ 5-10% de veinules de CB parfois avec du QZ sont injectées irrégulièrement.Des traces de PO et de PY sont disséminées irrégulièrement.Pas de contact inférieur.

17.70 18.00 CNRCore not recoveredcore non récupéré

18.00 77.30 V; V3A; Pw; Bre; MoVolcanic; Andesite/Dacite; Pillow; Breccia; MonomicticRoche volcanique fragmentaire: (plutôt andésitique ) Pyroclastique monomictique : lapillistone à bloc. Flow breccia (brèche de coulée)Semble une roche pyroclastique composée principalement de fragment felsique dans une matrice plus mafique, aphanitique, chloritisée et séricitisé ?).Tjs apparence de marge de pillow à phénocristaux séricitisés.Les fragments sont felsique (surtout andésiite, peut-être qqe rhyolite ?).La matrice est de couleur gris vert moyen et présente des qqe amygdules.Foliation ou déformation très visible à plus ou moins 50 degré A/C.Environ 5-10% de veinules de CB parfois avec du QZ sont injectées irrégulièrement.Des traces de PO et de PY sont disséminées irrégulièrement.Le contact inférieur approximatif

22.50 24.00 SrMvsericite/muscoviteCertains passages pourraient être des coulés massives avec phénocristaux séricitisé (22.5 à 24.0m).

77.30 96.88 V; V3A; Pw; Bre; MoVolcanic; Andesite/Dacite; Pillow; Breccia; MonomicticRoche volcanique fragmentaire: (plutôt dacitique ) Pyroclastique monomictique : lapillistone à surtout bloc. Flow breccia (brèche de coulée)Semble une roche pyroclastique composée principalement de fragment felsique dans une matrice plus mafique, aphanitique, chloritisée et séricitisé ?).Tjs apparence de marge de pillow à phénocristaux séricitisés.Les fragments sont felsique (surtout dacite, peut-être qqe rhyolite ?).La matrice est de couleur gris vert moyen et présente des qqe amygdules.Foliation ou déformation très visible à plus ou moins 50 degré A/C.Environ 5-10% de veinules de CB parfois avec du QZ sont injectées irrégulièrement.Des traces de PO et de PY sont disséminées irrégulièrement.Le contact inférieur difus mais marqué par augmentation des block clast plus dacitique qu'andésitique

96.88 118.50 V; V3A; TBL; MoVolcanic; Andesite/Dacite; Tuff Breccia/Lapillistone; MonomicticRoche volcanique fragmentaire: (plutôt andésitique ) Pyroclastique monomictique : lapillistone à bloc (moins de bloc que l'unité précédente, mais augmentation vers la fin de l'unité). passage lapilli toFlow breccia (brèche de coulée)Semble une roche pyroclastique composée principalement de fragment felsique dans une matrice plus mafique, aphanitique, chloritisée et séricitisé ?).Tjs apparence de marge de pillow à phénocristaux séricitisés.Les fragments sont felsique (surtout andésite, peut-être qqe rhyolite ?).La matrice supported est de couleur gris vert moyen et présente des qqe amygdules.



DESCRIPTION

Foliation ou déformation très visible à plus ou moins 50 degré A/C.Environ <5% de veinules de CB parfois avec du QZ sont injectées irrégulièrement.Des traces de PO et de PY sont disséminées irrégulièrement.Contact inférieur net avec lave massive à 45 degrés A/C

118.50 124.15 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique massive (dacite/andésitique )Composition: Plagioclase+ferromagnesian phase: amphibole, pyroxène and maybe some Qz?Lithofacies: massive.Matrice aphanitique à finepeu vesiculaireLa foliation visible, discontinue et à environs 55 degrés ?Alteration: chlorite, séricite.2 % de veinule de QzLe contact inférieur plus ou moins évident à 75 degrés A/C

124.15 137.70 V; V3R; TBL; QE; PoVolcanic; Rhyolite; Tuff Breccia/Lapillistone; Quartz eyes; PolymicticRoche volcanique fragmentaire: Pyroclastique polymictique (Ryolitique, andésite/dacite ) Lapillistone à bloc. Flow breccia (brèche de coulée)Semble une roche pyroclastique composée principalement de fragment plus felsique que les unités précédentes dans une matrice plus mafique, aphanitique, chloritisée et séricitisé ?).Marge de pillow peu évidente.Les fragments sont felsique (surtout rhyolite, mais peut-être qqea ndésite/dacite ?).La matrice medium-supported est de couleur gris vert moyen.Foliation ou déformation très visible à plus ou moins 45-50 degré A/C.Environ 2-3% de veinules de CB parfois avec du QZ sont injectées irrégulièrement.Des traces de PO et de PY sont disséminées irrégulièrement.Le contact inférieur difus mais marqué par augmentation des amygdules.

137.70 154.30 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique massive (dacite/andésitique )Composition: Plagioclase+ferromagnesian phase: amphibole, pyroxène and maybe some Qz?Lithofacies: massive.Matrice fineUnité marquée par l'abondance des amygdules (calcite/quartz).La foliation visible, discontinue et à environs 50 degrés ?Alteration: chlorite, séricite.2-3 % de veinule de QzLe contact inférieur plus ou moins évident entre

154.30 160.10 V; V3A; TBL; QE; PoVolcanic; Andesite/Dacite; Tuff Breccia/Lapillistone; Quartz eyes; PolymicticRoche volcanique fragmentaire: lapillistone polymictique :(C/F, qqe QE,), matrix supportedSemble une roche pyroclastique composée principalement de fragment felsique dans une matrice plus mafique (basalte), aphanitique, chloritisée et séricitisé ?).Les fragments sont felsique.La matrice supported est de couleur gris vert plutôt foncéPrésence de magnétite entre 177.63 et 161.60.Foliation ou déformation très visible à plus ou moins 50 degré A/C.Environ 2% de veinules de CB parfois avec du QZ sont injectées irrégulièrement.Des traces de PO et de PY sont disséminées irrégulièrement.Contact inférieur approximatif avec lave massive

160.10 165.15 V; V3A; V3B; MasVolcanic; Andesite/Dacite; Basalt; Massive



DESCRIPTION

Roche volcanique massive (dacite/andésitique/basalte )Composition: Plagioclase+ferromagnesian phase: amphibole, pyroxène and maybe some Qz?Lithofacies: massive.Matrice finePrésence amygdules (calcite/quartz).La foliation visible, discontinue et à environs 50 degrés ?Alteration: chlorite, séricite.2-3 % de veinule de QzLe contact inférieur approximatif

165.15 180.75 V; V3A; TBL; QE; PoVolcanic; Andesite/Dacite; Tuff Breccia/Lapillistone; Quartz eyes; PolymicticRoche volcanique fragmentaire: lapillistone à bloc polymictique :(C/F, qqe QE,), matrix supportedSemble une roche pyroclastique composée principalement de fragment felsique dans une matrice plus mafique (basalte), aphanitique, chloritisée et séricitisé ?).Les fragments sont felsique etplus grossier ou en bloc vers la fin de l'unité.La matrice supportante est de couleur gris vert plutôt foncéFoliation ou déformation très visible à plus ou moins 50 degré A/C.Environ 2% de veinules de CB parfois avec du QZ sont injectées irrégulièrement.Des traces de PO et de PY sont disséminées irrégulièrement.Contact inférieur approximatif avec lave massive

180.75 183.90 V; V3A; V3B; MasVolcanic; Andesite/Dacite; Basalt; MassiveRoche volcanique massive (dacite/andésitique/basalte )Composition: Plagioclase+ferromagnesian phase: amphibole, pyroxène and maybe some Qz?Lithofacies: massive.Matrice aphanitique à finePrésence d'amygduleLa foliation visible, discontinue et à environs 55 degrés ?Alteration: chlorite, séricite.2-5 % de veinule de QzLe contact inférieur plus ou moins évident à 75 degrés A/C

183.90 186.70 V; V3B; PwVolcanic; Basalt; PillowRoche volcanique fragmentaire: PillowMatrice plutôt mafique, aphanitique, chloritisée, séricitisé ? et de couleur gris vert moyen.Marges de pillow relativement évidentes.Foliation ou déformation très visible à plus ou moins 45-50 degré A/C.Environ 2-3% de veinules de CB parfois avec du QZ sont injectées irrégulièrement.Des traces de PO et de PY sont disséminées irrégulièrement.Le contact inférieur plus ou moins net à 50degrées A/C

186.70 196.50 V3A; V3B; MasAndesite/Dacite; Basalt; MassiveRoche volcanique massive (dacite/andésitique/basalte )Composition: Plagioclase+ferromagnesian phase: amphibole, pyroxène and maybe some Qz?Lithofacies: massive.Matrice aphanitique à finePas d'amygduleLa foliation visible, discontinue et à environs 55 degrés ?Alteration: chlorite, séricite.2-5 % de veinule de QzLe contact inférieur approximatif



DESCRIPTION

196.50 201.70 V; V3A; V3B; PwVolcanic; Andesite/Dacite; Basalt; PillowRoche volcanique (dacite/andésitique/basalte ),Composition: Plagioclase+ferromagnesian phase: amphibole, pyroxène and maybe some Qz?Lithofacies: pillow.Matrice aphanitique à finePas d'amygduleLa foliation visible, discontinue et à environs 55 degrés ?Alteration: chlorite, séricite.

201.70 209.25 V; V3A; V3B; MasVolcanic; Andesite/Dacite; Basalt; MassiveRoche volcanique massive (dacite/andésitique/basalte )Composition: Plagioclase+ferromagnesian phase: amphibole, pyroxène and maybe some Qz?Lithofacies: massive.Matrice aphanitique à finePas d'amygduleLa foliation visible, discontinue et à environs 55 degrés ?Alteration: chlorite, séricite.2-5 % de veinule de QzLe contact inférieur approximatif,mais marqué par ce qui semble un bloc.

209.25 210.30 V; V3A; TBL; MoVolcanic; Andesite/Dacite; Tuff Breccia/Lapillistone; MonomicticRoche volcanique fragmentaire: lapillistone à bloc polymictique :(C/F, qqe QE,), matrix supportedSemble une roche pyroclastique composée principalement de fragment felsique dans une matrice plus mafique (basalte), aphanitique, chloritisée et séricitisé ?).Les fragments sont felsique et grossier ou en blocLa matrice supportante est de couleur gris vert plutôt foncéFoliation ou déformation très visible à plus ou moins 50 degré A/C.Environ 2% de veinules de CB parfois avec du QZ sont injectées irrégulièrement.Des traces de PO et de PY sont disséminées irrégulièrement.Contact inférieur approximatif avec lave massive

210.30 223.90 V; V3A; V3B; MasVolcanic; Andesite/Dacite; Basalt; MassiveRoche volcanique massive (dacite )Composition: Plagioclase ± ferromagnésian phase : biotite, amphibole, pyroxène ±quartzLithofacies: massive.Matrice aphanitique à finePas d'amygduleLa foliation peu visible à environs 50 degrés ?Alteration: chlorite, séricite.2-5 % de veinule de QzLe contact inférieur approximatif.

223.90 232.50 V; V3B; Pw; BreVolcanic; Basalt; Pillow; BrecciaRoche volcanique: Pillow avec blocs probable (brèche de coulée ?)Matrice plutôt mafique, aphanitique, chloritisée, séricitisé ? et de couleur gris vert moyen.Marges de pillow relativement évidentes.Foliation ou déformation très visible à plus ou moins 45-50 degré A/C.Environ 5% de veinules de CB parfois avec du QZ sont injectées irrégulièrement.Des traces de PO et de PY sont disséminées irrégulièrement.Contact inférieur approximatif



DESCRIPTION

231.30 242.50 VEI;40;ClCc;;10°;Py01;Vein 40 Chlorite Calcite 10° Pyrite01Veine de qz + calcite

232.00 239.00 SrMvsericite/muscoviteAssocié à des veines de quatz

232.50 254.75 V; V3A; V3B; MasVolcanic; Andesite/Dacite; Basalt; MassiveRoche volcanique massive (dacite/andésitique/basalte) ou tuff (*?)*? L'unité est très influencé par des injections de quartz et donc difficile à identifier. Je semble distinguer un tuff dans la deuxième moitié de l'unité, mais c'est flou.Composition: Plagioclase+ferromagnesian phase: amphibole, pyroxène and maybe some Qz?Lithofacies: massiveMatrice fine séricitiséPas d'amygduleLa foliation visible, discontinue et à environs 55 degrés ?Alteration: chlorite, séricite.20 % de veinule de QzLe contact inférieur net avecnlechert à 65 degrés A/C

254.75 255.80 S5C; STChert; Stratified/LaminatedChert

255.80 257.10 V; V/S?; TaVolcanic; Volcanic/Sédiment?; Tuff /AshRoche volcanique fragmentaire : Bande massive de ash tuff laminé.Matrice medium supportedGray color.Altération : séricite et chlorite.Lithofacies: stratified laminated and non-graded visible.Foliation : 55 degrés A/CContact inférieur net à 45 degrés.

257.10 258.54 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique massive (dacite/andésite )Composition: Plagioclase+ferromagnesian phase: biotite amphibole, pyroxène and maybe some Qz?Lithofacies: massive.Matrice fineUnité marquée par l'abondance des amygdules (calcite/quartz).La foliation visible, discontinue et à environs 50 degrés ?Alteration: chlorite, séricite.2-3 % de veinule de QzLe contact inférieur net à 45-50 degrés C/A

258.54 259.40 V; V/S?; Ta; TBL; STVolcanic; Volcanic/Sédiment?; Tuff /Ash; Tuff Breccia/Lapillistone; Stratified/LaminatedRoche volcanique fragmentaire : Bande de ash tuff laminé alternant avec bandes de tuff à lapillis.Matrice : clast supportedGray color.Grain size passage de mud et passage à sand/sandstoneComposantes polymictiques : volcanique cristals fragments, lithic fragmentsLithofacies: stratifié (bedded)Bedding : <1mm to 10-30cm



DESCRIPTION

Altteration: chlorite, sériciteFoliation : 55 degrés A/CContact inférieur net à 45 degrés.

259.40 260.80 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique massive (dacite/andésite )Composition: Plagioclase+ferromagnesian phase: biotite amphibole, pyroxène and maybe some Qz?Lithofacies: massive.Matrice fineUnité marquée par l'abondance des amygdules (calcite/quartz).La foliation visible, discontinue et à environs 50 degrés ?Alteration: chlorite, séricite.2-3 % de veinule de QzLe contact inférieur plus ou moins net

260.80 279.50 V; V3A; Ta; TBL; MoVolcanic; Andesite/Dacite; Tuff /Ash; Tuff Breccia/Lapillistone; MonomicticRoche volcanique fragmentaire: alternance de lapillistone, tuff grossier et puis fin, monomictique :(C/F), et à matrix supportedSemble une roche pyroclastique composée principalement de fragment felsique dans une matrice aphanitique, chloritisée et séricitisé ?).Les fragments felsiques apparaissent par endroit fondus dans la matricede couleur grise , i.e.les bordures sont floues.L'unité apparaît granoclassé vers la fin : passage lapillis à fine (ash)Foliation ou déformation visible à plus ou moins 50 degré A/C.Environ 2% de veinules de CB parfois avec du QZ sont injectées irrégulièrement.Des traces de PO et de PY sont disséminées irrégulièrement.Contact inférieur net à 50 degrés A/C

279.50 304.60 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique massive (dacite/andésite )Composition: Plagioclase+ferromagnesian phase: biotite amphibole, pyroxène and maybe some Qz?Unité marqué au début par la présence de laminations et de petits horizons de mudstone. Aussi, qqe rip-up ou petits horizon de mudstone présent vers la fin de l'unité.Lafindel'unité estfortement injecté deveines et veinules de quartz et calcite probablement associés à une zone de déformation.Lithofacies: massive.Matrice finePrésence d'amygdules (calcite/quartz).La foliation visible, discontinue et à environs 55 degrés C/A?Alteration: chlorite, séricite.Env. 10 % de veinule de Qz, CaLe contact inférieur plutôt approximatif

301.50 303.30 VNL;;Cc;X;;;Veinule Calcite BrecciatedZone injectée de quartz/calcite

304.00 327.00 SrMv; Chsericite/muscovite; chloriteAssocié à uneveine de déformation (shear)

304.00 327.00 SheShearingShear, gauge de faille à 320.2 à 320.5.50 degrés A/C

304.60 322.60 CONGLO; GaG; Po; C/F; QEConglomerate; Gray Green; Polymictic; Felsic Clast; Quartz eyesSand to granule conglomerat gray green, medium supported à clast supported fabric, polymictique riche en clast felsique, altération séricite, chlorite



DESCRIPTION

Dans l'ensemble, la roche est de couleur gris moyen-foncé, localement beige.La matrice semble de couleur gris moyen-foncé à grains aphanitique (difficile à évaluer étant donnée qu'elle se confond parfois avec certains clasts de couleur semblable et qu'elle représente environ10-15% du conglomérat). Elle contient des fines traces de PY.Les fragments sont généralement felsiques et peu semble mafique. Qqe fragments lithique (rip-up argilite et peut-être autres ?) et cristaux sont présents (QE, mix vert ?)Leur morphologie est généralement sub-arrondie. La puissance des clasts varie entre 0.2-6cm, mais est généralement entre 0.5-2cm.Les clasts felsiques sont principalement de couleur gris moyen, beige-gris et quelques-uns blanc (QZ). Dans l'ensemble, l'origine des fragments semblent volcanique felsique (rhyolite, dacite, tuffmassif...) et aussi sédimentaire (siltstone, sandstone...).Les fragments suivent une orientation généralement à 50 degré A/C.Environ 3-4% de veinules de CB-QZ sont injectées irrégulièrement et déchirés.Le contact inférieur plus ou moins net, puisque veine de quartz .


322.60 394.00 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique massive (dacite/andésite )Composition: Plagioclase+ferromagnesian phase: biotite amphibole, pyroxène and maybe some Qz?Unité marqué au début par la présence de laminations et de petits horizons de mudstone. Aussi, qqe rip-up ou petits horizon de mudstone présent vers la fin de l'unité.Les 10 derniers mètres de la fin de l'unité présente une texture plus cahotiqueLithofacies: massive.Matrice aphanitique à finePrésence d'amygdules (calcite/quartz).La foliation visible, discontinue et à environs 50-55 degrés C/A?Alteration: chlorite, séricite.Env. 10 % de veinule de Qz, CaLe contact inférieur plutôt net et diffus

394.00 397.20 CONGLO; Ga; Po; C/F; QE; CtS; QEConglo; Gray; Polymictic; Felsic Clast; Quartz eyes; Clast-Supported; Quartz eyesConglomerat gris vert pâle, polymictic rich C/F et généralement clast-supported.La matrice correspond à environs 20% de la roche, elle est aphanitique à fine, de couleur gris vert et avec des traces de sulfure.Le conglomérat est princpalement composé de fragments felsiques et il semble y avoir peu de fragment mafique. Présence de QEFragments felsiques : couleur gris pâle, gris moyen et beige (alt séricite?) avec une granulométrie généralement aphanitique à fine mais avec quelques exeption à granulométrique moyen (Clast derhyolite). La morphologie est généralement arrondi à sub- anguleux. Leurs puissances varie entre 0.3-10cm, mais est généralement entre 1-5cm. L'origine de ces fragments semble principalementvolcaniques felsique (pyroclastique, massive et/ou pillow)Une foliation est visible, définie par l'alignement des clast et par la matrice et varie généralement entre 55 degré A/C.1 à 2% veinules de CB-QZ sont présente et injectées irrégulièrement.Le contact inférieur est approximatif et fct du changementde couleur de la matrice.


397.20 404.50 CONGLO; YG; Po; C/F; QEConglo; Yellow Green; Polymictic; Felsic Clast; Quartz eyesConglomerat yellow green, polymictic rich C/F et généralement clast-supported.La matrice correspond à environs 20% de la roche, elle est aphanitique à fine, de couleur gris vert et avec des traces de sulfure.Le conglomérat est princpalement composé de fragments felsiques et il semble y avoir peu de fragment mafique. Présence de QEFragments felsiques : couleur gris pâle, gris moyen et beige (alt séricite?) avec une granulométrie généralement aphanitique à fine mais avec quelques exeption à granulométrique moyen (Clast derhyolite). La morphologie est généralement arrondi à sub- anguleux. Leurs puissances varie entre 0.3-10cm, mais est généralement entre 1-5cm. L'origine de ces fragments semble principalementvolcaniques felsique (pyroclastique, massive et/ou pillow)Un certain bedding est marqué par des passages plus fin (granule)Une foliation est visible, définie par l'alignement des clast et par la matrice et varie généralement entre 55 degré A/C.



DESCRIPTION

1 à 2% veinules de CB-QZ sont présente et injectées irrégulièrement.Le contact inférieur est approximatif et fct du changementde couleur de la matrice.


404.50 434.30 CONGLO; GaG; Po; C/FConglo; Gray Green; Polymictic; Felsic ClastConglomerat gris vert pâle, polymictic rich C/FLa matrice clast-supported correspond à environs 20% de la roche, elle est aphanitique à fine, de couleur gris vert et avec des traces de sulfure.Le conglomérat est princpalement composé de fragments felsiques et il semble y avoir peu de fragment mafique. Présence de QEFragments felsiques : couleur gris pâle, gris moyen et beige (alt séricite?) avec une granulométrie généralement aphanitique à fine mais avec quelques exeption à granulométrique moyen (Clast derhyolite). La morphologie est généralement arrondi à sub- anguleux. Leurs puissances varie entre 0.3-10cm, mais est généralement entre 1-5cm. L'origine de ces fragments semble principalementvolcaniques felsique (pyroclastique, massive et/ou pillow)Une foliation est visible, définie par l'alignement des clast et par la matrice et varie généralement entre 55 degré A/C.1 à 2% veinules de CB-QZ sont présente et injectées irrégulièrement.Le contact inférieur est net à 60 degrése de A/C


434.30 453.00 ARG; SS; STArgillite; Sandstone; Stratified/LaminatedRoche sédimentaire : Argilites en alternance avec des bandes de sandstone/silstone.Unité composé de bandes (0.2-60cm) de sandstone/silstone (60%) en alternance avec des lits (0.1-5cm) d'argilites (40%). Les niveau d'argilite augmente vers la fin du sondageL'argilite est de couleur gris foncé et aphanitique.Le sandstone/silstone est de couleur gris moyen à pâle avec une granulométrie très fine à fine. Les lits sont généralement massifs, mais parfois littées. Très localement quelques grains sont plus grossiers(rip-up clasts de 2mm)Les lits (sandstone et argiles) ont une orientation de 60degré A/C. Les lits sont en bandes minces, en bandes larges et en bandes irrégulières.De plus, environ 2% de veinules de QZ et de CB sont présentes irrégulièrement à travers les lits et sont parfois déchirées.Des très fines traces de PY et PO sont disséminées irrégulièrement.Fin du sondage à 453m.





Section :Level :Work place : Leadbetter Initial

Drilled by : Foramex From : 2007-01-17 To : 2007-01-24Geologist : Bernard-Olivier Martel, géo Description date : 2007-01-25

Collar


Comments




671506.0005326501.000327.000








Type Depth Azimuth PlungeFlex-it 549.00m 257.50° -80.19°Flex-it 552.00m 258.78° -80.08°Flex-it 555.00m 258.08° -80.09°Flex-it 558.00m 258.04° -80.06°Flex-it 561.00m 258.90° -79.95°Flex-it 564.00m 258.80° -79.92°Flex-it 567.00m 257.28° -79.88°Flex-it 570.00m 257.72° -79.78°Flex-it 573.00m 259.41° -79.65°Flex-it 576.00m 258.64° -79.62°Flex-it 579.00m 258.98° -79.52°Flex-it 582.00m 257.54° -79.46°Flex-it 585.00m 258.77° -79.32°Flex-it 588.00m 258.64° -79.21°Flex-it 591.00m 257.38° -79.14°Flex-it 594.00m 258.43° -79.10°Flex-it 597.00m 257.01° -79.08°Flex-it 600.00m 257.59° -78.95°Flex-it 603.00m 258.24° -78.81°Flex-it 606.00m 256.87° -78.79°Flex-it 609.00m 256.74° -78.80°



DESCRIPTION

0.00 6.00 OBOverburdenMort terrain

6.00 24.80 V; V3A; PwVolcanic; Andesite/Dacite; PillowRoche volcanique : Pillow lavas andésitiqueComposition: Plagioclase + ferromagnesian phase: biotite, amphibole, pyroxène (±olivine et ±quartz)Lithofacies : pillow lavasFoliation visible à ±50 degrés A/CTexture: aphanitique à fin phénocrys,Alteration: chlorite, séricite et carbonate1% de veinule de Qz-Ca et Qz-Fp.Sulfures (calco, pyrrh) disséminés irrégulièrement (1%)Contact inférieur approximatif.

24.80 25.10 I1NQuartz VeinVeine de quartz-feldspath (?)

25.10 28.70 V; TBLVolcanic; Tuff Breccia/LapillistoneRoche volcanique d'aspect fragmentaire et brèchique : tuff à lapillis transposésGrain size: mud to pebbleComponents:, fragment litique (volcanic felsic(?), quartz veine (?), may be chert), QE, chlorite, séricite, carbonate. Fragments diffus dans la matriceForme : sub arrondie à angulaireLithofacies: Matrix to medium supportedAltteration: chlorite, séricite et carbonateSulfures (chalco,pyrrothine) disséminésFoliation à 50-55 degrés A/CContact inférieur ±net à 55 degrés A/C

28.70 30.00 V; TaVolcanic; Tuff /AshRoche volcanique fragmentaire : Tuff ash-sandGrain size: mud to sandComponents:, fragment litique (volcanic felsic, QE), chlorite, séricite,Forme : sub arondie et allongéeLithofacies: clast supportedAltteration: chlorite, sériciteSulfures (chalco,pyrrothine) disséminésFoliation à ±50 degrés A/CContact inférieur ± approximatif

30.00 31.80 V; TBLVolcanic; Tuff Breccia/LapillistoneRoche volcanique fragmentaire : Tuff à lapillis d'aspect fusionnés et fortement transposée.Grain size: mud à petit cobbleComponents:, fragment litique (volcanic felsic(?), quartz veine (?), may be chert), QE, chlorite, séricite. Fragments très diffus dans la matriceForme : indéterminée, mais allongéeLithofacies: Matrix to medium supportedAltteration: chlorite, sériciteSulfures (chalco,pyrrothine) disséminésFoliation à ±50-55 degrés A/CContact inférieur plutôt net à 55degrés A/C



DESCRIPTION

31.80 34.40 V; Ta; ST; SZVolcanic; Tuff /Ash; Stratified/Laminated; Silicified ZoneRoche volcanique fragmentaire : Tuff ash-sandGrain size: mud to sandComponents:, fragment litique (volcanic felsic, QE), chlorite, séricite,Forme : sub arondie et allongéeLithofacies: clast supportedAltteration: chlorite, sériciteSulfures (chalco,pyrrothine) disséminésFoliation à ±50 degrés A/CContact inférieur ± approximatif

34.40 36.90 V; TBL; I3GVolcanic; Tuff Breccia/Lapillistone; GabbroGabbro ou Roche volcanique fragmentaire d'aspect fortement fusionnée et transposée : Tuff à lapillisGrain size: mud to fine pebbleComponents:, fragment litique (volcanic felsic(?), quartz veine (?), may be chert), QE, chlorite, séricite, carbonate. Fragments très diffus dans la matriceForme : indéterminée, mais allongéeLithofacies: Matrix to medium supportedAltteration: chlorite, sériciteSulfures (chalco,pyrrothine) disséminésFoliation à ±50-55 degrés A/CContact inférieur ± approximatif marquée par changement de couleur

36.90 37.70 V; TBLVolcanic; Tuff Breccia/LapillistoneRoche volcanique d'aspect fragmentaire et brèchique : Tuff à lapillismême que 25.1 à 28.7Grain size: mud to pebbleComponents:, fragment litique (volcanic felsic(?), quartz veine (?), may be chert), QE, chlorite, séricite, carbonate. Fragments diffus dans la matriceForme : sub arrondie à angulaireLithofacies: Matrix to medium supportedAltteration: chlorite, séricite et carbonateSulfures (chalco,pyrrothine) disséminésFoliation à ±50-55 degrés A/CContact inférieur ±net à 50 degrés A/C

37.70 47.70 V; V3A; PwVolcanic; Andesite/Dacite; PillowRoche volcanique : Pillow lavas andésitiqueComposition: Plagioclase + ferromagnesian phase: biotite, amphibole, pyroxène (±olivine et ±quartz)Lithofacies : pillow lavasFoliation visible à ±50 degrés A/CTexture: aphanitique à fin phénocrys,Alteration: chlorite, séricite et carbonate1-2% de veinule de Qz-Ca et Qz-Fp.Sulfures (calco, pyrrh) disséminés irrégulièrement (1%)Contact inférieur approximatif.

47.70 61.50 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique massive : andésite/DaciteLithofacies: massiveTexture : Fine phénocrys, vesiculaire



DESCRIPTION

Alteration: chlorite, carbonate et sériciteSulfures (chalco,pyrrothine) disséminés (<1%) associé au carbonateVeines et veinules : Qz-Fp, Qz-Ca (1-2%)Foliation à 50-55 degrés A/C plus ou moins développéeContact inférieur approximatif

61.50 97.30 V; V3A; PwVolcanic; Andesite/Dacite; PillowRoche volcanique : Pillow lavas andésitiqueComposition: Plagioclase + ferromagnesian phase: biotite, amphibole, pyroxène (±olivine et ±quartz)Lithofacies : pillow lavasTexture: aphanitique à fin phénocrys,Alteration: chlorite, séricite et carbonate1-2% de veinule de Qz-Ca et Qz-Fp.Sulfures (calco, pyrrh) disséminés irrégulièrement (1%)Présence de magnétite par endroitFoliation visible à ±50-55 degrés A/CContact inférieur ±approximatif.

97.30 105.10 V; V3A; PwVolcanic; Andesite/Dacite; PillowRoche volcanique : Pillow lavas andésitique lessivé (couleur jaune-beige)d'aspect brèchique induit par les veines injectéesComposition: ?Lithofacies : pillow lavasTexture: aphanitique, verre volcanique (?)Alteration: séricite,chlorite et carbonate4-5% de veines et veinules de Qz-Ca et Qz-Fp.donnant un aspect brèchiqueSulfures (calco, pyrrh) disséminés irrégulièrement (1%)Foliation ±visible à ±50-55 degrés A/CContact inférieur ±approximatif.

105.10 108.00 V; TBLVolcanic; Tuff Breccia/LapillistoneRochevolcanique d'aspect fragmentaire (incertain) :

108.00 119.00 V; V3A; Pw; Bre; TBLVolcanic; Andesite/Dacite; Pillow; Breccia; Tuff Breccia/LapillistoneRoche volcanique : aphanitic pillow lavas breccia andésitiqueComposition: Plagioclase + ferromagnesian phase: biotite, amphibole, pyroxène (±olivine et ±quartz)Lithofacies : pillow lavas breccia, les marge de pillow semblent contenir des fragmentsTexture: aphanitique, modérément amygdulaireAlteration: chlorite, séricite et carbonate1-2% de veinule de Qz-Ca et Qz-Fp en toile d'araignéeSulfures (calco, pyrrh) disséminés irrégulièrement (1%)Foliation visible à ±50-55 degrés A/CContact inférieur ± net

119.00 123.20 V; TBLVolcanic; Tuff Breccia/LapillistoneRoche volcanique d'aspect fragmentaire : Tuff à lapillis (incertain compte tenu de la présence d'amygdules), donc peut-être pillow brecciaUnité influencée par veine de quartz. Certaines sections présentent des amygdules remplies de silice.Les fragments, de la taille des granules-pebble, sont flous et se confondent même avec des amygdules.Présence de magnétite par endroitFoliation à ±60degrés A/C



DESCRIPTION

Contact inférieur ±approx.123.20 137.60 V; V3A; Mas

Volcanic; Andesite/Dacite; MassiveRoche volcanique massive : aphanitic andésite/DaciteLithofacies: massiveTexture : aphanitic, modérément vesiculaireAlteration: chlorite, carbonate et sériciteSulfures (chalco,pyrrothine) disséminés (<1%) associé au carbonateVeines et veinules : Qz-Fp, Qz-Ca (1-2%)Foliation à 50-55 degrés A/C plus ou moins développéeContact inférieur approximatif

137.60 146.10 V; V3A; Pw; TBLVolcanic; Andesite/Dacite; Pillow; Tuff Breccia/LapillistoneRoche volcanique à passée fragmentaire : andésitique pillow lavas breccia à lapillis sand to cobbleLithofacies : pillow lavas breccia (les marge de pillow semblent contenir des fragments à matrice medium supportedUnité variable ayant à la fois un aspect de pillow, de lapillis mud to cobblerecoupée par des veine de quartz brèchique.Components:, fragment litique (volcanic felsic, QE, chlorite, séricite, carbonate, sulfure.Forme : sub arrondie à sub angulaire et étiréeAlteration: chlorite, séricite et carbonate3-4% de veinule de Qz-Ca et Qz-Fp.Sulfures (calco, pyrrh) disséminés irrégulièrement (1%) et dans les veines (3-4%)Foliation visible à ±50 degrés A/CContact inférieur ± approximatif

146.10 154.80 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique massive : plagioclase phyric andésite/daciteLithofacies: massiveTexture : Fine to medium phénocrys, peu amygdulaireAlteration: chlorite et séricite , carbonate à l'approche du contact inf.Sulfures (chalco,pyrrothine) disséminés (<1%) associé au carbonateMagnétite p/eVeines et veinules : Qz-Fp, Qz-Ca (1-2%)Foliation à 50 degrés A/CContact inférieur approximatif

154.80 155.05 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique massive : andésite amygdulaire (?)

155.05 160.35 V; V3A; PwVolcanic; Andesite/Dacite; PillowRoche volcanique : pillow lavas andésitiqueLithofacies: apparence de pillow lavasTexture : microcristallin peu ou pas vesiculaireAlteration: chlorite et sériciteSulfures (chalco,pyrrothine) disséminés (<1%)Veines et veinules : Qz-Fp, Qz-Ca (1-2%)Foliation à ±50 degrés A/CContact inférieur approximatif

160.35 162.25 I1N; TBLQuartz Vein; Tuff Breccia/Lapillistone



DESCRIPTION

Zone d'injection avec peut-être passage de lapillis granule-pebble162.25 185.46 V; V3B; V3A; Mas

Volcanic; Basalt; Andesite/Dacite; MassiveRoche volcanique massive : Basalte-Andésite massif à passée différentiéeLithofacies: massiveTexture : passage de pyroxène au plagioclase porphyritic à phénocrys fin à medium (<2mm) peu vesiculaireAlteration: chlorite et sériciteSulfures (chalco,pyrrothine) disséminés (<1%)Veines et veinules : Qz-Fp, Qz-Ca (1-2%)Foliation à ±50 degrés A/CContact inférieur ±approximatif

185.46 190.90 V; V3A; PwVolcanic; Andesite/Dacite; PillowRoche volcanique : pillow lavas andésitiqueLithofacies : pillow lavasTexture: aphanitique à fin phénocrys, peu amygdulaireAlteration: ++chlorite, séricite1% de veinule de Qz-Ca et Qz-Fp.Sulfures (calco, pyrrh) disséminés irrégulièrement (1%)Foliation visible à ±50 degrés A/CContact inférieur ±approximatif

190.90 194.90 V; TBL; I1NVolcanic; Tuff Breccia/Lapillistone; Quartz VeinRoche volcanique d'aspect fragmentaire dans une zone de déformation et d'injection : tuff à lapillis injecté et déforméUnité d'aspect à la fois fragmentaire et brèchique puisque recoupée de veine de quartz feldspath-calcite brèchique ou en toile d'araignée.contact inférieur approximatif

194.90 201.85 V; V3A; PwVolcanic; Andesite/Dacite; PillowRoche volcanique : andésite pillow lavasLithofacies : pillow lavasTexture: aphanitique à fin phénocrys, peu amygdulaireAlteration: ++chlorite, séricite et carbonate1% de veinule de Qz-Ca et Qz-Fp.Sulfures (calco, pyrrh) disséminés irrégulièrement (1%)Foliation visible à ±50 degrés A/CContact inférieur ±approximatif avec apparition plusi ntense de patch verte de chlorite (peut-être vesicule de chlorite)

201.85 208.10 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique massive : andésite massiveLithofacies: massiveTexture : microcristallin, amygdulaire (?) ou taches de chloriteAlteration: ++chlorite et sériciteSulfures (chalco,pyrrothine) disséminés (<1%)Veines et veinules : Qz-Fp, Qz-Ca (1%)Foliation à ±50 degrés A/CContact inférieur ± approximatif

208.10 233.00 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique massive : plagioclase phyric andésite/daciteLithofacies: massive



DESCRIPTION

Texture : Fine to medium phénocrys, peu amygdulaireAlteration: chlorite, séricite et carbonateSulfures (chalco,pyrrothine) disséminés (<1%) associé au carbonateMagnétite p/eVeines et veinules : Qz-Fp, Qz-Ca (1-2%)Foliation à ±50-55 degrés A/CContact inférieur plutôtnet à ±50-55 degrés A/C

233.00 260.80 V; V3A; Mas; Ta; TBL; I1N; BreVolcanic; Andesite/Dacite; Massive; Tuff /Ash; Tuff Breccia/Lapillistone; Quartz Vein; BrecciaRoche volcanique apparemment massive à passées fragmentaires probable soit de tuff-ash, de tuff à lapillis et de brèches d'injection de veines.La forte transposition des éléments rend difficile l'interprétation et l'identification des types de dépôts. Distinction entre tuff fin et coulées volcanique imposible.La roche, teintée verte, présente dans l'ensemble des marbrures ou horizons de différentes couleurs. En général passage de gris-vert à beige (surtout près des veines)Il y a présence de mouchetures verte et d'autres beiges avec quartz au centre.Apparence de passages de coulées massives, vacuolaires, de brèches de veines et des lapillis.Passages brèchique de veine et lapillis ± évidentsPassage apparent de lapillis granule-cobble entre 243 et 249Sulfures disséminés (1%) ou dans les veines(3-4%)Veine de qz-ca et qz-fp, qz-tm (5-6%)Altération : chlorite, séricite et carbonateFoliation à ±50degrés A/CContact inférieur plutôt approximatif

260.80 268.70 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique massive : plagioclase phyric andésite/daciteLithofacies: massiveTexture : Fine to medium phénocrys, peu amygdulaireAlteration: chlorite, séricite et carbonateSulfures (chalco,pyrrothine) disséminés (<1%) associé au carbonateMagnétite p/eVeines et veinules : Qz-Fp, Qz-Ca (1-2%)Foliation à ±50-55 degrés A/CContact inférieur plutôtnet à ±50-55 degrés A/C

268.70 324.60 V; V3A; Ta; TBL; I1N; BreVolcanic; Andesite/Dacite; Tuff /Ash; Tuff Breccia/Lapillistone; Quartz Vein; BrecciaRoche volcanique apparemment massive à passées fragmentaires moins présente soit de tuff, de tuff à lapillis et de brèches d'injection de veines (ressemble à 233-260.8)La forte transposition des éléments rend difficile l'interprétation et l'identification des types de dépôts. Distinction entre tuff fin et coulées volcanique imposible.La roche non teintée de vert présente dans l'ensemble des marbrures ou horizons de différentes couleurs. En général, passages brun-beige, gris-moyen, gris pâle et beige (Rare,puisque bcp moins injecté)Il y a présence de mouchetures verte et d'autres beiges (Rares) avec quartz au centre.Apparence de passage de coulées massives, vacuolaires, de brèches de veines et des lapillis.Passages brèchique de veine et lapillis relativement évidentPassage apparent de lapillis granule-pebble entre 268.7 et 271.5Passages brèchique apparent entre 274-275Sulfures disséminés (1%) ou dans les veines(3-4%)Veine de qz-ca et qz-fp, qz-tm (5-6%)Altération : chlorite, séricite et carbonateFoliation à ±50degrés A/C

324.60 347.80 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique massive : aphanitic andésite/DaciteLithofacies: massive



DESCRIPTION

Texture : aphanitic, modérément vesiculaireAlteration: chlorite, carbonate et sériciteSulfures (chalco,pyrrothine) disséminés (<1%) associé au carbonateVeines et veinules : Qz-Fp, Qz-Ca (1%)Foliation à ±50 degrés A/C plus ou moins développéeContact inférieur ± approximatif

347.80 360.50 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique massive : microcristaline andésite/DaciteLithofacies: massiveTexture : microcristalline très vesiculaireAlteration: chlorite, ++carbonate et sériciteSulfures (chalco,pyrrothine) disséminés (<1%) associé au carbonateVeines et veinules : Qz-Fp, Qz-Ca (2%)Foliation à ±50 degrés A/C bien développéeContact inférieur ± approximatif

360.50 377.00 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique massive : andésite/DaciteLithofacies: massiveTexture : aphanitic, modérément vesiculaireAlteration: chlorite, séricite et -- carbonateSulfures (chalco,pyrrothine) disséminés (<1%) associé au carbonateVeines et veinules : Qz-Fp, Qz-Ca (2%)Foliation à ±50 degrés A/C plus ou moins développéeContact inférieur ± approximatif

377.00 388.40 V; V3A; TBL; I1N; BreVolcanic; Andesite/Dacite; Tuff Breccia/Lapillistone; Quartz Vein; BrecciaRoche volcanique apparemment massive à passées fragmentaires de brèches d'injection de veines et peut-être de tuff à pebble-cobble (ressemble à 233-260.8)La roche, teintée verte, présente dans l'ensemble des marbrures ou horizons de différentes couleurs. En général passage de gris-vert à beige vert (surtout près des veines)Il y a présence de mouchetures verte et d'autres plus rares beiges avec quartz au centre.Apparence de passages de coulées massives, vacuolaires, de brèches de veines et peut-être de lapillis, mais incertain pour cedernierPassages brèchique de veine + évidentsSulfures disséminés (1%) ou dans les veines(3-4%)Veine de qz-ca et qz-fp, qz-tm (5-6%)Altération : chlorite, séricite et --carbonateFoliation à ±50degrés A/Ccontact inférieur approximatif

388.40 392.00 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique massive : microcristaline andésite/DaciteLithofacies: massiveTexture : microcristalline très vesiculaireAlteration: chlorite, ++carbonate et sériciteSulfures (chalco,pyrrothine) disséminés (1-2%) associé au carbonateVeines et veinules : Qz-Fp, Qz-Ca (2%)Foliation à ±50 degrés A/C bien développéeContact inférieur ± approximatif

392.00 420.00 V; V3A; Ta; TBLVolcanic; Andesite/Dacite; Tuff /Ash; Tuff Breccia/Lapillistone



DESCRIPTION

Roche volcanique fragmentaire.andésite? tuffGray green color.Grain size: mud to sandComponents: crystal fragment (quartz), lithic fragment (volcanic felsic, more monomictic). Fp-Qz, séricite, chlorite et 2% de sulfure )pyrhotite-pyrite cubique.Lithofacies: stratified (laminated to medium bedded) and non-graded visible. vesicular (moderately)Altteration: chlorite, sériciteContact inférieur approximatif veine de Qz.

420.00 440.00 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique massive : andésite/DaciteLithofacies: massiveTexture : aphanitic (fine max), aphyric and sparsely vesicularAlteration: chlorite, séricite et silicification (Dark gray color associate at dyke)Sulfures (chalco,pyrrothine) disséminés (1-2%) associé au carbonateVeines et veinules : Qz-Fp, Qz-Ca (2%)Foliation à ±50 degrés A/C peu développéeContact inférieur net à 35 degrés

433.70 440.00 SisilicifiedZone silicfiée dû à la mise en place du dyke.

440.00 447.40 I3LLamprophyreLe Dyke est foncé à grain très fin avec quelques traces de porphyres blanc-verdâtre (0.3 à 1 cm)Le contacte sup est à 35 deg Ac et le contact inf est à 40 deg AC

447.40 465.90 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique massive : andésiteLithofacies: massiveTexture : aphanitic (fine max), aphyric and sparsely vesicularAlteration: chlorite, séricite et silicification (Dark gray color associate at dyke)Sulfures (chalco,pyrrothine) disséminés (1-2%) associé au carbonateVeines et veinules : Qz-Fp, Qz-Ca (2%)Foliation à ±50 degrés A/C peu développéeContact inférieur net à 40 degrés

447.40 494.40 SisilicifiedZone silicfiée dû à la mise en place des deux dykes.

465.90 466.20 S5CChert

466.20 467.30 SS; STSandstone; Stratified/Laminated

467.30 494.40 V; V3A; MasVolcanic; Andesite/Dacite; MassiveRoche volcanique massive : andésite/DaciteLithofacies: massiveTexture : aphanitic (fine max), aphyric and sparsely vesicularAlteration: chlorite, séricite et silicification (Dark gray color associate at dyke)Sulfures (chalco,pyrrothine) disséminés (1-2%) associé au carbonate



DESCRIPTION

Veines et veinules : Qz-Fp, Qz-Ca (2%)Foliation à ±50 degrés A/C peu à bien développéeContact inférieur net à 35 degrés

494.40 500.30 CONGLO; DGaConglomerate; Dark GrayConglomérat polymictic medium-supported à matrice gris foncé (Dark Gray matrix) et silicifiée. On observe quelques fragments très flou : brun grisâtre, gris pâle, gris foncé et de couleur vairé : avecalignement de Mx mafique. L'origine des fragments est difficilement identifiable mais probablement volcanique (pyroclastic et coulées), sédimentaire et quelques métamorphiques (peut-être aussimassive flow folié). La morphologie des fragments est généralement sub-arrondis. Les plus gros fragments sont plus arrondis. La grosseur des clast est généralement de 0.5 à 3 cm avec plusieursexceptions supérieures à 3 cm (max 15cm) plus arrondis.Contact inférieur net à 50 degrés

500.30 519.00 I5D; MasDiabase; MassiveDyke mafique. Très massif, non déformé, à grain moyen et de couleur gris foncé. Très magnétique. Réseau de veinules de Cb est présent 1 %. Par endroit moyennement fracturé et présence de chloritedans les fractures.Contact inférieur net à 45 degrés.

519.00 536.50 CONGLO; DGa; PoConglomerate; Dark Gray; PolymicticRoche grise foncée (dark grey) avec 60% de fragments bien arrondis variant de 0.5 à 7 cm.La composition de fragments varient énormément mais les plus gros (2-7) sont composés de volcanites felsiques et mafique et d'intrusifs intermédiaires en plus petites quantitées . Ils sont arrondis àsub-arrondis.Un réseau de veinunles millimétriques de Quarts-Carbonate est présent et compose 5% de l'interval. La carbonatisation est irrégulière (la matrice n'est pas toujours carbonaté) mais quelques fractures etfragments réagissent bien à l'acid.La matrice est plutôt grisâtre et est composée de grains fins à grains moyens.Contact inférieur approximatif.

519.00 536.50 SisilicifiedZone silicfiée dû à la mise en place du dyke.

536.50 549.30 CONGLO; Ga; PoConglomerate; Gray; PolymicticRoche fragmentaireConglomerat polymictic clast-supported. GrayLa matrice, qui correspond à 15 % de la roche, est à grain très fin, de couleur gris, peu chloriteuse et avec 1% de sulfure déssiminé et en amas associée avec carbonate.Plusieurs types de fragments sont observés :1: fragments d'origine volcanique mafique (pyroclastique à eyes-qz et massive), généralement à grain fin, mais parfois à grain moyen. Ils sont de couleur vert, à morphologie sub-anguleux à arrondis.Principalement de taille moyenne (0.5 à 8 cm) et correspondent à 20 % de la roche.2: fragments d'origine intrusif de gabbro à grain fin mésocrate et/ou de gabbro à grain grossier leucocrate. Ils sont de couleur beige avec moucheture verte et à morphologie sub-arrondis à arrondis.Principalement de grande taille (1 à 20 cm) et correspondent à 5 % de la roche.3: fragments d'origine volcanique felsique, à grain fin, de couleur gris moyen, gris pâle et gris jaune. Ils sont à dureté élevée, à morphologie arrondis, principalement de plus petite taille (0.5 à 10 cm) etcorrespondent à 55 % de la roche.4: aucun fragment d'origine détritique sédimentaire n'est observé. Cependant, quelques fragments d'origine chimique sédimentaire (chert) sont relevés (1%).La foliation est visible, par endroit, définie par la matrice et l'alignement de certains clast et à environs 50- degrés.Le réseau de veinules Qz-Cb millimétrique à demi-centimétrique est présent (1-2%)Contact inférieur approximatif.

549.30 568.00 CONGLO; GaG; PoConglo; Gray Green; PolymicticRoche fragmentaireConglomerat polymictic felsic clast-supported. GrayLa matrice, qui correspond à 15 % de la roche, est à grain très fin, de couleur gris, peu chloriteuse et avec 1% de sulfure déssiminé et en amas associée avec carbonate.Plusieurs types de fragments sont observés :1: fragments d'origine volcanique mafique (pyroclastique à eyes-qz et massive), généralement à grain fin, mais parfois à grain moyen. Ils sont de couleur vert, à morphologie sub-anguleux à arrondis.



DESCRIPTION

Principalement de taille moyenne (0.5 à 8 cm) et correspondent à 5 % de la roche.2: fragments d'origine volcanique felsique, à grain fin, de couleur gris moyen, gris pâle et gris jaune. Ils sont à dureté élevée, à morphologie arrondis, principalement de plus petite taille (0.5 à 10 cm) etcorrespondent à 75 % de la roche.4: aucun fragment d'origine détritique sédimentaire n'est observé. Cependant, quelques fragments d'origine chimique sédimentaire (chert) sont relevés (5%).La foliation est visible, par endroit, définie par la matrice et l'alignement de certains clast et à environs 50- degrés.Le réseau de veinules Qz-Cb millimétrique à demi-centimétrique est présent (2%)Contact inférieur net 45 degrés.

568.00 612.00 SS; ARG; STSandstone; Argillite; Stratified/LaminatedRoche sédimentaire : Argilites en alternance avec des bandes de sandstone.Unité composé de lits (0.5-100cm) de sandstone (70%) en alternance avec des lits (0.1-10cm) d'argilites (30%).L'argilite est de couleur gris foncé et aphanitique.Le sandstone est de couleur gris moyen à pâle avec une granulométrie très fine à fine. Les lits sont généralement massifs, mais parfois littées. Très localement quelques grains sont plus grossiers (Qzeyes et rip-up clasts)Les lits sont en bandes minces, en bandes larges et en bandes irrégulières.De plus, environ 2% de veinules de QZ et de CB sont présentes irrégulièrement à travers les lits et sont parfois déchirées.Des très fines traces de PY et PO sont disséminées irrégulièrement.EOH


29

APPENDIX B

DIAMOND DRILL HOLE SECTIONS

f""'"'"

V J~ h f\---- -C\

... 0-'-

I I I ~ I ....,. iii .....

~ ~~ !lr-, , r.; • ~

(:l~ ~'" . '" "'lot",

/' "" "- -.... ,'"

j' ..... ~ ... ... ' ... '"

"'~ " <0,., '" , J. .....

I ~

~ iato 1 l2+OON. NQH0LE8.DIp_I ..... oIong380 __ ~T~ClPnI/:'_

a.bD54II(1_1,~(87m~~O(174mlAZ2'I!I-«l

0 _.1:2!IXI 100 I I I 1--..

--iL -fj

!l !l

~ !l ! I11I2II1711 M i i

~

~~" ~I ~

J It!. .. -'rt ""

' .. ~

,~ ~~

" ~ 2IIftd

'0" ."

,~

I I . i'-I ~

'."

~la*o 1 ,

~."

f "· 1_

L2+OON. NO HOLES. DIp_I_U ..... 980 a_ ~T"""'1p. QIIImt: 1243335 ~/'''II.-''' a.os.1' (DSm)AZ27U-4ID .. Q Ii) 100m I I I _l:ZIII

-'. c- -~

~ 'r ~

~ \~ ~ _l a ~ § ,.

CI ~06-20 Chab DII-35

~ ~C19 1011 p..-.

cotIGI.o: GaG; Pb -..... <l.> S8

Car I 00HclI.a; DGo,' Po 1aL; ....

• ~DQor;Po

~ CQNau>.o;Po

CONcat.o; Go; Po

' ... • 2IXftIrII

~ ' 8Zo, . ~ J~w

,J\, lIB

''''GJ.. /-~~ ,

\oJ\, A4!" .. q; '-..

11D1or11 1

~'4.t-~

. 1/,~o.;Po '~"" -

I I '~Po iii iii

~iato 1 L -11D1or11 UIoOON. NQ Ha..E&. 0-. __ ~ ~ 3!10 dog_. c_ T~ ClaIm" 1243335 ,/ -. 0'eb0II-20 (271m) AZ 270.eo end C_ (CIm)AZ 270 ~

0 110 100m I I _1:2&00 -Q41il

ji=---- -EJ I~ ~ ........ ""1;;)

~I

.-.1 II I I ~

" ~ Q ~ J" ,~ l ~ ~,

~ .. ~ -,

I "' ~~ """, " ... 4t-

" , .. '" .... ....... J. .......

~~

1.

f " '" "" ....

I " ..

)..~. '.", '. .'- ....... ......

,~ 10

I I ''l1o

~ ia~o 1 ,~ 10

j. L3+0UN. NQ HOLES. [lp --1III1IIong 3IIU dog_. ~ T_Ip. a." II< 1_

ChoIJOI>.21 (3CJ3m~ ChIbO&.22 (1_~ a..bO&ZI (138m) I\l. 270..eo 1_ ~;

a _1:2000 1111

I I ~ -

-~

If-~ - - - - - - r- - - - - - --E: - - - - -- - - - -

L I I I I

Cl~. , q,

~<\.

-.

~'1.

~<\.

~'1. ~~

~'1.

.. ~ .... ~~

~ .. -.

I I ~! I.

~ ia*o 1 L.3+5CIN. NQ HOI..E8. '* _ ~ .. ~ 380 a_ a-.oITOIIIIIIhIp. Clam '" ll143)S1!

CII.b05-2ii (214.:i1n) 1>2 2IQ .., .-0 _':2000 1111

I I I M_

1--" I I I~ I I ....

0.-

m-

...-

,~

"qo ;/ ¥~

j ... /

j' /

1>/ ~..,'" / /

l/ -J/~

// "' ...... / /

// // .....

// //

// /;/

li/

ii',

I

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~ Ta Nor 'II!i/IJ

* L.II+aJN. NQ Ha..ElI. DIp ..... -l1li DIng 27D dog_. a... ~ ~ I/: 1_

~ (1B2rn~1>Z 180-4ID

a ~.':ZIXI 100 I I I M_ ,-.

"' .......... ........ -"' ..... -Y;"M< ....

1_

Olbli

I--------r--------------~------------~-:~=-~~"~--------~/~~~~----------------+_----------____ ~--------------_+--------~~oo=~~~ I -- ,

~..,. 1'---. III; 18: ....... ~~:~ , ---~r-

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~m'<h Clt;,~

'''leo , .... /~..,.,.

1__------r-----~,~~------1----------------I---------------~------ ',.,. ' ..

IA+OON. NQ HOLE8. Dip __ ng liang 3111 dog .... ct._ TcMnIhI~. au...: 1243332

ClIob08-4!i (788mL Chob08-48 (124m) ..... Chob08-41 (l020ml A2 no-D

I I iE -7lID1bIi

O ______ S_mM~l:~~------l.00 ttI_

400NartI

Chab~D

JOS

3OONortI

\I; \139; Pw

V;Py

2IIINarII i'illB;Mao

r~~ If, Ta; nrt.

100Nar11

1f,~P\y

1f,~1daa 0N0rtI

/1 ~S;~

\I)R

l I*oto;~

-100Nar11

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-2IIINarII

~~

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/~

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~c ~q.~ .. ~ -7OONortI

~~ .'" ] ; ~

"" ~ ~ ~ 5i 5i iii

. ~., ~ iato1 . /It, ~~ -IO(Ijgrtt

~: L4+QOPII. IIIQ HOI.8!I. Dip _lDDIdng 010"" 3IID dIIg_ a--... r ......... lp. aam" 124S11311

1<J c .. 11011«1 (t 2lIIIm) M. 27D-{fT

I I)

I I I I 0 SO 100m

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pu II II R!<:()o~ §

t;1 f/, f/, t:i

<tl

f--- -- -- - - -- - - - - - - - - -- - - - - - - -- - -

7 {() f;;,

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NB7~ 67<100~ t:i 30 <tl ~~ fl1 fl1 <tl

. .;1'

;n ,. ,. (j ,. w w w

0 0 0 0 0

~ ~ ~

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300Nord 300N rd

CONG l.O:SS;Po;G8

ARG;SS; Si

55 200Nord 200N rd

~ss:8T

100Nord 100N rd

,. ,. w w

~ 0

~ ..... ,>,/311:,..

NQ HOLES. Dip view looking along N 70 degrees. Chabanel Township. Claim #: SSM 21166

'I",'J3B:h\d

l Chab 06-58 (333m) AZ. 198 DIP -87

c\'IJ'60s-&8

ONord ON rd

Scale: 1 :2000 0 10 20 30 40 60 60 70 60 90 100

,. I

,. W 0

W ~ ...- 0

300Nord

200Nord

100Nord

NQ HOLES. Dip view looking along N 70 degrees. Chabanel Township. Claim #: SSM 21166

Chab 06-61 (303m) AZ. 200 DIP -87 and Chab 06-65 (333m) AZ. 145 DIP -85

Scale: 1 :2000 10 ~ ~ ~ ~ ~ ro 00 ~ 100

Meters :n o

I !

1

300Nord

V;V3A;TBL

200Nord

100Nord

_S3S

CHAB 06-65

;n ;n 11l w 0 0 0

~ s:

Ci Cf 011

08

300Nord 300Nord

V;V3A

-,,",or

",V3A

AR,G;SS

200Nord 200Nord

CONGLO;ss

v-,V3Jo.:,f'Y ,toRG;SS

100Nord 11l 100Nord 0 ",V3A

~ _835 V; .... ~

~AAQ

NQ HOLES. Dip view looking along N 70 degrees. Chabanel Township. Claim #: SSM 21166 v;V3A;.Py

M(G;S3S;SS

v;'/'!J':. ...

V;V'JA

Chab 06-62 (309m) AZ. 125 DIP -87 and Chab 06-63 (312m) AZ. 099 DIP -85 _l _ L

CHABO&62 CHAB 06-63

Scale: 1 :2000 0 10 20 30 40 60 60 70 60 90 100 11l

;n w 0 ....... 0 s:

i CI ab06-Q9 CB

"" -.....

V:1IlIA; I'IiL

/::" -~~ . 'lit

~'Gt ...... t_

!:~ ~ 1it-~

~~ .....

~~

" ~~.~ .~

'" ~oI} '~'l>

1f';L, """ I*DrtI

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j. \'. ! J.t_

/..., ''\:')0 ~ ~ "",.

~ iato 1 ,. q., .,.

,,~ LII+tUIL NQ HOLES. ~_IDdU"clIIIDt1g380 ....... aa."'T ..... "1p. Cllliml/; 1_

"" a.t1D6-811 (812m) AZ 222-S7

4 -18~ I I 0 SI 100m

5 E' E' _1::IIIDD

C ab 06-101 08

II; V3A; Pw; an. CNR

II; \I3A; Tal.: Il1o

V; /SA; Mas

v; '3R; lBJ..; QE; Po

V; V ~ IIIas

~: ~ ~ TBL; Qe; Po • y" ... \138; Maa

OJ: 113. • TBl: QE; Po

~~ ~Maa ~V:IS;1.tu OJ: \I3A; vas; PIv

~~:;~ OJ: V3A; 3B; "'-

OJ: \138;,. • lila

II; ~ 118 >; IIIaa

1ffIf.TBt.;8T II; ~ Til: 8L: Mo

Chab 07-104

Cj 08

II; \I3A; Pw

1m

V;V3A;Pv. V; TBt.

II; \I3A; Pw; Bra; TBl

V;T9l

II;V3A:MIII

V; II3A; PIr, TaL

~V3A;,.. )7J.jgt;~1 1'N;~

; 1138; V3A; IIIaa

\; V3A; PIv ' ,,~' TaL; I1N

II3A; PIv V. \I3A; MIll

II""', ...... Ta; TBt.; 11/11: an.

II; \I3A; MI_

\I;~""

II; \I3A; l'BI.. 11/11; Bra \l;V3A;Mae

300Nortt

200Nortt

l00Nortt

ONortt

-100Nortt

~ __ ~ ______________________ +-____________________ -+ ___________ -"~~~~~~ ______________________ +-______ ~-2OON==~ortt~ 'UUS:Po

. CONGt.o; a..; Po

, -~ .. o,,"

Lll+IKIN. NQ Ha..ES. ~ _ -.g .. ng 3IID __ C ... _ T-...h\:I. ClaIm /I: 1243I11III

Chab06-101 (463m) and a.b07-104- (612m)AZ 226 ~

III 100m

30

APPENDIX C

DIAMOND DATA & LABORATORY CERTIFICATES

CHAB 05-08

SAMPLE LAB LAB From To Length Weight MICRONS TOTALNO. CERT metres metres metres Kgs -75 +75 +106 +150 +212 +300 +425 +600 +850 +1180 DIAMONDS15001 SRC 05-605 0.30 3.00 2.70 5.60 n/a 15 14 10 3 1 2 2 0 0 4715002 SRC 05-605 3.00 6.00 3.00 7.10 n/a 18 10 7 1 2 0 1 1 0 4015003 SRC 05-605 6.00 9.00 3.00 6.45 n/a 0 0 0 0 0 0 0 0 0 015004 SRC 05-605 9.00 12.00 3.00 7.25 n/a 4 3 3 2 1 0 0 0 0 1315005 SRC 05-605 12.00 15.00 3.00 6.55 n/a 0 1 3 3 2 0 0 0 0 915006 SRC 05-605 15.00 18.00 3.00 6.75 n/a 19 11 4 2 1 0 0 1 0 3815007 SRC 05-605 18.00 21.00 3.00 7.55 n/a 12 7 10 7 3 1 1 0 0 4115008 SRC 05-605 21.00 22.70 1.70 3.55 n/a 3 2 2 0 2 0 0 0 0 915009 SRC 05-605 22.70 27.00 4.30 4.85 n/a 10 4 6 3 0 1 0 0 0 2415009 SRC 05-605 22.70 27.00 4.30 4.85 n/a 0 0 0 0 0 0 0 0 0 015010 SRC 05-605 27.00 30.00 3.00 6.10 n/a 0 0 0 0 0 0 0 0 0 015011 SRC 05-605 30.00 33.00 3.00 5.35 n/a 0 0 0 0 0 0 0 0 0 015012 SRC 05-605 33.00 36.00 3.00 6.35 n/a 0 0 0 0 0 0 0 0 0 015013 SRC 05-605 36.00 39.00 3.00 6.25 n/a 0 0 0 0 0 0 0 0 0 015014 SRC 05-605 39.00 42.00 3.00 6.65 n/a 0 1 0 0 0 0 0 0 0 115015 SRC 05-605 42.00 45.00 3.00 6.50 n/a 0 0 0 0 0 0 0 0 0 015016 SRC 05-605 45.00 48.00 3.00 4.95 n/a 0 0 0 0 0 0 0 0 0 015017 SRC 05-605 63.00 66.00 3.00 5.80 n/a 0 0 0 0 0 0 0 0 0 0

108.45 81 53 45 21 12 4 4 2 0 222

QC/QA19001 SRC 05-679 3.00 6.00 3.00 5.80 0 5 3 1 1 3 1 0 0 0 1419002 SGS 19002 12.00 15.00 3.00 5.93 0 3 2 0 0 0 2 1 0 0 819003 SGS 19003 18.00 21.00 3.00 5.53 0 3 4 0 3 0 0 0 0 0 1019004 SGS 19004 21.00 22.70 1.70 3.83 2 5 2 2 0 0 0 0 0 0 1119005 SRC 05-679 27.00 30.00 3.00 6.35 0 0 0 0 0 0 0 0 0 0 019006 SGS 19006 42.00 45.00 3.00 5.49 0 0 0 0 0 0 0 0 1 0 119007 SGS 19007 63.00 66.00 3.00 5.46 1 1 0 0 0 0 0 0 0 0 2

38.39 3 17 11 3 4 3 3 1 1 0 46

146.84

SRC Geoanalytical Laboratories125 - 15 Innovation Blvd., Saskatoon, Saskatchewan, S7N 2X8

Tel: (306) 933-8118 Fax: (306) 933-5656 Email: [email protected]

Caustic Fusion Diamond ReportGeos Sciences Inc.Attention: John Ryder

Samples: 18PO #/Project:

August 23, 2005

Report No: 05-605

8) Number of QC/QA Tracers (-300+250microns) Recovered Chemical Treatment (QC 2)

9) Number of synthetic diamonds recovered (whole and fragments) (SYN)

1) Original Sample Weight in kilograms (SWT)

2) Bottom Sieve Size in microns (Sieve)

3) Diamonds > 500 microns (Macro)

4) Diamonds < 500 microns (Micro)

5) Weight of Diamonds > 500 microns in milligrams (Wt+)

6) Weight of Diamonds >75microns < 500 microns in milligrams (Wt-)

7) Number of QC/QA Tracers (-212+180microns) Recovered Fusion (QC 1)

QC 2Sample # SWT Sieve Macro Micro Wt+ Wt- QC 1 SYN

8/1015001 5.60 75 2 45 1.112 0.628 8/10 010/1015002 7.10 75 2 38 1.603 0.396 10/10 010/1015003 6.45 75 0 0 0 0 10/10 010/1015004 7.25 75 0 13 0 0.238 10/10 010/1015005 6.55 75 0 9 0 0.251 10/10 0

10/1015006 6.75 75 1 37 1.794 0.345 10/10 010/1015007 7.55 75 2 39 0.963 0.736 10/10 010/1015008 3.55 75 0 9 0 0.225 10/10 010/1015009 1/2 4.85 75 0 24 0 0.425 10/10 09/1015009 2/2 4.85 75 0 0 0 0 10/10 0

10/1015010 6.10 75 0 0 0 0 8/10 010/1015011 5.35 75 0 0 0 0 10/10 010/1015012 6.35 75 0 0 0 0 10/10 010/1015013 6.25 75 0 0 0 0 10/10 010/1015014 6.65 75 0 1 0 0.006 10/10 0

10/1015015 6.50 75 0 0 0 0 10/10 010/1015016 4.95 75 0 0 0 0 10/10 09/1015017 5.80 75 0 0 0 0 10/10 0

Total carats in this group is: 0.04361

1Page of 10



Caustic Fusion Diamond Description DetailGeos Sciences Inc.Attention: John RyderPO #/Project:

August 23, 2005

Report No: 05-605

Sample Number: 15001

Number of QC/QA Tracers (-300+250microns) Recovered Chemical Treatment (QC 2)

Number of synthetic diamonds recovered (whole and fragments) (SYN)

Original Sample Weight in kilograms (SWT)

Bottom Sieve Size in microns (Sieve)

Diamonds > 500 microns (Macro)

Diamonds < 500 microns (Micro)

Weight of Diamonds > 500 microns in milligrams (Wt+)

Weight of Diamonds >75microns < 500 microns in milligrams (Wt-)

Number of QC/QA Tracers (-212+180microns) Recovered Fusion (QC 1)

5.60

75

2

45

1.112

0.628

8/10

0

8/10

WidthLength Diamond DescriptionHeightIndividual

MicronsFraction Size

mm mm mm mgDiamond Weight

Total DiamondWeight in Fractions

mgDiamond

Count

1 0.86 0.84 0.70 Grey, opaque, polycrystalline aggregate, rough.0.680 1.112+ 6001 0.96 0.60 0.40 Grey, opaque, polycrystalline aggregate, rough.0.432+ 600

1 0.64 0.46 0.40 Yellow, clear, octahedron, stepped/ribbed, serrate laminae.0.174 0.292+ 4251 0.60 0.48 0.30 White, included, polycrystalline aggregate, rough.0.118+ 425

1 0.40 0.24 0.14 Grey, opaque, polycrystalline aggregate, rough.0.043 0.043+ 300

3 0.116+ 212

10 0.100+ 150

14 0.054+ 106

15 0.023+ 75

Total octacarats in this sample is: 870,000.00

2Page of 10




August 23, 2005

Report No: 05-605











7.10

75

2

38

1.603

0.396

10/10

0

10/10





mgDiamond

Count

1 1.34 0.80 0.72 Colorless, clear, distorted, broken, pits, rough.1.196 1.196+ 850

1 1.00 0.70 0.54 Colorless, clear, fragment, broken, rough.0.407 0.407+ 600

1 0.42 0.40 0.36 Yellow, clear, octahedron, twinned, stepped/ribbed, serratelaminae.

0.133 0.208+ 300

1 0.42 0.38 0.32 Colorless, clear, octahedron, stepped/ribbed, shield laminae.0.075+ 300

1 0.038+ 212

7 0.083+ 150

10 0.038+ 106

18 0.029+ 75


3Page of 10




August 23, 2005

Report No: 05-605











7.25

75

0

13

0

0.238

10/10

0

10/10





mgDiamond

Count

1 0.52 0.40 0.34 Colorless, included, distorted, pits, lamination.0.124 0.124+ 300

2 0.059+ 212

3 0.031+ 150

3 0.017+ 106

4 0.007+ 75


4Page of 10




August 23, 2005

Report No: 05-605











6.55

75

0

9

0

0.251

10/10

0

10/10





mgDiamond

Count

1 0.30 0.22 0.18 Colorless, included, octahedron, resorbed.0.072 0.136+ 3001 0.38 0.22 0.16 Amber, clear, octahedron, twinned, stepped/ribbed, pits.0.064+ 300

3 0.080+ 212

3 0.025+ 150

1 0.010+ 106


5Page of 10




August 23, 2005

Report No: 05-605











6.75

75

1

37

1.794

0.345

10/10

0

10/10





mgDiamond

Count

1 1.52 1.00 0.60 Amber, frosted, octahedroid, resorbed, stepped/ribbed, etchedtrigons, rough.

1.794 1.794+ 850

1 0.60 0.44 0.38 Colorless, included, octahedral, broken, resorbed.0.148 0.148+ 300

2 0.069+ 212

4 0.050+ 150

11 0.046+ 106

19 0.032+ 75

Total octacarats in this sample is: 1,069,500.00

6Page of 10




August 23, 2005

Report No: 05-605











7.55

75

2

39

0.963

0.736

10/10

0

10/10





mgDiamond

Count

1 1.02 0.80 0.66 Yellow, cloudy, distorted, broken, pits, rough.0.768 0.768+ 600

1 0.72 0.54 0.34 Yellow, clear, fragment, rough, lamination.0.195 0.195+ 425

3 0.252+ 300

7 0.300+ 212

10 0.124+ 150

7 0.034+ 106

12 0.026+ 75


7Page of 10




August 23, 2005

Report No: 05-605











3.55

75

0

9

0

0.225

10/10

0

10/10





mgDiamond

Count

1 0.50 0.40 0.32 Yellow, included, distorted, stepped/ribbed, shield laminae, pits.0.127 0.183+ 3001 0.54 0.36 0.20 Colorless, frosted, octahedron, broken, shield laminae, etched

trigons.0.056+ 300

2 0.021+ 150

2 0.011+ 106

3 0.010+ 75


8Page of 10




August 23, 2005

Report No: 05-605

Sample Number: 15009 1/2










4.85

75

0

24

0

0.425

10/10

0

10/10





mgDiamond

Count

1 0.60 0.50 0.42 Colorless, frosted, octahedron, resorbed, low relief surfaces.0.185 0.185+ 425

3 0.126+ 212

6 0.072+ 150

4 0.026+ 106

10 0.016+ 75


9Page of 10




August 23, 2005

Report No: 05-605











6.65

75

0

1

0

0.006

10/10

0

10/10





mgDiamond

Count

1 0.006+ 106


10Page of 10



Caustic Fusion Diamond ReportDianor Resources Inc.Attention: John Ryder


October 28, 2005

Report No: 05-679











10/1019001 5.80 75 0 14 0 1.774 10/10 010/1019005 6.35 75 0 0 0 0 10/10 0


1Page of 2



Caustic Fusion Diamond Description DetailDianor Resources Inc.Attention: John RyderPO #/Project:

October 28, 2005

Report No: 05-679











5.80

75

0

14

0

1.774

10/10

0

10/10





mgDiamond

Count

1 0.54 0.46 0.40 Green, opaque, cubic, resorbed, pits, crescentic steps.1.247 1.247+ 425

1 0.62 0.48 0.32 Colorless, clear, octahedroid, twinned, stepped/ribbed, serratelaminae, rough.

0.161 0.437+ 300

1 0.38 0.32 0.32 Green, opaque, cubic, resorbed, pits, rough.0.146+ 3001 0.60 0.36 0.30 Colorless, frosted, octahedral, twinned, broken, stepped/ribbed,

serrate laminae.0.130+ 300

1 0.046+ 212

1 0.020+ 150

3 0.014+ 106

5 0.010+ 75


2Page of 2

Lakefield Research Limited185 Concession St., Box 4300 Tel: (705) 652-2112Lakefield, Ontario Fax: (705) 652-3123K0L 2H0, CANADA

DIAMOND RECOVERY BY CAUSTIC DISSOLUTIONProject: 8901-463 Date: August 31, 2005Client: Geos-Sciences Inc. LIMS No. MI0001-AUG05

Sample No. 19007

Diamond Number of Group Weight Group CaratsSize Fractions Stones in Group (mg) (calculated)

+ 4.75 mm 0 0.000 0.000- 4.75 / + 3.35 mm 0 0.000 0.000- 3.35 / + 2.36 mm 0 0.000 0.000- 2.36 / + 1.70 mm 0 0.000 0.000- 1.70 / + 1.18 mm 0 0.000 0.000- 1.18 / + 0.85 mm 0 0.000 0.000-850 / + 600 µm 0 0.000 0.000-600 / + 425 µm 0 0.000 0.000-425 / + 300 µm 0 0.000 0.000-300 / +212 µm 0 0.000 0.000-212 / +150 µm 0 0.000 0.000-150 / +105 µm 0 0.000 0.000-105 / + 74 µm 1 0.006 0.000

- 74 µm 1 0.005 0.000TOTAL 2 0.011 0.000

Sample Weight: 5.46 kg Total Weight (carats)*: 0.000Number of Syndites: 0 Number of Diamonds: 2

* Total Weight (carats) was calculated from mg weights. All reported mg weights are weighed to within 0.002 mg.

Note: Lakefield Research Limited is not responsible for the determination of the origin, quality or value of any diamonds recovered. Each +35 mesh (Tyler sieve; +0.420 mm) stone was individually weighed, and the -35 mesh stones were weighed in groups.

Accredited by the Standards Council of Canada to the ISO/IEC Guide 25 standard for specific registered tests.

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Sample No. 19006



- 74 µm 0 0.000 0.000TOTAL 1 1.095 0.005





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Sample No. 19004



- 74 µm 2 0.010 0.000TOTAL 11 0.049 0.000





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Sample No. 19003



- 74 µm 0 0.000 0.000TOTAL 10 0.186 0.001





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Sample No. 19002



- 74 µm 0 0.000 0.000TOTAL 8 1.152 0.006





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Page 1

CHAB 05-09

SAMPLE LAB LAB From To Length Weight MICRONS TOTALNO. CERT metres metres metres Kgs -75 +75 +106 +150 +212 +300 +425 +600 +850 +1180 DIAMONDS15018 SRC 05-734 3.00 6.00 3.00 6.05 n/a 4 4 4 3 1 1 0 0 0 1715019 SRC 05-734 6.00 9.00 3.00 6.15 n/a 13 6 5 0 1 1 0 0 0 2615020 SRC 05-734 9.00 12.00 3.00 6.75 n/a 8 5 5 0 5 0 0 0 0 2315021 SRC 05-734 12.00 15.00 3.00 6.30 n/a 15 10 2 4 3 2 0 0 0 3615022 SRC 05-734 15.00 18.00 3.00 6.65 n/a 15 8 13 7 9 3 0 0 0 5515023 SRC 05-734 18.00 21.00 3.00 6.90 n/a 14 4 6 11 7 0 2 1 0 4515024 SRC 05-734 21.00 24.00 3.00 6.70 n/a 9 5 5 1 0 1 0 0 0 2115025 SGS 15025 24.00 27.00 3.00 6.38 2 0 6 2 3 3 0 0 0 0 1615026 SRC 05-734 27.00 30.00 3.00 6.80 n/a 18 9 12 5 2 1 0 0 0 4715027 SRC 05-734 30.00 33.00 3.00 6.70 n/a 17 10 5 14 4 0 1 0 0 5115028 SRC 05-734 33.00 36.00 3.00 6.85 n/a 13 10 5 2 0 1 1 1 1 3415029 SRC 05-734 36.00 39.00 3.00 6.60 n/a 27 30 27 6 6 2 0 0 0 9815030 SRC 05-734 39.00 42.00 3.00 6.70 n/a 11 3 3 2 3 0 1 0 0 2315031 SRC 05-734 42.00 45.00 3.00 6.45 n/a 12 6 9 1 3 1 0 0 0 3215032 SRC 05-734 45.00 48.00 3.00 6.80 n/a 14 5 3 1 3 0 0 0 0 2615033 SRC 05-734 48.00 51.00 3.00 6.25 n/a 5 8 4 1 1 0 0 0 0 1915034 SRC 05-734 51.00 54.00 3.00 6.98 n/a 7 3 5 3 1 0 0 0 0 1915035 SRC 05-734 54.00 57.10 3.10 6.98 n/a 15 3 2 2 0 1 1 0 0 2415036 SRC 05-734 57.10 60.00 2.90 6.25 n/a 0 0 0 0 0 0 0 0 0 015037 SRC 05-734 60.00 63.00 3.00 6.50 n/a 0 0 0 0 0 0 0 0 0 015038 SRC 05-734 63.00 66.00 3.00 6.60 n/a 0 0 0 0 0 0 0 0 0 015039 SGS 15039 66.00 69.00 3.00 6.75 2 0 0 0 2 0 0 0 0 0 4

66.00 145.09 4 217 135 117 68 52 14 6 2 1 616QA/QC

19008 SRC 05-734 9.00 12.00 3.00 7.30 0 7 8 4 3 3 0 0 0 0 2519009 SGS 19009 24.00 27.00 3.00 7.09 0 16 18 5 4 3 1 2 0 0 4919010 SGS 19010 39.00 42.00 3.00 6.85 0 4 6 3 2 4 3 2 0 0 2419011 SGS 19011 42.00 45.00 3.00 7.57 2 3 5 3 3 0 1 0 1 0 1819012 SRC 05-734 54.00 57.10 3.10 7.10 0 11 8 6 2 4 2 0 0 0 3319013 SGS 19013 66.00 69.00 3.00 6.69 0 0 0 0 0 0 0 0 0 0 0

18.10 42.60 2 41 45 21 14 14 7 4 1 0 149



Caustic Fusion Diamond ReportGeos Sciences Inc.Attention: Serge Caron


November 14, 2005

Report No: 05-734











10/100015018 6.05 75 1 16 0.197 0.296 10/10 010/100015019 6.15 75 0 26 0 0.362 10/10 010/100015020 6.75 75 0 23 0 0.564 10/10 010/100015021 6.30 75 1 35 0.427 0.741 10/10 09/100015022 6.65 75 1 54 0.298 1.729 10/10 0

10/100015023 6.90 75 3 42 2.748 1.281 8/10 010/100015024 6.70 75 0 21 0 0.336 10/10 010/100015026 6.80 75 0 47 0 0.765 10/10 010/100015027 6.70 75 1 50 1.230 1.152 9/10 010/100015028 6.85 75 3 31 16.645 0.357 10/10 0

10/100015029 6.60 75 1 97 0.378 1.603 10/10 010/100015030 6.70 75 1 22 0.602 0.371 10/10 010/100015031 6.45 75 1 31 0.308 0.435 10/10 010/100015032 6.80 75 0 26 0 0.506 10/10 010/100015033 6.25 75 0 19 0 0.295 10/10 0

10/100015034 6.98 75 0 19 0 0.282 10/10 010/100015035 6.98 75 2 22 0.627 0.178 10/10 010/100015036 6.25 75 0 0 0 0 10/10 010/100015037 6.50 75 0 0 0 0 10/10 010/100015038 6.60 75 0 0 0 0 10/10 0

10/1019008 7.30 75 0 25 0 0.757 10/10 09/1019012 7.10 75 1 32 0.374 0.767 8/10 0


1Page of 23



Caustic Fusion Diamond Description DetailGeos Sciences Inc.Attention: Serge CaronPO #/Project:

November 14, 2005

Report No: 05-734











6.05

75

1

16

0.197

0.296

10/10

0

10/10





mgDiamond

Count

1 0.64 0.54 0.38 Yellow, included, octahedron, stepped/ribbed, lamination.0.197 0.197+ 425

1 0.54 0.50 0.36 Amber, clear, aggregate, stepped/ribbed, rough.0.125 0.125+ 300

3 0.091+ 212

4 0.054+ 150

4 0.017+ 106

4 0.009+ 75


2Page of 23




November 14, 2005

Report No: 05-734











6.15

75

0

26

0

0.362

10/10

0

10/10





mgDiamond

Count

1 0.54 0.46 0.44 Colorless, frosted, dodecahedron, broken, pits, hillocks,lamination.

0.199 0.199+ 425

1 0.46 0.36 0.28 Colorless, frosted, dodecahedron, broken, hillocks, rough,lamination.

0.079 0.079+ 300

5 0.035+ 150

6 0.027+ 106

13 0.022+ 75


3Page of 23




November 14, 2005

Report No: 05-734











6.75

75

0

23

0

0.564

10/10

0

10/10





mgDiamond

Count

1 0.60 0.42 0.30 Colorless, clear, irregular, resorbed, serrate laminae, etchedtrigons, rough.

0.159 0.465+ 300

1 0.50 0.40 0.36 Yellow, clear, thh, resorbed, low relief surfaces.0.141+ 3001 0.76 0.60 0.40 Colorless, clear, octahedron, shield laminae, etched trigons.0.085+ 3001 0.70 0.40 0.30 Colorless, clear, fragment, broken, serrate laminae.0.079+ 300

1 0.30 0.30 0.16 Grey, opaque, aggregate, broken.0.021+ 300

5 0.054+ 150

5 0.027+ 106

8 0.018+ 75


4Page of 23




November 14, 2005

Report No: 05-734











6.30

75

1

35

0.427

0.741

10/10

0

10/10





mgDiamond

Count

1 0.58 0.54 0.50 Colorless, opaque, cubic, lamination.0.427 0.680+ 4251 0.80 0.50 0.44 White, included, octahedroid, broken, serrate laminae.0.253+ 425

1 0.64 0.50 0.28 Colorless, cloudy, octahedron, broken, serrate laminae, pits.0.140 0.271+ 3001 0.54 0.44 0.26 White, cloudy, octahedron, broken, serrate laminae, pits,

lamination.0.066+ 300

1 0.40 0.30 0.24 Colorless, included, octahedroid, stepped/ribbed, serratelaminae, pits, rough, lamination.

0.065+ 300

4 0.123+ 212

2 0.031+ 150

10 0.035+ 106

15 0.028+ 75


5Page of 23




November 14, 2005

Report No: 05-734











6.65

75

1

54

0.298

1.729

10/10

0

9/10





mgDiamond

Count

1 0.68 0.66 0.56 Yellow, clear, octahedron, broken, stepped/ribbed, shieldlaminae, etched trigons, rough.

0.298 0.764+ 425

1 0.72 0.52 0.50 Green, included, octahedron, stepped/ribbed, shield laminae,rough.

0.256+ 425

1 0.58 0.52 0.44 White, frosted, dodecahedron, hillocks, rough.0.210+ 425

1 0.60 0.42 0.40 Colorless, frosted, fragment, broken, stepped/ribbed, shieldlaminae, etched trigons.

0.180 0.777+ 300

1 0.36 0.34 0.34 Green, opaque, cubic, rough.0.088+ 3001 0.46 0.42 0.30 Grey, included, aggregate, broken, rough.0.086+ 3001 0.66 0.42 0.20 Pink, frosted, fragment, broken, rough, lamination.0.082+ 3001 0.58 0.54 0.16 White, cloudy, fragment, broken, rough, lamination.0.078+ 300

1 0.60 0.36 0.30 Pink, frosted, fragment, broken, pits, rough.0.073+ 3001 0.42 0.40 0.38 White, frosted, octahedroid, resorbed, hillocks.0.073+ 3001 0.50 0.44 0.28 Amber, included, fragment, broken, etched trigons, rough.0.059+ 3001 0.36 0.34 0.30 Yellow, opaque, octahedron, stepped/ribbed, shield laminae,

rough.0.058+ 300

7 0.236+ 212

6Page of 23




November 14, 2005

Report No: 05-734






mgDiamond

Count

13 0.182+ 150

8 0.041+ 106

15 0.027+ 75


7Page of 23




November 14, 2005

Report No: 05-734











6.90

75

3

42

2.748

1.281

8/10

0

10/10





mgDiamond

Count

1 1.22 1.02 0.80 Yellow, opaque, octahedroid, stepped/ribbed, hillocks, rough.1.613 1.613+ 850

1 0.94 0.90 0.72 Amber, included, fragment, broken, serrate laminae, rough,lamination.

0.585 1.135+ 600

1 0.90 0.86 0.46 Colorless, clear, distorted, stepped/ribbed, pits, hillocks, rough.0.550+ 600

1 0.74 0.48 0.28 Amber, clear, fragment, broken, hillocks, rough.0.156 0.794+ 3001 0.60 0.48 0.36 Colorless, clear, octahedral, broken, stepped/ribbed, serrate

laminae, shield laminae.0.154+ 300

1 0.62 0.44 0.42 Amber, frosted, octahedroid, broken, stepped/ribbed, shieldlaminae, hillocks, rough.

0.137+ 300

1 0.58 0.40 0.40 Amber, milky, octahedron, twinned, stepped/ribbed, shieldlaminae, pits, rough.

0.126+ 300

1 0.52 0.40 0.34 Amber, clear, octahedroid, broken, stepped/ribbed, rough,lamination.

0.086+ 300

1 0.48 0.40 0.28 White, frosted, distorted, resorbed, hillocks.0.076+ 3001 0.52 0.34 0.30 Colorless, frosted, distorted, stepped/ribbed, pits, rough.0.059+ 300

11 0.370+ 212

8Page of 23




November 14, 2005

Report No: 05-734






mgDiamond

Count

6 0.072+ 150

4 0.021+ 106

14 0.024+ 75


9Page of 23




November 14, 2005

Report No: 05-734











6.70

75

0

21

0

0.336

10/10

0

10/10





mgDiamond

Count

1 0.68 0.52 0.38 Amber, frosted, fragment, broken, rough, lamination.0.220 0.220+ 425

1 0.018+ 212

5 0.053+ 150

5 0.028+ 106

9 0.017+ 75


10Page of 23




November 14, 2005

Report No: 05-734











6.80

75

0

47

0

0.765

10/10

0

10/10





mgDiamond

Count

1 0.72 0.52 0.32 Yellow, frosted, fragment, broken, stepped/ribbed, pits.0.214 0.214+ 425

1 0.44 0.40 0.24 Amber, clear, octahedron, twinned, broken, stepped/ribbed, pits,rough.

0.071 0.129+ 300

1 0.42 0.34 0.30 Colorless, clear, octahedron, stepped/ribbed, shield laminae,pits, rough.

0.058+ 300

5 0.201+ 212

12 0.154+ 150

9 0.037+ 106

18 0.030+ 75


11Page of 23




November 14, 2005

Report No: 05-734











6.70

75

1

50

1.230

1.152

9/10

0

10/10





mgDiamond

Count

1 1.12 0.80 0.78 Colorless, clear, octahedron, broken, shield laminae, hillocks.1.230 1.230+ 600

1 0.76 0.38 0.36 White, milky, cubic, pits, rough.0.221 0.481+ 3001 0.40 0.38 0.36 White, frosted, cubic, pits.0.136+ 3001 0.44 0.40 0.32 Yellow, clear, fragment, broken, stepped/ribbed, hillocks, rough,

lamination.0.069+ 300

1 0.44 0.38 0.30 Yellow, clear, fragment, broken, rough.0.055+ 300

14 0.492+ 212

5 0.088+ 150

10 0.061+ 106

17 0.030+ 75


12Page of 23




November 14, 2005

Report No: 05-734











6.85

75

3

31

16.645

0.357

10/10

0

10/10





mgDiamond

Count

1 2.60 2.24 1.54 Yellow, included, octahedroid, stepped/ribbed, etched trigons,pits, hillocks.

13.910 13.910+1180

1 1.38 1.30 1.28 Colorless, frosted, octahedron, stepped/ribbed, shield laminae,pits, hillocks.

2.077 2.077+ 850

1 0.96 0.76 0.60 Colorless, clear, octahedral, twinned, broken, stepped/ribbed.0.658 0.658+ 600

1 0.58 0.48 0.38 Colorless, clear, octahedron, broken, hillocks, lamination.0.139 0.139+ 425

2 0.073+ 212

5 0.076+ 150

10 0.045+ 106

13 0.024+ 75


13Page of 23




November 14, 2005

Report No: 05-734











6.60

75

1

97

0.378

1.603

10/10

0

10/10





mgDiamond

Count

1 0.64 0.54 0.54 Amber, octahedron, stepped/ribbed, serrate laminae, shieldlaminae.

0.378 0.591+ 425

1 0.84 0.48 0.30 Grey, opaque, irregular, resorbed, pits, rough.0.213+ 425

1 0.62 0.32 0.26 Colorless, clear, fragment, lamination.0.152 0.687+ 3001 0.64 0.36 0.26 Colorless, included, octahedron, twinned, stepped/ribbed, etched

trigons.0.128+ 300

1 0.54 0.36 0.34 Colorless, clear, octahedral, stepped/ribbed, serrate laminae.0.118+ 3001 0.60 0.38 0.32 Amber, included, octahedron, resorbed, pits, hillocks.0.108+ 3001 0.54 0.38 0.34 Colorless, included, octahedral, broken.0.098+ 300

1 0.44 0.36 0.24 White, clear, thh, resorbed, hillocks.0.083+ 300

6 0.191+ 212

27 0.342+ 150

30 0.119+ 106

27 0.051+ 75

14Page of 23




November 14, 2005

Report No: 05-734



15Page of 23




November 14, 2005

Report No: 05-734











6.70

75

1

22

0.602

0.371

10/10

0

10/10





mgDiamond

Count

1 0.80 0.76 0.60 Colorless, clear, octahedron, stepped/ribbed, serrate laminae,shield laminae.

0.602 0.602+ 600

1 0.56 0.40 0.20 White, included, thh, broken, resorbed, low relief surfaces.0.086 0.211+ 3001 0.40 0.36 0.30 White, opaque, thh, broken, low relief surfaces.0.066+ 3001 0.40 0.40 0.30 Colorless, clear, octahedron, stepped/ribbed, serrate laminae,

shield laminae.0.059+ 300

2 0.067+ 212

3 0.043+ 150

3 0.026+ 106

11 0.024+ 75


16Page of 23




November 14, 2005

Report No: 05-734











6.45

75

1

31

0.308

0.435

10/10

0

10/10





mgDiamond

Count

1 0.54 0.50 0.48 White, cloudy, cubic, resorbed, pointed plates.0.308 0.308+ 425

1 0.50 0.34 0.32 Colorless, clear, octahedron, twinned, stepped/ribbed.0.100 0.269+ 3001 0.64 0.38 0.20 Colorless, clear, fragment, lamination.0.091+ 3001 0.36 0.34 0.24 Yellow, opaque, cubic, pits.0.078+ 300

1 0.044+ 212

9 0.081+ 150

6 0.025+ 106

12 0.016+ 75


17Page of 23




November 14, 2005

Report No: 05-734











6.80

75

0

26

0

0.506

10/10

0

10/10





mgDiamond

Count

1 0.38 0.36 0.30 Amber, frosted, cubic, broken, rough.0.127 0.324+ 3001 0.60 0.36 0.30 Colorless, clear, fragment, broken, stepped/ribbed, hillocks.0.123+ 3001 0.50 0.38 0.26 Colorless, clear, fragment, broken, hillocks, rough.0.074+ 300

1 0.086+ 212

3 0.048+ 150

5 0.027+ 106

14 0.021+ 75


18Page of 23




November 14, 2005

Report No: 05-734











6.25

75

0

19

0

0.295

10/10

0

10/10





mgDiamond

Count

1 0.30 0.30 0.30 Yellow, frosted, cubic, rough.0.105 0.105+ 300

1 0.060+ 212

4 0.062+ 150

8 0.052+ 106

5 0.016+ 75


19Page of 23




November 14, 2005

Report No: 05-734











6.98

75

0

19

0

0.282

10/10

0

10/10





mgDiamond

Count

1 0.66 0.36 0.32 Colorless, clear, octahedron, twinned, stepped/ribbed, serratelaminae, shield laminae.

0.140 0.140+ 300

3 0.060+ 212

5 0.038+ 150

3 0.023+ 106

7 0.021+ 75


20Page of 23




November 14, 2005

Report No: 05-734











6.98

75

2

22

0.627

0.178

10/10

0

10/10





mgDiamond

Count

1 0.80 0.78 0.40 Yellow, milky, fragment, broken, rough, lamination.0.386 0.386+ 600

1 0.74 0.60 0.40 Colorless, frosted, fragment, broken, hillocks.0.241 0.241+ 425

2 0.107+ 212

2 0.026+ 150

3 0.017+ 106

15 0.028+ 75


21Page of 23




November 14, 2005

Report No: 05-734











7.30

75

0

25

0

0.757

10/10

0

10/10





mgDiamond

Count

1 0.72 0.50 0.30 Colorless, clear, distorted, stepped/ribbed, serrate laminae.0.158 0.369+ 3001 0.54 0.40 0.38 Colorless, clear, distorted, resorbed, shield laminae.0.124+ 3001 0.30 0.30 0.30 Colorless, opaque, cubic, rough.0.087+ 300

3 0.212+ 212

4 0.084+ 150

8 0.070+ 106

7 0.022+ 75


22Page of 23




November 14, 2005

Report No: 05-734











7.10

75

1

32

0.374

0.767

8/10

0

9/10





mgDiamond

Count

1 0.56 0.54 0.48 Yellow, clear, cubic, resorbed, crescent steps, pointed plates.0.374 0.582+ 4251 0.56 0.48 0.18 White, clear, aggregate, resorbed, stepped/ribbed, serrate

laminae, hillocks.0.208+ 425

1 0.56 0.36 0.36 Colorless, clear, distorted, stepped/ribbed.0.147 0.375+ 3001 0.58 0.38 0.28 Colorless, clear, aggregate, stepped/ribbed, serrate laminae.0.086+ 3001 0.42 0.34 0.30 Colorless, clear, dodecahedron, broken, lamination.0.071+ 3001 0.32 0.32 0.32 White, cloudy, cubic, resorbed, low relief surfaces.0.071+ 300

2 0.050+ 212

6 0.063+ 150

8 0.049+ 106

11 0.022+ 75


23Page of 23


DIAMOND RECOVERY BY CAUSTIC DISSOLUTIONProject: 8901-463 Date: August 24, 2005Client: Geos-Sciences Inc. LIMS No. MI0015-JUL05

Sample No. 15025



- 74 µm 2 0.009 0.000TOTAL 16 0.566 0.003





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Sample No. 15039



- 74 µm 2 0.008 0.000TOTAL 4 0.070 0.000





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Sample No. 19009



- 74 µm 0 0.000 0.000TOTAL 49 2.218 0.011





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Sample No. 19010



- 74 µm 0 0.000 0.000TOTAL 24 3.170 0.016





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Sample No. 19011



- 74 µm 2 0.008 0.000TOTAL 18 2.225 0.011





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Sample No. 19013



- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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CHAB 05-10

SAMPLE LAB LAB From To Length Weight MICRONS TOTALNO. CERT metres metres metres Kgs -75 +75 +106 +150 +212 +300 +425 +600 +850 +1180 +1700 DIAMONDS15040 SRC 05-809 0.70 3.00 2.30 4.00 0 12 5 6 2 2 0 1 0 0 0 2815041 SRC 05-809 3.00 6.00 3.00 6.50 0 7 8 7 5 1 0 0 0 0 0 2815042 SRC 05-809 6.00 9.00 3.00 6.50 33 14 23 9 4 1 0 0 1 0 8515043 SRC 05-809 9.00 12.00 3.00 7.10 19 13 7 10 2 6 4 0 0 1 6215044 SRC 05-809 12.00 15.00 3.00 7.00 10 15 3 2 2 0 0 0 0 0 3215045 SGS 15045 15.00 18.00 3.00 7.34 7 47 22 10 1 1 0 1 0 0 0 8215046 SRC 05-809 18.00 21.00 3.00 6.70 0 1 2 1 0 1 2 0 0 0 715047 SRC 05-809 21.00 24.00 3.00 7.20 6 1 0 3 1 1 1 0 0 0 1315048 SRC 05-809 24.00 27.00 3.00 6.10 15 6 4 2 3 1 0 0 0 0 3115049 SRC 05-809 27.00 30.00 3.00 7.30 2 3 0 4 5 2 0 1 0 0 1715050 SRC 05-809 30.00 33.00 3.00 6.85 10 1 0 3 2 0 0 0 0 0 1615051 SRC 05-809 33.00 36.00 3.00 6.55 10 6 5 4 4 2 0 0 0 0 3115052 SRC 05-809 36.00 39.00 3.00 7.20 25 11 4 10 5 2 1 0 0 0 5815053 SRC 05-809 39.00 42.00 3.00 6.75 41 32 13 3 0 1 0 0 0 0 9015054 SRC 05-809 42.00 45.00 3.00 7.00 6 3 2 2 0 0 0 0 0 0 1315055 SRC 05-809 45.00 48.00 3.00 7.00 14 2 1 3 0 1 0 0 0 0 2115056 SRC 05-809 48.00 51.00 3.00 6.80 12 1 4 0 2 1 0 0 0 0 2015057 SRC 05-809 51.00 54.00 3.00 7.10 3 2 2 0 2 0 1 0 0 0 1015058 SRC 05-809 54.00 57.00 3.00 6.55 13 7 5 4 4 0 0 0 0 0 3315059 SRC 05-809 57.00 60.00 3.00 7.45 17 7 2 4 3 0 0 0 0 0 3315060 SGS 15060 60.00 63.00 3.00 7.24 0 4 7 6 2 2 0 0 0 0 0 2115061 SRC 05-809 63.00 66.00 3.00 7.25 18 2 2 2 0 0 1 1 0 0 2615062 SRC 05-809 66.00 69.00 3.00 6.85 3 1 1 3 0 1 0 0 0 0 915063 SRC 05-809 69.00 72.00 3.00 6.95 6 3 0 0 0 1 0 0 0 0 1015064 SRC 05-809 72.00 75.00 3.00 7.05 7 2 2 0 1 0 0 0 0 0 1215065 SRC 05-809 75.00 78.00 3.00 7.25 0 0 2 1 0 0 0 0 0 0 315066 SRC 05-809 78.00 81.75 3.75 9.00 8 6 1 3 0 0 0 0 0 0 1815067 SRC 05-809 81.75 84.00 2.25 5.10 6 2 0 1 0 0 0 0 0 0 915068 SRC 05-809 84.00 87.00 3.00 6.60 7 2 5 2 0 0 0 0 0 0 1615069 SRC 05-809 87.00 90.00 3.00 7.00 16 5 5 3 4 0 0 0 0 0 3315070 SRC 05-809 90.00 93.00 3.00 7.25 61 38 13 5 3 2 0 1 0 0 12315071 SRC 05-809 93.00 96.00 3.00 7.00 19 17 10 8 2 2 0 0 0 0 5815072 SRC 05-809 96.00 99.00 3.00 7.80 13 9 9 3 2 1 0 0 0 0 3715073 SRC 05-809 99.00 102.00 3.00 6.60 8 5 1 4 1 0 2 0 0 0 2115074 SRC 05-809 102.00 105.00 3.00 7.20 19 15 9 6 2 2 1 0 0 0 54

CHAB 05-10

SAMPLE LAB LAB From To Length Weight MICRONS TOTALNO. CERT metres metres metres Kgs -75 +75 +106 +150 +212 +300 +425 +600 +850 +1180 +1700 DIAMONDS15075 SGS 15075 105.00 108.00 3.00 7.26 0 8 4 2 4 4 2 1 0 0 0 2515076 SRC 05-809 108.00 111.00 3.00 7.00 13 9 5 0 1 0 0 0 0 0 2815077 SRC 05-809 111.00 114.00 3.00 7.35 6 6 1 0 0 0 0 0 0 0 1315078 SRC 05-809 114.00 117.00 3.00 7.25 41 8 7 4 4 2 1 0 0 0 6715079 SRC 05-809 117.00 120.00 3.00 7.50 16 6 3 3 3 2 1 1 0 0 3515080 SRC 05-809 120.00 123.00 3.00 7.10 60 23 3 5 2 0 0 0 0 0 9315081 SRC 05-809 123.00 126.00 3.00 7.20 11 10 2 1 0 1 1 0 0 0 2615082 SRC 05-809 126.00 129.00 3.00 7.00 25 5 6 4 4 1 1 0 0 0 4615083 SRC 05-809 129.00 132.00 3.00 7.10 7 5 7 5 4 0 2 0 0 0 3015084 SRC 05-809 132.00 135.00 3.00 7.65 12 6 3 2 0 1 0 0 0 0 2415085 SRC 05-809 135.00 138.00 3.00 7.05 5 2 0 3 2 0 1 0 0 0 1315086 SRC 05-809 138.00 141.00 3.00 6.80 0 2 0 0 0 0 0 0 0 0 215087 SRC 05-809 141.00 144.00 3.00 7.00 0 0 0 0 0 0 0 0 0 0 0 015088 SRC 05-809 144.00 147.00 3.00 6.70 0 0 0 0 0 0 0 0 0 0 0 015089 SRC 05-809 147.00 150.00 3.00 6.90 0 0 0 0 0 0 0 0 0 0 0 0Total 149.30 347.99 701 360 205 146 84 37 23 4 1 1 1562

QA/QC19014 SRC 05-809 0.70 3.00 2.30 4.05 0 3 5 1 4 1 0 0 0 0 0 1419015 SGS 19015 15.00 18.00 3.00 6.88 0 22 3 3 0 0 1 0 0 0 0 2919016 SGS 19016 30.00 33.00 3.00 6.53 0 15 19 7 8 5 1 1 0 0 0 5619017 SGS 19017 33.00 36.00 3.00 6.57 0 5 7 9 2 3 1 0 0 0 0 2719018 SRC 05-809 45.00 48.00 3.00 6.60 0 10 8 6 0 0 2 0 0 0 0 2619019 SGS 19019 60.00 63.00 3.00 6.33 0 2 1 0 1 1 0 0 0 0 0 519020 SGS 19020 75.00 78.00 3.00 6.85 0 2 2 1 0 1 0 0 0 0 0 619021 SGS 19021 78.00 81.75 3.75 8.52 0 7 3 3 0 1 0 0 0 0 0 1419022 SRC 05-809 90.00 93.00 3.00 6.70 0 28 12 6 3 4 1 3 0 0 0 5719023 SGS 19023 105.00 108.00 3.00 6.80 0 8 18 8 3 0 1 1 0 0 0 3919024 SGS 19024 120.00 123.00 3.00 6.63 0 347 378 150 12 0 0 0 1 0 0 88819025 SGS 19025 123.00 126.00 3.00 7.20 0 6 6 4 0 2 0 0 0 0 0 1819026 SRC 05-809 135.00 138.00 3.00 6.80 0 13 5 1 2 2 0 0 0 0 0 23Total 39.05 86.46 468 467 199 35 20 7 5 1 0 0 1202

434.45





December 20, 2005

Report No: 05-809











9/1015040 4.00 75 1 27 0.346 0.563 10/10 010/1015041 6.50 75 0 28 0 0.426 10/10 010/1015042 6.50 75 2 83 3.321 1.131 9/10 010/1015043 7.10 75 5 57 17.796 1.859 10/10 08/1015044 7.00 75 0 32 0 0.385 10/10 0

10/1015046 6.70 75 3 4 2.056 0.068 10/10 010/1015047 7.20 75 2 11 0.948 0.256 10/10 010/1015048 6.10 75 1 30 0.267 0.461 10/10 010/1015049 7.30 75 2 15 3.212 0.527 10/10 910/1015050 6.85 75 0 16 0 0.391 10/10 0

10/1015051 6.55 75 0 31 0 1.198 10/10 010/1015052 7.20 75 2 56 0.846 1.166 10/10 010/1015053 6.75 75 0 90 0 0.699 10/10 010/1015054 7.00 75 0 13 0 0.164 9/10 010/1015055 7.00 75 1 20 0.371 0.156 10/10 0

10/1015056 6.80 75 1 19 0.216 0.299 10/10 010/1015057 7.10 75 1 9 0.482 0.246 9/10 08/1015058 6.55 75 0 33 0 0.773 10/10 010/1015059 7.45 75 0 33 0 0.603 10/10 010/1015061 7.25 75 2 24 1.454 0.227 10/10 0

10/1015062 6.85 75 1 8 0.489 0.105 10/10 010/1015063 6.95 75 1 9 0.253 0.033 10/10 09/1015064 7.05 75 0 12 0 0.130 10/10 010/1015065 7.25 75 0 3 0 0.070 10/10 09/1015066 9.00 75 0 18 0 0.210 9/10 0

1Page of 63





December 20, 2005

Report No: 05-809


10/1015067 5.10 75 0 9 0 0.061 9/10 010/1015068 6.60 75 0 16 0 0.148 10/10 010/1015069 7.00 75 0 33 0 0.690 9/10 010/1015070 7.25 75 1 122 1.783 1.281 10/10 010/1015071 7.00 75 2 56 0.881 0.692 10/10 0

10/1015072 7.80 75 0 37 0 0.903 10/10 010/1015073 6.60 75 2 19 1.955 0.284 10/10 08/1015074 7.20 75 2 52 1.595 0.725 10/10 010/1015076 7.00 75 1 28 0.496 0.216 8/10 010/1015077 7.35 75 0 13 0 0.083 10/10 0

10/1015078 7.25 75 1 66 0.488 0.966 10/10 09/1015079 7.50 75 4 31 3.241 0.461 10/10 010/1015080 7.10 75 0 93 0 0.605 10/10 010/1015081 7.20 75 1 25 0.904 0.378 10/10 010/1015082 7.00 75 4 50 3.641 1.389 10/10 0

10/1015083 7.10 75 2 28 0.915 0.831 8/10 010/1015084 7.65 75 1 23 0.434 0.166 10/10 010/1015085 7.05 75 1 12 0.749 0.426 10/10 09/1015086 6.80 75 0 2 0 0.006 8/10 09/1015087 7.00 75 0 0 0 0 10/10 0

10/1015088 6.70 75 0 0 0 0 10/10 08/1015089 6.90 75 0 0 0 0 10/10 08/1019014 4.05 75 0 14 0 0.283 10/10 010/1019018 6.60 75 1 25 0.225 0.319 10/10 010/1019022 6.70 75 3 54 2.370 1.024 10/10 0

10/1019026 6.80 75 0 23 0 0.305 9/10 0


2Page of 63




December 20, 2005

Report No: 05-809











4.00

75

1

27

0.346

0.563

10/10

0

9/10





mgDiamond

Count

1 1.00 0.70 0.40 Colorless, included, distorted, stepped/ribbed, shield laminae,etched trigons.

0.346 0.346+ 600

1 0.74 0.52 0.40 Colorless, included, distorted, broken, resorbed, serrate laminae,low relief surfaces.

0.179 0.311+ 300

1 0.70 0.50 0.30 Colorless, opaque, thh, broken, resorbed, low relief surfaces.0.132+ 300

1 0.30 0.28 0.28 White, frosted, cubic, tetragonal pits.0.109+ 2121 0.26 0.26 0.24 Grey, cloudy, cubic, broken, resorbed, low relief surfaces.+ 212

6 0.081+ 150

5 0.024+ 106

12 0.038+ 75


3Page of 63




December 20, 2005

Report No: 05-809











6.50

75

0

28

0

0.426

10/10

0

10/10





mgDiamond

Count

1 0.56 0.42 0.30 Colorless, frosted, distorted, broken, serrate laminae.0.101 0.101+ 300

1 0.48 0.30 0.16 White, clear, fragment, lamination.0.166+ 2121 0.30 0.26 0.20 White, frosted, aggregate, broken, rough.+ 2121 0.26 0.26 0.26 Grey, cloudy, cubic, resorbed, low relief surfaces.+ 2121 0.26 0.24 0.24 White, frosted, fragment, rough, lamination.+ 2121 0.26 0.24 0.18 Colorless, clear, fragment, lamination.+ 212

7 0.100+ 150

8 0.044+ 106

7 0.015+ 75


4Page of 63




December 20, 2005

Report No: 05-809











6.50

75

2

83

3.321

1.131

9/10

0

10/10





mgDiamond

Count

1 1.68 1.32 0.84 Colorless, clear, distorted, stepped/ribbed, serrate laminae, pits.3.075 3.075+1180

1 0.62 0.60 0.52 Colorless, included, distorted, broken, serrate laminae.0.246 0.246+ 425

1 0.36 0.36 0.36 Yellow, cloudy, cubic, broken.0.089 0.288+ 3001 0.54 0.52 0.32 Colorless, clear, distorted, broken.0.087+ 3001 0.48 0.46 0.46 Yellow, clear, cubic, pointed plates.0.068+ 3001 0.40 0.40 0.20 Colorless, clear, thh, broken, serrate laminae.0.044+ 300

1 0.50 0.30 0.24 Colorless, clear, fragment, stepped/ribbed, lamination.0.361+ 2121 0.40 0.30 0.20 Colorless, milky, fragment, lamination.+ 2121 0.40 0.28 0.20 Black, opaque, fragment, lamination.+ 2121 0.38 0.36 0.12 Grey, opaque, fragment, rough.+ 2121 0.38 0.30 0.20 Yellow, clear, dodecahedron, broken, low relief surfaces.+ 212

1 0.36 0.30 0.26 Colorless, clear, aggregate, stepped/ribbed, serrate laminae.+ 2121 0.36 0.24 0.20 White, included, aggregate, broken, rough.+ 2121 0.32 0.26 0.16 White, frosted, fragment, lamination.+ 2121 0.30 0.26 0.24 White, frosted, distorted, broken, lamination.+ 212

5Page of 63




December 20, 2005

Report No: 05-809






mgDiamond

Count

23 0.321+ 150

14 0.077+ 106

33 0.084+ 75


6Page of 63




December 20, 2005

Report No: 05-809











7.10

75

5

57

17.796

1.859

10/10

0

10/10





mgDiamond

Count

1 2.54 2.48 2.06 Colorless, clear, distorted, broken, stepped/ribbed, pits.15.351 15.351+1700

1 1.20 0.98 0.74 Yellow, opaque, distorted, stepped/ribbed, serrate laminae,rough.

0.972 2.445+ 600

1 0.94 0.80 0.64 Colorless, clear, octahedron, broken, shield laminae.0.725+ 6001 0.90 0.64 0.52 Colorless, included, distorted, broken, pits, hillocks.0.378+ 6001 0.92 0.74 0.46 Colorless, included, distorted, broken, etched trigons.0.370+ 600

1 0.84 0.54 0.48 Colorless, included, distorted, broken, serrate laminae.0.245 1.265+ 4251 0.70 0.50 0.36 White, included, thh, resorbed, low relief surfaces.0.225+ 4251 0.64 0.52 0.40 Yellow, opaque, octahedron, resorbed, low relief surfaces.0.224+ 4251 0.76 0.68 0.40 White, frosted, irregular, broken, etched trigons.0.219+ 4251 0.70 0.60 0.40 Colorless, clear, octahedron, broken, stepped/ribbed, serrate

laminae, shield laminae.0.207+ 425

1 0.72 0.62 0.32 White, clear, fragment, broken, stepped/ribbed, serrate laminae.0.145+ 425

1 0.80 0.48 0.18 White, frosted, fragment, broken, shield laminae.0.074 0.133+ 3001 0.74 0.40 0.12 White, frosted, fragment, broken.0.059+ 300

7Page of 63




December 20, 2005

Report No: 05-809






mgDiamond

Count

1 0.52 0.30 0.22 Colorless, clear, fragment, lamination.0.269+ 2121 0.48 0.24 0.20 Colorless, clear, fragment, lamination.+ 2121 0.40 0.30 0.22 White, frosted, irregular, resorbed, rough.+ 2121 0.32 0.30 0.26 White, clear, fragment, rough.+ 212

1 0.32 0.30 0.24 Colorless, clear, irregular, resorbed, low relief surfaces.+ 2121 0.32 0.30 0.10 Colorless, clear, fragment, lamination.+ 2121 0.32 0.28 0.20 White, clear, fragment, lamination.+ 2121 0.32 0.26 0.14 White, clear, fragment, lamination.+ 2121 0.30 0.24 0.24 Colorless, clear, fragment, lamination.+ 212

1 0.30 0.20 0.10 Colorless, clear, fragment, lamination.+ 212

7 0.087+ 150

13 0.063+ 106

19 0.042+ 75


8Page of 63




December 20, 2005

Report No: 05-809











7.00

75

0

32

0

0.385

10/10

0

8/10





mgDiamond

Count

1 0.30 0.30 0.30 Yellow, frosted, cubic, low relief surfaces.0.090 0.160+ 3001 0.48 0.36 0.30 Colorless, clear, octahedron, twinned, pits.0.070+ 300

1 0.50 0.30 0.20 White, frosted, aggregate, resorbed, low relief surfaces.0.068+ 2121 0.30 0.20 0.16 White, included, fragment, rough.+ 212

3 0.046+ 150

15 0.078+ 106

10 0.033+ 75


9Page of 63




December 20, 2005

Report No: 05-809











6.70

75

3

4

2.056

0.068

10/10

0

10/10





mgDiamond

Count

1 0.64 0.64 0.64 White, opaque, cubic.0.974 1.743+ 6001 1.04 0.92 0.40 Colorless, included, octahedron, stepped/ribbed, serrate laminae,


1 0.68 0.60 0.40 White, included, distorted, resorbed, hillocks, low relief surfaces.0.313 0.313+ 425

1 0.30 0.28 0.20 Colorless, frosted, dodecahedron, broken, resorbed, low reliefsurfaces.

0.032+ 212

2 0.022+ 150

1 0.014+ 106


10Page of 63




December 20, 2005

Report No: 05-809











7.20

75

2

11

0.948

0.256

10/10

0

10/10





mgDiamond

Count

1 0.96 0.90 0.74 Colorless, included, thh, broken, resorbed, low relief surfaces,rough.

0.779 0.779+ 600

1 0.70 0.66 0.34 Colorless, clear, thh, broken, stepped/ribbed, serrate laminae,shield laminae, etched trigons.

0.169 0.169+ 425

1 0.60 0.50 0.40 Colorless, included, thh, resorbed, stepped/ribbed, serratelaminae.

0.107 0.107+ 300

1 0.50 0.30 0.20 White, clear, fragment, stepped/ribbed, rough.0.133+ 2121 0.40 0.28 0.26 Colorless, clear, octahedron, twinned, resorbed, low relief

surfaces.+ 212

1 0.36 0.28 0.26 Colorless, milky, octahedron, resorbed, stepped/ribbed, hillocks.+ 212

1 0.007+ 106

6 0.009+ 75


11Page of 63




December 20, 2005

Report No: 05-809











6.10

75

1

30

0.267

0.461

10/10

0

10/10





mgDiamond

Count

1 0.98 0.64 0.38 Pink, frosted, fragment, broken, pits, lamination.0.267 0.267+ 425

1 0.30 0.30 0.30 Yellow, opaque, cubic, rough.0.098 0.271+ 3001 0.64 0.32 0.24 Colorless, clear, fragment, broken, stepped/ribbed, etched

trigons, rough, lamination.0.091+ 300

1 0.40 0.36 0.30 White, frosted, cubic, rough.0.082+ 300

1 0.44 0.36 0.30 Colorless, clear, octahedral, broken, pits, rough.0.088+ 2121 0.34 0.32 0.16 White, included, distorted, broken, rough, lamination.+ 212

4 0.044+ 150

6 0.033+ 106

15 0.025+ 75


12Page of 63




December 20, 2005

Report No: 05-809











7.30

75

2

15

3.212

0.527

10/10

9

10/10





mgDiamond

Count

1 1.46 1.08 1.00 Colorless, clear, octahedron, broken, hillocks, rough.2.740 2.740+ 850

1 0.56 0.46 0.44 Green, opaque, cubic, rough.0.472 0.723+ 4251 0.66 0.60 0.40 Colorless, frosted, cubic, hillocks.0.251+ 425

1 0.40 0.34 0.30 Colorless, clear, octahedron, stepped/ribbed, serrate laminae,shield laminae.

0.049 0.188+ 300

1 0.52 0.30 0.20 Colorless, frosted, fragment, broken, stepped/ribbed, rough.0.044+ 3001 0.46 0.28 0.24 Yellow, frosted, fragment, broken, stepped/ribbed, shield

laminae, rough.0.042+ 300

1 0.30 0.26 0.20 Colorless, clear, octahedron, stepped/ribbed, serrate laminae,hillocks.

0.030+ 300

1 0.38 0.30 0.28 Colorless, frosted, octahedron, stepped/ribbed, serrate laminae,hillocks.

0.023+ 300

1 0.50 0.28 0.10 Colorless, frosted, fragment, broken, etched trigons, rough.0.076+ 2121 0.34 0.22 0.10 Colorless, clear, fragment, resorbed, stepped/ribbed, pits, rough.+ 2121 0.26 0.22 0.16 Colorless, clear, octahedron, stepped/ribbed, serrate laminae.+ 2121 0.22 0.22 0.20 Yellow, opaque, cubic, rough.+ 212

13Page of 63




December 20, 2005

Report No: 05-809






mgDiamond

Count

3 0.008+ 106

2 0.004+ 75


14Page of 63




December 20, 2005

Report No: 05-809











6.85

75

0

16

0

0.391

10/10

0

10/10





mgDiamond

Count

1 0.60 0.40 0.30 Colorless, clear, octahedron, broken, resorbed, hillocks.0.148 0.222+ 3001 0.36 0.36 0.36 Colorless, included, octahedron, resorbed, low relief surfaces.0.074+ 300

1 0.36 0.34 0.30 White, included, octahedron, twinned, shield laminae, low reliefsurfaces.

0.126+ 212

1 0.30 0.26 0.26 Yellow, included, distorted, resorbed.+ 2121 0.26 0.26 0.26 Grey, opaque, cubic, rough.+ 212

1 0.012+ 106

10 0.031+ 75


15Page of 63




December 20, 2005

Report No: 05-809











6.55

75

0

31

0

1.198

10/10

0

10/10





mgDiamond

Count

1 0.64 0.60 0.44 Yellow, frosted, distorted, stepped/ribbed, lamination.0.250 0.411+ 4251 0.64 0.50 0.40 White, frosted, distorted, broken, resorbed, pits, rough.0.161+ 425

1 0.90 0.48 0.40 Pink, opaque, distorted, resorbed, low relief surfaces.0.252 0.542+ 3001 0.30 0.30 0.30 Yellow, frosted, cubic, rough.0.160+ 3001 0.42 0.38 0.30 Colorless, clear, octahedron, stepped/ribbed, serrate laminae,


1 0.42 0.32 0.32 Yellow, frosted, distorted, resorbed, low relief surfaces, rough.0.063+ 300

1 0.44 0.30 0.20 Colorless, included, fragment, broken.0.154+ 2121 0.44 0.26 0.20 Colorless, clear, octahedron, twinned, stepped/ribbed, shield

laminae.+ 212

1 0.30 0.24 0.24 Grey, opaque, cubic, broken.+ 2121 0.24 0.20 0.10 Grey, frosted, cubic, broken.+ 212

5 0.046+ 150

6 0.029+ 106

10 0.016+ 75

16Page of 63




December 20, 2005

Report No: 05-809



17Page of 63




December 20, 2005

Report No: 05-809











7.20

75

2

56

0.846

1.166

10/10

0

10/10





mgDiamond

Count

1 0.90 0.84 0.72 Colorless, clear, octahedron, broken, hillocks.0.572 0.572+ 600

1 0.72 0.54 0.44 Colorless, included, fragment, broken, stepped/ribbed, serratelaminae, hillocks, rough.

0.274 0.548+ 425

1 0.50 0.48 0.46 Yellow, opaque, cubic, rough.0.274+ 425

1 0.66 0.50 0.34 Colorless, frosted, distorted, hillocks, rough.0.130 0.434+ 3001 0.56 0.40 0.32 Colorless, frosted, fragment, broken, etched trigons, hillocks,

rough.0.088+ 300

1 0.50 0.42 0.28 Colorless, frosted, fragment, broken, stepped/ribbed, rough,lamination.

0.079+ 300

1 0.56 0.48 0.36 White, frosted, fragment, broken, etched trigons, rough,lamination.

0.077+ 300

1 0.48 0.42 0.38 Colorless, frosted, distorted, rough, lamination.0.060+ 300

1 0.48 0.30 0.16 Colorless, clear, fragment, broken, stepped/ribbed, rough.0.316+ 2121 0.48 0.26 0.10 Colorless, frosted, fragment, broken, lamination.+ 2121 0.44 0.42 0.30 Colorless, frosted, octahedron, resorbed, lamination.+ 2121 0.44 0.38 0.24 Amber, milky, distorted, rough.+ 2121 0.44 0.22 0.20 Colorless, frosted, distorted, broken, rough.+ 212

18Page of 63




December 20, 2005

Report No: 05-809






mgDiamond

Count

1 0.40 0.36 0.24 Colorless, frosted, distorted, rough.+ 2121 0.40 0.36 0.22 Colorless, frosted, fragment, broken, rough, lamination.+ 2121 0.40 0.32 0.26 Colorless, clear, octahedron, broken, shield laminae, pits.+ 2121 0.40 0.30 0.28 Colorless, clear, octahedron, broken, rough.+ 212

1 0.38 0.24 0.24 Colorless, frosted, distorted, broken, rough.+ 212

4 0.057+ 150

11 0.050+ 106

25 0.035+ 75


19Page of 63




December 20, 2005

Report No: 05-809











6.75

75

0

90

0

0.699

10/10

0

10/10





mgDiamond

Count

1 0.50 0.50 0.44 Yellow, opaque, cubic, rough.0.243 0.243+ 425

1 0.50 0.30 0.20 Grey, included, polycrystalline aggregate, broken, rough.0.075+ 2121 0.30 0.30 0.20 Black, opaque, polycrystalline aggregate, broken.+ 2121 0.30 0.20 0.20 Grey, opaque, polycrystalline aggregate, broken.+ 212

13 0.168+ 150

32 0.156+ 106

41 0.057+ 75


20Page of 63




December 20, 2005

Report No: 05-809











7.00

75

0

13

0

0.164

9/10

0

10/10





mgDiamond

Count

1 0.32 0.30 0.30 White, frosted, cubic, pits, crescentic steps.0.103+ 2121 0.32 0.30 0.26 Green, frosted, cubic, twinned, resorbed, pits.+ 212

2 0.032+ 150

3 0.014+ 106

6 0.015+ 75


21Page of 63




December 20, 2005

Report No: 05-809











7.00

75

1

20

0.371

0.156

10/10

0

10/10





mgDiamond

Count

1 0.52 0.52 0.52 Yellow, frosted, cubic, pits.0.371 0.371+ 425

1 0.44 0.30 0.24 Colorless, included, distorted, resorbed, low relief surfaces.0.102+ 2121 0.34 0.30 0.20 Colorless, included, distorted, broken, rough.+ 2121 0.30 0.22 0.20 Yellow, clear, distorted, resorbed, low relief surfaces.+ 212

1 0.012+ 150

2 0.014+ 106

14 0.028+ 75


22Page of 63




December 20, 2005

Report No: 05-809











6.80

75

1

19

0.216

0.299

10/10

0

10/10





mgDiamond

Count

1 0.62 0.52 0.30 Colorless, frosted, octahedron, stepped/ribbed, serrate laminae,hillocks.

0.216 0.216+ 425

1 0.38 0.36 0.36 Amber, opaque, cubic, resorbed, hillocks.0.135 0.220+ 3001 0.30 0.30 0.28 Yellow, opaque, cubic, resorbed, hillocks.0.085+ 300

4 0.057+ 150

1 0.004+ 106

12 0.018+ 75


23Page of 63




December 20, 2005

Report No: 05-809











7.10

75

1

9

0.482

0.246

9/10

0

10/10





mgDiamond

Count

1 0.92 0.84 0.62 Colorless, clear, distorted, stepped/ribbed, serrate laminae,shield laminae.

0.482 0.482+ 600

1 0.44 0.42 0.40 Colorless, frosted, octahedron, resorbed, crescentic steps.0.115 0.191+ 3001 0.50 0.50 0.30 Colorless, clear, octahedron, stepped/ribbed, serrate laminae,


2 0.033+ 150

2 0.013+ 106

3 0.009+ 75


24Page of 63




December 20, 2005

Report No: 05-809











6.55

75

0

33

0

0.773

10/10

0

8/10





mgDiamond

Count

1 0.70 0.44 0.40 Colorless, clear, distorted, resorbed, serrate laminae, low reliefsurfaces.

0.213 0.494+ 300

1 0.66 0.52 0.30 Colorless, clear, fragment, broken, serrate laminae.0.112+ 3001 0.48 0.36 0.30 Yellow, cloudy, octahedron, resorbed.0.095+ 3001 0.54 0.40 0.20 Colorless, clear, fragment, broken.0.074+ 300

1 0.42 0.26 0.20 Colorless, clear, fragment, broken.0.112+ 2121 0.40 0.30 0.20 Colorless, clear, fragment, broken.+ 2121 0.40 0.20 0.16 Colorless, clear, fragment, broken.+ 2121 0.36 0.28 0.28 Colorless, clear, distorted, broken, serrate laminae.+ 212

5 0.087+ 150

7 0.042+ 106

13 0.038+ 75


25Page of 63




December 20, 2005

Report No: 05-809











7.45

75

0

33

0

0.603

10/10

0

10/10





mgDiamond

Count

1 0.56 0.40 0.36 Colorless, clear, aggregate, stepped/ribbed, serrate laminae,shield laminae.

0.134 0.362+ 300

1 0.58 0.48 0.40 Colorless, frosted, octahedron, broken, stepped/ribbed, serratelaminae.

0.124+ 300

1 0.62 0.50 0.20 White, frosted, distorted, broken, rough, lamination.0.105+ 300

1 0.50 0.30 0.12 Yellow, clear, fragment, broken, rough, lamination.0.132+ 2121 0.32 0.32 0.30 Colorless, frosted, octahedron, resorbed, pits.+ 2121 0.30 0.28 0.16 White, milky, octahedron, broken, pits, rough.+ 2121 0.26 0.22 0.20 Grey, cloudy, cubic, resorbed, pits.+ 212

2 0.032+ 150

7 0.035+ 106

17 0.042+ 75


26Page of 63




December 20, 2005

Report No: 05-809











7.25

75

2

24

1.454

0.227

10/10

0

10/10





mgDiamond

Count

1 1.00 0.80 0.60 Colorless, clear, distorted, twinned, stepped/ribbed, serratelaminae, shield laminae.

0.984 0.984+ 850

1 0.80 0.70 0.62 Yellow, distorted, resorbed, low relief surfaces.0.470 0.470+ 600

1 0.46 0.26 0.20 White, frosted, distorted, resorbed.0.107+ 2121 0.34 0.30 0.26 Colorless, included, octahedron, resorbed, low relief surfaces.+ 212

2 0.027+ 150

2 0.019+ 106

18 0.074+ 75


27Page of 63




December 20, 2005

Report No: 05-809











6.85

75

1

8

0.489

0.105

10/10

0

10/10





mgDiamond

Count

1 0.66 0.66 0.52 White, frosted, cubic, broken, rough.0.489 0.489+ 425

1 0.36 0.30 0.24 Colorless, frosted, fragment, broken, rough.0.056+ 2121 0.36 0.20 0.16 Colorless, opaque, fragment, serrate laminae, shield laminae.+ 2121 0.30 0.30 0.24 Colorless, included, octahedron, resorbed, shield laminae, low

relief surfaces.+ 212

1 0.019+ 150

1 0.010+ 106

3 0.020+ 75


28Page of 63




December 20, 2005

Report No: 05-809











6.95

75

1

9

0.253

0.033

10/10

0

10/10





mgDiamond

Count

1 0.66 0.56 0.54 Amber, frosted, dodecahedron, hillocks.0.253 0.253+ 425

3 0.021+ 106

6 0.012+ 75


29Page of 63




December 20, 2005

Report No: 05-809











7.05

75

0

12

0

0.130

10/10

0

9/10





mgDiamond

Count

1 0.54 0.48 0.24 Grey, opaque, polycrystalline aggregate, broken.0.084 0.084+ 300

2 0.026+ 150

2 0.008+ 106

7 0.012+ 75


30Page of 63




December 20, 2005

Report No: 05-809











7.25

75

0

3

0

0.070

10/10

0

10/10





mgDiamond

Count

1 0.24 0.22 0.22 Green, frosted, cubic, rough.0.035+ 212

2 0.035+ 150


31Page of 63




December 20, 2005

Report No: 05-809











9.00

75

0

18

0

0.210

9/10

0

9/10





mgDiamond

Count

1 0.46 0.30 0.28 Colorless, opaque, distorted, broken, serrate laminae.0.117+ 2121 0.34 0.34 0.26 Yellow, opaque, octahedron, stepped/ribbed, rough.+ 2121 0.30 0.26 0.20 Colorless, clear, octahedron, broken, serrate laminae, shield

laminae.+ 212

1 0.016+ 150

6 0.057+ 106

8 0.020+ 75


32Page of 63




December 20, 2005

Report No: 05-809











5.10

75

0

9

0

0.061

9/10

0

10/10





mgDiamond

Count

1 0.34 0.28 0.20 Colorless, clear, fragment, broken, rough, lamination.0.025+ 212

2 0.018+ 106

6 0.018+ 75


33Page of 63




December 20, 2005

Report No: 05-809











6.60

75

0

16

0

0.148

10/10

0

10/10





mgDiamond

Count

1 0.30 0.20 0.20 Colorless, clear, octahedron, serrate laminae, shield laminae.0.045+ 2121 0.24 0.24 0.22 Yellow, opaque, cubic.+ 212

5 0.075+ 150

2 0.011+ 106

7 0.017+ 75


34Page of 63




December 20, 2005

Report No: 05-809











7.00

75

0

33

0

0.690

9/10

0

10/10





mgDiamond

Count

1 0.56 0.38 0.32 Colorless, clear, octahedroid, resorbed, stepped/ribbed, hillocks.0.174 0.455+ 3001 0.56 0.34 0.28 Yellow, clear, cubic, resorbed, low relief surfaces, pointed plates.0.124+ 300

1 0.40 0.36 0.26 Colorless, included, cubic, resorbed, low relief surfaces, pointedplates.

0.108+ 300

1 0.40 0.38 0.28 White, included, polycrystalline aggregate, resorbed.0.049+ 300

1 0.38 0.28 0.28 White, included, polycrystalline aggregate, resorbed.0.114+ 2121 0.30 0.28 0.28 Yellow, opaque, cubic, twinned.+ 2121 0.30 0.24 0.10 White, clear, polycrystalline aggregate, resorbed.+ 212

5 0.083+ 150

5 0.015+ 106

16 0.023+ 75


35Page of 63




December 20, 2005

Report No: 05-809











7.25

75

1

122

1.783

1.281

10/10

0

10/10





mgDiamond

Count

1 1.72 0.98 0.44 White, frosted, distorted, resorbed, pits, hillocks.1.783 1.783+ 850

1 0.98 0.46 0.22 Colorless, clear, octahedron, resorbed, hillocks.0.314 0.463+ 4251 0.44 0.44 0.44 White, frosted, polycrystalline aggregate, broken, resorbed.0.149+ 425

1 0.46 0.36 0.30 White, frosted, cubic, resorbed, stepped/ribbed, low reliefsurfaces.

0.121 0.289+ 300

1 0.62 0.34 0.22 Colorless, clear, aggregate, stepped/ribbed, serrate laminae.0.094+ 3001 0.44 0.32 0.26 Colorless, included, octahedral.0.074+ 300

1 0.36 0.26 0.20 White, included, polycrystalline aggregate.0.155+ 2121 0.36 0.26 0.18 Yellow, clear, aggregate.+ 2121 0.34 0.28 0.28 Yellow, opaque, thh, resorbed, hillocks.+ 2121 0.34 0.24 0.18 Colorless, clear, octahedron, stepped/ribbed.+ 2121 0.32 0.22 0.12 White, included, polycrystalline aggregate.+ 212

13 0.113+ 150

38 0.176+ 106

36Page of 63




December 20, 2005

Report No: 05-809






mgDiamond

Count

61 0.085+ 75


37Page of 63




December 20, 2005

Report No: 05-809











7.00

75

2

56

0.881

0.692

10/10

0

10/10





mgDiamond

Count

1 0.94 0.58 0.38 White, clear, octahedroid, resorbed, hillocks.0.493 0.881+ 4251 0.64 0.56 0.32 Amber, clear, distorted, stepped/ribbed, serrate laminae.0.388+ 425

1 0.56 0.38 0.26 Black, opaque, bort.0.103 0.180+ 3001 0.30 0.30 0.30 White, milky, cubic, crescentic steps.0.077+ 300

1 0.50 0.24 0.12 Grey, included, fragment, resorbed, serrate laminae.0.258+ 2121 0.42 0.26 0.22 White, clear, aggregate, stepped/ribbed, serrate laminae.+ 2121 0.42 0.24 0.10 White, milky, irregular, resorbed, low relief surfaces.+ 2121 0.38 0.28 0.24 Yellow, clear, octahedroid, resorbed, serrate laminae.+ 2121 0.34 0.28 0.22 Colorless, clear, octahedral, etched trigons, low relief surfaces.+ 212

1 0.34 0.28 0.18 Colorless, clear, cubic, resorbed, low relief surfaces, crescenticsteps.

+ 212

1 0.28 0.24 0.20 White, frosted, thh, resorbed, hillocks.+ 2121 0.28 0.22 0.22 Yellow, clear, cubic, resorbed, pointed plates.+ 212

10 0.149+ 150

17 0.072+ 106

38Page of 63




December 20, 2005

Report No: 05-809






mgDiamond

Count

19 0.033+ 75


39Page of 63




December 20, 2005

Report No: 05-809











7.80

75

0

37

0

0.903

10/10

0

10/10





mgDiamond

Count

1 0.50 0.50 0.50 Yellow, opaque, cubic, rough.0.443 0.443+ 425

1 0.40 0.30 0.24 Colorless, included, octahedron, broken.0.072 0.135+ 3001 0.56 0.50 0.46 Grey, opaque, cubic, twinned, rough.0.063+ 300

1 0.50 0.36 0.20 Yellow, included, distorted, broken.0.125+ 2121 0.46 0.46 0.20 Colorless, included, octahedron, broken.+ 2121 0.30 0.28 0.26 Colorless, included, cubic, resorbed, pits, pointed plates.+ 212

9 0.113+ 150

9 0.045+ 106

13 0.042+ 75


40Page of 63




December 20, 2005

Report No: 05-809











6.60

75

2

19

1.955

0.284

10/10

0

10/10





mgDiamond

Count

1 1.28 0.80 0.76 White, included, dodecahedron, resorbed, hillocks.1.217 1.955+ 6001 1.00 0.66 0.52 Colorless, clear, distorted, resorbed, serrate laminae, hillocks.0.738+ 600

1 0.46 0.38 0.32 Yellow, clear, aggregate, rough.0.088 0.088+ 300

1 0.44 0.36 0.28 Colorless, clear, octahedron, stepped/ribbed, serrate laminae.0.144+ 2121 0.40 0.28 0.14 Colorless, clear, aggregate, serrate laminae.+ 2121 0.36 0.28 0.18 Colorless, clear, octahedroid, stepped/ribbed, serrate laminae.+ 2121 0.28 0.22 0.18 Colorless, clear, octahedroid, broken, stepped/ribbed, serrate

laminae.+ 212

1 0.007+ 150

5 0.024+ 106

8 0.021+ 75


41Page of 63




December 20, 2005

Report No: 05-809











7.20

75

2

52

1.595

0.725

10/10

0

8/10





mgDiamond

Count

1 1.34 0.84 0.78 White, included, octahedron, resorbed, stepped/ribbed, serratelaminae, shield laminae, hillocks.

1.276 1.276+ 600

1 0.76 0.72 0.46 Colorless, clear, octahedron, resorbed, hillocks, low reliefsurfaces.

0.319 0.492+ 425

1 0.64 0.50 0.42 Yellow, clear, octahedron, resorbed, hillocks.0.173+ 425

1 0.42 0.38 0.36 White, opaque, cubic, stepped/ribbed, rough.0.088 0.122+ 3001 0.38 0.36 0.28 Yellow, included, distorted, rough.0.034+ 300

1 0.48 0.30 0.28 White, included, irregular, stepped/ribbed, hillocks, rough.0.204+ 2121 0.46 0.36 0.24 White, clear, aggregate, resorbed, stepped/ribbed, etched

trigons.+ 212

1 0.36 0.24 0.22 White, clear, irregular, stepped/ribbed, serrate laminae, hillocks.+ 2121 0.34 0.32 0.24 White, opaque, octahedron, broken, resorbed, stepped/ribbed,

rough.+ 212

1 0.32 0.24 0.20 White, clear, octahedron, resorbed, stepped/ribbed, shieldlaminae, etched trigons, hillocks.

+ 212

1 0.28 0.24 0.16 Colorless, opaque, octahedral, resorbed, rough.+ 212

42Page of 63




December 20, 2005

Report No: 05-809






mgDiamond

Count

9 0.112+ 150

15 0.069+ 106

19 0.045+ 75


43Page of 63




December 20, 2005

Report No: 05-809











7.00

75

1

28

0.496

0.216

8/10

0

10/10





mgDiamond

Count

1 0.92 0.70 0.48 Colorless, clear, octahedral, broken, stepped/ribbed, serratelaminae.

0.496 0.496+ 600

1 0.44 0.36 0.30 Colorless, included, dodecahedron, resorbed, hillocks.0.098 0.098+ 300

5 0.059+ 150

9 0.038+ 106

13 0.021+ 75


44Page of 63




December 20, 2005

Report No: 05-809











7.35

75

0

13

0

0.083

10/10

0

10/10





mgDiamond

Count

1 0.010+ 150

6 0.060+ 106

6 0.013+ 75


45Page of 63




December 20, 2005

Report No: 05-809











7.25

75

1

66

0.488

0.966

10/10

0

10/10





mgDiamond

Count

1 1.02 0.76 0.38 Colorless, included, aggregate, stepped/ribbed, serrate laminae.0.488 0.488+ 600

1 0.74 0.44 0.36 Colorless, included, octahedron, broken, stepped/ribbed, hillocks,lamination.

0.184 0.317+ 425

1 0.56 0.48 0.36 Colorless, clear, aggregate, broken, stepped/ribbed, lamination.0.133+ 425

1 0.48 0.36 0.24 Colorless, clear, fragment, stepped/ribbed, lamination.0.091 0.278+ 3001 0.50 0.30 0.26 Colorless, clear, fragment, stepped/ribbed, serrate laminae,

shield laminae, lamination.0.077+ 300

1 0.54 0.28 0.24 Colorless, clear, fragment, stepped/ribbed, serrate laminae,lamination.

0.064+ 300

1 0.54 0.36 0.12 Colorless, clear, fragment, serrate laminae, lamination.0.046+ 300

1 0.48 0.28 0.22 Colorless, clear, fragment, low relief surfaces, lamination.0.127+ 2121 0.46 0.22 0.18 Colorless, included, fragment, resorbed, stepped/ribbed.+ 2121 0.32 0.24 0.14 Grey, included, fragment, resorbed.+ 2121 0.22 0.20 0.16 Yellow, opaque, cubic, resorbed, low relief surfaces.+ 212

7 0.092+ 150

46Page of 63




December 20, 2005

Report No: 05-809






mgDiamond

Count

8 0.055+ 106

41 0.097+ 75


47Page of 63




December 20, 2005

Report No: 05-809











7.50

75

4

31

3.241

0.461

10/10

0

9/10





mgDiamond

Count

1 1.10 1.04 1.00 White, milky, octahedron, resorbed, hillocks, low relief surfaces.1.931 1.931+ 850

1 0.80 0.70 0.42 White, opaque, distorted, resorbed, hillocks.0.600 0.600+ 600

1 1.00 0.64 0.34 Amber, frosted, distorted, resorbed.0.383 0.710+ 4251 0.86 0.60 0.48 Colorless, included, fragment, broken, shield laminae.0.327+ 425

1 0.38 0.38 0.38 Grey, opaque, cubic, rough.0.128 0.281+ 3001 0.46 0.42 0.40 Colorless, clear, octahedron, serrate laminae.0.107+ 3001 0.60 0.30 0.20 White, frosted, polycrystalline aggregate, broken.0.046+ 300

1 0.36 0.30 0.22 White, included, fragment.0.084+ 2121 0.28 0.26 0.20 Yellow, opaque, distorted.+ 2121 0.24 0.24 0.20 Yellow, opaque, polycrystalline aggregate.+ 212

3 0.047+ 150

6 0.018+ 106

16 0.031+ 75

48Page of 63




December 20, 2005

Report No: 05-809



49Page of 63




December 20, 2005

Report No: 05-809











7.10

75

0

93

0

0.605

10/10

0

10/10





mgDiamond

Count

1 0.50 0.36 0.30 White, clear, octahedron, twinned, resorbed, stepped/ribbed,serrate laminae, shield laminae, etched trigons.

0.081 0.160+ 300

1 0.48 0.46 0.30 Colorless, clear, fragment, resorbed, stepped/ribbed, hillocks.0.079+ 300

1 0.54 0.30 0.24 Colorless, milky, fragment, stepped/ribbed.0.178+ 2121 0.50 0.34 0.20 Colorless, opaque, fragment, stepped/ribbed, serrate laminae,

rough.+ 212

1 0.40 0.30 0.14 White, clear, octahedron, twinned, resorbed, stepped/ribbed, pits.+ 212

1 0.32 0.30 0.26 Yellow, clear, cubic, resorbed, hillocks, low relief surfaces.+ 2121 0.24 0.24 0.22 Colorless, opaque, cubic, low relief surfaces, rough.+ 212

3 0.039+ 150

23 0.116+ 106

60 0.112+ 75


50Page of 63




December 20, 2005

Report No: 05-809











7.20

75

1

25

0.904

0.378

10/10

0

10/10





mgDiamond

Count

1 1.00 0.76 0.48 Colorless, clear, octahedron, stepped/ribbed, hillocks.0.904 0.904+ 600

1 0.58 0.44 0.22 White, frosted, octahedroid, twinned, pits.0.207 0.207+ 425

1 0.34 0.34 0.14 Colorless, included, octahedron, twinned, stepped/ribbed, serratelaminae.

0.040+ 212

2 0.031+ 150

10 0.073+ 106

11 0.027+ 75


51Page of 63




December 20, 2005

Report No: 05-809











7.00

75

4

50

3.641

1.389

10/10

0

10/10





mgDiamond

Count

1 1.62 0.92 0.64 Colorless, included, fragment, resorbed, hillocks, trigonal pits.1.987 1.987+ 850

1 1.18 0.82 0.56 Colorless, included, octahedroid, broken, resorbed, pits, hillocks,lamination.

1.052 1.052+ 600

1 0.54 0.52 0.52 Yellow, cloudy, cubic, resorbed, crescentic steps, trigonal pits.0.372 1.144+ 4251 0.84 0.46 0.40 Colorless, clear, octahedron, twinned, stepped/ribbed, serrate

laminae.0.354+ 425

1 0.64 0.50 0.48 Colorless, clear, aggregate, stepped/ribbed, serrate laminae.0.230+ 4251 0.56 0.42 0.36 Colorless, included, octahedroid, resorbed, pits, hillocks.0.188+ 425

1 0.70 0.38 0.28 Colorless, included, dodecahedron, resorbed, hillocks.0.170 0.427+ 3001 0.70 0.38 0.20 Colorless, included, dodecahedron, resorbed, hillocks.0.106+ 3001 0.46 0.30 0.24 Yellow, clear, distorted, stepped/ribbed, serrate laminae.0.077+ 3001 0.70 0.38 0.22 Grey, included, irregular, resorbed.0.074+ 300

1 0.54 0.38 0.20 Yellow, clear, aggregate, stepped/ribbed, serrate laminae.0.295+ 2121 0.50 0.28 0.24 Colorless, clear, octahedroid, twinned, resorbed, etched trigons,

hillocks.+ 212

52Page of 63




December 20, 2005

Report No: 05-809






mgDiamond

Count

1 0.48 0.24 0.18 Colorless, included, fragment, stepped/ribbed, serrate laminae,lamination.

+ 212

1 0.44 0.28 0.24 Colorless, clear, octahedroid, resorbed, stepped/ribbed, serratelaminae, hillocks.

+ 212

1 0.30 0.28 0.14 Colorless, cloudy, irregular, resorbed.+ 2121 0.26 0.24 0.22 White, opaque, cubic.+ 212

5 0.052+ 150

8 0.039+ 106

25 0.034+ 75


53Page of 63




December 20, 2005

Report No: 05-809











7.10

75

2

28

0.915

0.831

8/10

0

10/10





mgDiamond

Count

1 0.88 0.78 0.74 White, clear, aggregate, broken, stepped/ribbed, serrate laminae,shield laminae, etched trigons, hillocks.

0.514 0.915+ 600

1 0.82 0.70 0.62 Colorless, clear, octahedron, broken, resorbed, stepped/ribbed,shield laminae, hillocks.

0.401+ 600

1 0.40 0.40 0.38 Grey, opaque, cubic, resorbed, rough.0.184 0.517+ 3001 0.80 0.52 0.38 White, clear, octahedron, broken, resorbed, serrate laminae,

hillocks.0.165+ 300

1 0.50 0.36 0.34 White, clear, octahedron, broken, resorbed, stepped/ribbed,shield laminae.

0.089+ 300

1 0.46 0.40 0.32 White, clear, octahedron, broken, resorbed, stepped/ribbed,shield laminae, hillocks.

0.079+ 300

1 0.48 0.36 0.26 Black, opaque, octahedron, broken, resorbed, rough.0.186+ 2121 0.48 0.30 0.22 White, clear, octahedron, twinned, resorbed, stepped/ribbed,

shield laminae, hillocks.+ 212

1 0.40 0.36 0.34 Colorless, clear, aggregate, stepped/ribbed, shield laminae.+ 2121 0.38 0.30 0.22 Colorless, clear, octahedron, stepped/ribbed, shield laminae, low

relief surfaces.+ 212

1 0.30 0.28 0.20 White, clear, octahedron, resorbed, stepped/ribbed, hillocks.+ 212

54Page of 63




December 20, 2005

Report No: 05-809






mgDiamond

Count

7 0.088+ 150

5 0.018+ 106

7 0.022+ 75


55Page of 63




December 20, 2005

Report No: 05-809











7.65

75

1

23

0.434

0.166

10/10

0

10/10





mgDiamond

Count

1 0.62 0.60 0.56 Colorless, included, distorted, hillocks.0.434 0.434+ 425

1 0.28 0.28 0.28 Yellow, opaque, cubic, broken, pits.0.083+ 2121 0.26 0.26 0.24 Yellow, opaque, octahedron, stepped/ribbed.+ 212

3 0.021+ 150

6 0.037+ 106

12 0.025+ 75


56Page of 63




December 20, 2005

Report No: 05-809











7.05

75

1

12

0.749

0.426

10/10

0

10/10





mgDiamond

Count

1 1.14 0.90 0.68 Colorless, opaque, octahedron, broken, stepped/ribbed, shieldlaminae.

0.749 0.749+ 600

1 0.60 0.42 0.40 White, clear, octahedron, stepped/ribbed, serrate laminae, shieldlaminae.

0.136 0.233+ 300

1 0.38 0.36 0.36 Colorless, cloudy, octahedron, resorbed, hillocks, low reliefsurfaces.

0.097+ 300

1 0.36 0.30 0.28 Colorless, opaque, aggregate, broken, resorbed.0.159+ 2121 0.32 0.30 0.30 Colorless, opaque, cubic, resorbed, rough.+ 2121 0.26 0.22 0.22 Colorless, opaque, octahedron, resorbed, hillocks, low relief

surfaces.+ 212

2 0.013+ 106

5 0.021+ 75


57Page of 63




December 20, 2005

Report No: 05-809











6.80

75

0

2

0

0.006

8/10

0

9/10





mgDiamond

Count

2 0.006+ 106


58Page of 63




December 20, 2005

Report No: 05-809











4.05

75

0

14

0

0.283

10/10

0

8/10





mgDiamond

Count

1 0.46 0.44 0.30 Colorless, clear, octahedron, twinned, shield laminae.0.097 0.097+ 300

1 0.50 0.36 0.24 Colorless, clear, distorted.0.143+ 2121 0.44 0.30 0.16 Grey, opaque, polycrystalline aggregate, broken.+ 2121 0.40 0.24 0.20 Black, opaque, polycrystalline aggregate, broken.+ 2121 0.30 0.28 0.28 Yellow, frosted, cubic, resorbed.+ 212

1 0.010+ 150

5 0.028+ 106

3 0.005+ 75


59Page of 63




December 20, 2005

Report No: 05-809











6.60

75

1

25

0.225

0.319

10/10

0

10/10





mgDiamond

Count

1 0.70 0.50 0.40 Yellow, frosted, distorted, pits.0.225 0.405+ 4251 0.56 0.52 0.40 White, opaque, octahedron, resorbed, hillocks.0.180+ 425

6 0.090+ 150

8 0.024+ 106

10 0.025+ 75


60Page of 63




December 20, 2005

Report No: 05-809











6.70

75

3

54

2.370

1.024

10/10

0

10/10





mgDiamond

Count

1 1.04 0.80 0.38 Yellow, included, thh, broken, lamination.0.945 2.370+ 6001 1.16 0.76 0.76 Black, included, irregular, resorbed.0.765+ 6001 1.00 0.64 0.54 Colorless, clear, octahedron, twinned, stepped/ribbed, serrate

laminae, trigonal pits.0.660+ 600

1 0.82 0.44 0.32 Grey, included, polycrystalline aggregate, resorbed.0.249 0.249+ 425

1 0.42 0.38 0.36 White, opaque, cubic.0.199 0.516+ 3001 0.38 0.36 0.32 White, opaque, cubic, crescentic steps.0.150+ 3001 0.52 0.38 0.36 Colorless, clear, octahedron, twinned, stepped/ribbed.0.119+ 3001 0.42 0.36 0.18 White, cloudy, fragment, lamination.0.048+ 300

1 0.44 0.24 0.20 Black, included, polycrystalline aggregate, resorbed.0.095+ 2121 0.38 0.26 0.20 Colorless, clear, irregular, resorbed.+ 2121 0.32 0.26 0.18 Colorless, clear, aggregate, resorbed.+ 212

6 0.060+ 150

12 0.067+ 106

61Page of 63




December 20, 2005

Report No: 05-809






mgDiamond

Count

28 0.037+ 75


62Page of 63




December 20, 2005

Report No: 05-809











6.80

75

0

23

0

0.305

9/10

0

10/10





mgDiamond

Count

1 0.34 0.32 0.28 White, opaque, cubic, pits.0.081 0.158+ 3001 0.50 0.32 0.24 Colorless, clear, distorted.0.077+ 300

1 0.34 0.24 0.18 Colorless, clear, macle, twinned, stepped/ribbed.0.085+ 2121 0.24 0.24 0.22 Green, opaque, cubic.+ 212

1 0.014+ 150

5 0.024+ 106

13 0.024+ 75


63Page of 63


DIAMOND RECOVERY BY CAUSTIC DISSOLUTIONProject: 8901-463 Date: September 20, 2005Client: Geos Sciences Inc. LIMS No. MI0008-AUG05

Sample No. 15045



- 74 µm 7 0.025 0.000TOTAL 89 1.329 0.007





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Sample No. 15060



- 74 µm 0 0.000 0.000TOTAL 21 0.363 0.002





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Sample No. 15075



- 74 µm 0 0.000 0.000TOTAL 25 1.512 0.008





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Sample No. 19015



- 74 µm 0 0.000 0.000TOTAL 29 0.530 0.003





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Sample No. 19016



- 74 µm 0 0.000 0.000TOTAL 56 2.045 0.010





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Sample No. 19017



- 74 µm 0 0.000 0.000TOTAL 27 0.962 0.005





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Sample No. 19019



- 74 µm 0 0.000 0.000TOTAL 5 0.165 0.001





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Sample No. 19020



- 74 µm 0 0.000 0.000TOTAL 6 0.161 0.001





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Sample No. 19021



- 74 µm 0 0.000 0.000TOTAL 14 0.209 0.001





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Sample No. 19023



- 74 µm 0 0.000 0.000TOTAL 39 1.904 0.010





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Sample No. 19024



- 74 µm 0 0.000 0.000TOTAL 888 7.226 0.036





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Sample No. 19025



- 74 µm 0 0.000 0.000TOTAL 18 0.356 0.002





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CHAB 05-11

SAMPLE LAB LAB From To Length Weight MICRONS TOTALNO. CERT metres metres metres Kgs +75 +106 +150 +212 +300 +425 +600 +850 +1180 DIAMONDS15090 SGS 15090 15.40 19.00 3.60 7.93 0 2 1 0 0 0 0 0 0 315091 SRC 05-1037 19.00 22.50 3.50 8.3 1 0 0 0 0 0 0 0 0 115092 SRC 05-1037 22.50 26.60 4.10 9.05 1 0 0 0 0 0 0 0 0 1

15093 1/2 SRC 05-1037 26.60 30.80 4.20 4.65 0 0 0 0 0 0 0 0 0 015093 2/2 SRC 05-1037 4.7 1 0 0 0 0 0 0 0 0 1

15094 SRC 05-1037 30.80 34.30 3.50 7.5 4 5 3 0 1 1 0 0 0 1415095 SRC 05-1037 34.30 37.80 3.50 8.25 52 26 24 13 4 2 1 1 0 12315096 SRC 05-1037 37.80 41.50 3.70 8.5 11 7 12 2 1 4 0 0 0 3715097 SRC 05-1037 41.50 44.96 3.46 8 4 3 1 1 0 0 0 0 0 915098 SRC 05-1037 44.96 48.50 3.54 8.55 4 1 0 0 0 0 0 0 0 515099 SRC 05-1037 48.50 52.00 3.50 7.5 0 0 0 0 0 0 0 0 0 0

RS-15100 SRC 05-1037 52.00 55.50 3.50 8 0 0 0 0 0 0 0 0 0 015101 SRC 05-1037 55.50 59.00 3.50 9.05 0 0 0 0 0 0 0 0 0 0

15102 1/2 SRC 05-1037 59.00 62.50 3.50 5 0 0 0 0 0 0 0 0 0 015102 2/2 SRC 05-1037 4.4 0 0 0 0 0 0 0 0 0 0

15103 SRC 05-1037 62.50 66.00 3.50 7.45 0 0 0 0 0 0 0 0 0 015104 SRC 05-1037 66.00 69.80 3.80 7.95 3 0 0 0 0 0 0 0 0 315105 SGS 15105 69.80 73.70 3.90 8.64 0 0 0 0 0 0 0 0 0 015106 SRC 05-1037 73.70 77.54 3.84 8.45 1 0 0 0 0 0 0 0 0 115107 SRC 05-1037 77.54 81.00 3.46 8.5 13 7 1 1 0 0 0 0 0 2215108 SRC 05-1037 81.00 84.00 3.00 7.85 22 17 13 6 4 1 1 0 0 6415109 SRC 05-1037 84.00 87.00 3.00 8.2 0 1 1 1 0 0 0 0 0 315110 SRC 05-1037 87.00 90.00 3.00 8.25 6 3 0 3 0 0 0 0 0 1215111 SRC 05-1037 90.00 93.00 3.00 8 8 4 3 0 0 1 0 0 0 1615112 SRC 05-1037 93.00 96.10 3.10 8.2 4 5 1 1 0 1 1 0 0 1315113 SRC 05-1037 96.10 99.20 3.10 8.3 8 0 1 2 1 1 0 0 0 1315114 SRC 05-1037 99.20 102.40 3.20 8.55 8 10 2 6 1 1 1 0 0 2915115 SRC 05-1037 102.40 103.58 1.18 2.9 0 0 0 0 0 0 0 0 0 0

15116 1/2 SRC 05-1037 103.58 107.75 4.17 5.7 1 1 3 0 3 1 0 0 0 915116 2/2 SRC 05-1037 5.65 5 1 2 0 1 1 0 0 0 10

15117 SRC 05-1037 107.75 111.30 3.55 6.8 4 6 5 3 0 1 1 0 0 2015118 SRC 05-1037 111.30 114.20 2.90 5.65 0 0 0 0 0 0 0 0 0 015119 SRC 05-1037 114.20 117.00 2.80 7.5 11 12 3 3 1 2 1 0 0 3315120 SGS 15120 117.00 120.00 3.00 7.73 21 20 11 4 8 0 0 0 0 6415121 SRC 05-1037 120.00 123.60 3.60 8.1 0 0 0 1 0 0 0 0 0 1

CHAB 05-11

SAMPLE LAB LAB From To Length Weight MICRONS TOTALNO. CERT metres metres metres Kgs +75 +106 +150 +212 +300 +425 +600 +850 +1180 DIAMONDS15122 SRC 05-1037 123.60 125.90 2.30 4.35 3 1 1 0 0 0 0 0 0 515123 SRC 05-1037 125.90 126.80 0.90 2.6 0 0 0 0 0 0 0 0 0 015124 SRC 05-1037 126.80 130.30 3.50 7.35 10 6 1 0 3 0 0 0 0 2015125 SRC 05-1037 130.30 132.70 2.40 5.45 29 13 5 3 0 1 0 0 0 5115126 SRC 05-1037 132.70 136.20 3.50 6.35 5 4 5 1 0 0 0 0 0 1515127 SRC 05-1037 136.20 139.70 3.50 7.05 71 68 27 18 11 7 4 0 2 20815128 SRC 05-1037 139.70 143.20 3.50 7.1 8 3 2 2 0 0 1 0 0 1615129 SRC 05-1037 143.20 146.80 3.60 6.7 7 2 3 0 0 0 0 0 0 1215130 SRC 05-1037 146.80 150.30 3.50 7 0 0 0 0 0 0 0 0 0 015131 SRC 05-1037 150.30 153.80 3.50 7.2 21 13 7 10 4 2 1 1 0 5915132 SRC 05-1037 153.80 157.30 3.50 7.05 7 0 3 2 0 0 0 0 0 1215133 SRC 05-1037 157.30 160.80 3.50 6.95 18 9 3 10 1 3 0 0 0 4415134 SRC 05-1037 160.80 164.30 3.50 7.3 18 8 11 7 3 1 1 0 0 4915135 SGS 15135 164.30 167.80 3.50 6.95 10 12 4 6 4 1 1 0 0 3815136 SRC 05-1037 167.80 171.30 3.50 7.8 10 3 6 4 3 1 0 0 0 2715137 SRC 05-1037 171.30 174.12 2.82 5.7 4 6 3 4 0 1 1 0 0 1915138 SRC 05-1037 174.12 177.60 3.48 6.95 8 6 3 1 2 0 0 0 0 2015139 SRC 05-1037 177.60 181.10 3.50 7.6 6 3 1 0 1 0 2 0 0 1315140 SRC 05-1037 181.10 184.60 3.50 7.65 5 5 0 3 1 0 0 0 0 1415141 SRC 05-1037 184.60 188.10 3.50 7.3 15 8 6 5 0 0 1 0 0 3515142 SRC 05-1037 188.10 191.40 3.30 6.75 8 7 7 6 6 1 0 0 0 3515143 SRC 05-1037 191.40 194.90 3.50 7.55 5 9 5 1 2 1 2 0 0 2515144 SRC 05-1037 194.90 199.34 4.44 8.95 9 10 2 2 2 2 0 1 0 2815145 SRC 05-1037 199.34 203.60 4.26 8.65 8 6 3 3 2 0 0 0 0 2215146 SRC 05-1037 203.60 205.40 1.80 3.55 0 2 3 2 0 0 0 0 0 715147 SRC 05-1037 205.40 209.31 3.91 7.8 25 16 8 11 4 4 0 0 0 6815148 SRC 05-1037 209.31 213.16 3.85 7.5 7 19 11 3 3 5 0 0 0 4815149 SRC 05-1037 213.16 215.38 2.22 4.95 0 0 0 0 0 0 0 0 0 015150 SGS 15150 215.38 218.85 3.47 6.54 7 1 7 5 2 1 0 0 0 2315151 SRC 05-1037 218.85 222.35 3.50 6.9 317 103 19 1 2 1 0 0 0 44315152 SRC 05-1037 222.35 225.80 3.45 7.25 9 4 3 4 2 1 0 0 0 2315153 SRC 05-1037 225.80 229.53 3.73 7.5 11 11 8 5 2 1 0 1 0 3915154 SRC 05-1037 229.53 232.85 3.32 8.6 13 12 6 2 2 1 0 0 0 3615155 SRC 05-1037 232.85 236.35 3.50 8.7 5 8 4 2 2 1 0 0 0 2215156 SRC 05-1037 236.35 239.28 2.93 7 10 9 7 0 1 2 0 0 0 29

CHAB 05-11

SAMPLE LAB LAB From To Length Weight MICRONS TOTALNO. CERT metres metres metres Kgs +75 +106 +150 +212 +300 +425 +600 +850 +1180 DIAMONDS15157 SRC 05-1037 239.28 241.90 2.62 7.1 8 6 0 2 1 0 0 0 0 17

15158 1/2 SRC 05-1037 241.90 245.40 3.50 4.5 0 1 0 0 0 0 0 0 0 115158 2/2 SRC 05-1037 4.65 0 0 0 0 0 0 0 0 0 0

15159 SRC 05-1037 258.00 260.95 2.95 8.15 0 0 0 0 0 0 0 0 0 015160 SRC 05-1037 260.95 264.50 3.55 8.45 0 0 0 0 0 0 0 0 0 015161 SRC 05-1037 264.50 367.32 2.82 6.2 0 0 0 0 0 0 0 0 0 015162 SRC 05-1037 367.32 271.32 4.00 6.95 0 0 0 0 0 0 0 0 0 015163 SGS 15163 271.32 271.97 0.65 1.86 0 0 0 0 0 0 0 0 0 0

243.97 546.20 890 525 271 172 91 55 20 4 2 2030QA/QC

19027 SGS 19027 15.40 19.00 3.60 7.56 1 0 0 0 0 0 0 0 0 119028 SGS 19028 34.30 37.80 3.50 7.77 19 21 15 10 5 1 0 1 0 7219029 SGS 19029 37.80 41.50 3.70 6.11 5 0 20 3 2 0 0 0 0 3019030 SRC 05-1037 52.00 55.50 3.50 8.15 0 0 0 0 0 0 0 0 0 019031 SGS 19031 69.80 73.70 3.90 9.16 0 2 0 0 0 0 0 0 0 219032 SGS 19032 87.00 90.00 3.00 5.89 0 1 3 1 2 1 0 0 0 819033 SGS 19033 90.00 93.00 3.00 5.68 5 0 4 1 1 1 0 0 0 1219034 SRC 05-1037 102.40 103.58 1.18 1.90 0 1 0 0 0 0 0 0 0 119035 SGS 19035 117.00 120.00 3.00 5.52 22 16 11 3 5 0 0 0 1 5819036 SGS 19036 130.30 132.70 2.40 5.58 0 0 0 0 0 0 0 0 0 019037 SGS 19037 132.70 136.20 3.50 8.93 8 8 8 2 3 0 0 0 0 29

19038 1/2 SRC 05-1037 146.80 150.30 3.50 4.60 7 0 3 0 0 1 0 0 0 1119038 2/2 SRC 05-1037 146.80 150.30 3.50 4.60 9 1 1 1 0 1 0 0 0 13

19039 SGS 19039 164.30 167.80 3.50 8.93 13 15 5 3 2 2 0 0 0 4019040 SGS 19040 181.10 184.60 3.50 8.67 5 5 3 1 0 1 1 0 0 1619041 SGS 19041 184.60 188.10 3.50 8.85 8 7 4 4 0 0 0 0 0 23

19042 1/2 SRC 05-1037 184.60 188.10 3.50 5.80 13 0 11 2 1 2 1 0 0 3019042 2/2 SRC 05-1037 199.34 203.60 4.26 5.85 6 3 1 0 4 0 1 0 0 15

19043 SGS 19043 215.38 218.85 3.47 8.70 17 15 3 1 4 1 0 0 0 4119044 SGS 19044 232.85 236.35 3.50 8.82 14 9 8 4 1 1 0 0 0 3719045 SGS 19045 236.35 239.28 2.93 6.51 9 5 6 2 2 0 0 0 0 2419046 SRC 05-1037 260.95 264.50 3.55 8.40 0 0 0 0 0 0 0 0 0 019047 SGS 19047 271.32 271.97 0.65 1.63 0 0 0 0 0 0 0 0 0 0

73.64 153.61 161 109 106 38 32 12 3 1 1 463





February 1, 2006

Report No: 05-1037











10/1015091 8.30 75 0 1 0 0.003 10/10 010/1015092 9.05 75 0 1 0 0.001 10/10 010/1015093 1/2 4.65 75 0 0 0 0 10/10 09/1015093 2/2 4.70 75 0 1 0 0.002 8/10 010/1015094 7.50 75 0 14 0 0.463 10/10 0

10/1015095 8.25 75 4 119 3.600 1.339 10/10 010/1015096 8.50 75 3 34 0.941 0.688 10/10 010/1015097 8.00 75 0 9 0 0.065 8/10 010/1015098 8.55 75 0 5 0 0.017 10/10 010/1015099 7.50 75 0 0 0 0 10/10 0

10/1015100 8.00 75 0 0 0 0 10/10 010/1015101 9.05 75 0 0 0 0 10/10 49/1015102 1/2 5.00 75 0 0 0 0 10/10 010/1015102 2/2 4.40 75 0 0 0 0 10/10 010/1015103 7.45 75 0 0 0 0 8/10 0

8/1015104 7.95 75 0 3 0 0.018 10/10 010/1015106 8.45 75 0 1 0 0.001 10/10 410/1015107 8.50 75 0 22 0 0.092 9/10 08/1015108 7.85 75 2 62 0.839 1.067 9/10 210/1015109 8.20 75 0 3 0 0.045 10/10 0

10/1015110 8.25 75 0 12 0 0.258 10/10 010/1015111 8.00 75 0 16 0 0.362 8/10 08/1015112 8.20 75 1 12 0.568 0.351 10/10 08/1015113 8.30 75 1 12 0.283 0.219 9/10 010/1015114 8.55 75 2 27 0.853 0.355 8/10 1

1Page of 64





February 1, 2006

Report No: 05-1037


9/1015115 2.90 75 0 0 0 0 10/10 010/1015116 1/2 5.70 75 0 9 0 0.556 10/10 09/1015116 2/2 5.65 75 0 10 0 0.326 10/10 010/1015117 6.80 75 2 18 0.829 0.179 9/10 29/1015118 5.65 75 0 0 0 0 9/10 0

9/1015119 7.50 75 2 31 0.782 0.471 10/10 09/1015121 8.10 75 0 1 0 0.012 10/10 210/1015122 4.35 75 0 5 0 0.021 9/10 09/1015123 2.60 75 0 0 0 0 8/10 010/1015124 7.35 75 0 20 0 0.247 10/10 1

10/1015125 5.45 75 1 50 0.560 0.307 10/10 310/1015126 6.35 75 0 15 0 0.122 10/10 010/1015127 7.05 75 10 198 18.995 2.530 10/10 110/1015128 7.10 75 1 15 1.005 0.216 10/10 010/1015129 6.70 75 0 12 0 0.162 9/10 0

8/1015130 7.00 75 0 0 0 0 9/10 1010/1015131 7.20 75 2 57 2.627 1.172 10/10 159/1015132 7.05 75 0 12 0 0.116 10/10 010/1015133 6.95 75 1 43 0.394 0.807 10/10 010/1015134 7.30 75 2 47 1.151 0.675 10/10 1

9/1015136 7.80 75 0 27 0 0.520 9/10 010/1015137 5.70 75 2 17 0.833 0.152 8/10 110/1015138 6.95 75 0 20 0 0.380 10/10 010/1015139 7.60 75 2 11 1.190 0.119 10/10 310/1015140 7.65 75 0 14 0 0.287 10/10 0

10/1015141 7.30 75 1 34 0.610 0.271 10/10 010/1015142 6.75 75 0 35 0 1.259 10/10 010/1015143 7.55 75 3 22 1.711 0.384 9/10 010/1015144 8.95 75 1 27 1.635 0.722 10/10 09/1015145 8.65 75 0 22 0 0.445 9/10 4

9/1015146 3.55 75 0 7 0 0.184 10/10 19/1015147 7.80 75 0 68 0 1.774 10/10 69/1015148 7.50 75 0 48 0 1.769 10/10 010/1015149 4.95 75 0 0 0 0 9/10 010/1015151 6.90 75 0 443 0 1.690 10/10 1

10/1015152 7.25 75 0 23 0 0.840 10/10 0

2Page of 64





February 1, 2006

Report No: 05-1037


10/1015153 7.50 75 1 38 1.764 0.536 8/10 010/1015154 8.60 75 0 36 0 0.797 10/10 010/1015155 8.70 75 1 21 0.487 0.367 10/10 09/1015156 7.00 75 0 29 0 0.722 10/10 09/1015157 7.10 75 0 17 0 0.165 10/10 4

10/1015158 1/2 4.50 75 0 1 0 0.010 10/10 010/1015158 2/2 4.65 75 0 0 0 0 10/10 010/1015159 8.15 75 0 0 0 0 10/10 09/1015160 8.45 75 0 0 0 0 10/10 010/1015161 6.20 75 0 0 0 0 9/10 0

10/1015162 6.95 75 0 0 0 0 8/10 010/1019030 8.15 75 0 0 0 0 10/10 010/1019034 1.90 75 0 1 0 0.004 10/10 010/1019038 1/2 4.60 75 1 10 0.306 0.068 10/10 010/1019038 2/2 4.60 75 0 13 0 0.271 10.10 0

10/1019042 1/2 5.80 75 1 29 0.744 0.647 10/10 010/1019042 2/2 5.85 75 1 14 0.769 0.364 10/10 010/1019046 8.40 75 0 0 0 0 10/10 0


3Page of 64




February 1, 2006

Report No: 05-1037











8.30

75

0

1

0

0.003

10/10

0

10/10





mgDiamond

Count

1 0.003+ 75


4Page of 64




February 1, 2006

Report No: 05-1037











9.05

75

0

1

0

0.001

10/10

0

10/10





mgDiamond

Count

1 0.001+ 75

Total octacarats in this sample is: 500.00

5Page of 64




February 1, 2006

Report No: 05-1037











4.70

75

0

1

0

0.002

8/10

0

9/10





mgDiamond

Count

1 0.002+ 75


6Page of 64




February 1, 2006

Report No: 05-1037











7.50

75

0

14

0

0.463

10/10

0

10/10





mgDiamond

Count

1 0.253+ 425

1 0.147+ 300

3 0.032+ 150

5 0.024+ 106

4 0.007+ 75


7Page of 64




February 1, 2006

Report No: 05-1037











8.25

75

4

119

3.600

1.339

10/10

0

10/10





mgDiamond

Count

1 1.46 1.08 1.02 White, included, distorted, serrate laminae, pits.2.552 2.552+ 850

1 0.555 0.555+ 600

1 0.365 0.493+ 4251 0.128+ 425

4 0.560+ 300

13 0.320+ 212

24 0.258+ 150

26 0.116+ 106

52 0.085+ 75


8Page of 64




February 1, 2006

Report No: 05-1037











8.50

75

3

34

0.941

0.688

10/10

0

10/10





mgDiamond

Count

1 0.451 1.178+ 4251 0.264+ 4251 0.226+ 4251+ 425

1 0.098+ 300

2 0.074+ 212

12 0.204+ 150

7 0.028+ 106

11 0.047+ 75


9Page of 64




February 1, 2006

Report No: 05-1037











8.00

75

0

9

0

0.065

8/10

0

10/10





mgDiamond

Count

1 0.034+ 212

1 0.018+ 150

3 0.007+ 106

4 0.006+ 75


10Page of 64




February 1, 2006

Report No: 05-1037











8.55

75

0

5

0

0.017

10/10

0

10/10





mgDiamond

Count

1 0.003+ 106

4 0.014+ 75


11Page of 64




February 1, 2006

Report No: 05-1037











7.95

75

0

3

0

0.018

10/10

0

8/10





mgDiamond

Count

3 0.018+ 75


12Page of 64




February 1, 2006

Report No: 05-1037











8.45

75

0

1

0

0.001

10/10

4

10/10





mgDiamond

Count

1 0.001+ 75

Total octacarats in this sample is: 500.00

13Page of 64




February 1, 2006

Report No: 05-1037











8.50

75

0

22

0

0.092

9/10

0

10/10





mgDiamond

Count

1 0.021+ 212

1 0.012+ 150

7 0.028+ 106

13 0.031+ 75


14Page of 64




February 1, 2006

Report No: 05-1037











7.85

75

2

62

0.839

1.067

9/10

2

8/10





mgDiamond

Count

1 0.373 0.373+ 600

1 0.466 0.466+ 425

4 0.558+ 300

6 0.245+ 212

13 0.153+ 150

17 0.070+ 106

22 0.041+ 75


15Page of 64




February 1, 2006

Report No: 05-1037











8.20

75

0

3

0

0.045

10/10

0

10/10





mgDiamond

Count

1 0.025+ 212

1 0.010+ 150

1 0.010+ 106


16Page of 64




February 1, 2006

Report No: 05-1037











8.25

75

0

12

0

0.258

10/10

0

10/10





mgDiamond

Count

3 0.219+ 212

3 0.020+ 106

6 0.019+ 75


17Page of 64




February 1, 2006

Report No: 05-1037











8.00

75

0

16

0

0.362

8/10

0

10/10





mgDiamond

Count

1 0.268+ 425

3 0.053+ 150

4 0.021+ 106

8 0.020+ 75


18Page of 64




February 1, 2006

Report No: 05-1037











8.20

75

1

12

0.568

0.351

10/10

0

8/10





mgDiamond

Count

1 0.568 0.568+ 600

1 0.234+ 425

1 0.047+ 212

1 0.026+ 150

5 0.028+ 106

4 0.016+ 75


19Page of 64




February 1, 2006

Report No: 05-1037











8.30

75

1

12

0.283

0.219

9/10

0

8/10





mgDiamond

Count

1 0.283 0.283+ 425

1 0.111+ 300

2 0.075+ 212

1 0.018+ 150

8 0.015+ 75


20Page of 64




February 1, 2006

Report No: 05-1037











8.55

75

2

27

0.853

0.355

8/10

1

10/10





mgDiamond

Count

1 0.497 0.497+ 600

1 0.356 0.356+ 425

1 0.076+ 300

6 0.221+ 212

2 0.012+ 150

10 0.030+ 106

8 0.016+ 75


21Page of 64




February 1, 2006

Report No: 05-1037











5.70

75

0

9

0

0.556

10/10

0

10/10





mgDiamond

Count

1 0.216+ 425

3 0.289+ 300

3 0.045+ 150

1 0.005+ 106

1 0.001+ 75


22Page of 64




February 1, 2006

Report No: 05-1037











5.65

75

0

10

0

0.326

10/10

0

9/10





mgDiamond

Count

1 0.183+ 425

1 0.076+ 300

2 0.044+ 150

1 0.007+ 106

5 0.016+ 75


23Page of 64




February 1, 2006

Report No: 05-1037











6.80

75

2

18

0.829

0.179

9/10

2

10/10





mgDiamond

Count

1 0.541 0.541+ 600

1 0.288 0.288+ 425

3 0.076+ 212

5 0.070+ 150

6 0.024+ 106

4 0.009+ 75


24Page of 64




February 1, 2006

Report No: 05-1037











7.50

75

2

31

0.782

0.471

10/10

0

9/10





mgDiamond

Count

1 0.482 0.482+ 600

1 0.300 0.462+ 4251+ 425

1 0.088+ 300

3 0.065+ 212

3 0.056+ 150

12 0.068+ 106

11 0.032+ 75


25Page of 64




February 1, 2006

Report No: 05-1037











8.10

75

0

1

0

0.012

10/10

2

9/10





mgDiamond

Count

1 0.012+ 212


26Page of 64




February 1, 2006

Report No: 05-1037











4.35

75

0

5

0

0.021

9/10

0

10/10





mgDiamond

Count

1 0.012+ 150

1 0.004+ 106

3 0.005+ 75


27Page of 64




February 1, 2006

Report No: 05-1037











7.35

75

0

20

0

0.247

10/10

1

10/10





mgDiamond

Count

3 0.204+ 300

1 0.013+ 150

6 0.018+ 106

10 0.012+ 75


28Page of 64




February 1, 2006

Report No: 05-1037











5.45

75

1

50

0.560

0.307

10/10

3

10/10





mgDiamond

Count

1 0.560 0.560+ 425

3 0.141+ 212

5 0.054+ 150

13 0.057+ 106

29 0.055+ 75


29Page of 64




February 1, 2006

Report No: 05-1037











6.35

75

0

15

0

0.122

10/10

0

10/10





mgDiamond

Count

1 0.034+ 212

5 0.055+ 150

4 0.019+ 106

5 0.014+ 75


30Page of 64




February 1, 2006

Report No: 05-1037











7.05

75

10

198

18.995

2.530

10/10

1

10/10





mgDiamond

Count

1 2.80 1.60 1.34 White, included, fragment, broken, rough, lamination.7.347 13.846+11801 2.38 1.28 0.92 White, included, fragment, broken, rough, lamination.6.499+1180

1 1.029 3.473+ 6001 0.909+ 6001 0.818+ 6001 0.717+ 600

1 0.556 2.161+ 4251 0.473+ 4251 0.366+ 4251 0.281+ 4253+ 425

11 0.896+ 300

18 0.535+ 212

27 0.256+ 150

31Page of 64




February 1, 2006

Report No: 05-1037






mgDiamond

Count

68 0.249+ 106

71 0.109+ 75


32Page of 64




February 1, 2006

Report No: 05-1037











7.10

75

1

15

1.005

0.216

10/10

0

10/10





mgDiamond

Count

1 1.005 1.005+ 600

2 0.106+ 212

2 0.040+ 150

3 0.020+ 106

8 0.050+ 75


33Page of 64




February 1, 2006

Report No: 05-1037











6.70

75

0

12

0

0.162

9/10

0

10/10





mgDiamond

Count

3 0.114+ 150

2 0.025+ 106

7 0.023+ 75


34Page of 64




February 1, 2006

Report No: 05-1037











7.20

75

2

57

2.627

1.172

10/10

15

10/10





mgDiamond

Count

1 1.38 1.02 0.78 Colorless, clear, octahedral, twinned, broken, stepped/ribbed,etched trigons, lamination, trigonal pits.

1.797 1.797+ 850

1 0.830 0.830+ 600

1 0.252 0.405+ 4251 0.153+ 425

4 0.330+ 300

10 0.284+ 212

7 0.081+ 150

13 0.042+ 106

21 0.030+ 75


35Page of 64




February 1, 2006

Report No: 05-1037











7.05

75

0

12

0

0.116

10/10

0

9/10





mgDiamond

Count

2 0.090+ 212

3 0.016+ 150

7 0.010+ 75


36Page of 64




February 1, 2006

Report No: 05-1037











6.95

75

1

43

0.394

0.807

10/10

0

10/10





mgDiamond

Count

1 0.394 0.828+ 4252+ 425

1 0.075+ 300

10 0.196+ 212

3 0.017+ 150

9 0.047+ 106

18 0.038+ 75


37Page of 64




February 1, 2006

Report No: 05-1037











7.30

75

2

47

1.151

0.675

10/10

1

10/10





mgDiamond

Count

1 0.588 0.588+ 600

1 0.563 0.563+ 425

3 0.201+ 300

7 0.220+ 212

11 0.146+ 150

8 0.057+ 106

18 0.051+ 75


38Page of 64




February 1, 2006

Report No: 05-1037











7.80

75

0

27

0

0.520

9/10

0

9/10





mgDiamond

Count

1 0.093+ 425

3 0.230+ 300

4 0.121+ 212

6 0.056+ 150

3 0.007+ 106

10 0.013+ 75


39Page of 64




February 1, 2006

Report No: 05-1037











5.70

75

2

17

0.833

0.152

8/10

1

10/10





mgDiamond

Count

1 0.503 0.503+ 600

1 0.330 0.330+ 425

4 0.081+ 212

3 0.028+ 150

6 0.031+ 106

4 0.012+ 75


40Page of 64




February 1, 2006

Report No: 05-1037











6.95

75

0

20

0

0.380

10/10

0

10/10





mgDiamond

Count

2 0.255+ 300

1 0.051+ 212

3 0.039+ 150

6 0.022+ 106

8 0.013+ 75


41Page of 64




February 1, 2006

Report No: 05-1037











7.60

75

2

11

1.190

0.119

10/10

3

10/10





mgDiamond

Count

1 0.604 1.190+ 6001 0.586+ 600

1 0.084+ 300

1 0.009+ 150

3 0.017+ 106

6 0.009+ 75


42Page of 64




February 1, 2006

Report No: 05-1037











7.65

75

0

14

0

0.287

10/10

0

10/10





mgDiamond

Count

1 0.063+ 300

3 0.161+ 212

5 0.032+ 106

5 0.031+ 75


43Page of 64




February 1, 2006

Report No: 05-1037











7.30

75

1

34

0.610

0.271

10/10

0

10/10





mgDiamond

Count

1 0.610 0.610+ 600

5 0.133+ 212

6 0.063+ 150

8 0.041+ 106

15 0.034+ 75


44Page of 64




February 1, 2006

Report No: 05-1037











6.75

75

0

35

0

1.259

10/10

0

10/10





mgDiamond

Count

1 0.311+ 425

6 0.566+ 300

6 0.214+ 212

7 0.102+ 150

7 0.045+ 106

8 0.021+ 75


45Page of 64




February 1, 2006

Report No: 05-1037











7.55

75

3

22

1.711

0.384

9/10

0

10/10





mgDiamond

Count

1 0.450+ 6001 1.084 1.534+ 600

1 0.177 0.177+ 425

2 0.196+ 300

1 0.026+ 212

5 0.071+ 150

9 0.061+ 106

5 0.030+ 75


46Page of 64




February 1, 2006

Report No: 05-1037











8.95

75

1

27

1.635

0.722

10/10

0

10/10





mgDiamond

Count

1 1.40 0.98 0.60 Amber, milky, distorted, stepped/ribbed, serrate laminae, pits,hillocks.

1.635 1.635+ 850

2 0.372+ 425

2 0.212+ 300

2 0.059+ 212

2 0.019+ 150

10 0.036+ 106

9 0.024+ 75


47Page of 64




February 1, 2006

Report No: 05-1037











8.65

75

0

22

0

0.445

9/10

4

9/10





mgDiamond

Count

2 0.201+ 300

3 0.132+ 212

3 0.047+ 150

6 0.040+ 106

8 0.025+ 75


48Page of 64




February 1, 2006

Report No: 05-1037











3.55

75

0

7

0

0.184

10/10

1

9/10





mgDiamond

Count

2 0.095+ 212

3 0.064+ 150

2 0.025+ 106


49Page of 64




February 1, 2006

Report No: 05-1037











7.80

75

0

68

0

1.774

10/10

6

9/10





mgDiamond

Count

4 0.750+ 425

4 0.449+ 300

11 0.352+ 212

8 0.104+ 150

16 0.074+ 106

25 0.045+ 75


50Page of 64




February 1, 2006

Report No: 05-1037











7.50

75

0

48

0

1.769

10/10

0

9/10





mgDiamond

Count

5 1.041+ 425

3 0.343+ 300

3 0.143+ 212

11 0.154+ 150

19 0.069+ 106

7 0.019+ 75


51Page of 64




February 1, 2006

Report No: 05-1037











6.90

75

0

443

0

1.690

10/10

1

10/10





mgDiamond

Count

1 0.195+ 425

2 0.185+ 300

1 0.028+ 212

19 0.214+ 150

103 0.493+ 106

317 0.575+ 75


52Page of 64




February 1, 2006

Report No: 05-1037











7.25

75

0

23

0

0.840

10/10

0

10/10





mgDiamond

Count

1 0.271+ 425

2 0.267+ 300

4 0.194+ 212

3 0.058+ 150

4 0.026+ 106

9 0.024+ 75


53Page of 64




February 1, 2006

Report No: 05-1037











7.50

75

1

38

1.764

0.536

8/10

0

10/10





mgDiamond

Count

1 1.14 1.04 0.84 White, cloudy, octahedron, broken, etched trigons, rough,lamination.

1.764 1.764+ 850

1 0.104+ 425

2 0.125+ 300

5 0.150+ 212

8 0.072+ 150

11 0.060+ 106

11 0.025+ 75


54Page of 64




February 1, 2006

Report No: 05-1037











8.60

75

0

36

0

0.797

10/10

0

10/10





mgDiamond

Count

1 0.319+ 425

2 0.237+ 300

2 0.051+ 212

6 0.101+ 150

12 0.066+ 106

13 0.023+ 75


55Page of 64




February 1, 2006

Report No: 05-1037











8.70

75

1

21

0.487

0.367

10/10

0

10/10





mgDiamond

Count

1 0.487 0.487+ 425

2 0.179+ 300

2 0.086+ 212

4 0.047+ 150

8 0.042+ 106

5 0.013+ 75


56Page of 64




February 1, 2006

Report No: 05-1037











7.00

75

0

29

0

0.722

10/10

0

9/10





mgDiamond

Count

2 0.458+ 425

1 0.117+ 300

7 0.070+ 150

9 0.042+ 106

10 0.035+ 75


57Page of 64




February 1, 2006

Report No: 05-1037











7.10

75

0

17

0

0.165

10/10

4

9/10





mgDiamond

Count

1 0.046+ 300

2 0.071+ 212

6 0.033+ 106

8 0.015+ 75


58Page of 64




February 1, 2006

Report No: 05-1037











4.50

75

0

1

0

0.010

10/10

0

10/10





mgDiamond

Count

1 0.00 0.00 0.00 0.010+ 106


59Page of 64




February 1, 2006

Report No: 05-1037











1.90

75

0

1

0

0.004

10/10

0

10/10





mgDiamond

Count

1 0.004+ 106


60Page of 64




February 1, 2006

Report No: 05-1037











4.60

75

1

10

0.306

0.068

10/10

0

10/10





mgDiamond

Count

1 0.306 0.306+ 425

3 0.040+ 150

7 0.028+ 75


61Page of 64




February 1, 2006

Report No: 05-1037











4.60

75

0

13

0

0.271

10.10

0

10/10





mgDiamond

Count

1 0.182+ 425

1 0.032+ 212

1 0.026+ 150

1 0.008+ 106

9 0.023+ 75


62Page of 64




February 1, 2006

Report No: 05-1037











5.80

75

1

29

0.744

0.647

10/10

0

10/10





mgDiamond

Count

1 0.744 0.744+ 600

2 0.383+ 425

1 0.092+ 300

2 0.055+ 212

11 0.089+ 150

13 0.028+ 75


63Page of 64




February 1, 2006

Report No: 05-1037











5.85

75

1

14

0.769

0.364

10/10

0

10/10





mgDiamond

Count

1 0.769 0.769+ 600

4 0.328+ 300

1 0.008+ 150

3 0.018+ 106

6 0.010+ 75


64Page of 64

SGS Minerals Services185 Concession St., Box 4300 Tel: (705) 652-2112Lakefield, Ontario Fax: (705) 652-3123K0L 2H0, CANADA

DIAMOND RECOVERY BY CAUSTIC DISSOLUTIONProject: 8901-463 Date: January 3, 2006Client: Geos Sciences Inc. LIMS No. MI0005-OCT05

Sample No. 15090



- 74 µm 0 0.000 0.000TOTAL 3 0.035 0.000

Sample Weight: 7.93 Kg Total Weight (carats)*: 0.000Number of Syndites: 0 Number of Diamonds: 3


Note: SGS Minerals Services is not responsible for the determination of the origin, quality or value of any diamonds recovered. Each +35 mesh (Tyler sieve; +0.420 mm) stone was individually weighed, and the -35 mesh stones were weighed in groups.


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Page 1



Sample No. 15105



- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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Page 1



Sample No. 15120



- 74 µm 0 0.000 0.000TOTAL 64 1.498 0.007





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Page 1



Sample No. 15135



- 74 µm 0 0.000 0.000TOTAL 38 1.900 0.010





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Page 1



Sample No. 15150



- 74 µm 0 0.000 0.000TOTAL 23 0.670 0.003





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Page 1



Sample No. 15163



- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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Page 1



Sample No. 19027



- 74 µm 0 0.000 0.000TOTAL 1 0.004 0.000





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Page 1



Sample No. 19028



- 74 µm 0 0.000 0.000TOTAL 72 4.363 0.022





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Page 1



Sample No. 19029



- 74 µm 0 0.000 0.000TOTAL 30 0.259 0.001





Ston

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ghed

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Sample No. 19031



- 74 µm 0 0.000 0.000TOTAL 2 0.011 0.000





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Sample No. 19032



- 74 µm 0 0.000 0.000TOTAL 8 0.789 0.004





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Sample No. 19033



- 74 µm 0 0.000 0.000TOTAL 12 0.620 0.003





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Sample No. 19035



- 74 µm 0 0.000 0.000TOTAL 58 11.725 0.059





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Sample No. 19036



- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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Sample No. 19037



- 74 µm 0 0.000 0.000TOTAL 29 0.551 0.003





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Sample No. 19039



- 74 µm 0 0.000 0.000TOTAL 40 1.090 0.005





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Sample No. 19040



- 74 µm 0 0.000 0.000TOTAL 16 1.690 0.008





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Sample No. 19041



- 74 µm 0 0.000 0.000TOTAL 23 0.243 0.001





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Sample No. 19043



- 74 µm 0 0.000 0.000TOTAL 41 0.827 0.004





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Sample No. 19044



- 74 µm 0 0.000 0.000TOTAL 37 0.538 0.003





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Sample No. 19045



- 74 µm 0 0.000 0.000TOTAL 24 0.610 0.003





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DIAMOND RECOVERY BY CAUSTIC DISSOLUTIONProject: 8901-463 Date: December 1, 2005Client: Geos Sciences Inc. LIMS No. MI0005-OCT05

Sample No. 19047



- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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CHAB 05-20

SAMPLE LAB LAB From To Length Weight MICRONS TOTALNO. CERT metres metres metres Kgs +75 +106 +150 +212 +300 +425 +600 +850 +1180 +1700 DIAMONDS

16978 SRC 06-717R2 36.40 40.00 3.60 7.85 n/r 0 0 0 0 0 0 0 0 0 016979 SRC 06-717R2 51.60 55.00 3.40 7.70 n/r 3 3 3 0 3 1 0 0 0 1316980 SRC 06-717R2 67.00 70.50 3.50 8.50 n/r 0 0 0 0 0 0 0 0 0 016981 SRC 06-717R2 79.00 82.50 3.50 7.80 n/r 0 0 0 0 0 0 0 0 0 016982 SRC 06-717R2 91.00 94.50 3.50 9.85 n/r 0 0 0 0 0 0 0 0 0 016983 SRC 06-717R2 103.00 106.50 3.50 7.25 n/r 0 0 0 0 0 0 0 0 0 016984 SRC 06-717R2 115.00 118.50 3.50 7.35 n/r 0 0 0 0 0 0 0 0 0 016985 SGS 16985 127.00 130.50 3.50 8.50 n/r 0 0 0 0 0 0 0 0 0 016986 SRC 06-717R2 139.00 142.50 3.50 7.55 n/r 0 0 0 0 0 0 0 0 0 016987 SRC 06-717R2 142.50 146.00 3.50 6.10 n/r 0 0 0 0 0 0 0 0 0 016988 SRC 06-717R2 146.00 149.00 3.00 4.95 n/r 0 0 0 1 0 0 0 0 0 116989 SRC 06-717R2 149.00 151.65 2.65 4.75 n/r 5 3 2 1 0 0 0 0 0 1116990 SRC 06-717R2 151.65 153.50 1.85 7.50 n/r 0 0 0 0 0 0 0 0 0 016991 SRC 06-717R2 153.50 157.00 3.50 6.65 n/r 0 1 0 0 0 0 0 0 0 116993 SRC 06-717R2 160.50 163.70 3.20 5.90 n/r 0 0 0 0 0 0 0 0 0 016994 SRC 06-717R2 163.70 167.50 3.80 7.55 n/r 0 0 0 0 0 0 0 0 0 016995 SRC 06-717R2 167.50 169.60 2.10 4.90 n/r 0 0 0 0 0 0 0 0 0 016996 SRC 06-717R2 169.60 173.00 3.40 7.05 n/r 1 2 0 0 0 0 0 0 0 316997 SRC 06-717R2 173.00 175.00 2.00 3.80 n/r 1 0 0 0 0 0 0 0 0 116998 SRC 06-717R2 175.00 178.50 3.50 8.10 n/r 15 12 6 5 2 2 0 0 1 4316999 SRC 06-717R2 178.50 182.00 3.50 7.50 n/r 19 13 4 0 0 0 0 0 0 3617000 SGS 17000 182.00 185.50 3.50 8.20 8 4 4 4 0 3 0 1 0 0 2417001 SRC 06-717R2 185.50 189.00 3.50 6.55 n/r 6 5 1 1 0 0 0 0 0 1317002 SRC 06-717R2 189.00 192.50 3.50 6.30 n/r 16 10 4 3 1 0 0 0 0 3417003 SRC 06-717R2 192.50 196.00 3.50 6.65 n/r 1 0 0 2 1 2 1 0 0 717004 SRC 06-717R2 196.00 199.50 3.50 6.90 n/r 1 1 1 1 0 1 0 1 0 617005 SRC 06-717R2 199.50 203.00 3.50 8.65 n/r 10 4 4 2 1 0 0 0 0 2117006 SRC 06-717R2 203.00 205.80 2.80 7.05 n/r 5 3 3 0 2 0 0 0 0 1317007 SRC 06-717R2 205.80 209.00 3.20 7.00 n/r 4 1 2 0 0 0 0 0 0 717008 SRC 06-717R2 209.00 212.50 3.50 7.30 n/r 3 3 0 1 1 1 0 0 0 917009 SRC 06-717R2 212.50 216.00 3.50 7.35 n/r 1 2 0 2 0 0 0 0 0 517010 SRC 06-717R2 216.00 219.50 3.50 7.95 n/r 18 5 6 3 0 0 0 0 0 3217011 SRC 06-717R2 219.50 223.00 3.50 7.75 n/r 3 2 2 1 0 1 0 0 0 917012 SRC 06-717R2 223.00 226.50 3.50 7.85 n/r 12 5 4 3 1 0 0 0 0 2517013 SRC 06-717R2 226.50 230.00 3.50 7.95 n/r 14 11 13 7 1 1 1 0 0 48

CHAB 05-20

SAMPLE LAB LAB From To Length Weight MICRONS TOTALNO. CERT metres metres metres Kgs +75 +106 +150 +212 +300 +425 +600 +850 +1180 +1700 DIAMONDS

17014 SRC 06-717R2 230.00 233.50 3.50 8.00 n/r 18 8 4 2 2 1 0 1 0 3617015 SGS 17015 233.50 237.20 3.70 2.00 2 4 4 1 2 0 0 0 0 0 1317016 SRC 06-717R2 237.20 239.05 1.85 4.55 n/r 0 0 0 0 0 0 0 0 0 017017 SRC 06-717R2 239.05 241.60 2.55 5.45 n/r 0 0 0 0 0 0 0 0 0 017018 SRC 06-717R2 241.60 245.00 3.40 7.45 n/r 0 0 0 0 0 0 0 0 0 017019 SRC 06-717R2 245.00 248.50 3.50 7.75 n/r 0 0 0 0 0 0 0 0 0 017020 SRC 06-717R2 248.50 252.00 3.50 7.60 n/r 0 0 0 0 0 0 0 0 0 017021 SRC 06-717R2 252.00 254.50 2.50 6.05 n/r 0 0 0 0 0 0 0 0 0 017022 SRC 06-717R2 254.50 258.00 3.50 8.00 n/r 0 0 0 0 0 0 0 0 0 017023 SRC 06-717R2 258.00 261.50 3.50 7.80 n/r 0 0 0 0 0 0 0 0 0 017024 SRC 06-717R2 261.50 265.00 3.50 7.75 n/r 0 0 0 0 0 0 0 0 0 017025 SRC 06-717R2 265.00 268.50 3.50 7.60 n/r 0 0 0 0 0 0 0 0 0 017026 SRC 06-717R2 268.50 271.00 2.50 5.90 n/r 0 0 0 0 0 0 0 0 0 0

156.50 336.45 10 164 102 64 37 18 10 3 2 1 411QA/QC19202 SRC 06-717R2 67.00 70.50 3.50 7.90 n/r 0 0 0 0 0 0 0 0 0 019203 SGS 19203 127.00 130.50 3.50 7.50 0 0 0 0 0 0 0 0 0 0 019204 SGS 19204 151.65 153.50 1.85 8.14 0 0 0 0 0 0 0 0 0 0 019205 SGS 19205 153.50 157.00 3.50 7.71 0 0 0 0 0 0 0 0 0 0 019206 SGS 19206 157.00 157.00 0.00 5.66 0 0 0 0 0 0 0 0 0 0 016992 SRC 06-717R2 157.00 157.00 0.00 6.65 0 0 0 0 0 0 0 0 0 0 019207 SRC 06-717R2 167.50 169.60 2.10 4.05 n/r 0 0 0 0 0 0 0 0 0 019208 SGS 19208 182.00 185.50 3.50 6.71 11 2 4 1 6 1 0 0 0 25 5019209 SGS 19209 199.50 203.00 3.50 6.51 2 3 3 0 1 0 0 0 0 9 1819210 SGS 19210 203.00 205.80 2.80 6.00 5 9 4 0 3 0 1 0 0 22 4419211 SRC 06-717R2 216.00 219.50 3.50 8.40 n/r 9 5 3 3 1 0 0 0 21 4219212 SGS 19212 233.50 237.20 3.70 8.40 7 5 5 2 4 0 1 0 0 17 4119213 SGS 19213 248.50 252.00 3.50 7.64 0 0 0 0 0 0 0 0 0 0 019214 SGS 19214 252.00 254.50 2.50 5.56 0 0 0 0 0 0 0 0 0 0 019215 SRC 06-717R2 265.00 268.50 3.50 7.35 n/r 0 0 0 0 0 0 0 0 0 0

40.95 104.18 25 28 21 6 17 2 2 0 0 94 195





Report No: 06-717

REVISED

March 02, 2007








6) Weight of Diamonds >106 microns < 500 microns in milligrams (Wt-)



10/1016978 7.85 106 0 0 0 0 10/10 010/1016979 7.70 106 1 12 0.860 0.728 10/10 010/1016980 8.50 106 0 0 0 0 9/10 010/1016981 7.80 106 0 0 0 0 9/10 010/1016982 1/2 4.85 106 0 0 0 0 10/10 0

10/1016982 2/2 5.00 106 0 0 0 0 9/10 010/1016983 7.25 106 0 0 0 0 8/10 010/1016984 7.35 106 0 0 0 0 10/10 010/1016986 7.60 106 0 0 0 0 8/10 010/1016987 7.55 106 0 0 0 0 10/10 0

10/1016988 6.10 106 0 1 0 0.124 10/10 010/1016989 4.95 106 0 11 0 0.233 10/10 010/1016990 4.75 106 0 0 0 0 9/10 09/1016991 7.50 106 0 1 0 0.018 10/10 010/1016992 6.65 106 0 0 0 0 9/10 0

10/1016993 5.90 106 0 0 0 0 9/10 010/1016994 7.55 106 0 0 0 0 10/10 010/1016995 4.90 106 0 0 0 0 10/10 010/1016996 7.05 106 0 3 0 0.023 10/10 010/1016997 3.80 106 0 1 0 0.005 9/10 0

9/1016998 8.10 106 4 39 12.611 1.214 9/10 014/1416999 7.50 106 0 36 0 0.338 10/10 010/1017001 6.55 106 0 13 0 0.232 10/10 010/1017002 6.30 106 1 33 0.460 0.759 10/10 010/1017003 6.65 106 3 4 4.929 0.403 10/10 0

1Page of 28





Report No: 06-717

REVISED

March 02, 2007


10/1017004 6.90 106 2 4 9.640 0.218 9/10 09/1017005 8.65 106 1 20 0.420 0.533 10/10 09/1017006 7.05 106 1 12 0.340 0.346 10/10 010/1017007 7.00 106 0 7 0 0.077 10/10 110/1017008 7.30 106 2 7 1.095 0.158 10/10 1

9/1017009 7.35 106 0 5 0 0.354 10/10 010/1017010 7.95 106 0 32 0 0.743 9/10 010/1017011 7.75 106 1 8 1.468 0.285 9/10 110/1017012 7.85 106 0 25 0 0.846 9/10 010/1017013 7.95 106 2 46 3.995 1.431 9/10 0

10/1017014 8.00 106 2 34 5.819 0.859 10/10 010/1017016 4.55 106 0 0 0 0 10/10 010/1017017 5.45 106 0 0 0 0 10/10 010/1017018 7.45 106 0 0 0 0 10/10 09/1017019 7.75 106 0 0 0 0 7/10 1

10/1017020 7.60 106 0 0 0 0 10/10 010/1017021 6.05 106 0 0 0 0 10/10 08/1017022 8.00 106 0 0 0 0 10/10 09/1017023 7.80 106 0 0 0 0 10/10 010/1017024 7.75 106 0 0 0 0 9/10 0

9/1017025 7.60 106 0 0 0 0 6/10 010/1017026 5.90 106 0 0 0 0 10/10 010/1019202 7.90 106 0 0 0 0 9/10 018/2019207 4.05 106 0 0 0 0 8/10 010/1019211 8.40 106 0 21 0 0.707 10/10 0

9/1019215 7.35 106 0 0 0 0 10/10 0..7/10 Synthetic tracers were recovered for sample # 17019.QC2 recovery was 9/10 and no other recovery deviations were reported for the group..6/10 Synthetic tracers were recovered for sample # 17025.QC2 recovery was 9/10 and no other recovery deviations were reported for the group.The method validation allows for a 95% confidence level for a minimum tracer recovery of 80%.The reported QC failure is therefore within acceptable limits set by the method.

2Page of 28




Report No: 06-717

REVISED

March 02, 2007



3Page of 28




Report No: 06-717

REVISED

March 02, 2007









Weight of Diamonds >106 microns < 500 microns in milligrams (Wt-)


7.70

106

1

12

0.860

0.728

10/10

0

10/10





mgDiamond

Count

1 0.860 0.860+ 600

1 0.267 0.595+ 4251 0.164+ 4251 0.164+ 425

3 0.093+ 212

3 0.024+ 150

3 0.016+ 106


4Page of 28




Report No: 06-717

REVISED

March 02, 2007











6.10

106

0

1

0

0.124

10/10

0

10/10





mgDiamond

Count

1 0.124 0.124+ 300


5Page of 28




Report No: 06-717

REVISED

March 02, 2007











4.95

106

0

11

0

0.233

10/10

0

10/10





mgDiamond

Count

1 0.104 0.104+ 300

2 0.072+ 212

3 0.032+ 150

5 0.025+ 106


6Page of 28




Report No: 06-717

REVISED

March 02, 2007











7.50

106

0

1

0

0.018

10/10

0

9/10





mgDiamond

Count

1 0.018+ 150


7Page of 28




Report No: 06-717

REVISED

March 02, 2007











7.05

106

0

3

0

0.023

10/10

0

10/10





mgDiamond

Count

2 0.019+ 150

1 0.004+ 106


8Page of 28




Report No: 06-717

REVISED

March 02, 2007











3.80

106

0

1

0

0.005

9/10

0

10/10





mgDiamond

Count

1 0.005+ 106


9Page of 28




Report No: 06-717

REVISED

March 02, 2007











8.10

106

4

39

12.611

1.214

9/10

0

9/10





mgDiamond

Count

1 2.90 2.16 White, clear, fragment, lamination.11.156 11.156+1700 1.20

1 0.655 1.100+ 6001 0.445+ 600

1 0.355 0.488+ 4251 0.133+ 425

1 0.316 0.705+ 3001 0.135+ 3001 0.122+ 3001 0.075+ 3001 0.057+ 300

6 0.167+ 212

12 0.144+ 150

15 0.065+ 106

10Page of 28




Report No: 06-717

REVISED

March 02, 2007



11Page of 28




Report No: 06-717

REVISED

March 02, 2007











7.50

106

0

36

0

0.338

10/10

0

14/14





mgDiamond

Count

4 0.115+ 212

13 0.145+ 150

19 0.078+ 106


12Page of 28




Report No: 06-717

REVISED

March 02, 2007











6.55

106

0

13

0

0.232

10/10

0

10/10





mgDiamond

Count

1 0.094 0.094+ 300

1 0.048+ 212

5 0.059+ 150

6 0.031+ 106


13Page of 28




Report No: 06-717

REVISED

March 02, 2007











6.30

106

1

33

0.460

0.759

10/10

0

10/10





mgDiamond

Count

1 0.460 0.460+ 425

1 0.198 0.415+ 3001 0.114+ 3001 0.103+ 300

4 0.142+ 212

10 0.125+ 150

16 0.077+ 106


14Page of 28




Report No: 06-717

REVISED

March 02, 2007











6.65

106

3

4

4.929

0.403

10/10

0

10/10





mgDiamond

Count

1 1.72 0.98 White, cloudy, dodecahedron, broken, hillocks.3.566 3.566+ 850 0.42

1 0.787 1.363+ 6001 0.576+ 600

1 0.194 0.194+ 425

1 0.108 0.199+ 3001 0.091+ 300

1 0.010+ 106


15Page of 28




Report No: 06-717

REVISED

March 02, 2007











6.90

106

2

4

9.640

0.218

9/10

0

10/10





mgDiamond

Count

1 2.50 1.66 Colorless, clear, fragment, lamination.8.102 8.102+1180 0.82

1 1.538 1.538+ 600

1 0.171 0.171+ 300

1 0.029+ 212

1 0.015+ 150

1 0.003+ 106


16Page of 28




Report No: 06-717

REVISED

March 02, 2007











8.65

106

1

20

0.420

0.533

10/10

0

9/10





mgDiamond

Count

1 0.420 0.420+ 425

1 0.161 0.268+ 3001 0.107+ 300

4 0.177+ 212

4 0.038+ 150

10 0.050+ 106


17Page of 28




Report No: 06-717

REVISED

March 02, 2007











7.05

106

1

12

0.340

0.346

10/10

0

9/10





mgDiamond

Count

1 0.340 0.544+ 4251 0.204+ 425

3 0.094+ 212

3 0.027+ 150

5 0.021+ 106


18Page of 28




Report No: 06-717

REVISED

March 02, 2007











7.00

106

0

7

0

0.077

10/10

1

10/10





mgDiamond

Count

2 0.049+ 212

1 0.015+ 150

4 0.013+ 106


19Page of 28




Report No: 06-717

REVISED

March 02, 2007











7.30

106

2

7

1.095

0.158

10/10

1

10/10





mgDiamond

Count

1 0.623 0.623+ 600

1 0.472 0.472+ 425

1 0.112 0.112+ 300

3 0.034+ 150

3 0.012+ 106


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Report No: 06-717

REVISED

March 02, 2007











7.35

106

0

5

0

0.354

10/10

0

9/10





mgDiamond

Count

1 0.248 0.332+ 3001 0.084+ 300

2 0.019+ 150

1 0.003+ 106


21Page of 28




Report No: 06-717

REVISED

March 02, 2007











7.95

106

0

32

0

0.743

9/10

0

10/10





mgDiamond

Count

1 0.242 0.407+ 3001 0.097+ 3001 0.068+ 300

6 0.182+ 212

5 0.065+ 150

18 0.089+ 106


22Page of 28




Report No: 06-717

REVISED

March 02, 2007











7.75

106

1

8

1.468

0.285

9/10

1

10/10





mgDiamond

Count

1 1.468 1.468+ 600

1 0.129 0.129+ 300

2 0.102+ 212

2 0.038+ 150

3 0.016+ 106


23Page of 28




Report No: 06-717

REVISED

March 02, 2007











7.85

106

0

25

0

0.846

9/10

0

10/10





mgDiamond

Count

1 0.212 0.212+ 425

1 0.143 0.369+ 3001 0.125+ 3001 0.101+ 300

4 0.145+ 212

5 0.058+ 150

12 0.062+ 106


24Page of 28




Report No: 06-717

REVISED

March 02, 2007











7.95

106

2

46

3.995

1.431

9/10

0

10/10





mgDiamond

Count

1 1.14 1.10 White, opaque, cubic, pits.3.290 3.290+ 850 1.10

1 0.705 0.705+ 600

1 0.146 0.146+ 425

1 0.120 0.681+ 3001 0.109+ 3001 0.104+ 3001 0.097+ 3001 0.093+ 300

1 0.090+ 3001 0.068+ 300

13 0.391+ 212

11 0.146+ 150

14 0.067+ 106

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Report No: 06-717

REVISED

March 02, 2007



26Page of 28




Report No: 06-717

REVISED

March 02, 2007











8.00

106

2

34

5.819

0.859

10/10

0

10/10





mgDiamond

Count

1 1.90 1.50 Colorless, clear, distorted, resorbed, stepped/ribbed.4.999 4.999+1180 1.24

1 0.820 0.820+ 600

1 0.154 0.277+ 4251 0.123+ 425

1 0.149 0.237+ 3001 0.088+ 300

4 0.133+ 212

8 0.115+ 150

18 0.097+ 106


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Report No: 06-717

REVISED

March 02, 2007











8.40

106

0

21

0

0.707

10/10

0

10/10





mgDiamond

Count

1 0.228 0.228+ 425

1 0.110 0.253+ 3001 0.078+ 3001 0.065+ 300

3 0.107+ 212

5 0.073+ 150

9 0.046+ 106


28Page of 28


DIAMOND RECOVERY BY CAUSTIC DISSOLUTIONProject: 8901-463 Date: September 13, 2006Client: Geos Sciences Inc. LIMS No. MI0018-MAY06

Sample No. 16985



- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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Sample No. 17000



- 74 µm 0 0.000 0.000TOTAL 24 1.953 0.010





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Sample No. 17015



- 74 µm 0 0.000 0.000TOTAL 13 0.505 0.003





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DIAMOND RECOVERY BY CAUSTIC DISSOLUTIONProject: 8901-463 Date: October 26, 2006Client: Geos Sciences Inc. LIMS No. MI0018-MAY06

Sample No. Set 1 NQ 19203



- 75 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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- 75 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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DIAMOND RECOVERY BY CAUSTIC DISSOLUTIONProject: 8901-463 Date: January 2, 2007Client: Geos Sciences Inc. LIMS No. MI0018-MAY06




- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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- 74 µm 0 0.000 0.000TOTAL 25 1.030 0.005





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- 74 µm 0 0.000 0.000TOTAL 9 0.096 0.000





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- 74 µm 0 0.000 0.000TOTAL 22 1.089 0.005





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- 74 µm 0 0.000 0.000TOTAL 24 2.044 0.010





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- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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Page 1

CHAB 05-21

SAMPLE LAB LAB From To Length Weight MICRONS TOTALNO. CERT metres metres metres Kgs +75 +106 +150 +212 +300 +425 +600 +850 +1180 DIAMONDS

17027 SRC 06-718 1.50 4.70 3.20 5.65 n/r 0 0 0 0 0 0 0 0 017028 SRC 06-718 4.70 5.50 0.80 1.60 n/r 0 0 0 0 0 0 0 0 017029 SRC 06-718 5.50 9.00 3.50 7.80 n/r 0 0 0 0 0 0 0 0 017030 SRC 06-718 9.00 12.50 3.50 7.75 n/r 0 0 0 0 0 0 0 0 017031 SRC 06-718 12.50 16.00 3.50 8.10 n/r 0 0 0 0 0 0 0 0 017032 SRC 06-718 16.00 19.80 3.80 8.40 n/r 0 0 0 0 0 0 0 0 017033 SRC 06-718 19.80 23.10 3.30 7.75 n/r 0 0 0 0 0 0 0 0 017034 SRC 06-718 23.10 26.60 3.50 8.30 n/r 0 0 0 0 0 0 0 0 017035 SGS 17035 26.60 30.10 3.50 7.70 n/r 0 0 0 0 0 0 0 0 017036 SRC 06-718 30.10 33.50 3.40 8.00 n/r 0 0 0 0 0 0 0 0 017037 SRC 06-718 33.50 37.00 3.50 8.20 n/r 0 0 0 0 0 0 0 0 017038 SRC 06-718 37.00 40.30 3.30 8.15 n/r 0 0 0 0 0 0 0 0 017039 SRC 06-718 40.30 43.60 3.30 7.35 n/r 5 4 0 2 0 0 0 0 1117040 SRC 06-718 43.60 47.00 3.40 6.95 n/r 0 1 2 0 0 0 0 0 317041 SRC 06-718 47.00 49.10 2.10 4.95 n/r 2 1 0 0 0 0 0 0 317042 SRC 06-718 49.10 51.20 2.10 4.65 n/r 1 0 0 0 0 0 0 0 117043 SRC 06-718 51.20 54.70 3.50 8.25 n/r 5 6 2 2 1 0 0 0 1617044 SRC 06-718 54.70 58.20 3.50 8.10 n/r 12 11 3 1 1 0 0 0 2817045 SRC 06-718 58.20 61.70 3.50 7.70 n/r 2 4 3 4 0 0 0 0 1317046 SRC 06-718 61.70 65.20 3.50 8.20 n/r 4 4 2 1 0 0 0 0 1117047 SRC 06-718 65.20 68.70 3.50 7.65 n/r 0 1 1 1 1 0 0 0 417048 SRC 06-718 68.70 72.20 3.50 8.55 n/r 0 3 4 6 0 0 0 0 1317049 SRC 06-718 72.20 75.70 3.50 8.55 n/r 16 5 4 1 0 0 0 0 2617050 SGS 17050 75.70 79.20 3.50 7.33 n/r 0 1 1 0 3 1 0 0 617051 SRC 06-718 79.20 82.70 3.50 8.10 n/r 18 4 5 2 0 0 1 0 3017052 SRC 06-718 82.70 86.20 3.50 8.05 n/r 14 6 7 2 1 2 0 1 3317053 SRC 06-718 86.20 89.70 3.50 8.30 n/r 7 5 4 2 0 1 0 0 1917054 SRC 06-718 89.70 93.20 3.50 7.85 n/r 10 5 7 0 1 0 0 0 2317055 SRC 06-718 93.20 96.70 3.50 8.05 n/r 4 5 0 1 2 0 0 0 1217056 SRC 06-718 96.70 100.20 3.50 7.95 n/r 4 5 6 2 1 0 1 0 1917057 SRC 06-718 100.20 103.70 3.50 8.50 n/r 6 4 1 1 1 1 0 0 1417058 SRC 06-718 103.70 107.20 3.50 8.10 n/r 27 10 4 2 1 0 1 1 4617059 SRC 06-718 107.20 110.70 3.50 8.10 n/r 7 5 8 1 0 0 0 0 2117060 SRC 06-718 110.70 114.20 3.50 8.40 n/r 8 11 4 0 3 0 0 0 2617061 SRC 06-718 114.20 117.70 3.50 7.85 n/r 5 4 4 2 1 1 1 0 18

CHAB 05-21


17062 SRC 06-718 117.70 121.20 3.50 8.20 n/r 6 2 4 3 3 2 0 0 2017063 SRC 06-718 121.20 124.70 3.50 7.95 n/r 17 0 3 1 0 0 1 0 2217064 SRC 06-718 124.70 128.20 3.50 7.80 n/r 8 3 1 0 1 0 0 0 1317065 SGS 17065 128.20 131.70 3.50 7.90 n/r 5 5 1 2 1 0 0 0 1417067 SRC 06-718 131.70 135.20 3.50 7.85 n/r 12 8 7 0 0 0 0 0 2717068 SRC 06-718 135.20 138.70 3.50 7.35 n/r 2 2 1 0 0 0 0 0 517069 SRC 06-718 138.70 142.20 3.50 8.40 n/r 8 6 1 4 2 0 0 0 2117070 SRC 06-718 142.20 145.70 3.50 7.90 n/r 10 5 1 0 0 0 0 0 1617071 SRC 06-718 145.70 149.20 3.50 8.05 n/r 12 1 3 2 1 0 0 0 1917072 SRC 06-718 149.20 152.70 3.50 7.90 n/r 3 5 2 2 3 2 0 0 1717073 SRC 06-718 152.70 156.20 3.50 7.95 n/r 5 4 4 1 1 0 0 0 1517074 SRC 06-718 156.20 159.50 3.30 7.70 n/r 7 1 3 3 0 0 0 0 1417075 SRC 06-718 159.50 163.00 3.50 7.90 n/r 5 1 2 1 0 0 0 0 917076 SRC 06-718 163.00 166.50 3.50 7.85 n/r 9 2 4 3 0 0 0 0 1817077 SRC 06-718 166.50 167.80 1.30 3.15 n/r 5 1 3 1 0 0 1 0 1117078 SRC 06-718 167.80 171.50 3.70 8.60 n/r 5 5 3 2 1 3 0 0 1917079 SRC 06-718 171.50 175.00 3.50 8.15 n/r 4 5 5 2 0 1 0 0 1717080 SRC 06-718 175.00 178.50 3.50 7.81 16 22 9 2 1 3 0 1 0 5417081 SGS 17081 178.50 182.00 3.50 8.05 n/r 9 6 3 1 0 0 0 0 1917082 SRC 06-718 182.00 185.50 3.50 7.65 n/r 8 5 5 2 1 1 0 0 2217083 SRC 06-718 185.50 189.00 3.50 8.25 n/r 8 7 5 1 0 0 0 1 2217084 SRC 06-718 189.00 192.50 3.50 7.65 n/r 8 2 4 6 1 0 1 0 2217085 SRC 06-718 192.50 196.00 3.50 7.25 n/r 6 9 5 3 1 0 0 0 2417086 SRC 06-718 196.00 199.50 3.50 7.80 n/r 9 9 9 1 1 0 0 0 2917087 SRC 06-718 199.50 203.00 3.50 7.80 n/r 4 4 9 2 1 0 1 0 2117088 SRC 06-718 203.00 206.50 3.50 7.80 n/r 2 4 0 0 0 0 0 0 617089 SRC 06-718 206.50 210.00 3.50 7.55 n/r 5 6 0 2 0 0 0 0 1317090 SRC 06-718 210.00 210.90 0.90 2.20 n/r 17 10 1 1 1 1 0 0 3117091 SRC 06-718 210.90 213.20 2.30 5.20 n/r 2 0 0 0 0 1 0 0 317092 SRC 06-718 213.20 215.00 1.80 3.65 n/r 0 0 0 1 0 0 0 0 117093 SRC 06-718 215.00 217.50 2.50 7.75 n/r 6 0 2 1 1 0 0 0 1017094 SRC 06-718 217.50 220.00 2.50 6.75 n/r 11 4 0 0 0 0 0 0 1517095 SRC 06-718 220.00 222.50 2.50 7.55 n/r 7 3 4 2 3 1 0 0 2017096 SRC 06-718 222.50 225.00 2.50 7.10 n/r 2 3 0 0 1 0 0 0 617097 SRC 06-718 225.00 227.50 2.50 7.05 n/r 7 7 1 0 2 0 0 0 17

CHAB 05-21


17098 SRC 06-718 227.50 230.00 2.50 6.90 n/r 4 5 1 5 0 0 0 0 1517099 SRC 06-718 230.00 232.50 2.50 6.85 n/r 8 6 4 2 0 4 0 0 2417100 SRC 06-718 232.50 235.00 2.50 7.35 n/r 7 3 1 2 1 0 0 0 1417101 SRC 06-718 235.00 237.50 2.50 7.35 n/r 5 6 4 1 0 1 0 0 1717102 SRC 06-718 237.50 240.00 2.50 6.95 n/r 7 3 4 2 0 0 0 1 1717103 SRC 06-718 240.00 242.50 2.50 7.25 n/r 14 6 8 4 2 1 0 0 3517104 SRC 06-718 242.50 245.00 2.50 7.20 n/r 7 4 5 2 2 1 0 0 2117105 SRC 06-718 245.00 247.50 2.50 7.00 n/r 4 0 2 1 1 2 0 0 1017106 SRC 06-718 247.50 250.00 2.50 7.15 n/r 1 0 1 1 0 0 0 0 317107 SRC 06-718 250.00 252.50 2.50 7.10 n/r 6 5 4 2 0 1 0 0 1817108 SRC 06-718 252.50 255.00 2.50 7.25 n/r 17 6 3 3 0 2 0 0 3117109 SRC 06-718 255.00 257.50 2.50 6.90 n/r 11 3 6 5 0 0 0 0 2517110 SRC 06-718 257.50 260.00 2.50 7.30 n/r 7 4 4 4 3 0 0 0 2217111 SRC 06-718 260.00 262.50 2.50 6.80 n/r 23 17 5 5 3 0 1 0 5417112 SRC 06-718 262.50 263.90 1.40 4.20 n/r 5 3 3 2 0 0 0 0 1317113 SRC 06-718 263.90 266.50 2.60 7.10 n/r 0 0 0 0 0 0 0 0 017114 SRC 06-718 266.50 269.00 2.50 6.80 n/r 0 0 0 0 0 0 0 0 017115 SRC 06-718 269.00 271.50 2.50 7.05 n/r 0 1 0 0 0 0 0 0 117116 SRC 06-718 271.50 274.00 2.50 6.80 n/r 0 0 0 0 0 0 0 0 017117 SRC 06-718 274.00 276.50 2.50 6.95 n/r 0 0 0 0 0 0 0 0 017118 SRC 06-718 276.50 279.00 2.50 7.10 n/r 0 0 0 0 0 0 0 0 017119 SRC 06-718 279.00 281.50 2.50 7.10 n/r 0 0 0 0 0 0 0 0 017120 SRC 06-718 281.50 284.00 2.50 7.00 n/r 0 0 0 0 0 0 0 0 017121 SRC 06-718 284.00 286.50 2.50 7.15 n/r 0 0 0 0 0 0 0 0 017122 SRC 06-718 286.50 289.00 2.50 6.70 n/r 0 0 0 0 0 0 0 0 0

287.50 693.64 539 321 225 125 58 30 10 4 1328QA/QC19216 SRC 06-718 9.00 12.50 3.50 7.80 n/r 0 0 0 0 0 0 0 0 019217 SGS 19217 26.60 30.10 3.50 7.70 0 0 0 0 0 0 0 0 0 019218 SGS 19218 43.60 47.00 3.40 7.20 1 1 2 0 0 1 0 0 0 519219 SGS 19219 47.00 49.10 2.10 4.96 0 1 0 0 0 0 0 0 0 119220 SRC 06-718 58.20 61.70 3.50 7.60 n/r 6 9 4 2 1 0 1 0 2319221 SGS 19221 75.70 79.20 3.50 7.56 11 8 6 4 2 2 0 1 0 3419222 SGS 19222 93.20 96.70 3.50 7.71 1.0 0 4 3 2 2 0 0 0 1219223 SGS 19223 96.70 100.20 3.50 9.00 6 3 4 3 1 1 0 0 0 18

CHAB 05-21


19224 SRC 06-718 110.70 114.20 3.50 8.15 n/r 12 9 5 1 0 0 0 0 2719225 SGS 19225 128.20 131.70 3.50 9.17 1 5 6 1 2 1 1 0 0 1719226 SGS 19226 131.70 131.70 0.00 5.90 0 0 0 0 0 0 0 0 0 017066 SRC 06-718 131.70 131.70 0.00 6.20 0 0 0 0 0 0 0 0 0 019227 SGS 19227 142.20 145.70 3.50 7.84 0 6 3 6 5 1 2 0 0 2319228 SGS 19228 145.70 149.20 3.50 7.92 4 2 2 2 2 3 0 0 0 1519229 SRC 06-718 159.50 163.00 3.50 7.90 n/r 8 5 3 0 3 1 0 0 2019230 SGS 19230 175.00 178.50 3.50 7.54 4 2 4 3 2 1 0 0 0 1619231 SGS 19231 192.50 196.00 3.50 7.25 0 5 6 2 2 0 0 0 0 1519232 SGS 19232 196.00 199.50 3.50 7.61 1 3 2 3 2 1 0 0 0 1219233 SRC 06-718 210.00 210.90 0.90 2.10 n/r 0 2 0 0 0 0 0 0 2

55.40 137.11 29 62 64 39 23 17 4 2 0 240





Report No: 06-718

March 22, 2007











9/1017027 5.65 106 0 0 0 0 9/10 09/1017028 1.60 106 0 0 0 0 10/10 010/1017029 7.80 106 0 0 0 0 9/10 010/1017030 7.75 106 0 0 0 0 10/10 010/1017031 8.10 106 0 0 0 0 10/10 0

10/1017032 8.40 106 0 0 0 0 10/10 010/1017033 7.75 106 0 0 0 0 8/10 010/1017034 8.30 106 0 0 0 0 10/10 19/1017036 8.00 106 0 0 0 0 10/10 010/1017037 8.20 106 0 0 0 0 10/10 0

9/1017038 8.15 106 0 0 0 0 9/10 010/1017039 7.35 106 0 11 0 0.333 10/10 010/1017040 6.95 106 0 3 0 0.110 10/10 010/1017041 4.95 106 0 3 0 0.024 10/10 09/1017042 4.65 106 0 1 0 0.003 9/10 0

10/1017043 8.25 106 0 16 0 0.565 10/10 010/1017044 8.10 106 0 28 0 0.521 9/10 09/1017045 7.70 106 0 13 0 0.680 9/10 010/1017046 8.20 106 0 11 0 0.197 9/10 010/1017047 7.65 106 1 3 0.281 0.158 10/10 0

17/1817048 8.55 106 0 13 0 0.973 10/10 010/1017049 8.55 106 0 26 0 0.380 9/10 010/1017051 8.10 106 1 29 3.347 0.710 10/10 010/1017052 8.05 106 3 30 8.526 0.769 10/10 08/1017053 8.30 106 1 18 1.142 0.630 10/10 0

1Page of 79





Report No: 06-718

March 22, 2007


10/1017054 7.85 106 1 22 0.435 0.442 10/10 08/1017055 8.05 106 0 12 0 0.763 8/10 010/1017056 7.95 106 1 18 2.581 0.736 9/10 010/1017057 8.50 106 1 13 1.131 0.398 10/10 09/1017058 8.10 106 3 43 10.515 0.693 10/10 0

9/1017059 8.10 106 0 21 0 0.383 10/10 010/1017060 8.40 106 0 26 0 0.971 10/10 010/1017061 7.85 106 3 15 2.477 0.572 10/10 010/1017062 8.20 106 5 15 3.416 0.452 10/10 010/1017063 7.95 106 1 21 1.957 0.352 10/10 0

10/1017064 7.80 106 0 13 0 0.329 10/10 010/1017066 6.20 106 0 0 0 0 10/10 010/1017067 7.85 106 0 27 0 0.381 10/10 010/1017068 7.35 106 0 5 0 0.081 9/10 010/1017069 8.40 106 1 20 0.362 0.736 10/10 0

9/1017070 7.90 106 0 16 0 0.184 10/10 010/1017071 8.05 106 0 19 0 0.538 9/10 09/1017072 7.90 106 5 12 2.586 0.325 9/10 010/1017073 7.95 106 1 14 0.428 0.342 10/10 310/1017074 7.70 106 0 14 0 0.525 14/15 0

20/2017075 7.90 106 0 9 0 0.224 9/10 010/1017076 7.85 106 0 18 0 0.489 10/10 010/1017077 3.15 106 1 10 1.364 0.255 9/10 09/1017078 8.60 106 4 15 1.945 0.408 10/10 09/1017079 8.15 106 1 16 0.931 0.432 8/10 1

9/1017081 8.05 106 0 19 0 0.296 10/10 09/1017082 7.65 106 2 20 0.874 0.486 10/10 010/1017083 8.25 106 1 21 4.193 0.435 9/10 010/1017084 7.65 106 2 20 2.593 0.673 10/10 010/1017085 7.25 106 1 23 0.394 0.660 10/10 0

7/1017086 7.80 106 0 29 0 0.684 10/10 19/1017087 7.80 106 1 20 2.507 0.814 10/10 110/1017088 7.80 106 0 6 0 0.058 10/10 110/1017089 7.55 106 0 13 0 0.339 10/10 010/1017090 2.20 106 1 30 0.997 0.477 10/10 1

10/1017091 5.20 106 1 2 0.528 0.012 10/10 0

2Page of 79





Report No: 06-718

March 22, 2007


9/1017092 3.65 106 0 1 0 0.146 10/10 010/1017093 7.75 106 1 9 0.272 0.196 10/10 010/1017094 6.75 106 0 15 0 0.125 10/10 010/1017095 7.55 106 3 17 1.423 0.547 10/10 09/1017096 7.10 106 0 6 0 0.295 10/10 0

10/1017097 7.05 106 1 16 0.334 0.415 10/10 010/1017098 6.90 106 0 15 0 0.584 7/10 010/1017099 6.85 106 4 20 3.204 0.459 10/10 09/1017100 7.35 106 0 14 0 0.431 9/10 010/1017101 7.35 106 1 16 0.957 0.332 9/10 0

10/1017102 6.95 106 1 16 5.196 0.325 10/10 09/1017103 7.25 106 2 33 1.059 0.988 9/10 010/1017104 7.20 106 1 20 0.518 0.811 10/10 010/1017105 7.00 106 2 8 2.481 0.415 10/10 09/1017106 7.15 106 0 3 0 0.097 9/10 0

10/1017107 7.10 106 1 17 0.882 0.474 10/10 010/1017108 7.25 106 2 29 0.744 0.528 12/12 09/1017109 6.90 106 0 25 0 0.625 10/10 010/1017110 7.30 106 1 21 0.363 1.300 10/10 010/1017111 6.80 106 3 51 1.955 1.253 10/10 0

10/1017112 4.20 106 0 13 0 0.337 9/10 09/1017113 7.10 106 0 0 0 0 10/10 07/1017114 6.80 106 0 0 0 0 8/10 010/1017115 7.05 106 0 1 0 0.004 10/10 07/1017116 6.80 106 0 0 0 0 8/10 0

10/1017117 6.95 106 0 0 0 0 10/10 010/1017118 7.10 106 0 0 0 0 10/10 09/1017119 7.10 106 0 0 0 0 9/10 09/1017120 7.00 106 0 0 0 0 6/10 08/1017121 7.15 106 0 0 0 0 10/10 0

10/1017122 6.70 106 0 0 0 0 10/10 010/1019216 7.80 106 0 0 0 0 9/10 010/1019220 7.60 106 2 21 2.309 0.553 10/10 08/1019224 8.15 106 0 27 0 0.484 10/10 010/1019229 7.90 106 3 17 2.168 0.318 10/10 0

9/1019233 2.10 106 0 2 0 0.029 10/10 0

3Page of 79





Report No: 06-718

March 22, 2007


.

.7/10 Synthetic tracers were recovered for sample # 17086.QC1 recovery was 10/10 and no other recovery deviations were reported for the group.7/10 Synthetic tracers were recovered for sample # 17098.QC2 recovery was 10/10 and no other recovery deviations were reported for the group.7/10 Synthetic tracers were recovered for sample # 17114.QC2 recovery was 8/10 and no other recovery deviations were reported for the group.7/10 Synthetic tracers were recovered for sample # 17116.QC1 recovery was 8/10 and no other recovery deviations were reported for the group.6/10 Synthetic tracers were recovered for sample # 17120.QC2 recovery was 9/10 and no other recovery deviations were reported for the group..The method validation allows for a 95% confidence level for a minimum tracer recovery of 80%.The reported QC failures are therefore within acceptable limits set by the method.


4Page of 79




Report No: 06-718

March 22, 2007











7.35

106

0

11

0

0.333

10/10

0

10/10





mgDiamond

Count

1 0.191 0.254+ 3001 0.063+ 300

4 0.060+ 150

5 0.019+ 106


5Page of 79




Report No: 06-718

March 22, 2007











6.95

106

0

3

0

0.110

10/10

0

10/10





mgDiamond

Count

2 0.092+ 212

1 0.018+ 150


6Page of 79




Report No: 06-718

March 22, 2007











4.95

106

0

3

0

0.024

10/10

0

10/10





mgDiamond

Count

1 0.014+ 150

2 0.010+ 106


7Page of 79




Report No: 06-718

March 22, 2007











4.65

106

0

1

0

0.003

9/10

0

9/10





mgDiamond

Count

1 0.003+ 106


8Page of 79




Report No: 06-718

March 22, 2007











8.25

106

0

16

0

0.565

10/10

0

10/10





mgDiamond

Count

1 0.228 0.228+ 425

1 0.088 0.165+ 3001 0.077+ 300

2 0.063+ 212

6 0.082+ 150

5 0.027+ 106


9Page of 79




Report No: 06-718

March 22, 2007











8.10

106

0

28

0

0.521

9/10

0

10/10





mgDiamond

Count

1 0.197 0.197+ 425

1 0.044 0.044+ 300

3 0.088+ 212

11 0.143+ 150

12 0.049+ 106


10Page of 79




Report No: 06-718

March 22, 2007











7.70

106

0

13

0

0.680

9/10

0

9/10





mgDiamond

Count

1 0.147 0.499+ 3001 0.143+ 3001 0.123+ 3001 0.086+ 300

3 0.068+ 212

4 0.046+ 150

2 0.067+ 106


11Page of 79




Report No: 06-718

March 22, 2007











8.20

106

0

11

0

0.197

9/10

0

10/10





mgDiamond

Count

1 0.104 0.104+ 300

2 0.040+ 212

4 0.036+ 150

4 0.017+ 106


12Page of 79




Report No: 06-718

March 22, 2007











7.65

106

1

3

0.281

0.158

10/10

0

10/10





mgDiamond

Count

1 0.281 0.281+ 425

1 0.100 0.100+ 300

1 0.039+ 212

1 0.019+ 150


13Page of 79




Report No: 06-718

March 22, 2007











8.55

106

0

13

0

0.973

10/10

0

17/18





mgDiamond

Count

1 0.212 0.794+ 3001 0.181+ 3001 0.113+ 3001 0.105+ 300

1 0.095+ 3001 0.088+ 300

4 0.135+ 212

3 0.044+ 150


14Page of 79




Report No: 06-718

March 22, 2007











8.55

106

0

26

0

0.380

9/10

0

10/10





mgDiamond

Count

1 0.120 0.120+ 300

4 0.116+ 212

5 0.069+ 150

16 0.075+ 106


15Page of 79




Report No: 06-718

March 22, 2007











8.10

106

1

29

3.347

0.710

10/10

0

10/10





mgDiamond

Count

1 1.72 0.98 White, clear, octahedron, resorbed, stepped/ribbed, hillocks.3.347 3.347+ 850 0.98

1 0.152 0.296+ 3001 0.144+ 300

5 0.253+ 212

4 0.059+ 150

18 0.102+ 106


16Page of 79




Report No: 06-718

March 22, 2007











8.05

106

3

30

8.526

0.769

10/10

0

10/10





mgDiamond

Count

1 3.70 1.62 White, included, thh, resorbed, hillocks.6.947 6.947+1180 1.08

1 0.862 1.579+ 6001 0.717+ 600

1 0.200 0.200+ 425

1 0.105 0.189+ 3001 0.084+ 300

7 0.238+ 212

6 0.086+ 150

14 0.056+ 106


17Page of 79




Report No: 06-718

March 22, 2007











8.30

106

1

18

1.142

0.630

10/10

0

8/10





mgDiamond

Count

1 1.142 1.142+ 600

1 0.216 0.390+ 3001 0.174+ 300

4 0.145+ 212

5 0.067+ 150

7 0.028+ 106


18Page of 79




Report No: 06-718

March 22, 2007











7.85

106

1

22

0.435

0.442

10/10

0

10/10





mgDiamond

Count

1 0.435 0.435+ 425

7 0.321+ 212

5 0.070+ 150

10 0.051+ 106


19Page of 79




Report No: 06-718

March 22, 2007











8.05

106

0

12

0

0.763

8/10

0

8/10





mgDiamond

Count

1 0.368 0.556+ 4251 0.188+ 425

1 0.122 0.122+ 300

5 0.065+ 150

4 0.020+ 106


20Page of 79




Report No: 06-718

March 22, 2007











7.95

106

1

18

2.581

0.736

9/10

0

10/10





mgDiamond

Count

1 1.04 1.02 White, cloudy, cubic, resorbed, crescentic steps.2.581 2.581+ 850 0.96

1 0.277 0.277+ 425

1 0.083 0.165+ 3001 0.082+ 300

6 0.199+ 212

5 0.055+ 150

4 0.040+ 106


21Page of 79




Report No: 06-718

March 22, 2007











8.50

106

1

13

1.131

0.398

10/10

0

10/10





mgDiamond

Count

1 1.131 1.131+ 600

1 0.192 0.192+ 425

1 0.085 0.085+ 300

1 0.029+ 212

4 0.067+ 150

6 0.025+ 106


22Page of 79




Report No: 06-718

March 22, 2007











8.10

106

3

43

10.515

0.693

10/10

0

9/10





mgDiamond

Count

1 2.10 1.88 White, clear, octahedroid, twinned, resorbed, stepped/ribbed,serrate laminae.

8.995 8.995+1180 1.46

1 1.00 0.94 Amber, clear, thh, resorbed, trigonal pits.1.166 1.166+ 850 0.68

1 0.354 0.354+ 425

1 0.157 0.275+ 3001 0.118+ 300

4 0.159+ 212

10 0.148+ 150

27 0.111+ 106


23Page of 79




Report No: 06-718

March 22, 2007











8.10

106

0

21

0

0.383

10/10

0

9/10





mgDiamond

Count

1 0.105 0.105+ 300

8 0.191+ 212

5 0.061+ 150

7 0.026+ 106


24Page of 79




Report No: 06-718

March 22, 2007











8.40

106

0

26

0

0.971

10/10

0

10/10





mgDiamond

Count

1 0.301 0.654+ 4251 0.202+ 4251 0.151+ 425

4 0.150+ 212

11 0.134+ 150

8 0.033+ 106


25Page of 79




Report No: 06-718

March 22, 2007











7.85

106

3

15

2.477

0.572

10/10

0

10/10





mgDiamond

Count

1 1.04 0.84 White, opaque, cubic, resorbed, knob-like asperities.1.456 1.456+ 850 0.50

1 0.774 0.774+ 600

1 0.247 0.247+ 425

1 0.174 0.343+ 3001 0.169+ 300

4 0.144+ 212

4 0.062+ 150

5 0.023+ 106


26Page of 79




Report No: 06-718

March 22, 2007











8.20

106

5

15

3.416

0.452

10/10

0

10/10





mgDiamond

Count

1 1.488 2.358+ 6001 0.870+ 600

1 0.379 1.058+ 4251 0.341+ 4251 0.338+ 425

1 0.100 0.237+ 3001 0.076+ 3001 0.061+ 300

4 0.164+ 212

2 0.027+ 150

6 0.024+ 106


27Page of 79




Report No: 06-718

March 22, 2007











7.95

106

1

21

1.957

0.352

10/10

0

10/10





mgDiamond

Count

1 1.36 0.84 White, opaque, thh, resorbed, hillocks, knob-like asperities.1.957 1.957+ 850 0.72

1 0.189 0.189+ 300

3 0.098+ 212

17 0.065+ 106


28Page of 79




Report No: 06-718

March 22, 2007











7.80

106

0

13

0

0.329

10/10

0

10/10





mgDiamond

Count

1 0.238 0.238+ 425

1 0.015+ 212

3 0.028+ 150

8 0.048+ 106


29Page of 79




Report No: 06-718

March 22, 2007











7.85

106

0

27

0

0.381

10/10

0

10/10





mgDiamond

Count

7 0.241+ 212

8 0.085+ 150

12 0.055+ 106


30Page of 79




Report No: 06-718

March 22, 2007











7.35

106

0

5

0

0.081

9/10

0

10/10





mgDiamond

Count

1 0.050+ 212

2 0.021+ 150

2 0.010+ 106


31Page of 79




Report No: 06-718

March 22, 2007











8.40

106

1

20

0.362

0.736

10/10

0

10/10





mgDiamond

Count

1 0.362 0.596+ 4251 0.234+ 425

1 0.098 0.347+ 3001 0.090+ 3001 0.090+ 3001 0.069+ 300

1 0.024+ 212

6 0.088+ 150

8 0.043+ 106


32Page of 79




Report No: 06-718

March 22, 2007











7.90

106

0

16

0

0.184

10/10

0

9/10





mgDiamond

Count

1 0.067+ 212

5 0.069+ 150

10 0.048+ 106


33Page of 79




Report No: 06-718

March 22, 2007











8.05

106

0

19

0

0.538

9/10

0

10/10





mgDiamond

Count

1 0.187 0.187+ 425

1 0.134 0.183+ 3001 0.049+ 300

3 0.101+ 212

1 0.006+ 150

12 0.061+ 106


34Page of 79




Report No: 06-718

March 22, 2007











7.90

106

5

12

2.586

0.325

9/10

0

9/10





mgDiamond

Count

1 0.786 1.341+ 6001 0.555+ 600

1 0.480 1.245+ 4251 0.403+ 4251 0.362+ 425

1 0.098 0.167+ 3001 0.069+ 300

2 0.077+ 212

5 0.067+ 150

3 0.014+ 106


35Page of 79




Report No: 06-718

March 22, 2007











7.95

106

1

14

0.428

0.342

10/10

3

10/10





mgDiamond

Count

1 0.428 0.428+ 425

1 0.090 0.090+ 300

4 0.178+ 212

4 0.056+ 150

5 0.018+ 106


36Page of 79




Report No: 06-718

March 22, 2007











7.70

106

0

14

0

0.525

14/15

0

10/10





mgDiamond

Count

1 0.159 0.368+ 3001 0.119+ 3001 0.090+ 300

3 0.093+ 212

1 0.018+ 150

7 0.046+ 106


37Page of 79




Report No: 06-718

March 22, 2007











7.90

106

0

9

0

0.224

9/10

0

20/20





mgDiamond

Count

1 0.100 0.100+ 300

2 0.078+ 212

1 0.018+ 150

5 0.028+ 106


38Page of 79




Report No: 06-718

March 22, 2007











7.85

106

0

18

0

0.489

10/10

0

10/10





mgDiamond

Count

1 0.115 0.278+ 3001 0.098+ 3001 0.065+ 300

4 0.129+ 212

2 0.036+ 150

9 0.046+ 106


39Page of 79




Report No: 06-718

March 22, 2007











3.15

106

1

10

1.364

0.255

9/10

0

10/10





mgDiamond

Count

1 1.22 0.84 Grey, opaque, polycrystalline aggregate, resorbed, rough.1.364 1.364+ 850 0.58

1 0.086 0.086+ 300

3 0.127+ 212

1 0.020+ 150

5 0.022+ 106


40Page of 79




Report No: 06-718

March 22, 2007











8.60

106

4

15

1.945

0.408

10/10

0

9/10





mgDiamond

Count

1 0.716 1.715+ 6001 0.620+ 6001 0.379+ 600

1 0.230 0.230+ 425

1 0.115 0.217+ 3001 0.102+ 300

3 0.110+ 212

5 0.053+ 150

5 0.028+ 106


41Page of 79




Report No: 06-718

March 22, 2007











8.15

106

1

16

0.931

0.432

8/10

1

9/10





mgDiamond

Count

1 0.931 0.931+ 600

1 0.094 0.157+ 3001 0.063+ 300

5 0.193+ 212

5 0.068+ 150

4 0.014+ 106


42Page of 79




Report No: 06-718

March 22, 2007











8.05

106

0

19

0

0.296

10/10

0

9/10





mgDiamond

Count

1 0.061 0.061+ 300

3 0.110+ 212

6 0.087+ 150

9 0.038+ 106


43Page of 79




Report No: 06-718

March 22, 2007











7.65

106

2

20

0.874

0.486

10/10

0

9/10





mgDiamond

Count

1 0.519 0.519+ 600

1 0.355 0.355+ 425

1 0.093 0.182+ 3001 0.089+ 300

5 0.190+ 212

5 0.080+ 150

8 0.034+ 106


44Page of 79




Report No: 06-718

March 22, 2007











8.25

106

1

21

4.193

0.435

9/10

0

10/10





mgDiamond

Count

1 1.88 1.24 White, cloudy, thh, resorbed, trigonal pits, knob-like asperities.4.193 4.193+1180 0.92

1 0.113 0.113+ 300

5 0.185+ 212

7 0.095+ 150

8 0.042+ 106


45Page of 79




Report No: 06-718

March 22, 2007











7.65

106

2

20

2.593

0.673

10/10

0

10/10





mgDiamond

Count

1 1.62 1.12 White, clear, octahedroid, resorbed, hillocks.2.290 2.290+ 850 0.52

1 0.303 0.303+ 425

1 0.109 0.454+ 3001 0.100+ 3001 0.082+ 3001 0.079+ 3001 0.055+ 300

1 0.029+ 300

4 0.161+ 212

2 0.024+ 150

8 0.034+ 106


46Page of 79




Report No: 06-718

March 22, 2007











7.25

106

1

23

0.394

0.660

10/10

0

10/10





mgDiamond

Count

1 0.394 0.394+ 425

1 0.112 0.281+ 3001 0.105+ 3001 0.064+ 300

5 0.217+ 212

9 0.139+ 150

6 0.023+ 106


47Page of 79




Report No: 06-718

March 22, 2007











7.80

106

0

29

0

0.684

10/10

1

7/10





mgDiamond

Count

1 0.127 0.127+ 425

1 0.154 0.154+ 300

9 0.244+ 212

9 0.110+ 150

9 0.049+ 106


48Page of 79




Report No: 06-718

March 22, 2007











7.80

106

1

20

2.507

0.814

10/10

1

9/10





mgDiamond

Count

1 0.94 0.92 Green, opaque, cubic, resorbed.2.507 2.507+ 850 0.80

1 0.202 0.202+ 425

1 0.138 0.250+ 3001 0.112+ 300

9 0.292+ 212

4 0.050+ 150

4 0.020+ 106


49Page of 79




Report No: 06-718

March 22, 2007











7.80

106

0

6

0

0.058

10/10

1

10/10





mgDiamond

Count

4 0.049+ 150

2 0.009+ 106


50Page of 79




Report No: 06-718

March 22, 2007











7.55

106

0

13

0

0.339

10/10

0

10/10





mgDiamond

Count

1 0.147 0.215+ 3001 0.068+ 300

6 0.102+ 150

5 0.022+ 106


51Page of 79




Report No: 06-718

March 22, 2007











2.20

106

1

30

0.997

0.477

10/10

1

10/10





mgDiamond

Count

1 0.997 0.997+ 600

1 0.181 0.181+ 425

1 0.080 0.080+ 300

1 0.041+ 212

10 0.097+ 150

17 0.078+ 106


52Page of 79




Report No: 06-718

March 22, 2007











5.20

106

1

2

0.528

0.012

10/10

0

10/10





mgDiamond

Count

1 0.528 0.528+ 600

2 0.012+ 106


53Page of 79




Report No: 06-718

March 22, 2007











3.65

106

0

1

0

0.146

10/10

0

9/10





mgDiamond

Count

1 0.146 0.146+ 300


54Page of 79




Report No: 06-718

March 22, 2007











7.75

106

1

9

0.272

0.196

10/10

0

10/10





mgDiamond

Count

1 0.272 0.272+ 425

1 0.118 0.118+ 300

2 0.046+ 212

6 0.032+ 106


55Page of 79




Report No: 06-718

March 22, 2007











6.75

106

0

15

0

0.125

10/10

0

10/10





mgDiamond

Count

4 0.060+ 150

11 0.065+ 106


56Page of 79




Report No: 06-718

March 22, 2007











7.55

106

3

17

1.423

0.547

10/10

0

10/10





mgDiamond

Count

1 0.818 0.818+ 600

1 0.326 0.799+ 4251 0.279+ 4251 0.194+ 425

1 0.079 0.148+ 3001 0.069+ 300

4 0.111+ 212

3 0.042+ 150

7 0.052+ 106


57Page of 79




Report No: 06-718

March 22, 2007











7.10

106

0

6

0

0.295

10/10

0

9/10





mgDiamond

Count

1 0.244 0.244+ 425

3 0.039+ 150

2 0.012+ 106


58Page of 79




Report No: 06-718

March 22, 2007











7.05

106

1

16

0.334

0.415

10/10

0

10/10





mgDiamond

Count

1 0.334 0.589+ 4251 0.255+ 425

1 0.046+ 212

7 0.079+ 150

7 0.035+ 106


59Page of 79




Report No: 06-718

March 22, 2007











6.90

106

0

15

0

0.584

7/10

0

10/10





mgDiamond

Count

1 0.132 0.484+ 3001 0.127+ 3001 0.079+ 3001 0.077+ 300

1 0.069+ 300

1 0.021+ 212

5 0.060+ 150

4 0.019+ 106


60Page of 79




Report No: 06-718

March 22, 2007











6.85

106

4

20

3.204

0.459

10/10

0

10/10





mgDiamond

Count

1 1.100 3.204+ 6001 0.944+ 6001 0.721+ 6001 0.439+ 600

1 0.138 0.242+ 3001 0.104+ 300

4 0.119+ 212

6 0.063+ 150

8 0.035+ 106


61Page of 79




Report No: 06-718

March 22, 2007











7.35

106

0

14

0

0.431

9/10

0

9/10





mgDiamond

Count

1 0.205 0.205+ 425

1 0.079 0.135+ 3001 0.056+ 300

1 0.037+ 212

3 0.026+ 150

7 0.028+ 106


62Page of 79




Report No: 06-718

March 22, 2007











7.35

106

1

16

0.957

0.332

9/10

0

10/10





mgDiamond

Count

1 0.957 0.957+ 600

1 0.063 0.063+ 300

4 0.163+ 212

6 0.084+ 150

5 0.022+ 106


63Page of 79




Report No: 06-718

March 22, 2007











6.95

106

1

16

5.196

0.325

10/10

0

10/10





mgDiamond

Count

1 1.80 1.38 White, included, fragment, serrate laminae, lamination, trigonalpits.

5.196 5.196+1180 0.82

1 0.103 0.185+ 3001 0.082+ 300

4 0.072+ 212

3 0.035+ 150

7 0.033+ 106


64Page of 79




Report No: 06-718

March 22, 2007











7.25

106

2

33

1.059

0.988

9/10

0

9/10





mgDiamond

Count

1 0.752 0.752+ 600

1 0.307 0.575+ 4251 0.268+ 425

1 0.133 0.351+ 3001 0.094+ 3001 0.082+ 3001 0.042+ 300

8 0.217+ 212

6 0.083+ 150

14 0.069+ 106


65Page of 79




Report No: 06-718

March 22, 2007











7.20

106

1

20

0.518

0.811

10/10

0

10/10





mgDiamond

Count

1 0.518 0.518+ 600

1 0.209 0.389+ 4251 0.180+ 425

1 0.116 0.198+ 3001 0.082+ 300

5 0.134+ 212

4 0.050+ 150

7 0.040+ 106


66Page of 79




Report No: 06-718

March 22, 2007











7.00

106

2

8

2.481

0.415

10/10

0

10/10





mgDiamond

Count

1 1.331 2.481+ 6001 1.150+ 600

1 0.246 0.246+ 425

1 0.066 0.066+ 300

2 0.081+ 212

4 0.022+ 106


67Page of 79




Report No: 06-718

March 22, 2007











7.15

106

0

3

0

0.097

9/10

0

9/10





mgDiamond

Count

1 0.051 0.051+ 300

1 0.043+ 212

1 0.003+ 106


68Page of 79




Report No: 06-718

March 22, 2007











7.10

106

1

17

0.882

0.474

10/10

0

10/10





mgDiamond

Count

1 0.882 0.882+ 600

1 0.169 0.225+ 3001 0.056+ 300

4 0.153+ 212

5 0.064+ 150

6 0.032+ 106


69Page of 79




Report No: 06-718

March 22, 2007











7.25

106

2

29

0.744

0.528

12/12

0

10/10





mgDiamond

Count

1 0.372 0.744+ 6001 0.372+ 600

1 0.114 0.294+ 3001 0.104+ 3001 0.076+ 300

3 0.109+ 212

6 0.066+ 150

17 0.059+ 106


70Page of 79




Report No: 06-718

March 22, 2007











6.90

106

0

25

0

0.625

10/10

0

9/10





mgDiamond

Count

1 0.078 0.327+ 3001 0.076+ 3001 0.065+ 3001 0.061+ 300

1 0.047+ 300

6 0.207+ 212

3 0.046+ 150

11 0.045+ 106


71Page of 79




Report No: 06-718

March 22, 2007











7.30

106

1

21

0.363

1.300

10/10

0

10/10





mgDiamond

Count

1 0.363 0.853+ 4251 0.246+ 4251 0.244+ 425

1 0.214 0.498+ 3001 0.108+ 3001 0.091+ 3001 0.085+ 300

4 0.222+ 212

4 0.059+ 150

7 0.031+ 106


72Page of 79




Report No: 06-718

March 22, 2007











6.80

106

3

51

1.955

1.253

10/10

0

10/10





mgDiamond

Count

1 0.88 0.86 Amber, cloudy, fragment, resorbed, serrate laminae.1.277 1.277+ 850 0.74

1 0.438 0.965+ 4251 0.240+ 4251 0.287+ 425

1 0.114 0.418+ 3001 0.101+ 3001 0.082+ 3001 0.081+ 3001 0.040+ 300

5 0.246+ 212

17 0.179+ 150

23 0.123+ 106


73Page of 79




Report No: 06-718

March 22, 2007











4.20

106

0

13

0

0.337

9/10

0

10/10





mgDiamond

Count

1 0.114 0.177+ 3001 0.063+ 300

3 0.090+ 212

3 0.047+ 150

5 0.023+ 106


74Page of 79




Report No: 06-718

March 22, 2007











7.05

106

0

1

0

0.004

10/10

0

10/10





mgDiamond

Count

1 0.004+ 150


75Page of 79




Report No: 06-718

March 22, 2007











7.60

106

2

21

2.309

0.553

10/10

0

10/10





mgDiamond

Count

1 1.20 1.02 Colorless, included, fragment, lamination.1.928 1.928+ 850 0.74

1 0.381 0.381+ 425

1 0.137 0.226+ 3001 0.089+ 300

4 0.165+ 212

9 0.141+ 150

6 0.021+ 106


76Page of 79




Report No: 06-718

March 22, 2007











8.15

106

0

27

0

0.484

10/10

0

8/10





mgDiamond

Count

1 0.102 0.102+ 300

5 0.211+ 212

9 0.111+ 150

12 0.060+ 106


77Page of 79




Report No: 06-718

March 22, 2007











7.90

106

3

17

2.168

0.318

10/10

0

10/10





mgDiamond

Count

1 1.664 1.664+ 600

1 0.320 0.588+ 4251 0.184+ 4251 0.084+ 425

3 0.124+ 212

5 0.073+ 150

8 0.037+ 106


78Page of 79




Report No: 06-718

March 22, 2007











2.10

106

0

2

0

0.029

10/10

0

9/10





mgDiamond

Count

2 0.029+ 150


79Page of 79


DIAMOND RECOVERY BY CAUSTIC DISSOLUTIONProject: 8901-463 Date: March 22, 2007Client: Geos Sciences Inc. LIMS No. MI0020-MAY06

Sample No. Set-2 NQ 17035



- 75 µm 0 0.000 0.000TOTAL 0 0.000 0.000





Ston

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In

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divi

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ly

Page 1


DIAMOND RECOVERY BY CAUSTIC DISSOLUTIONProject: 8901-463 Date: April 3, 2007Client: Geos Sciences Inc. LIMS No. MI0020-MAY06




- 74 µm 0 0.000 0.000TOTAL 6 1.770 0.009





Ston

es D

escr

ibed

In

divi

dual

ly /

Gro

up

Wei

ghed

Ston

es D

escr

ibed

and

W

eigh

ed In

divi

dual

ly

Page 1






- 75 µm 0 0.000 0.000TOTAL 20 0.704 0.004





Ston

es D

escr

ibed

In

divi

dual

ly /

Gro

up

Wei

ghed

Ston

es D

escr

ibed

and

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DIAMOND RECOVERY BY CAUSTIC DISSOLUTIONProject: 8901-463 Date: May 3, 2007Client: Geos Sciences Inc. LIMS No. MI0020-MAY06




- 75 µm 0 0.000 0.000TOTAL 54 2.521 0.013





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- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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- 74 µm 0 0.000 0.000TOTAL 5 0.374 0.002





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- 75 µm 0 0.000 0.000TOTAL 1 0.005 0.000





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DIAMOND RECOVERY BY CAUSTIC DISSOLUTIONProject: 8901-463 Date: February 28, 2007Client: Geos Sciences Inc. LIMS No. MI0020-MAY06




- 74 µm 0 0.000 0.000TOTAL 34 5.162 0.026





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- 75 µm 0 0.000 0.000TOTAL 12 1.059 0.005





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Sample No. 19223



- 74 µm 0 0.000 0.000TOTAL 18 0.427 0.002





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Sample No. 19225



- 74 µm 0 0.000 0.000TOTAL 17 1.013 0.005





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Sample No. 19226



- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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Sample No. 19227



- 74 µm 0 0.000 0.000TOTAL 23 3.105 0.016


* Total Weight (carats) was calculated from mg weights. All reported mg weights are weighed to within 0.002 mg.Note: One -212/+150 μm diamond was lost during transfer.



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Sample No. 19228



- 74 µm 0 0.000 0.000TOTAL 15 1.173 0.006


* Total Weight (carats) was calculated from mg weights. All reported mg weights are weighed to within 0.002 mg.NOTE: One -300/+212 μm diamond lost during transfer.



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Sample No. 19230



- 74 µm 0 0.000 0.000TOTAL 16 0.870 0.004





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Sample No. 19231



- 74 µm 0 0.000 0.000TOTAL 15 0.347 0.002





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Sample No. 19232



- 74 µm 0 0.000 0.000TOTAL 12 0.623 0.003





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CHAB 05-22

SAMPLE Lab Lab From To Length Weight MICRONS TOTALNO. Cert metres metres metres Kgs +74 +105 +150 +212 +300 +425 +600 +850 +1180 DIAMONDS

15763 SRC n/a 9.90 12.60 2.7015764 SRC n/a 12.60 16.00 3.4015765 SGS 15765 16.00 19.15 3.15 7.24 2 0 1 0 0 0 0 0 0 315766 SRC n/a 19.15 22.60 3.4515767 SRC n/a 39.30 42.80 3.5015768 SRC n/a 42.80 46.30 3.5015769 SRC n/a 46.30 49.80 3.5015770 SRC n/a 49.80 53.50 3.7015771 SRC n/a 53.50 57.00 3.5015772 SRC n/a 57.00 60.40 3.4015773 SRC n/a 60.40 64.00 3.6015774 SRC n/a 64.00 67.50 3.5015775 SRC n/a 67.50 71.00 3.5015776 SRC n/a 71.00 74.50 3.5015777 SRC n/a 74.50 77.60 3.1015778 SRC n/a 77.60 81.10 3.5015779 SRC n/a 81.10 84.24 3.1415780 SGS 15780 84.24 87.50 3.26 7.37 0 0 0 0 0 0 0 0 0 015781 SRC n/a 87.50 91.00 3.5015782 SRC n/a 91.00 94.50 3.5015783 SRC n/a 94.50 98.00 3.5015784 SRC n/a 98.00 101.50 3.5015785 SRC n/a 101.50 105.00 3.5015786 SRC n/a 105.00 108.50 3.5015787 SRC n/a 108.50 112.00 3.5015789 SRC n/a 112.00 115.50 3.5015790 SRC n/a 115.50 119.00 3.5015791 SRC n/a 119.00 122.50 3.5015792 SRC n/a 122.50 126.00 3.5015793 SRC n/a 126.00 127.46 1.4615794 SRC n/a 127.46 130.90 3.4415795 SGS 15795 130.90 134.50 3.60 8.69 0 0 0 0 0 0 0 0 0 015796 SRC n/a 134.50 138.00 3.5015797 SRC n/a 138.00 141.50 3.5015798 SRC n/a 141.50 145.00 3.50

CHAB 05-22


15799 SRC n/a 145.00 148.50 3.5015800 SRC n/a 148.50 152.00 3.50QA/QC19148 SRC n/a 9.90 12.60 2.7019149 SGS 19149 16.00 19.15 3.15 7.59 2 1 1 0 0 0 0 0 0 419150 SGS 19150 49.80 53.50 3.70 9.10 0 1 0 0 0 0 0 0 0 119151 SGS 19151 53.50 57.00 3.50 8.70 0 0 0 0 0 0 0 0 0 019152 SRC n/a 67.50 71.00 3.5019153 SGS 19153 84.24 87.50 3.26 7.83 0 0 0 0 0 0 0 0 0 019154 SGS 19154 101.50 105.00 3.50 8.02 0 0 0 0 0 0 0 0 0 019155 SGS 19155 105.00 108.50 3.50 7.40 0 0 0 0 0 0 0 0 0 019156 SGS 19156 112.00 112.00 0.00 5.60 0 0 0 0 0 0 0 0 0 015788 SRC n/a 112.00 112.00 0.0019157 SRC n/a 115.50 119.00 3.5019158 SGS 19158 130.90 134.50 3.60 7.22 0 0 0 0 0 0 0 0 0 019159 SGS 19159 145.00 148.50 3.50 8.38 0 0 0 0 0 0 0 0 0 019160 SGS 19160 148.50 152.00 3.50 7.56 0 0 0 0 0 0 0 0 0 0

41.22 100.70 4 2 2 0 0 0 0 0 0 8


DIAMOND RECOVERY BY CAUSTIC DISSOLUTIONProject: 8901-463 Date: June 16, 2006Client: Geos Sciences Inc. LIMS No. MI0003-DEC05

Sample No. 15765



- 74 µm 0 0.000 0.000TOTAL 3 0.033 0.000





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Sample No. 15780



- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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Sample No. 15795



- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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DIAMOND RECOVERY BY CAUSTIC DISSOLUTIONProject: 8901-463 Date: August 10, 2006Client: Geos Sciences Inc. LIMS No. MI0008-DEC05

Sample No. 19149



- 74 µm 0 0.000 0.000TOTAL 4 0.036 0.000





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Sample No. 19150



- 74 µm 0 0.000 0.000TOTAL 1 0.008 0.000





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Sample No. 19151



- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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Sample No. 19153



- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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Sample No. 19154



- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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Sample No. 19155



- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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Sample No. 19156



- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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Sample No. 19158



- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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Sample No. 19159



- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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Sample No. 19160



- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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CHAB 05-25

SAMPLE LAB LAB From To Length Weight MICRONS TOTALNO. CERT metres metres metres Kgs +106 +150 +212 +300 +425 +600 +850 +1180 DIAMONDS

15995 SRC 06-719 9.00 12.50 3.50 8.50 0 0 0 0 0 0 0 0 015996 SRC 06-719 24.00 27.50 3.50 7.40 0 0 0 0 0 0 0 0 015997 SRC 06-719 42.00 45.50 3.50 7.30 0 0 0 0 0 0 0 0 015998 SRC 06-719 63.00 66.50 3.50 7.80 0 0 0 0 0 0 0 0 015999 SRC 06-719 81.10 84.50 3.40 7.45 0 0 0 0 0 0 0 0 016000 SGS 16000 101.10 104.60 3.50 8.35 0 0 0 0 0 0 0 0 016001 SRC 06-719 104.60 106.78 2.18 4.20 0 0 0 0 0 0 0 0 016002 SRC 06-719 116.40 119.90 3.50 7.00 0 0 0 0 0 0 0 0 016003 SRC 06-719 132.00 135.50 3.50 7.75 0 0 0 0 0 0 0 0 016004 SRC 06-719 153.27 156.77 3.50 7.35 4 0 0 1 0 0 0 0 516005 SRC 06-719 156.77 160.20 3.43 6.90 0 0 0 0 0 0 0 0 016006 SRC 06-719 160.20 163.50 3.30 7.10 0 0 0 0 0 0 0 0 016007 SRC 06-719 163.50 167.00 3.50 7.05 0 0 0 0 0 0 0 0 016008 SRC 06-719 167.00 170.50 3.50 7.10 0 0 0 0 0 0 0 0 016009 SRC 06-719 170.50 174.00 3.50 7.15 1 0 0 0 0 0 0 0 116010 SRC 06-719 174.00 177.50 3.50 7.45 0 0 0 0 0 0 0 0 016011 SRC 06-719 177.50 181.00 3.50 7.40 0 0 0 0 0 0 0 0 016012 SRC 06-719 181.00 184.70 3.70 7.50 0 0 0 0 0 0 0 0 016013 SRC 06-719 184.70 188.43 3.73 7.55 0 0 0 0 0 0 0 0 016014 SRC 06-719 188.43 190.60 2.17 4.75 0 0 0 0 0 0 0 0 016015 SGS 16015 190.60 192.79 2.19 4.59 0 0 0 0 0 0 0 0 016016 SRC 06-719 192.79 196.20 3.41 7.45 0 0 0 0 0 0 0 0 016017 SRC 06-719 196.20 199.50 3.30 6.60 0 0 0 0 0 0 0 0 0

76.31 161.69 5 0 0 1 0 0 0 0 6QA/QC19195 SRC 06-719 9.00 12.50 3.50 6.70 0 0 0 0 0 0 0 0 019196 SGS 19196 101.10 104.60 3.50 7.19 0 0 0 0 0 0 0 0 019197 SGS 19197 156.77 160.20 3.43 8.10 0 0 0 0 0 0 0 0 019198 SGS 19198 160.20 163.50 3.30 7.84 0 0 0 0 0 0 0 0 019199 SRC 06-719 174.00 177.50 3.50 8.85 0 0 0 0 0 0 0 0 019200 SGS 19200 190.60 192.79 2.19 5.14 0 0 0 0 0 0 0 0 019201 SGS 19201 199.50 199.50 0.00 5.94 0 0 0 0 0 0 0 0 016018 SRC 06-719 199.50 199.50 0.00 4.75 0 0 0 0 0 0 0 0 0

19.42 54.51 0 0 0 0 0 0 0 0 0





Report No: 06-719

March 26, 2007











9/1015995 8.50 106 0 0 0 0 9/10 19/1015996 7.40 106 0 0 0 0 10/10 010/1015997 7.30 106 0 0 0 0 10/10 09/1015998 7.80 106 0 0 0 0 9/10 010/1015999 7.45 106 0 0 0 0 9/10 1

10/1016001 4.20 106 0 0 0 0 9/10 010/1016002 7.00 106 0 0 0 0 10/10 010/1016003 7.75 106 0 0 0 0 10/10 09/1016004 7.35 106 0 5 0 0.163 10/10 09/1016005 6.90 106 0 0 0 0 10/10 1

10/1016006 7.10 106 0 0 0 0 9/10 010/1016007 7.05 106 0 0 0 0 10/10 010/1016008 7.10 106 0 0 0 0 10/10 04/1016009 7.15 106 0 1 0 0.004 9/10 010/1016010 7.45 106 0 0 0 0 10/10 0

10/1016011 7.40 106 0 0 0 0 10/10 010/1016012 7.50 106 0 0 0 0 9/10 110/1016013 7.55 106 0 0 0 0 10/10 010/1016014 4.75 106 0 0 0 0 10/10 010/1016016 7.45 106 0 0 0 0 10/10 0

10/1016017 6.60 106 0 0 0 0 9/10 010/1016018 4.75 106 0 0 0 0 10/10 010/1019195 6.70 106 0 0 0 0 10/10 19/1019199 8.85 106 0 0 0 0 10/10 0

.

.

1Page of 4




Report No: 06-719

March 26, 2007


4/10 Synthetic tracers were recovered for sample #16009.The method validation allows for a 95% confidence level for a minimum tracer recovery of 80%.QC1 recovery was 9/10 and no other recovery deviations were reported for the group.The reported QC failure is therefore within acceptable limits set by the method.


2Page of 4




Report No: 06-719

March 26, 2007











7.35

106

0

5

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0.163

10/10

0

9/10





mgDiamond

Count

1 0.149 0.149+ 300

4 0.014+ 106


3Page of 4




Report No: 06-719

March 26, 2007











7.15

106

0

1

0

0.004

9/10

0

4/10





mgDiamond

Count

1 0.004+ 106


4Page of 4






- 75 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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DIAMOND RECOVERY BY CAUSTIC DISSOLUTIONProject: 8901-463 Date: May 14, 2007Client: Geos Sciences Inc. LIMS No. MI0022-MAY06




- 75 µm 0 0.000 0.000TOTAL 1 0.004 0.000





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- 75 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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DIAMOND RECOVERY BY CAUSTIC DISSOLUTIONProject: 8901-463 Date: June 26, 2007Client: Geos Sciences Inc. LIMS No. MI0022-MAY06




- 75 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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CHAB 05-27


15825 SRC n/a 4.25 7.75 3.5015826 SRC n/a 7.75 11.25 3.5015827 SRC n/a 11.25 14.50 3.2515828 SRC n/a 14.50 18.00 3.5015829 SGS 15829 18.00 21.50 3.5015830 SRC n/a 21.50 25.00 3.50 7.44 2 1 1 0 0 0 0 0 0 415831 SRC n/a 25.00 28.50 3.5015832 SRC n/a 28.50 32.00 3.5015833 SRC n/a 32.00 35.50 3.5015834 SRC n/a 35.50 39.00 3.5015835 SRC n/a 39.00 42.50 3.5015836 SRC n/a 42.50 45.20 2.7015837 SRC n/a 45.20 48.20 3.0015838 SRC n/a 48.20 50.30 2.1015839 SRC n/a 50.30 53.50 3.2015840 SRC n/a 53.50 57.00 3.5015841 SRC n/a 57.00 60.10 3.1015842 SRC n/a 60.10 62.60 2.5015843 SRC n/a 62.60 66.00 3.4015844 SRC n/a 66.00 69.50 3.5015845 SGS 15845 69.50 73.00 3.50 7.46 0 0 0 0 0 0 0 0 0 015846 SRC n/a 73.00 76.50 3.5015847 SRC n/a 76.50 80.00 3.5015848 SRC n/a 80.00 82.00 2.0015849 SRC n/a 82.00 84.00 2.0015850 SRC n/a 84.00 87.50 3.5015851 SRC n/a 87.50 91.00 3.5015852 SRC n/a 91.00 94.50 3.5015853 SRC n/a 94.50 98.00 3.5015854 SRC n/a 98.00 100.26 2.2615856 SRC n/a 100.26 105.00 4.7415857 SRC n/a 105.00 108.50 3.5015858 SRC n/a 108.50 112.00 3.5015859 SRC n/a 112.00 115.50 3.5015860 SRC n/a 115.50 119.00 3.50

CHAB 05-27


15875 SRC n/a 119.00 122.50 3.5015861 SRC n/a 122.50 126.00 3.5015862 SRC n/a 126.00 129.50 3.5015863 SRC n/a 129.50 133.00 3.5015864 SRC n/a 133.00 136.50 3.5015865 SRC n/a 136.50 139.50 3.0015866 SRC n/a 139.50 141.50 2.0015867 SRC n/a 141.50 145.00 3.5015868 SRC n/a 145.00 148.50 3.5015869 SRC n/a 148.50 152.00 3.5015870 SRC n/a 152.00 155.50 3.5015871 SRC n/a 155.50 159.00 3.5015872 SRC n/a 159.00 162.50 3.5015873 SRC n/a 162.50 166.00 3.5015874 SRC n/a 185.50 189.00 3.50

19167 SRC n/a 4.25 7.75 3.5019168 SGS 19168 21.50 25.00 3.50 8.12 1 2 0 0 0 0 0 0 0 319169 SGS 19169 39.00 42.50 3.50 8.37 3 11 8 6 7 3 1 0 0 3919170 SGS 19170 42.50 45.20 2.70 6.79 5 2 5 4 3 2 0 1 0 2219171 SRC n/a 53.50 57.00 3.5019172 SGS n/a 69.50 73.00 3.5019173 SGS n/a 84.00 87.50 3.5019174 SGS n/a 87.50 91.00 3.5019176 SRC n/a 100.16 105.00 4.8419175 SGS n/a 100.26 100.26 0.0015855 SRC n/a 100.26 100.26 0.0019177 SGS n/a 115.50 119.00 3.5019178 SGS n/a 136.50 139.50 3.0019179 SGS 19179 139.50 141.50 2.00 4.59 2 4 0 4 1 0 0 0 0 1119180 SRC n/a 152.00 155.50 3.5019181 SGS 19181 185.50 189.00 3.50 8.88 0 0 0 0 0 0 0 0 0 0



Sample No. 15830



- 74 µm 0 0.000 0.000TOTAL 4 0.115 0.001





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Sample No. 15845



- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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Sample No. 19168



- 74 µm 0 0.000 0.000TOTAL 3 0.014 0.000





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Sample No. 19169



- 74 µm 0 0.000 0.000TOTAL 39 2.230 0.011


* Total Weight (carats) was calculated from mg weights. All reported mg weights are weighed to within 0.002 mg.NOTE: Two diamonds were lost during sieving.



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Sample No. 19170



- 74 µm 0 0.000 0.000TOTAL 22 2.493 0.012





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DIAMOND RECOVERY BY CAUSTIC DISSOLUTIONProject: 8901-463 Date: September 8, 2006Client: Geos Sciences Inc. LIMS No. MI0012-DEC05

Sample No. 19179



- 74 µm 1 0.005 0.000TOTAL 12 0.232 0.001





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DIAMOND RECOVERY BY CAUSTIC DISSOLUTIONProject: 8901-463 Date: September 8, 2006Client: Geos Sciences Inc. LIMS No. MI0012-DEC05

Sample No. 19181



- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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CHAB 06-45


20257 SRC n/a 3.0 6.5 3.5020261 SGS 20261 12.6 16.0 3.39 8.30 0.00 0 0 0 0 0 0 0 0 020258 SRC n/a 21.0 24.5 3.5020263 SRC n/a 27.1 30.4 3.3220259 SRC n/a 45.0 48.5 3.5020260 SRC n/a 63.0 66.5 3.5020264 SRC n/a 68.9 72.4 3.5520265 SRC n/a 72.4 75.9 3.5020266 SRC n/a 81.3 84.7 3.4220268 SRC n/a 90.8 94.3 3.5020272 SRC n/a 108.0 111.5 3.5020273 SRC n/a 153.0 156.5 3.5020274 SRC n/a 164.9 168.4 3.5520276 SRC n/a 174.0 178.5 4.5020277 SRC n/a 183.0 186.5 3.5020278 SRC n/a 195.0 198.5 3.5020279 SGS 20279 213.0 216.5 3.50 7.80 0.00 0 0 0 0 0 0 0 0 020281 SRC n/a 231.0 234.5 3.5020282 SRC n/a 249.0 252.5 3.5020283 SRC n/a 258.7 262.2 3.5020284 SRC n/a 266.4 268.9 2.4920286 SRC n/a 294.7 298.3 3.6020288 SRC n/a 308.6 312.1 3.5020289 SRC n/a 312.1 315.7 3.6220290 SRC n/a 315.7 318.3 2.5820291 SRC n/a 318.3 321.0 2.7320293 SRC n/a 321.0 324.7 3.6720294 SRC n/a 324.7 328.1 3.3920295 SRC n/a 328.1 331.6 3.5320296 SRC n/a 331.6 335.1 3.4720297 SGS 20297 335.1 338.6 3.50 7.61 0 0 0 0 0 0 0 0 0 020299 SRC n/a 338.6 342.1 3.5020300 SRC n/a 342.1 345.6 3.5020301 SRC n/a 345.6 349.1 3.5020302 SRC n/a 349.1 352.6 3.50

CHAB 06-45


20304 SRC n/a 352.6 356.1 3.5020306 SRC n/a 356.1 359.6 3.5020307 SRC n/a 359.6 363.1 3.5020308 SRC n/a 363.1 366.6 3.5020309 SRC n/a 366.6 369.6 3.0020311 SRC n/a 369.6 372.2 2.5920312 SRC n/a 372.2 374.7 2.5920313 SRC n/a 384.0 387.5 3.5020314 SRC n/a 396.0 399.5 3.5020315 SGS 20315 409.6 413.1 3.50 6.54 0 0 0 0 0 0 0 0 0 020317 SRC n/a 413.1 416.6 3.5020318 SRC n/a 416.6 420.0 3.4920319 SRC n/a 420.0 423.6 3.5120320 SRC n/a 423.6 427.1 3.5020322 SRC n/a 427.1 430.6 3.5020326 SRC n/a 430.6 434.1 3.5020327 SRC n/a 434.1 437.6 3.5020328 SRC n/a 437.6 440.0 2.4520330 SRC n/a 440.0 442.7 2.6620331 SRC n/a 442.7 445.7 3.0820332 SRC n/a 445.7 449.4 3.6220333 SGS 20333 449.4 451.7 2.38 5.01 0 0 0 0 0 0 0 0 0 020335 SRC n/a 451.7 454.0 2.2620336 SRC n/a 454.0 457.5 3.5020337 SRC n/a 457.5 461.0 3.5020338 SRC n/a 461.0 464.3 3.3320340 SRC n/a 464.3 466.4 2.1020342 SRC n/a 466.4 468.5 2.1020343 SRC n/a 468.5 471.1 2.5420344 SRC n/a 471.1 473.7 2.6320345 SRC n/a 473.7 476.3 2.6020347 SRC n/a 476.3 479.9 3.5920348 SRC n/a 479.9 483.7 3.7620349 SRC n/a 483.7 487.2 3.5620350 SRC n/a 487.2 490.7 3.50

CHAB 06-45


20351 SGS 20351 490.7 494.2 3.50 8.18 0 0 0 0 0 0 0 0 0 020353 SRC n/a 494.2 497.7 3.5120354 SRC n/a 497.7 501.2 3.5020355 SRC n/a 501.2 503.8 2.5320356 SRC n/a 503.8 506.3 2.5320358 SRC n/a 506.3 509.3 3.0020360 SRC n/a 509.3 512.3 3.0020361 SRC n/a 512.3 514.5 2.2220362 SRC n/a 514.5 516.5 2.0020363 SRC n/a 516.5 520.0 3.5020365 SRC n/a 520.0 523.5 3.5020366 SRC n/a 523.5 527.0 3.5020367 SRC n/a 527.0 530.2 3.2320368 SRC n/a 530.2 532.5 2.2420369 SGS 20369 532.5 534.0 1.50 3.44 0 0 1 0 0 0 0 0 0 120371 SRC n/a 534.0 537.5 3.5020372 SRC n/a 537.5 541.0 3.5020373 SRC n/a 541.0 544.5 3.5020374 SRC n/a 544.5 547.0 2.5020376 SRC n/a 547.0 549.5 2.5420380 SRC n/a 549.5 553.0 3.5020381 SRC n/a 553.0 556.5 3.5020382 SRC n/a 556.5 560.0 3.5020384 SRC n/a 560.0 563.5 3.5020385 SRC n/a 563.5 567.0 3.5020386 SRC n/a 567.0 570.5 3.5020387 SGS 20387 570.5 573.5 2.99 6.96 0 0 0 0 0 0 0 0 0 020389 SRC n/a 573.5 576.1 2.5720390 SRC n/a 576.1 578.7 2.6320391 SRC n/a 578.7 581.2 2.4720392 SRC n/a 581.2 584.5 3.3320394 SRC n/a 584.5 588.0 3.4820396 SRC n/a 588.0 590.9 2.8920397 SRC n/a 590.9 593.8 2.8920398 SRC n/a 593.8 595.9 2.14

CHAB 06-45


20399 SRC n/a 595.9 598.0 2.1420401 SRC n/a 598.0 601.5 3.5020402 SRC n/a 601.5 604.5 3.0020403 SRC n/a 604.5 607.1 2.5220404 SRC n/a 607.1 609.6 2.5320405 SGS 20405 609.6 613.1 3.50 8.04 0 0 0 0 0 0 0 0 0 020407 SRC n/a 613.1 616.6 3.5020408 SRC n/a 616.6 620.1 3.5020409 SRC n/a 620.1 623.6 3.5020410 SRC n/a 623.6 627.1 3.5020412 SRC n/a 627.1 630.6 3.5020414 SRC n/a 630.6 634.1 3.5020415 SRC n/a 634.1 637.6 3.5020416 SRC n/a 637.6 641.1 3.5020417 SRC n/a 641.1 644.6 3.5020419 SRC n/a 644.6 648.1 3.5020420 SRC n/a 648.1 651.1 2.9820421 SRC n/a 651.1 654.1 2.9820422 SRC n/a 654.1 657.6 3.5020423 SGS 20423 657.6 660.6 3.00 6.92 0 0 0 0 0 0 0 0 0 020425 SRC n/a 660.6 663.1 2.5820426 SRC n/a 663.1 666.6 3.5020427 SRC n/a 666.6 670.1 3.5020428 SRC n/a 670.1 673.6 3.5020430 SRC n/a 673.6 677.1 3.5020434 SRC n/a 677.1 680.3 3.1220435 SRC n/a 680.3 683.8 3.5020436 SRC n/a 683.8 687.3 3.5020438 SRC n/a 687.3 690.3 3.0020439 SRC n/a 690.3 692.7 2.4620440 SRC n/a 692.7 695.2 2.4620441 SGS 20441 695.2 698.7 3.50 7.83 0 0 0 0 0 0 0 0 0 020443 SRC n/a 698.7 702.2 3.5020444 SRC n/a 702.2 705.7 3.5020445 SRC n/a 705.7 709.2 3.50

CHAB 06-45


20446 SRC n/a 709.2 712.3 3.1220448 SRC n/a 712.3 715.0 2.7120450 SRC n/a 715.0 717.7 2.7020451 SRC n/a 717.7 721.1 3.3520452 SRC n/a 721.1 724.6 3.5020453 SRC n/a 724.6 728.1 3.5020455 SRC n/a 728.1 731.6 3.5020456 SRC n/a 731.6 735.1 3.5020457 SRC n/a 735.1 738.6 3.5020458 SRC n/a 738.6 742.1 3.5020459 SGS 20459 742.1 745.6 3.50 7.49 0 1 0 0 0 0 0 0 0 120461 SRC n/a 745.6 749.1 3.5020462 SRC n/a 749.1 752.6 3.5020463 SRC n/a 752.6 756.1 3.5020464 SRC n/a 756.1 759.6 3.5020466 SRC n/a 759.6 763.1 3.5020468 SRC n/a 763.1 765.5 2.4720469 SRC n/a 765.5 768.0 2.48QA/QC20262 SGS n/a 12.62 16.01 3.39 6.00 0 0 0 0 0 0 0 0 0 020267 SGS n/a 81.30 84.72 3.42 6.65 0 0 0 0 0 0 0 0 0 020269 SGS n/a 90.76 94.26 3.50 7.00 1 0 0 0 0 0 0 0 0 120270 SRC 20270 94.26 94.26 0.0020271 SGS n/a 94.26 94.26 0.00 5.94 0 0 0 0 0 0 0 0 0 020275 SRC 20275 164.86 168.41 3.5520280 SGS n/a 213.00 216.50 3.50 7.60 0 0 0 0 0 0 0 0 0 020285 SGS n/a 266.39 268.88 2.49 5.36 0 0 0 0 0 0 0 0 0 020287 SGS n/a 294.66 298.26 3.60 7.72 0 0 0 0 0 0 0 0 0 020292 SRC 20292 318.27 321.00 2.7320298 SGS n/a 335.06 338.56 3.50 7.80 0 0 0 0 0 0 0 0 0 020303 SGS n/a 349.06 352.56 3.50 8.07 0 0 0 0 0 0 0 0 0 020305 SGS n/a 352.56 356.06 3.50 6.57 0 0 0 0 0 0 0 0 0 020310 SRC 20310 366.56 369.56 3.0020316 SGS n/a 409.55 413.05 3.50 6.63 0 0 0 0 0 0 0 0 0 020321 SGS n/a 423.55 427.05 3.50 6.43 0 0 0 0 0 0 0 0 0 0

CHAB 06-45


20323 SGS n/a 427.05 430.55 3.50 7.44 0 0 0 0 0 0 0 0 0 020324 SRC 20324 430.55 430.55 0.0020325 SGS n/a 430.55 430.55 0.00 5.72 0 0 0 0 0 0 0 0 0 020329 SRC 20329 437.55 440.00 2.4520334 SGS n/a 449.36 451.74 2.38 5.37 0 0 0 0 0 0 0 0 0 020339 SGS n/a 461.00 464.33 3.33 6.62 0 0 0 0 0 0 0 0 0 020341 SGS n/a 464.33 466.43 2.10 4.53 0 0 0 0 0 0 0 0 0 020346 SRC 20346 473.70 476.30 2.6020352 SGS n/a 490.71 494.21 3.50 8.25 0 0 0 0 0 0 0 0 0 020357 SGS n/a 503.75 506.28 2.53 5.96 0 0 0 0 0 0 0 0 0 020359 SGS n/a 506.28 509.28 3.00 5.88 0 0 0 0 0 0 0 0 0 020364 SRC 20364 516.50 520.00 3.5020370 SGS n/a 532.47 533.97 1.50 3.3 0 0 0 0 0 0 0 0 0 020375 SGS n/a 544.47 546.97 2.50 5.95 0 0 0 0 0 0 0 0 0 020377 SGS n/a 546.97 549.51 2.54 5.95 0 0 0 0 0 0 0 0 0 020378 SRC 20378 549.51 549.51 0.0020379 SGS n/a 549.51 549.51 0.00 6.4 0 0 0 0 0 0 0 0 0 020383 SRC 20383 556.51 560.01 3.5020388 SGS n/a 570.51 573.50 2.99 7.18 0 0 0 0 0 0 0 0 0 020393 SGS n/a 581.17 584.50 3.33 7.58 2 0 0 0 0 0 0 0 0 220395 SGS n/a 584.50 587.98 3.48 7.71 0 0 0 0 0 0 0 0 0 020400 SRC 20400 595.90 598.04 2.1420406 SGS n/a 609.59 613.09 3.50 7.4 0 0 0 0 0 0 0 0 0 020411 SGS n/a 623.59 627.09 3.50 7.39 0 0 0 0 0 0 0 0 0 020413 SGS n/a 627.09 630.59 3.50 6.9 0 0 0 0 0 0 0 0 0 020418 SRC 20418 641.09 644.59 3.5020424 SGS n/a 657.55 660.55 3.00 7.22 0 0 0 0 0 0 0 0 0 020429 SGS n/a 670.13 673.63 3.50 8.36 0 0 0 0 0 0 0 0 0 020431 SGS n/a 673.63 677.13 3.50 7.39 0 0 0 0 0 0 0 0 0 020432 SRC 20432 677.13 677.13 0.0020433 SGS n/a 677.13 677.13 0.00 5.74 0 0 0 0 0 0 0 0 0 020437 SRC 20437 683.75 687.25 3.5020442 SGS n/a 695.17 698.67 3.50 7.56 0 0 0 0 0 0 0 0 0 020447 SGS n/a 709.17 712.29 3.12 6.88 0 0 0 0 0 0 0 0 0 020449 SGS n/a 712.29 715.00 2.71 5.55 0 0 0 0 0 0 0 0 0 0

CHAB 06-45


20454 SRC 20454 724.55 728.05 3.5020460 SGS 20460 742.05 745.55 3.50 7.85 1 0 0 0 0 0 0 0 0 120465 SGS 20465 756.05 759.55 3.50 7.43 2 0 0 0 0 0 0 0 0 220467 SGS 20467 759.55 763.05 3.50 7.24 0 0 0 0 0 0 0 0 0 0

152.17 352.64 6 1 1 0 0 0 0 0 0 8


DIAMOND RECOVERY BY CAUSTIC DISSOLUTIONProject: 8901-463 Date: November 15, 2006Client: Geos Sciences Inc. LIMS No. MI0009-AUG06




- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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DIAMOND RECOVERY BY CAUSTIC DISSOLUTIONProject: 8901-463 Date: October 19, 2006Client: Geos Sciences Inc. LIMS No. MI0009-AUG06




- 74 µm 0 0.000 0.000TOTAL 1 0.004 0.000





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- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000



Selection and Description Quality Control#REF! #REF!#REF! #REF!



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- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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Mesh Fraction Dissolution Residue Description

+6 Ferromagnetic Non-mag Not applicable

-6+20 Ferromagnetic Non-mag Rock fragments and oxides

+200 Ferromagnetic Mag Oxides and silicates

-20+200 Ferromagnetic Non-mag (Fus. Res.) Oxides, silicates and rock fragments

-20+200 Paramagnetic Mag (0.3 amp) Not applicable

-20+200 Diamagnetic Mag (0.5 amp) Not applicable

-20+200 Diamagnetic Non-mag (0.5 amp) Not applicable


* Total Weight (carats) was calculated from mg weights. All reported mg weights are measured to within 0.002 mg.

Note: SGS Minerals Services is not responsible for the determination of the origin, quality or value of any diamonds recovered. Each +35 mesh (Tyler sieve; +0.420 mm) stone was individually weighed, and the -35 mesh stones were weighed in groups. Stone dimensions are limited to accuracy of three dimensional measurements of irregular shapes using a petrographic microscope.







-6+20 Ferromagnetic Non-mag Silicates

+200 Ferromagnetic Mag Oxides

-20+200 Ferromagnetic Non-mag (Fus. Res.) Oxides and silicates









DIAMOND RECOVERY BY CAUSTIC DISSOLUTIONProject: 8901-463 Date: January 2, 2007Client: Geos Sciences Inc. LIMS No. MI0011-AUG06




-6+20 Ferromagnetic Non-mag Silicates and oxides

+200 Ferromagnetic Mag Silicates

-20+200 Paramagnetic Mag (0.1 amp) Silicates, oxides and graphite













- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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-6+20 Ferromagnetic Non-mag Rock fragments

+200 Ferromagnetic Mag Not applicable

-20+200 Ferromagnetic Non-mag (Fus. Res.) Oxides and silicates













- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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- 74 µm 0 0.000 0.000TOTAL 1 0.015 0.000





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- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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DIAMOND RECOVERY BY CAUSTIC DISSOLUTIONProject: 8901-463 Date: December 12, 2006Client: Geos Sciences Inc. LIMS No. MI0014-AUG06




- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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- 74 µm 0 0.000 0.000TOTAL 2 0.009 0.000





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- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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- 74 µm 0 0.000 0.000TOTAL 1 0.006 0.000





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- 74 µm 0 0.000 0.000TOTAL 1 0.005 0.000





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- 74 µm 0 0.000 0.000TOTAL 2 0.008 0.000





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- 74 µm 0 0.000 0.000TOTAL 0 0.000 0.000





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DDH : CHAB 06-35

Drilled by : Foramex

Ressources Dianor Inc.

Claims title: 124335 Township : Chabanel Range Lot

Geologist : Laura Mancini et Bernard-Olivier Martel, geo From : 2006-04-22 Description date: 2006-05-03

Collar

Azimuth Plunge Length

: 270.00° : -87.00° : 474.00m

Down hole survey i Type ~"".'_".' .......... -,._D~I': ... p .. f ... b.

f'lex-Dip 90001 FleX-It 12.0001 Flex-it 15.0001 FleX-It 18.0001 FleX-It 210001 Flex-it 240001 FleX-It 27.0001 Flex-it 30.oom Flex-it 330001 FleX-I! 36.0001 Flex-it 39.00m Flex-it 42.0001 Flex-it 45.00111 FleX-It 48.0001 Flex-it 5 J .00m Flex-it 54.00m

size: NO

Project: Chab

Longitude (East) Latitude (North) Elevation

Azimutb

267.53° 266.96° 265.73° 26417° 264.42° 264.54° 264.29° 262.84° 263.61° 26112" 259.84° 258.70° 258.03° 257.72° 257.78°

-86.39" -86.20° -86.13° -85.95° -85.70° -85.46° -85.23° -85.05° -84.88° -84.76°

Left. NAD 83 Zone 16

671455.852 5326300.624 327.235

Flex-it Flex-it FleX-It Flex-!t FleX-It Flex-it FleX-It Flex-it Flex-!t Flex-a Flex-it Flex-it flex-II

Cemented: No

7500m 78.00m 810001 84.00m 87.00m 9000m 9300m 9600m 9900m 102.00m

Section Level Work place: Leadbetter

To: 2006-04-29

255.97° 255.96° 255.62· 255.35° 255.74° 255.75° 255.83° 255.16° 25544· 255.54°

....... - .. --~--......

Storage: Yes

-84.65° _84.48° -84.43° -84.27° -84. I30 _8391° -83.78° -83.55° -83.39° -83.26° -83.21 °

2007-10-08

Project: Chab

~yp~ __ ~h Flex-it Flex-It Flex-a Flex-It Flex-It Flex-it Flex-it FleX-It FleX-It Flex-it Flex-It FleX-It FleX-It Flex-it FleX-It Flex-it Flex-It Flex-it Flex-it Flex-it Flex-it Flex-it FleX-It FleX-It Flex-ll Flex-it FleX-It Flex-It Flex-it Flex-it Flex-it Flex-it Flex-It FleX-It Flex-it Flex-it fleX-It Flex-it Flex-it Flex-it FleX-It Flex-It FleX-I! FleX-II Flex-it Flex-it Flex-it Flex-it Flex-it FleX-II Fiex-ll

I 10500m 108.00m Ill.OOm 11400m I17.00m 120.00m 123.00111 126.00m 129.00111 132.00m 135.00111 138.00m 14100m I 44.00m 147.00m 150.00m 153.00m 156.00111 15900m 16200111 165.00111 168.00m 17100111 174.00111 I 77.00m 180.00m 183.00m 18600m 18900m !92.00m 19500m 198.00m 20100m 204.00m 20700111 210.00m 21300m 21600111 219.00m 222.00m 22500m 228.00m 23100m 23400m 237.00m 240.00111 24300111 246.00m 24900m 25200111 25500m


Azimuth Plunge II 255 32° ·:::.....----.--."""'83"-."13"0"""'=-.

'5 - yo .82.99° 125~4~O .82.81°

25554° -82.62' 255.43° -82.48° 255.53° -82.30° 25520° -82.18° 255.39° -82.10° 255.50° -81.91° 255.47° -8169° 255.07° .81.51 ° 254.95° -81.32° 25526° -81.11° 25499° -80.82° 254.21 ° -80.58° 25496° -80.55° 254.43° -80.57· 254.19° -80.41 ° 25453° -80.19° 254.77° -79.73° 25436° -79.08" 253.19° -78.48" 25204° -78.11· 251.62° -77.65" 25167° -77.38° 25173° -77.30° 25218° -77.31° 25195° -77.20° 251.62° .77. J40

251.56° 25 \.58° 251.50" 251.52° 251.60° 251.48° 251.27° 250.15° 251.29° 250.02° 247.60° 251.60° 249.93° 250.68° 250.71° 250.41 ° 25004° 249.94° 24963° 249.25°

.77.00° -76.90° -76.75° .76.67° -76.60° -76.54° .76.490

-76.37° -76.28° -76.21 0

-76.15° -7606° -7599° -75.92° -75.89° -75.80° .75.73° -75.68· -75.59° -75.52° -75.39° -7530°

FleX-I! Flex-It Flex-It Flex-tt Flex-it Flex-It Flex-it FleX-It Flex-it FleX-It Flex-it Flex-it Flex-it Flex-it Flex-it FleX-II FleX-It Flex-it Flex-it Flex-il Flex-it Flex-it Flex-it Flex-it fleX-It Flex-it Flex-it Flex-it Flex-it FleX-II Flex-it Flex-it Flex-it Flex-it Flex-it Fiex-it Flex-it FleX-It Flex-tt Flex·it Flex-it Flex-it Flex-it Flex-it FleX-It Flex-it FleX-It Flex-it FleX-I! FleX-I! Flex-it

25800111 261.00m 264.00m 267.00m 270.00111 273.00m 276.00m 279.00m 282.00111 285.00m 288.00m 29LOOm 294.00111 297.00m 300.00m 30300m 30600m 30900111 312.00111 315.00111 318.00111 321.00111 32400m 327.00m 330.0Om 333.00m 33600m 339.00111 342.00m 345.00111 348.00m 35 100m 35400m 357.00m 360.0Om 363.00m 366.00m 36900m 372.00m 37500111 378.00m 38 LOOm 384.00m 387.00111 39000m 393.00m 39600m 399.00m 40200m

DDH : CHAB 06-35 Page: 2

~ ~~- ~--- - --~~~- ~--~~~~~ _ ~ Plu~_-=:J r--!IP~- Dep!h ___ .~r~zimuth I Flex-it 41100m 252 170

[-70910 I

I Flex-It 414.00m 252.16" -7086° , I Flex-II 417.00m 252.30° ! -70.81° I Flex-II 420.00m 25248°

1-70

.

770 Flex-it 423.00m 251.61° -70.72° Flex-it 426.00m 252.49" -70.67° Flex-it 429.00111 252.41° • _70.62° Flex-it 432.00m 253.]2° I-70.56° Flcx-it 43S.00m 252.88° -70.51° Flex-it 438.0001 25275° I -70.46° Flex-it 441.0001 253.03° , -70.42° flex-It 444.00111 25302° -7035° Flex-it 447.00m 253.10° -70.29° Flex-it 450.00m 253.22" -70.28° Flex-it 45300m 253.28° -70.28° flex-it 456.00m 253.34° -70.26° Flex-it 459.00m 253.23° -70.24° Flex-it 462.00m 253.26° -70.21° FleX-It 46500m 253.40° -70.20° Flex-it 4680001 253.38° -70.21 ° Flex-it 47100m 25472° -70.21°

DDH : CHAB 06-35 Page: 3

49.64


DESCRIPTION

920 OB Overburden Overburden

25 07 CONGlO; GaG; Po Conglomerate; Gray Green; Polymictic The rock is a grey-green colored, polymictic (limited composition), conglomerate. The rock is medium-supported, but there are areas that are clast-supported or matnx-supported throughout the section Two thin sectIOns were taken, one coarse-grained (LGI9902-1), and one fine-gramed (LGI9902-2), within the same sequence for comparison to see if they are related. The clasts appear to be 100% telsic in composition and range in shape from sub-angular to sub-rounded and in size from I mm - 3 em There are several fine-grained grey and medium-grey clasts that could be sedimentary rock or a volcanic tuff. Also there are some fine-gramed light grey and pmkish-grey clasts that could be volcanic rock. There are only a couple of pieces of chert No obvious mafic clasts can be seen The clasts are oriented at 50" TCA The matrix is fine-gramed and is a grey-green color. There is a little disseminated pyrite and some carbonate throughout the matrix. There is <1% quartz veins (nun - em), in the rock Some of the veins have carbonate andlor epidote alterattons The contact at 2507 m is approximate. There is a gradual change into sandstone up to 25.07 m then there are no obvious clasts after this point

9.20 25.07 MmS

4964

43.68

49.37

5J67

49.64

SS

Medium-Supported conglomerate medium-supponed

Sandstone The rock is a coarse-grained grey colored sandstone The rock contains -2% quanz veins (mm - em), some With epidote and carbonate alteratIOn There is a large quartz vein with epidote alterations from -46.40 m - 46.70 m. There are foliations at -35" TCA throughout the section There are two faults from 4368 m - 43.80 m and 49.37 m - 49.64 m. The contact at 49.64 m is approximate. The fault at 49.37 m 49.64 m makes it ditficult to see if there is a sharpe contact between the sandstone and micro-conglomerate 43.80 Fai

Faulting Fault in sandstone

49.64 Fai Faulting Fault in sandstone

CONGlO; DGa, Po Conglomerate; Dark Gray; Polymictif The rock 15 a dark grey polymictic (limited composition), conglomerate The rock IS clast-supported with areas that are matnx-supported. The clasts appear to be almost 100% felsic and range in shape from sub-angular to sub-rounded and in size from lmm to I em. There are several fine-grained grey and medium-grey clast<; that could be sedimentary rock or a volcamc tuff The clasts m this section are similar in composition and size to the conglomerate trom 67.12 m - 73.52 m. The matrix is dark grey and fine-gramed with disseminated pyrite, There is <1% quartz veins (mm em) in the rock. At the contact zone with the dyke, the rock is a darker greenish-grey with the majority of the quarts veins in this area Tne contact at 5l.67 m is irregular and at _60" TCA. 51.67 CtS

Clast-Supported conglomerate clast-supported

6712 I3L Mas Lamprophyre; Massive The rock is a dark grey to black colored, fine-grained porphyritic lamprophyre The rock contains -2% yellowish-green colored porphyroblasts that range in size from Imm· 1 em There 1S <\% carbonate veins in the rock The rock contams a sandstone unit, possibly a xenolith, between 55.90 m - 5778 m The upper contact of the sandstone unit is sharp and at 45" TCA and the lower contact is Irregular and at 85" TCA. The chill margins on the dyke, at all the contacts.are a more brown color compared to the interior of the dyke section. The contact at 67.12 m IS irregular and runs from -parallel TCA to 45° TCA.

55.90 5778 SS Saudstone Sandstone unit, possibly a xenolith in lamprohyrc dyke

Project: Chab DOH: CHAB 06-35 Page : 4

I I

ii :1

II II I' I

I

12

73.52

73.52


DESCRIPTION

CONGLO: DGa. Po Conglomerate; Dark Gray; Polymictic The rock is a dark grey colored, limited polymictic conglomerate The rock is medium-supported, but there are small areas that are clast-supported or matrix-supported. The clasts appear to be almost 100% felsIC in compositIOn and range in shape from sub-rounded to rounded and In size from 1 mill - 2 em. There are several fine-grained grey and medium-grey clasts that could be sedimentary rock or a volcanic tuff Also there arc some fine-grained light grey and pmklsh-grey clasts that could be volcaniC rock There are a lew clasts that may be mafic but It is difficult to telL The matrix is a dark grey color and is fine-grained There IS a bit of carbonate m the matrix, There is <I % quartz veins (mm - cm), very few have carbonate alterations. This conglomerate IS much harder and darker than the one from 9.20 m - 2507 m. most likely due to the hot emplacement of the dyke

67.12 73.52 MmS

74.87 13L~ Mas

Medium-Supported conglomerate medium-supported.

Lamprophyre; Massive The rock is a dark grey to black colored, fine-grained porphyritic lamprophyre The rock contains -I % yellowish-green colored porphyroblasts that range in size from J mm - I em. There IS < I % carbonate veins in the rock. The contact at 73.52 m IS sharp and at _300 TCA The contact at 74.87 m IS Irregular and sub-parallel TCA

74.87 104.80 CONGLO; G; Po

10480

Conglomerate; Green; Polymictic The rock is a green colored polymictic conglomerate. The rock is composed 01'45% matrix, 29% felsic clasts, 25% mafic clasts and <I % quartz veins. The rock is medium-supported; the conglomerate grades from coarse to fine-grained and has the impression of both normal and inverse bedding. Two thin sections were taken, one coarse-grained (LG 19926), and one fine-grained (LG 19927). Within the same sequence for comparison to see If they are related The clasts range in shape from sub-angular to rounded and in size from I mm - 3 em TIle larger clasts tend to be mO[e rounded and the smaiier clasts tend to be a little more angular. There are a lot of fine-grained light to medIUm-grey and creamy colored felSIC clasts that could be a volcanic tuff There are a few dark-grey fine-grained clasts that could possibly be sedimentary or a dacite. There are a lot of green fine-grained mafic clasts that could be basaltic tuff Also, there are a few chert clasts scattered throughout the section. There are no obvious gabbroic clasts in this sectwn. The clasts from 78.00 m - -89.60 m appear to be Imbricated at 450 TCA The matrix is a fme-grained green color. In areas where the clasts arc very small, the matrix appears to be more grey than in the areas with the larger clasts. There is disseminated pyrite and pyrrhotite and carbonate alterations throughout the matrix. There are piles of pyrrhotite cubes from -91 68 m - 104 80 m. The quanz vems are 111m - em in size and some have carbonate alteratIOns. From -7874 m - 8 i .00 m there IS the Impression of a possible SO surface between fine-grained and coarser-grained matenal sub-parallcl TCA. The sectlon where the clasts appear to be imbricated could possibly be an SI surface. There is a smalllamprophyre dyke from &2.93 m 83.42 m. It appears to be the same as the dyke from 73.52 m - 74.87 m. The contact at 104.80 m is approximate. The rock gradual cbanges from green to grey.

74.87 82.93 MmS Medium-Supported Conglomerate medlUn .. supported~ has areas that arc either c1ast-supporteoj,or matrix-supported. (graded bedding coarse!O fine normal and Illverse)

82.93 83.42 BL Lamprophyre lamprophyre dyke in the conglomerate umt

83.42 104.80 MmS Medium-Supported Conglomerate medium-supported; has areas that are either clast-supported or matrix-supported, (graded bedding coarse to fine nOMal and inverse)

124,30 CONGLO; Ga: Po Conglomerate; Gray; Polymictic The rock is a grey colored polymictic conglomerate The rock is composed of 39% felsic clasts, 30% mafic clasts, 30% matrix and J % quartz veins. The rock 1$ medIUm-supported: the conglomerate grades from coarse to finc-grained and has the impression of both normal and inverse bedding. Two thin sections were taken, one coarse-gramcd (LG 19931-1 L and one fine-gramed (LG 19931-2), Within the same sequence fur comparison to see Ifthey are related The clasts range in shape from sub-angular to rounded and in size Irom I mm 2 cm. The larger clasts tend to be more rounded and the smaller clasts tend to be a little more angular. The clasts in tillS section appear to be stretched and imbricated at -50' TCA There are a lot of fine-grained light to medium-grey and creamy colored felSIC clasts that could be a volcanic tuff There arc a few slightly coarse-grained medium-grey clasts that possibly are sedimentary There arc a lot of green fine-grained mafic clasts that could be basaltic tuff Also, there are a f~w chert clasts. There arc no ObViOUS

gabbroic clasts

Project; Chab DOH: CHAB 06·35 Page 5


DESCRIPTION

The matrix IS grey m color and fine-grained with areas that are more coarse-grained There IS dIsseminated pyrite and carbonate alteratlons throughout Ihe section From 118.93 m - 120.00 m the rock IS a more ohve-bro~n color most Iikelv from an alteration There IS a 101 more quartz veming in this section compared to the previous section The veins are mm - cm in size plus tmy little spider vems Some oflhe velDS are deformed and have epidote alterations. Most of the veins have carbonate alterations. The contact at 124.30 m is approximate. The rock gradually changes from conglomerate to sandstone and there is a lot of veining at the contact so it is diffrcult to see it dearly.

104.80 124.30 MmS Medium-Supported Conglomerate medium-supported: has areas that are either clast-supported or matrix-supported, (graded beddmg coarse to tlne normal and mverse).

124.30 146.29 S2A Arkose Wacke The rock is a coarse-grained pale brov,msh-grey massive arkose (there is the slight impression of foliations in some sectIOns at -45" TCA) The color of the rock could be duc to alterations. The rock contains -20% quartz veins (nun - em), some with epidote and most with carbonate alterations Many of the veins are deformed and the core is brecciated in several places from vein implacemcnt

146.29 157.07 D: M Dyke; Mafique The rock is a dark grey fine-gramed mafic dyke, possibly a basalt There are <I % quartz veins (mm - cm) with carbonate alterations in the rock Both contacts are megular with the upper contact at _350 TCA, and the lower contact at -45° TCA

15707 164.55 SS

164.55

Sandstone The rock is a grey colored coarse-grained sandstone. The rock contains -15% quartz vems (mm - em). Many of the veins are deformed and have carbonate alterations There IS a shear zone with possible sericite alterations from-16270 m 16455 m. The contact at 164.55 is approximate The sandstone appears to gradual grades mto the conglomerate.

162.70 16455 She Shearing Shear zone in sandstone unit at contact with conglomerate

182.04 CONGLO; Ga, Po Conglomerllte; Gray; Polymictic The rock is a grey colored polynllctic (limited composition),conglomerate The rock is medium-supported and is approximately composed of 35% felsic clasts, 30% mafic clasts, 20% matrix, 20% quartz veins. There is a shear zone from -168.00 m - 175.70 m. It is unclear whether this sheared section is conglomerate or sandstone. It has been placed in the conglomerate descrrption based on there bemg clasts from 164.55 m - 168. 00 m and what appear to be clasts from 172 00 m - 175.70111 and definite clasts from 175.70 m - 18204. This shearing makes 11 very ditTicult to identify dIfferent clasts and matrix to get proper percentages Two thin secllons were taken within the same section (LG 19955-1 and LG 19955-2), for comparison to see if they are related and whether they are sandstone or conglomerate The clasts range in shape from sub-rounded to rounded and in size from 1 nun - 3 em lbere are a lot of fine-grained very Irght grey to white clasts which appear to be quartz, pOSSibly chunks of fractured veins. There are several tine-grained gray-green clasts that are poSSibly maftc volcaniC rock (basalt). There are a lot affine-grained grey to medium grey clasts which could be a felsic volcanic rock (dacite). There are a few fine-grained dirty-creamy colored clasts that could be a felsic vol.canic tutI There are no obvious gabbro!c clasts in this section The matrix is fine-grained and a grey color with disseminated pyrite a,'1Q pyrrhotite as well as carbonate and sericite alterations throughout 'I here are foliations in the matrix at _50" TCA The sheared areas have a coarser-grained matrix and the IDaJonly of the quartz vems. The veins range in size from nun - em plus tiny little spider veins. most of the vell1S are deformed and have carbonate alteratIOns. The contact at 182.04 m is approximate An alteration zone starts at this poml making it difficult to see a clear contact between conglomerate and volcalllcs

164.55 182.04 MmS Medium-Supported Conglomerate medium supported. There are areas that are mostly clast-supported and arcas that are sheared therefore appear to be matnx-supported

168.00 175.70 She Sbearing Shear zone within conglomerate umt

182.04 293.30 V; V3A; Py

Project: Chab

Volcanic; AndesitelDacitc; Pyroclastic The rock is a fine-grained grey colored volcanic rock, possibly a daclle tuft/ash or lapillistone. There IS no evidence of pillows and the unit does not have the look ofa massive t1ow. There IS an alteration lone, containing carbonate and sericite, at the beginning of the unit ll1 contact with the conglomerate from 182.04 m - 189.74 m. From -215.00 m - 228.00 I1l there are faint larger fragments which may be a further indicator that this is a Tallapillistone There are what appear to be layers of o5h throughout the unit (these could also Dc sericite alterations). the layers are at -45· TefL There are fiO obviou> fcidspmhlc phenocrysts. hom 212.00 111- 212.4 m there are well formed calcite crystals in several little veins From 213.4 m-

DOH: CHAB 06-35 Page 6


DESCRIPTION

214.53 m there are what appear to be quartz and rock fragments mixed together In what may have been a quartz vem (does not look like tYPIcal brecciation created by vein implacement) There is -5% quartz vell1s in the sectIon. The veins are all deformed and have altered the rock in many places making It difficult to really Identify the type of volcanic rock from -262 00 m- 270.00 m, there appears to be a shear zone that IS sub-parallel TCA It has very deformed veins that are sigmOIdal in form The contact at 293.30 m is approxlluate The rock appears to gradual grade mto the conglomerate

18204 189.74 Cb; SrMv carbonate; sericite/muscovite Alteration zone at begmning of volcanic unit Has carbonate and sericite alterations

293.30 307.72 CONGLO; Ga; Po Conglomerate; Gray; Polymictic The rock is a grey colored polymicllc (limited composition),conglomerate The rock IS medium-supported and IS approximately composed of 45% mafic clasts, 40% felsic clasts, 15% matrix, <I % quartz veins. The conglomerate IS deformed making it difficult to really make out matrix and clasts clearly There are a few places where felsic and mafic clasts are obvious. The clasts are elongated and imbricated at _50· TCA. The clasts range in shape from sub-angular to rounded and in size from I mill - 3 em. There are several fine-grained green clasts that are possibly mafic volcanic rock (basalt) There are a lot of fine-grained grey to medium grey clasts which could be a felsic volcanic rock (dacite). There arc a few small very fine-grained black clasts that arc soft enough to be argillite There are no obvIOUS gabbroic clasts in this section. The matrix is grey colored and fine-grained with disseminate pyrite, pyrrhotite (also piles of pyrrhotite cubes), and carbonate alterations throughout There are areas ofthe matrix where there is the impression of a foliation which is at -50" TCA. There are very few veins (mm - em l, in the section most are deformed with carbonate alterations. The vems have Sigmoidal and ptygmatic forms The contact at 293.30 m is approximate, it appears to be where the first famt clasts are seen The contact at 307.72 m is also approximate, It IS difficult to tell if the conglomerate stops here or sooner.

29330 307.72 MmS Medium-Supported Conglomerate medium-supported, very difficult to make out clasts and matrix clearly

30772 310.66 V; V3A, Py Volcanic; AndesitelDacite; Pyroclastic The rock is a fjne-gramed grey colored volcanic rock, possibly a dacite tuff/ash or lapillistone. There is no evidence of pillows and the unit does not have the look of a massive flow. There arc what appear to be layers of ash throughout the unit (these could also be sericite alterations), the layers are at -55" TCA. The section is deformed and altered, there arc very few features 10 really identifY the type of volcamc unit properly. There are no obvious feldspathic phenocrysts There are disseminate and piles of pyrrhotite throughout the section. The piles are associated with carbonate alterations between the layers. There ale very few quartz veins « I %), mm cm in size. There are carbonate alterations throughout the rock and in the veins. The contact at 310.66 m is approximate. There is an abrupt change 10 a more green color but hard to tell iflhe volcanic unit really finishes here and tbe conglomerate begms

310.66 396.25 CONGLO, GaG, Po Conglomerate; Gray Green; Polymictic The rock is a grey-green colored polymictic conglomerate The rock is composed of 45% felsic clasts, 27% mafic clasts, 20% matnx and 8% quartz veins. There are sections oflhe rock where it is difficult to discern between clast and matrix and the type of clast (scratch test was used to roughly determine felsic to mafic clast ratios). In generdl the rock appears to be more clast-supported The clasts range in shape fram sub-angular to rounded and in size from I mm - 13 em. There are several fllle to medllJm-grained grey and medIUm-grey clasts that could be sedlll1cntary rock or a volcanic tuff/ash. There are a few dark-grey to black fine-grained clasts that could possibly be sedimentary (argillite"), also there are a lot of green fine-grained mafic clasts that could be basaluc tuff There are a few fine-grained pinkish-brown clasts that could be a felsic volcanic rock with alterations. There are a few small coarse-grained gabbroic clasts but it is difficult to say whether they are leucocratic, mesocratlc, etc. There are several fme-grained creamy and pale grey colored clasts with a pmphyritic texture that could possibly be a pyroclastic (Iapillistone) rock. There are a few lIght grey to medium grey colored coarse-grained clasts that appear to be a felsic intrusive rock. The matrix is finc-grained with areas that arc slightly coarser-grained and is a grey color. There is dissemmated pynte. pyrrhotite seriCite and carbonate alterations throughout the matrix. The quartz vems are ll1lll em ill size, some with epidote and most with carbonate alterations The veins from -326.00 \11- 327.&& m runs sub-parallcl TCA. There are several areas that have large piles of pyrrhotite cubes assOCiated With the veins, partIcularly at 326.73 m The contact at 396.25 111 is approxlIllate. The rock gradually grades mto an argillite.

310.66 35676 MmS Medium-Supported Conglomerate medium-supported. There are areas where it IS dlft'tcult to make out clasts and matrix, therefore unsure if it is really clast-supported or matnx-supported

35676 367 33 CtS Clast-Supported Conglomerate clast-supported

367.33 370.&2 MmS

=====:.=========-= .... ~---~-=--=-=-----=-=--... ~---.===------.-. _. Project: Chab DOH: CHAB 06-35

_~. __ ~_:::-.=======-.::.::"J Page 7

Ressources Dianor Inc. ~=====~,~~.=====================~====~========

DESCRIPTION

Medium-Supported Conglomerate medium-supported TIlere are areas where it is difficult to make out clasts and matrix, therefore unsure If it IS really clast-supported or matrix-supported

370.82 37783 CtS Clast-Supported conglomerate clast-supported

377 83 39150 MmS Medium-Supported Conglomerate medium-supported There afe areas where it is diilicult to make oul clasts and matrix, therefore unsure if it IS really clast-supported or matrix-supported

391.50 39387 CtS Clast-Supported conglomerate cl ast-supported

393.87 .W625 MmS

39625 474.00 ARG; SS ARG;SS

!'\tedium-Supported Conglomerate medium-supported There are areas where It is difficult to make out clasts and matrix, !herefore unsure If it is really clast-supported or matrix-supported

The rock is a fine-grained grey sandstone with dark grey argillite layers. The rock is composed of 55% sandstone, 45% argiUite,.5 % quartz veins. from 390.00111 - 399.50 m and 458.70 m - 474.00 m, !he umt is mainly argillite With very little sandstone. From 438.84 m - 441.15 and 445.77 m 458.70111, the unit is mainly sandstone with very lIttle argillite There is a shear zone from 43730 m - 438.84 m. In general, the argillite layers range in Size from <1 mm - 30 em and the snadstone from 3 rnm - I m The contacts between the sandstone and argillite layers are generally irregular with some sharp ones The angle of the layers is at _700 Ie A. The quartz veins are mm - em in size and many of them are defonned with carbonate alterations. The deformed veins are sigmoidal and ptygmatic in form. The veins at -411.00 m are breCCiated. There IS disseminated pyrite and some pyrrhotite throughout the unit

396.25 399 79 ARG Argillite Mainly argillite section with very little sandstone in sandstone-argillite Uttlt

43730 438.84 She Shearing Shear zone wi!hin the sandstone-argillite unit

438.&4 441 15 SS Sandstone Mainly sandstone section with very little argillite in sandstone-argillite unit

445 77 458 70 SS Sandstone Mamly sandstone section with very little argillite in sandstone-argillite layer

458.70 47400 ARG Argillite Argillite section with very little sandstone within sandstone-argillite unit

DDHend Numberofsamples: 0 Number of samples QA/QC: 0 T otallengbt sampled: 0,00

Project: Chab DOH: CHAB 06-35 Page 8

diamond drilling rpt chabanel twp - ontario...inc's facility in thunder bay. the 298 tonnes of...

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