RECORDED HOLDER: SAME As ABOVE [ X 3

Transcription

1 DIAMOND DRILLING Brackin 42B05SW BRACKIN 010 Report No: 22 WORK PERFORMED FOR! canreos Minerals Ltd. RECORDED HOLDER: SAME As ABOVE [ X 3 : OTHER [ 3 CLAIM No HOLE No, FOOTAGE DATE NOTE ' 456' 426' 397' 300.5' 427' 485' 413.5' Jan/87 Jan/87 Jan/87 Jan/87 Jan/87 Jan/87 Jan/87 Jan/87 (D NOTES: (D #72-87 (filed in August/87)

2 Canrsos Minerals (1980) Ltd. HOLE NO. Page 87-1 Latitude Departure Elevation Azimuth Dip Length degrees degrees Feet Depth Azimuth Dip Depth Azimuth Dip Property Area Location Jedburg 30 Brackin Township L76W, 8LO Date Started Jan 11, 1987 Date Completed Jan 14, 1987 Logged by Roberta Bald Core Size 8Q From To Description- Sample From To Length Au Au ppb pz/ton OVERBURDEN Casing to 12 feet MAFIC TO INTERMEDIATE FLOWS Inhomogeneous material, with gradational contacts ; unit varies from dark green, chlorite rich fine-grained to medium-grained material to dark grey, fine-grained locally plagioclase phyric material ; local zones of fine-grained to medium-grained disseminated black magnetite crystals, results in magnetic core ; calcite occurs as veinlets or throughout core, (reacts to Hfil ) ; locally approximately U fine-grained disseminated pyrite crystals ; local red salmon coloured veinlets, randomly orientated ; blocky core with local weathered, oxidized zones Approximately 6 inch ue width white, coarse-grained quartz vein with irregular upper contact and somewhat irregular (but roughly 90 degrees to core axis ) ; lower contact ; quartz contains ace pyrite crystals, and minor red material ( possible potassium feldspar? ). At 23.9 less than one-half inch wide quartz and calcite veinlet, approximately 90 degrees to core axis with pyrite veinlet parallel to quartz calcite veinlet from approximately 27.0 to 31.0 approximately * vuggy, oxz zones over short sections. Material is quite variable and could possibly contains local tuffaceous sections. Local very chlorite rich short sections with milky white, coarse-grained barren quartz. Increasing amount of plagioclase phenocrysts within approximately 5 feet of lower contact. Local slightly foliation at 70 degrees to core axis. Lower contact ground ONTARIO GEOLOGICAL SUREY ASSESSMENT f RESEARCH MAY RECEIVED DIABASE Fine-grained near contacts to medium-grained, black to dark brown, massive, magnetic, local dark brown magnetite crystals, rare, very large, ( up to 1 inch long ), greenish yellow, waxy, zoned plagioclase crystals, fresh looking. Lower contact irregular with some diabase to approximately PORPHYRITIC DACITE Grey with greenish and blue spots generally fnass-'ve to locally

3 Canreos Minerals (1980) Ltd. Page ; HOLE NO. 87*1 From To Description Sample From Td Length Au Au ppb oz/ton foliated, plagioclase phyric intermediate volcanic flow ; plagioclase crystals are greenish yellow to light grey, locally ;0 102 zoned, up to 154 to 4, up to.25 inches long ; locally glomerocrysts.* unit contains up to 54 white to elecic blue quartz crystals, equant, up to approximately one-eighth inch diameter ; locally maix reacts to HC1, ( calcite ), local less than 54 quartz veinlets with disseminated fine-grained to rarely coarse-grained pyrite. Local fine-grained zone without plagioclase phenocrysts, about 1 inch wide. Quartz veins roughly 80 degrees to core axis at and with pyrite along vein margin ; quartz veins up to 1 inch wide. Plagioclase glomerocrysts up to one-half inch long near 180 feet. Fine-grained to medium-grained, non porphyritic zones up to approximately 1 foot wide. Local red salmon alteration, at red alteration with approximately one-quarter inch of calcite and pyrite veinlets ( threadlike ). Medium-grained to fine-grained, non- porphyritic zones from 221 feet to 224.4, { m* 24 large, up to one-quarter inch long quartz eyes, blueish grey, recrystallized ) ground to lower contact DIABASE Fine-grained to medium-grained, massive black to dark brown ; rare greenish plagioclase laths up to one-third inch long ; threadlike calcite veinlets, 24 randomly oriented. Lower contact ground PORPHYRITIC DACITE Similar 35.7 to Calcite throughout maix. Possibly baked by diabase dike. Rare, small plagioclase phenocrysts but abundant quartz phenocrysts ( blue ). Quartz vein from , irregular ; with 24 fine-grained to medium-grained pyrite along vein margin DIABASE Fine-grained, massive, black to dark brown. Upper contact ground. Lower contact ground? but appears sharp and about 80 degrees to core axis PORPHYRITIC DACITE : similar to to 245 ; and contains local quartz veins at ( less than one-half inch wide ansculert to milky ihits with 24 fine-grained pyrite along vein margins ) ; :5.0 -and ( coarse-gr.rned ans^ucsnt to ^'Iky white 29SOO j:"*:: -;H rv-; " Q FH cn'or-'te vein ^'f ^eo r '.et.-c" v':v'". ' : '.O 34

4 Canrsos Minerals (1980) Ltd. HOLE NO. Page 87-1 From To Descriptionone-half inch of vein margin vein cuts core at 10 degrees and is somewhat irregular ) ; at 256.1, one-half inch wide quartz vein with tt coarse-grained pyrite and red alteration in host rock : variable amount of sericite developed along with slight to moderate foliation ( songest foliation and sericite from to with pinkish tinge ). Foliation at is 80 degrees to core axis. Foliation at is 70 degrees to core axis. Foliation locally variable. Unit gradually becomes massive and porphyritic. From to : unit contains 5% ansculent to milky quartz veinlets up to one -half inch wide. Locally with calcite and rarely with dark green chlorite ; contains tt pyrite and along host rock near vein margins ; rarely vuggy ; with pink salmon coloured alteration along vein margins. From : about 80^ fine-grained, dark grey material, with snarp to gradational contacts with dacite porphyry, contacts at 80 to 85 degress to core axis ; similar material from to Unit is slightly foliated with sericite along foliation planes from to at 70 degrees to core axis. From : foliated, light brownish zone, fine-grained, with tt disseminated fine-grained pyrite, flattened parallel to foliation at 70 degrees to core axis ; calcite threadlike veinlets ; similar short zones at and 368.7, ( less than 2 inches wide ). From to : chlorite, quartz and calcite zone with tt disseminated pyrite. Unit is foliated from to and contains about 21 fine-grained to medium-grained disseminated pyrite from to and slightly more sericitic unit is foliated and contains some sericite along foliation planes ; at 70 degrees to core axis, near and F^orn to : quartz vein, coarse-grained ansculent to milky white, with grey to green host rock inclusions locally with pink salmon coloured possible potassium feldspar ; ace pyrite, contacts somewhat irregular but roughly 90 degrees to core axis from to : quartz vein similar to to but with massive chlorite patches and local dark grey, possibly ankerite aggregates with ace galena? ; locally slightly vuggy ace fine-grained pyrite with red altered host rock on lower margin. From to : quartz vein similar to to 491.0, but roughly!0 degrees to core axis, ( ue width unknown ). From to and to : irregular quartz veins similar to to 491.0, about 50* quartz no sulphides seen epidote veinlets, ( threadlike ) at Dark green chlorite and calcite rich zone from to with 105 quartz calcite veinlets, foliation somewhat irregular but generally 90 degrees to core axis END OF HOLE 12 Feet of bw casing left in hole. Sample From To S Length , Au ppb t r Au oz/ton A vf ^ (\ ^'^

5 Canreos Minerals (1980) Ltd. HOLE NO Latitude Departure Elevation.0 Depth Azimuth Dip Depth Azimuth Dip Property Area Location JE08URG 30 Brackin Township L76W, 7+4QS Azimuth Dip Length 45 degrees degrees Pest Date Started Jan 17, 1987 Date Completed Jan 19, 1987 Logged by Roberta Bald Core Size BQ From To Description- Sample From To Length Au Au ppb Qz/ton OVERBURDEN Casing to 12 feet, GABBRO Medium-grained to coarse-grained, dark green grey, massive to slightly foliated. Calcite as singers and throughout maix, reacts to hcl, dark green amphiboles and chlorite crystals. Local zones of quartz and calcite veins with ace pyrite, 10.5 to 11.3, 39.1 to 39.5 calcite and minor quartz 43.7 to 45.5 with quartz from 43.7 to to 48.6 with quartz from 47,4 to Local fine-grained zones, possibly mafic flow, from 21,8 to 22, from 26.5 gradually becoming medium-grained gabbro, 39.1 to Locally unit is coarse-grained, especially at 51. Foliation at 40 is 70 degrees to core axis. Lower contact masked by quartz calcite veining but sharp MAFIC VOLCANIC FLOW Dark green grey, fine-grained locally amygdaloidal with zones of calcite filled round to elliptical amygdules approximately one-eighth inch diameter. Lower contact ground PORPHYRITIC DACITE Dark to medium grey, fine-grained maix with up to one-third inch diameter light green plagioclase phenocrysts in zones massive to 'ol-'ated, 3t 30.0, 70 degrees to core axis, possible framsntal. Local red alteration with local aca fine-grained disseminated pyrite or pyrite singers especially from 81.0 to Low8r contact ground DIABASE Fine-grained, black, massive, slightly magnetic. Lower contact sharp at 30 degrees to core axis ORPHYRIT!C OACTE Similar to 55.3 to *U.9 but altered, baked by diabase and core

6 Canreos Minerals (1980) Ltd. Page HOLE NO l From To Descriptionsingers of massive pyrite approximately one-eighth inch wide. Lower contact at low angle to core axis about 10 degrees, Contact zone is from 85.3 to Dacite is coarse-grained along contact and contains pyrite. Sample From To Length Au Au ppb pz/ton DIABASE Fine-grained to coarse-grained, dark grey to black, massive, magnetic with local green plagioclase. Phenocrysts up to 2 inches long. Blocky broken core. Becomes finer-grained towards lower contact. Lower contact appears to be sharp but grade PORPHYRITIC DACITE Similar to 65.0 to Vary foliated from upper contact to approximately at 75 degrees to core axis. Possibly fragmental to approximately Grading into fine-grained to medium-grained material possible flow then becoming medium-grained to coarse-grained near Local quartz veinlets, anslucent quartz local 1 i fine-grained to medium-grained pyrite as singers and disseminated crystals locally vuggy plus or minus calcite. Local red alteration with epidote veinlets. Quartz vein zone from 145.O to contains about U fine-grained disseminated pyrite, quartz veins are irregular about 55^ quartz veining. Lower contact sharp at 25 degrees to core axis, crosscutting foliation of porphyritic dacite. Diabase chilled against porphyritic dacite , DIABASE Fine-grained to medium-grained, black, massive, magnetic. Contains approximately 2 \ f ine-grained disseminated pyrite and possible fine-grained pyrrhotite. Lower contact sharp at 30 degrees to core axis, diabase chilled against next unit. Con-act slightly irregular PORPHYRITIC DACITE Zones of red alternation from to 173.2, from to at locally alteration occurs in host rock along margins of dark grsen massive chlorite and or quartz and or calcite and or medium-grained to coarse-grained biotite veinlets no sulphides seen. Also from to Locally foliated at 137, at 191. Quartz veinlets to with fine-grained to coarse-grained pyri:e approximately 3i, : "cn "GO.3 "o 1.5 red alteration similar :o "u.7 to but icr? f'' ''c"" : -;; l : ;o

7 Canreos Minerals (1980) Ltd. Diamond On'11 Log HOLE NO. Pag* 87-2 From To Dsscription- Sample From To Length Au Au ppb fl : ,:o S6. 0, , Red to green, hard with coarse-grained ansculent quartz vein with dark green chlorite and minor grey carbonate, no sulphides seen. Local foliated sections with variable amount of sericite along foliation planes. Trace pyrite. Unit contains plagioclase and quartz crystals to 6.4 but gradually becomes fine-grained, possible a tuff with local quartz crystals to 218.6, gradual contact then unit is possibly a fragmental with local fine-grained zones throughout. Quartz vein from to coarse-grained ansculent quartz, almost 90 degrees to core axis no sulphides ssen chlorite and pink alteration spots along vein margins. Local red alteration along veinlets. Local fine-grained to medium-grained disseminated pyrite. From to local light grey, calcite bearing zones, about 75*. F"om to coarse-grained white to anslucent quartz vein with chlorite rich host rock. Inclusions-a*** medium-grained pyrite as blebs contacts subparallel to foliation about 80 degrees to core axis similar quartz veins from 344'.8 to and to 356.C definite fragments from approximately to end of hole. Fine-grained, disseminated magnetite crystals about 2i throughout core. From to 381.9, chlorite and calcite zone, possible mafic dike. From to irregular quartz vein up to approximately 1 inch wide with sericite in host rock near vein margin if1, t race fine-grained pyrite in pink, vuggy hose rock inclusions. Oz/ton m O F HOLE 12 Feet of casing left on hole.

8 Canreos Minerals (1980) Ltd. HOLE NO. Page 87-3 Laiuuoe Departure Elevation,u.0.0 LII (j lescs Depth Azimuth Dip Depth Azimuth Dip Property Area Location Jedburg 30 Brackin Townsh'ip L40W, 24+80S Azimuth Dip Length 45 degrees degrees Feet : Date Started Jan 21, 1987 Date Completed Jan 22, 1987 Logged by Roberta Bald Core Size 8Q Fnnm Tn Sample From To Length Au Au ppb bz/ton OVERBURDEN Casing to 10 feet MAFIC TO INTERMEDIATE TUFF Dark green grey, medium-grained, with calcite throughout, reacts to hcl foliated at approximately 70 degrees to core axis local calcite veinlets, mostly parallel to foliation dark green chlorite crystals throughout PORPHYRITIC DACITE Local fine-grained sections, from.5 to 21.5 with zone of quartz and calcite and chlorite veins from.6 to 21.5, no sulphides seen from 26.9 to 29.9 with zones of quartz and calcite and chlorite veins from 26.9 to 27.5 and 28.3 to 29.3 quartz is coarse-grained, anslucent to milky white lower contact sharp but partially masked by calcite veinlets Dark green maix contains euhedral white to slightly greenish, locally zoned plagioclase, about 10V up to one-third inch long minor calcite throughout quartz and chlorite and calcite zones from 30.7 to 31.2 ( vein runs roughly parallel to core axis ) and from 32.4 to 33.1 slightly vuggy, oxidized, no sulphides seen lower contact sharp at 50 to 50 degress to core axis, parallel to foliation of next unit MAFIC TO INTERMEDIATE TUFF Similar to 9.0 to Contains blueish quartz crystals less than one-tenth in diameter. From about 31.0, becoming fine-grained and light grey. Foliation at 46.0 feet, 70 degrees to core axis local ace fine-grained disseminated pyrite local black possible tourmaline contains calcite throughout, reacts songly to hcl local medium-grained sections with distinct calcite crystals from 51.3 and 5i.9.and 53.3 to 54.6 from 54.6 onward similar to 9.0 to 29.9 with blueish quartz crystals. Fron 65.5 to 57,0, iiediuin-grained to co^rsa-grained with up to approximately ^ calcite throughout, 'f-cm 53.3 to 73.7 unit contains dark green, chlchte rich wisps *hich are possibly mafic lapilli unit contains calcite throughout. : 0''a'ic"i a: approximately 'set, 70 degrees to corg axis. ~"3C3 fiie-^ined disseninated?yrt3 thrcugnouc. :.cca' quar:: vening 36.2 to 36.J, 91.J Co 9'.5, 92,' to 92.3, 93.' U ! jo ,9 1 js JO ;9 2 jo Q

9 Canreos Minerals (198C) Ltd. Page HOLE NO. 87*3 From To Descriptionto 93.4, 93.8 to 93.9, 97.9 to 98.0 quartz is anslucent to milky white, locally contains calcite plus or minus chlorite plus or minus ace fine-grained pyrite host rock between quartz veins appears silicified, contains variable amounts of black crystals, possibly tourmaline local bleached zones, calcite rich. Intense banding occurs from to 122.0, from approximately 5 to 50% white to light grey, soft bands of calcite amount of banding increases downhole foliation at 1 feet, 65 degrees to core axis local bleached zones from to lower contact as pink to buff white to greenish bands local ace fine-grained disseminated pyrite unit becoming darker, baked from about to lower contact. Lower contact sharp at approximately 80 degrees to core axis, parallel to foliation of tuff. Sample From To Length Au Au ppb oz/ton DIABASE Fine-grained, black maix, core yellow-white plagioclase phenocrysts up to 1 inch diameter, magnetic massive. Lower contact sharp at 60 degrees to core axis, parallel to foliation of next unit MAFIC TO INTERMEDIATE TUFF Similar to to 136.3, baked by diabase. At about 143 is a zone of quartz veins a***-dark grey carbonate and ace pyrrhotite, veins somewhat irregular DIABASE Similar to to 140. Becomes medium-grained to coarse-grained about 5 feet from upper contact. Lower contact sharp at about 80 degrees to core axis, slightly ground MAFIC TO INTERMEDIATE TUFF. Light to dark grey, medium-grained to fine-grained, foliation at 80 degrees to cor? axis local blueish quartz crystals and or plagioclase crystals, ( less than 51 ) local blades, hard elliptical spots up to one-third :nch long local fine-grained pyrite throughout, as disseminated crystals or as short singers parallel to foliation planes local quartz plus or minus calcite plus or minus pyrite veinlets and blffbs rarely a*** sericite and tourmaline also from to about 2i pyrite with local calcite veinlets and blebs from to 313 pinkish tinge, possible potassium alteration from to definite lapilli-sized fragments calcite throughout, reacts to hcl. Local white buff fragments flattened parallel to foliation at 30 degress to core axis. Local zones of black, possibly tourmaline along foliation planes, noticed from 295 to Fragments appear to decrease fro.m approx^rcate'y. j 1 :.: to lower contact and quart: crystals appeals to bs sma'^r * , , , ,.: ,

10 Canraos Minerals (1S80) Ltd. HOLE NO Page 3 From To Description- Alsc noticeable by colour difference. Sample From To Length Au Au ppb oz/ton MAFIC TUFF (?) Greenish grey, fine-grained, calcite throughout, locally very foliated at 30 degrees to core axis no fragments seen zones of approximately 50^ quartz and calcite veining from to 3.4, 3.9 to ace to 2* pyrite and ace tourmaline in veins quartz calcite veins up to 2 inches wide lower contact masked by quartz veining INTERMEDIATE LAPILLI TUFF Similar to to but appears to contain slightly more felsic fragments. About 2* to locally 54 pyrite in host rock from to pyrite occurs as fine-grained disseminated crystals or as short sangers parallel to foliation planes. Local quartz plus minor calcite veins from to to 326.4, to 332 with minor pyrite light grey, bleached zones from to from 336 to approximately 338 about 11 as crystal aggregates along foliation planes also at 338, possibly tourmaline as amorphous thin singers roughly parallel to foliation plane. Foliation at 336 feet 80 degrees to core axis. Lower contact sharp at 80 degrees to core axis, parallel to foliation of both units, slightly masked by quartz calcite veinlet ,9 2, MAFIC DIKE Fine-grained to medium-grained, massive, to foliated near contacts dark greenish grey, magnetic contains about 34 fine-grained, disseminated magnetite and about 34 randomly orientated calcite veinlets local light green zone lower contact sharp at 80 degrees to core axis, parallel to foliation of both units partially masked by calcite veinlets MAFIC TO INTERMEDIATE TUFF Similar to to 343.4, Lower contact sharp at 30 degrees to core axis, parallel to foliation of both units i MAFIC DIKE Or tuff. Dark graenish grey, foliated fine-grained, with calcite and or quartz veinlets parallel to foliation especially within 2 inches of lower contact, with approximately 1* fine-grained disseminated pyrite Lower contact sharp, at 65 degrees to core axis, parallel to

11 Canreos Minerals (1930) Ltd. Pag8 HOLE NO From To Description Sample From To Length Au Au ppb oz/ton GRANTITIC DIKE Medium grained, massive to slightly foliated, light pink brownish, contains rounded dark grey quartz crystals up to one-third inch long. Hard, rare vuggy quartz and calcite veinlets ace disseminated fine-grained pyrite. Lower contact sharp at 80 degress to core axis, parallel to foliation of both units DIKE Mafic dike or tuff. Similar to or Lower contact sharp at 70 degrees to core axis, parallel to foliation of both units PORPHYRITIC DACITE Dark grey, foliated, medium-grained, with anslucent to white plagioclase crystals. Randomly orientated throughout local tourmaline crystals and pyrite and rare quartz calcite veinlets. Lower contact sharp at 80 degrees to core axis, parallel to foliation of both units MAFIC DIKE Similar to to, Lower contact sharp at 80 degrees to core axis. Parallel to foliation of both units PORPHYRITIC DACITE Similar to to O.8 Three-quarters inch wide quartz and calcite and tourmaline vein at parallel to foliation at 70 degrees to core axis lower contact sharp at 80 degrees to core axis. Parallel to foliation at 70 degrees to core axis MAFIC OIKE Or tuff. Similar to to Lower contact sharp at 70 degrees to core axis, parallel to foliation of both units PORPHYRITIC DACITE Similar to 338 to END OF HOLE 'C Feec of bw :2S'''i'j lef" in he's.

12 Canreos Minerals (1980) Ltd. Page HOLE NO. 87*4 Latitude.0 Dip Tests Property Jedburg 30 Departure.0 Depth Azimuth Dip Depth Azimuth Dip Area Brackin Township Elevation Location L60W, 44+66S Azimuth IS degrees Date Started Jan 21, 1987 ' Dip degrees Date Completed Jan 2 2, Logged by Dave Hullen Length Feet Core Size 8Q From To Description Semple From To Length Au ; Au ppb Oz/ton CASING INTERMEDIATE FELSIC LAPILLI TUFFS Songly foliated at 65 to 70 degrees to core axis. Weak lineation on foliation plane, also occasional kinking of foliation as near 47 feet, kinking degrees to core axis, 90 degrees to foliation. Lineation at 30 degrees to core axis of left of long axis to core ellipse looking downhole. Clasts are very setched, fairly siliceous, sericitic and occasionally quartz porphyritic. Clasts range from.5 to 10 cm, medium to light grey. Maix is dark grey green to green, somewhat granular, weakly chloritic, actinolitic sericitic and occasionally flecked with biotite. Also rare quaz eyes. Weakly to moderately calcitic Cm wide zone with irregular ankerite clots, Cm quartz vein in short broken core section, with orthoclase fractures. Quite chloritic within 6 inches of lower contact MAFIC DIKE Passive, dark green, fine-grained margin, grades into coarse-grained amphibolide spotted interior. Upper contact songly foliated at 45 degrees to core axis, chloritic with quartz veining, possibly fault contact. Lower contact at BO degrees to core axis. fa f l INTERMEDIATE FELSIC UNIT Fine-grained, songly foliated at 30 degrees to core axis, siliceous sariciti:ed. No good evidence of clastic texture prominent in previous section. Light to medium gray, initially quite dark next to dike. 33TS blue opalescent quartz ey?. Lower contact broken. 3! FELSIC INTRUSION ^uite darn jrey green ''n colour, unusua" granular texture ,0 33. G ".O t? n /-

13 Canreos Minerals (1930) Ltd. HOLE NO. Page 87-4 From To Description- Quartz porphyritic, chloritic weakly ankeritic Narrow quartz vein with ace pyrite, chalcopyrite to 88.4 quartz vein with calcite, ankerite and tourmaline calcite at upper marginn, tourmaline at lower. Vague lower contact. Sample From To Length Au Au ppb Oz/ton INTERMEDIATE FELSIC UNIT Weakly foliated at 60 to 65 degrees to core axis. Siliceous, sericitic, fine-grained light to medium grey Cm quartz vein with tourmaline, ace ankerite to songly foliated zone at 40 degrees to core axis Quartz vein with orangy hematitic stain plus ace tourmaline Quartz chlorite calcite ankerite vein marking a possible fault, chlorite occurs as fractures in quartz vein MAFIC DIKE Dark green, fine-grained. Contact difficult to see due to drill grease on core. Lower contact sharp at 50 degrees to core axis INTERMEDIATE FELSIC UNIT Intermediate unit. Very dark grey green, chloritic, quartz porphyritic plus unusual textured zone with ankerite and calcite rhombs MAFIC DIKE Dark green, fine-grained, weakly foliated at 60 degrees to core axis. Chlorite spotting is partly elongated parallel to foliation. Songly calcitic Cm quartz calcite vein with tourmaline at lower contact. Lower contact at 70 degrees to core axis INTERMEDIATE FELSIC UNIT Light to medium grey, foliated at 50 degrees to core axis, i^'nor kinking of foliation. Pink hernatitic stain adjacsnt to quartz vein with tourmaline and biotite at lower contact. J FELSIC INTRUSION Massive, medium grey, fine to medium-grained, weakly ^oliated at 75 degrees to core axis. Cutting by quart: tourmaline vein at to 129.D. Weakly calcitic '30.9 '32.1 WIC DIKE

14 Canreos Minerals (1980) Ltd. HOLE NO. 87*4 From TO Description- Sample From To Length Foliation weakly Granulated Inch felsic dike. Au ppb Au oz/ton ' 35.2 FELSIC INTRUSION Massive, uniform, fine to medium-grained. Weakly quartz porphyritic, more abundant near contact MAFIC INTRUSION Dark green, fine-grained initially, chloritic, foliated to 140 feet adjacent to quartz calcite veins at to Possible shear zone, foliated at 50 degrees to core axis shallowing to 30 degrees to core axis next to veins, veins contain ace pyrite and tourmaline. Spotted texture elongated in foliated zone. Contains minor opalescent blue quartz eyes Calcite patch. Uniform downhole to Fault zone, songly, calcitic, biotitic. Cutting by quartz veins with kinked biotite, calcite, ace ankerite, minor broken core on both sides of fault. Becoming finer grained and foliated at 70 degrees to core axis near 218, foliation is in part crenulated fl! INTERMEDIATE FELSIC UNIT Quite massive looking to 267. Weakly foliated at 70 degrees to core axis. Moderate pervasive calcite alteration, weakly ankeritic. Light to medium grey, siliceous, weakly sericitic. Cutting by several irregular quartz veins in section to Vein near with 2 \ p yrite. Narrow epidote patch near Chlorite speckled zone to Narrow quartz vein running subparallel to core axis, ace tourmaline. Tuffaceous texture evident after Also unit becoming darker green and weakly chloritic Thin pyrrhotite seam CHERT MAGNETIC SULPHIDE IRON FORMATION Alternating bands of glassy chert, magnetite 0.1 to 5 cm thick. Banding at 55 degrees to core axis. Sulphide rich section with 5 to 10 \ w isps, seams and singers of pyr"hotite, miner pyrite Chalcopyrite seam. Weakly calcitic, sca chlorite. Seme magnetite is speckled and partly altered to grunerite C :S7.' INTERMEDIATE -ELSIC UN P

15 Canreos Minerals (1980) Ltd. HOLE NO From To Description- Si! icified baked, moderately sericitic. Cut by calcite fractures. Lower contact broken. Sample From To Length Au Au ppb oz/ton DIABASE DIKE Massive, dark grey, uniform, weakly magnetic. Irregular contacts FELSIC INTERMEDIATE UNIT Quite siliceous, moderately feldspar porphyritic, quartz porphyritic. Pink tinged, foliated at 60 degrees to core axis DIABASE DIKE As above, with waxy green feldspar et lower contact. Lower contact sharp at 60 degrees to core axis FELSIC INTERMEDIATE LAPILLI UNIT Medium grey to light yellowy grey. Silicified, moderately sericitic, moderately foliated at 40 to 50 degrees to core axis. Songly foliated near ductile shear zones. Foliation at times contorted especially near shear zones. Clasts are setched parallel to foliation and often are feldspar porphyritic, with rare quartz eyes. Weakly calcitic plus cut by calcite fractures. Trace pyrite, pyrrhotite, some bleaching. Maix is flecked with biotite. Shear zones at 313.5, at degrees to core axis, songly sericitic. Folding evident at 326.5, 331. Fold axis at 70 degrees to core axis and at 70 degrees to foliation of 40 degrees to core axis DIABASE DIKE Dark grey to black, fine to medium-grained, uniform. Weakly calcitic fractures. Glomeroporphyritic over 0.5 feet at upper contact. Feldspars sericitized, waxy green, up to 2 cm in diameter FELSIC INTERMEDIATE TUFF Medium to dark grey to greenish gray. With lapilli sized felsic clasts setched parallel to moderate to song foliation at 70 to 30 degrees to core axis. Only weakly feldspar.and quartz porphyr ; tic. Rare blue quartz eyes. Minor thin xisps, seams of pyrrhjtit?, pyrite notably Jt to Quartz ve't *r, ^o'.vnc" ': oe, ca'c'"?, t-acs ankerite, pyrite at i : :3.5.5,4.1.0 ^i :

16 Canreos Minerals (1980) Ltd. Diamond On'11 Log HOLE NO Page 5 Frorn To Description to dark green foliated chloritic zone, quartz vein with singers of pyrite Quartz calcite chlorite patches. Finer grained towards end of hole. Clasts not as distinguishable as previously, possibly ash tuff. Still foliated at 70 degrees to core axis. Sample From To Length Au Au ppb oz/ton END OF HOLE

17 Canreos Minerals (1980) Ltd. HOLE NO. ' o 1, i uiue Departure Elevation.V ~~ ~ * IM J 'BMS ~. 0 Depth Azimuth Dip Depth Azimuth J3.0 Dip Property Are? Local ion; Jedburg 30 Brackin Toi* L52w 44*" Azimuth Dip Length 15 degrees degrees Feet D.ite Started Jan, 1937 Date Completed Jan, 1937 Loggo( Ijy pgyp Mil Core Siz*? 60 Prnm Tn Sample From To Length Au A" ppb or/to" CASING INTERMEDIATE FELSIC LAPILLI TUFFS Nell foliated banded st 65 degrees to core axis. Contains setched clasts of felsic volcanic and quartz felsic porphyry to 4 inches, light to medium grey. Maix i? d ark green to greenish g r ey. Wnakly act'nolitic, biolitic, occasional quartz phenocryst variable calcite alteration, weak to song. Although both boxes 2 and 3 were spilled and are totally jumbled, attempted reconstuction suggests this unit becomes dark green in colour. Chloritic towards lower contact. Lower contact assumed to be marked by 2 inch quartz calcite chlorite vein with ace pyrite, tourmaline cbout 33 feet t r MAFIC INTRUSION All core from this unit is jumbled. Unit is green medium-grained with a spotted granular texture while close to its contact finer grained material predominated chilled margins. Cut by calcite veins with weak pink hematitic tinge INTERMEDIATE FELSIC LAPILLI TUFFS Initially dark green, weakly biotitic. Grades into lighter grey sericitized tuff, ace, pyrite, tourmaline INTERMEDIATE FELSIC UNIT Relatively massive, uniform fine to medium-grained, granular. Weakly quartz porphyritic. Initially dark grey and weakly feldspar pyritic but grades into lighter grey pink rock to 97.5 rose coloured alteration patch with calcite, chlorite, possible k feldspar to 97.7 chlorite zone with \ \ p yrite to 99.6 dark green moderately calcitic banded chloritized zone, altered inclusion of intermediate felsic unit. Larger quartz eyes towards lower connet ,

18 Canreos Minerals (19HO) 1 1''. id Drill Log HOLE NO. From Tc Description.Sample Frofr To Length AM ?1.9 INTERMEDIATE FFJ.5IC LAPILLI TUFFS Massive, indium grey with faint pink ting^ Medium-grained, granular. Quartz porphyritic with phencrysts to 5 mm, Trace pyrite weakly chlorite. Flecks of biotite towards lower contact MAFIC INTRUSION Contact songly calcitic, biotitic over 0.5 feet. Foliated at 75 degrees to core axis. Unit is generally massive, medium to coarse-grained. Dark green, often or amphibolite spotted. Weakly calcitic decreasing downhole to moderately foliated zone sheared cened ankerite quartz vein with ace ankerite at 128 to 128.3, zone is chloritic, weakly biotitic with ace pyrite. And foliated at 60 degrees to core axis A few narrow quartz epidote veins Foliated zone sheared at 50 degrees to core axis, contain? quartz, sericite, chlorite, calcite and tourmaline, foliation is crenulated at Mafic away from sheared zone developing a weak foliation at 50 degrees to core axis and becoming sericitized downhole Narrow fine-grained sheared zone at 80 degrees to core axis INTERMEDIATE FELSIC UNIT Very blocky and partly weathered core. Possibly lapilli tuff Light grey, sericitized, moderately, calcitic. Songly foliated at 80 to 90 degrees to core axis, good lineation developed on foliation plane pitching to right side of core axis at 30 degrees to long axis of core ellipse looking downhole. Cut by several irregular quartz calcite veins, ace pyrite. Becoming weakly chlorite and dark green after 2. Accompanied by rare thin seam of pyrite, pyrrhotite ? CHERT MAGNETIC SULPHIDE IRON FORMATION Very glassy cho rt band? to 0.5 cm interlayered with?p?ckl?r) magnetite bands cut by irregular singers and seams of pyrrhotite, pyrite. Banded st 55 to 75 degree? to core axis. 5^ Total sulphide, predominantly pyrrhotite. Weakly chloritic, possibly minor grunerite. Cut by quartz veins core magnetite at to and to fi ??, INTERMEDIATE r f l.?'.c Initially light cieaniy groy, sericitized ,9 M

19 Canreos Minerals (1980) ltd. p*'3l? HOLF NO. 37-*; r rom To - Description Sample From To Length Au S'i ppb o.-./t'."- Foliated at 80 degrees to core ax.i?. Fine-grained, weakly quartz pocphyritic. Grade into dark grey green material near 250 feet. Colour changes also accompanied by increase in pervasive calcite alteration. Opalescent blue quartz eyes and garnet porphyroblast? now evident. Box to 277 was spilled and core is jumbled, pieces were found in box to 49, lots of missing core, approximately!5 to ^. Partial reconsuction indicates garnetiferous dark green intermediate to Felsic Lapilli Tuffs with blue opalescent quartz eyes and less than H wisp? of pyrrhotite, pyrite from 25? to 262. Rest of unit is sericitized and siliceous. Lower contact missing. Arbritarily set at MAFIC INTRUSION Reconsucted core for initial 6 feet Fine-grained near upper contact. Medium to dark green, coarser gnd towards cene of dike. Chlorite, moderately calcitic. Moderately foliated at 50 degrees to core axis. Lower contact biotitic and marked by quartz vein with ace ankerite INTERMEDIATE FELSIC UNIT Medium grey lo greenish grey, weakly quartz porphyritic. Foliated banded at 70 degrees to core axis. Rare thin seams of pyrite, pyrrhotite, very siliceous, moderately sericitic, weakly chlorite, biotitic. Trace tourmaline END OF HOLE

20 Canreos Minerals (1980) Ltd. HOLE NO. Page 87^6 LSI uuub Departure Elevation.u.0.0 Depth Azimuth Dip Depth Azimuth Dip Property Area Location Brackin Township L44W Azimuth Dip Length 45 degrees degrees Feet y Date Started Jan 17, 1S87 Date Completed Jan; 19, 1987 Logged by Dave Mullen Core Size 3Q Prnm Tn Sample From To Length Au Au ppb dz/ton.0 21.O CASING- 21.O 55.5 INTERMEDIATE FELSIC LAPILLI TUFFS Well banded, foliated at 70 degrees to core axis. Alternating medium to dark grey, bands { maix ) and light creamy grey siliceous bands ( setched clasts ). Weakly to moderately calcitic, sericite. A few zones with scattered pink garnets to 3 mm. Maix contains flecks of biotite, minor feldspar and ace pyrite Cm quartz vein with ace pyrite, chlorite and ankerite DIABASE DIKE Dark grey, fins-grained. Weakly magnetic, calcitic. Sharp upper contact at 35 degrees to core axis. Lower contact at 25 degrees to core axis INTERMEDIATE FELSIC LAPILLI TUFFS Weakly foliated at 70 to 75 degrees to core axis. Quartz eyes near lower contact. Moderate to weak pervasive calcite alteration FELSIC DIKE Contact not sharp. Massive, fine-grained, flecked with biotite. Minor quartz eyes to 3 mm. Narrow weakly foliated zones at 55 degrees to core axis to 89.3 quartz vein somewhat glassy, devoid of sulphide INTERMEDIATE TUFF Alternating light to dark grey bands at 65 degrees to core axis. Moderately calcitic, more abundant iear upper contjct. Weakly developed Tineation on Foliation plane at 40 degrees to right of long axis of core ellipse looking downhole '01.0 Quartz tourmaline calcite vein. Abundan: ban-is o : black tourmaline adjacent to lower contact wo He calcite cornmom -it jpper connet. 10 Cd *i*je i-3i'k jresn chloritic weakly actir.olitic zones next to ,.0.3 ft. n ,.0 103, ,.3 103, j.2 i ft** f J407 ia."/,. J 165, i ,. -1 ;0! 6,. -J ,.7 1C3,.2 i.s l i 1.5

21 Cenreos Minerals (1980) Ltd. HOLE NO From To Descriptionvein. 102 Pink feldspathic fracturing Quartz tourmaline calcite vein, ace ankerite and sericite again tourmaline occurs at lower contact, calcite at upper contact Quartz veined zone with 15 finely disseminated pyrite and clots of cnlorite Quartz vein with inclusion of buff colored sen'citized material. Sen'citized and somewhat silicified margins Minor fold. ; Sample From To Length Au Au ppb oz/ton MAFIC DIKE Medium green, fine-grained somewhat granular, weakly chloritic. Songly calcitic weakly foliated at 55 to 70 degrees to core axis. Trace pyrite INTERMEDIATE FELSIC UNIT Possible tuff (? ) not as well banded as previously. More massive looking. Medium grey to grey green, weakly sericitized. Some silicification next to rare quartz vein. Minor disseminated tourmaline especially near Dark green with chlorite slips from 127 to lower contact. Garnetiferous from 129 feet. Garnet porphyroblasts are buff pink in calcite, up to 2 mm, Chlorite zone cut by rare quartz calcite veins. Some veins appears boudinaged. Minor small quartz and possibly feldspar phenocrysts. Trace wisps of pyrite especially Irregular quartz vein with ace pyrite at lower contact MAFIC INTRUSION Massive, dark green, fine to medium-grained. Song pervasive calcite alteration. Chloritic, biotitic, minor magnetite, ace pyrite. Rare blue opaiescant quartz eyes. Kteakly foliated at 70 degrees to core axis. Chlorite spotting from 145 to to 153,5 songly foliated zone ( shear ) at 30 to 35 degrees to core axis, finer grained. Chloritic, margins of zone are quartz calcite veined, part of cilorite ipcttsc fabric still evident in sheared zone. Heak lineation developed on shyar plane normal to long axis of core ellipse. 163,5 to 169 foliated banded zone by ankerite calcite quartz vns at 154 to , '57.: 163.5, 167 :57.;, ' Ending 5: 30 degrees to ccra 3 x i s, ace pyrite, molybdenite J to

22 Canreos Minerals (1980) Ltd. Page HOLE NO From To Description Sample From To Length Au Au ppb oz/ton , quartz veined zone with ace pyrite, pyrrhotite, chalcopyrite, tourmaline Crenulatad zone Some epidote and folding Chlorite spotted zones INTERMEDIATE FELSIC TUFF Well banded { foliated ) at 75 degrees to core axis. Medium to dark grey to greenish grey with lighter grey bleached somewhat silicified zones. Rare thin seams and disseminations of pyrite. Sericitized, weakly chloritic. Moderately to songly calcitic. Becoming weakly garnetiferous towards lower contact. Rare quartz eyes MAFIC DIKE Dark green, fine-grained, granular towards lower contact. Foliated at 65 degrees to core axis. Songly calcitic, moderately chloritic, ace pyrite. Cut by occasional quartz calcite veins CHERT MAGNETIC SULPHIDE IRON FORMATION Interlayered white to medium grey chert, magnetite and pyrrhotite, ace pyrite. Minor ankerite present as well. Approximately 10^ sulphide over entire unit but pyrrhotite most abundant in zones at 250 to to to Sulphide seams are more irregular than chert or magnetite generally at 80 degrees to core axis. Except for tight isoclinal folding at 249.6, Minor green chlorite and possibly grunerite. Foliated, sericitized zone at to INTERMEDIATE FELSIC UNIT (TUFF?) Well foliated at 70 degrees to core axis Initially light creamy gray, songly sericitized gradational into medium to dark grey unit Some darker sections are garnetiferous especially 275 to Garnets are sometimes quite ragged looking. Scattered quartz eyes include a blue opalescent variety. Minor pyrite wisps, less than U. Weathered zona at 274 feet. Quartz veins at 231 to 281.4, to 283.4, to 235.4, to quartz is milky white with minor grey patches, ace ankerite, less than i* pyrite, pyrrhotite, minor sericite and chlorite. Intermediate unit is scngly quartz porphyritic next to above Quartz :one. c? i-., ^7 s ---a* ; ;:ur y nissing core, sec t-'on is very blocky or

23 Canreos Minerals (1980) Ltd. Page HOLE NO l From To Description- tag 307 nrisslabelled, 302 feet. Sample From To Length Au Au ppb oz/ton MAFIC DIKE D-ark green, granular, massive. Songly calcitic, vague contacts. S INTERMEDIATE FELSIC UNIT Fairly siliceous, sericitic, fine-grained. Initially quartz porphyritic with blue opalescent quartz eyes to S mm Medium grey initially, darker grey downhole. Foliatad at 80 degrees to core axis to quartz vein with sericitic margins to 338 quartz veined silicified section with black tourmaline, ankerite and sericite. Rare garnet to 3 mm. Weakly to moderately calcitic. Trace, wisps, seams of pyrite pyrrhotite. Dark green zones are possibly dikes. 355 Poikiloplastic garnets up to 7 mm with quartz inclusions in chlorite patch. Silicified from 357 possibly setched felsic fragments ( lapilli tuff? ) to pyritic zone, 5t, wisps and seams, minor pyrrhotite Trace tourmaline Mafic dike (? ) vague contacts, dark, green, granular moderately pervasive calcite alteration. Lower contact broken DIABASE DIKE Broken contact. Dark g^ey, fine-grained, massive INTERMEDIATE FELSIC UNIT Fairly massive, not as banded, foliated, as previously. Still with blue opalescent quartz eyes. Variable in calcite from light to dark grey. Silicified, sericitized. 403 to fins-grained diabase or mafic (? ) upper contact. narked by quartz calcite vein to feldspar porphyritic zone ( dike ). Care becoming dark cowards end of hole. Still quite silicified. Foi'atsd at 30 degrees to core axis wich weak lineation at degrees to long axis of core ellipse. i:7.3 1:7.3 End of hole.

24 Canreos Minerals (1980) Ltd, HOLE NO tai. i(.uue Departure Elevation.u.0.0 Depth Azimuth Dip Depth Azimuth Dip Property Area Location Jedburg 30 Brackin Township L96W, 3+50S Azimuth Dip Length 45 degrees degrees Feet i/ Date Started Jan 25, 1987 Date Completed Jan 27, 1987 Logged by i Roberta Bald Core Size BQ Frnoi Tn Sample From To Length Au Au ppb oz/ton OVERBURDEN Casing to 12 feet PORPHYRITIC DACITE From 5.9 to 16.2 feet mainly quartz phyric with about 151 slightly blueish quartz phenocrysts up to one-quarter inch diameter in dark gray fine-grained maix, generally massive from 9.3 to 9.9 calcite and epidote veinlets ac 60 degrees to core axis containing Hi fine-grained pyrite. From 10.9 to 11.3 feet zone of red alteration associated with quartz and chlorite vein, irregular. From 16.2 to 112 quartz and plagioclase phyric, contact gradational similar quartz phenocrysts but locally up to one-third inch diameter plagioclase phenocrysts slightly greenish up to one-quarter inch long, euhedral, locally zoned. Randomly oriented local fine-grained slightly foliated zones, possibly tuff beds or slightly sheared zones at 70 degrees to core axis. From 28.4 to 29.8 white coarse-grained quartz vein, broken core no sulphides seen slightly red alteration within 1 inch of vein margin. Quartz vein at 46, vein less than 1 inch wide no sulphides seen. From 50.5 to 51 zone of sericite and red alteration along margins of vuggy quartz vein, less than 1 inch wide and dark green, massive ' chlorite no sulphides seen. From 57,6 to 57.8 irregular quartz vein coarse-grained anslucent. to white quartz, no sulphides seen. From 60.6 to 60.9 zone of quartz veinlets with pyrite singers, approximately 2*. Local quartz and or calcite veinlets, locally with red alteration and locally vuggy. From 96.9 to 97.2 and 97,9 to 98.2 and 98.5 to 98.9 zones of green epidote and quartz, locally with calcite no sulphides seen. Blocky core. Lower contact sharp at 50 degrees to core axis DIABASE F''ne-'jraineQ, massive dark grey Co black, locally plagioclase phyric local zones of.apple green epidote alteration from 112 to and 114.' to with associated quart: veining loc^l narrower zones. Non-magnet "'c. Lower contact ;Haro -at 55 deirees to core axis ,6 13

25 Canreos Minerals (1980) Ltd. Page HOLE NO. 874? From To Description Sample From T6 Length Au Au ppb dz/ton PORPHYRITIC DACITE Similar to 16.2 to 112 but dark grey, baked by diabase dike, local green epidote and chlorite and quartz veinlets at approximately 121. Lower contact sharp at 70 degrees to core axis DIABASE Magnetic, black, fine-grained from upper contact to approximately 127 feet, containing greenish plagioclase phenocrysts, becoming medium-grained, then coarse-grained with dark mafic minerals interstitial to plagioclase lath shaped crystals, randomly oriented blocky core. Locally plagioclase phenocrysts up to one-half inch long, porphyritic Becoming fine-grained from feet to lower contact. Lower contact sharp at approximately 90 degrees to core axis, slightly irregular INTERMEDIATE TUFF Inhomogeneous dark grey with variable amounts of white to greenish spots, plagioclase crystals plagioclase phenocrysts are euhedral to rounded, up to one-quarter inch long occurs from less than 1* to locally 25^ unit also contains about U evenly disibuted blueish quartz crystals up to one-tenth inch in diameter rounded unit is cut by locally up to * thin epidote plus or minus calcite plus or minus quartz veinlets, less than one-quarter inch wide, randomly oriented. From to thin diabase dikelet, irregular, magnetic fine-grained, bleached, up to 2 inches wide. F n om to coarse-grained white quartz vein with dark green chlorite and salmon coloured feldspar no sulphides seen irregular vain. Local possible fine-grained to medium-grained, black tourmaline needle-like crystals in local light greenish, narrow zones, possible epidote alteration zones.,i,;.--, v Locally, unit contains dark green to iaatksr randomly oriented amphibole crystals, blades. Lower contact sharp at approximately 55 degrees to core axis but irregular and broken MAFIC DIKE Upper contact and lower contact chilled ageinst intermediate tuff. Fine-grained, dark green, massive with up to approximately 5ii calcite veinlets, randomly oriented. Lower contact at low angle to core axis from to irregular i INTERMEDIATE TUF- Sitfilar to Ci4.9 to

26 Canreos Minerals (1930) Ltd. HOLE NO Page 3 From To Descriptiori- At 85 to 90 degrees to core axis. Lower contact ground. Sample From Td Length Au Au ppb oz/ton GA88RO Slightly chilled upper contact. Medium-grained to coarse-grained amphibole-rich, massive to locally foliation inusive rock dark green with interstitial white plagioclase crystals. Local quartz and calcite and chlorite veins containing up to approximately 5% fine-grained to coarse-grained disseminated pyrite at at at to from to 343.8, less than one-half inch wide, at 10 to 15 degrees to core axis. Unit locally contains less than H fine-grained to medium-grained disseminated pyrite. From 346 to 347 feet, unit becoming fine-grained to 355 feet, then becoming medium-grained. Local quartz and calcite and pyrite zones feet to to to with 3 inch wide foliated section at 50 degrees to core axis to vuggy at 385 no sulphides seen to no sulphides seen up to 5* fine-grained to coarse-grained pyrite. From approximately 364 to feet unit contains white, hard, wispy minerals, parallel to foliation, possible plagioclase crystals foliation at 80 degrees to core axis. Lower contact becoming fine-grained within last foot, appears sharp but possibly ground , c t INTERMEDIATE LAPILLI TUFF Dark grey, fine-grained maix containing plagioclase and quartz phyric fragments up to one and one-half inches wide inhorcogeneous unit massive fe- With local green epidote veinlets plus or minus quartz. Pink salmon alteration with pyrite singers from to feet From approximately 412 feet to lower contact, fragments are difficult to see, unit is possible silicified, foliated at approximately 80 to 90 degrees to core axis. Quartz vein from to with silicified host rock along vein margins and and fine-grained to medium-grained pyrite as disseminated crystals and singers from approximately to up to approximately l \ f ine-grained disseminated pyrite locally, and local silicified zones with grey carbonate veinlets. Lower contact slightly gr-adational over one-quarter inch, marked by colour change, parallel to foliation of next unit at 60 degrees to core axis !8.4 4i GA88RO r ine-'jrained, dark gregn, foliated unit at both upper contact and lower contact from 1C2.5 to 421 feat and to 1-14,2. Sharp connet? -nth "^st of unit w h''c h -'s isdnim-grained to coarse-grained, dark green and whit-j, niassive randomly oriented ;JPI/ jr e ;-i."'c"11":o'-;, ic* 1'-'?"it? 3cv! *hi'9.j'ag'oclase crystal-? !4077 i

27 Canreos Minerals (1980) Ltd. HOLE NO. Page 87-7 From To Description- Sample From To with.ninor local quartz crystals. Unit contains quartz veins from and containing carbonate, aca pyrite, possible tourmaline and minor chlorite quartz is anslucent to milky white. From to grey to anslucent quartz core carbonate and chlorite and possible minor tourmaline no sulphides seen. Both quartz veins are at approximately 50 to 60 degrees to core axis. Lower contact ground. Length Au Au ppb oz/ton INTERMEDIATE LAPILLI TUFF Similar to 396 to but very few fragments seen inhomogeneous, dark grey, massive unit. Lower contact sharp at 80 degrees to core axis, parallel to foliation of next unit MAFIC DIKE Similar to to 424. Containing about 14 fine-grained pyrite as disseminated crystals and short singers. Lower contact sharp at 80 degrees to core axis, parallel to upper contact INTERMEDIATE LAPILLI TUFF Similar to to Lower contact sharp at 80 degrees to core axis MAFIC DIKE Similar to to 463. Lower contact sharp at 80 degrees to core axis INTERMEDIATE LAPILLI TUFF Similar to to feat. Slightly silicized from to with approximately 14 fine-grained disseminated pyrite END OF HOLE 12 Feet of bw casing left in hole.

28 ' Canreos Minerals (1980) Ltd. Page HOLE NO. 87*8 Latitude.0 Dip Tests Property Jedburg 30 Departure.0 Depth Azimuth Dip Depth Azimuth Dip Area Brackin Township Elevation Location L96W, 7+CON ; : Azimuth 45 degrees Date Started Jan 29, 1987 Dip degrees Date Completed Jan 30, 1987 Length j Feet J Logged by Core Size Roberta Bald 8Q From To Description Sample From To Length Au Au ppb Oz/ton OVERBURDEN Casing to 12 feet INTERMEDIATE TUFF : Dark grey to locally greenish grey, massive to slightly foliated, ,0 5 inhomogeneous, medium-grained tuff no definite fragments seen fine-grained, chloritic to sericite maix core from approximately li to 151 milky white, hard euhedral to anhedral rounded plagioclase phenocrysts, no bedding or banding seen ace fine-grained blueish quartz crystals ace to locally 1i pyrite throughout, as disseminated crystals and short singers, rare pyrrhotite near 38 feet as one-tenth inch wide singer, with pyrite sulphide singers generally roughly parallel to foliation at 38 feet 80 degrees to core axis. Local sericite rich zones less than 1 inch wide. Lower contact sharp at 75 degrees to core axis, parallel to foliation of next unit MAFIC DIKE Dark green, fine-grained, foliated chlorite rich mafic material, core Si calcite veinlets, parallel to foliation, and 1i disseminated pyrite. Lower contact sharp, parallel to upper contact INTERMEDIATE TUF : Similar to 9.6 to 59.2, possibly core calcite. Lower contact sharp, at 35 to 40 degrees to core axis, parallel to foliation of next unit MAFIC DIKE Similar to 59.2 to Quart: and calcite vs''n *'rom 50 to 50.4, paralls 1 to upper contact and foliation of unit, ue width 3 inches, with approximately li pyrite as singers in host rock along vein margin and massive. dark green chlorite in host rock near vein Tiargins, locally associated with pyrite, fine-grained crystal aggregates, locally as large ireas filling in between the massive chlorite. L:wer ccnccc: sharp, at approximate 1 ^1 30 degrees to ':ore axis, r.r*." z' ~- f: i " -. c ion sf botn 'jnits.

29 Canreos Minerals (1980) Ltd. HOLE NO. Page 87r8 From To Description-- Sample From To Length Au Au ppb oz/ton INTERMEDIATE TUFF Similar to 9.5 to 59.2 from upper contact to approximately 62.5 feet, gradational contact. From 52.6 to 67.9 becomes fine-grained, without plagioclase phenocrysts and containing wispy chlorite rich mafic fragments setched parallel to foliation at 70 degrees to core axis at 63 feet Lower contact sharp at 80 to 85 degrees to core axis, cross-cuts foliation of next unit LAMPROPHYRE DIKE Very foliated at 75 degrees to core axis. Consists of alternating thin lenses of dark brown biotite aggregates and white carbonate. Lower contact sharp at 75 degrees to core axis, parallel to foliation of lamprophyre INTERMEDIATE TUFF Upper contact slightly bleached Similar to 9.6 to At about 74 feet, three thin mafic dikelets, parallel to each other less than 1 inch wide. At 74.9 to 80.2 unit contains about 15 to \ p lagioclase phenocrysts, possible crystal tuff bedded within approximately 3 inches of lower contact, unit is khaki coloured. Possibly silicified. Lower contact irregular khaki material appears to locally cross-cut next unit. ; MAFIC DIKE Similar to 59.2 to 59.5 but locally medium-grained, massive. Lower contact irregular but generally at 50 degrees to core axis. Either contact is drag folded or shows soft sediment deformation. ; INTERMEDIATE TUFF Similar to 9.6 to ,7 5 From 37.7 to 95 more quartz and plagioclase crystals than i est of unit quart! crystals up to one-quarter inch diameter, blueish sericite rich :one from 94.3 to 95 and unit takes on quartz eyes ssricits schis: texture. Sharp contact at 95 feet. Local red pink alteration at 95 feet. Increase in quartz and plagioclase crystals within 1.5 feet of lower contact. Lsiner contact sharp ^c 90'Degrees to core ixis. 'O*.5 '03.9 'lafic "IKS ".:is* '"' " '02 3 ';i 5

30 Canreos Minerals (1980) Ltd. HOLE NO. 87*8 From To Description Sample From To Length Au Au ppb oz/ton Dark to medium grey, fine-grained along margins to medium-grained, massive, with approximately 5* white carbonate veinlets. Unit contains approximately 2^ fine-grained disseminated pyrite. Unit locally slightly greenish. Lower contact sharp at 80 degrees to core axis INTERMEDIATE TUFF Similar to 37.7 to Local red pink alteration at approximately feet to feet. Lower contact ground MAFIC DIKE Similar to to feet with fine-grained to medium-grained pyrite. Lower contact sharp but slightly irregular at approximately 90 dsgraes to core axis INTERMEDIATE TUFF From upper contact to about 118, similar to 87.7 to 95 with gradational lower contact. From 118 to lower contact similar to 9.5 to 59,2. At approximately 3 inches zone of red alteration with irregular veinlet of tourmaline crystal aggregates needle-shaped crystals no sulphides seen. From to 1.4 zone of quartz, calcite and red alteration with sericite patches variable directions ace fine-grained pyrite. Lower contact sharp at approximately 80 degrees to core axis, slightly masked by quartz and calcite veinlets MAFIC DIKE Similar to to Lower contact sharp ac 50 degrees to core axis INTERMEDIATE TUFF Similar to 9.6 to Lower contact sharp at 55 degrees to core axis, somewhat irregular. Parallel to foliation of next unit MAFIC OIKE Similar to 59,2 to Lower contact sharp at 15 degrees to core axis, parallel to foliation INTERMEDIA^ TUFF Similar to 9.5 to Lower contact sharp but irregular.

31 Canreos Minerals (1980) Ltd. HOLE NO. Pags 87-8 From To Description- Sample From To Length MAFIC DIKE Similar to to fine-grained. Lower contact sharp but irregular. Au ppb Au Oz/ton INTERMEDIATE TUFF Similar to 9.6 to 59.2 feet with possible fragments. Core massive, dark green chlorite aggregates. Lower contact ground and irregular, sharp MAFIC DIKE Similar to to irregular contact grey to anslucent coarse-grained quartz veins at 135.1, 1 inch to with calcite and massive biotite and chlorite aggregates ace pyrite 142 to with chlorite and ace pyrite. Lower contact masked by quartz vein INTERMEDIATE TUFF Similar to 9.6 to Local rare sericite bleached zones. From to about 5i calcite threadlike veinlets and red alteration ace pyrite, local chlorite and calcite veinlet amount of pyrite, as disseminated fine-grained to medium-grained crystals, increasing slightly within approximately 2 feet of lower contact. Lower contact sharp at 55 degrees to core axis, parallel to foliation of next unit MAFIC DIKE Similar to to Lower contact sharp at degrees to core axis INTERMEDIATE TUFF Similar to 9.5 to 59.2 feet with zone of mafic dike near possible mafic dike cutting core at low angles. Lower contact 90 degrees to core axis, sharp MAFIC DIKE Similar to to fee: with dark chlorite wisps. Lower contact irregular, sharp INTERMEDIATE TUFF Sinilar to 9.5 to Quartz vein with massive, dark grgen chlorite at low angle to pan i lei to core axis from 2.5 tc ;eet with saiition alteration in last fsw inches. Lcca" Ijpill"' sized 'rvigments :o i3 76

32 Canreos Minerals (1380) Ltd. HOLE NO. Page 37-8 From To Description Sample From To Length MAFIC DIKE Similar to to but fine-grained and massive throughout and only ace pyrite. Local salmon-coloured threadlike veinlets, randomly oriented, possible potassium alteration. From 235 to 236 salmon alteration associated with calcite, sericite, chlorite and possibly tourmaline veinlets and masses. Quartz vein from to coarse-grained white to ansclucent quartz, contact at 70 degrees to core axis upper contact and 50 degrees to core axis lower contact. Contains local black inclusions, biotite rich no sulphides seen. Salmon alteration along lower margin for about 1 inch. Alteration zone from to feet similar to 235 to 236. Lower contact sharp at 45 degrees to core axis, parallel to foliation of next unit Au ppb Au oz/ton 255' INTERMEDIATE TUFF Similar to 9.6 to 59.2 but with large cream-coloured fragments locally core coarse-grained magnetite crystals. Lower contact sharp at 65 degrees to core axis, LAMPROPHYRE DIKE Similar to 67.9 to From to zone of quartz calcite chlorite veining no sulphides seen, Lower contact sharp at approximately 80 degrees to core axis INTERMEDIATE TUFF Similar to Lower contact sharp at 70 degrees to core axis GABBRO Fine-grained, chlorite rich, foliated material within 2 to 4 inches of contacts massive, medium-grained in cene dark green, with pale grey carbonate interstitial to amphiboles crystals local calcite veinlets, randomly oriented. Lower contact sharp approximately 85 to 90 degrees to core axis INTERMEDIATE TUFF Similar to 9.5 to Lower contact irregular but sharp MAFIC DIKE Similar to to Lower contact sharp at T0 degrees to :ore axis.

33 Canreos Minerals (1980) Ltd. HOLE NO Page 6 From To Description INTERMEDIATE TUFF Similar to 9.6 to 59.2 from upper contact to then gradational contact to fine-grained tuff with only minor zones core plagioclase and quartz phenocrysts. Lower contact sharp at 70 degrees to core axis, parallel to foliation of next unit. Sample From To Length Au Au ppb oz/ton GABBRO Similar to to but becoming medium-grained to coarse-grained in cene. Fins-grained from approximately 362 to lower contact. Lower contact sharp a; 30 degrees to core axis INTERMEDIATE TUFF Similar to 9.6 to 59.2 feet. Lower contact sharp at 50 degrsss to core axis MAFIC DIKE Similar to 362 to Lower contact sharp but core broken INTERMEDIATE TUFF Similar to 9.6 to 59.2 feet but about i plagioclase phenocrysts,. Appear lineated. Lower contact sharp at 90 degrees to core axis but slightly irregular DIABASE Fine-grained to medium-grained, massive, black, magnetic dike END OF HOLE 12 Feet of casing left in hole. ONTARIO ASStiSoMc MAYl FILE OSFICE 1997 krt RECEIVE D

34 Ontario Name and Minisy of Natural Resources Report of Work U) X- The Minin 42B85SW BRACKIN dress of Recorded Holder 900 CANRE^PMINERALS (1980) LIMITED Suite 1215, 111 Richmond St. West, Toronto,. Ontario M5H 2G4 Summary of Work Performance and Disibution of Credits Total Work Days Cr. claimed 573 for Performance of the following work. (Check one only) Q] Manual Work Qshaft Sinking Drifting or other Lateral Work. [^Compressed Air, other Power driven or mechanical equip. ^J Power Sipping gj Diamond or other Core drilling ^JLand Survey All the work was performed on Mining Claim(s):, , Required Information eg: type of equipment, Names, Addresses, etc. (See Table Below) Drill NO. l ONTARIO D: ill 19R7 EC E l VE J.T. Thomas Diamond Drilling Ltd* ^ P.O. BOX 944 R ECORDED Timmins, Ontario, P4N 7H5 ' K BQ Core JKS 300 Diamond Drill A*t John Deere 850SKidder N. Morissette l Station Road, P.O. Box 789 Haileybury, Ontario, POJ 1KO Longyear 38 Drill Clark Skidder BQ Core Receipt No.,te D!''. T), Certification Verifying Report of Work Date of Report April 21, 1987 l hereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work annpxed^iereto, nnexe having performed the work or witnessed same during and/or after its completion and the annexed report is ue. Name and Postal Address of Person Certifying J.E. McCombe, 78 Tenoga Drive Mississauga, Ontario, L5H 3K2 Table of Information/Attachments Required by the Mining Recorder Date Certified April 21, 1987 Type of Work Specific information per type Other information (Common to 2 or More types) Attachments Manual Work Shaft Sinking, Drifting or other Lateral Work Compressed air, other power driven or mechanical equip. Power Sipping Diamond or other core drilling Type of equipment Nil Type of equipment and amount expended. Note: Proof of actual cost must be submitted within 30 days of recording. Signed core log showing; footage, diameter of core, number and angles of holes. Names and addresses of men who performed manual work /operated equipment, together with dates and hours of employment. Names and addresses of owner or operator together with dates when drilling/sipping done. Work Sketch: these are required to show the location and extent of work in relation to the nearest claim post. Work Sketch (as above) in duplicate Land Survey Name and address of Ontario land surveyor. Nil Nil 768 ('ffr/j;

35 Ontario Minisy of Natural Resources Report of Work -73/3-7 The Mining Act Name and Pos^^Hldress of Recorded Holder JEDBURGH RESOURCES LIMITED, P.O. Box 960 Postal Station Q, Toronto, Ontario, M4T 2P1 Summary of Work Performance and Disibution of Credits Total Work Days Cr. claimed 2878 for Performance of the following work. {Check one only) Prefix Mining Claim Number see Work Days Cr. f~l Manual Work Qshaft Sinking Drifting or other Lateral Work. Q] Compressed Air, other Power driven or mechanical equip. L]Power Sipping j*j Diamond or other Core drilling LjLand Survey Schedule A Mining Claim Prefix Number Insuctions - Supply required data on a separate form for each type of work to be recorded (see table below). - For Geo-technical work use form no "Report of Work (Geological, Geophysical, Geochemical and Expenditures)". Work Days Cr. Prospectors Licence No. T-1496 Mining Claim Prefix Number All the work was performed on Mining Claim(s): , , , , , ~ Required Information eg: type of equipment, Names, Addresses, etc. (See Table Below) Drill No. l Drill No. 2.Z). Certification Verifying Report of Work J.T. Thomas Diamond Drilling Ltd. P.O. Box 944 Timmins, Ontario, P4N 7H5 jrecordeb BQ Core JKS 300 Diamond Drill John Deere 850 Skidder APR N. Morissette Receipt NO.. l Station Road, P.O. Box 789 Haileybury, Ontario, POJ 1KO Longyear 38 Drill. ;:r::wg D:V. Clark Skidder BQ Core \ 87-8 p-t A ir* /n April 21, 1987 Work Days Cr. Recorded Holder or/agent/ksignature 1 hereby certify that 1 have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is ue. S i Name and Postal Address of Person Certifying J. E. McCombe, 78 Tenoga Drive Mississauga, Ontario, L5H 3K2 Table of Information/Attachments Required by the Mining Recorder Type of Work Specific information per type Manual Work Shaft Sinking, Drifting or other Lateral Work Compressed air, other power driven or mechanical equip. Power Sipping Diamond or other core drilling Type of equipment Nil Type of equipment and amount expended. Note: Proof of actual cost must be submitted within 30 days of recording. Signed core log showing; footage, diameter of core, number and angles of holes. Names and addresses of men who derformed nual work/operated equipment! together ploymfnt. Names and addresses of owner or operator together with dates when drilling/sipping done. Work Sketch: these are required to (how the location and extent of work in relation to the nearest claim post. WOrk Sketch (as above) in duplicate Land Survey Name and address of Ontario land surveyor. Nil Nil 768 (81/3)