l/ ;; : '.';!':""' 86i4QV.i;:*, p l 1:'-. REPORT NO: 50

Transcription

1 p l :'-. DIAMND DRILLING se KAWASHE LAKE 00 l AREA:.Kawashe Lake WRK PERFRMED FR: ^^ Gold Canada Inc. ; ''. i RECRDED HLDER: SAME AS ABVE k J. REPRT N: 50 : THER [ J CLAIM N. HLE N. FTAGE DATE NTE ^ WMI* l/ ;; l MN MN m 28.0m June 986 June 986 (D (D 85090^ j ' MN m June, 986 (D l ^; : ', f; ; j ';.,;- ', ' MN m June 986 (D f-- -:85b9lo i;^ ; - MN m July 986 (D f; ". -'- ;,;^( J/.';-.. " ' ?!^ :'"-. : 86400'.';!':""' ;. MN m * July ' 986 (D f 86i4QV.i;:*, MN m July 986 (D NTE; ; (i) W903.0, filed in February 99

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5 NAME F M, r M o LAT,T,,D F PRPERTY MN L39+W EL E VAT IN STARTED Ju 23, 986 Muskeg Lakg^Property LENGTH 06.5m FPAPT.^F 0+25N onco 4co AZIMUTH ^u:j DIP * J F, M,,M,n J^e 24, 986 METERS m 50m 00m DIP 45" 45" 44 0 AZIMUTH FTAGE DIP AZIMUTH er/77 HLE NoMN SHEET N. R EMARKS No Pajar LGGED BY Angela Gasparetto CD to S i 8 o a m w 8 LANGfll CASING St VERBURDEN MAFIC TUFF (R METASEDIMENT) FELDSPAR PRPHYRY SUMMARY LG MAFIC VLCANICS, TUFFS, FINE-GRAINED FLWS FELDSPAR PRPHYRY BANDED VLCANIC (ALTERED) FELDSPAR PRPHYRY MAFIC VLCANICS (ALTERED) BANDED IRN FRMATIN AND ALTERED UNIT FELDSPAR PRPHYRY METASEDIMENT, MAFIC, ALTERED FELDSPAR PRPHYRY MAFIC VLCANIC (ALTERED, AMPHIBLITIC) MAFIC METASEDIMENTS: BANDED IRN FRMATIN, m MAFIC VLCANICS (FINE-GRAINED, AMPHIBLITIC) FELDSPAR DYKLET AND BLEACHED ZNE MAFIC VLCANICS, (FINE-GRAINED, BANDED) CHLRITE-CARBNATE SCHIST MAFIC FLW, (FINE-GRAINED, BANDED) J/j^^TX^;^,^^ ^fjc/r I^J/iCA^*^ *- N. SULPH IDES Mr.f-prppp TAL 74 K g "^ *- ^^ jjqt g** 3 e ^33 ASSAYS Z/N s: Ir ^ t7 i i ' ^ 3 ) ~ r * * Co Z/N C S ^ ^ M

6 NAME F HLE N. MN Muskeg Lake Property SHEET N. l f 9 M. H. SUIPM ICS THU T* l AU ASSAYS -. l 07 M 0* M S if i e g i ID 8 oc Z j CASING 6 VERBURDEN MAFIC TUFF (R METASEDIMENT): - dark green to black, very fine-grained with felsic carbonates. poorly 62" to Core Axis - slightly magnetic; minor magnetite throughout FELDSPAR PRPHYRY: - pink, medium-grained feldspar porphyry with sub to euhedral feldspar phenocrysts l-5mm in diameter - sericitic in sections, weak to moderate; in l-3mm bands with thin magnetite singers - l-z'fc pyrrhotite and ace epidote - weakly magnetic - Upper 35 0 to Core Axis - Lower 70" to Core Axis MAFIC TUFF (R METASEDIMENT): - as m with 3cm quartz-carbonate 48" to Core Lower Contact FELDSPAR PRPHYRY: - as m - intense sericite alteration, banded with magnetite^ chlorite, 36" to Core Axis from m at Lower Contact; with 2-3"fc disseminated pyrrhotite - Upper Contact indistinct due to ground core SERICITIC UNIT (probable mafic tuff): - pale grey, fine-grained, poorly bedded unit - 44" to Core Axis - moderately to songly sericitic in sections - slightly to moderately sheared, moderately carbonatized throughout - moderately magnetic - Z-3% disseminated pyrrhotite - minor magnetite MAFIC INTERMEDIATE TUFF: - pale green to green-grey, fine-grained, poorly bedded tuffaceouslooking unit, moderately carbonatized and sericitized - weakly sheared; minor talc

7 NAME F P.PQP.FP-TV Muskeg Lake Property M! P M MN SHEFT N 2 f 9 to to o R z C tu fi: i PRM occasional quartz-carbonate 40" to Core Axis - unit contains -2?S disseminated pyrite, minor magnetite, and is slightly magnetic throughout MAFIC INTERMEDIATE TIFF: - well bedded carbonaceous- chloritic tuff, green- grey in colour with 20% quartz-carbonate bands, 3-5cm in diameter - bedding and banding 52" to Core Axis - slightly sericitic throughout, moderately sericitic and songly carbonatized in patches, giving a "bleached" look to core - /6 pyrrhotite disseminated throughout - minor talc MAFIC TUFF: - dark green to green-black, poorly bedded, sheared unit moderately magnetic - fine-grained with 3-4"fc magnetite, # pyrrhotite MAFIC VLCANIC; FINE-GRAINED: - very fine-grained to aphanitic, light green volcanic, massive with occasional quartz-carbonate 48" to Core Axis - "bleached" look throughout (slight silicification?) QUARTZ VEIN: - Upper 54" to Core Axis - blue-grey quartz vein with pyrrhotite singers at both upper and lower contacts - minor pyrite MAFIC FINE-GRAINED VLCANIC: - as m QUARTZ VEINLETS IN FINE-GRAINED VLCANIC: - 2-6cm quartz 60" to Core Axis in a very fine-grained carbonate-sericite-rich tuffaceous green-grey volcanic - contacts of these blue-grey veinlets are sericite and pyrrhotiterich FINE-GRAINED MAFIC VLCANIC: - as m SAMPUE neterage "~"~ i SuT PH " MJQ.*^ rt*^-^. f. SUI.PH, ICS TRM TAl.26.4 Au ASSAYS T. Z, M I M

8 PIAJMND DRILL RECRD NAME F PRPERTY Muskeg Lake Property MLE N. MN SHEET N. 3 f 9 00 ( I i 0 cc. p s 8c oz FINE-GRAINED MAFIC VLCANIC: - dark green to medium green fine-grained volcanic with 0/6 quartz veinlets (f 65" to Core Axis - unit is slightly sericitic, with 4-5?^ pyrrhotite as singers and disseminated crystals - moderately magnetic FINE-GRAINED VLCANIC: - as m QUARTZ VEIN: - guartz vein from with very chloritic, pyrrhotite- ri eh contacts - Upper 67" to Core Axis - contacts have sericite-rich bands with minor epidote paralleling them MAFIC VLCANIC: - very fine-grained, dark to medium green volcanic with quartzcarbonate swirls and patches throughout - slightly sheared; ending 5 0 to Long Core Axis - -2/6 disseminated pyrrhotite, i-2% magnetite as tiny black singers haloing quartz-carbonate swirls - slightly magnetic MAFIC VLCANIC: - very fine-grained, dark green to black moderately to songly chloritic unit with minor quartz-carbonate banding (S 64" to Core Axis - slightly sheared FINE-GRAINED VLCANIC: - medium green, fine-grained poorly bedded volcanic with S-0% quartz-carbonate 64 0 to Core Axis - weakly to moderately magnetic, S-4% magnetite as tiny concordant singers along a second set of quartz-carbonate "wisps" ending 20 " to Core Axis as fracture fillings - 3a disseminated pyrrhotite, minor pyrite N t. SULPH ICS TAL AU ASSAYS 7 M.0 Z M

9 NAME F Muskeg Lake Property MLE N. MN SHEET N 4 f FINE-GRAINED VLCANIC: dark green to green-black fine-grained volcanic with ID-5% quartz carbonate 36 to Core Axis slightly sheared veining is "haloed" by singers of magnetite and pyrrhotite (totalling 5%); moderately magnetic minor talc FINE-GRAINED VLCANIC: fine-grained, light to medium green, slightly to moderately serici tized unit with minor quartz-carbonate 68 to Core Axis singers are intercalated with singers of pyrrhotite (2/0, magnetite (22), chlorite and sericite occasional small patches exhibiting 2mm feldspar phenocrysts ALTERED VLCANIC: fine to medium grained, light to medium green volcanic with 5% carbonate "clots" m quartz-feldspar dykelet Upper 44 to Core Axis, Lower 44, accompanied by singers of magnetite, pyrite, pyrrhotite and chlorite FELDSPAR PRPHYRY; exemely sericitized porphyry llm pale green, aphanitic to fine-grained sections grading in and out of recognizable medium-grained pinkish-green porphyry pale sericitic sections are moderately sheared - unit slightly magnetic - l-2% pyrrhotite, l-2% magnetite Upper 42 to Core Axis sericitically altered feldspar porphyry dyke pinkish-green feldspar porphyry - l-2% disseminated pyrite - weakly magnetic tiny l~2mm vugs are lined with reddish-brown limonite - pinkishgreen colour grades towards Lower Contact Lower Contact indistinct due to severe sericitic alteration of the volcanic, but is estimated Q 46 to Core Axis li SUIPH rots Hetefaje" AU ASSAYS or W oz M

10 NAME F ppopfrtv Muskeg Lake Property HLE N. MN SHEET N 5 of 9 M. J. SUIPM ICS rrou neterage TAL Au ASSAYS \! M Z W BANDED ALTERED VLCANIC: - fine-grained to aphanitic greenish-black to light green in patches with severe sericite alteration remnant banding can be seen but is obliterated in the severely altered sections - banding (quartz-carbonate) 56 to Core Axis - weak to moderate shearing - sericitic patches are moderately magnetic - 2-3% disseminated pyrrhotite, -2!? magnetite in tiny singers : Feldspar Porphyry - relatively unaltered pink medium-grained feldspar porphyry - l-2% disseminated pyrrhotite : Banded Altered Volcanic - as S e g o m Ul IGC FELDSPAR PRPHYRY: - pinkish-green, medium-grained - moderately sericitized throughout - lmm-4mm euhedral to subhedral feldspar phenocrysts - very weakly magnetic, Z-3% disseminated pyrrhotite - Upper 64. Indistinct lower due to alteration of volcanic and porphyry MAFIC VLCANIC - ALTERATIN ZNE: MAFIC VLCANIC UNIT: - dark to medium green, fine-grained possible tuff with occasional quartz-carbonate 78 to Core Axis - microfaulting alonj Core Axis (0-5 ) has been infilled with quartz-carbonate - 2-3% pyrrhotite in tiny singers, ace magnetite - slightly magnetic ; - fine-grained unit, light to medium green sericitically altered, 2-37, pyrrhotite, l-2% magnetite in singei s along remnant (quartz-carbonate?) 72 to Core Axis ^

11 ^^.^ HU E N( T R T Y MN Muskeg Lake Property SHEET N. 6 of 9 * BANDED IRN FRMATIN WITH DYKELET: - dark green-black bands of magnetite 5/6) and chlorite alternate with quartz-carbonate and pyrrhotite 5/6) singers (a) 55" to Core Axis - songly magnetic - feldspar porphyry m, slightly sericitized 23- disseminated pyrrhotite - Upper Contact (a) 36" to Core Axis M. 525 SUIPM, ICS neterage TAL.37 ASSAYS -, X l, M Z N SERICITIC UNIT: - pale green bedded unit, possibly tuff, consistently moderately sericitized - 3-4/6 pyrrhotite throughout - bedding i) 64" to Core Axis - 2-3^ magnetite singers, moderately magnetic FELDSPAR PRPHYRY: - contacts are fractured and irregular - porphyry as m METASEDIMENT (MAFIC, ALTERED): : as m - sericitic unit : Amphibolitized Mafic Volcanic - dark to medium green, medium-grained volcanic with 3-5mm chlorite clots throughout - "L-2% pyrrhotite in large crystals (disseminated! : Mafic Metasediment LANQRIG6S RN very fine-grained, light grey-green metasediment - weakly foliated : Mafic Metasediment - fine-grained, well foliated, moderately chloritic, with minor talc dark green-grey unit - quartz-carbonate in l-3tnm 54" to Core Axis

12 NAME F HUE N. Muskeg Lake Property MN SHEET N.. 7 f 9 C (0 5 oo g z g e i C lu S. i : Sericite Altered - as above - to a pale green - L-2% magnetite in singers - -2^ pyrrhotite, weakly magnetic - well 46" to Core Axis - slightly sheared FELDSPAR PRPHYRY: - very sericitically altered dyke - grades in and out of patches of pinkish-green phenocrystic dyke to yellowish-green aphanitic units - minor pyrrhotite ALTERED ZNE: - probable mafic volcanic "bleached" by sericitic alteration to a pale yellow-green mildly magnetic AMPHIBLITE: - as m - moderately sheared MAFIC METASEDIMENT: - fine-grained, medium to light green chloritic, well sheared unit. with small 2-6mm vugs, infilled with iron-stained quartz-carbo nate - 2-3/6 pyrrhotite, mildly magnetic BANDED IRN FRMATIN: - quartz-carbonate, magnetite (5-7/6) chlorite and pyrrhotite (3/6) 570 to Core Axis - songly magnetic FINE-GRAINED VLCANIC R SEDIMENT: - light to medium green, fine-grained - poorly foliated unit, moderately chloritic, slightly sericitic. minor talc AMPHIBLrTE: - as m N X SULPM, ICS SAMPUE necerage TAL ASSAYS *. \ Z/IM Z M

13 NAME F PRPERTY Muskeg Lake Property MLE N. MN SHEET N 8 f FINE-GRAINED VLCANIC (PSSIBLE SEDIMENT): massive, medium green, fine-grained CHLRITE SCHIST: green-black schist. Upper Contact f) 48" to Core Axis, Lower Contact d) 50" to Core Axis intensely sheared, with "slickensides" on shear facies small vugs infilled with hematite-stained quartz-carbonate 2-3^ pyrrhotite FINE-GRAINED VLCANIC: as m FINE-GRAINED VLCANIC: as m with 0/6 quartz-carbonate singers with concor dant chlorite and pyrrhotite (2-3/6) singers 62" to Core Axis MAFIC FINE-GRAINED VLCANIC: as m with several vuggy sections: m, m, with 2-5mm vugs infilled with quartz-carbonate hematically-stained, and minor magnetite BANDED MAFIC VLCANIC: fine-grained, medium green, moderately chloritic with some talc, slightly sericitic 0/6 quartz-carbonate 60" to Core Axis FELDSPAR DYKELET AND "BLEACHED" ZNE: dykelet from m Upper Contact d) 66" to.core Axis, Lower 64 0 to Core Axis both contacts ringed with 5mm chlorite singers and small pyrrhotite singers pyrrhotite is greenish-pink in colour (sericitic) and contains -2/6 disseminated pyrite crystals bleached zone, very sericitic, sheared, hosts dykelet MAFIC FINE-GRAINED VLCANIC: medium to dark green, slightly chloritic, massive to poorly foliated. StHPM ICS ASSAYS hetefage t I, M l M

14 BANDED MAFIC FLW: - fine-grained, medium to dark green, well foliated unit, moderately chloritic, some talc - 5% quartz-carbonate 58" to Core Axis CHLRITE-CARBNATE SCHIST: - fine-grained, light green, sheared 60" to Core Axis - fair amount of talc alteration : exhibits tight "s" microfolding BANDED MAFIC FLW: - as m : Fine-Grained Mafic Volcanic END F HLE - slightly schistose, moderately chloritic, carbonaceous, minor talc - foliation 60" to Core Axis N. NAME F HLE N. t SIPH ICS PRPERTY MN SAMPUE TAL Muskeg Lake Property SHEET N. ASSAYS x x 07 H Z W N PAJARI DUE MAGNETICS ea to i e o s 5

15 NAME F PRPERTY Muskeg Lake Property MN m HLE N. LCATIN LATITUDE ELEVATIN STARTED d-u'v L 27+W June w. ^o9 20, 986. LENGTH ^ ;4/^/^ EPARTIIRF AZIMUTH FINISHED 6+32N June 2, 986 DIP 45 0 METERS DIP AZIMUTH METERS PAJARI 43 DIP AZIMUTH 2080 at 28 m MN l of 8 HLE N. SHEET N. REMARKS LGGED B Robert Giberson N. SutEPH. Mpf-PT-^PP TAL ^ Au A K S S A Y S Z/N Z/N CASING FELDSPAR PRPHYRY DYKE Feldspar Porphyry Chlorite Schist FELDSPAR PRPHYRY DYKE AMPHIBLITIZED BANDED IRN FRMATIN FELDSPAR PRPHYRY DYKE END F HLE CASING PULLED HLE NT CEMENTED ^ Z T ^ r; T^ ^ j XI p; Q fc'^ rn C CD n rsa C 3* * * JC. C G W to to cc w Ul 8 (T i l\ A K t \jtat\i[ "7 vo Y^\i''l f y* (^^[(^{A,^^^-^"^ -^ j ^\j \f \

16 NAME F PRPERTY Muskeg Lake Property N. MLE N. MN SHEET N. 2 of ~ " - - *. SULPM, IDES Au ASSAYS neterage frm TAL 7. 0 M Tonne -H 0.5 CASING Broken Core cm subrounded to angular fragments of mafic flow. Surface oxidation along fracture seams Light grey-green fine-grained flow. - Massive to weakly foliated. - Minor fracturing with quartz-carbonate infilling Moderately foliated (weakly laminated). - Thin (^0.25 mm wide) bands of light greenbrown biotite altered flow are intercalated with thin light green chloritic layers. - Minor layers of carbonate between bands. - Minor ductile deformation of banding. - C. A. A. approximately 85 at. m (foliation) FELDSPAR PRPHYRY DYKE Sto eo Fine-grained intermediate porphyry dyke with S-6% fine to medium-grained anhedral to euhedral feldspar phenocrysts. - Colour varies from light grey along the contacts to a grey pink. - Massive. - Trace-% disseminated pyrite. - Upper contact 56 to the Core Axis. o - Lower contact 87 to the Core Axis. 2 8 oc - Light grey-green metacrystic flow with 2-33, fine-grained feldspar metacrysts. - Massive to weakly foliated. - Minor fracturing with quartz-carbonate infilling.

17 NAME F PRPERTY. Muskeg Lake Property HLE N. MN SHEET N.. 3 of 8 N. SUtPH, IDES neterage TAL Au ASSAYS -. ^ o r W I M ^^ cm wide light grey quartz vein with minor fracturing. - Trace-% chloritic flow within healed fractures. - l-2% disseminated pyrite, ace chalcopyrite. - Irregular brecciated contacts, estimated 50 to Core Axis Moderately fractured massive to weakly foliated flow. - Trace-% thin (-3 mm wide) light grey quartz veinlets. - C. A. A. 750 at 8. m (foliation) cm wide light grey, fine-grained feldspar porphyry dyke Moderately foliated, weakly fractured flow. - l-3% fine-grained feldspar metacrysts locally. - Weakly developed flow banding. - Microfracturing increases downhole. - C. A. A. 660 at 26. m ^foliation). - C. A. A. 650 at 35.0 m (foliation). oo CD JGRIDGES RN l-2% quartz-carbonate pods and veinlets. - Trace yellow-green epidote, minor weak biotite alteration adjacent to the quartzcarbonate veinlets. - Trace sericite Well developed flow banding. - Moderately foliated. - l-2% light grey quartz-carbonate veinlets parallel foliation. - Trace pyrite along fracture seams. - C. A. A. 750 at 37.8 m (foliation). *-

18 ip^tirt:^-":^; DIAMND DRILL RECRD NAME F PRPERTY. HLE N. MN Muskeg Lake Property SHEET N.. 4 f 8 M. SL PH IDES neterage TAL Au ASSAYS -i -T Z W Z W ^ Chlorite schist. - Moderate to songly developed schistosity % carbonate along schistose planes. - Trace talc (?). - Trace-% fine-grained cubic pyrite along carbonate coated fracture seams. - C. A. A. 430 at 39. m (foliation) Massive to weakly foliated flow. - Minor microfracturing with quartz-carbonate infilling. - ^ l% very fine-grained feldspar metacrysts cm wide milky white quartz vein with very minor chloritic inclusions along healed fractures % light grey to milky white quartz veins and pods with 2-3% dark green chloritic inclu sions and fracture coating. - Contacts vary from 47 to subparallel to the quartz axis. - Trace pyrite Massive to weakly foliated light grey-green fine-grained flow. - ^ 5S fine-grained feldspar metacrysts. - Minor to locally moderate microfracturing with quartz-carbonate infilling. - C. A. A. 730 at 53.5 m (foliation) Weakly to moderately foliated mafic volcanic flow. - Moderately developed flow banding locally. - l-2% disconformable quartz-carbonate veinlets. - Thin (^ mm wide) biotite alteration haloes border the quartz-carbonate veinlets. - C. A. A. 530 at 58.0 m (foliation).

19 ,,,.,, -,.,, HI E" N RTY Muskeg Lake Property MN of 8 SHEET N. N. a SULPM IDES TAL Au ASSAYS -. -i 02 M t M^ Biotite altered, fine-grained, thinly laminated mafic tuff (?) (shear?). - Songly foliated. l% carbonate in thin bands parallelling foliation. - Trace sericite alteration. - (Similar in appearance to the hanging wall of the main mineralized "Paicia Vein"). - C. A. A at 62.2 m (foliation) FELDSPAR PRPHYRY DYKE - Light pink to grey-green porphyry; colouration varies with sericite and the degree of iron metasomatism (?). - Bimodal disibution of feldspar phenocrysts, () fine-grained subhedral to anhedral crystals and (2) medium-grained euhedral zoned phenocrysts. - Sericite (2-3/ increases downhole. - l-2% fine-grained, blue-black disseminated magnetite throughout. - Upper contact 70 to the Core Axis. o - Lower contact 6 to the Core Axis ( R p T 8 cc i Songly foliated (schistose), flow with thin layers of carbonate parallelling foliation. - Trace talc (?). - Trace pyrite. - C. A. A. 620 at 64.7 m (foliation) Light grey-green fine-grained mafic flow. - Weakly foliated with up to 2% fine-grained feldspar metacrysts parallelling foliation. - Minor flow banding locally. - Pairs of thin quartz veinlets bordered by epidote-chlorite alteration haloes (pillow

20 NAME F PRPERTY M"skeg Lake Property HLE N. MN SHEET N 6 of 8 M. ". SL PH IDES TAL Au ASSAYS -. f. 02 M l W ^ selvages?) occur randomly throughout the section. - C. A. A. 70 at Metacrystic mafic flow. - Z-3% fine-grained feldspar metacrysts aligned to foliation. - Moderately foliated. - Minor microfracturing with quartz-carbonate infilling Moderately developed flow banding with minor offset along microfaults associated with fracturing. - IK quartz-carbonate veinlets parallelling foliation. - Thin (^ mm wide) chlorite epidote haloes border quartz-carbonate veinlets cm wide milky white quartz vein with light green patches. - Very minor fracturing. - Trace pyrite within the quartz. - Poorly defined contacts C. A. A. 780 at 86.6 m (foliation). S 5 C (T) i R i tn Ul 8 o: AMPHIBLITIZED - Light to medium, grey-green, fine-grained flow. - S-0% fine and medium-grained, dark green chlorite clots. - ^.55 fine-grained feldspar metacrysts. - Very minor fracturing with quartz-carbonate infilling. - Gradational contacts into fine-grained tnetacrystic mafic flow.

21 NAME F PRPER-TV Muskeg Lake Property HLE N. m SHEET N. 7 of 8 M. TT, S L PH IDES TAL Au ASSAYS ^ "i l 02 M g/tonn a Light grey-green fine-grained flow. - Moderately to songly foliated. - Weak flow banding developed locally. - Moderately fractured with quartz-carbonate infilling Thinly laminated, biotite altered mafic flow. - Songly foliated. - Pervasively carbonatized. C. A. A. 520 at 05.5 m (foliation). C. A. A. 800 at 2.0 m (foliation) BANDED IRN FRMATIN Thin (l-3mm wide) intercalated bands of olive green mafic tuff (?), light grey-white quartz and ^ mm wide bands of smokey grey magnetite. - Moderate to locally song ductile deformation of the banding (micro Z-folds). - Trace-2% pyrrhotite. - C. A. A. 67 at 2.7 m (foliation) C to 5 8 i f g of- i c/5 tu (T Weakly to moderately flow banded, fine-grained flow. Moderately fractured with quartz carbonate infilling. - ^l% quartz-carbonate veihlets - Weak biotite alteration adjacent to quartzcarbonate veinlets Metacrystic mafic flow , fine-grained feldspar metacrysts aligned to foliation. - Moderately foliated.

22 NAME F HLE N. Muskeg Lake Property MNr86-69 SHEET N.. 8 of 8 N. r; SULPH IDES neterage TAL Au ASSAYS "i ~. 0 N l M ^ - Minor fracturing with quartz-carbonate in filling bordered by thin (^2 mm wide) epidote-chlorite alteration haloes with ace biotite. - Trace-% pyrite, pyrrhotite. Up to 2% quartz-carbonate veinlets. - C. A. A. 59 at 23. m (foliation) Songly foliated mafic flow with thin layers of carbonate parallelling folia tion. - Minor biotite alteration % carbonate FELDSPAR PRPHYRY DYKE Fine-grained, massive, light grey-pink porphyry dyke. - Bimodal disibution of fine-grained anhedral to subhedral feldspar phenocrysts and medium-grained zoned euhedral crystals. - 5S fine-grained disseminated magnetite. - Upper contact 6 to the Core Axis. - Lower contact 63 to the Core Axis Moderately to songly foliated fine-grained flow. - Thin carbonate layer parallels foliation. - Very minor fracturing with quartz-carbonate infilling. - Trace-2% fine-grained feldspar metacrysts. 5( o tn Ul o cm wide milky white to light grey quartz vein. - Sucrosic in appearance. ^ 7, fine grained fragments of mafic flow. - 7, disseminated pyrite concenated along the contacts. - C. A. A. 60 at 25.5 m (foliation). END F HLE CASING PULLED, NT CEMENTED

23 NAME F PRPERTY Muskeg Lake Property HLE N. MN LENGTH CU', 'BS'^/C LCATIN LATITUDE ELEVATIN June Wv L 32+W 2, 986 i/fcoj/i/fa/'i DEPARTURE. AZ IMUTH FINISHED 34.0 m io~^ 2050 June 22, 4+60N DIP METERS P AZIMUTH METERS PAJARI 4 DIP AZIMUTH e 34m MN-86-7 HLE N. SHEET R E MA R K S LGGED*BY Robert Giberson 2 N. SULPH IDES Mpfpr^PP TAL K AU ASSAYS K Z/N Z/N CD ( S ' ( 0 o (T 0 tn w 8 ir z CASING FELDSPAR PRPHYRY DYKE AMPHIBLITIZED BANDED IRN FRMATIN AMPHIBLITIZED FELDSPAR PRPHYRY DYKE Sericite Schist FELDSPAR PRPHYRY DYKE FELDSPAR PRPHYRY DYKE Sericite Schist Feldspar Porphyry Dyke Feldspar Porphyry Dyke Sericite Altered Mafic Flow FELDSPAR PRPHYRY DYKE Sericite Altered Mafic Flow Sericite Altered Mafic Flow FELDSPAR PRPHYRY DYKE Sericite Altered Mafic Flow Carbonate Chlorite Schist Sericite Schist END F HLE CASING PULLED A HLE CEMENTED '/pf/ld A' ~~ T C? ^jj jjfj p Y IIA l-// tn "^ ^ ** J " **^^*^^s*^ ~~*' j^/ f^r r ' \f \*S*^ L C^"**^ "^*^ -' cr : cr ' :- ~\ m..~ ~Z T*~~~- "rt'"" CI o 5 " ea ~ r.: ~ Q r 7^ ^ ~ "~ C z: -^ 33 rr ^ C _

24 NAME F PRPERTY. Muskeg Lake Property HLE N. UN SHEET N 2 f 2 f RM M. -, SUIPM iors TAl Au ASSAYS ^ -\ o J M I N CASING Broken Core cm long segments of broken metacrystic flow. - Minor oxidation along fracture surfaces Metacrystic flow. - Fine-grained grey-green weakly foliated flow. - l-2% randomly orientated fine-grained feldspar metacrysts. - Moderately fractured with quartz-carbonate in-fillin - Massive to weakly foliated. Gradational lower conts Songly foliated flow. - l-2% fine-grained feldspar metacrysts aligned to foliation. - Intensity of foliation increases downhole. - Minor biotite alteration within "thinly laminated" flow adjacent to the porphyry dyke. - Trace pyrite in thin lenses orientated to the foliation direction. - C. A. A. 620 at 9.7m (foliation). l- :t FELDSPAR PRPHYRY DYKE K36S- RN Light pink fine-grained feldspar porphyry. - Colour varies from pink to pink-green with the abundance of sericite. - Massive to weakly foliated. - S-4% medium-grained subhedral feldspar phenocrysts. - l% fine-grained blue-grey disseminated magnetite. - Trace-% fine-grained disseminated pyrite. - Upper contact 66 to the Core Axis. - Lower contact 58 to the Core Axis. Q

25 NAME F PRPERTY Muskeg Lake Property MLE N. MN-86-7 SHEET N. N * SUIPH IDES rnom neterage TAL Au ASSAYS ~- l at N fll N AMPHIBLITIZED Intensely foliated thinly laminated flow. - Minor biotite alteration decreasing downhole. - Pervasively carbonatized. - Trace pyrite. - C. A. A. 6 0 at. m (foliation) Light green-grey, massive mafic flow , fine to medium-grained chlorite clots disibuted throughout. - ^ 7, fine-grained feldspar metacrysts. - Minor shear bands (^ cm wide) within the unit. - Very minor microfracturing with quartzcarbonate infilling Moderately foliated flow , fine-grained feldspar metacrysts aligned to foliation. - ^7, fine-grained chlorite clots. - Minor microfracturing. - C. A. A. 650 at 25.2 m (foliation) BANDED IRN FRMATIN Crenulating intercalated layers of grey-brown biotite altered flow and milky white quartz pyrite % light grey to milky white quartz with thin band (-4 mm wide) of medium olive green flow - 3-7, pyrrhotite, pyrite in thin vuggy bands and discontinuous discordant singers , light grey to milky white quartz bands with

26 NAME F PRPERTY Muskeg Lake Property HLE N. MN-66-7 SHEET M 4 f 2 M. SUIPM ICS TAL Au ASSAYS l t l N (li N % light yellow-green to olive green flow. (cont'd) - /2 smokey grey magnetite-rich bands within the quartz bands. - C. A. A. 520 at 26.0 (foliation) AMPHIBLITIZED - Massive to weakly foliated fine-grained flow /S poorly defined fine-grained chlorite clots % randomly orientated fine-grained feldspar metacrysts. - Minor fracturing with quartz-carbonate infilling. - Local -2 cm wide shear zones within massive flow Fine-grained massive to weakly foliated mafic flow ? fine-grained feldspar metacrysts aligned to foliation. - ^ Z milky white to light grey quartz in thin discordant quartz veinlets. - Minor fracturing with carbonate infilling cm quartz-rich zone (70%) with angular biotite altered fragments of mafic flow. - Thin (^ mm wide) crenulating boudinaged quartz veinlets occur within the wall rock adjacent to the quartz vein. J 5 s i ez g 2 C til 8 c o z5 C. A. A. 730 at 48.2 m (foliation) Carbonate-rich mafic flow /S carbonate along foliation planes and fracture surfaces. - Songly to intensely foliated, locally schistose. - Trace-2% pyrite concenated within the carbonate. - Minor ductile deformation of veinlets within the - flow. - C. A. A. 260 at 50. n (foliation).

27 NAME F PRPERTY Muskeg Lake Property HLE N. MN-86-7 SHEET N. * Clll DU M,i-i*-^~- ~~ Sill PH, tots TAL Au ASSAYS or M Z N Moderately foliated, weakly laminated flow. - Thin carbonate layers parallel foliation. - Trace pyrite along fractures. - C. A. A. 590 at 58.3 m (foliation) FELDSPAR PRPHYRY DYKE Light pinkish-green, fine-grained feldspar porphyry. - Bimodal disibution of subhedral fine-grained crystals and medium-grained euhedral phenocrysts. - Zonation is evident within the larger phenocrysts. - lq-5% light yellow-green sericite throughout. - l-2% disseminated pyrite. - l% disseminated magnetite. - Upper contact 83 to the Core Axis. - Lower contact 35 to the Core Axis Quartz vein, milky white to light grey. - Numerous thin chloritic "healed" fractures and minor "open" fractures. - Trace-% pyrite adjacent to or within the chloritic seams. - Upper contact 59 to the Core Axis. - Lower contact 63 to the Core Axis. (D to to S g i o l Vi Ul 5. z Thinly laminated, moderately to songly foliated tuff. - Minor ductile deformation of the laminated layers. - Minor biotite alteration of chloritic layers adjacent to quartz-carbonate veinlets. - Up to 2Z disseminated pyrite. - C. A. A. 530 at 6.0 m (foliation).

28 NAME F PRPERTY Muskeg Lake Property HLE N. MN-86-7 sneer N 6 of 2 M. X SI PH ICS rnom neterage TAL Au ASSAYS - 0 M t W Moderately to weakly foliated flow. - ^l% fine-grained feldspar metacrysts aligned to foliation. - Minor fracturing with quartz-carbonate infilling. - Up to 7, pyrite within the quartz-carbonate filled fractures. - C. A. A. 520 at 68.6 m (foliation) Moderately fractured to brecciated with quartzcarbonate infilling. - Vuggy carbonate singers (-3 mm in size) contain up to 2% pyrite. - Weakly foliated to massive Sericite schist. - Gradational from sericite-rich light green flow to light yellow-green sericite schist % sericite. - 27, disseminated magnetite (fine-grained, smokey grey in colour). - Up to Z disseminated pyrite. - C. A. A. 680 at m (foliation) FELDSPAR PRPHYRY DYKE C 4D s ojo Q o 3 - Light rusty pink to pinkish-green fine-grained porphyry. - Fine to medium-grained anhedral to subhedral feldspar phenocrysts , dark rusty red spots (oxidized pyrite) throughout. - l-2% disseminated cubic pyrite, some within the rusty red spots described above. - Light green "bleached" haloes (-3 mm wide) border fractures cm wide discordant glassy, light grey quartz veinlet with l-2% black medium-grained acicular tourmaline crystals.

29 NAME F PRPERTY Muskeg Lake Property M MN-86-7 SHEET N 7 of 2 r RM N. ^ itiil ou M r*. ** **- *~ **- SIPM tots TAt Au ASSAYS N 02 W Upper contact 67 to the Core Axis. (cont'd) - Lower contact 6 to the Core Axis Sericite altered flow. - Moderate to intense sericitization. - Weakly silicified. - Moderately to songly foliated. - Light yellow-green in colour. - l-2% disseminated magnetite. - Up to l% disseminated pyrite Light grey-green moderately foliated flow banded flow. - Thin (^ rom wide) carbonate veinlets parallel foliation. - Trace disseminated magnetite. - Trace pyrite cm wide milky white glassy quartz vein. - Lower contact is marked by a light milky white-green seam containing three 4-5 mm vugs. - Trace pyrite. - Upper contact 57 to the Core Axis. - Lower contact 49 to the Core Axis s 2 S i o Sericite altered mafic flow. - Same as C. A. A. 630 at 79.6 m (foliation) f r- C w i o FELDSPAR PRPHYRY DYKE - Light pink with 2-4 mm wide light green patches. - 2% fine and medium-grained subhedral to euhedral feldspar crystals

30 NAME F HLE N. Muskeg Lake Property ^^..^^^^^^ MN-86-7 SHEET N. jo* 2 N. t. SIPM ICS rnom TAl Au ASSAYS ~ N t W - Minor oxidation of fine-grained disseminated pyrite. - Thin (^ mm wide) sericite alteration haloes bordering fractures. Upper contact 45 to the Core Axis. - Lower contact 47 to the Core Axis Sericite altered mafic flow, - Similar to Minor talc Mafic flow. - Moderately to weakly foliated, fine-grained flow. - Trace-2% fine-grained feldspar metacrysts aligned to foliation. - l-2% carbonate in thin layers parallelling foliation. - Minor microfracturing with quartz-carbonate infilling. 0 ( 5 C f Feldspar porphyry dyke. - Light grey to grey-pink fine-grained porphyry. - S-4% fine and medium-grained subhedral to euhedral feldspar phenocrysts. - Zonation is evident in medium-grained feldspar phenocrysts. - Weakly magnetic. - Trace olivine (?). - Trace-% disseminated cubic pyrite. o - Upper contact 66 to the Core Axis. - Lower contact 74 to the Core Axis ) Ul 8a. i C. A. A. 76 at 85.6 m (foliation) Feldspar porphyry dyke. - Light grey fine-grained vuggy porphyry dyke.

31 NAME F PRPERTY^ Muskeg Lake Property HLE N MN-86-7l SHEET N 9 f (cent f d) % subhedral fine phenocrysts. - Moderately fractured. - ^l% disseminated pyrite. - Upper contact 76 - Lower contact 85 to medium grained to the Core Axis, to the Core Axis. - Moderately fractured mafic flow with carbonate infilling of fractures. - Weak to moderately foliated. - l-2% carbonate in thin layers parallelling foliation. - Trace biotite alteration adjacent to fractures - Carbonate-rich mafic flow. - 2-^ carbonate in thin wisps, lenses and veinlets throughout the flow. - Moderately to songly foliated. - Minor patchy silicification. - C.A.A at 04.9 m (foliation) Light grey to grey-green intensely silicified zone. - ne l cm wide yellow-buff sericite-rich band parallels foliation disseminated magnetite throughout. - Trace pyrite within thin (/l mm wide) discordant light grey quartz veinlets Sericite altered mafic flow. - Same as m. - C.A.A. 530 at 07.5 m (foliation). FELDSPAR PRPHYRY DYKE - Light pink fine-rgrained porphyry with -27. light pink fine and medium-grained subhedral to euhedral feldspar phenocrysts.

32 NAME F HLE N. Muskeg Lake Property MN-86-7 ^^^ SHEET N. 0 of 2 M- v cm no p^**- "- - - f. S l PH, tots neterage TAL Au ASSAYS -. ~. 07 N 7 N - Thin (^ 2 mm wide) light green sericite alteration haloes border fractures. Trace Z quartz in thin discordant quartz veinlets. - Trace-% disseminated pyrite. - Upper contact 55 to the Core Axis. - Lower contact 54 o to the Core Axis Sericite altered mafic flow. - Same as m. - Up to 3% disseminated magnetite. - C. A. A. 570 at 09.5 m (foliation) Moderately foliated light green-grey fine grained flow. - Weakly to moderately foliated. - &Z quartz-carbonate in thin layers parallelling foliation. - Up to J.% disseminated pyrite Sericite altered mafic flow. - Same as m FELDSPAR PRPHYRY DYKE J (D - Same as J08.8 m. - Upper contact 27 to the Core Axis. - Lower contact 28 to the Core Axis. *) s o * z 0 a:2i ( Ul 8 C < -j Sericite altered mafic flow. - Same as C. A. A. 400 at 4.9 m (foliation) Carbonate chlorite schist

33 r BM necerage ~ i Sol SUIPM CM M**r*"-ao.o ICS rao** T*t Au ASSAYS - 7 N o; W carbonate in thin lenses and wisps (cont'd) parallelling schistosity. - Minor deformation of the schistose planes. - Trace sericite as pods within the chloriterich schistose layers Sericite schist. - Sericitlzed mafic f low/ tuff. - Thinly laminated sericlte-rich (S-60%) layers separated by light grey siliceous layers. - 2 disseminated smokey grey magnetite throughout. - Moderately carbonatlzed. - ^2 thin (-3 mm wide) light grey discordant quartz veinlets. - Trace-% disseminated pyrite cm wide light pink feldspar porphyry dyke. - Similar to m. C.A.A. 4l" at 5.9 m (foliation). C.A.A. 23 at 7.6 m (foliation) I l g g 2 i ) Ul E Mafic flow. - Light grey-green fine-grained flow. - Moderately to weakly foliated. - Minor fracturing with quartz-carbonate infilling fine-grained feldspar metacrysts. - Weak flow banding locally Carbonate-rich (3-4Z). - Moderately brecciated with quartzcarbonate cementing. - Trace-lZ pyrite in small pods within the quartz-carbonate. ^^^

34 NAME F" PRPERTY HLE N MN-86-7 Muskeg Lake Property SHEET M 2 of 2 N S. SUIPM ICS neterage r RM T* l '- Au ASSAYS or * o z N cm wide light pink feldspar porphyry dyke. - Contacts 27 to the Core Axis END F HLE CASING PULLED NT CEMENTED

35 tf) NAME F PRPERTY HLE LCATIN LATITUDE. ELEVATIN STARTED Muskeg Lake Property MN N..... ^ 50+W June 28, 986 LENGTH DEPARTURE 2+88N AZIMUTH. FINISHED 205 DIP June 29, 986 METERS DIP 45 U 450 A30 43 U AZIMUTH FTAGE DIP AZMUTH N. 56 M f, t P -rat* f TAL REMARKS. Q LGGED y, * A. H. Vogt Au ASSAYS Z/N Z/N x 0.65 CASING ', "MYLNITE" l li AMPHIBLITIZED lj MAFIC ULTRAMAFIC INTRUSIVE (?) UNIT~V\ ^ MAFIC ULTRAMAFIC INTRUSIVE (?) UNIT ( ' ' ' ^ ~^~^ *7*~ is? -{ICIA : DIVISIN HiCRDER C CD C AMPHIBLITIZED /(^ i.\ * * -c. C BANDED IRN FRMATIN, with intercalation of mafic volcanic flow )N-366-tl m^op END F HLE Ae 5: LANGRIGES -

36 METERAGE rwom M. X SUIPH, ICS ME lemfle TAL f - ; ', f -, f - t. x Z'N I W CASING J5 Fine-grained, massive to well foliated Banded flow, partly carbonatized, fractured with calcite infillings. 2.77: Minor fault/shear zone, C. A. A. 33, with internal microscale folding Flow with wispy calcite layers and nests Fine-grained, partly weakly banded flow. - Massive to weak foliation indicated by small (^0.5 mm) feldspar laths. - Weakly fractured with calcite infillings : Quartz-calcite sucture with halo of carbonatization. Upper contact C. A. A. 72, lower contact C. A. A : Irregular quartz-calcite veins and pods, aces of sulphides, minor biotitization : Wispy calcite layers. CD to 5CD t H- o l C Ul 8GC : Quartz-calcite sucture, C. A. A. 32, with mm-sized chloritized host rock fragments, very fine biotite rims : Irregular pod of feldspathic quartz and calcite with tourmaline (?) and aces of chalcopyrite : Wispy calcite. * z -

37 METERAGE NAME F HLE N. SUIPM H. ICS Muskeg Lake Property MN SHEET N.. 3 of : Light grey quartz vein, C.A.A : Wispy calcite, pods of light grey quartz with calcite J Velning and brecciation, host rock fragments \ rimmed by fine layers of biotite, calcitic X maix, pods of grey quartz, song chlor itization, epidotization, no sulphides, in flow with foliation, C.A.A : Calcite sucture with epidote, biotitiza tion, aces of chalcopyrite : Calcite-quartz vein, C.A.A : Songly fractured with calcite, quartz, epidote infilllngs, biotitization, aces of chalcopyrite : Brecciated and sheared flow with calcite, quartz, epidote in maix, biotitization, aces of sulphides : Shear, C.A.A. 40, with grey quartz in cene N o: e i V) ut gac : Brecciation/shear zone, 3.5 cm wide grey quartz vein with orientation from I parallel to core axis to C.A.A. 37, song chloritization, biotitization Fracturing with calcite inftilings, weak folia tion, elongated feldspar metacrysts Brecciation with calcite and quartz veining and maix, biotitization

38 NAME F PRPERTY Muskeg Lake Property HLE N. MN SHEET N. 4 of 0 METERAGE ME' ' ' ' '.:: _. l fjin^iaaal Lj**t l SULPM, N. ERASE ICS TAL Au ASSAYS T. ; 'N o; N Weakly banded, fine-grained flow, chloritized, fractured with calcite-quartz infillings Fine-grained, weakly foliated flow with mmsized feldspar metacrysts aligned parallel to foliation. - C. A. A. of foliation 60. Fractured, with infillings of calcite, quartz, epidote : 7 cm (ue width) milky to light greg quartz vein, upper contact C. A. A. 35, o lower contact 3, minor pyrite in frac tures in the quartz Massive to weakly banded flow, partly carbonatized, fractured with calcite fillings Weakly foliated flow with small (<mm) feldspar metacrysts aligned parallel to foliation. - C. A. A Slightly fractured with quartz-calcite infill ings. s go p. l R i C IJ 8 (T Songly fractured to brecciated, well-foliated (foliation C. A. A. 64 ). - Fine-grained flow, partly carbonatized ) Quartz-calcite sucture with intercalated ) bands of chlorite, C. A. A ) Brecciatlon : Intensive veining and brecciation, aces of pyrrhotite I * -

39 '"- * ' -- - Ut^-MI*- tu "ilv!* -.i X, Sill, m, N. ICS MfcJUtKAWb r*m TAL x T,?/ W : Intensive brecciation and veining, calcite, quartz, iron-carbonate, C. A. A. foliation at 49.65, : Calcite-quartz vein 3.5 cm (ue width) with aces of sulphides, silicified halo, C. A. A : Quartz (calcite) vein, ue width 5cm, C. A. A : Calcite-epidote sucture, upper contact 64, lower contact 55. C. A. A. foliation at ; increasing foliation and carbonatization towards the contact at "MYLNITE" Light yellow-green. - Intensely foliated. - C. A. A. foliation Weakly silicified. - Songly sericitized. - Traces of disseminated sulphides CD V ito e w ut Grading into intensely foliated, banded flow with sheared sulphides (mainly pyrite) parallel to foliation. - Decreasing intensity of foliation downhole, gradual ansition to the underlying amphibolitized mafic flow. AMPHIBLITIZED Coarse-grained (0.5 cm) chlorite clots. - Massive to slightly foliated..

40 METERAGE r RM iocs mow T* i I/W I M - Minor fracturing with calcite-quartz fillings (minor epidote). - Traces of disseminated sulphides. - Contact at marked by a 0.5 cm-wide calcite-pyrite filled vein cm above contact, intensely foliated; C.A.A MAFIC ULTRAMAFIC INTRUSIVE (?) UNIT - Gradation from well foliated into massive, coarse-grained, carbonate-rich, black-green rock with -**l% disseminated pyrite; porous Well foliated to banded, fine-grained flow, fractured and partly brecciated, disseminated pyrite and pyrite parallel to the foliation C.A.A. at ) ) Fracturing and brecciation with quartz and chlorite infillings, aces of sulphides Banded iron formation. o - C.A.A. foliation at " % pyrite parallel foliation in a weak shear zone with quartz and calcite. - C.A.A. foliation Song chloritization and epidotization. i o o cc S Songly foliated, sulphide-rich D-4%, pyrite and aces of chalcopyrite) with quartzcalcite veining, microfolds mm-wide. - Layers of chloritized host rock in veins. - C.A.A

41 ICS TAl 02 M t N MAFIC ULTRAMAFIC INTRUSIVE (?) UNIT - Dark green, fine-grained, with abundant wispy calcite layers. - Disseminated pyrite f^..0%. - Porous. - Minor epidote formation. - Contact with overlying flow C.A.A Chloritized and epidotized. - Slightly banded on foliated flow with aces of pyrite. - Lower contact C.A.A Fine-grained, weakly to well foliated. - Slightly fractured with calcite and quartz infillings, minor epidote. - Localized disseminated sulphides (mainly pyrite) ^7,. - Small sections with nun-sized feldspar metacrysts. C.A.A. foliation at Calcite-filled fracturing with ansition into intensive foliation and small scale banding. - C.A.A Intensely foliated/sheared. - C.A.A Abundant calcite as wispy layers and nests. g 2 l ID W sac ) Quartz veins with inclusions and layers of ; chloritized host rock. True width 3 and 5 cm. C.A.A C.A.A. foliation at

42 ) Irregular, banded feldspathic quartz-calcite ) chlorite veins. s 2 l 2 ii C. A. A C. A. A v* * f\ * J\ * foliation at Nest of brovmish quartz surrounded by chlorite and silicified halo cm quartz-calcite vein with 7, sulphides, C.A.A Song foliation with minor banding, C.A.A Foliation around a cm-wide sucture (C.A.A. 50 ) with quartz, calcite, epidote, aces of sulphides Song foliation (C.A.A ), discontinuous bands vith lenses of light green in dark green flow mm-sized feldspar metacrystic flow with weak foliation Weak banding, C.A.A Fine-grained feldspar metacrystic flow, foliation at Fine-grained feldspar metacrystic flow, foliation at

43 T"T". ":* r RM ICS ) ) Songer foliation with some quartz-calcite veining and biotitization AMPHIBLITIZED - Gradual ansition. - Fine to medium-grained flow. - Massive to weakly foliated. - Chlorite clots up to 2 mm. - Metacrystic feldspar laths Quartz vein, C.A.A Intercalation of fine-grained mafic volcanic flow. - Gradational ansition from/to amphibolitized flow : Fine banding with wispy layers of calcite, minor quartz veining. - C.A.A S - Feldspar metacrystic flow. - Gradual ansition from amphibolitized flow. - Decrease of size and abundance of chlorite clots, increase of the amount of feldspar downhole (40!fc feldspar, 607, mafic phases). - Slightly fractured BANDED IRN FRMATIN with intercalated mafic volcanic flow ) Fine banding, with mm to 0.5 cm wide bands of ; magnetite, sulphides (pyrrhotite, pyrite), ) granular silica with disseminated magnetite ; and sulphides, dark green chloritic bands. C.A.A. of bands 64 to 7Q

44 MLE N. NN-8-JL/U SHEET M -I-U Pi. J.U METERAGE M. n sut^, ICS Meteraqe rnom TAC Au ASSAYS x x Z/M QZ N M Bands slightly folded and broken up into fragments Medium-grained flow with 20-40% feldspar metacrysts, grading into fine-grained flow downhole. - Massive to weakly foliated. Weakly fractured with calcite quartz infillings. - Sections with medium-sized (-2 mm) chlorite clots. C. A. A. foliation at Song carbonatization, wispy layers of calcite and fractures filled with calcite. - Bleached to a light greenish colour Intensive veining with calcite infillings. C. A. A. foliation at Songly fractured, filled with calcite, minor biotitization. - S l g e i i 76.0 EH

45 IAJMND DRILL RECRD NAME F HLE N. LCATIN LATITUDE ELEVATIN STARTED PRPERTY MN W July 5. 9b6 Muskeg Lake Property l2" FMC.TM DEPARTURE, AZ IMUTH FINISHED 5+7SN 205 D p July 6, METERS m 50m 00m DIP -45" -46" AZIMUTH FTAGE DIP AZIMUTH MLE REMARKS LGGEDI0Y ' 'A.M. Vogt CASING SUMMARY LG N. S,fe Mpf-praop TAL * X ASSAYS Z/N Z/N FELDSPAR PRPHYRY DYKE FELDSPAR PRPHYRY DYKE CD t AMPHIBLITIZED FELDSPAR PRPHYRY DYKE AMPHIBLITIZED BANDED IRN FRMATIN FELDSPAR PRPHYRY DYKE FELDSPAR PRPHYRY DYKE Lb -^ x- DIVISIN!CIA ^ i ^ z o C C c r c X 8 ' -n C m i4 0 D 3 33 M C- C- CD l 2.00 END F HLE 2 i 0) Uf I -J /W r- ^cjyh \0(j^iP/^^^^- "" v

46 NAME r PRPERTY HLE N. LCATIN LATITUDE. ELEVATIN STARTED MN W July 5, 986 Muskeg Lake Property - LENGTH DEPARTUR A7 IMUTM FINISHED. 2m 5+75N f 205" July 6, 986 DIP -45" HJ METER S m 50m 00m DIP -45" " AZIMUTH FTAGE DIP AZIMUTH MLE REMARKS LGGED BY A.H. Vogt N. PRN S.ANGRIG6S CASING DESCRIPTIVE LG, Chloritic: - aphanitic to fine-grained - weakly to moderately foliated - partly banded - slightly fractured with mainly calcite infillings - aces of sulphides along fractures (mainly pyrite) : broken core : silicif ication/serici tization - aces of pyrite : biotitization around calcite- filled fractures : quartz vein CAA - 76" with calcite, epidote, silicified halo : patchy light silicification - intermittent : siliceous alteration halo around silica, calcite, epidote veinlets with aces of pyrrhotite and pyrite.62-.8: fine banding (CAA banding = 79") - bands slightly offset along calcite-filled fractures sub-parallel to Core Axis - biotitization around the latter fractures and parallel to banding - aces of disseminated pyrite and pyrrhotite :\ siliceous- sericitic alteration around small : 7 quartz veinlets :V :) N. X safcs* Mpfpvaop TAL AU ASSAYS K X Z/N Z/N

47 NAME F PRPERTY. HLE N. MN Muskeg Lake Property N. ICS necerage T* t AU ASSAYS x I W 0 N CAA (foliation) at 6.70m ^ 60 0 o i i S i m Ul s (C z : banded, CAA ^ 59" : songly fractured (CAA ^ 5") with quartz and calcite infillings - disseminated pyrite - biotitization and carbonatization FELDSPAR PRPHYRY DYKE: -.5")!, feldspar phenocrysts, slightly pinkish coloured, up to 0.7cm - mm-sized clots of chlorite - dark green to greyish maix - moderately silicified - magnetic susceptibility disseminated euhedral to anhedral pyrite; "-0.5/6 - Upper and Lower Contact CAA = 70", Chloritic: - fine-grained; well foliated; CAA = 59" - slightly fractured with calcitic infillings - partly banded - small t^rom) feldspar aligned parallel to foliation - increasing carbonatization towards the contact with the under lying feldspar porphyry FELDSPAR PRPHYRY DYKE: - similar to m - Upper Contact CAA s 33", Lower Contact CAA ^ 40" - magnetic susceptibility , Chloritic: - -similar to m - CAA foliation = 63" - fine-grained (to aphanitic) partly banded flow alternating with flow containing mm-sized feldspar crystals : songly foliated (CAA ~ 60") with song biotitization and carbonatization *

48 NAME F PRPERTY Muskeg Lake Property^ HLE N. MN ( w i Ig i m Ul 8IE i FWM :7 siliceous alteration with epidote and aces of :\ pyrite :) \*r : biotitization around calcite- f i lied fractures : broken core : broken core : quartz ± epidote vein, CAA = 68" surrounding flow songly carbonatized from m : quartz -epidote-calci te vein - CAA = 73" - aces of sulphides - minor biotitization : silicification and epidotization - aces of pyrrhotite and chalcopyrite : quartz nest with minor tourmaline AMPHIBLITIZED MAFIC FLW: - gradual ansition - medium-grained; massive texture - chlorite clots l-2mm in size and mm-sized feldspar (meta) crysts - increasing carbonatization towards the contact with the feldspar porphyry FELDSPAR PRPHYRY DYKE: - similar to m - Upper Contact CAA = magnetic susceptibility Lower Contact CAA ^ zone of circa 6cm with song silicification with decreasing size and abundance of feldspar phenocrysts towards the contact AMPHIBLITIZED MAFIC FLW: - similar to m - medium-grained with anhedral to euhedral clots - laths of chloritized hornblende several mm in size - massive texture - some quartz veinlets N t SI PH ICS ne t e rage TAl AU ASSAYS -. o;. M I W

49 NAME F PRPERTY Muskeg Lake Property MLE N. MN SHEET N 4 f 5 to W io I8i C c L : song carbonatized ansition zone with song foliation - disseminated pyrite - wisps of carbonate gradational ansition into a MAFIC VLCANIC FLCW, Chloritic: - aphanitic to fine-grained - weakly to moderately foliated (CAA = 65") - slightly fractured - fine-grained flow alternating with flow containing.imm-sized feldspar crystals - Contact ^ CAA 66" - orientation of primary layering? : veinlet (0.4cm wide) CAA 20" - widening to a nest of quartz and calcite with inclusions of chlorite ansition into BANDED IRN FRMATIN, Sulphide-Enriched: - with intercalated carbonate-chlorite schist and banded mafic flow :) mm to cm-wide magnetite- rich, chloritic, calcitic : siliceous bands, planar, songly fractured or :\ intensely folded; sulphides (pyrite, pyrrhotite : \ chalcopyrite) occupies small fissures parallel :/ to the banding - overall sulphide content 2/6 - minor epidote - banding CAA 86", Chloritic: - fine-grained, weakly to moderately foliated - partly banded (CAA s 68")- partly weak biotitization - fractured with calcite infillings - wisps of carbonate - some quartz-calcite veinlets; locally with epidote and aces of sulphides (pyrite) M X SI.PM, IDtS ne t e rage TAI AU ASSAYS i i. 0, M l M

50 NAME F HLE N Muskeg Lake Property MN SHEET 5 of 5 M. SUIPM, IDE* neterage TAl AU ASSAYS -. \!. M J W FELDSPAR PRPHYRY DYKE: - similar to m - chilled margin; contacts at 82" CAA, Chloritic: - similar to m : medium-grained with mm-sized feldspar crystals without preferred orientation in chloritic maix - disseminated euhedral pyrite : increasing carbonatization and wisps of calcite towards the contact at 05.20m *D V FELDSPAR PRPHYRY DYKE: - similar to m - Upper Contact 74 " - Lower Contact 45* - magnetic susceptibility , Chloritic: - similar to m : songly sericitic and foliated adjacent to the contact with the inusive - disseminated magnetite and pyrite - ansition to a carbonate schist at 07.5m : abundant wisps of calcite.: calcite veinlet - CAA = 32", with associated disseminated pyrite ^^ END F HLE ! 07.!.50 C I l e e i T IU 8 o: i 5

51 NAME F PRPERTY HLE N. MN-86-9 LCATIN LATITUDE '- J*3. 'vy- ELEVATIN STARTED T.akc Prooertv 3509 LE 04m TH "7 26+W DEPARTUR E 6+30N AZIMUTH 205 DP July r, H,* Ufn July 5, 986 METER S m 50m 04m DIP -A AZIMUTH rtage DIP AZIMUTH HLE N. MELz8fLJL2.sHEET N. REMARKS. LGGED BY 'A. H. Vogt SUMMARY LG N. sulpm IDES MP t" r* r A P r* Vo TAL * 36 ASSAYS Z/N Z/N 0.80 GAS ING /VERBURDEN BANDED IRN FRMATIN FELDSPAR PRPHYRY DYKE AMPHIBLITIZED BANDED IRN FRMATIN END F HLE ; ^ : ' Q ' 2oc d ; * C ) J \ F * r c "y f\ o T ) ) ' 3^ ' j * S s s fg en 8 (X o -J A ^

52 8 i 2 R i V) l S z.,s--fm., :*-.-~*s DIAMND DRILL RECRD NAME F PRPERTY _ HLE N. LCATIN LATITUDE ELEVATIN STARTED 0.80 MN ^ Muskeg Lake Property 04m LENGTH 26+W DEPARTURE 6+30N AZ IMUTH ^ Julv 4, 986 FiNi^HFn Julv CASING/VERBURDEN : DESCR P T N DESCRIPTIVE LG - aphanitic to fine-grained - fine feldspar metacrysts - weakly to well foliated - partly fine banding - slightly fractured with calcite and quartz infillings - locally weak carbonatization - chloritized haloes around calcite-quartz-f illed fractures at 6.00: foliation CAA = 650 METER S m 50m 04m at 4.66: cm-wide quartz-calcite vein (CAA = b5 ) cross cutting foliation at right angle - diffuse contacts at 7.00: foliation CAA = : black with greenish tint - aphanitic - appearance of a basaltic dyke but no obvious contacts : discontinuous silicification parallel to the foliation - bleaching of the rock to a light green colour 3.90:4.02:^ possible pillow margins :/ setched and silicified vesicles 4.45:( CAA ^ 62" 4.53.A : \ 4.82:,) DIP AZIMUTH FTAGE DIP AZIMUTH N. SULPH IDES MP f- P -ra oo Yo TAL HLE N. MN-86- N.^J REMARKS - LGGED BY A.M. Vogt AU ASSAYS K * Z/N Z/N. -J

53 NAME F PRPERTY. Muskeg Lake Property HLE N. MN-86-9 SHEET N 2 f 4 r RM M. t SULPM, ICS neterage TAL AU ASSAYS X or /* * M V D Z 8 i f f o to : calcite vein with CAA ^ 70" : fine banding with locally song biotitization - CAA banding 65" - calcite bands - fractured and slightly offset by calcite- f i lied fractures sub-parallel to Core Axis : calcite-filled fractures and wisps with associated biotitization Foliation at 29.00m CAA ^ 68" : calcite-filled fracturing sub-parallel to Core Axis with minor brecciation : fine banding (CAA ^ 65") : fine banding with biotitization increasing fracturing and biotitization towards the contact with the underlying banded formation BANDED IRN FRMATIN: - banding CAA 55" - aces of pyrrhotite and pyrite - irregular quartz-epidote and calcite bands parallel to the banding - in the down hole part abundance of complexly folded and disrupted light green cherty layers : - feldspar-phyric - weakly foliated FELDSPAR PRPHYRY DYKE: - Upper Contact CAA = 67" /C feldspar phenocrysts, zoned, in light grey, siliceous maix - feldspar up to ijcm in size - dissemianted euhedral to anhedral pyrite - fine fractures with pyrite sub-parallel to Core Axis - Lower Contact irregular, -~CAA s 65"

54 NAME F PPP.FRTV Muskeg Lake Property - HLE N. MN-86-9, UM.r ^ 3 of 4 SHEET N : - fine-grained, chloritic - weakly to well foliated - partly banded - songly foliated (CAA = 65") close to the contact with the porphyry dyke - slightly fractured with calcite infillings; sub-parallel to Core Axis - fine-grained feldspar metacrysts and feldspar-phyric flow with feldspar up to 0.4cm in diameter Foliation at 50m CAA - 70" - alternating fine-grained and feldspar metacrystic flow : intercalation of fine-grained amphibolitized mafic volcanic flow with mm-sized chlorite clots and feldspar metacrysts in chloritic maix : fine banding CAA = 57" : songly fractured with calcite infillings - associated biotitization : fine banded intercalation (CAA banding *± 65 0 ) bordered at both sides by a layer of setched and altered silicified fragments - biotitization - tuffaceous intercalation AMPHIBLITIZED : - massive to weakly foliated - fine to medium-grained - m-sized clots, slightly setched parallel to the foliation, and laths of chloritized hornblende and feldspar metacrysts in chloritic maix at 76.93: quartz vein, lcm wide - CAA s 80 e : intercalation of fine-grained, songly foliated (CAA s 60") mafic volcanic flow with calcite bands and nests M. SI.PM, ICS SAMPUE neterage THU T* L AU ASSAYS -. i ot W I N -

55 NAME F PRPERTY Muskeg Lake Property MLE N. MN-86-9 SHEET N. 4 of 4 FWM a so L PH, IDES SAMPUE " TAl ASSAYS or-n oz N decreasing grain size of the amphiboli tized flow and ansition into : - similar to m CAA foliation at 88.50m ^ 66" BANDED IRN FRMATIN: : fine banding (CAA ^ 70"), carbonate-rich - songly fractured with calcite infillings - song biotitization - alternating chlorite and biotite-rich bands : minor shear zone with calcite wisps cross cutting banding (CAA ^ 30") : minor shear zone - CAA = 5" : Magnetite Iron Formation - CAA banding ~ 64-66" - alternating mm to cm-wide bands (chloritic, magnetite-rich, siliceous, calcitic bands) - magnetic susceptibility up to 50,000 - complexly folded bands in between unfolded bands, suggesting synsedimentary origin of the "folding" - -2/6 sulphides - pyrrhotite and pyrite - dissemi nated, along fissures parallel to the banding, and along small fractures crosscutting the banding - garnets in the chloritic bands - locally epidote-rich : fine-grained partly banded weak to well foliated; slightly fractured fine feldspar metacrysts aligned parallel to foliation chloritic alteration haloes around calcite-filled fractures locally song maix silicification C Foliation at 03m CAA ^ 65" END F HLE

56 NAME F PRPERTY Muskeg Lake Property HLE N. LCATIN LATITUDE 28+W ELE VAT IN STARTED MN July 5, 986 LENGTH DEPARTUR E AZ IMUTH. FINISHED 92.65m 5+90N 205" DIP -45" July 6, 986 METERS m 50m 92.65m DIP -45" -44" -43" AZIMUTH FTAGE DIP AZIMUTH HLE N. REMARKS LGGED BY No A.H. Vogt N.! DESCRIPTI N DESCRIPTIVE LG N. 0{, SULPH IDES MpfT'T~a{*p Yo TAL 'b AU ^ ASSAYS Z/N Z/N CASING AND VERBURDEN : - aphanitic to fine-grained - weakly to well foliated - slightly fractured with mainly calcitic infillings and chloritic alteration haloes around the fractures - partly fine feldspar metacrysts - locally banded - partly carbonatized CAA foliation at 8m ^ 75" : fine banding - song carbonatization - brownish haloes around calcitic bands - biotitization : song carbonatization and foliation : quartz vein CAA = 70" - foliation CAA = 72" to 0 i o : calcite-epidote-quartz sucture - Upper Contact CAA ^ 65" - Lower Contact CAA ~ 80" : quar tz-cal cite veinlet (CAA = 7") with abundant coarse crystalline epidote l LANGRIGES I : song carbonatization : fine banding (CAA z: 68") with alternating calcitic chloritic and quartz bands - biotitization - banding offset along calcite-filled fractures sub- parallel and at low angle to Core Axis

57 NAME F HUE N. Muskeg Lake Property MN SHEET N.. 2 f 4 g 3 S ffr- ) 8 i r RM - some small pods with quartz and chlorite Foliation at 25.5m CAA = 63" Foliation at 32.00m CAA :^ 65" : quartz-epidote-calcite sucture - Upper Contact CAA = 67" - Lower Contact irregular, with minor garnet and aces of pyrrhotite and pyrite - adjacent hosock weakly silicified : irregular light, siliceous bands and lenses parallel to the foliation with calcite, chlorite, minor epidote and aces of sulphides : banding with siliceous and extensive epidote-rich siliceous bands crosscut by calcite and quartzfilled fractures - CAA banding = 7" : calcite bands parallel foliation songly fracturec and crosscut by quartz -calcite vein - CAA = 45" : intercalations of fine to medium-grained amphibolitized mafic volcanic flow with mm-sized chlorite clots and feldspar metacrysts in chloritic maix : quartz vein - CAA = 67" with calcite ± epidote : epidote-rich siliceous alteration halo around small quartz veinlets Foliation at 4m CAA - 67" : white to bluish-grey quartz vein and pods - Lower Contact CAA = 22" - chlorite along fractures in the quartz : song foliation (CAA ~ 20") with abundant wisps of calcite parallel to the foliation - disseminated pyrite : song foliation (CAA = 35") with wisps of calcite parallel to the foliation M. i sutct^ ICS neterage TAl AU ASSAYS x x Z/H CZ N

58 S is i e o *- Jjj s DIAMND DRILL RECRD : songly foliated (CAA = 50") and fine banded - circa. /6 disseminated pyrite bands partly complexly folded - crosscutting calcite and quartz- f i lied fractures - sericitic alteration : song foliation (CAA = 43") with abundant wisps of calcite parallel to foliation - aces of disseminated pyrite AMPHIBLITIZED : - gradual ansition - medium-grained, mm-sized clots and laths of chloritized hornblende in chloritic maix - massive to weakly foliated - small intercalations of fine-grained mafic flow - down hole decreasing grain size to fine-grained amphibolitized mafic flow - slightly fractured - ansition into underlying fine-grained mafic volcanic flow : - similar to m CAA foliation at 73.50m = 63 0 BANDED IRN FRMATIN: : fine banding with calcitic and chloritic bands - aces of pyrite and pyrrhotite - banding CAA * 8" :) bluish-grey quartz veins, contacts parallel :j banding - chlorite on fractures in the quartz : mm to cm-wide bands of alternating siliceous. chloritic, calcitic, magnetite- rich layers - CAA banding 75" to 85" - rich in pyrrhotite, which occurs in bands parallel to the general banding - pyrite mainly on the banding crosscutting fractures N NAME F HLE N. MN \ X SUIPH tots y* l/ FBM necerage III Jn ia Y /y y Muskeg Lake Property l l i 7/ fr TAL i SHEET N. 3 f 4! folij -*co: bee AU ASSAYS i "' tion/s ncides ding? ot. M.0 III tear r with.08 f / I M tates rimar

59 '4AME F Muskeg Lake Property _ : - section between and 78.85m circa 55")!, quartz and 25"fc pyrrhotite -similar to m with intercalations of fine-grained amphibolitized mafic flow CAA foliation at 8.50m ~ 67" CAA foliation at 84.00m = 66" - locally weak silicification and sericitization : intercalation of fine-grained, amphibolitized mafic flow with ^Imm-sized chlorite clots and fine feldspar metacrysts 88.68: irregular singers with bluish-grey quart: : fine banding (CAA ~ 68") with bands of calcite and quartz - associated chlorite and epidote alteration and biotitization - slightly fractured with calcite-filled fractures : fine to medium-grained amphibolitized mafic flow with feldspar (tneta) crysts several mm in length END F HLE N. NLE N. MN SHEET N 4 of 4, n AU ASSAYS n so IPS' ICS a j. 0 N Z W neterage TAL V S I e l e i C w 8 (C

60 NAME F PRPERTY Muskeg Lake Property HLE N. MN LENGTH 92.65m a.'w. Ae8(?/^* 0 l LCATIN 5+90N LATITUDE ELEVATIN STARTED 28+W July 5, 986 DEPARTURE AZ IMUTM FINISHED 205" DIP -45- July 6, 986 METERS m 50m 92.65m DIP -45" " AZIMUTH FTAGE DIP AZIMUTH HLE N. MN-86-92^.^ N. REMARKS No Pajari "l LGGED B' CASING/VERBURDEN DESCRIPTI N SUMMARY LG N. K SULPH IDES M^T-praop TAL Jl, * ASSAYS Z/N Z/N APHIBLITIZED BANDED IRN FRMATIN END F HLE i l li ; ' f f \ ' U) : i i sc If tf ^ 5 a ) y ) l y * 9 f w m t s (6 (D i co LANGRlGf m^^^^ \

61 Minisy or Northern Deveiooment Mines ining Act.b Najge and Address ot Record od Holder ' 'HP - &D Summary of Disibution of Credits and Work Performance Mining Division Townsnip or Area /^^6 ffsh^ (-j^rkc' Total Assessment Credits Claimed Prefix Mining Claim DCUMENT No W9K)3*0// 52oaesE0ee2 se KAWASHE LAKE 900 requirements and the reverse side of this form tor tad** of information. Report of Work Number G. /ec/xj ' Work Days Cr. Mining Claim Prefix l Number Work Day* Cr. ; Prospector's Licence No. Telepnone No. Prefix M ning Claim j Number Work Days Cr. Type of Work Performed (Check one only) l LJ Manual Work Shaft Sinking Drifting or other L- Lateral Work ^2 Mechanical equipment ^ Power Sioomg other than Manual i (maximum credit allowed - 00 days per. claim) 5[ Diamond or other Core drilling ( _ Core Specimens l ' i 4 if 7^ T" t Dates wnen work was performed, Total NW of Days Performed i Total No. ot Days Claimed Total No. ot Days to be Claimed at a From: pfc - C)(^ ~~ '^! To: Qb~ C^-f ~lb ' *^ f*^ lit All the work was penormea on Mining Claim(s): Mining Claim No. of Days Mining Claim N. ol ayi Mining Claim No, ot ayi Indicate no. of days performed on each claim. /X (See note No. on reverse side) w 385/ /0 V3/.5 Mining Claim No ol Days Mining Claim No. ol Days Mining Claim No. ot ayi Mining Claim No. ol Day* Mining Claim No. ol Diyi Mining Claim o. ol Diyi Required Information eg. type of equipment, Names, Addresses, etc. (See Table on reverse side) if space below is insufficient, attach schedules with required information and location sketches JAM 2' 3 0 ). Certification of Beneficial interest ' (See Note No. 2 on reverse side) l hereoy cenity that, at the time me worn was performed, the claims covered m this report of work were recorded in the current recorded holder's name or held under a Peneficial interest by the current recorded holder. Certification Verifying Report of Work hereoy certify that 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. Name ano Address of Person Certifying Date For ffice Use nly Work Assignments (89/06)

62 SCHEDULE Hole No. Claim No. Start Finish Dip/ Azimuth Lencrth Jm) AssessBN Credits MN86-67 MN86-69 MN86-7 MN86-76 MN e&oo-ii* wo June 23/86 June 20/86 June 2/86 r 6CC.w**J.f - t June 28/86 July 5/86 June 24/86 June 2/86-45 / /205 June 22/86-45 CV205?e^t,ve^ tfosro 2*y *sisi*va*avr June 29/86-45^205 July 6/86-45 CV rfr a*. I T, ^s 67-;- ^ 2 oo ^ MN86-9 MN July 4/86 July 5/86 July 5/86-45^205 0 July 6/86-45^ Z ^ H)- NtSIAtCI 9N!N'!H- 8203QB

63 .4 Vi \i ^f t S^ ' 64* * I3I/ 845 W Pa 84(509 tssri" - - to ^ ^-. rcuf"f l In^nnoi ' 849 "3. l, * "' J-840I 84IS \ I04 l 6390S V839S asses? esssae./i ' I392V ^ H & o I 8SI47 ' 86MI : - ^ nzwzi j Pa *8S L -J- -^ Jp* 'ssidss ' J \ /249^ r e^8su3? i. l,.; \369077\ /eil " f E6I! i ' y 840* l M '8833( ^ ^ S83384 sesawy 88^Si6 M/^ " ; * '85235 I 85^^42 l J244TeSI2S2 ' ""r "i-h '86576 J l- -L i*7t 86^79 86, K X 84BS * T7 8*582 ~! KX3864., i i j j d**^tzl l 87^75^7g72S,' \ - l 8658 J j /7779.TTTSC j l \ f l: ' \ 7 ' i ~^ ' (7 J S T2664 i ~ l * J ^ \ lil B *7" V7T*5.7r?*ss S, l \ \ {872/72 j 87272* ^J-, ; --t" h M 8* '(8^254 rt V r\,l! SJJ8689I6 ^ , l \, *7Z J 87268xi f, ft l *, goe I.-h ' l "j~ l l l 77786oJ "872668VZ729 ^ l B7273I ' J *wfe l l -4 l a '* ' 't ' l j b"9i " 0472 l W4f76 l n l I, * t,, 'l ^872* ^^ ' ' 8907 M04H75I f ^nmj t7779t6 ^79"7^7W T" ^ J^T^^g^-- - ' 4- ' JY^J^"*3 **"** ^^ l ' ' ' l\? j pg^fjuittur^bfttit l T274^ J L^/j ' ' l b^^^7^ii^87t.^7a87"t^8r^7s4- f ',! i l i/ l xi8727^.s.itw^xl^it^r l 7779T ' M i -V Xi