Report No; 23. Area: Resources RECORDED HOLDER: SAME As ABOVE [ x l : OTHER I l WORK PERFORMED FOR: CLAIM No, NOTES: # DIAMOND DRILLING

Transcription

1 DIAMOND DRILLING 42C13SE WABIKOBA LAKE 010 Area: Wabikoba Lake WORK PERFORMED FOR: Resources RECORDED HOLDER: SAME As ABOVE [ x l : OTHER I l CLAIM No, TB HOLE No, TY-02 TY-03A FOOTAGE Report No; 23 DATE Jan/86 i. NOTE d) d) NOTES: #115-86

2 NORANDA EXPLORATION COMPANY, LIMITED Diamond Drill Summary Property: TYLOX Hole No.: TY-02 Location: 45+OOW, 4 + OON Azimuth: 035O Dip: -55 Casing: 2.4 m Length: 134 m Core Size: NQ Acid Tests: 50 m - 52 O 100 m m Drilled By: Midwest Start: Jan. 4/85 Finish: Jan. 7/85 Logged By: John Gagnon Date: January 7, 1985 O 2.4 CASING O 33.7 t, -. \ O NTARIO GEGI.OGiCAL SURVEY SOqpaV.cINT FiL.ES RESEAfiCH OfcFiCL: M AY 2 7 if-iho R E C E! V E D QUARTZ-FELDSPAR-BIOTITE (SERICITE) SCHIST (5b. g) Medium to light grey, fine grained, poorly to fairly well banded, occasional calcareous bands, weakly to moderately sericitic throughout. Some mottly textured sericitic sections, occasional silicified bands m: Medium to coarse grained section, massive, schistose, vaguely feldspar porphyritic m: Feldspar Porphyry (7a): Medium grey, fine grained biotitic ground mass somewhat vague subhedral to anhedral feldspar phenocrysts less than l mm to 2-3 mm in size. Fairly sharp concordant contacts m: Feldspar Porphyry (7a): White, euhedral feldspar phenocrysts 1-5 mm in size, in a dark grey, fine grained, somewhat schistose, biotitic ground mass. (Similar to inequigranular porphyry in deposit.) Sharp concordant contacts.

3 m: Feldspar Porphyry (7a): Similar to but with many more smaller (<l mm) feldspar crystals. IX disseminated pyrite m: Feldspar Porphyry (7a): Same as m m: Feldspar Porphyry (7a): Massive, homogeneous, feldspar phenocrysts 1-2 mm in size in a dark grey, fine grained, biotitic ground mass m: Feldspar Porphyry (7a): Same as m m: Feldspar Porphyry (7a): Similar to m but has a hornblende bearing matrix. 1-2X euhedral pyrite crystals m: Bleached Section: Light grey with pale greenish hue, fine grained, mottly textured bleaching, sericitization, calcareous hairline fractures, 1-2X disseminated pyrite m: Feldspar Porphyry (7a): Same as m* 1-2Z disseminated pyrite m: Feldspar Porphyry (7a): Same as m m: Weakly laminated silicified section, minor quartz veining, some associated calcite, minor blebs pyrite m: Mafic Dike: Dark green, fine to medium grained, massive, moderately calcareous, irregular discordant contacts. Some dark greenish - black fine grained clots with fragmental appearance m: Section containing up to 5H l aminar pyrite, mild pale greenish bleaching m: Feldspar Porphyry (7a): Same as m m: Biotite Schist (5c): Fine to medium grained, dark grey, schistose, some calcareous bands minor disseminated pyrite. Angle of foliation to core axis 57o at 21 m FELDSPAR CRYSTAL TUFF ( 3e) Light to medium grey, fine grained, biotitic ground mass, up to

4 white anhedral to euhedral feldspar grains/crystals, less than l mm to about 3 mm in size. Somewhat similar in appearance to feldspar porphyry, but upper and lower contacts are gradational tending to blend in with overlying and underlying units, and proportions of feldspar crystals in the tuff are considerably more variable through the unit. Tuff also is weakly banded with some mild sericitization. Contains minor disseminated pyrite, tiny blebs and strangers. Weakly calcareous, occasional very calcareous bands. Angle of foliation to core axis 64 O at 40 m QUARTZ-FELDSPAR-BIOTITE GNEISS (5b) Dark grey, fine grained, weakly banded. Several quartz-calcite veins, and light greenish coloured calcareous bands. Mild pale greenish bleaching around hairline fractures. Intense bleaching around 43.5 m and m. Minor disseminated pyrite in places. FELDSPAR CRYSTAL TUFF (3e) Similar to above unit, mild sericitization throughout, weakly calcareous, occasional quartz eyes observed, minor blebs of pyrite. QUARTZ-FELDSPAR-BIOTITE-MUSCOVITE (SERICITE) SCHIST (SbTTy Generally medium brownish grey, fine to medium grained, poorly to fairly well banded, alternating light muscovite/sericite rich bands and darker brownish biotite rich bands. Sericitization is not intense, comprising about of the unit overall. Occasional cherty appearing siliceous bands, and calcite rich bands, minor garnet observed m: Sericitic Band (5g): Light grey, fine grained, schistose, few mafics, some biotite m: Moderate bleaching, sericitization.

5 FRAGMENTAL UNIT (5e) Light greyish siliceous and felsic clasts a few mm to 3-4 cm in size* elongated, in a dark grey fine grained biotite rich matrix* Scattered garnets from around 63.5 m increasing downwards* m: Mafic Dike/Sill: Dark green, fine grained, massive homogeneous with no apparent fabric* Contacts somewhat irregular but appear concordant* m: Same as m. Quartz vein within dike roughly parallel to core axis m: Spotty pyrite and pyrrhotite mineralization as disseminations, blebs and laminae, 1-2X overall m: Numerous garnets in this section. Two 5 mm wide sillimanite bearing bands m: Bleached, silicified section, weak hematization, 1-2X pyrite QUARTZ-FELDSPAR-BIOTITE SCHIST (5b) Medium to dark grey, quite fine grained, massive, poorly banded, some calcite rich bands. Minor bleaching, sericitization m: Section containing about ls-20% pyrite and pyrrhotite m: Section contains abundant dark green mafic material (hornblende). Unit contains about S-10% pyrite and pyrrhotite mineralization down to about 70 m. Mineralization occuring mainly in bands a few cm thick FELDSPAR CRYSTAL TUFF (3e) Medium to light grey, angular to subrounded white feldspar grains l crystals in a darker fine grained biotitic or sericitic ground mass, quite schistose, weakly banded. Occasional quartz - calcite veins, some hematization, minor pyrite blebs.

6 BIOTITE-QUARTZ GNEISS (5c) Dark grey to black, quite fine grained, hard, massive, poorly banded, weakly calcareous. Lower half metre is mildly silicified with some hematization near bottom. Lower contact fairly sharp. FELDSPAR CRYSTAL TUFF (3e) Similar to m, weakly calcareous, some mild sericitization, hematization. FELSIC VOLCANIC/TUFF (3a) Light grey, fine grained, massive, gneissic texture, only S-10% mafic minerals (hornblende) m: Strongly hematized section, numerous epidote veins, stringers, some calcite stringers m: Quartz Vein: some associated calcite. QUARTZ-FELDSPAR-BIOTITE GHEISS (5b) Dark brownish, fine grained, fairly well banded with light coloured bands, occasional weakly calcareous bands. QUARTZ ETE-SERICITE-BIOTITE SCHIST (3e. f) Possible felsic volcanic. Light grey, fine grained, schistose, poorly to well banded. Vague feldspar grains, occasional quartz eyes. Angle of foliation to core axis 59 0 at 82 m. MAFIC DIKE Dark green, fine grained, massive, homogeneous, weakly calcareous, irregular discordant contacts. QUARTZ-FELDSPAR-BIOTITE GNEISS/SCHIST T5bT Essentially the same as m, less well banded. Sporadic occurrences of pyrite in sections a few cm thick carrying 1-23! disseminated pyrite. Lower metre contains minor garnet, a few bands 1-5 cm thick containing small feldspar grains l mm in size or less.

7 MAFIC DIKE Dark green, fine grained, massive, contacts somewhat obscure, core broken up QUARTZ-FELDSPAR-BIOTITK-GARNET GNEISS/SCHIST (5dT Dark grey to blackish, fine grained, poorly to fairly well banded, varying schistose to gneissic in texture* Scattered, garnet porphyroblasts less than l mm to 3-4 mm in size throughout. Occasional light calcareous bands, quartz - calcite veins. Some spotty pyrite and pyrrhotite mineralization as blebs, disseminations, tiny laminae FRAGMENTAL (5e) Essentially the same as , basically a biotitic gneiss l schist with light greyish-white elongated clasts. Unit poorly to well banded, some calcareous bands. Clasts appear as thin lenses, flattened up to about 10: QUARTZ-FELDSPAR-BIOTITE GNEISS/SCHIST (5b) As described in previous sections m: Feldspar Porphyry (7a): Dark grey, fine grained biotitic ground mass containing white subhedral to euhedral feldspar crystals less than l mm to 2-3 mm is size. Sharp concordant contacts m: Silicified, bleached zones, some calcite veins, hairline fractures m: Quartz Vein: barren MAFIC VOLCANIC (Ib. 5b) Considerable intermixing of dark green, fine grained mafic material with brown biotitic bands. Numerous calcite veins, stringers and bands m: Section contains more intermixed biotitic sediment, slightly bleached.

8 FELSIC VOLCANIC/TUFF (3a) Light to medium grey, fine grained, massive, poorly banded. Basically a quartz-feldspar-biotite +Xsericite schist/gneiss, biotite comprising 5-10X or less of the rock. Somewhat mottly textured,. weak to moderate sericitization, minor quartz eyes observed. Upper metre bleached, silicified. 2-3X disseminated pyrite throughout most of the unit. Could be an altered sediment m: Feldspar Porphyry (7a): Same as m m: Feldspar Porphry (7a): Same as m m: Mafic Sill?: Dark green, medium grained, quite schistose, hornblende bearing, with many small biotite lenses, moderately calcareous throughout, sharp concordant contacts. May represent thin mafic volcanic beds. MAFIC VOLCANIC (Ib) Dark green to blackish, fine grained, schistose textured, quite calcareous throughout, many quartz - calcite veins, calcite bands and laminae. Many biotite rich bands and lenses. Unit may be a sediment m: Quartz - Feldspar - Sericite Schist/ Feldspar Crystal Tuff (3a, e): Light grey, fine grained, schistose, poorly banded, weakly calcareous, subrounded to subangular feldspar grains 1-2 mm in size. Moderate bleaching, sericitization, possible vague quartz eyes. Less sericltized parts contain more feldspar grains. QUARTZ EYE-SERICITE-BIOTITE-FELDSPAR SCHIST (3f) Light to medium grey, fine grained, schistose, poorly banded, numerous quartz eyes less than l mm to 3-4 mm in size. Feldspar grains appear to occur in less sericitized, more biotitic sections.

9 m: Mafic Volcanic (Ib) As described m. Angle of foliation to core axis *5 0 a t 130 m 60' at 61' at 53' at m m m END OF HOLE 134 aetres

10 NORANDA EXPLORATION COMPANY, LIMITED Diamond Drill Summary Property: TYLOX H ole No.: TY-03A Location: 37+OOW, 3+OON Azimuth: 035 O Dip: -55 O Casing: 6.1 m Length: 177 m Core S ize: NQ Acid Tests: 50 m - 51 O 101 m m m Drilled By: Midwest Start: Jan. 7/85 Finish: Jan. 11/85 Logged By: John Gagnon Date: January 14, 1985 O CASING LAMINATED QUARTZ-FELDSPAR-BIOTITE HORNBLENDE SCHIST (5b. Ib) Dark brown to dark green, fine grained, well laminated alternating biotite and hornblende rich bands less frequent light greyish coloured felsic bands. Occasional calcite rich bands with associated quartz and dark green coloured hornblende. Some scattered garnet as aggregates up to l cm long m: Feldspar Porphyry (7a): Light grey, massive, homogeneous. Subhedral feldspar porphyroblasts less tham l mm to 2 mm in size in a biotite bearing ground mass m: Feldspar Porphyry (7a): As described above QUARTZ-FELDSPAR-BIOTITE-SERICITE SCHIST (5b. g) Dark brown to dark grey, fine grained, well laminated. Similar to above unit but contains only minor hornblende and has some light buff coloured sericitic bands and laminae which comprise S-10% of the

11 unit. Also quite calcareous throughout m: Coarse grained blotitic schist QUARTZ-FELDSPAR-BIOTITK GNEISS/SCHIST (5b) Dark grey to black, fine grained; poorly banded overall, some fine light greyish calcareous laminae. Weakly to moderately calcareous throughout m: Bleached Zone: Mildly silicified moderate hematite alteration, calcite filled hairline fractures. Angle of foliation to core axis 53 O at 20 m FELDSPAR CRYSTAL TUFF/QUARTZ EYES SERICITE SCHIST (3e. f T~~ Overall medium to light grey, fine grained, schistose textured. Crystal tuff is biotitic with subhedral to euhedral white feldspar crystals less than l mm to 2-3 mm in size. Feldspar crystals comprising up to 15X of the rock* Quartz eye - sericite schist appears to be an alteration of the crystal tuff as the two are considerably intermixed and gradational to one another. Minor blebs of pyritic observed m: Quartz-Feldspar-Biotite Gneiss (5b): Similar to previous units, moderately calcareous HORNBLENDE-FELDSPAR-QUARTZ-BIOTITE SCHIST (lb, 5b) Dark green to dark brown, fine grained, poorly to well laminated. Numerous white calcite rich bands/laminae, moderately schistose textured. Probably is a mafic volcanic or tuff or volcanically derived sediment m: Quartz Vein: Considerable intermixed calcite, mafic material m: Feldspar Porphyry (7a): Subhedral to euhedral feldspar phenocrysts less than l mm to 2 mm

12 in size, in a dark grey, fine grained biotitic ground mass FELDSPAR CRYSTAL TUFF (3e) Subhedral feldspar crystals/grains less than l mm to about 2 mm in a medium grey, fine grained biotite bearing ground mass. Moderately' schistose, occasional bleached or mildly sericitic bands. Angle of foliation to core axis 6S O at 43 m BIOTITE-FELDSPAR-QUARTZ-HORNBLEHDE GNEISS (5b. Ib7 Fine grained, fairly well laminated, dark brown to dark grey with thin dark green bands. Numerous white calcite rich bands, occasional quartz-calcite veins* Unit is quite calcareous throughout* Lower contact is gradational QUARTZ-FELDSPAR-BIOTITE GNEISS (5b) Dark brown to dark grey, fine grained, poorly banded, gneissic texture. Moderately to strongly calcareous, minor dark green mafic bands. Essentially the same as previous unit but with only very little mafic. Gradational contacts m: Strong epidote alteration with moderate hematization, many epidote and calcite filled hairline fractures m: Moderate sericitic alteration, minor quartz and calcite veins m: Mafic Dike: Coarse grained, dark green, massive, somewhat schistose, hornblende rich with some thin biotite laminae. Angle of foliation to core axis 53o at 51 m BIOTITE-HORNBLENDE-FELDSPAR-QUARTZ GNEISS (5b. IcT As described previously, well laminated, calcareous.

13 SERICITIC SCHIST (3f) Light grey to white, fine grained schistose, minor quartz eyes observed, some biotitic bands, minor blebs pyrite, vague feldspar grains in more biotitic bands. QUARTZ-FELDSPAR-BIOTITE GNEISS (5b) Dark brownish grey, fine grained, generally - * massive, unlaminated, mildly calcareous* A half metre section through middle of unit is coarse grained, light greyish, strongly calcareous with some dark green mafic bands. HORHBLEHDE-BIOTITE-FELDSPAR-QUARTZ GNEISS (le. 5b) As described previously. Well laminated, some medium to coarse grained strongly calcareous bands m: Quartz Vein: Contains abundant calcite, dark green mafic bands. GARNETIFEROUS SCHIST (Id. 5d) Mixture of dark green mafic hornblende rich rock and dark brown biotite bearing sediment. Garnet porphyroblasts up to 3 mm in size comprise as much as 25Z of the uni t. Angle of foliation to core axis 68 O at 69 m. QUARTZ-FELDSPAR-BIOTITE GNEISS (5b) Dark grey to blackish to sometimes dark brown, quite fine grained, generally poorly banded observed as lighter coloured calcitic bands. Minor dark green mafic laminae. Has a fine, granular almost sugary texture, may be an intermediate grade tuff or tuffaceous sediment. Small fold closure? at 77.3 m or boudinage m: Section contains several bands 1-2 cm wide which contain small (less than l mm) subrounded to subangular, white feldspar grains. contacts with these bands are gradational, with feldspar grains observed scattered between

14 bands, i.e. feldspar clastic in origin m: Feldspar Crystal Tuff (3e): White, generally subhedral feldspar crystals/grains 1-5 mm in size; light grey, fine grained biotite bearing ground mass. Some sericitic laminae, somewhat schistose. Unit possibly clastic in origin, contacts sharp but feldspars diminish toward bottom m: Quartz Vein: Mirior pyrite observed, calcite associated m: Feldspar Porphyry (7a): Dark grey, schistose, biotitic ground mass, white subangular feldspar phenocrysts less than l to 2 mm in size m: Similar to m but contains less feldspar, contacts are not as sharp though not gradational; may be clastic. Angle of foliation to core axis 72 O at 83 m QUARTZ-FELDSPAR-BIOTITE-GARNET GNEISS/ GARNETIFEROUS MAFIC VOLCANICS ( 5b-d." Id) Essentially the same as m but containing scattered garnets, and coarsely garnetiferous dark green mafic volcanic bands. Dark grey to blackish, occasionally brown, poorly to well laminated in some sections, weakly to moderately calcareous. Numerous light greyish calcite rich bands and laminae. Scattered sections containing small white feldspar grains. Occasionally quite biotitic m: Garnetiferous Mafic Volcanic (Id): Up to 25X garnet as coarse aggregates to l cm across. Also contains quartz veins with associated calcite m: Garnetiferous Mafic Volcanic (Id): Same as m m: Garnetiferous Mafic Volcanic (Id): Same as above, some interbedded biotitic sediment (5b).

15 m: Mildly bleached section. Angle of foliation to core axis 70 O at 104 m QUARTZ EYK-SKRICITE SCHIST/FELDSPAR CRYSTAL TUFF (3f. 3e) Light grey, fine grained, mildly to moderately sericitic, occasional quartz eyes to 2-3 mm in size interbanded with medium grey, biotitic crystal tuff, feldspars generally l mm or less, massive' unlaminated; moderately schistose where sericitized, weakly to moderately calcareous, some quartz calcite veins. Fuzzy contacts between sericitic schist and crystal tuff QUARTZ-FELDSPAR-BIOTITK GNEISS (5b. le, Minor 5d) Dark grey to brownish to light grey, quite fine grained, granular, sugary texture, thickly to thinly banded, numerous light grey calcareous bands and laminae, occasional dark green mafic bands. Minor garnet observed, a few aphanitic light grey cherty appearing laminae. A few dark green, fine grained mafic bands (hornblende-feldspar gneiss) up to 10 cm wide. QUARTZ-FELDSPAR-BIOTITE GNEISS. GARNETIFEROUS GNEISS. GARNETIFEROUS MAFIC VOLCANICS (5b. d. Id) Quartz-feldspar-biotite gneiss similar to previous units, some scattered garnets, numerous dark green mafic bands l cm to 10 cm wide containing up to 252 garnet as coarse aggregates up to l cm in size. Mafic bands comprise about ls-20% of the unit. Moderately to strongly calcareous especially around mafic bands. Moderately well to poorly banded/laminated. Numerous thin brown biotitic laminae. Contacts with upper and lower units gradational. Fold closure at m.

16 m: Biotite-Feldspar- Quartz Schist (Se): Dark grey, fine to medium grained, massive, homogeneous, foliated but with no banding. Somewhat gradational contacts HORNBLENDE-FELDSPAR GNEISS (MAFIC VOLCANIC). QUARTZ-FKLDSPAR-BIOTITE GNEISS. MINOR GARHKTIFEROUS MAFIC VOLCANIC (le. d. 5b) Mainly dark green to dark greyish, fine grained, hornblende-feldspar gneiss with fine grained, dark brown biotitic bands. Unit is somewhat massive, poorly to moderately well banded, moderately calcareous, occasional white quartz-calcite veins 1-3 cm wide. Some light greyish calcite-rich bands m: Garnetiferous Band: garnet porphyroblasts up to 3-4 mm in size m: Quartz-Feldspar- Biotite Gneiss (5b): Dark brownish-grey, fine grained, moderately well banded, fairly typical. Angle of foliation to core axis 77 O at 130 m QDARTZ-FELDSPAR-BIOTITE-HORNBLEHDE SCHIST (2a-5b) Possible intermediate volcanic. Dark brownish grey to greenish, fine grained, schistose, poorly banded, moderately calcareous. Scattered small, white, subangular feldspar grains (tuffaceous?), minor garnet HORNBLENDE-BIOTITK-FELDSPAR-GARNET SCHIST (Ib-d. SbTdT Dark greenish to dark brownish, fine grained, schistose, poorly banded, some light greyish calcareous bands, garnet as coarse aggregates up to about 7-8 mm in size m: Feldspar Porphyry (7a): Medium grey, massive, homogeneous, biotitic ground mass, white

17 feldspar crystals less than l mm to 3-4 mm in size. ^ m: Feldspar Porphyry '(7a): Same as m m: Feldspar Porphyry (7a): Same as above. Contacts of porphyries are sharp, concordant some are obscured by quartz veins at the margins HORNBLENDE-FELDSPAR GNEISS (le) (MAFIC VOLCANICT Dark green, fine grained, massive, poorly banded, moderately to strongly calcareous, occasional quartz-calcite veins. QUARTZ-FELDSPAR-BIOTITE GNEISS (5b) Dark brown to dark grey, fine grained, weakly laminated, moderately calcareous. Some dark green mafic bands. QUARTZ-FELDSPAR-HORNBLENDE- BIOTITE-GARNET SCHIST ( Id. 5d) Fine grained, schistose, poorly banded, dark green to dark brown, weakly calcareous. Garnets as aggregates up to l cm across. QUARTZ-FELDSPAR-BIOTITE-HORNBLENDE GNEISS/SCHIST (5b. IbT Dark brown to dark green, fine grained, poorly to moderately well laminated, weakly to moderately calcareous m: Contains scattered small white feldspar grains generally less than l mm m: Biotite rich with garnet porphyroblasts 1-4 mm in size. Angle of foliation to core axis 76 O at 151 m. HORNBLENDE-FELDSPAR SCHIST (Ib) Dark green, fine grained well laminated in places, some dark brown biotitic bands moderate to strongly calcareous.

18 QUARTZ EYE-SERICITE SCHIST (3f) Typical, light greyish, quartz eyes up to about 3 mm, some-biotitic bands, vague feldspar crystals QUARTZ-FELDSPAR-BIOTITE GNEISS. HORNBLENDE-FELDSPAR SCHIST (5b. Ib) Both rock types fairly typical, moderately well banded, weakly to strongly calcareous. Lower metre or so contains less hornblende schist and more biotitic sediment. Overall about 40Z mafic, 602 biotite gneiss m: Garnetiferous Band (5d): Coarse garnet aggregates up to l cm in size, in a biotitic schist. QUARTZ-FELDSPAR-BIOTITE-HORNBLENDE GNEISS (5b-lc) Medium grey with dark green and dark brown, bands and laminae, somewhat massive poorly banded, weakly calcareous, minor calcite veins BLEACHED ZONE Light g rey, f ine g rained, m assive poorly banded, moderately schistose, small b iotite nae. Vague feldspar crystals, weakly calcareous, a few thin bands l cm 5 cm quartz eye sericite schist ONTARIO GEOLOGICAL SURVEY ASSESSMENT FILES RESEARCH OSFICL- MAY 2 y RECEIVED QUARTZ-FELDSPAR-BIOTITE GNEISS (5b) Dark grey, fine grained, thickly to thinly banded, thin cherty laminae, moderately calcareous. HORNBLENDE-FELDSPAR GNEISS (le) Dark greenish black, fine grained, massive, weakly calcareous, occsional quartz calcite veins. Angle of foliation to core axis 75 O at 171 m. END OF HOLE metres

19 Ontario ^ Ministry of Se'l'rces Report "Wo* Name a^^kpstal Address of Recorded Holder TYLO^PRE SOURCE s CORPORTATION,:.\., l, v - ^ c ' v,v. U, l. C- i- ^ Z 42C13SE WABIKOBA LAKE The Mini 300 vobc:,- iijj Prospector'* TCAnce No7 T1298 Suite Howe Street, Summary of Work Performance and Distribution of Credits Total Work Days Cr. claimed for Performance of the following work. (Check one only) Vancouver, British Columbia V6C 2T6 Q Manual Work t Sinking Drifting or "other Lateral Work. ]Compressed Air, other Power driven or mechanical equip. j Power Stripping J Diamond or other Core drilling l Land Survey All the work was performed on Mining Claim(s): Required Information eg: type of equipment, Names, Addresses, etc. (See Table Below) Hole No. Az. Dip TY " Footage 439.6' Core Size Dates Claim drilled on NQ Jan. 4-8, TY-03A ' NQ Jan. 9-11, Drilled by Midwest.Dialling; tf trm jpegj LfMSfl -,l OGiCflL SoRVtY ASSESSMENT FILES i l RESEARCH GXr-'iCLi MAY o ifjwta -THUNDER BAY ir* ^^ REG E 1 V E D 7lftl9llOll^l^ i ' ' Certification Verifying Report of Work Date of Report May 14, 1986 Recordjjd Holder or Agerit (Signature) ^J^^-^C^y^^^ t hereby certify that l 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 true. Name and Postal Address of Person Certifying Peter Cooper, Bag Service #8, Marathon, Ontario POT 2EO Date Certified May 14, 1986 Table of Information l Attachments Required by the Mining Recorder Certified by (Signat 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 Stripping 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, "lumber 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/stripping 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 Lsnct Survey Name and address of Ontario land surveyer. Nil Nil

20 ROUS LAKE G-611 l o i -lw SS^'/'Jl X LORNA LAKE G-598 j i** "5T -P" 5T~ ~ i"? -i i ^ -i oo H t "IS m i t ro ' ^ "Mr " WHITE LAKE (N. PT.) G-622

21 WABIKOBA LAKE: i * * YjjD BTRtC MINING DIVISI6N-* MINING DIVISION

22 Theresa Lake Solong Lake C 100 l^of metres f i i i i i SCALE KOBA LAKE 220 REVISED PROJ N? INC.. NTS DWGN? DIAMOND DRILL HOLE l OCATION PROJECT TYLOX J.V. PL AN Surveyed by NorandO Date Fet), I Q 86 Drawn by. vj COflPOn Scale l 5QQQ noranda NORANDA EXPLORATION CO. LTD - Wl NNl PEG