DIAMOND DRILLING. CLAIM Ho. HOLE No. FOOTAGE DATE NOTE NOTES: (D # (2) # July/81 July/Bl. TOWNSHIP: Lendrum REPORT No,: 11
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1 DIAMOND DRILLING 42C02SWe301 LENDRUM!eel LENDRUM 010 TOWNSHIP: Lendrum REPORT No,: 11 WORK PERFORMED BY: Algoma Steel Corp. CLAIM Ho. HOLE No. DATE NOTE SSM SSM MB-5-81 MB July/81 July/Bl (D (2) NOTES: (D # (2) #108-81
2 ALGOMA ORE DIVISION P0Q* l el 6 EXP LORATION PROPERTY' MICHIPICOTEN BASE METALS - ANOMALY #7B DIAMOND DRILL HOLE NO. MB-5-81 COORDINATES OF COLLAR At L 40 H B: S AZIMUTH AT COLLAR DIP AT COLLAR ELEVATION at 200' at 310' HOLE LENGTH 309 feet CORE SIZE AQ STARTED July 6, 1981 FINISHED juiy 7, 198i LOGGED BY B. J. 7693^ SUMMARY LOG oz/ton oz/ton O ' Boulders^ ' Andesite Flow Flow Top Sediments CA to pyritte, O to 5% pyrrhotite % pyrrhotite, 5% pyrite i pyrrhotite, 2% pyrite ' ' Andesite Flow Interflow Sediments % pyrrhotite, 4% pyrite, 25i vein quartz ' 309.0' 5 Andesite Flows with 6" to 7.5' of interflow sedimentary beds. END OF HOLE S. S. MARIE MINiNG DIV. E8EIV E AM
3 ALGOMA ORE DIVISION 'ihe ALGOMA STEEL CORPORATION, LIMITED 2 of EXP LORATION PROPERTY* M ICHIPICOTEN BASE METALS - ANOMALY *7B DIAMOND DRILL HOLE NO. MB-5-81 COORDINATES OF COLLAR A' L 40 W B: S AZIMUTH AT COLLAR 3530 DIP AT COLLAR -450 ELEVATION HOLE LENGTH 309 feet CORE SIZE AQ STARTED July 6, 1981 FINISHED July l, LOGGED BY R. J. Rupert ' 309.0' Casing AW Core AQ Core ' * Boulders - andesite, granite,' chlorite schist Andesite Flow ' Pale grey to gray, fine grained andesite with calcite amygdules. Amygdule size decreases to 39.5*. Colour darkens and chlorite conten increases to 39.5'. Lower contact gradational and patch from 37.5 to 41.5' with l" 0 angulir carbonate-quartz amygdules ' Dark grey, green chloritic, schistose-andesite. Ainygdules decrease in size to 52.0'. Weak chloritic banding and pyrite in sections suggest pillow selvages. ^ 1/2* pyrite. CA on schistosity 70O ' Transition zone 2* pyrrhotite, minor pyrite at 58.
4 CONTINUED ALGOMA ORE DIVISION 3 ol 6 PROPERTY MICHIPICOTEN BASE METALS - ANOMALY #7B DIAMOND DRILL HOLE NO MB ' Flow Top Sediments and included andesite ' Dark green schistose banded chloritic netagreywacke and pebbly netagreywacke. Pebbles are quartz and andesite, 1/8" to 1/2" angular. D-15% disseminated fine grained to medium grained cubic pyrite. Average B \ pyrite. D-5% pyrrhotite, fine grained in seams and as rims around clasts or pyritic cubes. CA 600 to 750 on banding ' Pale grey amygdalar andesite. 72.8' bleached ' ' ' ' ' Laminated brown siltstone and Chloritic shale. A few siliceous bands. 20i pyrrhotite, S \ pyrite CA 750 to 800 Amygdular grey andesite As from ', but less chloritic laminae. ls-40% pyrrhotite, average 25% pyrrhotite, 2% pyrite Medium grained andesite Dark grey, banded choritic schist 4% pyrrhotite, l i pyrite 72,5-74.Q
5 CONTINUED Pool 4 of 6 ALGOMA ORE DIVISION PROPERTY MICHIPICOTEN BASE METALS - ANOMALY #7B DIAMOND DRILL HOLE NO MB-5-81 FOOTAOE ' Andesite Flow, amygdular O 1 Pale grey ' Chloritic seams and alteration. "Reverse dalmationite" 2% pyrite, 3% pyrrhotite ' Page grey, fine grained, amygdule r ' Coarse amygdules 1/8" to 1/2" loi g Chloritic bands with pyrite crysi als CU pyrite ' Paler colour. Chloritic bands (selvages) at 6" to 2' spacing with pyrite, <l% pyrite ' Auto breccia, l" fragments ' 1\ pyrrhotite Selvages of chlorite, pyrrhotite and quartz at 2'-4' intervals, Average 2i pyrrhotite, J.% pyrite Pyrrhotite in l" salvages up to 40* ' Flow top breccia. Fragments to 6". Chloritic matrix. C i \ c ubic fine grained to mediui grained pyrite. < \\ pyrrhotite ' ' Amygdular Pillow breccia with chloritic streaks Interflow Se d i mentis, greywacke, siltstone and chert Greywacke. Fragments of quartz and andesite to V long by V wide, 2-3i fine grained leucoxene Very fine grained to very coarse grained grain size, about 50% chloritic matrix % contorted laminae and shartstone fragments of buff clayston or siltstone, 10i chert laminae and fragments, 20% quartz fragments in a matrix of chlorit* pyrrhotite and pyrite <:2% pyrrhotite % pyrrhotie, 5% fine grained p} % ^ein quartz, coarse grained 10% pyrrhotite rite
6 CONTINUED.. ALGOMA ORE DIVISION Pog* 5 of 6 PROPERTY MICHIPICOTEN BASE METALS - ANOMALY #7B DIAMOND DRILL HOLE NO MB ' Andesite Flow Pale grey to creamy coloured, very fine grail ed to fine grained andesite. Becomes darker towards 167.5' ' Banded, contorted chert. ^ pyrrhotite * pyrite CA ' Ditto, Andesite Flow Interflow Sediments, Greywacke Laminated claystone, siltstone, chert ' Laminated brown claystone and chert. CA 75O-85O Coarse grained grades to buff laminated siltstone at 183.5' ' ' ' Massive medium grained to fine grained Andesite Flow Pale grey to gray. Occasional chloritic bands and possible flow structures. From 222.0' there are fine araygdules and probable chloritic selvages. Green, chloritic Laminar Schist CA on banding 75O CA on schistosity 85O Gradational contacts over 2' widths. Andesite Flow Variable grey to greenish grey andesite. Chloritic selvages 6" to l' wide with quartz carbonate and minor pyrite. Sheared contact at 276.5' with 6" laminar chert fragments and buff siltstone. Andesite Flow As above.
7 CONTINUED.. ALGOMA ORE DIVISION 6 of 6 PROPERTY MICHIPICOTEN BASE METALS - ANOMALY #7B DIAMOND DRILL HOLE NO MB Andesite Flow ' ' Massive fine grained to medium.grained grey andesite. Quartz veinlets from 1/8" to l" with irregular boundaries at 6" to 2' intervals. Ditto with green selvages and inter-pillow (?) breccia textures up to l' long at 2 to 3' intervals 309.0' END OF HOLE t/
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10 ALGOMA ORE DIVISION Pogt l of PROPERTY' MICHIPICOTEN BASE METALS - ANOMALY #7C DIAMOND DRILL HOLE NO. MB-7-81 COORDINATES OF COLLAR A' L 24 W - HOLE LENGTH 703 feet CORE SIZE AQ B: 1+85 N STARTED July 18, 1981 AZIMUTH AT COLLAR Grid South FINISHED July 20, DIP AT COLLAR 300/ LOGGED BY * -310 e 500/-230 g 700 uwuocw D 1 R - ELEVATION O SUMMARY LOG Casing in overburden - muskeg, boulders, sane Banded medium grained to coarse grained biotite-feldspar-quartz schist or gneiss. CA averages approximately 18O on quartz banding, which may be tectonic. Probably metasediments. Chloritic schist. Variable textures with banding on quartz-rich seams at low CA, approximately ' - 2 to 4t pyrite in narrow (1/8") but electronicly continuous seams Sericitic to chloritic rhyolite pyroclastics mainly fine grained tuffs. Laminated chert, iron sulphides, sericitic laminae and very graphitic chlorite. Average approximately B \ pyrrhotite, 4* pyrite, trace chalcopyrite. CA generally 25O to 30O, Phyolitic tuff and lapilli tuff. Disseminati d pyrrhotite and pyrite up to n \ i n short l t( sections at top and bottom. Laminated chert and iron sulphides. Approximately 201 pyrrhotite, 20V pyrite, trace chalcopyrite. Rhyolite - very fine grained to fine grained massive. Quartz porphyry. 40i 2 to 4 mm quartz eyes in fine grained sericitic matrix. Massive aid uniform. END OF HOLE
11 ALGOMA ORE DIVISION Pogt 2 ol PROPERTY' MICHIPICOTEN BASE METALS - ANOMALY #7C DIAMOND DRILL HOLE NO. MB-7-81 COORDINATES A' L 24 W B: 1+85 N AZIMUTH AT COLLAR OF COLLAR Grid South DIP AT COLLAR -400/-390 e 300/ -310 g 500/-230 e 700 ELEVATION HOLE LENGTH 703 feet CORE SIZE AQ STARTED July 18, 1981 FINISHED July 20, 1981 BY R. J. Rupert DETAIL LOG O Casing, no core Biotite-feldspar-quartz gneiss. CA 200 to 250, on bands of quartz spaced a few inches apart - medium grained to coarse grained Dacite or rhyolite dykr? Quartz amygdules Soft biotite-feldspar-quartz gneiss. CA 12 0 to 250, Average 16O. Uniform character. Pale gray biotite-chlorite-schist. Chloritic metacrysts. Dark grey biotite-chlorite, schist becomes more intensely schistose and banded by quartz bands towards 318.0'. Fragmental {tectonic breccia?) banded chlorite schist with bands of quartz grains or broken bands of quartz. CA 310' 180 g 301' ' Transition
12 CONTINUED ALGOMA ORE DIVISION 3 of PROPERTY MICHIPICOTEN BASE METALS - ANOMALY *7C DIAMOND DRILL HOLE NO MB Chloritic schist * - Banded chloritic schist 204 quartz bands CA 200 at 392* ' - Banded chloritic schist 304 feldspar phenocrysts from medium grained to very coarse grained in fine grained chlorite - quartz (biotite?! sq list. CA 39B' on banding 403' 408' ' O 426* contorted CA on schistosity is 5O to 100 higher ' - Ditto. Core is badly broken. Driller reports lost water ' - Ditto CA ' 442' *457.0' - Chlorite-quartz-feldspar schi with no feldspar metacrysts. (5-204) cherty bands 1/8" wid increasing towards 457.0' Banded chloritic schist with cherty bands. Trace pyrite to minor pyrite. About 204 cherty bands to 462', then 304 to 492'. CA 100 g ' 458' 490' Massive chloritic- feldspar schist. No phenocrysts, fine grained. Banded chlorite-quartz-feldspar (biotite?) schist. Approximately 154 quartz bands to 525.0', decreasing to 54 from '.
13 ' CONTINUED.. ALGOMA ORE DIVISION 4 of PROPERTY MICHIPICOTEN BASE METALS ANOMALY #7C DIAMOND DRILL HOLE NO MB-7-81 i j l, i Con d O 1-2* to 4* pyrite in continuous seams up to 1/8" wide. CA 600 to -1QO g 512 to 514' ' - CA IB0 g 527' 532 i 130 e 537' Increasing pyrite in final 6*. j i j i Transition zone Mottled chloritic schist with. 30* 1/8" chloritic spots in sericitic quartz-chlorite schist. CA 547.0' Tuff, felsic. t t j ', J4- - *T" O 1-5* to 25* 2 iron quartz eyes in yrey sericite-chlorite-quar tzfeldspar schist. Massive ( appearance. Lower contact 3" wide at a high angle. l ' - As from ' ' - Pale grey massive to weakly * f foliated fine grained to very fine grained rhyolite. 30* pale brown altered feldspa i Becomes finer downwards. Lowe contact is sharp. Possibly a flow?! Laminated chert, iron sulphides, graphitic laminae and sericitic laminae. CA generally 250 to ' - Laminated talcose sericitechlorite schist with 10* chert laminae to 2 mm increasing to 70* up to 15 mm at end of sect 3* to 10* pyrrhotite, minor py ' - Graphitic laminated chert. 6* pyrite, 3* pyrrhotite, trace chalcopyrite. CA ' Sharpstone breccia from with some sericite schist frac but mainly chert fragments. Transitional from ' f ion. * rite. us- ; nents j. ' l i 1 i
14 CONTINUED ALGOMA ORE DIVISION Pogt 5 of PROPERTY MICHIPICOTEN BASE METALS - ANOMALY #7C DIAMOND DRILL HOLE NO MB-7-B Cor td ' - 80% coarse banded chert. 15* pyrrhotite, 5* pyrite, minor chalcopyrite (C ^*1. Chert bands are discontinuous but at uniform core angles, with interstitial pyrrhotite, pyrite and chalcopyrite. CA apprcoc. 3QO ' - Sericite schist 1Q* canary yellow laminae to 0.5 mm wide. 70* chert laminj to 3 mm wide. 10% pyrrhotite, l* pyrite, trace chalcopyrite ' - Sericitic laminar tuff 301 cherty bands 15* pyrrhotite, 3* pyrite CA 250 to 300 i?,' Rhyolitic pyroclastics ' - Massive to weakly foliated very fine grained rhyolite wit 4* dark.5 mm pyrrhotite spec!s. Buff grey colour Tuff and lapilli tuff. 30* to 80* fragments of quarts and 4hyolite up to l" diametei in a chloritic matrix. *i to l* disseminated pyrite ' - As from ' 12* pyrrhotite, 5* pyrite Laminated chert and iron sulphides * chert laminae up to 4 mm. 10* sericit ic pyrrhotite and pyrite laminae. Estimated 20* very fine grained to fine grained pyrrhot ite, 20* very fine grained to coarse grained pyrit Trace chalcopyrite. Very fine grained to fine grained massive grt y rhyolite which becomes coarser downwards. Porphyry. 40* 2 mm diameter quartz eyes a fine grained sericitic matrix. END OF HOLE
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