Notes: ( i) - SEE #218/73 NOVA TWP. Township: O F BELFORD Report NQ: 18. Diamond Drilling. Claim N9. Hole NQ Footage Date. Note (D

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1 42B09SWe BELFORD 010 Diamond Drilling wnship: O F BELFORD Report NQ: 18 Work performed by: AMAX POTASH Claim N9 P Hole NQ Footage Date TX ' JULY/73 Note (D Notes: ( i) - SEE #218/73 NOVA TWP. - ALSO SEE REPORT # 17, NOVA TWP. AWL.OO-4(7-69)i v.9-72

2 8 2, /S 1 1, : -l 'l V O S S-VAO/V V) (f? U.( t) t Q.'f/.S X VW LJ TT G ' J. V /V

3 ^o o o TYRTTT ") TV t lc T O Hole NO TX Sliw,f 1 i^no-tt, 346' Property. Nova-3 R^rmjv 168 O Azimuth wnship. rr^balf^ol n;p J500 Lo^j^tion Grid 1 Line 12+OOE nhwtiw test an AEM and 11+OON ground conductor S.N. Watowich T Timmins Logged By - Core Locatioi Remarks M,m.. ronimpn^ July 6, 1973 nip: r^iur 50 r-nmpm^ July HrilUno- Co Bradley BrOS. Ltd. Etch Test Depth Rdg. True Corp SizP M..... rnrfnjrt^tinwnlp All CdSl fig COU.ld not be removed. Location Sketch Jl \ T X ' '*?'73 \ ' ^ Nortti L No P Claii n Scali 1" ' ' Prom Footajje DESCRIPTION Length 0.0 I3b OVERBURDEN clay and fine sand gravel and boulders - MtlAUACilh tine grained, grey, strongly foliated felsic rock; foliation at 50 0 to C. A. FELDSPAR PORPHYRY contact at 600 to C. A /16" sized subrounded white feldspar phenocrysts, very fine siliceous grey matrix METADACITE similar to above; scattered red garnet blebs I-25&; mafic content distinct very fine perhaps amphibole crystals of rock. The light grey colour tone is due to the predominent felsic composition; foliation averages to C. A. ; FELDSPAR PORPHYRY contact 70 0 to C. A.; lower contact 75 0 to C. A. uniform a massive appearance in contrast to the metadacite; similar to , METADACTTF similar to : locallv garnets developed along a band mav form up to 52 of rock. ' FFI.DSPAR PORPHYRY similar to description at

4 189.5 Footajje o C) o METADACITE-META ANDESITE DESCRIPTION rvrtt.t. similar to but garnet content is uniformly increased to ID-15%; qarnet porphyroblasts ranae from 1/16" to 1/4"; mafic content appears sliqhtly increased due to the sliqhtlv darker colour. Length * C* j?ase7 Z?? -S"* Hole J? s-x? S J?/ /S S FELDSPAR PORPHYRY similar to contacts at about 600 to C.A METADACITE similar to garnet content reduced slightly ranging from 5-1 0^; rock is siliceous very fine grained, and coloured grey lost core SILICIFIED AND ALTERED ZONE light, grey, siliceous, narrow 6" bands of feldspar porphyry are silicified and altered bv foliation; locally fine bedded chert-like laminae occur: foliation at 5S0-600 C. A.; rare hair-line cross fractures with carbonate and pvrite; occassional pyrit.p sperlcs GRAPHITIC ZONE this is characterized by massive, black graphite bands containing scattered pyrite grains, nodules and fracture filling; graphite with 102 pyrite lost core massive graphite with IDS pyrite as fracture filling felsic-silicified zone, virtually pure quartz lost core chert zone similar to lost core graphite with 302 felsic inclusions and 32 pyrite felsic-silicified; possiblj^a chert zone massive qarphite with felsic nodules and fragments and pyrite qenerally as fracture fillings and veinlets ? E 5.0 Z./0 /36 /SV JZZ? O.f 0.~7

5 O ro o TVT K "K av-viv T-I V TYDTT T Hole No- Foot 3RC r* o v K i Jr 1 1 U Pi graphite zone - an equally mixed 2one of massive graphite and felsic bands and fragments. The fragments of felsic fragments are more easily discerned hecajt5 p the graphite flows to form the interstices; fragments are up to 3" in length and vary from oval to lensoid in form: pvrite is. negligible lo 2ZQJQ Length 5.0 C*. J2. s^3 - Z^ #*?f* A 70^ ^- c*r-r x?'. /i 5 ///'s*s CHERT ZONE light grey to light tan cherty zone with rare massive 1" to 3" graphite lenses graphite and 302 pyrite as swarms of veinlets. Dvrite is scarce in the chert; the chert is fractured heavily in multiple directions and healed by silica and carbonate pyrite 602 with graphite. "' GRAPHITE ZONE generally massive araohite with pyrite and minor sections of chert mass, graphite with 102 pvrite as nodules and veinlets chert with narrow graphite lenses chert massive graphite with fragments of chert massive graphite with pvrite as nodules pvrite 7one 3?? pyrite 402 graphite pvrite pvrite 402 graphite finely handed and locally fragmented felsic tuff and graphitic sediment: laminae dip from 30 0 to 60 0 to C. A.; crenulated folding is common: pyrite ranges from * '~'~ *7 3?/ 2?3 ^f^o 3 1 S e.(? S f FELSIC TUFF very fine grained, light grey, generally massive less than 12 pvrite. h-.,-

6 Footaee - lyom o o.. -o DIAMOND DRTT.T. RECORD DESCRIPTION GKAPH1IIU ZONh mi- xed fraaments of felsic tuff and massive graphitic bands graphite 80% qraohite 30% qraphite 505S graphite Length 4.0 C*. Z^ /o J r. *f s?es - 2.5'? /3Z0 Hole *f\ '&S7 S*'//. j.ff END OF HOLE. r *

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