*/#+#OWc9 7ܽ+/UW@?{ N#@HHqxAY@=N@QFPMedium grey/green quartz feldspar porphyry dyke.} KL-15-285 ףp=N@p= SR@GRDTrace to weak potassic/propyllitic altered granodiorite.~ KL-15-285p= SR@RS@GRDModerate phyllic envelope around a polymetallic quartz/carbonate/sulphide breccia. Phyllic alteration transitions to argillic/potassic/propyllitic and potassic/propyllitic alteration distally from breccia. KL-15-285RS@QS@GRDTrace to weak potassic/propyllitic altered granodiorite. Conact brecciat at dyke contact. KL-15-285QS@GzU@QFPSilicified grey/brown quartz feldspar porphyry dyke. KL-15-285GzU@fffffV@GRDSilicified patchy moderate argillic/potassic and potassic/propyllitic altered granodiorite. Contact breccia at dyke contact. KL-15-285fffffV@GzW@GRDWeak to moderate potassic/propyllitic altered granodiorite with patchy moderate argillic alteration. KL-15-285GzW@{GY@GRDMineralized fault(?) zone. Silicified moderate phyllic/propyllitic with large moderate to intense patches of gouge alteration. Much of the gouge alteration hosts disseminated pyrite along with a few quartz/sulphide veins. Interval is rubbly. Patchy trace KL-15-285{GY@33333\@GRDWeak to moderate propyllitic and weak phyllic altered granodiorite with large patches of strong gouge alteration. KL-15-28533333\@)\x]@QFPGouge altered silicified orange/grey quartz feldspar porphyry dyke. Sporadic rubbly patches. KL-15-285)\x]@)\^@GRDSilicified moderate phyllic and weak propyllitic altered granodiorite with patchy moderate to strong gouge alteration. Occasional rubbly patches. KL-15-285)\^@ _@GRDFaulted(?) mineralized Central BYG vein zone. Strongly gouge altered, silicified strong phyllic altered granodiorite hosting ~3 polymetallic quartz/carbonate/sulphide with disseminated to blebby pyrite in the granodiorite between them. Silicification and KL-15-285 _@)\a@GRDSilicified moderate phyllic/propyllitic altered granodiorite with the occasional patches of argillic/potassic alteration. Hosts multiple quartz/carbonate/sulphide veins. KL-15-285)\a@Rib@GRDTrace to weak potassic/propyllitic altered granodiorite with patchy moderate propyllitic alteration. KL-15-285Rib@c@GRDModerate phyllic/propyllitic with patch argillic/potassic alteration. Hosts occasional quartz/carbonate/sulphide veining and alarge zone of gouge alteration. KL-15-285c@Qd@GRDModerate argillic/potassic and weak propyllitic altered granodiorite. Rubbly in patches. KL-15-285Qd@yd@GRDStrongly gouge altered and rubbly fault zone(?) consisting what appears to be primarily moderate propyllitic/potassic altered granodiorite. Gouge obscures rock texture. KL-15-285yd@p= e@GRDTrace to weak potassic/propyllitic altered granodiorite with small propyllitic/phyllic halos around milky white quartz veining. KL-16-308 ףp= @OVBOverburden KL-16-308 ףp= @= ףp=@OVBHeavily weathered, oxidized, and broken down granodiorite. KL-16-308= ףp=@Q&@GRDGranodiorite alternating between patches of weak propylitic alteration and patchy oxidation. KL-16-308Q&@(\1@QVNArgillic/phyllic altered granodiorite with a 6m quartz vein zone intersecting at 5-7 *TCA. Quartz vein displays strong oxidation in patches, which has begun to pit out both mineralization and fractures and joints. Flooded quartz zone contains crosscuttin KL-16-308(\1@(\2@QFPBrown quartz feldspar porphyry dyke. Dyke displays patches of moderate oxidation, and geothite formation along micro fractures within dyke. Dyke contact hosts blebby galena. KL-16-308(\2@(\3@GRDQuartz flooded granodiorite with moderate patchy oxidation and propylitic alteration. KL-16-308(\3@4@FLRExtremely broken down zone of tan fault gouge. Gouge resembles extremely soft clay.  KL-16-3084@@N@GRDPatchy zones of granodiorite alternating between weak to moderate propylitic argillic alteration, weak to moderate argillic/phyllic alteration, moderate argillic alteration, argillic/potassic alteration, and unaltered granodiorite. Patchy zones of modera  KL-16-308@N@(\N@QFPStrongly gouge altered Dyke contact  KL-16-308(\N@GzP@QFPHighly fractured tan quartz feldspar porphyry dyke that has undergone moderate to high silicification. Dyke displays weak to moderate gouge alteration throughout.  KL-16-308GzP@HzgQ@QFPHighly fractured tan quartz feldspar porphyry dyke that has undergone moderate to high silicification. Dyke displays weak to moderate gouge alteration throughout, as well as weak to slightly moderate gouge alteration.  KL-16-308HzgQ@33333R@GRDHighly faulted and gouge altered granodiorite. Granodiorite has undergone phyllic alteration (impossible to distinguish intensity, but green colour and associated mineralization present), strong quartz flooding, and silicification, but gouge alteration KL-16-30833333R@ ףp=R@SILBrown silicious dyke. Zone of competent rock within heavily faulted and gouge altered granodiorite. KL-16-308 ףp=R@ ףp=*U@GRDSeverely faulted and gouge altered granodiorite. Granodiorite shows patchy moderately argillic altered with trace phyllic overprinting, that alternate with strong to intense quartz flooding and silicification. A portion of tranned to brown quartz feldspa KL-16-308 ףp=*U@RV@GRDGranodiorite that has been weakly quartz flooded. Granodiorite displays patchy weak to moderate phyllic, argillic/phyllic, and propylitic alteration throughout. KL-16-308RV@QNZ@GRDModerate to strongly gouge altered granodiorite. Granodiorite shows patchy rubble zones. Quartz veins intersects phyllic altered granodiorite with blebby galena. KL-16-308QNZ@Q`@GRDAlternating patches of altered granodiorite. Alteration ranges from moderate argillic/phyllic, moderate to strong propylitic, and moderate to strong propylitic/phyllic altered granodiorite. Moderate to strong quartz flooding and silicification is present KL-16-308Q`@a@GRDUnaltered granodiorite. Contains carbonate joint infill. KL-11-025Gz@OVBOverburden, scattered granodiorite cobbles and boulders throughout. DDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDDD KL-11-025Gz@Q@GRDStrongly Oxidized Clay Altered Granodiorite. KL-11-025Q@333333D@GRDUnaltered Granodiorite. Moderatly oxidized and limonite tsained along fracture surface. KL-11-025333333D@QEF@GRDClay Altered White purple Green Granodiorite. Heamatite staining varies from weak to strong throughout the interval. KL-11-025QEF@= ףp=J@GRDStrongly Phylic and Clay Altered Green Yellow Granodiorite KL-11-025= ףp=J@{GP@GRDStrongly Pyllic Altered Granodiorite with weak to strong amounts of clay alteration throughout the interval. High abundance of black breccia throughout the interval. KL-11-025{GP@q= ףQ@QFPTan Grey Quartz Feldspar Prophyry Dyke. Vuggs ~1-4cm wide, are scattered throughout the interval and have tiny quartz(?) crystals forming in them. KL-11-025q= ףQ@p= Q@GRDPhyllic and Clay altered Granodiorite with patches of strong clay alteration. KL-11-025p= Q@V@GRDWeak to Moderate Phyllic altered Grey Green Granodiorite. White quartz stringers are present throughout the interval. Phyllic envelopes areound some of the stringers. KL-11-025V@̬W@QFPTan Green quartz Feldspar Porphyry Dyke zone of dark grey purple alteration for approx 2m in the center of the interval. KL-11-025̬W@zG1\@GRDPhyllic and Clay Altered Granodiorite. Phyllic and clay alteration intensity vary throughout the interval. Pyrite mineralization occurs in the more phyllic areas. KL-11-025zG1\@Qn\@GRDSilica Altered Stringly Phyllic, Vuggy Granodiorite. Contains Moderate- strong amounts of disseminated pyrite. Black sulphide veinlets are abundant throughout the interval. Light orange quartz carbonate veinlets in the center of the interval form a whis KL-11-025Qn\@RQ]@QFPTan Green Quartz Feldspar Porphyry Dyke. The dyke contains areas of weak to fair clay alteration. KL-11-025RQ]@33333c]@GRDIntensely Silicified Granodiorite. Light orange quartz veins form a net texture in the center of the interval. KL-11-02533333c]@̬]@GRDModeratly silicifed, strongly phyllic altered granodiorite. Fair to strong amounts of disseminated pyrite and pyrite blebs throughout the interval. KL-11-025̬]@p= S^@GRDPhyllic and Clay Altered Green Orange Granodiorite KL-11-025p= S^@Hz`@GRDClay and Phyllic Altered Granodioirte. KL-11-025Hz`@= ףp`@QFPTan Brown Quartz Feldspar Prophyry Dyke. Upper and lower contacts of the interval have been strongly clay altered. It contains a high abundance of grey quartz veinlets and stringers in the second half of the interval. They branch out in all directions an KL-11-025= ףp`@HzWa@GRDAlternating Grey/Dark Green propylitic Altered Granodiorite and Yellow/Green Phyllic envelopes surrounding veins and veinlets.U,U,6UG^60ŕ^-z@ -z}A!P{4A!G6G}`H W6GO|Gx @}O|}.;}` X`Q& ;E&9ƙQ %ƙ,9 Ѐ9 ,F G F + 64 +   Bi   [- <52i8 O^~52ࣤ<Xd6ࣤ%h3m%UuU+o{+i& Vi&{;vȁ$A{;vqΞ؁&pΞM~Aq|~AA3M &31A~1(*D8@ JHD8.[Xi.[krxh\\rxk h! ݤhV"V*#5R*@$Ђ3@'%j'7&#"07&];'.I];pV&(wYpV>)0 ͶH>*P(33 H) Ͷ+xĒ ) ! ,Ҡ ǥ =Ъ !-L =Ъ ǵ .^ qǵ ˢ / ~ 1| ˢ0ЃYT | + 11 Y+  2 0*  ]oG 3vS doG l~_ ]4(| ~_ lٝ l5@ ,ٝ  l6PO7  1De 7h/ -De  18 p"{4"N#9n*|4":ܛ|<^; '-AJ<^ ǜ\<؄qMǜ\   =*   -d >& -d oN ?Χ oN O @ } O0  A00 BH(*gLCX#L3DpJ [%3E\6%6[F~96*3<GQ*3<igHUlyigfIЅyf1gJ_gʿ1K'3ʿs#L ;Us#4yNM("!% t!N8eҤ OPҤ SP`\mSU  QxŚ &URn&S {gUT0`caLqtUІ.qHLVHo vW  v .o X_ .  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