Zinc-Rich Massive Sulphides Confirmed East of Garibaldi's E&L Deposit

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[{"type":"text","content":"\n\n\n\nZinc-Rich Massive Sulphides Confirmed East of Garibaldi's E&L Deposit\n\n/* Style Definitions */\nspan.prnews_span\n{\nfont-size:8pt;\nfont-family:\"Arial\";\ncolor:black;\n}\na.prnews_a\n{\ncolor:blue;\n}\nli.prnews_li\n{\nfont-size:8pt;\nfont-family:\"Arial\";\ncolor:black;\n}\np.prnews_p\n{\nfont-size:0.62em;\nfont-family:\"Arial\";\ncolor:black;\nmargin:0in;\n}\n\n\n\n\n\n\nZinc-Rich Massive Sulphides Confirmed East of Garibaldi's E&L Deposit\nCanada NewsWire\nVANCOUVER, Oct. 28, 2016\n\n\n\nTSXV: GGI OTC: GGIFFFrankfurt: RQM\n\n\n\nVANCOUVER, Oct. 28, 2016 /CNW/ - Garibaldi Resources (TSX.V: GGI) (the \"Company\" or \"Garibaldi\") is pleased to report that recent regional sampling of several sulphide and precious metal occurrences has returned exceptionally high zinc values and highly anomalous gold and copper at the new Brass Hill target within the Company's expanded E&L Project. Brass Hill is 2.7 km northeast of the E&L Ni-Cu-Au deposit at Nickel Mountain in northwest B.C.'s prolific Golden Triangle.\n\nThe newly-acquired Brass Hill area rests along faults trending east-west toward the E&L Ni-Cu-Au deposit and the associated \"Q\" magnetic anomaly which remains untested below the massive sulphide outcrop. Located in a volcanogenic setting that's geologically distinct from the nickel-rich massive sulphide system to the southwest, Brass Hill forms what Garibaldi is now referring to as E&L \"East\" which is about 15 km southwest of Eskay Creek.\n\nSteve Regoci, Garibaldi President and CEO, stated: \"Brass Hill helps confirm the geologically robust diversity of this very under-explored area which covers the 23 sq. km E&L Project, highlighted by the Ni-Cu-Au deposit we're advancing at Nickel Mountain where detailed progress updates are expected soon. Much has been overlooked the last 50 years in this rich district, and we're taking full advantage of that.\"\n\nThe impressive outcrops at Brass Hill feature a cluster of mineralized surface showings of different styles in close proximity to one another, while the potential scale of a mineralized system or systems has expanded due to a nearby receding glacier. Significantly, for the first time, this area and these showings discovered in the late 1980's are being systematically investigated for extent and continuity of mineralization.\n\nChip Sam...

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