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Location: 10 km SE from Greenwood, British Columbia, Canada
888 Dunsmuir Street, Suite 888VancouverBritish Columbia, CanadaV6C 3K4
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Mining scale, mining and mill throughput capaciites.Full profiles of select mines and projects.
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The Lexington-Grenoble Deposit is a porphyry-hosted, high-sulphidation gold/copper pyritic sheeted stockwork. There is a strong affinity to a porphyry copper hydrothermal system by virtue of its fluid composition and alteration but strongly influenced by structure.The geological setting of the Lexington Property is dominated by a major 600 m wide tectonic shear zone, the No. 7 Fault. The Lexington-Grenoble Deposit is focused above or at the Lower Serpentinite/Dacite contact (a subthrust of the No. 7 Fault) and is composed of massive pyritelesser chalcopyrite (and rarely magnetite) veins, veinlets and disseminations. The series of shallow to moderately dipping en echelon overlapping sheeted massive sulfide zones, stringers and disseminations are hosted within the basal 25 m of a dacitic pyroclastic unit to the “Dacite” unit, confined to an area 525 m along its long axis, 20-60 m wide normal to the long axis and 25 m thick vertically.
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