Canada One Mining Corp
OTC:COMCF
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Canada One Mining Corp
Canada One Mining Corp. operates as an exploration company. The company is headquartered in Vancouver, British Columbia. The company is focused on the exploration of its resource properties in British Columbia and has not yet determined whether its exploration and evaluation assets contain mineral reserves, which are economically recoverable. Its Franelle Copper project hosts four mineralized zones, Franelle, Bennelle, Beluet and Reuben. The Franelle zone trends north northwest approximately 2600 meters (m) along an approximately 7000 m long gabbro dyke with an average width of approximately 60-75 m. Mineralization consists of native copper, and copper oxides and sulfides with some supergene enrichment. The Bennelle zone consists of veins, veinlets and disseminations of copper mineralization intersecting a gabbro sill intruded into arkosic red sandstone. The Reuben zone, a 30 m wide stockwork of gabbro hosting calcite and epidote veins carrying chalcopyrite and malachite and has been traced intermittently approximately 425 m along strike.
Canada One Mining Corp. operates as an exploration company. The company is headquartered in Vancouver, British Columbia. The company is focused on the exploration of its resource properties in British Columbia and has not yet determined whether its exploration and evaluation assets contain mineral reserves, which are economically recoverable. Its Franelle Copper project hosts four mineralized zones, Franelle, Bennelle, Beluet and Reuben. The Franelle zone trends north northwest approximately 2600 meters (m) along an approximately 7000 m long gabbro dyke with an average width of approximately 60-75 m. Mineralization consists of native copper, and copper oxides and sulfides with some supergene enrichment. The Bennelle zone consists of veins, veinlets and disseminations of copper mineralization intersecting a gabbro sill intruded into arkosic red sandstone. The Reuben zone, a 30 m wide stockwork of gabbro hosting calcite and epidote veins carrying chalcopyrite and malachite and has been traced intermittently approximately 425 m along strike.
