Business
Norseman Silver Inc. Updates on Silver Switchback Property in British Columbia
(TheNewswire) Vancouver, British Columbia - TheNewswire - November 6, 2020 ...
About this update from Fitzroy Minerals Inc
[{"type":"text","content":"Norseman Silver Inc. Updates on Silver Switchback Property in British Columbia\n \n \n (TheNewswire)\n \n \n \n Vancouver, British Columbia -\n \n \n TheNewswire -\n \n \n November 6, 2020\n \n - Norseman Capital\nLtd. (TSXV:NOC) (\"\n \n Norseman\n \n \" or the \"\n \n Company\n \n \") is pleased to an announce that it has\ncompleted its initial program on the Silver Switchback (the\n \n \"the Property\n \n \").\nExploration was conducted across the property adding to the geologic\nunderstanding across the property.\n \n \n \n \n A total of 444 soil samples and 50 rock samples have been collected\nduring this campaign on Silver Switchback. The Longford Exploration\nfield crew was composed of 5 person field crew who conducted\nprospecting, mapping and soil sampling. This program was designed to\nbuild on the anomalous and prospective findings of the previous\nexploration conducted on the property and further prospecting of the 3\nMinfile occurrences on the property (Silver Switchback, Snowflake,\nKitnayakwa River). New access continues to be created through\nadditional forestry operations reducing cost and creating increased\nexposure which was how the main showing was originally discovered on\nthe property.\n \n \n The property is located 55Km east-southeast of Terrace, BC in the\nStikine terrane. The rocks on the property are of the Hazelton Group\nvolcanics and sedimentary rocks. To date, only Limited reconnaissance\nprograms have been conducted on the property, which include a small,\nanomalous for Cu and Ag, soil grid over the northern portion of the\nSwitchback Showing. The outcrop sampling includes samples that assays\nreturned 626.3 g/t Ag and 4.39% Cu located roughly in the center\nportion of the claims (and the showing) and 138 g/t Ag and 4.02% Cu in\nan outcrop approximately 100m to the north.\n \n \n Volcanic Redbed Copper (VRC) deposits occur as concordant and\npeneconcordant disseminated crosscutting vein and fault-controlled\ncopper sulphide and/or native copper deposits in predominantly\nsubaerial volcanic sequences. Mineralization can typically be\ncomprised of chalcopyrite, chalcocite, bornite covellite and/or native\ncopper which contain silver, this style of mineralization is distinct\nfrom VMS deposits. Common textures and structures are open space\nfilling, vein and veinlets, replacement, disseminated and l...