According to Gustafson, " There is evidence that the ore has been introduced into an old, already folded, rock and has replaced certain favourable layers of that rock, particle by particle, with large tonnages of garnet, rhodonite, fluorite, marmatite ( and wurtzite ), galena, and other minerals that constitute the orebodies . " The Potosi-Footwall Gneiss is found on both sides of the main lode.
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