Originally posted by Anonymous
The mineralization in the Wendlandt Mine area occurs as epithermal
disseminations of pyrite and arsenopyrite with subsidiary silver sulphides,
silver and gold tellurides, and chalcopyrite in structurally controlled quartz
veinlets which are hosted by silicified rhyolite porphyry dykes, a rhyolite
porphyry plug, quartz diorite dykes and a silicified rhyolite breccia. Fury
geologists noted that an obvious surface oxidized area with a diameter of
approximately 300m surrounds the area of the old mines.
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