Report (English, PDF)
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- 2026-08-26
The Munson occurrence consists of massive black sphalerite, galena chalcopyrite, pyrrhotite and magnetite exposed in bulldozer trenches on the floor of a cirque. The sulphides are associated with siliceous breccia and actinolite skarn along the contact betweeen siliceous metavolcanic rocks and limestone which also passes through the Mod showing, 2.4 km to the west. The contact appears locally discordant and is interpreted as a steep reverse fault.
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