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Thursday, 02/18/2021 9:17:03 AM

Thursday, February 18, 2021 9:17:03 AM

Post# of 491
$ASKDF Silver mineralization occurs in quartz and carbonate veins intersecting felsic to mafic lavas and locally in massive sulphides. These volcanics belong to the Landrienne Formation. The mineralization is mainly in the form of sulphides (pyrite, chalcopyrite, pyrrhotite) disseminated in quartz and carbonate veins and also locally in the form of lenses of massive sulphides.