Dan property, south Yukon

Massive black sphalerite occurs with pyrrhotite and magnetite in up to 3 irregular but roughly concordant layers at the contact between massive white marble and hard green and white-banded meta-tuff. The mineralization is believed to have replaced brecciated marble in the footwall of a south-dipping thrust fault which passes through the DAN prospect and extends through the Crescent Lake area 5.8 km to the east.

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Éditeur

Producteur Yukon Geological Survey


Renseignements sur la publication

Licence Open Government Licence - Yukon
Date de publication 2011-04-04
Date de mise à jour 2011-04-04


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Étiquettes