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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Info additionnelle

Champ Valeur
Dernière modification avril 17, 2026, 22:11 (TU)
Créé le avril 17, 2026, 22:11 (TU)
contact_email eservices@gov.yk.ca
contact_person {"en": "Yukon Geological Survey", "fr": "Yukon Geological Survey"}
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open_canada_date_published 2011-04-04 00:00:00
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