Canyon property, southeastern Yukon

Galena and pyrrhotite occur in manganese-stained quartz-carbonate breccia beneath rusty limestone. Surface geology of the area suggests that the mineralization is a replacement of brecciated limestone in the footwall of a low-angle fault. Results from previous exploration have proved disappointing but the host structure is probably regional in extent and larger deposits may exist along strike.

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Champ Valeur
Dernière modification avril 17, 2026, 21:20 (TU)
Créé le avril 17, 2026, 21:20 (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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