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.

Data and Resources

Additional Info

Field	Value
Last Updated	April 17, 2026, 22:11 (UTC)
Created	April 17, 2026, 22:11 (UTC)
contact_email	eservices@gov.yk.ca
contact_person	{"en": "Yukon Geological Survey", "fr": "Yukon Geological Survey"}
criticality_level	[]
data_dictionary	[]
geographic_scope	[]
open_canada_collection	federated
open_canada_date_published	2011-04-04 00:00:00
open_canada_keywords	{"en": ["ygs-import", "ygs-import-20250711", "ygs-publications", "yukon-geological-survey"], "fr-t-en": ["importation d'ygs", "ygs-import-20250711", "publications de l'YGS", "enquête géologique du yukon"]}
open_canada_subject	["science_and_technology"]
sensitivity_level	unrestricted
title_fr
update_frequency	unknown