Abstract: 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.

Authors: Bremner, T. and Liverton, T.

Map Scale: 1 : 0

NTS Mapsheet(s): 105B03

Citation: Bremner, T. and Liverton, T., 1991. Dan property, south Yukon. In: Yukon Exploration 1990, Yukon Exploration and Geological Services , Indian & Northern Affairs Canada/Department of Indian & Northern Development: Exploration & Geological Services Division.

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