General Information
Abstract: 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.
Authors: Bremner, T.
Map Scale: 1 : 0
NTS Mapsheet(s): 105H01
Citation: Bremner, T., 1991. Canyon property, southeastern 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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| Report | File is 5.41 MB | Download PDF |
Location Map
NTS Mapsheet(s): 105H01
Related Occurrences
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Related Publications
| Number | Relationship | Authors | Title |
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| YEG1990 | Contained By | Yukon Exploration and Geological Services | Yukon Exploration 1990 |
