General Information
Abstract: The southwestern Yukon Coast Belt mapping project is a joint Yukon Geological Survey/Geological Survey of Canada initiative operated under Natural Resources Canada’s GEM (Geomapping for Energy and Minerals) program. This project is aimed at investigating the geological relationships and mineral potential of the Kluane Schist, the Ruby Range batholith and the Yukon-Tanana terrane in southwestern Yukon. Bedrock mapping at 1:50 000-scale followed a 400 m line-spaced aeromagnetic survey flown in the winter of 2010. Preliminary results indicate the presence of a northeast-dipping structural stack through an ~40 km-thick crustal section, whereby the Kluane Schist occupies the lowest structural level and the Yukon-Tanana terrane the highest. The Ruby Range batholith intruded along the contact between the Kluane Schist and the Yukon-Tanana terrane, and was emplaced late in the deformation history. An orthogneiss/paragneiss unit of unknown tectonic affinity was mapped structurally between the Ruby Range and the Kluane Schist. Detrital zircon analyses from two samples of Kluane Schist indicate that the onset of deposition for this metasedimentary sequence occurred after ca. 94 Ma. Two significant metamorphic events, dated at 82 and 70 Ma, affected the Kluane Schist. This indicates that original structural juxtaposition between the Kluane Schist and the Yukon-Tanana terrane pre-dated intrusion of the Ruby Range batholith.
Mineral potential in the Coast Belt area is significant and includes porphyry Cu-Mo-Au, epithermal Au-Ag and orogenic Au occurrences. The upper level of the Ruby Range batholith is most prospective for porphyry and epithermal mineralization, while the Kluane Schist is most prospective for orogenic Au mineralization.
Mineral potential in the Coast Belt area is significant and includes porphyry Cu-Mo-Au, epithermal Au-Ag and orogenic Au occurrences. The upper level of the Ruby Range batholith is most prospective for porphyry and epithermal mineralization, while the Kluane Schist is most prospective for orogenic Au mineralization.
Authors: Israel, S., Murphy, D., Bennett, V., Mortensen, J. and Crowley, J.
Keywords: Kluane Schist, mineral potential, orogenic, Ruby Range batholith, Yukon-Tanana terrane
NTS Mapsheet(s): 115G, 115H
Citation: Israel, S., Murphy, D., Bennett, V., Mortensen, J. and Crowley, J., 2011. New insights into the geology and mineral potential of the Coast Belt in southwestern Yukon. In: Yukon Exploration and Geology 2010, MacFarlane, K.E., Weston, L.H., and Relf, C. (eds.), Yukon Geological Survey, p. 101-123.
Downloads
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Report | File is 4.31 MB | Download PDF |
Location Map
NTS Mapsheet(s): 115G, 115H
Related Occurrences
Name | Number | Type | Status |
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Hopper Porphyry Zone | 115H 034 | Hard-rock | Prospect |
Copper Castle | 115H 019 | Hard-rock | Prospect |
Bowen | 115H 053 | Hard-rock | Showing |
Shut | 115H 047 | Hard-rock | Prospect |
Lib | 115H 055 | Hard-rock | Prospect |
Slayer | 115H 071 | Hard-rock | Showing |
Related Compilations
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Related Publications
Number | Relationship | Authors | Title |
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YEG2010 | Contained By | MacFarlane, K.E., Weston, L.H. and Relf, C. (eds.) | Yukon Exploration and Geology 2010 |