Deformation History of the Black Bay Fault, Northwest Territories, Canada
The Black Bay Fault is a major Paleoproterozoic, NE-SW-trending, crustal-scale feature that separates different tectonometamorphic domains of the southern Rae craton in the Canadian Shield. This structure extends from the edge of Lake Athabasca northward for 100’s km into the Northwest Territories a...
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Format: | Master Thesis |
Language: | English |
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University of Waterloo
2018
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Online Access: | http://hdl.handle.net/10012/13772 |