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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Bibliographic Details
Main Author: Jamison, Dylan
Format: Master Thesis
Language:English
Published: University of Waterloo 2018
Subjects:
Rae
Online Access:http://hdl.handle.net/10012/13772