Structural geology of part of the Crooked Lake area, Quesnel Highlands, British Columbia
The Crooked Lake area, which lies at the boundary of the Omineca Crystalline Belt and the Intermontane Belt of the Canadian Cordillera, has been examined with close attention being paid to the detailed structural relations of the five lithologies that comprise this map area - the late Proterozoic Sn...
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| Language: | English |
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University of British Columbia
2010
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| Online Access: | http://hdl.handle.net/2429/25855 |