Lithospheric structure across the Canadian cordillera of Northeastern British Columbia from seismic refraction and potential field data
The region of northeastern British Columbia includes the transition from cratonic North America to the deformed Canadian Cordillera. While geological mapping has progressed for over 120 years in the northern Cordillera, the subsurface has remained terra incognita as few geophysical surveys have b...
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| Language: | English |
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2009
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| Online Access: | http://hdl.handle.net/2429/10539 |