Crustal velocity structure in the southern coast belt, British Columbia, from a seismic refraction survey
The Coast Belt is one of five morphogeological belts of the Canadian Cordillera. It was created through the complex tectonic processes that accommodated the Mesozoic accretion of the allochthonous Insular superterrane to the Intermontane superterrane, then the leading edge of western North America,...
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| Format: | Others |
| Language: | English |
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2008
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| Online Access: | http://hdl.handle.net/2429/2547 |