Structure of the Cascadia subduction zone off Vancouver Island : new evidence from seismic refraction data
The Cascadia subduction zone forms the present convergent margin between the North American plate and the oceanic Gorda, Juan de Fuca and Explorer plates from approximately 40°N to 50°N. This thesis examines a subset of the offshore-onshore seismic refraction/wide-angle reflection data recorded d...
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| Format: | Others |
| Language: | English |
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2009
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| Online Access: | http://hdl.handle.net/2429/7688 |