Active deformation of the Cascadia forearc : implications for great earthquake potential in Oregon and Washington
Nine west-northwest-trending faults on the continental margin of Oregon and Washington, between 43° 05'N and 470 20'N latitude, have been mapped using seismic reflection, sidescan sonar, submersibles, and swath bathymetry. Five of these oblique faults are found on both the Juan de Fuca and...
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| Language: | en_US |
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2013
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| Online Access: | http://hdl.handle.net/1957/36664 |