Rupture models of the great 1700 Cascadia earthquake based on microfossil paleoseismic observations
Past earthquake rupture models used to explain paleoseismic estimates of coastal subsidence during the great AD 1700 Cascadia earthquake have assumed a uniform slip distribution along the megathrust. Here, we infer heterogeneous slip for the Cascadia margin in AD 1700 that is analogous to slip distr...
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| Language: | English en |
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2012
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| Online Access: | http://hdl.handle.net/1828/4167 |