1887

Abstract

Since the Earth is elastic, it is worth the computational burden to process multicomponent data for elastic phenomena with fully coupled time-domain wave-equation propagators. At every time sample in the back-propagated model domain, the complete wave fie

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/content/papers/10.3997/2214-4609.201400143
2009-06-08
2021-10-21
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400143
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