1887

Abstract

Changes in shear-wave splitting before earthquakes are now observed routinely at large distances whenever appropriate source-receiver-earthquake geometries exist.

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/content/papers/10.3997/2214-4609.201407618
1999-06-07
2020-04-03
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201407618
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