1887

Abstract

Azimuthally varying seismic shear-waves splitting is seen with almost identical characteristics in almost all sedimentary, igneous, and metamorphic rocks below about 1 km-depth in the Earth's crost.

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/content/papers/10.3997/2214-4609.201406734
2001-04-30
2020-04-02
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201406734
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