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Abstract

Shear-wave splitting (shear-wave- bi-refringence) diagnostic of some form of azimuthal anisotropy is widely observed in all types of rock in the uppermost 15km of the Earth's crust (Crampin and Lovell 1991).

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/content/papers/10.3997/2214-4609.201409354
1995-05-29
2024-09-15

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