1887

Abstract

The analysis of rock anisotropy in terms of seismic velocities and within the context of rock-physics (Biot-Gassmann theory of poroelasticity) provides important information for the evaluation of the stress state (tensors) of rocks, detection of the direc

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/content/papers/10.3997/2214-4609.201400195
2009-06-08
2021-10-19
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400195
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