Anisotropy pattern arising from application of a triaxial stress to a dry isotropic rock

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Anisotropy pattern arising from application of a triaxial stress to a dry isotropic rock

Elastic wave velocities in rocks vary with stress due to the presence of discontinuities and microcracks within the rock. We analytically derive a model for seismic anisotropy caused by small triaxial stresses applied on a linearly isotropic elastic medium permeated by a distribution of cracks with...

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Bibliographic Details
Main Authors:	Gurevich, Boris, Collet, O., Pervukhina, M., Madadi, M.
Other Authors:	EAGE
Format:	Conference Paper
Published:	EAGE 2013
Online Access:	http://www.earthdoc.org/publication/publicationdetails/?publication=73419 http://hdl.handle.net/20.500.11937/15342

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