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...
| Main Authors: | , , , |
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| Other Authors: | |
| Format: | Conference Paper |
| Published: |
EAGE
2013
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| Online Access: | http://www.earthdoc.org/publication/publicationdetails/?publication=73419 http://hdl.handle.net/20.500.11937/15342 |