Frequency dependence of anisotropy in fluid saturated rocks - Part II: Stress-induced anisotropy case
A major cause of attenuation in fluid-saturated media is the local fluid flow (or squirt flow) induced by a passing wave between pores of different shapes and sizes. Several squirt flow models have been derived for isotropic media. For anisotropic media, however, most of the existing squirt flow mod...
| Main Authors: | , |
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| Format: | Journal Article |
| Published: |
Wiley-Blackwell
2016
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| Online Access: | http://hdl.handle.net/20.500.11937/44414 |