Frequency dependence of anisotropy in fluid saturated rocks – Part I: aligned cracks 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 mode...
| Main Authors: | , |
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| Format: | Journal Article |
| Published: |
Wiley-Blackwell
2016
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| Online Access: | http://hdl.handle.net/20.500.11937/10340 |