Frequency dependence of anisotropy in fluid saturated rocks - Part II: Stress-induced anisotropy case

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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...

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Bibliographic Details
Main Authors:	Collet, O., Gurevich, Boris
Format:	Journal Article
Published:	Wiley-Blackwell 2016
Online Access:	http://hdl.handle.net/20.500.11937/44414

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