Frequency dependence of anisotropy in fluid saturated rocks – Part I: aligned cracks case

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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...

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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/20.500.11937/10340

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