Compressional wave dispersion due to rock matrix stiffening by clay squirt flow

Abstract The standard Biot‐Gassmann theory of poroelasticity fails to explain strong compressional wave velocity dispersion experimentally observed in 12 tight siltstone with clay‐filled pores. In order to analyze and understand the results, we developed a new double‐porosity model of clay squirt fl...

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Bibliographic Details
Main Authors: Jing Ba, Jianguo Zhao, José M. Carcione, Xingxing Huang
Format: Article
Language:English
Published: Wiley 2016-06-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1002/2016GL069312
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