P-wave dispersion and attenuation due to scattering by aligned fluid saturated fractures with finite thickness: theory and experiment-Reference-Cited by-同舟云学术

P-wave dispersion and attenuation due to scattering by aligned fluid saturated fractures with finite thickness: theory and experiment

Published:2018-10-01 Issue:3 Volume:215 Page:2114-2133
ISSN:0956-540X
Container-title:Geophysical Journal International
language:en
Short-container-title:

Author:

Guo Junxin¹²,Shuai Da³,Wei Jianxin³,Ding Pinbo³,Gurevich Boris²⁴

Affiliation:

1. Department of Earth and Space Sciences, Southern University of Science and Technology, Shenzhen 518055, China

2. WA School of Mines: Minerals, Energy and Chemical Engineering, Curtin University, GPO Box U1987, Perth 6845, Western Australia, Australia

3. State Key Laboratory of Petroleum Resources and Prospecting and CNPC Key Laboratory of Geophysical Exploration, China University of Petroleum, Beijing 102249, China

4. CSIRO, 26 Dick Perry Avenue, Kensington 6152, Western Australia, Australia

Funder

National Key R&D Program of China

National Natural Science Foundation of China

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/gji/article-pdf/215/3/2114/27719174/ggy406.pdf

Reference61 articles.

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2. Rock anelasticity due to patchy saturation and fabric heterogeneity: a double double-porosity model of wave propagation;Ba;J. geophys. Res.,2017

3. Velocity field of wave-induced local fluid flow in double-porosity media;Ba;Sci. China Phys. Mech. Astron.,2014

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