Seismic Wave Propagation in Partially Saturated Rocks With a Fractal Distribution of Fluid‐Patch Size-Reference-Cited by-同舟云学术

Seismic Wave Propagation in Partially Saturated Rocks With a Fractal Distribution of Fluid‐Patch Size

Published:2022-02 Issue:2 Volume:127 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Zhang Lin¹²,Ba Jing¹^ORCID,Carcione José M.³^ORCID,Wu Chunfang¹

Affiliation:

1. School of Earth Sciences and Engineering Hohai University Nanjing China

2. Earth, Atmospheric, and Planetary Sciences Department Purdue University West Lafayette IN USA

3. National Institute of Oceanography and Applied Geophysics – OGS Trieste Italy

Funder

National Natural Science Foundation of China

Natural Science Foundation of Jiangsu Province

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JB023809

Reference88 articles.

1. Seismic wave attenuation in carbonates;Adam L.;Journal of Geophysical Research: Solid Earth,2009

2. Effect of CO2 on P- and S-wave velocities at seismic and ultrasonic frequencies

3. Biot critical frequency applied to description of failure and yield of highly porous chalk with different pore fluids

4. Velocity dispersion and attenuation of P waves in partially‐saturated rocks: Wave propagation equations in double‐porosity medium;Ba J.;Chinese Journal of Geophysics,2012

5. Biot-Rayleigh theory of wave propagation in double-porosity media

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