Frequency‐Dependent P Wave Anisotropy Due to Wave‐Induced Fluid Flow and Elastic Scattering in a Fluid‐Saturated Porous Medium With Aligned Fractures-Reference-Cited by-同舟云学术

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Frequency‐Dependent P Wave Anisotropy Due to Wave‐Induced Fluid Flow and Elastic Scattering in a Fluid‐Saturated Porous Medium With Aligned Fractures

Published:2020-08 Issue:8 Volume:125 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Guo Junxin¹²^ORCID,Gurevich Boris³^ORCID

Affiliation:

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

2. School of Earth and Space Sciences University of Science and Technology of China Hefei China

3. Centre for Exploration Geophysics Curtin University Perth Western Australia Australia

Funder

China Postdoctoral Science Foundation

National Natural Science Foundation of China

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/10.1029/2020JB020320

Reference56 articles.

1. Rock anelasticity due to patchy saturation and fabric heterogeneity: A double double-porosity model of wave propagation

2. Mechanics of Deformation and Acoustic Propagation in Porous Media

3. A model forP-wave attenuation and dispersion in a porous medium permeated by aligned fractures

4. Frequency-dependent anisotropy due to meso-scale fractures in the presence of equant porosity

5. Derivation of a microstructural poroelastic model

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3. Attenuation analysis in coal based on a fractal viscoelastic model;Acta Geophysica;2024-04-12

4. Frequency-dependent elastic properties of fracture-induced VTI rocks in a fluid-saturated porous and microcracked background;GEOPHYSICS;2024-04-05

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