2-D poroelastic wave modelling with a topographic free surface by the curvilinear grid finite-difference method-Reference-Cited by-同舟云学术

2-D poroelastic wave modelling with a topographic free surface by the curvilinear grid finite-difference method

Published:2019-06-05 Issue:3 Volume:218 Page:1961-1982
ISSN:0956-540X
Container-title:Geophysical Journal International
language:en
Short-container-title:

Author:

Sun Yao-Chong¹²,Ren Hengxin¹,Zheng Xu-Zhen¹,Li Na³,Zhang Wei¹,Huang Qinghua⁴,Chen Xiaofei¹

Affiliation:

1. Department of Earth and Space Sciences, Southern University of Science and Technology, Shenzhen, Guangdong 518055, China. E-mail: renhx@sustech.edu.cn

2. Department of Geophysics, School of Geodesy and Geomatics, Wuhan University, Wuhan, Hubei 430079, China

3. Beijing Geoscience Center, Schlumberger, Beijing 100096, China

4. School of Earth and Space Sciences, Peking University, Beijing 100871, China

Funder

China Postdoctoral

National Natural Science Foundation of China

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/gji/advance-article-pdf/doi/10.1093/gji/ggz263/28770233/ggz263.pdf

Reference86 articles.

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3. Modeling poroelastic wave propagation in a real 2-D complex geological structure obtained via self-organizing maps;Balam;Pure appl. Geophys,2018

4. A perfectly matched layer for the absorption of elemetromagnetic waves;Berenger;J. Comput. Phys,1994

5. Theory of propagation of elastic waves in a fluid-saturated porous solid. I. Low-Frequency range;Biot;J. acoust. Soc. Am,1956

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