Direct Inversion for Three‐Dimensional Shear Wave Speed Azimuthal Anisotropy Based on Surface Wave Ray Tracing: Methodology and Application to Yunnan, Southwest China-Reference-Cited by-同舟云学术

Direct Inversion for Three‐Dimensional Shear Wave Speed Azimuthal Anisotropy Based on Surface Wave Ray Tracing: Methodology and Application to Yunnan, Southwest China

Published:2019-11 Issue:11 Volume:124 Page:11394-11413
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Liu Chuanming¹²^ORCID,Yao Huajian¹³^ORCID,Yang Hsin‐Ying¹³^ORCID,Shen Weisen⁴^ORCID,Fang Hongjian¹⁵^ORCID,Hu Shaoqian¹^ORCID,Qiao Lei¹

Affiliation:

1. Laboratory of Seismology and Physics of Earth's Interior, School of Earth and Space Sciences University of Science and Technology of China Hefei China

2. Department of Physics University of Colorado Boulder Boulder CO USA

3. CAS Center for Excellence in Comparative Planetology Hefei China

4. Department of Geosciences State University of New York at Stony Brook Stony Brook NY USA

5. Now at Department of Earth, Atmospheric and Planetary Sciences Massachusetts Institute of Technology Cambridge MA USA

Funder

China Earthquake Administration

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/10.1029/2018JB016920

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5. A Fast and Reliable Method for Surface Wave Tomography

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