A new algorithm for three‐dimensional joint inversion of body wave and surface wave data and its application to the Southern California plate boundary region-Reference-Cited by-同舟云学术

A new algorithm for three‐dimensional joint inversion of body wave and surface wave data and its application to the Southern California plate boundary region

Published:2016-05 Issue:5 Volume:121 Page:3557-3569
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Fang Hongjian¹,Zhang Haijiang¹,Yao Huajian¹,Allam Amir²³,Zigone Dimitri²⁴,Ben‐Zion Yehuda²,Thurber Clifford⁵,van der Hilst Robert D.⁶

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 Earth Sciences University of Southern California Los Angeles California USA

3. Now at Geophysical Institute and Department of Geology and Geophysics University of Alaska Fairbanks Fairbanks Alaska USA

4. Now at Department of Meteorology and Geophysics University of Vienna Vienna Austria

5. Department of Geoscience University of Wisconsin‐Madison Madison Wisconsin USA

6. Department of Earth, Atmospheric, and Planetary Sciences Massachusetts Institute of Technology Cambridge Massachusetts USA

Funder

U.S. Department of Energy

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/10.1002/2015JB012702

Reference48 articles.

1. Seismic velocity structures in the southern California plate-boundary environment from double-difference tomography

2. J362D28: a new joint model of compressional and shear velocity in the Earth's mantle

3. San Andreas Fault dip, Peninsular Ranges mafic lower crust and partial melt in the Salton Trough, Southern California, from ambient-noise tomography

4. Joint inversion of Rayleigh-wave dispersion and P-wave refraction data for laterally varying layered models

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