Joint Inversion of Body Wave Arrival Times, Surface Wave Dispersion Data and Receiver Functions: Method and Application to South China-Reference-Cited by-同舟云学术

Joint Inversion of Body Wave Arrival Times, Surface Wave Dispersion Data and Receiver Functions: Method and Application to South China

Published:2022-09 Issue:9 Volume:127 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Han Shoucheng¹^ORCID,Zhang Haijiang¹²³^ORCID,Gao Lei¹,Liu Ying¹²,Chai Chengping⁴^ORCID,Maceira Monica⁴^ORCID

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. Mengcheng National Geophysical Observatory University of Science and Technology of China Hefei China

3. CAS Center for Excellence in Comparative Planetology University of Science and Technology of China Hefei China

4. Oak Ridge National Laboratory Oak Ridge TN USA

Funder

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/10.1029/2022JB024083

Reference114 articles.

1. Determination of three-dimensional velocity anomalies under a seismic array using first P arrival times from local earthquakes: 1. A homogeneous initial model

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

5. Two crustal low-velocity channels beneath SE Tibet revealed by joint inversion of Rayleigh wave dispersion and receiver functions

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