Shear‐Wave Velocity Structure Beneath Northeast China From Joint Inversion of Receiver Functions and Rayleigh Wave Phase Velocities: Implications for Intraplate Volcanism-Reference-Cited by-同舟云学术

Shear‐Wave Velocity Structure Beneath Northeast China From Joint Inversion of Receiver Functions and Rayleigh Wave Phase Velocities: Implications for Intraplate Volcanism

Published:2022-04-29 Issue:5 Volume:127 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Tang Zheng¹^ORCID,Julià Jordi²^ORCID,Mai P. Martin³^ORCID,Mooney Walter D.⁴^ORCID,Wu Yanqiang¹^ORCID

Affiliation:

1. The First Monitoring and Application Center China Earthquake Administration Tianjin China

2. Departamento de Geofisica Universidade Federal do Rio Grando do Norte Natal Brazil

3. Earth Science and Engineering Program King Abdullah University of Science and Technology Thuwal Saudi Arabia

4. Earthquake Science Center United States Geological Survey Menlo Park CA USA

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/10.1029/2022JB023956

Reference97 articles.

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2. Processing seismic ambient noise data to obtain reliable broad-band surface wave dispersion measurements

3. Moho depth determinations based on spectral-ratio analysis of NORSAR long-period P waves

4. Mantle seismic anisotropy beneath NE China and implications for the lithospheric delamination hypothesis beneath the southern Great Xing'an range

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