Two crustal low-velocity channels beneath SE Tibet revealed by joint inversion of Rayleigh wave dispersion and receiver functions-Reference-Cited by-同舟云学术

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

Published:2015-04 Issue: Volume:415 Page:16-24
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Bao Xuewei,Sun Xiaoxiao,Xu Mingjie,Eaton David W.,Song Xiaodong,Wang Liangshu,Ding Zhifeng,Mi Ning,Li Hua,Yu Dayong,Huang Zhouchuan,Wang Pan

Funder

China National Special Fund for Earthquake Scientific Research in Public Interest

China Postdoctoral Science Foundation

Key Laboratory of Seismic Observation and Geophysical Imaging

Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference64 articles.

1. Lithospheric thickness of the Chinese continent;An;Phys. Earth Planet. Inter.,2006

2. Crustal deformation of the eastern Tibetan Plateau revealed by magnetotelluric imaging;Bai;Nat. Geosci.,2010

3. High resolution regional seismic attenuation tomography in eastern Tibetan Plateau and adjacent regions;Bao;Geophys. Res. Lett.,2011

4. High-resolution lithospheric structure beneath Mainland China from ambient noise and earthquake surface-wave tomography;Bao;Earth Planet. Sci. Lett,2015

5. Crust and upper mantle structure of the North China Craton and the NE Tibetan Plateau and its tectonic implications;Bao;Earth Planet. Sci. Lett.,2013

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