Low velocity crustal flow and crust–mantle coupling mechanism in Yunnan, SE Tibet, revealed by 3D S-wave velocity and azimuthal anisotropy-Reference-Cited by-同舟云学术

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Low velocity crustal flow and crust–mantle coupling mechanism in Yunnan, SE Tibet, revealed by 3D S-wave velocity and azimuthal anisotropy

Published:2016-08 Issue: Volume:685 Page:8-20
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Chen Haopeng,Zhu Liangbao,Su Youjin

Funder

National Natural Science Foundation of China

China Postdoctoral Science Foundation

Surveying and Mapping Basic Research Program of National Administration of Surveying, Mapping and Geoinformation

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference59 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. Two crustal low-velocity channels beneath SE Tibet revealed by joint inversion of Rayleigh wave dispersion and receiver functions;Bao;Earth Planet. Sci. Lett.,2015

4. Anisotropy gradients from QL surface waves: evidence for vertically coherent deformation in the Tibet region;Chen;Tectonophysics,2013

5. Low wave speed zones in the crust beneath SE Tibet revealed by ambient noise adjoint tomography;Chen;Geophys. Res. Lett.,2014

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