Crustal anisotropy and deformation of the southeastern margin of the Tibetan Plateau revealed by Pms splitting-Reference-Cited by-同舟云学术

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Crustal anisotropy and deformation of the southeastern margin of the Tibetan Plateau revealed by Pms splitting

Published:2016-05 Issue: Volume:121 Page:120-126
ISSN:1367-9120
Container-title:Journal of Asian Earth Sciences
language:en
Short-container-title:Journal of Asian Earth Sciences

Author:

Cai Yan^ORCID,Wu Jianping,Fang Lihua,Wang Weilai,Yi Shuang^ORCID

Funder

National Science Foundation Grant of China

China National Special Fund for Earthquake Scientific Research in Public Interest

Institute of Geophysics, China Earthquake of Administration

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference46 articles.

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

2. A quantitative evaluation of the contribution of crustal rocks to the shear-wave splitting of teleseismic SKS waves;Barruol;Phys. Earth Planet. Inter.,1993

3. The relationship between maximum entropy spectra and maximum likelihood spectra;Burg;Geophysics,1972

4. Upper mantle anisotropy of the eastern Himalayan syntaxis and surrounding regions from shear wave splitting analysis;Chang;Sci. China, Ser. D Earth Sci.,2015

5. Crustal anisotropy from Moho converted Ps wave splitting analysis and geodynamic implications beneath the eastern margin of Tibet and surrounding regions;Chen;Gondwana Res.,2013

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1. Low-velocity middle-and-lower crustal materials blocked by the red river fault in the SE margin of the Tibetan plateau;Earth and Planetary Science Letters;2024-11

2. Lithospheric electrical structure and geodynamic model of the red river fault zone and its adjacent areas in southwest China: Constraints from 3-D magnetotelluric imaging;Journal of Asian Earth Sciences;2024-09

3. Crustal 3‐D S‐Wave Velocity and Azimuthal Anisotropy in the Sanjiang Lateral Collision Zone in the SE Margin of the Tibetan Plateau;Journal of Geophysical Research: Solid Earth;2024-09

4. The crustal deformation mechanism of southern Chuandian block: constrained by S wave velocity and its azimuthal anisotropy;Geoscience Letters;2024-08-27

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