Decoupled anisotropy in the lower crust and upper mantle extracted by the Wave Gradiometry method resolves the differential deformation mechanisms beneath the northeastern Tibetan Plateau-Reference-Cited by-同舟云学术

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Decoupled anisotropy in the lower crust and upper mantle extracted by the Wave Gradiometry method resolves the differential deformation mechanisms beneath the northeastern Tibetan Plateau

Published:2024-05 Issue: Volume:633 Page:118654
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Dai Yixin^ORCID,Liang Chuntao,Cao Feihuang^ORCID,Chen Ling^ORCID,Liu Zhen,Fan Xingli^ORCID,Wang Chaoliang^ORCID

Funder

National Key Research and Development Program of China

National Natural Science Foundation of China

Institute of Geology, China Earthquake Administration

Ministry of Science and Technology of the People's Republic of China

Science and Technology Department of Sichuan Province

Key Research and Development Program of Sichuan Province

Publisher

Elsevier BV

Reference69 articles.

1. Episodic lithospheric deformation in eastern Tibet inferred from seismic anisotropy;Bao;Geophys. Res. Lett.,2020

2. Reconciling lithospheric deformation and lower crustal flow beneath central Tibet;Bendick;Geology,2007

3. 3D velocity and anisotropy of the southeastern Tibetan Plateau extracted by joint inversion of wave gradiometry, ambient noise, and receiver function;Cao;Tectonophysics,2023

4. Seismic Azimuthal Anisotropy for the Southeastern Tibetan Plateau Extracted by Wave Gradiometry Analysis;Cao;J. Geophys. Res. Solid Earth,2020

5. Vertical coherence of deformation in lithosphere in the NE margin of the Tibetan Plateau using GPS and shear-wave splitting data;Chang;Tectonophysics,2017

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