Southeastward extrusion of the Tibetan Plateau limited by the strong Emeishan large igneous province from earthquake surface wave tomography

Active deformation is ongoing in the southeastern margin of the Tibetan Plateau due to the collision of the Indian and Eurasian continents. While large-scale motion of the surface occurs, the nature of deformation at depth remains unresolved. We construct new lithospheric seismic anisotropic (radial...

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Bibliographic Details

Published in:	Physics of the earth and planetary interiors Vol. 348; p. 107153
Main Authors:	Fu, Yuanyuan V., Li, Lun, Ma, Junwei, Sun, Nannan
Format:	Journal Article
Language:	English
Published:	Elsevier B.V 01.03.2024
Subjects:	Azimuthal anisotropy Radial anisotropy Shear wave velocity Southeastern Tibetan Plateau Shear wave velocity Azimuthal anisotropy Radial anisotropy Southeastern Tibetan Plateau
ISSN:	0031-9201, 1872-7395
Online Access:	Get full text
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