Episodic Lithospheric Deformation in Eastern Tibet Inferred From Seismic Anisotropy

Abstract Mechanisms for uplift and deformation of the Tibetan Plateau remain vigorously debated; hypotheses include stepwise growth, distributed thickening, and crustal channel flow, each with a distinct anisotropic signature. We have developed a new azimuthally anisotropic shear velocity model for...

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Bibliographic Details
Main Authors: Xuewei Bao, Xiaodong Song, David W. Eaton, Yixian Xu, Hanlin Chen
Format: Article
Language:English
Published: Wiley 2020-02-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2019GL085721
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