Seismic-velocity structure of the lithosphere beneath the southeastern margin of the Tibetan Plateau: Insights into geodynamic processes and deformation mechanisms
Author:
Funder
National Natural Science Foundation of China
Publisher
Elsevier BV
Reference74 articles.
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4. 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
5. Crustal anisotropy and deformation of the southeastern margin of the Tibetan Plateau revealed by Pms splitting;Cai;J. Asian Earth Sci.,2016
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