作者: Tao Zhu , Xiaoxi Ma
DOI: 10.1016/J.EARSCIREV.2020.103437
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摘要: Abstract Seismic anisotropy, as a ubiquitous feature in the Earth’s interior, could record past lithospheric deformation and map directly mantle flow within our planet, thus becomes bridge to understand interaction between crust subcrustal or different tectonic blocks. Plenty of high quality shear-wave splitting (SWS) measurements have been performed Mainland China. In this paper, we compile these measurements, then analyze their characteristics, estimate contribution from crust, asthenosphere, explore mechanisms tectonic/geodynamic implications.