Anisotropic tomography of the Cascadia subduction zone

The first P-wave tomography of 3-D azimuthal and radial anisotropy of the Cascadia subduction zone is determined by inverting local and teleseismic arrival-time data. Fast-velocity directions (FVDs) of azimuthal anisotropy in the crust are generally trench-parallel, reflecting N-S compression along...

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Bibliographic Details
Published in:Physics of the earth and planetary interiors Vol. 318; p. 106767
Main Authors: Zhao, Dapeng, Hua, Yuanyuan
Format: Journal Article
Language:English
Published: Elsevier B.V 01.09.2021
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ISSN:0031-9201, 1872-7395
Online Access:Get full text
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