P wave azimuthal and radial anisotropy of the Hokkaido subduction zone

We present the first three‐dimensional P wave radial anisotropy tomography of the Hokkaido subduction zone, as well as P wave azimuthal anisotropy and S wave tomography, which are determined by inverting 298,430 P wave and 233,934 S wave arrival times from 14,245 local earthquakes recorded by 344 se...

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Veröffentlicht in:Journal of geophysical research. Solid earth 2016-04, Vol.121 (4), p.2636-2660
Hauptverfasser: Niu, Xiongwei, Zhao, Dapeng, Li, Jiabiao, Ruan, Aiguo
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Sprache:eng
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