Seismic tomography of the Pacific slab edge under Kamchatka

We determine a 3-D P-wave velocity structure of the mantle down to 700 km depth under the Kamchatka peninsula using 678 P-wave arrival times collected from digital seismograms of 75 teleseismic events recorded by 15 portable seismic stations and 1 permanent station in Kamchatka. The subducting Pacif...

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Bibliographic Details
Published in:Tectonophysics
Main Authors: Jiang Guoming, Zhao Dapeng, Zhang Guibin
Format: Text
Language:English
Published: 2009
Subjects:
Online Access:http://repo.kscnet.ru/2557/
http://www.sciencedirect.com/science/article/pii/S0040195108005842