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Tomographic structure of East Asia: Ⅰ.No fast (slab) anomalies beneath 660 km discontinuity

Shunping Pei Yongshun John Chen

地震学报（英文版）2010，Vol.23Issue(6)：597-611,15.

地震学报（英文版）2010，Vol.23Issue(6)：597-611,15.DOI:10.1007/s11589-010-0759-7

Tomographic structure of East Asia: Ⅰ.No fast (slab) anomalies beneath 660 km discontinuity

Shunping Pei ¹Yongshun John Chen²

作者信息

1. Key Laboratory of Continental Collision and Plateau Uplift,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100085,China
2. Computational Geodynamics Laboratory,Department of Geophysics,School of Earth and Space Sciences,Peking Unive
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摘要

关键词

tomography/stagnant slab/mantle wedge

Key words

tomography/stagnant slab/mantle wedge

分类

天文与地球科学

引用本文复制引用

Shunping Pei,Yongshun John Chen..Tomographic structure of East Asia: Ⅰ.No fast (slab) anomalies beneath 660 km discontinuity[J].地震学报（英文版）,2010,23(6):597-611,15.

基金项目

We thank two anonymous reviewers for their valuable comments.The manuscript was written during John Chen's four-month visit in 2004 as a visiting professor at Geodynamics Research Center,Ehime University,Japan by grants(B-11440134,S-12002006)to Dapeng Zhao from the Japan Society for the Promotion of Science.Support for Shunping Pei came from a postdoct grant of Peking University.This study was also supported by the Chinese Academy of Sciences(No.KZCX2-EW-QN102)and the National Natural Science Foundation of China(Nos.41074041,90814002 and 40125011). （B-11440134,S-12002006）

地震学报（英文版）

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