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Crustal Structure across the Northwestern Margin of South China Sea:Evidence for Magma-poor Rifting from a Wide-angle Seismic Profile

DING Weiwei Michael SCHNABEL Dieter FRANKE RUAN Aiguo WU Zhenli

地质学报（英文版）2012，Vol.86Issue(4)：854-866,13.

Crustal Structure across the Northwestern Margin of South China Sea:Evidence for Magma-poor Rifting from a Wide-angle Seismic Profile

DING Weiwei ¹Michael SCHNABEL ²Dieter FRANKE ²RUAN Aiguo ¹WU Zhenli¹

作者信息

1. The Second Institute of Oceanography, State Oceanic Administration, Hangzhou, Zhejiang 310012, China
2. Federal Institute for Geoscience and Natural Resource(BGR), Hannover 30655, Germany
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摘要

关键词

P-wave/velocity model/magma-poor rifting/lower crust flow/South China Sea

Key words

P-wave/velocity model/magma-poor rifting/lower crust flow/South China Sea

引用本文复制引用

DING Weiwei,Michael SCHNABEL,Dieter FRANKE,RUAN Aiguo,WU Zhenli..Crustal Structure across the Northwestern Margin of South China Sea:Evidence for Magma-poor Rifting from a Wide-angle Seismic Profile[J].地质学报（英文版）,2012,86(4):854-866,13.

基金项目

We are grateful to the technical staff from KLSB and SIO,and the crew members of the R/V Fendou Seven of the First Brigade of Marine Geological Survey,Shanghai Marine Oil Bureau,who took part in the field work at sea.We thank BGR for offering a half-year visitor's position and the great cooperation during the seismic data processing.This work was financially supported by the National Basic Research Program (973) of China (No.2007CB41170403) and the National Natural Science Foundation of China (No.91028006 and 41074066). （973）

地质学报（英文版）

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ISSN：1000-9515

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