The role of magmatism in the thinning and breakup of the South China Sea continental margin

被引:8
|
作者
Zhen Sun [1 ,2 ]
Jian Lin [1 ,3 ]
Ning Qiu [1 ,2 ]
Zhimin Jian [4 ]
Pin Xian Wang [4 ]
Xiong Pang [5 ]
Jinyun Zheng [5 ]
Benduo Zhu [6 ]
机构
[1] CAS Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology,Chinese Academy of Sciences
[2] Innovation Academy of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences
[3] Department of Geology and Geophysics, Woods Hole Oceanographic Institution
[4] School of Ocean and Earth Science, Tongji University
[5] East South China Sea Petroleum Research Institute, Shenzhen branch of China National Offshore Oil Corporation
[6] Guangzhou Marine Geological Survey, Ministry of Natural Resources
基金
中国国家自然科学基金;
关键词
SCS; The role of magmatism in the thinning and breakup of the South China Sea continental margin; China;
D O I
暂无
中图分类号
P736 [海洋地质学];
学科分类号
070704 ; 0709 ;
摘要
INTRODUCTION Magmatism plays a key role in the process of continental margin breakup and ocean formation.Even in the extremely magma-poor Iberia and Newfoundland margin, studies of field outcrops have shown that syn-rift magmatism had participated in rifting from a very early
引用
收藏
页码:871 / 876
页数:6
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