加入收藏 | 设为首页 
   
科技导报  2020, Vol. 38 Issue (18): 35-39    DOI: 10.3981/j.issn.1000-7857.2020.18.005
  专题:南海深海探索 本期目录 | 过刊浏览 | 高级检索 |
南海成因:岩石圈破裂与俯冲带相互作用新认识
林间1,2,3,4, 孙珍1,3,5, 李家彪6, 周志远1,3,5, 张帆1,3,5, 罗怡鸣1,3,4
1. 中国科学院南海海洋研究所边缘海与大洋地质重点实验室, 广州 510301;
2. 美国伍兹霍尔海洋研究所地质与地球物理系, 马萨诸塞州伍兹霍尔 02543;
3. 南方海洋科学与工程广东省实验室(广州), 广州 511458;
4. 南方科技大学海洋科学与工程系, 深圳 518055;
5. 中国科学院南海生态环境工程创新研究院, 广州 510301;
6. 自然资源部第二海洋研究所, 杭州 310012
South China Seabasin opening: Lithospheric rifting and interactionwith surroundingsubduction zones
LIN Jian1,2,3,4, SUN Zhen1,3,5, LI Jiabiao6, ZHOU Zhiyuan1,3,5, ZHANG Fan1,3,5, LUO Yiming1,3,4
1. Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;
2. Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA;
3. Southern Marine Science and Engineering Guangdong Laboratory(Guangzhou), Guangzhou 511458, China;
4. Department of Ocean Science and Engineering, Southern University of Science and Technology of China, Shenzhen 518055, China;
5. Innovation Academy of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences, Guangzhou 510301, China;
6. Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China
版权所有 © 《科技导报》编辑部    京ICP备14028469号-1
地址:北京市海淀区学院南路86号科技导报社 邮编:100081
电话:010-62138113,传真:010-62138113 电子信箱:kjdbbjb@cast.org.cn