南海西部断裂系研究及其物理模拟实验证据

孙龙涛; 孙珍; 詹文欢; 孙宗勋; 赵明辉; 夏少红

南海西部断裂系研究及其物理模拟实验证据

1.
中国科学院, 南海海洋研究所, 广东, 广州, 510301;中国科学院边缘海地质重点实验室, 广东, 广州, 510301;中国科学院, 研究生院, 北京, 100039
2.
中国科学院, 南海海洋研究所, 广东, 广州, 510301;中国科学院边缘海地质重点实验室, 广东, 广州, 510301
3.
中国科学院, 南海海洋研究所, 广东, 广州, 510301

基金项目: 国家自然科学基金资助项目(40476026);广东省自然科学基金资助项目(04001309);中国科学院边缘海地质重点实验室基金资助项目(MSGL0510)

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出版历程
- 收稿日期: 2005-04-20
- 修回日期: 2005-07-18

Western fault zone of South China Sea and its physical simulation evidences

1.
South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;Key Laboratory of Marginal Sea Geology of Chinese Academy of Sciences, Guangzhou 510301, China;Graduate School, Chinese Academy of Sciences, Beijing 100039, China
2.
South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;Key Laboratory of Marginal Sea Geology of Chinese Academy of Sciences, Guangzhou 510301, China
3.
South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China

摘要

摘要: 南海西部断裂系是由四条典型的走滑断裂所组成的断裂系统,是南海扩张的西部边界.此断裂系主要是在白垩纪以来的印-藏碰撞、新生代印支挤出和南海扩张的共同作用下形成的.通过模拟实验,探讨此断裂系的成因、演化过程,认识到此断裂系经历了五期构造运动.
- 南海西部 /
- 断裂系 /
- 模拟试验
Abstract: The western fault zone of South China Sea is a strike-slip fault system and consists of five typical strike-slip faults.It is the western border of the South China Sea opening.The formation of the system has been due to the collision of India with Tibet since Cretaceo us,the extrusion of Indo-China Peninsula and the spreading of the South China Sea in Ceno zoic.There are five times of tectonic movement of this fault zone and it plays an important role in the Cenozoic evolution of the South China Sea.So the tectonic model experiments are done to study the orient ation and motion of the fault zone.
- western margin of South China Sea /
- fault zone /
- simulation modeling experiment

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