东亚大陆边缘的板块重建与构造转换

李三忠; 余珊; 赵淑娟; 刘鑫; 龚淑云; 索艳慧; 戴黎明; 马云; 许立青; 曹现志; 王鹏程; 孙文军; 杨朝; 朱俊江

doi:10.3724/SP.J.1140.2013.03065

东亚大陆边缘的板块重建与构造转换

1. 海底科学与探测技术教育部重点实验室, 青岛 266100;

2. 中国海洋大学海洋地球科学学院, 青岛 266100;

3. 深圳市地质局, 深圳 518023;

4. 中国科学院南海海洋研究所, 广州 510301

基金项目:
国家自然科学基金重大项目(41190072,41190070)；中国海洋大学中央高校财政专项；山东省自然科学基金项目

详细信息

作者简介: 李三忠(1968-),男,博士,教授,博导,从事构造地质学及海洋地质学的教学和研究工作,E-mail:sanzhong@ouc.edu.cn

中图分类号: P736.1

收稿日期: 2012-11-30

修回日期: 2013-05-20

TECTONIC TRANSITION AND PLATE RECONSTRUCTIONS OF THE EAST ASIAN CONTINENTAL MAGIN

1. Key Lab of Submarine Geosciences and Exploration Techniques, Ministry of Education, Qingdao 266003, China;

2. College of Marine Geoscience, Ocean University of China, Qingdao 266003, China;

3. Geology Bureau of Shenzhen, Shenzhen 518023, China;

4. South China Sea Institute of Oceanology, Chinese Academy of Science, Guangzhou 510301, China

Received Date: 30 November 2012

Revised Date: 20 May 2013

摘要

摘要: 东亚大陆边缘中新生代期间的动力学演化始终是地质研究的难点和热点,特别是对其大陆边缘性质、类型和演化过程始终不明朗,并存在巨大争论。系统综述了40多年来已有东亚大陆边缘二叠纪以来板块重建的主要方案,特别是近10年来东亚陆缘新的研究成果,侧重探讨了晚三叠世以来东亚大陆边缘类型转换、不同构造域的交接-转换过程。认为东亚陆缘总体经历了三叠纪前的被动陆缘阶段、晚三叠世-早白垩世的大陆岩浆弧发育的安第斯型活动陆缘阶段、早白垩世晚期-始新世的走滑拉分盆地发育的安第斯型活动陆缘阶段和渐新世以来的日本型活动大陆边缘阶段。这对于认识中国东部海域渤海湾、黄海、东海和南海盆地成因具有指导意义。同时,分析了各阶段海-陆分布特征及其变迁规律、板块格局变动过程及其动力学背景。
- 板块构造 /
- 东亚 /
- 板块重建 /
- 太平洋 /
- 印度洋 /
- 大陆边缘
Abstract: It is a hot debate on the Meso-Cenozoic dynamics of the East Asian continental margins, since the nature, type and evolution of its continental margins are not well-known.. This paper systematically summarizes the results of plate reconstructions on the East Asian continental margin since Permian over the past 40 years with emphasis on the new research results in the past 10 years. The paper mainly focuses on the variation in types of the East Asian continental margin since Late Triassic, the transitions among different tectonic domains. Our data suggests that the East Asian continental margins as a whole experienced a pre-Triassic passive continental margin, a Late Triassic-Early Cretaceous continental magmatic arc of the Andean-type active continental margin, a Late Cretaceous-Eocene strike-slipping Andean-type active continental margin with of pull-apart basins, and a post-Oligocene Japanese-type active continental margin successively. Tectonic trasition is important for understanding of the formation of the Bohaisx Bay, the Yellow Sea, the East China Sea and the South China Sea basins in East China. The changes of the continent-ocean distribution, plate configuration and dynamics at the various stages are also discussed.
- plate tectonics /
- East Asia /
- plate resonstruction /
- Pacific Ocean /
- India Ocean /
- continental margin

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东亚大陆边缘的板块重建与构造转换

1. 海底科学与探测技术教育部重点实验室, 青岛 266100; 2. 中国海洋大学海洋地球科学学院, 青岛 266100; 3. 深圳市地质局, 深圳 518023; 4. 中国科学院南海海洋研究所, 广州 510301

作者简介: 李三忠(1968-),男,博士,教授,博导,从事构造地质学及海洋地质学的教学和研究工作,E-mail:sanzhong@ouc.edu.cn

TECTONIC TRANSITION AND PLATE RECONSTRUCTIONS OF THE EAST ASIAN CONTINENTAL MAGIN

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1. 海底科学与探测技术教育部重点实验室, 青岛 266100;

2. 中国海洋大学海洋地球科学学院, 青岛 266100;

3. 深圳市地质局, 深圳 518023;

4. 中国科学院南海海洋研究所, 广州 510301