TECTONIC TRANSITION AND PLATE RECONSTRUCTIONS OF THE EAST ASIAN CONTINENTAL MAGIN

Li Sanzhong, Shan Yu, Shujuan Zhao, Xin Liu, Shuyun Gong, Y. Suo, L. Dai, Yun Ma, Liqing Xu, X. Cao, Pengcheng Wang, Wenjun Sun, Zhao Yang, Junjiang Zhu
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引用次数: 58

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.
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东亚大陆的构造转变与板块重建
由于对东亚大陆边缘的性质、类型和演化的认识尚不清楚,东亚大陆边缘中新生代动力学一直是争论的热点。本文系统总结了近40年来东亚大陆边缘二叠系以来的板块重建成果,重点介绍了近10年来的新研究成果。本文主要讨论了晚三叠世以来东亚大陆边缘的类型变化,以及不同构造域之间的过渡。东亚大陆边缘总体上经历了前三叠纪被动大陆边缘、晚三叠世—早白垩世安第斯型活动大陆边缘的大陆岩浆弧、晚白垩世—始新世带拉分盆地的走滑安第斯型活动大陆边缘和渐新世后日本型活动大陆边缘。构造转换对于认识中国东部渤海湾、黄海、东海和南海盆地的形成具有重要意义。讨论了各阶段陆-洋分布、板块构造和动力学的变化。
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