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南海的盆地群与盆地动力学

李三忠 安慧婷 薛友辰 熊莉娟 曹现志 许立青 索艳慧 刘鑫 戴黎明 余珊 赵淑娟 马云 王霄飞 程世秀

海洋地质与第四纪地质2012,Vol.32Issue(6):55-78,24.
海洋地质与第四纪地质2012,Vol.32Issue(6):55-78,24.DOI:10.3724/SP.J.1140.2012.06055

南海的盆地群与盆地动力学

BASIN DYNAMICS AND BASIN GROUPS OF THE SOUTH CHINA SEA

李三忠 1安慧婷 2薛友辰 1熊莉娟 2曹现志 1许立青 2索艳慧 1刘鑫 2戴黎明 1余珊 2赵淑娟 1马云 2王霄飞 1程世秀2

作者信息

  • 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
  • 折叠

摘要

Abstract

The South China Sea was formed in Cenozoic. Basins in the South China Sea could be divided into different types, such as continental shelf basins, continental slope basins and deep sea basins, which are closely related with the rifting and transition of the continental margins, and thus could be grouped into strike-slip-related pull-apart and extensional basins, extrusion-escape-related rifting basins, extension- and subduction-related buckling basins. They developed further into some ndge-spreading-related oceanic sub-basins in different stages. These basins were formed not under a single dynamics but under a very complex and changeable dynamics. These basins have suffered from a series of Cenozoic tectonic movements, such as the Shenhu, the South China Sea, the Dongsha, resulting in the formation and spatial-temperal migration of complex angular unconformities in these basins. Accompanying with the tectonic migrations and evolutions in these basins, faulting, magmatism, shifting of sedimentary subsidence centers and depo-centers, oil accumulation and geohazards show a significant feature of jumping. The complex dynamic settings of the South China Sea have caused many controversies on their origin. The plate dynamic factors include the Pacific Plate subduction and the indentation of the Philippine Sea Plate along the Taiwan Orogen to the east side of the South China Sea, and the Indian Plate oblique subduction and mid-ocean ridge subduction to the west side. They may also be responsible for the uplifting of the Tibetan Plateau and the related extrusions of continental blocks to the north side. At the same time, the mantle dynamics of deep-seated magma underplating, delamination, mantle plume and mantle-hydrated process should not be ignored. At last, this paper proposes one strike-slipping pull-apart model to explain the onset of the South China Sea Basin which is closely related to the tectonic evolution of the Pacific Tectonic Domain.

关键词

盆地群/深海盆地/陆架盆地/盆地动力学/南海

Key words

basin group/ deep sea basin continental shelf basin/ basin dynamics/ South China Sea

分类

海洋科学

引用本文复制引用

李三忠,安慧婷,薛友辰,熊莉娟,曹现志,许立青,索艳慧,刘鑫,戴黎明,余珊,赵淑娟,马云,王霄飞,程世秀..南海的盆地群与盆地动力学[J].海洋地质与第四纪地质,2012,32(6):55-78,24.

基金项目

中国海洋大学中央高校财政专项资助成果 ()

海洋地质与第四纪地质

OA北大核心CSCDCSTPCD

0256-1492

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