吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (1): 96-105.doi: 10.13278/j.cnki.jjuese.20180131

• 大陆架科学钻探 • 上一篇    

南黄海有关地层与构造的研究进展及问题讨论

侯方辉1,2, 郭兴伟1,2, 吴志强1,2, 朱晓青1,2, 张训华2,3, 祁江豪1,2, 王保军1,2, 温珍河1,2, 蔡来星1,2, 庞玉茂1,2   

  1. 1. 中国地质调查局青岛海洋地质研究所, 山东 青岛 266071;
    2. 青岛海洋科学与技术试点国家实验室海洋矿产资源评价与探测技术功能实验室, 山东 青岛 266071;
    3. 中国地质调查局南京地质调查中心, 南京 210016
  • 收稿日期:2018-05-25 发布日期:2019-01-18
  • 通讯作者: 吴志强(1964-),男,研究员,博士,主要从事海洋构造与油气地质和地球物理方面的研究,E-mail:wuzq_1964@163.com E-mail:wuzq_1964@163.com
  • 作者简介:侯方辉(1979-),男,博士,主要从事大陆边缘构造与盆地分析方面的研究,E-mail:houfanghui3993@163.com
  • 基金资助:
    国家自然科学基金项目（41776081，41210005）；青岛海洋科学与技术试点国家实验室鳌山科技创新计划项目（2015ASKJ03）；国家海洋地质专项（DD20160147，DD20179393）

Research Progress and Discussion on Formation and Tectonics of South Yellow Sea

Hou Fanghui1,2, Guo Xingwei1,2, Wu Zhiqiang1,2, Zhu Xiaoqing1,2, Zhang Xunhua2,3, Qi Jianghao1,2, Wang Baojun1,2, Wen Zhenhe1,2, Cai Laixing1,2, Pang Yumao1,2   

  1. 1. Qingdao Institute of Marine Geology, China Geological Survey, Qingdao 266071, Shandong, China;
    2. Laboratory for Marine Mineral Resources, Pilot National Laboratory for Marine Science and Technology(Qingdao), Qingdao 266071, Shandong, China;
    3. Nanjing Center, China Geological Survey, Nanjing 210016, China
  • Received:2018-05-25 Published:2019-01-18
  • Supported by:
    Supported by National Natural Science Foundation of China(41776081,41210005),Aoshan Technological Innovation Projects of National Laboratory for Marine Science and Technology(Qingdao)(2015ASKJ03), and National Marine Geology Special Project of China (DD20160147,DD20179393)

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摘要： 南黄海为一叠置于下扬子地块变质基底之上的中、古生代海相与中、新生代陆相多旋回叠合盆地，经历了长期的构造演化及多期次构造改造。有关南黄海多期次盆地地层格架及分布特征、构造变形及动力机制、盆地性质及成因机制等问题，仍存在诸多争论。本文在总结前人研究的基础上，利用近几年最新获得的地质、地球物理数据，对南黄海有关地层与构造相关的主要问题进行了探讨。地球物理及综合研究表明：南黄海北部燕山晚期以来陆相断陷盆地之下并不存在印支-早燕山期的前陆盆地；朝鲜半岛西缘断裂带是存在的，扬子地块与华北地块汇聚碰撞过程中存在壳内多层次的互相楔入构造；南黄海海相中、古生界广泛分布，往东抬升剥蚀，可能主要残留下古生界，中部隆起残留有完整的下三叠统-震旦系。

关键词: 地层, 构造特征, 复合盆地, 南黄海

Abstract: The South Yellow Sea basin is a multi-cycle basin with a sandwich-type construction on the pre-Sinian metamorphic basement of the lower Yangtze platform. The geologic evolution of the basin can be divided into three stages:the Sinian-Early Triassic marine basin, the Cretaceous-Paleogene graben fault basin and the Neogene-Quaternary depression basin stages. There are still a lot of debates on the stratigraphic framework and distribution characteristics of multistage basins, basin deformation and dynamics mechanism, basin property and genetic mechanism at present. In this paper, some problems about strata and tectonics in South Yellow Sea are discussed based on geological-geophysical data obtained in recent years,combined with the previous research. The comprehensive research shows that:There is no Indo-Early Yanshanian foreland basin under the fault depression basin since Late Yanshanian in the northern basin of South Yellow Sea. There is indeed a fault zone in the western edge of the Korean Peninsula. In the collision between the Yangtze block and the North China block, there were many multi-layer interwedging structures formed in the crust. The Mesozoic-Paleozoic marine strata are widely distributed in the South Yellow Sea and denuded eastward,and maybe only the lower Paleozoic remains. The whole Lower Triassic-Sinian strata remain in the Central Uplift.

Key words: formation, tectonic characteristics, composite basin, South Yellow Sea

中图分类号: 

  • P548
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