南黄海区域地质与地球物理调查研究进展
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  • 英文篇名:Survey and research progress in regional geology and geophysics of South Yellow Sea
  • 作者:吴德城 ; 侯方辉
  • 英文作者:WU De-cheng;HOU Fang-hui;Hebei GEO University;Function laboratory for Marine Mineral Resource Geology and Exploration,Qingdao National Oceanography Laboratory;Key Laboratory of Marine Hydrocarbon Resource and Environmental Geology,Ministry of Land and Resources;Qingdao Institute of Marine Geology;
  • 关键词:南黄海 ; 地质特征 ; 构造演化 ; 地层分布
  • 英文关键词:South Yellow Sea;;geology characters;;tectonic;;stratigraphic distribution
  • 中文刊名:DQWJ
  • 英文刊名:Progress in Geophysics
  • 机构:河北地质大学;青岛海洋科学与技术国家实验室海洋矿产资源评价与探测技术功能实验室;国土资源部海洋油气资源与环境地质重点实验室;青岛海洋地质研究所;
  • 出版日期:2017-12-15
  • 出版单位:地球物理学进展
  • 年:2017
  • 期:v.32;No.146
  • 基金:国家自然科学基金(41210005);; 鳌山科技创新计划项目(2015ASKJ03);; 地调专项(121201102000150009)联合资助
  • 语种:中文;
  • 页:DQWJ201706053
  • 页数:10
  • CN:06
  • ISSN:11-2982/P
  • 分类号:413-422
摘要
历经50余年的调查研究,特别是随着近年来调查技术方法的进步和工作量的加大,南黄海区域地质调查研究取得了多项成果.长排列+立体震源多道地震勘探新技术的创新应用,获得了深部中-古生代海相残余地层的有效地震反射;海底地震仪(OBS)深部地震探测工作的实施,获得了深达莫霍面的深部地震速度结构;最新的钻探资料证实了中部隆起存在厚度较大的海相残余地层,北部坳陷发育侏罗系等推断.结合这些调查成果,区域地质对比研究得出了南黄海是下扬子块体的主体部位,南黄海盆地为新生代、中生代、古生代叠合盆地,中-古生代海相残留盆地分布面积大,地层较齐全、厚度大等主要认识.这些成果与认识对南黄海区域地质的深入研究提供了重要的参考与基础资料.同时,关于盆地的演化过程和动力学机制还存在不同的看法.本文在总结南黄海区域地质调查研究进展的基础上,提出了下一步调查研究工作建议.
        The South Yellow Sea is a multi-cycle superimposed basin consisting of the marine Mesozoic-Paleozoic basin overlaid by the continental Mesozoic-Cenozoic basin on the basis of the Presiniancratonic basement. It is a strategically important area in oil and gas resource assessment. Study on the regional geological survey of the achievements have been made after more than 50 years of geological survey and research works. These results are mainly showed as: The effective seismic reflection of deep MesozoicPaleozoic marine residual strata is obtained by the innovative application of the new multi-channel seismic exploration technique of long spread and multi-level source; The wide-angle reflection and refraction deep seismic line-OBS2013 using Ocean Bottom Seismometers( OBS) deployed for the first time in the northern part of South Yellow Sea,a 2 D P-wave velocity model from seabed to Moho along the line is constructed by seismic phase analysis and travel time fitting; There are large marine residual strata in Central Uplift and Jurassic in Northern Sag confirmed by the latest drilling data. Combining these findings,the following conclusions are drawn from the regional geological study that South Yellow Sea is the main part of the lower Yangtze block,and the South Yellow Sea basin is the Cenozoic, Mesozoic and Paleozoic superimposed basins,Mesozoic-Paleozoic marine residual basin has large distribution area and more completed formation and larger thickness. The stratigraphic distribution of the southern Yellow Sea residual basin is determined and a relatively complete stratigraphic sequence is established.These achievements and understanding of the South Yellow Sea area of geological research in depth has played a great role in promoting.At the same time,There are different views for basin evolution and geodynamics system in the Southern Yellow Sea. The next step of the research work is put forward based on the summary of regional geological investigation on the South Yellow Sea.
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