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南黄海南部与东海北部之间的深部构造

Deep tectonics between South Yellow Sea and North East China Sea

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【作者】 王谦身刘建华郝天珧Suh. Mancheol戴明刚

【Author】 WANG Qian-shen1, LIU Jian-hua1, HAO Tian-yao1, SUH Mancheol2, DAI Ming-gang1(1. Institute of Geology and Geophysics, Chinese Academy of Sciences,Beijing 100029, China; 2. Kongju National University, Kobngju 314-701, Korea)

【机构】 中国科学院地质与地球物理研究所韩国公州大学中国科学院地质与地球物理研究所 北京100029北京100029公州314-701北京100029

【摘要】 针对南黄海南部与东海之间的深部构造 ,根据前一段地球物理研究的结果 ,与有关文献进行对比探讨 ,发现其差异 .在重力和三维地震层析成像结果基础上 ,探讨分析了该海域的深部构造 ,给出分布在南黄海南部与东海北部之间的苏浙—济州岛构造带的分布位置、形态特征 ,并讨论了该构造带的性质、与周边构造体系和构造演化的关系 ,并指出这一构造由于朝鲜半岛西缘断裂带的存在而并未延伸进入朝鲜半岛 .

【Abstract】 The deep tectonics between south Yellow Sea and North East China Sea has been studied in this paper. According to the research recently result, some features of deep structure and differences have been found comparing with the result of others. On the basement of tomography research, the sharp, position, extension and velocity features of the deep upheaval and igneous belts have been discussed. We call this upheaval as SuZhe-Jeju Island Upheaval Belt. It is different with Fujian-Lingnan Upheaval Belt. It does not extend into Korea peninsula because of west marginal fault of Korea Peninsula. The relationship between Upheaval Belt and other tectonic units and its tectonic evolution have also been discussed.

【关键词】 南黄海东海深部构造隆起带
【Key words】 South Yellow SeaEast China Seadeep structureupheaval belt
【基金】 国家自然科学基金项目 ( 4 0 0 740 2 1);国家基础研究 973项目 (G2 0 0 0 0 467-0 1)联合资助 .
  • 【文献出处】 地球物理学进展 ,Progress In Geophysics , 编辑部邮箱 ,2003年02期
  • 【分类号】P736.12
  • 【被引频次】17
  • 【下载频次】302
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