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中朝-扬子板块碰撞结合带东部边界及海域延伸

岳保静 廖晶 刘鸿 曾洁 施剑

岳保静, 廖晶, 刘鸿, 曾洁, 施剑. 中朝-扬子板块碰撞结合带东部边界及海域延伸[J]. 海洋地质与第四纪地质, 2014, 34(1): 75-85. doi: 10.3724/SP.J.1140.2014.01075
引用本文: 岳保静, 廖晶, 刘鸿, 曾洁, 施剑. 中朝-扬子板块碰撞结合带东部边界及海域延伸[J]. 海洋地质与第四纪地质, 2014, 34(1): 75-85. doi: 10.3724/SP.J.1140.2014.01075
YUE Baojing, LIAO Jing, LIU Hong, ZENG Jie, SHI Jian. EAST BOUNDARY OF THE COLLISION BELT BETWEEN SINO-KOREAN AND YANGTZE PLATES IN EASTERN CHINA AND THEIR EXTENSION IN THE SEA[J]. Marine Geology & Quaternary Geology, 2014, 34(1): 75-85. doi: 10.3724/SP.J.1140.2014.01075
Citation: YUE Baojing, LIAO Jing, LIU Hong, ZENG Jie, SHI Jian. EAST BOUNDARY OF THE COLLISION BELT BETWEEN SINO-KOREAN AND YANGTZE PLATES IN EASTERN CHINA AND THEIR EXTENSION IN THE SEA[J]. Marine Geology & Quaternary Geology, 2014, 34(1): 75-85. doi: 10.3724/SP.J.1140.2014.01075

中朝-扬子板块碰撞结合带东部边界及海域延伸


doi: 10.3724/SP.J.1140.2014.01075
详细信息
    作者简介:

    岳保静(1981-),女,硕士,海洋地质与地球物理专业,E-mail:selinayue1022@yahoo.com.cn

  • 基金项目:

    国家自然科学基金项目(41106060);国土资源部海洋油气资源与环境地质重点实验室开放基金项目(MRE201122)

  • 中图分类号: P736.1

EAST BOUNDARY OF THE COLLISION BELT BETWEEN SINO-KOREAN AND YANGTZE PLATES IN EASTERN CHINA AND THEIR EXTENSION IN THE SEA

More Information
  • 摘要: 总结了中朝-扬子板块碰撞结合带的边界划分的各类观点,分析了存在争议的原因以及研究的不足之处。通过对苏鲁造山带及黄海海区的重磁资料、周缘断裂特征、典型地震剖面等最新研究成果的收集整理,研究认为华北扬子板块的碰撞结合带应为苏鲁超高压变质带-千里岩隆起,结合带在陆地的北边界可能为五莲-青岛-牟平断裂;南边界为连云港-黄梅断裂;千里岩南缘断裂在印支期是一条千里岩超高压变质带折返的边界断裂,白垩纪以来反转为一条控制南黄海北部坳陷的大型边界断裂,并指出加强黄海海域重磁震资料的精细研究及海陆结合带的构造关系研究是进一步研究重点。
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出版历程
  • 收稿日期:  2012-08-05
  • 修回日期:  2012-09-15

中朝-扬子板块碰撞结合带东部边界及海域延伸

doi: 10.3724/SP.J.1140.2014.01075
    作者简介:

    岳保静(1981-),女,硕士,海洋地质与地球物理专业,E-mail:selinayue1022@yahoo.com.cn

基金项目:

国家自然科学基金项目(41106060);国土资源部海洋油气资源与环境地质重点实验室开放基金项目(MRE201122)

  • 中图分类号: P736.1

摘要: 总结了中朝-扬子板块碰撞结合带的边界划分的各类观点,分析了存在争议的原因以及研究的不足之处。通过对苏鲁造山带及黄海海区的重磁资料、周缘断裂特征、典型地震剖面等最新研究成果的收集整理,研究认为华北扬子板块的碰撞结合带应为苏鲁超高压变质带-千里岩隆起,结合带在陆地的北边界可能为五莲-青岛-牟平断裂;南边界为连云港-黄梅断裂;千里岩南缘断裂在印支期是一条千里岩超高压变质带折返的边界断裂,白垩纪以来反转为一条控制南黄海北部坳陷的大型边界断裂,并指出加强黄海海域重磁震资料的精细研究及海陆结合带的构造关系研究是进一步研究重点。

English Abstract

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