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渤海的形成及其深部动力学机制

牛树银 孙爱群 王孟科 左丽明 张训华 张福祥 侯江龙 徐萌 张建珍 陈超

牛树银, 孙爱群, 王孟科, 左丽明, 张训华, 张福祥, 侯江龙, 徐萌, 张建珍, 陈超. 渤海的形成及其深部动力学机制[J]. 海洋地质与第四纪地质, 2014, 34(6): 63-71. doi: 10.3724/SP.J.1140.2014.06063
引用本文: 牛树银, 孙爱群, 王孟科, 左丽明, 张训华, 张福祥, 侯江龙, 徐萌, 张建珍, 陈超. 渤海的形成及其深部动力学机制[J]. 海洋地质与第四纪地质, 2014, 34(6): 63-71. doi: 10.3724/SP.J.1140.2014.06063
NIU Shuyin, SUN Aiqun, WANG Mengke, ZUO Liming, ZHANG Xunhua, ZHANG Fuxiang, HOU Jianglong, XU Meng, ZHANG Jianzhen, CHEN Chao. THE FORMATION OF BOHAI SEA AND ITS DEEP DYNAMICS[J]. Marine Geology & Quaternary Geology, 2014, 34(6): 63-71. doi: 10.3724/SP.J.1140.2014.06063
Citation: NIU Shuyin, SUN Aiqun, WANG Mengke, ZUO Liming, ZHANG Xunhua, ZHANG Fuxiang, HOU Jianglong, XU Meng, ZHANG Jianzhen, CHEN Chao. THE FORMATION OF BOHAI SEA AND ITS DEEP DYNAMICS[J]. Marine Geology & Quaternary Geology, 2014, 34(6): 63-71. doi: 10.3724/SP.J.1140.2014.06063

渤海的形成及其深部动力学机制


doi: 10.3724/SP.J.1140.2014.06063
详细信息
    作者简介:

    牛树银(1952-),男,教授,主要从事构造地质学与构造成矿的教学与科研工作,E-mail:niusy@sjzue.edu.cn

  • 基金项目:

    河北省海洋综合图集(2013006);东方人类探源工程——泥河湾人类起源、地质及环境背景研究(13277611D);国家自然科学基金项目(40872137)

  • 中图分类号: P736.1

THE FORMATION OF BOHAI SEA AND ITS DEEP DYNAMICS

More Information
  • 摘要: 燕山运动以来,华北东部地区发生了翻天覆地之构造转变,构造体制从印支期末的地体拼贴、大陆增生,转变为地幔热柱多级演化——渤海海盆伸展裂陷的发展阶段。地形地貌上亦从东部的隆升高原转变为华北东部盆-岭构造,形成了以渤海地幔热柱为中心的大规模裂陷与外围一系列幔枝构造快速隆升的有机组合。渤海的形成是地幔热柱演化的浅部反映,表现为遍及全区强烈的构造运动、大规模的岩浆活动、区域性超变质作用,反映了燕山-喜马拉雅期强烈的幔壳活动。
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  • 收稿日期:  2014-03-21
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渤海的形成及其深部动力学机制

doi: 10.3724/SP.J.1140.2014.06063
    作者简介:

    牛树银(1952-),男,教授,主要从事构造地质学与构造成矿的教学与科研工作,E-mail:niusy@sjzue.edu.cn

基金项目:

河北省海洋综合图集(2013006);东方人类探源工程——泥河湾人类起源、地质及环境背景研究(13277611D);国家自然科学基金项目(40872137)

  • 中图分类号: P736.1

摘要: 燕山运动以来,华北东部地区发生了翻天覆地之构造转变,构造体制从印支期末的地体拼贴、大陆增生,转变为地幔热柱多级演化——渤海海盆伸展裂陷的发展阶段。地形地貌上亦从东部的隆升高原转变为华北东部盆-岭构造,形成了以渤海地幔热柱为中心的大规模裂陷与外围一系列幔枝构造快速隆升的有机组合。渤海的形成是地幔热柱演化的浅部反映,表现为遍及全区强烈的构造运动、大规模的岩浆活动、区域性超变质作用,反映了燕山-喜马拉雅期强烈的幔壳活动。

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