石油与天然气地质 ›› 1998, Vol. 19 ›› Issue (1): 63-67.doi: 10.11743/ogg19980111

• 论文 • 上一篇    下一篇

渤海湾盆地构造格架及演化

李军1, 王燮培2   

  1. 1. 江汉石油学院物探系, 湖北荆州434102;
    2. 中国地质大学, 湖北武汉430074
  • 收稿日期:1997-06-20 出版日期:1998-03-25 发布日期:2012-01-18

STRUCTURAL FRAMEWORK AND EVOLUTION OF BOHAI BAY BASIN

Li Jun1, Wang Xiepei2   

  1. 1. Jianghan Petroleum Institute, Jingzhou, Hubei;
    2. China University of Geosciences, Wuhan, Hubei
  • Received:1997-06-20 Online:1998-03-25 Published:2012-01-18

PDF (PC)

1298

被引次数

34

摘要：

渤海湾盆地早第三纪存在独特的构造格局,呈以渤中凹陷为中心的放射状断裂体系和环状断裂体系,这种格局是地幔物质底辟作用的结果。盆地自早第三纪以来经历了两次构造热冷缩沉降过程。地幔初始隆起时,地壳减薄盆地进入断层控制的沉降阶段,之后地幔温度降低,盆地进入热冷缩沉降阶段

关键词: 盆地, 构造格架, 演化, 地幔, 渤海湾

Abstract:

An unique structural framework of Early Tertiary exists in Bohai Bay Basin,its radiate fault system and circular fault system are distributed around Bozhong Depression.The framework resulted from mantle diapirism.The Bohai Bay Basin has undergone two faulting thermal contraction stages ever since Early Tertiary.When the mantle swelled initially,the earth crust thinned,the basin began its faulting-controlled subsidence.Then the mantle’s temperature decreased,the basin entered its thermal contraction subsidence.