地学前缘 ›› 2009, Vol. 16 ›› Issue (4): 117-137.

• 论文 • 上一篇    下一篇

济阳坳陷深层构造及其对中新生代盆地发育的控制作用

  

  1. 1中国地质大学(武汉) 教育部构造与油气资源重点实验室, 湖北 武汉 430074
    2教育部 含油气盆地构造研究中心, 湖北 武汉 430074
    3中国石油化工集团公司 胜利油田有限公司 地球物理勘探研究院, 山东 东营 257001
    4中国地质大学(武汉) 经济管理学院, 湖北 武汉 430074

  • 出版日期:2009-08-01 发布日期:2009-08-01
  • 作者简介:任建业(1963—),男,博士,教授,博士生导师,资源勘查工程专业,现主要从事沉积盆地分析和构造地质方面的教学和研究工作。Email: jyren@cug.edu.cn
  • 基金资助:

    国家自然科学基金项目(40672089)

 Structures of deep bed in Jiyang Sag and their control over the development of Mesozoic and Cenozoic basins.

  1. 1Key Laboratory of Tectonics and Petroleum Resources,Ministry of Education and Sinopec, China University of Geosciences, Wuhan 430074, China
    2Tectonic Research Center of HydrocarbonBearing Basin, Ministry of Education, Wuhan 430074, China
    3Geophysical Research Institute, Shengli Oilfield, SINOPEC, Dongying 257001, China
    4School of Economy and Management, China University of Geosciences, Wuhan 430074, China

  • Online:2009-08-01 Published:2009-08-01

PDF (PC)

1101

摘要：

以3D地震资料和钻井资料的解释为基础,通过对济阳坳陷深层进行构造地层分析和构造解析,系统阐明了中、新生代各期构造运动在研究区的地质表现,确定出收缩构造系统、伸展构造系统和走滑构造系统等多期构造样式;提出印支期逆冲断层系由多条显著向NE或NNE向凸出的弧形展布断裂系组成;识别出代表燕山主期构造运动的不整合界面(Tgm),确定了J3—K1时期断陷盆地的分布格局;认为印支期逆冲断裂系统是控制本区晚中生代和新生代早期盆地发育的重要的控制性先存基底构造。在区域动力学分析的基础上探讨了该盆地复杂的叠合结构和山脉盆地的转换过程及机制。从盆地研究的角度,揭示了华北东部中、新生代陆内动力学过程,对于研究区油气勘探实践具有重要意义。

关键词: 关键词：济阳坳陷;负反转构造;构造体制转折;中、新生代盆地

Abstract:

 Based on interpretations of the 3D seismic  and well data, we have systematically elucidated the geological representations of Mesozoic and Cenozoic tectonic movements in Jiyang Sag, Bohaiwan Basin. The compressional tectonic system, the extensional tectonic system and the strike slipping tectonic system, which developed in different tectonic evolution stages, have been determined in this paper. The thrusts during Indosinian Movement consist of several arc thrusts protruding to NE or NNE direction, and negative inversion of these thrust controlled strongly the development of late Mesozoic and early Cenozoic basins. The unconformity (Tgm) indicating the main episode of Yanshan Movement has been identified clearly in seismic profiles, and the distribution pattern and the type of late Mesozoic basin in Jiyang Sag have also been determined. Combined with the analysis of regional tectonic dynamic setting, the complicated superposition structure and basinmountain conversion mechanism have been discussed. From the study of tectonic and evolution of sedimentary basin, we have revealed the Mesozoic and Cenozoic intracontinental dynamic process of eastern North China Block, which will be of benefit to the hydrocarbon exploration in the study area.

Key words:

Key words: Jiyang Sag; negative inversion structure; transform of tectonic mechanism; Mesozoic and Cenozoic basins

中图分类号: