天然气地质学

潮水盆地与酒西盆地中新生代构造对比

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  • 中国石化中原油气高新股份有限公司; 河南郑州;
李双泉(1963-),男,河南安阳人,经济师,在职博士,主要从事油气开发地质研究.E-mail:zje33@sina.com.

收稿日期: 2005-06-11

  修回日期: 2005-07-19

  网络出版日期: 2005-08-20

STRUCTURAL COMPARABLITY OF CHAOSHUI BASIN AND JIUXI BASIN IN MESOZOIC AND CENOZOIC

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  • Zhongyuan Oil and Natural Gas High-technique Limited Company, SINOPEC, Zhengzhou 457000, China

Received date: 2005-06-11

  Revised date: 2005-07-19

  Online published: 2005-08-20

摘要

指出潮水盆地与酒西盆地的中新生代构造具有很好的相似性:中生代盆地为走滑拉分盆地,发育张扭伸展断层系(边界走滑断裂,盆内伸展正断层),一级构造单元为断陷、断隆;新生代盆地是陆内前陆盆地,发育扭压逆冲断裂系,盆地一侧发育逆冲推覆体,一级构造单元为逆掩冲断褶皱区、坳陷、斜坡。认为可以利用酒西盆地的资料和勘探成果认识潮水盆地,借助酒西盆地的勘探经验指导潮水盆地的下一步勘探。

本文引用格式

李双泉 . 潮水盆地与酒西盆地中新生代构造对比[J]. 天然气地球科学, 2005 , 16(4) : 464 -468 . DOI: 10.11764/j.issn.1672-1926.2005.04.464

Abstract

The structure of Chaoshui basin and Jiuxi basin have better comparability in Mesozoic and Cenozoic: the basins in Mesozoic are both skip and pull apart basins, the basin in Cenozoic are both intracontinental foreland basins, they both develop tenso-shear and extension fault systems in Mesozoic (the boundary is skip fault, the interior of basin is extension fault), they both develop shear-compression and thrust fault systems in Cenozoic, and develop thrust nappe on one side of the basin.

参考文献

[1]严宝年,陈建军,范铭涛.酒泉盆地酒西坳陷前陆冲断带成藏条件及勘探前景[A].贾承造.中国中西部前陆盆地冲断带油气勘探文集[C].北京:石油工业出版社, 2002.256-267.
[2]肖文华,魏军.祁连山北缘逆掩推覆带构造及成藏特征[J].新疆石油地质,2003,24(6): 533-535.
[3] 赵应成,周晓峰,王崇孝,等酒西盆地青西油田白垩系泥云岩裂缝油藏特征和裂缝形成的控制因素[J].天然气地球科学,2005,16(1):12-15.
[4]河西走廊盆地前陆冲断带勘探前景及对策[A].贾承造.中国中西部前陆盆地冲断带油气勘探文集[C].北京: 石油工业出版社,2002.234-255.

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