STRUCTURAL COMPARABLITY OF CHAOSHUI BASIN AND JIUXI BASIN IN MESOZOIC AND CENOZOIC
Received date: 2005-06-11
Revised date: 2005-07-19
Online published: 2005-08-20
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.
Key words： Mesozoic; Cenozoic; Petroliterous basin; Structure; Comparability; Chaoshui basin; Jiuxi basin.
LI Shuang-quan . STRUCTURAL COMPARABLITY OF CHAOSHUI BASIN AND JIUXI BASIN IN MESOZOIC AND CENOZOIC[J]. Natural Gas Geoscience, 2005 , 16(4) : 464 -468 . DOI: 10.11764/j.issn.1672-1926.2005.04.464
[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.
/
| 〈 |
|
〉 |
甘公网安备 62010202000678号