THE INFLUENCE TO THE ACCUMULATION OF OIL AND GAS, OF THEDEVELOPMENT OF THE ARCUATE STRUCTURE ZONE IN THE TRANSITION ZONE FRO M THE PLAT TO THE GEOSYNCLINE IN THE WEST OF ORDOS BASIN
Received date: 2005-06-02
Revised date: 2005-07-06
Online published: 2005-08-20
In the transition zone from the plat to the geosyncline in the west of Ordos Basin, because of the development of Paleozoic arcuate rift system, the land mass was deformed into arcuate structure zone with structural blocks north and south, structural zones east and west, swells and sags. And the distribution and accumulation of oil and gas was controlled by the arcuate structure zone. And the zone, which experienced the later transformation and coupling and deformation, is an important exploration region.
Key words： Rift; Arcuate structure zone; Impactogen; Hydrocarbon accumulation.
WANG Shao-chang +1, FU Suo-tang +2, LI Xi-zhe +1, FU Jin-hua +2, SUN Fen-jin +1, JIANG Zheng-long +1 . THE INFLUENCE TO THE ACCUMULATION OF OIL AND GAS, OF THEDEVELOPMENT OF THE ARCUATE STRUCTURE ZONE IN THE TRANSITION ZONE FRO M THE PLAT TO THE GEOSYNCLINE IN THE WEST OF ORDOS BASIN [J]. Natural Gas Geoscience, 2005 , 16(4) : 421 -427 . DOI: 10.11764/j.issn.1672-1926.2005.04.421
[1]王少昌.鄂尔多斯盆地上古生界煤成气地质条件分析[J].石油勘探与开发，1982.
[2]王红岩，张建博，陈孟晋，等鄂尔多斯盆地煤层气与深盆气的关系[J].天然气地球科学，2003，14(6)：453-455.
[3]张抗.鄂尔多斯断块构造和资源[M].西安：陕西科学技术出版社，1989.
[4]杨俊杰.鄂尔多斯盆地西缘掩冲带构造与油气[M].兰州：甘肃科学出版社，1990.
[5] 李振宏，郑聪斌鄂尔多斯盆地东部奥陶系储层特征及控制因素[J].天然气地球科学，2004，15(6)：604-609.
[6] 长庆油田石油地质志编写组.中国石油地质志(卷十二)[M].北京：石油工业出版社，1993.
[7] 林畅松.贺兰拗拉槽充填演化分析[M].北京：地质出版社，1995.
[8] 煤田地质总局.鄂尔多斯盆地聚煤规律及煤炭资源评价[M].北京：煤炭工业出版社，1996.
[9] 尚冠雄.华北地台晚古生代煤地质学研究[M].太原：山西科学技术出版社，1997.
[10] 戴金星.我国煤系的气油地球化学特征，煤成气藏形成条件及资源评价[M].北京：石油工业出版社，2001.
[11] 戴金星，秦胜飞，陶士振，等中国天然气工业发展趋势和天然气地学理论重要进展[J].天然气地球科学，2005，16(2)：127-142.
[12] 杨俊杰.鄂尔多斯盆地构造演化与油气分布规律[M].北京：石油工业出版社，2002.
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