收稿日期: 2006-11-15
修回日期: 2007-03-02
网络出版日期: 2008-06-20
基金资助
“十五”国家重点科技攻关项目(编号:2001BA605A-06)资助.
HYDROCARBON ACCUMULATION OF FOUR ASSOCIATION TYPES OF FORELAND BASINS IN CENTRAL AND WESTERN CHINA:PART Ⅰ.GEOLOGICAL CONDITIONS
Received date: 2006-11-15
Revised date: 2007-03-02
Online published: 2008-06-20
赵孟军,宋 岩,柳少波,秦胜飞,洪 峰,傅国友,达 江 . 中国中西部4种组合类型前陆盆地成藏研究:I.油气成藏地质条件分析[J]. 天然气地球科学, 2007 , 18(2) : 181 -186 . DOI: 10.11764/j.issn.1672-1926.2007.02.181
Foreland basins are important areas of exploration for petroleum in China. According to the basin construction and evolution, the foreland basins in central andwestern China can be divided into four types of assemblages including the presenile, the reconstructed, the regenerated and the superimposed. This paper discusses the geological conditions of accumulation, such as the assemblages of sourcerock, reservoir and seal, in different foreland basins based on the examples ofnorthwestern Junggar foreland basin (the presenile), western Sichuan foreland basin (the reconstructed), northern Chaidamu foreland thrust (the regenerated) and southern Junggar foreland basin (the superimposed). The thermal evolutionsof main source rocks are stated in the four types of foreland basins. The foreland development in the late period of Himalayan movement has an obvious control on the thermal evolution of source rocks in the Chaidamu foreland thrust (the regenerated) and southern Junggar foreland basin (the superimposed).
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