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A study on fluid inclusion of Permian-Jurassic in Turpan-Hami basin.

LIU Yi qun; et al. (Northwest University,Shanxi 710069, P. R. China).  
The research method of fluid inclusion has been adopted in the research procession of geothermal history of Turpan Hami basin in order to understand the origin, formation period and migration of oil and gas. Research results of fluid inclusion distributed in quartzs in Jurassic and pre Jurassic in Turpan Hami basin represent the features of the mixed hydrocarbon generation.The dominant hydrocarbon generating matters come from lacustrine low forms of life and high plants and their forming environment is of brackish and reduction. Measurement of homogenization temperature indicates the formation temperatures of organic inclusions are in the range of 60 195℃. The geothermal gradients of the Jurassic mostly fall from about 2.76℃/100m in the western basin to 3.41 ℃/100m in the eastern basin. The geothermal gradients in the Permian in the south of the basin are in the range of 3.37 4.12 ℃/100m. The maturing and migrating time of oil and gas is in the times of Jurassic Tertiary in Taibei sag located in the north of the basin and Toksum sag located in the southwest of the basin and in the times of Triassic in Tainan sag located in the south of the basin. The paleo fluid potential in the Triassic and Jurassic all shows the trend of being higher in the north than in the south, and indicates a regularity of oil and gas migration from north to south of the basin. The organic inclusion in these areas entered reservoirs along microfractures in tectonic movements.
【CateGory Index】: P618.13
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