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《ACTA PETROLEI SINICA》 1997-01
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TAPHROGENY OF TARIM SOUTH CHINA MASSIFAND ITS RELATED TO LOW PALEOZOIC OIL GAS IN SICHUAN BASIN

An Zuoxiang (Petroleum Industry Press)  
The Tarim south China massif was taphrogensised after Middle Triassic.Due to the change of the reginal tectonic pattern during the formation of the Sichuan basin,the lower Paleozoic hydrocarbon has been originated in Sichuan basin and has undertaken two and one proccesses of migration accumulation before and after the traphrogeny respectively.It is predicted that the present gas pools should be disduted at the margins of the broom anticlinal areas of the southeast Sichuan,where the conservation features would be better in the anticlines of the structural highs.
【CateGory Index】: P618.13
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