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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2009-04
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Characteristic and accumulation process of the natural gas from Sinian to Lower Paleozoic in Sichuan Basin,China

LIU Shu-gen1,MA Yong-sheng2,CAI Xun-yu2,XU Guo-sheng1,WANG Guo-zhi1,YONG Zi-quan1,SUN Wei1,YUAN Hai-feng1,PAN Chang-lin2 1.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology,Chengdu 610059,China;2.Southern Exploration and Development Branch Co.,SINOPEC,Chengdu 610041,China  
There are three sets of oil-type hydrocarbon source rocks from Sinian to Lower Paleozoic in Sichuan basin.These source rocks are good in the oil-generating potential and hydrocarbon-generating intensity and have secondly generating hydrocarbon capacity by the influence of the Caledonian uplifting movement.The Triassic is the period of forming the main traps and the peak of the secondary oil generation,and the huge amount of oil migrated and accumulated in the area of the Leshan-Longnüsi paleo-uplift and formed Sinian to Lower Paleozoic paleo-oil pools.With the increase of buried depth and the rise of temperature and pressure,the oil cracked to gas,and the paleo-oil pools became the source of gas and formed paleo-gas pools.The traps were modified and the gas pools were rearranged by strong uplifts and erosion during Himalayan movement.Finally the present gas pools formed.Hence,the accumulation process of natural gas from Sinian to Lower Paleozoic in Sichuan basin is a transforming process from paleo-oil pools to paleo-gas pools to present gas pools with the characteristics of difference in generation and expulsion,multi-stage migration and accumulation,early accumulation and late pool formation.
【Fund】: 国家重点基础研究发展计划“973”项目(2005CB422106)
【CateGory Index】: P618.13
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