摘要
In this paper, the authors studied the properties and characteristics of the fluid,and found the changes of natural gas components and carbon isotope which confirm the accumulation of water-soluble gas by degasification,namely,such accumulation far away from gas source features high methane,high drying factor,high ratio of isoalkane to normal paraffin hydrocarbons,and heavy carbon isotope in methane and ethane. The authors conclude that the accumulation of water-soluble gas by degasification is not only one of the important mechanisms of development of large lithologic gas reservoirs and large gas accumulations in Central Sichuan,but also a key reason for poor source rocks in the Xu1 Member but large gas accumulation in the Xu2 Member in the Hechuan-Anyue area.