摘要
Generally, the time of natural gas accumulation is late. But the filling history of the Carboniferous natural gas in the Dinan uplift-Wucaiwan of Junggar Basin gives a special sample. Natural gas has low dryness coefficient of 0.92 and N2 content of 3.04%, but the δ13C1 value of -32.12‰ indicates that natural gas would be at the highly mature stage. By means of genetic origin of natural gas and recovery of filling history, the authors consider that natural gas was formed at early stage but accumulate at late stage in the Dinan uplift-Wucaiwan of Junggar basin. There are three stages of gas accumulation, including late Hercynian, late Indo-Chinese and middle Yanshan, but the Yanshan is the main stage of gas accumulation. At Yanshan Era, natural gas was derived from the Carboniferous source rock with thermal maturity of 0.8%~1.2%RO, causing methane enriched in 13C.