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1An analysis of the types and distribution characteristics of natural gas reservoirs in China显示文摘The natural gas reservoir beds of different areas in China can be divided into three kinds,clastic natural gas reservoir bed,carbonate natural gas reservoir bed and special natural gas reservoir bed.They have different combination patterns controlled by deposition,diagenesis and tectonism.Our analysis indicates that the natural gas reservoirs are mainly distributed in the Precambrian,Palaeozoic,Mesozoic,and Tertiary-Quaternary.Craton basin,foreland basin and intracontinental rift basin which contain most of natural gas in China have special geological features and favorable accumulation conditions,and will be important exploration areas in the future.Xu Zhangyou Yue Dali Wu Shenghe Zhang Xiaoyu Chen Ce Ni Yuqiang 2009Petroleum Science2009,6,1:6
2Using geochemical tracing system to identify new types of gas sources in marine strata of the Hotan River Gas Field in the Tarim Basin显示文摘There are natural gas sources of various modes of occurrence in superimposed basins. Besides the conventional kerogen and ancient oil reservoir, dispersed soluble organic matter (DSOM) is an important direct gas source. Because of its wide distribution, great potential to generate gas and proneness to crack under catalysis, DSOM is an important type of gas source in the highly evolved zones in marine strata. Through the geological and geochemical analysis that reflects the long-period evolvement and multiple gas accumulation processes in marine strata, and using the ternary geochemical tracing system, here we study the origin and accumulation of the natural gas in the Hotan River Gas Field in the Tarim Basin. The natural gas is produced from highly evolved and cracked DSOM in the Hotan River Gas Field, and it is accumulated after migrating for a long distance along faults. This conclusion is of great significance to the further expansion of the oil and gas exploration fields in the Tarim Basin.WenHui Liu DianWei Zhang Bo Gao Ming Fan 2010Science China Earth Sciences2010,53,6:2
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