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Water-soluble gas accumulation process of Hetianhe gas field in Tarim Basin,NW China

QIN Sheng-fei~(1),ZOU Cai-neng~(1),DAI Jin-xing~(1),LI Mei~(2),HU Jian-feng~(2),ZHANG Qiu-cha~(2),LU Yu-hong~(2)(1.Research Institute of Petroleum Exploration & Development,PetroChina,Beijing 100083,China;2.Exploration & Development Research Institute,Tarim Oilfield Company,Xinjiang 841000,China)  
The Hetianhe gas field of Tarim Basin has excellent geological conditions for water-soluble gas accumulation.The gases exhibit very good water-soluble characteristics.The traps were formed during the Late Himalaya orogeny,when the gases generated by highly mature Cambrian source rock were largely dissolved in water.Subsequent faulting allowed the gas charged water to migrate towards Ordovician and Carboniferous traps in the eastern part of the field.As the pressure and temperature decreased,some gases were released from water and gas reservoirs were formed.The water beneath the gas-water interface subsequently migrated along the unconformity for a long distance from the eastern high-pressure part towards the western low-pressure part of the field.During the horizontal migration,the gases were gradually released as pressure decreased.A chain-like cluster of gas pools was formed.The migration history has made the migration parameters of the water soluble gases increase significantly from west to east and caused a drier gas coefficient,a higher CO_(2) content and heavier δ~(13)C_(1).
【Fund】: “十五”国家重点科技攻关项目“中国大中型气田勘探开发关键技术研究”(2001BA605A-06)
【CateGory Index】: P618.13
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