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Geochemical characteristics and accumulation of hydrocarbon in Lower Jurassic tight sandstone in Wenjisang area, Turpan Basin, NW China

机译:NW中国吐鲁番地区下侏群地区下侏罗斯封砂岩中烃地球化学特征及积累

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摘要

In order to investigate the geochemical characteristics, sources and accumulation process of Lower-Jurassic Sangonghe Formation tight sandstone oil, multiple geochemical analyses were performed on source rocks, oil samples and sandstone particles from Wenjisang area in Turpan Basin. The results show that coal-measure source rocks have relatively higher organic matter abundance and type-ll organic matter for Xishanyao and Badaowan Formations, with the potential of liquid hydrocarbon generation. Oil samples of Sangonghe Formation have the characteristics of coal-measure-formed oil. Higher maturity indicate the oil may be mainly generated by Lower-Jurassic Badaowan Formation source rocks. Quantitative fluorescence parameters also reflect that hydrocarbons charged into Sangonghe Formation through continuous migration from the bottom of sand body to the top gradually. In down dip direction of Wenjisang area may develope continuous tight oil and gas reservoirs in Lower Jurassic.
机译:为了研究下侏罗统三工河组致密砂岩油的地球化学特征、油源及成藏过程,对吐鲁番盆地温吉桑地区的烃源岩、油样和砂岩颗粒进行了多种地球化学分析。结果表明,西山窑组和八道湾组煤系烃源岩具有较高的有机质丰度和ll型有机质,具有液态烃生成潜力。三工河组油样具有煤系成油特征。成熟度越高,表明原油可能主要由下侏罗统八道湾组烃源岩生成。定量荧光参数也反映了油气从砂体底部逐渐向顶部连续运移进入三工河组。文济桑地区下倾方向下侏罗统可能发育连续致密油气藏。

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