施和生, 牛成民, 胡安文, 李慧勇, 于海波. 渤中西南环中深层油气相态特征及其控制因素[J]. 石油钻采工艺, 2018, 40(S1): 9-13. DOI: 10.13639/j.odpt.2018.S0.003
引用本文: 施和生, 牛成民, 胡安文, 李慧勇, 于海波. 渤中西南环中深层油气相态特征及其控制因素[J]. 石油钻采工艺, 2018, 40(S1): 9-13. DOI: 10.13639/j.odpt.2018.S0.003
SHI Hesheng, NIU Chengming, HU Anwen, LI Huiyong, YU Haibo. Phase characteristic of middle and deep hydrocarbon in the southwest zone of Bozhong sag and its controlling factors[J]. Oil Drilling & Production Technology, 2018, 40(S1): 9-13. DOI: 10.13639/j.odpt.2018.S0.003
Citation: SHI Hesheng, NIU Chengming, HU Anwen, LI Huiyong, YU Haibo. Phase characteristic of middle and deep hydrocarbon in the southwest zone of Bozhong sag and its controlling factors[J]. Oil Drilling & Production Technology, 2018, 40(S1): 9-13. DOI: 10.13639/j.odpt.2018.S0.003

渤中西南环中深层油气相态特征及其控制因素

Phase characteristic of middle and deep hydrocarbon in the southwest zone of Bozhong sag and its controlling factors

  • 摘要: 在渤中西南环中深层已发现3个油气藏,油气相态分布复杂。结合油气藏形成与分布的地质和地球化学条件,综合分析了渤中西南环中深层油气相态分布特征和控制因素。结果表明:渤中西南环北部曹妃甸18-2和渤中13-1构造的油气相态分别带油环的凝析气藏和高挥发性油藏,南部渤中19-6构造油气相态为凝析气藏。油气相态主要受烃源岩差异热演化、气侵和温压条件所控制。曹妃甸18-2和渤中13-1构造油气主要来源为邻近东营组三段烃源岩;渤中19-6油气主要来源为邻近沙河街组烃源岩,东营组三段和沙河街组三段烃源岩热演化程度差异决定了其烃类物质的差异,是造成目前油气相态的主要原因。晚期渤中19-6构造气侵明显较曹妃甸18-2和渤中13-1强,是影响油气相态的关键因素。温度和压力是影响油气相态的重要因素。

     

    Abstract: Three oil and gas reservoirs have been discovered in the middle and deep layers in the southwest zone of Bozhong sag, and their phase distribution of hydrocarbon is complicated.In this paper, the phase distribution characteristic of middle and deep hydrocarbons in the southwest zone of Bozhong sag and its controlling factors are analyzed comprehensively based on the geological and geochemical conditions for the formation and distribution of oil and gas reservoirs.It is indicated that the phase behavior of hydrocarbon in Caofeidian 18-2 structure and Bozhong 13-1 structure in the northern part of southwest zone of Bozhong sag is a condensate gas reservoir with oil rim and a high volatile oil reservoir, respectively, and that in Bozhong 19-6 structure in the southern part is a condensate gas reservoir.The phase behavior of hydrocarbon is mainly controlled by differential thermal evolution of source rocks, gas invasion and temperature-pressure condition.The hydrocarbons in Caofeidian 18-2 structure and Bozhong 13-1 structure are mainly generated by the adjacent Ed3 source rocks, and the hydrocarbon in Bozhong 19-6 structure are mainly derived from the adjacent source rocks of Shahejie Formation.The difference of thermal evolution degree between Ed3 source rocks and Shahejie Formation source rocks playsa decisive role in the difference of hydrocarbons, and it is the main reason for the current phase behavior of hydrocarbon.Gas invasion is the key factor influencing the phase behavior of hydrocarbon, and the gas invasion in Bozhong 19-6 structure is much stronger than that in Caofeidian 18-2 structure and Bozhong 13-1 structure in the late stage.And temperature and pressure are the important factors influencing the phase behavior of hydrocarbon.

     

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