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作 者:杨申谷[1,2] 胥洪成[3] 何幼斌[4] 吴东胜[4] 李世雄[4]
机构地区:[1]中国地质大学(武汉)资源学院,湖北武汉430074 [2]长江大学期刊社,地球科学学院,河北廊坊065007 [3]中国科学院渗流流体力学研究所,中石油勘探开发研究院廊坊分院,湖北荆州434023 [4]长江大学地球科学学院
出 处:《石油天然气学报》2006年第6期35-37,共3页Journal of Oil and Gas Technology
基 金:国家自然科学基金项目(40272060);高等学校优秀青年教师教学科研奖励计划项目(教人司[2002]123号)。
摘 要:叙述了曙一区馆陶组稠油至超稠油的地质特征,查明了油藏的形成机理及油藏分布的控制因素;认为该油藏为自凝结型稠油油藏,原油来自下伏兴隆台油层,原油在运移和成藏过程中,经历水洗作用,使原油粘度增加、凝固点降低,由于原油凝固点温度高于地层温度,原油自凝结形成沥青壳圈闭而聚集成藏,油藏的分布受油源位置、原油密度、粘度和凝固点的控制。The geologic characteristics of viscous and super-viscous oil reservoirs in Guantao Formation of Shuyi Region are denoted. The reservoir forming mechanism and the control factors of reservoir distribution are investigated. It is considered that the reservoir is a self condensate viscous reservoir, where oil is from the underlying Xinglongtai reservoir and it is water flushed during the migration and reservoir forming process. Thus its viscosity increases, condensate point decreases. Because the temperature at its condensate point is higher than that of formation, an asphaltic trap resulted by oil of self condensation is accumulated to be the reservoir, its distribution is controlled by oil position, density, viscosity and its condensate point.
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