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Types of subtle buried-hill oil reservoirs and their accumulation simulation in Jizhong Depression, Bohai Bay Basin

机译:渤海湾盆地冀中De陷隐蔽潜山油藏类型及成藏模拟

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The types of subtle buried-hill resevoirs and their accumulation characteristics are analyzed based on the exploration progression of subtle buried-hill reservoirs in the Jizhong Depression in recent years. These reservoirs are classified into buried-hill head reservoirs that are easy to discover, and buried-hill-slope reservoirs and intra-buried-hill reservoirs that are difficult to discover. Effective seal is the key factor for the formation of intra-buried-hill reservoirs, and hill controlling faults are the important hydrocarbon migration pathways. As for buried-hill-slope reservoirs, two sealing conditions must be satisfied, including argillaceous caprocks on top of the unconformities and intra-buried-hill barriers on the flank, as well as unconformities acting as primary migration pathways. Simulation experiments on petroleum migration and accumulation using a 2D experimental model show that the preferential charging location of hydrocarbons is determined by the charging force and the permeability ratio of transport pathways (faults or unconformities) to buried-hill reservoirs. When faults or unconformities are highly efficient transport pathways, hydrocarbons will preferentially charge the top of the buried hills, thus forming buried-hill head reservoirs. If faults or unconformities are poor in permeability or highly heterogeneous, hydrocarbons will charge the internal layers or slopes of buried hills, forming intra-buried-hill reserovirs or buried-hill-slope reservoirs when there are high-permeability reservoir rocks within the internal layers or slopes of the buried hills.
机译:根据近年来冀中De陷潜山隐蔽油藏的勘探进展,分析了潜山隐蔽储层的类型及其成藏特征。这些油藏分为容易发现的潜山头储层和难以发现的潜山坡储层和潜山内储层。有效的封闭是形成潜山内储层的关键因素,而控山断层是重要的油气运移路径。对于潜山斜坡油藏,必须满足两个密封条件,包括不整合顶部的泥质盖层和侧面的潜山内部屏障,以及不整合作为主要的迁移途径。使用二维实验模型进行的石油运移和聚集模拟实验表明,碳氢化合物的优先装填位置取决于装填力和运输路径(断层或不整合面)对潜山油藏的渗透率。当断层或不整合面是高效的运输途径时,碳氢化合物将优先向潜山顶部充填,从而形成潜山头储层。如果断层或不整合面的渗透性差或高度非均质性,则当内层中存在高渗透性储集层岩石时,碳氢化合物将使潜山的内层或斜坡充填,从而形成潜山内的反渗透病毒或潜山斜坡油藏。或埋山的斜坡。

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