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Relationship between sandstone architecture and remaining oil distribution pattern: A case of the Kumkol South oilfield in South Turgay Basin, Kazakstan

机译:砂岩构造与剩余油分布模式之间的关系:以哈萨克斯坦南部图尔盖盆地的库姆库尔南部油田为例

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Taking the Kumkol South oilfield in South Turgay Basin, Kazakstan as an example, this article summarizes the controlling pattern of different types of sandstone architecture on remaining oil distribution through examining architecture characteristics, development effect and remaining oil distribution characteristics of meandering river sandstone, braided river sandstone and delta sandstone. The braided river sandstone has simple architecture which is extensive connecting body with horizontal mud-interlayers. The water flooding sweeps evenly and the edge-bottom water drives quickly in braid river sandstone. And the remaining oil distribution pattern of braid river sandstone is the vertical blocking pattern controlled by the horizontal mud-interlayers at the high water cut stage. The meandering river sandstone is a half connecting body with abandoned channels and the lateral accretion mud-interlayers, so the injected water sweeps through the middle and lower parts of point bar sandstone, and its remaining oil distribution pattern is the horizontal blocking pattern controlled by abandoned channels and the lateral accretion mud-interlayers. The delta sandstone has a complex architecture of mosaic structure with abundant horizontal and vertical mud-interlayers and mud-interbeds, in which the injected water sweeps along preferential path, with low sweeping efficiency, and the remaining oil distribution pattern is the complex blocking pattern controlled by horizontal and vertical mud-interlayers and mud-interbeds. The results show that different techniques should be used to enhance the remaining oil recovery because of the different remaining oil distribution patterns in different kind of sand bodies.
机译:以哈萨克斯坦南部图尔盖盆地的库姆库尔南部油田为例,通过研究曲流河砂岩,辫状河的建筑特征,开发效果和剩余油分布特征,总结了不同类型砂岩建筑对剩余油分布的控制模式。砂岩和三角洲砂岩。辫状河砂岩结构简单,连通体与水平泥浆夹层广泛。洪水泛滥,辫状河砂岩中的底水迅速驱散。辫状河砂岩的剩余油分布模式是在高含水期由水平泥浆夹层控制的垂直阻塞模式。蜿蜒的河砂岩是一个半连接体,具有废弃的河道和横向增生的泥质夹层,因此注入的水扫过点状棒砂岩的中下部,其剩余的油分布模式是由废弃控制的水平阻塞模式。通道和横向增生的泥质夹层。三角洲砂岩具有复杂的镶嵌构造,水平和垂直泥浆夹层和泥浆夹层丰富,其中注入的水沿优先路径扫掠,扫掠效率低,剩余的油分布模式是控制的复杂阻塞模式。由水平和垂直泥浆夹层和泥浆夹层组成。结果表明,由于不同种类砂体中剩余油分布方式的不同,应采用不同的技术来提高剩余油的采收率。

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