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Patterns of intercalation in alluvial fan reservoirs—A case study of Lower Karamay Formation, Yizhong Area, Karamay Oilfield, NW China

机译:冲积扇储层的夹层模式-以西北地区克拉玛依油田宜中地区下克拉玛依组为例

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This paper discusses the overall distribution characteristics of alluvial fan in the Triassic Lower Karamay Formation, Yizhong Area, the Karamay Oilfield, with core, outcrop, logging and seismic data. On this basis, the shapes, sizes and stacking patterns of intercalations in different levels and sub-facies are analyzed using the hierarchy bounding surfaces method. In the study area, the Lower Karamay Formation contains (from bottom to top) root fan, middle fan and outer fan deposits, with size-reducing grains, as a complete retrograding sedimentary sequence. The intercalation in the alluvial fan reservoir can be divided into two types: lithological intercalation (fine sediments) and physical intercalation (argillaceous sandstone/conglomerate). Origin, pattern and size of intercalations vary significantly in different sub-facies zones. In particular, the intercalations in root fan are “scattered generally and interlaced locally”, presenting as partially discontinuous screen in a high-permeable network; the intercalations in middle fan are relatively stable intercalations and lateral intercalations, with a higher capacity to shade or screen the seepage; the intercalations in outer fan present as a layered cake, with reservoir bodies mosaic-like along the source and lenticular in perpendicularity to the source that are separated by thick barrier beds, showing the highest capacity of screen.
机译:通过岩心,露头,测井和地震资料,探讨了克拉玛依油田宜中地区三叠系下克拉玛依组冲积扇的总体分布特征。在此基础上,利用层次边界面方法分析了不同层次和亚相的插层的形状,大小和堆积方式。在研究区,下克拉玛依组包含(从下到上)根扇形,中扇形和外扇形沉积物,并具有减小粒径的颗粒,作为完整的逆行沉积序列。冲积扇储层的插层可分为两种:岩性插层(细小沉积物)和物理插层(泥质砂岩/砾岩)。插层的成因,样式和大小在不同的亚相区域差异很大。尤其是,根扇形中的插层“普遍散布并局部交错”,在高渗透性网络中呈现为部分不连续的筛网。中间风机的插层为相对稳定的插层和横向插层,具有较高的遮挡或遮挡渗流能力。外扇的夹层以层状蛋糕的形式出现,储层体沿水源呈马赛克状,与水源垂直的双凸透镜被厚厚的屏障层隔开,显示出最高的筛分能力。

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