Research on Reservoir Sedimentary and Pore Characteristics of Chang 6 in Wuqi Oilfield

Fengxia Li, Zhengku Wang
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Abstract

In this paper, we utilized comprehensive geological analysis methods to identify sedimentary micro-facies in Wuqi Oilfield. Based on identification marks of sedimentary facies such as lithologic features, sedimentary structures and paleontological fossil, we classified the sedimentary micro-facies in this field into 4 types, including underwater distributary channel, mouth bar, distal bar and interdistributary bay facies. According to the observation of cores and casting thin sections, we made analysis on the pore characteristics of Chang 6 reservoir. The pore characteristic of target area is mainly intergranular space, which takes 3.27%, followed by feldspar and rock debris dissolution pore. The analysis shows that, the sedimentary thichness and grain size of underwater distributary channel are both quite big. The content of flake silicate mineral, for example, mica, is relatively low, but its porosity and permeability is high compared with mouth bar and distal bar. Interdistributary bay facies that has the lowest porosity and permeability are very strong.
吴起油田长6储层沉积及孔隙特征研究
本文利用综合地质分析方法对吴起油田沉积微相进行了识别。根据岩性特征、沉积构造和古生物化石等沉积相识别标志,将本区沉积微相划分为水下分流河道相、河口坝相、远端坝相和分流间湾相4种类型。根据岩心和铸体薄片观察,对长6储层孔隙特征进行了分析。靶区孔隙特征以粒间孔隙为主,占3.27%,其次为长石孔隙和岩屑溶蚀孔隙。分析表明,水下分流河道的沉积厚度和粒度均较大。云母等片状硅酸盐矿物的含量相对较低,但其孔隙度和渗透率均高于口砂和远砂。而孔隙度和渗透率最低的分流间湾相则非常强。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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