ISSN 1009-6248CN 61-1149/P 双月刊

主管单位:中国地质调查局

主办单位:中国地质调查局西安地质调查中心
中国地质学会

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    延安气田延川东区山西组致密砂岩储层特征及有利区预测

    Characteristics of Shanxi Formation Tight Sandstone Reservoir in Yanchuan East Area of Yan'an Gas Field and Prediction of Favorable Areas

    • 摘要: 延安气田延川东区山西组致密砂岩储层具有复杂的岩石学特征与非均质性,明确其储层特征及有利区分布对天然气勘探开发具有重要意义。笔者通过岩石薄片鉴定、高压压汞实验、物性分析等手段,系统研究了山西组储层的岩石组分、孔隙结构、物性特征及成岩演化过程。结果表明:山西组储层以岩屑石英砂岩为主,石英平均含量为67.1%~71.8%,发育残余粒间孔、岩屑溶孔及微裂缝,孔喉结构以微细喉型为主,储层整体为特低孔、致密特征。山2段储集性能优于山1段,其孔隙度平均为4.74%,渗透率平均为0.764 mD。储层物性受粒度、塑性岩屑含量及碳酸盐胶结作用控制,粗粒砂岩及低塑性岩屑含量区域物性更优。结合沉积微相、砂体展布及构造特征,预测山1段有利区位于研究区中南部,山2段有利区呈条带状分布于中部及北部。本研究为鄂尔多斯盆地山西组致密气藏高效勘探提供了重要地质依据。

       

      Abstract: The tight sandstone reservoir of Shanxi Formation in Yanchuan East Area of Yan'an Gas Field has complex petrological characteristics and heterogeneity. Clarifying its reservoir characteristics and favorable area distribution is of great significance for natural gas exploration and development. This article systematically studied the rock composition, pore structure, physical properties, and diagenetic evolution process of the Shanxi Formation reservoir through methods such as rock thin section identification, high-pressure mercury injection experiments, and physical property analysis. The results show that the Shanxi Formation reservoir is mainly composed of lithic quartz sandstone, with an average quartz content of 67.1%~71.8%. Residual intergranular pores, lithic dissolution pores, and microcracks are developed, and the pore throat structure is mainly micro throat type. The overall reservoir is characterized by ultra-low porosity and compactness. The reservoir performance of Shan 2 section is better than that of Shan 1 section, with an average porosity of 4.74% and an average permeability of 0.764 mD. The physical properties of the reservoir are controlled by particle size, plastic rock fragment content, and carbonate cementation, and the physical properties of coarse-grained sandstone and areas with low plastic rock fragment content are better. Based on sedimentary microfacies, sand body distribution, and structural characteristics, it is predicted that the favorable area of Shan 1 is located in the central southern part of the study area, while the favorable area of Shan 2 is distributed in a strip like pattern in the central and northern parts. This study provides geological basis for efficient exploration of tight gas reservoirs in the Shanxi Formation of the Ordos Basin.

       

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