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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    石南地区侏罗系西山窑组碎屑岩储层主控因素分析

    Main Controlling Factors of Clastic Reservoir in Jurassic Xishanyao Formation,Shinan Area

    • 摘要: 通过电镜扫描、铸体薄片和X射线等技术手段,结合录井和测井资料,研究了石南地区西山窑组碎屑岩储层的岩石学特征、孔隙类型、沉积环境和成岩作用等,并分析了储层物性的主控因素,指出了优质储层的分布区域,为后期油田勘探开发提供了理论指导。研究表明西山窑组储层发育于辫状河三角洲前缘,以三角洲前缘水下分流河道微相为主,岩性以灰色或灰绿色的细砂岩和中砂岩为主,孔隙类型以剩余粒间孔、原生粒间孔和粒间溶孔为主,属于中孔低渗储层;成岩作用中压实作用和胶结作用对储层物性起破坏作用,分别造成原生孔隙的损失约在30%~70%和5%~30%,溶蚀作用形成的次生孔隙占整个孔隙空间的30%左右,起建设性作用;储层物性主要受控于其沉积环境,成岩作用的对储层物性的控制作用较小,优质储层分布在辫状河三角洲前缘水下分流河道微相中。

       

      Abstract: Combined with geology logging and well logging data, the petrological characters, pore types, sedimentary environment and diagenesis of clastic reservoir in Xishanyao Formation have been studied by SEM, casting thin sections, X-ray diffraction, and then the main controlling factors of this clastic reservoir have been analyzed, the high-quality reservoir distribution has been cleared, providing theoretical guide for further exploration and development.The results show that the Xishanyao Formation reservoir was developed in braided delta front, with underwater distributary channel facies as its main microfacies, being dominated by gray or celadon fine and medium sandstone, while its pore types contain residual intergranular pore, primary intergranular pore and intergranular solution pore, belonging to medium porosity and low permeability formation.The reservoir characteristics were destroyed by compaction and cementation during the diagenesis, reducing about 40%~70%and 5%~30% of primary pores, irrespectively; The secondary pores formed by the dissolution is constructive and take up 30% of the whole pores.Reservoir characteristics are mainly controlled by sedimentary environment compared to diagenesis; The high-quality reservoir is distributed in the underwater distributary channel microfacies of braided delta front.

       

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