陕北富县地区直罗油田上三叠统延长组长6储层成岩作用与有利成岩相带

    Diagenesis and favorable diagenetic facies of Chang 6 Reservoir in the Zhiluo Oilfield, northern Shaanxi

    • 摘要: 根据物性分析、高压压汞、薄片观察、扫描电镜及X衍射资料,以及陕北直罗油田长6储层的成岩作用特征,认为该区长6储层处于晚成岩A期阶段。强烈的压实及胶结作用破坏了砂岩的原生孔隙结构,其中碳酸盐、硅质和粘土矿物胶结物是造成砂岩物性降低的重要原因,碎屑颗粒周围形成的绿泥石衬边阻止了部分石英、长石次生加大及碳酸盐胶结物的沉淀,使部分原生粒间孔隙得以保存。溶蚀作用形成次生孔隙,使储层物性得到一定程度的改善。研究区长6储层发育4种成岩相,优质储层与成岩相关系密切,其中次生孔隙成岩相物性最好,绿泥石膜相次之,它们成为储层发育的有利成岩相带。

       

      Abstract: According to physical property analysis, mercury injection, cast section SEM and X-ray diffractions,the authors studied the diagenetic features of Chang 6 reservoir in the Zhiluo oilfield of northern Shaanxi, and have reached the conclusion that Chang 6 reservoir belongs to the "A" stage of late diagenesis. The impact and consolidated filling have destroyed the porosity of the sandstones. Carbonate, hydrosyalite and quartz-feldspar overgrowths were the main cements that reduced the reservoir quality of the sandstones. Thin chlorite film around detrital grains prevented overgrowth of part of quartz and feldspar and precipitation of carbonate cements, thus preserving a part of primary pores. Dissolution produced secondary pores and improved the physical property. Four kinds of diagenetic facies were recognized in the study area. There exists intimate relationship between qualified reservoirs and diagenetic facies: the physical properties of secondary pore diagenetic facies are the best, followed by chlorite cementation facies. These facies constitute the favorable diagenetic facies for the reservoir development.

       

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