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MICROPORE STRUCTURE CHARACTERISTICS OF TIGHT OIL RESERVOIRS IN THE YANCHANG FORMATION IN THE ORDOS BASIN, CHINA

机译:鄂尔多斯盆地延长组致密油储层微观构造特征

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Pore structure is an important factor affecting the reserve and recovery of tight reservoir. In this paper, taking shale samples from the Triassic Chang 7 Member in the Ordos Basin as examples, the porosity, pore type, and pore size distribution of tight oil reservoirs were studied using scanning electron microscopy, high-pressure mercury tests, and CO2 and N2 adsorption methods. The key factors affecting the pore structure of shale were discussed. The results show that the porosity of the Late Triassic shale in the Ordos region is 1.3013.37%, with an average of 4.56%. The types of shale micropores are intergranular pores, organic pores and intragranular pores. Organic pores are the main type of pores. The shale mainly has micropores ( 50 nm. Shale pore structure is affected by shale organic carbon content, organic matter maturity, and mineral content. As shale porosity and pore volume increase, its maturity R increases and clay mineral content increases, but shale porosity and pore volume gradually decrease.
机译:孔隙结构是影响致密油藏储量和采收率的重要因素。本文以鄂尔多斯盆地三叠系长7段的页岩样品为例,利用扫描电镜,高压汞试验,CO2和CO2对致密油储层的孔隙度,孔隙类型和孔径分布进行了研究。 N2吸附方法。讨论了影响页岩孔隙结构的关键因素。结果表明,鄂尔多斯地区晚三叠世页岩的孔隙率为1.3013.37%,平均为4.56%。页岩微孔的类型是粒间孔,有机孔和粒内孔。有机毛孔是毛孔的主要类型。页岩主要具有微孔(50 nm)。页岩孔隙结构受页岩有机碳含量,有机质成熟度和矿物含量的影响,随着页岩孔隙度和孔隙体积的增加,其成熟度R增大,粘土矿物含量增加,但页岩孔隙度和孔体积逐渐减小。

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