致密砂岩储层成岩作用及孔隙演化定量评价——以鄂尔多斯盆地南部延长组为例

Meng Xiao, G. Qiu, Xuanjun Yuan, Songtao Wu, Dawei Cheng, Chunfang Chen
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引用次数: 0

摘要

在致密砂岩致密油勘探中,孔隙演化评价是更好地认识石油运移和聚集的关键;为研究致密砂岩储层的成岩作用和孔隙演化,通过岩心观察、薄片观察、阴极发光、扫描电镜和测井资料分析,对延长8段致密砂岩储层进行了分析。结果表明:(1)典型致密砂岩储层在埋藏深度1300 ~ 1400 m和1500 ~ 1600 m范围内发育大量次生孔隙。(2)压实作用是影响储层密度最大的因素,压实作用使储层平均孔径减小了24.8%。碳酸盐胶结使孔隙度降低8.2%。溶蚀作用是增加储层孔隙度最重要的成岩作用,使储层孔隙度增加5.1%。绿泥石在抑制次生石英生长和保存原生孔隙方面发挥了积极作用。(3)早期气侵抑制成岩作用,后期油产生的有机酸增加溶蚀作用,使高含油饱和度现象更加明显。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Quantitative evaluation of the diagenesis and porosity evolution of tight sandstone reservoirs: A case study of the Yanchang formation in the Southern Ordos basin, China
Evaluation of the pore evolution is key to gaining a better understanding of oil migration and accumulation in tight oil exploration for tight sandstone; to study the diagenesis and porosity evolution of tight sandstone reservoirs, we analysed the 8th member of the Yanchang Formation by core observation, thin section observation, cathodoluminescence, scanning electron microscopy, and logging data analysis. The following conclusions can be drawn (1) In the typical tight sandstone reservoir, numerous secondary pores developed at burial depths in the range of 1300 m to 1400 m, and approximately 1500 m to 1600 m. (2) Compaction was the most influential factor of reservoir density and decreased the average pore size by 24.8%. Carbonate cementation decreased the porosity by 8.2%. The most important diagenetic process for increasing the reservoir porosity was dissolution, which increased the pore size by 5.1%. In addition, chlorite played an active role in inhibiting secondary quartz growth and preserving primary pores. (3) The early gas invasion can inhibit diagenesis, and the organic acids produced by the later oil can increase dissolution, so that the high oil saturation phenomenon becomes more obvious.
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