孙相灿, 杨传胜, 于兴河, 李梅. 冀中坳陷深县凹陷古近系碎屑岩储层成岩作用及成岩演化序列分析[J]. 海洋地质与第四纪地质, 2014, 34(2): 135-142. DOI: 10.3724/SP.J.1140.2014.02135
引用本文: 孙相灿, 杨传胜, 于兴河, 李梅. 冀中坳陷深县凹陷古近系碎屑岩储层成岩作用及成岩演化序列分析[J]. 海洋地质与第四纪地质, 2014, 34(2): 135-142. DOI: 10.3724/SP.J.1140.2014.02135
SUN Xiangcan, YANG Chuansheng, YU Xinghe, LI Mei. DIAGENESIS AND DIAGENETIC SEQUENCE OF PALEOGENE SANDSTONE RESERVOIR IN SHENXIN DEPRESSION, JIZHONG SUB-BASIN[J]. Marine Geology & Quaternary Geology, 2014, 34(2): 135-142. DOI: 10.3724/SP.J.1140.2014.02135
Citation: SUN Xiangcan, YANG Chuansheng, YU Xinghe, LI Mei. DIAGENESIS AND DIAGENETIC SEQUENCE OF PALEOGENE SANDSTONE RESERVOIR IN SHENXIN DEPRESSION, JIZHONG SUB-BASIN[J]. Marine Geology & Quaternary Geology, 2014, 34(2): 135-142. DOI: 10.3724/SP.J.1140.2014.02135

冀中坳陷深县凹陷古近系碎屑岩储层成岩作用及成岩演化序列分析

DIAGENESIS AND DIAGENETIC SEQUENCE OF PALEOGENE SANDSTONE RESERVOIR IN SHENXIN DEPRESSION, JIZHONG SUB-BASIN

  • 摘要: 通过运用岩心化验分析资料、薄片、扫描电镜资料及X射线衍射等资料,对深县凹陷古近系砂岩储层岩石特征、成岩作用类型、成岩阶段、成岩演化序列和孔隙演化进行了系统的分析。研究结果表明:深县凹陷古近系砂岩类型为长石岩屑砂岩或岩屑长石砂岩,岩石的结构成熟度和成分成熟度均较低;影响该区储层物性的成岩作用主要是压实作用、胶结作用、溶蚀作用和交代作用;在此基础上,通过成岩阶段划分与孔隙演化研究,深县凹陷古近系砂岩储层位于成岩阶段的早成岩B期至晚成岩B期。不同成岩阶段的成岩作用强度不同,因此,不同成岩阶段的储层物性变化较大。

     

    Abstract: Using the conventional core analysis data, such as the data of thin sections, scanning electron microscopy(SEM) and X-ray diffraction, the petrographic characteristics, diagenetic types, diagenetic stages and sequences as well as porosity evolution of the Paleogene sandstone reservoir in the Shenxian Depression are systematically studied. The results indicate that the lithology of Paleogene sandstone reservoir in the Shenxian Depression is primarily feldspathic lithic sandstone and lithic sandstone of low maturity. Compaction, cementation, dissolution and metasomatism are the main types of diagenesis influencing reservoir property in the study area. Based on the study of diagenetic stages and porosity evolution, the Paleogene sandstone reservoir in the study area is mainly remained in the stage B of early diagenesis upto the stage B of late diagenesis. The reservoir properties change drastically in different diagenetic stages.

     

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