ISSN 1673-8217 CN 41-1388/TE
主管:中国石油化工集团有限公司 主办:中国石油化工股份有限公司河南油田分公司
孙意博, 杨永剑, 操延辉, 杨映涛, 张玲, 马森. 2020: 龙门山前带沙溪庙组储层发育特征及主控因素分析. 石油地质与工程, 34(02): 19-22.
引用本文: 孙意博, 杨永剑, 操延辉, 杨映涛, 张玲, 马森. 2020: 龙门山前带沙溪庙组储层发育特征及主控因素分析. 石油地质与工程, 34(02): 19-22.
SUN Yibo, YANG Yongjian, CAO Yanhui, YANG Yingtao, ZHANG Ling, MA Sen. 2020: Reservoir development features and the controlling factors of Jurassic Shaximiao formation in piedmont zone of Longmen mountain. Petroleum Geology and Engineering, 34(02): 19-22.
Citation: SUN Yibo, YANG Yongjian, CAO Yanhui, YANG Yingtao, ZHANG Ling, MA Sen. 2020: Reservoir development features and the controlling factors of Jurassic Shaximiao formation in piedmont zone of Longmen mountain. Petroleum Geology and Engineering, 34(02): 19-22.

龙门山前带沙溪庙组储层发育特征及主控因素分析

Reservoir development features and the controlling factors of Jurassic Shaximiao formation in piedmont zone of Longmen mountain

  • 摘要: 沙溪庙组是四川盆地的主力产气层,针对龙门山前带沙溪庙组的储层特征及主控因素的研究相对较少。通过岩心观察、实验分析等综合研究,明确其储层发育特征,分析储层发育主控因素。结果表明,龙门山前带沙溪庙组砂岩主要由岩屑砂岩、岩屑石英砂岩组成,成分成熟度总体较低,碎屑含量呈低长石、高碎屑特征。储层孔隙总体上以原生孔隙和溶蚀孔隙为主,物性较差,储层连通性较差。压实作用和胶结作用是储层孔隙减少的主要因素,而溶蚀作用则是本区最主要的建设性成岩作用。

     

    Abstract: Shaximiao formation of piedmont zone of Longmen mountain is the main gas producing layer of Sichuan basin, which is lacking of research on its reservoir development features and controlling factors. Based on cuttings, core observation and experimental analysis, the reservoir development features and controlling factors in the research area have been confirmed. The results show that the sandstones of Shaximiao formation in piedmont zone of Longmen mountain are mainly composed of lithic sandstones and lithic quartz sandstones. The composition maturity of sandstones is generally low, and the clastic content is characterized by low feldspar and high clastic. The reservoir pores are mainly primary pores and dissolution pores, with poor physical properties and poor connectivity. Compaction and cementation are the main factors of reservoir porosity reduction, while dissolution is the main constructive diagenesis in this area.

     

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