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
陈刚, 阚洪阁, 陈登祺, 刘熠, 杜奎甫, 于代国. 2019: 延113–延133井区山1、山2~3储层特征及差异性研究. 石油地质与工程, 33(06): 1-4.
引用本文: 陈刚, 阚洪阁, 陈登祺, 刘熠, 杜奎甫, 于代国. 2019: 延113–延133井区山1、山2~3储层特征及差异性研究. 石油地质与工程, 33(06): 1-4.
CHEN Gang, KAN Hongge, CHEN Dengqi, LIU Yi, DU Kuifu, YU Daiguo. 2019: Reservoir characteristics and differential study of Shan 1 and Shan 2~3 reservoirs in Yan113-Yan133 well blocks. Petroleum Geology and Engineering, 33(06): 1-4.
Citation: CHEN Gang, KAN Hongge, CHEN Dengqi, LIU Yi, DU Kuifu, YU Daiguo. 2019: Reservoir characteristics and differential study of Shan 1 and Shan 2~3 reservoirs in Yan113-Yan133 well blocks. Petroleum Geology and Engineering, 33(06): 1-4.

延113–延133井区山1、山2~3储层特征及差异性研究

Reservoir characteristics and differential study of Shan 1 and Shan 2~3 reservoirs in Yan113-Yan133 well blocks

  • 摘要: 通过薄片、扫描电镜、压汞、核磁等分析手段,对比研究延113–延133井区山1和山2~3储层岩石学、物性、储集空间、孔喉结构等特征,结果表明,山1储层主要发育岩屑砂岩与岩屑石英砂岩,山2~3储层主要发育石英砂岩与岩屑石英砂岩,山2~3储层的成分和结构成熟度高于山1储层。山1储层发育较多岩屑溶孔和晶间孔,小孔喉占比高;山2~3储层以粒间溶孔为主,孔喉结构均一。两套储层特征的显著差异是沉积环境和成岩作用共同影响的结果,山1储层属陆相湖泊三角洲前缘沉积,粒内溶孔较发育;山2~3储层属海相三角洲前缘沉积,粒间溶孔发育。

     

    Abstract: By means of thin section, scanning electron microscope, mercury injection and nuclear magnetism, the petrology, physical properties, reservoir space, pore throat structure and other characteristics of Shan1 and Shan2~3 reservoirs in Yan113-Yan133 well blocks were compared and studied. The results show that Shan1 reservoir is mainly composed of lithic sandstone and lithic quartz sandstone, Shan2~3 reservoir is mainly composed of quartz sandstone and lithic quartz sandstone, and Shan2~3 reservoir has higher composition and structural maturity than that of in Shanyi reservoir. Shan 1 reservoir has more cuttings dissolved pores and inter-crystalline pores, with high proportion of pore throat. Shan2~3 reservoir is mainly composed of intergranular dissolved pores with uniform pore throat structure. The significant difference between the two sets of reservoir characteristics is the result of the combined influence of sedimentary environment and diagenesis. Shan1 reservoir belongs to a continental lacustrine delta front deposit, with developed dissolution pores in the grains. Shan2~3 reservoir belongs to a marine delta front deposit, with developed intergranular dissolution pores.

     

/

返回文章
返回