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四川盆地焦石坝地区龙马溪组海相页岩储层非均质性特征

易积正 王超

易积正, 王超. 四川盆地焦石坝地区龙马溪组海相页岩储层非均质性特征[J]. 石油实验地质, 2018, 40(1): 13-19. doi: 10.11781/sysydz201801013
引用本文: 易积正, 王超. 四川盆地焦石坝地区龙马溪组海相页岩储层非均质性特征[J]. 石油实验地质, 2018, 40(1): 13-19. doi: 10.11781/sysydz201801013
YI Jizheng, WANG Chao. Differential pore development characteristics in various shale lithofacies of Longmaxi Formation in Jiaoshiba area, Sichuan Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(1): 13-19. doi: 10.11781/sysydz201801013
Citation: YI Jizheng, WANG Chao. Differential pore development characteristics in various shale lithofacies of Longmaxi Formation in Jiaoshiba area, Sichuan Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(1): 13-19. doi: 10.11781/sysydz201801013

四川盆地焦石坝地区龙马溪组海相页岩储层非均质性特征

doi: 10.11781/sysydz201801013
基金项目: 国家科技重大专项(2016ZX05060)和中国石化科技项目(P17014-2)资助。
详细信息
    作者简介:

    易积正(1962-),男,教授级高级工程师,从事油气勘探开发与管理。E-mail:498703979@qq.com

  • 中图分类号: TE122.2

Differential pore development characteristics in various shale lithofacies of Longmaxi Formation in Jiaoshiba area, Sichuan Basin

  • 摘要: 以四川盆地焦石坝地区下志留统龙马溪组海相页岩为研究对象,综合利用全岩X衍射、薄片鉴定、阴极发光、氩离子抛光扫描电镜、高压压汞-气体吸附联测、核磁孔隙度等实验数据,开展不同岩相储层特征差异性研究。研究结果揭示:(1)焦石坝地区龙马溪组海相页岩岩相主要分为硅质类页岩、混合类页岩和黏土类页岩;(2)硅质类页岩有机孔隙非常发育,混合类页岩和黏土类页岩中无机孔隙较为发育,其中黏土类页岩有机孔隙发育程度较弱;(3)不同页岩岩相非均质性特征显著。总有机碳含量、孔隙度、孔隙体积、比表面积和含气量方面,硅质类页岩最为发育,黏土类页岩发育程度最低,混合类页岩介于两者之间;(4)硅质类页岩沉积期古生物繁盛有利于有机质富集和有机质孔隙发育,混合类页岩和黏土类页岩分别受底流和陆源碎屑沉积作用影响,总有机碳含量较低且有机质孔隙相对欠发育。

     

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出版历程
  • 收稿日期:  2017-10-13
  • 修回日期:  2017-12-12
  • 刊出日期:  2018-01-28

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