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沁水盆地海陆交互相页岩脆性指数预测与测井响应分析

付娟娟 郭少斌

付娟娟, 郭少斌. 沁水盆地海陆交互相页岩脆性指数预测与测井响应分析[J]. 石油实验地质, 2019, 41(1): 108-112. doi: 10.11781/sysydz201901108
引用本文: 付娟娟, 郭少斌. 沁水盆地海陆交互相页岩脆性指数预测与测井响应分析[J]. 石油实验地质, 2019, 41(1): 108-112. doi: 10.11781/sysydz201901108
FU Juanjuan, GUO Shaobin. Prediction of brittle index and its relationship with log data in marine-terrigenous shale of Qinshui Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2019, 41(1): 108-112. doi: 10.11781/sysydz201901108
Citation: FU Juanjuan, GUO Shaobin. Prediction of brittle index and its relationship with log data in marine-terrigenous shale of Qinshui Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2019, 41(1): 108-112. doi: 10.11781/sysydz201901108

沁水盆地海陆交互相页岩脆性指数预测与测井响应分析

doi: 10.11781/sysydz201901108
基金项目: 

国家科技重大专项“不同类型页岩生成机理与富集规律研究”(2016ZX05034-001)资助。

详细信息
    作者简介:

    付娟娟(1981-),女,博士研究生,工程师,矿产普查与勘探专业。E-mail:jessietx2009@hotmail.com。

    通讯作者:

    郭少斌(1962-),男,教授,博士生导师,从事层序地层学、储层评价和油气资源评价方面的教学和科研工作。E-mail:guosb58@126.com。

  • 中图分类号: TE122.23

Prediction of brittle index and its relationship with log data in marine-terrigenous shale of Qinshui Basin

  • 摘要: 沁水盆地煤系地层勘探开发时间长,但测井系列简单,通过全岩分析获取矿物组分的岩心数量十分有限,因此,目前该地区页岩储层的脆性评价以定性为主,缺少定量表征。基于XRD全岩分析的矿物组分信息,通过矿物法计算了沁水盆地海陆交互相页岩岩心的脆性矿物指数,分析了页岩地层的测井响应特征及对脆性矿物指数的影响,采用多元回归方法,建立了该区石炭-二叠系页岩地层矿物指数的计算模型。研究区内石英、长石、菱铁矿及黄铁矿对储层脆性有主要贡献,其含量与页岩脆性指数成正比;而黏土矿物含量较高,有利于提高岩石塑性,不利于裂缝伸展。不同测井响应对脆性指数的反映程度不同,脆性矿物指数与密度值呈正相关,与自然伽马值呈负相关,而与电阻率和声波时差的关系不明显,呈微弱的负相关。多元线性回归方法计算得到的脆性矿物指数与矿物法得到的结果吻合度较好。

     

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出版历程
  • 收稿日期:  2018-09-28
  • 修回日期:  2018-12-14
  • 刊出日期:  2019-01-28

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