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鄂尔多斯盆地北缘近源砂砾质辫状河砂体构型与含气性

齐荣 李良 秦雪霏

齐荣, 李良, 秦雪霏. 鄂尔多斯盆地北缘近源砂砾质辫状河砂体构型与含气性[J]. 石油实验地质, 2019, 41(5): 682-690. doi: 10.11781/sysydz201905682
引用本文: 齐荣, 李良, 秦雪霏. 鄂尔多斯盆地北缘近源砂砾质辫状河砂体构型与含气性[J]. 石油实验地质, 2019, 41(5): 682-690. doi: 10.11781/sysydz201905682
QI Rong, LI Liang, QIN Xuefei. Sand body configuration and gas-bearing properties of near source sand-gravel braided river on the northern margin of Ordos Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2019, 41(5): 682-690. doi: 10.11781/sysydz201905682
Citation: QI Rong, LI Liang, QIN Xuefei. Sand body configuration and gas-bearing properties of near source sand-gravel braided river on the northern margin of Ordos Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2019, 41(5): 682-690. doi: 10.11781/sysydz201905682

鄂尔多斯盆地北缘近源砂砾质辫状河砂体构型与含气性

doi: 10.11781/sysydz201905682
基金项目: 

国家科技重大专项“低丰度致密低渗油气藏开发关键技术”(2016ZX05048);中国石化科技部项目“鄂尔多斯盆地大中型气田目标评价与勘探关键技术”(P17009)联合资助。

详细信息
    作者简介:

    齐荣(1986-),女,博士研究生,主要从事石油天然气成藏规律研究。E-mail:qirong1996@163.com。

  • 中图分类号: TE121.3

Sand body configuration and gas-bearing properties of near source sand-gravel braided river on the northern margin of Ordos Basin

  • 摘要: 鄂尔多斯盆地北缘杭锦旗地区独贵加汗一带的二叠系下石盒子组盒1段沉积期处于公卡汉古陆的南坡,形成了一套近物源的砂砾质辫状河沉积。河道砂体的物性与含气性具有良好的相关性,但河道砂体内部的非均质性很强,造成含气性差异也大。对该区盒1段砂砾质辫状河砂体构型进行了分析研究,明确了其岩相特征和主要构型单元。通过岩心观察和测井资料分析,在盒1段划分出6种典型岩相,心滩和水道充填为主要构型单元。心滩砂体在纵向上一般具有Gm-Sgt-Sm、Gm-Sm-Sp、Sgt-Sm、Sm-Sp等4种岩相组合,水道充填砂体一般具有Gm-Sp、Gm-St、Sgt-Sp、Sgt-St等4种岩相组合,砂体内部这种岩相变化是形成强非均质性的主要原因。利用直井、水平井和地震资料统计心滩长度为230~1 050 m,根据经验公式计算心滩宽度为43~386 m。心滩砂体与水道充填砂体侧向共生,但其物性和含气性有明显差异。统计资料表明,心滩砂体的物性和含气性优于水道充填砂体。

     

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出版历程
  • 收稿日期:  2019-03-21
  • 修回日期:  2019-07-01
  • 刊出日期:  2019-09-28

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