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塔里木盆地巴麦地区东河塘组储集层特征与成岩作用

张永东 邵志兵 乔桂林 韩彧

张永东, 邵志兵, 乔桂林, 韩彧. 塔里木盆地巴麦地区东河塘组储集层特征与成岩作用[J]. 石油实验地质, 2014, 36(2): 176-181. doi: 10.11781/sysydz201402176
引用本文: 张永东, 邵志兵, 乔桂林, 韩彧. 塔里木盆地巴麦地区东河塘组储集层特征与成岩作用[J]. 石油实验地质, 2014, 36(2): 176-181. doi: 10.11781/sysydz201402176
Zhang Yongdong, Shao Zhibing, Qiao Guilin, Han Yu. Reservoir characteristics and diagenesis of Devonian Donghetang Formation in Bachu-Maigaiti area[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2014, 36(2): 176-181. doi: 10.11781/sysydz201402176
Citation: Zhang Yongdong, Shao Zhibing, Qiao Guilin, Han Yu. Reservoir characteristics and diagenesis of Devonian Donghetang Formation in Bachu-Maigaiti area[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2014, 36(2): 176-181. doi: 10.11781/sysydz201402176

塔里木盆地巴麦地区东河塘组储集层特征与成岩作用

doi: 10.11781/sysydz201402176
基金项目: 中国石化科技部项目“巴麦地区古生界油气成藏条件与勘探方向”(P10023)资助。
详细信息
    作者简介:

    张永东(1982-),男,工程师,从事沉积储层特征和成岩作用研究。E-mail:gentleman10001@163.com。

  • 中图分类号: TE122.2

Reservoir characteristics and diagenesis of Devonian Donghetang Formation in Bachu-Maigaiti area

  • 摘要: 通过普通薄片、铸体薄片、扫描电镜以及测井等分析手段,对巴麦地区东河塘组上砂岩段和下砂岩段的沉积特征、岩石学特征、成岩作用进行了详细分析。东河塘组沉积环境为滨岸相,具有较高的成分成熟度和结构成熟度,且上砂岩段的成分成熟度和结构成熟度都要高于下砂岩段。储集空间类型主要为溶蚀孔隙,其分布主要受粒度和粒间胶结物的影响,粒度较粗和钙质胶结的砂岩段溶蚀孔隙发育。主要的成岩作用为压实、胶结、胶结物溶蚀、石英颗粒碱性溶蚀、交代、重结晶以及构造破裂。根据成岩阶段划分标准,东河塘组处在中成岩阶段的B期。

     

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出版历程
  • 收稿日期:  2013-02-26
  • 修回日期:  2014-01-16
  • 刊出日期:  2014-03-28

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