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二连盆地阿南凹陷白垩系腾格尔组致密油储层特征及主控因素

付小东 张天付 吴健平 王小芳 周进高 江涛 李彬 李长新

付小东, 张天付, 吴健平, 王小芳, 周进高, 江涛, 李彬, 李长新. 二连盆地阿南凹陷白垩系腾格尔组致密油储层特征及主控因素[J]. 石油实验地质, 2021, 43(1): 64-76. doi: 10.11781/sysydz202101064
引用本文: 付小东, 张天付, 吴健平, 王小芳, 周进高, 江涛, 李彬, 李长新. 二连盆地阿南凹陷白垩系腾格尔组致密油储层特征及主控因素[J]. 石油实验地质, 2021, 43(1): 64-76. doi: 10.11781/sysydz202101064
FU Xiaodong, ZHANG Tianfu, WU Jianping, WANG Xiaofang, ZHOU Jingao, JIANG Tao, LI Bing, LI Changxin. Characteristics and main controlling factors of tight oil reservoirs in Cretaceous Tengger Formation, A'nan Sag, Erlian Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2021, 43(1): 64-76. doi: 10.11781/sysydz202101064
Citation: FU Xiaodong, ZHANG Tianfu, WU Jianping, WANG Xiaofang, ZHOU Jingao, JIANG Tao, LI Bing, LI Changxin. Characteristics and main controlling factors of tight oil reservoirs in Cretaceous Tengger Formation, A'nan Sag, Erlian Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2021, 43(1): 64-76. doi: 10.11781/sysydz202101064

二连盆地阿南凹陷白垩系腾格尔组致密油储层特征及主控因素

doi: 10.11781/sysydz202101064
基金项目: 

中国石油天然气股份有限公司重大科技专项 2014E-35

详细信息
    作者简介:

    付小东(1980-), 男, 博士, 高级工程师, 主要从事油气地质研究。E-mail: fuxd_hz@petrochina.com.cn

    通讯作者:

    王小芳(1980-), 女, 博士, 高级工程师, 主要从事沉积储层研究。E-mail: wangxf_hz@petrochina.com.cn

  • 中图分类号: TE122.2

Characteristics and main controlling factors of tight oil reservoirs in Cretaceous Tengger Formation, A'nan Sag, Erlian Basin

  • 摘要: 二连盆地阿南凹陷白垩系腾格尔组一段下亚段广泛发育一套与火山活动相关的“特殊岩性”致密储层,是致密油勘探的主要目的层。基于岩石薄片观察和储层物性系统分析,结合扫描电镜、压汞、CT扫描和核磁共振等分析,对该层段不同岩性致密储层特征和“甜点”发育主控因素进行综合研究。结果表明:腾一下亚段主要发育凝灰质岩、砂岩、白云岩和泥岩四大岩类,凝灰质岩和砂岩是致密油储层发育的有利岩性。储层中主要发育溶蚀孔、晶间微孔、残余粒间孔、泄水孔和微裂缝等5类储集空间,其中凝灰岩中以脱玻化晶间孔和溶蚀孔占主导,砂岩中以残余粒间孔和溶蚀孔最有利。储层孔隙结构可划分为3类4亚类,薄层凝灰岩和溶孔发育的细砂岩储层孔隙结构较好,沉凝灰岩与白云岩孔隙结构较差。不同类型储层含油非均质性强,含油量受储层岩性、孔渗条件和孔隙结构控制。凝灰质岩致密储层“甜点”发育主要受火山碎屑沉积方式、脱玻化作用和溶蚀作用控制,砂岩类储层“甜点”发育主要受沉积微相、岩石结构和溶蚀作用共同控制。

     

  • 图  1  二连盆地阿南凹陷区域构造(a)与腾一下亚段地层综合柱状图(b)

    Figure  1.  Regional tectonic map (a) and composite stratigraphic section of the lower submember of first member of Cretaceous Tengger Formation(b), A'nan Sag, Erlian Basin

    图  2  二连盆地阿南凹陷腾一下亚段致密储层岩石学特征

    a.晶屑岩屑凝灰岩,凝灰结构,阿密2井,1 545.97 m,正交偏光;b.岩屑凝灰岩,火山尘胶结,阿密2井,1 561.92 m,单偏光;c.含灰晶屑凝灰岩,方解石、白云石交代凝灰质,阿密2井,1 568.35 m,正交偏光;d.含灰沉凝灰岩,示底构造,阿43井,2 067.78 m,单偏光;e.灰化、云化沉凝灰岩,自形晶白云石去云化,阿密2井,1 566.8 m,正交偏光;f.沉凝灰岩,泄水孔被白云石半充填,阿43井,2 054.8 m,单偏光;g.含内碎屑泥晶云岩,阿密2井,1 578.17 m,单偏光;h.长石岩屑细砂岩,方解石连晶胶结,阿密2井,1 595.23 m,正交偏光;i.长石岩屑中粗砂岩,方解石胶结,阿密2井,1 602.58 m,正交偏光;j.凝灰质泥岩,阿密2井,2 056.07 m,单偏光;k.凝灰岩,阿密2井,1 565.22 m,荧光薄片;l.样品同e,荧光薄片;m.长石岩屑细砂岩,阿密2井,1 591.52 m,荧光薄片;n.样品同g,荧光薄片;o.样品同j,荧光薄片

    Figure  2.  Rock types and structural characteristics of tight reservoirs in lower submember of first member of Cretaceous Tengger Formation, A'nan Sag, Erlian Basin

    图  3  二连盆地阿南凹陷腾一下亚段致密储层主要孔隙空间类型

    a.含晶屑凝灰岩,溶蚀孔发育,阿密2井,1 568.50 m,激光共聚焦;b.样品同a,脱玻化晶间孔,氩离子抛光—场发射电镜;c.岩屑凝灰岩,脱玻化晶间孔发育,阿密2井,1 561.92 m,氩离子抛光—场发射电镜;d.沉凝灰岩,斑状方解石/白云石晶间孔、晶间溶孔,阿密2井,1 566.80 m;e.沉凝灰岩,泄水孔被方解石、方沸石充填,方沸石发生溶蚀,阿43井,2 054.80 m,铸体薄片;f.灰化沉凝灰岩,粒间、晶间微孔发育,阿密2井,1 584.66 m,氩离子抛光—场发射电镜;g.泥晶白云岩,晶间微孔发育,阿密2井,1 578.17 m,氩离子抛光—场发射电镜;h.长石岩屑细砂岩,粒间溶孔、粒内溶孔发育,阿密2井,1 591.60 m,铸体薄片;i.长石岩屑中粗砂岩,残余粒间孔、粒间溶孔、岩屑粒内溶孔发育,阿密2井,1 603.51 m,铸体薄片

    Figure  3.  Pore space types of tight oil reservoir in lower submember of first member of Cretaceous Tengger Formation, A'nan Sag, Erlian Basin

    图  4  二连盆地阿南凹陷腾一下亚段致密储层核磁共振T2谱峰分布特征

    Figure  4.  T2 spectrum of NMR of tight oil reservoir in lower submember of first member of Cretaceous Tengger Formation, A'nan Sag, Erlian Basin

    图  5  二连盆地阿南凹陷腾一下亚段致密储层压汞曲线特征

    Figure  5.  Mercury-injection curves of tight reservoirs in lower submember of first member of Cretaceous Tengger Formation, A'nan Sag, Erlian Basin

    图  6  二连盆地阿南凹陷腾一下亚段致密储层含油性与储层物性关系

    Figure  6.  Relationship between oil content and physical properties of tight reservoirs in lower submember of first member of Cretaceous Tengger Formation, A'nan Sag, Erlian Basin

    表  1  二连盆地阿南凹陷腾一下亚段致密储层恒速压汞孔隙结构参数

    Table  1.   Pore structure parameters of constant rate mercury injection of tight reservoirs in lower submember of first member of Cretaceous Tengger Formation, A'nan Sag, Erlian Basin

    岩性 深度/m 最终进汞饱和度/% 单位体积岩样有效喉道体积/cm3 单位体积岩样有效孔隙体积/cm3 单位体积岩样有效孔隙喉道个数/个 有效孔喉半径比加权平均值
    总进汞 喉道进汞 孔隙进汞
    凝灰岩 1 546.0 46.47 20.75 25.72 0.012 0.015 1 209 419.18
    凝灰岩 1 565.4 78.59 52.15 26.44 0.063 0.032 6 383 332.92
    凝灰岩 1 568.6 81.69 48.11 33.58 0.081 0.056 8 178 192.18
    云质沉凝灰岩 1 558.1 37.63 26.79 10.84 0.004 0.002 289 23.47
    凝灰质云岩 1 578.2 4.20 1.28 2.92 0.001 0.002 87 17.50
    粉砂质云岩 1 555.5 10.95 3.32 7.63 0.001 0.003 149 19.25
    凝灰质粉砂岩 1 580.4 7.67 3.41 4.26 0.002 0.002 176 17.82
    长石岩屑细砂岩 1 591.8 70.94 46.61 24.33 0.094 0.049 9 532 87.29
    凝灰质粉细砂岩 1 597.4 31.98 16.11 15.87 0.028 0.027 3 210 287.16
    长石岩屑粗砂岩 1 602.8 66.49 45.29 21.20 0.075 0.035 6 623 91.23
    下载: 导出CSV

    表  2  二连盆地阿南凹陷腾一下亚段致密储层孔隙结构特征

    Table  2.   Pore structure characteristics of tight reservoirs in lower submember of first member of Cretaceous Tengger Formation, A'nan Sag, Erlian Basin

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  • 收稿日期:  2020-04-16
  • 修回日期:  2020-12-24
  • 刊出日期:  2021-01-28

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