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    东营凹陷沙四上亚段陆相页岩岩相特征、成因及演化

    马义权 杜学斌 刘惠民 陆永潮

    马义权, 杜学斌, 刘惠民, 陆永潮, 2017. 东营凹陷沙四上亚段陆相页岩岩相特征、成因及演化. 地球科学, 42(7): 1195-1208. doi: 10.3799/dqkx.2017.097
    引用本文: 马义权, 杜学斌, 刘惠民, 陆永潮, 2017. 东营凹陷沙四上亚段陆相页岩岩相特征、成因及演化. 地球科学, 42(7): 1195-1208. doi: 10.3799/dqkx.2017.097
    Ma Yiquan, Du Xuebin, Liu Huimin, Lu Yongchao, 2017. Characteristics, Depositional Processes, and Evolution of Shale Lithofaceis of the Upper Submember of Es4 in the Dongying Depression. Earth Science, 42(7): 1195-1208. doi: 10.3799/dqkx.2017.097
    Citation: Ma Yiquan, Du Xuebin, Liu Huimin, Lu Yongchao, 2017. Characteristics, Depositional Processes, and Evolution of Shale Lithofaceis of the Upper Submember of Es4 in the Dongying Depression. Earth Science, 42(7): 1195-1208. doi: 10.3799/dqkx.2017.097

    东营凹陷沙四上亚段陆相页岩岩相特征、成因及演化

    doi: 10.3799/dqkx.2017.097
    基金项目: 

    构造与油气资源"教育部重点实验室开放研究基金课题 TPR-2016-09

    国家重点基础研究发展计划("973"计划)项目 SQ2013CB021013

    国家十三五科技重大专项《中国典型盆地陆相页岩油勘探开发选区与目标评价》子课题四《济阳坳陷页岩油勘探开发目标评价》 2017ZX05049004

    详细信息
      作者简介:

      马义权(1988-), 男, 副研究员, 博士, 主要从事非常规油气储层非均质性研究.ORCID:0000-0001-7792-5165.E-mail:343559902@qq.com

      通讯作者:

      杜学斌, ORCID:0000-0002-1325-0039.E-mail:basindu@163.com

    • 中图分类号: P586

    Characteristics, Depositional Processes, and Evolution of Shale Lithofaceis of the Upper Submember of Es4 in the Dongying Depression

    • 摘要: 我国陆相湖盆页岩具有较大的生烃潜力,但是对其研究起步较晚,目前存在诸多不足,尤其对富生烃页岩岩相特征及其沉积作用过程、成因演化等方面的研究工作均处于探索阶段.综合岩心、薄片、XRD矿物含量分析、主微量元素和测井等数据,在沉积学、元素地球化学以及-R(湖进-湖退)层序理论的指导下,详细研究了东营凹陷沙四上亚段页岩的岩相特征及其沉积过程、岩相发育与层序耦合关系以及古气候和湖泊的演化过程.结果表明,沙四上亚段页岩自下而上主要由硬石膏薄夹层页岩相、含粉砂富粘土质页岩相、块状灰质页岩相和纹层状灰质页岩相组成,分别沉积于盐湖环境、前三角洲环境、浅湖环境和深湖-半深湖环境.页岩岩相组合的垂向演化与体系域的纵向分布具有明显的耦合关系,揭示了古气候由干旱转为潮湿、湖盆由小型湖泊演化为大型湖泊,并推断古气候的变化和控盆正断层的活动是控制研究区古湖泊演化的两个重要因素.

       

    • 图  1  东营凹陷构造地质简图(a)、东营凹陷构造单元组成及主要沉积地层分布(b)和东营凹陷地层综合柱状图(c)

      图a据Feng et al.(2013)修改;图b据Guo et al.(2012)修改;图c据Guo et al.(2012)修改

      Fig.  1.  The structural geological map (a), structural units and main sedimentary strata (b) and comprehensive stratigraphic column (c) of the Dongying depression

      图  2  NY1井沙四上亚段页岩岩相、岩相组合、矿物成分和TOC垂向变化

      Fig.  2.  Lithofacies, lithofacies associations, mineral composition and TOC variation of the upper submember of Es4 in well NY1

      图  3  页岩不同岩相矿物组成三端元图

      Fig.  3.  Ternary diagrams of mineralogy of different lithofacies in well NY1

      图  4  纹层状灰质页岩相沉积特征

      a.纹层普遍呈平直、连续和平行的形态;b.丰富的亮晶方解石纹层;c.亮晶方解石主要由垂直于层面发育的纤维状方解石组成,它们具有清晰轮廓且不规则的边缘;d.方解石透镜体切割和扭曲原始的页岩纹层;e.富粘土质纹层与隐晶方解石纹层韵律互层;f.鱼化石的横截面;g.介形虫碎片;h.颗石藻化石

      Fig.  4.  Sedimentary characteristics of the laminated calcareous shale

      图  5  块状灰质页岩相沉积特征

      a.块状构造;b.介形虫化石及石英粉砂;c.块状构造及介形虫化石

      Fig.  5.  Sedimentary characteristics of the massive calcareous shale

      图  6  含粉砂富粘土质页岩相沉积特征

      a.砂纸条带底部可见侵蚀面;b.波纹交错层理;c.稳定-强烈的生物扰动构造;d.单晶石英粉砂局部条带状富集

      Fig.  6.  Sedimentary characteristics of the silt-bearing clay-rich shale

      图  7  硬石膏薄夹层页岩相沉积特征

      a.硬石膏薄层;b.菱柱状硬石膏颗粒;c.硬石膏薄层与富有机质页岩韵律互层

      Fig.  7.  Sedimentary characteristics of the interbedded evaporate shale

      图  8  东营凹陷沙四上亚段页岩岩相组合发育与层序耦合关系

      Fig.  8.  Shale lithofacies associations and sequence unit for the upper submember of Es4 in Dongying depression

      图  9  东营凹陷沙四上亚段页岩岩相组合发育背景分析

      Fig.  9.  Shale lithofacies associations develop setting analysis of the upper submember of Es4 in Dongying depression

      图  10  东营凹陷沙四上亚段页岩岩相组合及同时期湖泊演化模式

      Fig.  10.  Shale lithofacies associations and lake evolution model for the upper submember of Es4

      表  1  各页岩岩相沉积特征及成因

      Table  1.   Characteristics and depositional processes of each shale lithofacies

      岩相名称颜色沉积构造生物特征岩相成因
      纹层状灰质页岩相黑棕色平直、连续和平行的纹层鱼类、介形虫、颗石藻、无生物扰动潮湿气候背景下温度分层的深湖-半深湖环境
      块状灰质页岩相浅灰-深灰色块状少量介形虫、轻微生物扰动浅湖环境
      含粉砂富粘土质页岩相浅灰色块状,夹粉砂质条带强烈生物扰动前三角洲沉积环境
      硬石膏薄夹层页岩相浅灰色块状,页岩与硬石膏薄层互层各类生物较少,无生物扰动干旱气候下的盐湖环境
      下载: 导出CSV

      表  2  各页岩岩相中主要的矿物组成及含量

      Table  2.   Mineral composition and contents of each shale lithofacies

      纹层状灰
      质页岩相
      块状灰质
      页岩相
      含粉砂富粘
      土质页岩相
      硬石膏薄夹
      层页岩相
      石英
      (%)
      5~35 20~47 22~53 0~24
      (18) (30) (30) (15)
      长石
      (%)
      1~15 1~18 6~21 3~17
      (3) (5) (11) (9)
      粘土矿物
      (%)
      2~31 9~41 12~54 2~49
      (15) (24) (43) (25)
      方解石
      (%)
      2~76 9~60 0~9 0~79
      (47) (35) (5) (18)
      白云石
      (%)
      0~76 0~8 3~12 0~38
      (13) (4) (6) (18)
      黄铁矿
      (%)
      0~11 0~4 1~5 0~5
      (3) (2) (4) (3)
       注:表中数据范围为最小值至最大值,括号内为平均值.
      下载: 导出CSV

      表  3  各页岩岩相的矿物学特征及划分标准

      Table  3.   Mineral characteristics and division standard of each shale lithofacies

      纹层状灰
      质页岩相
      块状灰质
      页岩相
      含粉砂富粘
      土质页岩相
      硬石膏薄夹
      层页岩相
      碳酸盐含
      量(%)
      >40 <70 10附近 <70
      石英和长
      石含量(%)
      <30 大于20小于50 >30 大于20小于40
      粘土矿物
      含量(%)
      <30 大于10小于40 >50 大于10小于70
      下载: 导出CSV
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    • 收稿日期:  2016-12-07
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