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鄂尔多斯盆地东缘成家庄地区二叠系山西组三角洲前缘露头构型分析

师学耀, 高超利, 孟旺才, 赵逸, 陈立军, 王彩霞, 冷丹凤, 马洪志, 马裕武, 孙宁亮

师学耀,高超利,孟旺才,等. 鄂尔多斯盆地东缘成家庄地区二叠系山西组三角洲前缘露头构型分析[J]. 西北地质,2025,58(1):135−149. doi: 10.12401/j.nwg.2023039
引用本文: 师学耀,高超利,孟旺才,等. 鄂尔多斯盆地东缘成家庄地区二叠系山西组三角洲前缘露头构型分析[J]. 西北地质,2025,58(1):135−149. doi: 10.12401/j.nwg.2023039
SHI Xueyao,GAO Chaoli,MENG Wangcai,et al. Delta Front Outcrop Architecture Analysis of Permian Shanxi Formation in Chengjiazhuang, Liulin, East Ordos Basin[J]. Northwestern Geology,2025,58(1):135−149. doi: 10.12401/j.nwg.2023039
Citation: SHI Xueyao,GAO Chaoli,MENG Wangcai,et al. Delta Front Outcrop Architecture Analysis of Permian Shanxi Formation in Chengjiazhuang, Liulin, East Ordos Basin[J]. Northwestern Geology,2025,58(1):135−149. doi: 10.12401/j.nwg.2023039

鄂尔多斯盆地东缘成家庄地区二叠系山西组三角洲前缘露头构型分析

基金项目: 国家科技重大专项项目“大型油气田及煤层气开发−砂页岩储层特征及有利区带评价(2016ZX05066001-003)”,延长油田股份有限公司科技项目基金“志丹油田爬子洼区石油地质评价及勘探建议(ycsh2021ky-B-15-1-3)”联合资助。
详细信息
    作者简介:

    师学耀(1987−),男,工程师,从事石油勘探工作。E−mail:44421381@qq.com

  • 中图分类号: P535;TE122.2

Delta Front Outcrop Architecture Analysis of Permian Shanxi Formation in Chengjiazhuang, Liulin, East Ordos Basin

  • 摘要:

    通过野外露头精细解剖,基于露头的岩性、沉积构造、颜色及沉积环境,开展了鄂尔多斯盆地东缘山西柳林成家庄地区二叠系山西组三角洲前缘砂体构型研究。结果表明:研究区共有10种岩相类型及7种沉积单元,根据沉积旋回特征及岩相组合类型,识别出了分流河道、分流砂坝、潮汐砂坝、河口坝、远砂坝、席状砂6种4级构型单元,它们又以复杂的组合方式构成三角洲前缘5级构型单元。构型单元的组合样式可分为垂向叠置、侧向拼接及孤立式3种。通过实地测量对构型单元进行了定量表征,分流河道、分流砂坝、河口坝、远砂坝砂体厚度和宽度之间存在线性关系,且具有较高的相关性,能够为地下构型单元建模提供一定的地质依据。

    Abstract:

    Through detailed analysis of outcrop sections, based on lithology, sedimentary structures, colors and sedimentary environment, sand body architecture of delta front is researched in Chengjiazhuang district, east Ordos basin of Permian Shanxi formation. Results show that there are ten kinds of lithofacies and seven sedimentary units in the study area. According to sedimentary cycle and lithofacies assemblage characteristics, six types of fourth level architectural units, i.e., distributary channel, distributary bar, tide sand-dam, estuarine dam, distal bar and sheet sands are identified. They also formed fifth level architectural units in delta front in a complicated assemblage style. Assemble patterns of architectural units are divided into vertical stacking type, lateral joining type and isolated type. Through field measurement, architectural units are quantitative characterized. Result show that there is a linear relationship with a high relativity between thickness and width of distributary channel, distributary bar, estuarine dam and distal bar, which can provide a geological basis for modeling of subsurface architectural units.

  • 图  1   山西柳林成家庄山西组露头位置示意图

    Figure  1.   Location of Permian Shanxi Formation outcrop in Chengjiazhuang, Liulin, Shanxi Province

    图  2   柳林成家庄山西组露头岩性剖面及其沉积微相解释

    Figure  2.   Lithological profile and sedimentary microfacies interpretation of Shanxi Formation in Chengjiazhuang, Liulin

    图  3   柳林成家庄山西组主要的岩相类型

    a. 底部块状层理含砾中粗砂岩相,顶部槽状交错层理中细砂岩相;b. 块状层理中细砂岩相;c. 槽状交错层理中细砂岩相;d. 板状交错层理中细砂岩相;e. 平行层理中砂岩相;f. 羽状交错层理细砂岩相;g. 透镜状层理细砂岩相;h. 流水沙纹层理细砂岩相;i. 薄煤层及深灰色泥岩

    Figure  3.   Main lithofacies types of Shanxi Formation in Chengjiazhuang, Liulin

    图  4   柳林成家庄山西组露头剖面基本沉积单元

    Figure  4.   Basic sedimentary units of Shanxi Formation in Chengjiazhuang, Liulin

    图  5   柳林成家庄山西组典型岩相组合

    Figure  5.   Typical lithofacies associations of Shanxi Formation in Chengjiazhuang, Liulin

    图  6   剖面1构型要素综合解释成果及W1构型单元垂向叠置关系

    Figure  6.   Comprehensive interpretation results of field profile 1 and vertical stacking relationships of W1

    图  7   剖面2构型要素综合解释成果及W2构型单元垂向叠置关系

    Figure  7.   Comprehensive interpretation results of field profile 2 and vertical stacking relationships of W2

    图  8   剖面3构型要素综合解释成果及W3构型单元垂向叠置关系

    Figure  8.   Comprehensive interpretation results of field profile 3 and vertical stacking relationships of W3

    图  9   柳林成家庄地区山西组露头剖面构型单元侧向拼接及孤立式分布样式

    a. 构型单元的侧拼接型细砂岩1.5 m;b. 构型单元的似侧拼接型;c. 构型单元的孤立式分布

    Figure  9.   Lateral joining type and isolated type patterns of architecture units of Shanxi Formation in Chengjiazhuang, Liulin

    图  10   柳林成家庄地区山西组露头剖面构型单元组合模式图

    Figure  10.   Assemble patterns of architectural units of Shanxi Formation in Chengjiazhuang, Liulin

    图  11   柳林成家庄地区山西组露头剖面构型单元参数相关性分析

    Figure  11.   Correlation of architecture unit parameters of Shanxi Formation in Chengjiazhuang, Liulin

    表  1   研究区三角洲前缘露头沉积单元及构型界面级次划分

    Table  1   Sedimentary units and architecture boundary level division of delta front in the study area

    构型界面级别构型沉积单元沉积成因及特征界面特征
    1层系流体底形迁移无明显侵蚀
    2层系组流体底形迁移无明显侵蚀
    3大型底形内部的增生体,如分流河道、分流砂坝及潮汐砂坝内的侧积体,三角洲前缘河口坝的前积体流体顺流加积或者侧向加积微弱侵蚀面
    4大型沉积底形,如分流河道、分流砂坝、潮汐砂坝、单一河口坝、单一远砂坝、单一席状砂等由多个增生体在垂向或侧向加积形成的沉积单元具明显侵蚀,可见侵蚀面
    5单一河道复合沉积体、潮汐砂坝复合沉积体、河口坝复合体、远砂坝复合体、席状砂复合体具侵蚀界面的连续沉积体,表现为垂向加积、侧向加积及填积形成的复合沉积单元具侵蚀的基底,底部滞留沉积,重要的岩性及物性界面
    下载: 导出CSV

    表  2   柳林成家庄地区山西组露头剖面构型单元参数表

    Table  2   Architecture unit parameters of Shanxi Formation in Chengjiazhuang, Liulin

    剖面
    编号
    分流河道分流砂坝潮汐砂坝河口坝远砂坝席状砂
    宽(m)厚(m)宽/
    宽(m)厚(m)宽/
    宽(m)厚(m)宽/
    宽(m)厚(m)宽/
    宽(m)厚(m)宽/
    宽(m)厚(m)宽/
    剖面13565.8101.56.7
    24.554.991.27.5
    剖面287117.92664.31326.5
    121.58.0
    剖面3281.125.5280.835.0130.265.0
    301.323.1210.635.015.70.352.3
    260.928.9230.732.927.50.468.8
    260.737.1160.353.3
    30130.0230.546.0
    210.452.5


    其他
    剖面
    365.56.5196.03.2121.67.5150.818.8260.552.0
    747.310.1141.68.8101.28.3221.120.0210.370.0
    513.514.6121.48.6170.534.0
    346.05.7223.85.8321.521.3
    171.214.2
    615.511.1
    下载: 导出CSV
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  • 收稿日期:  2022-04-07
  • 修回日期:  2022-05-24
  • 网络出版日期:  2023-03-16
  • 刊出日期:  2025-02-19

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