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    银川盆地清水营组咸化湖盆沉积特征与湖盆演化

    徐清海 吴楠 王健 海连富 曹日洲

    徐清海, 吴楠, 王健, 海连富, 曹日洲, 2023. 银川盆地清水营组咸化湖盆沉积特征与湖盆演化. 地球科学, 48(1): 317-328. doi: 10.3799/dqkx.2021.257
    引用本文: 徐清海, 吴楠, 王健, 海连富, 曹日洲, 2023. 银川盆地清水营组咸化湖盆沉积特征与湖盆演化. 地球科学, 48(1): 317-328. doi: 10.3799/dqkx.2021.257
    Xu Qinghai, Wu Nan, Wang Jian, Hai Lianfu, Cao Rizhou, 2023. Sedimentary Characteristics and Lake Basin Evolution of Salinized Lake Basin of Qingshuiying Formation in Yinchuan Basin. Earth Science, 48(1): 317-328. doi: 10.3799/dqkx.2021.257
    Citation: Xu Qinghai, Wu Nan, Wang Jian, Hai Lianfu, Cao Rizhou, 2023. Sedimentary Characteristics and Lake Basin Evolution of Salinized Lake Basin of Qingshuiying Formation in Yinchuan Basin. Earth Science, 48(1): 317-328. doi: 10.3799/dqkx.2021.257

    银川盆地清水营组咸化湖盆沉积特征与湖盆演化

    doi: 10.3799/dqkx.2021.257
    基金项目: 

    国家自然科学基金项目 42202150

    国家自然科学基金项目 42172179

    宁夏自然科学基金项目 2021AAC05024

    湖北省教育厅中青年人才项目 Q20211306

    详细信息
      作者简介:

      徐清海(1988—),男,副教授,博士,主要从事储层沉积学和非常规油气地质学研究. ORCID:0000-0003-4769-6052. E-mail:qinghai.xu@yangtzeu.edu.cn

      通讯作者:

      吴楠,E-mail: nan.w@qq.com

    • 中图分类号: P531

    Sedimentary Characteristics and Lake Basin Evolution of Salinized Lake Basin of Qingshuiying Formation in Yinchuan Basin

    • 摘要: 银川盆地发育厚层新生界,其中清水营组是咸化湖盆发育的时期,也是烃源岩最为发育的层段,因此明确清水营组的沉积特征及湖盆演化具有重要的地质意义和勘探意义. 综合利用野外露头、钻井岩心、测井及有机地球化学资料,对银川盆地古近纪晚期清水营组的岩性、岩相类型进行分析总结,明确沉积环境. 利用岩电特征、小波变换对清水营组进行沉积旋回识别与划分,在此基础上分析湖盆演化. 清水营组岩性主要为灰色泥岩、棕红色泥岩、含石膏泥岩、石膏及薄层细砂岩、粉砂岩等,共有四种岩相组合类型. 清水营组可划分3个四级旋回,对应清水营组咸化湖盆的3个演化阶段:SQ1为裂陷初期咸化湖盆的发育阶段;SQ2为强烈裂陷期,湖盆水体深度有所增大,盐湖鼎盛阶段;SQ3期水体变浅,湖盆范围变大,封闭性减弱,由咸水湖演化成淡水湖.

       

    • 图  1  银川盆地区域构造图及盆地地层与新近系岩性柱状图

      范高功和王利(2002)何宗昊等(2013)修改.∈.寒武系;O.奥陶系;C.石炭系;P.二叠系;M.中生界;E.古近系

      Fig.  1.  Regional tectonic map and basin stratigraphy and Neoproterozoic lithology column of Yinchuan Basin

      图  2  银川盆地南部牛首山烽台坡清水营组野外露头剖面

      a.清水营组与干河沟组不整合接触,清水营组发育厚层棕红色泥岩;b.清水营组棕红色泥岩近照;c.清水营组棕红色泥岩夹薄层细砂岩;d.清水营组棕褐色泥岩泥岩夹薄层细砂岩近照;e.清水营组灰色泥岩夹薄层石膏岩;f.薄层石膏近照

      Fig.  2.  Field outcrop section of the Qingshuiying Formation on Niushoushan, southern part of the Yinchuan Basin

      图  3  红墩子清水营组野外露头岩性特征

      a.剖面顶部清水营组灰绿色泥岩,厚度约0.4 m;b.红柳沟组(彰恩堡组)与清水营组地层,清水营组发育灰绿色泥岩;c. 剖面顶部细砂岩,下部为厚层灰绿色泥岩夹薄层棕红色粉细砂岩;d.剖面显示清水营组发育多套灰绿色泥岩,最上部一套泥岩最厚约0.5 m

      Fig.  3.  Field outcrop lithologic characteristics of the Qingshuiying Formation in Hongdunzi

      图  4  燕子湖清水营组野外露头岩性特征

      a.燕子湖露头剖面全景;b.栅栏外上部灰绿色泥岩,厚度约1 m,下部棕红色泥岩;c.棕红色泥岩夹薄层细砂岩

      Fig.  4.  Field outcrop lithologic characteristics of the Qingshuiying Formation at Yanzi Lake area

      图  5  银参4井钻井取心岩性特征

      a. 块状灰色泥岩,清水营组,3 175.00 m;b. 块状灰色膏质泥岩,石膏成团块状,清水营组,3 715.80 m;c. 厚层盐岩,清水营组,3 582.00~ 3 595.50 m;d. 块状棕红色泥岩,清水营组,3 563.20 m;e. 块状深灰色泥岩,清水营组,2 581.10 m;f. 块状棕红色膏质泥岩,石膏呈脉状分布,清水营组,3 660.00 m;g. 水平层理灰色泥岩,清水营组,2 519.55 m;h. 脉状层理细砂岩,与底部泥岩突变接触,清水营组,3 576.25 m;i. 块状灰色细砂岩,碳屑发育,清水营组,2 183.00 m

      Fig.  5.  Lithologic characteristics of the core drilled from the Yincan4 Well

      图  6  银堑1井清水营组岩心特征

      a. 块状灰色泥岩,清水营组,3 743.25 m;b. 块状灰色细砂岩,清水营组,4 248.37 m;c. 块状灰色膏质泥岩,清水营组,3 744.53 m;d. 块状棕红色泥岩,清水营组,4 244.60 m;e. 砂泥岩薄互层,清水营组,4 250.35 m

      Fig.  6.  Core characteristics of the Qingshuiying Formation in the Yinqian1 Well

      图  7  清水营组岩性组合类型

      Fig.  7.  Lithologic combination type of Qingshuiying Formation

      图  8  清水营组泥岩有机地化特征

      Fig.  8.  Organic geochemical characteristics of Qingshuiyingzu Formation

      图  9  银堑1井层序划分及沉积综合柱状图

      Fig.  9.  Stratigraphic division and sedimentary synthesis bar chart of Yinqian1 Well

      表  1  清水营组岩相类型划分

      Table  1.   Petrographic type classification of Qingshuiying Formation

      分类 颜色 岩性 岩相
      泥岩类 棕红色 泥岩 棕红色泥岩相
      浅棕色 泥岩 浅棕色泥岩
      灰绿色 泥岩 灰绿色泥岩
      灰白色 泥岩 灰白色泥岩
      砂岩类 浅棕色 粉砂岩 浅棕色粉砂岩
      浅棕色 泥质粉砂岩 浅棕色泥质粉砂岩
      灰色 细砂岩 灰色细砂岩
      盐岩类 棕褐色 膏质白云岩 棕褐色膏质白云岩
      黄灰色 膏岩 黄灰色膏岩
      混合岩类 棕红色 含灰泥岩 棕红色含灰泥岩
      棕褐色 白云质泥岩 棕褐色白云质泥岩
      下载: 导出CSV
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    出版历程
    • 收稿日期:  2021-09-14
    • 网络出版日期:  2023-02-01
    • 刊出日期:  2023-01-25

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