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    沧东凹陷孔二段混合细粒沉积岩相特征及形成环境

    李圯 刘可禹 蒲秀刚 陈世悦 韩文中 张伟 汪虎 梁超 赵建华

    李圯, 刘可禹, 蒲秀刚, 陈世悦, 韩文中, 张伟, 汪虎, 梁超, 赵建华, 2020. 沧东凹陷孔二段混合细粒沉积岩相特征及形成环境. 地球科学, 45(10): 3779-3796. doi: 10.3799/dqkx.2020.167
    引用本文: 李圯, 刘可禹, 蒲秀刚, 陈世悦, 韩文中, 张伟, 汪虎, 梁超, 赵建华, 2020. 沧东凹陷孔二段混合细粒沉积岩相特征及形成环境. 地球科学, 45(10): 3779-3796. doi: 10.3799/dqkx.2020.167
    Li Yi, Liu Keyu, Pu Xiugang, Chen Shiyue, Han Wenzhong, Zhang Wei, Wang Hu, Liang Chao, Zhao Jianhua, 2020. Lithofacies Characteristics and Formation Environments of Mixed Fine-Grained Sedimentary Rocks in Second Member of Kongdian Formation in Cangdong Depression, Bohai Bay Basin. Earth Science, 45(10): 3779-3796. doi: 10.3799/dqkx.2020.167
    Citation: Li Yi, Liu Keyu, Pu Xiugang, Chen Shiyue, Han Wenzhong, Zhang Wei, Wang Hu, Liang Chao, Zhao Jianhua, 2020. Lithofacies Characteristics and Formation Environments of Mixed Fine-Grained Sedimentary Rocks in Second Member of Kongdian Formation in Cangdong Depression, Bohai Bay Basin. Earth Science, 45(10): 3779-3796. doi: 10.3799/dqkx.2020.167

    沧东凹陷孔二段混合细粒沉积岩相特征及形成环境

    doi: 10.3799/dqkx.2020.167
    基金项目: 

    国家科技重大专项 2017ZX05009001

    中国科学院战略性先导科技专项(A类) XDA14010401

    泰山学者工程资助 TSQN201812030

    中央高校基本科研业务费专项 19CX07003A

    详细信息
      作者简介:

      李圯(1996-), 硕士研究生, 从事沉积学与层序地层学研究.ORCID:0000-0002-7245-842X.E-mail:s18010024@s.upc.edu.cn

      通讯作者:

      刘可禹, E-mail:liukeyu@upc.edu.cn

      蒲秀刚, E-mail:puxgang@petrochina.com.cn

    • 中图分类号: P588.21

    Lithofacies Characteristics and Formation Environments of Mixed Fine-Grained Sedimentary Rocks in Second Member of Kongdian Formation in Cangdong Depression, Bohai Bay Basin

    • 摘要: 沧东凹陷孔二段页岩层系广泛发育混合细粒沉积岩.混合细粒沉积岩的岩石类型划分和沉积环境分析是其成因研究的重要组成部分,有助于总结混合细粒沉积岩的沉积规律,寻找有利勘探目标.通过岩心与薄片观察、二维XRF(X射线荧光光谱)扫描,结合XRD(X射线衍射)、元素地球化学测试等资料,以矿物成分和沉积构造为主要依据,将孔二段混合细粒沉积岩划分为21种岩相;通过Sr/Cu、Mg/Ca、Sr/Ba、V/(V+Ni)、Al、Ti含量、Fe/Mn和(Fe+Al)/(Ca+Mg)等地球化学指标的垂向变化及岩相分析沉积环境演化.沧东凹陷孔二段混合细粒沉积岩主要发育在气候干旱、微咸水-咸水相、水体贫氧、陆源输入较强的半深湖-深湖环境中;岩相类型的发育同时受到水体的高盐度和陆源输入的影响,均一细粒沉积岩分布最广,其次为灰云细粒沉积岩,黏土细粒沉积岩不发育.

       

    • 图  1  沧东凹陷构造简图

      赵贤正等(2018)Mao et al.(2018)

      Fig.  1.  Location structural subdivision and stratigraphic-structural cross section of the Cangdong depression

      图  2  沧东凹陷新生代地层

      Luo et al.(2017), 叶琳(2013)

      Fig.  2.  Cenozoic strata of the Cangdong sag

      图  3  沧东凹陷孔二段矿物特征

      a.石英颗粒独立分布和顺层分布形成粉砂质纹层(普通薄片,正交光),2 972.91 m;b.石英颗粒(扫描电镜),3 002.00 m;c.长石颗粒(扫描电镜),3 011.00 m;d.方沸石颗粒全消光(普通薄片,正交光),2 928.74 m;e.方沸石颗粒(扫描电镜),3 010.00 m;f.黏土矿物(扫描电镜),3 036.00 m;g.泥晶铁白云石颗粒均匀分布(普通薄片,正交光),2 928.74 m;h.铁白云石(扫描电镜),3 023.00 m;i.生物碎屑(普通薄片,正交光),2 928.74 m

      Fig.  3.  Occurrence of various minerals in Ek2 within the Cangdong depression

      图  4  沧东凹陷孔二段GX井矿物含量垂向分布

      Fig.  4.  Vertical distributions of mineral contents of well GX in Ek2 within the Cangdong depression

      图  5  沧东凹陷GX井孔二段典型沉积构造

      a.混合型块状构造(普通薄片,正交光),3 311.34 m;b.灰云质块状构造(普通薄片,正交光),2 928.74 m;c.长英质纹层(普通薄片,正交光),3 229.80 m;d.方沸石纹层全消光现象(普通薄片,正交光),3 120.00 m;e.波状灰云质纹层(普通薄片,正交光),3 120.00 m;f.波状灰云质纹层(XRF),3 120.00 m;g.生物碎屑顺层分布形成灰云质纹层(普通薄片,正交光),2 930.45 m;h.水平灰云质纹层(普通薄片,正交光),3 120.00 m;i.水平灰云质纹层(普通薄片,正交光),3 120.00 m;j.方沸石纹层、灰云质纹层、黏土质纹层叠置(普通薄片,正交光),2 971.19 m;k.混合纹层界限模糊(普通薄片,正交光),2 972.21 m;l.混合纹层间主要矿物含量渐变(XRF),2 930.92 m

      Fig.  5.  Typical sedimentary structure in Ek2 within the Cangdong depression

      图  6  沧东凹陷孔二段主要矿物类型及含量分布

      Fig.  6.  Mineral types and contents in Ek2 within the Cangdong depression

      图  7  沧东凹陷孔二段混合细粒岩主要岩相类型

      Fig.  7.  Main lithofacies of mixed fine-grained rock in Ek2 within the Cangdong depression

      图  8  沧东凹陷孔二段灰云细粒沉积岩

      a.块状灰云细粒沉积岩碳酸盐矿物占主导地位(XRF),2 928.74 m;b.块状灰云细粒沉积岩碎屑物质均匀分布于碳酸盐矿物中(普通薄片,正交光), 2 928.74 m;c.块状灰云细粒沉积岩中可见软沉积物变形构造(岩心照片),2 928.74 m;d.纹层状灰云细粒沉积岩中主要为灰云质纹层(XRF),3 120.00 m;e.纹层状灰云细粒沉积岩灰云质纹层厚度较大(普通薄片,正交光),3 120.00 m;f.纹层状灰云细粒沉积岩褐色-灰黑色纹层叠置(岩心照片),3 120.00 m;g.纹层状灰云细粒沉积岩中灰云质纹层与粉砂质纹层叠置(普通薄片,正交光),3 120.00 m;h.纹层状灰云细粒沉积岩灰白色纹层与灰黑色纹层叠置(岩心照片),3 120.00 m

      Fig.  8.  Lime-dolomite fine-grained sedimentary rocks in Ek2 within the Cangdong depression

      图  9  沧东凹陷孔二段长英细粒沉积岩

      a.纹层状长英细粒沉积岩主要发育粉砂质纹层(XRF),2 971.19 m;b.纹层状长英细粒沉积岩长英质纹层与黏土质纹层互层(普通薄片,正交光),2 971.19 m;c.纹层状长英细粒沉积岩岩心呈灰黑色(岩心照片),2 972.66 m

      Fig.  9.  Felsic fine-grained sedimentary rocks in Ek2 within the Cangdong depression

      图  10  沧东凹陷孔二段均一细粒沉积岩

      a.块状均一细粒沉积岩碳酸盐矿物与碎屑物质均匀混合(XRF),3 310.00 m;b.块状均一细粒沉积岩长英质矿物局部富集(普通薄片,正交光),3 310.00 m;c.块状均一细粒沉积岩中泄水构造(岩心照片),3 249.90 m;d.纹层状均一细粒沉积岩混合纹层间矿物含量差异小(XRF),3 043.53 m;e.纹层状均一细粒沉积岩中混合纹层颜色差别小(普通薄片,正交光),3 043.53 m;f.纹层状均一细粒沉积岩中混合纹层边界模糊(岩心照片),3 249.90 m;g.单一组分纹层组成的纹层状均一细粒沉积岩纹层间矿物含量差别大(XRF),3 050.26 m;h.单一组分纹层组成的纹层状均一细粒沉积岩(普通薄片,正交光),3 050.26 m;i.单一组分纹层组成的纹层状均一细粒沉积岩纹层清晰、界限明显(岩心照片),3 250.74 m

      Fig.  10.  Homogeneous fine-grained clastic-carbonate sedimentary rocks in Ek2 within the Cangdong depression

      图  11  沧东凹陷GX井孔二段二亚段沉积环境演化

      1.粉砂岩; 2.盆地边缘相(三角洲平原、三角洲前缘等); 3.块状均一细粒沉积岩(BPH); 4.纹层状均一细粒沉积岩(LPH); 5.块状含方沸石均一细粒沉积岩(BCH); 6.纹层状含方沸石均一细粒沉积岩(LCH); 7.块状方沸石质均一细粒沉积岩(BHH); 8.纹层状方沸石质均一细粒沉积岩(LHH); 9.块状方沸石均一细粒沉积岩(BRH); 10.块状长英细粒沉积岩(BPFE); 11.纹层状长英细粒沉积岩(LPFE); 12.块状含方沸石长英细粒沉积岩(BCFE); 13.纹层状含方沸石长英细粒沉积岩(LCFE); 14.块状方沸石质长英细粒沉积岩(BHFE); 15.纹层状方沸石长英细粒沉积岩(LRFE); 16.块状灰云细粒沉积岩(BPCA); 17.纹层状灰云细粒沉积岩(LPCA); 18.块状含方沸石灰云细粒沉积岩(BCCA); 19.纹层状含方沸石灰云细粒沉积岩(LCCA); 20.纹层状方沸石灰云细粒沉积岩(LRCA)

      Fig.  11.  Sedimentary environment variations through time in Ek22 within the Cangdong depression

      表  1  沧东凹陷孔二段混合细粒沉积岩岩相类型

      Table  1.   Lithofacies of mixed fine-grained rock in Ek2 within the Cangdong depression

      主要矿物含量 沉积构造 方沸石含量 岩相类型
      灰云细粒沉积岩 块状 > 50% 块状方沸石灰云细粒沉积岩(BRCA)
      25%~50%
      10%~15% 块状含方沸石灰云细粒沉积岩(BCCA)
      < 10% 块状灰云细粒沉积岩(BPCA)
      纹层状 > 50% 纹层状方沸石灰云细粒沉积岩(LRCA)
      25%~50%
      10%~15% 纹层状含方沸石灰云细粒沉积岩(LCCA)
      < 10% 纹层状灰云细粒沉积岩(LPCA)
      长英细粒沉积岩 块状 > 50% 块状方沸石长英细粒沉积岩(BRFE)
      25%~50% 块状方沸石质长英细粒沉积岩(BHFE)
      10%~15% 块状含方沸石长英细粒沉积岩(BCFE)
      < 10% 块状长英细粒沉积岩(BPFE)
      纹层状 > 50% 纹层状方沸石长英细粒沉积岩(LRFE)
      25%~50%
      10%~15% 纹层状含方沸石长英细粒沉积岩(LCFE)
      < 10% 纹层状长英细粒沉积岩(LPFE)
      均一细粒沉积岩 块状 > 50% 块状方沸石均一细粒沉积岩(BRH)
      25%~50% 块状方沸石质均一细粒沉积岩(BHH)
      10%~15% 块状含方沸石均一细粒沉积岩(BCH)
      < 10% 块状均一细粒沉积岩(BPH)
      纹层状 > 50% 纹层状方沸石均一细粒沉积岩(LRH)
      25%~50% 纹层状方沸石质均一细粒沉积岩(LHH)
      10%~15% 纹层状含方沸石均一细粒沉积岩(LCH)
      < 10% 纹层状均一细粒沉积岩(LPH)
      下载: 导出CSV
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    • 收稿日期:  2019-12-31
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