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    二连盆地阿南凹陷下白垩统腾格尔组湖相云质岩成因

    魏巍 朱筱敏 朱世发 孙书洋 何明薇 杨德相 吴建平 王名巍

    魏巍, 朱筱敏, 朱世发, 孙书洋, 何明薇, 杨德相, 吴建平, 王名巍, 2017. 二连盆地阿南凹陷下白垩统腾格尔组湖相云质岩成因. 地球科学, 42(2): 258-272. doi: 10.3799/dqkx.2017.019
    引用本文: 魏巍, 朱筱敏, 朱世发, 孙书洋, 何明薇, 杨德相, 吴建平, 王名巍, 2017. 二连盆地阿南凹陷下白垩统腾格尔组湖相云质岩成因. 地球科学, 42(2): 258-272. doi: 10.3799/dqkx.2017.019
    Wei Wei, Zhu Xiaomin, Zhu Shifa, Sun Shuyang, He Mingwei, Yang Dexiang, Wu Jianping, Wang Mingwei, 2017. Origin of Lacustrine Dolomitic Rocks of the Lower Cretaceous Tengge'er Formation in Anan Sag, Erlian Basin. Earth Science, 42(2): 258-272. doi: 10.3799/dqkx.2017.019
    Citation: Wei Wei, Zhu Xiaomin, Zhu Shifa, Sun Shuyang, He Mingwei, Yang Dexiang, Wu Jianping, Wang Mingwei, 2017. Origin of Lacustrine Dolomitic Rocks of the Lower Cretaceous Tengge'er Formation in Anan Sag, Erlian Basin. Earth Science, 42(2): 258-272. doi: 10.3799/dqkx.2017.019

    二连盆地阿南凹陷下白垩统腾格尔组湖相云质岩成因

    doi: 10.3799/dqkx.2017.019
    基金项目: 

    国家“十二五”科技重大专项 2011ZX05001-002

    中国石油华北油田项目 HBYT-YJY-2014-JS-307

    详细信息
      作者简介:

      魏巍(1988-),女,博士,从事储层沉积和成岩研究.ORCID:0000-0003-3569-448X.E-mail: hunqiu8854@gmail.com

      通讯作者:

      朱筱敏,ORCID:0000-0002-5167-4975.E-mail: xmzhu@cup.edu.cn

    • 中图分类号: P618.13

    Origin of Lacustrine Dolomitic Rocks of the Lower Cretaceous Tengge'er Formation in Anan Sag, Erlian Basin

    • 摘要: 二连盆地阿南凹陷下白垩统腾格尔组发育一套湖相的富含致密油云质岩段,包括云质泥岩、云质沉凝灰岩和云质砂岩,但这类云质岩中的白云石岩石学特征及成因尚不明确.通过岩心、薄片、扫描电镜及碳氧同位素分析,将云质岩中的白云石分为两类:(1) 分布在纹层状和星点状云质泥岩或云质沉凝灰岩的非平直晶面、半自形微粉晶白云石;(2) 分布在块状云质沉凝灰岩或云质砂岩的非平直-平直晶面、自形粉细晶白云石.两类白云石的成因机制不同:(1) 半自形微粉晶白云石具偏高的δ13CPDB值(平均为5.4‰),主要受产甲烷菌的代谢活动影响,其δ18OPDB值负偏移量较小(平均为-13.0‰),计算形成温度约50~75 ℃,推测为成岩早期成因白云石,Mg2+离子主要来源于富火山灰的凝灰物质大量水解.(2) 自形粉细晶白云石晶体较大、晶形好,其δ13CPDB值偏低(0.2‰~0.7‰),受产甲烷菌的代谢活动和深层有机质热催化共同影响,其δ18OPDB值较低(平均为-19.4‰),计算形成温度约119 ℃,推测为成岩晚期埋藏成因白云石,Mg2+离子可能与粘土矿物水解及深部流体上涌有关.

       

    • 图  1  二连盆地阿南凹陷区域地质概况及综合柱状图

      a.地理位置;b.构造分区划分;c.剖面图;d.综合柱状图

      Fig.  1.  Location and stratigraphic column of Anan sag in Erlian basin

      图  2  阿南凹陷腾一段云质岩产出特征与薄片照片

      a.纹层状云质泥岩岩心,阿密2,1 506.40 m;b.纹层状云质泥岩薄片照片,阿密2,1 506.40 m;c.星点状云质沉凝灰岩岩心,阿密2,1 562.77 m;d.星点状云质沉凝灰岩薄片照片,阿密2,1 562.77 m;e.细晶白云石和云质砂岩,哈81,1 855.77 m;f.细晶白云石和云质沉凝灰岩,阿43,2 052.60 m

      Fig.  2.  The core and thin-section micrographs of the dolomitic rocks in the first member of Tenggeer Formation in Anan sag

      图  3  阿南凹陷腾一段云质岩中白云石的扫描电镜特征

      a.微晶白云石,纹层状云质泥岩,阿36,1 287.2 m;b.粉晶白云石,星点状云质沉凝灰岩,阿43,2 053.4 m;c.粉晶白云石,云质粉砂岩,阿35,1 593.8 m;d.粉晶白云石,云质粉砂岩,哈71,1 848.02 m

      Fig.  3.  SEM characteristics of dolomitic rocks in the first member of Tenggeer Formation in Anan sag

      图  4  阿南凹陷腾一段云质岩古地温分布

      Fig.  4.  Pale-temperature distribution of dolomitic rocks in the first member of Tenggeer Formation in Anan sag

      图  5  阿南凹陷腾一段云质岩碳、氧同位素值分布

      A.他形-半自形泥粉晶白云石分布区域;B.自行微细晶白云石分布区域;据Mazzullo (2000) 修改

      Fig.  5.  Distribution of carbon and oxygen isotopes of dolomitic rocks in the first member of Tenggeer Formation in Anan sag

      图  6  云质岩中斑晶和基质扫描电镜镜下特征及成分分析结果

      a.纹层状云质泥岩,阿36,1 287.20 m;b.图a中斜长石的能谱分析;c.云质沉凝灰岩,阿40,1 518.16 m;d.图c中粘土的X衍射分析结果

      Fig.  6.  SEM characteristics and composition analyses of phenocryst and matrix in dolomitic rocks

      图  7  阿南凹陷腾一段云质岩成因模式

      Fig.  7.  Simplified model for dolomitisation in the first member of Tenggeer Formation in Anan sag

      表  1  阿南凹陷腾一段云质岩中白云石岩石学特征

      Table  1.   Petrological characteristics of the dolomitic rocks in the first member of Tenggeer Formation in Anan sag

      产状 岩性 晶型 晶体大小 沉积环境
      粉微晶白云石 纹层状 云质泥岩 非平直晶面他形-半自形 5~40 μm 深湖-半深湖
      粉微晶白云石 星点状 云质沉凝灰岩云质泥岩 非平直晶面他形-半自形 10~30 μm 滨浅湖
      细晶白云石 团块状 云质沉凝灰岩 非平直晶面、半自形 50~70 μm 近岸水下扇外扇滨浅湖
      细晶白云石 小型交错层理 云质砂岩 平直晶面、自形 20~110 μm 扇三角洲前缘
      下载: 导出CSV

      表  2  阿南凹陷腾一段泥岩的微量元素特征

      Table  2.   Trace element concentration of mudrocks in the first member of Tenggeer Formation in Anan sag

      井号 A23 A3 H23-1 H84 A43-1 H16 H23-2 H46 A43-2
      岩性 云质泥岩 云质泥岩 云质泥岩 云质泥岩 云质泥岩 泥岩 泥岩 钙质泥岩 钙质泥岩
      方解石绝对含量 1.7 / 9.4 0.9 7.9 12.0 / 22.8 32.1
      白云石绝对含量 38.5 32.0 16.3 34.4 21.7 10.0 17.0 4.3 0.0
      Ni (10-6) 62.9 57.8 115.0 50.5 30.8 67.7 78.5 44.1 64.4
      V (10-6) 103.0 119.0 51.6 52.1 98.6 82.8 72.8 86.7 46.8
      Sr (10-6) 438 484 450 302 459 451 396 377 711
      Ba (10-6) 356 438 405 240 472 463 404 301 432
      Cu (10-6) 21.8 39.7 25.3 14.8 28.2 23.3 21.2 26.6 18.7
      V/Ni 1.64 2.06 0.45 1.03 3.20 1.22 0.93 1.97 0.73
      V/(V+Ni) 0.62 0.67 0.31 0.51 0.76 0.55 0.48 0.66 0.42
      Sr/Ba 1.23 1.10 1.11 1.26 0.97 0.97 0.98 1.25 1.65
      Sr/Cu 20.11 12.19 17.80 20.49 16.30 19.36 18.75 14.17 37.99
      下载: 导出CSV

      表  3  阿南凹陷腾一段云质岩的碳氧同位素特征

      Table  3.   Carbon and oxygen isotopes characteristics of dolomitic rocks in the first member of Tenggeer Formation in Anan sag

      样品 岩性 晶体特征 方解石含量(%) 白云石含量(%) δ13CPDB(‰) δ18OPBD(‰) Z 温度(℃)
      A3 云质泥岩 他形-半自形微粉晶白云石 粉晶 / 32.0 5.7 -12.0 133.00 63.87
      H23-1 云质沉凝灰岩 微晶 / 26.0 5.6 -13.1 132.25 71.18
      H71 含云泥岩 粉晶 4 19.6 6.1 -10.1 134.76 52.00
      A35-1 云质泥岩 微晶 / 23.1 4.8 -15.0 129.66 84.55
      H16 含云粉砂岩 粉-细晶 / 19.0 5.3 -13.5 131.43 73.92
      H72 云质泥岩 粉晶 2 16.1 6.0 -9.8 134.70 50.20
      A35-2 云质粉砂岩 自形粉细晶白云石 细晶 / 26.2 4.7 -20.6 126.67 129.47
      H84-1 云质粉砂岩 细晶 / 34.0 0.2 -18.1 118.70 108.40
      H84-2 云质粉砂岩 细晶 4 18.0 0.7 -18.0 119.77 107.60
      下载: 导出CSV
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