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    利津洼陷沙四上亚段深部砂岩的成岩环境演化

    唐鑫萍 黄文辉 李敏 董果果 吴刚 王文勇 姜在兴

    唐鑫萍, 黄文辉, 李敏, 董果果, 吴刚, 王文勇, 姜在兴, 2013. 利津洼陷沙四上亚段深部砂岩的成岩环境演化. 地球科学, 38(4): 843-852. doi: 10.3799/dqkx.2013.082
    引用本文: 唐鑫萍, 黄文辉, 李敏, 董果果, 吴刚, 王文勇, 姜在兴, 2013. 利津洼陷沙四上亚段深部砂岩的成岩环境演化. 地球科学, 38(4): 843-852. doi: 10.3799/dqkx.2013.082
    TANG Xin-ping, HUANG Wen-hui, LI Min, DONG Guo-guo, WU Gang, WANG Wen-yong, JIANG Zai-xing, 2013. Diagenetic Environment Evolution of Deep Sandstones in the Upper Es4 of the Palaeogene in Lijin Sag. Earth Science, 38(4): 843-852. doi: 10.3799/dqkx.2013.082
    Citation: TANG Xin-ping, HUANG Wen-hui, LI Min, DONG Guo-guo, WU Gang, WANG Wen-yong, JIANG Zai-xing, 2013. Diagenetic Environment Evolution of Deep Sandstones in the Upper Es4 of the Palaeogene in Lijin Sag. Earth Science, 38(4): 843-852. doi: 10.3799/dqkx.2013.082

    利津洼陷沙四上亚段深部砂岩的成岩环境演化

    doi: 10.3799/dqkx.2013.082
    基金项目: 

    国家科技重大专项 2011ZX05009-002

    详细信息
      作者简介:

      唐鑫萍(1987-), 男, 硕士研究生, 研究方向为应用沉积学.E-mail: cugbtxp@126.com

      通讯作者:

      黄文辉, E-mail: huangwh@cugb.edu.cn

    • 中图分类号: P588.21

    Diagenetic Environment Evolution of Deep Sandstones in the Upper Es4 of the Palaeogene in Lijin Sag

    • 摘要: 为研究利津洼陷沙四上亚段深部砂岩成岩环境, 对岩心样品进行偏光、荧光、阴极发光显微镜和扫描电镜观察, 辅以粘土矿物含量、元素含量测试.识别出酸性和碱性2种成岩环境, 酸性环境以硅质沉淀、碳酸盐矿物溶解、长石溶解或蚀变为高岭石等现象组合为标志, 碱性环境以碳酸盐矿物沉淀、长石次生加大、石英溶解等现象组合为标志.总体演化为: 同生期, 原始沉积流体造成碱性环境; 早成岩期, 未熟有机质演化形成短期的酸性环境, 继承流体形成主体的碱性环境; 中成岩A1期(埋深约2700~3200m), 有机质成熟形成酸性环境; 中成岩A2期(埋深约3200~4200m), 深部断裂活动形成碱性环境; 中成岩B期(埋深约4200~4400m), 第二期充注油气的热演化形成酸性环境.

       

    • 图  1  利津洼陷位置示意

      Fig.  1.  Sketch map showing the position of Lijin sag

      图  2  利津洼陷沙四上亚段砂岩的酸性成岩环境特征

      a.方解石溶蚀孔,滨660井,2813.9m,正交偏光200倍;b.石英次生加大,梁756井,3067.5m,正交偏光200倍;c.长石溶蚀,溶孔内发育黄铁矿,滨660井,2813.9m,扫描电镜2120倍;d.自生石英,梁756井,3067.5m,扫描电镜2080倍

      Fig.  2.  Characteristics of acidic diagenetic environment in sandstones of the upper Es4 in Lijin sag

      图  3  利津洼陷沙四上亚段砂岩的碱性成岩环境特征

      a.方解石泥晶套,滨660井,2764.4m,正交偏光200倍;b.钙质胶结较紧密,可见方解石交代石英,滨442井,3928m,正交偏光200倍;c.铁白云石晶体充填孔隙,自生铁白云石胶结物一般大量出现于中成岩阶段A期之后,利672井,4014.35m,扫描电镜532倍;d.钠长石加大Ⅲ级,丝状伊利石,滨440井,3851.8m,扫描电镜875倍

      Fig.  3.  Characteristics of alkaline diagenetic environment in sandstones of the upper Es4 in Lijin sag

      图  4  利津洼陷沙四上亚段砂岩粘土矿物含量的垂向分布图(根据21口井的357个样品的XRD测试统计)

      高岭石、伊利石、绿泥石、伊蒙混层的含量,分别指其在样品粘土矿物总量中的百分含量;“伊蒙混层比”为蒙脱石层在伊蒙混层中的百分含量

      Fig.  4.  Vertical distribution for the relative contents of clay of sandstones in the upper Es4 in Lijin sag

      图  5  利津洼陷沙四上亚段砂岩的阴极发光、荧光以及偏光显微照片——烃类流体的充注与长石溶蚀伴生

      a.荧光显微照片中,有两种颜色的荧光显示,分别为基质溶孔中的绿色光、方解石胶结物的黄色光,因有机质的荧光颜色会随其成分和含量而变化,可初步判别出两期油气聚集;b.结合对应的正交偏光显微照片可知,基质溶蚀后发生第一期油气聚集,方解石沉淀之后第二期聚集;c.阴极发光中钾长石因富钾而发亮蓝色光,亮蓝色的钾长石边缘已被不发光的蚀变产物取代,而且蚀变接触面呈现港湾状;d.结合对应的单偏光照片可看出,钾长石颗粒边缘有蚀变的痕迹,可知是钾长石被溶蚀所致,而在钾长石溶蚀边缘和钾长石粒内溶孔中,均有沥青质的分布.滨442井,4228.75m;a,b.400倍;c,d.100倍

      Fig.  5.  Fluorescent and cathodoluminescence photomicrographs of sandstones in the upper Es4 in Lijin Sag

      图  6  利津洼陷沙四上砂岩岩心照片(利672井,4019.8m)

      Fig.  6.  Photographs of core samples of sandstones in the upper Es4 in Lijin sag

      图  7  利津洼陷沙四上砂体成岩环境演化模式

      a.滨660井,2764.4m,铸体薄片正交偏光200倍;b.滨440井,3851.2m,铸体薄片正交偏光200倍;c.梁756井,3070.1m,铸体薄片正交偏光200倍;d.滨440井,3852.5m,扫描电镜6260倍;e.滨442井,4228.75m,扫描电镜倍7850

      Fig.  7.  Evolution model for diagenetic environment of sandstones in the upper Es4 in Lijin Sag

      表  1  利津洼陷沙四上亚段岩心特征元素含量测试值

      Table  1.   Part of the chemical composition data of sandstones in the upper Es4 in Lijin sag

      井位 深度(m) 岩性 CaO(%) Sr(10-6) Ba(10-6) Sr/Ca Sr/Ba
      滨666 3075.09 白云质粉砂岩 7.92 659.30 286.00 102.32 2.14
      滨666 3106.52 白云质粉砂岩 10.17 748.15 2482.00 93.26 1.16
      滨667 2925.43 灰质粉砂岩 13.24 1317.58 1495.80 118.98 2.43
      滨667 2922.90 隐晶白云岩 14.29 2013.29 811.20 169.79 11.91
      利935 3065.40 灰质粉砂岩 15.77 1759.64 570.15 139.46 8.25
      利935 3139.40 灰质粉砂岩 15.82 1700.32 509.02 134.34 5.95
      利95 2619.35 隐晶白云岩 14.36 1554.66 457.31 135.50 4.71
      利95 2738.70 白云质粉砂岩 9.37 1033.48 331.01 140.73 3.61
      梁218 3238.70 白云质粉砂岩 13.64 1511.74 313.90 139.80 5.16
      梁218 3236.20 白云质粉砂岩 11.15 1251.15 250.75 142.41 4.60
      注:CaO含量采用x射线荧光(XRF)测试,最低检测限为0.001%;Sr、Ba值由电感耦合等离子体质谱(ICP-MS),最低检测限为0.001μg/g;实验由中国矿业大学(北京)煤炭资源与安全开采国家重点实验室完成.
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    • 收稿日期:  2012-07-17
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