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    陇东地区延长组疑源类组合特征及其古环境意义

    吉利明 王少飞 徐金鲤

    吉利明, 王少飞, 徐金鲤, 2006. 陇东地区延长组疑源类组合特征及其古环境意义. 地球科学, 31(6): 798-806.
    引用本文: 吉利明, 王少飞, 徐金鲤, 2006. 陇东地区延长组疑源类组合特征及其古环境意义. 地球科学, 31(6): 798-806.
    JI Li-ming, WANG Shao-fei, XU Jin-li, 2006. Acritarch Assemblage in Yanchang Formation in Eastern Gansu Province and Its Environmental Implications. Earth Science, 31(6): 798-806.
    Citation: JI Li-ming, WANG Shao-fei, XU Jin-li, 2006. Acritarch Assemblage in Yanchang Formation in Eastern Gansu Province and Its Environmental Implications. Earth Science, 31(6): 798-806.

    陇东地区延长组疑源类组合特征及其古环境意义

    基金项目: 2002年度中国科学院“西部之光”人才培养计划项目; 2003年度甘肃省中青年科技基金项目
    详细信息
      作者简介:

      吉利明(1963-),男,副研究员,主要从事微体古生物学与石油地质学研究。E-mail:liming_ji@163.com

    • 中图分类号: P531

    Acritarch Assemblage in Yanchang Formation in Eastern Gansu Province and Its Environmental Implications

    • 摘要: 为了明确中晚三叠世延长组形成时期鄂尔多斯盆地陆相沉积的属性, 用孢粉分析方法详细研究了陇东西峰油田钻井岩心的微古植物组合, 在主要源岩层——延长组长7段发现了极为丰富的疑源类, 化石丰度高, 但属种单调; 以光面球藻(Leiosphaeridia) 绝对占优势, 经常出现具刺的微刺藻(Micrhystridium).同时代疑源类, 特别是具刺型疑源类生态分布和组合特征对比分析认为, 陇东地区中晚三叠世主要为淡水湖泊环境.出现的具刺疑源类不仅类型单调, 而且棘刺明显弱化, 推测是个别海生具刺类型在淡水环境中经历长期演化的结果.本地区主要烃源岩长7段沉积时期恰好处于湖水淡化过程, 也是最大湖进期, 大规模的湖水补给来源于陆地, 并非海侵.表明中晚三叠世鄂尔多斯盆地已经结束早中三叠世近海湖泊的性质.

       

    • 图  1  陇东地区延长组疑源类钻井地层分布

      Fig.  1.  Distribution of acritarch from well core of Yanchang Formation in eastern Gansu Province

      图  2  荧光显示的光球型疑源类(Leiosphaeridia spp.)

      a.分散个体, 20-X44, ×320;b.块状聚合体, 12-X44, ×350

      Fig.  2.  Fluorescence image of Leiosphaeridia spp.

      图  3  陇东延长组疑源类主要类型电镜扫描照片

      a.Leiosphaeridia sp.; b.Comasphaeridium sp.; c.Micrhystridium sp.: c1.整体, c2.局部

      Fig.  3.  Scanning photograph of main acritarch types under electron microscope

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