卢进才, 魏仙样, 魏建设, 李玉宏. 2010: 内蒙古西部额济纳旗雅干地区二叠系埋汗哈达组烃源岩的特征. 地质通报, 29(2-3): 341-345.
    引用本文: 卢进才, 魏仙样, 魏建设, 李玉宏. 2010: 内蒙古西部额济纳旗雅干地区二叠系埋汗哈达组烃源岩的特征. 地质通报, 29(2-3): 341-345.
    LU Jin-cai, WEI Xian-yang, WEI Jian-she, LI Yu-hong. 2010: Characteristics of hydrocarbon source rocks in the Permian Maihanhada Formation in Yagan area of Ejina Banner, western Inner Mongolia, China. Geological Bulletin of China, 29(2-3): 341-345.
    Citation: LU Jin-cai, WEI Xian-yang, WEI Jian-she, LI Yu-hong. 2010: Characteristics of hydrocarbon source rocks in the Permian Maihanhada Formation in Yagan area of Ejina Banner, western Inner Mongolia, China. Geological Bulletin of China, 29(2-3): 341-345.

    内蒙古西部额济纳旗雅干地区二叠系埋汗哈达组烃源岩的特征

    Characteristics of hydrocarbon source rocks in the Permian Maihanhada Formation in Yagan area of Ejina Banner, western Inner Mongolia, China

    • 摘要: 在对内蒙古额济纳旗雅干地区二叠系埋汗哈达组岩性特征、暗色泥页岩油气地球化学特征研究的基础上,总结了烃源岩的纵向分布特征,以及有机质丰度、干酪根类型和热演化的特征。二叠系埋汗哈达组烃源岩分布层段集中,暗色泥页岩累计厚度达296.9m。总有机碳(TOC)含量平均为0.59%,TOC大于0.3%的样品占92.86%。干酪根类型为Ⅱ—Ⅲ型,Ro平均为1.08%,表明干酪根演化进入成熟阶段。生物标志化合物分析结果显示,Pr/Ph为0.64~0.78,为强还原环境的沉积。综合评价认为,二叠系埋汗哈达组具有较好的生烃条件。

       

      Abstract: Based on the study on the lithologic features and hydrocarbon geochemical characteristics of dark mudstone and shale of Permian Maihanhada Formation, the authors summarize longitudinal distribution of source rocks, organic matter abundance, kerogen type and thermal evolution characteristics. The source rocks of Permian Maihanhada Formation are centralized distributed, and the total thickness of dark mudstone and shale is 296.9m. The average organic carbon content is 0.59%, and the values of sample more than 0.3% account for 92.86%. The kerogen type is dominated by Ⅱ-Ⅲ type, and the average vitrinite reflectance is 1.08%, which shows that kerogen has turned into mature stage. Analysis on biomarker of Pr/Ph ranges from 0.64 to 0.78, which shows strong reduction. It is concluded that the source rocks of Permian Maihanhada Formation have good hydrocarbon generation conditions.

       

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