徐黎明, 周立发, 邓昆, 杨文敬. 鄂尔多斯盆地西缘二叠系事件地层及其地球化学特征[J]. 煤田地质与勘探, 2006, 34(6): 4-8.
引用本文: 徐黎明, 周立发, 邓昆, 杨文敬. 鄂尔多斯盆地西缘二叠系事件地层及其地球化学特征[J]. 煤田地质与勘探, 2006, 34(6): 4-8.
XU Li-ming, ZHOU Li-fa, DENG Kun, YANG Wen-jing. Geochemical characteristics of Permian event strata in western margin of Ordos Basin[J]. COAL GEOLOGY & EXPLORATION, 2006, 34(6): 4-8.
Citation: XU Li-ming, ZHOU Li-fa, DENG Kun, YANG Wen-jing. Geochemical characteristics of Permian event strata in western margin of Ordos Basin[J]. COAL GEOLOGY & EXPLORATION, 2006, 34(6): 4-8.

鄂尔多斯盆地西缘二叠系事件地层及其地球化学特征

Geochemical characteristics of Permian event strata in western margin of Ordos Basin

  • 摘要: 通过钻井岩心的观察及镜下岩矿鉴定,同时依据地球化学和沉积学特征,把区内发育的事件地层分为两类:火山事件层和海退事件层,其中太原组火山事件层和海退事件层各1层,山西组火山事件层1层,石盒子组火山事件层3层。所体现的常量、微量和稀土元素质量分数及岩石学特征具明显的差异。研究事件地层获得的成果,可以为区域地层划分和对比提供更加准确的依据。

     

    Abstract: It is of importance for gas prospecting that the section of Permian strata in the western margin of Ordos Basin has been systematically studied.Based on the research in terms of petrographyic,sedimentological and geochemical data,event layers which can be divided into two types have been discovered.These are volcanic event layer and regressive layer,which are developed in Taiyuan Formation respectively,one volcanic event layer in Shanxi Formation and three in Shihezi Formation.Major element,trace element and rare earth element data exhibit considerable variability.The results indicate that the event layers are better tools for regional stratigraphic division and correlation.

     

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