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Late Cambrian-Early Ordovician Condensed Oceanic Siliceous Deposits in the Iradyr Zone, Northern Kazakhstan

机译:哈萨克斯坦北部伊拉迪尔地区晚寒武世-早奥陶纪凝缩型海洋硅质矿床

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摘要

The data on conodonts and the geological structure of the siliceous sections in the Ishkeolmes and Iradyr Formations within the Iradyr Zone of the Northern Kazakhstan are reported. The layer-by-layer collection of conodonts provided the possibility to establish a wide (from the Upper Cambrian to the mid-Floian of the Lower Ordovician) age range of both formations and their relatively small thickness. The age intervals of the Ishkeolmes and Iradyr Formations are almost identical, and thus it is senseless to distinguish two formations with similar composition and age.
机译:报告了哈萨克斯坦北部伊拉迪尔地区伊斯凯尔摩斯和伊拉迪尔组硅质岩中牙形质和地质构造的数据。牙形石的逐层收集提供了建立两个地层的较宽年龄范围(从上寒武统到下奥陶纪中弗洛伊安)的可能性。 Ishkeolmes和Iradyr地层的年龄间隔几乎相同,因此区分具有相似组成和年龄的两个地层是毫无意义的。

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  • 来源
    《Doklady Earth Sciences》 |2012年第2期|p.681-686|共6页
  • 作者单位

    Karpinskii Russian Geological Research Institute,Russian Academy of Sciences, St. Petersburg, Russia;

    Geological Institute, Russian Academy of Sciences,Moscow, Russia;

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