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首页> 外文期刊>Doklady Earth Sciences >Zirconology of Navysh Volcanic Rocks of the Ai Suite and the Problem of the Age of the Lower Riphean Boundary in the Southern Urals
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Zirconology of Navysh Volcanic Rocks of the Ai Suite and the Problem of the Age of the Lower Riphean Boundary in the Southern Urals

机译:艾套房的纳什什火山岩锆石学和南部乌拉尔山脉下里菲安边界年龄问题

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摘要

Volcanic rocks of the Navysh Complex occur in the base of the Lower Riphean Ai Formation of the Burzyan Series within the Bashkirian meganticlinorium (Southern Urals). They represent practically the only object suitable by the material—geological and geochronolog-ical criteria for estimation of the age of the lower boundary of not only the Ai Formation, but the whole strato-typical Riphean section of the Southern Urals.
机译:Navysh情结的火山岩出现在Bashkirian meganticlinorium(南部乌拉尔)内Burzyan系列下Riphean Ai组的底部。实际上,它们是唯一适合该物质的对象-地质和年代学标准,不仅可以估算Ai地层下界的年龄,而且可以估算整个南乌拉尔地层典型的Riphean段。

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  • 来源
    《Doklady Earth Sciences》 |2013年第2期|185-190|共6页
  • 作者单位

    Zavaritskii Institute of Geology and Geochemistry, Ural Branch, Russian Academy of Sciences, Yekaterinburg;

    Institute of Geology, Ufa Science Center, Russian Academy of Sciences, Ufa,Bashkirian State University;

    Institute of Geology, Ufa Science Center, Russian Academy of Sciences, Ufa;

    Institute of Geology, Ufa Science Center, Russian Academy of Sciences, Ufa;

    Zavaritskii Institute of Geology and Geochemistry, Ural Branch, Russian Academy of Sciences, Yekaterinburg;

    Bashkirian State University,Karpinskii Russian Geological Research Institute, Saint Petersburg;

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