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The results of geochronological and isotope–geochemical study of zircons from tuff of the Sylvitsa Group (western slope of the Middle Urals): The origin of ash layers in Vendian rocks of the East European Platform

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Abstract

New LA-ICP-MS data on the U–Pb isotope age, Hf isotope characteristics, and concentrations of trace elements in zircons from volcanic tuff of the Upper Vendian Sylvitsa Group on the western slope of the Middle Urals are reported.

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Authors and Affiliations

  1. Geological Institute, Russian Academy of Sciences, Moscow, 119017, Russia

    N. B. Kuznetsov

  2. Gubkin Russian State University of Oil and Gas, Moscow, 119991, Russia

    N. B. Kuznetsov & T. V. Romanyuk

  3. Australian Research Council Centre of Excellence for Core to Crust Fluid Systems, GEMOC, Macquarie University, Sydney, Australia

    N. B. Kuznetsov, E. A. Belousova & T. V. Romanyuk

  4. Zavaritskii Institute of Geology and Geochemistry, Ural Branch, Russian Academy of Sciences, Yekaterinburg, 620016, Russia

    M. T. Krupenin & A. V. Maslov

  5. Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russia

    N. B. Kuznetsov & T. V. Romanyuk

Authors
  1. N. B. Kuznetsov
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  2. E. A. Belousova
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  3. M. T. Krupenin
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  4. T. V. Romanyuk
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  5. A. V. Maslov
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Corresponding author

Correspondence to T. V. Romanyuk.

Additional information

Original Russian Text © N.B. Kuznetsov, E.A. Belousova, M.T. Krupenin, T.V. Romanyuk, A.V. Maslov, 2017, published in Doklady Akademii Nauk, 2017, Vol. 473, No. 3, pp. 86–90.

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Kuznetsov, N.B., Belousova, E.A., Krupenin, M.T. et al. The results of geochronological and isotope–geochemical study of zircons from tuff of the Sylvitsa Group (western slope of the Middle Urals): The origin of ash layers in Vendian rocks of the East European Platform. Dokl. Earth Sc. 473, 359–362 (2017). https://doi.org/10.1134/S1028334X17030254

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  • DOI: https://doi.org/10.1134/S1028334X17030254

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