Doklady Earth Sciences

, Volume 473, Issue 1, pp 359–362 | Cite as

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

  • N. B. Kuznetsov
  • E. A. Belousova
  • M. T. Krupenin
  • T. V. Romanyuk
  • A. V. Maslov


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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Copyright information

© Pleiades Publishing, Ltd. 2017

Authors and Affiliations

  • N. B. Kuznetsov
    • 1
    • 2
    • 3
    • 5
  • E. A. Belousova
    • 3
  • M. T. Krupenin
    • 4
  • T. V. Romanyuk
    • 2
    • 3
    • 5
  • A. V. Maslov
    • 4
  1. 1.Geological InstituteRussian Academy of SciencesMoscowRussia
  2. 2.Gubkin Russian State University of Oil and GasMoscowRussia
  3. 3.Australian Research Council Centre of Excellence for Core to Crust Fluid Systems, GEMOCMacquarie UniversitySydneyAustralia
  4. 4.Zavaritskii Institute of Geology and Geochemistry, Ural BranchRussian Academy of SciencesYekaterinburgRussia
  5. 5.Schmidt Institute of Physics of the EarthRussian Academy of SciencesMoscowRussia

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