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Hf isotopes and trace elements as indicators of zircon genesis in the evolution of the alkaline-carbonatite magmatic system (Il’meno-Vishnevogorskii Complex, Urals, Russia)

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Authors and Affiliations

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

    I. L. Nedosekova

  2. GEMOC ARC National Key Centre, Macquarie University, Sydney, Australia

    E. A. Belousova

  3. Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, St. Petersburg, Russia

    B. V. Belyatsky

Authors
  1. I. L. Nedosekova
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  2. E. A. Belousova
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  3. B. V. Belyatsky
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Corresponding author

Correspondence to I. L. Nedosekova.

Additional information

Original Russian Text © I.L. Nedosekova, E.A. Belousova, B.V. Belyatsky, 2015, published in Doklady Akademii Nauk, 2015, Vol. 461, No. 5, pp. 569–574.

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Nedosekova, I.L., Belousova, E.A. & Belyatsky, B.V. Hf isotopes and trace elements as indicators of zircon genesis in the evolution of the alkaline-carbonatite magmatic system (Il’meno-Vishnevogorskii Complex, Urals, Russia). Dokl. Earth Sc. 461, 384–389 (2015). https://doi.org/10.1134/S1028334X1504011X

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  • DOI: https://doi.org/10.1134/S1028334X1504011X

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