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Neoproterozoic granitoids on Wrangel Island

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Abstract

Based on geochronological U–Pb studies, the age of Wrangel Island granitoids was estimated as Neoproterozoic (Cryogenian). Some granitoids contain zircons with inherited cores with an estimated age of 1010, 1170, 1200, and >2600 Ma, assuming the presence of ancient (Neoarchean–Mesoproterozoic) rocks in the Wrangel Island foundation and their involvement in partial melting under granitoid magma formation.

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Authors and Affiliations

  1. Geological Institute, Russian Academy of Sciences, Pyzhevskii per. 7, Moscow, 109017, Russia

    M. V. Luchitskaya, S. D. Sokolov & M. I. Tuchkova

  2. Karpinskii Russian Geological Research Institute, Russian Academy of Sciences, Sredny pr. 74, St. Petersburg, 191126, Russia

    S. A. Sergeev

  3. Institute of Earth Sciences, St. Petersburg State University, Universitetskaya nab. 7–9, St. Petersburg, 199034, Russia

    S. A. Sergeev

Authors
  1. M. V. Luchitskaya
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  2. S. A. Sergeev
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  3. S. D. Sokolov
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  4. M. I. Tuchkova
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Correspondence to M. V. Luchitskaya.

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Original Russian Text © M.V. Luchitskaya, S.A. Sergeev, S.D. Sokolov, M.I. Tuchkova, 2016, published in Doklady Akademii Nauk, 2016, Vol. 469, No. 2, pp. 195–198.

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Luchitskaya, M.V., Sergeev, S.A., Sokolov, S.D. et al. Neoproterozoic granitoids on Wrangel Island. Dokl. Earth Sc. 469, 652–655 (2016). https://doi.org/10.1134/S1028334X16070126

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  • DOI: https://doi.org/10.1134/S1028334X16070126

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