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U-Pb isotope and REE composition of zircon from the pyroxene crystalline schists of the Irkut terrane, Sharyzhalgai Uplift: Evidence for the Neoarchean magmatic and metamorphic events

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Authors and Affiliations

  1. Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia

    O. M. Turkina & L. N. Urmantseva

  2. Center of Isotopic Research, Karpinskii All-Russia Geological Research Institute, Srednii pr. 74, St. Petersburg, 199026, Russia

    N. G. Berezhnaya & I. P. Paderin

  3. Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, nab. Makarova 2, St. Petersburg, 199034, Russia

    S. G. Skublov

Authors
  1. O. M. Turkina
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  2. N. G. Berezhnaya
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  3. L. N. Urmantseva
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  4. I. P. Paderin
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  5. S. G. Skublov
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Correspondence to O. M. Turkina.

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Original Russian Text © O.M. Turkina, N.G. Berezhnaya, L.N. Urmantseva, I.P. Paderin, S.G. Skublov, 2009, published in Doklady Akademii Nauk, 2009, Vol. 429, No. 4, pp. 527–533.

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Turkina, O.M., Berezhnaya, N.G., Urmantseva, L.N. et al. U-Pb isotope and REE composition of zircon from the pyroxene crystalline schists of the Irkut terrane, Sharyzhalgai Uplift: Evidence for the Neoarchean magmatic and metamorphic events. Dokl. Earth Sc. 429, 1505–1510 (2009). https://doi.org/10.1134/S1028334X09090207

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  • DOI: https://doi.org/10.1134/S1028334X09090207

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