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Late mesozoic adakite volcanism of the Ugan volcanic structure (Southeastern Margin of the North Asian Craton): 40Ar/39Ar geochronological and geochemical evidence

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Authors and Affiliations

  1. Institute of Geology and Nature Management, Far East Branch, Russian Academy of Sciences, per. Relochnyi 1, Blagoveshchensk, 675000, Russia

    A. A. Sorokin & A. P. Sorokin

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

    V. A. Ponomarchuk & A. V. Travin

  3. Far East Geological Institute (DVGI), Far East Branch, Russian Academy of Sciences, pr. Stoletiya Vladivostoka 159, Vladivostok, 660022, Russia

    Yu. A. Martynov

  4. Institute of Precambrian Geology and Geochronology (IGGD), Russian Academy of Sciences, nab. Makarova 2, St. Petersburg, 199034, Russia

    A. M. Larin

Authors
  1. A. A. Sorokin
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  2. A. P. Sorokin
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  3. V. A. Ponomarchuk
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  4. Yu. A. Martynov
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  5. A. M. Larin
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  6. A. V. Travin
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Additional information

Original Russian Text © A.A. Sorokin, A.P. Sorokin, V.A. Ponomarchuk, Yu.A. Martynov, A.M. Larin, A.V. Travin, 2012, published in Doklady Akademii Nauk, 2012, Vol. 445, No. 4, pp. 445–449.

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Sorokin, A.A., Sorokin, A.P., Ponomarchuk, V.A. et al. Late mesozoic adakite volcanism of the Ugan volcanic structure (Southeastern Margin of the North Asian Craton): 40Ar/39Ar geochronological and geochemical evidence. Dokl. Earth Sc. 445, 947–950 (2012). https://doi.org/10.1134/S1028334X12080089

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  • DOI: https://doi.org/10.1134/S1028334X12080089

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