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Initial H2O content and conditions of parent magma origin for Gorely volcano (Southern Kamchatka) estimated by trace element thermobarometry

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Abstract

The formation conditions of the parental magmas of Gorely volcano, which is located behind a volcanic front in Southern Kamchatka, have been evaluated using the modern methods of micro-element thermobarometry. These magmas contained 1.7 ± 0.8 (2σ) wt % of H2O, the majority (82%) of which has been lost from inclusions. They crystallized at 1121 ± 17°C and an oxygen fugacity of ΔQFM 1.2 ± 0.2, and could have been produced by about 11% melting of an enriched MORB source (E–DMM) at a temperature of about 1270°C, and a pressure of about 1.5 GPa. A distinctive feature of Gorely volcano, compared with frontal volcanoes of Kamchatka, is the unusually high temperature (925 ± 20°C) of formation of the subduction component corresponding to the region of existence of water-bearing melts.

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Authors and Affiliations

  1. Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, Moscow, 119991, Russia

    D. P. Nazarova, M. V. Portnyagin, S. P. Krasheninnikov, N. L. Mironov & A. V. Sobolev

  2. GEOMAR Helmholtz Centre for Ocean Research, Kiel, Germany

    M. V. Portnyagin

  3. Université Grenoble Alpes, Institute Science De la Terre (ISTerre), Grenoble, France

    A. V. Sobolev

Authors
  1. D. P. Nazarova
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  2. M. V. Portnyagin
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  3. S. P. Krasheninnikov
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  4. N. L. Mironov
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  5. A. V. Sobolev
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Correspondence to D. P. Nazarova.

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Original Russian Text © D.P. Nazarova, M.V. Portnyagin, S.P. Krasheninnikov, N.L. Mironov, A.V. Sobolev, 2017, published in Doklady Akademii Nauk, 2017, Vol. 472, No. 3, pp. 311–314.

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Nazarova, D.P., Portnyagin, M.V., Krasheninnikov, S.P. et al. Initial H2O content and conditions of parent magma origin for Gorely volcano (Southern Kamchatka) estimated by trace element thermobarometry. Dokl. Earth Sc. 472, 100–103 (2017). https://doi.org/10.1134/S1028334X1701024X

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  • DOI: https://doi.org/10.1134/S1028334X1701024X

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