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Foidite and Meimechite Lavas of Polar Siberia (Some Questions of Petrogenesis)

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Abstract

For the Permian–Triassic foidite and meimechite lavas of Polar Siberia, both the whole-rock petrochemistry and geochemistry and that of melt inclusions in olivine phenocrysts from the same rocks have been demonstrated to be similar. In addition, their isotope characteristics imply the possibility of their generation from an abyssal parental melt compositionally resembling a high–Mg alkaline picrite.

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Authors and Affiliations

  1. Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russia

    Yu. R. Vasil’ev, M. P. Gora & D. V. Kuzmin

  2. Novosibirsk State University, Novosibirsk, Russia

    Yu. R. Vasil’ev & D. V. Kuzmin

Authors
  1. Yu. R. Vasil’ev
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  2. M. P. Gora
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  3. D. V. Kuzmin
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Correspondence to Yu. R. Vasil’ev.

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Original Russian Text © Yu.R. Vasil’ev, M.P. Gora, D.V. Kuzmin, 2018, published in Doklady Akademii Nauk, 2018, Vol. 478, No. 3, pp. 323–327.

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Vasil’ev, Y.R., Gora, M.P. & Kuzmin, D.V. Foidite and Meimechite Lavas of Polar Siberia (Some Questions of Petrogenesis). Dokl. Earth Sc. 478, 103–107 (2018). https://doi.org/10.1134/S1028334X18010282

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  • DOI: https://doi.org/10.1134/S1028334X18010282

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