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On the dynamics of the rhythmic crystallization of magmatic bodies during the directional solidification of cotectic melts

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Abstract

A problem on the directional crystallization of melt was solved taking into account heat and mass exchange between the two-phase zone and the cooling volume of a magmatic body. Conditions were determined for the development of rhythmic crystallization by the example of the solidification of the pseudobinary Di-An system.

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Authors and Affiliations

  1. Khristianovich Institute of Theoretical and Applied Mechanics, Siberian Branch, Russian Academy of Sciences, ul. Institutskaya 4/3, Novosibirsk, 630090, Russia

    V. K. Cherepanova & A. N. Cherepanov

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

    V. N. Sharapov

  3. Novosibirsk State Pedagogical University, ul Vilyuiskaya 28, Novosibirsk, 630126, Russia

    S. I. Plaksin

Authors
  1. V. K. Cherepanova
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  2. A. N. Cherepanov
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  3. V. N. Sharapov
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  4. S. I. Plaksin
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Correspondence to V. K. Cherepanova.

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Original Russian Text © V.K. Cherepanova, A.N. Cherepanov, V.N. Sharapov, S.I. Plaksin, 2009, published in Geokhimiya, 2009, No. 5, pp. 481–489.

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Cherepanova, V.K., Cherepanov, A.N., Sharapov, V.N. et al. On the dynamics of the rhythmic crystallization of magmatic bodies during the directional solidification of cotectic melts. Geochem. Int. 47, 454–462 (2009). https://doi.org/10.1134/S0016702909050024

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