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Effects of Fluid Composition on Melting Phase Relationships: The Application of Korzhinskii’s Open Systems

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Physical Chemistry of Magmas

Part of the book series: Advances in Physical Geochemistry ((PHYSICAL GEOCHE,volume 9))

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Abstract

Melting phase relationships in the alumino-silicate systems are important in explaining the diversity and the regularity governing the formation of magmatic rocks. An important thing about these natural processes is that they take place against the background of the ever-changing external conditions. Therefore, to build a quantitative theory of these processes, it is imperative to know how the various factors (parameters) of the environment influence the crystal-liquid equilibria in the magmatic systems.

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Authors
  1. Aleksey D. Kuznetsov
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  2. Mark B. Epel’baum
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Editors and Affiliations

  1. Institute of Experimental Mineralogy, USSR Academy of Sciences, Moscow District, Chernogolovka, 142432, Russia

    Leonid L. Perchuk

  2. Geological Institute, Faculty of Science, University of Tokyo, Tokyo, 113, Japan

    Ikuo Kushiro

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Kuznetsov, A.D., Epel’baum, M.B. (1991). Effects of Fluid Composition on Melting Phase Relationships: The Application of Korzhinskii’s Open Systems. In: Perchuk, L.L., Kushiro, I. (eds) Physical Chemistry of Magmas. Advances in Physical Geochemistry, vol 9. Springer, New York, NY. https://doi.org/10.1007/978-1-4612-3128-8_11

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  • DOI: https://doi.org/10.1007/978-1-4612-3128-8_11

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