Annotation
Periodic temperature variations are accompanied bу а separation of the Earth's mantle into mineralogical fractions at temperatures below the solidus point of rock. А physical model is put forward for the formation of magmatic melts of different chemical compositions.
© 2016 Publisher M.V.Lomonosov Moscow State University
Authors
М.V. Avdulov
Chair of Physics of the Earth
Chair of Physics of the Earth
Science News of the Faculty of Physics, Lomonosov Moscow State University
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