Annotation
Separation of the Earth's mantle into mineralogical fractions at a temperature below the solidus point of the rock occurs with periodic changes in temperature under the effects of polymorphous transformations. Estimations of the influence of the Bjerknes forces and the force of radial pressure on the kinetics of the process are cited.
© 2016 Publisher M.V.Lomonosov Moscow State University
Authors
M.V. Avdulov
Department of Earth Physics, Faculty of Physics, Moscow State University, Leninskie Gory, Moscow, 119992, Russia
Department of Earth Physics, Faculty of Physics, Moscow State University, Leninskie Gory, Moscow, 119992, Russia
Science News of the Faculty of Physics, Lomonosov Moscow State University
This new information publication, which is intended to convey to the staff, students and graduate students, faculty colleagues and partners of the main achievements of scientists and scientific information on the events in the life of university physicists.