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This book provides an analysis of an actual problem of the
evolution of deep matter under the conditions of the upper mantle,
transition zone, and uppermost lower mantle. This issue has a
fundamental importance in geochemistry, petrology, mineralogy, and
crystalochemistry of the mantle, at different depths. The authors
discuss new experimental research on the composition and conditions
of the chromium-bearing minerals genesis and their associations in
the Earth's mantle. The experimental data are compared with the
natural mineral assemblages, allowing a refinement of the structure
and composition of the deep Geospheres of the Earth. The results of
the physicochemical experiments in the "MgO-SiO2-Cr2O3" model and
the multicomponent systems play a major role in understanding the
phase diagrams of these systems, the structural patterns of
chromium-bearing phases and the influence of Cr on P-T parameters
in the Earth's mantle.
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