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Geochemistry of Chromium in the Earth’s Mantle: Springer Geology

Autor Ekaterina A. Matrosova, Andrey V. Bobrov, Luca Bindi
en Limba Engleză Hardback – 11 sep 2019
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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Specificații

ISBN-13: 9783030270179
ISBN-10: 3030270173
Pagini: 128
Ilustrații: VIII, 128 p.
Dimensiuni: 155 x 235 mm
Greutate: 0.37 kg
Ediția:1st ed. 2020
Editura: Springer International Publishing
Colecția Springer
Seria Springer Geology

Locul publicării:Cham, Switzerland

Cuprins

Introduction.- Chromium and chromium-bearing phases in the Earth.- Experimental study of Cr-bearing phases at high pressures.- Implication of experimental results to geochemistry of Cr in the Earth’s mantle.

Textul de pe ultima copertă

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.


Caracteristici

Solves open problems in the geochemistry of the Earth’s mantle Broadens your understanding of the composition and structure of deep Earth interiors Summarizes the latest studies of high-pressure chromium-rich phases