Springer Advances in Experimental and Genetic Mineralogy: Special Publication to 50th Anniversary of DS Korzhinskii Institute of Experimental Mineralogy of the Russian Academy of Sciences

Product Description This book presents fundamental experimental data and experiment-based theoretical conclusions on, as well as physico-chemical models of, the natural hydrothermal, metasomatic, metamorphic, magmatic and ore-producing processes in the Earth’s crust, upper mantle, transition zone and lower mantle. The topics discussed concern the interactions of oil and aqueous fluids as revealed by aqueous-hydrocarbonic inclusions in synthetic quartz and applied to the natural evolution of oil; determining the solubility and inter-phase partitioning of trace and strategic elements and their components; and experimentally validating physico-chemical mechanisms in the ultrabasic-basic evolution of deep-mantle magmatic and diamond-forming systems. In addition, the book presents experimental studies on the physico-chemical properties of supercritical water and hydrothermal fluids, viscosity of acidic ultramafic magmatic materials melts, peculiarities of metamorphism in basic rocks, kinetics of mineral nucleation in silicate melts and hydrothermal solutions, and influence of complex H2O-CO2-HCl fluids on melting relations in mantle-crust rocks, together with novel results and conclusions. Given its scope, the book will be of great interest to all Earth scientists, lecturers and students specialized in experimental and genetic mineralogy, petrology and geochemistry. From the Back Cover This book presents fundamental experimental data and experiment-based theoretical conclusions on, as well as physico-chemical models of, the natural hydrothermal, metasomatic, metamorphic, magmatic and ore-producing processes in the Earth’s crust, upper mantle, transition zone and lower mantle. The topics discussed concern the interactions of oil and aqueous fluids as revealed by aqueous-hydrocarbonic inclusions in synthetic quartz and applied to the natural evolution of oil; determining the solubility and inter-phase partitioning of trace and strategic elements and their components; and experimentally validating physico-chemical mechanisms in the ultrabasic-basic evolution of deep-mantle magmatic and diamond-forming systems. In addition, the book presents experimental studies on the physico-chemical properties of supercritical water and hydrothermal fluids, viscosity of acidic ultramafic magmatic materials melts, peculiarities of metamorphism in basic rocks, kinetics of mineral nucleation in silicate melts and hydrothermal solutions, and influence of complex H2O-CO2-HCl fluids on melting relations in mantle-crust rocks, together with novel results and conclusions. Given its scope, the book will be of great interest to all Earth scientists, lecturers and students specialized in experimental and genetic mineralogy, petrology and geochemistry. About the Author Oleg G. Safonov is Director of the Korzhinskii Institute of Experimental Mineralogy, Russian Academy of Sciences, Russia (since 2017), an Honored Young Professor of the Russian Academy of Science (since 2015), Professor at the Department of Petrology, Geological Faculty of Moscow State University, Russia, and Visiting Professor at the Department of Geology, University of Johannesburg, South Africa. Holding a Ph.D. (1997) and postdoctoral degree (2007) from Moscow State University, Prof. Safonov’s research and teaching focus on various fields of magmatic and metamorphic petrology, experimental petrology, mineralogy and geochemistry, mineral thermodynamics and geothermobarometry. His recent publications in peer-reviewed journals concern the petrology, geochemistry and geodynamics of Precambrian granulite complexes and cratons, fluid-rock-melt interaction during high-grade metamorphism, mantle magmatism and metasomatism. Using original experiments, Prof. Safonov has put forward a thermodynamic model for using potassium-bearing clinopyroxene to monitor potassium activity and pressure in the upper mantle, and has developed models for the evolution of alkaline chlorid