Titlebook: High-Pressure Silicates and Oxides; Phase Transition and Masaki Akaogi Book 2022 Springer Nature Singapore Pte Ltd. 2022 High pressure.High

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书目名称High-Pressure Silicates and Oxides影响因子(影响力)




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Introduction,dition, high-pressure and high-temperature experiments are widely used to invent new functional materials for industrial use. Mineral names, including those of high-pressure minerals described in the following chapters, are summarized in the final section.

Eulogy

Post-perovskite Transition in , and Phase Transitions in ,O,n studied at high pressures as analogue materials to examine high-pressure transitions of SiO. stishovite. This chapter is focused on the phase relations and crystal-chemical characteristics of .X. post-perovskites and high-pressure .O. phases.

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Phase Transitions in Mantle Rocks,ty differences lead to the subduction or stagnation of basaltic crust and harzburgite in the transition zone and the lower mantle. In addition, phase transitions in subducted continental crust materials are described. The post-perovskite transition in the lowermost mantle is discussed in the final section.

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Crystal Chemistry and Thermodynamics of High-Pressure Phase Transition,essure phases are expressed in terms of chemical thermodynamics. Calculation methods of phase equilibria in simple systems at high pressure and high temperature are shown in the thermodynamic framework for applications in mantle minerals.

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High-Pressure and High-Temperature Experiments with Large-Volume Apparatus,s for measurements of various physical and chemical properties. Experimental techniques for generation of high pressure and high temperature, accurate pressure determination and temperature measurement, etc., are discussed for quenching experiments and in situ synchrotron X-ray diffraction experiments that involve large-volume apparatus.

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Phase Transitions of Pyroxene and Garnet, and Post-spinel Transition Forming Perovskite,onsible for the 660-km seismic discontinuity. This chapter is concerned with high-pressure experimental and thermodynamic studies on these phase transitions, which lead to the formation of perovskite-type silicate phases.