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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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發(fā)表于 2025-3-21 16:46:34 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱High-Pressure Silicates and Oxides
副標(biāo)題Phase Transition and
編輯Masaki Akaogi
視頻videohttp://file.papertrans.cn/427/426710/426710.mp4
概述Presents a comprehensive overview of high-pressure phase transitions of silicates and oxides.Describes both high-pressure experimental methods and thermodynamic approaches for determination of phase r
叢書名稱Advances in Geological Science
圖書封面Titlebook: High-Pressure Silicates and Oxides; Phase Transition and Masaki Akaogi Book 2022 Springer Nature Singapore Pte Ltd. 2022 High pressure.High
描述.This book presents a summary of high-pressure phase transitions of minerals and related inorganic compounds. The first part reviews the methods to investigate phase transitions by direct high-pressure and high-temperature experiments together with thermodynamic approaches that consist of calorimetric measurements and thermodynamic calculation. In the second part, phase relations and thermodynamic properties of olivine, pyroxene, garnet, spinel, perovskite, rutile, and related inorganic compounds with A.2.BO.4., ABO.3., AB.2.O.4., and AO.2. stoichiometries are described. Particular emphasis is placed on spinel- and perovskite-structured phases and their high-pressure polymorphs called post-spinel and post-perovskite phases. The last part of the book focuses on phase relations of mantle rocks and on natural high-pressure minerals from the Earth’s deep mantle and in shocked meteorites.??.
出版日期Book 2022
關(guān)鍵詞High pressure; High temperature; Thermodynamics; Phase transition; Silicate and oxide minerals; Compositi
版次1
doihttps://doi.org/10.1007/978-981-19-6363-6
isbn_softcover978-981-19-6365-0
isbn_ebook978-981-19-6363-6Series ISSN 2524-3829 Series E-ISSN 2524-3837
issn_series 2524-3829
copyrightSpringer Nature Singapore Pte Ltd. 2022
The information of publication is updating

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沙發(fā)
發(fā)表于 2025-3-21 23:42:28 | 只看該作者
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.
板凳
發(fā)表于 2025-3-22 00:51:04 | 只看該作者
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.
地板
發(fā)表于 2025-3-22 06:17:03 | 只看該作者
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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發(fā)表于 2025-3-22 11:25:45 | 只看該作者
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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發(fā)表于 2025-3-22 14:02:05 | 只看該作者
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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發(fā)表于 2025-3-23 08:54:51 | 只看該作者
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.
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