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Titlebook: Advances in Physical Geochemistry; Surendra K. Saxena Book 1982 Springer Science+Business Media New York 1982 Geochemie.Mineral.geochemist

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期刊全稱Advances in Physical Geochemistry
影響因子2023Surendra K. Saxena
視頻videohttp://file.papertrans.cn/150/149381/149381.mp4
學(xué)科分類Advances in Physical Geochemistry
圖書封面Titlebook: Advances in Physical Geochemistry;  Surendra K. Saxena Book 1982 Springer Science+Business Media New York 1982 Geochemie.Mineral.geochemist
影響因子The second volume of this series consists of three parts. Part I focuses on the research on intracrystalline reactions. This work, which began nearly two decades ago, is critically reviewed by Ghose and Ganguly in Chapter 1. Besides the review, the authors include some of their previously unpublished work to demonstrate how future research could aid in obtaining data on thermodynamics of solid solutions and in understanding the cooling history of igneous and metamorphic rocks. The latter is also the theme adopted by Kretz in the second chapter, which examines the redistribution of Fe and Mg in coexisting silicates during cooling. Chapter 3 contains new data on Fe-Mg distribution in clinopyroxenes. Dal Negro and his co-authors have selected a series of clinopyroxenes from volcanic rocks and present site occupancy data on several clinopyroxenes of intermediate compositions. The data set has not been published before and is the first of its kind. Part II of this book begins with a chapteron melts by Gaskell, who explores the relationship between density and structure of silicate melts. This is followed by the synthesis of data generated in the U.S.S.R. by Shmulovich and his co-authors
Pindex Book 1982
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Daniel Kossmann,Donald Kossmanne orientation, structure, and composition of exsolution lamellae in several igneous and metamorphic pyroxene crystals have been investigated by optical microscopy, X-ray diffraction, electron probe analysis, transmission electron microscopy, and analytical electron microscopy. One might suppose, the
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The K-Method in Other Industriestions have been conducted over the past decade in the laboratory of hydrothermal systems at the Institute of Experimental Mineralogy, USSR Academy of Sciences. Scientists have long been interested in hydrothermal solutions due to their importance in the formation of many ore bodies and of virtually
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https://doi.org/10.1007/978-3-642-32817-6cally important substances. It is, therefore, appropriate to consider suitable techniques of calculating multicomponent phase equilibria. Geochemists and petrologists are familiar with the method of equilibrium constants used in the calculation of equilibrium pressure and temperature for single or m
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àngels Massip-Bonet,Albert Bastardas-Boada the use of aluminum in the elimination of colloids and organic matter through flocculation and in other water treatment processes, and to improve the general analytical chemistry of aluminum and the processes for commercial aluminum extraction. Schoen and Roberson (1970) have stated that “our princ
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