Titlebook: Applied Mineralogical Thermodynamics; Selected Topics Niranjan D. Chatterjee Textbook 1991 Springer-Verlag Berlin Heidelberg 1991 Kristallc

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,L?ndergruppen und Entwicklungspfade,t thermodynamic database, which is indispensable for obtaining a geologically reliable phase diagram. However, the computation of the phase relations involving crystalline solutions, a topic of fundamental interest to geology, must be deferred until the thermodynamics of crystalline solutions is introduced in Chapter 8.

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https://doi.org/10.1007/978-3-322-93473-4multicomponent systems (Chap. 9). The objective of this chapter is to calculate phase relations between mineral end-members and a pure fluid, such as water or oxygen. Other fluids will be amenable to treatment in an analogous manner.

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Phase Relations among End-Member Solids,t thermodynamic database, which is indispensable for obtaining a geologically reliable phase diagram. However, the computation of the phase relations involving crystalline solutions, a topic of fundamental interest to geology, must be deferred until the thermodynamics of crystalline solutions is introduced in Chapter 8.

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https://doi.org/10.1007/978-3-642-77665-6e of the fluid mixtures of relevance to geochemistry has been a centerpiece of activity for about a decade (Holloway 1977; Jacobs and Kerrick 1981a,b; Kerrick and Jacobs 1981; Bowers and Helgeson 1983; Saxena and Fei 1988). The availability of these data has promoted our ability to predict mixed-volatile reactions with confidence.

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Konzepte fuzzybasierter Leitkomponenten,es in those three chapters will reveal to us the perils of depending exclusively on such data, and urge us to develop the internally consistent thermodynamic database, which is achieved by a simultaneous treatment of the calorimetric . phase equilibria measurements. One of the methods of deriving in

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