Titlebook: Kinetics and Equilibrium in Mineral Reactions; Surendra K. Saxena Book 1983 Springer Science+Business Media New York 1983 Chemische Reakti

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Geospeedometry: An Extension of Geothermometry,ermal history, we have relied on an understanding of thermodynamics and phase equilibria. The assumption is made that the various minerals and their chemical compositions measured today will reveal a temperature and pressure which are geologically significant. This procedure is quite valid if equili

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Mg-Fe Fractionation in Metamorphic Environments, phase. Walther and Orville (1982) believe that.Whichever is the case, this fluid is the principal transport medium for chemical exchanges between reactants and product minerals. The composition of this fluid must be known in order to define concentration gradients and calculate mass balance conditi

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Geobarometry in Granulites, detailed knowledge of metamorphic pressure is essential to the accurate formulation of any tectonic model attempting to incorporate metamorphic pressure—temperature—time relationships. There is, therefore, a need for pressure data of greater accuracy and precision than has been available. Of greate

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The Cordierite-Garnet-Sillimanite-Quartz Equilibrium: Experiments and Applications,t aureoles. Since Korzhinskii (1936) considered it as a potential indicator of metamorphic conditions, this assemblage has been of great interest to petrologists. Qualitative thermodynamic analysis by Marakushev (1965) showed that Cor + Gr + Sil + Qz paragenesis could be treated as divariant assembl

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Thermodynamics of Complex Phases,relations does not seem to have the same impetus. This is unfortunate because smoothing and interpolation/extrapolation of thermodynamic data can only be accomplished satisfactorily using thermodynamics.

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Timothy P. Loomiss interest among both practical reasoners and logical theorists. It is not clear why this is so: perhaps it is because the truth shines more brilliantly than error and hence needs less display to prevail and flourish than error does in order to be avoided. I am inclined to think that a fundamental r

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