Ganguly, J. (1977) Compositional Variables and Chemical Equilibrium in Metamorphism. In Energetics of Geological Processes. Springer Berlin Heidelberg. p.250-284. doi:10.1007/978-3-642-86574-9_13
Reference Type | Book (chapter) | ||
---|---|---|---|
Title | Compositional Variables and Chemical Equilibrium in Metamorphism | ||
Book Title | Energetics of Geological Processes | ISBN | 9783642865763 |
Authors | Ganguly, J. | Author | |
Year | 1977 | ||
Page(s) | 250-284 | ||
Publisher | Springer Berlin Heidelberg | ||
DOI | doi:10.1007/978-3-642-86574-9_13Search in ResearchGate | ||
Mindat Ref. ID | 10445144 | Long-form Identifier | mindat:1:5:10445144:3 |
GUID | c2ebe682-7117-4f3c-b02c-45ec390b5600 | ||
Full Reference | Ganguly, J. (1977) Compositional Variables and Chemical Equilibrium in Metamorphism. In Energetics of Geological Processes. Springer Berlin Heidelberg. p.250-284. doi:10.1007/978-3-642-86574-9_13 | ||
Plain Text | Ganguly, J. (1977) Compositional Variables and Chemical Equilibrium in Metamorphism. In Energetics of Geological Processes. Springer Berlin Heidelberg. p.250-284. doi:10.1007/978-3-642-86574-9_13 | ||
In | (1977) Energetics of Geological Processes. Springer Berlin Heidelberg. doi:10.1007/978-3-642-86574-9 |
References Listed
These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.
Callen, H. B.: Thermodynamics. New York: Wiley, 1963. | |
Condie, K. C.: Oxygen, carbon dioxide, and sulfur fugacities during diagenesis and low-grade metamorphism of late precambrian subgraywackes from Northern Utah. Am. Mineral. 52, 1153–1160 (1967). | |
Eugster, H. P., Skippen, G. B.: Igneous and metamorphic reactions involving gas equilibria. In: Researches in geochemistry, vol. II, Abelson, P. H. (ed.). London-New York: Wiley (1967b), pp. 492–520. | |
Gordon, T. M., Greenwood, H. J.: Stability of grossularite in H2O-CO2 mixtures. Am. Mineral., 56, 1674–1688 (1971). | |
Greenwood, H. J.: Mineral equilibria in the system MgO-SiO2-H2O-CO2. In: Researches in geochemistry, Vol. II. Abelson, P. H. (ed.) London-New York: Wiley (1967b), pp. 542–547. | |
Greenwood, H. J.: AlIV-SiIV disorder in sillimanite and its effect on phase relations of the aluminum silicate minerals. Geol. Soc. Am. Mem. 132, 533–571 (1972). | |
Harte, B.: Displacement of the kyanite ‘isograd’ by the local variations of oxygen fugacity within pelitic schists in Glen Lethnot, Angus, Scotland. EOS Am. Geophys. Union 56, 466 (1975). | |
Hlabse, T., Kleppa, O. J.: The thermochemistry of jadeite. Am. Mineral. 53, 1281–1292 (1968). | |
Holdaway, M. J.: Effect of rock and fluid composition on chloritoid-staurolite equilibria, Picuris, New Mexico. Geol. Soc. Amer., Abstracts with Programs, 7, 1119 (1975). | |
Kerrick, D. M.: Review of metamorphic mixed volatile (H2O-CO2) equilibria. Am. Mineral. 59, 729–762 (1974). | |
Korzhinskii, D. S.: Physicochemical analysis of the paragenesis of minerals. Translation in English, Consultants Bureau, Inc. New York (1959). | |
Mueller, R. F.: Stability fbiolite: A discussion. Am. Mineral. 57, 300–316 (1972). | |
Prigogine, J., Defay, R.: Chemical Thermodynamics. London: Longmans, 1954. | |
Ramberg, H.: Patrologic significance of subsolidus phase transitions in mixed crystals. Norsk. Geol. Tidsskr. 24, 43–74 (1944). | |
Ramberg, H.: The Origin of Metamorphic and Metasomatic Rocks. Chicago: Univ. Chicago, 1952a. | |
Rosenberg, P. E.: Pyrophyllite solid solutions in the system Al2O3-SiO2-H22. Am. Mineral. 59, 254–260 (1974). | |
Rumble, D., III.: Gibbs phase rule and its application in geochemistry. J. Washington Acad. Sci. 64, 199–208 (1974). | |
Swalin, R. A.: Thermodynamics of Solids. New York-London: Wiley, 1962. | |
Thompson, J. B. Jr.: Local equilibrium in metasomatic processes. In: Researches in Geochemistry. Abelson, P. H. (ed), New York-London: Wiley, 1959, pp. 427–457. | |
Yui, S.: Results of equilibrium calculation on the reaction between graphite and a H2O-CO2 fluid at 300–500°C and 1000–2000 bars, and its implication to relict graphite in pyrometasomatic ore deposits. J. Mining College Akita Univ. Ser. A., 4, 29–39 (1968). |
See Also
These are possibly similar items as determined by title/reference text matching only.