Abstract
Temperature and pressure are the physical factors that control the process of mnetamorphism. Metamorphism, in general, refers to the reactions between neighboring minerals of a rock in response to conditions of temperature and pressure prevailing at depth. A certain mineral paragenesis, formed at some given temperature and pressure, becomes unstable if subjected to different conditions; the minerals react to form a new paragenesis in equilibrium at the new conditions. If carbonates and H2O- or OH-bearing minerals take part in the reaction, CO2 and H20 are liberated. The higher the temperature of metamorphism, the smaller the amount of CO2 and H2O combined in the stable minerals. Therefore, a fluid phase composed of volatile constituents is always present during metamorphism of such rocks.
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References
Brace, W. F., Ernst, W. G., and Kallberg, R. W. 1970. Geol. Soc. Am. Bull. 81: 1325–1338.
Carmichael, D. M. 1978. Am. J. Sci. 278: 769–797.
Clark, S. P. 1961. Am. J. Sci. 259: 641–650.
Correns, C. W. 1949. Einfauuhrung in die Mineralogie. Springer-Verlag, BerlinGöttingen-Heidelberg.
Dachille, F. and Roy, R. 1960. In J. H. de Boer, et al., eds. Reactivity of Solids. Elsevier, Amsterdam.
Dachille, F. and Roy, R. 1964. J. Geol. 72: 243–247.
Dobretsov, N. L., et al. 1967. Geochem Intern. 4: 772–782.
Ernst, W. G. 1971. Am. J. Sci. 270: 81–108.
Eugster, H. P. 1959. Reduction and oxidation in metamorphism. In P. H. Abelson, ed. Researches in Geochemistry. John Wiley & Sons, New York.
Eugster, H. P. and Skippen, G. B. 1967. Igneous and metamorphic reactions involving gas equilibria. In P. H. Abelson, ed. Researches in Geochemistry, Vol. 2. John Wiley & Sons, New York.
Eugster, H. P. and Wones, D. R. 1962. J. Petrol. 3: 82ff.
Flinn, D. 1965. Deformation in metamorphism. In W. S. Pitscher and W. G. Flinn, eds. Controls of Metamorphism. pp. 46–72. Oliver and Boyd, Edinburgh and London.
French, B. M. 1966. Rev. Geophys. 4: 223–253.
Fyfe, W. S., Turner, F. J., and Verhoogen, J. 1958. Geol. Soc. Am. Memoir 73.
Griggs, D. T. and Blasic, J. D. Science 147: 292–295.
Heard, H. C. 1963. J. Geol. 71: 162–195.
Heard, H. C. and Raleigh, C. B. 1972. Geol. Soc. Amer. Bull. 83: 935–956.
Jäger, E.. 1970. Fortschr. Mineral. 47: 82.
Jäger, E.. 1973. Eclogae geol. Helv. 66: 11–21.
Pitcher, W. S. and Berger, A. R. 1972. The Geology of Donegal. 435 pp., WileyInterscience, New York.
Ronov, A. B., Migdisov, A. A., and Lobach-Zhuchenko, S. B. 1977. Geochem. Int. 14: 90–112.
Rutland, R. W. R. 1965. Tectonic overpressure, In W. S. Pitcher and G. W. Flinn, eds. Controls of Metamorphism. pp. 119–139. Oliver and Boyd, Edinburgh and London.
Thompson, J. B. 1955. Am. J. Sci. 253: 65–103.
Wones, D. R. and Gilbert, M. C. 1969. Am. J. Sci. 267A: 480ff.
Yui, S. 1968. J. Mining Col. Akita Univ., Ser A. 4: 29–39.
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Winkler, H.G.F. (1979). Factors of Metamorphism. In: Petrogenesis of Metamorphic Rocks. Springer Study Edition. Springer, New York, NY. https://doi.org/10.1007/978-1-4757-4215-2_3
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DOI: https://doi.org/10.1007/978-1-4757-4215-2_3
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