Factors of Metamorphism

  • Helmut G. F. Winkler


Temperature and pressure are the physical factors that control the process of metamorphism. 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 H2O 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.


Metamorphic Rock Fluid Phase Equilibrium Temperature Oxygen Fugacity Load Pressure 
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  1. Brace, W. F., Ernst, W. G., and Kallberg, R. W. 1970. Geol. Soc. Am. Bull. 8: 1325–1338.CrossRefGoogle Scholar
  2. Clark, S. P. 1961. Am. J. Sci. 259: 641–650.CrossRefGoogle Scholar
  3. Correns, C. W. 1949. Einführung in die Mineralogie. Springer-Verlag, Berlin-Göttingen-Heidelberg.Google Scholar
  4. Dachille, F. and Roy, R. 1960. In J. H. Boer, et al., eds. Reactivity of Solids. Elsevier, Amsterdam.Google Scholar
  5. Dachille, F. and Roy, R.1964. J. Geol. 72: 243–247.CrossRefGoogle Scholar
  6. Dobretsov, N. L., et al. 1967. Geochem Intern. 4: 772–782.Google Scholar
  7. Ernst, W. G. 1971. Am. J. Sci. 270: 81–108.CrossRefGoogle Scholar
  8. Eugster, H. P. 1959. Reduction and oxidation in metamorphism. In P. H. Abelson, ed. Researches in Geochemistry. John Wiley & Sons, New York.Google Scholar
  9. Eugster, H. P. and Skippen, G. B. 1967. Igneous and metamorphic reactions involving gas equilibria. In P. H. Abelson, ed. Researches in Geochemistry. John Wiley & Sons, New York.Google Scholar
  10. Eugster, H. P. and Wones, D. R. 1962. J. Petrol. 3: 82ff.Google Scholar
  11. 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.Google Scholar
  12. French, B. M. 1966. Rev. Geophys. 4: 223–253.CrossRefGoogle Scholar
  13. Fyfe, W. S., Turner, F. J., and Verhoogen, J. 1958. Geol. Soc. Am. Memoir 73.Google Scholar
  14. Griggs, D. T. and Blasic, J. D. Science 147: 292–295.Google Scholar
  15. Heard, H. C. 1963. J. Geol. 71: 162–195.CrossRefGoogle Scholar
  16. Jäger, E. 1970. Fortschr. Mineral 47: 82.Google Scholar
  17. Rutland, R. W. R. 1965. Tectonic overpressure. In W. S. Pitscher and G. W. Flinn, eds. Controls of Metamorphism. pp. 119–139. Oliver and Boyd, Edinburgh and London.Google Scholar
  18. Thompson, J. B. 1955. Am. J. Sci. 253: 65–103.CrossRefGoogle Scholar
  19. Wones, D. R. and Gilbert, M. C. 1969, Am. J. Sci. 261A: 480ff.Google Scholar
  20. Yui, S. 1968. J. Mining Col. Akita Univ., Ser A. 4: 29–39.Google Scholar

Copyright information

© Springer-Verlag New York Inc. 1974

Authors and Affiliations

  • Helmut G. F. Winkler
    • 1
  1. 1.Institute of Mineralogy and PetrologyUniversity of GöttingenGermany

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