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Die Bildung von Pyrophyllit und Andalusit zwischen 2000 und 7000 Bar H2O-Druck

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  • Kristallographie und Mineralogie
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Literatur

  1. Aramaki, S., u.R. Roy: Am. Mineralogist48, 1322–1347 (1963).

    Google Scholar 

  2. Carr, R.M., u.W.S. Fyfe: Geochim. et Cosmochim. Acta21, 99–109 (1960).

    Google Scholar 

  3. Carr, R.M.: Geochim. et Cosmochim. Acta27, 133–135 (1963).

    Google Scholar 

  4. Roy, R., u.E.F. Osborn: Am. Mineralogist39, 853–885 (1954).

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  5. Winkler, H.G.F.: Die Genese der metamorphen Gesteine. Berlin-Heidelberg-New York: Springer 1965.

    Google Scholar 

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Authors and Affiliations

  1. Mineralogisch-Petrologisches Institut der Universität, Göttingen

    Egon Althaus

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  1. Egon Althaus
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Althaus, E. Die Bildung von Pyrophyllit und Andalusit zwischen 2000 und 7000 Bar H2O-Druck. Naturwissenschaften 53, 105–106 (1966). https://doi.org/10.1007/BF00601471

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  • DOI: https://doi.org/10.1007/BF00601471

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