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Mineralogie pp 425–450Cite as

Phasengleichgewichte und Mineralreaktionen in metamorphen Gesteinen

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Zusammenfassung

Wie wir im vorausgehenden Kapitel gezeigt hatten, führt die Gesteinsmetamorphose zu tiefgreifenden Veränderungen im Gefüge und im Mineralbestand von Gesteinen. Durch prograde und retrograde Mineralreaktionen entstehen neue Mineralgesellschaften, die eine schrittweise Anpassung an die sich verändernden P-T-Bedingungen dokumentieren. Dabei kann – zumindest beim Höhepunkt der Metamorphose – ein thermodynamisches Gleichgewicht erreicht oder annähernd erreicht werden, so dass man von Gleichgewichtsparagenesen sprechen kann. Im folgenden Kapitel wollen wir wichtige Mineralreaktionen und die dabei entstehenden Paragenesen näher kennenlernen. Darüber hinaus sollen die Methoden diskutiert werden, mit denen man die Stabilitätsbedingungen metamorpher Paragenesen quantitativ abschätzen kann.

†Deceased

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Authors and Affiliations

  1. Lehrstuhl für Geodynamik und Geomaterialforschung Universität Würzburg, Am Hubland, 97074, Würzburg, Germany

    Dr. Martin Okrusch (Professor)

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  1. Dr. Martin Okrusch
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  2. Dr. Siegfried Matthes †
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Okrusch, M., Matthes †, S. (2010). Phasengleichgewichte und Mineralreaktionen in metamorphen Gesteinen. In: Mineralogie. Springer-Lehrbuch. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-540-78201-8_25

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