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Metamorphe Gesteine

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Zusammenfassung

Unter Gesteinsmetamorphose (von grch. μεταμóρϕωσις = Umwandlung) versteht man sämtliche Umwandlungsprozesse, mit denen ein Gestein auf Veränderungen der physikalisch-chemischen Bedingungen im Erdinnern, insbesondere von Druck und Temperatur, reagiert. Dabei entstehen aus magmatischen, sedimentären oder (bereits) metamorphen Ausgangsgesteinen neue, metamorphe Gesteine (Metamorphite), die sich in ihrem Gefüge, ihrem Mineralbestand, bisweilen sogar in ihrem Chemismus vom Ausgangsgestein unterscheiden. Während der Metamorphose bleibt der feste Zustand des Gesteins erhalten, obwohl gewöhnlich eine intergranulare fluide Phase vorhanden ist.

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Authors and Affiliations

  1. Institut für Geographie und Geologie, Universität Würzburg, Würzburg, Deutschland

    Martin Okrusch & Hartwig E. Frimmel

  2. Department of Geological Sciences, University of Cape Town, Rondebosch, Südafrika

    Hartwig E. Frimmel

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Okrusch, M., Frimmel, H.E. (2022). Metamorphe Gesteine. In: Mineralogie. Springer Spektrum, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-64064-7_26

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