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Metamorphe Gesteine

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Zusammenfassung

Unter Gesteinsmetamorphose versteht man die Summe aller Umwandlungen, 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 bei der konventionellen Metamorphose der feste Zustand im Wesentlichen erhalten bleibt, kann es bei hochgradiger Metamorphose zum teilweisen Aufschmelzen von Gesteinen kommen (partielle Anatexis). Mit der beginnenden Absonderung von Schmelze ist das Grenzgebiet zur Magmenbildung erreicht (Ultrametamorphose). Polymetamorphe Gesteinehaben mehrere verschiedene Metamorphoseakte erlebt.

†Deceased

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

    Dr. Martin Okrusch (Professor)

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Okrusch, M., Matthes †, S. (2010). Metamorphe Gesteine. In: Mineralogie. Springer-Lehrbuch. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-540-78201-8_24

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