Zusammenfassung
Metamorphe Gesteine der hochgradigen Amphibolitfazies sind eng vergesellschaftet mit Migmatiten. Diese generelle Geländebeobachtung beschreibt READ (1957) folgendermaßen: „One of the most firmly established facts in metamorphic geology is the close association in the field of highest-grade metamorphic rocks and migmatites“.
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Literatur
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Winkler, H.G.F. (1965). Anatexis, Migmatitbildung und Palingenese granitischer Magmen. In: Die Genese der metamorphen Gesteine. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-29030-9_16
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DOI: https://doi.org/10.1007/978-3-662-29030-9_16
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