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Anatexis, Formation of Migmatites, and Origin of Granitic Magmas

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Petrogenesis of Metamorphic Rocks

Part of the book series: Springer Study Edition ((SSE))

Abstract

In metamorphic terrains, high-grade metamorphic rocks are spatially, and presumably genetically, related to migmatites. Read (1957) describes this general observation as follows: “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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Authors and Affiliations

  1. Institute of Mineralogy and Petrology, University of Göttingen, Federal Republic of Germany

    Helmut G. F. Winkler (Professor Emeritus)

Authors
  1. Helmut G. F. Winkler
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© 1979 Springer Science+Business Media New York

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Winkler, H.G.F. (1979). Anatexis, Formation of Migmatites, and Origin of Granitic Magmas. In: Petrogenesis of Metamorphic Rocks. Springer Study Edition. Springer, New York, NY. https://doi.org/10.1007/978-1-4757-4215-2_18

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  • DOI: https://doi.org/10.1007/978-1-4757-4215-2_18

  • Publisher Name: Springer, New York, NY

  • Print ISBN: 978-0-387-90413-9

  • Online ISBN: 978-1-4757-4215-2

  • eBook Packages: Springer Book Archive

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