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Anatexis, Formation of Migmatites, and Origin of Granitic Magmas

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Petrogenesis of Metamorphic Rocks
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Abstract

Metamorphic rocks of the higher-temperature range of the amphibolite facies are closely associated with 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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References

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Winkler, H.G.F. (1967). Anatexis, Formation of Migmatites, and Origin of Granitic Magmas. In: Petrogenesis of Metamorphic Rocks. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-00866-9_16

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  • DOI: https://doi.org/10.1007/978-3-662-00866-9_16

  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-540-04023-1

  • Online ISBN: 978-3-662-00866-9

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