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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Winkler, H.G.F. (1976). Anatexis, Formation of Migmatites, and Origin of Granitic Magmas. In: Petrogenesis of Metamorphic Rocks. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-22283-6_18
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DOI: https://doi.org/10.1007/978-3-662-22283-6_18
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