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Anatexis, Formation of Migmatites, and Origin of Granitic Magmas

  • Helmut G. F. Winkler
Part of the Springer Study Edition book series (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.”

Keywords

Water Pressure Partial Melting Metamorphic Rock Granitic Rock Granitic Magma 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© Springer Science+Business Media New York 1979

Authors and Affiliations

  • Helmut G. F. Winkler
    • 1
  1. 1.Institute of Mineralogy and PetrologyUniversity of GöttingenFederal Republic of Germany

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