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Metamorphism of Mafic Rocks

  • Helmut G. F. Winkler

Abstract

Basalts and pyroxene-andesites comprise by far the largest amount of mafic rocks and greatly predominate over their plutonic equivalents. Basalts and andesites are widespread in most geosynclines in the forms of lava flows, pillow lavas, tuff layers, sills, and dykes. At least three fundamentally different cases of metamorphism of mafic igneous rocks must be distinguished:
  1. a.

    Water has had access to the rock.

     
  2. b.

    Water has not had access and load pressure was not very high.

     
  3. c.

    Water has not had access but load pressure was very high.

     

Keywords

Metamorphic Rock Mafic Rock Geothermal Gradient White Mica Metamorphic Zone 
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-Verlag New York Inc. 1974

Authors and Affiliations

  • Helmut G. F. Winkler
    • 1
  1. 1.Institute of Mineralogy and PetrologyUniversity of GöttingenGermany

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