Metamorphism of Marls

  • Kurt Bucher
  • Martin Frey


Marls are carbonate-bearing pelitic sediments covering a large range of comm position between “impure” carbonate rocks and “true” pelites. In the Anglo American literature, this group of sedimentary rocks is better known as argillaceous carbonate rocks, calcareous sediments, calcic pelitic rocks, or calcpelites.


Contrib Mineral Petrol White Mica Greenschist Facies Plagioclase Composition Prograde Metamorphism 
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 Berlin Heidelberg 1994

Authors and Affiliations

  • Kurt Bucher
    • 1
  • Martin Frey
    • 2
  1. 1.Mineralogisch-Petrographisches InstitutFreiburg im BreisgauGermany
  2. 2.Mineralogisch-Petrographisches InstitutBaselSwitzerland

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