Quartz Grain Coarsening by Collective Crystallization in Contact Quartzites

  • G. Buntebarth
  • G. Voll

Abstract

Clastic minerals of the Appin Quartzite are: ca. 85 vol % quartz, ca. 15% alkali feldspars, heavy minerals (zircone, rutile — partly formed from titanomagnetite during diagenesis, and apatite and tourmaline as very rare exceptions.

Keywords

Crystallization Migration Quartz Zircone Hydration 

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Copyright information

© Springer-Verlag Berlin Heidelberg 1991

Authors and Affiliations

  • G. Buntebarth
  • G. Voll

There are no affiliations available

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