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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

Quartz Vein Heavy Mineral Subgrain Boundary Regional Metamorphism Cylindrical Model 
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 1991

Authors and Affiliations

  • G. Buntebarth
  • G. Voll

There are no affiliations available

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