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The Setting of the Ballachulish Intrusive Igneous Complex in the Scottish Highlands Read chapter Read first chapter

1991 | OriginalPaper | Chapter

Quartz Grain Coarsening by Collective Crystallization in Contact Quartzites

Authors : G. Buntebarth, G. Voll

Published in: Equilibrium and Kinetics in Contact Metamorphism

Publisher: Springer Berlin Heidelberg

Included in: Professional Book Archive

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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.

previous chapter Microtextures and Reaction Mechanisms of Carbonate Rocks: A Comparison Between the Thermoaureoles of Ballachulish and Monzoni (N. Italy)
next chapter Disordering, Re-Ordering and Unmixing in Alkali Feldspars from Contact-Metamorphosed Quartzites
Metadata
Title
Quartz Grain Coarsening by Collective Crystallization in Contact Quartzites
Authors
G. Buntebarth
G. Voll
Copyright Year
1991
Publisher
Springer Berlin Heidelberg
Book
Equilibrium and Kinetics in Contact Metamorphism

Print ISBN: 978-3-642-76147-8

Electronic ISBN: 978-3-642-76145-4

Copyright Year: 1991

DOI
https://doi.org/10.1007/978-3-642-76145-4_12