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2010 | OriginalPaper | Chapter

3. Quartzofeldspathic Rocks

Author : Rodney Grapes

Published in: Pyrometamorphism

Publisher: Springer Berlin Heidelberg

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Abstract

Pyrometamorphosed quartzofeldspathic rocks (sandstone, shale, claystone) and sediments (sand-silt, clay, glacial till, diatomaceous earth), and their metamorphosed equivalents (phyllite, schist, gneiss), are characterised by the presence of tridymite, mullite/sillimanite, cordierite, orthopyroxene, clinopyroxene, sanidine-anorthoclase, plagioclase (oligoclase–anorthite), corundum, hercynite-rich spinel, magnetite, ilmenite, hematite, pseudobrookite, sulphides and in carbonaceous protoliths, native metals. Ti-rich biotite and osumilite are less common; sapphirine is rare. These minerals are usually associated with acidic (rhyolitic) to intermediate (dacitic) glass that is frequently abundant enough for the rocks to be termed buchites and paralavas. Partly melted granite-granodiorite may contain tridymite, Ca-plagioclase, orthopyroxene and magnetite.

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Title: Quartzofeldspathic Rocks
Author: Rodney Grapes
Publisher: Springer Berlin Heidelberg
Book: Pyrometamorphism
Print ISBN: 978-3-642-15587-1

Electronic ISBN: 978-3-642-15588-8

Copyright Year: 2010
DOI: https://doi.org/10.1007/978-3-642-15588-8_3