Dehydration of metapelites during high-Pmetamorphism: The coupling between fluid sources and fluid sinks
Author:
Affiliation:
1. Department of Geological Sciences; University of Cape Town; Cape Town South Africa
2. Institute of Earth Sciences; University of Graz; Graz Austria
Publisher
Wiley
Subject
Geochemistry and Petrology,Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/jmg.12296/fullpdf
Reference63 articles.
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3. Using calculated chemical potential relationships to account for replacement of kyanite by symplecite in high pressure granulites;Baldwin;Journal of Metamorphic Geology,2015
4. Mineral hydrogen isotopes and water contents in ultrahigh-pressure metabasite and metagranite: Constraints on fluid flow during continental subduction-zone metamorphism;Chen;Chemical Geology,2011
5. Devolatilization-generated fluid pressure and deformation-propagated fluid flow during prograde regional metamorphism;Connolly;Journal of Geophysical Research,1997
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