An Eocene/Oligocene blueschist-/greenschist facies P-T loop from the Cycladic Blueschist Unit on Naxos Island, Greece: Deformation-related re-equilibration vs . thermal relaxation
Author:
Affiliation:
1. Department of Geological Sciences; Stockholm University; Stockholm Sweden
2. Deutsches GeoForschungsZentrum; GFZ; Telegrafenberg Potsdam Germany
Funder
Vetenskapsrådet
Publisher
Wiley
Subject
Geochemistry and Petrology,Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/jmg.12256/fullpdf
Reference66 articles.
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3. Low angle faults underneath and above a blueschist belt - Tinos Island, Cyclades, Greece;Avigad;Terra Nova,1989
4. Isotopic and petrological evidence for the infiltration of water-rich fluids during the Miocene M2 metamorphism on Naxos, Greece;Baker;Geochimica et Cosmochimica Acta,1989
5. An integrated zircon geochronological and geochemical investigation into the Miocene plutonic evolution of the Cyclades, Aegean Sea, Greece: Part 1 - Geochronology;Bolhar;Contributions to Mineralogy and Petrology,2010
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