Pristine microstructures in pseudotachylytes formed in dry lower crust, Lofoten, Norway

Feldspar-rich pseudotachylytes from the island of Moskenesøya, Lofoten, formed in dry granulites under lower crustal conditions during the Caledonian orogeny. The central parts of the pseudotachylytes, where the cooling rates were slowest, are characterized by microlites and spherulites of plagiocla...

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Bibliographic Details
Main Authors: Dunkel, Kristina G., Morales, Luiz F.G., Jamtveit, Bjørn
Format: Article in Journal/Newspaper
Language:English
Published: Royal Society 2021
Subjects:
Online Access:https://hdl.handle.net/20.500.11850/470677
https://doi.org/10.3929/ethz-b-000470677