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...
Published in: | Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences |
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Main Authors: | , , |
Other Authors: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
The Royal Society
2021
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Subjects: | |
Online Access: | http://dx.doi.org/10.1098/rsta.2019.0423 https://royalsocietypublishing.org/doi/pdf/10.1098/rsta.2019.0423 https://royalsocietypublishing.org/doi/full-xml/10.1098/rsta.2019.0423 |