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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...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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The Royal Society Publishing
2021
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7898121/ https://www.ncbi.nlm.nih.gov/pubmed/33517873 http://dx.doi.org/10.1098/rsta.2019.0423 |