Fluorine-rich hydrogarnet, prehnite and pumpellyite in monzodioritic basement of the Rhine Rift Valley produced by in-situ low-grade metamorphism at 200 °C and 5 km depth
Abstract The Basel-1 geothermal deep well has been drilled in 2006 to a final depth of 5 km. The recovered core material from 4.9 km depth shows coarse grained biotite-hornblende quartz-monzodiorite from the Variscan basement. The primary igneous rock is locally altered and contains prehnite, pumpel...
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| Autori principali: | , , , |
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| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
Pensoft Publishers
2025-02-01
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| Serie: | Swiss Journal of Geosciences |
| Soggetti: | |
| Accesso online: | https://doi.org/10.1186/s00015-024-00476-1 |
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