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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

Crossref DOI link: https://doi.org/10.1186/s00015-024-00476-1

Published Online: 2025-02-06

Published Print: 2025-12

Update policy: https://doi.org/10.1007/springer_crossmark_policy

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