Carbonate complexation enhances hydrothermal transport of rare earth elements in alkaline fluids
Rare earth elements (REE), essential metals for the transition to a zero-emission economy, are mostly extracted from REE-fluorcarbonate minerals in deposits associated with carbonatitic and/or peralkaline magmatism. While the role of high-temperature fluids (100
| Verfasser: | |
|---|---|
| Dokumenttypen: | Artikel |
| Medientypen: | Text |
| Erscheinungsdatum: | 2022 |
| Publikation in MIAMI: | 05.09.2023 |
| Datum der letzten Änderung: | 05.09.2023 |
| Angaben zur Ausgabe: | [Electronic ed.] |
| Quelle: | Nature Communications 13 (2022), 1456, 1-11 |
| Schlagwörter: | Geochemistry; Petrology |
| Fachgebiet (DDC): | 550: Geowissenschaften, Geologie |
| Lizenz: | CC BY 4.0 |
| Sprache: | English |
| Förderung: | Finanziert über die DEAL-Vereinbarung mit Wiley 2019-2022. |
| Format: | PDF-Dokument |
| URN: | urn:nbn:de:hbz:6-29928497237 |
| Weitere Identifikatoren: | DOI: 10.17879/69928556849 |
| Permalink: | https://nbn-resolving.de/urn:nbn:de:hbz:6-29928497237 |
| Verwandte Dokumente: |
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| Onlinezugriff: | 10.1038_s41467-022-28943-z.pdf |
Rare earth elements (REE), essential metals for the transition to a zero-emission economy, are mostly extracted from REE-fluorcarbonate minerals in deposits associated with carbonatitic and/or peralkaline magmatism. While the role of high-temperature fluids (100