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Transition from carbonatitic magmas to hydrothermal brines: Continuous dilution or fluid exsolution?
Carbonatites are the most important primary sources for the rare earth elements (REEs). While fractional crystallization of carbonate minerals results in the enrichment of volatiles, alkalis, and REEs in the remaining melts, the transition from carbonatitic magmas to hydrothermal brines remains uncl...
| Autores principales: | , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
American Association for the Advancement of Science
2023
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10355818/ https://www.ncbi.nlm.nih.gov/pubmed/37467324 http://dx.doi.org/10.1126/sciadv.adh0458 |