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...

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Detalles Bibliográficos
Autores principales: Yuan, Xueyin, Zhong, Richen, Xiong, Xin, Gao, Jing, Ma, Yubo
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2023
Materias:
Earth, Environmental, Ecological, and Space Sciences
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

Internet

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

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