Immiscible hydrous Fe–Ca–P melt and the origin of iron oxide-apatite ore deposits

The origin of iron oxide-apatite deposits is controversial. Silicate liquid immiscibility and separation of an iron-rich melt has been invoked, but Fe–Ca–P-rich and Si-poor melts similar in composition to the ore have never been observed in natural or synthetic magmatic systems. Here we report exper...

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Detalles Bibliográficos
Autores principales: Hou, Tong, Charlier, Bernard, Holtz, François, Veksler, Ilya, Zhang, Zhaochong, Thomas, Rainer, Namur, Olivier
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5897329/
https://www.ncbi.nlm.nih.gov/pubmed/29650951
http://dx.doi.org/10.1038/s41467-018-03761-4

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5897329/
https://www.ncbi.nlm.nih.gov/pubmed/29650951
http://dx.doi.org/10.1038/s41467-018-03761-4

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