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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...
| Autores principales: | , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2018
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| Materias: | |
| 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 |