Immiscible hydrous Fe–Ca–P melt and the origin of iron oxide-apatite ore deposits
The origin of iron oxide-apatite deposits remains enigmatic and controversial. Here, the authors perform experiments on intermediate magmas and show that increasing aH2O and fO2 enlarges the two-liquid field thus allowing the Fe–Ca–P melt to separate easily from host silicic magma and produce iron o...
| Main Authors: | , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Nature Publishing Group
2018-04-01
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| Series: | Nature Communications |
| Online Access: | https://doi.org/10.1038/s41467-018-03761-4 |