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

Tong Hou (), Bernard Charlier, François Holtz, Ilya Veksler, Zhaochong Zhang, Rainer Thomas and Olivier Namur
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Tong Hou: Leibniz Universtät Hannover
Bernard Charlier: University of Liege
François Holtz: Leibniz Universtät Hannover
Ilya Veksler: GFZ German Research Center for Geosciences
Zhaochong Zhang: China University of Geosciences
Rainer Thomas: GFZ German Research Center for Geosciences
Olivier Namur: Leibniz Universtät Hannover

Nature Communications, 2018, vol. 9, issue 1, 1-8

Abstract: Abstract 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 experiments on intermediate magmas that develop liquid immiscibility at 100 MPa, 1000–1040 °C, and oxygen fugacity conditions (fO2) of ∆FMQ = 0.5–3.3 (FMQ = fayalite-magnetite-quartz equilibrium). Some of the immiscible melts are highly enriched in iron and phosphorous ± calcium, and strongly depleted in silicon (

Date: 2018
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DOI: 10.1038/s41467-018-03761-4

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