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...

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Autores principales:	Tong Hou, Bernard Charlier, François Holtz, Ilya Veksler, Zhaochong Zhang, Rainer Thomas, Olivier Namur
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2018
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/00f2aae4c3b14c88ab39434e0dbb4f78
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spelling	oai:doaj.org-article:00f2aae4c3b14c88ab39434e0dbb4f782021-12-02T16:49:34ZImmiscible hydrous Fe–Ca–P melt and the origin of iron oxide-apatite ore deposits10.1038/s41467-018-03761-42041-1723https://doaj.org/article/00f2aae4c3b14c88ab39434e0dbb4f782018-04-01T00:00:00Zhttps://doi.org/10.1038/s41467-018-03761-4https://doaj.org/toc/2041-1723The 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 oxide-apatite ores.Tong HouBernard CharlierFrançois HoltzIlya VekslerZhaochong ZhangRainer ThomasOlivier NamurNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-8 (2018)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Tong Hou Bernard Charlier François Holtz Ilya Veksler Zhaochong Zhang Rainer Thomas Olivier Namur Immiscible hydrous Fe–Ca–P melt and the origin of iron oxide-apatite ore deposits
description	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 oxide-apatite ores.
format	article
author	Tong Hou Bernard Charlier François Holtz Ilya Veksler Zhaochong Zhang Rainer Thomas Olivier Namur
author_facet	Tong Hou Bernard Charlier François Holtz Ilya Veksler Zhaochong Zhang Rainer Thomas Olivier Namur
author_sort	Tong Hou
title	Immiscible hydrous Fe–Ca–P melt and the origin of iron oxide-apatite ore deposits
title_short	Immiscible hydrous Fe–Ca–P melt and the origin of iron oxide-apatite ore deposits
title_full	Immiscible hydrous Fe–Ca–P melt and the origin of iron oxide-apatite ore deposits
title_fullStr	Immiscible hydrous Fe–Ca–P melt and the origin of iron oxide-apatite ore deposits
title_full_unstemmed	Immiscible hydrous Fe–Ca–P melt and the origin of iron oxide-apatite ore deposits
title_sort	immiscible hydrous fe–ca–p melt and the origin of iron oxide-apatite ore deposits
publisher	Nature Portfolio
publishDate	2018
url	https://doaj.org/article/00f2aae4c3b14c88ab39434e0dbb4f78
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Immiscible hydrous Fe–Ca–P melt and the origin of iron oxide-apatite ore deposits

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