PALLADIUM SOLUBILITY IN WATER-BEARING SILICATE MELTS: EVIDENCE FROM EXPERIMENTAL DATA

dc.contributor.author	Bezmen N.I.
dc.contributor.author	Gorbachev P.N.
dc.contributor.author	Azif E.
dc.contributor.author	Naldrett A.J.
dc.date.accessioned	2024-10-19T07:54:44Z
dc.date.available	2024-10-19T07:54:44Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13503740
dc.identifier.citation	Doklady Earth Sciences, 2006, 406, 1, 65-68
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46048
dc.description.abstract	One of the most interesting geological problems, bearing both theoretical and practical significance, is the study of PGE geochemistry in the formation of the Earth’s crust and mantle and in differentiated maficultramafic magmatic complexes, as well as in related PGM mineralization. An important part of this problem is the experimental study of PGE solubility in natural and model silicate melts depending on oxygen fugacity—the main parameter of redox conditions of the magmatic process.
dc.title	PALLADIUM SOLUBILITY IN WATER-BEARING SILICATE MELTS: EVIDENCE FROM EXPERIMENTAL DATA
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06010168

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