PLATINUM SOLUBILITY IN WATER-BEARING MAGNESIAN BASALTIC MELTS AT 1200°C AND 2 KBAR

dc.contributor.author	Bezmen N.I.
dc.contributor.author	Gorbachev P.N.
dc.contributor.author	Shalynin A.I.
dc.date.accessioned	2024-10-23T07:15:49Z
dc.date.available	2024-10-23T07:15:49Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13509528
dc.identifier.citation	Doklady Earth Sciences, 2006, 406, 1, 122-127
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46122
dc.description.abstract	The study of the chemical behavior of highly siderophile elements, including platinum group metals (PGM), is of great theoretical and practical significance for understanding the early differentiation of the Earth, mantle and core formation, and the conditions of PGM formation in mafic–ultramafic magmatic complexes. The experimental study of PGM solubility in silicate melts under different physicochemical conditions, together with geochemical investigation, plays an important role in the solution of this problem. Increasingly greater attention has recently been focused on the role of fluids in these processes.
dc.title	PLATINUM SOLUBILITY IN WATER-BEARING MAGNESIAN BASALTIC MELTS AT 1200°C AND 2 KBAR
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06010302

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