MINERALS OF RARE EARTH ELEMENTS IN THE PHOSPHATE FRACTION OF FERROMANGANESE CRUSTS ON SEAMOUNTS

dc.contributor.author	Baturin G.N.
dc.contributor.author	Dubinchuk V.T.
dc.contributor.author	Azarnova L.A.
dc.contributor.author	Mel'nikov M.E.
dc.date.accessioned	2024-10-27T02:28:48Z
dc.date.available	2024-10-27T02:28:48Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13518441
dc.identifier.citation	Doklady Earth Sciences, 2006, 411, 9, 1362-1365
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46270
dc.description.abstract	Ferromanganese crusts on seamounts are among the major forms of solid fossil minerals in the ocean. They contain a significant amount of nonore inclusions, including calcium phosphates that often represent the crust-underlying and closely associated substrate. Phosphate is an undesirable impurity in ores, on the one hand, and an independent form of chemical raw material containing not only phosphorus, but also rare earth elements (REE) and several other valuable components, on the other hand.
dc.title	MINERALS OF RARE EARTH ELEMENTS IN THE PHOSPHATE FRACTION OF FERROMANGANESE CRUSTS ON SEAMOUNTS
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06090066

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