HYDROXYLELLESTADITE METASOMATITES FROM THE GUMESHEV SKARN PORPHYRY COPPER DEPOSIT, MIDDLE URALS

dc.contributor.author	Grabezhev A.I.
dc.contributor.author	Gmyra V.G.
dc.contributor.author	Pal'gueva G.V.
dc.date.accessioned	2022-07-25T04:36:23Z
dc.date.available	2022-07-25T04:36:23Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13461006
dc.identifier.citation	Doklady Earth Sciences, 2004, 395, 2, 196-198
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38376
dc.description.abstract	On the Gumeshevsk deposit a massive metasomatite body is discovered, formed primarily by hydroxylellestadite. Thus the completing member of ellestadite mineral group is established (containing only 0.12% P2O5). Metasomatites were formed in the period of hysterogenic decomposition of skarns in marble or andradite-wollastonite skarn to pyrite-chalcopirite mineralization development. These metasomatites can be separated as individual type.
dc.title	HYDROXYLELLESTADITE METASOMATITES FROM THE GUMESHEV SKARN PORPHYRY COPPER DEPOSIT, MIDDLE URALS
dc.type	Статья

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