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