TOBERMORITE-PLOMBIERITE METASOMATITES OF THE GUMESHEVSK SKARN-PORPHYRY COPPER DEPOSIT, MIDDLE URALS

dc.contributor.author	Zadov A.E.
dc.contributor.author	Grabezhev A.I.
dc.contributor.author	Pribavkin S.V.
dc.contributor.author	Pertsev N.N.
dc.contributor.author	Chukanov N.V.
dc.date.accessioned	2024-10-23T07:15:54Z
dc.date.available	2024-10-23T07:15:54Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13510843
dc.identifier.citation	Doklady Earth Sciences, 2006, 407, 3, 495-497
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46136
dc.description.abstract	Although calcic hydrosilicates with tobermorite-type structure (tobermorite, plombierite, and tacherenite) are rare minerals, they are rather typical of low-temperature mineral assemblages in some Ca-silicate rocks. Owing to defect structure and micrometer-size crystals, minerals of the tobermorite group are studied insufficiently, and each finding attracts interest. Most often, these minerals fill fissures. At the Gumeshevsk skarn–porphyry copper deposit, we detected them as massive metasomatite bodies.
dc.title	TOBERMORITE-PLOMBIERITE METASOMATITES OF THE GUMESHEVSK SKARN-PORPHYRY COPPER DEPOSIT, MIDDLE URALS
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06030330

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