SHEATHLIKE METASOMATIC GARNET CRYSTALS FROM THE MAKSYUTOVO METAMORPHIC COMPLEX, THE SOUTHERN URALS

dc.contributor.author	Zhdanov V.V.
dc.contributor.author	Glikin A.E.
dc.date.accessioned	2024-10-23T07:15:55Z
dc.date.available	2024-10-23T07:15:55Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13510855
dc.identifier.citation	Doklady Earth Sciences, 2006, 409, 5, 814-817
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46139
dc.description.abstract	The Maksyutovo Complex is located in the southern Urals as a near-meridional belt 180 km long and 12–16 km wide. Eclogites and products of their metasomatic alteration (schists) are widespread in this complex. The alteration begins from the alkaline sodic metasomatism that fostered replacement of eclogites with glaucophane schists. Sodic metasomatism gave way to potassic metasomatism. Both the relict eclogites and glaucophane schists were replaced with phengite schists.
dc.subject	Maksyutovo Complex
dc.subject	southern Urals
dc.title	SHEATHLIKE METASOMATIC GARNET CRYSTALS FROM THE MAKSYUTOVO METAMORPHIC COMPLEX, THE SOUTHERN URALS
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X0605031X

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