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

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dc.contributor.authorZhdanov V.V.
dc.contributor.authorGlikin A.E.
dc.date.accessioned2024-10-23T07:15:55Z
dc.date.available2024-10-23T07:15:55Z
dc.date.issued2006
dc.description.abstractThe 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.identifierhttps://www.elibrary.ru/item.asp?id=13510855
dc.identifier.citationDoklady Earth Sciences, 2006, 409, 5, 814-817
dc.identifier.doi10.1134/S1028334X0605031X
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/46139
dc.subjectMaksyutovo Complex
dc.subjectsouthern Urals
dc.titleSHEATHLIKE METASOMATIC GARNET CRYSTALS FROM THE MAKSYUTOVO METAMORPHIC COMPLEX, THE SOUTHERN URALS
dc.typeСтатья

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