CHARNOCKITES FROM EAST ANTARCTICA AND THEIR GEOLOGICAL TYPIFICATION

dc.contributor.author	Mikhalsky E.V.
dc.contributor.author	Sheraton J.W.
dc.contributor.author	Vladykin N.V.
dc.date.accessioned	2024-10-27T02:28:49Z
dc.date.available	2024-10-27T02:28:49Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13514447
dc.identifier.citation	Doklady Earth Sciences, 2006, 408, 4, 662-666
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46273
dc.description.abstract	Charnockitic rocks (orthopyroxene-bearing granitoids) are important and characteristic rocks exposed in East Antarctica. The origin of these rocks and their tectonic setting has been a matter of hot debate since the pioneering studies in Antarctica. The emplacement of intrusive charnockites was interpreted as an indication of cratonization of the Early Precambrian Antarctic Shield or its subsequent tectonic activity. The charnockitic rocks were regarded as intracontinental and anorogenic formations.
dc.subject	charnockite
dc.subject	Antarctica
dc.title	CHARNOCKITES FROM EAST ANTARCTICA AND THEIR GEOLOGICAL TYPIFICATION
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06040349

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