ISOTOPE AGE OF SUBVOLCANIC GRANITOID ROCKS OF THE EARLY PROTEROZOIC PANARECHKA VOLCANOTECTONIC STRUCTURE, KOLA PENINSULA

dc.contributor.author	Skuf'in P.K.
dc.contributor.author	Bayanova T.B.
dc.contributor.author	Mitrofanov F.P.
dc.date.accessioned	2024-11-09T08:38:28Z
dc.date.available	2024-11-09T08:38:28Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13530908
dc.identifier.citation	Doklady Earth Sciences, 2006, 409, 5, 774-778
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46469
dc.description.abstract	The Panarechka volcanotectonic calderalike structure (PVTS) was found in the Early Proterozoic Pechenga–Varzuga Rift Belt (fault-lineament) of the Kola region. This is an oval body (21 × 8 km in size) that extends in a NW direction and is discordant with host rocks of the Il’mozero Formation and Tominga Group of the Imandra–Varzuga structural zone. The volcanic structure is filled with arkosic and graywacke sandstones and basaltic lavas of the Panarechka Formation ~1000 km thick.
dc.subject	Panarechka
dc.subject	Kola peninsula
dc.subject	Proterozoic
dc.title	ISOTOPE AGE OF SUBVOLCANIC GRANITOID ROCKS OF THE EARLY PROTEROZOIC PANARECHKA VOLCANOTECTONIC STRUCTURE, KOLA PENINSULA
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06050229
dc.subject.age	Precambrian::Proterozoic
dc.subject.age	Докембрий::Протерозой

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