THE U-PB AGE OF THE FEDOROV SEQUENCE OF THE ALDAN GRANULITE-GNEISS MEGACOMPLEX, THE ALDAN SHIELD

dc.contributor.author	Velikoslavinsky S.D.
dc.contributor.author	Kotov A.B.
dc.contributor.author	Sal'nikova E.B.
dc.contributor.author	Glebovitsky V.A.
dc.contributor.author	Kovach V.P.
dc.contributor.author	Zagornaya N.Yu.
dc.contributor.author	Belyaevsky N.A.
dc.contributor.author	Yakovleva S.Z.
dc.contributor.author	Fedoseenko A.M.
dc.date.accessioned	2022-01-14T04:15:15Z
dc.date.available	2022-01-14T04:15:15Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=13437471
dc.identifier.citation	Doklady Earth Sciences, 2003, 393, 8, 1151-1155
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34307
dc.description.abstract	The results of geochronological investigation confirm the assumption of the Early Proterozoic age of Fedorov rock mass. The estimated age (2006±3 mln years) of metaandesite protolytes of this series agrees with age estimates for tonalite-trondiemite orthogneiss of the Timpton complex (2011±2 mln ears) and for Ungrin gabbro-diorite-tonalite-trondiemite complex (2016±5 mln ears). It permits to consider formation of Fedorov group and the mentioned complexes in the framework of geodynamic system: active edge of Olekmo-Aldan continental platform - Fedorov island arc.
dc.title	THE U-PB AGE OF THE FEDOROV SEQUENCE OF THE ALDAN GRANULITE-GNEISS MEGACOMPLEX, THE ALDAN SHIELD
dc.type	Статья

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