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

dc.contributor.authorVelikoslavinsky S.D.
dc.contributor.authorKotov A.B.
dc.contributor.authorSal'nikova E.B.
dc.contributor.authorGlebovitsky V.A.
dc.contributor.authorKovach V.P.
dc.contributor.authorZagornaya N.Yu.
dc.contributor.authorBelyaevsky N.A.
dc.contributor.authorYakovleva S.Z.
dc.contributor.authorFedoseenko A.M.
dc.date.accessioned2022-01-14T04:15:15Z
dc.date.available2022-01-14T04:15:15Z
dc.date.issued2003
dc.description.abstractThe 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.identifierhttps://www.elibrary.ru/item.asp?id=13437471
dc.identifier.citationDoklady Earth Sciences, 2003, 393, 8, 1151-1155
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/34307
dc.titleTHE U-PB AGE OF THE FEDOROV SEQUENCE OF THE ALDAN GRANULITE-GNEISS MEGACOMPLEX, THE ALDAN SHIELD
dc.typeСтатья

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