METAMORPHIC EVOLUTION OF GRANULITES FROM THE KURUL'TA BLOCK, ALDAN SHIELD: U-PB SINGLE ZIRCON STUDY

dc.contributor.author	Sal'nikova E.B.
dc.contributor.author	Glebovitsky V.A.
dc.contributor.author	Kotov A.B.
dc.contributor.author	Larin A.M.
dc.contributor.author	Yakovleva S.Z.
dc.contributor.author	Berezhnaya N.G.
dc.contributor.author	Kovach V.P.
dc.contributor.author	Drugova G.M.
dc.contributor.author	Anisimova I.V.
dc.date.accessioned	2022-08-14T03:31:10Z
dc.date.available	2022-08-14T03:31:10Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13472142
dc.identifier.citation	Doklady Earth Sciences, 2004, 398, 7, 968-972
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38541
dc.description.abstract	Stanovoy fold system (DSFS) is a giant tectonic melange zone (Fig. 1) that includes the Kalar, Kurul'ta, Zverev, Sutam, Ayumkan, and Dzhugdzhur tectonic blocks composed of granulite-facies rocks. The study of the granulite complexes of the Aldan Shield-DSFS junction and the deciphering of their metamorphic evolution is the key to understanding the interaction between these large lithospheric segments in the Early Precambrian. The present paper presents the results of U-Pb dating of single zircons from charnockites of the Kurul'ta Block.
dc.title	METAMORPHIC EVOLUTION OF GRANULITES FROM THE KURUL'TA BLOCK, ALDAN SHIELD: U-PB SINGLE ZIRCON STUDY
dc.type	Статья

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