THE KUZNECHENSKY MASSIF OF POTASSIC PORPHYRITIC GRANITES: RESULTS OF U-PB DATING AND SUBSTANTIATION OF THE TECTONIC POSITION (BALTIC SHIELD)

dc.contributor.author	Baltybaev Sh.K.
dc.contributor.author	Sal'nikova E.B.
dc.contributor.author	Glebovitsky V.A.
dc.contributor.author	Berezhnaya N.G.
dc.contributor.author	Yakovleva S.Z.
dc.contributor.author	Kovach V.P.
dc.date.accessioned	2022-08-14T03:31:04Z
dc.date.available	2022-08-14T03:31:04Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13468099
dc.identifier.citation	Doklady Earth Sciences, 2004, 398, 7, 1024-1028
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38509
dc.description.abstract	The high-grade metamorphism (no lower than the high-temperature amphibolite facies) and involvement of the massif in the intricate folding suggest its emplacement at the orogenic stage of Svecofennide evolution. To date, we have obtained a sufficiently precise age interval (1.87-1.89 Ga) for this stage. This communication presents results of U-Pb-dating of zircon and monazite from granites of the Kuznechensky Massif that support their emplacement at the orogenic stage.
dc.title	THE KUZNECHENSKY MASSIF OF POTASSIC PORPHYRITIC GRANITES: RESULTS OF U-PB DATING AND SUBSTANTIATION OF THE TECTONIC POSITION (BALTIC SHIELD)
dc.type	Статья

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