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dc.contributor.author Kovach V.P.
dc.contributor.author Kotov A.B.
dc.contributor.author Salnikova E.B.
dc.contributor.author Zagornaya N.Yu.
dc.contributor.author Berezkin V.I.
dc.contributor.author Smelov A.P.
dc.date.accessioned 2020-12-01T08:34:52Z
dc.date.available 2020-12-01T08:34:52Z
dc.date.issued 1996
dc.identifier https://elibrary.ru/item.asp?id=13241717
dc.identifier.citation Stratigraphy and Geological Correlation, 1996, , 3, 213-219
dc.identifier.issn 0869-5938
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/19998
dc.description.abstract The first data on the Nd isotopic composition in high-AI gneisses and associated gamet-hypersthene-biotite plagiogneisses of the Kurumkan Subgroup, the lengra Group of Aldan Shield are presented. The obtained results show that rocks of the subgroup accumulated after ∼2.9 Ga, i.e., during the Late Archean or Early Proterozoic, and not the Early Archean evolutionary stage of the shield. Protoliths of garnet-hypersthenebiotite gneisses were not older than 2.3 Ga, and their formation marks the Early Proterozoic stage of continental crust generation in the Aldan granulite-gneiss region.
dc.subject Archean en
dc.subject Proterozoic en
dc.title SM-ND ISOTOPIC SYSTEMATICS OF THE KURUMKAN SUBGROUP, THE IENGRA GROUP OF ALDAN SHIELD
dc.type Статья
dc.subject.age Precambrian::Archean en
dc.subject.age Precambrian::Proterozoic en
dc.subject.age Докембрий::Архей ru
dc.subject.age Докембрий::Протерозой ru


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