SM-ND ISOTOPIC SYSTEMATICS OF THE KURUMKAN SUBGROUP, THE IENGRA GROUP OF ALDAN SHIELD
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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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