PB-PB ISOCHRON AGE AND SR-ISOTOPIC SIGNATURE OF THE UPPER YUDOMA CARBONATE SEDIMENTS (VENDIAN OF THE YUDOMA-MAYA TROUGH, EASTERN SIBERIA)
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dc.contributor.author | Semikhatov M.A. | |
dc.contributor.author | Petrov P.Yu. | |
dc.contributor.author | Obchinnikova G.V. | |
dc.contributor.author | Gorokhov I.M. | |
dc.contributor.author | Kuznetsov A.B. | |
dc.contributor.author | Kaurova O.K. | |
dc.date.accessioned | 2022-01-14T04:15:16Z | |
dc.date.available | 2022-01-14T04:15:16Z | |
dc.date.issued | 2003 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=13437507 | |
dc.identifier.citation | Doklady Earth Sciences, 2003, 393, 8, 1093-1097 | |
dc.identifier.issn | 1028-334X | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/34309 | |
dc.description.abstract | The carbonate rock investigation was based on the combined analysis of U-Pb- and Rb-Sr-systematism for the same samples. For the first time in the practice of studying the Upper Yudoma carbonate rocks of Eastern Siberia obtained is methodically reliable estimate of their Pb-Pb isochronous age, conforming to the stratigraphic location of the Yudoma-Maya trough and the basic ratio 87Sr/ 86Sr in these carbonates is determined, that characterizes Sr isotopic composition in Late Vendian ocean. | |
dc.subject | Vendian | |
dc.title | PB-PB ISOCHRON AGE AND SR-ISOTOPIC SIGNATURE OF THE UPPER YUDOMA CARBONATE SEDIMENTS (VENDIAN OF THE YUDOMA-MAYA TROUGH, EASTERN SIBERIA) | |
dc.type | Статья | |
dc.subject.age | Precambrian::Proterozoic::Neoproterozoic::Vendian | |
dc.subject.age | Докембрий::Протерозой::Неопротерозойская::Вендский | ru |
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