The Rb–Sr Age of Authigenic Glauconite and U–Pb Age of Detrital Zircons from Riphean and Vendian Deposits of the Mezen Syneclise, East European Platform (Keltmen-1 Borehole)

Zaitseva, T.S.; Golubkova, E.Y.; Kuznetsov, A.B.; Kuznetsov, N.B.; Romanyuk, T.V.; Dovzhikova, E.G.; Kaurova, O.K.

Авторы: Zaitseva T.S., Golubkova E.Yu, Kuznetsov A.B., Kuznetsov N.B., Romanyuk T.V., Dovzhikova E.G., Kaurova O.K.
Журнал: Doklady Earth Sciences
Год издания: 2024
Издательство: Maik Nauka/Interperiodica Publishing
Местоположение издательства: Russian Federation
DOI: 10.1134/s1028334x24603419
Аннотация: The Rb–Sr age of glauconite and the U–Pb LA-ICP-MS age of detrital zircon from sandstones ofthe Riphean Okos Formation and the Vendian Ust-Pinega Formation were determined in the Keltmen-1parametric borehole, drilled in the Vychegda trough of the Mezen syneclise in the northern part of EuropeanRussia. The model Rb–Sr age of glauconite (870–820 Ma) and the U–Pb age of the youngest detrital zircon(1005 ± 14 Ma) limit the time of accumulation of the Okos Formation to the first half of the Late Riphean,which is in good agreement with the biostratigraphic data available. The U–Pb age of the youngest detritalzircon from the lower part of the Ust-Pinega Formation suggests that supply of Late Vendian sandstones intothe Mezen Basin began about 575 Ma. Thus, the duration of the stratigraphic hiatus between the Riphean andVendian is estimated to be about 250–300 Ma. In the Late Riphean and Late Vendian, the Mezen basin wasfilled with terrigenous material of Archean–Late Proterozoic age (from 3.25 to 1.02 Ga), the sources of whichwere rocks of the Baltic Shield. In the lower part of the Ust-Pinega Formation, a population of detrital zirconof Vendian age (730–575 Ma) was discovered, a possible source of which could have been rocks of the Proto-Ural–Timan Orogen.
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The Rb–Sr Age of Authigenic Glauconite and U–Pb Age of Detrital Zircons from Riphean and Vendian Deposits of the Mezen Syneclise, East European Platform (Keltmen-1 Borehole)статья

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