Abstract
In order to determine the provenance and age of terrigenous-carbonate stratified units exposed in the region of Bagrush Mountains, Bashkirian uplift, U–Pb dating of detrital zircons from these units has been carried out. A comparison of the data results with analogous data on five stratigraphic levels within the Riphean section of the Bashkirian uplift has shown that the studied sequence should be, most likely, correlated to the uppermost Lower Riphean or the lowermost Middle Riphean.
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Funding
This work was performed within the framework of a state contract of the Schmidt Institute of Physics of the Earth, Russian Academy of Sciences (Moscow) and Institute of Geology and Geochemistry, Russian Academy of Sciences, Ekaterinburg (no. AAAA-A18-118052590032-6), and a state contract of the Institute of Geology, Ufa Federal Research Center, Russian Academy of Scineces, Ufa (no. 0252-2014-0002).This work was supported by a grant from the Government of the Russian Federation, no. 075-15-2019-1883.
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Romanyuk, T.V., Kuznetsov, N.B., Puchkov, V.N. et al. Age and Stratigraphic Position of Sedimentary Sequences of the Bagrush Mountains (Southern Urals) Based on the Results of U–Pb Dating (LA–ICP–MS) of Detrital Zircons. Dokl. Earth Sc. 493, 593–599 (2020). https://doi.org/10.1134/S1028334X20080188
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DOI: https://doi.org/10.1134/S1028334X20080188