Abstract
Detrital monazite from Upper Jurassic sediments in the central part of the Frolov megadepression, West Siberian megabasin, is studied. Chemical composition of the mineral is studied and data on its age (chemical dating) are presented. Most monazite clasts are characterized by low roundness and their age corresponds to the Lower Paleozoic. Upper Jurassic sediments were likely derived not only from the local Early Paleozoic rock complexes (altaides), which make up the pre-Jurassic basement of the Frolov megadepression, but also from rocks located east and south of this megadepression.
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ACKOWLEDGMENTS
The authors are grateful to V.A. Volkov (Scientific-Analytical Center of Rational Subsurface Resource Management, Tyumen, Khanti-Mansiisk) for providing the possibility to study the core material from deep boreholes, which recovered Upper Jurassic sediments in the Frolov megadepression, and to the peer reviewer for valuable remarks and suggestions.
This work was supported by of the state assignment of the Institute of Geology and Geochemistry (state registration no. АААА-А18-118052590032-6).
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Erokhin, Y.V., Khiller, V.V. & Ivanov, K.S. Detrital Monazite from Upper Jurassic Sediments in the Central Part of the Frolov Megadepression, Western Siberia: Chemical Dating and Provenances. Lithol Miner Resour 54, 262–271 (2019). https://doi.org/10.1134/S0024490219030027
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DOI: https://doi.org/10.1134/S0024490219030027