Paleotectonic analysis of the territory of Krasnoleninskiy arch of the West Siberian Plate is executed. The contribution of each selected period of time in the tectonic development of the territory is considered. The main lines of tectonic movements, the relative increase of the basic structures of Krasnoleninskiy arch are revealed. It was come out with a suggestion about tectonic movements relationship with the re-formation of deposits of vikulovskoye sediments.
Keywords: Krasnoleninskiy arch, paleotectonics, vikulovskoye sediments, horizons, layers, deposits.
References
1. Nassonova N.V. Belousov S.L. Zverev K.V., Otchet “Detal'nye paleogeograficheskie postroeniya po plastam VK na Em-Egovskom, Kamennom i Talinskom LU zapada KhMAO” (The report, "Detailed paleogeographic build layers of west KhMAO licence blocks: Em-Egovskiy, Kamenny, and Talinskiy"), Tyumen': OOO “TNNTs”, 2009.
