Paleozoic facies megazones in the basement of the West Siberian geosyncline
E.A. Yolkin a , A.E. Kontorovich a , N.K. Bakharev a , S.Yu. Belyaev a , A.I. Varlamov b , N.G. Izokh a , A.V. Kanygin a , V.A. Kashtanov a , N.P. Kirda a , A.G. Klets a , V.A. Kontorovich a , V.I. Krasnov b , V.A. Krinin c , S.A. Moiseev a , O.T. Obut a , S.V. Saraev a , N.V. Sennikov a , V.M. Tishchenko d , Yu.F. Filippov a , A.V. Khomenko a , V.G. Khromykh a
a Institute of Petroleum Geology and Geophysics, Siberian Branch of the RAS, 3 prosp. Akad. Koptyuga, Novosibirsk, 630090, Russia
b Siberian Research Institute of Geology, Geophysics and Mineral Resources, 67 Krasny prosp., Novosibirsk, 630091, Russia
c Vankorneft' Ltd., 51 ul. Respubliki, Krasnoyarsk, 660075, Russia
d Nordimperial Ltd., 7 ul. K. Marksa, Tomsk, Russia
Keywords: Facies zonation; biochronology; paleogeography; geodynamics; terrane; continent; Paleozoic; West Siberian geosyncline
Pages: 491-504
Abstract
Facies zonation of the Paleozoic basement of West Siberian geosyncline and its surroundings is presented. Facies megazones are distinguished according to types of sedimentation. Analysis of lateral and successive sedimentary sequences shows that the available data are insufficient to map the facies distribution over the whole territory of the geosyncline for short time slices. Only the Late Devonian section is supported by data sufficient for the proposed facies zonation. Five megazones, I, II, III, IV, and V, are distinguished in the westward direction. First three megazones make up a single lateral facies succession and represent sedimentary environments on and around the Siberian continent. Megazone IV includes shallow-water volcanic and sedimentary rocks that compose the Kazakhstan continent bounded by Early and Middle Carboniferous sutures in the west and east. Megazone V comprises fold-thrust (island arc) complexes of the eastern Urals.
The main events in the geologic history of the region were associated with the interaction of two major crustal masses (Siberian and East European continents) and the young Kazakhstan continent in the oceanic space called the Paleoasian ocean. Only few fragments of this space occur in the present-day framework of the territory, the greatest part being sunk in subduction zones, especially in the large zone of the Main Uralian Fault.
Production and accumulation of organic matter in pre-Mesozoic deposits occurred on continental shelves, which are most promising for Precambrian and Paleozoic oil and gas.
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