Geomorphological formations of the South of Western Siberia and adjacent territories

Capa

Citar

Texto integral

Acesso aberto Acesso aberto
Acesso é fechado Acesso está concedido
Acesso é fechado Somente assinantes

Resumo

Within the south of Western Siberia and adjacent territories, 23 types of Land systems (parageneses of genetically homogeneous surfaces/land units) have been identified, belonging to three physiographic zones: flat, foothill and mountain, as well as one type of extrazonal formations. The use of formational analysis has made it possible to identify genetic relationships between large spatially separated geomorphological elements, considering them as formational series. For the first time, a catafluvial geomorphological formation has been identified for the south of Western Siberia, and its place among other geomorphological formations in the region has been shown. A connection has been established between the ancient drainage troughs of Western Siberia, transit erosion valleys and catafluvial events (superfloods).

Sobre autores

I. Novikov

Sobolev Institute of Geology and Mineralogy of SB RAS

Autor responsável pela correspondência
Email: novikov@igm.nsc.ru
Rússia, Novosibirsk

Bibliografia

  1. Arkhipov S.A., Vdovin V.V., Mizerov B.V. et al. (1970). Zapadno-Sibirskaya ravnina (West Siberian Plain). M.: Nauka (Publ.). 279 p. (in Russ.)
  2. Arkhipov S.A., Volkov I.A., Volkova V.S. (1965). The main problems of paleogeography of the Quaternary period in the south of Western Siberia. In: Osnovnye problemy izucheniya chetvertichnogo perioda. M.: Nauka (Publ.). P. 218–228. (in Russ.)
  3. Astahov V.I. (2006). Evidence of Late Pleistocene ice-dammed lakes in West Siberia. Boreas. V. 35. P. 607–621. https://doi.org/10.1111/j.1502-3885.2006.tb01167.x
  4. Butvilovsky V.V. (1993). Paleogeografiya poslednego oledeneniya i golotsena Altaya: sobytiino-katastroficheskaya model’ (Paleogeography of the last glaciation and Holocene of Altai: an event-catastrophic model). Tomsk: Tomsk Universitet (Publ.). 252 p. (in Russ.)
  5. Devyatkin E.V. (1981). Kainozoi vnutrenney Azii (Cenozoic Inner Asia). M.: Nauka (Publ.). 196 p. (in Russ.)
  6. Dobretsov N.L. (Eds.). (1981). Metamorficheskie formatsii i metamorfogennye mestorozhdeniya (Metamorphic formations and metamorphogenic deposits). Novosibirsk: IGiG SO AN USSR (Publ.). 90 p. (in Russ.)
  7. Florensov N.A. (1964). On some general concepts in geomorphology. Geologiya i geofizika. № 10. P. 78–89. (in Russ.)
  8. Florensov N.A. (1971). On geomorphological formations. Geomorfologiya. № 2 P. 3–10. (in Russ.)
  9. Gadzhiev I.M. (Ed.). (1988). Geograficheskie i inzhenerno-geologicheskie usloviya Stepnogo (Geographical and engineering-geological conditions of Steppe Altai). Novosibirsk: Nauka. Sibirskoe otdelenie (Publ.). 97 p. (in Russ.)
  10. Ganeshin G.S. (Ed.). (1967). Geomorfologicheskaya karta SSSR. Masshtab 1:7500000 (Geomorphological map of the USSR. Scale 1:7500000). M.: Vsesoyuznyi aerogeologicheskii trest Ministerstva geologii SSSR (Publ.). 4 p. (in Russ.)
  11. Groswald M.G. (1965). Razvitie rel’efa Sayano-Tuvinskogo nagor’ya (Development of the relief of the Sayano-Tuva highlands). M.: Nauka (Publ.). 167 p. (in Russ.)
  12. Haq B.U., Al-Qahtani A.M. (2005). Phanerozoic cycles of sea-level change on the Arabian Platform. GeoArabia. № 10. Р. 127–160. https://doi.org/10.2113/geoarabia1002127
  13. Ivanov K.E., Novikov S.M. (Eds.). (1976). Bolota Zapadnoi Sibiri, ikh stroenie i gidrologicheskii rezhim (Swamps of Western Siberia, their structure and hydrological regime). L.: Gidrometeoizdat (Publ.). 448 p. (in Russ.)
  14. Kuznetsov Yu.A. (1964). Glavnye tipy magmaticheskikh formatsii (Main types of magmatic formations). M.: Nedra (Publ.). 387 p. (in Russ.)
  15. Mamedov G.M., Novikov I.S. (2015). Geomorphology of the Dzhungar Plain and its mountain frame. Geomorfologiya. № 1. P. 88–100. (in Russ.) https://doi.org/10.15356/0435-4281-2015-1-88-100
  16. Nikolaev V.A. (Ed.). (1978). Geomorfologicheskie formatsii Sibiri (Geomorphological formations of Siberia). Novosibirsk: IGiG SO AN USSR (Publ.). 162 p. (in Russ.)
  17. Novikov I.S. (2001). Сenozoic Strike-slip Tectonics in Altai. Geologiya i geofizika. Iss. 42. № 9. Р. 1311–1321. (in Russ.)
  18. Novikov I.S. (2003). Morphotectonics of Altai. Geomorfologiya. № 3. P. 10–25. (in Russ.) https://doi.org/10.15356/0435-4281-2003-3-10-25
  19. Novikov I.S. (2021). Changes in the global basis of denudation in the Late Mesozoic and Cenozoic and its influence on the formation of geomorphological structure in areas with different neotectonic regimes Geologiya i mineral’no-syr’evye resursy Sibiri. № 10s. P. 68–84. (in Russ.) https://doi.org/10.20403/2078-0575-2021-10c-69-85
  20. Novikov I.S., Mamedov G.M. (2018). Maps of transport permeability on a geomorphological basis (methodology and implementation using the example of the territory of northern Xinjiang). Vestnik Akademii voennykh nauk. № 2(63). P. 146–160. (in Russ.)
  21. Novikov I.S., Nazarov D.V., Mikharevich M.V. et al. (2023). The Azas Ice Sheet and Its Role in the Formation of Late Pleistocene Ice-Dammed Lakes in Southern Siberia: Case Study of Upper Kharal Paleolake. Geologiya i geofizika. Iss. 64. № 5. P. 595–606. (in Russ.) https://doi.org/10.15372/GiG2022146
  22. Shatsky N.S. (1965). Fatsii i formatsii (Facies and formations). M.: Nauka (Publ.). 232 p. (in Russ.)
  23. Sugorakova A.M., Yarmolyuk V.V., Lebedev V.I. (2023). Kainozoiskii vulkanizm Tuvy (Cenozoic volcanism of Tuva). Kyzyl: TuviKOPR (Publ.). 90 p. (in Russ.)
  24. Svarichevskaya Z.A. (1961). Drevnii peneplen Kazakhstana (Ancient peneplain of Kazakhstan). Leningrad: LGU (Publ.). 295 p.
  25. Zolnikov I.D. (2021). On the stratigraphic significance of the low terraces of the Suzun strata of the Upper Ob region under the regime. Geologiya i mineral’no-syr’evye resursy Sibiri. № 10s P. 7–17. (in Russ.) https://doi.org/10.20403/2078-0575-2021-10c-7-17

Arquivos suplementares

Arquivos suplementares
Ação
1. JATS XML
Baixar
2. Fig. 1. Layout of the territory under consideration.

Baixar (892KB)
Metadados
3. Fig. 2. Morphological types of relief in the south of Western Siberia and adjacent territories. 1 – river valleys (1.1 – Irtysh, 1.2 – Ob, 1.3 – Yenisei); 2 – plains (2.1 – Irtysh, 2.2 – Vasyugan, 2.3 – Baraba, 2.4 – Kulunda, 2.5 – Ob, 2.6 – Ketsko-Tym, 2.7 – Chulym); 3 – plateaus (3.1 – Zaangarskoe, 3.2 – Priangarskoe); 4 – low hills (4.1 – Kazakh); 5 – foothills (5.1 – Bugotaksko-Sokur, 5.2 – Chumysh); 6 – plains of large intermountain basins (6.1 – Kuznetsk, 6.2 – North Minusinsk, 6.3 – South Minusinsk, 6.4 – Todzhinsk, 6.5 – Tuva, 6.6 – Zaisan, 6.7 – Kyndyktykul-Achitnur, 6.8 – Ubsunur, 6.9 – Bolshie Ozeri, 6.10 – Darkhat, 6.11 – Tunka-Khubsugul); 7 – mountain structures (7.1 – Yenisei Ridge, 7.2 – Salair Ridge, 7.3 – Kuznetsk Alatau and Mountain Shoria, 7.4 – Rudny Altai, 7.5 – Russian (Mountain) and Mongolian Altai, 7.6 – Western Sayan, 7.7 – Eastern Sayan, 7.8 – Tannu-Ola, 7.9 – Academician Obrucheva, 7.10 – Selinga Highlands, 7.11 – Turgein-Nuru, 7.12 – Han-Hukhiin Ula, 7.13 – Hangai).

Baixar (388KB)
Metadados
4. Fig. 3. Land systems of the south of Western Siberia and adjacent territories. Accumulative. Plains: 1 – alluvial terrace, 2 – alluvial-proluvial, 3 – proluvial sloping, 4 – sandy eolian, 5 – upland bog plains, 6 – lacustrine, 7 – moraine, 8 – volcanogenic, 9 – catafluvial, 10 – small intermountain basins. Denudation. Plains: 11 – sheet, developed in clayey deposits of the early and middle Cenozoic, 12 – sheet, developed in deposits of the early and middle Cenozoic and covered by a cover of upper Cenozoic subaerial deposits, 13 – inclined, developed in rocks of the middle and upper Mesozoic, 14 – structural plateaus, developed in late Paleozoic and Mesozoic rocks; small hills: 15 – denudation, developed in Paleozoic rocks, 16 – denudation, developed in Paleozoic rocks, covered by a thin cover of Upper Cenozoic subaerial deposits, 17 – cuesta, developed in Upper Paleozoic and Middle Mesozoic rocks, 18 – foothills, developed in Upper Paleozoic, Mesozoic and Cenozoic rocks, 19 – linear forberg; mountains: 20 – lowlands, 21 – middle mountains, 22 – highlands; extra-zonal: 23 – transit erosional valleys.

Baixar (1MB)
Metadados
5. Fig. 4. Reflection of catafluvial events of the Pleistocene in the south of Western Siberia in the spatial distribution of geomorphological formations. 1 – areas of the flooding during catafluvial events; 2 – areas of development of glacial-dammed lakes; 3 – discharge channels and flow directions.

Baixar (619KB)
Metadados

Declaração de direitos autorais © Russian Academy of Sciences, 2024