Megafloods deposits in the middle Yenisei river valley
- 作者: Zolnikov I.D.1,2, Filatov E.A.1, Novikov I.S.1, Shpansky A.V.1,3, Klementyev A.M.4, Anoikin A.A.5, Vybornov A.V.1,5, Glushkov N.V.1,2, Dzhumanov A.T.1,3, Bordyugova E.A.1,2, Rogozin D.E.1,2
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隶属关系:
- Sobolev Institute of Geology and Mineralogy Siberian Branch of the RAS
- Novosibirsk state university
- Tomsk State University
- Institute of the Earth’s Crust Siberian Branch of the RAS
- Institute of Archaeology and Ethnography Siberian Branch of the RAS
- 期: 卷 55, 编号 4 (2024)
- 页面: 58-77
- 栏目: CATAFLUVIAL EVENTS IN THE QUATERNARY HISTORY OF NORTHERN EURASIA
- URL: https://modernonco.orscience.ru/2949-1789/article/view/682332
- DOI: https://doi.org/10.31857/S2949178924040053
- EDN: https://elibrary.ru/FGUOTI
- ID: 682332
如何引用文章
详细
As a result of recent field studies in the Middle Yenisei Valley, the absence of high terraces of alluvial and periglacial origin, which traditionally formed the basis of the Quaternary stratigraphy of the Minusinsk basins, has been established. Sediments previously attributed to the alluvium of high terraces are super-flood. The article provides lithofacies characteristics of subaerial and megaflood deposits, as well as the features of their relationships in space. Information on paleontological and archaeological objects from stratified locations of the study area, for which geodatabases have been compiled, has been summarized and cartographically visualized. In the North Minusinsk Basin, the analysis of reference sections of the Kurtak region, worked out in detail stratigraphically and published by previous researchers, made it possible to determine the stratigraphic position of megaflood strata based on the occurrence between subaerial packs with paleosols. The geochronometric, paleontological, and geoarchaeological characteristics of the sequence of the studied geological deposits are given. On the basis of systematization of already known materials and generalization of new field data, the presence of deposits of three megaflood strata in the Middle Yenisei Valley was established: Razlog (II4 rz), Chaninskaya (III2 chn), Divninskaya (III4 dv).
作者简介
I. Zolnikov
Sobolev Institute of Geology and Mineralogy Siberian Branch of the RAS; Novosibirsk state university
编辑信件的主要联系方式.
Email: zol@igm.nsc.ru
俄罗斯联邦, Novosibirsk; Novosibirsk
E. Filatov
Sobolev Institute of Geology and Mineralogy Siberian Branch of the RAS
Email: zol@igm.nsc.ru
俄罗斯联邦, Novosibirsk
I. Novikov
Sobolev Institute of Geology and Mineralogy Siberian Branch of the RAS
Email: zol@igm.nsc.ru
俄罗斯联邦, Novosibirsk
A. Shpansky
Sobolev Institute of Geology and Mineralogy Siberian Branch of the RAS; Tomsk State University
Email: zol@igm.nsc.ru
俄罗斯联邦, Novosibirsk; Tomsk
A. Klementyev
Institute of the Earth’s Crust Siberian Branch of the RAS
Email: zol@igm.nsc.ru
俄罗斯联邦, Irkutsk
A. Anoikin
Institute of Archaeology and Ethnography Siberian Branch of the RAS
Email: zol@igm.nsc.ru
俄罗斯联邦, Novosibirsk
A. Vybornov
Sobolev Institute of Geology and Mineralogy Siberian Branch of the RAS; Institute of Archaeology and Ethnography Siberian Branch of the RAS
Email: zol@igm.nsc.ru
俄罗斯联邦, Novosibirsk; Novosibirsk
N. Glushkov
Sobolev Institute of Geology and Mineralogy Siberian Branch of the RAS; Novosibirsk state university
Email: zol@igm.nsc.ru
俄罗斯联邦, Novosibirsk; Novosibirsk
A. Dzhumanov
Sobolev Institute of Geology and Mineralogy Siberian Branch of the RAS; Tomsk State University
Email: zol@igm.nsc.ru
俄罗斯联邦, Novosibirsk; Tomsk
E. Bordyugova
Sobolev Institute of Geology and Mineralogy Siberian Branch of the RAS; Novosibirsk state university
Email: zol@igm.nsc.ru
俄罗斯联邦, Novosibirsk; Novosibirsk
D. Rogozin
Sobolev Institute of Geology and Mineralogy Siberian Branch of the RAS; Novosibirsk state university
Email: zol@igm.nsc.ru
俄罗斯联邦, Novosibirsk; Novosibirsk
参考
- Arkhipov S.A. (1966). The problem of correlation of alluvial and glacial deposits: Yenisei terraces of the non-glacial zone of the West Siberian Lowland. In: Chetvertichnyi period Sibiri (The Quaternary period of Siberia). Moscow: Nauka (Publ.). P. 50–70. (in Russ.)
- Arkhipov S.A. (1971). Chetvertichnyi period v Zapadnoi Sibiri (The Quaternary period in Western Siberia). Novosibirsk: Nauka (Publ.). 1971. 329 p. (in Russ.).
- Arkhipov S.A., Gnibidenko Z.N., Zykina V.S. et. al. (1992). Geological structure and general strategy for chronostratigraphic study of the Kurtak archaeological region. In: Paleoekologiya i rasselenie drevnego cheloveka v Serernoi Azii i Amerike. Krasnoyarsk. 1992. P. 10–14. (in Russ.)
- Arkhipov S.A., Matveeva O.V. (1964). Antropogen yuzhnoi okrainy Yeniseiskoi depressii (Anthropogen of the southern margin of the Yenisei depression). Novosibirsk: SO RAN (Publ.). 127 p. (in Russ.)
- Arzhannikov S., Arzhannikova A., Braucher R., Komatsu G. (2023). Darhad megaflood (southern Siberia): Cause, age and consequence. Quat. Int. V. 643. P. 1–21. https://doi.org/10.1016/j.quaint.2022.10.002
- Arzhannikova A.V., Arzhannikov S.G., Akulova V.V. et. al. (2014). On the origin of sand deposits in the South Minusinsk basin. Geologiya i geofizika. V. 55. № 10. P. 1495–1508. https://doi.org/10.15372/GiG20141004. (in Russ.).
- Chekha V.P. (1990). Fossil soils of the Kurtak archaeological region. In: Kurtak archaeological region. Issue 3. New data on the chronostratigraphy of the Paleolithic of the Kurtak archaeological region. Krasnoyarsk: PA Siberia (Publ.). P. 19–32.
- Drozdov N.I., Chekha V.P., Khazarts P. (2005). Geomorfologiya i chetvertichnye otlozheniya Kurtakskogo geoarkheologicheskogo raiona (Severo-Minusinskaya vpadina) [Geomorphology and quaternary deposits of the Kurtak geoarchaeological region (North Minusinsk depression)] (Publ.). Krasnoyarsk: RIO. KGPU im. V.P. Astaf'yeva. 112 p. (in Russ.)
- Gorshkov S.P. (1966). On the stratigraphy of anthropogenic deposits of the extraglacial zone of the Yenisei Siberia. In: Chetvertichnyi period Sibiri. Moscow: Nauka (Publ.). P. 71–81. (in Russ.)
- Gorshkov S.P. (1986). The problem of comparing Pleistocene deposits of the extraglacial zone of Yenisei Siberia with events in the glacial zone. In: Chetvertichnye oledeneniya Srednei Sibiri. Moscow: Nauka (Publ.). P. 95–101. (in Russ.)
- Gorshkov S.P., Minervin A.V. (1966). Conditions for the formation of accumulative formations of a 30–40-meter “camp” terrace Yenisey. In: Chetvertichnyi period Sibiri. Moscow: Nauka (Publ.). P. 101–108. (in Russ.).
- Guskov S.A. (2009). Middle-Late Pleistocene marine transgressions in the north of Western Siberia. Byulleten’ komissii po izucheniyu chetvertichnogo perioda. Spetsial’nyi vypusk. Chetvertichnyi period Zapadnoi Sibiri: rezul’taty i problemy noveishikh issledovanii. № 69. Moscow: GEOS (Publ.). P. 40–47. (in Russ.)
- Kheraskov N.N., Anisimova N.D. (1963). Geologicheskaya karta masshtaba 1:200 000. Seriya Zapadno-Sayanskaya. List N-46-XXVI. Ob”yasnitel’naya zapiska (Geological map scale 1:200 000. West Sayan series. Sheet N-46-XXVI. Explanatory letter). Moscow: Gos. Nauchno-tekhnicheskoe izd-vo literatury po geologiii okhrane nedr (Publ.). 96 p. (in Russ.)
- Kind N.V. (1974). Geokhronologiya pozdnego antropogena po izotopnym dannym (Geochronology of the late anthropogen according to isotopic data). Moscow: Nauka (Publ.). 255 p. (in Russ.)
- Komatsu G., Arzhannikov S., Gillespie A., Burk R. et al. (2009). Quaternary paleolake formation and cataclysmic flooding along the upper Yenisei River. Geomorphology. V. 104. P. 143–164. https://doi.org/10.1016/j.geomorph.2008.08.009
- Krivonogov S.K., Yi.S., Kashiwaya K. et. al. (2012). Solved and unsolved problems of sedimentation, glaciocation and paleolakes of The Darhad Basin, Northen Mongolia. Quat. Sci. Rev. V. 56. P. 142–163. https://doi.org/10.1016/j.quascirev.2012.08.013
- Kurtakskiy arkheologicheskiy rayon (Kurtak archaeological region). Iss. 1. (1990 а). Krasnoyarsk: IAET SB RAS (Publ.). 88 p. (in Russ.)
- Kurtakskiy arkheologicheskiy rayon (Kurtak archaeological region). Iss. 2. (1990 б). Krasnoyarsk: IAET SB RAS (Publ.). 111 p. (in Russ.)
- Kurtakskiy arkheologicheskiy rayon (Kurtak archaeological region). Iss. 3. (1990 в). Krasnoyarsk: IAET SB RAS (Publ.). 113 p. (in Russ.)
- Mikharevich M.V., Shpansky A.V. (2021). Problems of age and genetic diagnosis of quaternary deposits in the valley of the middle reaches of the river. Yenisei (Yenisei-Nizhneangarsky stratigraphic area and the area of the Minusinsk basins). Geologiya i mineral’no-syr’evye resursy Sibiri. № 10c. P. 57–68. (in Russ.). https://doi.org/10.20403/2078-0575-2021-10c-57-68
- Novikov I.S. (2021). Changes in the global denudation basis in the late Mesozoic and Cenozoic and its influence on the formation of the geomorphological structure in areas with different neotectonic regimes. Geology and mineral resources of Siberia. № 10c. P. 68–84. https://doi.org/10.20403/2078-0575-2021-10c-69-85.
- Ravsky E.I. (1972). Osadkonakoplenie i klimaty Vnutrennei Azii v antropogene (Sedimentation and climates of Inner Asia in anthropogen). Moscow:: Nauka (Publ.). 334 p. (in Russ.)
- Resheniya Vsesoyuznogo stratigraficheskogo soveshchaniya po dokembriyu, paleozoyu i chetvertichnoi sisteme Srednei Sibiri (Novosibirsk, 1979 g.). Chast’ III. Chetvertichnaya sistema (Decisions of the All-Union Stratigraphic Meeting on the Precambrian, Paleozoic and Quaternary System of Central Siberia (Novosibirsk, 1979). Part III. The quaternary system). (1983) Leningrad: VSEGEI (Publ.). 84 p. (in Russ.)
- Sekretarev M.N., Lipishanov A.P., Mikhailenko V.V. et. al. (2015). Gosudarstvennaya geologicheskaya karta Rossiiskoi Federatsii. Masshtab 1:200 000. Izdanie vtoroe. Seriya Minusinskaya. List N-46-XIII (Sorsk). Ob”yasnitel’naya zapiska (State Geological Map of the Russian Federation. Scale 1:200 000. Second edition. The Minusinskaya series. Sheet N-46-XIII (Sorsk). Explanatory note). Moscow: MT VSEGEI (Publ.). 205 p. (in Russ.)
- Shatalina T.A., Sosnovskaya O.V., Alexandrovsky Yu.S., et.al. (2019). Gosudarstvennaya geologicheskaya karta Rossiiskoi Federatsii masshtaba 1:200 000. Izdanie vtoroe. Seriya Zapadno-Sayanskaya. List N-46-XXVI (Sayanogorsk). Ob”yasnitel’naya zapiska (State Geological Map of the Russian Federation scale 1:200 000. Second edition. The Western Sayan series. Sheet N-46-XXVI (Sayanogorsk). Explanatory note). St. Petersburg: VSEGEI (Publ.). 224 p. (in Russ.)
- Tseitlin S.M. (1979). Geologiya paleolita Severnoi Azii (Geology of the Paleolithic of Northern Asia). Moscow: Nauka (Publ.). 284 p. (in Russ.)
- Yamskikh A.F. (1993). Osadkonakoplenie terrasoobrazovanie v rechnykh dolinakh Yuzhnoi Sibiri (Sedimentation and terracing in the river valleys of Southern Siberia). Krasnoyarsk: KSPI (Publ.). 226 p. (in Russ.)
- Yendrikhinsky A.S. (1982). The sequence of the main geological events on the territory of Southern Siberia in the Late Pleistocene and Holocene. In: Pozdnii pleistotsen i golotsen yuga Vostochnoi Sibiri. Novosibirsk: Nauka (Publ.). P. 6–35. (in Russ.)
- Zander A., Frechen M., Zykina V., Boenigk W. (2003). Luminescence chronology of the Upper Pleistocene loess record at Kurtak in Middle Siberia. Quat. Sci Rev. V. 22. P. 999–1010.
- Zolnikov I.D., Novikov I.S., Deev E.V. et al. (2021). On the facies composition and stratigraphic position of the Quaternary Upper Yenisei strata in the Tuva and Minusinsk depressions. Geologiya i geofizika. V. 62. № 10. P. 1377–1390. (in Russ.). https://doi.org/10.15372/GiG2020186
- Zolnikov I.D., Vybornov A.V., Kirginekov E.N. et al. (2024). Super-flood deposits of the Upper Neopleistocene of the Koibal steppe (Minusinsk depression). Geosphere Research. № 1. P. 26–39.
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