Buried River Valleys of the Neogene and Early Quaternary in the Middle Volga Region, European Russia
Buried river valleys from the Neogene–Quaternary time are widespread throughout the Middle Volga region of the Russian Plain. They have been studied for a long period, since the 1940s, with the last major generalizations dating back to the 1980s. This paper presents new results based on GIS mapping...
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| Language: | English |
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MDPI AG
2023-04-01
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| Series: | Quaternary |
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| Online Access: | https://www.mdpi.com/2571-550X/6/2/29 |
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| author | Elena V. Petrova Artyom V. Gusarov Achim A. Beylich |
| author_facet | Elena V. Petrova Artyom V. Gusarov Achim A. Beylich |
| author_sort | Elena V. Petrova |
| collection | DOAJ |
| description | Buried river valleys from the Neogene–Quaternary time are widespread throughout the Middle Volga region of the Russian Plain. They have been studied for a long period, since the 1940s, with the last major generalizations dating back to the 1980s. This paper presents new results based on GIS mapping using materials from the state geological study of the region in 1960–1970, 1984–1996 and 2000–2002. On the whole, the pattern of the buried valley network is close to the modern valley network of the region. During the Quaternary, the right-sided displacement of the valley incisions prevailed. The incisions of modern river valleys are located above the Neogene (pre-Akchagyl) incisions almost throughout the entire territory. The vertical displacement amplitude ranges from 30 to 200 m. The morphometric characteristics of the paleovalleys (the depth and width of the incisions, as well as the gradients of the bottoms of the paleovalleys) exceeded modern ones. The maximum values were typical for the middle Paleo-Volga valley: the width of the valley reached 10 km, the incision depth was−201.4 m below sea level and the bottom gradient was 0.9–5.0 m/km. The most important factor that influenced the position of paleovalleys and their morphological appearance was fluctuations in the level of the Caspian paleowaterbody. According to this study, the development of paleovalleys began in the Miocene and ended in the Early Quaternary. The alluvial–lacustrine type of sedimentation was predominant. The results of this work contribute to the study of the paleogeography of the Cenozoic of the southeast of the Russian Plain. |
| first_indexed | 2024-03-11T01:59:32Z |
| format | Article |
| id | doaj.art-0753b0ab21a84e20b0f6ef80ecf9354d |
| institution | Directory Open Access Journal |
| issn | 2571-550X |
| language | English |
| last_indexed | 2024-03-11T01:59:32Z |
| publishDate | 2023-04-01 |
| publisher | MDPI AG |
| record_format | Article |
| series | Quaternary |
| spelling | doaj.art-0753b0ab21a84e20b0f6ef80ecf9354d2023-11-18T12:21:51ZengMDPI AGQuaternary2571-550X2023-04-01622910.3390/quat6020029Buried River Valleys of the Neogene and Early Quaternary in the Middle Volga Region, European RussiaElena V. Petrova0Artyom V. Gusarov1Achim A. Beylich2Institute of Environmental Sciences, Kazan Federal University, 420008 Kazan, RussiaInstitute of Geology and Petroleum Technologies, Kazan Federal University, 420008 Kazan, RussiaGeomorphological Field Laboratory (GFL), 7584 Selbustrand, NorwayBuried river valleys from the Neogene–Quaternary time are widespread throughout the Middle Volga region of the Russian Plain. They have been studied for a long period, since the 1940s, with the last major generalizations dating back to the 1980s. This paper presents new results based on GIS mapping using materials from the state geological study of the region in 1960–1970, 1984–1996 and 2000–2002. On the whole, the pattern of the buried valley network is close to the modern valley network of the region. During the Quaternary, the right-sided displacement of the valley incisions prevailed. The incisions of modern river valleys are located above the Neogene (pre-Akchagyl) incisions almost throughout the entire territory. The vertical displacement amplitude ranges from 30 to 200 m. The morphometric characteristics of the paleovalleys (the depth and width of the incisions, as well as the gradients of the bottoms of the paleovalleys) exceeded modern ones. The maximum values were typical for the middle Paleo-Volga valley: the width of the valley reached 10 km, the incision depth was−201.4 m below sea level and the bottom gradient was 0.9–5.0 m/km. The most important factor that influenced the position of paleovalleys and their morphological appearance was fluctuations in the level of the Caspian paleowaterbody. According to this study, the development of paleovalleys began in the Miocene and ended in the Early Quaternary. The alluvial–lacustrine type of sedimentation was predominant. The results of this work contribute to the study of the paleogeography of the Cenozoic of the southeast of the Russian Plain.https://www.mdpi.com/2571-550X/6/2/29paleoriverpaleovalleyvalley incisionsedimentationalluviumvalley morphometry |
| spellingShingle | Elena V. Petrova Artyom V. Gusarov Achim A. Beylich Buried River Valleys of the Neogene and Early Quaternary in the Middle Volga Region, European Russia Quaternary paleoriver paleovalley valley incision sedimentation alluvium valley morphometry |
| title | Buried River Valleys of the Neogene and Early Quaternary in the Middle Volga Region, European Russia |
| title_full | Buried River Valleys of the Neogene and Early Quaternary in the Middle Volga Region, European Russia |
| title_fullStr | Buried River Valleys of the Neogene and Early Quaternary in the Middle Volga Region, European Russia |
| title_full_unstemmed | Buried River Valleys of the Neogene and Early Quaternary in the Middle Volga Region, European Russia |
| title_short | Buried River Valleys of the Neogene and Early Quaternary in the Middle Volga Region, European Russia |
| title_sort | buried river valleys of the neogene and early quaternary in the middle volga region european russia |
| topic | paleoriver paleovalley valley incision sedimentation alluvium valley morphometry |
| url | https://www.mdpi.com/2571-550X/6/2/29 |
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