КФУ. Карточка публикации. Buried River Valleys of the Neogene and Early Quaternary in the Middle Volga Region, European Russia

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BURIED RIVER VALLEYS OF THE NEOGENE AND EARLY QUATERNARY IN THE MIDDLE VOLGA REGION, EUROPEAN RUSSIA

Форма представления

Статьи в зарубежных журналах и сборниках

Год публикации

2023

Язык

английский

Авторы, сотрудники КФУ

Гусаров Артем Викторович, автор

Петрова Елена Витальевна, автор

Другие авторы

Beylich Achim , автор

Библиографическое описание на языке оригинала

Petrova, E.V.; Gusarov, A.V.; Beylich, A.A. Buried River Valleys of the Neogene and Early Quaternary in the Middle Volga Region, European Russia // Quaternary, 2023, 6, 29.

Аннотация

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.

Ключевые слова

Paleoriver; paleovalley; valley incision; sedimentation; alluvium; valley morphometry; Miocene; Pliocene; Pleistocene; Akchagyl; Kama River; Caspian Sea; Russian Plain

Название журнала

Quaternary

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https://repository.kpfu.ru/?p_id=283907

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Полная запись метаданных

Поле DC	Значение	Язык
dc.contributor.author	Гусаров Артем Викторович	ru_RU
dc.contributor.author	Петрова Елена Витальевна	ru_RU
dc.contributor.author	Beylich Achim	ru_RU
dc.date.accessioned	2023-01-01T00:00:00Z	ru_RU
dc.date.available	2023-01-01T00:00:00Z	ru_RU
dc.date.issued	2023	ru_RU
dc.identifier.citation	Petrova, E.V.; Gusarov, A.V.; Beylich, A.A. Buried River Valleys of the Neogene and Early Quaternary in the Middle Volga Region, European Russia // Quaternary, 2023, 6, 29.	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/?p_id=283907	ru_RU
dc.description.abstract	Quaternary	ru_RU
dc.description.abstract	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.	ru_RU
dc.language.iso	ru	ru_RU
dc.subject		ru_RU
dc.title	Buried River Valleys of the Neogene and Early Quaternary in the Middle Volga Region, European Russia	ru_RU
dc.type	Статьи в зарубежных журналах и сборниках	ru_RU