The influence of the Early Khvalynian transgression of the Caspian Sea on the structure of the Volga River and its tributaries valleys (Maliy Karaman key site, Saratov Region)
https://doi.org/10.31857/S2949178925010069
EDN: DNXQPH
Abstract
The Early Khvalynian transgression of the Caspian Sea is one of the largest in the late Pleistocene. In connection with this, an extensive paleo-estuary was formed in the valley of the Volga River and its tributaries. The formation of terraces in the river valleys of the region is thus closely related to the transgressive-regressive dynamics of the Caspian Sea. This paper examines a key section of the river valley. Maliy Karaman (left tributary of the Volga River), its morphology and structure, lithological composition and age of the sediments composing the terraces, to establish the influence of the Early Khvalynian transgression of the Caspian Sea on the structure of the valley.
Keywords
About the Authors
R. R. MakshaevRussian Federation
E. Yu. Matlakhova
Russian Federation
N. T. Tkach
Russian Federation
D. M. Lobacheva
Russian Federation
I. E. Lysenko
Russian Federation
A. A. Tkach
Russian Federation
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For citations:
Makshaev R.R., Matlakhova E.Yu., Tkach N.T., Lobacheva D.M., Lysenko I.E., Tkach A.A. The influence of the Early Khvalynian transgression of the Caspian Sea on the structure of the Volga River and its tributaries valleys (Maliy Karaman key site, Saratov Region). Geomorfologiya i Paleogeografiya. 2025;56(1):116-129. (In Russ.) https://doi.org/10.31857/S2949178925010069. EDN: DNXQPH