Aleksey Sidorchuk

Biographic Data

ID7713457
NAMEAleksey Sidorchuk
GIVEN NAMESAleksey
FAMILY NAMESidorchuk
SIGNATURESIDORCHUK A
AFFILIATIONSLomonosov Moscow State University
ORCID0000-0002-6750-5463
VERIFIEDYes
TOTAL WORKS4
TOTAL CITATIONS0
WORKS AS AUTHOR4
WORKS AS EDITOR0
FIRST PUBLICATION YEAR2020
LATEST PUBLICATION YEAR2024
H-INDEX0

  • Hydrological Regime of Rivers in the Periglacial Zone of the East European Plain in the Late MIS 2

    Open AccessAleksey Sidorchuk, A V Panin et al.ARTICLEQuaternary2024

    At the end of the Pleniglacial and the first half of the Late Glacial period, approximately between 18 and 14 ka BP, rivers of the central and southern parts of the East European Plain had channels up to 10 times as large as the present day channels of the same rivers. These ancient channels, called large meandering palaeochannels, are widespread in river floodplains and low terraces. The hydrological regime of these large rivers is of great inte…

  • The Processes of Aggradation and Incision in the Channels in the Terek River Basin, the North Caucasus

    Open AccessAleksey SidorchukARTICLEQuaternary2023

    The rates of incision and aggradation in the channels in the Terek River basin (North Caucasus) for the last 50–85 years were estimated at 18 gauging stations. The stage–discharge method (annual low water stages at the same discharges) was applied. The stability of the Terek River channel was recorded on the tectonically subsiding Tersko–Kuma Lowland. On the subsiding Kabardian Plain, channel aggradation up to 14 mm a−1 was registered. The rapid …

  • Evolution of the Upper Reaches of Fluvial Systems within the Area of the East European Plain Glaciated during MIS 6

    Open AccessA V Panin, Andrey Panin et al.ARTICLEQuaternary2022

    The headwaters of fluvial systems on the East European Plain between the boundaries of the Marine Isotope Stage 2 (MIS 2) and MIS 6 glaciations evolved during the last 150,000 years. At least three main events of high surface runoff caused intensive erosion: at the end of MIS 6, at the end of MIS 2 and in the Middle Holocene. Erosion developed in the territory with variable resistance of geological substrate, from hard-to-erode tills to weak sand…

  • The Late Quaternary Evolution of the Upper Reaches of Fluvial Systems in the Southern East European Plain

    Open AccessA V Panin, О К Борисова et al.ARTICLEQuaternary2020

    Networks of dry valleys (or balkas) and hollows in the upper reaches of fluvial basins in extraglacial areas in the Penultimate Glaciation (Marine Isotope Stage 6—MIS 6) regions of the East European Plain demonstrate clear incision/aggradation rhythms corresponding to global glacial/interglacial climate cycles. The first phase of each incision/aggradation rhythm began after the global glacial maximum and was characterized by a cool and humid clim…