Abstract
The ground penetrating radar (GPR) and electrical resistivity tomography (ERT) geophysical methods were used for geological mapping, location of lithological boundaries, and description of the inner structure of sediments of the Upper Dnieper zone, as well as for locating optimal sites for drilling and correlating borehole cores. The geophysical information we obtained allowed restructuring of the upper Dnieper valley due to Valdaian glaciation to be identified. The GPR data in the frequency range of 50–250 MHz enabled description of the upper part of the geological section; ERT provided data up to a 80–100-m depth. Modified focusing inversion based on the major boundaries obtained with GPR was performed to correct the ERT inversion model.
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ACKNOWLEDGEMENTS
The authors express their gratitude to the staff of the Contemporary Problems of Geophysics seminar and personally to Professor M.L. Vladov for fruitful discussions of the research results. We would like to thank the staff and students of the Departments of Geology and Geography of the Moscow State University: D.K. Bolshakov, D.V. Shmurak, N. Korneeva, G. Titov, D. Minyaylov, A. Kuvinov and T. Saetgoreyev for their assistance in field work and geodetic survey.
Funding
The research was carried out with the financial support of the Russian Science Foundation (project no. 17-17-01289). Data processing was performed using the infrastructure of IGRAS within the framework of the State Task Force 0148-2019-0005.
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Translated by M. Hannibal
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Bricheva, S.S., Modin, I.N., Panin, A.V. et al. The Structure of Quaternary Deposits in the Upper Dnieper Valley According to Integrated (Combined) Geophysical Data. Moscow Univ. Geol. Bull. 75, 413–424 (2020). https://doi.org/10.3103/S014587522004002X
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DOI: https://doi.org/10.3103/S014587522004002X