Email this article The Study of Sub-Bottom Sediments in Petrozavodsk Bay of Lake Onega Using Complex Geological-Geophysical Methods of Data Analysis
- Authors: Aleshin M.I.1,2, Gaynanov V.G.1, Tokarev M.J.1, Rybalko A.E.3, Subetto D.A.4
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Affiliations:
- Department of Geology, Moscow State University
- Split Scientific Company
- Institute of Earth Sciences, St. Petersburg State University
- Institute of Water Problems of the North, Karelian Research Center, Russian Academy of Sciences
- Issue: Vol 74, No 5 (2019)
- Pages: 525-531
- Section: Short Communications
- URL: https://journals.rcsi.science/0145-8752/article/view/175085
- DOI: https://doi.org/10.3103/S0145875219050028
- ID: 175085
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Abstract
The results of geological interpretation of data of engineering seismic surveys obtained during the field works at Lake Onega are given. Seismic-stratigraphic units specified on processed seismograms are characterized. The survey enabled us to compile a seismic-stratigraphic column of the Quaternary sediments of Lake Onega, which may be used to analyze the structure of the open part of the lake.
About the authors
M. I. Aleshin
Department of Geology, Moscow State University; Split Scientific Company
Author for correspondence.
Email: maan@ifz.ru
Russian Federation, Moscow, 119991; Moscow, 121205
V. G. Gaynanov
Department of Geology, Moscow State University
Email: maan@ifz.ru
Russian Federation, Moscow, 119991
M. J. Tokarev
Department of Geology, Moscow State University
Email: maan@ifz.ru
Russian Federation, Moscow, 119991
A. E. Rybalko
Institute of Earth Sciences, St. Petersburg State University
Email: maan@ifz.ru
Russian Federation, St. Petersburg, 199178
D. A. Subetto
Institute of Water Problems of the North, Karelian Research Center, Russian Academy of Sciences
Email: maan@ifz.ru
Russian Federation, Petrozavodsk, 185000
