The Study of Sub-Bottom Sediments in Petrozavodsk Bay of Lake Onega Using Complex Geological-Geophysical Methods of Data Analysis
- Autores: 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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Afiliações:
- 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
- Edição: Volume 74, Nº 5 (2019)
- Páginas: 525-531
- Seção: 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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Resumo
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.
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Sobre autores
M. Aleshin
Department of Geology, Moscow State University; Split Scientific Company
Autor responsável pela correspondência
Email: maan@ifz.ru
Rússia, Moscow, 119991; Moscow, 121205
V. Gaynanov
Department of Geology, Moscow State University
Email: maan@ifz.ru
Rússia, Moscow, 119991
M. Tokarev
Department of Geology, Moscow State University
Email: maan@ifz.ru
Rússia, Moscow, 119991
A. Rybalko
Institute of Earth Sciences, St. Petersburg State University
Email: maan@ifz.ru
Rússia, St. Petersburg, 199178
D. Subetto
Institute of Water Problems of the North, Karelian Research Center, Russian Academy of Sciences
Email: maan@ifz.ru
Rússia, Petrozavodsk, 185000
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