Lake Gusinoye (the southern part of East Siberia, Russia): sedimentary history inferred from high-resolution reflection seismic data

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Abstract

This paper studies the formation of the sediment cover in Lake Gusinoye. For this purpose, we used high-resolution seismic data. Depression of Lake Gusinoye has a tectonic origin; however, there is no evidence of recent tectonic activity. Sediment thickness in Lake Gusinoye is less than 9 m, and its history is short (<35-45 ka). In addition, seismic stratigraphy records contain three contrasting episodes when the lake level dramatically decreased. It is very likely that there were also other shorter episodes of low-level stands. Thus, seismic structures of lakes Gusinoye and Kotokel have a strong resemblance, and it is most likely that their history began at the same time, ca. 40 ka BP.

About the authors

D. A. Chensky

National Research Irkutsk State Technical University

Email: mix@lin.irk.ru
Russian Federation, Lermontov st., 83, Irkutsk

K. A. Grigorev

Boreskov Institute of Catalysis the Siberian Branch of RAS

Email: mix@lin.irk.ru
Russian Federation, Lavrentiev Ave. 5 Novosibirsk

A. G. Chensky

National Research Irkutsk State Technical University

Email: mix@lin.irk.ru
Russian Federation, Lermontov st., 83, Irkutsk

E. V. Parkhomchuk

Boreskov Institute of Catalysis the Siberian Branch of RAS

Email: mix@lin.irk.ru
Russian Federation, Lavrentiev Ave. 5 Novosibirsk

A. P. Fedotov

Limnological Institute of the Siberian Branch of the Russian Academy of Sciences

Author for correspondence.
Email: mix@lin.irk.ru
Russian Federation, Ulan-Batorskaya 3, 664 033 Irkutsk

References

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Copyright (c) 2019 Chensky D.A., Grigorev K.A., Chensky A.G., Parkhomchuk E.V., Fedotov A.P.

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