TRACES OF HIGH SEISMIC ACTIVITY IN THE UPPERMOST SEDIMENTS OF LAKE BAIKAL, SIBERIA
Sedimentation in Lake Baikal is significantly affected by continuous seismic activity in the Baikal Rift Zone. Our study shows that historical earthquakes, as well as recent seismic events, considerably influenced sedimentation in this deep tectonic basin. Here we present some of the results of exte...
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Formato: | Artículo |
Lenguaje: | English |
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Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
2021-09-01
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Colección: | Геодинамика и тектонофизика |
Materias: | |
Acceso en línea: | https://www.gt-crust.ru/jour/article/view/1239 |
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author | E. G. Vologina M. Sturm Ya. B. Radziminovich |
author_facet | E. G. Vologina M. Sturm Ya. B. Radziminovich |
author_sort | E. G. Vologina |
collection | DOAJ |
description | Sedimentation in Lake Baikal is significantly affected by continuous seismic activity in the Baikal Rift Zone. Our study shows that historical earthquakes, as well as recent seismic events, considerably influenced sedimentation in this deep tectonic basin. Here we present some of the results of extensive international research activities during the period of 1996–2019. To identify traces of seismic events in the uppermost sediments (<1.5 m), short cores were recovered from many coring stations throughout the entire lake. Based on lithological descriptions, measurements of magnetic susceptibility, and concentration of inorganic and organic components, we identified earthquake indicators in the sediment cores. Impacts of historical earthquakes were traced within South Baikal (near the Sharyzhalgai Station and the Station 106-km of the Circum-Baikal railway, hereafter CBR) and Proval Bay (near the Selenga River delta). |
first_indexed | 2024-04-09T20:27:15Z |
format | Article |
id | doaj.art-02a6a64a81a04cc5801b415d894c1dcb |
institution | Directory Open Access Journal |
issn | 2078-502X |
language | English |
last_indexed | 2025-03-14T08:29:34Z |
publishDate | 2021-09-01 |
publisher | Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust |
record_format | Article |
series | Геодинамика и тектонофизика |
spelling | doaj.art-02a6a64a81a04cc5801b415d894c1dcb2025-03-02T13:02:50ZengRussian Academy of Sciences, Siberian Branch, Institute of the Earth's crustГеодинамика и тектонофизика2078-502X2021-09-0112354456210.5800/GT-2021-12-3-0538539TRACES OF HIGH SEISMIC ACTIVITY IN THE UPPERMOST SEDIMENTS OF LAKE BAIKAL, SIBERIAE. G. Vologina0M. Sturm1Ya. B. Radziminovich2Institute of the Earth’s Crust, Siberian Branch of the Russian Academy of ScienceSwiss Federal Institute of Aquatic Science and TechnologyInstitute of the Earth’s Crust, Siberian Branch of the Russian Academy of ScienceSedimentation in Lake Baikal is significantly affected by continuous seismic activity in the Baikal Rift Zone. Our study shows that historical earthquakes, as well as recent seismic events, considerably influenced sedimentation in this deep tectonic basin. Here we present some of the results of extensive international research activities during the period of 1996–2019. To identify traces of seismic events in the uppermost sediments (<1.5 m), short cores were recovered from many coring stations throughout the entire lake. Based on lithological descriptions, measurements of magnetic susceptibility, and concentration of inorganic and organic components, we identified earthquake indicators in the sediment cores. Impacts of historical earthquakes were traced within South Baikal (near the Sharyzhalgai Station and the Station 106-km of the Circum-Baikal railway, hereafter CBR) and Proval Bay (near the Selenga River delta).https://www.gt-crust.ru/jour/article/view/1239lake baikalsedimentationearthquakebottom sedimentssedimentation ratepelagic mudturbiditesoxidized layers |
spellingShingle | E. G. Vologina M. Sturm Ya. B. Radziminovich TRACES OF HIGH SEISMIC ACTIVITY IN THE UPPERMOST SEDIMENTS OF LAKE BAIKAL, SIBERIA Геодинамика и тектонофизика lake baikal sedimentation earthquake bottom sediments sedimentation rate pelagic mud turbidites oxidized layers |
title | TRACES OF HIGH SEISMIC ACTIVITY IN THE UPPERMOST SEDIMENTS OF LAKE BAIKAL, SIBERIA |
title_full | TRACES OF HIGH SEISMIC ACTIVITY IN THE UPPERMOST SEDIMENTS OF LAKE BAIKAL, SIBERIA |
title_fullStr | TRACES OF HIGH SEISMIC ACTIVITY IN THE UPPERMOST SEDIMENTS OF LAKE BAIKAL, SIBERIA |
title_full_unstemmed | TRACES OF HIGH SEISMIC ACTIVITY IN THE UPPERMOST SEDIMENTS OF LAKE BAIKAL, SIBERIA |
title_short | TRACES OF HIGH SEISMIC ACTIVITY IN THE UPPERMOST SEDIMENTS OF LAKE BAIKAL, SIBERIA |
title_sort | traces of high seismic activity in the uppermost sediments of lake baikal siberia |
topic | lake baikal sedimentation earthquake bottom sediments sedimentation rate pelagic mud turbidites oxidized layers |
url | https://www.gt-crust.ru/jour/article/view/1239 |
work_keys_str_mv | AT egvologina tracesofhighseismicactivityintheuppermostsedimentsoflakebaikalsiberia AT msturm tracesofhighseismicactivityintheuppermostsedimentsoflakebaikalsiberia AT yabradziminovich tracesofhighseismicactivityintheuppermostsedimentsoflakebaikalsiberia |