gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2021-12-3-0538gtcrust-1239Research ArticleСОВРЕМЕННАЯ ГЕОДИНАМИКАRECENT GEODYNAMICSСЛЕДЫ ВЫСОКОЙ СЕЙСМИЧЕСКОЙ АКТИВНОСТИ В ПОВЕРХНОСТНЫХ ОТЛОЖЕНИЯХ ОЗЕРА БАЙКАЛ, СИБИРЬTRACES OF HIGH SEISMIC ACTIVITY IN THE UPPERMOST SEDIMENTS OF LAKE BAIKAL, SIBERIAВологинаЕ. Г.VologinaE. G.

664033, Иркутск, ул. Лермонтова, 128

128 Lermontov St, Irkutsk 664033

vologina@crust.irk.ruШтурмМ.SturmM.

CH-8600, Дюбендорф, п/я 611

CH-8600 Dubendorf, 611

РадзиминовичЯ. Б.RadziminovichYa. B.

664033, Иркутск, ул. Лермонтова, 128

128 Lermontov St, Irkutsk 664033

Институт земной коры СО РАНРоссияInstitute of the Earth’s Crust, Siberian Branch of the Russian Academy of ScienceRussian FederationШвейцарский федеральный институт науки и технологии окружающей средыШвейцарияSwiss Federal Institute of Aquatic Science and TechnologySwitzerland202117092021123544562Copyright © Вологина Е.Г., Штурм М., Радзиминович Я.Б., 20212021Вологина Е.Г., Штурм М., Радзиминович Я.Б.Vologina E.G., Sturm M., Radziminovich Y.B.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/1239

Осадконакопление в озере Байкал происходит на фоне постоянной сейсмической активности Байкальской рифтовой зоны. Современные и исторические землетрясения оказывают значительное влияние на формирование донных отложений в этом глубоком тектоническом бассейне. В статье представлены результаты международных исследований за период 1996–2019 гг. Для обнаружения следов сейсмических событий в самых верхних слоях отложений (<1.5 м) были отобраны короткие керны по всему озеру. Приведены карты с точками отбора кернов и сейсмичностью озера. Литологический состав, данные измерения магнитной восприимчивости, оценка органических и неорганических компонентов осадков позволяют определить индикаторы землетрясений в донных отложениях озера. Следы исторических землетрясений были обнаружены в пределах Южной котловины Байкала (районы станций Шарыжалгай и 106-й км Кругобайкальской железной дороги) и в заливе Провал рядом с дельтой р. Селенги.

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).

озеро Байкалосадконакоплениеземлетрясениедонные отложенияскорость осадконакопленияпелагический илтурбидитыокисленные слоиLake Baikalsedimentationearthquakebottom sedimentssedimentation ratepelagic mudturbiditesoxidized layersРабота выполнена при частичной поддержке EAWAG (проект № 85145) и в рамках тем госзадания ИЗК СО РАН (№ 0346-2019-0005, 0346-2018-0003). В работе частично задействовалось оборудование ЦКП «Геодинамика и геохронология» Института земной коры СО РАН.The research was partially supported by EAWAG and published under the state assignment of the Institute of the Earth’s Crust SB RAS (Tasks 0346-2019-0005 and 0346-2018-0003). In part, this work involved the equipment of the Centre of Geodynamics and Geochronology (Institute of the Earth's Crust, Siberian Branch of the Russian Academy of Sciences).ReferencesAshurkov S.V., Sankov V.A., Miroshnichenko A.I., Lukhnev A.V., Sorokin A.P., Serov M.A., Byzov L.M., 2011. 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The authors declare that there are no conflicts of interest present.