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Doklady Earth Sciences - 相似文献
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Boyarskikh I. G. Agatova A. R. Syso A. I. Klyuchevskaya A. I. 《Izvestiya Atmospheric and Oceanic Physics》2020,56(8):773-798
Izvestiya, Atmospheric and Oceanic Physics - Integrated geological, geophysical, geochemical, and botanical studies in the Kuraika River Valley (Kurai Ridge, Gorny Altai) have revealed sharp... 相似文献
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Klyuchevskii A. V. Demyanovich V. M. Klyuchevskaya A. A. 《Doklady Earth Sciences》2012,442(1):130-134
Based on the general physical nature of tsunami generation, it is established that it is an attribute of seismically hazardous
areas and regions adjacent to large water reservoirs and is threatening to the population and infrastructure of the coastal
zones. The main preconditions and possibilities for the occurrence of tsunami on Lake Baikal are considered: the information
on earthquakes in the Baikal hollow during the instrumental-historical period (1724–2011) is generalized in the map of epicenters
of shocks of magnitude M ⩾ 5 and histograms of the distribution of numbers of shocks with respect to magnitude. It is shown that the tsunami waves
start forming on Baikal if the earthquake magnitude M is ≈5, but since a system of tsunami monitoring on Baikal is absent,
it can be observed only during the strongest earthquakes of M > 7. The catastrophic Tsagan earthquake (1861, M ≈ 7.5) is given as an example. It happened near the eastern coast of Lake Baikal and caused a tsunami with people’s deaths. 相似文献
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