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V. A. Pavlenov Ya. B. Radziminovich S. G. Arzhannikov A. S. Gladkov I. A. Dzyuba 《Journal of Volcanology and Seismology》2007,1(6):421-428
The present study is devoted to the assessment of shaking intensities due to the September 17, 2003, earthquake occurring in the Khoito-Gol basin (southwestern flank of the Baikal Rift System). The instrumental and macroseismic data used here were acquired during an investigation into the impact of this seismic event. The highest intensity of shaking, VI, was recorded at Khoito-Gol, the human settlement that was the nearest to the instrumental epicenter. A nonuniform distribution of intensity was found for different directions from the epicenter. A scatter of as much as two intensity units was recorded at one settlement. 相似文献
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Radziminovich Ya. B. Filippova A. I. Gileva N. A. Melnikova V. I. 《Izvestiya Atmospheric and Oceanic Physics》2022,58(8):936-953
Izvestiya, Atmospheric and Oceanic Physics - We study in detail the source parameters, seismotectonic position, and macroseismic effects of the February 3, 2016, earthquake that occurred in the... 相似文献
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The territory of Transbaikalia (Russia) is subject to occasional large-scale flooding. One of the most significant events in terms of scale and consequences is the historical flood that occurred in August 1897. In this article, we have tried to reconstruct the flood event. For this purpose, we have used all available historical sources (official statistical data, newspaper publications). The flood was observed almost simultaneously in two river basins (the Selenga and Shilka rivers). The main cause of the catastrophic flood was the abnormally intensive rainfall in the Hentey Mountains (Mongolia) and in Chikokonsky Ridge (southern Transbaikalia) in summer 1897. We have singled out four flood stages on the basis of the dates of flooding in different settlements. The flooding was accompanied by silting of considerable areas, and formation of new channels in local places. The flood in August 1897 in Transbaikalia, Russia, clearly demonstrated the vulnerability of both the environment and society to such catastrophic events. 相似文献
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Emanov A. F. Emanov A. A. Chechel’nitskii V. V. Shevkunova E. V. Radziminovich Ya. B. Fateev A. V. Kobeleva E. A. Gladyshev E. A. Arapov V. V. Artemova A. I. Podkorytova V. G. 《Izvestiya Physics of the Solid Earth》2022,58(3):443-443
Izvestiya, Physics of the Solid Earth - An Erratum to this paper has been published: https://doi.org/10.1134/S1069351322100019 相似文献
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We discuss historical evidence for seismicity on the southern margin of the Siberian craton collected from old local newspapers. The reported earthquakes vary in magnitude from M = 2.5 to 4.5, and their macroseismic locations agree well with the regional tectonic framework. The new data prove seismic activity in the area and can be used in seismic risk assessment. 相似文献
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Seismicity of the southern Siberian platform: Spatiotemporal characteristics and genesis 总被引：1，自引：0，他引：1
Analysis of instrumental data on earthquakes of 1960–2005 in the Irkutsk amphitheater shows that the majority of the earthquakes form a wide (150–300 km) band of diffuse seismicity along the marginal suture of the Siberian platform. In accordance with established regular spatiotemporal patterns of the distribution of earthquakes, this band belongs to the Sayan-Baikal seismic belt, associated with the destruction process at the boundary of large lithospheric blocks. The band is located on the northern periphery of the belt and, the deformable substrate being highly monolithic, this sharply weakens the seismicity within the band. Because of the tectonic origin of earthquakes in such a vast platform territory, undoubted evidence for induced seismicity around the Angara cascade reservoirs, and the intense economic development of the region, the problem of seismic hazard in the southern Siberian platform should be regarded as one of the most significant objects of geodynamic research. 相似文献
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Focal depths of earthquakes in the Baikal region: A review 总被引：3，自引：0，他引：3
N. A. Radziminovich 《Izvestiya Physics of the Solid Earth》2010,46(3):216-229
Conditions and specific features in the determination of the focal depths of the earthquakes in the Baikal region are considered.
Particular attention is given to the procedure of relocation of the hypocenters in accordance with the programs based on the
method of minimization of rms residuals in the seismic wave traveltimes, which is widely used at present. The advantages and
shortcomings of this approach are demonstrated. The available determinations of the source depths are reviewed, and examples
for the interpretation of the results are presented. The averaged depth distribution of the hypocenters shows that the strongest
seismic activity is observed in the depth range 10–20 km. The bottom of the seismically active layer corresponding to the
level, above which 90% of sources are located, lies at a depth of 25 km. The trend of the deepening of seismic sources is
observed at the northeast flank of the rift zone, where seismic activity involves the lower part of the crust. 相似文献