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Yan B. Radziminovich

Researcher at Russian Academy of Sciences

Publications -  7
Citations -  53

Yan B. Radziminovich is an academic researcher from Russian Academy of Sciences. The author has contributed to research in topics: Seismic moment & Focal mechanism. The author has an hindex of 4, co-authored 7 publications receiving 30 citations.

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The M w 4.3 January 17, 2014, earthquake: very rare seismic event on the Siberian platform

TL;DR: In this paper, the authors described the 2014 January 17 earthquake on the Siberian platform in the area of sublongitudinal part of the Angara river in the zone of possible influence of two large reservoirs.
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Seismicity of the Erguna Region (Northeastern China): Evidence for Local Stress Redistribution

TL;DR: In this paper, the authors considered the seismicity of the Erguna region in northeast China and calculated focal parameters (focal mechanisms, scalar seismic moments, moment magnitudes, and hypocentral depths) for seven regional earthquakes with Mw 4.2-4.6.
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The February 1, 2011 M w 4.7 earthquake: Evidence of local extension in western Transbaikalia (Eastern Siberia)

TL;DR: In this article, the authors considered the rare February 1, 2011 earthquake M w 4.7 that occurred in the low active region of western Transbaikalia, Russia and calculated earthquake source parameters (hypocentral depth, moment magnitude, scalar seismic moment and focal mechanism) from the data on amplitude spectra of surface waves and the first body-wave arrivals recorded on regional stations.
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Source process of the September 21, 2020 Mw 5.6 Bystraya earthquake at the South-Eastern segment of the main Sayan fault (Eastern Siberia, Russia)

TL;DR: In this article, the authors study the Mw 5.6 Bystraya earthquake and its largest aftershock, which occurred on September 21, 2020 at the SW flank of the Baikal rift zone in the area, in which only few small seismic events have been detected during the whole period of instrumental observations.
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The catastrophic flood in Transbaikalia (Central Asia) in 1897: case study

TL;DR: In this article, the authors tried to reconstruct the flood event in Transbaikalia using all available historical sources (official statistical data, newspaper publications) and found that the flood was observed almost simultaneously in two river basins (the Selenga and Shilka rivers) and that the main cause of the catastrophic flood was the abnormally intensive rainfall in the Hentey Mountains (Mongolia) and in Chikokonsky Ridge (southern Transbaiya) in summer 1897.