Author:
Dobrynina A. A.,Sankov V. A.,Bornyakov S. A.,Korol S. A.,Sankov A. V.
Abstract
Abstract
Studies have been conducted on the variations of microseismic noise recorded by broadband and short-period seismic stations in the area of South Baikal before and after the large December 9, 2020 Kudara earthquake with Mw = 5.6. Ten days before the earthquake, there was a gradual increase of oscillation amplitudes in the frequency range from 0.01 to 0.1 Hz, with an increasing background observed also during 4 days after the main shock (period from December 1, 2020 to January 12, 2021). The maximum amplitude increase is 19.5 against the background. During this time, there were recorded 48 aftershocks. The analysis of direction of particle motion in seismic waves over the reporting period showed an abrupt change in the orientation of oscillations, which is fully consistent with the azimuth for the main shock epicenter. The analysis of seismograms over the next period (from December 13) did not show similar effects in the microseismic noise field. Apparently, the microseismic noise field reflected the process of slow faulting before the earthquake and after the main shock with subsequent attenuation.
Subject
General Earth and Planetary Sciences,Earth and Planetary Sciences (miscellaneous)
Reference14 articles.
1. V. A. Saltykov, Izv., Phys. Solid Earth 53 (2), 250–261 (2017).
2. G. A. Sobolev, Izv., Phys. Solid Earth 40 (6), 455–464 (2004).
3. G. A. Sobolev, A. A. Lyubushin, and N. A. Zakrzhevskaya, J. Volcanol. Seismol. 2, 118–134 (2008).
4. A. A. Lyubushin, Geofiz. Protsessy Biosfera 10 (1), 9–35 (2011).
5. G. A. Sobolev, The Concept of Earthquake Predictability on the Base of Seismicity Dynamics under Trigger Impact (Schmidt Inst. Phys. Earth Earth, Moscow, 2011) [in Russian].