On analysis of signals of seismic acoustic emission of surface sedimentary rocks in kamchatka
Vestnik KRAUNC. Fiziko-matematičeskie nauki, Tome 34 (2021) no. 1, pp. 150-158 Cet article a éte moissonné depuis la source Math-Net.Ru

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In Kamchatka, at the observation point “Karymshina”, using a measuring system based on a three-component piezoceramic seismic receiver, the signals of seismoacoustic emission of near-surface sedimentary rocks are monitored. At the output of the measuring system, an oscillatory acceleration is recorded in the frequency range of 0.5-400 Hz. The analysis is based on records of seismoacoustic signals from several regional earthquakes in 2019 with an energy class of Ks > 10:0. The probability density distribution function of such a signal is not always described by the normal distribution law; therefore, statistical physics methods are suitable for studying such stochastic time series, within which the properties of self-similarity of these signals are considered.
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V. N. Sychev; M. E. Cheshev; M. A. Mishenko. On analysis of signals of seismic acoustic emission of surface sedimentary rocks in kamchatka. Vestnik KRAUNC. Fiziko-matematičeskie nauki, Tome 34 (2021) no. 1, pp. 150-158. http://geodesic.mathdoc.fr/item/VKAM_2021_34_1_a12/

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