Geodesic
Estimation of long-range correlation scales by seismoacoustic emission signals of near-surface sedimentary rocks in Kamchatka
Vestnik KRAUNC. Fiziko-matematičeskie nauki, Tome 29 (2019) no. 4, pp. 190-200 
V. N. Sychev; M. A. Mishenko; S. A. Imashev; M. E. Cheshev. Estimation of long-range correlation scales by seismoacoustic emission signals of near-surface sedimentary rocks in Kamchatka. Vestnik KRAUNC. Fiziko-matematičeskie nauki, Tome 29 (2019) no. 4, pp. 190-200. http://geodesic.mathdoc.fr/item/VKAM_2019_29_4_a19/
@article{VKAM_2019_29_4_a19,
     author = {V. N. Sychev and M. A. Mishenko and S. A. Imashev and M. E. Cheshev},
     title = {Estimation of long-range correlation scales by seismoacoustic emission signals of near-surface sedimentary rocks in {Kamchatka}},
     journal = {Vestnik KRAUNC. Fiziko-matemati\v{c}eskie nauki},
     pages = {190--200},
     year = {2019},
     volume = {29},
     number = {4},
     language = {ru},
     url = {http://geodesic.mathdoc.fr/item/VKAM_2019_29_4_a19/}
}
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%A M. E. Cheshev
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Voir la notice de l'article provenant de la source Math-Net.Ru

A measurement complex is installed on the ground surface at Karymshina complex geophysical observation site of IKIR FEB RAS (Kamchatka) to record seismoacoustic emission signals. A three-component piezoceramic seismic receiver, which records oscillatory acceleration in the frequency range from 0.2 to 400 Hz, is used as the signal sensor. A series of seismoacoustic responses on regional earthquakes of 2017-2018 with the energy class Ks 11:0 has been considered. Self-similarity of their structures has been established in a limited interval of time scales by statistical methods. That, in its turn, indicates the presence of long-range correlations in the system under consideration and allows one to estimate correlation scales.

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