2019
DOI: 10.1134/s1069351319050094
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Joint Perturbation in Geoacoustic Emission, Radon, Thoron, and Atmospheric Electric Field Based on Observations in Kamchatka

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Cited by 9 publications
(2 citation statements)
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“…It was shown in [1,2] that AE intensity increases at the frequency of 25 kHz 2-3 days before strong earthquakes. According to [19,20], anomalies in the form of signal level increase appear in the frequency range of more than 6.5 kHz in the AE signals accumulated by 1 s. The results of time-frequency analysis of single AE pulses registered 1-7 days before earthquakes are presented in [21,22]. According to these results, the number of pulses of a certain frequency increases before strong earthquakes.…”
Section: Examples Of Identification Of Pre-seismic Ae Anomaliesmentioning
confidence: 99%
“…It was shown in [1,2] that AE intensity increases at the frequency of 25 kHz 2-3 days before strong earthquakes. According to [19,20], anomalies in the form of signal level increase appear in the frequency range of more than 6.5 kHz in the AE signals accumulated by 1 s. The results of time-frequency analysis of single AE pulses registered 1-7 days before earthquakes are presented in [21,22]. According to these results, the number of pulses of a certain frequency increases before strong earthquakes.…”
Section: Examples Of Identification Of Pre-seismic Ae Anomaliesmentioning
confidence: 99%
“…Continuous monitoring of geophysical signals at various stages of the deformation process has been carried out for more than 20 years at the IKIR FEB RAS geodynamic polygon in the seismically active region (Kamchatka Peninsula). The dynamics of pulse flow parameters of the recorded geophysical signals can be considered as an indicator of the stress-strain state of the geophysical system that generates these signals [1][2][3][4].…”
Section: Introductionmentioning
confidence: 99%