ESTIMATION OF LONG-RANGE CORRELATION SCALES BY SEISMOACOUSTIC EMISSION SIGNALS OF NEAR-SURFACE SEDIMENTARY ROCKS IN KAMCHATKA

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...

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Main Authors: V. N. Sychev, M. A. Mishchenko, S. A. Imashev, M. E. Cheshev
Format: Article
Language:English
Published: KamGU by Vitus Bering 2019-11-01
Series:Vestnik KRAUNC: Fiziko-Matematičeskie Nauki
Subjects:
Online Access:http://krasec.ru/wp-content/uploads/2020/01/%D0%A1%D1%8B%D1%87%D0%B5%D0%B2.pdf
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spelling doaj-aeee69989fc849c9b7528aeb6e2c0a342020-11-25T02:54:27ZengKamGU by Vitus BeringVestnik KRAUNC: Fiziko-Matematičeskie Nauki2079-66412079-665X2019-11-0129419020010.26117/2079-6641-2019-29-4-190-200ESTIMATION OF LONG-RANGE CORRELATION SCALES BY SEISMOACOUSTIC EMISSION SIGNALS OF NEAR-SURFACE SEDIMENTARY ROCKS IN KAMCHATKAV. N. Sychev0https://orcid.org/0000-0001-7508-9087M. A. Mishchenko1S. A. Imashev2https://orcid.org/0000-0003-3293-3764M. E. Cheshev3https://orcid.org/0000-0001-7902-4934Research Station RAS, 720049, Bishkek-49, KyrgyzstanInstitute of Cosmophysical Researches and Radio Wave Propagation FEB RAS, 684034, Kamchatsky Kray, Paratunka, Mirnaya st., 7, RussiaResearch Station RAS, 720049, Bishkek-49, KyrgyzstanResearch Station RAS, 720049, Bishkek-49, KyrgyzstanA 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.http://krasec.ru/wp-content/uploads/2020/01/%D0%A1%D1%8B%D1%87%D0%B5%D0%B2.pdfgeoacoustic noisestructural functionsautocorrelationcorrelation scalesself-similarity
collection DOAJ
language English
format Article
sources DOAJ
author V. N. Sychev
M. A. Mishchenko
S. A. Imashev
M. E. Cheshev
spellingShingle V. N. Sychev
M. A. Mishchenko
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
geoacoustic noise
structural functions
autocorrelation
correlation scales
self-similarity
author_facet V. N. Sychev
M. A. Mishchenko
S. A. Imashev
M. E. Cheshev
author_sort V. N. Sychev
title ESTIMATION OF LONG-RANGE CORRELATION SCALES BY SEISMOACOUSTIC EMISSION SIGNALS OF NEAR-SURFACE SEDIMENTARY ROCKS IN KAMCHATKA
title_short ESTIMATION OF LONG-RANGE CORRELATION SCALES BY SEISMOACOUSTIC EMISSION SIGNALS OF NEAR-SURFACE SEDIMENTARY ROCKS IN KAMCHATKA
title_full ESTIMATION OF LONG-RANGE CORRELATION SCALES BY SEISMOACOUSTIC EMISSION SIGNALS OF NEAR-SURFACE SEDIMENTARY ROCKS IN KAMCHATKA
title_fullStr ESTIMATION OF LONG-RANGE CORRELATION SCALES BY SEISMOACOUSTIC EMISSION SIGNALS OF NEAR-SURFACE SEDIMENTARY ROCKS IN KAMCHATKA
title_full_unstemmed ESTIMATION OF LONG-RANGE CORRELATION SCALES BY SEISMOACOUSTIC EMISSION SIGNALS OF NEAR-SURFACE SEDIMENTARY ROCKS IN KAMCHATKA
title_sort estimation of long-range correlation scales by seismoacoustic emission signals of near-surface sedimentary rocks in kamchatka
publisher KamGU by Vitus Bering
series Vestnik KRAUNC: Fiziko-Matematičeskie Nauki
issn 2079-6641
2079-665X
publishDate 2019-11-01
description 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.
topic geoacoustic noise
structural functions
autocorrelation
correlation scales
self-similarity
url http://krasec.ru/wp-content/uploads/2020/01/%D0%A1%D1%8B%D1%87%D0%B5%D0%B2.pdf
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