Analysis of the seismic process of the Bishkek geodynamic test site (Northern Tien Shan)

Various characteristics of seismic process on the territory of Bishkek geodynamic proving ground are considered. Seismicity analysis is performed on the basis of earthquake catalogue, according to KNET network data. The catalog includes more than 10,000 seismic events that occurred from 1994 to 2019...

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Main Authors: Sychev Vladimir, Sycheva Naylya
Format: Article
Language:English
Published: EDP Sciences 2020-01-01
Series:E3S Web of Conferences
Online Access:https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/56/e3sconf_strpep2020_02006.pdf
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spelling doaj-9c0e4c8634474b6aa66ffb849006ff692021-04-02T12:22:41ZengEDP SciencesE3S Web of Conferences2267-12422020-01-011960200610.1051/e3sconf/202019602006e3sconf_strpep2020_02006Analysis of the seismic process of the Bishkek geodynamic test site (Northern Tien Shan)Sychev VladimirSycheva NaylyaVarious characteristics of seismic process on the territory of Bishkek geodynamic proving ground are considered. Seismicity analysis is performed on the basis of earthquake catalogue, according to KNET network data. The catalog includes more than 10,000 seismic events that occurred from 1994 to 2019. To describe the energy distribution function of earthquakes, the Gutenberg - Richter law was used, as well as the position of nonequilibrium thermodynamics with the use of Tsallis statistics, which generalizes classical thermodynamics to the case of nonextensive systems. It is shown that the flow of earthquakes on the territory of the Bishkek geodynamic proving ground is a system with memory and long-range spatial correlations, and the study region itself is characterized as seismically active. The following seismic process characteristics are distributed in space and in time: KSR seismogenic fracture parameter, seismotectonic deformation intensity, seismic activity, Tsallis parameter q and constants a, as well as a parameter characterizing the slope of the repeatability graph (b-value).https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/56/e3sconf_strpep2020_02006.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Sychev Vladimir
Sycheva Naylya
spellingShingle Sychev Vladimir
Sycheva Naylya
Analysis of the seismic process of the Bishkek geodynamic test site (Northern Tien Shan)
E3S Web of Conferences
author_facet Sychev Vladimir
Sycheva Naylya
author_sort Sychev Vladimir
title Analysis of the seismic process of the Bishkek geodynamic test site (Northern Tien Shan)
title_short Analysis of the seismic process of the Bishkek geodynamic test site (Northern Tien Shan)
title_full Analysis of the seismic process of the Bishkek geodynamic test site (Northern Tien Shan)
title_fullStr Analysis of the seismic process of the Bishkek geodynamic test site (Northern Tien Shan)
title_full_unstemmed Analysis of the seismic process of the Bishkek geodynamic test site (Northern Tien Shan)
title_sort analysis of the seismic process of the bishkek geodynamic test site (northern tien shan)
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2020-01-01
description Various characteristics of seismic process on the territory of Bishkek geodynamic proving ground are considered. Seismicity analysis is performed on the basis of earthquake catalogue, according to KNET network data. The catalog includes more than 10,000 seismic events that occurred from 1994 to 2019. To describe the energy distribution function of earthquakes, the Gutenberg - Richter law was used, as well as the position of nonequilibrium thermodynamics with the use of Tsallis statistics, which generalizes classical thermodynamics to the case of nonextensive systems. It is shown that the flow of earthquakes on the territory of the Bishkek geodynamic proving ground is a system with memory and long-range spatial correlations, and the study region itself is characterized as seismically active. The following seismic process characteristics are distributed in space and in time: KSR seismogenic fracture parameter, seismotectonic deformation intensity, seismic activity, Tsallis parameter q and constants a, as well as a parameter characterizing the slope of the repeatability graph (b-value).
url https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/56/e3sconf_strpep2020_02006.pdf
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AT sychevanaylya analysisoftheseismicprocessofthebishkekgeodynamictestsitenortherntienshan
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