PARAMETERS OF KAMCHATKA SEISMICITY IN 2008
The paper describes seismicity of Kamchatka for the period of 2008 and presents 2D distribution of background seismicity parameters calculated from data published in the Regional Catalogue of Kamchatka Earthquakes. Parameters under study are total released seismic energy, seismic activity A10, slope...
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Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
2015
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ftdoajarticles:oai:doaj.org/article:96e558bbbbb1427593e45ff916e422df 2023-05-15T16:58:44+02:00 PARAMETERS OF KAMCHATKA SEISMICITY IN 2008 Vadim A. Saltykov Nadezhda M. Kravchenko 2015-09-01T00:00:00Z https://doi.org/10.5800/GT-2010-1-2-0014 https://doaj.org/article/96e558bbbbb1427593e45ff916e422df EN RU eng rus Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust https://www.gt-crust.ru/jour/article/view/105 https://doaj.org/toc/2078-502X 2078-502X doi:10.5800/GT-2010-1-2-0014 https://doaj.org/article/96e558bbbbb1427593e45ff916e422df Геодинамика и тектонофизика, Vol 1, Iss 2, Pp 186-196 (2015) seismicity monitoring kamchatka earthquake Science Q article 2015 ftdoajarticles https://doi.org/10.5800/GT-2010-1-2-0014 2022-12-30T23:02:19Z The paper describes seismicity of Kamchatka for the period of 2008 and presents 2D distribution of background seismicity parameters calculated from data published in the Regional Catalogue of Kamchatka Earthquakes. Parameters under study are total released seismic energy, seismic activity A10, slope of recurrence graph γ, parameters of RTL, ΔS and Z-function methods, and clustering of earthquakes. Estimations of seismicity are obtained for a region bordered by latitude 50.5–56.5N, longitude 156E–167E, with depths to 300 km. Earthquakes of energy classes not less than 8.5 as per the Fedotov’s classification are considered. The total seismic energy released in 2008 is estimated. According to a function of annual seismic energy distribution, an amount of seismic energy released in 2008 was close to the median level (Fig. 1). Over 2/3 of the total amount of seismic energy released in 2008 resulted from three largest earthquakes (МW ≥ 5.9). About 5 percent of the total number of seismic events are comprised of grouped earthquakes, i.e. aftershocks and swarms. A schematic map of the largest earthquakes (МW ≥ 5.9) and grouped seismic events which occurred in 2008 is given in Fig. 2; their parameters are listed in Table 1. Grouped earthquakes are excluded from the catalogue. A map showing epicenters of independent earthquakes is given in Fig. 3. The slope of recurrence graph γ and seismic activity A10 is based on the Gutenberg-Richter law stating the fundamental property of seismic process. The recurrence graph slope is calculated from continuous exponential distribution of earthquakes by energy classes. Using γ is conditioned by observations that in some cases the slope of the recurrence graph decreases prior to a large earthquake. Activity A10 is calculated from the number of earthquakes N and recurrence graph slope γ. Average slopes of recurrence graph γ and seismic activity A10 for the area under study in 2008 are calculated; our estimations give evidence that the year of 2008 was not anomalous in terms of ... Article in Journal/Newspaper Kamchatka Directory of Open Access Journals: DOAJ Articles Geodynamics & Tectonophysics 1 2 186 196 |
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seismicity monitoring kamchatka earthquake Science Q |
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seismicity monitoring kamchatka earthquake Science Q Vadim A. Saltykov Nadezhda M. Kravchenko PARAMETERS OF KAMCHATKA SEISMICITY IN 2008 |
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seismicity monitoring kamchatka earthquake Science Q |
description |
The paper describes seismicity of Kamchatka for the period of 2008 and presents 2D distribution of background seismicity parameters calculated from data published in the Regional Catalogue of Kamchatka Earthquakes. Parameters under study are total released seismic energy, seismic activity A10, slope of recurrence graph γ, parameters of RTL, ΔS and Z-function methods, and clustering of earthquakes. Estimations of seismicity are obtained for a region bordered by latitude 50.5–56.5N, longitude 156E–167E, with depths to 300 km. Earthquakes of energy classes not less than 8.5 as per the Fedotov’s classification are considered. The total seismic energy released in 2008 is estimated. According to a function of annual seismic energy distribution, an amount of seismic energy released in 2008 was close to the median level (Fig. 1). Over 2/3 of the total amount of seismic energy released in 2008 resulted from three largest earthquakes (МW ≥ 5.9). About 5 percent of the total number of seismic events are comprised of grouped earthquakes, i.e. aftershocks and swarms. A schematic map of the largest earthquakes (МW ≥ 5.9) and grouped seismic events which occurred in 2008 is given in Fig. 2; their parameters are listed in Table 1. Grouped earthquakes are excluded from the catalogue. A map showing epicenters of independent earthquakes is given in Fig. 3. The slope of recurrence graph γ and seismic activity A10 is based on the Gutenberg-Richter law stating the fundamental property of seismic process. The recurrence graph slope is calculated from continuous exponential distribution of earthquakes by energy classes. Using γ is conditioned by observations that in some cases the slope of the recurrence graph decreases prior to a large earthquake. Activity A10 is calculated from the number of earthquakes N and recurrence graph slope γ. Average slopes of recurrence graph γ and seismic activity A10 for the area under study in 2008 are calculated; our estimations give evidence that the year of 2008 was not anomalous in terms of ... |
format |
Article in Journal/Newspaper |
author |
Vadim A. Saltykov Nadezhda M. Kravchenko |
author_facet |
Vadim A. Saltykov Nadezhda M. Kravchenko |
author_sort |
Vadim A. Saltykov |
title |
PARAMETERS OF KAMCHATKA SEISMICITY IN 2008 |
title_short |
PARAMETERS OF KAMCHATKA SEISMICITY IN 2008 |
title_full |
PARAMETERS OF KAMCHATKA SEISMICITY IN 2008 |
title_fullStr |
PARAMETERS OF KAMCHATKA SEISMICITY IN 2008 |
title_full_unstemmed |
PARAMETERS OF KAMCHATKA SEISMICITY IN 2008 |
title_sort |
parameters of kamchatka seismicity in 2008 |
publisher |
Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust |
publishDate |
2015 |
url |
https://doi.org/10.5800/GT-2010-1-2-0014 https://doaj.org/article/96e558bbbbb1427593e45ff916e422df |
genre |
Kamchatka |
genre_facet |
Kamchatka |
op_source |
Геодинамика и тектонофизика, Vol 1, Iss 2, Pp 186-196 (2015) |
op_relation |
https://www.gt-crust.ru/jour/article/view/105 https://doaj.org/toc/2078-502X 2078-502X doi:10.5800/GT-2010-1-2-0014 https://doaj.org/article/96e558bbbbb1427593e45ff916e422df |
op_doi |
https://doi.org/10.5800/GT-2010-1-2-0014 |
container_title |
Geodynamics & Tectonophysics |
container_volume |
1 |
container_issue |
2 |
container_start_page |
186 |
op_container_end_page |
196 |
_version_ |
1766050826406592512 |