Model of seismic hazard of the northwestern part of the Black Sea

Characteristics of seismic hazard assessment of marine areas have been considered. Modeling of seismic hazard of northwestern part of the Black Sea shelf is made on the basis of the developed models of seismicity, seismic sources, attenuation of the intensity and zones of earthquakes occurrence. Map...

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Datum:2012
Hauptverfasser: Pustovitenko, B. G., Kulchitsky, V. E., Pustovitenko, A. A.
Format: Artikel
Sprache:Russisch
Veröffentlicht: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2012
Online Zugang:https://journals.uran.ua/geofizicheskiy/article/view/116665
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Geofizicheskiy Zhurnal
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author Pustovitenko, B. G.
Kulchitsky, V. E.
Pustovitenko, A. A.
author_facet Pustovitenko, B. G.
Kulchitsky, V. E.
Pustovitenko, A. A.
author_sort Pustovitenko, B. G.
baseUrl_str
collection OJS
datestamp_date 2020-10-07T12:21:20Z
description Characteristics of seismic hazard assessment of marine areas have been considered. Modeling of seismic hazard of northwestern part of the Black Sea shelf is made on the basis of the developed models of seismicity, seismic sources, attenuation of the intensity and zones of earthquakes occurrence. Maps of general seismic zoning of the shelf are presented for return periods of seismic effects once in each 500 and 1000 years. According to these maps the entire territory of the shelf refers to the seismically dangerous zone with estimated intensities of 6 and 7 points.
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spelling journalsuranua-geofizicheskiy-article-1166652020-10-07T12:21:20Z Model of seismic hazard of the northwestern part of the Black Sea Pustovitenko, B. G. Kulchitsky, V. E. Pustovitenko, A. A. Characteristics of seismic hazard assessment of marine areas have been considered. Modeling of seismic hazard of northwestern part of the Black Sea shelf is made on the basis of the developed models of seismicity, seismic sources, attenuation of the intensity and zones of earthquakes occurrence. Maps of general seismic zoning of the shelf are presented for return periods of seismic effects once in each 500 and 1000 years. According to these maps the entire territory of the shelf refers to the seismically dangerous zone with estimated intensities of 6 and 7 points. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2012-10-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116665 10.24028/gzh.0203-3100.v34i5.2012.116665 Geofizicheskiy Zhurnal; Vol. 34 No. 5 (2012); 87-101 Геофизический журнал; Том 34 № 5 (2012); 87-101 Геофізичний журнал; Том 34 № 5 (2012); 87-101 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/116665/110739 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle Pustovitenko, B. G.
Kulchitsky, V. E.
Pustovitenko, A. A.
Model of seismic hazard of the northwestern part of the Black Sea
title Model of seismic hazard of the northwestern part of the Black Sea
title_full Model of seismic hazard of the northwestern part of the Black Sea
title_fullStr Model of seismic hazard of the northwestern part of the Black Sea
title_full_unstemmed Model of seismic hazard of the northwestern part of the Black Sea
title_short Model of seismic hazard of the northwestern part of the Black Sea
title_sort model of seismic hazard of the northwestern part of the black sea
url https://journals.uran.ua/geofizicheskiy/article/view/116665
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