Valuation of extinction parameters of anisotropic macro-seismic wave intensities

A method is proposed for calculating the parameters of macroseismic intensity decay of anisotropic fields. Macroseismic field are described by the model of Blake-Shebalin to the attenuation depending on the azimuth direction «epicenter-point-score». Intensity decay function is represented as a Fouri...

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Datum:2014
1. Verfasser: Kulchitsky, V. E.
Format: Artikel
Sprache:Russisch
Veröffentlicht: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2014
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Online Zugang:https://journals.uran.ua/geofizicheskiy/article/view/116127
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Geofizicheskiy Zhurnal
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author Kulchitsky, V. E.
author_facet Kulchitsky, V. E.
author_sort Kulchitsky, V. E.
baseUrl_str
collection OJS
datestamp_date 2020-10-07T11:58:11Z
description A method is proposed for calculating the parameters of macroseismic intensity decay of anisotropic fields. Macroseismic field are described by the model of Blake-Shebalin to the attenuation depending on the azimuth direction «epicenter-point-score». Intensity decay function is represented as a Fourier series in azimuth. The coefficients of the Fourier series are found by the least squares method. Mechanism of optimization for model assumed to real macroseismic field has been described. The proposed method is demonstrated on examples of Vrancea, the Crimea and the Black Sea earthquakes. A good agreement between the estimates obtained with the results of other methods has been demonstrated.
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spelling journalsuranua-geofizicheskiy-article-1161272020-10-07T11:58:11Z Valuation of extinction parameters of anisotropic macro-seismic wave intensities Kulchitsky, V. E. macroseismic field isoseists earthquake intensity attenuation model A method is proposed for calculating the parameters of macroseismic intensity decay of anisotropic fields. Macroseismic field are described by the model of Blake-Shebalin to the attenuation depending on the azimuth direction «epicenter-point-score». Intensity decay function is represented as a Fourier series in azimuth. The coefficients of the Fourier series are found by the least squares method. Mechanism of optimization for model assumed to real macroseismic field has been described. The proposed method is demonstrated on examples of Vrancea, the Crimea and the Black Sea earthquakes. A good agreement between the estimates obtained with the results of other methods has been demonstrated. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2014-04-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116127 10.24028/gzh.0203-3100.v36i2.2014.116127 Geofizicheskiy Zhurnal; Vol. 36 No. 2 (2014); 138-149 Геофизический журнал; Том 36 № 2 (2014); 138-149 Геофізичний журнал; Том 36 № 2 (2014); 138-149 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/116127/110216 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle macroseismic field
isoseists
earthquake
intensity
attenuation model
Kulchitsky, V. E.
Valuation of extinction parameters of anisotropic macro-seismic wave intensities
title Valuation of extinction parameters of anisotropic macro-seismic wave intensities
title_full Valuation of extinction parameters of anisotropic macro-seismic wave intensities
title_fullStr Valuation of extinction parameters of anisotropic macro-seismic wave intensities
title_full_unstemmed Valuation of extinction parameters of anisotropic macro-seismic wave intensities
title_short Valuation of extinction parameters of anisotropic macro-seismic wave intensities
title_sort valuation of extinction parameters of anisotropic macro-seismic wave intensities
topic macroseismic field
isoseists
earthquake
intensity
attenuation model
topic_facet macroseismic field
isoseists
earthquake
intensity
attenuation model
url https://journals.uran.ua/geofizicheskiy/article/view/116127
work_keys_str_mv AT kulchitskyve valuationofextinctionparametersofanisotropicmacroseismicwaveintensities