The Possibility of Estimating the Coseismic Deformation from Water Level Observations in Wells
A method for point estimation of coseismic volume deformation from amplitudes of earthquake generated changes in the water level and from the tidal sensitivity of the water level is presented. Application of this method is illustrated by six Kamchatka earthquakes of 1997–2004 with mw = 6.2–7.8 that...
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ftinstvs:oai:repo.kscnet.ru:2744 2023-05-15T16:59:11+02:00 The Possibility of Estimating the Coseismic Deformation from Water Level Observations in Wells Kopylova G.N. Steblov G.M. Boldina S.V. Sdelnikova I.A. 2010 text http://repo.kscnet.ru/2744/ http://repo.kscnet.ru/2744/7/Kop_Steb_10_1_angl.pdf ru en rus eng http://repo.kscnet.ru/2744/7/Kop_Steb_10_1_angl.pdf Kopylova G.N. <http://repo.kscnet.ru/view/creators/Kopylova=3AG=2EN=2E=3A=3A.html>, Steblov G.M. <http://repo.kscnet.ru/view/creators/Steblov=3AG=2EM=2E=3A=3A.html>, Boldina S.V. <http://repo.kscnet.ru/view/creators/Boldina=3AS=2EV=2E=3A=3A.html>, Sdelnikova I.A. <http://repo.kscnet.ru/view/creators/Sdelnikova=3AI=2EA=2E=3A=3A.html> (2010) The Possibility of Estimating the Coseismic Deformation from Water Level Observations in Wells // Izvestiya, Physics of the Solid Earth. Vol. 46, No. 1. pp. 47-56. doi:10.1134/S1069351310010040 <http://doi.org/10.1134/S1069351310010040>. 37.31.19 Сейсмология 37.31.27 Земные приливы 38.61.15 Динамика и режим подземных вод Статья PeerReviewed 2010 ftinstvs https://doi.org/10.1134/S1069351310010040 2022-10-03T23:59:25Z A method for point estimation of coseismic volume deformation from amplitudes of earthquake generated changes in the water level and from the tidal sensitivity of the water level is presented. Application of this method is illustrated by six Kamchatka earthquakes of 1997–2004 with mw = 6.2–7.8 that occurred 128–316 km from the YuZ-5 well. Estimates of coseismic deformation provided by the level gage observations and by the model agree in amplitude and sign. The model reproduces an extended dislocation source in a homogeneous elastic isotropic half-space. Source rupture parameters correspond to focal mechanisms from the CMT international catalog. Consistence in experimental and theoretical estimates of the volume coseismic deformation indicates the high strain-resistance properties of YuZ-5 borehole and the possibility of quantitative estimation of seismotectonic deformation from high-precision water level measurements with time resolution not lower than 10 minutes. Text Kamchatka Institute of Volcanology and Seismology, Petropavlovsk-Kamchatsky: IVS FEB RAS Repository Izvestiya, Physics of the Solid Earth 46 1 47 56 |
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Open Polar |
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Institute of Volcanology and Seismology, Petropavlovsk-Kamchatsky: IVS FEB RAS Repository |
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ftinstvs |
language |
Russian English |
topic |
37.31.19 Сейсмология 37.31.27 Земные приливы 38.61.15 Динамика и режим подземных вод |
spellingShingle |
37.31.19 Сейсмология 37.31.27 Земные приливы 38.61.15 Динамика и режим подземных вод Kopylova G.N. Steblov G.M. Boldina S.V. Sdelnikova I.A. The Possibility of Estimating the Coseismic Deformation from Water Level Observations in Wells |
topic_facet |
37.31.19 Сейсмология 37.31.27 Земные приливы 38.61.15 Динамика и режим подземных вод |
description |
A method for point estimation of coseismic volume deformation from amplitudes of earthquake generated changes in the water level and from the tidal sensitivity of the water level is presented. Application of this method is illustrated by six Kamchatka earthquakes of 1997–2004 with mw = 6.2–7.8 that occurred 128–316 km from the YuZ-5 well. Estimates of coseismic deformation provided by the level gage observations and by the model agree in amplitude and sign. The model reproduces an extended dislocation source in a homogeneous elastic isotropic half-space. Source rupture parameters correspond to focal mechanisms from the CMT international catalog. Consistence in experimental and theoretical estimates of the volume coseismic deformation indicates the high strain-resistance properties of YuZ-5 borehole and the possibility of quantitative estimation of seismotectonic deformation from high-precision water level measurements with time resolution not lower than 10 minutes. |
format |
Text |
author |
Kopylova G.N. Steblov G.M. Boldina S.V. Sdelnikova I.A. |
author_facet |
Kopylova G.N. Steblov G.M. Boldina S.V. Sdelnikova I.A. |
author_sort |
Kopylova G.N. |
title |
The Possibility of Estimating the Coseismic Deformation from Water Level Observations in Wells |
title_short |
The Possibility of Estimating the Coseismic Deformation from Water Level Observations in Wells |
title_full |
The Possibility of Estimating the Coseismic Deformation from Water Level Observations in Wells |
title_fullStr |
The Possibility of Estimating the Coseismic Deformation from Water Level Observations in Wells |
title_full_unstemmed |
The Possibility of Estimating the Coseismic Deformation from Water Level Observations in Wells |
title_sort |
possibility of estimating the coseismic deformation from water level observations in wells |
publishDate |
2010 |
url |
http://repo.kscnet.ru/2744/ http://repo.kscnet.ru/2744/7/Kop_Steb_10_1_angl.pdf |
genre |
Kamchatka |
genre_facet |
Kamchatka |
op_relation |
http://repo.kscnet.ru/2744/7/Kop_Steb_10_1_angl.pdf Kopylova G.N. <http://repo.kscnet.ru/view/creators/Kopylova=3AG=2EN=2E=3A=3A.html>, Steblov G.M. <http://repo.kscnet.ru/view/creators/Steblov=3AG=2EM=2E=3A=3A.html>, Boldina S.V. <http://repo.kscnet.ru/view/creators/Boldina=3AS=2EV=2E=3A=3A.html>, Sdelnikova I.A. <http://repo.kscnet.ru/view/creators/Sdelnikova=3AI=2EA=2E=3A=3A.html> (2010) The Possibility of Estimating the Coseismic Deformation from Water Level Observations in Wells // Izvestiya, Physics of the Solid Earth. Vol. 46, No. 1. pp. 47-56. doi:10.1134/S1069351310010040 <http://doi.org/10.1134/S1069351310010040>. |
op_doi |
https://doi.org/10.1134/S1069351310010040 |
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Izvestiya, Physics of the Solid Earth |
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46 |
container_issue |
1 |
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47 |
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56 |
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1766051409157947392 |