Anomalies of electroconductivity and intraplate earthquakes of the western part of the Ukrainian Shield and Volyno-Podolian Plate

Threedimensional geoelectric model of the Earth’s crust and upper mantle of the MogilevPodolNovodnestrovian seismically dangerous area is characterized by electroconducting zones at the depths from 3 to 5 km with ρ=10 Om·m, from 15 to 30 km with ρ=30 Оm·m and from 50-70 to 120 km with ρ=30 Оm·m. On...

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Date:2012
Main Authors: Kushnir, A. N., Burakhovich, T.K.
Format: Article
Language:Russian
Published: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2012
Online Access:https://journals.uran.ua/geofizicheskiy/article/view/116764
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Journal Title:Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal
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author Kushnir, A. N.
Burakhovich, T.K.
author_facet Kushnir, A. N.
Burakhovich, T.K.
author_sort Kushnir, A. N.
baseUrl_str
collection OJS
datestamp_date 2020-10-07T12:21:33Z
description Threedimensional geoelectric model of the Earth’s crust and upper mantle of the MogilevPodolNovodnestrovian seismically dangerous area is characterized by electroconducting zones at the depths from 3 to 5 km with ρ=10 Om·m, from 15 to 30 km with ρ=30 Оm·m and from 50-70 to 120 km with ρ=30 Оm·m. On the base of the results of geoelectric studies, characteristics of MogilevPodolNovodnestrovian seismically dangerous zone which is confined to joint areas of Podolian, Belotserkovian, Zhmerynskiy and other ones of deep faults with lower range have been replenished and specified.
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publisher S. Subbotin Institute of Geophysics of the NAS of Ukraine
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spelling journalsuranua-geofizicheskiy-article-1167642020-10-07T12:21:33Z Anomalies of electroconductivity and intraplate earthquakes of the western part of the Ukrainian Shield and Volyno-Podolian Plate Kushnir, A. N. Burakhovich, T.K. Threedimensional geoelectric model of the Earth’s crust and upper mantle of the MogilevPodolNovodnestrovian seismically dangerous area is characterized by electroconducting zones at the depths from 3 to 5 km with ρ=10 Om·m, from 15 to 30 km with ρ=30 Оm·m and from 50-70 to 120 km with ρ=30 Оm·m. On the base of the results of geoelectric studies, characteristics of MogilevPodolNovodnestrovian seismically dangerous zone which is confined to joint areas of Podolian, Belotserkovian, Zhmerynskiy and other ones of deep faults with lower range have been replenished and specified. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2012-08-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116764 10.24028/gzh.0203-3100.v34i4.2012.116764 Geofizicheskiy Zhurnal; Vol. 34 No. 4 (2012); 157-165 Геофизический журнал; Том 34 № 4 (2012); 157-165 Геофізичний журнал; Том 34 № 4 (2012); 157-165 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/116764/110827 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle Kushnir, A. N.
Burakhovich, T.K.
Anomalies of electroconductivity and intraplate earthquakes of the western part of the Ukrainian Shield and Volyno-Podolian Plate
title Anomalies of electroconductivity and intraplate earthquakes of the western part of the Ukrainian Shield and Volyno-Podolian Plate
title_full Anomalies of electroconductivity and intraplate earthquakes of the western part of the Ukrainian Shield and Volyno-Podolian Plate
title_fullStr Anomalies of electroconductivity and intraplate earthquakes of the western part of the Ukrainian Shield and Volyno-Podolian Plate
title_full_unstemmed Anomalies of electroconductivity and intraplate earthquakes of the western part of the Ukrainian Shield and Volyno-Podolian Plate
title_short Anomalies of electroconductivity and intraplate earthquakes of the western part of the Ukrainian Shield and Volyno-Podolian Plate
title_sort anomalies of electroconductivity and intraplate earthquakes of the western part of the ukrainian shield and volyno-podolian plate
url https://journals.uran.ua/geofizicheskiy/article/view/116764
work_keys_str_mv AT kushniran anomaliesofelectroconductivityandintraplateearthquakesofthewesternpartoftheukrainianshieldandvolynopodolianplate
AT burakhovichtk anomaliesofelectroconductivityandintraplateearthquakesofthewesternpartoftheukrainianshieldandvolynopodolianplate