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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Дата: | 2012 |
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Subbotin Institute of Geophysics of the NAS of Ukraine
2012
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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. 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 rus https://journals.uran.ua/geofizicheskiy/article/view/116764/110827 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
institution |
Geofizicheskiy Zhurnal |
collection |
OJS |
language |
rus |
format |
Article |
author |
Kushnir, A. N. Burakhovich, T.K. |
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 |
author_facet |
Kushnir, A. N. Burakhovich, T.K. |
author_sort |
Kushnir, A. N. |
title |
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_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_sort |
anomalies of electroconductivity and intraplate earthquakes of the western part of the ukrainian shield and volyno-podolian plate |
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. |
publisher |
Subbotin Institute of Geophysics of the NAS of Ukraine |
publishDate |
2012 |
url |
https://journals.uran.ua/geofizicheskiy/article/view/116764 |
work_keys_str_mv |
AT kushniran anomaliesofelectroconductivityandintraplateearthquakesofthewesternpartoftheukrainianshieldandvolynopodolianplate AT burakhovichtk anomaliesofelectroconductivityandintraplateearthquakesofthewesternpartoftheukrainianshieldandvolynopodolianplate |
first_indexed |
2024-04-21T19:41:19Z |
last_indexed |
2024-04-21T19:41:19Z |
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1796974554254409728 |