Geoelectric studies of the Belgorod-Sumy megablock of the northern slope of the Dnieper-Donets Trough
Processing of long-term Earth’s electromagnetic field observations was performed using two software systems (PRC_MTMV and PTS), frequency distribution of the amplitude and phase of impedance, apparent resistivity, horizontal components of the magnetic tensor and tipper were obtained. Minimum on the...
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Дата: | 2015 |
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Мова: | Ukrainian |
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Subbotin Institute of Geophysics of the NAS of Ukraine
2015
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journalsuranua-geofizicheskiy-article-1111632020-10-07T11:38:43Z Geoelectric studies of the Belgorod-Sumy megablock of the northern slope of the Dnieper-Donets Trough Shirkov, B. Perestyuk, O. Kushnir, A. magnetotelluric sounding magnetovariational profiling the Dnieper-Donets Trough Processing of long-term Earth’s electromagnetic field observations was performed using two software systems (PRC_MTMV and PTS), frequency distribution of the amplitude and phase of impedance, apparent resistivity, horizontal components of the magnetic tensor and tipper were obtained. Minimum on the descending part of ρk curves according to the results of a qualitative assessment corresponds to the conductor at a depth of 50—150 km. Subbotin Institute of Geophysics of the NAS of Ukraine 2015-10-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/111163 10.24028/gzh.0203-3100.v37i5.2015.111163 Geofizicheskiy Zhurnal; Vol. 37 No. 5 (2015); 176-182 Геофизический журнал; Том 37 № 5 (2015); 176-182 Геофізичний журнал; Том 37 № 5 (2015); 176-182 2524-1052 0203-3100 uk https://journals.uran.ua/geofizicheskiy/article/view/111163/106027 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
institution |
Geofizicheskiy Zhurnal |
collection |
OJS |
language |
Ukrainian |
topic |
magnetotelluric sounding magnetovariational profiling the Dnieper-Donets Trough |
spellingShingle |
magnetotelluric sounding magnetovariational profiling the Dnieper-Donets Trough Shirkov, B. Perestyuk, O. Kushnir, A. Geoelectric studies of the Belgorod-Sumy megablock of the northern slope of the Dnieper-Donets Trough |
topic_facet |
magnetotelluric sounding magnetovariational profiling the Dnieper-Donets Trough |
format |
Article |
author |
Shirkov, B. Perestyuk, O. Kushnir, A. |
author_facet |
Shirkov, B. Perestyuk, O. Kushnir, A. |
author_sort |
Shirkov, B. |
title |
Geoelectric studies of the Belgorod-Sumy megablock of the northern slope of the Dnieper-Donets Trough |
title_short |
Geoelectric studies of the Belgorod-Sumy megablock of the northern slope of the Dnieper-Donets Trough |
title_full |
Geoelectric studies of the Belgorod-Sumy megablock of the northern slope of the Dnieper-Donets Trough |
title_fullStr |
Geoelectric studies of the Belgorod-Sumy megablock of the northern slope of the Dnieper-Donets Trough |
title_full_unstemmed |
Geoelectric studies of the Belgorod-Sumy megablock of the northern slope of the Dnieper-Donets Trough |
title_sort |
geoelectric studies of the belgorod-sumy megablock of the northern slope of the dnieper-donets trough |
description |
Processing of long-term Earth’s electromagnetic field observations was performed using two software systems (PRC_MTMV and PTS), frequency distribution of the amplitude and phase of impedance, apparent resistivity, horizontal components of the magnetic tensor and tipper were obtained. Minimum on the descending part of ρk curves according to the results of a qualitative assessment corresponds to the conductor at a depth of 50—150 km. |
publisher |
Subbotin Institute of Geophysics of the NAS of Ukraine |
publishDate |
2015 |
url |
https://journals.uran.ua/geofizicheskiy/article/view/111163 |
work_keys_str_mv |
AT shirkovb geoelectricstudiesofthebelgorodsumymegablockofthenorthernslopeofthednieperdonetstrough AT perestyuko geoelectricstudiesofthebelgorodsumymegablockofthenorthernslopeofthednieperdonetstrough AT kushnira geoelectricstudiesofthebelgorodsumymegablockofthenorthernslopeofthednieperdonetstrough |
first_indexed |
2024-04-21T19:40:07Z |
last_indexed |
2024-04-21T19:40:07Z |
_version_ |
1796974478828240896 |