Electromagnetic monitoring in seismically active regions of Siberia

Field data of the electromagnetic monitoring of controlled source have been obtained in two seismically active regions of Siberia. The article demonstrates an approach to the interpretation of regime observations data and it attempts to explain the variation of the electromagnetic parameters due to...

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Бібліографічні деталі
Дата:2012
Автори: Nevedrova, N. N., Epov, M. I.
Формат: Стаття
Мова:rus
Опубліковано: Subbotin Institute of Geophysics of the NAS of Ukraine 2012
Онлайн доступ:https://journals.uran.ua/geofizicheskiy/article/view/116775
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Назва журналу:Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal
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spelling journalsuranua-geofizicheskiy-article-1167752020-10-07T12:21:33Z Electromagnetic monitoring in seismically active regions of Siberia Nevedrova, N. N. Epov, M. I. Field data of the electromagnetic monitoring of controlled source have been obtained in two seismically active regions of Siberia. The article demonstrates an approach to the interpretation of regime observations data and it attempts to explain the variation of the electromagnetic parameters due to geodynamic processes, taking into account the peculiarities of the nontectonic structure. For the territory of the Baikal polygon, which is located on the southwestern shore of the Baikal Lake, geoelectric characteristics of the main seismogenic structures and fault disturbances have been provided. The analysis of monitoring measurements interpretation at constant current in the regime point VES has been presented and the relationship with the geoelectric structure has been proved; the sensitivity of the VES setting was determined. In the Altai geodynamic polygon the measurements were conducted by a complex of electromagnetic methods (VES, TEM in several modifications). The investigations were aimed at the study of a structure and variations of electrical conductivity associated with the devastating Chui earthquake and development of aftershock process. Interpretation of the regime TEM data with an inductive source has been considered. On the basis of the complex geologo-geophysical analysis the processes of geological array consolidation disturbed by the strong seismic influence have been described. Subbotin Institute of Geophysics of the NAS of Ukraine 2012-08-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116775 10.24028/gzh.0203-3100.v34i4.2012.116775 Geofizicheskiy Zhurnal; Vol. 34 No. 4 (2012); 209-223 Геофизический журнал; Том 34 № 4 (2012); 209-223 Геофізичний журнал; Том 34 № 4 (2012); 209-223 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/116775/110832 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
institution Geofizicheskiy Zhurnal
collection OJS
language rus
format Article
author Nevedrova, N. N.
Epov, M. I.
spellingShingle Nevedrova, N. N.
Epov, M. I.
Electromagnetic monitoring in seismically active regions of Siberia
author_facet Nevedrova, N. N.
Epov, M. I.
author_sort Nevedrova, N. N.
title Electromagnetic monitoring in seismically active regions of Siberia
title_short Electromagnetic monitoring in seismically active regions of Siberia
title_full Electromagnetic monitoring in seismically active regions of Siberia
title_fullStr Electromagnetic monitoring in seismically active regions of Siberia
title_full_unstemmed Electromagnetic monitoring in seismically active regions of Siberia
title_sort electromagnetic monitoring in seismically active regions of siberia
description Field data of the electromagnetic monitoring of controlled source have been obtained in two seismically active regions of Siberia. The article demonstrates an approach to the interpretation of regime observations data and it attempts to explain the variation of the electromagnetic parameters due to geodynamic processes, taking into account the peculiarities of the nontectonic structure. For the territory of the Baikal polygon, which is located on the southwestern shore of the Baikal Lake, geoelectric characteristics of the main seismogenic structures and fault disturbances have been provided. The analysis of monitoring measurements interpretation at constant current in the regime point VES has been presented and the relationship with the geoelectric structure has been proved; the sensitivity of the VES setting was determined. In the Altai geodynamic polygon the measurements were conducted by a complex of electromagnetic methods (VES, TEM in several modifications). The investigations were aimed at the study of a structure and variations of electrical conductivity associated with the devastating Chui earthquake and development of aftershock process. Interpretation of the regime TEM data with an inductive source has been considered. On the basis of the complex geologo-geophysical analysis the processes of geological array consolidation disturbed by the strong seismic influence have been described.
publisher Subbotin Institute of Geophysics of the NAS of Ukraine
publishDate 2012
url https://journals.uran.ua/geofizicheskiy/article/view/116775
work_keys_str_mv AT nevedrovann electromagneticmonitoringinseismicallyactiveregionsofsiberia
AT epovmi electromagneticmonitoringinseismicallyactiveregionsofsiberia
first_indexed 2024-04-21T19:41:20Z
last_indexed 2024-04-21T19:41:20Z
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