Electrical Conductivity of the Earth's Mantle in the «Academic Vernadsky» Station region

In the regional magnetovariational sounding method on the base of relationship between spectra of vertical and horizontal geomagnetic field variations and a priori known structure of the field source, the medium response function is calculated, which interpretation allows to obtain the subsurface co...

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Datum:2014
1. Verfasser: Ladanovsky, B.
Format: Artikel
Sprache:Ukrainisch
Veröffentlicht: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2014
Online Zugang:https://journals.uran.ua/geofizicheskiy/article/view/111577
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Geofizicheskiy Zhurnal
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author Ladanovsky, B.
author_facet Ladanovsky, B.
author_sort Ladanovsky, B.
baseUrl_str
collection OJS
datestamp_date 2020-10-07T11:55:34Z
description In the regional magnetovariational sounding method on the base of relationship between spectra of vertical and horizontal geomagnetic field variations and a priori known structure of the field source, the medium response function is calculated, which interpretation allows to obtain the subsurface conductivity distribution model. Hourly mean values of geomagnetic field components acquired by "Argentine Islands" (AIA) observatory with 13 years of data (1996—2008) were used for calculations. The 1D conductivity distribution model of medium for the "Academic Vernadsky" Station region was obtained as a result of geoelectrical interpretation, which was carried out by numerical methods.
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spelling journalsuranua-geofizicheskiy-article-1115772020-10-07T11:55:34Z Electrical Conductivity of the Earth's Mantle in the «Academic Vernadsky» Station region Ladanovsky, B. In the regional magnetovariational sounding method on the base of relationship between spectra of vertical and horizontal geomagnetic field variations and a priori known structure of the field source, the medium response function is calculated, which interpretation allows to obtain the subsurface conductivity distribution model. Hourly mean values of geomagnetic field components acquired by "Argentine Islands" (AIA) observatory with 13 years of data (1996—2008) were used for calculations. The 1D conductivity distribution model of medium for the "Academic Vernadsky" Station region was obtained as a result of geoelectrical interpretation, which was carried out by numerical methods. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2014-10-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/111577 10.24028/gzh.0203-3100.v36i5.2014.111577 Geofizicheskiy Zhurnal; Vol. 36 No. 5 (2014); 156-164 Геофизический журнал; Том 36 № 5 (2014); 156-164 Геофізичний журнал; Том 36 № 5 (2014); 156-164 2524-1052 0203-3100 uk https://journals.uran.ua/geofizicheskiy/article/view/111577/106565 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle Ladanovsky, B.
Electrical Conductivity of the Earth's Mantle in the «Academic Vernadsky» Station region
title Electrical Conductivity of the Earth's Mantle in the «Academic Vernadsky» Station region
title_full Electrical Conductivity of the Earth's Mantle in the «Academic Vernadsky» Station region
title_fullStr Electrical Conductivity of the Earth's Mantle in the «Academic Vernadsky» Station region
title_full_unstemmed Electrical Conductivity of the Earth's Mantle in the «Academic Vernadsky» Station region
title_short Electrical Conductivity of the Earth's Mantle in the «Academic Vernadsky» Station region
title_sort electrical conductivity of the earth's mantle in the «academic vernadsky» station region
url https://journals.uran.ua/geofizicheskiy/article/view/111577
work_keys_str_mv AT ladanovskyb electricalconductivityoftheearthsmantleintheacademicvernadskystationregion