Correlation of constant magnetic field anomalies and crustal geo-electric structures within the western slope of the Voronezh massif

Correlation of constant magnetic field anomalies and crustal geo-electric structures within the western slope of the Voronezh massif

Simultaneous magnetotelluric and magnetovariation soundings carried out recently at the western slope of the Voronezh Massif in the network of the international project KIROVOGRAD outlined bright quasi-linear conductivity anomalies in the lower crust, having a complex junction southwards from Brians...

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Бібліографічні деталі
Дата:2012
Автори: Abramova, D. Yu., Abramova, L. M., Varentsov, Iv.M., Kulikov, V. A., Lozovskiy, I. N.
Формат: Стаття
Мова:rus
Опубліковано: Subbotin Institute of Geophysics of the NAS of Ukraine 2012
Онлайн доступ:https://journals.uran.ua/geofizicheskiy/article/view/116753
Теги: Додати тег
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Назва журналу:Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal
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spelling journalsuranua-geofizicheskiy-article-1167532020-10-07T12:21:33Z Correlation of constant magnetic field anomalies and crustal geo-electric structures within the western slope of the Voronezh massif Abramova, D. Yu. Abramova, L. M. Varentsov, Iv.M. Kulikov, V. A. Lozovskiy, I. N. Simultaneous magnetotelluric and magnetovariation soundings carried out recently at the western slope of the Voronezh Massif in the network of the international project KIROVOGRAD outlined bright quasi-linear conductivity anomalies in the lower crust, having a complex junction southwards from Briansk. The nature of these anomalies is clarified in the correlation study of electromagnetic (primarily, horizontal magnetovariation) responses and related geoelectrical models with anomalies of the permanent magnetic field resulted from the ground and satellite observations. The approaches for distinction of relatively low frequency lithosphere magnetic anomalies produced by low-crustal sources are further discussed. Subbotin Institute of Geophysics of the NAS of Ukraine 2012-08-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116753 10.24028/gzh.0203-3100.v34i4.2012.116753 Geofizicheskiy Zhurnal; Vol. 34 No. 4 (2012); 62-69 Геофизический журнал; Том 34 № 4 (2012); 62-69 Геофізичний журнал; Том 34 № 4 (2012); 62-69 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/116753/110815 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
institution Geofizicheskiy Zhurnal
collection OJS
language rus
format Article
author Abramova, D. Yu.
Abramova, L. M.
Varentsov, Iv.M.
Kulikov, V. A.
Lozovskiy, I. N.
spellingShingle Abramova, D. Yu.
Abramova, L. M.
Varentsov, Iv.M.
Kulikov, V. A.
Lozovskiy, I. N.
Correlation of constant magnetic field anomalies and crustal geo-electric structures within the western slope of the Voronezh massif
author_facet Abramova, D. Yu.
Abramova, L. M.
Varentsov, Iv.M.
Kulikov, V. A.
Lozovskiy, I. N.
author_sort Abramova, D. Yu.
title Correlation of constant magnetic field anomalies and crustal geo-electric structures within the western slope of the Voronezh massif
title_short Correlation of constant magnetic field anomalies and crustal geo-electric structures within the western slope of the Voronezh massif
title_full Correlation of constant magnetic field anomalies and crustal geo-electric structures within the western slope of the Voronezh massif
title_fullStr Correlation of constant magnetic field anomalies and crustal geo-electric structures within the western slope of the Voronezh massif
title_full_unstemmed Correlation of constant magnetic field anomalies and crustal geo-electric structures within the western slope of the Voronezh massif
title_sort correlation of constant magnetic field anomalies and crustal geo-electric structures within the western slope of the voronezh massif
description Simultaneous magnetotelluric and magnetovariation soundings carried out recently at the western slope of the Voronezh Massif in the network of the international project KIROVOGRAD outlined bright quasi-linear conductivity anomalies in the lower crust, having a complex junction southwards from Briansk. The nature of these anomalies is clarified in the correlation study of electromagnetic (primarily, horizontal magnetovariation) responses and related geoelectrical models with anomalies of the permanent magnetic field resulted from the ground and satellite observations. The approaches for distinction of relatively low frequency lithosphere magnetic anomalies produced by low-crustal sources are further discussed.
publisher Subbotin Institute of Geophysics of the NAS of Ukraine
publishDate 2012
url https://journals.uran.ua/geofizicheskiy/article/view/116753
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first_indexed 2024-04-21T19:41:16Z
last_indexed 2024-04-21T19:41:16Z
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