Geoelectric studies of the south Voronezhcrystalline massif

The first results of interpretation of magnetic variation data, focused on the three profiles in the southern part of the Voronezh crystalline massif by the two-dimensional inversion have been pre-sented. Several objects of low resistance, the roof of which is located at the depth of less than 10 km...

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Datum:2014
Hauptverfasser: Logvinov, I., Tregubenko, V. I., Tarasov, V. N.
Format: Artikel
Sprache:Russisch
Veröffentlicht: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2014
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Online Zugang:https://journals.uran.ua/geofizicheskiy/article/view/116119
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Geofizicheskiy Zhurnal
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author Logvinov, I.
Tregubenko, V. I.
Tarasov, V. N.
author_facet Logvinov, I.
Tregubenko, V. I.
Tarasov, V. N.
author_sort Logvinov, I.
baseUrl_str
collection OJS
datestamp_date 2020-10-07T11:58:11Z
description The first results of interpretation of magnetic variation data, focused on the three profiles in the southern part of the Voronezh crystalline massif by the two-dimensional inversion have been pre-sented. Several objects of low resistance, the roof of which is located at the depth of less than 10 km have been subdivided. The most reliable object spatially correlates with the Belgorod-Mikhailovsk greenstone belt (and the spread of ferruginous quartzites of the Kursk Magnetic Anomaly).
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spelling journalsuranua-geofizicheskiy-article-1161192020-10-07T11:58:11Z Geoelectric studies of the south Voronezhcrystalline massif Logvinov, I. Tregubenko, V. I. Tarasov, V. N. electrical conductivity the crust Voronezh Massif The first results of interpretation of magnetic variation data, focused on the three profiles in the southern part of the Voronezh crystalline massif by the two-dimensional inversion have been pre-sented. Several objects of low resistance, the roof of which is located at the depth of less than 10 km have been subdivided. The most reliable object spatially correlates with the Belgorod-Mikhailovsk greenstone belt (and the spread of ferruginous quartzites of the Kursk Magnetic Anomaly). S. Subbotin Institute of Geophysics of the NAS of Ukraine 2014-04-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116119 10.24028/gzh.0203-3100.v36i2.2014.116119 Geofizicheskiy Zhurnal; Vol. 36 No. 2 (2014); 75-84 Геофизический журнал; Том 36 № 2 (2014); 75-84 Геофізичний журнал; Том 36 № 2 (2014); 75-84 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/116119/110205 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle electrical conductivity
the crust Voronezh Massif
Logvinov, I.
Tregubenko, V. I.
Tarasov, V. N.
Geoelectric studies of the south Voronezhcrystalline massif
title Geoelectric studies of the south Voronezhcrystalline massif
title_full Geoelectric studies of the south Voronezhcrystalline massif
title_fullStr Geoelectric studies of the south Voronezhcrystalline massif
title_full_unstemmed Geoelectric studies of the south Voronezhcrystalline massif
title_short Geoelectric studies of the south Voronezhcrystalline massif
title_sort geoelectric studies of the south voronezhcrystalline massif
topic electrical conductivity
the crust Voronezh Massif
topic_facet electrical conductivity
the crust Voronezh Massif
url https://journals.uran.ua/geofizicheskiy/article/view/116119
work_keys_str_mv AT logvinovi geoelectricstudiesofthesouthvoronezhcrystallinemassif
AT tregubenkovi geoelectricstudiesofthesouthvoronezhcrystallinemassif
AT tarasovvn geoelectricstudiesofthesouthvoronezhcrystallinemassif