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...
Saved in:
Date: | 2014 |
---|---|
Main Authors: | , , |
Format: | Article |
Language: | rus |
Published: |
Subbotin Institute of Geophysics of the NAS of Ukraine
2014
|
Subjects: | |
Online Access: | https://journals.uran.ua/geofizicheskiy/article/view/116119 |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Journal Title: | Geofizicheskiy Zhurnal |
Institution
Geofizicheskiy Zhurnalid |
journalsuranua-geofizicheskiy-article-116119 |
---|---|
record_format |
ojs |
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). 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 rus https://journals.uran.ua/geofizicheskiy/article/view/116119/110205 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
institution |
Geofizicheskiy Zhurnal |
collection |
OJS |
language |
rus |
topic |
electrical conductivity the crust Voronezh Massif |
spellingShingle |
electrical conductivity the crust Voronezh Massif Logvinov, I. Tregubenko, V. I. Tarasov, V. N. Geoelectric studies of the south Voronezhcrystalline massif |
topic_facet |
electrical conductivity the crust Voronezh Massif |
format |
Article |
author |
Logvinov, I. Tregubenko, V. I. Tarasov, V. N. |
author_facet |
Logvinov, I. Tregubenko, V. I. Tarasov, V. N. |
author_sort |
Logvinov, I. |
title |
Geoelectric studies of the south Voronezhcrystalline massif |
title_short |
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_sort |
geoelectric studies of the south voronezhcrystalline massif |
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). |
publisher |
Subbotin Institute of Geophysics of the NAS of Ukraine |
publishDate |
2014 |
url |
https://journals.uran.ua/geofizicheskiy/article/view/116119 |
work_keys_str_mv |
AT logvinovi geoelectricstudiesofthesouthvoronezhcrystallinemassif AT tregubenkovi geoelectricstudiesofthesouthvoronezhcrystallinemassif AT tarasovvn geoelectricstudiesofthesouthvoronezhcrystallinemassif |
first_indexed |
2024-04-21T19:40:34Z |
last_indexed |
2024-04-21T19:40:34Z |
_version_ |
1796974507821367296 |