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Geoelectric models of the earth's crust of Ukraine by the results of the magnetotelluric studies using new methods of inversions
Application of 1D anisotropic inversion (using methods of stochastic and directional decomposition analysis) and 3D inversion (by thin layer) to magnetotelluric data in the territory of Ukraine allowed to prove quantitatively the existence of conductive objects located at different depths and extend...
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Subbotin Institute of Geophysics of the NAS of Ukraine
2016
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journalsuranua-geofizicheskiy-article-918712020-10-07T11:18:21Z Geoelectric models of the earth's crust of Ukraine by the results of the magnetotelluric studies using new methods of inversions Kovachikova, S. Logvinov, I.M. Pek, J. Tarasov, V.N. conductivity structure Earth’s crust Ukrainian Carpathians Kirovograd anomaly of conductivity Voronezh massif decline Application of 1D anisotropic inversion (using methods of stochastic and directional decomposition analysis) and 3D inversion (by thin layer) to magnetotelluric data in the territory of Ukraine allowed to prove quantitatively the existence of conductive objects located at different depths and extending in intersecting directions. The importance of the use of these methods has been demonstrated by examples, linking results in the Carpathians, the Dnieper-Donets Basin, the slope of the Voronezh massif, Ukrainian shield with accommodation areas and areas of specific minerals, seismic and geo- and hydrothermal resources Subbotin Institute of Geophysics of the NAS of Ukraine 2016-12-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/91871 10.24028/gzh.0203-3100.v38i6.2016.91871 Geofizicheskiy Zhurnal; Vol. 38 No. 6 (2016); 83-100 Геофизический журнал; Том 38 № 6 (2016); 83-100 Геофізичний журнал; Том 38 № 6 (2016); 83-100 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/91871/87647 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
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Geofizicheskiy Zhurnal |
collection |
OJS |
language |
rus |
topic |
conductivity structure Earth’s crust Ukrainian Carpathians Kirovograd anomaly of conductivity Voronezh massif decline |
spellingShingle |
conductivity structure Earth’s crust Ukrainian Carpathians Kirovograd anomaly of conductivity Voronezh massif decline Kovachikova, S. Logvinov, I.M. Pek, J. Tarasov, V.N. Geoelectric models of the earth's crust of Ukraine by the results of the magnetotelluric studies using new methods of inversions |
topic_facet |
conductivity structure Earth’s crust Ukrainian Carpathians Kirovograd anomaly of conductivity Voronezh massif decline |
format |
Article |
author |
Kovachikova, S. Logvinov, I.M. Pek, J. Tarasov, V.N. |
author_facet |
Kovachikova, S. Logvinov, I.M. Pek, J. Tarasov, V.N. |
author_sort |
Kovachikova, S. |
title |
Geoelectric models of the earth's crust of Ukraine by the results of the magnetotelluric studies using new methods of inversions |
title_short |
Geoelectric models of the earth's crust of Ukraine by the results of the magnetotelluric studies using new methods of inversions |
title_full |
Geoelectric models of the earth's crust of Ukraine by the results of the magnetotelluric studies using new methods of inversions |
title_fullStr |
Geoelectric models of the earth's crust of Ukraine by the results of the magnetotelluric studies using new methods of inversions |
title_full_unstemmed |
Geoelectric models of the earth's crust of Ukraine by the results of the magnetotelluric studies using new methods of inversions |
title_sort |
geoelectric models of the earth's crust of ukraine by the results of the magnetotelluric studies using new methods of inversions |
description |
Application of 1D anisotropic inversion (using methods of stochastic and directional decomposition analysis) and 3D inversion (by thin layer) to magnetotelluric data in the territory of Ukraine allowed to prove quantitatively the existence of conductive objects located at different depths and extending in intersecting directions. The importance of the use of these methods has been demonstrated by examples, linking results in the Carpathians, the Dnieper-Donets Basin, the slope of the Voronezh massif, Ukrainian shield with accommodation areas and areas of specific minerals, seismic and geo- and hydrothermal resources |
publisher |
Subbotin Institute of Geophysics of the NAS of Ukraine |
publishDate |
2016 |
url |
https://journals.uran.ua/geofizicheskiy/article/view/91871 |
work_keys_str_mv |
AT kovachikovas geoelectricmodelsoftheearthscrustofukrainebytheresultsofthemagnetotelluricstudiesusingnewmethodsofinversions AT logvinovim geoelectricmodelsoftheearthscrustofukrainebytheresultsofthemagnetotelluricstudiesusingnewmethodsofinversions AT pekj geoelectricmodelsoftheearthscrustofukrainebytheresultsofthemagnetotelluricstudiesusingnewmethodsofinversions AT tarasovvn geoelectricmodelsoftheearthscrustofukrainebytheresultsofthemagnetotelluricstudiesusingnewmethodsofinversions |
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2024-04-21T19:39:44Z |
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2024-04-21T19:39:44Z |
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1796974454178316288 |