Geoelectric model of consolidated Earth's crust and upper mantle along the geotraverse EUROBRIDGE-97

Along the profile EUROBRIDGE-97 11 local objects of low resistance (OLR) on the results of the two-dimensional inversion of magnetotelluric sounding have been found. Most of the objects are located in the transition layer of the crust. In the upper mantle of the northern part of the Pripyat Trough a...

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Date:2014
Main Authors: Astapenko, V.N., Logvinov, I.
Format: Article
Language:Russian
Published: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2014
Online Access:https://journals.uran.ua/geofizicheskiy/article/view/111575
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Journal Title:Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal
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author Astapenko, V.N.
Logvinov, I.
author_facet Astapenko, V.N.
Logvinov, I.
author_sort Astapenko, V.N.
baseUrl_str
collection OJS
datestamp_date 2020-10-07T11:55:34Z
description Along the profile EUROBRIDGE-97 11 local objects of low resistance (OLR) on the results of the two-dimensional inversion of magnetotelluric sounding have been found. Most of the objects are located in the transition layer of the crust. In the upper mantle of the northern part of the Pripyat Trough and of the south of the Ukrainian Shield conductivity objects spatially consistent with the high values of heat flow were found. Connection of OPS with seismic sections along the profile has been considered.
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publisher S. Subbotin Institute of Geophysics of the NAS of Ukraine
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spelling journalsuranua-geofizicheskiy-article-1115752020-10-07T11:55:34Z Geoelectric model of consolidated Earth's crust and upper mantle along the geotraverse EUROBRIDGE-97 Astapenko, V.N. Logvinov, I. Along the profile EUROBRIDGE-97 11 local objects of low resistance (OLR) on the results of the two-dimensional inversion of magnetotelluric sounding have been found. Most of the objects are located in the transition layer of the crust. In the upper mantle of the northern part of the Pripyat Trough and of the south of the Ukrainian Shield conductivity objects spatially consistent with the high values of heat flow were found. Connection of OPS with seismic sections along the profile has been considered. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2014-10-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/111575 10.24028/gzh.0203-3100.v36i5.2014.111575 Geofizicheskiy Zhurnal; Vol. 36 No. 5 (2014); 143-155 Геофизический журнал; Том 36 № 5 (2014); 143-155 Геофізичний журнал; Том 36 № 5 (2014); 143-155 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/111575/106564 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle Astapenko, V.N.
Logvinov, I.
Geoelectric model of consolidated Earth's crust and upper mantle along the geotraverse EUROBRIDGE-97
title Geoelectric model of consolidated Earth's crust and upper mantle along the geotraverse EUROBRIDGE-97
title_full Geoelectric model of consolidated Earth's crust and upper mantle along the geotraverse EUROBRIDGE-97
title_fullStr Geoelectric model of consolidated Earth's crust and upper mantle along the geotraverse EUROBRIDGE-97
title_full_unstemmed Geoelectric model of consolidated Earth's crust and upper mantle along the geotraverse EUROBRIDGE-97
title_short Geoelectric model of consolidated Earth's crust and upper mantle along the geotraverse EUROBRIDGE-97
title_sort geoelectric model of consolidated earth's crust and upper mantle along the geotraverse eurobridge-97
url https://journals.uran.ua/geofizicheskiy/article/view/111575
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AT logvinovi geoelectricmodelofconsolidatedearthscrustanduppermantlealongthegeotraverseeurobridge97