Geoelectric model of the crust and upper mantle along DSS profile Novoazovsk—Titovka

The results of two-dimensional inversion of magnetoteluric data, focused along the DSS profile Novoazovsk—Titovka have been presented. On the territory of Donbas two objects have been distinguished with low resistance (causing Donbass conductivity anomaly) which occur: in the southern part in sedime...

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Datum:2015
Hauptverfasser: Logvinov, I., Tarasov, V.
Format: Artikel
Sprache:Russisch
Veröffentlicht: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2015
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Online Zugang:https://journals.uran.ua/geofizicheskiy/article/view/111115
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Geofizicheskiy Zhurnal
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author Logvinov, I.
Tarasov, V.
author_facet Logvinov, I.
Tarasov, V.
author_sort Logvinov, I.
baseUrl_str
collection OJS
datestamp_date 2020-10-07T11:39:25Z
description The results of two-dimensional inversion of magnetoteluric data, focused along the DSS profile Novoazovsk—Titovka have been presented. On the territory of Donbas two objects have been distinguished with low resistance (causing Donbass conductivity anomaly) which occur: in the southern part in sedimentary rocks (at a depth of 1—10 km), in the central part (at a depth of 1—18 km) in sedimentary rocks and penetrating into consolidated crust. Total cumulative integral conductivity of the objects is about 3×108 S×m. The most reliably the objects spatially correlate with the coal-bearing rocks of the Carboniferous.
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spelling journalsuranua-geofizicheskiy-article-1111152020-10-07T11:39:25Z Geoelectric model of the crust and upper mantle along DSS profile Novoazovsk—Titovka Logvinov, I. Tarasov, V. electroconductivity crust and upper mantle Donbas The results of two-dimensional inversion of magnetoteluric data, focused along the DSS profile Novoazovsk—Titovka have been presented. On the territory of Donbas two objects have been distinguished with low resistance (causing Donbass conductivity anomaly) which occur: in the southern part in sedimentary rocks (at a depth of 1—10 km), in the central part (at a depth of 1—18 km) in sedimentary rocks and penetrating into consolidated crust. Total cumulative integral conductivity of the objects is about 3×108 S×m. The most reliably the objects spatially correlate with the coal-bearing rocks of the Carboniferous. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2015-06-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/111115 10.24028/gzh.0203-3100.v37i3.2015.111115 Geofizicheskiy Zhurnal; Vol. 37 No. 3 (2015); 139-152 Геофизический журнал; Том 37 № 3 (2015); 139-152 Геофізичний журнал; Том 37 № 3 (2015); 139-152 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/111115/105981 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle electroconductivity
crust and upper mantle
Donbas
Logvinov, I.
Tarasov, V.
Geoelectric model of the crust and upper mantle along DSS profile Novoazovsk—Titovka
title Geoelectric model of the crust and upper mantle along DSS profile Novoazovsk—Titovka
title_full Geoelectric model of the crust and upper mantle along DSS profile Novoazovsk—Titovka
title_fullStr Geoelectric model of the crust and upper mantle along DSS profile Novoazovsk—Titovka
title_full_unstemmed Geoelectric model of the crust and upper mantle along DSS profile Novoazovsk—Titovka
title_short Geoelectric model of the crust and upper mantle along DSS profile Novoazovsk—Titovka
title_sort geoelectric model of the crust and upper mantle along dss profile novoazovsk—titovka
topic electroconductivity
crust and upper mantle
Donbas
topic_facet electroconductivity
crust and upper mantle
Donbas
url https://journals.uran.ua/geofizicheskiy/article/view/111115
work_keys_str_mv AT logvinovi geoelectricmodelofthecrustanduppermantlealongdssprofilenovoazovsktitovka
AT tarasovv geoelectricmodelofthecrustanduppermantlealongdssprofilenovoazovsktitovka