Results of experimental electromagnetic studies of the Crimean region

Spatial-temporal pattern of distribution of geomagnetic variations and the electric field on the Earth’s surface was obtained as a result of the modern experimental observations conducted in 2007—2013 along 9 profiles (48 points) by the methods of magnetotelluric sounding (MTS) and magnetovariation...

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Datum:2016
Hauptverfasser: Burakhovich, T. K., Kushnir, A. M., Nikolaev, I. Yu., Sheremet, E. M., Shirkov, B. I.
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Sprache:Russisch
Veröffentlicht: S. Subbotin Institute of Geophysics of the NAS of Ukraine 2016
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Online Zugang:https://journals.uran.ua/geofizicheskiy/article/view/107765
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Geofizicheskiy Zhurnal
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author Burakhovich, T. K.
Kushnir, A. M.
Nikolaev, I. Yu.
Sheremet, E. M.
Shirkov, B. I.
author_facet Burakhovich, T. K.
Kushnir, A. M.
Nikolaev, I. Yu.
Sheremet, E. M.
Shirkov, B. I.
author_sort Burakhovich, T. K.
baseUrl_str
collection OJS
datestamp_date 2020-10-07T11:34:21Z
description Spatial-temporal pattern of distribution of geomagnetic variations and the electric field on the Earth’s surface was obtained as a result of the modern experimental observations conducted in 2007—2013 along 9 profiles (48 points) by the methods of magnetotelluric sounding (MTS) and magnetovariation profiling (MVP). These profiles cross various geological structures of the Crimean region. It is possible to estimate the value of the electrical conductivity and vertical and horizontal geoelectric structure. The processing of these data is done using modern software system PRC_MTMV (author Varentsov Iv. M.) that provides the common noise-protected evaluation of the impedance, tipper, horizontal magnetovariation response according to the synchronous MT/MV records.The main result of qualitative interpretation of geoelectric research is the detection of high conductivity regions in the Earth's crust and upper mantle of the Crimea, that are characterized by the variations of conductivity, depth and configuration. They characterize the various geological structures differently. The subvertical conductive zones often coincide with the fault structures, most of these objects are confined to the suture zones between tectonic elements such as the East European platform and the Scythian plate, the Scythian plate and the Crimea mountain, North and South Kerch zone. This fact may reflect the high permeability of the suture zones for deep fluids in the process of their formation.Some high conductivity anomalies are well-described in the literature and are known. For example, the unique Tarhankut conductivity anomaly, located not only on the eponymous peninsula of Crimea, but also under the water area of the north-western part of the Black sea. This anomaly was detailed and precised and involves a complex multi-level deep structure of the region. In addition, the structurally complex conductivity anomaly is assumed in the Sivash graben and the Kerch Peninsula.Although the qualitative interpretation of the experimental data of magnetotelluric sounding (MTS) and magnetovariation profiling (MVP) provides the inconsistent understanding of the depth distribution of the Crimean region electrical conductivity, the combination of these methods allows to construct the model of the resistivity distribution within a three-dimensional environment much more accurately and adequately to the observed experimental data.
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spelling journalsuranua-geofizicheskiy-article-1077652020-10-07T11:34:21Z Results of experimental electromagnetic studies of the Crimean region Burakhovich, T. K. Kushnir, A. M. Nikolaev, I. Yu. Sheremet, E. M. Shirkov, B. I. experimental electromagnetic studies anomalies of conductivity the Earth's crust and upper mantle the Crimean region Spatial-temporal pattern of distribution of geomagnetic variations and the electric field on the Earth’s surface was obtained as a result of the modern experimental observations conducted in 2007—2013 along 9 profiles (48 points) by the methods of magnetotelluric sounding (MTS) and magnetovariation profiling (MVP). These profiles cross various geological structures of the Crimean region. It is possible to estimate the value of the electrical conductivity and vertical and horizontal geoelectric structure. The processing of these data is done using modern software system PRC_MTMV (author Varentsov Iv. M.) that provides the common noise-protected evaluation of the impedance, tipper, horizontal magnetovariation response according to the synchronous MT/MV records.The main result of qualitative interpretation of geoelectric research is the detection of high conductivity regions in the Earth's crust and upper mantle of the Crimea, that are characterized by the variations of conductivity, depth and configuration. They characterize the various geological structures differently. The subvertical conductive zones often coincide with the fault structures, most of these objects are confined to the suture zones between tectonic elements such as the East European platform and the Scythian plate, the Scythian plate and the Crimea mountain, North and South Kerch zone. This fact may reflect the high permeability of the suture zones for deep fluids in the process of their formation.Some high conductivity anomalies are well-described in the literature and are known. For example, the unique Tarhankut conductivity anomaly, located not only on the eponymous peninsula of Crimea, but also under the water area of the north-western part of the Black sea. This anomaly was detailed and precised and involves a complex multi-level deep structure of the region. In addition, the structurally complex conductivity anomaly is assumed in the Sivash graben and the Kerch Peninsula.Although the qualitative interpretation of the experimental data of magnetotelluric sounding (MTS) and magnetovariation profiling (MVP) provides the inconsistent understanding of the depth distribution of the Crimean region electrical conductivity, the combination of these methods allows to construct the model of the resistivity distribution within a three-dimensional environment much more accurately and adequately to the observed experimental data. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2016-07-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/107765 10.24028/gzh.0203-3100.v38i2.2016.107765 Geofizicheskiy Zhurnal; Vol. 38 No. 2 (2016); 57-78 Геофизический журнал; Том 38 № 2 (2016); 57-78 Геофізичний журнал; Том 38 № 2 (2016); 57-78 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/107765/102719 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
spellingShingle experimental electromagnetic studies
anomalies of conductivity
the Earth's crust and upper mantle
the Crimean region
Burakhovich, T. K.
Kushnir, A. M.
Nikolaev, I. Yu.
Sheremet, E. M.
Shirkov, B. I.
Results of experimental electromagnetic studies of the Crimean region
title Results of experimental electromagnetic studies of the Crimean region
title_full Results of experimental electromagnetic studies of the Crimean region
title_fullStr Results of experimental electromagnetic studies of the Crimean region
title_full_unstemmed Results of experimental electromagnetic studies of the Crimean region
title_short Results of experimental electromagnetic studies of the Crimean region
title_sort results of experimental electromagnetic studies of the crimean region
topic experimental electromagnetic studies
anomalies of conductivity
the Earth's crust and upper mantle
the Crimean region
topic_facet experimental electromagnetic studies
anomalies of conductivity
the Earth's crust and upper mantle
the Crimean region
url https://journals.uran.ua/geofizicheskiy/article/view/107765
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