Multiparameter approach in the deep geoelectrics
The main provisions of geoelectrics are described, the importance of taking into account the ambiguity of its inverse problem is emphasized. Three main methods of deep geoelectrics which use natural fields of ionospheric-magnetospheric origin are considered: geomagnetic deep sounding (GDS), magnetot...
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Subbotin Institute of Geophysics of the NAS of Ukraine
2021
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fturanojs:oai:ojs.journals.uran.ua:article/244081 2023-05-15T17:05:03+02:00 Multiparameter approach in the deep geoelectrics Многопараметрический подход в глубинной геоэлектрике Багатопараметричний підхід у глибинній геоелектриці Рокитянський, І. І. Терешин, А. В. 2021-11-24 application/pdf http://journals.uran.ua/geofizicheskiy/article/view/244081 rus rus Subbotin Institute of Geophysics of the NAS of Ukraine http://journals.uran.ua/geofizicheskiy/article/view/244081/242799 http://journals.uran.ua/geofizicheskiy/article/view/244081 http://creativecommons.org/licenses/by/4.0 CC-BY Geophysical Journal; Том 43 № 5 (2021); 193-207 Geofizicheskiy Zhurnal; Vol. 43 No. 5 (2021); 193-207 Геофизический журнал; Том 43 № 5 (2021); 193-207 2524-1052 0203-3100 глубинная геоэлектрика функции отклика электропроводность Земли deep geoelectrics response function Earth electrical conductivity глибинна геоелектрика функції відгуку електропровідність Землі info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2021 fturanojs 2022-09-06T03:26:08Z The main provisions of geoelectrics are described, the importance of taking into account the ambiguity of its inverse problem is emphasized. Three main methods of deep geoelectrics which use natural fields of ionospheric-magnetospheric origin are considered: geomagnetic deep sounding (GDS), magnetotelluric sounding (MTS), and magnetovariational profiling (MVP). The response functions of each method are described. Each response function carries its own specific information about some parameters of the studied object and is characterized by the degree of reliability of the information about the object extracted from it. For example, the most reliable information about electrical conductivity anomalies (if any in the study area) is contained in the MVP response functions. The horizontal tensor of the anomalous field contains information about the electrical conductivity under the observation point, and the tipper (induction vector) contains information from the surrounding areas. In general, MVP information is less susceptible to distortions than MTS information and deserves more trust. Artificial field sources in deep geoelectrics are rarely used due to their high cost. Since 1970, two powerful sources created for other purposes arised on the Kola Peninsula and were used for deep sounding. In the center of these studies found themself young talented geologist-geophysicist and organizer of major projects AbdulkhaiAzimovichZhamaletdinov. The «Khibiny» project with an MHD generator and an ultra-deep well as one of the objects of the study, the «Zeus» low-frequency emitter, the signals of which were recorded in China at a distance of 7000 km, and a number of projects conceived and organized by Zhamaletdinov and executed under his leadership: «Volgograd-Donbass» (1979, 1986), experiments «PHOENIX» (2007, 2009, 2014, 2019) and others. At the same time, methods of interpretation were developed for sounding with artificial EM sources and new response functions were obtained which make it possible to «see» the object of ... Article in Journal/Newspaper kola peninsula Scientific Periodicals of Ukraine (Ukrainian Research and Academic Network) Khibiny ENVELOPE(33.210,33.210,67.679,67.679) Kola Peninsula Zeus ENVELOPE(140.020,140.020,-66.661,-66.661) |
institution |
Open Polar |
collection |
Scientific Periodicals of Ukraine (Ukrainian Research and Academic Network) |
op_collection_id |
fturanojs |
language |
Russian |
topic |
глубинная геоэлектрика функции отклика электропроводность Земли deep geoelectrics response function Earth electrical conductivity глибинна геоелектрика функції відгуку електропровідність Землі |
spellingShingle |
глубинная геоэлектрика функции отклика электропроводность Земли deep geoelectrics response function Earth electrical conductivity глибинна геоелектрика функції відгуку електропровідність Землі Рокитянський, І. І. Терешин, А. В. Multiparameter approach in the deep geoelectrics |
topic_facet |
глубинная геоэлектрика функции отклика электропроводность Земли deep geoelectrics response function Earth electrical conductivity глибинна геоелектрика функції відгуку електропровідність Землі |
description |
The main provisions of geoelectrics are described, the importance of taking into account the ambiguity of its inverse problem is emphasized. Three main methods of deep geoelectrics which use natural fields of ionospheric-magnetospheric origin are considered: geomagnetic deep sounding (GDS), magnetotelluric sounding (MTS), and magnetovariational profiling (MVP). The response functions of each method are described. Each response function carries its own specific information about some parameters of the studied object and is characterized by the degree of reliability of the information about the object extracted from it. For example, the most reliable information about electrical conductivity anomalies (if any in the study area) is contained in the MVP response functions. The horizontal tensor of the anomalous field contains information about the electrical conductivity under the observation point, and the tipper (induction vector) contains information from the surrounding areas. In general, MVP information is less susceptible to distortions than MTS information and deserves more trust. Artificial field sources in deep geoelectrics are rarely used due to their high cost. Since 1970, two powerful sources created for other purposes arised on the Kola Peninsula and were used for deep sounding. In the center of these studies found themself young talented geologist-geophysicist and organizer of major projects AbdulkhaiAzimovichZhamaletdinov. The «Khibiny» project with an MHD generator and an ultra-deep well as one of the objects of the study, the «Zeus» low-frequency emitter, the signals of which were recorded in China at a distance of 7000 km, and a number of projects conceived and organized by Zhamaletdinov and executed under his leadership: «Volgograd-Donbass» (1979, 1986), experiments «PHOENIX» (2007, 2009, 2014, 2019) and others. At the same time, methods of interpretation were developed for sounding with artificial EM sources and new response functions were obtained which make it possible to «see» the object of ... |
format |
Article in Journal/Newspaper |
author |
Рокитянський, І. І. Терешин, А. В. |
author_facet |
Рокитянський, І. І. Терешин, А. В. |
author_sort |
Рокитянський, І. І. |
title |
Multiparameter approach in the deep geoelectrics |
title_short |
Multiparameter approach in the deep geoelectrics |
title_full |
Multiparameter approach in the deep geoelectrics |
title_fullStr |
Multiparameter approach in the deep geoelectrics |
title_full_unstemmed |
Multiparameter approach in the deep geoelectrics |
title_sort |
multiparameter approach in the deep geoelectrics |
publisher |
Subbotin Institute of Geophysics of the NAS of Ukraine |
publishDate |
2021 |
url |
http://journals.uran.ua/geofizicheskiy/article/view/244081 |
long_lat |
ENVELOPE(33.210,33.210,67.679,67.679) ENVELOPE(140.020,140.020,-66.661,-66.661) |
geographic |
Khibiny Kola Peninsula Zeus |
geographic_facet |
Khibiny Kola Peninsula Zeus |
genre |
kola peninsula |
genre_facet |
kola peninsula |
op_source |
Geophysical Journal; Том 43 № 5 (2021); 193-207 Geofizicheskiy Zhurnal; Vol. 43 No. 5 (2021); 193-207 Геофизический журнал; Том 43 № 5 (2021); 193-207 2524-1052 0203-3100 |
op_relation |
http://journals.uran.ua/geofizicheskiy/article/view/244081/242799 http://journals.uran.ua/geofizicheskiy/article/view/244081 |
op_rights |
http://creativecommons.org/licenses/by/4.0 |
op_rightsnorm |
CC-BY |
_version_ |
1766059428530880512 |