Electromagnetic signals of crust creep motion

A method of registration and allocation of the nearest located sources of natural electromagnetic radiation is developed. Most likely, these sourses in seismically active regions originate from lithisperes. A short description of this method is given. We have carried out a field experiment in the re...

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Main Authors: Uvarov, V. N., Drushin, G. I., Sannikov, D. V.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/sed-3-335-2011
https://se.copernicus.org/preprints/se-2010-26/
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spelling ftcopernicus:oai:publications.copernicus.org:sed9985 2023-05-15T16:58:57+02:00 Electromagnetic signals of crust creep motion Uvarov, V. N. Drushin, G. I. Sannikov, D. V. 2018-09-26 application/pdf https://doi.org/10.5194/sed-3-335-2011 https://se.copernicus.org/preprints/se-2010-26/ eng eng doi:10.5194/sed-3-335-2011 https://se.copernicus.org/preprints/se-2010-26/ eISSN: 1869-9529 Text 2018 ftcopernicus https://doi.org/10.5194/sed-3-335-2011 2020-07-20T16:26:09Z A method of registration and allocation of the nearest located sources of natural electromagnetic radiation is developed. Most likely, these sourses in seismically active regions originate from lithisperes. A short description of this method is given. We have carried out a field experiment in the region with small levels of technical noise and high levels of micro-seismic activity (Kamchatka, r. Karimschyna). A number of fragments of the received data are analysed. A large variety of registered signals are shown. It is shown that the most probable source of these signals has lithospheres origin. Text Kamchatka Copernicus Publications: E-Journals
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description A method of registration and allocation of the nearest located sources of natural electromagnetic radiation is developed. Most likely, these sourses in seismically active regions originate from lithisperes. A short description of this method is given. We have carried out a field experiment in the region with small levels of technical noise and high levels of micro-seismic activity (Kamchatka, r. Karimschyna). A number of fragments of the received data are analysed. A large variety of registered signals are shown. It is shown that the most probable source of these signals has lithospheres origin.
format Text
author Uvarov, V. N.
Drushin, G. I.
Sannikov, D. V.
spellingShingle Uvarov, V. N.
Drushin, G. I.
Sannikov, D. V.
Electromagnetic signals of crust creep motion
author_facet Uvarov, V. N.
Drushin, G. I.
Sannikov, D. V.
author_sort Uvarov, V. N.
title Electromagnetic signals of crust creep motion
title_short Electromagnetic signals of crust creep motion
title_full Electromagnetic signals of crust creep motion
title_fullStr Electromagnetic signals of crust creep motion
title_full_unstemmed Electromagnetic signals of crust creep motion
title_sort electromagnetic signals of crust creep motion
publishDate 2018
url https://doi.org/10.5194/sed-3-335-2011
https://se.copernicus.org/preprints/se-2010-26/
genre Kamchatka
genre_facet Kamchatka
op_source eISSN: 1869-9529
op_relation doi:10.5194/sed-3-335-2011
https://se.copernicus.org/preprints/se-2010-26/
op_doi https://doi.org/10.5194/sed-3-335-2011
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