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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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 |
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Open Polar |
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Copernicus Publications: E-Journals |
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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 |
_version_ |
1766051095216390144 |