A new approach to earthquake precursors distinction

A lithospheric ultra low frequency (ULF) magnetic activity is recently considered as very promising candidate for application to short-time earthquake (EQ) forecasting. However the ULF lithospheric magnetic field is very weak and masked by much stronger ionospheric and magnetospheric signals. The st...

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Бібліографічні деталі
Дата:2012
Автори: Korepanov, V. E., Dudkin, F. L.
Формат: Стаття
Мова:rus
Опубліковано: Subbotin Institute of Geophysics of the NAS of Ukraine 2012
Онлайн доступ:https://journals.uran.ua/geofizicheskiy/article/view/116763
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Назва журналу:Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal
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spelling journalsuranua-geofizicheskiy-article-1167632020-10-07T12:21:33Z A new approach to earthquake precursors distinction Korepanov, V. E. Dudkin, F. L. A lithospheric ultra low frequency (ULF) magnetic activity is recently considered as very promising candidate for application to short-time earthquake (EQ) forecasting. However the ULF lithospheric magnetic field is very weak and masked by much stronger ionospheric and magnetospheric signals. The study of pre-earthquake magnetic activity is very hard problem which consists of identification and localization of weak signal sources in seismo-hazardous area of the Earth crust. A new approach is developed to find a source of pre-EQ ULF electromagnetic activity of lithospheric origin. For separation and localization of EQ magnetic precursors the polarization ellipse technique has been developed to process the measurements data acquired from 3-component magnetometers. The method efficiency is illustrated at the example of the data from fluxgate magnetometers installed in Sichuan province. The Panzhihua earthquake with magnitude Mw 6,0 was happened in the southern part of Sichuan province on August 30, 2008 at 8:30:52 UT. The EQ hypocentre was located in point 26,28 N, 101,92 E at depth 10 km. Subbotin Institute of Geophysics of the NAS of Ukraine 2012-08-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116763 10.24028/gzh.0203-3100.v34i4.2012.116763 Geofizicheskiy Zhurnal; Vol. 34 No. 4 (2012); 150-156 Геофизический журнал; Том 34 № 4 (2012); 150-156 Геофізичний журнал; Том 34 № 4 (2012); 150-156 2524-1052 0203-3100 rus https://journals.uran.ua/geofizicheskiy/article/view/116763/110826 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0
institution Geofizicheskiy Zhurnal
collection OJS
language rus
format Article
author Korepanov, V. E.
Dudkin, F. L.
spellingShingle Korepanov, V. E.
Dudkin, F. L.
A new approach to earthquake precursors distinction
author_facet Korepanov, V. E.
Dudkin, F. L.
author_sort Korepanov, V. E.
title A new approach to earthquake precursors distinction
title_short A new approach to earthquake precursors distinction
title_full A new approach to earthquake precursors distinction
title_fullStr A new approach to earthquake precursors distinction
title_full_unstemmed A new approach to earthquake precursors distinction
title_sort new approach to earthquake precursors distinction
description A lithospheric ultra low frequency (ULF) magnetic activity is recently considered as very promising candidate for application to short-time earthquake (EQ) forecasting. However the ULF lithospheric magnetic field is very weak and masked by much stronger ionospheric and magnetospheric signals. The study of pre-earthquake magnetic activity is very hard problem which consists of identification and localization of weak signal sources in seismo-hazardous area of the Earth crust. A new approach is developed to find a source of pre-EQ ULF electromagnetic activity of lithospheric origin. For separation and localization of EQ magnetic precursors the polarization ellipse technique has been developed to process the measurements data acquired from 3-component magnetometers. The method efficiency is illustrated at the example of the data from fluxgate magnetometers installed in Sichuan province. The Panzhihua earthquake with magnitude Mw 6,0 was happened in the southern part of Sichuan province on August 30, 2008 at 8:30:52 UT. The EQ hypocentre was located in point 26,28 N, 101,92 E at depth 10 km.
publisher Subbotin Institute of Geophysics of the NAS of Ukraine
publishDate 2012
url https://journals.uran.ua/geofizicheskiy/article/view/116763
work_keys_str_mv AT korepanovve anewapproachtoearthquakeprecursorsdistinction
AT dudkinfl anewapproachtoearthquakeprecursorsdistinction
AT korepanovve newapproachtoearthquakeprecursorsdistinction
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first_indexed 2024-04-21T19:41:19Z
last_indexed 2024-04-21T19:41:19Z
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