DETECTION PRECURSORY ANOMALIES OF ZHUPANOVSKY EARTHQUAKE ON JANUARY 30, 2016 WITH MW = 7.2 AND A DEPTH OF FOCUS 171 KM (KAMCHATKA) BY EIGENOSCOPY METHOD
This paper describes application of the eigenoscopy technique for analyzing the collective behavior of soil radon time series in order to detect the precursory anomalies before the deep Zhupanovsky earthquake with M = 7.2. Eigenoscope (from English .eigenvector.) or analyzer of eigenvectors and sign...
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ftdoajarticles:oai:doaj.org/article:ae5878349cfa4040828f4f7de5635b1b 2023-05-15T16:59:11+02:00 DETECTION PRECURSORY ANOMALIES OF ZHUPANOVSKY EARTHQUAKE ON JANUARY 30, 2016 WITH MW = 7.2 AND A DEPTH OF FOCUS 171 KM (KAMCHATKA) BY EIGENOSCOPY METHOD P.P. Firstov D.V. Isakevich V.V. Isakevich D.I. Budilov E.O. Makarov L.V. Grunskaya 2017-12-01T00:00:00Z https://doi.org/10.18454/2079-6641-2017-20-4-109-120 https://doaj.org/article/ae5878349cfa4040828f4f7de5635b1b EN RU eng rus KamGU by Vitus Bering http://krasec.ru/wp-content/uploads/2017/12/Firstov.pdf https://doaj.org/toc/2079-6641 https://doaj.org/toc/2079-665X doi:10.18454/2079-6641-2017-20-4-109-120 2079-6641 2079-665X https://doaj.org/article/ae5878349cfa4040828f4f7de5635b1b Vestnik KRAUNC: Fiziko-Matematičeskie Nauki, Iss 4(20), Pp 109-120 (2017) soil radon eigenoscopy reference point precursory anomaly earthquake forecast Science Q article 2017 ftdoajarticles https://doi.org/10.18454/2079-6641-2017-20-4-109-120 2022-12-31T08:11:26Z This paper describes application of the eigenoscopy technique for analyzing the collective behavior of soil radon time series in order to detect the precursory anomalies before the deep Zhupanovsky earthquake with M = 7.2. Eigenoscope (from English .eigenvector.) or analyzer of eigenvectors and signal components. is a virtual device that allows us to detect the reference points of collective behavior in multidimensional time series. The multidimensional time series (01.08.2015-17.02.2016), obtained at the network of subsoil radon monitoring stations of the Petropavlovsk-Kamchatsky geodynamic test area, are considered. Before the deep earthquake with M = 7.2, which occurred at a distance of 120 km from the registration point, a reference point in the dynamics of soil radon, which can be considered as a precursory anomaly, was confidently detected with the help of the eigenoscopy method. Article in Journal/Newspaper Kamchatka Directory of Open Access Journals: DOAJ Articles Petropavlovsk ENVELOPE(158.626,158.626,53.067,53.067) Petropavlovsk-Kamchatsky ENVELOPE(158.651,158.651,53.044,53.044) |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English Russian |
topic |
soil radon eigenoscopy reference point precursory anomaly earthquake forecast Science Q |
spellingShingle |
soil radon eigenoscopy reference point precursory anomaly earthquake forecast Science Q P.P. Firstov D.V. Isakevich V.V. Isakevich D.I. Budilov E.O. Makarov L.V. Grunskaya DETECTION PRECURSORY ANOMALIES OF ZHUPANOVSKY EARTHQUAKE ON JANUARY 30, 2016 WITH MW = 7.2 AND A DEPTH OF FOCUS 171 KM (KAMCHATKA) BY EIGENOSCOPY METHOD |
topic_facet |
soil radon eigenoscopy reference point precursory anomaly earthquake forecast Science Q |
description |
This paper describes application of the eigenoscopy technique for analyzing the collective behavior of soil radon time series in order to detect the precursory anomalies before the deep Zhupanovsky earthquake with M = 7.2. Eigenoscope (from English .eigenvector.) or analyzer of eigenvectors and signal components. is a virtual device that allows us to detect the reference points of collective behavior in multidimensional time series. The multidimensional time series (01.08.2015-17.02.2016), obtained at the network of subsoil radon monitoring stations of the Petropavlovsk-Kamchatsky geodynamic test area, are considered. Before the deep earthquake with M = 7.2, which occurred at a distance of 120 km from the registration point, a reference point in the dynamics of soil radon, which can be considered as a precursory anomaly, was confidently detected with the help of the eigenoscopy method. |
format |
Article in Journal/Newspaper |
author |
P.P. Firstov D.V. Isakevich V.V. Isakevich D.I. Budilov E.O. Makarov L.V. Grunskaya |
author_facet |
P.P. Firstov D.V. Isakevich V.V. Isakevich D.I. Budilov E.O. Makarov L.V. Grunskaya |
author_sort |
P.P. Firstov |
title |
DETECTION PRECURSORY ANOMALIES OF ZHUPANOVSKY EARTHQUAKE ON JANUARY 30, 2016 WITH MW = 7.2 AND A DEPTH OF FOCUS 171 KM (KAMCHATKA) BY EIGENOSCOPY METHOD |
title_short |
DETECTION PRECURSORY ANOMALIES OF ZHUPANOVSKY EARTHQUAKE ON JANUARY 30, 2016 WITH MW = 7.2 AND A DEPTH OF FOCUS 171 KM (KAMCHATKA) BY EIGENOSCOPY METHOD |
title_full |
DETECTION PRECURSORY ANOMALIES OF ZHUPANOVSKY EARTHQUAKE ON JANUARY 30, 2016 WITH MW = 7.2 AND A DEPTH OF FOCUS 171 KM (KAMCHATKA) BY EIGENOSCOPY METHOD |
title_fullStr |
DETECTION PRECURSORY ANOMALIES OF ZHUPANOVSKY EARTHQUAKE ON JANUARY 30, 2016 WITH MW = 7.2 AND A DEPTH OF FOCUS 171 KM (KAMCHATKA) BY EIGENOSCOPY METHOD |
title_full_unstemmed |
DETECTION PRECURSORY ANOMALIES OF ZHUPANOVSKY EARTHQUAKE ON JANUARY 30, 2016 WITH MW = 7.2 AND A DEPTH OF FOCUS 171 KM (KAMCHATKA) BY EIGENOSCOPY METHOD |
title_sort |
detection precursory anomalies of zhupanovsky earthquake on january 30, 2016 with mw = 7.2 and a depth of focus 171 km (kamchatka) by eigenoscopy method |
publisher |
KamGU by Vitus Bering |
publishDate |
2017 |
url |
https://doi.org/10.18454/2079-6641-2017-20-4-109-120 https://doaj.org/article/ae5878349cfa4040828f4f7de5635b1b |
long_lat |
ENVELOPE(158.626,158.626,53.067,53.067) ENVELOPE(158.651,158.651,53.044,53.044) |
geographic |
Petropavlovsk Petropavlovsk-Kamchatsky |
geographic_facet |
Petropavlovsk Petropavlovsk-Kamchatsky |
genre |
Kamchatka |
genre_facet |
Kamchatka |
op_source |
Vestnik KRAUNC: Fiziko-Matematičeskie Nauki, Iss 4(20), Pp 109-120 (2017) |
op_relation |
http://krasec.ru/wp-content/uploads/2017/12/Firstov.pdf https://doaj.org/toc/2079-6641 https://doaj.org/toc/2079-665X doi:10.18454/2079-6641-2017-20-4-109-120 2079-6641 2079-665X https://doaj.org/article/ae5878349cfa4040828f4f7de5635b1b |
op_doi |
https://doi.org/10.18454/2079-6641-2017-20-4-109-120 |
_version_ |
1766051396638998528 |