Dynamic analysis of earthquake phenomena by means of pseudo phase plane

Detalhes bibliográficos
Autor(a) principal: Lopes, António M.
Data de Publicação: 2013
Outros Autores: Machado, J. A. Tenreiro
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://hdl.handle.net/10400.22/3760
Resumo: This paper analyses earthquake data in the perspective of dynamical systems and its Pseudo Phase Plane representation. The seismic data is collected from the Bulletin of the International Seismological Centre. The geological events are characterised by their magnitude and geographical location and described by means of time series of sequences of Dirac impulses. Fifty groups of data series are considered, according to the Flinn-Engdahl seismic regions of Earth. For each region, Pearson’s correlation coefficient is used to find the optimal time delay for reconstructing the Pseudo Phase Plane. The Pseudo Phase Plane plots are then analysed and characterised.
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spelling Dynamic analysis of earthquake phenomena by means of pseudo phase planePseudo phase planePearson’s correlationOptimal time delaySeismic eventThis paper analyses earthquake data in the perspective of dynamical systems and its Pseudo Phase Plane representation. The seismic data is collected from the Bulletin of the International Seismological Centre. The geological events are characterised by their magnitude and geographical location and described by means of time series of sequences of Dirac impulses. Fifty groups of data series are considered, according to the Flinn-Engdahl seismic regions of Earth. For each region, Pearson’s correlation coefficient is used to find the optimal time delay for reconstructing the Pseudo Phase Plane. The Pseudo Phase Plane plots are then analysed and characterised.SpringerRepositório Científico do Instituto Politécnico do PortoLopes, António M.Machado, J. A. Tenreiro2014-02-06T15:53:48Z20132013-01-01T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10400.22/3760eng0924-090X10.1007/s11071-013-1034-1info:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2023-03-13T12:43:36Zoai:recipp.ipp.pt:10400.22/3760Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-19T17:24:45.247376Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse
dc.title.none.fl_str_mv Dynamic analysis of earthquake phenomena by means of pseudo phase plane
title Dynamic analysis of earthquake phenomena by means of pseudo phase plane
spellingShingle Dynamic analysis of earthquake phenomena by means of pseudo phase plane
Lopes, António M.
Pseudo phase plane
Pearson’s correlation
Optimal time delay
Seismic event
title_short Dynamic analysis of earthquake phenomena by means of pseudo phase plane
title_full Dynamic analysis of earthquake phenomena by means of pseudo phase plane
title_fullStr Dynamic analysis of earthquake phenomena by means of pseudo phase plane
title_full_unstemmed Dynamic analysis of earthquake phenomena by means of pseudo phase plane
title_sort Dynamic analysis of earthquake phenomena by means of pseudo phase plane
author Lopes, António M.
author_facet Lopes, António M.
Machado, J. A. Tenreiro
author_role author
author2 Machado, J. A. Tenreiro
author2_role author
dc.contributor.none.fl_str_mv Repositório Científico do Instituto Politécnico do Porto
dc.contributor.author.fl_str_mv Lopes, António M.
Machado, J. A. Tenreiro
dc.subject.por.fl_str_mv Pseudo phase plane
Pearson’s correlation
Optimal time delay
Seismic event
topic Pseudo phase plane
Pearson’s correlation
Optimal time delay
Seismic event
description This paper analyses earthquake data in the perspective of dynamical systems and its Pseudo Phase Plane representation. The seismic data is collected from the Bulletin of the International Seismological Centre. The geological events are characterised by their magnitude and geographical location and described by means of time series of sequences of Dirac impulses. Fifty groups of data series are considered, according to the Flinn-Engdahl seismic regions of Earth. For each region, Pearson’s correlation coefficient is used to find the optimal time delay for reconstructing the Pseudo Phase Plane. The Pseudo Phase Plane plots are then analysed and characterised.
publishDate 2013
dc.date.none.fl_str_mv 2013
2013-01-01T00:00:00Z
2014-02-06T15:53:48Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
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dc.identifier.uri.fl_str_mv http://hdl.handle.net/10400.22/3760
url http://hdl.handle.net/10400.22/3760
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv 0924-090X
10.1007/s11071-013-1034-1
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
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dc.publisher.none.fl_str_mv Springer
publisher.none.fl_str_mv Springer
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