A source time reversal method for seismicity induced by mining

In this work, we present a modified Time-Reversal Mirror (TRM) Method, called Source Time Reversal (STR), to find the spatial distribution of a seismic source induced by mining activity. This methodology is based on a known full description of the temporal dependence of the source, the Duhamel'...

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Detalles Bibliográficos
Autores: Brevis, R.I., Ortega, J.H., Pardo, D.
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2017
País:España
Institución:Basque Center for Applied Mathematics (BCAM)
Repositorio:BIRD. BCAM's Institutional Repository Data
OAI Identifier:oai:bird.bcamath.org:20.500.11824/365
Acceso en línea:http://hdl.handle.net/20.500.11824/365
Access Level:acceso embargado
Palabra clave:Source time reversal
time-reversal mirror
acoustic waves
induced seismicity
inverse problems
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spelling A source time reversal method for seismicity induced by miningBrevis, R.I.Ortega, J.H.Pardo, D.Source time reversaltime-reversal mirroracoustic wavesinduced seismicityinverse problemsIn this work, we present a modified Time-Reversal Mirror (TRM) Method, called Source Time Reversal (STR), to find the spatial distribution of a seismic source induced by mining activity. This methodology is based on a known full description of the temporal dependence of the source, the Duhamel's principle, and the time-reverse property of the wave equation. We also provide an error estimate of the reconstruction when the measurements are acquired over the entire boundary, and we show experimentally the influence of measuring on a subdomain of the boundary. Numerical results indicate that the methodology is able to recover continuous and discontinuous sources, and it remains stable for partial boundary measurements.info201720172017info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttp://hdl.handle.net/20.500.11824/365reponame:BIRD. BCAM's Institutional Repository Datainstname:Basque Center for Applied Mathematics (BCAM)Ingléshttp://www.aimsciences.org/journals/displayArticlesnew.jsp?paperID=13597info:eu-repo/grantAgreement/EC/H2020/644202info:eu-repo/grantAgreement/MINECO//SEV-2013-0323info:eu-repo/grantAgreement/MINECO//MTM2013-40824-Pinfo:eu-repo/grantAgreement/Gobierno Vasco/BERC/BERC.2014-2017info:eu-repo/grantAgreement/Gobierno Vasco/ELKARTEK/Reconocimiento-NoComercial-CompartirIgual 3.0 Españahttp://creativecommons.org/licenses/by-nc-sa/3.0/es/info:eu-repo/semantics/embargoedAccessoai:bird.bcamath.org:20.500.11824/3652026-06-19T12:47:47Z
dc.title.none.fl_str_mv A source time reversal method for seismicity induced by mining
title A source time reversal method for seismicity induced by mining
spellingShingle A source time reversal method for seismicity induced by mining
Brevis, R.I.
Source time reversal
time-reversal mirror
acoustic waves
induced seismicity
inverse problems
title_short A source time reversal method for seismicity induced by mining
title_full A source time reversal method for seismicity induced by mining
title_fullStr A source time reversal method for seismicity induced by mining
title_full_unstemmed A source time reversal method for seismicity induced by mining
title_sort A source time reversal method for seismicity induced by mining
dc.creator.none.fl_str_mv Brevis, R.I.
Ortega, J.H.
Pardo, D.
author Brevis, R.I.
author_facet Brevis, R.I.
Ortega, J.H.
Pardo, D.
author_role author
author2 Ortega, J.H.
Pardo, D.
author2_role author
author
dc.subject.none.fl_str_mv Source time reversal
time-reversal mirror
acoustic waves
induced seismicity
inverse problems
topic Source time reversal
time-reversal mirror
acoustic waves
induced seismicity
inverse problems
description In this work, we present a modified Time-Reversal Mirror (TRM) Method, called Source Time Reversal (STR), to find the spatial distribution of a seismic source induced by mining activity. This methodology is based on a known full description of the temporal dependence of the source, the Duhamel's principle, and the time-reverse property of the wave equation. We also provide an error estimate of the reconstruction when the measurements are acquired over the entire boundary, and we show experimentally the influence of measuring on a subdomain of the boundary. Numerical results indicate that the methodology is able to recover continuous and discontinuous sources, and it remains stable for partial boundary measurements.
publishDate 2017
dc.date.none.fl_str_mv 2017
2017
2017
info
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dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv http://www.aimsciences.org/journals/displayArticlesnew.jsp?paperID=13597
info:eu-repo/grantAgreement/EC/H2020/644202
info:eu-repo/grantAgreement/MINECO//SEV-2013-0323
info:eu-repo/grantAgreement/MINECO//MTM2013-40824-P
info:eu-repo/grantAgreement/Gobierno Vasco/BERC/BERC.2014-2017
info:eu-repo/grantAgreement/Gobierno Vasco/ELKARTEK/
dc.rights.none.fl_str_mv Reconocimiento-NoComercial-CompartirIgual 3.0 España
http://creativecommons.org/licenses/by-nc-sa/3.0/es/
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