Uncertainties in earthquake source spectrum estimation using empirical green functions

We analyze the problem of reliably estimating uncertainties of the earthquake source spectrum and related source parameters using Empirical Green Functions (EGF). We take advantage of the large dataset available from 10 seismic stations at hypocentral distances (10 km < d < 50 km) to average s...

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Autores:
Tipo de recurso:
Fecha de publicación:
2006
Institución:
Universidad del Rosario
Repositorio:
Repositorio EdocUR - U. Rosario
Idioma:
eng
OAI Identifier:
oai:repository.urosario.edu.co:10336/28503
Acceso en línea:
https://doi.org/10.1029/170GM08
https://repository.urosario.edu.co/handle/10336/28503
Palabra clave:
Seismic wave
Energy dissipation
Faults (Geology)
Seismology
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Restringido (Acceso a grupos específicos)
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oai_identifier_str oai:repository.urosario.edu.co:10336/28503
network_acronym_str EDOCUR2
network_name_str Repositorio EdocUR - U. Rosario
repository_id_str
spelling 54d3cf55-abf5-4c96-969b-892f39e5c062-1dddac7f0-2082-42ef-ae39-3d1dc8d17221-192527665-562f-4ccd-aa5c-19c67e0825ad-139f2a157-2c33-410e-870a-ef94610cd1d0-1db7aa959-69e1-4d38-b551-81056a3dd198-12020-08-28T15:49:14Z2020-08-28T15:49:14Z2006-01-01We analyze the problem of reliably estimating uncertainties of the earthquake source spectrum and related source parameters using Empirical Green Functions (EGF). We take advantage of the large dataset available from 10 seismic stations at hypocentral distances (10 km < d < 50 km) to average spectral ratios of the 2001 M5.1 Anza earthquake and 160 nearby aftershocks. We estimate the uncertainty of the average source spectrum of the M5.1 target earthquake by performing propagation of errors, which, due to the large number of EGFs used, is significantly smaller than that obtained usingasingle EGF. Our approach provides estimates of both the earthquake source spectrum and its uncertainties, plus confidence intervals on related source parameters such as radiated seismic energy or apparent stress, allowing the assessment of statistical significance. This is of paramount importance when comparing different sized earthquakes and analyzing source scaling of the earthquake rupture process. Our best estimate of radiated energy for the target earthquake is 1.24 × 1011 Joules with 95% confidence intervals (0.73 × 1011 , 2.28 × 1011). The estimated apparent stress of 0.33 (0.19, 0.59) MPa is relatively low compared to previous estimates from smaller earthquakes (1MPa) in the same region.application/pdfhttps://doi.org/10.1029/170GM08ISBN: 9780875904351EISBN: 9781118666272https://repository.urosario.edu.co/handle/10336/28503engAmerican Geophysical Union7469Earthquakes: Radiated Energy and the Physics of FaultingEarthquakes: Radiated Energy and the Physics of Faulting, ISBN: 9780875904351;EISBN: 9781118666272 (2006); pp. 69-74https://agupubs.onlinelibrary.wiley.com/doi/10.1029/170GM08Restringido (Acceso a grupos específicos)http://purl.org/coar/access_right/c_16ecEarthquakes: Radiated Energy and the Physics of Faultinginstname:Universidad del Rosarioreponame:Repositorio Institucional EdocURSeismic waveEnergy dissipationFaults (Geology)SeismologyUncertainties in earthquake source spectrum estimation using empirical green functionsIncertidumbres en la estimación del espectro de fuentes de terremotos utilizando funciones verdes empíricasbookPartParte de librohttp://purl.org/coar/version/c_970fb48d4fbd8a85http://purl.org/coar/resource_type/c_3248Prieto, Germán A.Parker, Robert L.Vernon, Frank L.Shearer, Peter M.Thomson, David J.10336/28503oai:repository.urosario.edu.co:10336/285032021-06-03 00:49:51.026https://repository.urosario.edu.coRepositorio institucional EdocURedocur@urosario.edu.co
dc.title.spa.fl_str_mv Uncertainties in earthquake source spectrum estimation using empirical green functions
dc.title.TranslatedTitle.spa.fl_str_mv Incertidumbres en la estimación del espectro de fuentes de terremotos utilizando funciones verdes empíricas
title Uncertainties in earthquake source spectrum estimation using empirical green functions
spellingShingle Uncertainties in earthquake source spectrum estimation using empirical green functions
Seismic wave
Energy dissipation
Faults (Geology)
Seismology
title_short Uncertainties in earthquake source spectrum estimation using empirical green functions
title_full Uncertainties in earthquake source spectrum estimation using empirical green functions
title_fullStr Uncertainties in earthquake source spectrum estimation using empirical green functions
title_full_unstemmed Uncertainties in earthquake source spectrum estimation using empirical green functions
title_sort Uncertainties in earthquake source spectrum estimation using empirical green functions
dc.subject.keyword.spa.fl_str_mv Seismic wave
Energy dissipation
Faults (Geology)
Seismology
topic Seismic wave
Energy dissipation
Faults (Geology)
Seismology
description We analyze the problem of reliably estimating uncertainties of the earthquake source spectrum and related source parameters using Empirical Green Functions (EGF). We take advantage of the large dataset available from 10 seismic stations at hypocentral distances (10 km < d < 50 km) to average spectral ratios of the 2001 M5.1 Anza earthquake and 160 nearby aftershocks. We estimate the uncertainty of the average source spectrum of the M5.1 target earthquake by performing propagation of errors, which, due to the large number of EGFs used, is significantly smaller than that obtained usingasingle EGF. Our approach provides estimates of both the earthquake source spectrum and its uncertainties, plus confidence intervals on related source parameters such as radiated seismic energy or apparent stress, allowing the assessment of statistical significance. This is of paramount importance when comparing different sized earthquakes and analyzing source scaling of the earthquake rupture process. Our best estimate of radiated energy for the target earthquake is 1.24 × 1011 Joules with 95% confidence intervals (0.73 × 1011 , 2.28 × 1011). The estimated apparent stress of 0.33 (0.19, 0.59) MPa is relatively low compared to previous estimates from smaller earthquakes (1MPa) in the same region.
publishDate 2006
dc.date.created.spa.fl_str_mv 2006-01-01
dc.date.accessioned.none.fl_str_mv 2020-08-28T15:49:14Z
dc.date.available.none.fl_str_mv 2020-08-28T15:49:14Z
dc.type.eng.fl_str_mv bookPart
dc.type.coarversion.fl_str_mv http://purl.org/coar/version/c_970fb48d4fbd8a85
dc.type.coar.fl_str_mv http://purl.org/coar/resource_type/c_3248
dc.type.spa.spa.fl_str_mv Parte de libro
dc.identifier.doi.none.fl_str_mv https://doi.org/10.1029/170GM08
dc.identifier.issn.none.fl_str_mv ISBN: 9780875904351
EISBN: 9781118666272
dc.identifier.uri.none.fl_str_mv https://repository.urosario.edu.co/handle/10336/28503
url https://doi.org/10.1029/170GM08
https://repository.urosario.edu.co/handle/10336/28503
identifier_str_mv ISBN: 9780875904351
EISBN: 9781118666272
dc.language.iso.spa.fl_str_mv eng
language eng
dc.relation.citationEndPage.none.fl_str_mv 74
dc.relation.citationStartPage.none.fl_str_mv 69
dc.relation.citationTitle.none.fl_str_mv Earthquakes: Radiated Energy and the Physics of Faulting
dc.relation.ispartof.spa.fl_str_mv Earthquakes: Radiated Energy and the Physics of Faulting, ISBN: 9780875904351;EISBN: 9781118666272 (2006); pp. 69-74
dc.relation.uri.spa.fl_str_mv https://agupubs.onlinelibrary.wiley.com/doi/10.1029/170GM08
dc.rights.coar.fl_str_mv http://purl.org/coar/access_right/c_16ec
dc.rights.acceso.spa.fl_str_mv Restringido (Acceso a grupos específicos)
rights_invalid_str_mv Restringido (Acceso a grupos específicos)
http://purl.org/coar/access_right/c_16ec
dc.format.mimetype.none.fl_str_mv application/pdf
dc.publisher.spa.fl_str_mv American Geophysical Union
dc.source.spa.fl_str_mv Earthquakes: Radiated Energy and the Physics of Faulting
institution Universidad del Rosario
dc.source.instname.none.fl_str_mv instname:Universidad del Rosario
dc.source.reponame.none.fl_str_mv reponame:Repositorio Institucional EdocUR
repository.name.fl_str_mv Repositorio institucional EdocUR
repository.mail.fl_str_mv edocur@urosario.edu.co
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