Low-parametric modeling of Mw8.3 Illapel 2015, Chile earthquake

Autores
Bollini, María Celeste; Sabbione, Nora Cristina; Plicka, V.; Zahradník, J.
Año de publicación
2017
Idioma
inglés
Tipo de recurso
documento de conferencia
Estado
versión publicada
Descripción
The Mw 8.3 (GCMT) Illapel megathrust earthquake is investigated. The objective is to find out which features of the previously published rupture scenarios can be resolved using a regional strong-motion network and source models with few parameters only. Low-frequency waveforms (<0.05 Hz), at nine stations (Centro Sismológico Nacional, Chile - CSN), are subjected to modeling. Various representations of the source are used: (i) Multiple-point-source models based either on iterative deconvolution or simultaneous inversion of source pairs, (ii) Models of circular and elliptical uniform-slip patches, employing synthetic and empirical Green’s functions, respectively. This variety of methods provides consistent results. The earthquake appears to be a segmented rupture progressing from an early (deep) moment release to a later (shallow) one, towards the NW. The source models of slip-uniform patches synchronously suggest a low rupture speed 1-2 km/s. Despite different data sets and methods, this estimate of rupture speed is consistent with independent publications. As for ambiguity in literature regarding depth and timing of the rupture, our paper clearly prefers the models including a ~20-30 s delay of the shallow moment release compared to the initial deep one. The strong-motion data set and low-parametric models proved to be competitive with more sophisticated approaches. This result implies a need to improve regional accelerometer networks in South America, which might eventually help in resolving source process of possible future large events, e.g. in Patagonia.
Eje: Estudio del Interior Terrestre.
Facultad de Ciencias Astronómicas y Geofísicas
Materia
Geofísica
Geología
low-frequency modeling
multiple-point-source models
empirical green’s functions
Chile
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/licenses/by/4.0/
Repositorio
SEDICI (UNLP)
Institución
Universidad Nacional de La Plata
OAI Identificador
oai:sedici.unlp.edu.ar:10915/60961

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spelling Low-parametric modeling of Mw8.3 Illapel 2015, Chile earthquakeBollini, María CelesteSabbione, Nora CristinaPlicka, V.Zahradník, J.GeofísicaGeologíalow-frequency modelingmultiple-point-source modelsempirical green’s functionsChileThe Mw 8.3 (GCMT) Illapel megathrust earthquake is investigated. The objective is to find out which features of the previously published rupture scenarios can be resolved using a regional strong-motion network and source models with few parameters only. Low-frequency waveforms (<0.05 Hz), at nine stations (Centro Sismológico Nacional, Chile - CSN), are subjected to modeling. Various representations of the source are used: (i) Multiple-point-source models based either on iterative deconvolution or simultaneous inversion of source pairs, (ii) Models of circular and elliptical uniform-slip patches, employing synthetic and empirical Green’s functions, respectively. This variety of methods provides consistent results. The earthquake appears to be a segmented rupture progressing from an early (deep) moment release to a later (shallow) one, towards the NW. The source models of slip-uniform patches synchronously suggest a low rupture speed 1-2 km/s. Despite different data sets and methods, this estimate of rupture speed is consistent with independent publications. As for ambiguity in literature regarding depth and timing of the rupture, our paper clearly prefers the models including a ~20-30 s delay of the shallow moment release compared to the initial deep one. The strong-motion data set and low-parametric models proved to be competitive with more sophisticated approaches. This result implies a need to improve regional accelerometer networks in South America, which might eventually help in resolving source process of possible future large events, e.g. in Patagonia.Eje: Estudio del Interior Terrestre.Facultad de Ciencias Astronómicas y Geofísicas2017-04info:eu-repo/semantics/conferenceObjectinfo:eu-repo/semantics/publishedVersionResumenhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfhttp://sedici.unlp.edu.ar/handle/10915/60961enginfo:eu-repo/semantics/altIdentifier/isbn/978-950-34-1471-2info:eu-repo/semantics/reference/hdl/10915/60718info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by/4.0/Creative Commons Attribution 4.0 International (CC BY 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2025-10-22T16:49:00Zoai:sedici.unlp.edu.ar:10915/60961Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-10-22 16:49:00.599SEDICI (UNLP) - Universidad Nacional de La Platafalse
dc.title.none.fl_str_mv Low-parametric modeling of Mw8.3 Illapel 2015, Chile earthquake
title Low-parametric modeling of Mw8.3 Illapel 2015, Chile earthquake
spellingShingle Low-parametric modeling of Mw8.3 Illapel 2015, Chile earthquake
Bollini, María Celeste
Geofísica
Geología
low-frequency modeling
multiple-point-source models
empirical green’s functions
Chile
title_short Low-parametric modeling of Mw8.3 Illapel 2015, Chile earthquake
title_full Low-parametric modeling of Mw8.3 Illapel 2015, Chile earthquake
title_fullStr Low-parametric modeling of Mw8.3 Illapel 2015, Chile earthquake
title_full_unstemmed Low-parametric modeling of Mw8.3 Illapel 2015, Chile earthquake
title_sort Low-parametric modeling of Mw8.3 Illapel 2015, Chile earthquake
dc.creator.none.fl_str_mv Bollini, María Celeste
Sabbione, Nora Cristina
Plicka, V.
Zahradník, J.
author Bollini, María Celeste
author_facet Bollini, María Celeste
Sabbione, Nora Cristina
Plicka, V.
Zahradník, J.
author_role author
author2 Sabbione, Nora Cristina
Plicka, V.
Zahradník, J.
author2_role author
author
author
dc.subject.none.fl_str_mv Geofísica
Geología
low-frequency modeling
multiple-point-source models
empirical green’s functions
Chile
topic Geofísica
Geología
low-frequency modeling
multiple-point-source models
empirical green’s functions
Chile
dc.description.none.fl_txt_mv The Mw 8.3 (GCMT) Illapel megathrust earthquake is investigated. The objective is to find out which features of the previously published rupture scenarios can be resolved using a regional strong-motion network and source models with few parameters only. Low-frequency waveforms (<0.05 Hz), at nine stations (Centro Sismológico Nacional, Chile - CSN), are subjected to modeling. Various representations of the source are used: (i) Multiple-point-source models based either on iterative deconvolution or simultaneous inversion of source pairs, (ii) Models of circular and elliptical uniform-slip patches, employing synthetic and empirical Green’s functions, respectively. This variety of methods provides consistent results. The earthquake appears to be a segmented rupture progressing from an early (deep) moment release to a later (shallow) one, towards the NW. The source models of slip-uniform patches synchronously suggest a low rupture speed 1-2 km/s. Despite different data sets and methods, this estimate of rupture speed is consistent with independent publications. As for ambiguity in literature regarding depth and timing of the rupture, our paper clearly prefers the models including a ~20-30 s delay of the shallow moment release compared to the initial deep one. The strong-motion data set and low-parametric models proved to be competitive with more sophisticated approaches. This result implies a need to improve regional accelerometer networks in South America, which might eventually help in resolving source process of possible future large events, e.g. in Patagonia.
Eje: Estudio del Interior Terrestre.
Facultad de Ciencias Astronómicas y Geofísicas
description The Mw 8.3 (GCMT) Illapel megathrust earthquake is investigated. The objective is to find out which features of the previously published rupture scenarios can be resolved using a regional strong-motion network and source models with few parameters only. Low-frequency waveforms (<0.05 Hz), at nine stations (Centro Sismológico Nacional, Chile - CSN), are subjected to modeling. Various representations of the source are used: (i) Multiple-point-source models based either on iterative deconvolution or simultaneous inversion of source pairs, (ii) Models of circular and elliptical uniform-slip patches, employing synthetic and empirical Green’s functions, respectively. This variety of methods provides consistent results. The earthquake appears to be a segmented rupture progressing from an early (deep) moment release to a later (shallow) one, towards the NW. The source models of slip-uniform patches synchronously suggest a low rupture speed 1-2 km/s. Despite different data sets and methods, this estimate of rupture speed is consistent with independent publications. As for ambiguity in literature regarding depth and timing of the rupture, our paper clearly prefers the models including a ~20-30 s delay of the shallow moment release compared to the initial deep one. The strong-motion data set and low-parametric models proved to be competitive with more sophisticated approaches. This result implies a need to improve regional accelerometer networks in South America, which might eventually help in resolving source process of possible future large events, e.g. in Patagonia.
publishDate 2017
dc.date.none.fl_str_mv 2017-04
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