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
.jpg)
- Institución
- Universidad Nacional de La Plata
- OAI Identificador
- oai:sedici.unlp.edu.ar:10915/60961
Ver los metadatos del registro completo
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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. |
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2017 |
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