DinSAR coseismic deformation measurements of the Mw 8.3 Illapel earthquake (Chile)
- Autores
- Calvet, Agustín; Balbarani, Sebastian; Gende, Mauricio Alfredo
- Año de publicación
- 2023
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The beginning of radars goes back to the 1930s where its main boost was related to the second world war. Nowadays, the techniques associated with radars are focused around a vast variety of civil, geodetic, and military applications. The development of the synthetic aperture principle, in the 1950s and 1960s, gave birth to a lot of new applications, and together with the technological progress of the last decades, the technique of interferometry with synthetic aperture radar (SAR) data became one of the most powerful ones for sensing remotely, with high quality and a vast spatial coverage. We used Sentinel-1 data and the differential interferometry SAR (DinSAR) technique to map and measure the surface deformation related to the 2015 Mw 8.3 Illapel earthquake (Chile). We also validated the results, by analysing the temporal variation of coordinates acquired from global navigation satellite system observations and projecting them in the geometry of the SAR system. Using this application we prove the DinSAR technique to be useful and powerful for the observation and analysis of surface deformation caused by the release of stress during the Mw 8.3 Illapel earthquake. It proved to be an efficient tool to detect and map the surface deformation with high spatial resolution in an approximate area of 20,000 km2.
Fil: Calvet, Agustín. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Balbarani, Sebastian. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Departamento de Agrimensura (departamento de Agrimensura) ; Facultad de Ingenieria ; Universidad de Buenos Aires; . Universidad de la Defensa Nacional. Facultad de Ingenieria del Ejercito.; Argentina
Fil: Gende, Mauricio Alfredo. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina. Universidad de la Defensa Nacional. Facultad de Ingenieria del Ejercito.; Argentina - Materia
-
DIFFERENTIAL INTERFEROMETRY
ILLAPEL EARTHQUAKE
SENTINEL-1
SURFACE DEFORMATION - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/220550
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DinSAR coseismic deformation measurements of the Mw 8.3 Illapel earthquake (Chile)Calvet, AgustínBalbarani, SebastianGende, Mauricio AlfredoDIFFERENTIAL INTERFEROMETRYILLAPEL EARTHQUAKESENTINEL-1SURFACE DEFORMATIONhttps://purl.org/becyt/ford/2.7https://purl.org/becyt/ford/2The beginning of radars goes back to the 1930s where its main boost was related to the second world war. Nowadays, the techniques associated with radars are focused around a vast variety of civil, geodetic, and military applications. The development of the synthetic aperture principle, in the 1950s and 1960s, gave birth to a lot of new applications, and together with the technological progress of the last decades, the technique of interferometry with synthetic aperture radar (SAR) data became one of the most powerful ones for sensing remotely, with high quality and a vast spatial coverage. We used Sentinel-1 data and the differential interferometry SAR (DinSAR) technique to map and measure the surface deformation related to the 2015 Mw 8.3 Illapel earthquake (Chile). We also validated the results, by analysing the temporal variation of coordinates acquired from global navigation satellite system observations and projecting them in the geometry of the SAR system. Using this application we prove the DinSAR technique to be useful and powerful for the observation and analysis of surface deformation caused by the release of stress during the Mw 8.3 Illapel earthquake. It proved to be an efficient tool to detect and map the surface deformation with high spatial resolution in an approximate area of 20,000 km2.Fil: Calvet, Agustín. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Balbarani, Sebastian. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Departamento de Agrimensura (departamento de Agrimensura) ; Facultad de Ingenieria ; Universidad de Buenos Aires; . Universidad de la Defensa Nacional. Facultad de Ingenieria del Ejercito.; ArgentinaFil: Gende, Mauricio Alfredo. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina. Universidad de la Defensa Nacional. Facultad de Ingenieria del Ejercito.; ArgentinaDe Gruyter2023-03info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/220550Calvet, Agustín; Balbarani, Sebastian; Gende, Mauricio Alfredo; DinSAR coseismic deformation measurements of the Mw 8.3 Illapel earthquake (Chile); De Gruyter; Journal of Geodetic Science; 13; 1; 3-2023; 1-102081-9943CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1515/jogs-2022-0154info:eu-repo/semantics/altIdentifier/url/https://www.degruyter.com/document/doi/10.1515/jogs-2022-0154/htmlinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-15T15:14:21Zoai:ri.conicet.gov.ar:11336/220550instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-10-15 15:14:21.72CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
DinSAR coseismic deformation measurements of the Mw 8.3 Illapel earthquake (Chile) |
title |
DinSAR coseismic deformation measurements of the Mw 8.3 Illapel earthquake (Chile) |
spellingShingle |
DinSAR coseismic deformation measurements of the Mw 8.3 Illapel earthquake (Chile) Calvet, Agustín DIFFERENTIAL INTERFEROMETRY ILLAPEL EARTHQUAKE SENTINEL-1 SURFACE DEFORMATION |
title_short |
DinSAR coseismic deformation measurements of the Mw 8.3 Illapel earthquake (Chile) |
title_full |
DinSAR coseismic deformation measurements of the Mw 8.3 Illapel earthquake (Chile) |
title_fullStr |
DinSAR coseismic deformation measurements of the Mw 8.3 Illapel earthquake (Chile) |
title_full_unstemmed |
DinSAR coseismic deformation measurements of the Mw 8.3 Illapel earthquake (Chile) |
title_sort |
DinSAR coseismic deformation measurements of the Mw 8.3 Illapel earthquake (Chile) |
dc.creator.none.fl_str_mv |
Calvet, Agustín Balbarani, Sebastian Gende, Mauricio Alfredo |
author |
Calvet, Agustín |
author_facet |
Calvet, Agustín Balbarani, Sebastian Gende, Mauricio Alfredo |
author_role |
author |
author2 |
Balbarani, Sebastian Gende, Mauricio Alfredo |
author2_role |
author author |
dc.subject.none.fl_str_mv |
DIFFERENTIAL INTERFEROMETRY ILLAPEL EARTHQUAKE SENTINEL-1 SURFACE DEFORMATION |
topic |
DIFFERENTIAL INTERFEROMETRY ILLAPEL EARTHQUAKE SENTINEL-1 SURFACE DEFORMATION |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/2.7 https://purl.org/becyt/ford/2 |
dc.description.none.fl_txt_mv |
The beginning of radars goes back to the 1930s where its main boost was related to the second world war. Nowadays, the techniques associated with radars are focused around a vast variety of civil, geodetic, and military applications. The development of the synthetic aperture principle, in the 1950s and 1960s, gave birth to a lot of new applications, and together with the technological progress of the last decades, the technique of interferometry with synthetic aperture radar (SAR) data became one of the most powerful ones for sensing remotely, with high quality and a vast spatial coverage. We used Sentinel-1 data and the differential interferometry SAR (DinSAR) technique to map and measure the surface deformation related to the 2015 Mw 8.3 Illapel earthquake (Chile). We also validated the results, by analysing the temporal variation of coordinates acquired from global navigation satellite system observations and projecting them in the geometry of the SAR system. Using this application we prove the DinSAR technique to be useful and powerful for the observation and analysis of surface deformation caused by the release of stress during the Mw 8.3 Illapel earthquake. It proved to be an efficient tool to detect and map the surface deformation with high spatial resolution in an approximate area of 20,000 km2. Fil: Calvet, Agustín. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Balbarani, Sebastian. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Departamento de Agrimensura (departamento de Agrimensura) ; Facultad de Ingenieria ; Universidad de Buenos Aires; . Universidad de la Defensa Nacional. Facultad de Ingenieria del Ejercito.; Argentina Fil: Gende, Mauricio Alfredo. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina. Universidad de la Defensa Nacional. Facultad de Ingenieria del Ejercito.; Argentina |
description |
The beginning of radars goes back to the 1930s where its main boost was related to the second world war. Nowadays, the techniques associated with radars are focused around a vast variety of civil, geodetic, and military applications. The development of the synthetic aperture principle, in the 1950s and 1960s, gave birth to a lot of new applications, and together with the technological progress of the last decades, the technique of interferometry with synthetic aperture radar (SAR) data became one of the most powerful ones for sensing remotely, with high quality and a vast spatial coverage. We used Sentinel-1 data and the differential interferometry SAR (DinSAR) technique to map and measure the surface deformation related to the 2015 Mw 8.3 Illapel earthquake (Chile). We also validated the results, by analysing the temporal variation of coordinates acquired from global navigation satellite system observations and projecting them in the geometry of the SAR system. Using this application we prove the DinSAR technique to be useful and powerful for the observation and analysis of surface deformation caused by the release of stress during the Mw 8.3 Illapel earthquake. It proved to be an efficient tool to detect and map the surface deformation with high spatial resolution in an approximate area of 20,000 km2. |
publishDate |
2023 |
dc.date.none.fl_str_mv |
2023-03 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
format |
article |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
http://hdl.handle.net/11336/220550 Calvet, Agustín; Balbarani, Sebastian; Gende, Mauricio Alfredo; DinSAR coseismic deformation measurements of the Mw 8.3 Illapel earthquake (Chile); De Gruyter; Journal of Geodetic Science; 13; 1; 3-2023; 1-10 2081-9943 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/220550 |
identifier_str_mv |
Calvet, Agustín; Balbarani, Sebastian; Gende, Mauricio Alfredo; DinSAR coseismic deformation measurements of the Mw 8.3 Illapel earthquake (Chile); De Gruyter; Journal of Geodetic Science; 13; 1; 3-2023; 1-10 2081-9943 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/doi/10.1515/jogs-2022-0154 info:eu-repo/semantics/altIdentifier/url/https://www.degruyter.com/document/doi/10.1515/jogs-2022-0154/html |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/2.5/ar/ |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by/2.5/ar/ |
dc.format.none.fl_str_mv |
application/pdf application/pdf |
dc.publisher.none.fl_str_mv |
De Gruyter |
publisher.none.fl_str_mv |
De Gruyter |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
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CONICET Digital (CONICET) |
collection |
CONICET Digital (CONICET) |
instname_str |
Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.name.fl_str_mv |
CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.mail.fl_str_mv |
dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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1846083290724827136 |
score |
13.22299 |