GPS observations of coseismic deformation following the 2016, August 24, Mw 6 Amatrice earthquake (central Italy): data, analysis and preliminary fault model
We used continuous Global Positioning System (GPS) measurements to infer the fault geometry and the amount of coseismic slip associated to the August 24, 2016 Mw 6 Amatrice earthquake. We realized a three dimensional coseismic displacement field by combining different geodetic solutions generated by...
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Format: | Article |
Language: | English |
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Istituto Nazionale di Geofisica e Vulcanologia (INGV)
2016-11-01
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Series: | Annals of Geophysics |
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Online Access: | http://www.annalsofgeophysics.eu/index.php/annals/article/view/7269 |
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record_format |
Article |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Daniele Cheloni Enrico Serpelloni Roberto Devoti Nicola D'Agostino Grazia Pietrantonio Federica Riguzzi Marco Anzidei Antonio Avallone Adriano Cavaliere Gianpaolo Cecere Ciriaco D'Ambrosio Alessandra Esposito Luigi Falco Alessandro Galvani Giulio Selvaggi Vincenzo Sepe Stefano Calcaterra Roberta Giuliani Maurizio Mattone Piera Gambino Luigi Abruzzese Vincenzo Cardinale Angelo Castagnozzi Giovanni De Luca Angelo Massucci Antonio Memmolo Franco Migliari Felice Minichiello Luigi Zarrilli |
spellingShingle |
Daniele Cheloni Enrico Serpelloni Roberto Devoti Nicola D'Agostino Grazia Pietrantonio Federica Riguzzi Marco Anzidei Antonio Avallone Adriano Cavaliere Gianpaolo Cecere Ciriaco D'Ambrosio Alessandra Esposito Luigi Falco Alessandro Galvani Giulio Selvaggi Vincenzo Sepe Stefano Calcaterra Roberta Giuliani Maurizio Mattone Piera Gambino Luigi Abruzzese Vincenzo Cardinale Angelo Castagnozzi Giovanni De Luca Angelo Massucci Antonio Memmolo Franco Migliari Felice Minichiello Luigi Zarrilli GPS observations of coseismic deformation following the 2016, August 24, Mw 6 Amatrice earthquake (central Italy): data, analysis and preliminary fault model Annals of Geophysics Amatrice earthquake Central Apennines Global Positioning System Coseismic deformation Normal faults |
author_facet |
Daniele Cheloni Enrico Serpelloni Roberto Devoti Nicola D'Agostino Grazia Pietrantonio Federica Riguzzi Marco Anzidei Antonio Avallone Adriano Cavaliere Gianpaolo Cecere Ciriaco D'Ambrosio Alessandra Esposito Luigi Falco Alessandro Galvani Giulio Selvaggi Vincenzo Sepe Stefano Calcaterra Roberta Giuliani Maurizio Mattone Piera Gambino Luigi Abruzzese Vincenzo Cardinale Angelo Castagnozzi Giovanni De Luca Angelo Massucci Antonio Memmolo Franco Migliari Felice Minichiello Luigi Zarrilli |
author_sort |
Daniele Cheloni |
title |
GPS observations of coseismic deformation following the 2016, August 24, Mw 6 Amatrice earthquake (central Italy): data, analysis and preliminary fault model |
title_short |
GPS observations of coseismic deformation following the 2016, August 24, Mw 6 Amatrice earthquake (central Italy): data, analysis and preliminary fault model |
title_full |
GPS observations of coseismic deformation following the 2016, August 24, Mw 6 Amatrice earthquake (central Italy): data, analysis and preliminary fault model |
title_fullStr |
GPS observations of coseismic deformation following the 2016, August 24, Mw 6 Amatrice earthquake (central Italy): data, analysis and preliminary fault model |
title_full_unstemmed |
GPS observations of coseismic deformation following the 2016, August 24, Mw 6 Amatrice earthquake (central Italy): data, analysis and preliminary fault model |
title_sort |
gps observations of coseismic deformation following the 2016, august 24, mw 6 amatrice earthquake (central italy): data, analysis and preliminary fault model |
publisher |
Istituto Nazionale di Geofisica e Vulcanologia (INGV) |
series |
Annals of Geophysics |
issn |
1593-5213 2037-416X |
publishDate |
2016-11-01 |
description |
We used continuous Global Positioning System (GPS) measurements to infer the fault geometry and the amount of coseismic slip associated to the August 24, 2016 Mw 6 Amatrice earthquake. We realized a three dimensional coseismic displacement field by combining different geodetic solutions generated by three independent analyses of the raw GPS observations. The coseismic deformation field described in this work aims at representing a consensus solution that minimizes the systematic biases potentially present in the individual geodetic solutions. Because of the limited number of stations available we modeled the measured coseismic displacements using a uniform slip model, deriving the geometry and kinematics of the causative fault, finding good agreement between our geodetically derived fault plane and other seismological and geological observations. |
topic |
Amatrice earthquake Central Apennines Global Positioning System Coseismic deformation Normal faults |
url |
http://www.annalsofgeophysics.eu/index.php/annals/article/view/7269 |
work_keys_str_mv |
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doaj-0ba14267257440259fb3b9513af8b6802020-11-25T00:26:00ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2016-11-0159010.4401/ag-72696142GPS observations of coseismic deformation following the 2016, August 24, Mw 6 Amatrice earthquake (central Italy): data, analysis and preliminary fault modelDaniele Cheloni0Enrico Serpelloni1Roberto Devoti2Nicola D'Agostino3Grazia Pietrantonio4Federica Riguzzi5Marco Anzidei6Antonio Avallone7Adriano Cavaliere8Gianpaolo Cecere9Ciriaco D'Ambrosio10Alessandra Esposito11Luigi Falco12Alessandro Galvani13Giulio Selvaggi14Vincenzo Sepe15Stefano Calcaterra16Roberta Giuliani17Maurizio Mattone18Piera Gambino19Luigi Abruzzese20Vincenzo Cardinale21Angelo Castagnozzi22Giovanni De Luca23Angelo Massucci24Antonio Memmolo25Franco Migliari26Felice Minichiello27Luigi Zarrilli28Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Bologna,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,ISPRA, Servizio Geofisica, Istituto Superiore per la Protezione e la Ricerca Ambientale,Dipartimento Protezione Civile, Dipartimento Protezione Civile, Ufficio Rischio Sismico e Vulcanico,Dipartimento Protezione Civile, Dipartimento Protezione Civile, Ufficio Rischio Sismico e Vulcanico,ISPRA, Servizio Geofisica, Istituto Superiore per la Protezione e la Ricerca Ambientale,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti,We used continuous Global Positioning System (GPS) measurements to infer the fault geometry and the amount of coseismic slip associated to the August 24, 2016 Mw 6 Amatrice earthquake. We realized a three dimensional coseismic displacement field by combining different geodetic solutions generated by three independent analyses of the raw GPS observations. The coseismic deformation field described in this work aims at representing a consensus solution that minimizes the systematic biases potentially present in the individual geodetic solutions. Because of the limited number of stations available we modeled the measured coseismic displacements using a uniform slip model, deriving the geometry and kinematics of the causative fault, finding good agreement between our geodetically derived fault plane and other seismological and geological observations.http://www.annalsofgeophysics.eu/index.php/annals/article/view/7269Amatrice earthquakeCentral ApenninesGlobal Positioning SystemCoseismic deformationNormal faults |