Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9150
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dc.contributor.authorallCheloni, D.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallGiuliani, R.; Ufficio Rischio Sismico e Vulcanico, DPC, Romaen
dc.contributor.authorallD'Anastasio, E.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallAtzori, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallWalters, R. J.; COMET+, School of Earth and Environment, University of Leeds, Leedsen
dc.contributor.authorallBonci, L.; ISPRA, Romaen
dc.contributor.authorallD'Agostino, N.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallMattone, M.; Ufficio Rischio Sismico e Vulcanico, DPC, Romaen
dc.contributor.authorallCalcaterra, S.; ISPRA, Romaen
dc.contributor.authorallGambino, P.; ISPRA, Romaen
dc.contributor.authorallDeninno, F.; IGM, Firenzeen
dc.contributor.authorallMaseroli, R.; IGM, Firenzeen
dc.contributor.authorallStefanelli, G.; IGM, Firenzeen
dc.date.accessioned2014-11-17T14:19:37Zen
dc.date.available2014-11-17T14:19:37Zen
dc.date.issued2014-03-15en
dc.identifier.urihttp://hdl.handle.net/2122/9150en
dc.description.abstractAfter the April 6th 2009 MW 6.3 (ML 5.9) L'Aquila earthquake (central Italy), we re-measured more than 100 km of high-precision levelling lines in the epicentral area. The joint inversion of the levelling measurements with InSAR and GPS measurements, allowed us to derive new coseismic and post-seismic slip distributions and to de- scribe, with high resolution details on surface displacements, the activation and the slip distribution of a second- ary fault during the aftershock sequence that struck the Campotosto area (major event MW 5.2). Coseismic slip on the Paganica fault occurred on one main asperity, while the afterslip distribution shows a more complex pattern, occurring on three main patches, including both slips on the shallow portions and on the deeper parts of the rup- ture plane. The comparison between coseismic and post-seismic slip distributions strongly suggests that afterslip was triggered at the edges of the coseismic asperity. The activation of a segment of the Campotosto fault during the aftershock sequence, with a good correlation between the estimated slipping area, moment release and distribution of aftershocks, raises the opportunity to discuss the local seismic hazard following the occurrence of the 2009 L'Aquila mainshock. The Campotosto fault appears capable of generating earthquakes as large as his- torical events in the region (M N 6.5) or as small as the ones associated with the 2009 sequence. In the case that the Campotosto fault is accumulating a significant portion of the current interseismic deformation, the 2009 MW N 5 events will have released only a small amount of the accumulated elastic strain, and then a significant hazard still remains in the area. Continuing geodetic monitoring and a densification of the GPS networks in the region are therefore needed to estimate the tectonic loading across the different recognized active fault systems in this part of the Apennines.en
dc.language.isoEnglishen
dc.publisher.nameElsevier Science Limiteden
dc.relation.ispartofTectonophysicsen
dc.relation.ispartofseries/622(2014)en
dc.subjectHigh-precision leveling; InSAR; GPS; Earthquake source; Normal faulting; Seismic hazarden
dc.titleCoseismic and post-seismic slip of the 2009 L'Aquila (central Italy) MW 6.3 earthquake and implications for seismic potential along the Campotosto fault from joint inversion of high-precision levelling, InSAR and GPS dataen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber168-185en
dc.subject.INGV04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformationsen
dc.subject.INGV04. Solid Earth::04.03. Geodesy::04.03.07. Satellite geodesyen
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.01. Earthquake faults: properties and evolutionen
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.11. Seismic risken
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.01. Continentsen
dc.identifier.doi10.1016/j.tecto.2014.03.009en
dc.description.obiettivoSpecifico2T. Tettonica attivaen
dc.description.journalTypeJCR Journalen
dc.description.fulltextrestricteden
dc.relation.issn0040-1951en
dc.relation.eissn1879-3266en
dc.contributor.authorCheloni, D.en
dc.contributor.authorGiuliani, R.en
dc.contributor.authorD'Anastasio, E.en
dc.contributor.authorAtzori, S.en
dc.contributor.authorWalters, R. J.en
dc.contributor.authorBonci, L.en
dc.contributor.authorD'Agostino, N.en
dc.contributor.authorMattone, M.en
dc.contributor.authorCalcaterra, S.en
dc.contributor.authorGambino, P.en
dc.contributor.authorDeninno, F.en
dc.contributor.authorMaseroli, R.en
dc.contributor.authorStefanelli, G.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentUfficio Rischio Sismico e Vulcanico, DPC, Romaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentCOMET+, School of Earth and Environment, University of Leeds, Leedsen
dc.contributor.departmentISPRA, Romaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentUfficio Rischio Sismico e Vulcanico, DPC, Romaen
dc.contributor.departmentISPRA, Romaen
dc.contributor.departmentISPRA, Romaen
dc.contributor.departmentIGM, Firenzeen
dc.contributor.departmentIGM, Firenzeen
dc.contributor.departmentIGM, Firenzeen
item.grantfulltextrestricted-
item.languageiso639-1en-
item.fulltextWith Fulltext-
item.openairetypearticle-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.cerifentitytypePublications-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptDipartimento Protezione Civile, Ufficio Rischio Sismico-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptCOMET, Department of Earth Sciences, University of Oxford, Oxford, UK.-
crisitem.author.deptISPRA, Roma-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptDipartimento Protezione Civile, Roma, Italy-
crisitem.author.deptAgenzia per la Protezione dell'Ambiente e per i Servizi Tecnici, Via Curtatone, Roma, Italua-
crisitem.author.deptISPRA-
crisitem.author.deptIGM, Firenze-
crisitem.author.deptIGM, Firenze-
crisitem.author.deptIGM, Firenze-
crisitem.author.orcid0000-0002-0958-2129-
crisitem.author.orcid0000-0001-9906-0801-
crisitem.author.orcid0000-0003-3043-8604-
crisitem.author.orcid0000-0002-5031-9904-
crisitem.author.orcid0000-0002-0444-6240-
crisitem.author.orcid0000-0002-5055-3362-
crisitem.author.orcid0000-0002-1890-9752-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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