Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5440
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dc.contributor.authorallWalters, R. J.; COMET, Department of Earth Sciences, University of Oxford, Oxford, UK.en
dc.contributor.authorallElliott, J. R; COMET, Department of Earth Sciences, University of Oxford, Oxford, UK.en
dc.contributor.authorallD’Agostino, N.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallEngland, P. C.; COMET, Department of Earth Sciences, University of Oxford, Oxford, UK.en
dc.contributor.authorallHunstad, I.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallJackson, J. A.; COMET, Department of Earth Sciences, University of Cambridge, Cambridge, UK.en
dc.contributor.authorallParsons, B.; COMET, Department of Earth Sciences, University of Oxford, Oxford, UK.en
dc.contributor.authorallPhillips, R. J.; School of GeoSciences, University of Edinburgh, Edinburgh, UK.en
dc.contributor.authorallRoberts, G.; Research School of Earth Sciences, University College London, London, UK.en
dc.date.accessioned2010-01-07T13:54:02Zen
dc.date.available2010-01-07T13:54:02Zen
dc.date.issued2009-09-05en
dc.identifier.urihttp://hdl.handle.net/2122/5440en
dc.descriptionAn edited version of this paper was published by AGU. Copyright (2009) American Geophysical Union.en
dc.description.abstractWe use InSAR and body-wave seismology to determine independent source parameters for the 6th April 2009 Mw 6.3 L’Aquila earthquake and confirm that the earthquake ruptured a SW-dipping normal fault with 0.6–0.8 m slip. The causative Paganica fault had been neglected relative to other nearby range-frontal faults, partly because it has a subdued geomorphological expression in comparison with these faults. The L’Aquila earthquake occurred in an area with a marked seismic deficit relative to geodetically determined strain accumulation. We use our source model to calculate stress changes on nearby faults produced by the L’Aquila earthquake and we find that several of these faults have been brought closer to failure.en
dc.language.isoEnglishen
dc.publisher.nameAGU Journalen
dc.relation.ispartofGeophysical Research Letteren
dc.relation.ispartofseries/36 (2009)en
dc.relation.isversionofhttp://europa.agu.org:8005/?view=article&uri=/journals/gl/gl0917/2009GL039337/2009GL039337.xml&t=gl,10.1029/2009GL039337en
dc.subjectL'Aquila earthquakeen
dc.subjectInSARen
dc.titleThe 2009 L’Aquila earthquake (central Italy): A source mechanism and implications for seismic hazarden
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumberL17312en
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.01. Earthquake faults: properties and evolutionen
dc.identifier.doi10.1029/2009GL039337en
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dc.description.obiettivoSpecifico3.2. Tettonica attivaen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorWalters, R. J.en
dc.contributor.authorElliott, J. Ren
dc.contributor.authorD’Agostino, N.en
dc.contributor.authorEngland, P. C.en
dc.contributor.authorHunstad, I.en
dc.contributor.authorJackson, J. A.en
dc.contributor.authorParsons, B.en
dc.contributor.authorPhillips, R. J.en
dc.contributor.authorRoberts, G.en
dc.contributor.departmentCOMET, Department of Earth Sciences, University of Oxford, Oxford, UK.en
dc.contributor.departmentCOMET, Department of Earth Sciences, University of Oxford, Oxford, UK.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentCOMET, Department of Earth Sciences, University of Oxford, Oxford, UK.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentCOMET, Department of Earth Sciences, University of Cambridge, Cambridge, UK.en
dc.contributor.departmentCOMET, Department of Earth Sciences, University of Oxford, Oxford, UK.en
dc.contributor.departmentSchool of GeoSciences, University of Edinburgh, Edinburgh, UK.en
dc.contributor.departmentResearch School of Earth Sciences, University College London, London, UK.en
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptCOMET, Department of Earth Sciences, University of Oxford, Oxford, UK.-
crisitem.author.deptCOMET, Department of Earth Sciences, University of Oxford, Oxford, UK.-
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.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptCOMET, Department of Earth Sciences, University of Cambridge, Cambridge, UK.-
crisitem.author.deptCOMET, Department of Earth Sciences, University of Oxford, Oxford, UK.-
crisitem.author.deptSchool of GeoSciences, University of Edinburgh, Edinburgh, UK.-
crisitem.author.deptUniversity of London,-
crisitem.author.orcid0000-0002-0444-6240-
crisitem.author.orcid0000-0002-3573-873X-
crisitem.author.orcid0000-0003-2769-0665-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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