Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/5440
DC Field | Value | Language |
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dc.contributor.authorall | Walters, R. J.; COMET, Department of Earth Sciences, University of Oxford, Oxford, UK. | en |
dc.contributor.authorall | Elliott, J. R; COMET, Department of Earth Sciences, University of Oxford, Oxford, UK. | en |
dc.contributor.authorall | D’Agostino, N.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italia | en |
dc.contributor.authorall | England, P. C.; COMET, Department of Earth Sciences, University of Oxford, Oxford, UK. | en |
dc.contributor.authorall | Hunstad, I.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italia | en |
dc.contributor.authorall | Jackson, J. A.; COMET, Department of Earth Sciences, University of Cambridge, Cambridge, UK. | en |
dc.contributor.authorall | Parsons, B.; COMET, Department of Earth Sciences, University of Oxford, Oxford, UK. | en |
dc.contributor.authorall | Phillips, R. J.; School of GeoSciences, University of Edinburgh, Edinburgh, UK. | en |
dc.contributor.authorall | Roberts, G.; Research School of Earth Sciences, University College London, London, UK. | en |
dc.date.accessioned | 2010-01-07T13:54:02Z | en |
dc.date.available | 2010-01-07T13:54:02Z | en |
dc.date.issued | 2009-09-05 | en |
dc.identifier.uri | http://hdl.handle.net/2122/5440 | en |
dc.description | An edited version of this paper was published by AGU. Copyright (2009) American Geophysical Union. | en |
dc.description.abstract | We 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.iso | English | en |
dc.publisher.name | AGU Journal | en |
dc.relation.ispartof | Geophysical Research Letter | en |
dc.relation.ispartofseries | /36 (2009) | en |
dc.relation.isversionof | http://europa.agu.org:8005/?view=article&uri=/journals/gl/gl0917/2009GL039337/2009GL039337.xml&t=gl,10.1029/2009GL039337 | en |
dc.subject | L'Aquila earthquake | en |
dc.subject | InSAR | en |
dc.title | The 2009 L’Aquila earthquake (central Italy): A source mechanism and implications for seismic hazard | en |
dc.type | article | en |
dc.description.status | Published | en |
dc.type.QualityControl | Peer-reviewed | en |
dc.description.pagenumber | L17312 | en |
dc.subject.INGV | 04. Solid Earth::04.06. Seismology::04.06.01. Earthquake faults: properties and evolution | en |
dc.identifier.doi | 10.1029/2009GL039337 | en |
dc.relation.references | Bagnaia, R., A. D’Epifanio, and S. Sylos Labini (1992), Aquila and Subequan basins: An example of Quaternary evolution in central Apennines, Italy, Quat. Nova, 2, 187–209. Boncio, P., G. Lavecchia, and B. Pace (2004), Defining a model of 3D seismogenic sources for Seismic Hazard Assessment applications: The case of central Apennines (Italy), J. Seismol., 8, 407 – 425, doi:10.1023/B:JOSE.0000038449.78801.05. D’Agostino, N., J. A. Jackson, F. Dramis, and R. Funiciello (2001), Interactions between mantle upwelling, drainage evolution and active normal faulting: An example from the central Apennines (Italy), Geophys. J. Int., 147, 475– 497, doi:10.1046/j.1365-246X.2001.00539.x. D’Agostino, N., A. Avallone, D. Cheloni, E. D’Anastasio, S. Mantenuto, and G. Selvaggi (2008), Active tectonics of the Adriatic region from GPS and earthquake slip vectors, J. Geophys. Res., 113, B12413, doi:10.1029/ 2008JB005860. Farr, T. G., et al. (2007), The Shuttle Radar Topography Mission, Rev. Geophys., 45, RG2004, doi:10.1029/2005RG000183. Galli, P., F. Galadini, M. Moro, and C. Giraudi (2002), New paleoseismological data from the Gran Sasso d’Italia area (central Apennines), Geophys. Res. Lett., 29(7), 1134, doi:10.1029/2001GL013292. Giraudi, C., and M. Frezzotti (1995), Palaeoseismicity in the Gran Sasso Massif (Abruzzo, central Italy), Quat. Int., 25, 81–93, doi:10.1016/1040- 6182(94)P3716-L. Goldsworthy, M., and J. Jackson (2001), Migration of activity within normal fault systems: Examples from the Quaternary of mainland Greece, J. Struct. Geol., 23, 489– 506, doi:10.1016/S0191-8141(00)00121-8. Hunstad, I., G. Selvaggi, N. D’Agostino, P. England, P. Clarke, and M. Pierozzi (2003), Geodetic strain in peninsular Italy between 1875 and 2001, Geophys. Res. Lett., 30(4), 1181, doi:10.1029/ 2002GL016447. Jonsson, S., H. Zebker, P. Segall, and F. Amelung (2002), Fault slip distribution of the Mw 7.2 Hector Mine earthquake estimated from satellite radar and GPS measurements., Bull. Seismol. Soc. Am., 92, 1377– 1389, doi:10.1785/0120000922. King, G. C. P., R. S. Stein, and J. Lin (1994), Static stress changes and the triggering of earthquakes, Bull. Seismol. Soc. Am., 84, 935–953. Lin, J., and R. S. Stein (2004), Stress triggering in thrust and subduction earthquakes and stress interaction between the southern San Andreas and nearby thrust and strike-slip faults, J. Geophys. Res., 109, B02303, doi:10.1029/2003JB002607. Okada, Y. (1985), Surface deformation due to shear and tensile faults in a half-space, Bull. Seismol. Soc. Am., 75, 1135– 1154. Roberts, G., and A. M. Michetti (2004), Spatial and temporal variations in growth rates along active normal fault systems: An example from the Lazio Abruzzo Apennines, central Italy, J. Struct. Geol., 26, 339– 376, doi:10.1016/S0191-8141(03)00103-2. Rosen, P. A., S. Henley, G. Peltzer, and M. Simons (2004), Updated Repeat Orbit Interferometry package released, Eos Trans. AGU, 85(5), doi:10.1029/2004EO050004. Tondi, E. (2000), Geological analysis and seismic hazard in the central Apennines (Italy), J. Geodyn., 29, 517 – 533, doi:10.1016/S0264- 3707(99)00048-4. Wright, T. J., Z. Lu, and C. Wicks (2003), Source model for the Mw 6.7, 23 October 2002, Nenana Mountain earthquake (Alaska) from InSAR, Geophys. Res. Lett., 30(18), 1974, doi:10.1029/2003GL018014. | en |
dc.description.obiettivoSpecifico | 3.2. Tettonica attiva | en |
dc.description.journalType | JCR Journal | en |
dc.description.fulltext | reserved | en |
dc.contributor.author | Walters, R. J. | en |
dc.contributor.author | Elliott, J. R | en |
dc.contributor.author | D’Agostino, N. | en |
dc.contributor.author | England, P. C. | en |
dc.contributor.author | Hunstad, I. | en |
dc.contributor.author | Jackson, J. A. | en |
dc.contributor.author | Parsons, B. | en |
dc.contributor.author | Phillips, R. J. | en |
dc.contributor.author | Roberts, G. | en |
dc.contributor.department | COMET, Department of Earth Sciences, University of Oxford, Oxford, UK. | en |
dc.contributor.department | COMET, Department of Earth Sciences, University of Oxford, Oxford, UK. | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia | en |
dc.contributor.department | COMET, Department of Earth Sciences, University of Oxford, Oxford, UK. | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia | en |
dc.contributor.department | COMET, Department of Earth Sciences, University of Cambridge, Cambridge, UK. | en |
dc.contributor.department | COMET, Department of Earth Sciences, University of Oxford, Oxford, UK. | en |
dc.contributor.department | School of GeoSciences, University of Edinburgh, Edinburgh, UK. | en |
dc.contributor.department | Research School of Earth Sciences, University College London, London, UK. | en |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | restricted | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | COMET, Department of Earth Sciences, University of Oxford, Oxford, UK. | - |
crisitem.author.dept | COMET, Department of Earth Sciences, University of Oxford, Oxford, UK. | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia | - |
crisitem.author.dept | COMET, Department of Earth Sciences, University of Oxford, Oxford, UK. | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia | - |
crisitem.author.dept | COMET, Department of Earth Sciences, University of Cambridge, Cambridge, UK. | - |
crisitem.author.dept | COMET, Department of Earth Sciences, University of Oxford, Oxford, UK. | - |
crisitem.author.dept | School of GeoSciences, University of Edinburgh, Edinburgh, UK. | - |
crisitem.author.dept | University of London, | - |
crisitem.author.orcid | 0000-0002-0444-6240 | - |
crisitem.author.orcid | 0000-0002-3573-873X | - |
crisitem.author.orcid | 0000-0003-2769-0665 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
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