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The 2009 L'Aquila earthquake (central Italy): A source mechanism and implications for seismic hazard
Author(s) -
Walters R. J.,
Elliott J. R.,
D'Agostino N.,
England P. C.,
Hunstad I.,
Jackson J. A.,
Parsons B.,
Phillips R. J.,
Roberts G.
Publication year - 2009
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2009gl039337
Subject(s) - seismology , geology , seismic hazard , seismic microzonation , interferometric synthetic aperture radar , seismic gap , fault (geology) , slip (aerodynamics) , synthetic aperture radar , physics , remote sensing , thermodynamics
We use InSAR and body‐wave seismology to determine independent source parameters for the 6th April 2009 M w 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.