The 2009 L'Aquila earthquake (central Italy): A source mechanism and implications for seismic hazard

被引:172
作者
Walters, R. J. [1 ]
Elliott, J. R. [1 ]
D'Agostino, N. [2 ]
England, P. C. [1 ]
Hunstad, I. [2 ]
Jackson, J. A. [3 ]
Parsons, B. [1 ]
Phillips, R. J. [4 ]
Roberts, G. [5 ]
机构
[1] Univ Oxford, Dept Earth Sci, COMET, Oxford OX1 3PR, England
[2] Ist Nazl Geofis & Vulcan, Ctr Nazl Terremoti, I-00143 Rome, Italy
[3] Univ Cambridge, Dept Earth Sci, COMET, Cambridge CB3 0EZ, England
[4] Univ Edinburgh, Sch Geosci, Edinburgh EH8 9XP, Midlothian, Scotland
[5] UCL, Res Sch Earth Sci, London WC1E 6BT, England
关键词
NORMAL-FAULT SYSTEMS; CENTRAL APENNINES; ABRUZZO; EXAMPLE; MODEL;
D O I
10.1029/2009GL039337
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
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 similar to 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. Citation: Walters, R. J., J. R. Elliott, N. D'Agostino, P. C. England, I. Hunstad, J. A. Jackson, B. Parsons, R. J. Phillips, and G. Roberts (2009), The 2009 L'Aquila earthquake (central Italy): A source mechanism and implications for seismic hazard, Geophys. Res. Lett., 36, L17312, doi:10.1029/2009GL039337.
引用
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页数:6
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