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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10111

Authors: Lavecchia, G.*
Boncio, P.*
Brozzetti, F.*
de Nardis, R.*
Di Naccio, D.*
Ferarini, F.*
Pizzi, A.*
Pomposo, G.*
Editors: Guarnieri, P.; Università di Catania
Title: The April 2009 Aquila (central Italy) seismic sequence (Mw6.3): A preliminary seismotectonic picture,
Publisher: Nova Science Publishers, New York
Issue Date: 2011
ISBN: 978-1-60876-147-0
Keywords: L’Aquila, Apennines, central Italy
seismogenic source
normal fault
fault segmentation
Abstract: On April 6, 2009, an Mw 6.3 earthquake struck the town of L’Aquila in the Abruzzo region in central Italy. It was followed by a long seismic crisis with other four events with Mw between 5.1 and 5.6. Seismological and geological data point out an upper crust extensional stress field with an average WSW-ENE tensional axis. In the course of the seismic sequence, two distinct en échelon fault sources were activated: first, the SW-dipping Paganica normal fault, which is associated with the Mw 6.3 event; and, subsequently, the southern part of the WSW-dipping Gorzano normal fault.Co-seismic ground deformation (open fissures, en échelon cracks and shear planes with centimetric downthrows) was surveyed for ~ 13 km along the Paganica fault. The integration of the information from this last Italian earthquake with the previous seismotectonic background has allowed us to further detail the 3-D shape and the size of some of the individual seismogenic sources of the Apennine active extensional belt.
Appears in Collections:Book chapters
04.07.07. Tectonics

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