Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8354
AuthorsTertulliani, A.* 
Arcoraci, L.* 
Berardi, M.* 
Bernardini, F.* 
Brizuela, B.* 
Castellano, C.* 
Del mese, S.* 
Ercolani, E.* 
Graziani, L.* 
Maramai, A.* 
Rossi, A.* 
Sbarra, M.* 
Vecchi, M.* 
TitleThe Emilia 2012 sequence: a macroseismic survey
Issue DateAug-2012
Series/Report no.4/55 (2012)
DOI10.4401/ag-6140
URIhttp://hdl.handle.net/2122/8354
Keywordsmacroseismics
Subject Classification04. Solid Earth::04.06. Seismology::04.06.06. Surveys, measurements, and monitoring 
AbstractOn May 20, 2012, at 4:03 local time (2:03 UTC), a large part of the Po Valley between the cities of Ferrara, Modena and Mantova was struck by a damaging earthquake (Ml 5.9). The epicenter was located by the Istituto Nazionale di Geo-fisica e Vulcanologia (INGV) seismic network [ISIDe 2010] at 44.889 ˚N and 11.228 ˚E, approximately 30 km west of Ferrara (Figure 1). The event was preceded by a foreshock that occurred at 01:13 local time, with a magnitude of Ml 4. The mainshock started an intense seismic sequence that lasted for weeks, counting more than 2,000 events, six of which had Ml >5. The strongest earthquakes of this sequence occurred on May 29, 2012, with Ml 5.8 and Ml 5.3, recorded at 9:00 and 12:55 local time, respectively. The epicenters of the May 29, 2012, events were located at the westernmost part of the rupture zone of the May 20, 2012, earthquake (Figure 2). The May 20 and 29, 2012, earthquakes were felt through the whole of northern and central Italy, and as far as Switzerland, Slovenia, Croatia, Austria, south-eastern France and southern Germany. Historical information reveals that the seismic activity in the Po Valley is moderate […]
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