期刊论文详细信息
Annals of Geophysics
Technologies and new approaches used by the INGV EMERGEO Working Group for real-time data sourcing and processing during the Emilia Romagna (northern Italy) 2012 earthquake sequence
Maurizio Pignone1  Carlo Alberto Brunori1  Anna Nardi1  Laura Colini1  Marco Moro1  Paolo Marco De Martini2  Pierfrancesco Burrato2  Francesca Romana Cinti2  Antonio Patera2  Stefania Pinzi2  Riccardo Civico2  Emanuela Falcucci2  Luigi Cucci2  Paola Vannoli2  Daniela Pantosti2  Maria Teresa Mariucci2  Stefano Pucci2  Paola Montone2  Fabrizio Galadini2  Stefano Gori2  Fabio Villani2  Alessandra Venuti3  Laura Alfonsi3  Giuseppe Casula4  Arianna Pesci4  Rosa Nappi5  Rosa Nave5  Giuliana Alessio5  Germana Gaudiosi5 
[1] Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti, Roma;Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma 1, Roma;Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma 2, Roma;Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Bologna, Bologna;Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Napoli, Osservatorio Vesuviano, Napoli;
关键词: Earthquake geology and paleoseismology;    Coseismic effects;    Liquefaction;    GIS;    Po Plain;   
DOI  :  10.4401/ag-6117
来源: DOAJ
【 摘 要 】

On May 20, 2012, a Ml 5.9 seismic event hit the Emilia Po Plain, triggering intense earthquake activity along a broad area of the Po Plain across the provinces of Modena, Ferrara, Rovigo and Mantova (Figure 1). Nine days later, on May 29, 2012, a Ml 5.8 event occurred roughly 10 km to the SW of the first main shock. These events caused widespread damage and resulted in 26 victims. The aftershock area extended over more than 50 km and was elongated in the WNW-ESE direction, and it included five major aftershocks with 5.1 ≤Ml ≤5.3, and more than 2000 minor events (Figure 1). In general, the seismic sequence was confined to the upper 10 km of the crust. Minor seismicity with depths ranging from 10 km to 30 km extended towards the southern sector of the epicentral area (ISIDe, http://iside.rm.ingv.it/). […]


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