GNGTS 2016 - Atti del 35° Convegno Nazionale

GNGTS 2016 S essione 1.1 107 Dipartimento della Protezione Civile; 2009: Manuale per la compilazione della scheda di 1° livello di rilevamento di danno, pronto intervento e agibilità per edifici ordinari nell’emergenza post-sismica (AeDES) . Drago C., Ferlito R. Zucconi M.; 2015: Equivalent Damage Validation by Variable Cluster Analysis . ICNAAM 2015, 13th International Conference of Numerical Analysis and Applied Mathematics. Falcucci E. et al. ; 2009: Surface faulting due to the L’Aquila earthquake of April 6th 2009 - Seismological Research Letters , in press. Ferlito R., Guarascio M., Zucconi M.; 2013: Assessment of a vulnerability model against post-earthquake damage data: The case study of the historic city centre of L’Aquila in Italy . vol. 132, 2013, p. 393–404. doi:10.2495/ ERES130321. Galadini F., Galli P.; 2000: Active tectonics in the central Apennines (Italy) - input data for seismic hazard assessment. Nat. Haz. 22, 225–270. Galli P., Molin D., Giuliani R., Bosi V., Mattone M., Gruppo QUEST; 2003: Il terremoto del31/10/2002: sismicità storica di San Giuliano, rilievo macrosismico e deformazione superficiale cosismica. Ingegneria Sismica, 33, 8-18. Galli P., Camassi R. (eds.); 2009: Rapporto sugli effetti del terremoto aquilano del 6 aprile 2009, Rapporto congiunto DPC-INGV. 12 pp. http://portale.ingv.it/real-time-monitoring/quest/macrodef_sito.pdf Galli P. et al. ; 2009: Il Terremoto Aquilano del 6 Aprile 2009: Rilievo Macrosismico, Effetti di superficie ed implicazioni sismotettoniche. Il Quaternario Italian Journal of Quaternary Sciences, 22(2), 235-246 Giaccio B. et al; 2004: Caratteristiche geologiche-geomorfologiche ed effetti di sito a San Giuliano di Puglia (CB) e in altri abitati colpiti dalla sequenza sismica dell’ottobre-novembre 2002. Il Quaternario Italian Journal of Quaternary Sciences, 17(1), 83-99. Istituto Nazionale di Geofisica e Vulcanologia; 2002: L’epicentro della scossa del 31 ottobre 2002 ore 11:32 e del 1 novembre 2002 ore 16:08. http://www.ingv.it/~roma/reti/rms/terremoti/italia/molise/molise.html. Mele F., Amato A.; 2009: L’inizio e la fine della sequenza sismica dell’Aquila. https://ingvterremoti.wordpress . com/2014/11/09. Towards new insights into seismic hazard of the Salento Peninsula (Puglia, Southern Italy) from the analysis of far and near field seismicity G. Alessio 1 , M. De Lucia 1 , G. Gaudiosi 1 , R. Nappi 1 , S. Porfido 2 1 Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Napoli Osservatorio Vesuviano, Italy 2 CNR-IAMC Napoli, Italy Introduction. The Salento peninsula (Puglia, southern Italy) has been generally considered almost aseismic, but it has been hit by some high energy earthquakes over the last centuries. The strong earthquake affecting the Salento peninsula is represented by the February 20, 1743 earthquake (I 0 = IX, Mw =7.1, Rovida et al. , 2011), which caused severe damage in the Salento area. Moreover the Salento has been damaged by the strongest earthquakes occurred in Northern Apulia, Southern Apennines, Adriatic and Ionian sea, Albania and Greece that also triggered significant environmental effects. The purpose of this study is opening new insights into the seismicity of Salento, through the analysis of far and near field seismicity, for providing a more realistic assessment of its seismic hazard. Near and far field seismicity. The Salento Peninsula (Apulia, southern Italy) over the last centuries has been epicentral area of several low and medium energy earthquakes with magnitude 3 ≤ Mw ≤5, apart from the February 20, 1743, earthquake with I 0 = IX and Mw = 7.1 (Rovida et al. , 2011). Analyzing the CFTI4Med catalogue (Guidoboni et al ., 2007), 13 earthquakes occurred in the XX century, with 3.2<Mw<4.6, and located in the Salento peninsula have been added to the CPTI11 extracted events (Fig.1).