GNGTS 2014 - Atti del 33° Convegno Nazionale

GNGTS 2014 S essione 1.1 101 Burrato, P., F. Ciucci and G. Valensise (2003). An inventory of river anomalies in the Po Plain, northern Italy: evidence for active blind thrust faulting, Annals of Geophys., 46 (5), 865-882. Cesca S., F. Grigoli, S. Heimann, A. González, S. Buforn, S. Maghsoudi, E. Blanch, and T. Dahm (2014) The 2013 September–October seismic sequence offshore Spain: a case of seismicity triggered by gas injection? Geophys. J. Int., 198 (2): 941-953. Caloi, P., M. De Panfilis, D. Di Filippo, L. Marcelli e M. C. Spadea (1956). Terremoti della Val Padana del 15-16 maggio 1951. Annali di Geofisica, 9(1), 63-105. Cartlidge, E. (2014). Human activity may have triggered fatal Italian earthquakes, panel says. Science, 344, 141, 11 April 2014, doi: 10.1126/science.344.6180.141. Casero, P. (2004). Structural setting of petroleum exploration plays in Italy. In: Geology of Italy, Special Volume of the Italian Geological Society Special Volume for the, IGC 32 Florence, Chieti, Italy, 189–199. Devoti, R., A. Esposito, G. Pietrantonio, A.R. Pisani and F. Riguzzi (2011). Evidence of large scale deformation patterns from GPS data in the Italian subduction boundary, Earth Planet. Sci. Lett., 311, 230-241, doi:10.1016/ j.epsl. 2011.09.034. DISS Working Group (2010). Database of Individual Seismogenic Sources (DISS), Version 3.1.1 A compilation of potential sources for earthquakes larger than M 5.5 in Italy and surrounding areas, http://diss.rm.ingv.it/diss/, © INGV 2010 - Istituto Nazionale di Geofisica e Vulcanologia, 2010. Ellsworth, W.L. (2013), Injection-induced earthquakes, Science, 341, DOI:10.1126/science.1225942. ENI (1996). Area ENI. Dominio appenninico orientale. Lineamenti geologico minerari. Technical report (www. videpi.com ) International Commission on Hydrocarbon Exploration and Seismicity in the Emilia-Romagna region (ICHESE) (2014). Report on the Hydrocarbon Exploration and Seismicity in Emilia Region, 213 pp. (http://mappegis. regione.emilia-romagna.it/gstatico/documenti/ICHESE/ ICHESE_Report.pdf) Keranen K. M., H. M. Savage, G. A. Abers and E. S. Cochran (2013) Potentially induced earthquakes in Oklahoma, USA: Links between wastewater injection and the 2011 Mw 5.7 earthquake sequence, Geology, v. 41 no. 6 p. 699-702 Mucciarelli, M. (2013). Induced seismicity and related risk in Italy, Ingegneria Sismica, 30, 118-122. Nardon S., Marzorati D., Bernasconi A., Cornini S., Gonfalini M., Romano A. and Terdich P. (1991), Fractured carbonate reservoir characterisation and modelling: a multisciplinary case study from the Cavone oil field, Italy. First Break, 9, 12, 553-565, doi: 10.3997/1365-2397.1991027 Rovida, A., R. Camassi, P. Gasperini and M. Stucchi, eds. (2011). CPTI11, the 2011 version of the Parametric Catalogue of Italian Earthquakes, Milano, Bologna; available at: http://emidius.mi.ingv.it/CPTI/ . Scholz, C. H. (2002). The Mechanics of Earthquakes and Faulting. 2nd Edition, May 2002, Cambridge University Press, 464 pp., ISBN: 9780521655408. Vannoli, P., Burrato, P., and Valensise, G. (2014). The seismotectonics of the Po Plain (northern Italy): tectonic diversity in a blind faulting domain, Pure and Applied Geophysics, doi: 10.1007/s00024-014-0873-0. A CRITICAL REVISION OF THE SALENTO PENINSULA SEISMICITY: THE CASE OF THE FEBRUARY 20, 1743 EARTHQUAKE AND RELATED ENVIRONMENTAL EFFECTS R. Nappi 1 , G. Alessio 1 , G. Gaudiosi 1 , M. De Lucia 1 , S. Porfido 2 1 Istituto Nazionale di Geofisica e Vulcanologia, Sezione Osservatorio Vesuviano, Napoli, Italy 2 CNR-IAMC Napoli, Italy Introduction. The area of the Salento peninsula (Apulia, southern Italy) is considered the stable foreland of the southern Apennines chain (Cinque et al. , 1993), although it has been hit by several low energy and a few high energy earthquakes over the last centuries. The aim of this study is a critical revision of the historical and recent seismicity of the Salento peninsula and surrounding seismogenetic areas, for re-evaluating the macroseismic effects in MCS scale and ground effects in natural environment, according to the ESI 2007 scale (Michetti et al. , 2007; Guerrieri et al. , 2012). In particular, the February 20, 1743 earthquake, the strongest of the area, was reviewed and new MCS intensity values were attributed to some