GNGTS 2016 - Atti del 35° Convegno Nazionale

184 GNGTS 2016 S essione 1.1 by strong earthquakes capable to originated significant surface effects such as surface faulting. In association with all the other evidences collected by previous papers, it is thus possible to adfirm that the Calore river fault systems can be considered as one of the most important seismogenetic zone of southern Apennines. References Cole P.D., Scarpati C.; 1993: A facies interpretation of the eruption and emplacement mechanism of the upper part of the Neapolitan yellow Tuff, Campi Flegrei, Southern Italy. Bulletin of volcanology, 55(5), 1993, pp. 311-326 Deino A.L., Orsi G., De Vita S., Piochi M.; 2004: The age of the Neapolitan Yellow Tuff caldera-forming eruption (Campi Flegrei caldera-Italy) assessed by 40Ar/39Ar dating method. Journal of Volcanology and Geothermal Research 133, 157–170. Ispra (2010): Note illustrative della Carta Geologica d’Italia alla scala 1:50.000, foglio 431 Caserta Est . , pp. 140. Di Bucci D., Massa, B. & Zuppetta, A.;2005: Structural setting of the 1688 Sannio earthquake epicentral area (Southern Italy) from surface and subsurface data . Journal of Geodynamics 40 (2005) 294–315 Di Bucci, D., Massa, B. & Zuppetta, A.;2006 : Relay ramps in active normal fault zones: A clue to the identification of seismogenic sources (1688 Sannio earthquake, Italy). ��� ��������� ���� ���� �������� GSA Bulletin, 118, 3/4, 430-448. Gruppo di Lavoro CPTI; 1999: Catalogo Parametrico dei Terremoti Italiani . ING, GNDT, SGA, SSN, Bologna, 92 pp. Patacca, E., & Scandone, P.;2007: Geology of the Southern Apennines . ���������� ����� ������� ��������� ��������� Bollettino della Società Geologica Italiana, 7, 75–119. Santangelo N., Ciamo G., Di Donato V., Esposito P., Petrosino P., Romano P., Russo Ermolli E., Santo A., Toscano F. Villa I. ;2010: Late Quaternary buried lagoons in the northern Campania plain (southern Italy): evolution of a coastal system under the influence of volcano-tectonics and eustatism. Ital. J. Geos., 129, 156-175. Santo A., Ascione A., Del Prete S., Di Crescenzo G., Santangelo N.; 2011: Collapse sinkholes distribution in the carbonate massifs of central and southern Apennines. Acta carsologica, 40/1, 95-112. Santo A., Santangelo N., Forte G., De Falco M.; 2016: Post flash flood survey: the October 14th and 15th 2015 event in the Paupisi-Solopaca area (Southern Italy). Journal of Maps, in print. Kinematics, seismotectonics and seismic potential of the eastern sector of the European Alps from GPS and seismic deformation data E. Serpelloni 1 , G. Vannucci 2 , L. Anderlini 1 , R.A. Bennett 3 1 Istituto Nazionale di Geofisica e Vulcanologia, Centro Nazionale Terremoti, Roma, Italy 2 Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Bologna, Italy 3 Dept. of Geoscience, University of Arizona, Tucson (AZ), USA We present a first synoptic view of the seismotectonics and kinematics of the eastern sector of the EuropeanAlps using geodetic and seismological data. The study area marks the boundary between the Adriatic and the Eurasian plates, through a wide zone of deformation including a variety of tectonic styles within a complex network of crustal and lithospheric faults. A new dense GPS velocity field, new focal mechanisms and seismic catalogues, with uniformly recalibrated magnitudes (from 1005), are used to estimate geodetic and seismic deformation rates and to develop interseismic kinematic and fault locking models. Kinematic indicators from seismological and geodetic data are remarkably consistent at different spatial scales. In addition to large-scale surface motion, GPS velocities highlight more localized deformation features revealing a complex configuration of interacting tectonic blocks, for which new constraints are provided in this work accounting for elastic strain build up at faults bonding rotating blocks. The geodetic and seismological data highlight two belts of higher deformation rates running WSW-ENE along the Eastern Southern Alps (ESA) in Italy and E-W in Slovenia, where deformation is more distributed. The highest geodetic strain-rates are observed in the Montello- Cansiglio segment of the ESA thrust front, for which the higher density of the GPS network