GNGTS 2016 - Atti del 35° Convegno Nazionale

116 GNGTS 2016 S essione 1.1 Current vertical deformation in the study area is inferred from the analysis of PS-InSAR datasets for the 1992-2010 time span. In particular, the analysis shows that the pattern of homogeneous kinematic domains follows that of faults showing evidence of recent activity in the Volturno River alluvial plain, while a more complex pattern is observed in the eastern part of the Campania Plain. The integrated datasets provide a comprehensive picture of the recent and active deformation scenario in this densely populated area, and of the time-space migration of extensional fault activity. Acknowledgements. This work was financially supported by the Regione Campania L.R. 05/2002 - 2007, responsible S. Mazzoli. References Argnani, A., Bortoluzzi, G., Bozzani, A., Canepa, A., Ligi, M., Palumbo, V., Serracca, P. and Trincardi, F.; 1989: Sedimentary dynamics on the Eastern Tyrrhenian Margin, Italy. PS/87 Cruise report. Giorn. Geol., s. III, 51, 1, 165-178. 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