GNGTS 2015 - Atti del 34° Convegno Nazionale
GNGTS 2015 S essione 1.2 107 on the Oristano offshore are probably associated to the Pliocene magmatic layer outcropping in the adjacent Sinis Peninsula. Aretrodeformation of a complex block geometries, recognized in a Plio-Quaternary marginal basin near the shoreline, seems to suggest a correlation between the fracture system and the coeval magmatic activity. Acknowledgements. The authors gratefully acknowledge OGS-Trieste for the seismic data set used in this work, Shlumberger through the Petrel academic grant for interpretation software and Midland Valley through the Move Software Suite academic grant to the University of Trieste. References Beccaluva L., Brotzu P., Maciotta G., Morbidelli L., Serri G., Traversa G.; 1987, 80: Cainozoic tectono-magmatic evolution and inferred mantle in the Sardo-Tyrrhenian area. The lithosphere in Italy . Advanced in Science Research, Accad. Naz. Lincei, 80 , 229-248. Cherchi A., Montadert L.; 1982. Oligo-Miocene rift of Sardinia and the early history of the Western Mediterranean Basin. Nature, 298 , 736-739. Clauzon G., Suc J.P., Gautier F., Berger A., Loutre M.F.; 1996: Alternate interpretation of the Messinian Salinity Crisis: controversy resolved?. Geology, 24, pp. 363–366. Cornnée J.J., Maillard A., Conesa G., García F., Saint Martin J.P., Sage F., Münch P.; 2008: Onshore to offshore reconstruction of the Messinian erosion surface in western Sardinia, Italy: MSC implications . Sediementary Geology, 210 (1-2), 48-60. Fais F., Klingele E.E., Lecca L.; 1996: Oligo-Miocene half graben structure in Western Sardinian Shelf (western Mediterranean): reflection seismic and aeromagnetic data comparison. Marine Geology, 133 , 293-222. Geletti R., Zugur F., Del Ben A., Buriola F., Fais S., Fedi M., Forte E., Mocnik A., Paoletti V., Pipan M., Ramella R., Romeo R., Romi A.; 2014: The Messinian Salinity Crisis: New seismic evidence in the West-Sardinian Margin and Eastern Sardo-Provençal basin (West Mediterranean Sea) . Marine Geology, 351 , 76-90. Lofi J., Déverchére J., Gaullier V., Gillet H., Gorini C., Guennoc P., Loncke L., Maillard A., Sage F., Thinon I.; 2001: Seismic Atlas of the “ The Messinian Salinity Crisis” makers in the Mediterranean and Black Sea . Geological Map of the World Ed., Paris, France. Lustrino M., Melluso L., Morra V.; 2000: The role of lower continental crust and lithospheric mantle in the genesis of Plio-Pleistocene volcanic rocks from Sardinia (Italy). EPSL, 180 , 259-270. Maillard A., Mauffret A., Watts A.B., Torné M., Pascal G., Buhl P., Pinet B.; 1992: Tertiary sedimentary history of the Valencia trough (western Mediterranean). Tectonophysics, 203 , 57-75. Yilmaz O.; 2001: Seismic Data Analysis . SEG publication, S.M. Doherty Ed., Tulsa OK, USA. Analysis of geological, seismological and gravimetric data for the identification of active faults in Abruzzo area (Central Italy) P. Luiso 1 , V. Paoletti 1 , G. Gaudiosi 2 , R. Nappi 2 , F. Cella 3 , M. Fedi 1 1 Dipartimento di Scienze della Terra, Università degli Studi «Federico II», Napoli, Italy 2 Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italy 3 Dipartimento di Scienze della Terra, Università degli Studi della Calabria, Arcavacata di Rende (CS), Italy Introduction. The aim of the study is to identify and better constrain the geometry of the seismogenic structures (������� ����������� ��� ������ ����� �������� �� ��� ������� ���� active, outcropping and buried fault systems) in the Abruzzo area (central Italy), through an ���������� �������� �� ��������������� ������� ��� ����������� ����� integrated analysis of geo-����������� � structural, seismic and gravimetric data. The studied area is one of the most active zones from a geodynamic point of view of the Italian Apennines, characterized by the occurrence of intense and widely spread seismic activity. The integrated analysis of structural, seismic and gravimetric data (Gaudiosi et al. , 2012) of the areas was carried out through the use of Geographic Information System (GIS).
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