GNGTS 2023 - Atti del 41° Convegno Nazionale

Session 1.1 GNGTS 2023 geological interest as highlighted by the whole 3-D resistivity model (Fig. 1). Further research and integration with the available high-resolution seismic and electrical resistivity 2-D models will allow us a detailed reconstruction of the Quaternary evolution of this tectonic basin and the long-term history of its bounding faults. Fig. 1. Location of the 3-D FullWaver survey (red squares: transmissions; white circles: dipolar receivers) and the 2-D ancillary resistivity profiles (yellow line: 2-D FullWaver transect; green and blue lines: 2-D high-resolution ERT). References Benedetti, L., Manighetti, I., Gaudemer, Y., Finkel, R., Malavieille, J., Pou, K., et al.; 2013: Earthquake synchrony and clustering on Fucino faults (Central Italy) as revealed from in situ 36Cl exposure dating . J. Geoph. Res.: Solid Earth, 118 , 4948–4974, DOI 10.1002/jgrb.50299. Giraudi, C., Bodrato, G., Lucchi, M. R., Cipriani, N., Villa, I. M., Giaccio, B., & Zuppi, G. M.; 2011: Middle and late Pleistocene glaciations in the Campo Felice Basin (central Apennines, Italy) . Quat. Res., 75 , 219–230, DOI 10.1016/j.yqres.2010.06.006. Giraudi, C., & Giaccio, B.; 2017: Middle Pleistocene glaciations in the Apennines, Italy: new chronological data and preservation of the glacial record . Geol. Soc., 433 , 161-178, DOI 10.1144/SP433.1.