GNGTS 2019 - Atti del 38° Convegno Nazionale

GNGTS 2019 S essione 3.2 627 Bibliografia Bosman A., Casalbore D., Anzidei M., Muccini et al. , (2015). The first ultra-high resolution Marine Digital Terrain Model of the shallow-water sector around Lipari Island (Aeolian archipelago, Italy). Annals of Geophysics. Doi: 10.4401/ag-6746. Colbo K., Ross T., Brown C., Weber T. (2014). A review of oceanographic applications of water column data from multibeam echosounders. Estuarine, Coastal and Shelf Science 145 (2014) 41-56. Dattola, L., Rende, S. F., Dominici, R., Lanera, P., Di Mento, R., Scalise, S., ... & Aramini, G. (2018, October). Comparison of Sentinel-2 and Landsat-8 OLI satellite images vs. high spatial resolution images (MIVIS and WorldView-2) for mapping Posidonia oceanica meadows. In Remote Sensing of the Ocean, Sea Ice, Coastal Waters, and Large Water Regions 2018 (Vol. 10784, p. 1078419). International Society for Optics and Photonics. Rende, S. F., Irving, A. D., Bacci, T., Parlagreco, L., Bruno, F., De Filippo, F., ... & Cicero, A. M. (2015a). Advances in micro-cartography: A two-dimensional photo mosaicing technique for seagrass monitoring. Estuarine, Coastal and Shelf Science, 167, 475-486. Rende, F. S., Irving, A. D., Lagudi, A., Bruno, F., Scalise, S., Cappa, P., ... & Di Mento, R. (2015b). Pilot application of 3D underwater imaging techniques for mapping Posidonia oceanica (L.) delile meadows. The International Archives of Photogrammetry, Remote Sensing and Spatial Information Sciences, 40(5), 177. Villarreal J.S., Lovelock E.C., Saunders M.I., Roelfsema C., Mumby P.J., (2016). Organic carbon in seagrass sediments is influenced by seagrass canopy complexity, turbidity, wave height, and water depth. Limnology and Oceanography. 00, 2016, 00–00. doi: 10.1002/lno.10262 PRELIMINARY RESULTS OF THE SEISMIC RESPONSE STUDY OF THE POGGIO CANCELLI VALLEY (CAMPOTOSTO, AQ) F. Bozzano 1 , M. Fiorucci 1 , A. Gallo 1 , S. Hailemikael 2 , R. Iannucci 1 , S. Martino 1 , S. Rivellino 1 1 Earth Sciences Department of “Sapienza” University of Rome and CERI - Research Centre for Geological Risk, Rome, Italy 2 ENEA Centro Ricerche Frascati, Italy Introduction. In this paper, we present preliminary results obtained by geological surveys and geophysical investigations for the evaluation of the local seismic response of the Poggio Cancelli valley (Campotosto, AQ). Poggio Cancelli Valley. The Poggio Cancelli valley is located in the Central Apennine, at the NNW bounder of Campotosto Lake (Campotosto, AQ) and hosts the Poggio Cancelli village as well as an earthfill dam built in 1939. In this sector of the Apennines, a thick silico-clastic synorogenic succession known as Laga Formation (Adamoli et al. , 2007) was deposited since Messinian. The Laga Fm. includes three members among which the Campotosto Lake one widely outcropping in the study area and representing the geologic bedrock. It is composed by thick arenaceous strata interlayer with gypsum-arenite levels (Centamore et al. , 1991; Artoni, 2003; Milli et al. , 2007). Alluvial deposits consisting of sands, silts and clays with levels of gravel, directly overlying the Laga Fm., fill the Poggio Cancelli valley. The valley is bordered by Laga Fm. reliefs, which are covered by debris at the foot of the slope. In addition, alluvial fans can be also recognised at the transition between the ridge slopes and valley edges, where the alluvial fan deposits overlay the alluvia. The NE side of Campotosto Lake basin is bounded by the Monti della Laga Fault System (MLFS), with a NW-SE trend and a length of about 30 km. MLFS is arranged in three splays with evidence of recent faulting (Galadini and Galli, 2003). Materials and methods. In the last years, engineering geological surveys and geophysical investigations were largely applied in seismic microzonation and local seismic response studies (Delgado et al ., 2000; LeBrun et al. , 2006). Field engineering geological surveys, single station