Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10189
AuthorsDi Giulio, G.* 
de Nardis, R.* 
Boncio, P.* 
Milana, G.* 
Rosatelli, G.* 
Stoppa, F.* 
Laecchia, G.* 
TitleSeismic response of a deep continental basin including velocity inversion: the Sulmona intramontane basin (Central Apennines, Italy)
Issue Date1-Jan-2016
Series/Report no.1/204(2016)
DOI10.1093/gji/ggv444
URIhttp://hdl.handle.net/2122/10189
KeywordsFourier analysis, Earthquake ground motions, Site effects
Subject Classification04. Solid Earth::04.06. Seismology::04.06.04. Ground motion 
AbstractThe Sulmona plain (central Italy) is an intramontane basin of the Abruzzi Apennines that is known in the literature for its high seismic hazard. We use extensive measurements of ambient noise to map the fundamental frequency and to detect the presence of geological heterogeneities in the basin. We perform noise measurements along two basin-scale orthogonal transects, in conjunction with 2-D array experiments in specific key areas. The key areas are located in different positions with respect to the basin margins: one at the eastern boundary (fault-controlled basin margin) and one in the deepest part of the basin. We also collect independent data by using active seismic experiments (MASW), down-hole and geological surveys to characterize the near-surface geology of the investigated sites. In detail, the H/V noise spectral ratios and 2-D array techniques indicate a fundamental resonance (f0) in the low-frequency range (0.35–0.4 Hz) in the Sulmona Basin. Additionally, our results highlight the important role that is played by the alluvial fans near the edge-sectors of the basin, which are responsible for a velocity inversion in the uppermost layering of the soil profile. The H/V ratios and the dispersion curves of adjacent measurements strongly vary over a few dozens of meters in the alluvial fan area. Furthermore, we perform 1-D numerical simulations that are based on a linear-equivalent approach to estimate the site response in the key areas, using realistic seismic inputs. Finally, we perform a 2-D simulation that is based on the spectral element method to propagate surface waves in a simple model with an uppermost stiff layer, which is responsible for the velocity inversion. The results from the 2-D modelling agree with the experimental curves, showing deamplified H/V curves and typical shapes of dispersion curves of a not normally dispersive site.
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