Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9753
AuthorsDi Giulio, G.* 
Amoroso, S.* 
Di Naccio, D.* 
Falcucci, E.* 
Gori, S.* 
Hailemikael, S.* 
Vassallo, M.* 
Ciampaglia, A.* 
De Luca, G.* 
Del Grosso, A.* 
Di Marcantonio, P.* 
D'Onofrio, K.* 
Porreca, M.* 
Trotta, D.* 
Villani, F.* 
Milana, G.* 
TitleThe Seismic Microzonation of San Gregorio Through a Multidisciplinary Approach. Seismic Amplification in a Stiff Site
Issue Date2014
URIhttp://hdl.handle.net/2122/9753
KeywordsUrban Geology, Sustainable Planning, Landscape Exploitation
Subject Classification04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous 
AbstractThe village of San Gregorio (L'Aquila, Italy) was severely damaged by the April 6, 2009 earthquake. San Gregorio is situated at the base of a carbon- ate relief bounded by the Aterno river alluvial plain. The geological features of the area are very complex: jointed carbonate bedrock, cemented gravels and alluvial fan crop out in the village. Co-seismic ground fractures were seen along SW dip- ping active fault segments crossing San Gregorio. We integrated the microzona- tion studies with new geological, geotechnical and geophysical data for supporting the reconstruction planning of the village. Noise measurements show strong and polarized peaks in the horizontal-to-vertical spectral ratios (H/V) in the 3-7 Hz frequency band. Interestingly, the alluvial fan and the outcropping rock masses show both H/V peaks. To understand the influence of rock mass joint condition on site effect, we performed structural surveys on carbonate bedrock to look for a possible correlation between rock fracturing and ground-motion amplification
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