Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/705
Authors: Gasparini, C.* 
Di Maro, R.* 
Pagliuca, N. M.* 
Pirro, M.* 
Marchetti, A.* 
Title: Recent seismicity of the «Acque Albule» travertine basin
Issue Date: 2002
Series/Report no.: 45 (3-4)
URI: http://hdl.handle.net/2122/705
Keywords: seismicity
neotectonic
Subject Classification04. Solid Earth::04.06. Seismology::04.06.04. Ground motion 
04. Solid Earth::04.06. Seismology::04.06.06. Surveys, measurements, and monitoring 
04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonics 
Abstract: The seismic period which occurred in a portion of Guidonia Montecelio and Tivoli territory, two towns situated about twenty kilometres NE of Rome, affected four areas with a high density of population: Guidonia, Collefiorito, Villalba and Bagni di Tivoli. Even though the events had a very low magnitude (less than 3.0), local phenomena, like rumbles and strong vibrations of the ground, frightened inhabitants also because some months before (January 26, 2001) in a village named Marcellina situated a few kilometres away from Guidonia, a large sinkhole (600 m) had appeared without fore signals. The «Istituto Nazionale di Geofisica e Vulcanologia» (INGV) installed some digital stations that monitored the seismic phenomena. This paper has the aim to process all the information acquired during the period, both from the micro and macro seismic point of view, in order to explain the phenomenology that involved the area. The synergy of the two methodologies lead us to the conclusion that two different seismotectonic structures originated the events, one in an anti-apenninic direction, the other in a N-S direction.
Appears in Collections:Manuscripts
Annals of Geophysics
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