Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5131
AuthorsDi Bucci, D.*
Ridente, D.*
Fracassi, U.* 
Trincardi, F.*
Valensise, G.* 
TitleMarine paleoseismology from Very High Resolution seismic imaging: the Gondola Fault Zone (Adriatic foreland)
Issue Date2009
Series/Report no./ (2009)
URIhttp://hdl.handle.net/2122/5131
KeywordsChirp-Sonar profiles
fault reactivation
right-lateral shear
Adriatic Sea
Italy
Subject Classification04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismology 
04. Solid Earth::04.04. Geology::04.04.04. Marine geology 
04. Solid Earth::04.04. Geology::04.04.08. Sediments: dating, processes, transport 
04. Solid Earth::04.04. Geology::04.04.09. Structural geology 
04. Solid Earth::04.06. Seismology::04.06.05. Historical seismology 
04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonics 
AbstractWe present a marine paleoseismology analysis of a dense network of very high resolution seismic profiles along the Gondola Fault Zone (GFZ), a right-lateral, E-W–striking, active fault system in the Adriatic foreland. This case-study aims to show how time and space variations in the activity of a dominantly right-lateral fault system can be assessed based on the vertical component of slip alone. The GFZ has been investigated for a length of 50 km. It includes two parallel subvertical fault sets and two main anticlines. The distribution of the late Middle Pleistocene to Holocene vertical component of displacement along-fault is bell-shaped, suggesting that in the long-term the fault zone acts as a single, kinematically coherent structure. Slip rates on individual fault segments, however, suggest that they may rupture independently. Vertical slip rates calculated for late Middle Pleistocene-Holocene intervals fall in a narrow range and are consistently small (0-0.18 mm/a).
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