Please use this identifier to cite or link to this item:
Authors: Di Bucci, D.* 
Ridente, D.* 
Fracassi, U.* 
Trincardi, F.* 
Valensise, G.* 
Title: Marine paleoseismology from Very High Resolution seismic imaging: the Gondola Fault Zone (Adriatic foreland)
Journal: Terra Nova 
Series/Report no.: 5/ 21 (2009)
Publisher: Wiley - Blackwell
Issue Date: 2009
DOI: 10.1111/j.1365-3121.2009.00895.x
Keywords: Chirp-Sonar profiles
fault reactivation
right-lateral shear
Adriatic Sea
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 
Abstract: We 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).
Appears in Collections:Article published / in press

Files in This Item:
File Description SizeFormat
Di Bucci et al., 2009_accettato.pdf2.43 MBAdobe PDFView/Open
Show full item record

Citations 50

checked on Feb 10, 2021

Page view(s) 50

checked on Jul 3, 2022

Download(s) 50

checked on Jul 3, 2022

Google ScholarTM