Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/1505
AuthorsDi Bucci, D.* 
Ravaglia, A.* 
Seno, S.* 
Toscani, G.* 
Fracassi, U.* 
Valensise, G.* 
TitleSeismotectonics of the Southern Apennines and Adriatic foreland: insights on active regional E-W shear zones from analogue modeling
Issue Date11-Aug-2006
Series/Report no.25 (2006)
DOI10.1029/2005TC001898
URIhttp://hdl.handle.net/2122/1505
KeywordsActive strike-slip fault
sandbox model
southern Italy
Subject Classification04. Solid Earth::04.01. Earth Interior::04.01.02. Geological and geophysical evidences of deep processes 
04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations 
04. Solid Earth::04.04. Geology::04.04.09. Structural geology 
04. Solid Earth::04.06. Seismology::04.06.01. Earthquake faults: properties and evolution 
04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonics 
AbstractThe active tectonics at the front of the Southern Apennines and in the Adriatic foreland is characterized by E-W striking, right-lateral seismogenic faults, interpreted as reactivated inherited discontinuities. The best studied among these is the Molise-Gondola shear zone (MGsz). The interaction of these shear zones with the Apennines chain is not yet clear. To address this open question we developed a set of scaled analogue experiments, aimed at analyzing: 1) how dextral strike-slip motion along a pre-existing zone of weakness within the foreland propagates toward the surface and affects the orogenic wedge; 2) the propagation of deformation as a function of displacement; 3) any insights on the active tectonics of Southern Italy. Our results stress the primary role played by these inherited structures when reactivated, and confirm that regional E-W dextral shear zones are a plausible way of explaining the seismotectonic setting of the external areas of the Southern Apennines.
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