Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3703
Authors: Vignaroli, G.* 
Faccenna, C.* 
Jolivet, L.* 
Piromallo, C.* 
Rossetti, F.* 
Title: Subduction polarity reversal at the junction between the Western Alps and the Northern Apennines, Italy
Journal: Tectonophysics 
Series/Report no.: 1-4 /450 (2008)
Publisher: Elsevier
Issue Date: 28-Dec-2007
DOI: 10.1016/j.tecto.2007.12.012
URL: http://www.sciencedirect.com/science/journal/00401951
Keywords: Western Alps
Northern Apennines
Voltri Massif
Tomography
Kinematic reconstruction
Extensional detachment
Toroidal flow
Subject Classification04. Solid Earth::04.07. Tectonophysics::04.07.02. Geodynamics 
Abstract: The controversial relationship between the orogenic segments of the Western Alps and the Northern Apennines is here explored integrating recently published 3D tomographic models of subduction with new and re-interpreted geological observations from the eclogitic domain of the Voltri Massif (Ligurian Alps, Italy), where the two belts joint each other. The Voltri Massif is here described as an extensional domain accommodating the opposing outward migration of the Alpine and Apennine thrust fronts, since about 30–35 Ma. Using tomographic images of the upper mantle and paleotectonic reconstructions, we propose that this extensional setting represents the surface manifestation of an along strike change in polarity of the subducted oceanic slab whose polarity changed laterally in space and in time. Our tectonic model suggests that the westward shift of the Alpine thrust front from the Oligocene onward was the consequence of the toroidal asthenospheric flow induced by the retreat of the Apenninic slab.
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