Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8277
AuthorsVignaroli, G.* 
Minelli, L.* 
Rossetti, F.* 
Balestrieri, M. L.* 
Faccenna, C.* 
TitleMiocene thrusting in the eastern Sila Massif: Implication for the evolution of the Calabria-Peloritani orogenic wedge (southern Italy)
Issue Date2012
Series/Report no./538-540 (2012)
DOI10.1016/j.tecto.2012.03.011
URIhttp://hdl.handle.net/2122/8277
KeywordsAFT thermochronology
orogenic wedge
Calabria-Peloritani Arc
Subject Classification04. Solid Earth::04.04. Geology::04.04.09. Structural geology 
AbstractAlpine orogens in the central Mediterranean region have revealed the concomitance of crustal extension in back-arc domain and crustal shortening in frontal domain. Quantitative data of deformation in the frontal orogenic wedges are necessary to understand how the shortening-extension pair evolves in terms of structures, orogenic transport, timing, and exhumation rate. This paper deals with kinematics and ages of the frontal thrust systems of the Calabria-Peloritani Arc (Italy) exposed in the eastern Sila Massif. We first present structural fieldwork, onshore and offshore well log data, and new apatite fission-track (AFT) thermochronology. Then, we describe the structural architecture of the studied area as an ENE-verging stacking of thrust sheets involving basement units and syn-orogenic sediments. The AFT study documents that thrust sheets entered the partial annealing zone from 18 Ma to 13 Ma. This Early-Middle Miocene thrusting phase was coeval with exhumation of high-pressure/low temperature metamorphic rocks in the hinterland of the orogen (Coastal Chain area), mainly driven by top-to-the-W extensional tectonics. Opposite kinematic shear senses (contractional top-to-the-E and extensional top-to-the-W) and different exhumation rates (slow in the frontal, more rapid in the hinterland) are framed in a tectonic scenario of a critically tapered orogenic wedge during the eastward retreating of the Apennine slab.
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