Brittle vs. ductile strain during the synorogenic exhumation of HP-LT rocks: An example from the Lungro-Verbicaro Unit mylonites (northern Calabria, Italy)

We present a study on the mylonites exposed in the Cirella area along the Tyrrhenian coast of northern Calabria(southern Italy), in order to understand the role of ductile and brittle deformation on the exhumation process ofthese rocks. The analyzed shear zone is located in the footwall of a regional tectonic contact between metao-phiolites (Ligurian Complex) on the top, and the continental Lungro-Verbicaro Unit (Adria plate) at the bottom.The latter consists of a metasedimentary succession with Triassic shallow-water carbonates at the base of it,evolving upward to Jurassic-lower Miocene slope to deep basin carbonates and foredeep siliciclastic rocks. Bothoceanic and continental successions are characterized by high-pressure and low-temperature (HP-LT) meta-morphism. The analyzed mylonites show different degrees of strain, ranging from protomylonites to ultra-mylonites, the latter characterized by well-marked foliation and stretching lineations. Several micro- and me-soscale progressive deformation structures, including two fold sets, S-C’structures are present in these rocks, anda late oblique foliation, indicating a NW sense of shear. A successive shortening stage produced thrust faults andrelated folds, indicating a tectonic transport toward SE. We associate the mylonitic deformation with the activityof the overlying detachment fault, which is responsible for the synorogenic exhumation of the Lungro-VerbicaroUnit during the Miocene time. However, the ductile strain, recorded by the studied mylonites, accounted for asmall displacement during the exhumation of this tectonic slice. In fact, the calculated displacement achieved bythe Lungro-Verbicaro Unit, during exhumation, is much larger than the one estimated considering only theductile zones activity. This evidence suggests that, synchronously with ductile strain, brittle deformation oc-curred along the detachment fault located at the top of the thrust sheet. In addition, a severe erosion due to thetectonic exhumation of the HP-LT rocks (in the late Miocene) produced a large amount of clastic sediment thatfilled the extensional basins widespread in northern Calabria.