Architecture and evolution of an extensionally-inverted thrust (Mt. Tancia Thrust, Central Apennines). Geological, structural, geochemical, and K–Ar geochronological constraints
Fault inversion may lead to significant obliteration of earlier tectonic structures, thus preventing the straightforward interpretation of the complete kinematics and deformation history of faults. We adopt a multidisciplinary approach to: (1) reconstruct the tectonic evolution through space and in time of the extensionally-inverted Mt.