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During the orogenic development of the Hellenides, the "Frontal Thrust of Internal Zones" (FTIZ) localised tectonic superposition of the Internal Zones over the External Zones. The belt was subsequently subject to a major extensional deformation responsible for a negative tectonic inversion of the FTIZ, along a major detachment called here "Main Pelagonian Detachment" (MPD). The along-strike changes in the geometry and the kinematics of the MPD suggest different tectonic configurations largely inherited fromthe flat-ramp-flat initial geometry of the thrust. The distribution of the recent basins, mainly located within the Internal Zones, illustrates the major role of the FTIZ reactivation in the overall collapse of Internal Hellenides. [ABSTRACT FROM AUTHOR]

In the 60s, the Hellenic belt was taken as the "Geosyncline model". Here we take a modern look at this Hellenic/Aegean region which as a concentrate encompasses all the main geodynamic processes known in orogens. This region documents the fundamental characteristics of the geodynamic processes related to mountain building, namely continental rifting, oceanic spreading, oceanic then continental subduction, collision i.e., closure of oceanic basins. In particular, the Mesozoic obduction events in northern Hellenides, and the effects of a still ongoing major extension linked to the active subduction under the Aegean domain. [ABSTRACT FROM AUTHOR]