The frontal zone of the Dinarides and its foreland are characterized by the presence of major late orogenic northwest-southeast faults trending parallel to and locally dissecting the leading edge of the thin-skinned thrust belt. On the basis of their geometry and regional distribution, these structures are interpreted as right-lateral strike-slip faults and are related to the formation of en echelon compressional structures in the Split-Dubrovnik area of the central Adriatic region and to the opening of the post-Messinian pull-apart Albanian foredeep (South Adriatic Basin) in the Pliocene-Holocene. These strike-slip faults represent the last stage of the mountain-building process in the Pliocene and Holocene, when the forelandward propagation of the Dinaric thrust belt was inhibited by stacking of thrust sheets and by overall thickening of the colliding continental crust. In that respect, the Dinaric side of the Apulia (Adria) differs from the Apenninic side, where the thin-skinned thrusting progressed normally toward the foreland until the Pliocene. On a regional scale, these northwest-southeast-trending strike-slip faults in the frontal Dinarides and their apparent continuation to the Hellenides of western Greece, as well as the dextral Vardar fault system, indicate the existence of escape tectonics in the Dinaric-Hellenic region. During the last stage of orogeny, the strikeslip faults provided a means of tectonic transport from the collision zone of Apulia with Europe toward the subduction zone of the Hellenic Trench. In southern Greece, the southeastward-moving Dinaric-Hellenic blocks apparently interfered with the westward-moving Anatolian plate and deflected it southwestward. The Albanian foredeep, in terms of tectonic setting, resembles the pull-apart Vienna basin, which formed within the attenuated southwest-northeast-trending transfer zone of the West Carpathians during the last stages of the Alpine orogeny.