Vlore-Elbasan-Diber transversal is identified through: 1. Activity of the evaporitic intrusion of Dumrese 2. The tectonic windows of Okshtun and the Peshkopise 3. Segmentation of Krasta subzone 4. Spatial position of ultrabasic massif of Shpat-Kuterman, Labinot Fushe tectonic unit, anticline structure of Patos-Verbas, buried carbonate structures 5. Oil and thermo-mineral waters 6. Seismicity of the region 7. New tectonic movements.