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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.

Produktbeschreibung
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.
Autorenporträt
Petraq Naço: Born in 1955, in 1979 Finished the Faculty of Geology and Mines, branch: Oil Geology, work at Geo-Science institute, in 1999 take PHD degree.Rakip Hysenaj: Born in 1955, In 1979 Finished the Faculty of Geology and Mines, branch Geology, Work at Albanian Geological Survey. In 2010 take the PHD degree.