Vlorë - Elbasan - Dibër Tectonic Fault in Albania
978-3-659-31068-3
3659310689
64
2019-08-02
39,90 €
eng
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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.
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Geoscienze
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