Fig. 7: The cross seismic time section I-I, which offer obvious information on the geological setting of the area westward to the thrust front of the Mali Gjere anticline. Thus, OTC is Orogeny top carbonates and FTC is the Foreland top carbonates below evaporitic sequence T₃ev of the Albanides thrust belts. But there is a total black out on the eastern part of this section, where locates the Delvina field, due to improper methodology of 2D seismic, while shooting on the eroded carbonate section of Mesozoic.