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Fig. 5: Cross geo-seismic profile II-II of the De gas condensate field below the thrusted anticline of Mali Gjere and seismic detection of the Apulia Foreland (A), below the Albanides thrust belts (B). (After Prenjasi E, et al.,1994). Q - Quaternary, N11b Burdigalian, N11a Aquitanian, Pg31, 2, 3 Lower, Middle, Upper Oligocene, Pg1+Pg2 Paleocene + Eocene, Cr1, 2 Lower, Upper Cretaceous, J1, 2, 3 Lower, Middle, Upper Jurassic, T3 e, d Upper Triassic evaporitic and dolomitic deposits, — Proved gas condensate-water contact.