SSW-ENE interpreted seismic section through the southern part of the Campidano (see location on Figs. 5 and 14) with the same markers than in Figure 15. It shows the thick syntectonic pre-Aquitanian (blak marker) sedimentary section like in the northern Campidano. It could include Oligocene and even Late Eocène sediments like in the northern Campidano, and even below older Eocene and Mesozoic. Same markers as on Figure 15A. The black arrow suggests the crest of a tilted fault block bound by a major fault mainly active during the pre-SGS Oligocene.