Gas seeps linked to salt structures in the Central Adriatic Sea

The analyses of about 800 kmofChirp sub-bottompro¢lers and 600 km2 ofMultibeamdata acquired during the 2005 and 2007 surveys of the R/VOGS Explora, and their correlation with one new, and several public, multichannel seismic pro¢les, allow us to propose a relation between the distribution of gas seepages, fracture systems and deep salt features present in the Central Adriatic Sea.Gas seepage is evident from pockmarks on the seabed and in the shallow sub-bottom, where acoustic chimneys and bright spots have been highlighted and analyzed.TheMid-Adriatic Depression (MAD) is a distinct morphological feature in the Central Adriatic Sea elongated in aNE^SW direction.The area is a¡ected by salt doming of Triassic evaporites which cause the two main alignments of theMid-Adriatic Ridge as far as the PalagruzaHigh and the Jabuka Ridge.These salt tectonics have existed since, at least,Paleogene times and are still active: they characterize sectors with less resistance to deformation produced by successive regional compressive regimes that have a¡ected the area di¡erently during the di¡erent geodynamic phases.Gas- seep features are distributed preferentially above and along the fracture systems produced above and around the salt mounds.