J. Mascle et al., PRELIMINARY-RESULTS OF THE MULTICHANNEL S EISMIC-REFLECTION CRUISE PRISMED ACROSS THE LONIAN MEDITERRANEAN RIDGE, Comptes rendus de l'Academie des sciences. Serie II. Mecanique, physique, chimie, astronomie, 318(5), 1994, pp. 651-657
A recent multichannel seismic line collected during the PRISMED cruise
(March 1993) across the western branch of the Mediterranean Ridge (Ce
ntral Mediterranean) allows interpretation of this feature as a tecton
o-sedimentary accretionary prism. Seismic processing however clearly d
emonstrates that most of the tectonic shortening is due to thrusting a
nd piling up of Messinian evaporite sediments. The main decollement le
vel could be located near the basis of Messinian evaporites.