Jp. Saintmartin et al., GEOMETRY OF THE MALTA MESSINIAN PLATFORM - EVIDENCE FOR A MEDITERRANEAN SEA-LEVEL RISE DURING THE MESSINIAN TIMES, Comptes rendus de l'Academie des sciences. Serie II. Sciences de la terre et des planetes, 324(9), 1997, pp. 729-736
The Messinian carbonate platform of the Maltese islands is composed of
successive sigmoidal sedimentary bodies prograding towards the ENE. T
he last one includes stromatolitic layers and emergent levels. The sup
erimposition of the bodies indicates successive pulse rises of the rel
ative sea level. As such a setting is similar to those in other carbon
ate platforms of the Mediterranean it was probably related rather thro
ugh eustacy, than tectonics.