Common Reflection Surface stacking and Common Scatter Point data mapping improve high-resolution seismic data.
Sea-level stagnancies during the Messinian Salinity Crisis created vast amount of accommodation space.
Deposition of an unusual thick Pliocene–Pleistocene mixed cool-water carbonate-siliciclastic prograding wedge.
Aggrading slope deposits cause seaward prolongation of accommodation space for seaward prograding shelf deposits.