Table comparing sedimentation rates (sticks) and relative intensity of diapiric movements (curves) for each transgressive-regressive sequence. The relative intensity of diapiric movements is inferred from bedding geometry on the flanks of the diapiric ridges, and more precisely from the ratio of sequence thickness between the center of the mini- basins and the flanks of the ridges. Sedimentation rates are calculated from non-decompacted thicknesses, therefore only their relative value is meaningful. The estimation of the intensity of diapiric movements should also be considered in a relative manner.