Detailed stratigraphic correlation of Priabonian deposits along a 2 km-long N-S transect at the southeastern border of the Guzargues basin, showing differential subsidence and onlap geometries induced by the syndepositional growth of the Lirou anticline. See Figure 7 for location of logs. Horizontal correlation lines set at the maximum of progradation recorded by several meters-thick, stacked conglomeratic channels that closely rests on Lutetian limestones at the apex of the Lirou anticline.