Fig. 8From: Growth-strata geometry in fault-propagation folds: a case study from the Gafsa basin, southern Tunisian AtlasGeological cross section oriented NW–SE through Gafsa basin (for location, see Fig. 4). The horizontal shortening of the different fault-propagation folds splaying off the main decollement is noted above each structure, giving a total shortening of the whole section of 8.8 kmBack to article page