Fig. 15From: Growth-strata geometry in fault-propagation folds: a case study from the Gafsa basin, southern Tunisian AtlasDip trends of growth-strata bedding in other southern flanks of Gafsa basin folds a Jebel Khasfa, b Jebel Satah. Both examples show horizontal trend lines, confirming the general constant dip of all growth-strata beds, including recent sedimentsBack to article page