“…The study of the geometry and evolution of diapiric structures that were active from Early to Middle Jurassic times in the central High Atlas, and their interaction with the flanking rocks, has been addressed in later years (Bouchouata, Canerot, Souhel, & Almeras, ; Ettaki, Ibouh, Chellaï, & Milhi, ; Martín‐Martín et al, ; Michard, Ibouh, & Charrière, ; Moragas et al, ; Saura et al, ; Teixell, Barnolas, Rosales, & Arboleya, ; Vergés et al, ). The presented study of diagenesis in the Tazoult salt wall is part of a prolonged work of our group in the Central High Atlas, detailed below, in which extensive field work and remote sensing mapping was carried out.…”