Syn- and post-accretionary structures in the Neoproterozoic Central Allaqi-Heiani suture zone, Southeastern Egypt

▶ We model tectonic evolution of the Allaqi-Heiani suture zone in southeastern Egypt. ▶ The suture separates the South Eastern Desert terrane from the Gabgaba terrane. ▶ Poly-phase structural deformation affected the suture zone. ▶ Deformation was achieved through N-S and E-W compressions, respectively.