This research derives paleostress tensors for deformation affecting late Cretaceous rocks between Amman and Al-Hallabat, northern Jordan reconstructs the region's tectonic history. Three distinct formations are exposed in investigated area: Wadi As Sir (Turonian), Umm Ghudran (Santonin), silicified limestone (Campanian). The stress inversion is derived from data collected on fault-slip at four ...