Permian sediments that is characterized by a gravity maximum. To explain the positive
gravity signature over the Jeffara sedimentary basin and to obtain a more quantitative
representation of the subsurface structure, a regional 2.5 D gravity model constrained by
seismic reflection and borehole data was constructed along a NE–SW trending profile. The
depth to the crust/mantle implies that the Jeffara basin is associated with crustal thinning …