Abstract
Gravity data integrated with geological data and mining well data are analysed to constrain the shape of the Triassic evaporitic body at Jebel El Mourra (N Tunisian Atlas) and the mechanism of its emplacement at the surface. The gravity data analysis included the construction of gravity anomaly maps, and synthetic and forward 2.5D gravity models. The complete Bouguer and residual gravity anomaly maps indicate a positive amplitude gravity anomaly over the Triassic evaporitic outcrops and prominent NE-SW-trending features associated with the boundary of the Triassic rocks and surrounded layers. A NW-SE-trending gravity model that crosses the Triassic evaporitic outcrop at Jebel El Mourra shows that the positive gravity anomaly can be explained by a deep-rooted salt diapir. Conventional models of salt dome formation suggest that they produce negative gravity anomalies, but this study shows that this model is not universal. The studied area is an example of a diapir expressed by positive gravity anomaly and synthetic gravity models support this result at different stages of salt piercing.