GRAVITY ANALYSIS OF THE KEF BASIN AND SURROUNDING REGIONS, NORTHEAST TUNISIA

The geology of the northern Atlas of Tunisia is characterized by NE-trending structures taking place as response to the NW compressive stress from Eocene to early Quaternary period. These structures were cutting by trough structures as evidenced by a series of grabens. These grabens were oriented orthogonally to the Atlasic deformation direction and were probably associated to E-W fault systems or to conjugated strike slip fault systems.

In order to characterize the subsurface structural makeup of this region and of the Kef basin in particular, we undertook a detailed gravity data analysis using publically available Bouguer gravity anomaly data and newly acquired 1 kilometer spaced data obtained by the National Office of Mines. The Bouguer gravity values show a gradual increase between almost -12 and 2 mGals within the Kef basin. The anomalies are represented by positive and negative responses separated by high gravity gradient interpreted as tectonic contacts shown in the derivatives gravity maps. Euler deconvolution solutions with SI=0 reveals the dominance of two principal directions of faults NE-SW and NW-SE, and a 3D inverse model indicates that the Kef basin contains at least 6-7 km of Cenozoic and Mesozoic sediments and the basin is bounded by set of faults oriented NE-SW, NW-SE and NS. A positive density region at 7.5 km situated northeast the basin is interpreted as NW-trending fault.