The 2-D modeling of gravity and magnetic datasets helped us to clarify the geological structure of the study area.
The depths to the basement rocks generally increase from the SE (3 km) to the NW (>8 km).
The 3-D magnetic inversion shows a magnetized basement rocks at depths of 3 km in the SE and deeper than 10 km in the NW.
The main structural trending of the detected subsurface structures is striking NE direction.