Abstract:
Geologically, Dhermund area is located in the western foothills of Himalayas,
Potwar Basin, northern Pakistan. The primary reason for investigation is to understand
the structure of the area and hydrocarbon potential. Seismic interpretation of the area
reveals that area has an open structure. There is no major fault in the area but has some
minor faults. Geoseismic section is a part of seismic interpretation which describes the
lithology of the area laterally. There is no structural trap present in the area as the
Formations are exposed on the surface.
