“…The main thrust of this study is to con firm the exis tence and loca tion of the Ifew ara shear zone (ISZ) using inte grated geo phys i cal meth ods involv ing dipole-dipole resis tiv ity (imag ing tech nique), and mag netic methods. Also, to deter mine the struc tural attri butes like dip, strike and width and depth extent of the shear zone.The use of inte gra tion of geo phys i cal meth ods such as elec tri cal resis tiv ity, elec tro mag netic and mag netic tech niques as a geo log ical and litho struc tur al map ping tool have been con firmed by several authors (e.g., Kowa lik and Glenn, 1987;Barker et al, 1992). A resis tiv ity sur vey is com monly used to map frac ture zones in hard rock ter rains (e.g., Car ru thers and Smith, 1992;Ako et al, 1978) because high resis tiv ity con trasts usu ally occur between solid rocks and sat u rated frac ture zones (Adepe lu mi et al, 2006).…”