Application of Werner Deconvolution Method in the Direct Interpretation of Residual Aeromagnetic Anomalies

The total field aeromagnetic contour map located between geographic latitude 11 0 00'N to 11 0 30'N and longitude 7 0 30'E to 8 0 00'E was acquired, digitized and residualized in order to assess the Werner deconvolution method in the interpretation of geophysical data. Three profiles were selected for the interpretation of residual aeromagnetic anomalies. The result obtained from the data of Zaria area using Werner deconvolution method was filtered and shows that the depth to magnetic source values vary from 0.1 to 2.6km below the ground surface indicating the shallow nature of the magnetic source, while the susceptibility vary from 6.7x10 -5 to 2.193 S.I unit approximately. The result obtained shows much correlation with some of the