Total field aeromagnetic anomalies over Ilorin (bounded by longitude 4030’- 5030’ E and latitude 80 - 8030’ N) have been interpreted using Fast Fourier Transform method in order to estimate the sedime
Total magnetic intensity (TMI) data measures variations in the intensity of the Earth's magnetic field caused by the contrasting content of rock-forming minerals in the Earth crust. Magnetic anomalies
