Werner Deconvolution Technique for the Interpretation of Residual Aeromagnetic Anomalies of Igbeti Schist Belt; Implication for Marble Exploration

DOI:10.17014/ijog.9.2.209-217 Determination of the straight down range geologic formation between geographic latitude 8.30 0 N to 9 and longitude 3.30 E 4.30 Igbeti schist belt became a thing interest due on-going exploration in region. Aeromagnetic field intensity anomaly data bound were then acquired, separated off regional corresponding residual map obtained was later used applying Werner deconvolution method filtering tool. Three magnetic profiles selected labelled for interpretation on anomalies. The result shows that depth source has maximum value 1,000 m toward subsurface all selected, indicating shallow nature area. Based structural index shown, it further reveals solutions contact dyke which indicates there are boundaries separate rocks from one another presence formation. implication identical signature is marble deposit relative uniform extending great