Enhancement of the total horizontal gradient of magnetic anomalies using tilt derivatives: Part II — Application to real data

We propose a new magnetic anomaly enhancement method based on the tilt derivative of the total horizontal gradient. We illustrate the effectiveness of the method in structural mapping by applying it to reduced-to-the-pole aeromagnetic data and comparing the results to those obtained from other methods reported in literature. The anomalies generated by our method show good correlation with geological structures and Euler deconvolution results.