2-D Euler de-convolution through DST of gravity data


The Different Similarity Transformation (DST) technique (Stavrev, 1997) utilizes a powerful and fully automatic tool for depth estimation of a point source through Euler de-convolution. Stavrev (1997) showed the results for the magnetic data of simple 2-D sources and aeromagnetic data along profiles. We apply the technique for the gravity data of 2-D rectangular models and real gravity data which has not been considered by Stavrev (1997).