Locating the sources of potential fields in areal data using the singularity method

In an effort to develop and improve potential geophysical field interpretation we suggest that the singularity method should be extended toward areal data. This procedure enables mass and fast calculation of singularities in area and stable solutions. Studying the behavior of model fields and localization of singularities in the phase planes of vector fields permits the use of findings in interpreting geopotential fields. Model and real-life cases of this procedure as applied to tectonic dislocations and local geologic features are exemplified. We show that the proposed procedure significantly enhances the application of the singularity method to interprete geopotential fields.