General usage techniques of 2-D gradient geometrical analysis for gravity data of any geologic structure

Gradient space plots' rules are applied to noninterfering anomaly associate with isolated geologic sources in conditions that: (1) this method is used as an assistant analysis instrument (2) it is assumed that only a limit number of isolated geologic structures (classified in Butler catalogue) must be given as an interpretation target. In this paper, gradient method assumptions for geologic structure were ignored initially. common gradient methodology was used for observed gravity data analysis of without previous imagination of anomaly description and geologic structure. Acquisition lattice with topography are mentioned. Ability of gradient method in this manner (for geologic structure not suggested in Butler catalogue) is depth and their location along profile. Comparison of estimated depths by Euler deconvolution method with general usage of gradient one (discussed in this study) demonstrates accuracy and correctness. Some additional techniques in this work avoid limitations of easy and powerful gradient method announced by Butler; Geometrical method which offers the chance of following its visible steps by analyzer to check the progressing procedure during interpretation

Keywords:

general gradient method , geologic structure