The calculated anomaly of gravity includes effects – combinations of structures that have the different density and depth - of study area and beyond it. In this paper, a method for the separation of regional and residual fields is used, is the finite element method. This method has been used in the interpretation of potential field and can be easily resolved complex issues in the last few decades. The detected regional gravity anomaly is based on the interpolation functions of the elements that used in the finite element analysis. The first stage of FEM is selection of element and then the decision of boundary conditions. In this step, the solution space is divided into elements. After designation of the geometric structure of solution space, the most suitable elements must be selected for this structure. The compatibility between the geometry and the elements to achieve the best possible solution is important. Regional gravity will be approximated by weighted set from finite gravity values of eight stations according to eight nodes of one element that has similar second parameter which is located in the map The calculation is performed via interpolation functions, which act as weighting factors, in a reference space which has no dimension. In this study, the FEM method was used for gravity data of minoo salt dome, for calculating regional and residual anomaly. In conclusion, the results were obtained via FEM method, which is more accurate than other methods.