The Normalized Full Gradient (NFG) was developed to determine anomalous bodies. In this research, NFG's ability to find the gravity anomaly model was studied. For this aim, we used synthetic data and studied the NFG recovered model. The recovered model compares with up-to-date inversion results. The weakness of the NFG is the 3D modeling limitation, only we can calculate the 2D response in practice. On the other hand, we have normalized responses that could not be able to describe the negative and positive parts of the anomaly. Despite the limitation, the results have shown the NFG has similar responses to the inversion results. But a unique advantage of NFG is, that it does not need the primary information for gravity data modeling.