Abstract:
Satellite measurements provide Tempo-Spatial variations of the Earth's magnetism with a uniform coverage. These data allow us to obtain important information about crustal magnetic anomaly and its relationship with tectonic plates. In this research, we use the magnetic data received from Champ satellite. The MF7 model was prepared using Champ satellite magnetic data. In the separation of regional and residual anomalies, the Upward Continuation Filter has been used. By comparing the Upward Continuation Filter maps, it can be concluded that the source of the anomaly field is relatively deep.

Keywords: magnetic data, anomaly, Geophysical filter, Red Sea, upward continuation.