Combined analytic signal and Euler method (AN-EUL) for depth estimation of gravity anomalies



The method expressed by Salem and Ravat. (2003) for depth estimation of magnetic sources is used on gravity anomalies for the first time.
The depth of some rectangular prisms as synthetic models are estimated through the method. The gravity effect of these models is also considered with a relatively high value of random noise. A field example is also included and the depth of the main anomaly has been estimated using this method.