Bouguer anomaly
On the question of the dependency of the Bouguer anomaly from a height
Dependence of the Bouguer anomaly on the average relief heights
3d euler deconvolution for the depth determination of the sources of the gravity field in the Ukrainian Carpathian
Main equation of the method of Euler deconvolution is considered. In contrast to the other works, the least squares method is used here to solve the equation. Depths of the geological objects of different shapes in the region of the Ukrainian Carpathians have been calculated.