Gravity Method Data Reduction
Latitudinal correction, correcting for the Earth’s rotation
Elevation correction, correcting for large-scale $1/r^2$ dependency
Tidal correction, correcting for
Point masses and anomalies of spatially extended point masses
Video: Theory 3 of gravity measurements
In this video we go through the main data reduction steps required in order to isolate signals from the sub-surface.

Lecture slides Lecture Slides
Lecture notes Lecture Notes