FIG. G-7. Corrections to gravity data and the names of the resulting anomalies. The terrain correction is not always applied to free-air data. Eötvös corrections also have to be made if the meter was moving during the measurement.
↑Sheriff, Robert (1989). Geophysical methods. Englewood Cliffs, N.J: Prentice Hall. p. 60. ISBN978-0-13-352568-7.
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