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A comment on depths of sources of anomalies in the Earth's gravity field
Authors:A K Goodacre
Institution:Gravity and Geodynamics Division, Earth Physics Branch, Department of Energy, Mines and Resources, Ottawa K1A OY3, Ontario, Canada
Abstract:Summary. One method to determine the depths of sources of anomalies in the Earth's gravity field is to plot log (2 n + 1) σ n ] versus n where σ n is the n th term in the amplitude spectrum of the Earth's gravitational potential. This procedure assumes that the amplitude spectrum of the anomalous density variations does not vary with n. Such an assumption may not apply to the Earth.
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