Abstract
A simple method to interpret gravity gradients over a thin infinite dipping sheet is discussed. The Hilbert transform is used to compute the vertical gradient from the horizontal gradient of the gravity field. The method is illustrated with a theoretical example.
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Sundararajan N, Mohan N L and Seshagiri Rao S V 1983 Interpretation of gravity anomalies due to some two-dimensional structures: A Hilbert transform technique;Proc. Indian Acad. Sci. (Earth Planet. Sci.) 92 179–188
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Sundararajan, N., Kumar, I.A. & Mohan, N.L. Analysis of gravity gradients over a thin infinite sheet. Proc. Indian Acad. Sci. (Earth Planet Sci.) 96, 11–14 (1987). https://doi.org/10.1007/BF02842633
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DOI: https://doi.org/10.1007/BF02842633