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.
|Number of pages
|Proceedings of the Indian Academy of Sciences - Earth and Planetary Sciences
|Published - Mar 1987
- Hilbert transform
ASJC Scopus subject areas
- Earth and Planetary Sciences (miscellaneous)