Summary
Fourier transforms of theoretical magnetic anomalies of vertical and inclined dikes are computed. In all the cases it is shown that for a particular type of dike the amplitude spectra of horizontal and vertical components of the anomalous field remain exactly the same, whereas the phase spectra show a constant difference of π/2. The different parameters like depth to the top of the dike, width, susceptibility contrast and inclination can be calculated from the amplitude and phase spectra.
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Sengupta, S., Das, S.K. Interpretation of magnetic anomalies of dikes by fourier. PAGEOPH 113, 625–633 (1975). https://doi.org/10.1007/BF01592947
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DOI: https://doi.org/10.1007/BF01592947