ISSN:
1420-9136
Source:
Springer Online Journal Archives 1860-2000
Topics:
Geosciences
,
Physics
Notes:
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.
Type of Medium:
Electronic Resource
URL:
http://dx.doi.org/10.1007/BF01592947
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