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The quantitative interpretation of magnetic anomalies aims at finding out the location, depth, dip, size, and susceptibility contrast of causative geological sources. In this paper an easy method of interpreting magnetic anomalies over simple geometric shapes of dyke, sheet and vertical step has been proposed by using the easily recognisable characteristic positions on the magnetic anomaly profiles. The method does not require prior knowledge of origin and datum. For determining the source parameters, mathematical expressions and graphical procedure are given.
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