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Magnetic surveys can be used to detect circular anomalies associated with kimberlites. However, not all kimberlites have the same magnetic character. Some show a positive expression, some negative, others no expression at all. Additional tools must be utilized in diamond exploration.
At Peddie, the MAG signature is very strong and sharp, indicating that we are dealing with fresh kimberlite rocks, of the hypabyssal facies.
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The IP signature of Peddie kimberlite exhibits a short time constant, characteristic of oxides (magnetite is associated with hypabysal facies).
For kimberlite at diatreme or crater facies, the IP response would show a long time constant, resulting from the effect of clay minerals formed by weathering.
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