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ID: past-exam-of-the-year-2-of-the-earth-sciences-geology-course-of-the-university-of-oxford/2025/paper-3/2/d

The sketches assume the car can be approximated by a compact magnetic dipole whose induced magnetic moment is parallel to the local geomagnetic field. The host contributes negligible local contrast. Real steel also has remanent magnetization and shape-dependent magnetization, so the car's actual profile need not follow this idealization. A proton-precession magnetometer observes
when . This scalar total-field magnetic anomaly must not be confused with a fixed vertical field component. For induced , the magnetic dipole field gives
Reversing both the inducing field and induced moment leaves this total-field magnetic anomaly unchanged, exactly for the magnitude definition as well as in the weak-anomaly approximation.[ref]
Figure 1.
Induced magnetic dipole profiles at the magnetic poles and equator
. Original ideal profiles in arbitrary units for a dipole at unit burial depth. The polar curves coincide. At the equator, a north–south traverse has a central low and positive shoulders, whereas an east–west traverse has a central low without positive shoulders. Car shape and remanence are excluded. Details.

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