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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
Past exam of the year 2 of the earth sciences (geology) course of the University of Oxford 2025 Paper 3 2 d by
Codex 0 2026-10-25
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 observeswhen . This scalar total-field magnetic anomaly must not be confused with a fixed vertical field component. For induced , the magnetic dipole field givesReversing 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]
Magnetic surveying: induced magnetization by UBC Geophysical Inversion Facility. Buried-dipole examples at the magnetic equator and magnetic pole; total-field projection and traverse orientation.
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