The paper describes a method for measuring the geomagnetic field vector using a scalar magnetometer and a three-axis flux-gate magnetometer rotating about two defined axes. The proposed method is an alternative to DI -flux measurement ( D : declination; I : inclination), which is based on a theodolite-borne one-component flux-gate magnetometer. The basic idea is that the calibration of the magnetometer and the determination of the field in the direction of the rotation axis can be carried out using the same procedure. Requirements concerning the three-component magnetometer and the mechanics will be discussed. The method presented will be compared with the DI -flux procedure.
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Auster et al. (2003) studied this question.
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