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n] coefficients control the variation of the period as function of the geomagnetic latitude.
5-10 ka, we calculate geomagnetic latitude from geographic latitude and the palaeopole positions of Ohno & Hamano (1992) by subtracting the palaeocolatitude from 90[degrees] (Eq.
These variables are the geographical longitude, the geomagnetic latitude, the horizontal component and the magnetic inclination.