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• W2100030246 abstract "The frozen flux approximation of Roberts & Scott is a constraint on the core field that can be used to aid interpretation of the very sparse datasets that palaeomagnetism and archaeomagnetism provide. It gives bounds on the size of the components of the magnetic field at a point, of the Gauss coefficients, and, if valid over such long time periods, limits the shape of the field during transitions between normal and reversed polarities. The maximum intensity at a point, consistent with the present flux, is 281 μT or 4 times the maximum field observed today. The present dipole is about 50 per cent of its upper bound. Polarity reversal is impossible if the transition field is purely axisymmetric. None of the measurements we consider violate the frozen flux approximation." @default.
• W2100030246 created "2016-06-24" @default.
• W2100030246 creator A5052962641 @default.
• W2100030246 creator A5088178438 @default.
• W2100030246 date "1983-06-01" @default.
• W2100030246 modified "2023-10-09" @default.
• W2100030246 title "Use of the frozen flux approximation in the interpretation of archaeomagnetic and palaeomagnetic data" @default.
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• W2100030246 doi "https://doi.org/10.1111/j.1365-246x.1983.tb03339.x" @default.
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