Palaeomagnetists' basic assumption that Earth's magnetic field is a GAD, that is, a geocentric axial dipole, has been challenged by anomalous magnetic data from ancient Canadian basalts. At a closer look, fast continental drift could explain this anomaly.
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Meert, J. In GAD we trust. Nature Geosci 2, 673–674 (2009). https://doi.org/10.1038/ngeo635
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DOI: https://doi.org/10.1038/ngeo635
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The (Paleo)Geography of Evolution: Making Sense of Changing Biology and Changing Continents
Evolution: Education and Outreach (2012)