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. 2002 Feb 19;99(Suppl 1):2546–2553. doi: 10.1073/pnas.022582599

Fig 7.

Fig 7.

Paleointensity of the intensity of Earth's magnetic field as inferred from sediment cores for the past 4 Ma from Meynadier et al. (23). The data are expressed as the virtual axial dipole moment (VADM) with reversed polarity data given by negative values.