Fig. 8.From: Paleointensity determination of Late Cretaceous basalts in northwest South Korea: implications for low and stable paleofield strength in the Late CretaceousVirtual (axial) dipole moments for the Late Cretaceous obtained from the PINT database. The solid horizontal line represents the strength of the present geomagnetic dipole moment. The geomagnetic polarity timescale based on Walker et al. (2012) is shown at the bottom of the figure.Back to article page