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Earth, Planets and Space
Fig. 5 | Earth, Planets and Space

Fig. 5

From: Paleomagnetic inclination variations during the last 200 kyr in the Okhotsk Sea and their relation to persistent non-axial-dipole field

Fig. 5

Inclination stack of the Okhotsk Sea and comparison with the western equatorial Pacific. a Individual and b stacked inclination records at the nine sites in the Okhotsk Sea during the last 200 kyr, c inclination stacks [blue Yamazaki and Ioka (1994), black Yamazaki et al. (2008), note that the average inclination of each core was set to zero for stacking] and a inclination record of Yamazaki and Oda (2002) (red) from the West Caroline Basin in the western equatorial Pacific, and d relative paleointensity stacks of Yamazaki et al. (2008) from the West Caroline Basin (blue) and the PISO-1500 paleointensity stack of Channell et al. (2009) (red). Light green bands indicate periods of shallower inclinations in the Okhotsk Sea and coeval steeper negative inclinations in the West Caroline Basin in the western equatorial Pacific

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