Fig. 3From: Paleomagnetic inclination variations during the last 200 kyr in the Okhotsk Sea and their relation to persistent non-axial-dipole fieldRelative paleointensity and inclination of the three composite core sites. Relative paleointensity (upper) and inclination (lower) records of individual sites are superimposed. Paleointensity records are after Yamazaki et al. (2013). Blue Site GC1 + PC7, green Site GC8 + PC6, red Site GC9 and PC5Back to article page