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Fig. 6 | Earth, Planets and Space

Fig. 6

From: Paleomagnetic direction and paleointensity variations during the Matuyama–Brunhes polarity transition from a marine succession in the Chiba composite section of the Boso Peninsula, central Japan

Fig. 6

Remanent magnetization and rock-magnetic properties of samples from the Yoro-River and Yoro-Tabuchi sections. From top to bottom, relative paleointensity, declination, inclination, maximum angular deviation (MAD) values, the S-ratios, the ratio of ARM susceptibility (k ARM) to magnetic susceptibility (k), and k (red) or k ARM (blue) are shown. Shading represents the polarity transition zone of the M–B boundary. All the properties were derived from the all (213) sample horizons except for the S-ratios which were from the selected 52 horizons (Additional file 1)

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