Fig. 5From: Geomagnetic relative paleointensity and direction during the last 40,000 years obtained from a sediment core in the Nankai TroughMaximum angular deviation (MAD), declination, inclination, and relative paleointensity (from left to right) obtained from Core PC04. Blue and red diamonds along the age axis indicate age-control points based on 14C dating and volcanic ashes, respectively. Black triangles show the locations of core-section boundaries. Error bars in declination and inclination are based on MAD values, and those in relative paleointensity are from the uncertainties of the best-fitting slopes in NRM-ARM demagnetization diagrams (Kono and Tanaka 1984)Back to article page