Fig. 5From: Wavelet-based verification of a relative paleointensity record from the North PacificDown-core variations in rock magnetic parameters. a S-ratio (S300), b magnetic susceptibility (χ), c susceptibility of anhysteretic remanent magnetization (χARM), d isothermal remanent magnetization acquired in a DC field of 1 T (IRM1T), and e grain-size parameters (χARM/χ and χARM/IRM1T). Selected depths for the hysteresis measurements are marked as open diamonds on the right of the plotBack to article page