Fig. 3From: Wavelet-based verification of a relative paleointensity record from the North PacificDown-core variations in a natural remanent magnetization (NRM) intensity at each AF demagnetization step, b declination and c inclination of characteristic remanent magnetization (ChRM) directions, and d maximum angular deviation (MAD). The reference magnetic polarity is indicated on the right side of the figureBack to article page