Figure F44. Polarity stratigraphy from the GHMT tool string: susceptibility (RMGS), magnetic field anomaly resulting from the remanence (generated by subtracting from the total field measurement [MAGB] the Earth's field, the field produced by the BHA, and the field caused by the sediment's induced magnetization), inferred polarity (normal polarity corresponds to negative remanence anomaly), the magnetic inclination from core, and the polarity stratigraphy of Cande and Kent (1995). Age assignments, except those from below 480 mbsf, are those proposed in "Paleomagnetism," in "Site 1095". Log depths have been reduced by 5 m in this figure to aid comparison with core depths.