Figure F5. The original total field (B₀) and susceptibility () logs for Hole 1095B and the remanent and induced borehole field anomalies derived from them. The background field value and the pipe effect are subtracted from the measured B₀ to leave B_f. B_fi is subtracted from B_f to leave B_fr, the anomaly caused by the sediment's remanent magnetization. The results from the two passes of the geological high-resolution magnetic tool (GHMT) were computed independently and are plotted alongside the core paleomagnetic results for the 20-mT AF demagnetization step.