Figure F22. Comparison of magnetic intensity (after AF demagnetization) and MST magnetic susceptibility. The marked high-intensity and high-susceptibility zones at the upper part of Hole 1173A occur in Subunits IA (turbidite successions) and IB (sedimentary transition zone from turbidites to hemipelagite). In contrast, the sediments below 140 mbsf show low values of magnetic intensity and susceptibility.