
Figure F11. Comparison of U-channel (PCA) and split-core (20 mT) inclinations from the upper part of Hole 1095A illustrating the lack of agreement that occurs within some intervals of the core. The inset shows the details of the inclination variations in the transition zone of the Brunhes/Matuyama reversal. The reversal boundary (dashed line in the inset), as given in Table T1
is placed in the middle of this zone.

