Figure F13. Split-core (20 mT) inclinations from Holes 1095A, 1095B, and 1095D plotted in the (A) mbsf and (B) mcd depth scales. Coeval reversal boundaries and other variations in the inclinations are artificially offset by inaccuracies in the mbsf depth scale, which are overcome by use of the mcd scale. For the reversal boundaries, o = onset and t = termination.

Figure F13. Split-core (20 mT) inclinations from Holes 1095A, 1095B, and 1095D plotted in the (A) mbsf and (B) mcd depth scales. Coeval reversal boundaries and other variations in the inclinations are artificially offset by inaccuracies in the mbsf depth scale, which are overcome by use of the mcd scale. For the reversal boundaries, o = onset and t = termination.