Figure F37. Geometry of structures identified at Site 1114 from core observations and FMS images. A. Schematic structural log of Hole 1114A. Bedding dip attitudes along the uppermost part of the log (between 0 and 100 mbsf) are deduced from core measurements and seismic reflection. S = south; N = north. B. Map view of the bedding and fault patterns at shallow level (~100-120 mbsf). Only two examples of northeast-dipping faults are documented. C. Map view of the bedding and fault patterns at greater depth (~180-220 mbsf). F = trace of faults; B = strike of bedding. The mutual angular relationships between the different types of structures are correct, but their location is only indicative. Note that at shallow level the dip of the fault decreases, whereas both faults and beds have suffered an anticlockwise rotation of ~20º-30º with respect to the deeper structures.