Figure F92. Schematic, true-scale cross section showing the relative locations of Holes 1270A, 1270B, and 1270D, their crystal-plastic intensity with depth, and the paleomagnetically reoriented dips of the fabrics in the holes. Rocks from Hole 1270B are assumed to record a reversed polarity, whereas rocks from Holes 1270C and 1270D are assumed to record normal polarity magnetization.

Figure F92. Schematic, true-scale cross section showing the relative locations of Holes 1270A, 1270B, and 1270D, their crystal-plastic intensity with depth, and the paleomagnetically reoriented dips of the fabrics in the holes. Rocks from Hole 1270B are assumed to record a reversed polarity, whereas rocks from Holes 1270C and 1270D are assumed to record normal polarity magnetization.