Figure F86. Variation in the dip of different categories of crystal-plastic foliation with depth. A. Mylonitic foliations (fabric intensity 4). B. Retrograde (mainly amphibolite to transitional greenschist grade) and semi-brittle shear zones. C. Shear zones with normal and reverse sense of shear in the core reference frame. The location of major faults (dashed lines) and a major reverse shear zone (solid line; see Fig. F85) are shown in all three plots.