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5.6  ·  Microscopic Shear Sense Indicators in Mylonite  149









































                 Fig. 5.36. Truncated sillimanite fish in ultramylonite. In the matrix fine-grained ilmenite outlines an oblique foliation inclined to the mylonitic
                 foliation. The inclusion in the sillimanite is apatite. Dextral shear sense. Monte Mary, Italy. PPL. (Photograph courtesy Giorgio Pennacchioni)

                 porphyroclast lies between two large rigid objects, its
                 asymmetry may reflect the relative movement of these
                 two objects rather than the bulk shear sense in the shear
                 zone. Therefore, mantled clasts are most reliable as shear
                 sense indicators where they occur isolated in a fine-
                 grained mylonitic matrix, e.g. in ultramylonite.
                   Sigmoids have the same shape and orientation as
                 σ-type mantled clasts and, although their development
                 is not completely understood, their shape can be used to
                 determine shear sense in the same way (Fig. 5.20).
                   The geometry of porphyroclasts with pressure shad-
                 ows and fringes is formed in a different way as mantled
                 porphyroclasts, and both structures should not be con-
                 fused. Mantled clasts occur exclusively in mylonites, while
                 strain shadows can also be found in low strain rocks. Their
                 use as shear sense indicators is explained in Chap. 6.  Fig. 5.37. Schematic diagram showing the geometry of normal min-
                   All mineral fish are good shear sense indicators, ir-  eral fish and truncated fish
                 respective of their mechanisms of development. The
                 inclination of the long axis of fish with respect to the  can be used as a shear sense indicator as in the case of
                 foliation and a commonly developed monoclinic shape  mantled clasts. An exception are mica fish of group 6
                 symmetry, with one curved and one planar side, can  (Fig. 5.28), which are localised on shear bands, and
                 be used as shear sense indicators (Figs. 5.20, 5.28, 5.30,  truncated sillimanite fish (Fig. 5.37; Type 2 of Manckte-
                 5.31). If trains of small fragments trail away from the  low et al. 2002) which have a different geometry from
                 tips of the fish, these will show stair stepping which  other types.
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