Abstract
Poles of deformation lamellae in quartz in a folded quartz-mica-schist show two maxima in an incomplete girdle normal to the fold axis and are symmetrically situated with reference to late tension cracks in garnet. The deformation lamellae have thus formed late in the movement history of the rock, coinciding with the conjugate shear planes developed because of non-rotational strain after the megascopic fold with monoclinic symmetry was formed.
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