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Study of structures associated with shear zones is a crucial aspect to understand the deformation mechanism associated with such zones. For the sake of brevity, research papers cannot show all possible variation in structures found in shear zones.
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A number of ‘new’ microscopic structures such as ‘flanking microstructures’, trapezoid-shaped mineral grains, reversal of ductile shear sense, micro-duplexes, V-pull aparts, and new minerals nucleating inside host minerals have recently been described in individual manuscripts.