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The document discusses the classification of deformation in structural geology, distinguishing between Pure Shear and Simple Shear, with Pure Shear being irrotational and maintaining symmetry, while Simple Shear involves rotation of material lines. It also defines faults, fault zones, and shear zones, highlighting their characteristics and differences, particularly in relation to brittle and ductile deformation. Additionally, the document emphasizes the importance of understanding these concepts for analyzi
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