Titlebook: Evolution of Geological Structures in Micro- to Macro-scales; S. Sengupta Book 1997 Springer Science+Business Media Dordrecht 1997 Deforma

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Overthrust shear in mountain buildingformation is needed. This is the result of an analysis of a comprehensive data set, comprising fold axial plane and cleavage orientations, and finite and incremental strain. There is a tendency for the strain to be concentrated at the nappe boundaries. The orientation of the finite strain stretching

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Practical analysis of general shear zones using the porphyroclast hyperbolic distribution method: An76), among others. In general shear zones, rigid ellipsoidal grains may rotate either forwards (with the sense of shear) or backwards (counter to the sense of shear) according to their axial ratios and orientations. Grains of a critical shape have their forward motion exactly countered by backward m