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 building shows again a swing to the west from the normal to the inverted limb directions, and rotates more rapidly than the finite strain fabric..A model consisting of overthrust shear zones is proposed. The shear zones occur in a top-downwards sequence analogous to thrust faults. Each shear zone starts bro

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Practical analysis of general shear zones using the porphyroclast hyperbolic distribution method: Anvious assumptions of predominantly simple shear strain with .>1000 throughout nappe emplacement history. Changes in orientation of mafic dikes and deformed cross-bedded sandstones across the shear zone boundary allow us to use the general shear equation . = cot (θ ’) — ..cot(θ), where 7 is the shear

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Development of compressional and extensional structures during progressive ductile shearing, Main Ce have developed during the same progressive ductile shear deformation and their development in a particular outcrop depends merely on the orientation of the layers with respect to the strain ellipsoid of the instantaneous flow field. Extensional structures in the Himalaya, as in other orogenic belts

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Deformed lineation in ductile shear zones: a case study from the Proterozoic fold belt of Singhbhum,sity of deformation. The patterns have been theoretically deduced by applying simple shear deformation to gentle initial flexural perturbations. It has been demonstrated that at the initial stages of progressively increasing simple shear the deformed lineation is of Type 1 (l. ^ f. acute angle openi

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Epitope Mapping by Antibody Competition,o describe the accumulation of displacement on faults, with recent models emphasizing the importance of fault interaction and other mechanical effects in causing variations in the displacement characteristics of faults. Faults have been shown to display power-law scaling relationships for displaceme

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Gianluigi Lichinchi,Tariq M. Ranaelf, lithotectonic stratigraphy of the sedimentary package, and deformation conditions (determined mainly by variations in the geothermal gradient). The differences in structural geometry and tectonic evolution between adjoining segments of the FTB result from broad variations in original taper, lit