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In this model, thin deformation bands formed as porosity was reduced during quartz diagenesis.
We attribute the transition from thick deformation bands to thin deformation bands to pore-space reduction caused by syn-faulting quartz dissolution and precipitation that changed the mechanical properties of the rock.
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Field data show that Segment A developed from an early stage of (thick) deformation band formation and that distinctively thinner deformation bands and fractures were subsequently added to its damage zone at a later stage.
In addition, analysis of experimental data demonstrated bead penetration, clamping force and material flow stress as the dominant factors on drawbead restraint force and blank thinning deformation for both materials.
The finite element method is a powerful tool to predict material thinning deformations before prototypes are made.
Exceptions might occur when grains become thin during deformation, which is also accompanied by a decrease in the dihedral angle θ or at higher homologous deformation temperatures.
Analytical forms for the thin film deformation can be obtained, and the stress in the film can be easily determined using the proposed model through the constitutive law.
Composition dependences of the glass transition temperature (Tg), the molecular weight between entanglements (Me) and the thin film deformation behaviour have been studied in two series of methyl methacrylate-based random copolymers.
The results from the two flow fields differ in the driving force behind film thinning: shear deformation of the major component drives film thinning under steady, simple-shear flow; interfacial-tension drives it under quiescent conditions.
Motion along these faults allows a piece of crust to become longer and thinner as deformation progresses.
Based on these results, we propose a model of thin-film deformation based on dislocation glide and constrained diffusional creep.
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