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In rubbing and extrusion mechanism, the strain zone almost parallels to the cutting direction.
In rubbing and extruding mechanism, the strain zone almost parallels to the cutting direction.
In eastern Nepal the unconformity does not coincide with a discrete structural or metamorphic discontinuity and is not a discrete high strain zone.
In the rubbing mechanism, the strain happens at the surface of the workpiece material which is under the tool edge, and the shear strain zone also merges with the TDZ during the action of tool flank face.
The degree of local strain discontinuity along the strengthened girder is dependent upon the level of post-tensioning and an effective strain zone is found beyond which such a post-tensioning effect does not influence the girder concrete.
At depth, a high strain zone characterized by greenschist facies metamorphic rocks and a top-to-the-NW ductile shearing corresponds to a ductile décollement zone that accommodated the deformation of the Neoproterozoic to Early Triassic sedimentary series.
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Also, it was observed that coarser nanoparticles broke down high strain zones (HSZs) during tensile deformation.
These Cadomian blocks are separated by high strain zones containing the record of subduction-related processes.
In recognition of this, we introduce the term Himalayan Unconformity to distinguish it from high strain zones in the Himalayan Metamorphic Front.
Traditionally the high strain zones are interpreted as sutures between one or more postulated lithospheric microplates sandwiched between the two major plates.
Using a high-resolution optical digital image correlation, low and high strain zones in off-axis woven composite samples loaded in uniaxial tension are identified and the corresponding full-field strains are quantified.
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