Results 251 to 260 of about 442,027 (272)
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1991
A fundamental message of this work is the advantage gained from the separation of volumetric and deviatoric phenomena in the study of the physical and mechanical behavior of soils. With respect to the treatment of the volumetric phenomenon, consolidation, there is almost no discrepancy between this and the tri axial consolidation tests as they are in ...
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A fundamental message of this work is the advantage gained from the separation of volumetric and deviatoric phenomena in the study of the physical and mechanical behavior of soils. With respect to the treatment of the volumetric phenomenon, consolidation, there is almost no discrepancy between this and the tri axial consolidation tests as they are in ...
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Shear strain analysis and periodicity within shear gradients of metagranite shear zones
Journal of Structural Geology, 1995Abstract The distribution of natural ductile strain is studied by mapping continuous shear strain gradients across shear zones with widths of the order of tens of centimetres. The shear zones are derived from granites and the most ductile mineral (quartz) accommodates most of the rock deformation.
Gérard Dutruge +3 more
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Circular plates with shearing strain
Computers & Structures, 1990Abstract The shearing strain of plates is studied. The space position of the normal, which before deformation is perpendicular to the middle surface of plates can, after deformation, be fixed with the help of the rotations ψr(r, φ) and ψφ(r, φ) about the axes →er and →eφ.
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Shearing Strained Elastic Elements
2011Under the name of shearing strained elastic elements one can identify all the elastic elements where strain gauges are located at ± ( 45° angles on the load application direction. There are bidirectional rosettes specially marked for these angles. Two layouts are presented in Figures 26.1a (“cross” type) and 26.1b (“square”). Within these shear-bridges
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Strain within ductile shear zones
Tectonophysics, 1976Abstract The intensity of strain has been measured from the change in shape of clusters of mafic and felsic minerals within a ductile shear zone of short finite length from Botswana and a much longer planar shear zone from North Uist, Scotland. The strain measurements from North Uist have been supported by measurements of the anisotropy of magnetic ...
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Shear band formulations in finite strain elastoplasticity
International Journal of Solids and Structures, 1994zbMATH Open Web Interface contents unavailable due to conflicting licenses.
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