nounIngeology, the attenuation or actual rupture of a mass of rock by a compressive strain, especially by one applied transversely to the bedding or foliation. It results in dragging out the component minerals into thin bands and, it may be, in rupturing their former continuity. ...
Define Shear rheology. Shear rheology synonyms, Shear rheology pronunciation, Shear rheology translation, English dictionary definition of Shear rheology. n. The study of the deformation and flow of matter. rhe′o·log′i·cal adj. rhe′o·log′i·cal·l
Soil shear strength refers to the resistance of soil to deformation under shear stress, which is a combination of cohesion between particles and frictional resistance to sliding. It can be influenced by factors such as soil mineralogy, water content, and the presence of plant roots. ...
The definition ofshear layerthickness adopted in the present work is the normalised maximum slope of the mean longitudinalvelocity profileat anydownstream section. Thus, in the vertical direction, normal to the wall, the thickness is defined as; ...
1d for axis definition). By making this assumption, we neglect other components of the strain tensor and uncorrelated motion of the beads. If the beads move accordingly to this shear field, the decorrelation can then be related to the local shear as (see Supplementary Methods 2 and ...
τxyis the shear stress γxyis the shear strain A is the area over which the force acts Δx is the transverse displacement l is the initial length Shear strain is Δx/l = tan θ or sometimes = θ, where θ is the angle formed by the deformation produced by the applied force. ...
The percentage of the observed disparity with respect to the average reference model albeit is small, becomes significant at certain depths and is associated with the existence of strong vertical discontinuities, thus introducing an uncertainty on the interface definition between the main formations. On...
We acquired a ~9-km long, high-resolution reflection seismic profile in the Centennial Valley, Montana, to better understand the kinematics of basin bounding faults and their role in accommodating proposed right-lateral shear in the Northern Basin and Ra
To extend this definition into 2–D, we define a deformation field where pure–shear occurs within a fixed half-width, W1/2, axial zone in the lithosphere. A wide zone of pure–shear leads to slow thinning of the lithosphere, whereas a narrow zone of pure–shear results in very fast ...
. For better definition of the upper age limit of mineralization and to investigate the potential relationship between emplacement of the felsic porphyry dikes and formation of the mineralization, a polished mount was also prepared from the zircon grains which had been previously separated and analysed...