Sentence examples for parallel slip from inspiring English sources
Open image in new window Fig. 6 A double cross-slipped segment may act as a Frank-Read source on a parallel slip plane.
On two coupled parallel slip bands, some oppositely signed dislocations, which can be regarded as equivalent prismatic dislocation loops, glide toward the void/crack-tip surface and thus drive the void growth and the crack tip further blunting.
In contrast, highly irradiated specimens exhibit pronounced shear localization on parallel slip planes, which we ascribe to the onset of defect free channels normally seen in bulk irradiated materials.
For the particular case of a population of parallel screw dislocations of the same sign moving on parallel slip planes the solution for the pair distribution function is found analytically.
For the surface nanoindentation, the slip systems can be activated under a smaller external load and two parallel slip planes yield around the indenter tip.
Figure 3 (left) depicts the top view of a situation some time after near-screw segments of two loops moving on parallel slip planes have merged by cross slip.
The fault is comprised of a core bounded by two major, non-parallel slip surfaces.
The evolution of the fault from a buried structure with associated fault-propagation folding, to a surface-breaking structure with associated surface faulting, has led to enhanced bedding-parallel slip at lower levels that is absent at higher levels.
The corrugated surfaces extend from near the trench to several kilometres down-dip, exhibit high reflection amplitudes (consistent with high fluid content/pressure) and trend 11 18° oblique to subduction, suggesting 15 to 25 mm yr−1 of trench-parallel slip partitioning across the plate boundary.
Compared to a case where the slip bands are oriented parallel to the surface, a less pronounced decrease of the hardness with increasing indentation depth is observed for the non-parallel slip band orientation.
In its initial form, our extension amounted to assuming all these facets oriented either parallel to slip planes or normal to slip directions, what is proved convenient for large enough grains.
