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Open image in new window Fig. 6 A double cross-slipped segment may act as a Frank-Read source on a parallel slip plane.
The slip plane spacing was approximately 15 30 nm.
The slip plane position does not change the ΔCRS S
The model is based on the glide of a leading partial dislocation on a basal slip plane and double-cross-slip to the next-but-one slip plane.
Three groups of Cu bicrystals with their component grains sharing one common {111} slip plane were cyclically deformed.
Crystal lattice simulation identified potential slip plane within CRV crystals, where fractures are the most likely to occur.
Zeolite veins in volcaniclastic units form poorly-connected, spaced sets, parallel to the slip plane, hence sequence permeability remains low.
The crack growth along one slip plane was then followed by crack deflection or kinking.
The slip plane observed in tension is {202̄1̄}, which is different from {112̄1̄} observed in compression.
DFT finds the slip plane to be altered by Re alloying.
Stress concentration occurs at the places those are ±0.5 m from the slip plane.
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