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Effect of overlapping of stacking faults on the fault width was discussed.
The stacking fault width and nanoindentation hardness measured in the CAC simulations agrees well with existing experimental data.
Both the decreasing stacking fault width and the plateau of velocities in the first transonic regime, indicating the existence of a radiation-free state, are in agreement with theoretical predictions.
Namely, the stacking fault width is found to depend non-monotonically on the percentage of nitrogen with a maximum critical shear stress at 1 wt.% (4 at.%) N, in agreement with experiment, and also suggests a non-monotonic critical shear stress dependence on nitrogen content.
b Model 5 (Model 2 × 2.0 fault width factor for an offshore fault).
A double-couple point source is located at —58 km along the fault width.
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First-principles density functional theory can be used to calculate the GSFE curves to link continuum-scale dislocation properties and stacking fault widths, on pyramidal slip systems.
The fault models have different fault widths of 25 km, 50 km, and 100 km, respectively.
Fault widths were estimated using seismicity and coastal deformation patterns as interpreted from uplifted coral terraces in west Luzon [e.g., (Ramos and Tsutsumi 2010)].
In addition, we note in Fig. 4 that the shapes of the spectra cover the fault zone width, indicating the zone width size as well as fracturing in the fault line boundary of the measured fault segment.
This observation affects the various faulting parameters which include fault length, width, depth and average slip.
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