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thickness of damage zone.
Podymova et al. [102, 103] measured the thickness of damage layer in the mono-crystalline silicon wafer with the laser optoacoustic method.
In addition, the thickness of damage zones along planar fault segments does not appear to grow indefinitely with displacement, as might be envisaged from some scaling laws.
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The design parameters are the amount of loss in wall thickness, extent of damage along tube height, and the damage angle around the circumference.
The criterion of the material damage nanocutting has a lot of statements, such as the thickness of the damage subsurface[3] and the variation of potential energy[2].
Open image in new window Fig. 15 Relation to throw and thickness of the damage zone Open image in new window Fig. 16 Fault combination and safe distance from the high-angle well to the fault zone.
Since A t is likely to be not controlled by the thickness of fault damage zone, the coseismic stress changes by the mainshock are suggested as one of the plausible factors for affecting A t. Nodal planes of the focal mechanisms oblique to the mainshock fault plane (Fig. 8) may reflect the contribution of stress changes.
The thickness of the brittle damage zone near the fault core is a few to several meters in the hanging wall but as large as 100 m in the footwall.
Thus, depending on sample thickness the lateral size of damage could only be determined from reflections measurements from both sides or from transmission measurements.
The thickness of the surface damaged layer is dependent on the treatment temperature.
The thickness of the surface damaged layer was estimated by spectroscopic ellipsometry.
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