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Furthermore, a larger fraction of stacking faults was observed in the coarse-grained material.
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In this study, active faults as well as many subsurface faults are observed at the surface.
Both three-layer twinning faults and stacking faults are observed in the Cu substrate.
The sediments in this trench are laterally continuous, and no faults are observed.
Many faults were observed in the sedimentary unit on the reflection profile (Figs. 2 and 8).
Twinning faults are observed in Cu substrate both during the indentation and retraction processes.
Landward of first significant gullies, a distinct network of margin parallel, small scale arcuate faults is observed.
Six other fracture zones (potentially faults) were observed to affect the Muschelkalk and the Buntsandstein units in GPK-1, and the Keuper, Muschelkalk and Buntsandstein in GPK-2.
Dense twin faults are observed perpendicular to the nanowire growth direction due to the fluctuation of In atoms in the droplet originating from the surface diffusion effect.
In our simulation, two three-layer two three-layer are observed beneatwinningp at the maximum indentation depth as seen in faultsd.
Many faults were observed in the sedimentary unit on the seismic reflection profile, whereas possible lower segments of the faults were imaged as high-attenuation stripes in the oceanic crust on the seismic attenuation profile.
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