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Many faults were observed in the sedimentary unit on the reflection profile (Figs. 2 and 8).
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.
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.
The strike-slip faults along with the thrust faults that were also determined by the fault plane solutions of the aftershocks, and tensional cracks possibly related to the normal or left-lateral strike-slip faults, were observed especially in the overlapping northern block due to the NW-SE compression among the micro-scaled continental plates.
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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.
Twinning faults are observed in Cu substrate both during the indentation and retraction processes.
Furthermore, a larger fraction of stacking faults was observed in the coarse-grained material.
Landward of first significant gullies, a distinct network of margin parallel, small scale arcuate faults is observed.
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.
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