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Meanwhile, softer actuators generated less deformation on the deformable target compared to harder actuators.
It creates uplift offshore, but little deformation on land.
The deformation on both sides of the fault is asymmetric.
Moreover, GPS measures only the horizontal deformation (on the surface).
Fig. 4 Schematic illustration of inelastic deformation on Kyushu Island.
An example of static deformation on a complex configuration is depicted in Figure 8. Fig. 8 Static deformation on complex aircraft configuration.
We measured the deformation on specific zones in an objective way.
We observed strain-induced deformation on the spot of graphite G 002) at 1,300°C.
Using the data from ALOS-2, several groups present models of coseismic deformation on faults.
Uneven subsidence can cause deformation on the highway surface and the railway tracks [1, 2].
We clearly observed strain-induced deformation on the spot of graphite G 002).
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