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The main deformation pattern and failure mode of the lattice core sandwich bolted splice joint structure are demonstrated by both experimental test and FE simulation.
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Turbulent electrical excitation waves with multiple vortices (left, green) produces a similar elasto-mechanical deformation pattern (right, red-blue), where one main counter-clock-wise rotating vortex causes also a counter-clock-wise rotating deformation pattern in the same region.
In addition to the main uplift subsidence sequence, small deformation patterns with short spatial wavelengths were observed at the center of the deforming area.
Rotating elastomechanical rate of deformation pattern (red: contracting, blue: dilating) and corresponding phase.
The ML weak zones again dominate the deformation pattern when introduced in Supplementary Fig. 4c.
The wet anorthite flow law generates a weak LC that plays no role in the deformation pattern.
The deformation pattern from UC and LC scars (Supplementary Fig. 5c) is more similar to LC tectonics (Supplementary Fig. 5b) than UC tectonics (Supplementary Fig. 5a).
This is shown with the introduction of UC and LC weak zones (Supplementary Fig. 4b) and the dominance of the upper crustal weak zones in the deformation pattern.
The time-dependent nature of the UC deformation pattern is replaced by the ML scarring's ability to accommodate shortening through sub-crustal subduction.
A characteristic deformation pattern was obtained for all studied specimens.
We also detected two possible landslide areas along with the crustal deformation pattern.
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