4.3 Article

Elastoplastic Deformations of Layered Structures

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Summary: Kinking is a common deformation mechanism in layered systems, from nanometer scale in layered crystalline solids to kilometer scale in geological formations. Through multiscale experiments and atomistic simulations, the origins of kinking in the former have been demonstrated. The unique mechanical properties of layered crystalline solids heavily rely on their ability to deform by kinking, which in turn affects the compressive strength of natural and engineered layered systems.

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