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Folds are created in rock when they experience compressional stress. This is when the rock is being pushed inward from both sides. This is like if you put a spring between your hands and push them together. As you push, you're compressing the spring, and rock can be compressed in the same way over long periods of time.
The simplest hyperelastic material model is the Saint VenantâKirchhoff model which is just an extension of the linear elastic material model to the nonlinear regime. This model has the form. where is the second PiolaâKirchhoff stress and is the Lagrangian Green strain, and and are the Lame lamÃ©. constantsor isotropic hyperelastic materials, the Cauchy stress can be expressed in terms of the invariants of the left CauchyâGreen deformation tensor (or right CauchyâGreen deformation tensor).