@article{b921982e70f54b65b5ba6d86e1d34134,
title = "Localized folding of thick layers",
abstract = "We describe the localized folding of thick layers embedded in a viscoelastic framework. Higher-order partial differential equations such as the Swift-Hohenberg equation are standard for modelling the folding process. Using a high-order shear theory, we modify the Swift-Hohenberg equation to describe the buckling of thick layers and consider the folded layer's viscoelastic behavior. The use of thick layers enables us to consider shear strains parallel to the layers during folding. Our model naturally captures the softening-stiffening behavior by including a non-linear viscoelastic description using a Winkler-type foundation. Next, we study the linear stability behavior of the system and derive the dispersion relations. Finally, we simulate this new model using a robust custom-built isogeometric analysis solver, which allows us to describe thick folded layers with localized folding. The numerical results show that the folding of an elastic layer produces periodic patterns while a viscoelastic layer deflects locally. When the horizontal forces are unequal, the periodic folds initiate in the direction of the smaller force and the localized deformations occur parallel to the larger force. Later, the nonlocal deformation occurs in the direction of a smaller force. Domes and basins or more linear ridges and valleys are formed according to the relative magnitudes of the applied forces. Domes and basins are the results of equal horizontal applied forces, and non-equal forces result in ridges and valleys.",
keywords = "Analysis, Dispersion, Folding, Isogeometric analysis, Viscoelasticity",
author = "Pouria Behnoudfar and Hobbs, {Bruce E.} and Alison Ord and Luis Espath and Calo, {Victor M.}",
note = "Funding Information: This publication was made possible in part by the Professorial Chair in Computational Geoscience at Curtin University and the Deep Earth Imaging Enterprise Future Science Platforms of the Commonwealth Scientific Industrial Research Organisation, CSIRO, of Australia . This project has received funding from the European Union's Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie grant agreement No 777778 (MATHROCKS). The Curtin Corrosion Centre kindly provides ongoing support. Funding Information: The authors declare the following financial interests/personal relationships which may be considered as potential competing interests: Victor Calo reports financial support was provided by European Union{\textquoteright}s Horizon 2020 research . Victor Calo reports financial support was provided by Curtin Corrosion Centre . Funding Information: The authors declare the following financial interests/personal relationships which may be considered as potential competing interests: Victor Calo reports financial support was provided by European Union's Horizon 2020 research. Victor Calo reports financial support was provided by Curtin Corrosion Centre.This publication was made possible in part by the Professorial Chair in Computational Geoscience at Curtin University and the Deep Earth Imaging Enterprise Future Science Platforms of the Commonwealth Scientific Industrial Research Organisation, CSIRO, of Australia. This project has received funding from the European Union's Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie grant agreement No 777778 (MATHROCKS). The Curtin Corrosion Centre kindly provides ongoing support. Publisher Copyright: {\textcopyright} 2022",
year = "2022",
month = aug,
doi = "10.1016/j.jsg.2022.104669",
language = "English",
volume = "161",
journal = "Journal of Structural Geology",
issn = "0191-8141",
publisher = "Elsevier",
}