FINITE STRAIN ANALYSIS OF LIMESTONE/BASALTIC MAGMA INTERACTION AND FRACTURE: LOW ORDER MIXED TETRAHEDRON AND REMESHING

• Autor(a) principal: AREIAS, P.
• Data de Publicação: 2018
• Outros Autores: CARRILHO LOPES, J., DOS SANTOS, M.P., RABCZUK, T., REINOSO, J.
• Tipo de documento: Artigo
• Idioma: por
• Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
• Texto Completo: http://hdl.handle.net/10174/24490; https://doi.org/10.1016/j.euromechsol.2018.09.003
• topic: dike intrusion; computational fracture; limestone basaltic magma

In this investigation, we use a recent constitutive framework and remising technique for tetrahedra to analyse the pressure-driven crack propagation of limestone intruded by basaltic magma. Limestone is represented by an least-plastic capped Drucker-Prager model with an hypo elastic term in order to account for inelastic effects from plastic signature. Kinematic hardening is considered for limestone, whereas magma is modelled by means of a compressible Bingham fluid. Classical limit surfaces of the capped model are used to initiate the crack events in the limestone. Propagation is performed by a local remising technique with mesh smoothing for untracked elements. Arnold's MINI element is used to avoid locking in the quasi-incompressible case. Verification (for limestone) examples and a crack propagation example in 3D are performed. A mesh convergence study is performed, exhibiting very promising results.