Fig. 5From: Evolution of the geological structure and mechanical properties due to the collision of multiple basement topographic highs in a forearc accretionary wedge: insights from numerical simulationsThe stress state (mean stress, deviatoric stress, and differential of the horizontal to vertical stress) and porosity around the monitoring particles. a The reference model without BTHs (Fig. 2) and b the model for multiple BTH collisions (Fig. 3)Back to article page