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Progress in Earth and Planetary Science
Fig. 3 | Progress in Earth and Planetary Science

Fig. 3

From: 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 simulations

Fig. 3

Simulation results for multiple BTH collisions: geological structure (left), horizontal compressional stress (middle), and porosity (right). The geological structures are overlain on the horizontal stress and porosity as a translucent layer. Thick red lines in the left panels show the most active fault at that time. Thick blue lines in the left panels are the previously active faults. The green symbols on the geological structures (left) mark the locations of monitoring particles, which are monitoring points for the stress state and porosity (Fig. 5). The red arrows indicate the locations of the BTHs

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