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Formation and evolution of a population of strike-slip faults in a multiscale cellular automaton model

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Academic year: 2021

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Figure 1. (a) The two states of fracturing used in the model: an active state represents an actively slipping fault segment; a stable state represents an ‘intact’
Fig. 3 shows the most frequent geometric patterns of neighbouring active fault segments in the model and how they are associated with real tectonic structures
Figure 3. Schematic representations of the faulting patterns associated with different configurations of neighbouring active cells
Figure 4. (a) Cooperative configurations of active cells. These configurations are those for which the shear and extensional zones associated with motions along dextral vertical strike-slip fault overlap
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