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Earth, Planets and Space
Fig. 5 | Earth, Planets and Space

Fig. 5

From: Dip angles of active faults from the surface to the seismogenic zone inferred from a 2D numerical analysis of visco-elasto-plastic models: a case study for the Osaka Plain

Fig. 5

Strain weakening behavior of material. Strain weakening is initiated after an accumulated strain εII = 0. Initial friction angle and cohesion (φi, Ci) both linearly decrease between εII = 0 and εII = 1 to the weakened values (φw, Cw), which they keep

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