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On finite thickness of shear bands in frictional viscoplasticity, and implications for lithosphere dynamics

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Academic year: 2021

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Figure

Fig. 1b), with a viscous damper added in series to the previous rheology (Maxwell-type
Table 2. Number of Newton-Raphson iterations required to reach global equilibrium for different resolu- resolu-tions using either the E-P or the E-VP model
Figure 1. Investigated rheological models for deformation of the lithosphere: a) Maxwell elasto-plastic model
Figure 2. Spatial distribution of accumulated strain ( I I ) calculated with an elasto-plastic rheology for three different mesh resolutions (51 2 , 101 2 , and 201 2 nodes)
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