Figure 9From: Towards scaling laws for subduction initiation on terrestrial planets: constraints from two-dimensional steady-state convection simulationsStress structure of steady state cases with R a=3×107, θ=16, a=0.75. Cases (a-d) use Arrhenius viscosity with (a) T 0=0.6, (b) T 0=0.8, (c) T 0=1.2, and (d) T 0=2.0. Case (e) uses exponential viscosity. Color scale shows the values of log(τ). White lines represent streamlines.Back to article page