Figure S3. Simulated coseismic changes in mean stress to demonstrate stress transfer within the wedge for each earthquake.
(a) 2010 Maule earthquake, (b) 1960 Valdivia earthquake, and (c) 2011 Tohoku earthquake. Red indicates increase in mean stress blue indicates decrease. The black dashed line locates the boundary between the inner and outer wedges, marking a change in basal friction behavior.