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.