Fig. 1From: Rheology and stress in subduction zones around the aseismic/seismic transitionThe seismic-aseismic transition in a subduction zone. Isotherms after Peacock et al. (2011). Slow earthquakes: source region of tectonic tremor and slow slip events. Dehydration processes contributing water to the subduction zone in green. Distribution of serpentinized mantle is schematicBack to article page