Abstract
Subducting plate (SP) curvature exerts a key control on the amount of bending dissipation associated with subduction, and the magnitude of the subduction-resisting bending force. However, the factors controlling the development of SP curvature are not well understood. We use numerical models to quantify the role of SP rheology on the minimum radius of curvature, R (sub min) . We find that R (sub min) depends strongly on the SP thickness when the rheology is viscous. This dependence is substantially reduced when the SP behaves plastically, in line with the lack of correlation between R (sub min) and SP thickness on Earth. In contrast, plasticity leads to a strong positive correlation between R (sub min) and the overriding plate (OP) thickness. Using an analysis of R (sub min) versus OP thickness, we show that such a positive correlation exists on Earth. This suggests that OP structure, in conjunction with SP plasticity, is crucial in generating slab curvature systematics on Earth. Abstract Copyright (2015), . American Geophysical Union. All Rights Reserved.
