Fig. 1From: The role of glacial isostatic adjustment in the present-day crustal motion and sea levels of East AsiaLateral perturbation in log10 of the mantle viscosity (in Pa s) in East Asia for the four mantle layers of the laterally-heterogeneous Earth model RF3L20(β=0.4). The name of the layer, the depth range, and numeric range are shown above each map.Back to article page