Fig. 5From: The sensitivity of ocean tide loading displacements to the structure of the upper mantle and crust of Taiwan IslandSimilar to Fig. 4 except that we perturb layers of 20 km thickness. The sensitivities of displacement Green’s functions to + 1% linear perturbations of the bulk modulus, shear modulus, and density in layers with a fixed thickness of 20 km at depths from 0 to 700 km instead of the major regions of TW1Back to article page