Fig. 5: Sensitivity test results regarding the lithospheric thickness (model setup in Fig. S3).
From: Lens effect of remnant blocks on deep mantle upwelling causing anomalous subsidence
a–d Summary of topographical variations. e Comparison of the topography at 3.5 Myr in four representative models. In the presented models, the belt widths of both mantle transitions are 25 km. γ410 and Δρ410 (5%)- the Clapeyron slope and the complete density-jump ratio of the 410 km phase transformations. γ660 and Δρ660 (9.6%)- the Clapeyron slope and the complete density-jump ratio of the 660 km phase transformations. Other plotting habits are the same as in Fig. 4.
