Effect of lithospheric mantle on isostatic topography is not neglectable.
Isostatic topography is uncertain, this hampers dynamic topography determination.
Residual and dynamic topography maps correlate poorly (∼–0.48 < r < 0.55).
Dynamic topography maps from mantle flow modelling present elevated amplitudes.
SPANI Vp and Vs components do not yield same temperature for a given composition.