Modelling Earth’s surface topography: Decomposition of the static and dynamic components
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文摘

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.

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