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Isostatic deformations and polar wander induced by redistribution of mass within the Earth

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Academic year: 2021

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Figure

TABLE 1. Physical Properties of the Eight Earth Models
TABLE 2. Relaxation Times of the Viscoelastic Modes
Fig. 2. Same as in Figure 1 but for Earth models with a nonadiabatic stratification at the 670-km depth interface
Fig. 3. Geoid perturbations induced by a mass anomaly of degree 2 located in the mantle
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