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Titlebook: Global Dynamics of the Earth: Applications of Viscoelastic Relaxation Theory to Solid-Earth and Plan; Roberto Sabadini,Bert Vermeersen,Gab

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TPW Driven by Subduction: Non-linear Rotation Theory,for a stratified, viscoelastic, incompressible Earth. We show how mantle convection TPW represents a very powerful constraint for the mantle viscosity profile, and our finding is that the lower mantle has to be definitively stiffer than the upper mantle.
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Rolando Jr. C. Villamero,Leda Kamenopoulouhe rotation equation is considered, and a linearized theory for TPW driven by mantle convection is provided. The Earth, Mars and Venus are compared in terms of the ability of their rotation axis to wander.
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Inclusive Education in African Contexts substantially stiffer lower mantle. The path of the rotation pole is analyzed in terms of mantle viscosity and of the rheology of the lithosphere, being elastic or viscoelastic. The effects of a non-hydrostatic bulge, due to asymmetric density distribution in the mantle, is then studied in terms of its effects on TPW driven by ice-ages.
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