Global Dynamics of the Earth: Applications of Viscoelastic Relaxation Theory to Solid-Earth and Planetary Geophysics pp 257-267 | Cite as
TPW Driven by Subduction: Non-linear Rotation Theory
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Abstract
This chapter deals with the development of a non-linear rotation theory, driven by internal density anomalies, as for those due to mantle convection, 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.
Keywords
Lower Mantle Mantle Convection Inertia Tensor Love Number Geophysical Process
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