Effects of low-viscosity post-perovskite on thermo-chemical mantle convection in a 3-D spherical shell

Details Effects of low-viscosity post-perovskite on thermo-chemical mantle convection in a 3-D spherical shell Effects of low-viscosity post-perovskite on thermo-chemical mantle convection in a 3-D spherical shell

Feb 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011georl..3804309n&link_type=abstract

Geophysical Research Letters, Volume 38, Issue 4, CiteID L04309

Physics

6

Tectonophysics: Dynamics: Convection Currents, And Mantle Plumes, Tectonophysics: Earth'S Interior: Composition And State (1212, 7207, 7208, 8105), Structural Geology: Rheology: Mantle (8162)

Scientific paper

Numerical simulations of thermo-chemical, multi-phase mantle convection in a 3-D spherical shell are performed to determine how a low viscosity of post-perovskite affects dynamics and structures in the deep mantle. Low-viscosity post-perovskite weakens the deepest part of slabs, allowing them to more effectively spread over the core-mantle boundary (CMB), and it also results in a greater volume of basalt segregating, both of which increase the size of dense chemical piles, the horizontal lengthscale of regions of pooled slab material, and the steepness of piles' edges (in composition and phase), consistent with the existence of steep, sharp-sided edges found in seismic analyses. CMB heat flux is strongly enhanced in regions of low-viscosity post-perovskite (consistent with a theoretical prediction) and both CMB and surface heat flux are increased on average by a low-viscosity of post-perovskite, which could have important implications for the evolution of Earth's core and mantle.

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