Mathematics
Scientific paper
Jun 1994
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1994sci...264.1437v&link_type=abstract
Science (ISSN 0036-8075), vol. 264, no. 5164, p. 1437-1439
Mathematics
28
Convective Heat Transfer, Earth Mantle, Geodynamics, Geoids, Geology, High Temperature, Melting, Perovskites, Temperature Effects, Topography, Creep Properties, Ductility, Estimating, Heating, Linearization, Mathematical Models, Rayleigh Number, Viscosity
Scientific paper
Recent studies have implied that (Mg,Fe)SiO3-perovshite, a likely dominant mineral phase in the lower mantle, may have a high melting temperature. The implications of these findings for the dynamics of the lower mantle were investigated with the use of numerical convection models. The results showed that low homologous temperatures (0.3 to 0.5) would prevail in the modeled lower mantle, regardless of the effective Rayleigh number and internal heating rates. High-temperature ductile creep is possible under relatively cold conditions. In models with low rates of internal heating, local maxima of viscosity developed in the mid-lower mantle that were similar to those obtained from inversion of geoid, topography, and plate velocities.
van den Berg Arie P.
van Keken Peter E.
Yuen David A.
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