Tectonic plates, D (double prime) thermal structure, and the nature of mantle plumes

Details Tectonic plates, D (double prime) thermal structure, and the nature of mantle plumes Tectonic plates, D (double prime) thermal structure, and the nature of mantle plumes

Aug 1994

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1994jgr....9915697l&link_type=abstract

Journal of Geophysical Research (ISSN 0148-0227), vol. 99, no. B8, p. 15,697-15,708

Mathematics

Logic

14

Earth Mantle, Geotemperature, Plates (Tectonics), Plumes, Rheology, Tectonics, Temperature Effects, Thermodynamics, Boundary Layers, Mars (Planet), Mathematical Models, Venus (Planet), Viscosity

Scientific paper

It is proposed that subducting tectonic plates can affect the nature of thermal mantle plumes by determining the temperature drop across a plume source layer. The temperature drop affects source layer stability and the morphology of plumes emitted from it. Numerical models are presented to demonstrate how introduction of platelike behavior in a convecting temperature dependent medium, driven by a combination of internal and basal heating, can increase the temperature drop across the lower boundary layer. The temperature drop increases dramatically following introduction of platelike behavior due to formation of a cold temperature inversion above the lower boundary layer. This thermal inversion, induced by deposition of upper boundary layer material to the system base, decays in time, but the temperature drop across the lower boundary layer always remains considerably higher than in models lacking platelike behavior. On the basis of model-inferred boundary layer temperature drops and previous studies of plume dynamics, we argue that generally accepted notions as to the nature of mantle plumes on Earth may hinge on the presence of plates. The implication for Mars and Venus, planets apparently lacking plate tectonics, is that mantle plumes of these planets may differ morphologically from those of Earth. A corollary model-based argument is that as a result of slab-induced thermal inversions above the core mantle boundary the lower most mantle may be subadiabatic, on average (in space and time), if major plate reorganization timescales are less than those acquired to diffuse newly deposited slab material.

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