Computer Science
Scientific paper
Oct 2011
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011epsc.conf..165k&link_type=abstract
EPSC-DPS Joint Meeting 2011, held 2-7 October 2011 in Nantes, France. http://meetings.copernicus.org/epsc-dps2011, p.165
Computer Science
Scientific paper
Differentiation in the transitional zone D'' at the mantle-core interface leads to transition of metallic components from the mantle into the core and to formation of a light fraction in the mantle. Additionally, the eclogite-alteration effect of the downwelling oceanic crust in subduction zones has been taken into consideration, because it determines the appearance of a heavy fraction in the mantle. The model has taken the origin and drift of light crustal substance, which forms with differentiation of upwelling hot substance, into consideration. The cause of mantle layering in our model is restricted by the combined action of the phase transition, chemical heterogeneities, and surges in density and viscosity at this interface.
Kotelkin V.
Lobkovsky L.
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