High spatial resolution models of time-dependent, layered mantle convection.

Details High spatial resolution models of time-dependent, layered mantle convection. High spatial resolution models of time-dependent, layered mantle convection.

Oct 1986

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1986geoji..87..241b&link_type=abstract

Geophysical Journal International, Vol. 87, No. 1, p. 241 - 264

Physics

Convection:Earth Mantle, Earth Mantle:Convection

Scientific paper

The degree of geochemical mixing that occurred during the mantle's early evolution is dependent on the history of convective motions in the mantle. The authors present time-dependent models of mantle convection that show, for certain conditions in the newly formed earth's mantle, a transient phase of layered convection results, during which geochemical differences between the upper and lower mantle could have been preserved.

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