Temperatures in the mantle as inferred from simple compositional models

This investigation tests the mixed-oxide model against the elastic and density requirements of the mantle within the region immediately below the 650 km discontinuity (approximately 650 to 1200 km). Mixed-oxide compositions containing combinations of (Mg.Fe)O and SiO/sub 2/ which correspond to dunite-peridotite and pyroxenite were emphasized in the modelling procedure. Models in the compositional range dunite-peridotite were found to satisfy the P and S-wave velocities, as well as the density requirements below the 650 km discontinuity; satisfactory solutions were provided by such models when Fe/(Mg + Fe) = 0.15 +- 0.05 along an adiabatic temperature gradient of 1300/sup 0/C at zero pressure. Models of pyroxenite composition do not satisfy the physical properties of the mantle in the region of interest. The successful dunite-peridotite mixed-oxide compositional models provide an estimate of the geotherm in the 650 to 1200 km region of the mantle. Since the physical properties within the region of interest are satisfied along an adiabat, the problem is reduced to calculating the increase of temperature with depth for the preferred model along the adiabatic gradient (initial temperature 1300/sup 0/C). This procedure yields a geotherm which is consistent with several independent upper mantle temperature estimates. The present results indicate amore » temperature of 1600 +- 400/sup 0/C at 671 km; the primary source of uncertainty is the accuracy of the seismic model interpretations.« less

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