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Implications for Mantle Dynamics from the High Melting Temperature of Perovskite

Science
3 Jun 1994
Vol 264, Issue 5164
pp. 1437-1439

Abstract

Recent studies have implied that (Mg,Fe)SiO3-perovskite, 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.

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Published In

Science
Volume 264 | Issue 5164
3 June 1994

Submission history

Received: 11 January 1994
Accepted: 4 April 1994
Published in print: 3 June 1994

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Authors

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Peter E. van Keken
Army High Performance Computing Research Center, University of Minnesota, 1100 Washington Avenue South, Minneapolis, MN 55415, USA.
David A. Yuen
Minnesota Supercomputer Institute, University of Minnesota, 1200 Washington Avenue South, Minneapolis, MN 55415, USA.
Arie P. van den Berg
Department of Theoretical Geophysics, Institute of Earth Sciences, Postal Box 80.021, 3508 TA, Utrecht, Netherlands

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