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Enhancement of Cation Diffusion Rates Across the 410-Kilometer Discontinuity in Earth's Mantle
S. Chakraborty, R. Knoche, H. Schulze, D. C. Rubie, D. Dobson, N. L. Ross and R. J. Angel
New Series, Vol. 283, No. 5400 (Jan. 15, 1999), pp. 362-365
Published by: American Association for the Advancement of Science
Stable URL: http://www.jstor.org/stable/2896801
Page Count: 4
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Rates of cation diffusion (magnesium, iron, and nickel) have been determined in olivine and its high-pressure polymorph, wadsleyite, at 9 to 15 gigapascals and 1100° to 1400°C for compositions that are relevant to Earth's mantle. Diffusion in olivine becomes strongly dependent on composition at high pressure. In wadsleyite, diffusion is one to two orders of magnitude faster than in olivine, depending on temperature. Homogenization of mantle heterogeneities (chemical mixing) and mineral transformations involving a magnesium-iron exchange will therefore occur considerably faster in the transition zone than at depths of less than 410 kilometers.
Science © 1999 American Association for the Advancement of Science