Abstract
The concentration of Fe3+ in mantle minerals determines many of their physical and chemical properties. Traditionally iron in major mantle phases has been assumed to be predominantly Fe2+, but results from both high-pressure experiments and inclusions in diamonds from the lower mantle suggest that approximately half of the iron in lower mantle (Mg,Fe)(Si,Al)O3 perovskite is Fe3+. This paper reviews the current state of knowledge of iron oxidation state and oxygen fugacity in the mantle based on Mössbauer results from natural and synthetic samples, and discusses new ideas that have arisen from these results.
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McCammon, C. A., Hyp. Interact. 90 (1994), 89.
McCammon, C. A., Chaskar, V. and Richards, G. G., Meas. Sci. Technol. 2 (1991), 657.
McCammon, C. A., Hyp. Interact. 92 (1994), 1235.
Anderson, D. L., Theory of the Earth, Blackwell Science Inc., 1989.
Haggerty, S. E. and Sautter, V., Science 248 (1990), 993.
Sautter, V., Haggerty, S. E. and Field, S., Science 252 (1991), 827.
Collerson, K. D., Hapugoda, S., Kamber, B. S. and Williams, Q., Science 288 (2000), 1215.
O'Neill, H. St. C., Rubie, D. C., Canil, D., Geiger, C. A., Ross II, C. R., Seifert, F. and Woodland, A. B., In: T. Takahashi, R. Jeanloz and D. C. Rubie (eds), Evolution of the Earth and Planets, American Geophysical Union, Washington, DC, 1993, p. 73.
Wood, B. J. and Virgo, D., Geochim. Cosmochim. Acta 53 (1989), 1277.
Wood, B. J., Bryndzia, L. T. and Johnson, K. E., Science 248 (1990), 337.
Woodland, A. B., EOS, Suppl. 81 (2000), F1278.
Ballhaus, C., Earth Planet. Sci. Lett. 132 (1995), 75.
O'Neill, H. St. C., McCammon, C. A., Canil, D. C., Rubie, D. C., Ross II, C. R. and Seifert, F., Amer. Mineral. 78 (1993), 456.
Hutchison, M., Ph.D. thesis, University of Edinburgh, 1997.
Stachel, T., Brey, G. P. and Harris, J.W., Contrib. Mineral. Petrol. 140 (2000), 1.
McCammon, C. A., Phys. Chem. Minerals 25 (1998), 292.
Harte, B., Harris, J. W., Hutchison, M. T., Watt, G. R. and Wilding, M. C., In: Y. Fei, C. M. Bertka and B. O. Mysen (eds), Mantle Petrology: Field Observations and High-Pressure Experimentation: A Tribute to Francis R. (Joe) Boyd, Geochemical Society, USA, 1999, p. 125.
McCammon, C., Science 293 (2001), 813.
McCammon, C. A., Hutchison, M. and Harris, J., Science 278 (1997), 434.
McCammon, C. A., Stachel, T. and Harris, J. W., Eur. J. Mineral. (Beihefte) 12 (2000), 123.
McCammon, C. A., Nature 387 (1997), 694.
Lauterbach, S., McCammon, C. A., van Aken, P., Langenhorst, F. and Seifert, F., Contrib. Mineral. Petrol. 138 (2000), 17.
Jackson, I., Geophys. J. Int. 134 (1998), 291.
Irifune, T., Nature 370 (1994), 131.
McCammon, C. A., Peyronneau, J. P. and Poirier, J.-P., Geophys. Res. Lett. 25 (1998), 1589.
Zhang, J. and Weidner, D. J., Science 284 (1999), 782.
Xu, Y. and McCammon, C. A., J. Geophys. Res., in press.
Dobson, D. P. and Brodholt, J. P., Geophys. Res. Lett. 27 (2000), 2325.
van der Hilst, R., Widiyantoro, S. and Engdahl, E., Nature 386 (1997), 578.
Deines, P., Geochim. Cosmochim. Acta 44 (1980), 943.
McDonough, W. F. and Sun, S.-S., Chemical Geology 120 (1995), 223.
Takahashi, E. and Ito, E., In: M. H. Manghnani and Y. Syono (eds), High-Pressure Research in Mineral Physics, Terra Scientific Publishing Company, Tokyo, 1987, p. 427.
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McCammon, C.A. From Diamonds to Defects: New Ideas about the Earth's Interior. Hyperfine Interactions 141, 73–81 (2002). https://doi.org/10.1023/A:1021293617741
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DOI: https://doi.org/10.1023/A:1021293617741