Abstract
ESTIMATES of the amount of magnetite in a Type I carbonaceous meteorite have ranged from 6 per cent by weight1 to about 40 per cent by weight2. We have applied the technique of quantitative X-ray diffractometry to a sample of the Orgueil meteorite in an attempt to narrow these limits.
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References
Boström, K., and Fredriksson, K., Smithsonian Miscellaneous Collections, 151, 39 (1966).
DuFresne, E. R., and Anders, E., Geochim. Cosmochim. Acta, 26, 1085 (1962).
Copeland, I. E., and Bragg, R. H., Amal. Chem., 30, 196 (1958).
Wiik, H. B., Geochim. Cosmochim. Acta, 9, 279 (1956).
Kerridge, J. F., Ann. NY Acad. Sci., 119, 41 (1964).
Wood, J. A., Geochim. Cosmochim. Acta, 31, 2095 (1967).
Keil, K., and Fredriksson, K., J. Geophys. Res., 69, 3487 (1964).
Larimer, J. W., and Anders, E., Geochim. Cosmochim. Acta, 31, 1239 (1967).
Harris, P. G., and Tozer, D. C., Nature, 215, 1449 (1967).
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KERRIDGE, J., CHATTERJI, S. Magnetite Content of a Type I Carbonaceous Meteorite. Nature 220, 775–776 (1968). https://doi.org/10.1038/220775b0
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DOI: https://doi.org/10.1038/220775b0
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