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Magnetic susceptibilities of chromites from Oman

Published online by Cambridge University Press:  05 July 2018

A. Rais ,
A. A. Yousif ,
M. A. Worthing  and
Z. Al-Alawi
A. Rais
Affiliation:
Department of Physics, Sultan Qaboos University, P.O.Box 36 Al-Khod 123, Muscat, Sultanate of Oman
A. A. Yousif
Affiliation:
Department of Physics, Sultan Qaboos University, P.O.Box 36 Al-Khod 123, Muscat, Sultanate of Oman
M. A. Worthing
Affiliation:
Department of Earth Sciences, Sultan Qaboos University, P.O. Box 36 Al-Khod 123, Muscat, Sultanate of Oman
Z. Al-Alawi
Affiliation:
Department of Earth Sciences, Sultan Qaboos University, P.O. Box 36 Al-Khod 123, Muscat, Sultanate of Oman
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Abstract

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Keywords

Magnetic susceptibilitynatural chromiteparamagnetismmagnetic moments
Type
Short Communications
Information
Mineralogical Magazine , Volume 61 , Issue 408 , October 1997 , pp. 726 - 728
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1997

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References

Al-Alawi, Z., Gismelseed, A.M., Yousif, A.A., Worthing, M.A., Sutherland, H.H., Rais, A., Elzain, M.E. and Rawas, A.D. (1996) Cation distribution in natural chromites from Oman. Science & Technology, 1, 55—61.Google Scholar
Fatseas, G.A., Dormann, J.L., and Blanchard, H. (1976) Study of the Fe3+/Fe2+ ratio in natural chromites (FexMg1-x)(Cr1-y-zFeyAl7)O4 . J. de Phys., 12, 787-92.Google Scholar
Lodya, J.A., Pollack, H., Nell, J., and Albers, A. (1994) Mossbauer spectroscopy and magnetic susceptibility of natural chromites. Hyp. Int., 93, 1789-94.CrossRefGoogle Scholar
Mitra, S., Pal, T., and Pal, T. (1991) Petrogenetic implication of the Mössbauer hyperfine parameters of Fe3+-chromites from Sukinda (India) ultramafites. Mineral. Mag., 55, 535-42.CrossRefGoogle Scholar
Murad, E. and Johnston, J.H. (1987) In Mossbauer Spectroscopy Applied to Inorganic Chemistry, Volume 2, Long, G.J., ed., Plenum, New York, p. 507.Google Scholar
Nell, J., and Pollak, H. Characterization of natural chromite ((Mg,FeII)(Al,FeIIICr)2O4) samples from the Bushveld Complex, South Africa. Hyp. Int., 84, 427-31.CrossRefGoogle Scholar
Robins, M., Wertheim, G.K., Sherwood, R.C. and Buchanan, D.N.E. (1971) Magnetic properties and site distributions in the system FeCr2O4-Fe3O4- (Fe2+Cr2-xFex 3+O4). J. Phys. Chem. Solids, 32, 717-29.CrossRefGoogle Scholar

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