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The atomic arrangement of ojuelaite, ZnFe23+(AsO4)2(OH)2·4H2O

Published online by Cambridge University Press:  05 July 2018

John M. Hughes ,
Erich S. Bloodaxe ,
Kyle D. Kobel  and
John W. Drexler
John M. Hughes
Affiliation:
Department of Geology, Miami University, Oxford, OH 45056, USA
Erich S. Bloodaxe
Affiliation:
Department of Geology, Miami University, Oxford, OH 45056, USA
Kyle D. Kobel
Affiliation:
Department of Geology, Miami University, Oxford, OH 45056, USA
John W. Drexler
Affiliation:
Department of Geological Sciences, University of Colorado, Boulder, CO 80309, USA
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Extract

Ojuelaite was described from its occurrence at the Ojuela mine in Mapimi, Mexico by Cesbron et al. (1981). Those authors suggested that the phase was isostructural with whitmoreite (Moore et al., 1974), a phase of interest because of the unique arrangement of Fe octaheda in its octahedral sheet.

Keywords

ojuelaitecrystal structureMexico
Type
Short Communications
Information
Mineralogical Magazine , Volume 60 , Issue 400 , June 1996 , pp. 519 - 521
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1996

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References

Cesbron, F., Romero, S.M. and Williams, S.A. (1981) Bull Mineral, 104, 582—6.Google Scholar
Keller, P. and Hess, H. (1978) Neues Jahrb. Mineral Abh. 133, 291–302. Google Scholar
Moore, P.B., Kampf, A.R. and Irving, A.J. (1974) Amer. Mineral. 59, 900—5.Google Scholar
Ni, Y., Hughes, J.M. and Mariano, A.N. (1993) Amer. Mineral. 78, 415—8.Google Scholar