Tripuhyite

Tripuhyite is an iron antimonate mineral with composition FeSbO4.

Tripuhyite
General
CategoryAntimonate mineral
Formula
(repeating unit)
FeSbO4
Strunz classification4.DB.05
Crystal systemTetragonal
Crystal classDitetragonal dipyramidal (4/mmm)
H-M symbol: (4/m 2/m 2/m)
Space groupP41/mnm
Unit cella = 4.63, c = 9.14 [Å]; Z = 2
Identification
ColorYellowish brown, lemon-yellow, brown-black
Crystal habitFibrous to fine-grained aggregates
Mohs scale hardness6 - 7
LusterDull to earthy
StreakCanary-yellow to dark brown with a greenish tinge
DiaphaneityTranslucent
Specific gravity5.82
Optical propertiesUniaxial (+), canary-yellow color (transmitted light)
Refractive indexnω = 2.190 nε = 2.330
Birefringenceδ = 0.140
PleochroismNone
SolubilityInsoluble in acids
Other characteristicsAntiferromagnetic
References[1][2][3]

Nomenclature

The name of the mineral comes from the locality of Tripuhy, Ouro Preto, Minas Gerais, Brazil, where it was discovered. Hussak and Prior[4] first described the mineral tripuhyite as an oxide of iron and antimony, and assigned it the composition Fe2Sb2O7. When a mineral with composition FeSbO4 was later discovered in Squaw Creek, New Mexico (US), it was considered erroneously as a new mineral and it was given the name squawcreekite.[5] However, other studies had shown that the original tripuhyite was also FeSbO4.[6] In 2002, the Commission on New Minerals and Mineral Names (CNMMN) of the International Mineralogical Association (IMA), approved the redefinition of tripuhyite as FeSbO4 and the discreditation of squawcreekite.[7]

Crystal Structure

FeSbO4 exhibits the rutile structure, with a tetragonal unit cell. The cations are octahedrally coordinated to oxygen anions, with the octahedra sharing edges along the c-direction. Fe(III) and Sb(V) cations are distributed in a disordered way over the octahedral sites.

References

  1. Mindat.org
  2. Handbook of Mineralogy
  3. Webmineral data
  4. Hussak, E.; Prior, G. T. (1897). "On Tripuhyite, a New Antimonate of Iron, from Tripuhy, Brazil". Mineralogical Magazine. 11: 302–303. doi:10.1180/minmag.1897.011.53.04.
  5. Foord, E. E.; P. F. Hlava; J. J. Fitzpatrick; R. C. Erd; R. W. Hinton (1991). Neues Jahrbuch für Mineralogie - Monatshefte. 8: 363–384. Missing or empty |title= (help)
  6. Tavora, E. (1955). "X-ray diffraction powder data for some minerals from Brazilian localities". Anais da Academia Brasileira de Ciências. 27: 7–27.
  7. Berlepsch, P.; T. Armbruster; J. Brugger; A. J. Criddle; S. Graeser (2003). "Tripuhyite, FeSbO4, revisited". Mineralogical Magazine. 67: 31–46. doi:10.1180/0026461036710082.

Bibliography

  • Palache, P.; Berman H.; Frondel, C. (1960). "Dana's System of Mineralogy, Volume II: Halides, Nitrates, Borates, Carbonates, Sulfates, Phosphates, Arsenates, Tungstates, Molybdates, Etc. (Seventh Edition)" John Wiley and Sons, Inc., New York, pp. 1024.


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