Colchesterite, Bi <sup>3+</sup> <sub>2</sub> O[Mo <sup>6+</sup> <sub>2</sub> O <sub>8</sub> ], a new Bi molybdate mineral from the Kingsgate mines, New South Wales, Australia
Colchesterite, Bi 3+2 OMo 6+ 2 O 8 , is a new mineral from the Kingsgate mines, Gough Co., New South Wales, Australia.It forms greenish-yellow to brownish-yellow, equant to prismatic crystals to 1.1 mm in length.The mineral is transparent, with a vitreous luster.The crystals show excellent cleavage on {001}.The hardness is 2½ based on scratch tests and the tenacity is brittle with an uneven, stepped fracture.The calculated density is 6.522 g/cm -3 for the empirical formula.Colchesterite is nonpleochroic, biaxial (+), with calculated indices of refraction of α = 2.18, β = 2.20 and γ = 2.23.The measured 2V is 80(5)° and the optical orientation is Z = b, X ^ c = 20° in obtuse angle β.Dispersion is r < v, strong and crossed.Colchesterite is monoclinic, space group P2 1 /n, with the unit-cell parameters: a = 8.1030( 16), b = 8.5396(17), c = 11.209(2)Å, β = 93.58(3)º,V = 774.1(3)Å 3 and Z = 4.The crystal structure was refined to an R 1 index of 2.39% for 1719 observed reflections with I > 2σ I .The structure consists of layers of Bi 4 O 22 tetrameric clusters comprised of edge-sharing Bi1O 8 and Bi2O 7 polyhedra that share edges with Mo 2 O 8 dimers to form a dense framework.
Authors
- Peter Elliott (ORCID: https://orcid.org/0000-0002-4869-9071)
- Anthony R. Kampf
Institutions
- South Australian Museum (AU)
- Natural History Museum of Los Angeles County (US)
- The University of Adelaide (AU)
Publication Details
- Journal
- Mineralogical Magazine
- Published
- 2026-05-28
- DOI
- https://doi.org/10.1180/mgm.2026.10234
- Primary Topic
- Crystal Structures and Properties
- Type
- article
- Field-Weighted Citation Impact
- 0.00