Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/79953
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dc.contributor.authorElliott, P.en
dc.contributor.authorKolitsch, U.en
dc.contributor.authorWillis, A.en
dc.contributor.authorLibowitzky, E.en
dc.date.issued2013en
dc.identifier.citationMineralogical Magazine, 2013; 77(4):509-522en
dc.identifier.issn0026-461Xen
dc.identifier.issn1471-8022en
dc.identifier.urihttp://hdl.handle.net/2440/79953-
dc.description.abstractDomerockite, Cu₄(AsO₄)(AsO₃OH)(OH)₃·H₂O, is a new mineral from the Dome Rock Mine, South Australia. It occurs as aggregates of bluish green, equant to short prismatic and tabular crystals up to 0.3 mm long and 0.2 mm across. Domerockite is translucent, with a vitreous lustre and pale green streak. It displays no fluorescence under UV irradiation. The mineral is brittle with an uneven fracture, a Mohs hardness of ∼3 and a calculated density of 4.44 g/cm³ (based on the structure refinement). Optically, it is biaxial negative, with α = 1.798(4), β = 1.814(4), γ = 1.817(4), 2V(calc). = 46°; pleochroism is very weak; X pale greenish yellow, Y greenish blue, Z greenish blue; absorption X < Y = Z; orientation is uncertain. Chemical analysis by electron microprobe gave CuO 52.04, ZnO 0.78, BaO 0.11, As₂O₅37.67, P₂O₅0.32, SiO₂0.24, H₂O 8.84, total 100.00 wt.%, with H₂O calculated by difference. The empirical chemical formula is (Cu₃.₉₄, Zn₀.₀₆)Σ₄.₀₀H₀.₉₁(As₁.₉₇, P₀.₀₃, Si₀.₀₂)Σ₂.₀₂O₈(OH)₃.₀₀˙H₂O based on 12 oxygen atoms. Domerockite is triclinic, space group P1, with a = 5.378(11), b = 8.962(18) c = 9.841(2) Å, α = 75.25(3), β = 83.56(3), γ = 79.97(3)°, V = 450.5(16) ų and Z = 2. The eight strongest lines in the X-ray powder diffraction pattern are [d (Å), (I)(hkl)]: 4.716 (30)(101, 002, 111), 3.697 (25)(121), 3.605 (30)(120, 121), 3.119 (60)(121), 3.073 (100)(121), 2.856 (40)(022, 030), 2.464 (50)(212, 113), 2.443 (40)(014). The crystal structure of domerockite has been solved by direct methods and refined to an R index of 7.44% using 2635 observed reflections. The structure comprises [Cu₄] ( = O, OH) chains of edge-sharing sharing, distorted octahedra that extend along [101] and are decorated by AsO4 tetrahedra to form sheets in the (010) plane. Dimers of edge-sharing [CuO₄(OH)(H₂O)] octahedra share corners with dimers of edge-sharing [CuO₄(OH)] square pyramids to form zigzag chains which extend along [101]. The chains lie between and link to the sheets by sharings corners of octahedra, square pyramids and tetrahedra to form a heteropolyhedral framework.en
dc.description.statementofresponsibilityP. Elliott, U. Kolitsch, A. C. Willis, and E. Libowitzkyen
dc.language.isoenen
dc.publisherMineralogical Societyen
dc.rights© 2013 The Mineralogical Societyen
dc.subjectcopper arsenate; crystal structure; dome rock mine; domerockite; new mineral speciesen
dc.titleDescription and crystal structure of domerockite, Cu₄(AsO₄)(AsO₃OH)(OH)₃·H₂O, a new mineral from the Dome Rock Mine, South Australiaen
dc.title.alternativeDescription and crystal structure of domerockite, Cu(4)(AsO(4))(AsO(3)OH)(OH)(3)(.)H(2)O, a new mineral from the Dome Rock Mine, South Australiaen
dc.typeJournal articleen
dc.identifier.doi10.1180/minmag.2013.077.4.10en
pubs.publication-statusPublisheden
dc.identifier.orcidElliott, P. [0000-0002-4869-9071]en
Appears in Collections:Earth and Environmental Sciences publications

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