Galeaclolusite, [Al6(AsO4)3(OH)9(H2O)4]•8H2O, a new bulachite-related mineral from Cap Garonne, France

被引:4
|
作者
Grey, Ian E. [1 ]
Favreau, George [2 ]
Mills, Stuart J. [3 ]
Mumme, W. Gus [1 ]
Bougerol, Catherine [4 ,5 ]
Brand, Helen E. A. [6 ]
Kampf, Anthony R. [7 ]
MacRae, Colin M. [1 ]
Shanks, Finlay [8 ]
机构
[1] CSIRO Mineral Resources, Private Bag 10, Clayton, Vic 3169, Australia
[2] 421 Ave Jean Monnet, F-13090 Aix En Provence, France
[3] Museums Victoria, Geosci, GPO Box 666, Melbourne, Vic 3001, Australia
[4] Univ Grenoble Alpes, F-38000 Grenoble, France
[5] Inst Neel, CNRS, F-38000 Grenoble, France
[6] Austraiian Synchrotron, 800 Blackburn Rd, Clayton, Vic 3168, Australia
[7] Nat Hist Museum Los Angeles Cty, Mineral Sci Dept, 900 Exposit Blvd, Los Angeles, CA 90007 USA
[8] Monash Univ, Sch Chem, Clayton, Vic 3800, Australia
关键词
bulachite; galeaclolusite; new mineral; Cap Garonne; crystal structure; synchrotron; CRYSTAL-STRUCTURE; CYANOTRICHITE FAMILY; STRUCTURAL VARIATION; ALUMINUM ARSENATE;
D O I
10.1180/mgm.2020.98
中图分类号
P57 [矿物学];
学科分类号
070901 ;
摘要
Galeaclolusite, [Al-6(AsO4)(3)(OH)(9)(H2O)(4)]center dot 8H(2)O, is a new secondary hydrated aluminium arsenate mineral from Cap Garonne, Var, France. It forms crusts and spheroids of white fibres up to 50 mu m long by 0.4 mu m wide and only 0.1 mu m thick. The fibres are elongated along [001] and flattened on (100). The calculated density is 2.27 g.cm(-3). Optically, galeaclolusite is biaxial with alpha = 1.550(5), beta not determined, gamma = 1.570(5) (white light) and partial orientation: Z = c (fibre axis). Electron microprobe analyses coupled with crystal structure refinement results gives an empirical formula based on 33 O atoms of Al5.72Si0.08As2.88O33H34.12. Galeaclolusite is orthorhombic, Pnma, with a = 19.855(4), b = 17.6933(11), c = 7.7799(5) angstrom, V = 2733.0(7) angstrom(3) and Z = 4. The crystal structure of galeaclolusite was established from its close relationship to bulachite and refined using synchrotron powder X-ray diffraction data. It is based on heteropolyhedral layers, parallel to (100), of composition Al-6(AsO4)(3)(OH)(9)(H2O)(4) and with H-bonded H2O between the layers. The layers contain [001] spiral chains of edge-shared octahedra, decorated with corner-connected AsO4 tetrahedra, that are the same as in the mineral liskeardite.
引用
收藏
页码:142 / 148
页数:7
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