Hostname: page-component-cd9895bd7-lnqnp Total loading time: 0 Render date: 2024-12-23T23:29:35.956Z Has data issue: false hasContentIssue false

Feinglosite, a new mineral related to brackebuschite, from Tsumeb, Namibia

Published online by Cambridge University Press:  05 July 2018

A. M. Clark
Affiliation:
Department of Mineralogy, The Natural History Museum, Cromwell Road, London SW7 5BD, UK
A. J. Criddle
Affiliation:
Department of Mineralogy, The Natural History Museum, Cromwell Road, London SW7 5BD, UK
A. C. Roberts
Affiliation:
Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario, Canada KIA 0E8
M. Bonardi
Affiliation:
Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario, Canada KIA 0E8
E. A. Moffatt
Affiliation:
Canadian Conservation Institute, 1030 Innes Road, Ottawa, Ontario, Canada K1A 0C8

Abstract

Feinglosite, the zinc analogue of arsenbrackebuschite, was found lining a cavity in a sample of massive chalcocite from Tsumeb, Namibia. In this cavity it is associated with wulfenite, anglesite and goethite. The mean of seven electron-microprobe analyses (wt.%) is: PbO 61.4, ZnO 7.3, FeO 1.8, As2O5 22.1, SO3 5.3, H2O (by difference) [2.1], total = [100.00]%, leading to the ideal formula: Pb2(Zn,Fe)[(As,S)O4]·H2O. Feinglosite is monoclinic, space group P21 or P21/m, a 8.973(6), b 5.955(3), c 7.766(6) Å, β 112.20(6)°, with Z = 2. The strongest five reflections of the X-ray powder diffraction pattern are [d in Å (I) (hkl)]: 4.85 (50) (110), 3.246 (100) (112), 2.988 (60) (301), 2.769 (60) (300/211), 2.107 (50) (321). The mineral is pale olive-green, transparent, sectile, and has a white streak and adamantine lustre. It overgrows clusters of goethite crystals and forms globular microcrystalline aggregates up to 0.5–0.75mm in size. The hardness on Mohs' scale is 4–5: the mean micro-indentation hardness is 263 at VHN100. Its calculated density is 6.52 g cm−3. The mineral is pale brownish grey in reflected light (when compared with goethite). Visible spectrum reflectance data are presented. Feinglosite is named for Mark N. Feinglos who first recognised the mineral on a specimen in his collection.

Type
Mineralogy
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1997

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Footnotes

*

Present address: I.S.D.G.M., S. Polo 1364, 30125 Venice, Italy

References

Abraham, K., Kantz, K., Tillmanns, E. and Walenta, K. (1978) Arsenbrackebuschite, Pb2(Fe,Zn)(OH,H2O) [AsO4]2, a new arsenate mineral. Neues Jahrb. Mineral., Mh., 193-6.Google Scholar
Hofmeister, W. and Tillmanns, E. (1978) Strukturelle Untersuchungen an Arsenbrackebuschit. Tschermaks Mineral. Petrog. Mitt., 25, 153-63.CrossRefGoogle Scholar
Roberts, A.C., Ercit, T.S., Criddle, A.J., Jones, G.C., Cureton, F.F. II and Jensen, M.C. (1994) Mcalpineite, Cu3TeO6.H20, a new mineral from the McAlpine mine, Tuolumne County, California, and from the Centennial Eureka mine, Juab County, Utah. Mineral. Mag., 58, 417-24.CrossRefGoogle Scholar