Hostname: page-component-77c89778f8-cnmwb Total loading time: 0 Render date: 2024-07-17T17:53:26.018Z Has data issue: false hasContentIssue false
  • English
  • Français

A new mineral, scotlandite (PbSO3) from Leadhills, Scotland; the first naturally occurring sulphite

Published online by Cambridge University Press:  05 July 2018

W. H. Paar ,
R. S. W. Braithwaite ,
T. T. Chen  and
P. Keller
W. H. Paar
Affiliation:
Institut für Geowissenschaften (Mineralogie) der Universität Salzburg, Akademiestrasse 26, A-5020 Salzburg, Austria
R. S. W. Braithwaite
Affiliation:
Chemistry Department, University of Manchester Institute of Science and Technology, Manchester M60 1QD, Englan
T. T. Chen
Affiliation:
Mineral Sciences Laboratories, Canada Centre for Mineral and Energy Technology, 555 Booth Street, Ottawa, Ontario K1A OG1, Canada
P. Keller
Affiliation:
Institut für Mineralogie und Kristallchemie der Universität Stuttgart, Pfaffenwaldring 55, D-7000 Stuttgart 80, Federal Republic of Germany
Get access Rights & Permissions [Opens in a new window]

Abstract

Electron microprobe analysis of the new mineral scotlandite yielded Pb 72.27, S 9.95, corresponding to PbO 77.85, SO2 19.88, sum 97.73 wt.%. Secondary ion mass spectrometry showed the absence of Li, Be, B, C, N, and F, but the presence of very small amounts of Br. Infrared spectroscopy showed that the mineral is a sulphite with neither OH nor any other polyatomic anions. The empirical formula, calculated on the basis of Pb+S = 2 is Pb1.06S0.94O2.94 or ideally PbSO3.

The mineral has the following vibrations of the sulphite ion in the infrared spectrum: v3 920, 865; v1 970 (?); v2 620, 600; v4 488, 470 cm−1.

Scotlandite is monoclinic, with possible space groups P21 or P21/m. The unit cell dimensions are: a 4.542(2), b 5.333(2), c 6.413(2) Å, β 106.22(4)°, Z = 2. The strongest lines in the powder diffraction pattern are: 3.99(10) (011), 3.38(7) (110), 3.25(8) (11), 3.07(4) (002), 2.66(7) (020, 012), 2.56(4) (11), 2.24(5) (12, 102), 2.01(5)(210, 022), 1.707(4) (031), 1.538(4) (032, 004).

Scotlandite occurs as chisel-shaped or bladed crystals elongated along the c-axis, with a tendency to form radiating clusters. The following forms have been determined: {100}, {010}, {011}, {021}, {031}, and {032}. The new mineral has a pronounced cleavage along {100}, and a less good one along {010}. The crystals are pale yellow to greyish-white and colourless, sometimes transparent. Their lustre is adamantine, pearly on cleavage planes.

The mineral is optically biaxial positive, 2Vmeas. 35° 24' (Na). The refractive indices are: α ~ 2.035, β ~ 2.040, and γ ~ 2.085 (Na). Dispersion is strong, v >> r. The extinction is β//b, and α [001] = 20° (γ: [100] = 4°) in the obtuse angle β. H (Mohs) ≤ 2. D = 6.37 and calculated Dx = 6.40 g cm-3.

Scotlandite occurs in cavities in massive baryte and anglesite, and is closely associated with lanarkite and susannite; it represents the latest phase in the crystallization sequence of the associated lead secondary minerals. The label locality of the specimen is the Susanna vein, Leadhills, Scotland.

Type
Research Article
Information
Mineralogical Magazine , Volume 48 , Issue 347 , June 1984 , pp. 283 - 288
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1984

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.)

References

Blix, R. (1931) Am. Mineral. 16, 455–60.Google Scholar
Dunn, P. J., Norberg, J. A., and Leavens, P. B. (1982) Mineral. Mag. 46, 341–2.CrossRefGoogle Scholar
Foit, F. F. (1966) Am. Mineral. 51, 504–8.Google Scholar
Lutz, H. D., and El Suradi, S. (1976) Z. anorg. allg. Chem. 425, 134–44.CrossRefGoogle Scholar
Mandarino, J. A. (1965) Can. Mineral. 8, 149–58.Google Scholar
Mandarino, J. A. (1976) Ibid, 14, 498–502.Google Scholar
Odin, I. N., and Popovkin, B. A. (1967) Vestn. Most Univ., Khim. 22 (3), 100–1.Google Scholar
Penfield, S. L., and Foote, H. W. (1897) Am. J. Sci., Ser. 4, 3. 413–15.Google Scholar
Rocchiccioli, C. (1957) Compt. rend. 244, 2704–6.Google Scholar
Rucklidge, J. C, and Gasparrini, E. (1969) Specifications of a computer program for processing electron microprobe analytical data (EMPADR VII), Dept. Geol. Univ. Toronto.Google Scholar
Wilfong, R. L., and Maust, E. E. (1974) U.S. Bur. Mines, Rep. Invest. R. I. 7963.Google Scholar