Hostname: page-component-586b7cd67f-g8jcs Total loading time: 0 Render date: 2024-11-20T06:23:33.609Z Has data issue: false hasContentIssue false
  • English
  • Français

Watanabeite, Cu4(As,Sb)2S5, a new mineral from the Teine mine, Sapporo, Hokkaido, Japan

Published online by Cambridge University Press:  05 July 2018

M. Shimizu ,
A. Kato ,
S. Matsubara ,
A. J. Criddle  and
C. J. Stanley
M. Shimizu
Affiliation:
Department of Petrology and Mineral Deposits, University Museum, University of Tokyo, 7-3-1 Hongo, Bunkyo-ku, Tokyo 113, Japan
A. Kato
Affiliation:
Department of Geology, National Science Museum, 3-23-1 Hyakunin-cho, Shinjuku-ku, Tokyo 169, Japan
S. Matsubara
Affiliation:
Department of Geology, National Science Museum, 3-23-1 Hyakunin-cho, Shinjuku-ku, Tokyo 169, Japan
A. J. Criddle
Affiliation:
Department of Mineralogy, The National History Museum, Cromwell Road, London SW7 5BD
C. J. Stanley
Affiliation:
Department of Mineralogy, The National History Museum, Cromwell Road, London SW7 5BD
Get access Rights & Permissions [Opens in a new window]

Abstract

Watanabeite Cu4(As,Sb)2S5, in which As>Sb, is a new copper sulphosalt that occurs with quartz in a hydrothermal vein at the Teine mine, Sapporo, Hokkaido, Japan. It is silvery lead-grey in colour with lead-grey streak. VHN100 = 253-306 kg/mm2, brittle. It has no cleavage and the fracture is uneven. The measured density = 4.66(2) g/cm3. The mean of six microprobe analyses gave Cu 41.1, Ag 0.1, Mn 0.3, As 15.4, Sb 14.3, Bi 2.4, S 26.2, a total of 99.8 wt.%, corresponding to: (Cu3.94Mn0.03− Ag0.01)∑3.98(As1.25Sb0.72Bi0.07)∑2.04S4.98 (basis: total atoms = 11), or ideally, Cu4(As,Sb)2S5, with As > Sb. The X-ray powder pattern resembles that of tetrahedrite but has subsidiary diffractions and is similar to that of synthetic Cu24As12S31 (Maske and Skinner, 1971). It is indexed on an orthorhombic cell with a = 14.51 Å, b = 13.30 Å, c = 17.96 Å (all ± 0.01 Å), and Z = 16. Calculated density is 4.66 g/ cm3. It is optically similar to tetrahedrite but is grey and weakly bireflectant. No internal reflections were observed. The maximum and minimum reflectance values in air and in oil (nD = 1.515) for the COM wavelengths are: 470 nm −32.5, 31.5; 17.7, 17.0, 546 nm −32.0, 31.1; 17.0, 16.3,589 nm −31.1, 30.3; 16.1 m 15.5, 650 nm −30.0, 29.3; 15.0, 14.5%, respectively. Watanabeite forms masses composed of aggregates of minute grains up to 50 μm in diameter. Apart from some minute inclusions of emplectite, native bismuth and tennantite, it is almost monominerallic.

Keywords

watanabeitenew mineralTeine mineJapancopper sulphosalt
Type
Mineralogy
Information
Mineralogical Magazine , Volume 57 , Issue 389 , December 1993 , pp. 643 - 649
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1993

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

Criddle, A. J., Stanley, C. J., Chisholm, J. E., and Fejer, E. E. (1983). Bull. Minér., 106, 511–518.Google Scholar
Marumo, F. (1967) Z. Krist., 124, 352–368.Google Scholar
Marumo, F. and Nowacki, W. (1964). Schweiz. rain. pert. Mitt., 44, 439–454.Google Scholar
Maske, F. and Skinner, B. J. (1971). Econ. Geol., 66, 901–918.Google Scholar