Hostname: page-component-cd9895bd7-gbm5v Total loading time: 0 Render date: 2024-12-26T16:35:19.977Z Has data issue: false hasContentIssue false
  • English
  • Français

Sulphosahs of the plagionite group

Published online by Cambridge University Press:  05 July 2018

J. L. Jambor
J. L. Jambor*
Affiliation:
Geological Survey of Canada, Ottawa
Get access Rights & Permissions [Opens in a new window]

Summary

Three of the members of the plagionite group, fülöppite Pb3S8S15, plagionite Pb5Sb8S17, and semseyite Pb9Sb8S21, show linear correlations of cell volume and density versus PbS:Sb2S3 mol ratios. This relationship can be used better to define the nature of the fourth member of the group, heteromorphite, Pb7Sb8S19. The cell dimensions derived for heteromorphite are a 13·60, b 11·93, c 21·22 Å, β 90° 50′.

Type
Research Article
Information
Mineralogical Magazine , Volume 37 , Issue 288 , December 1969 , pp. 442 - 446
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1969

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

Jambor, (J. L.), 1967. Canad. Min. 9, 7-24.Google Scholar
Mozgova, (N. N.), Borodayev, (Yu. S.), and Senderova, (V. M.) 1967. Doklady Acad. Sci. U.S.S.R., 173, 141-4 (transl. of ).Google Scholar
Nuffield, (E. W.), 1946. Univ. Toronto Studies Geol. Series, 50, 49-62.Google Scholar
Nuffield, (E. W.) and Peacock, (M. A.), 1945. Ibid. 49, 17-39.Google Scholar
Palache, (C.), Berman, (H.), and Frondel, (C.), 1944. The System of Mineralogy, 1, 834, New York (Wiley).Google Scholar