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The herzenbergite-teallite series

Published online by Cambridge University Press:  05 July 2018

Luke L. Y. Chang  and
William R. Brice
Luke L. Y. Chang
Affiliation:
Department of Geological Sciences, Cornell University, Ithaca, New York
William R. Brice
Affiliation:
Department of Geological Sciences, Cornell University, Ithaca, New York
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Summary

Equilibrium relations of lead-tin sulphides in the system SnS-PbSnS2 were studied using a sealed silica-tube technique. A complete series of solid solutions forms in the system, and lattice parameters were found to vary lineally with composition. The melting temperature of the solid solution decreases with increasing amount of PbS from herzenbergite at 880 °C to teallite at 725 °C.

Evidences were found to indicate the existence of this series of solid solution in ore deposits.

Type
Research Article
Information
Mineralogical Magazine , Volume 38 , Issue 294 , June 1971 , pp. 186 - 189
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2013

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