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Erlichmanite /OsS sub 2/, a new mineral.Natural osmium disulfide (termed erlichmanite) was recognized in two occurrences on the basis of electron probe and X-ray data. One occurrence is in grains of platinum-metal sand from California, the other in a platinum-metal nugget from Western Ethiopian laterites. California erlichmanite has Os 68.0, Ir 2.6, Rh 3.8, Ru 0.4, Pd 0.5, and S 25.2, summation of 100.5 wt. %, the number of metal atoms being 1.06 on the basis of 2.00 sulfurs. Ethiopian material has higher Rh and Ir and lower Os. Both are optically isotropic. Spotty X-ray reflections from a 15-micron particle of California erlichmanite give rise to d spacing which match those of synthetic cubic osmium disulfide. Erlichmanite is defined as a cubic disulfide in which osmium is the most abundant metal atom.
Document ID
19720030703
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Snetsinger, K. G.
(NASA Ames Research Center Space Sciences Div., Moffett Field, Calif., United States)
Date Acquired
August 6, 2013
Publication Date
October 1, 1971
Publication Information
Publication: American Mineralogist
Volume: 56
Subject Category
Geophysics
Accession Number
72A14369
Distribution Limits
Public
Copyright
Other

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