Chemistry:Aurostibite
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Aurostibite | |
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Aurostibite found in the Czech Republic | |
General | |
Category | Sulfide minerals |
Formula (repeating unit) | AuSb 2 |
Strunz classification | 2.EB.05a |
Crystal system | Isometric |
Crystal class | Diploidal (m3) H-M Symbol: (2/m 3) |
Space group | Pa3 |
Identification | |
Formula mass | 440.47 g/mol |
Color | White to grey with bornite-like tarnish |
Cleavage | Indistinct |
Tenacity | Brittle |
Mohs scale hardness | 3 |
|re|er}} | metallic |
Diaphaneity | Opaque |
Specific gravity | 9.98 |
References | [1][2][3] |
Aurostibite is an isometric gold antimonide mineral which is a member of the pyrite group. Aurostibite was discovered in 1952 and can be found in hydrothermal gold-quartz veins, in sulfur-deficient environments that contain other antimony minerals. The mineral can be found in Yellowknife in the Northwest Territories of Canada , and the Timiskaming District in Ontario, Canada. Antimonides are rare and are normally placed in the sulfide class by mineralogists.
See also
References
Original source: https://en.wikipedia.org/wiki/Aurostibite.
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