Gold chalcogenides
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The interesting thing about gold chalcogenides is the reversal in stability going from O to S to Se to Te. For gold the tellurides are the most stable (even as minerals), the sulfide and oxide are metastable. For most other metals it is the other way around.
AuTe2 is present as a number of minerals, the most common being calaverite[?]. Calaverite[?] is the most important source of gold after native gold]].
AuSe exists in two forms, AuSe and Au2Se3.
Au2S is metastable, but mixed silver-gold sulfides like AgAuS do exist.
No studies of gold polonides have been conducted yet, as polonium is very rare in nature.
Table of contents
1 Gold tellurides
2 Gold selenides
3 Gold sulphides
Gold tellurides
Gold selenides
Gold sulphides See also