Also known as fahlerz, panabase, tetrahedrite
Tetrahedrite is a copper antimony sulfosalt mineral with the formula: . It is the antimony endmember of the continuous solid solution series with arsenic-bearing tennantite. Pure endmembers of the series are rarely if ever seen in nature. Of the two, the antimony rich phase is more common. Other elements also substitute in the structure, most notably iron and zinc, along with less common silver, mercury and lead. Bismuth also substitutes for the antimony site and bismuthian tetrahedrite or annivite is a recognized variety. The related, silver dominant, mineral species freibergite, although rar
黝銅礦是一種銅、銻的硫盐礦物,分子式為(Cu,Fe)12Sb4S13,通常與銅、銀、鉛和鋅的礦物共生,雖然黝銅礦的主要成分是銅,但有的時候會被銀、鋅、汞、鐵等物質置換,例如如、黑黝銅礦(含汞)。銀黝銅礦的銀含量高達18%,所以有的时候黝銅礦也是一種很值錢的礦物。黝銅礦是1845年在德國的薩克森被鑑別出來。
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Discovered by embedding cosine similarity (sentence-transformers MiniLM, 384-dim).