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- Tetrahedrite - Wikipedia
Tetrahedrite occurs in low to moderate temperature hydrothermal veins and in some contact metamorphic deposits It is a minor ore of copper and associated metals It was first described in 1845 for occurrences in Freiberg, Saxony, Germany
- Tetrahedrite Subgroup: Mineral information, data and localities.
Although originally considered a series between tetrahedrite-(Fe)and tetrahedrite-(Zn), the two most common end-members, there are now (as of November 2023) seven IMA-recognized end-members
- Tetrahedrite Mineral Data
Comments: Bright sharp metallic tetrahedrite crystals to 1 cm in size on pinkish to colorless crystalline calcite matrix Location: Cavnic (Kapnik), Maramures, Romania
- Tetrahedrite | Copper Ore, Sulfide Crystals | Britannica
tetrahedrite, common sulfosalt mineral, an antimony sulfide of copper, iron, zinc, and silver [ (Cu,Fe,Zn,Ag) 12 Sb 4 S 13], that is an important ore of copper and sometimes of silver It forms gray to black metallic crystals or masses in metalliferous hydrothermal veins
- Tetrahedrite (Cu, Fe, Ag, Zn)12Sb4S13 - Handbook of Mineralogy
Occurrence: Typically in hydrothermal veins or contact metamorphic deposits of low to medium temperature of formation Association: Chalcopyrite, galena, sphalerite, pyrite, bornite, acanthite, calcite, dolomite, siderite, barite, fluorite, quartz Distribution: One of the most common of the sulfosalts
- Tetrahedrite — Grokipedia
Tetrahedrite is a sulfosalt mineral belonging to the tetrahedrite group, characterized by the general chemical formula (Cu,Fe)₁₂Sb₄S₁₃, where copper is the dominant cation and antimony serves as the key semimetal component [1]
- Tetrahedrite - National Gem Lab
Tetrahedrite forms a solid solution series with the rather rare mineral Tennantite (Copper Arsenic Sulfide) The two share the same crystal structure but they differ in the percentage of arsenic versus antimony Antimony rich specimens are Tetrahedrite while arsenic rich specimens are Tennantite
- Crystal chemistry of tetrahedrite - Mineralogical Society of America
Initial solution of the tetrahedrite structure was by Ma-chatschki (1928a, 1928b) who noted a marked similarity of the tetrahedrite and sphalerite powder patterns
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