Overview
Argentotetrahedrite is a silver-rich member of the tetrahedrite group of sulfosalt minerals, the silver-dominant counterpart of the familiar copper mineral tetrahedrite. The recognised species is argentotetrahedrite-(Fe), in which silver takes the leading role normally held by copper. Where it is abundant, silver-rich tetrahedrite can be an important silver ore, and the mineral is of strong interest to both economic geologists and collectors of sulfosalts.
Composition & structure
Argentotetrahedrite-(Fe) has the idealised formula Ag6(Cu4Fe2)Sb4S13, part of a complex group in which silver, copper, iron, zinc, antimony, arsenic and sulfur substitute in varying proportions. It crystallises in the cubic (isometric) system, like other tetrahedrite-group minerals, and can form tetrahedron-shaped crystals as well as massive and granular aggregates. Its precise name within the group depends on the dominant metals: an iron-dominant, silver-dominant composition is argentotetrahedrite-(Fe), distinguishing it from zinc- or arsenic-dominant relatives.
| Formula | Ag6(Cu4Fe2)Sb4S13 (argentotetrahedrite-(Fe)) |
| Crystal system | Cubic (isometric) |
| Mohs hardness | About 3.5–4 |
| Lustre | Metallic |
| Colour | Steel-grey to iron-black |
| Type locality | Defined within the tetrahedrite group following its 2019–2024 nomenclature revision |
Formation & occurrence
Like other tetrahedrite-group minerals, argentotetrahedrite forms in hydrothermal ore veins, typically alongside other sulfides and sulfosalts in deposits that also carry copper, lead, zinc and silver. Silver enrichment occurs where mineralising fluids are silver-rich, so the silver-dominant species tends to appear in polymetallic vein systems and in the silver-bearing zones of larger ore districts. It commonly occurs with minerals such as chalcopyrite, galena, sphalerite and other members of the tetrahedrite-tennantite series.
Identification & similar species
In hand specimen argentotetrahedrite is a steel-grey to black metallic mineral that closely resembles ordinary tetrahedrite and tennantite, and the silver-dominant species cannot be confirmed visually. Quantitative chemical analysis is required to establish that silver, rather than copper, is the dominant metal and to assign the correct group name. The whole tetrahedrite group was reorganised in a detailed nomenclature revision finalised in the early 2020s, which formally defined argentotetrahedrite-(Fe) and its relatives by their dominant constituents.
Notable localities & collecting
Silver-rich tetrahedrites occur in many classic silver districts worldwide, and historically such material was lumped under older varietal names like “freibergite” before modern analytical work refined the classification. Because identification depends on chemistry, labelled argentotetrahedrite specimens are most reliable when backed by analysis. For collectors, well-formed tetrahedral crystals are the most desirable, while for industry the mineral is significant mainly as a silver-bearing ore where it is sufficiently concentrated.