Tetrahedrite-(Mn)
Chemical formula: Cu<sup>1+</sup><sub>6</sub>(Cu<sup>1+</sup><sub>4</sub>Mn<sup>2+</sup><sub>2</sub>)Sb<sup>3+</sup><sub>4</sub>S<sup>2-</sup><sub>13</sub>
A rare sulfosalt from the tetrahedrite group, in which manganese is the dominant divalent metal, forming black, metallic crystals.
Properties
- Mohs hardness
- 3.5-4
- Luster
- Metallic
- Streak
- Black
- Density
- 4.9-5.1
- Cleavage
- None
- Fracture
- Uneven to sub-conchoidal
- Transparency
- Opaque
- Crystal system
- Cubic
Diagnostic features
## Identification Visual identification of tetrahedrite-(Mn) is impossible without chemical analysis. In the field or in a collection, it can be identified as a member of the tetrahedrite group based on its regular crystallographic system, crystal form (tetrahedra), steel-gray to black color, metallic luster, and black streak. It is relatively soft and brittle. ## Distinguishing from Similar Minerals It can be confused with other members of the tetrahedrite group (such as tetrahedrite-(Fe), tetrahedrite-(Zn), tennantite), as well as with other black, metallic sulfides and sulfosalts, such as sphalerite, galena, or chalcopyrite. It differs from sphalerite by its black streak (sphalerite has a light streak), and from galena by the lack of distinct cleavage and lower density. Final distinction within the tetrahedrite group requires chemical composition analysis (e.g., by EDS method). ## Crystal Forms Crystals most often occur as tetrahedra, often with modifications of other faces. They can form twins. It also occurs in granular, massive aggregates or as inclusions in other minerals.
Geological environment
## Genesis Tetrahedrite-(Mn) forms in low- to medium-temperature hydrothermal ore veins. It is an accessory mineral in polymetallic deposits, often associated with precious metals. ## Mineral Associations It most commonly co-occurs with other sulfides and sulfosalts, such as pyrite, chalcopyrite, sphalerite, galena, tennantite, as well as with quartz, barite, dolomite, and other vein minerals. ## Localities As a member of the tetrahedrite group, it is a widely distributed mineral, but specimens specifically identified as tetrahedrite-(Mn) are much rarer. Confirmed occurrences include the Uchucchacua mine in Peru (an important locality), the Casapalca mine in Peru, as well as localities in Bulgaria, Japan (Akenobe mine), and Sweden (Garpenberg mine).
Rarity
Rare
For collectors
## Quality Criteria For collectors, well-formed, sharp, and lustrous crystals are most desirable, especially those with a distinct tetrahedral shape. Specimens where tetrahedrite-(Mn) crystals are embedded on a contrasting matrix (e.g., on white quartz or pink rhodochrosite) are highly valued. Crystal size, lack of damage, and attractive associations with other minerals (e.g., with hübnerite in the case of Peruvian specimens) significantly increase collectible value. ## Popular Localities The most known and prized tetrahedrite-(Mn) specimens by collectors come from the Uchucchacua mine in Oyon Province, Peru. They are characterized by exceptionally well-formed crystals, often in association with rhodochrosite, alabandite, and other manganese minerals.
Care and storage
## Cleaning Specimens should only be dry-cleaned, using a soft brush to remove dust. Compressed air can also be used from a safe distance. Avoid water and chemical agents. ## What to Avoid Tetrahedrite-(Mn) is sensitive to moisture and oxidation, which can lead to its slow decomposition and the formation of secondary minerals on the surface. Avoid contact with water, acids, detergents, and other chemicals. It should not be heated or exposed to sudden temperature changes. ## Storage It is recommended to store specimens in a dry environment, preferably in sealed boxes or display cases with a desiccant (e.g., silica gel). To prevent oxidation, some collectors store sensitive sulfides in an oxygen-free atmosphere.