Zinkgruvanite
Chemical formula: Ba<sub>4</sub>Mn<sup>2+</sup><sub>4</sub>Fe<sup>3+</sup><sub>2</sub>(Si<sub>2</sub>O<sub>7</sub>)<sub>2</sub>(S<sup>6+</sup>O<sub>4</sub>)<sub>2</sub>O<sub>2</sub>(OH)<sub>2</sub>
Zinkgruvanite is a very rare, dark brown to black sorosilicate mineral, discovered in the Zinkgruvan mine in Sweden.
Properties
- Luster
- Sub-metallic to greasy
- Streak
- Brownish
- Cleavage
- Perfect on {100}
- Transparency
- Opaque
- Crystal system
- Monoclinic
Diagnostic features
## Identification Identification of zinkgruvanite is impossible without advanced analytical techniques, such as Raman spectroscopy or chemical analysis using an electron microprobe (EDS/WDS). Preliminary indications may include its association with other rare minerals from the type locality (Zinkgruvan) and its dark color and submetallic luster. ## Distinguishing from Similar Minerals Macroscopically, it is indistinguishable from many other black, fine-grained oxide and silicate minerals. Definitive differentiation requires specialized laboratory analyses. ## Crystal Forms Zinkgruvanite forms very fine, elongated, lath-like crystals that combine into fan-shaped or spherical (spherulitic) aggregates.
Geological environment
## Genesis Zinkgruvanite forms as a result of metamorphic processes within iron, manganese, and zinc ore deposits. At its type locality (Zinkgruvan, Sweden), it occurs in skarns, which are metamorphic rocks formed at the contact of a magmatic intrusion with carbonate sedimentary rocks. ## Mineral Associations This mineral occurs in association with other rare minerals such as baryte, hedyphane, magnetite, filipstadite, manganoberyllite, eveite, and brandtite. It also co-occurs with more common minerals like calcite and quartz. ## Localities The only confirmed occurrence of zinkgruvanite in the world is its type locality – the Zinkgruvan mine, located near the town of the same name, in the Närke region of Sweden.
Rarity
Extremely rare
For collectors
## Quality Criteria As a microscopic mineral, the main criterion of value for a collector is the richness and quality of the aggregates visible under the microscope. The most desirable specimens are those with clearly formed, fan-shaped or spherulitic zinkgruvanite clusters, well-distinguished from the host rock. Association with other rare minerals from this locality is also important. ## Popular Localities The only source of specimens is the Zinkgruvan mine in Sweden. Collector material is extremely difficult to obtain and appears on the market very sporadically, usually from specialized rare mineral dealers.
Care and storage
## Cleaning Due to its extreme rarity and microscopic nature, zinkgruvanite specimens should not be cleaned by any mechanical or chemical means. It is best to leave them in their untouched state. ## What to Avoid Avoid any contact with chemicals, ultrasonics, as well as attempts at mechanical cleaning (e.g., with brushes), which could irreversibly damage the delicate crystals. The specimen should be protected from dust and vibrations. ## Storage Specimens should be stored exclusively in stable, sealed "micromount" boxes to protect them from physical damage and contamination. Display is only possible under a microscope.