Chatkalite
Chemical formula: Cu¹⁺₆Fe²⁺Sn⁴⁺₂S²⁻₈
Chatkalite is a very rare, metallic copper, iron, and tin sulfide mineral, found in gold and quartz deposits.
Properties
- Mohs hardness
- 4.5
- Luster
- Metallic
- Streak
- Black
- Density
- 0
- Cleavage
- None
- Fracture
- Uneven
- Transparency
- Opaque
- Crystal system
- Tetragonal
Diagnostic features
## Identification Identification of chatkalite is almost exclusively possible using advanced laboratory methods, such as chemical analysis (electron microprobe - EDS/WDS) and X-ray diffraction (XRD). Under a reflected light microscope, it is creamy white with a pinkish tint and exhibits weak anisotropy. Its small size and occurrence as inclusions make visual identification impossible. ## Distinguishing from Similar Minerals It can be confused with other rare tin sulfides, such as stannite, kesterite, or cernyite, with which it often co-occurs. Differentiation requires precise chemical analysis, as all these minerals have similar appearance and physical properties. ## Crystal Forms Chatkalite crystallizes in the tetragonal system. It occurs exclusively as anhedral, irregular grains and aggregates, without visible crystal faces.
Geological environment
## Genesis Chatkalite is a hydrothermal mineral. It forms in quartz-gold veins that cut through volcanic andesite rocks. It forms at relatively low temperatures, in association with other sulfides and sulfosalts. ## Mineral Associations It most commonly co-occurs with native gold, pyrite, chalcopyrite, sphalerite, galena, stannite, kesterite, cernyite, tetrahedrite, mawsonite, and aikinite. It often forms intergrowths with these minerals. ## Localities The only confirmed and well-studied occurrence of chatkalite in the world is its type locality – the Kairagach gold deposit in the Chatkal Mountains, eastern Uzbekistan. This is one of the rarest mineralogical sites in the world.
Rarity
Extremely rare
For collectors
## Quality Criteria The quality of a chatkalite specimen is determined almost exclusively by its presence and identifiability. Since it occurs as microscopic grains, the most important criterion is the abundance of these grains in the sample and their clear differentiation from the surrounding rock matrix. Specimens where chatkalite is intergrown with clearly visible native gold are the most desirable. ## Popular Localities The only source of specimens is the Kairagach deposit in Uzbekistan. Material from this locality is extremely difficult to obtain and appears on the collector's market sporadically, mainly circulating among specialized collectors and research institutions.
Care and storage
## Cleaning Specimens containing chatkalite, which are usually microscopic inclusions in the host rock, do not require cleaning. Any attempts at mechanical or chemical cleaning may damage or destroy the delicate mineral grains. If dust removal is necessary, a photographic air blower can be used to blow it off. ## What to Avoid Avoid contact with chemicals, acids, and ultrasonic cleaners. As a sulfide, the mineral may be sensitive to moisture and oxidation over the long term, which can lead to changes in its surface. It should be protected from extreme temperatures. ## Storage Specimens with chatkalite are best stored in stable conditions, in closed "micromount" boxes that protect them from dust, moisture, and mechanical damage. Exposure to light is not harmful, but direct sunlight should be avoided.