Kitkaite
Chemical formula: NiTeSe
Kitkaite is a very rare nickel selenide-telluride, occurring as microscopic, metallic grains in hydrothermal deposits.
Properties
- Luster
- Metallic
- Streak
- Black
- Density
- 8.18
- Cleavage
- Perfect on {0001}
- Transparency
- Opaque
- Crystal system
- Trigonal
Diagnostic features
## Identification Amateur identification of kitkaite is impossible. Recognition is based on chemical analysis of its composition (ratio of nickel, selenium, and tellurium) under laboratory conditions. A preliminary indication may be its occurrence in association with other rare selenides and tellurides in a specific geological environment. ## Distinguishing from Similar Minerals Kitkaite is visually indistinguishable from many other rare minerals with a metallic luster, such as sederholmite, mäkinenite, clausthalite, or other nickel tellurides and selenides. Definitive differentiation requires quantitative analysis of the elemental composition. ## Crystal Forms Most often, it forms irregular, microscopic grains embedded in other minerals. Less commonly, small, hexagonal lamellae or plates are observed.
Geological environment
## Genesis Kitkaite is a hydrothermal mineral, crystallizing under low-temperature conditions. It forms in calcite-uraninite veins cutting metamorphic rocks or within differentiated mafic and ultramafic intrusions. ## Mineral Associations This mineral co-occurs with other rare selenides and tellurides. Its typical associated minerals include: sederholmite, wilkmanite, mäkinenite, penroseite, clausthalite, as well as uraninite, calcite, karelianite, and pyrite. ## Localities The most important localities for this very rare mineral are: - Kuusamo, Finland (type locality). - Uranium deposits in the Athabasca Basin, Saskatchewan, Canada (including Key Lake and Eagle Point mines). - Příbram district, Czech Republic. - Hope's Nose, Devon, England.
Rarity
Very rare
For collectors
## Quality Criteria The quality of kitkaite specimens is not assessed based on aesthetics, but on scientific and documentary value. The most valuable samples are those in which the presence of the mineral has been confirmed by chemical analysis. An additional advantage is the rich association with other rare selenides and tellurides on a single rock fragment. ## Popular Localities The most known and best-documented specimens, in scientific and collecting circulation, come from hydrothermal uranium veins in the Athabasca Basin, Canada, and from the type locality in Kuusamo, Finland.
Care and storage
## Cleaning Kitkaite specimens are typically microscopic grains embedded in the host rock. They do not require and should not be subjected to mechanical or chemical cleaning. If necessary, dust can be gently removed with compressed air. ## What to Avoid Contact with acids and other chemicals that can destroy the mineral should be strictly avoided. As a selenide-telluride, it is susceptible to oxidation, so it should be protected from moisture and sudden temperature changes. Brittle grains are sensitive to any mechanical damage and abrasion. ## Storage Kitkaite specimens are best stored under stable conditions, in sealed "micromount" containers, which protect them from dust, moisture, and physical damage.