Kihlmanite-(Ce)
Chemical formula: Ce³⁺₂Ti⁴⁺O₂(SiO₄)(HCO₃)₂·H₂O
Kihlmanite-(Ce) is a very rare silicate mineral, found as small, tabular crystals in nepheline-syenite pegmatites.
Properties
- Mohs hardness
- 3
- Color
- Brown, reddish-brown
- Luster
- Vitreous to resinous
- Streak
- Pale yellowish-brown
- Density
- 3.66
- Cleavage
- on {010}
- Fracture
- Step-Like
- Transparency
- Transparent
- Crystal system
- Triclinic
Diagnostic features
## Identification Identification of kihlmanite-(Ce) is possible almost exclusively through advanced analytical methods, such as Raman spectroscopy or chemical analysis (EDS/WDS). In collector conditions, identification relies on the label and knowledge of the locality. Its tabular habit and occurrence in a specific geological environment are characteristic. ## Distinguishing from Similar Minerals It can be confused with other rare titanium and cerium silicates from alkaline massifs, such as tikhonenkovite or some minerals from the ewaldite group. Differentiation requires specialized laboratory tests. ## Crystal Forms The crystals are very small, thin, and tabular, with a hexagonal outline. They occur as single lamellae or form small, radial aggregates on the surface of other minerals.
Geological environment
## Genesis Kihlmanite-(Ce) forms in the late stages of hydrothermal processes within nepheline-syenite pegmatites, cutting through alkaline massifs. It forms in cavities and fissures of these pegmatites. ## Mineral Associations This mineral co-occurs with other rare minerals typical of this environment, such as lorenzenite, eudialyte-(Ce), cancrinite, natrolite, vinogradovite, katenaite, and tikhonenkovite. ## Localities The only confirmed occurrences of kihlmanite-(Ce) in the world are the alkaline massifs on the Kola Peninsula in Russia. It has been found in the Khibiny Massif (Mount Kukisvumchorr) and in the Lovozero Massif (Mount Karnasurt and Kedykvyrpakhk).
Rarity
Very rare
For collectors
## Quality Criteria Due to its extreme rarity, every analytically confirmed specimen of kihlmanite-(Ce) is valuable to specialized collectors of rare minerals (so-called "micromounters"). The most prized specimens are those with well-formed, even microscopic, crystals with a distinct outline, set against a contrasting background. The size of the aggregates and the abundance of occurrence on the rock matrix also increase the specimen's value. ## Popular Localities The most known and essentially sole source of specimens are the Khibiny and Lovozero massifs on the Kola Peninsula in Russia. Specimens from these localities are the standard for this mineral.
Care and storage
## Cleaning Due to the extreme rarity and small size of the crystals, mechanical cleaning is not recommended. If necessary, compressed air can be used to remove dust. Avoid contact with water and other chemicals. ## What to Avoid Avoid contact with acids, which can damage the mineral. The crystals are brittle and susceptible to mechanical damage. Do not subject it to ultrasound or sudden temperature changes. ## Storage Specimens of kihlmanite-(Ce) should be stored under stable conditions, in sealed "micromount" containers, to protect them from dust, moisture, and physical damage. Avoid exposure to direct sunlight.