Biraite-(Ce)
Chemical formula: Ce<sup>3+</sup><sub>2</sub>Fe<sup>2+</sup>Si<sub>2</sub>O<sub>7</sub>(CO<sub>3</sub>)
Biraite-(Ce) is a very rare silicate group mineral, distinguished by a unique combination of cerium, iron, and a carbonate group in its structure.
Properties
- Mohs hardness
- 4
- Luster
- Vitreous
- Streak
- Yellowish
- Density
- 4.85
- Cleavage
- Good on {100}
- Fracture
- Uneven
- Transparency
- Translucent
- Crystal system
- Monoclinic
Diagnostic features
## Identification Identification of biraite-(Ce) is only possible using advanced analytical methods, such as Raman spectroscopy, X-ray diffraction (XRD), and chemical analysis (EDS/WDS). In field conditions or a typical collection, recognizing it "by eye" is impossible. Its characteristic feature is its occurrence in a specific geological environment – skarns. ## Distinguishing from Similar Minerals Due to its microscopic size and color, it can be confused with many other rare silicates found in skarns. Definitive differentiation requires specialized laboratory analysis. ## Crystal Forms Biraite-(Ce) forms very small, thin, tabular or platy crystals, often gathered in irregular aggregates. The crystals are too small to observe details of their structure with the naked eye.
Geological environment
## Genesis Biraite-(Ce) forms in skarns, which are metamorphic rocks created at the contact of magmatic intrusions (in this case, granites) with carbonate rocks (limestones). It is a product of metasomatic processes occurring at high temperatures. ## Mineral Associations This mineral coexists with other minerals typical of skarns, such as andradite (melanite variety), hedenbergite, wollastonite, microcline, titanite, fluorite, as well as rarer cerium minerals like bastnäsite-(Ce) and allanite-(Ce). ## Localities The only confirmed locality of biraite-(Ce) in the world is its type locality – the Bira iron deposit, in Khabarovsk Krai in the Russian Far East.
Rarity
Extremely rare
For collectors
## Quality Criteria The quality of a biraite-(Ce) specimen is primarily assessed based on the richness and quantity of the mineral itself on the rock matrix, as well as its association with other well-formed minerals. Since the crystals are microscopic, their individual form or color is less significant than the confirmed presence and abundance in a given cluster. The most valuable specimens are those with the highest concentration of yellow biraite-(Ce) aggregates on a contrasting background of the host rock. ## Popular Localities The only source of specimens is the type locality in Russia. Material from this location is extremely difficult to obtain and appears on the collector's market sporadically.
Care and storage
## Cleaning Due to its extreme rarity and fragility, biraite-(Ce) specimens should not be cleaned mechanically or chemically. Any contaminants are best left undisturbed. If absolutely necessary, compressed air can be used from a safe distance to remove loose dust. ## What to Avoid Avoid contact with all chemicals, including acids and bases, which can damage the mineral. It should be protected from ultrasound, high temperatures, and sudden thermal changes. Specimens are very brittle and susceptible to mechanical damage. ## Storage Biraite-(Ce) specimens should be stored exclusively in specialized, sealed "micromount" boxes to protect them from dust, humidity, and physical damage. Avoid exposure to direct sunlight.