Huanghoite-(Ce)
Chemical formula: BaCe<sup>3+</sup>(CO<sub>3</sub>)<sub>2</sub>F
A rare mineral from the carbonate group, a barium and cerium fluorocarbonate, forming tabular or pyramidal crystals with a yellowish hue.
Properties
- Mohs hardness
- 4.5-5
- Luster
- Vitreous to greasy
- Streak
- White
- Density
- 4.42-4.58
- Cleavage
- Perfect on {0001}
- Fracture
- Conchoidal to uneven
- Transparency
- Transparent to translucent
- Crystal system
- Trigonal
Diagnostic features
## Identification Helpful identification features include: characteristic crystal habit (hexagonal tablets, sharp pyramids), typical yellowish coloration, vitreous or slightly greasy luster, and relatively high density. The environment of occurrence is crucial – it is almost exclusively found in carbonatites and alkaline rocks. ## Distinguishing from Similar Minerals Huanghoite-(Ce) is visually almost impossible to distinguish from other rare REE fluorocarbonates, such as bastnäsite-(Ce), parisite-(Ce), or synchysite-(Ce), with which it often co-occurs. It is a member of the synchysite group with dominant barium. Certain identification requires advanced analytical methods, such as EDS spectroscopy or X-ray diffraction (XRD). It differs from bastnäsite by a slightly higher density. ## Crystal Forms It most commonly forms thin to thick tabular crystals with a hexagonal outline. It also occurs as steep, pyramidal and rhombohedral crystals. Crystals can form fan-like or rosette aggregates, and can also grow on each other in a parallel manner.
Geological environment
## Genesis It is a hydrothermal mineral, genetically associated with intrusions of alkaline rocks and carbonatites. It forms as a late accessory mineral in calcite or dolomite veins cutting these rocks. ## Mineral Associations Huanghoite-(Ce) often co-occurs with other rare earth minerals and minerals typical of carbonatites. Its most common associations include: aegirine, riebeckite, magnetite, barite, fluorite, calcite, dolomite, as well as other REE fluorocarbonates such as bastnäsite-(Ce), parisite-(Ce), and cebaite-(Ce). ## Localities The most important and type locality is the vast iron ore and rare earth deposit of Bayan Obo in Inner Mongolia (China). Significant specimens also come from the famous locality of Mont Saint-Hilaire in Quebec (Canada). Other reported occurrences include the alkaline massifs of the Kola Peninsula (Russia), the Amba Dongar complex (India), and the Mountain Pass deposit in California (USA).
Rarity
Rare
For collectors
## Quality Criteria Specimens with sharp, well-formed, and undamaged crystals are most highly valued. Intense, honey-yellow color, transparency, and crystal size increase the value. The attractiveness of a specimen is also enhanced by its placement on a contrasting rock matrix or co-occurrence with other rare minerals, such as parisite or bastnäsite. ## Popular Localities The Bayan Obo deposit in China and the quarries in the Mont Saint-Hilaire massif in Canada are considered the source of the world's best collector specimens. Specimens from these localities fetch the highest prices and are most sought after by collectors specializing in rare minerals.
Care and storage
## Cleaning Specimens should be cleaned very carefully, using a soft brush and distilled water. Due to its perfect cleavage, ultrasonic cleaners and strong water jets should be avoided, as they could cause delamination or cracking of the crystals. ## What to Avoid The mineral is sensitive to acids, with which it reacts violently. It should be protected from impacts and mechanical pressure due to its brittleness and cleavage. Avoid contact with strong chemicals and sudden temperature changes. ## Storage To prevent scratches and mechanical damage, huanghoite-(Ce) specimens are best stored in individual, padded boxes or display cases. When on display, ensure they have a stable base and protection from dust and direct contact with harder minerals.