Olekminskite
Chemical formula: Sr₂(CO₃)₂
Olekminskite is a rare strontium carbonate, forming colorless or white, transparent crystals with a vitreous luster.
Properties
- Mohs hardness
- 3
- Luster
- Vitreous
- Streak
- White
- Density
- 3.650
- Transparency
- Transparent
- Crystal system
- Trigonal
Diagnostic features
## Identification Olekminskite can be identified by its white color, vitreous luster, and characteristic radial aggregates of small, bladed crystals. Low hardness (3 on the Mohs scale) is also an important feature. It reacts with acids, which is typical for carbonates. ## Distinguishing from Similar Minerals It can be confused with other white carbonates, such as aragonite or strontianite. It differs from aragonite in its crystallographic system (trigonal, not orthorhombic). From strontianite, with which it often co-occurs, it can be difficult to distinguish without advanced chemical analyses (XRD analysis), although strontianite more often forms acicular or prismatic crystals. ## Crystal Forms Olekminskite crystals are usually very small, with a tabular or bladed habit. They most often occur in the form of radial or fibrous aggregates and clusters, as well as thin veins in the host rock.
Geological environment
## Genesis Olekminskite is a hydrothermal mineral. It forms in the late stages of crystallization within pegmatites and carbonatite veins associated with alkaline intrusive complexes. It forms at relatively low temperatures from strontium-rich solutions. ## Mineral Associations This mineral often co-occurs with other rare minerals typical of alkaline massifs. The most common associations include quartz, microcline, aegirine, calcite, strontianite, as well as rarer minerals such as lorenzenite or tinaksite. ## Localities Olekminskite is an extremely rare mineral. Its type and main locality is the Kedrovyi alkaline massif within the Aldan Shield in Siberia, Russia. This is the only place in the world where the occurrence of this mineral in well-formed specimens has been confirmed.
Rarity
Very rare
For collectors
## Quality Criteria For collectors, the abundance and quality of olekminskite aggregates on the rock matrix are most important. Specimens with clearly formed, radial clusters of white crystals, contrasting with the darker host rock, are most valued. The size of the crystals, although always small, also affects the value – the larger and better-formed they are, the more valuable the specimen. ## Popular Localities The only source of collectible olekminskite specimens is its type locality – the Murun massif in Siberia, Russia. All specimens available on the market come from this single location.
Care and storage
## Cleaning Olekminskite specimens should be cleaned very carefully, using a soft brush to remove dust. Due to its low hardness, all scrubbing should be avoided. If liquid is necessary, distilled water is recommended, followed by thorough drying of the specimen. ## What to Avoid Olekminskite, as a carbonate, is sensitive to acids, which can damage or completely dissolve it. Contact with household chemicals should be avoided. The mineral is soft and brittle, so it must be protected from impacts and scratching by harder minerals. ## Storage The safest way to store olekminskite specimens is in separate, padded display boxes to prevent contact with other minerals. It should be protected from dust and moisture. Display should be in a closed cabinet.