Faizievite
Chemical formula: Li<sub>6</sub>K<sub>2</sub>Na(Ca<sub>6</sub>Na)Ti<sup>4+</sup><sub>4</sub>(Si<sub>6</sub>O<sub>18</sub>)<sub>2</sub>(Si<sub>12</sub>O<sub>30</sub>)F<sub>2</sub>
An extremely rare cyclosilicate mineral, distinguished by its complex chemical composition containing lithium, potassium, sodium, calcium, and titanium.
Properties
- Mohs hardness
- 4-4.5
- Color
- Colorless
- Luster
- Vitreous
- Streak
- White
- Density
- 2.83
- Cleavage
- None
- Fracture
- Uneven
- Transparency
- Transparent
- Crystal system
- Triclinic
Diagnostic features
## Identification Identification of faizievite is only possible using advanced laboratory methods, such as X-ray microanalysis (EDS/WDS) and X-ray diffraction (XRD), due to its microscopic size and occurrence as inclusions. Visually, it is indistinguishable from many other colorless minerals. ## Distinguishing from Similar Minerals At its occurrence locality (Dara-i-Pioz Glacier), it can be confused with other colorless microminerals, such as quartz, leucite, or reedmergnerite, in which it most often forms inclusions. Certain differentiation requires specialized chemical and structural analysis. ## Crystal Forms Faizievite forms very small, isometric, rounded grains, typically 0.1 to 0.3 mm in size. No well-formed, euhedral crystals have been observed.
Geological environment
## Genesis Faizievite forms under unique geological conditions, within syenite pegmatites extremely enriched in alkaline elements. It is a mineral of the late stage of magmatic crystallization. ## Mineral Associations This mineral occurs in close association with reedmergnerite (in which it forms inclusions), as well as with microcline, aegirine, nepheline, sodalite, eudialyte, lorenzenite, wilhelminite, and pectolite. ## Localities The only confirmed locality of faizievite in the world is its type locality - the Dara-i-Pioz Glacier in the Alai Mountains, Tajikistan. This is one of the world's most famous sites for rare alkaline minerals.
Rarity
Extremely rare
For collectors
## Quality Criteria As a micromineral, the collector's value of faizievite primarily depends on the confirmation of its identity through analysis. The most valuable specimens are those where faizievite grains are relatively "large" (for a micromineral), clearly visible, and well-documented photographically and analytically. The richness of associated minerals on the same sample enhances its attractiveness. ## Popular Localities All known collector specimens come from a single location in the world: the Dara-i-Pioz Glacier in Tajikistan. This is the sole source of this mineral.
Care and storage
## Cleaning Specimens containing faizievite, typically microminerals, do not require cleaning. Any attempts at mechanical or chemical cleaning may damage the delicate mineral inclusions or the host rock. ## What to Avoid Avoid contact with chemicals, ultrasound, and extreme temperature changes. As a mineral occurring as inclusions, its stability depends on the surrounding host mineral. ## Storage Micromineral specimens, such as faizievite, are best stored in specialized, sealed boxes (micromount boxes) that protect them from dust, moisture, and mechanical damage. Avoid exposure to direct sunlight.