Lobanovite
Chemical formula: K<sub>2</sub>Na(Fe<sup>2+</sup><sub>4</sub>Mg<sub>2</sub>Na)Ti<sup>4+</sup><sub>2</sub>(Si<sub>4</sub>O<sub>12</sub>)<sub>2</sub>O<sub>2</sub>(OH)<sub>4</sub>
Lobanovite is a rare, dark green to black mineral from the astrophyllite group, forming tabular crystals and radial aggregates.
Properties
- Mohs hardness
- 3
- Luster
- Vitreous to submetallic
- Streak
- Greenish brown
- Density
- 3.35
- Cleavage
- Perfect on {001}
- Fracture
- Uneven
- Transparency
- Translucent to opaque in thin fragments, Opaque
- Crystal system
- Triclinic
Diagnostic features
## Identification Characteristic features of lobanovite include its dark green to black color, tabular crystal habit, and tendency to form radial aggregates. Perfect cleavage in one direction and vitreous-metallic luster are also important indicators. ## Distinguishing from Similar Minerals Lobanovite is very similar to other minerals from the astrophyllite group, especially astrophyllite itself. Distinguishing it requires advanced analytical methods, such as chemical analysis (EDS/WDS) or X-ray diffraction (XRD), as the differences lie in the proportions of key elements (magnesium, iron, sodium). ## Crystal Forms It forms flattened, tabular, or lath-like crystals, often grouped into fan-shaped, radial, or stellate aggregates. Crystals rarely occur as single, well-formed individuals.
Geological environment
## Genesis Lobanovite is a mineral of magmatic origin. It forms in the late stages of crystallization in alkaline or peralkaline magmatic intrusions, such as nepheline syenites and associated pegmatites. ## Mineral Associations It most commonly co-occurs with minerals typical of alkaline environments, such as microcline, nepheline, aegirine, eudialyte, lamprophyllite, and other minerals from the astrophyllite group. ## Localities The type and so far main locality, from which the best-studied specimens originate, is the Khibiny Massif on the Kola Peninsula in Russia. This is a classic locality for many rare alkaline minerals.
Rarity
Very rare
For collectors
## Quality Criteria Specimens with well-formed, sharp crystals forming aesthetic, radial or stellate aggregates are most valued by collectors. Contrast with a light matrix rock (e.g., white nepheline or microcline) significantly enhances the specimen's attractiveness. The size of the aggregates and the intensity of the luster are also important. ## Popular Localities The only significant source of collectible lobanovite specimens is the Khibiny Massif on the Kola Peninsula in Russia.
Care and storage
## Cleaning Specimens should be cleaned very carefully, using a soft brush to remove dust. Due to its perfect cleavage, avoid washing under running water and using ultrasonic cleaners. If liquid is necessary, a brief immersion in distilled water and immediate drying is recommended. ## What to Avoid Avoid contact with acids and other chemicals. The mineral is brittle, so it must be protected from impacts and falls. Do not subject it to sudden temperature changes. ## Storage Lobanovite specimens are best stored in individual, padded display boxes to protect them from mechanical damage and scratching by other minerals. Avoid exposure to humid environments.