Jinshajiangite
Chemical formula: BaNaFe²⁺₄Ti⁴⁺₂(Si₂O₇)₂O₂(OH)₂F
Jinshajiangite is a rare mineral from the astrophyllite group, forming tabular, reddish-brown crystals with a characteristic lamellar appearance.
Properties
- Mohs hardness
- 4.5-5
- Color
- Brown-red, yellow-red, black, black-red
- Luster
- Vitreous
- Streak
- Light yellow
- Density
- 4.2
- Cleavage
- [010] Perfect, [100] Perfect
- Fracture
- Uneven
- Transparency
- Transparent,Translucent
- Crystal system
- Triclinic
Diagnostic features
## Identification Jinshajiangite is most easily recognized by its characteristic lamellar or tabular crystal habit, often forming radial aggregates. The reddish-brown color, metallic luster, and excellent, unidirectional cleavage are key features. Crystals are flexible but not elastic. ## Distinguishing from Similar Minerals Jinshajiangite is visually almost identical to astrophyllite, which has a similar habit and color (usually more brownish-golden). Definitive differentiation requires advanced chemical analysis (EDS) to confirm the presence of barium, which is a key component of jinshajiangite but not present in astrophyllite. It can also be confused with lamprophyllite, which, however, usually has a lighter, yellowish-brown color. ## Crystal Forms This mineral forms flattened, tabular crystals with a rectangular or lath-like outline. These crystals often arrange themselves into fan-shaped, radial, or star-shaped aggregates, sometimes forming rosettes on the surface of the host rock.
Geological environment
## Genesis Jinshajiangite is an igneous mineral, crystallizing in the late stages from alkaline, silica-undersaturated melts. It occurs mainly in nepheline syenites and associated pegmatites. ## Mineral Associations This mineral often coexists with other minerals typical of alkaline environments, such as aegirine, nepheline, microcline, albite, eudialyte, lorenzenite, and lamprophyllite. ## Localities The most important and well-known localities of jinshajiangite are in Russia on the Kola Peninsula, in the Khibiny and Lovozero alkaline massifs. Most collector specimens originate from there. The mineral also occurs in the Mont Saint-Hilaire igneous complex in Quebec (Canada) and at its type locality in China (Sichuan Province).
Rarity
Rare
For collectors
## Quality Criteria The most valued specimens by collectors are those with well-formed, sharp crystals forming aesthetic, radial or star-shaped aggregates. Color contrast with a light host rock (e.g., white nepheline or albite) is important. Large, undamaged crystal rosettes fetch the highest prices. The luster and intensity of the reddish-brown color also increase the specimen's value. ## Popular Localities By far the most sought-after jinshajiangite specimens come from the alkaline massifs of the Kola Peninsula in Russia. Specimens from Mont Saint-Hilaire in Canada are also valued, but often have smaller crystals.
Care and storage
## Cleaning Specimens should be cleaned only mechanically, using a soft brush to remove dust. If necessary, compressed air can be used. The use of water is not recommended due to its lamellar, delicate structure and the potential presence of unstable associated minerals. ## What to Avoid Contact with acids and other chemicals, which can damage the mineral's surface, should be strictly avoided. Jinshajiangite is brittle and sensitive to impacts and bending. It should not be heated or exposed to prolonged strong sunlight. ## Storage Collector specimens of jinshajiangite, especially those in the form of radial aggregates, are best stored in closed display boxes to protect them from dust and mechanical damage. Due to its brittleness, it is not suitable for mounting in jewelry.