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蓝晶石:宝石产地、颜色及特点

【摘要】:Kyanite蓝晶石是一种硅酸铝矿物,产于片麻岩和云母片岩中,与红柱石和矽线石为同质异象变体。蓝晶石呈透明至半透明,玻璃光泽。蓝晶石以浅至深蓝色为主,也有蓝绿色和黄褐色等。世界上有许多大型的蓝晶石矿床,但极少可用作宝石。优质的宝石级蓝晶石晶体主要产自肯尼亚,深蓝色和绿色晶体主要产自美国。蓝晶石密集平行排列的内含物会导致猫眼效应。

Kyanite

蓝晶石是一种硅酸铝矿物,产于片麻岩和云母片岩中,与红柱石和矽线石为同质异象变体。三斜晶系,晶体呈长扁柱状,常见放射状集合体,晶面有平行的深色条纹。因随晶体的不同方向出现不同的硬度,故有“二硬石”之称,这也给宝石的琢磨和抛光造成一定的困难。

蓝晶石呈透明至半透明,玻璃光泽。透明晶体常被琢磨成刻面宝石,半透明晶体大多磨制成弧面宝石或扁平的串珠。

蓝晶石以浅至深蓝色为主,也有蓝绿色和黄褐色等。平行色带是它最典型的特征,往往肉眼可见。世界上有许多大型的蓝晶石矿床,但极少可用作宝石。优质的宝石级蓝晶石晶体主要产自肯尼亚,深蓝色和绿色晶体主要产自美国。

蓝晶石密集平行排列的内含物会导致猫眼效应。

·蓝晶石纤维状集合体

·蓝晶石通常出现平行色带

One of three Al SiO polymorphs—the others being sillimanite and andalusite—kyanite is a aluminum silicate that occurs primarily as flat, blade-like crystals and occasionally as aggregates of radiating columns. It is usually dark blue but can also be gray, green, brown or colorless. Kyanite’s hardness depends on the direction from which the crystal is scratched, falling between 4 and 5 on the Moh scale when scratched parallel to the c axis and falling between 6 and 7 when scratched perpendicular to it.

Kyanite is commonly color zoned.

·扁柱状蓝晶石晶体