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Glorius Garnets

机译:光彩石榴石

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摘要

The garnets are silicate minerals, forming a group with a shared crystallographic structure but with wide variation in chemical composition. What all of them have in common is a very regular framework structure of silicon and oxygen atoms, often giving rise to their characteristically very symmetrical crystals. Most are isometric (cubic crystal system, although the rare garnet-family member henritermierite is tetragonal), and they are relatively hard and brittle, with no cleavage planes. As a result, crushed garnet makes a good abrasive, and is still used to make some grades of "sand paper". Most of us are familiar with garnets as red, dodecahedral crystals, but they occur in all colours of the rainbow except blue.
机译:石榴石是硅酸盐矿物,形成具有共同晶体结构但化学成分差异很大的基团。它们的共同点是硅和氧原子的非常规则的框架结构,通常会产生其特征性非常对称的晶体。大多数是等距的(立方晶系,尽管稀有的石榴石家族成员变白云母是四方的),并且它们相对坚硬而脆,没有解理面。结果,石榴石碎成为很好的磨料,仍被用于制造某些等级的“砂纸”。我们大多数人都熟悉石榴石,它是红色的十二面体晶体,但是它们以彩虹中除蓝色以外的所有颜色出现。

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