晶簇是指由生長在巖石的裂隙或空洞中的許多礦物單晶體所組成的簇狀集合體，它們一端固定于共同的基地巖石上，另一端自由發(fā)育而具有良好的晶型。晶簇可以有單一的同種礦物的晶體組成，也可以由幾種不同的礦物的晶體組成。
晶簇種類
石英晶簇、方解石晶、白晶簇、源質(zhì)晶簇、草酸鈣簇、晶花團晶簇、晶洞晶簇
折疊 晶簇特點
折疊 晶簇特性
SiO2
晶系:六方晶系
硬度:7
比重:2.60
折射率:1.54-1.55
The cluster is a cluster aggregate composed of many mineral single crystals grown in the rock fracture or cavity, one end of which is fixed on the common base rock, and the other end is free development and has good crystal form. The crystal clusters can be composed of a single crystal of the same species, and can also be composed of several different minerals. Types of clusters
石英晶簇、方解石晶、白晶簇、源質(zhì)晶簇、草酸鈣簇、晶花團晶簇、晶洞晶簇
Shi Yingjing, Shi Jing, Bai Jingcu, calcite cluster elementium druse, clusters of calcium oxalate crystal flowers, crystal cluster and geode Crystal Cluster
折疊 晶簇特點
Characteristics of folded crystal clusters
有無色、煙色、茶色、黃色、綠色、墨色
A colorless, brown, brown, yellow, green, black
折疊 晶簇特性
Folding characteristics of clusters
SiO2
SiO2
晶系:六方晶系
System: Six Party System
硬度:7
Hardness: 7
比重:2.60
Specific gravity: 2.60
折射率:1.54-1.55
Refractive index: 1.54-1.55 |
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