晶簇是指由生长在岩石的裂隙或空洞中的许多矿物单晶体所组成的簇状集合体，它们一端固定于共同的基地岩石上，另一端自由发育而具有良好的晶型。晶簇可以有单一的同种矿物的晶体组成，也可以由几种不同的矿物的晶体组成。

晶簇种类

折叠 晶簇特点

折叠 晶簇特性

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、源质晶簇、草酸钙簇、晶花团晶簇、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

折叠 晶簇特点

Characteristics of folded crystal clusters

有无色、烟色、茶色、黄色、绿色、墨色

A colorless, brown, brown, yellow, green, black

折叠 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