The Greatest Guide To Crystal
The Greatest Guide To Crystal
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This idea applies Similarly in one, two, and three-dimensional Areas. The complete crystal lattice can be manufactured by continuously reproducing the sample in the device cell in all directions.
③、粗抛光：是将模具压出之毛胚，以金刚石盘直接磨出成品之刻线。④、细抛光：在粗抛光之后，以抛光粉来磨成品至晶莹剔透为止。
结晶的形状非常细小，需要用显微镜才能看得清楚，外观上看起来是平滑、块状。常见最多的是各式玛瑙
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You will also find several resources that resemble crystals but are actually polycrystals. Polycrystals variety when microscopic crystals fuse collectively to sort a good. These components never consist of requested lattices.
无色水晶与无色长石因折射率和密度十分接近故较难区分。主要方法是放大检查。长石有两组极完全解理，显微镜下可见两组解理相交而成的“娱蛤状”包裹体或细直的纹理，而水晶则无解理发育，仅有时可见断续不规则的裂理。
水晶原石观赏石，从字面意义理解：观赏水晶石的原貌，即经过抛光去皮后的包裹体水晶和原色水晶，不需雕刻不求象形就具有非常高的观赏价值和收藏价值。此类水晶观赏石对质地要求非常之高，水晶晶体通透干净，颜色艳丽，意境鲜明深刻的价值就高，它的价值特点就好比钻石，实实在在石头本身的价值。
There exists a equivalent directive about crystal glass which differentiates amongst full lead crystal, direct crystal and crystal.
水晶常以晶簇、晶洞形式产出，其中水晶洞一般存在于由火山喷发而形成的巨厚熔岩流层的火成岩与玄武岩中。火山喷发时所含的气体或热水溶蚀等作用导致岩层中出现大量的孔隙，当富含硅质矿物的流体进入较薄的熔岩孔隙中，且温、压条件合适时将结晶沉淀出水晶等矿物。
Solids that have small-assortment get but deficiency prolonged-vary get are identified as amorphous. Almost any material may be manufactured amorphous by quick solidification from your melt (molten point out). This ailment is unstable, and the solid will crystallize in time. Should the timescale for crystallization is many years, then the amorphous condition appears secure.
地质学家目前为止对晶洞形成还没有广泛认同的理论，但相信晶洞可以在任何埋藏的空腔内形成。这些空腔可以是火成岩中的气泡、树根下的空穴，甚至动物挖的地洞。经过漫长时间，空腔的外壁变硬，溶解的矽酸盐或方解石沉积到内壁。再经过漫长的时间，缓慢渗入的矿物使得晶体在空腔内部结晶。
Crystallography could be the examine of crystals, and it bargains with everything from best geometric styles to seemingly random conglomerations of particles and minerals.
在透明的水晶中，隐裂纹呈亮晶晶的片状，有时还会有晕彩效应。这些裂纹是水晶在生长过程中，遇到外力挤压而在内部产生的一些隐形裂纹，隐裂纹在芙蓉石、紫水晶、白水晶球及白水晶柱中都很常见。有的裂纹后来被物质填充，形成愈合的裂纹，也就是原来的裂纹又长住了。这种裂纹对水晶的影响相对要小一些。
21You all know how if you take a crystal prism and move a beam of sunlight by way website of it, you will get a spectrum, which seems like a ongoing band of rainbow hues.