透过小小的蓝色云母，颜色从72绿变成深蓝色，然后变成紫色……就像神奇的海浪。
Through the little blue mica, colors turned 72green to dark blue, and then to purple… just like the fantastic sea waves.
通过小蓝色云母，颜色从绿色变成深蓝色，然后变成紫色。
Through the little blue mica colors turned from green to dark blue, and then to purple.
地质学家认为花岗岩是石英，长石和云母的混合物非常好。
The geologist does well to regard granite as a compound of quartz, felspar, and mica.
长石石英云母片岩与副片麻岩一起构成了古老的表壳结构。
The quartz-mica schist together with paragneiss constituted the old supracrustal series.
主要组成矿物有斜长石、黝帘石、角闪石、另有云母类矿物、榍石、葡萄石等次要矿物。
The main minerals are plagioclase, zoisite, hornblende, and the minor minerals were mica, sphene, prehnite and so on.
属于这类物质的有云母、瓷器、石英、玻璃、木材等等。
To this class of substance belong mica, porcelain, quartz, glass, wood, etc.
白云母包括白云母和少见的钠云母。
它主要由云母岩组成，但也有少量的石英岩。
It consisted mainly of micaschists, but also minor quartzites.
采用高梯度磁选可将铁锂云母从尾矿中有效分离。
Zinnwaldite can be separated effectively by the high gradient magnetic separation from the tailing.
在这些条件下，新的矿物如黑云母、透辉石和菱角石生长起来。
Under these conditions, new minerals like biotite, diopside and scapolite grew.
一种由石英和云母构成的花岗石。
绢云母是一种质优价廉的矿物填料。
干燥是绢云母生产的关键工艺之一。
它不能通过云母这样的不透水的物质。
It could not pass through material impervious to water such as mica.
与钾长石、酸性斜长石、黑云母共生。
Symbiosis with acidic potassium feldspar, plagioclase, biotite.
现在我们的云母销售网络已经遍布世界各地！
马车发出明晰的竖琴似的砰砰响声在云母般的车辙中滚动。
The seasons are come to a stagnant stop, the trees blench and wither, the wagons roll in the mica ruts with slithering harplike thuds.
云母是我们的主打产品，也是我们引以为豪的产品。
黑云母一般是镁铁质及超镁铁质岩石中的次要成分。
Biotite is a subordinate constituent of the mafic and ultramafic rocks generally.
四川丹巴白云母矿是我国开发最早的白云母矿之一。
Danba Muscovite mine, Sichuan is one of earliest Muscovite mines in China.
近矿蚀变岩石中存在石英、绢云母、白云母、钠长石和碳酸盐。
There are quartz, sericite, muscovite, albite and carbonate in near-ore altered rocks.
氟铁云母是三八面体云母类矿物新种，属铁云母的富氟类似物。
Fluorannite is a new mineral of trioctahedral mica group, belonging to the F_rich analogue of annite.
水云母是钒的主要赋存体，钒是以类质同象的形式产于水云母的晶格中。
Navajoite is as isomorphism hosting in the lattice of hydromica which is the major hosting ore for navajoite.
另外，遭受风化后的角闪石常具绿色色调，而黑云母风化后常具褐色色调。
In addition, amphibole weathering after often with green shades, and biotite weathering often with brown color.
另外，遭受风化后的角闪石常具绿色色调，而黑云母风化后常具褐色色调。
In addition, amphibole weathering after often with green shades, and biotite weathering often with brown color.
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