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Biotite

_biote_

(K(Mg,Fe)3(AlSi3O10)(OH)2)

(K(Mg,Fe)₃(AlSi₃O₁₀)(OH)₂)

Biotite and muscovite are aluminum-containing silicates which cleave in thin sheets and are called micas. Biotite is a general field term for dark micas. Biotite has the general formula (K(Mg,Fe)3(AlSi3O10)(OH)2) . The presence of iron and magnesium in biotite makes it darker in color than muscovite. With a higher crystallization temperature, biotite is viewed as occurring earlier in the Bowen reaction series. Sheetlike layer-silicates are the major constituents of clays and muds.

白云母和biotite都是含铝的硅酸盐,它们以薄片状裂开,被称为云母。biotite是暗色云母的通用术语。biotite的一般化学式为(K(Mg,Fe)3(AlSi3O10)(OH)2)。biotite中含铁和镁,使其颜色比白云母更深。由于结晶温度较高,biotite被认为在Bowen反应系列中形成较早。层状硅酸盐是黏土和泥质岩的主要组成成分。
This sample from the Smithsonian Museum of Natural History shows the darker biotite with a center of the lighter muscovite. The sample is from Spruce Pine, North Carolina and is about 11 cm wide.

According to Mindat, biotite is now a discouraged name because it refers to a series of similar minerals from the mica family. The more specific mineral names annite, eastonite, phlogopite and siderophyllite are used in technical literature.

根据Mindat,生物石(biotite)现在被 discouraged,因为它指的是从云母族中一系列相似矿物中的一类。在技术文献中,更具体的矿物名称如安蒂(annite)、埃斯顿(eastonite)、磷灰石(phlogopite)和铁云母(siderophyllite)被使用。
这件来自史密森尼自然历史博物馆的样本显示了暗色的生物云母,其中心是较浅的云母。该样本来自北卡罗来纳州斯普林松 Pine,宽约11厘米。

Mindat: Biotite

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