- 更多网络例句与云母相关的网络例句 [注：此内容来源于网络，仅供参考]
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Confirmation of high-pressure pelitic rocks in the north. The mineral assemblage of the early stage is gamet-Mg-rich chloritoid +phegite +quartz ±kyanite ±aragonite or gamet+Mg-rich chloritoid+phengite+paragonite+quartz, P-T conditions are 550±30℃ and 1.4～2.0GPa; the mineral assemblage of the late stage is muscovite +chlorite+quartz±albite, which undergone retrograde metamorphism of greenschist facies, P-T conditions are ＜550℃ and ＜0.6GPa.
确定北部高压变泥质岩石，早期矿物组合为石榴子石+富镁硬绿泥石+多硅白云母+石英±蓝晶石±文石或石榴子石+富镁硬绿泥石+多硅白云母+钠云母+石英，对应的温压条件为550±30℃和1.4～2.0GPa；晚期矿物组合为白云母+绿泥石+石英±钠长石，经受了绿片岩相的退变质作用，其温度小于550℃，压力低于0.6GPa。
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The Laser microprobe analysis shows that the argon isotope is evenly distributed in the muscovite. The preliminary conclusion is (1) muscovite in high-pressure metamorphic orthogneiss does not contain excess argon and can be the object for 40Ar/39Ar dating;(2) muscovite in the Qinglongshan eclogite contains large amounts of excess ...
由此得出的初步结论是：①高压变质的正片麻岩中的白云母中不含过剩Ar，这类矿物可以作为~(40)Ar/~(39)Ar同位素测年的对象；②青龙山榴辉岩中的白云母含大量过剩氩，而作为其围岩的超高压正片麻岩中的白云母却不含过剩氩，这一事实证明了榴辉岩中白云母的过剩氩不是来自围岩，而是榴辉岩自身继承的。
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In this research project, we have got a series conclusions:(1) there is no excess argon in the high-pressure white micas being in the orthogneiss;(2) The distribution of excess argon in eclogite is positive correlative with the ratio of Mg/, but negative with the ratio of Na/;(3) The in-situ analyses by using the method of laser probe 39Ar-40Ar show that the age radius from central to margin in a single grain of high-pressure white mica in eclogite;(4) There is no any evidence to prove that the excess argon in eclogite comes from fluid;(5) The excess argon in eclogite inherited from primitive rock during high-ultra high pressure metamorphism;(6) There is no excess argon in the eclogite when its surrounding rock is carbonate.
本项目用综合手段，研究了高压白云母中过剩氩的来源、赋存、分布与岩性、产状、矿物元素和矿物显微结构之间的相关关系，以确定过剩氩在高压白云母中赋存的主要控制因素。初步得出了以下结果：1、高压变质的正片麻岩中的白云母中不含过剩氩；2、高压白云母中过剩氩的赋存和Mg/有着正相关关系，而和Na/呈负相关；3、激光微区氩-氩分析表明，榴辉岩中的单颗粒多硅白云母存在年龄梯度；4、初步否定了高压白云母中过剩氩来自于流体的说法；5、初步认定，榴辉岩中多硅白云母中过剩氩主要是在高压-超高压变质过程中由内部继承的；6、在阿尔金及柴北缘等地围岩为碳酸岩的榴辉岩中的高压白云母不含过剩氩。上述研究结果将推动过剩氩成因研究走向深入。
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According to petrologic analysis of 18 samples of altered rock, phlogopite rock , with regard to its B 2O 3 content, it is generally restricted to the outside of the ore bed, having certain ties with the boron minerlization while no ties are found in altered rock of the same type associated with veins of diorite porphyrite.
其中金云母岩多分布在含矿层外带，通过对 1 8件金云母岩样品中B2 O3含量分析，表明正常蚀变岩中的金云母岩与硼矿有一定的关系，而由闪长玢岩脉体侵入影响下形成的金云母岩则与矿化无关。
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We can offer three types of this mica tape, they're HY450-5 Silicone Glass Phlogopite Mica Paper Tape, HY460-5 Silicone Glass Phlogopite Mica Paper Tape (low binder content, reinfored only on surface), HY460-5S Silicone Glass Phlogopite Mica Paper Tape.
本公司目前已具备了一定的生产能力，生产的耐火电缆用粉云母带有三种类型，其分别为HY450-5有机硅玻璃粉金云母带，HY460-5有机硅少胶单面玻璃粉金云母带和HY460-5S有机硅少胶玻璃粉金云母带。
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It is found that there is a mineral association, micro-crystal muscovite and phengite, in this deposit. The mineral assemblage contains about 80% micro-crystal muscovite and about 20% phengite. Their crystallinity is very high and their polytype is 2M1. Both of them are dioctahedral because the d and b of micro-crystal muscovite and phengite are 0.1502 nm, 0.9012 nm and 0.1505 nm, 0.9030 nm, respectively. For their d and b are larger than those of common muscovite, the reason why Fe(superscript 2+)+Fe(superscript 3+) and Mg(superscript 2+) are high in the ore is that Al(superscript 3+) in the octahedron is replaced by Fe(superscript 2+)+Fe(superscript 3+) and Mg(superscript 2+), and this is a phengite series mineral association formed through isomorphic replacement.
该矿物组合中的微晶白云母和多硅白云母结晶度高，多型为2M1，其含量分别为80%和20%左右；二者都属二八面体型白云母类矿物，但d060和b值偏大，微晶白云母的d060=0.1502nm，b=0.9012nm，多硅白云母的d060=0.1505nm，b=0.9030nm；微晶白云母矿铝含量较低、铁镁含量较高，其原因是白云母晶体铝氧八面体中的Al离子被Fe、Mg等离子所取代，这一矿物组合是通过矿物类质同象作用所形成一种多硅白云母系列矿物。
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The quality index is lower, sericite content about 85%, brightness about 80%, grain size larger and ratio to diameter to thickness small. As sericite is developed and used in more wide-ranging field, it does not meet the requirements of user anymore.
随着近几年绢云母开发水平的不断提高，绢云母粉的应用领域不断扩大，对绢云母的质量要求也不断提高，目前企业的选矿加工工艺已不能满足市场对绢云母的质量要求。
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Main nonmetal mineral products of Dalitong are as follows: Raw vermiculite (annual export about 10,000 tons), expended vermiculite (annual output 20,000 tons), white mica, mica powder and mica pieces (annual output about 6,000 tons), meroxene and mica pieces (annual output 2,000 tons), bronze mica and mica pieces (annual output 2,000 tons), natural sand (annual output over 50,000 tons), quartz sand and flour (annual output over 20,000 tons), rock slice, taltalit, medical stone, calcined kaolin and so on.
达利通主要非金属矿产品有：蛭石原矿、膨胀蛭石（年产2万吨）、白云母、云母粉、云母碎（干磨和水磨，去掉。年产6千吨）、黑云母、云母碎（年产2000吨）、金云母、云母碎（年产2000吨）、天然彩砂（年产5万吨以上）、石英砂、石英粉（年产2万吨以上）、岩片、电气石、麦饭石、煅烧高岭土等
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The advantages of Fluorphlogopite Mica are: good penetrativity of light and wave; long time operation at the temperature up to 1100°C; anticorruption of strong acid and alkali and nocuous gases; almost no loss in high frequency medium; 2000-time-smaller vacuum deflation at high temperature than inartificial mica while 1000-time-higher body resistance than inartificial mica.
氟晶云母优于其他云母的关键点在于：优秀的光、波透过率；可长期在高达1100℃的高温环境下工作；抗强酸、强碱及有害气体的腐蚀；在高频介质环境下基本没有损耗；高温真空放气量比天然云母小2000倍，体电阻率比天然云母高1000倍。氟晶云母是替代天然云母、聚四氟乙烯、石英玻璃等低性能材料的新型耐高温、高频、绝缘材料。
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The author found that the big piece-size muscovites of China are the normal muscovites; the small-size muscovites in the metamorphic rock area are mainly phengite. The Indian muscovites studied both big and small piece-size of muscovite, are normal muscovites. The surface activity of Indian muscovite substrate is higher than China ones. Acid is easy to erode paralleling to the direction of the muscovite substrate face. Although acid treating does not destroy the muscovite structure, the thermal stability of muscovite has be decreased.
研究发现我国白云母主要产地的大片白云母均为普通白云母，变质岩地区的碎白云母以多硅白云母为主；本文研究的印度的大片白云母、碎白云母均为普通白云母；印度白云母基片的表面活性高于我国白云母；酸处理容易沿平行于白云母基面的方向侵蚀，虽未使白云母晶体结构产生破坏，但造成了白云母热稳定性降低。
- 更多网络解释与云母相关的网络解释 [注：此内容来源于网络，仅供参考]
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mica cloth：云母布,云母片
mica clip 云母绝缘夹 | mica cloth 云母布,云母片 | mica collar 云母圈
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mica schist：云母片岩,云母片岩
mica ring 云母环 | mica schist 云母片岩,云母片岩 | mica schist porphyry 云母片麻斑岩
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paragonite：钠云母
钠云母(Paragonite) 钠云母是一种含水的钠铝硅酸盐,是一种云母,常和白云母共生,并与它可以其物理性质相区别,两种云母的区别在于它们的化学成份. 在钠云母中钠离子占据着白云母中钾...
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sericite：绢云母
绢云母(Sericite)是一种天然细粒白云母,属白云母的亚种,是层状结构的硅酸盐,结构由两层硅氧四面体夹着一层铝氧八面体构成的复式硅氧层. 可劈成极薄的片状,片厚可达1u以下,径厚比大;与白云母相比:具有天然粒径小,易加工超细的特点.
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sericite：绢云母 绢云母
绢云母 绢云母(Sericite)是一种天然细粒白云母,属白云母的亚种,是层状结构的硅酸盐,结构由两层硅氧四面体夹着一层铝氧八面体构成的复式硅...
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sericite schist：绢云母片岩
"绢云母片麻岩","sericite-gneiss" | "绢云母片岩","sericite-schist" | "绢云母化蚀变,绢云母质换质","sericitic alternation"
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micaceous：云母的;云母状
micaceous sandstone 云母砂岩 | micaceous 云母的;云母状 | micacization 云母化
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micacite：云母片岩,云母片岩
micaceousstructure 云母构造 | micacite 云母片岩 云母片岩 | micaclip 云母绝缘夹
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sericitic alternation：绢云母化蚀变,绢云母质换质
"绢云母片岩","sericite-schist" | "绢云母化蚀变,绢云母质换质","sericitic alternation" | "绢云母岩","sericitic rock"
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mica schist：云母片岩,云母片岩
mica ring ==> 云母环 | mica schist ==> 云母片岩,云母片岩 | mica schist porphyry ==> 云母片麻斑岩