绿长石

基本解释 (translations)

amazonite

与绿长石相关的网络例句 [注：此内容来源于网络，仅供参考]

Through electron probe\'s analysis to the albite jade, union grinding sample thin slice under polarizing microscope observation as well as X powder crystal diffraction data analysis. Discovery like Chen zhenqiang and "System Gemology" said that secondary mineral for actinolite, green mudstone, epidote and quart.

通过对钠长石玉进行电子探针的分析，结合磨制的样品薄片在偏光显微镜下的观察以及X粉晶衍射数据分析，可知钠长石玉中的主要成分为钠长石，次要矿物为硬玉、角闪石、绿辉石、钠铬辉石；并未发现如陈振强等人以及《系统宝石学》中所说的次要矿物为阳起石、绿泥石、绿帘石、石英。

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钻石戒指收盘接触，哈尔顿花园珠宝商，经营的钻石戒指，你自己设计钻石戒指接触，预订结婚戒指、英国白金戒指、金戒指胶质，承担戒指、蓝宝石戒指接触，接触红宝石戒指，伦敦珠宝商，奢侈品珠宝交战的Tiffany戒指、社会学的Tiffany，Etoile的Tiffany，预订珠宝，手工戒指接触英国订造接触戒指，戒指手工接触，接触不同寻常戒指，豪华珠宝商，手作戒指，用手写，英国伦敦车间，哈尔顿花园钻石戒指，白金、黄金、白银全部由手工及手工大师金帜钻石戒指、钻石戒指接触英国，翡翠戒指接触，红宝石戒指接触，品味珠宝钻石罚款、质量保证金街，伦敦珠宝商，聘请黄钻石戒指，钻石戒指婚纱、钻石贴片，钻石制造先驱钻石，钻石抛光机，出色禁钻石、白金钻石戒指、钻石永恒戒指，珠宝设计师独家钻石戒指的纸牌，迪拜钻石、钻石戒指廉价迪拜白金钻石戒指，cooldiamonds，dejoria，大卫莫里斯酷钻石，凉爽设计师、黄金钻石戒指，集束钻石戒指，英国钻石戒指，白金钻石戒指接触，史永恒戒指、钻石戒指三部曲，黑色钻石戒指，钻石戒指粉红、设计师钻石戒指，红宝石钻石戒指、白金钻石戒指永恒、古董钻石戒指，周年钻石戒指，汉语石榴石、钻石金戒指接触白色，蓝宝石钻石戒指、1克拉钻石戒指，原厂制造永恒戒指、钻石戒指接触的纸牌，金刚石engagemen296、昂贵的钻石戒指，kelsall的Harriet，镶有钻石戒指、白金钻石戒指婚礼、热点钻石、钻石耳环、钻石首饰松散钻石粉红蓝宝石及粉红蓝宝石戒指，英文英国豪华珠宝、钻石伦理道德珠宝、宝石伦理、黄色钻石献血钻石、冲突钻石、清洁钻石戒指珍接触，接触红宝石戒指、蓝宝石戒指接触，接触珍珠戒指、翡翠戒指接触、玛瑙、宝石、呈色、琥珀、紫晶、红柱石、磷灰石、宋瓷、绿柱石、钻石黑、蓝钻石、褐色钻石，钻石的金丝雀、玛瑙、猫眼玉髓、香槟钻石、宝石、chrysoprase，柠檬黄，钻石白兰地、友谊集团、同性恋结婚戒指，同性恋friendsh叶珊瑚、茱、刚玉、长征-立方氧化锆、demantoid石榴石、祖母绿、长石、萤石、蛋白石火灾、石榴石、玻璃绿钻石，或haematite赤铁矿、 BBC等，hiddenite、iolite、色情、象牙、玉石、翡翠、喷气、Rappaport，kunzite、晕、蜜腊、铁矿、硅石、钾长石、morganite、玉、玛瑙、蛋白石、橙色钻石，padparascha或padparadscha、珍珠、橄榄石、粉红色钻石，prase，紫色的钻石，水晶，红色钻石，镶嵌水晶、玫瑰石英、宝石、红宝石、蓝宝石、可持续农业、sardonyx，榍，尖晶石、锂、星光宝石，sunstone，Tanzanite、黄玉、topazolite、乌龟、电气石、tsavolite、绿松石、黄钻、锆石、晶石

The presence of REE tetrad effects in apatites and whole rocks of S-type granites has been reported by Sha and Chappell (1999) and Zhao et al.(1999), respectively. The REE tetrad effect in minerals, such as apatite, spessartite, beryl, alkali feldspar and spodumene, from all zones of Altay No. 3 pegmatite has been found remarkable, and the fractionations among isovalent incompatible elements in these minerals are also significant. This paper puts forward that the REE tetrad effect is one of the basic features of peraluminous melts and the origin of REE tetrad effect might be probably related to some processes prior to the formation of pegmatite magma. The immiscibile liquid separation between silicate melt and hydrosaline melt may be responsible for it.

由于阿尔泰3号伟晶岩脉各带磷灰石以及与其共生的石榴石、绿柱石、碱性长石、锂辉石矿物均存在明显的稀土"四重效应"以及相同电价、相似离子半径的不相容元素间存在显著的分异，并结合最近赵振华等(1999)和Sha and Chappell(1999)报道S型花岗岩全岩和单矿物(磷灰石、独居石、长石、黄玉等)均存在稀土"四重效应"这一现象，本文研究提出，稀土"四重效应"是富挥发分过铝质岩浆体系的一个基本特征，其机制既不可能由含稀土的副矿物早期结晶引起残余熔体相中REE含量变化的结果，也不能定性地归因于流体相与熔体相相互作用过程中稀土元素在流体/熔体之间分异的结果，而很可能与伟晶岩岩浆形成之前某些过程密切相关，S型花岗岩岩浆在液相线以上存在硅酸盐熔体与高盐熔体的不混溶液相分离有可能是过铝质岩浆体系产生稀土"四重效应"的主要原因。

On the Ute Indian Trail out of Salida that went to Manitou Springs near Colorado Springs, one can find peridot , epidote, pink and white quartz, muscovite, biotite and gold mica, pink feldspar, pyrite, magnetite, hematite, limonite, white and gray marble, gold, beryl, black obsidian "Apache Tears", red garnets and topaz.

在乌特印度径出萨利达是到马尼图斯普林斯科罗拉多斯普林斯附近，人们可以找到橄榄石，绿帘石，粉红色和白色的石英，白云母，黑云母和金云母，粉红色的长石，黄铁矿，磁铁矿，赤铁矿，褐铁矿，白色和灰色大理石，黄金，绿柱石，黑色黑曜石"阿帕奇泪"，红色的石榴石和黄玉。

Field obserbation and laboratory study indicate the main type of rock alterationwere K-feldsparization, biotitization, sericitization, silication, epidotization,chloritization and carbonatization. From early to late, these alteration could dividedinto three epochs: early-stage was K-feldsparization-biotitization, middle-stage wasquartzification -sericitization, late-stage was silication, carbonatization, epidotizationand chloritization.

通过野外观察及室内研究表明，围岩蚀变类型主要有钾长石化、黑云母化、绢云母化、硅化、绿帘石化、绿泥石化和碳酸盐化，从早至晚可分为三期：早期为钾长石-黑云母化；中期为石英-绢云母化；晚期为硅化、碳酸盐化和绿泥石、绿帘石化。

A green variety of microcline, often used as a semiprecious stone .

天河石，绿长石一种绿色微斜长石，常用作半宝石

The tectonic rocks along the fault zone are composed of cataclastic rocks and mylonites formed in higher, middle and lower temperature. Respectively, both of structural features and rocks have the features of multiple phase's of deformation. The deformation features of main minerals in the high temperature mylonites show that: the quartz has the form of long single crystal and the fabric feature of point maximum near X axis; the feldspar has the form of recrystallization assemblage, They present a high amphibolite-granulite facies with temperature ＞600℃ and depth ＞20km. The deformation features of mylonites formed in middle temperature show that: the quartz has the form of polycrystal banding and the fabric feature of point maximum near Y axis and small circle girdle with Y rotational axis; the feldspar has the form of a coremantle structure, They reflect a high greenschist-lower amphibolite facies with temperature from 400℃ to 600℃ and depth from 15km to 20km.

其中，高温糜棱岩主要矿物变形特征组合为：石英为长矩状或长条状单晶、组构为近X轴的点极密，长石为几乎完全重结晶的集合体，形成温度＞600℃，相当于高角闪岩—麻粒岩相，形成深度＞20km；中温糜棱岩主要矿物变形特征组合为：石英为多晶条带、组构为近Y轴点极密和以Y轴为旋转轴的小圆环带，长石发育核幔结构，形成温度为400～600℃，相当于高绿片岩—低角闪岩相，形成深度为15～20km；低温糜棱岩主要矿物变形特征组合为：石英发育核幔结构、组构特征为近Z轴点极密，长石以碎裂为主，形成温度＜400℃，相当于中低绿片岩相，形成深度为8～12km；碎裂岩则主要代表了地表浅层的变形。

The coesite-diamond-bearing eclogite distributed in the northern part of the UHPM belt suffered three stages of metamorphism. The first stage is the Ep amphibolite facies metamorphism, which is represented by the paragenesis of phe+Qtz+Cro/Bar Bar+Ep+Ab occurred as inclusions in Grt and Omp; The second stage is the peak metamorphism of eclogite facies with mineral assembledge of Grt+Omp+Coe±Dia±Ky±Zo±Phe+Rt. The P -T condition is 800±50℃,≥28Kb; The third stage is the amphibolite facies retrograded metamorphism from the peak one, which can be divided intothe early amphibolite facies stage with the mineral assembledge of Amp+ Pl+Di+Qtz±Ep+Ilm/Ttn and the late greenschist facies one with the mineral assembledge of Ep+Chl+Bi+Tr+Ab.

分布于超高压变质带北侧的柯石英榴辉岩经历了3个阶段的变质作用：(1)早期绿帘—角闪岩相阶段，以出现在石榴石和绿辉石中的包体矿物多硅白云母、石英、冰蓝闪石或青铝闪石、钠长石等为代表；(2)峰期柯石英榴辉岩相阶段，其矿物组合为Grt+Omp+Ky+Phe±Zo+Coe±Dia+Rt，其变质温度压力为800±50℃，≥28Kb；(3)退化变质作用阶段，早期为角闪岩相，以Amp+Pl+Di±Ep+Qtz+Tit等退变矿物组合为代表；晚期为绿片岩相，以绿帘石、绿泥石、黑云母、透闪石及钠长石等矿物为代表。

"The earliest Egyptian bead s (c. 4000 BC) were made of stone, feldspar, lapis lazuli, carnelian, turquoise, hematite, or amethyst and were variously shaped (sphere, cone, shell, animal head)."

最古的埃及珠饰年代约为公元前4000年，一般为石制(绿长石、杂青金石、光玉髓、绿松石、赤铁矿和紫晶)，形状有球形、圆柱形、贝壳形或动物头形。

"The earliest Egyptian beads (c. 4000 BC) were made of stone, feldspar, lapis lazuli, carnelian, turquoise, hematite, or amethyst and were variously shaped (sphere, cone, shell, animal head)."

最古的埃及珠饰年代约为公元前4000年，一般为石制(绿长石、杂青金石、光玉髓、绿松石、赤铁矿和紫晶)，形状有球形、圆柱形、贝壳形或动物头形。

与绿长石相关的网络解释 [注：此内容来源于网络，仅供参考]

amazonite：天河石, 绿长石

Alexandrite 紫翠玉 | Amazonite 天河石, 绿长石 | Amber 琥珀

Feldspar, Amazonite 1：绿长石,天河石 1

Feldspar, Albite 1.525 长石,钠长石 1.525 | Feldspar, Amazonite 1.525 绿长石,天河石 1.525 | Feldspar, Labradorite 1.565 拉长石 1.565

blue elvan：绿岩

青土 blue earth | 绿岩 blue elvan | 天蓝石,蓝长石 blue feldspar

grossularite：钙铝榴石(绿榴石)

uvarovite 钙铬榴石 | grossularite 钙铝榴石(绿榴石) | albite 钠长石

Feldspar, Labradorite 1：拉长石 1

Feldspar, Amazonite 1.525 绿长石,天河石 1.525 | Feldspar, Labradorite 1.565 拉长石 1.565 | Feldspar, Microcline 1.525 微斜长石 1.525

Moldavite 1：捷克玻陨石,绿玻陨石 1

Methanol 1.329 甲醇 1.329 | Moldavite 1.500 捷克玻陨石,绿玻陨石 1.5 | Moonstone Adularia 1.525 月长石,冰长石 1.525

unakite：绿帘花岗岩

花绿石:即绿帘花岗岩(unakite)又称"尤纳克石",因产自美国北卡罗来纳州的Unaka山区而得名. 是一种含绿泥石、绿帘石及钠长石的花岗岩. 津巴布韦和坦桑尼亚也有出产. 拥有丰富的色泽和变幻莫测的优美纹理.

allalinite：蚀变辉长石

"绿辉矿","allagite" | "蚀变辉长石","allalinite" | "褐帘石","allanite; cerine; orthite"

bytownite：倍长石地质

byssolite 绿石棉 | byssus 足丝 | bytownite 倍长石地质

teschenite：沸绿岩

另外,霞斜岩(theralite)可用于霞石辉长岩.沸绿岩(teschenite)可用于方沸辉15 区- 本区岩石的基本名称为副长石深成岩(foidolite)与副长石火山岩(foidite).