绿石英

基本解释 (translations)

prase

与绿石英相关的网络例句 [注：此内容来源于网络，仅供参考]

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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

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。

The translucent stripes and bands of agates, the rich opaque green and brown of fine-grained jasper, the plant like forms of moss agate, the green and red pattern of bloodstone, the rich translucent orange-red of carnelian and apple-green of chrysoprase, and the opaque black of onyx are all faces of the versatile quartz gem.

半透明并带条纹玛瑙、绿、棕富人不透明细粒碧玉、苔藓植物喜欢形式玛瑙、绿、红格局鸡血石、富人半透明橙红色的玛瑙和苹果的chrysoprase绿、不透明和黑色的玛瑙，都面临了多才多艺石英板。

Plate and λ/2 plate were placed inside the Nd∶YVO4KTP green laser cavity with angle 90°between their fast axis.The composite plate composed of HWP,QWP and KTP has the function of QWP.The composite plate with Nd∶YVO4 can effectively suppress the coupling of polarized modes,and multi-longitudinal-mode lownoise green laser was obtained.Since the composite plate counteracted the phase shift induced by temperature sensitivity of quartz plate,the green laser operated with lownoise reliability in different output power and different operation temperature.The threelongitudinalmode, the noise of less than 0.5% and output power stability of less then 1% for 12 hour are obtained in the green laser.

介绍了一种LD泵浦腔内倍频全固体Nd∶YVO4KTP多纵模、低噪音、高功率稳定绿激光器在Nd∶YVO4KTP绿激光器组成的谐振腔内放置厚度约相等的石英晶体λ2波片和λ4波片，使两波片快轴夹角互呈90°，HWP、QWP与KTP构成复合波片，其作用相当于QWP，此复合波法与各相异性Nd∶YVO4共同作用有效抑制了腔内偏振模耦合，获得多纵模低噪音绿光输出此复合波片相互作用由于抵消了石英晶体波片温度敏感引起的相位延迟量漂移，所以此激光器在不同功率、不同工作温度下，均能稳定可靠地运转于低噪音状态实验结果为，绿光输出纵模数为3个，噪音小于0.5%，12 h功率稳定性优小于1

Results show that the Spiti shale in Zanskar terminated 15Ma later than that in southern Tibet, while the lowermost Cretaceous quartz sandstone in Zanskar appeared 18Ma later than that in southern Tibet. The age of volcanic sandstone in southern Tibet is very poorly time constraint and their deposition occurred somewhere within Berriasian～early Albian. In Thakkhola, the Chukh Group volcanic sandstone are of late Hauterivian-early Albian age (duration about 20Ma), while in Zanskar, the volcanic sandstones facies only appeared in Albian (duration of less than 10Ma). Therefore, it can be concluded that the onsets of both quartz sandstone and volcanic sandstone occurred earlier in eastern Tethys Himalayas than in western Tethys Himalayas .

侏罗纪末～白垩纪初印度大陆的北缘同时期存在大陆向上挠曲，导致陆源碎屑输入量的快速增加，石英砂岩广泛存在；早白垩世火山岩屑砂岩对应着的印度大陆北缘地层侵蚀加深，使得较深部的深成火山岩暴露并遭受侵蚀；石英砂岩和早白垩世岩屑砂岩所代表的印度大陆剥露时间在空间上的&东早西晚&，说明构造运动首先是从特提斯喜马拉雅的东部开始（大印度与澳大利亚的彻底分离），然后逐渐波及西部的，东西时间差为15～20Ma；由于地壳均衡作用，大陆分离后原先地壳挠曲转变为地壳下沉，发生强烈的构造沉降，故Albian之后沉积一套深水环境下的海绿石、磷酸盐和黑色页岩沉积。

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。

Coesite + garnet + omphacite + rutile and coesite + phengite + apatite in zircons from phengite-bearing rutile quartz eclogite.

金红石石英榴辉岩锆石中保存的典型超高压包体矿物组合为柯石英+石榴石、柯石英+石榴石+绿辉石+金红石和柯石英+多硅白云母+磷灰石。

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。

This paper has investigated the microstructures, quartz fabrics, and mineral chemistry of mylonites from the ductile shear zone of the granite-greenstone belt in Seerteng area, Inner Mongolia. Synthetic analyses reveal that the mylonites underwent four evolutionary processes of deformation and metamorphism, such as lower-amphibolite facies regional metamorphism, retrograde epidote-amphibolite facies metamorphism and deformation, progressive recrystallization and retrograde greenschist facies metamorphism and deformation.

通过对色尔腾山地区花岗绿岩带中韧性剪切带的糜棱岩显微构造、石英组构、矿物化学等综合分析，发现该区糜棱岩在经历了低角闪岩相区域变质及绿帘角闪岩相退变质变形之后，发生了不均匀进变质重结晶作用及中低绿片岩相退变质变形等几个演化阶段。

Full color, including green quartz, gray quartz, pink quartz, yellow quartz,°×, black quartz, ocean green, red peony, sorghum red, flower wood, yellow wood, white sandstone, siltstone, purple rock, jen brown plate and other varieties.

花色齐全，包括绿石英、灰石英、粉石英、黄石英、白石英、黑石英、海洋绿、牡丹红、高粱红、花木紋、黄木紋、白砂岩、粉砂岩、紫砂岩、仁棕板等品种。

与绿石英相关的网络解释 [注：此内容来源于网络，仅供参考]

aventurine：东陵石

东陵石(Aventurine)又称"冬陵石",还称"印度玉",为含铬云母的油绿石英岩,其色很美. 但现今人们则推而广泛,把地壳里一切色泽艳丽、质地致密坚韧的石英岩或次生石英统称为"东陵石".

quartz diorite：石英闪绿岩

4409,"quartz arenite","石英アレナイト" | 4410,"quartz diorite","石英闪绿岩" | 4411,"quartz keratophyre","石英角斑岩","石英ケラトファイアー"

quartz dolerite：石英煌绿岩

石英闪长斑岩 quartz-diorite-porphyry | 石英煌绿岩 quartz-dolerite | 石英霏细岩 quartz-felsite

greenstone belt：绿岩带

"南非的绿岩带(Greenstone Belt)刚好有这种岩石:其中的石英晶体不到两毫米长,根植于石英晶体中含铁磁铁矿为纳米级大小. 塔都诺说:"石英起到了完美的'太空舱'的作用,它没有受到后来事件的影响,但它里面包含有那些我们需要研究的铁. "

Brazilian pebble：巴西石英

Brazilian emerald | 绿碧硒, 绿电气石 磷铝钠石 | Brazilian pebble | 巴西石英 | Brazilian province | 巴西部

prase：绿石英

prartition 磁盘分区 | prase 绿石英 | praseodymium 镨

prase：葱绿玉髓;绿石英

practical unit 实用单位 | prase 葱绿玉髓;绿石英 | praseodymium halide 镨卤化物

verd antique：古绿岩;蛇纹大理岩

"发金红石(石英包体)","Venus hair" | "古绿岩;蛇纹大理岩","verd-antique" | "古绿岩;蛇纹大理岩","verde antique"

glauconitic quartzarenite：海绿石石英砂岩

海绿石 glauconite | 海绿石石英砂岩 glauconitic quartzarenite | 海绵[体] sponge

quartz keratophyre：石英角斑岩","石英

4410,"quartz diorite","石英闪绿岩" | 4411,"quartz keratophyre","石英角斑岩","石英ケラトファイアー" | 4412,"quartz latite","石英レータイト"