绿尖晶石

基本解释 (translations)

chlorospinel

与绿尖晶石相关的网络例句 [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

Affordable gemstones include amethyst, citrine, spinel, many colours of garnet, blue topaz, chrome diopside, fire opal, white opal, iolite, kuzite, peridot, coral, turquoise, lapis lazuli, chalcedony, and freshwater and saltwater cultured pearls.

包括紫晶宝石得起、柠檬黄、尖晶石、石榴石多种颜色，蓝黄玉、铬透辉石、火欧泊、白欧泊、iolite、kuzite、橄榄石、珊瑚、绿松石、蜜腊、玉髓、淡水及咸水养殖珍珠。

Characteristics of these two kinds of spinels not only indicate that the whole terrain underwent granulite facies metamorphism but also provide direct mineralogical evidence for the argument that Yushugou ophiolite suite of granulite facies lies in an environment of oceanic basin.

这两类尖晶石的特征一方面说明该地体遭受了麻粒岩相的变质作用改造，另一方面也提供了榆树沟麻粒岩相蛇绿岩套属洋盆构造环境的直接矿物学证据。

This paper reports the investigation on the petrology of spinel harzburgite and olivine pyroxenite in the Darbut ophiolitic mélange, as well as the worm-like intergrowth texture composed of Cr-spinel and orthopyroxene wide-spreading in harzburgite. Our study shows that the observed intergrowth texture is not a graphic texture or a symplectite as assumed by previous research, instead, it is a product of the evolution of the Cr-rich magma formed after the melting of the primitive mantle.

通过研究西准噶尔达拉布特蛇绿混杂岩中方辉橄榄岩和橄榄辉石岩的岩石学特征，分析方辉橄榄岩广泛发育的铬尖晶石和斜方辉石构成的蠕虫状共生连晶结构的成因，得出结论认为：这种共生连晶结构不是前人所认为的文象结构或者石榴石的后成合晶，而是原始地幔岩熔融形成富铬岩浆的演化产物。

We also report the exsolution texture of Crspinel in orthopyroxene in the studied harzburgite, and suggest that it is the result of a metamorphic reaction induced by the drastic increase of oxygen fugacity during the rapid emplacement of Darbut ophiolite.

方辉橄榄岩中的斜方辉石发育铬尖晶石出溶结构，出溶棒的成分特点表明，该结构是达拉布特蛇绿岩在快速就位过程中环境氧逸度突然升高诱发变质反应的结果。

We also report the exsolution texture of Cr-spinel in orthopyroxene in the studied harzburgite, and suggest that it is the result of a metamorphic reaction induced by the drastic increase of oxygen fugacity during the rapid emplacement of Darbut ophiolite.

方辉橄榄岩中的斜方辉石发育铬尖晶石出溶结构，出溶棒的成分特点表明，该结构是达拉布特蛇绿岩在快速就位过程中环境氧逸度突然升高诱发变质反应的结果。

Based on the field survey, we analyzed geochemical characteristics of more than 500 spinel samples from the Yarlung-Zangbu ophiolites, in order to present and discuss geneses and geodynamics of the Yarlung-Zangbu ophiolites. Mineral chemistry has revealed that the Yarlung-Zangbu ophiolites are the product of suprasubduction. This conclusion is similar to that of other related researched in recent years.

在野外调查基础上，对雅鲁藏布江蛇绿岩中500多个尖晶石样品的地球化学特征进行了分析研究，以探讨蛇绿岩的成因及其动力学背景，提出雅鲁藏布江蛇绿岩带属于超俯冲作用的产物，与近年来其他研究成果的认识一致。

The ultramafic rocks outcropped at the Altyn region are all harzburgites. Remant grains of primary minerals have melted residual texture and elastic deformation texture under high temperature and pressure. The whole-rock analyses show their low TiO〓 contents (0.01～0.04%), low Al, Ca and high MgO contents and wide Mg〓 range (89.35～95.57). Rare earth patterns have two types, namely tabacco pipe-shped and LREE-shaped, of which the former is often seen. The chondrite-nomalized Yb values of these analyses are all lower than 1. The spinels have low Ti and high Cr content and most spinels have Cr# higher than 60. All of the above characteristics show that the ultramafic rocks in the Altyn fault zone are components of metmorphic peridotites of ophiolite from depleted mantle source and most ophiolites from this zone belong to supra-subduction zone type ophiolite with a few mid-ocean ridge basalt type.

阿尔金露头区的超基性岩全为方辉橄榄岩，残余的新鲜矿物颗粒发育有熔融残余结构和高温高压下塑性变形结构，全岩分析显示样品TiO〓的含量低，为0.01～0.04％，具有低的Al和Ca，MgO含量高，Mg〓为89.35～95.57；稀土配分型式有两种，即烟斗型和LREE亏损型，前者占绝大多数，Yb球粒陨石标准化后的值全都小于1；尖晶石低Ti高Cr，大部分尖晶石的Cr〓大于60，上述特征说明阿尔金超基性岩是蛇绿岩的地幔橄榄岩成员，来自亏损的地幔源区，阿尔金蛇绿岩大多属于俯冲带之上型蛇绿岩，有少量的大洋中脊型蛇绿岩。

Jasper was green or dark green, sometimes shows a black dirty points, including minerals and other impurities such as chromium spinels due.

碧玉呈绿或暗绿色，有时可见黑色脏点，是含杂质如铬尖晶石矿物等所致。

与绿尖晶石相关的网络解释 [注：此内容来源于网络，仅供参考]

chlorospinel：绿尖晶石

氯量 chlorosity | 绿尖晶石 chlorospinel | 钾氯胆矾 chlorothionite

chrome spinel：铬尖晶石

chromepidote 铬绿 石 | chrome spinel 铬尖晶石 | chromic iron 铬铁矿 同 chromite

chlorotic：萎黄病的

chlorospinel 绿尖晶石 | chlorotic 萎黄病的 | chlorous 亚氯酸的

Zeuxite：绿碧玺

Zeros 吉羅斯 | Zeuxite 綠碧璽 | Zeylanite 錫蘭石,鐵鎂尖晶石