查询词典 garnet-red

Natural garnet powder is based on the material of natural almandine with modern technique.

是以天然铁铝石榴子石矿为原料，按现代工艺技术精制而成。

The Ds of amphibole, clinopyroxene and garnet are consistent with the previous studies under similar conditions, which indicates that the state of the starting material has little effect on the Ds between minerals and melt.

这说明无论实验的初始物质是粉末状还是块状，对元素的分配没有太大的影响。

By the detailed geological survey in the field, the garnet-bearing amphibolite and gneiss enclaves were discovered in the Tongbai complex.

通过详细的野外地质调查，在桐柏杂岩中发现了含有石榴石的斜长角闪岩和片麻岩包体。

Based on the mineral distribution and assemblage in the run products at 1035 GPa and 950 ℃ for 20300 h, the textural development of amphibolite during the partial melting process, the metamorphic reaction, and the garnet corona generation are discussed.

依据实验产物的矿物组合和新生矿物的分布特征，讨论了950℃、10~35 GPa、恒温(20~300 h)条件下，斜长角闪岩部分熔融过程的结构变化、变质反应以及石榴石冠状体的成因。

The large volume of garnet granite is possibly direct products of anatexis of the Khondalite series, which is indicated by their feldspar Pb composition consistence and some petrological evidences.

花岗岩中长石Pb同位素组成显示，石榴石花岗岩是孔兹岩系部分熔融的直接产物，而淡色花岗岩不是孔兹岩系简单的部分熔融产物。

In spring 1994, first gemmy sample of grossular andradite garnet piece was brought to Idar Oberstein , Germany , which caused the sensation to the gem world.

1994年在非洲马里葡萄石的产地，发现了极其稀有美丽的钙铝榴石、钙铁榴石和红榴石，一度成为宝石爱好者的宝地。

Clogite along the eclogite boudin margin. The assemblagesof garnet , amphibole and plagioclase record retrograde

12 GPa ，t = 635 ±44 ℃。研究结果显示榴辉岩的 pT 轨迹具有"发卡"型特点，表明鱼卡榴辉岩经历了快速俯冲和

Main productions: The gem and cabochon kind: Amethyst,Swiss blue,Sky blue,Green amethyst,Pink amethyst, Grape stone,Whisky,Green lemon,Peridot,Garnet,The cottonrose store,Smoky QZ,Crystal and all kinds of natural gems.

主要生产：戒面宝石类：紫晶、瑞士蓝、天空蓝、绿紫晶、粉紫晶、葡萄石、威士忌、柠檬绿、橄榄石、石榴石、芙蓉石、茶晶、白水晶等各种天然宝石。

Well-documented Lu-Hf isotope data from the oceanic basalts show that,the starting area of magma melting for the MORBs derived from the DMM component would be in the the depth of garnet peridotite,i.e.at the depth of 80―90 km instead of less than 60 km,which is at the depth of spinel peridotite as proposed early.The HIMU component,which is characterized by its high rediogenic lead,is refered as a special mantle component differentiated at some time in geological history from the lower mantle.A correlation study of Hf-Nd isotope between the chondrite and oceanic basalts implies that no isolated primitive mantle might have remained.

大量的大洋玄武岩Lu-Hf同位素研究表明：具亏损地幔端元来源的洋中脊玄武岩岩浆部分熔融的初熔区位于石榴石稳定场深度，即深度为80-90 km的石榴石二辉橄榄岩地幔，而不是原来所认为的尖晶石二辉橄榄岩区(深度小于60 km)；以高放射成因Pb为特征的高U地幔端元应代表了下地幔物质在某一特定时期发生分异作用的结果；球粒陨石与大洋玄武岩Hf同位素对比研究表明，没有原始地幔物质能保留至今的迹象。

"It is the most abundant metallic element in Earth's crust, chiefly in bauxite, feldspars, mica s, clay minerals, and laterite. It also occurs in gemstones, such as topaz, garnet, and chrysoberyl; emery, corundum, ruby, and sapphire are crystalline aluminum oxide."

为地壳中丰度最高的金属元素，多存在于铝土矿、长石、云母、黏土等矿物和砖红壤中，也存在于宝石之内，如黄宝石、红宝石及金绿宝石；而刚玉金刚砂、深红宝石及蓝宝石则为晶透的氧化铝。

In her eyes, because that is the doorway toher heart * the place where love resides.

女人的漂亮必須從她的眼睛中去看，因為那是她心靈的窗戶和愛居住的地方

I will send some postcards to you.

我会向你发送一些明信片。