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garnet相关的网络例句

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与 garnet 相关的网络例句 [注:此内容来源于网络,仅供参考]

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。

"It is the most abundant metallic element in Earth's crust, chiefly in bauxite, feldspars, micas, 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。

The results show that the film circulator can be realized from 1.0GHz to 3.0GHz by perfecting garnet film preparing technology, however, it is still needs a long time to be realized because of its restriction conditions in high frequency band.

结果表明在较低频段(1.0-3.0GHz),经过进一步完善薄膜的制备工艺,薄膜环行器的实现是可能的;而在高频段存尚存在一定的制约因素。

Garnet varies in coloration from colorless to black though it is often thought of as only red.

石榴石不同的色彩,从无色到黑色虽然这是通常被认为是唯一的红色。

Well, you can get your fill of this uniquely colored garnet in this lovely ...

那么,你就可以在这个独特的各色石榴石填补这个可爱

In the past, Garnet was important to Christians who felt it reminded them of the crucifixion of Christ.

在过去,石榴石重要的是基督徒谁觉得提醒他们对基督的受难。

The age of adakitic dacite is about 514.2±8.5 Ma, and the age of eclogite from the northern margin of Qaidam basin is 494.6±6.5 Ma. Therefore, it is considered that the slab started its subduction in Late Cambrian, that the adakitic magma was formed at the subduction depth of about 75~85 km, and that the partial melting residues with garnet facies continued subducting and finally formed eclogite in Early Ordovician.

据其地球化学研究结果并结合该区埃达克质英安岩(5 14.2± 8.5Ma)和榴辉岩(494.6± 6 。5Ma)的年龄数据,推测柴北缘板片在晚寒武世开始俯冲,俯冲板片在 75~ 85km深处开始部分熔融形成埃达克质岩浆,而熔融残留部分继续俯冲,在早奥陶世形成含石榴石残留相的榴辉岩。

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