- 更多网络例句与绿透辉石相关的网络例句 [注：此内容来源于网络，仅供参考]
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Diopside is typically white, blue, purple, brown, green, colorless and grey with a glassy luster.
透辉石典型色有白、蓝、紫、褐、绿、无色及带有玻璃光泽灰色。
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The conclusion is that celeste color relate to the mica which contain chromium, the emerald jade has the same cause, the cause of green color of the green- pink jade has some relativity to epidote, green part of the white-green jade is found that the mineral is diopside which contain mass of iron and chromium.
通过显微镜下观察、电子探针、X射线粉晶衍射等常规岩石测试方法，并结合阴极发光，得出天蓝玉与翠绿玉的绿色部分主要为含铬的云母；绿粉玉中的绿色部分颜色产生与绿帘石有关，且由于Fe的含量比较高，造成了绿色部分比较暗淡，不鲜艳，且颜色较浅；绿白玉中绿色部分，经矿物分析主要为透辉石，且Cr、Fe含量都比较高，暗绿颜色成因与透辉石有关。
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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。
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Is around ore shoots to be distribute with symmetry, that show the block and brecciated ores of the Tongmugou zinc deposit are fluid metasomatic reformed deposit.
后生流体交代岩（主要由透闪石、绿帘石、透辉石、黑云母、石英、绿泥石等矿物组成）显著受层间断层控制，它是流体交代原热水沉积层和热水沉积闪锌矿纹层而形成的，该矿床为热水沉积-流体交代改造矿床。
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Varieties of Diopside include "Russian Diopside"(a chromium-rich Diopside known for its deep green color),"Violan"(a rare blue variety found in Italy ),"Cat's Eye Diopside"(green with the effect due to inclusions of rutile needles),"Malacolite","Salaite","Dekalbite" and "Star Diopside".
透辉石的品种包括&俄透辉石&、&青辉石&、&猫眼透辉石&（因含有金红石会状包体而产生绿猫眼发光效果）、&白透辉石&、&次透辉石&、&纯透浑石&以及&星芒透辉石&。
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The article has researched occupation of ions in jadeite, diopside and omphacite in jadeite jade on the base of 222 components data. The author has calculated all theie formula and testified that ∑ and ∑ should be positive correlation.
以222点电子探针的化学成分为依据，研究了翡翠中重要组分矿物硬玉、绿辉石和钠铬辉石的离子占位，离子间交换规律等，着重讨论了透辉石—绿辉石—硬玉固溶体系列的类质同象替换，并通过对所有成分点的晶体化学式的计算，验证了∑与∑呈正相关等理论。
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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。
- 更多网络解释与绿透辉石相关的网络解释 [注：此内容来源于网络，仅供参考]
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dioptase：绿铜矿
diopside 透辉石 | dioptase 绿铜矿 | diopter 屈光度
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dioptase：透视石,绿铜矿
透辉石岩 diopsidite | 透视石,绿铜矿 dioptase | 透视石 dioptasite
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alaite：红苔钒矿
红苔钒矿 alaite | 绿透辉石 alalite | 铅灰石 alamosite
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alalite：绿透辉石
alajites 着色石 | alalite 绿透辉石 | alaqueca 血石
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alalite：绿透辉石, 淡绿辉石
alalia | 言语不清, 哑 | alalite | 绿透辉石, 淡绿辉石 | alameda | (尤指美国西南部多植杨树的)林荫散步道路
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byssolite：绿石棉,纤闪石
chrome diopside 铬透辉石 | byssolite 绿石棉,纤闪石 | twinning 双晶
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RW OMPHACITE：绿辉石
RV AEGIRINE-DIOSPIDE 霓透辉石 | RW OMPHACITE 绿辉石 | RX SODIC 钠质
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ALAMOS：偶氮磷
alalite 绿透辉石 | alamode 阿拉莫德绸 | Alamos 偶氮磷
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Alamode：阿拉莫德绸
alalite 绿透辉石 | alamode 阿拉莫德绸 | Alamos 偶氮磷
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Alagoas cotton：阿拉戈斯棉
alagai 阿拉盖绸 | Alagoas cotton 阿拉戈斯棉 | alalite 绿透辉石