- 更多网络例句与绿闪石相关的网络例句 [注：此内容来源于网络，仅供参考]
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The results indicate that the main mineral components of the jade are epidote and tremolite, and the auxiliary mineral components are quartz, calcite, chlorite, limonite and sphene.
结果显示，其主要矿物组成为透闪石和绿帘石，含有少量的石英、方解石、绿泥石、褐铁矿和榍石等，因此，将其定名为"青花玉"不恰当，建议定名为"绿帘石透闪石玉"。
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Mineral deposits; crystal structure; silicate minerals; clay minerals; amphibole minerals; epidote minerals; pyroxene minerals; micaceous minerals
关键词：矿物沉积晶体结构硅酸盐矿物粘土矿物闪石矿物；绿帘石矿物；辉石矿物；云母矿物
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Parisite is associated with secondary minerals, such as quartz, carbonate minerals, arfvedsonite, albite, chlorite, epidote and clay minerals and has intrinsic relation with reservoir.
氟碳钙铈矿常与石英、碳酸盐、钠铁闪石、钠长石、绿泥石、绿帘石、粘土矿物等次生矿物共生，并与天然气储层有着一种内在的联系。
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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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The zircon mineralogy and chronology of the eclogite show that a lot of primary inclusions of omphacite,phengite,garnet,bariosite etc.occur in the zircons,so the zircon should be formed during eclogite facies metamorphism.SHRIMP dating for zircons suggests the age of eclogite facies metamorphism range from 230 to 243Ma.
锆石矿物学和SHRIMP年代学研究表明，榴辉岩锆石中含有大量的绿辉石、多硅白云母、石榴子石、冻蓝闪石等矿物原生包裹体，锆石为榴辉岩相变质作用过程中从形成的变质锆石，锆石SHRIMP U—Pb年龄在230～243Ma之间，代表榴辉岩相变质作用的时代。
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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。
- 更多网络解释与绿闪石相关的网络解释 [注：此内容来源于网络，仅供参考]
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amphibole group：闪石类
通称之玉,今属角闪石类(Amphibole group), 缜密而温润,有白者质与透闪石(Tremolite)为近,绿者与阳起石(Actinolite)为近. 新西兰谓之绿玉者是也,今尚产和阗以北葱岭一带最有名,又产东土耳其斯坦(国外分裂者曾对我国新疆的称呼--笔者)及俄属乌拉尔山.
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Paris green：巴黎绿;乙醯亚砷酸铜
"韭闪石;钙镁闪石","Pargasite" | "巴黎绿;乙醯亚砷酸铜","Paris green" | "丹粉","Paris red"
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smaragd：纯绿柱石
smalto /玻璃马赛克/ | smaragd /纯绿柱石/ | smaragdite /绿闪石/
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smaragdite：绿闪石
smaltite 砷钴矿 | smaragdite 绿闪石 | smectite 绿土
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Smaragdite 1：绿闪石 1
Sinhalite 1.699 硼铝镁石 1.699 | Smaragdite 1.608 绿闪石 1.608 | Zirconia, Cubic 2.170 氧化锆,立体的 2.17
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QG BARKEVIKITE：棕闪石
QF ARFVEDSONITE 钠铁闪石 | QG BARKEVIKITE 棕闪石 | QH HASTINGSITE 绿钠闪石
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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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hastingsite：绿钙闪石
铝质岩|aluminous rock | 绿钙闪石|hastingsite | 绿辉石|omphacite
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QH HASTINGSITE：绿钠闪石
QG BARKEVIKITE 棕闪石 | QH HASTINGSITE 绿钠闪石 | QI KAERSUTITE 钛闪石
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smectite：绿土
smaragdite 绿闪石 | smectite 绿土 | smelting 熔解