钠闪石

基本解释 (translations)

riebeckite

与钠闪石相关的网络例句 [注：此内容来源于网络，仅供参考]

Therefore, I on raise the question to Chen Zhenqiang and "System Gemology" about the albite jade chapter, and the opposite amphibole\'s subspecies have carried on the division.

因此，本人对陈振强以及《系统宝石学》上关于钠长石玉章节的钠长石玉的矿物组成以及组成矿物化学成分部分提出质疑，并对角闪石的亚种进行了划分。

This rock zone, with a NE striking, the whole length of 1 400 km and the width of 100～150 km, is characterized by not onlyalkaline rocks (analcite biotite olivine melilitites, leucititic alnoites, nephelite syenites, aegirite augite syenites, melanite syenites, riebeckite syenite and aegirite bearing quartz syenites) and alkaline granite (riebeckite granite, and aegitite augite riebeckite granite), but also a lot of syenites, monzonites and alkaline feldspar granites or miarolitic K feldspar granites.

该岩带全长约1400km，宽100～150km，不仅发育有狭义的碱性岩(方沸黑云橄榄黄长岩、白榴黄长煌斑岩、霞石正长岩、霓辉石正长岩、黑榴石正长岩和含霓石石英正长岩)和碱性花岗岩(钠闪石花岗岩、霓辉石钠闪石花岗岩)，还发育有大量的正长岩类二长岩类碱长花岗岩或晶洞钾长花岗岩。

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。

The study shows that almost all the feldspar in the alkali-granite is perthite, the host-crystal is microcline, the chadcrystal could be either albiter or oligoclase. The Alkali-amphibole is either manganese-magnesia-arfvedsonite or arfvedsonite, and all the alkali-pyroxene is aegirine.

结果表明，该区富碱花岗岩几乎所有的长石均为条纹长石，主晶为微斜长石或高微斜长石，客晶为钠长石或更长石，碱性角闪石为含锰镁质钠铁闪石或钠闪石，碱性辉石均为霓石。

Hongxing area which is locating in Yichun, southeast Heilongjiang province, is geologically at the binding site of Bulieya-Jiamusi block and Zhangguangcailing orogenic belt. The late Triassic alkali-granite of this area is composing of syenogranite, alkali-feldspar granite and sodium-amphibole and aegirine bearing alkali-granite.

黑龙江省伊春红星地区大地构造上位于布列亚－佳木斯地块和张广才岭造山带结合部位，区内出露晚三叠世碱性花岗岩，其岩石组合为正长花岗岩、碱长花岗岩、含钠闪石、霓石碱性花岗岩。

Na-rich rocks include albitite ,arfvedsonite-bearing albitite dyke,arfvedsonite dyke,and arfvedsonite-bearing .

富钠岩石包括富钠长石岩、含钠闪石钠长岩脉、钠闪石岩脉及钠闪石碳酸岩脉和钠闪石化蚀变白云岩。

The riebeckite granite in the region is formed in anorogenic setting, which is located inside the plate and relatively steady.

研究区出露的钠闪石花岗岩形成于板块内部非造山的相对稳定的构造环境。

Through detailed research on sample analysis result from energy spectrum,scanning electron microscope and ordinary optical microscope,an unusual amphibole mineral is discovered— magnesium rich arfvedsonite ,sourcing from secondary alteration of titanite,which is a very unusual mineral metasomatic alteration phenomenon,that is,natrium and ma.

通过单矿物提取获得了松辽盆地北部深层砾岩层高碱砾石中的一种光性特殊的矿物颗粒样品，通过对样品的能谱、扫描电镜、普通光学显微镜分析结果的深入研究，发现了一种罕见的闪石类矿物——富镁亚铁钠闪石。

The Baorilajinwola riebeckite granite body, located in the eastern flank of the middle section of Daxing'an Mountains, was formed in the late stage of Early Cretaceous or later.

宝日拉锦乌拉钠闪石花岗岩岩体位于大兴安岭中段东坡，形成于早白垩世晚期或更晚些。

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。

与钠闪石相关的网络解释 [注：此内容来源于网络，仅供参考]

arfvedsonite：亚铁钠闪石

areopyknometer 液体比重计 | arfvedsonite 亚铁钠闪石 | arg 放射自显影法

QG BARKEVIKITE：棕闪石

QF ARFVEDSONITE 钠铁闪石 | QG BARKEVIKITE 棕闪石 | QH HASTINGSITE 绿钠闪石

cummingtonite：镁铁闪石

镁钠闪石|magnesioriebekite | 镁铁闪石|cummingtonite | 镁铁质岩|mafic rock

hastingsite：富铁钠闪石

hartmannite 红锑镍矿 | hastingsite 富铁钠闪石 | hatchettite 伟晶蜡石

hastingsite：绿钠闪石

hastingofmaturity 加速成熟 | hastingsite 绿钠闪石 | hastingvariety 早熟品种

QH HASTINGSITE：绿钠闪石

QG BARKEVIKITE 棕闪石 | QH HASTINGSITE 绿钠闪石 | QI KAERSUTITE 钛闪石

Osannite hornblendite：钠闪石岩

"钠闪石;铁钠闪石","Osannite" | "钠闪石岩","Osannite hornblendite" | "奥森分类(火成岩)","Osann's classification"

riebeckite-quartz keratophyre：钠闪石英角斑岩

钠闪石 riebeckite | 钠闪石英角斑岩 riebeckite-quartz keratophyre | 钠闪微冈岩 paisanite

riebeckite：钠闪石

rider 导向架 | riebeckite 钠闪石 | riffle 格条

QL SODIC：钠质

QR RIEBECKITE 钠闪石 | QL SODIC 钠质 | QM AENIGMATITE 三斜闪石