闪石的

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。

On the basis of petrography and mineral chemistry of the xenoliths, the amphiboles in them can be subdivided into four kinds of occurrences ,i.e., 1 the early amphibole inclusions within garnet, being maganesio-hornblende; 2 the primary amphiboles equilibrated with omphacite and garnet in eclogite, belonging to pargasite and pargasitic hornblende; 3 the retrograde amphiboles around garnet and clinopyroxene, mainly being edenitic and actinolitic hornblendes; and 4 the exsolving amphiboles within clinopyroxenes, mainly being edenite, edenitic hornblende and/or ferroan pargasitic hornblende.

对该类捕虏体的岩相学和矿物化学研究表明，其中的角闪石具有4种产状：1位于石榴石中的早期角闪石包裹体，为镁质普通角闪石；2与榴辉岩中矿物平衡存在的原生角闪石，为韭闪石或韭闪石质普通角闪石；3位于石榴石和单斜辉石周边的退变角闪石，主要为浅闪石质和阳起石质普通角闪石；4沿单斜辉石解理分布的出溶角闪石，主要为浅闪石、浅闪石质角闪石和含亚铁韭闪石质普通角闪石。

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"。

But not beneficial to the dissolution of tremolite.

对透闪石的溶解影响不大。

Results show that the incorporation of tremolite has the function of heterogeneous nucleation to nylon 1010 crystallization. With the increase in tremolite, the crystallization rate of nylon 1010 is enhanced and the Avrami exponent n is slightly decreased.

结果表明：透闪石对尼龙1010结晶起到了异相成核的作用，尼龙1010的结晶速率随透闪石的含量的增加而提高，Avrami指数n略有降低。

Combined with the data from early investigations for glaucophane in the Zhangbaling area,and con...

结合前人对张八岭地区的&蓝闪石&的研究资料，并对比作者等对天山昭苏、库车地区和西藏羌塘地区的蓝闪石分析数据，认为张八岭地区并没有真正意义上的蓝闪石存在，张八岭群中&蓝片岩&是否存在以及是否经历低温高压变质作用需要进一步的详细研究。

The existence of large quan tities of glaucophane, a characteristic metamorphic mineral, indicates that these basic lavas have undergone high –P low –T metamorphism.

特征变质矿物——蓝闪石的大量出现表明其经历过高压低温变质作用。

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。

Below is a time line of events transpiring in the history of the

1497'''夜地精夺取了Gunbad的金矿——世界边缘山脉最大的矿山——同时是闪石的主要出产地。

Intermediate revisions not shown.- Below is a time line of events transpiring in the history of the

1497'''夜地精夺取了Gunbad的金矿——世界边缘山脉最大的矿山——同时是闪石的主要出产地。

In the United States, chronic alcoholism and hepatitis C are the most common ones.

在美国，慢性酒精中毒，肝炎是最常见的。

If you have any questions, you can contact me anytime.

如果有任何问题，你可以随时联系我。