绿帘石

Through electron probe\'s analysis to the albite jade, union grinding sample thin slice under polarizing microscope observation as well as X powder crystal diffraction data analysis. Discovery like Chen zhenqiang and "System Gemology" said that secondary mineral for actinolite, green mudstone, epidote and quart.

通过对钠长石玉进行电子探针的分析，结合磨制的样品薄片在偏光显微镜下的观察以及X粉晶衍射数据分析，可知钠长石玉中的主要成分为钠长石，次要矿物为硬玉、角闪石、绿辉石、钠铬辉石；并未发现如陈振强等人以及《系统宝石学》中所说的次要矿物为阳起石、绿泥石、绿帘石、石英。

Epidote and quartz were formed at a very late stage as a result of fluid activity along micro-fractures.

绿帘石与石英是最晚期流体沿微裂隙活动的产物。

Although mappingprecision of other minerals is better,chlorite and epidote, illite and muscovite areconfused and identified falsely.

同时结果发现虽然其它填绘矿物的精度较好，但在绿泥石与绿帘石、伊利石与白云母等相似矿物的区分上仍然存在不少混淆和误判的现象。

Since 2 ~ 5MM a grain of rice contains a lot of different colors like almond-shaped filling material, such as the white quartz, green debris, green epidote, pink long stone, the shape of plum blossom in full bloom of a thousand, hence the name.

由于含有大量2~5MM米粒状颜色各异的杏仁状充填物，如白色的石英、绿色的泥石、绿帘石、浅红色的长石等，形似盛开的万点梅花，故名。

The late period of loess accumulation with high contents of hornblende and epidote is mainly far-source sedimentary with wind transport, and the early and middle periods of loess accumulation with high contents of magnetite and dens are mainly near-source sedimentary with complex transport.

普通角闪石、绿帘石含量较高的黄土堆积后期是以远源沉积为主，且以风力搬运为主；磁铁矿、岩屑含量较高的早、中期是以近源沉积为主，搬运动力较复杂。

The late period of loess accumulation with high contents of hornblende and epidote is mainly far source sedimentary with wind transport, and the early and middle periods of loess accumulation with high contents of magnetite and deris are mainly near-source sedimentary with comp lex transport.

普通角闪石、绿帘石含量较高的黄土堆积后期是以远源沉积为主，且以风力搬运为主；磁铁矿、岩屑含量较高的早、中期是以近源沉积为主，搬运动力较复杂。

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。

A —Sample ZM641 , garnet porphyroblast with inclusionsof amphibole , epidote , plagioclase concentrated in the core of crystal , the rimof the garnet

a —样品ZM641 ，角闪石、绿帘石和斜长石包体分布在石榴石变斑晶核部，边部有绿辉石包体，基质矿物主要为绿辉石背散射电子图像

On the Ute Indian Trail out of Salida that went to Manitou Springs near Colorado Springs, one can find peridot , epidote, pink and white quartz, muscovite, biotite and gold mica, pink feldspar, pyrite, magnetite, hematite, limonite, white and gray marble, gold, beryl, black obsidian "Apache Tears", red garnets and topaz.

在乌特印度径出萨利达是到马尼图斯普林斯科罗拉多斯普林斯附近，人们可以找到橄榄石，绿帘石，粉红色和白色的石英，白云母，黑云母和金云母，粉红色的长石，黄铁矿，磁铁矿，赤铁矿，褐铁矿，白色和灰色大理石，黄金，绿柱石，黑色黑曜石&阿帕奇泪&，红色的石榴石和黄玉。

On the Ute Indian Trail out of Salida that went to Manitou Springs near Colorado Springs, one can find peridot , epidote, pink and white quartz, muscovite, biotite and gold mica, pink feldspar, pyrite, magnetite, hematite, limonite, white and gray marble, gold, beryl, black obsidian "Apache Tears", red garnets and topaz.

在乌特印度径的萨利达指出，到附近的科罗拉多斯普林斯的马尼图斯普林斯，人们可以找到橄榄石，绿帘石，粉红色和白色的石英，白云母，黑云母和金云母，粉红色的长石，黄铁矿，磁铁矿，赤铁矿，褐铁矿，白色和灰色大理石，黄金，绿柱石，黑色黑曜石&阿帕奇泪&，红色的石榴石和黄玉。

According to the clear water experiment, aeration performance of the new equipment is good with high total oxygen transfer coefficient and oxygen utilization ratio.

曝气设备的动力效率在叶轮转速为120rpm～150rpm时取得最大值，此时氧利用率和充氧能力也具有较高值。

The environmental stability of that world - including its crushing pressures and icy darkness - means that some of its most famous inhabitants have survived for eons as evolutionary throwbacks, their bodies undergoing little change.

稳定的海底环境─包括能把人压扁的压力和冰冷的黑暗─意谓海底某些最知名的栖居生物已以演化返祖的样态活了万世，形体几无变化。