长石

The main mineral were quartz,mica,albite,calcite,chlorite.The difference waslittle between dustfall and local soil.

降尘中的主要矿物为石英、云母、钠长石、方解石、绿泥石，与当地土壤差异较小。

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。

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。

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。

Field obserbation and laboratory study indicate the main type of rock alterationwere K-feldsparization, biotitization, sericitization, silication, epidotization,chloritization and carbonatization. From early to late, these alteration could dividedinto three epochs: early-stage was K-feldsparization-biotitization, middle-stage wasquartzification -sericitization, late-stage was silication, carbonatization, epidotizationand chloritization.

通过野外观察及室内研究表明，围岩蚀变类型主要有钾长石化、黑云母化、绢云母化、硅化、绿帘石化、绿泥石化和碳酸盐化，从早至晚可分为三期：早期为钾长石-黑云母化；中期为石英-绢云母化；晚期为硅化、碳酸盐化和绿泥石、绿帘石化。

You will find her on Feldspar St.

你会发现她的长石街

Based on the comprehensive analysis of previous studies, we summarizes the experimental studies of feldspar dissolution.

在综合分析前人研究成果基础上，对长石溶解模拟实验研究进行了综述。

I analyzed the mineral content. It's feldspar and quartz.

我验过它的成分是由长石和石英构成的

Feldspar is the most abundant mineral on the Earth's surface.

长石是地球表面最丰富的矿物质。

These rocks were originally formed by molten residues, and contain the main components of quartz and feldspar.

这些岩石最初形成的熔融残留物，并且包含的主要成分是石英和长石。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。