钠长石是我省的一个新发现矿种。
Albite is a new mineral to Zhejiang province, which was just discovered recently.
经研究，水沫子为钠长石玉。
伴生的石英和钠长石亦为常见的热水矿物。
The associated quartz and albite are also commonly identified as thermal-water minerals.
钠长石化与铁的萃取有关，而碳酸盐化则与铁的沉淀有关。
Albitization is only related to the extraction of iron, whereas carbonatization with the precipitation of the same metal.
地下蕴藏丰富的瓷泥、铁矿、钠长石资源更是让其名声在外。
Underground rich porcelain clay, iron, sodium feldspar resources is allowed to fame.
近矿蚀变岩石中存在石英、绢云母、白云母、钠长石和碳酸盐。
There are quartz, sericite, muscovite, albite and carbonate in near-ore altered rocks.
研究表明：平武花岗岩体造岩矿物组合为石英、钠长石、钾长石和白云母；
The forming minerals of the granite mass rock are composed of quartz, albite, potassium feldspar and phlogopite in Pingwu.
扫描电镜观察发现，重晶石均为完整自形晶，并与同为自形的石英及钠长石共生。
Under scanning electron microscope, barite in these samples occurs as euhedral crystal, co-existing with authigenic quartz and albite with the same idiomorph.
次生石英、钠长石、方解石和浊沸石等的形成不同程度地影响了砂岩的储集物性。
The formation of secondary quartz, albitite, calcite and laumontite affected the storage physical properties of sandstone in different degrees.
原生绿柱石形成于早期岩浆阶段，与造岩矿物石英、白云母、钠长石、锂辉石共生。
The primary beryl crystals were crystallized early from the pegmatitic magma in association with rock forming minerals such as quartz, Muscovite, albite and spodumene.
因此，斜长石的钠长石化可见于成岩早期，而钾长石的钠长石化只发生于成岩晚期。
Therefore, the albitization of plagioclase is shown in the early stage of diagenesis and albitization of potash feldspar appears only in the late stage of diagenesis.
长石矿物特别是钠长石作为翡翠的常见次要矿物，与硬玉矿物之间存在着密切的关系。
As a common secondary mineral, feldspar minerals, especially albite, have Shared a close relationship with jadeite minerals.
联合法赤泥物相组成主要为石英和钙铝黄长石，其次为钠长石、钙铁榴石和钙钛榴石。
Combined red mud phase is mainly composed of quartz and calcium aluminum melilite, followed by albite, andradite garnet, and perovskite garnet.
条纹长石是正长石或微斜长石与钠长石交生的产物，其中正长石或微斜长石多于钠长石。
Perthite is orthoclase or microcline and albite over the product, which is more than orthoclase or microcline albite.
斜长石碎屑中钠长石组分逐渐增多，钙长石组分逐渐减少，最终形成纯钠端元的钠长石。
The albite component increases while anorthic component decreases in detrital plagioclase. The plagioclase turned into an end - member component of albite.
矿床赋存于震旦系C组地层中，中型规模，矿床类型为岩浆作用形成的白云母钠长石伟晶岩铌钽矿床。
It is hosted in the stratum of the group C of the Sinian system. Its deposit type belongs to the Niobium-Ta...
大义山硅灰石矿床矿石矿物组合复杂，由硅灰石、透辉石、符山石、钾长石、钠长石、方解石、石英等组成。
The ore mineral assemblage of Dayishan wollastonite deposit is complex being composed of wollastonite, diopside, idocrase, k-feldspar, albite, calcite and quartz.
主要组成矿物为硬玉、霓辉石、镁纳闪石、蓝透闪石、镁角闪石、阳起石、石英、钠长石、金红石和榍石。
Mineral constituents consist mainly of jadeite, aegirine - augite, magnesio - riebeckite, winchite, magnesio - hornblende, actinolite, quartz, albite, rutile and sphene.
主要组成矿物为硬玉、霓辉石、 镁纳闪石、蓝透闪石、镁角闪石、阳起石、石英、钠长石、金红石和榍石。
Mineral constituents consist mainly of jadeite, aegirine - augite, magnesio - riebeckite, winchite , magnesio - hornblende , actinolite , quartz, albite, rutile and sphene.
次生长石与长石的钠长石化过程有关，斜长石钠长石化始于成岩早期，而钾长石的钠长石化则需较高的成岩条件才能进行。
Secondary feldspar was related to the albitization process of feldspar, the albitization of plagioclase began at the early stage of diagenesis, and the albi.
长石的钠长石化作用和长石、岩屑的水化水解作用、溶解作用，导致了不稳定组分的转变以及大量离子游离于孔隙水中，同时导致大量的自生矿物沉淀。
The hydration-hydrolysis and dissolution rock fragments and feldspar and albitization of feldspar make many ions free from their framework and go into pore-water.
镜下鉴定和激光拉曼测试结果表明预先导孔（CCSD-PP2）第一段榴闪岩的主要矿物为角闪石、石榴石、黑云母和钠长石，是榴辉岩退变质作用的产物。
The main mineral assemblage of the garnet-amphibolite from the first part in CCSD-PP2 is amphibole, garnet, biotite and albite, which resulted from retrograde metamorphism.
结果表明：长石在水中碱溶出量比较少，溶出的碱主要是钠碱。
The results showed that only small amount of alkalis in feldspar were extracted when autoclaved with water, and the majority of extract is sodium oxide.
本发明是涉及制取类似天然矿泉水的矿物溶质。本发明是取蛭石、长石、碳酸氢钠的重量比为4～8∶3～6∶3～6均合混合即可制成矿泉水的溶质。
The mineral solute is produced by mixing vermiculite, feldspar and sodium bicarbonate in the weightratio of 4-8 to 3-6 to 3-6.
基性斜长石由于遭受钠黝帘石化，其蚀变产物常带绿色色调；
The mafic due to sodium zoisitization, its alteration products often with green color;
基性斜长石由于遭受钠黝帘石化，其蚀变产物常带绿色色调；
The mafic due to sodium zoisitization, its alteration products often with green color;
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