角闪石的出现反映上地幔流体的渗透及交代作用。
The occurrence of pargasite reflects the participation of the upper mantle fluids and the metasomatism.
含角闪石的变种填补了带状和脉状角闪岩的中间相。
Hornblende bearing varieties bridge the gap over to amphibolites which are in bands and dikes.
蓝石棉是碱性角闪石的纤维变种，是一种较为稀见的特种非金属矿产。
Blue asbestos is a fibrous variety (morph) derived from alkali hornblende and is a kind of special non-metallic mineral resources seldom seen.
文章综合分析研究了中国2 1个夕卡岩矿床中的1 30个角闪石的成分分析数据。
Based on 130 analyses of amphiboles from 21 skarn deposits in China, the authors have studied their types, optical properties, composition characteristics, and parageneses.
最后登场的是各式镶缀水晶闪石的配饰及富有戏剧色彩的晚装，不禁令人联想起蓝碧嘉的时代。
A final presence of DE Lempicka is felt as crystal deco accessories and dramatically draped gowns evoke her era.
角闪石的化学成分及不同成矿岩体的微量元素和同位素特征是区分区内两类不同成矿岩体的有效判别标志。
The major compositions of amphibole in the granites, trace element composition and isotopic composition of granites were effective index to distinguish different metallogenic granitic bodies.
在侵入岩中的角闪石多呈长柱状晶体，但在某些花岗岩、花岗闪长岩中，角闪石的一向伸长的结晶习性并不显著。
Amphibole in the intrusive rock in a long columnar crystal, but in some granite, granodiorite, hornblende has elongated crystal habit is not significant.
另外，遭受风化后的角闪石常具绿色色调，而黑云母风化后常具褐色色调。
In addition, amphibole weathering after often with green shades, and biotite weathering often with brown color.
结果表明：四川软玉猫眼的主要成分为透闪石。
The results indicate that the main composition of nephrite cat's eye is tremolite.
在闪石类石棉中，组成的原子呈链状排列。
In amphibole asbestos the constituent atoms are arranged in chain-like conformation.
角闪石给出的坪年龄为124。
在闪石类石棉中，组成的原子呈链状排列。
In amphibole asbestos the constituent atoms are arranged in chain -like conformation.
因52个样品中，也包含钠钙闪石亚族，故对整个闪石族用X射线衍射估算阳离子占位的问题已基本解决。
As Na-Ca sub-amphiboles appeared among the 52 samples, the method of estimating canon occupancied by X-ray diffraction is suitable to all amphiboles.
讲稿详细地介绍了火成岩矿物，如：石英及它的同构异形体、柯石英、鳞石英、方石英、长石、斜长石、似长石、辉石、闪石等矿物。
The notes describe the common minerals such as quartz and its polymorphs, coesite, tridymite and cristobalite, feldspar, plagioclase, feldspathoids, pyroxenes, amphiboles, etc.
利用增量方法和同位素交换技术，对角闪石族矿物的氧同位素分馏进行了理论计算和实验测定。
Oxygen isotope fractionation in amphiboles was determined by theoretical calculation using the increment method and by experimental measurement using isotope exchange technique.
钻芯详细检查的结果，橄榄石全部蚀变为蛇纹石、滑石及角闪石。
Olivine has been completely altered to serpentine, talc, and amphibole in the bore-hole examined in detail.
钻芯详细检查的结果，橄榄石全部蚀变为蛇纹石、滑石及角闪石。
Olivine has been completely altered to serpentine, talc, and amphibole in the bore - hole examined in detail.
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.
普通角闪石是闪长岩、正长岩中常出现的矿物，也常出现在花岗岩中。
Hornblende is often diorite, syenite in minerals, often appear in granite.
包体中发育针状磷灰石和角闪石，显示为岩浆淬冷的结果。
Needle shape of the apatites and amphiboles in MMEs implying the process of fast cooling.
十字石—铝直闪石之间的堇青石冠状体；
绿帘石透闪石玉是市场上发现的一新品种，主体呈特征的黑绿色和黄绿色，商家称其为“青花玉”。
Epidote-tremolite jade called "Qinghua jade"by sellers is a new species in the market, and its main colour is blackish green or yellowish green.
利用岩石薄片X衍射技术，在松辽盆地深层富碱酸性火山岩中识别出特征的碱性暗色矿物——钠铁闪石，从而确定其为碱流岩。
Using thin section X-ray diffraction techniques, his paper identified arfvedsonite in volcanic rocks from Songliao Basin, and thus confirmed that the volcanic rocks are composed of pantellerite.
通过X射线粉晶衍射分析确定了青海软玉中的“水线”主要由透闪石组成。
The XRD analysis shows the "water line" in Qinghai nephrite jade is mainly composed of tremolite.
辉石最常见的次生变化是蛇纹石化和纤闪石化。
The most common secondary changes of pyroxene are the petrochemistry and the petrochemistry.
造岩矿物的概念、橄榄石、长石、角闪石、辉石、云母、石英、方解石和常见金属和非金属矿物。
Rock-forming mineral, olivine, pyroxene, hornblende, orthoclase, feldspar, plagioclase, mica, quartz, biotite, calcite and other common metal and nonmetal minerals.
麻粒岩和榴辉岩中退变质阶段的角闪石主要形成于中压相系角闪岩相的温压条件。
The amphiboles of retrogressive metamorphic stages in the granulite and eclogite were mainly formed under the condition of amphibolite facies of medium pressure facies series.
晚期的钠质角闪石构成了现存片理，可能与后期构造变形有关。
While, the sodium amphibolites in the later stage compatible with the present foliation, might be related to the structure deformation.
详细的岩相学研究表明，TTG岩类中存在岩浆结晶的绿帘石、角闪石和黑云母等。
The petrographical facies studies indicate that the magma-crystallined epidotes , bornblendesand biotites were distributed in TTG rocks.
详细的岩相学研究表明，TTG岩类中存在岩浆结晶的绿帘石、角闪石和黑云母等。
The petrographical facies studies indicate that the magma-crystallined epidotes , bornblendesand biotites were distributed in TTG rocks.
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