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翡翠由辉石族、角闪石族、长石族矿物组成。Jadeite jade consists of minerals of pyroxene, amphibole and feldspar groups.

主要岩石类型为二云石英片岩和斜长角闪片岩。The main rock types are two-mica quartz schist and plagioclase amphibole schist.

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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.

介绍了闪滑石粉的化学组成和结构,及其在环氧涂料中的应用。This article has described chemical composition, structure, and application of amphibole talc.

角闪石在解理、光泽、硬度上与辉石相近,因此易与辉石混淆。In amphibole cleavage, gloss and hardness and therefore easy to pyroxene similar confusion and pyroxene.

其主要造岩矿物为橄榄石、斜方辉石、单斜辉石、斜长石和角闪石。The major rock forming minerals include olivine, orthopyroxene, clinopyroxene, plagioclase and amphibole.

此岩系由黑色或暗灰色橄榄石、普通辉石玄武岩、角闪石安山岩等大小石块构成。The rock stack is made up of various sized black or dark grey olivine, augite basalt, amphibole and andesite.

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结果表明闪石类、帘石类、片状矿物、自生黄铁矿和金属矿物为优势重矿物。The result showed that dominant minerals were amphibole group, epidote group, schistose minerals, authigenous pyrite and metallic minerals.

韩国闪石玉的质量评价主要从质地、颜色、光泽、块度、创意和技艺五大因素来考虑。The quality evaluation of Korea Amphibole Jade mainly takes five factors into account, which are texture, color, gloss, originality and artistry.

其主要造岩矿物为橄榄石、斜方辉石、单斜辉石、斜长石和角闪石。They show layered intrusion features. The major rock -forming minerals include olivine, orthopyrox ene, clinopyroxene, plagioclase and amphibole.

角闪石作为南太行山地区中基性侵入岩中主要组成矿物,其详细的成因矿物学研究对了解该套岩石的形成机理具有重要意义。As one of major mineral phases in the intermediate-mafic intrusions in Southern Taihang Mountains, amphibole can be used to constrain its petrogenesis.

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.

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结合矿石化学分析和镜下鉴定结果,证实闪石类矿物与磁性铁有着密切关系。Combined with the chemical analysis and the microscopic identification results, it is confirmed that amphibole minerals have a close relationship with magnetic iron.

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.