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1)  BSP-1 hornblende
BSP-1角闪石
2)  hornblende [英]['hɔ:nblend]  [美]['hɔrn,blɛnd]
角闪石
1.
In this study, Ar-Ar isotope dating of muscovite, hornblende and phlogopite was carried out in order to con.
文章以金云母、角闪石和白云母为测试对象,利用40Ar/39Ar同位素定年的方法,精确厘定了芙蓉超大型锡矿床的形成时间。
2.
To gain a better understanding of the age of gold mineralization and its relationship with the evolution of the ductile shear zone,40Ar/39Ar plateau age analysis was made on biotitefrom biotite-quartz gneiss and on hornblende from biotite-hornblende mylonite.
对采自十八顷毫金矿区的黑云母、角闪石用阶段升温法进行40Ar/39Ar年龄谱研究,结合矿区地质特征,认为黑云母近似直线年龄谱的坪年龄(277Ma)及角闪石稳定坪年龄(288Ma)代表了韧性剪切带最新活动的时代;角闪石矿物年龄谱反映的后期热扰动(268Ma)反映区域退化变质作用发生的时代,269~277Ma的年龄可能代表了与退化变质同时的金矿化时代。
3.
Based on the characteristics of hornblendes, we classified the alkali granitoids as two types.
角闪石的种类、化学组成、微量元素特征显示所研究的碱性花岗岩分为两类 :达拉布特型和恰库尔特型。
3)  amphibole [英]['æmfibəul]  [美]['æmfɪ,bol]
角闪石
1.
Crystallographic preferred orientation of amphibole in retrograded eclogites;
退变质榴辉岩中角闪石的组构特征
2.
On the basis of petrography and mineral chemistry of the xenoliths,the amphiboles in them can be subdivided into four kinds of occurrences,i.
对该类捕虏体的岩相学和矿物化学研究表明,其中的角闪石具有4种产状:1)位于石榴石中的早期角闪石包裹体,为镁质普通角闪石;2)与榴辉岩中矿物平衡存在的原生角闪石,为韭闪石或韭闪石质普通角闪石;3)位于石榴石和单斜辉石周边的退变角闪石,主要为浅闪石质和阳起石质普通角闪石;4)沿单斜辉石解理分布的出溶角闪石,主要为浅闪石、浅闪石质角闪石和含亚铁韭闪石质普通角闪石。
3.
As one of major mineral phases in the intermediate-mafic intrusions in Southern Taihang Mountains, amphibole can be used to constrain its petrogenesis.
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。
4)  The ZBJ hornblende
ZBJ角闪石
1.
The ZBJ hornblende,as K-Ar age geostandard of China,was sampled from the Fangshan granodiorite in southwestern Beijing.
为了满足K-Ar定年中K和40Ar*分析的质量监控及Ar-Ar法样品在反应堆照射时中子通量监测的需要,我国氩同位素年代学工作者研制了一个K-Ar法年龄标准物质ZBJ角闪石,它采自北京房山花岗闪长岩体。
5)  hornblendite
角闪石岩
1.
The hornblendite in Danailingou, with clear cryptoexplosion brecciated structure and mi-crolitic texture, occurs within Jurassic intermediate to acid volcanic rocks in a vein shape.
内蒙古克什克腾旗同兴乡大乃林沟角闪石岩呈脉状产于侏罗纪中酸性火山岩中,具明显的隐爆特征,晶洞构造发育。
2.
This paper chooses the Yaogou hornblendite body, one of the two major ultramafic outcrops in the Laiyuan batholith, as a representative to carry out detailed research.
以窑沟橄榄辉石角闪石岩岩体为代表 ,研究了涞源岩基中超镁铁质岩石。
6)  Hornblend Jade
角闪石玉
补充资料:普通角闪石
      见闪石。
  

说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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