- 更多网络例句与铁黑云母相关的网络例句 [注：此内容来源于网络，仅供参考]
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Two common minerals in this group are dark-colored biotite which contains iron and magnesium and white-colored muscovite in which iron and magnesium are absent.
在这类矿物中，黑色的云母称为黑云母，它内含有铁和镁；而白色的云母称为白云母，它不含铁和镁。
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Two common minerals in this group are ark-colored biotite which contains iron and magnesium and white-colored muscovite in which iron and magnesium are absent.
在这类矿物中，黑色的云母称为黑云母，它内含有铁和镁；而白色的云母称为白云母，它不含铁和镁。
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Biotite at different stages are always rich in iron, and the w/w ratios increase from 0.80 to 0.96 from the earliest stage to the last stage.
黑云母都是富铁的，从早期到晚期富铁程度增加，w/w从0.80增加到0.96。
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In mineral chemistry, the plagioclase in the granitic gneisses from southern Dabie mountain was high riching in Na, and the biotite and hornblende were characterized by riching in Fe, showing clearly the continental crust source.
在矿物化学成分上，南大别花岗片麻岩中的斜长石高度富钠，黑云母和角闪石总体以富铁为特征，明显具有大陆地壳源的性质。
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Mineralogically these granites contain annite-rich biotite and/or alkali amphiboles and commonly sodic pyroxene.
矿物学上常含富铁黑云母、碱性角闪石和钠辉石。
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The study revealed that: 1 chlorite occurred in vein, agglomerate or had the false pattern of biotite type, or the worm or bladed configuration; 2 Fe/Si diagram revealed mast of the chlorite occurred in the ferroamesite and aphrosiderite areas, few in the pycnochlorite area; 3 the formation temperature of chlorite varied from 179-276℃, mainly within the range of 230-260℃ as calculated by the empirical equation presented by Battaglia; 4 chlorite was formed in the reducing condition, the main formation mechanisms were dissolution-precipitation and dissolution-migration-precipitation.
研究表明：①岩石中绿泥石主要呈脉状、黑云母假象或团块状等产出，具有蠕虫状、叶片状等形貌特征；②绿泥石的Fe/Si图解显示201和361铀矿床中绿泥石主要为铁镁绿泥石和蠕绿泥石，少数属密绿泥石；③根据Battaglia提出的经验方程式计算了201和361铀矿床绿泥石的形成温度变化于179~276℃之间，且主要介于230~260℃之间；④绿泥石主要形成于还原环境，其主要的形成机制是溶解－沉淀和溶解－迁移－沉淀。
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Indeed, the Grand Canal was constructed partly utilizing the pre-existing channels connecting these lowland swamps and lakes (3) Several rivers have produced deltaic forms on the western side of the lakes;(4) A series of artificial islands have been constructed upon the natural bars or barriers located in the lakes and wetlands, and are locally termed Duo, Dun or Wei (meaning artificial bars or crossways in Chinese).
钻孔B/M界线之下(4078 m～4530 m)的泛滥平原河湖相沉积物中局部地段富含铁锰鲕粒，其主要矿物组成为蛋白石、铁的氢氧化物(包括纤铁矿、水纤铁矿、针铁矿、水针铁矿，统称褐铁矿)、铁锰氧化物(包括硬锰矿和软锰矿，以硬锰矿为主)及极少量的细小碎屑矿物(钾长石、蚀变黑云母、含铁白云母、锆石、独居石、金红石和含钛磁铁矿)。
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Hydrobiotite is destroyed to forsterite at 1100℃.
在800℃～900℃，水黑云母脱去与八面体铁有关的羟基。
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The rework of peak composition in core of garnet far away from biotite and other Mafic minerals is much slighter than those surrounded by biotite.
远离黑云母等铁镁矿物的石榴石晶体成分受改造的程度明显低于那些靠近黑云母的石榴石晶体。
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On the basis of comprehensive discipline research, the rocks subfacies and microfacies of hydrothermal rocks facies have been initially studied and the their characteristic have been come to conclusions frist time.
在多学科综合研究基础上，首次系统提出研究并总结了热水沉积岩相的亚相及微相特征，亚相包括有：钠长岩-似碧玉岩亚相、硅质白云岩→硅质岩亚相、碱性钠长石质-碳酸质岩亚相、铁镁碳酸盐岩亚相、重晶石岩亚相、黑云母方柱石岩/黑云母岩亚相及铁绿泥石岩亚相。
- 更多网络解释与铁黑云母相关的网络解释 [注：此内容来源于网络，仅供参考]
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amphibolite：角闪岩
斜长角闪岩(amphibolite) 斜长角闪岩 主要由角闪石和斜长石组成的中,高级区域变质岩.又称角闪岩.角闪石和斜长石的含 量相近.可含少量石英,铁铝榴石,黑云母,单斜辉石和斜方辉石.常为中,细粒纤状变晶 结构,可具有块状,
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biotite：黑云母
方解石(calcite) 碳酸钙矿物. ...橄榄岩(dunite) 主要由橄榄石和辉石组成的深成超基性岩浆岩. ...黑云母(biotite) 含铁、镁的云母.
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dunite：橄榄岩
方解石(calcite) 碳酸钙矿物. ...橄榄岩(dunite) 主要由橄榄石和辉石组成的深成超基性岩浆岩. ...黑云母(biotite) 含铁、镁的云母.
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gabbro：辉长岩
辉长岩(gabbro) 暗色的深成基性岩. gabbro一词是1768年由 T.托泽蒂用来称呼异剥石质蛇纹石,现在用来命名辉长岩. 辉长岩主要矿物成分为单斜辉石和富钙斜长石,两者含量近于相等. 次要矿物为橄榄石、角闪石、黑云母、石英、正长石和铁的氧化物等.
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haughtiness：傲慢/不逊/傲气
haughtily /傲慢地/骄傲地/ | haughtiness /傲慢/不逊/傲气/ | haughtonite /富铁黑云母/
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iron meteorite：陨铁;铁陨石
iron metavanadate 钒酸铁 | iron meteorite 陨铁,铁陨石 | iron mica 铁黑云母,铁云母,黑云母
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haughtonite：富铁黑云母
富铁白云石ankerite | 富铁黑云母haughtonite | 富铁辉石ferroaugite
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lepidomelane：铁黑云母
lepidolitelithionite 锂云母 | lepidomelane 铁黑云母 | lepidopteranlepidopteron 鳞翅类
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oxyblepsia：视觉锐敏
oxybiotite 氧黑云母 高铁黑云母 | oxyblepsia 视觉锐敏 | oxyboostedblast 富氧鼓风
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potassic zone：钾化带
(1) 钾化带(potassic zone) 主由次生正长石和黑云母组成,也有正长石-绿泥石或正长石-黑云母-绿泥石组合,交代原生的正长石、斜长石和铁镁矿物. 此带中还常有大量硬石膏,伴有绢云母、磷灰石和金红石,一般只有低品位的铜矿化. ?