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铁黑云母

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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。

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。

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。

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。

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。

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。

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)。

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。

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。

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。

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