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蓝晶石

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According to mineral components, ores of the Daixian rutile deposit can be classified into the following types: actinolite- bearing anthothyllitite, actinolite-garnet- bearing anthothyllitite, staurolite- actinolite- bearing anthothyllitite, actinolite-biotite-bearing anthothyllitite, kyanite-bearing anthothyllitite, talc-actinolite- bearing anthothyllitite and chlorite-actinolite-bearing anthothyllitite, etc.

山西代县金红石矿床的含矿岩石按岩石中矿物组成可以划分以下几种类型:阳起直闪岩、直闪阳起直闪岩、石榴石阳起直闪岩、十字石阳起直闪岩、阳起黑云直闪岩、阳起直闪岩、蓝晶石直闪岩、滑石阳起直闪岩、绿泥阳起直闪岩等。按金红石的颜色可以划分为两类,即红色金红石矿石、黑色金红石矿石。

The lithologies of the Al rich rocks under ultra high pressure metamorphism in central China are characterized by kyanite topaz quartzite which has special mineral associations of kyanite, rich topaz,Mg rich chloritoid,coesite and diaspore.

我国中部在超高压条件下形成的高铝质变质岩石,以蓝晶黄玉石英岩为特征,具有以蓝晶石、富水黄玉、富镁硬绿泥石、柯石英、硬水铝石等为代表的高压-超高压变质矿物,矿物组合主要为蓝晶石+黄玉+石英、蓝晶石+蓝刚玉±富镁硬绿泥石等。

Confirmation of high-pressure pelitic rocks in the north. The mineral assemblage of the early stage is gamet-Mg-rich chloritoid +phegite +quartz ±kyanite ±aragonite or gamet+Mg-rich chloritoid+phengite+paragonite+quartz, P-T conditions are 550±30℃ and 1.4~2.0GPa; the mineral assemblage of the late stage is muscovite +chlorite+quartz±albite, which undergone retrograde metamorphism of greenschist facies, P-T conditions are <550℃ and <0.6GPa.

确定北部高压变泥质岩石,早期矿物组合为石榴子石+富镁硬绿泥石+多硅白云母+石英±蓝晶石±文石或石榴子石+富镁硬绿泥石+多硅白云母+钠云母+石英,对应的温压条件为550±30℃和1.4~2.0GPa;晚期矿物组合为白云母+绿泥石+石英±钠长石,经受了绿片岩相的退变质作用,其温度小于550℃,压力低于0.6GPa。

In this paper,the Raman spectrum were used to study sapphire,dichroite,aquamarinl,topaz and kyanite,it is found that the characteristic Raman translocations of sapphire which are caused by Al-O vibration are 413cm-1,640cm-1 and 668cm-1,the characteristic Raman translocations of dichroite which are caused by Si-O vibration are 550cm-1,662cm-1,964cm-1and 1176cm-1,the characteris.

本文通过对蓝宝石、堇青石、蓝色托帕石、海蓝宝石和蓝晶石的拉曼光谱进行测试与研究,得到蓝宝石具有由Al-O振动引起的特征拉曼位移413cm-1,640cm-1和668cm-1;堇青石具有由Si-O振动引起的特征拉曼位移550cm-1,662cm-1,964cm-1和1176cm-1;海蓝宝石具有由Si-O振动引起的特征拉曼位移678cm-1,1064cm-1,1232cm-1;蓝色托帕石具有由Si-O振动引起的特征拉曼位移844cm-1和924cm-1;蓝晶石具有由Si-O引起的特征拉曼位移933cm-1和1133cm-1。

The associated minerals are topaz, lazulite, gorceixite, pyrophyllite, rutile etc. which constitute a suit of mineral assemblage of muddy or muddysandy muscovite schist in high pressure metamorphic belt.

蓝晶石共生的黄玉、天蓝石、磷钙铝石、叶腊石、金红石等矿物构成高压变质带里原岩为泥质、泥砂质的白片岩或类白片岩的一套矿物组合。

Andalusite is a polymorph with two other minerals, Kyanite and Sillimanite.

红柱石属多晶型物,含蓝晶石和硅线石两种不同矿物。

The low-pressure andalusite sequence metamorphic belt includes biotite zone, garnet zone, staurolite zone, staurolite-andalusite zone, sillimanite zone and cordierite-sillimanite zone. It is calculated that the P-T conditions are 445~550℃, 0.2~0.6GPa for biotite zone, 480~566℃, 0.54± 0.22GPa for the garnet zone, 601±20℃, 0.8±0.25GPa for the staurolite zone, 540±20℃, 0.32± 0.05GPa for the staurolite-andalusite zone, 640℃, 0.43GPa for sillimanite zone, 740~800℃, 0.4~0.7GPa for the cordierite-sillimanite zone.

黑云母带的变质条件估计在445~550℃、压力在0.2~0.6GPa范围变化;石榴石带温度在480~566℃、压力在0.54±0.22GPa的范围;十字石带范围为601±20℃、0.8±0.25GPa;十字石-红柱石带为540±20℃、0.32±0.05GPa,而利632.4℃、0.785GPa,这个值不是红柱石的稳定范围,这可能是其早期中压变质条件;矽线石带的条件640℃、0.43GPa左右,由于其石榴石中有蓝晶石包体,因此其早期也可能有中压条件的变质;堇青石-夕线石带范围大致为740~800℃、0.4~0.7GPa之间。

ILLUSION Mineral: Kyanite Kyanite holds the vibration of illusion in the language of light.

幻相 矿石:蓝晶石蓝晶石持有光之语中幻相的振动。

Resources Engineering School,UST Beijing, Beijing100083, China)ABSTRACT The behaviour of kyanite decomposing into mullite and SiO2 in differenttemperatures, different medium conditions and different grain sizes was studied.

蓝晶石在不同环境中分解行为倪文刘风梅摘要研究了蓝晶石在不同温度、不同介质条件和不同粒度下转化为莫来石和SiO2的变化规律。

When the kyanite is contacting with amelt which produced in decomposing process, the decomposing temperature can besignificantly dicreased and the decomposing speed can be largely increased.

当介质中出现熔体时能够大幅度地进步蓝晶石的分解速度和降低分解温度。关键词蓝晶石;加热分解;莫来石

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