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Our factory is a production and processing operation Qingshi sandstone mainly of individual and private enterprises.

我厂是一家以生产加工经营砂岩青石为主的个体私营企业。

Within pelitic metamorphic rocks, even though sillimanite is well developed and the low-pressure minerals like andalusite and cordeirite etc.

新疆阿尔泰古生代造山带以低压变质及花岗质岩浆作用广泛发育闻名国内外,泥质变质岩系中矽线石较发育,红柱石和堇青石等低压特征矿物相当常见,但是,石榴石—十字石的组合更普遍。

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。

The shaped and unshaped refractories manufactured by our Co.,such as bricks of clay,high AL,silicon,AL-C,carbon corundum,cordierite,corundum,sillimanite,andalusite,etc.,which are used in blast furnace,hot stove,mixer furnace,melton iron ladle and torpedo car,have gained customers'good commendation on its steady quality and good results.

我公司可生产各种高炉、热风炉、混铁炉、铁水包、鱼雷罐用粘干质、高铝质、硅质、铝碳质、碳化硅、堇青石、刚玉质、硅线石砖、红柱石砖等制品和不定型耐火材料,以质量稳定,使用效果好而得到用户一致好评。

The Altai Paleozoic orogenic belt of Xinjiang Autonomous Rejoin is geologically wellknown both domestic and abroad by the intensive development of low-pressure metamorphism and granitic magmatism. Within pelitic metamorphic rocks, even though sillimanite is well developed and the low-pressure minerals like andalusite and cordeirite etc. are quite common, the assemblage of garnet and staurolite is more important.

中文题名阿尔泰海西造山带中-低压递增变质作用特征及其地球动力学副题名外文题名 Features and geodynamics of the low-to mid-pressure progressive metamorphism in the Altai hercynian orogenic belt 论文作者郑常青导师卢良兆徐学纯教授学科专业矿物学、岩石学、矿床学研究领域\研究方向变质地质学学位级别博士学位授予单位吉林大学学位授予日期2001 论文页码总数132页关键词阿尔泰造山带造山带构造地质馆藏号BSLW /2003 /P542 /1 新疆阿尔泰古生代造山带以低压变质及花岗质岩浆作用广泛发育闻名国内外,泥质变质岩系中矽线石较发育,红柱石和堇青石等低压特征矿物相当常见,但是,石榴石—十字石的组合更普遍。

During the second crystallization peak, XRD continues to detect spodumene indicating, however, the additional production of cordierite and indialite which are, now, the main crystalline phases.

在第2个结晶化高峰间,XRD分析显示锂辉石仍然存在,但主要的结晶态为额外产生的堇青石和印度石。

Several conclusions are drawn from the study. The ore deposit mainly occurs in the lower Cambrian Shuigoukou Formation, which is situated at the limbs of Qingshixia-Yujiatai overturned multiple syncline. The ore-hosted rocks are silicalite and mudstone. The content of SiO2 is high in the rocks of V ore deposit. Silicalites are mainly aphanitic quartz and chalcedony and the barite is sedimentogenic. The correlation between V and Cr, U, Ba is good. The rare earth element distribution patterns show Ce-negative or positive anomaly, obviously Eu positive anomaly and the right dip graphics.

研究结果表明,该区钒矿主要产出于青石峡-余家台倒转复式向斜两翼下寒武统水沟口组下岩段硅质岩夹泥岩的泥岩中,矿体产状与地层产状基本一致;钒矿床中所有岩石都含有较高的SiO2,硅质岩以隐晶质石英和玉髓为主,有沉积成因重晶石;V与Cr、U、Ba相关性好;稀土元素球粒陨石标准化模式具有或正或负的Ce异常和明显的Eu正异常、向右倾的图形。

I stopped the hitchy treads,learned on a blue stone,staring.Some ever choked thoughs was awaked by some further hopes.

停住蹒跚的脚步,伫一方青石,久久地凝视,一些更深远的愿望,激活了曾经窒息的思想。

Helium results of Kuanyinshan clino-pyroxene, Lutao clino-pyroxene and cordierite all indicate the signature of crust contamination.

观音山斜辉石、绿岛斜辉石及绿岛堇青石等样品之氦同位素比值分析结果均指出有地壳混染的讯号。

There is a long standing debate about the magma origin of Lutao. Two different models of crust contamination and source contamination are proposed. Combining helium results with strontium ratios of Lutao lavas, it shows that Lutao arc magma has experienced approximately 5% of crust contamination.

绿岛岩浆成因长久以来存在有地壳混染或是源区混染的争论,本研究利用绿岛斜辉石及堇青石巨晶的3He/4He比值及其母岩浆的87Sr/86Sr比值,得到了绿岛岩浆经历过5%左右地壳混染的结果。

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