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铬铁矿是生产铬铁合金的重要原料。Chromite is main raw material for smelting ferrochromium.

该地区的铬铁矿异常属于矿致异常。Local chromite anomaly caused mineral anomaly in this area.

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对于铬铁矿矿层产状的了解同样是不完整的。Knowledge of the occurrence of chromite deposits is likewise incomplete.

目前为至，不锈钢行业是对铬矿需求量最大。The stainless steel industry is by far the largest user of chromite ore.

对铬铁矿中亚铁的测定方法进行了探讨。A method for the determination of ferrous in chromite ores was developed.

这是一种由重烧镁砂制成的混合型低铬镁砖。This is a hybrid magnesia low chromite brick made from dead burned magnesia.

究竟平衡作用发生在铬铁矿和矽酸盐下沉之前，还是在其后？Did equilibration take place before or after setting of chromite and silicates?

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锌络铁矿棕色尖晶石色料及其制备方法和应用。Brown spinel pigments based on zinc chromite method of their production and use.

究竟平衡作用发生在铬铁矿和硅酸盐下沉之前，还是在其后？Did equilibration take place before or after setting of chromite and silicates ?

在穆斯科克斯杂岩体中，铬铁矿矿层仅产于长石质橄榄岩中。The chromite deposits in the muskox complex occur only in feldspathic peridotite.

结果表明，两者的还原反应都是按间接还原进行的。Result shows that the reduction of chromite pellet with carbon is carried indirectly.

铬砂制作的砂模可让铸件有较快的冷却速率，但也产生较多的微孔隙。The cooling rate is faster in chromite sand mold, but also causes more porosity in castings.

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蛇绿岩套中的豆荚状铬铁矿提供了中国存在新太古代蛇绿岩的确切证据。The podiform chromite associated with these structural lenses is only reported in ophiolites.

铬铁矿主要产在穆斯林巴格、若布、瓦齐里斯坦、达加等蛇绿岩体内。The Chromite mainly produces in the ophiolites in Muslimbagh, Zhob, Waziristan , Dagh and etc.

对赤铁矿、假像赤铁矿、镜铁矿、褐铁矿、菱铁矿、锰矿、铬铁矿等的分选。To separate hematite, supposed hematite, specularite, limonite, siderite, manganese ore, chromite and so on.

介绍了使用烧结铬矿冶炼炭素铬铁的工业性试验情况。This paper introduces the industrial-scale experiment of carbon ferrochrome manufacture with sintered chromite.

土耳其是一个铬铁矿的主产国和出口国，蕴藏着铁矿石、煤炭、褐煤、矾土和铜矿。Turkey is a major producer and exporter of chromite and also mines iron ore, coal, lignite, bauxite, and copper.

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矿体总体上向南倾斜，成带分布、成群出现、分段集中。The chromite body generally south slope, Distributed along zones, appeared in groups, and concentrated on section.

超基性岩型软玉多为亮绿色，常有磁铁矿、铁矿和硫化物浸染。Many ultrabasics type nephrites have bright green colour and have ore dissemination with magnetite, chromite and sulfide.

因此，铬尖晶石与辉石的共生连晶结构可以作为豆荚状铬铁矿的重要找矿标志。Therefore, the intergrowth texture of Cr-spinel and pyroxene can be an important indicator for podiform chromite exploration.