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罗布莎低品位铬铁矿工艺矿物学研究

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为查清西藏罗布莎低品位铬铁矿的矿石性质,采用化学分析、光学显微镜鉴定、扫描电镜分析、EDS微区成分分析等岩矿测试手段,对矿样的化学组成、矿物组成、矿物嵌布特征、主要矿物的工艺粒度、铬元素的赋存状态进行了详细的工艺矿物学研究.结果表明:矿石有价成分Cr2O3含量18.50%,有害成分MgO和SiO2含量分别为35.32%,26.55%,主要含铬矿物为铝-铁镁铬铁矿,脉石矿物主要为含铬硅酸盐矿物橄榄石和蛇纹石,另含少量的绿泥石、辉石、方解石和铁白云石,以及微量的钾长石、黄铁矿等;铬铁矿嵌布粒度粗细不均,通常与橄榄石、蛇纹石、绿泥石紧密共生,部分微细粒铬铁矿被橄榄石包裹,不易解离;铬元素主要赋存在铬铁矿中,少量赋存在橄榄石、蛇纹石和绿泥石中,铬铁矿单矿物平均含铬 39.17%,橄榄石和蛇纹石单矿物平均含铬 0.44%,绿泥石单矿物平均含铬1.15%.
Study on Process Mineralogy of Luobusha Low-grade Chromite Ore
In order to find out the ore properties of Luobusha low-grade chromite in Tibet,chemical analysis,optical microscope identification,scanning electron microscope analysis,EDS micro-area compo-sition analysis and other rock and mineral testing methods were used to study the chemical composition,mineral composition,mineral dissemination characteristics,process particle size of main minerals and oc-currence state of chromium elements of ore samples in detail.The results show that the content of Cr2O3 is 18.50%,and the contents of harmful components MgO and SiO2 are 35.32%and 26.55%respectively.The main chromium-containing minerals are aluminum-iron-magnesium chromite.The gangue minerals are mainly chromium-containing silicate minerals olivine and serpentine,and a small amount of chlorite,pyrox-ene,calcite and ankerite,as well as trace amounts of potassium feldspar and pyrite.The grain size of chro-mite is uneven,and it is usually closely associated with olivine,serpentine and chlorite.Some fine chromite is wrapped by olivine,which is not easy to dissociate.Chromium mainly occurs in chromite,and a small amount occurs in olivine,serpentine and chlorite.The average chromium content of chromite single mineral is 39.17%,the average chromium content of olivine and serpentine single mineral is 0.44%,and the aver-age chromium content of chlorite single mineral is 1.15%.

chromitelow gradeprocess mineralogydissemination characteristics

陈洲、王帅、于茜、王亚琴

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东北大学资源与土木工程学院

中钢集团马鞍山矿山研究总院股份有限公司

华唯金属矿产资源高效循环利用国家工程研究中心有限公司

铬铁矿 低品位 工艺矿物学 嵌布特征

2024

现代矿业
中钢集团马鞍山矿山研究院有限公司

现代矿业

影响因子:0.33
ISSN:1674-6082
年,卷(期):2024.40(3)
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