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辽宁鞍山胡家庙贫赤铁矿石工艺矿物学特征

张春浩 陈永静 翁存建 陈亮亮 罗仙平

有色金属科学与工程2015,Vol.6Issue(5):97-101,5.
有色金属科学与工程2015,Vol.6Issue(5):97-101,5.DOI:10.13264/j.cnki.ysjskx.2015.05.018

辽宁鞍山胡家庙贫赤铁矿石工艺矿物学特征

Process mineralogy characteristics of a lean hematite

张春浩 1陈永静 2翁存建 3陈亮亮 2罗仙平1

作者信息

  • 1. 赣州金环磁选设备有限公司,江西 赣州 341000
  • 2. 江西理工大学资源与环境工程学院 ,江西 赣州 341000
  • 3. 赣州市环境科学研究所,江西 赣州 341000
  • 折叠

摘要

Abstract

To provide basis for the dressing process of a lean hematite, this paper studies the process mineralogy adopting X-ray diffraction, microscopy, QuantLab-CD image analyzer analysis and detection methods. The results show that the iron ore with the grade of 25.88 % exists in the forms of hematite, martite and magnetite. Magnetite and hematite are closely associated with coarse disseminated granularity. Some martites of micro-fine particles are coated by quartz or other gangues. The gangue minerals, including quartz , tremolite, actinolite, chlorite and a small amount of clay minerals, are observed in a coarse-grained dissemination, have a slight effect on dressing.

关键词

贫赤铁矿/工艺矿物学/嵌布特征

Key words

lean hematite/processing mineralogy/dissemination characteristic

分类

矿业与冶金

引用本文复制引用

张春浩,陈永静,翁存建,陈亮亮,罗仙平..辽宁鞍山胡家庙贫赤铁矿石工艺矿物学特征[J].有色金属科学与工程,2015,6(5):97-101,5.

基金项目

江西省科技支撑计划项目(2010BGA00200) (2010BGA00200)

有色金属科学与工程

OACSTPCD

1674-9669

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