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任群智, 姚玉增, 金成洙. 鞍山黑石砬子铁矿地质特征[J]. 地质与资源, 2007, 16(2): 95-98,101. doi: 10.13686/j.cnki.dzyzy.2007.02.009
引用本文: 任群智, 姚玉增, 金成洙. 鞍山黑石砬子铁矿地质特征[J]. 地质与资源, 2007, 16(2): 95-98,101. doi: 10.13686/j.cnki.dzyzy.2007.02.009
shu
REN Qun-zhi, YAO Yu-zeng, JIN Chen-zhu. GEOLOGICAL CHARACTERISTICS OF HEISHILAZI IRON DEPOSIT IN ANSHAN,LIAONING PROVINCE[J]. Geology and Resources, 2007, 16(2): 95-98,101. doi: 10.13686/j.cnki.dzyzy.2007.02.009
Citation: REN Qun-zhi, YAO Yu-zeng, JIN Chen-zhu. GEOLOGICAL CHARACTERISTICS OF HEISHILAZI IRON DEPOSIT IN ANSHAN,LIAONING PROVINCE[J]. Geology and Resources, 2007, 16(2): 95-98,101. doi: 10.13686/j.cnki.dzyzy.2007.02.009
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鞍山黑石砬子铁矿地质特征

  • 1.

    东北大学 地质系, 辽宁 沈阳 110004;

  • 2.

    辽宁冶金地勘局地勘院, 辽宁 鞍山 114002

详细信息
    作者简介: 任群智(1963-),男,教授级高级工程师,1983年毕业于中南矿冶学院矿产普査及勘探专业,现为辽宁冶金地勘局地质勘查研宄院总工程师,东北大学博士研宄生,主要从事矿床勘查研宄及地质经济技术管理工作.
    通讯作者: 姚玉增,沈阳市和平区文化路3-11号东北大学265#,邮政编码 110004.

  • 中图分类号: P618.31

GEOLOGICAL CHARACTERISTICS OF HEISHILAZI IRON DEPOSIT IN ANSHAN,LIAONING PROVINCE

  • 1.

    Geology Department, Northeastern University, Shenyang 110004, China;

  • 2.

    Institute of Geological Exploration, Liaoning Bureau of Metallurgic Geological Exploration, Anshan 114002, Liaoning Province, China

More Information
    Corresponding author: YAO Yu-zeng

    摘要
  • 鞍山黑石砬子铁矿床位于东鞍山铁矿与大孤山铁矿之间，是近年来鞍本地区发现的大型铁矿床.Ⅱ-1号矿体是主要的工业矿体，延长2000余米，水平厚度百余米，控制延深1000余米.有用矿物主要为磁铁矿和赤铁矿，矿体品位在走向和垂向上基本稳定，但FeO有随深度增加而增加的趋势.矿石化学成分和矿物组成简单，有害物质含量低，矿体中夹石率较低，属于沉积变质型的鞍山式铁矿床.
    The Heishilazi iron deposit, which lies between Donganshan iron mine and Dagushan iron mine in Anshan, Liaoning Province, is a large iron deposit of Anshan type found in Anshan-Benxi area recently. The Ⅱ -1 ore body is the major industrial one, with length of over 2000 m, horizontal thickness of more than 100 m and controlled depth of about 2000 m. The useful minerals are mainly magnetite and hematite. The grade is steady in strike and vertically, but the FeO content gradually increases with the increasing of the depth. The chemical and mineral components are simple, with less deleterious impurities and low ratio of horse-rocks. All these indicate that the ore deposit belongs to sedimentary-metamorphic iron deposit of Anshan type.
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出版历程
收稿日期:  2006-11-14
修回日期:  2007-01-17
刊出日期:  2007-06-30

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