DOI:
矿床地质:2004,Vol.>>Issue(1):93-100

中国钴资源及其开发利用概况
中国地质科学院矿产资源研究所
Cobalt Resources of China and Their Exploitation and Utilization
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中文摘要:文章概述了中国钴矿床的类型、时空分布、最新研究进展及开发利用 现状,指出世界上共(伴)生主要钴矿床类型在中国均已发现,可归纳为4大类,其中以岩浆 型Ni-Cu-Co硫化物矿床、热液及火山成因钴多金属矿床最为重要;中国钴矿的形成可分为6 个重要成矿期,划分出7个重要成矿带;尽管钴多以伴生组分产在镍、铜、铁等矿床中,但 近年来中国先后发现了一些不同元素组合、不同成因类型的独立钴矿床。鉴于中国当前钴资 源比较紧缺和钴消费快速增长,建议既要充分利用好国内外资源,又要加大钴资源勘查及开 发利用力度,以满足国民经济发展的需要。
Abstract:Cobalt is a very important kind of strategic metal used in a great variety of fi elds. This paper has summarized the classification, temporal and spatial distrib ution and recent exploration, exploitation and utilization of cobalt deposits in China. The major types of cobalt deposits in the world have been almost all fou nd in China, and they can be classified into four types, of which magmatic Ni_Cu _Co sulfide deposits and hydrothermal and volcanogenic cobalt polymetallic depos its are most important. There exist six principal metallogenic epochs and seven important metallogenic belts according to concentrative distribution and tectoni c positions of the cobalt deposits. Although cobalt often occurs as an associate d metal in Cu_Ni, Cu and Fe deposits, the exploration of independent cobalt depo sits has made good progress in China in recent years. This is evidenced by the d iscovery of varied element assemblages and different genetic types of cobalt dep osits in such areas of China as the eastern part of the north margin of the Nort h China platform, the Central China orogenic belt, western Jiangxi Province and northeastern Hunan Province. In view of the shortage of cobalt resources and the rapid increase of cobalt consumption in China, it is suggested that not only th e cobalt resources at home and from abroad should be utilized in a better way bu t the exploration and development of the cobalt deposits should be strengthened as well.
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基金项目:国家自然科学基金(编号:40302019)和国家地质调查项目(编号:DKD2001027_4)
引用文本:
丰成友;张德全;党兴彦.2004.中国钴资源及其开发利用概况[J].矿床地质,23(1):93~100
.2004.Cobalt Resources of China and Their Exploitation and Utilization[J].Mineral Deposits23(1):93~100
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