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海南石碌铁多金属矿床碳酸盐岩地球化学特征及其地质意义
王展; 王智琳; 许德如; 郭飞
Source Publication第八届全国成矿理论与找矿方法学术讨论会论文摘要文集
2017-12-09
Conference Date2017-12-09
Conference Place中国江西南昌
Country中国
Indexed By其他
Language中文
Keyword铁多金属矿床 碳酸盐岩
Abstract石碌铁多金属矿床位于海南省昌江县境内,曾誉为"亚洲最大的富赤铁矿矿床",该矿床还共伴生有钴、铜、镍、铅锌、银、金等多金属和白云岩、重晶石、石膏、硫等非金属矿产。目前研究倾向于将石碌铁多金属矿床归为受构造和热液叠加改造的BIF型矿床(Xu et al.,2013,2014;Wang et al.,2015),碳酸盐岩作为石碌铁多金属矿床主要赋矿围岩—石碌群的重要组成部分,研究其地球化学组成对于揭示石碌铁多金属
Document Type会议论文
Identifierhttp://ir.gig.ac.cn/handle/344008/35609
Collection中国科学院矿物学与成矿学重点实验室_会议论文
Recommended Citation
GB/T 7714
王展,王智琳,许德如,等. 海南石碌铁多金属矿床碳酸盐岩地球化学特征及其地质意义[C],2017.
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