[1]李传华 廖航.广西镇龙山锑金多金属矿床成矿模式初论——以小圣矿区为例[J].大众科技,2014,16(09):139-141.
Discussion on mineralization model of gold-antinomy poly metal ores fromZhenlongshan,Guangxi——Taking Xiaosheng deposit as example[J].Popular Science & Technology,2014,16(09):139-141.
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广西镇龙山锑金多金属矿床成矿模式初论——以小圣矿区为例()
《大众科技》[ISSN:1008-1151/CN:45-1235/N]
- 卷:
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第16卷
- 期数:
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2014年09期
- 页码:
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139-141
- 栏目:
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资源与环境
- 出版日期:
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2014-12-29
文章信息/Info
- Title:
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Discussion on mineralization model of gold-antinomy poly metal ores fromZhenlongshan,Guangxi——Taking Xiaosheng deposit as example
- 文章编号:
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1008-1151(2014)09-0139-03
- 作者:
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李传华1 廖航2
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1.广西有色金属集团资源勘查有限公司，广西 南宁 530021；2.广西有色金属集团有限公司，广西 南宁 530021
- 关键词:
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镇龙山; 锑金多金属矿; 成矿模式
- Keywords:
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Zhen Long Shan; antimony gold polymetallic deposit; metallogenic model
- 分类号:
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TD1
- 文献标志码:
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A
- 摘要:
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镇龙山小圣矿区发育锑金等多种矿体，严格受断裂控制，且以岩体为中心存在明显的元素分带。通过分析，认为其成矿物质来源与地层和岩浆岩都有密切关系。结合华南板块构造演化史，认为镇龙山锑金多金属矿床的成因为先改造富集，后受岩浆热液富集并沿断裂充填成矿。
- Abstract:
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A wide variety of ore bodies, such as antimony and gold, are developed in Xiaosheng deposit, Zhenglongshan. They arestrictly controlled by fault and elementary zonation centering on intrusive rock exists. Mineralization material is related to not only layerbut also intrusive rock by analyze, combining with tectonic evolution history of Southern China Block that antimony and goldpolymetallic deposits of Zhenglongshan experienced modification and enrichment first and then enrichment by magma hydrothermalfluid and filling in fault to mineralize.
参考文献/References:
[1] 王亚雄.无水氯化亚锡制备工艺研究[J].锡业科技, 2000,(1):9-11.[2] 卡伊榭失.晶体形成与生长的基本理论[J].物理通报,1962,(1):1-12.
备注/Memo
- 备注/Memo:
-
【收稿日期】2014-08-11【作者简介】李传华，供职于广西有色金属集团资源勘查有限公司。
更新日期/Last Update:
2016-03-28