| 云南保山黑牛凹破碎带蚀变岩型金矿 |
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| 引用本文： | 马云良,邹蓉蓉,王基元.云南保山黑牛凹破碎带蚀变岩型金矿[J].云南地质,2014(1):22-27. |
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| 作者姓名： | 马云良 邹蓉蓉 王基元 |
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| 作者单位： | 云南黄金矿业集团股份有限公司,云南昆明650215 |
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| 摘 要： | 上寒武统核桃坪组上段赋矿,近南北向断层控矿,含金矿化主要为硅化、黄铁矿化、磁黄铁矿化、黄铜矿化、绿泥石化构造角砾岩;云南保山黑牛凹金矿属中—低温热液交代型蚀变岩型金矿床.
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| 关 键 词： | 中—低温热液交代型蚀变岩型金矿床 控矿条件 核桃坪组 云南保山黑牛凹 |
HEINIUWA AU DEPOSIT OF ALTERATION ROCK TYPE OF FRACTURE ZONE IN BAOSHAN,YUNNAN |
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| MA Yun-liang,ZOU Rong-rong,WANG Ji-yuan.HEINIUWA AU DEPOSIT OF ALTERATION ROCK TYPE OF FRACTURE ZONE IN BAOSHAN,YUNNAN[J].Yunnan Geology,2014(1):22-27. |
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| Authors: | MA Yun-liang ZOU Rong-rong WANG Ji-yuan |
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| Institution: | ( Limited Company of Yunnan Gold Mining Group, Kunming 650215 ) |
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| Abstract: | The ore deposit is in Upper Cambrian Heitaoping Formation Upper Member, controlled by the nearly NS fault. The Au-bearing metallogenesis mainly silicification, pyritization, pyrrhotitization, chalcopyritiza- tion, chloritization structure breccia. It belongs to the middle-low T Au deposit of metasomatic alteration rock type. |
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| Keywords: | Middle-Low TCondition Heitaoping Formation Hydrothermal Au Deposit of Metasomatic Alteration Rock Type Ore ControlHeiniuwa Baoshan Yunnan |
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