| 镇康天生桥矽卡岩型铁矿 |
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| 引用本文： | 邓云,张兴恒,王华,付冬梅.镇康天生桥矽卡岩型铁矿[J].云南地质,2009,28(2):148-151. |
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| 作者姓名： | 邓云 张兴恒 王华 付冬梅 |
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| 作者单位： | 云南南方地勘工程总公司保山分公司,云南,保山,678000 |
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| 摘 要： | 矿床产于上寒武统变质岩系中，形成与深部热液上升交代碳酸盐岩有关，明显受岩性、层位及构造控制。成因上与隐伏酸性岩体热液上升交代与有关，为矽卡岩型铁矿。
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| 关 键 词： | 变质岩系 矽卡岩型铁矿 热液上升交代 云南镇康 |
THE TIANSHENGQIAO SKARN FE DEPOSIT IN ZHENKANG |
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| DENG Yun,ZHANG Xing-heng,WANG Hua,FU Dong-mei.THE TIANSHENGQIAO SKARN FE DEPOSIT IN ZHENKANG[J].Yunnan Geology,2009,28(2):148-151. |
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| Authors: | DENG Yun ZHANG Xing-heng WANG Hua FU Dong-mei |
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| Institution: | ( Baoshan Branch, South Geoexploration Engineering Company of Yunnan General, Baoshan 678000) |
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| Abstract: | The Tianshengqiao Fe deposit is formed in Late Cambrian metamorphic rock series, which is in relation to the metasomasis of rising deep thermal fluid with carbonate rock and evidently controlled by the lithological character, horizon and structure. The genesis of this ore deposit is related with the metasomasis of rising thermal fluid of a blind acid rock body, which belongs to the Fe deposit of skam type. |
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| Keywords: | Metamorphic Rock Series Fe Deposit of Skarn Type Metasomasis of Rising Thermal Fluid Zhenkang Yunnan |
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