| 滇西云龙混合岩化高温热液锡矿床 |
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| 引用本文： | 王玲,孙杭军. 滇西云龙混合岩化高温热液锡矿床[J]. 云南地质, 2012, 0(1): 32-35 |
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| 作者姓名： | 王玲 孙杭军 |
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| 作者单位： | 云南省地质矿产勘查院大理矿产所;云南黄金矿业集团股份有限公司 |
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| 摘 要： | 矿床产于区域性主干断裂旁侧、向斜轴部发育的断裂带中,严格受构造控制。混合岩化花岗岩与锡的形成、富集关系密切,是成矿的母岩。
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| 关 键 词： | 混合岩化 高温热液 锡石—石英电气石型 云南云龙 |
THE YUNLONG MIGMATIZED HIGH T HYDROTHERMAL SN DEPOSIT IN W YUNNAN |
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| WANG Ling,SUN Hang-jun. THE YUNLONG MIGMATIZED HIGH T HYDROTHERMAL SN DEPOSIT IN W YUNNAN[J]. Yunnan Geology, 2012, 0(1): 32-35 |
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| Authors: | WANG Ling SUN Hang-jun |
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| Affiliation: | 1.Yunnan Exploration Institute of Geology&Mineral Resources,Dali 671000)(2.Yunnan Company(Ltd)of Au Mining Group,Heqing 671507) |
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| Abstract: | The ore deposit exists in the fault zone of syncline axis beside the main regional fault,which is controlled strictly by the structure.The Sn formation and concentration are in close relation with the migmatized granite which is the mother rock of metallogenesis. |
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| Keywords: | Migmatization High T Thermal Fluid Cassiterite-Quartz Tourmaline Type Yunlong,Yunnan |
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