| 香格里拉县地苏嘎铜多金属矿矿床成因浅析 |
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| 引用本文： | 张海鸥,缪磊.香格里拉县地苏嘎铜多金属矿矿床成因浅析[J].云南地质,2014(2):226-229. |
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| 作者姓名： | 张海鸥 缪磊 |
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| 作者单位： | 云南省地质矿产勘查院大理地质矿产所,云南大理671000 |
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| 摘 要： | 地苏嘎铜多金属矿位于三江成矿域中甸斑岩型铅锌铜多金属成矿带.含矿岩石主要为白云岩、砂质绢云板岩或石英脉等,矿床属中—低温热液充填交代与变质岩层状矿床等复合的铜多金属矿床.
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| 关 键 词： | 铜多金属矿 中—低温热液矿床 云南云南省香格里拉县地苏嘎 |
A PRELIMINARY GENETIC ANALYSIS OF DISUGA CU MULTIMETALLIC DEPOSIT IN XIANGGELILA |
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| ZHANG Hai-ou,MIAO Lei.A PRELIMINARY GENETIC ANALYSIS OF DISUGA CU MULTIMETALLIC DEPOSIT IN XIANGGELILA[J].Yunnan Geology,2014(2):226-229. |
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| Authors: | ZHANG Hai-ou MIAO Lei |
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| Affiliation: | (Dali Institute, Yunnan Exploration Institute of Geology ＆ Mineral Resources, Dali 671000) |
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| Abstract: | Disuga Cu multimetallic deposit is in Zhongdian porphyry Pb-Zn-Cu muhimetallic metallogenetic zone of Sanjiang metallogenetie domain. The main ore-bearing rocks are dolomitite, sandy serieitic slate or quartz vein, etc. It belongs to the composite Cu multimetallic deposit of middle-low T hydrothermal filling metasomasis and metamorphic rock bedded ore deposit. |
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| Keywords: | Cu Muhimetallic Deposit Middle-Low T Hydrothermal Deposit Disuga Xianggelila Yunnan |
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