| 塔里木西南缘MVT型铅锌矿床流体包裹体研究 |
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| 引用本文： | 王书来,汪东波,祝新友.塔里木西南缘MVT型铅锌矿床流体包裹体研究[J].矿产与地质,2001,15(4):238-242. |
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| 作者姓名： | 王书来 汪东波 祝新友 |
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| 作者单位： | 北京矿产地质研究所, |
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| 摘 要： | 对塔里木板块西南缘塔木、卡兰古、乌苏里克、卡拉牙斯卡克等铅锌矿区的矿物流体包裹体研究表明，流体包裹体类型单一，多为流相包裹体，成矿流体具有低温、中高盐度、高密度特征、是富含Ca^2 ,Mg^2 ,Na^ 离子及有机烃类物质和硫化氢气体的热卤水。矿化剂主要是Cl^-离子，可与北美典型密西西比河谷型铅锌矿类比。
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| 关 键 词： | 成矿流体 MTV铅型锌矿床 塔里木盆地 流体包裹体 矿床地质 盐度 温度 |
| 文章编号： | 1001-5663(2001)04-0238-05 |
| 修稿时间： | 2000年12月12 |
THE FLUID INCLUSION IN MVT LEAD ZINC DEPOSIT IN SOUTHWEST MARGIN OF TARIM |
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| WANG Shu lai,WANG Dong bo,ZHU Xin you.THE FLUID INCLUSION IN MVT LEAD ZINC DEPOSIT IN SOUTHWEST MARGIN OF TARIM[J].Mineral Resources and Geology,2001,15(4):238-242. |
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| Authors: | WANG Shu lai WANG Dong bo ZHU Xin you |
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| Abstract: | MVT lead zinc deposit occurred in late Proterozoic carbonate platform in the southwest margin of Tarim plate in Xingjiang Orebody is controlled by brecciated zone among the carbonate rock.Research the ore fluid inclusion's chemical composition of the mineral district in Tamu?Kalangu?Wusulike?Kalayasikake and so on. It make known:the ore fluid inclusion's type simple. It is liquidoid inclusion majority, ore fluid has the feature: low temperature? High salinity? high density and so on, It is rich in Ca 2+ Mg 2+ Na + ionic and organic hydrocarbon material and hepatic gas's hot brine.mineralizer is Cl , ion mainly. It is similar to typical Mixixibi valley type lead zinc deposit in Northem American. |
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| Keywords: | Xinjiang Southwest margin of Tarim ore fiuid MVT Lead Zinc deposit |
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