| 江西银山铅锌矿床成矿流体特征 |
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| 引用本文： | 乐小横,张志辉.江西银山铅锌矿床成矿流体特征[J].地质找矿论丛,2001,16(1):28-31. |
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| 作者姓名： | 乐小横 张志辉 |
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| 作者单位： | 江西铜业公司银山铅锌矿, |
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| 摘 要： | 银山铅锌矿床产于前震旦系地层中 ,容矿围岩主要为千枚岩 ,矿体呈脉状受构造裂隙控制。流体包裹体及同位素研究表明金属元素及硫主要来自上地幔 ,流体主要是岩浆水。矿床属中低温岩浆热液矿床 ,为燕山期成矿
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| 关 键 词： | 银山铅锌矿 流体包裹体 同位素 成矿流体特征 江西 |
| 文章编号： | 1001-1412(2001)01-0028-04 |
| 修稿时间： | 2000年6月9日 |
GEOLOGY AND ORE—FORMING FLUID TYPYS OF THE YINSHAN COPPER—LEAD—ZINC DEPOSIT， JIANGXI |
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| LE Xiao heng,ZHANG Zhi hui.GEOLOGY AND ORE—FORMING FLUID TYPYS OF THE YINSHAN COPPER—LEAD—ZINC DEPOSIT， JIANGXI[J].Contributions to Geology and Mineral Resources Research,2001,16(1):28-31. |
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| Authors: | LE Xiao heng ZHANG Zhi hui |
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| Abstract: | Yinshan lead zinc deposit lies in the Presinian strata.The ore bodies occur in phyllite,are controlled by fault.Fluid inclusion and isolope studies show that the ore forming metals and sulfur came mainly from the mamtle,fluids were mixtures of mantle water and meteoric water.The ore deposit is a medium low temperature deposit formed in the Yanshanian epoch. |
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| Keywords: | Yinshan Pb Zn deposit fluid inclusion isotope ore forming fluid Jiangxi |
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