| 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,(1):28-31,51 |
| 江西银山铅锌矿床成矿流体特征 |
| GEOLOGY AND ORE—FORMING FLUID TYPYS OF THE YINSHAN COPPER-LEAD-ZINC DEPOSIT, JIANGXI |
| 投稿时间：2000-06-09 修订日期：2001-01-29 |
| DOI：10.6053/j.issn.1001-1412.2001.1. 006 |
| 中文关键词: 银山铅锌矿 流体包裹体 同位素 成矿流体特征 江西 |
| 英文关键词:Yinshan Pb, Zn deposit fluid inclusion isotope ore-forming fluid Jiangxi |
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| 摘要点击次数: 1673 |
| 全文下载次数: 1948 |
| 中文摘要: |
| 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。 |
| 英文摘要: |
| 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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