| 内蒙古中兴屯铜多金属矿的地球化学化学异常特征 |
| |
| 引用本文： | 李伟, 毕中伟, 付俊彧. 内蒙古中兴屯铜多金属矿的地球化学化学异常特征[J]. 地质与资源, 2010, 19(3): 267-270. doi: 10.13686/j.cnki.dzyzy.2010.03.015 |
| |
| 作者姓名： | 李伟 毕中伟 付俊彧 |
| |
| 作者单位： | 沈阳地质矿产研究所, 辽宁 沈阳 110031 |
| |
| 摘 要： | 中兴屯铜多金属矿发育在古生界泥鳅河组浅变质岩与早侏罗世细粒花岗闪长岩外接触带上，属典型夕卡岩型铜多金属矿床.在1：5万水系沉积物异常区进行的1：1万土壤测量等地球化学勘察研究表明，异常主要为Cu、Au、Ag、Bi组合，并伴有W异常.通过对中兴屯铜多金属矿地球化学异常特征的分析，为在该区寻找夕卡岩型铜多金属矿提供了较好的前景.
|
| 关 键 词： | 铜多金属矿 地球化学 异常特征 中兴屯 内蒙古 |
| 收稿时间： | 2009-12-11 |
| 修稿时间： | 2010-01-05 |
GEOCHEMICAL ANOMALY CHARACTERISTICS OF THE ZHONGXINGTUN COPPER-POLYMETAL DEPOSIT IN INNER MONGOLIA |
| |
| LI Wei, BI Zhong-wei, FU Jun-yu. GEOCHEMICAL ANOMALY CHARACTERISTICS OF THE ZHONGXINGTUN COPPER-POLYMETAL DEPOSIT IN INNER MONGOLIA[J]. Geology and Resources, 2010, 19(3): 267-270. doi: 10.13686/j.cnki.dzyzy.2010.03.015 |
| |
| Authors: | LI Wei BI Zhong-wei FU Jun-yu |
| |
| Affiliation: | Shenyang Institute of Geology and Mineral Resources, Shenyang 110034, China |
| |
| Abstract: | The Zhongxingtun copper-polymetal deposit,located in the outer contacting belt between the epimetamorphic rocks of Paleozoic Niqiuhe formation of and the Early Jurassic fine-grained granodiorite,is of typical skarn-type.Stream sediment anomaly survey in 1∶50000 scale and soil geochemical survey in 1∶10000 scale show that the anomalies are mainly assemblage of Cu,Au,Ag and Bi,accompanied with W anomaly.Analysis on the geochemistry characteristics of Zhongxingtun Cu-polymetallic deposit reveals a great potential for the searching of ores of the same type in the area. |
| |
| Keywords: | Cu-polymetallic geochemistry anomaly characteristics Zhongxingtun deposit Inner Mongolia |
| 本文献已被 维普 万方数据 等数据库收录！ |
| 点击此处可从《地质与资源》浏览原始摘要信息 |
|
点击此处可从《地质与资源》下载全文 |
|
