首页 | 本学科首页   官方微博 | 高级检索  
     检索      

云南大平掌铜-多金属矿床成矿金属来源初探
引用本文:钟宏,胡瑞忠,叶造军.云南大平掌铜-多金属矿床成矿金属来源初探[J].地质科学,2001,36(1):72-82.
作者姓名:钟宏  胡瑞忠  叶造军
作者单位:1. 中国科学院地质与地球物理研究所岩石圈构造演化开放研究实验室 北京 100029;2. 中国科学院地球化学研究所 贵阳 550002
摘    要:大平掌铜-多金属矿床是我国西南“三江”地区新发现的火山岩型块状硫化物矿床,微量元素、稀土元素及铅同位素地球化学研究表明,成矿金属元素主要来源于对流循环的海底热卤水对火山岩围岩的淋滤作用。成矿过程中细碧岩、角斑岩、石英角斑岩均可能提供较多的Cu、Au,角斑岩、石英角斑岩可能贡献较多的Pb,而角斑岩则可能提供较多的Zn。

关 键 词:块状硫化物矿床  成矿金属  火山岩  大平掌
收稿时间:1999-12-30
修稿时间:1999年12月30

PRELIMINARY STUDY ON ORIGIN OF ORE-FORMING MATERIALS IN DAPINGZHANG COPPER-METALLIC DEPOSIT, YUNNAN PROVINCE
Zhong Hong , Hu Ruizhong Ye Zaojun.PRELIMINARY STUDY ON ORIGIN OF ORE-FORMING MATERIALS IN DAPINGZHANG COPPER-METALLIC DEPOSIT, YUNNAN PROVINCE[J].Chinese Journal of Geology,2001,36(1):72-82.
Authors:Zhong Hong  Hu Ruizhong Ye Zaojun
Institution:1. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029;2. Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002
Abstract:The Dapingzhang copper metallic deposit is volcanic hosted massive sulfide (VHMS) deposit recently found in the Sanjiang region, SW China. The characteristics of trace element, rare earth element and lead isotope geochemistry indicate that the ore forming metals were mostly leached from the volcanic rocks through the convective circulation of hot brine water on seafloor. Furthermore, Cu, Au are possibly mainly derived from the spilite, keratophyre and quartz keratophyre, while Pb mostly came from the keratophyre and quartz keratophyre, and Zn could be provided by the keratophyre. The volcanic rocks and ores characterized by high concentrations of radiogenic lead indicate the same original area.
Keywords:Volcanic  hosted massive sulfide (VHMS) deposit  Ore  forming metals  Volcanic rocks    Dapingzhang
本文献已被 CNKI 维普 万方数据 等数据库收录!
点击此处可从《地质科学》浏览原始摘要信息
点击此处可从《地质科学》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号