| 银山西区铜金铅锌矿床微量元素地球化学特征 |
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| 引用本文： | 周刚,韩东南. 银山西区铜金铅锌矿床微量元素地球化学特征[J]. 地质找矿论丛, 1997, 12(4): 23-34 |
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| 作者姓名： | 周刚 韩东南 |
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| 作者单位： | 中国有色金属工业总公司北京矿产地质研究所!北京，100012 |
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| 摘 要： | 对矿床微量元素的研究表明，矿区双桥山群地层和英安斑岩中，主要成矿元素Ｃｕ，Ａｕ，Ｐｂ，Ｚｎ等丰度很高，具有明显的富集，可以为矿床的形成提供足够的矿质来源，矿床的铜金矿化与铅锌矿化系不同的成矿阶段形成的，并存在矿化发带现象，在矿体中不同类型矿化生的微量元素存在着明显的差异，可以作为相应矿体的近矿指示元素。
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| 关 键 词： | 微量元素 铅锌矿床 地球化学 铜矿床 金矿床 |
| 收稿时间： | 1997-05-04 |
| 修稿时间： | 1997-08-05 |
STUDY ON MINOR ELEMENTS OF YINSHAN XIQU Cu-Au-Pb-Zn DEPOSIT, JIANGXI |
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| Zhou Gang and Han Dongnan. STUDY ON MINOR ELEMENTS OF YINSHAN XIQU Cu-Au-Pb-Zn DEPOSIT, JIANGXI[J]. Contributions to Geology and Mineral Resources Research, 1997, 12(4): 23-34 |
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| Authors: | Zhou Gang and Han Dongnan |
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| Affiliation: | Beijing Institute of geology for Mineral Resources, CNNC, Beijing 1000l2;Beijing Institute of geology for Mineral Resources, CNNC, Beijing 1000l2 |
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| Abstract: | tudy on minor elements in deposit indicates that 'main ore-forming elements are high inShuangqiaoshan Group stratum and dacite-potphyry and show enrichment indicating that theycan' provide enough ore materials during mineralizing process. The dePOist is characterized by Cu-Au, Pb~Zn mineralizations and ore zonation. The mineralhations were formed in different stagesand varied in minor elements which can be regarded as markers for the corresP0ndant ore bodies. |
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| Keywords: | minor element Cu-Au-Pb-Zn deposit Jiangxi Yinshan Xiqu |
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