| 江西大背坞金矿床地球化学研究 |
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| 引用本文： | 刘建民,王平安,董法先,陈柏林.江西大背坞金矿床地球化学研究[J].矿物岩石地球化学通报,1997(4). |
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| 作者姓名： | 刘建民 王平安 董法先 陈柏林 |
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| 作者单位： | 中国地质科学院地质力学研究所 |
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| 摘 要： | 江西大背坞金矿床地球化学研究刘建民王平安董法先陈柏林（中国地质科学院地质力学研究所，北京１０００８１）关键词地球化学金矿床大背坞江西１矿床地质特征及矿区地球化学场大背坞金矿床位于江西省浮梁县，属含金石英脉型高中温岩浆热液矿床。矿区地层为中元古代双桥山...
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| 关 键 词： | 地球化学 金矿床 大背坞 江西 |
Study on Geochemistry of Dabeiwu Gold Deposit,Jiangxi Province |
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| Liu Jianmin,Wang Pingan,Dong Faxian,Chen Bailin.Study on Geochemistry of Dabeiwu Gold Deposit,Jiangxi Province[J].Bulletin of Mineralogy Petrology and Geochemistry,1997(4). |
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| Authors: | Liu Jianmin Wang Pingan Dong Faxian Chen Bailin |
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| Abstract: | The Dabeiwu gold deposit is a magmatic hydrothermal deposit.Based on the analysis and comparison of the trace elements, REE and isotope characteristics of metamorphic rocks in the Shuangqiaoshan group and of the magmatic rocks and different ores, it was suggested that the metamorphic rocks were the main source bed of the gold ores,and part of ore forming material was derived from the magmatic rocks. Changes of contents and main ratios of trace elements and their combination in different ore belts along the depth indicated that the discovered orebodies were located in the mid upper section of the whole deposit,so it is very possible that there exists a good prospect in the lower section of this deposit. |
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| Keywords: | geochemistry gold deposit Dabeiwu Jiangxi Province |
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