| 八卦庙超大型金矿地球化学特征及物源 |
| |
| 引用本文： | 吴烈善,韦龙明. 八卦庙超大型金矿地球化学特征及物源[J]. 地质找矿论丛, 1999, 14(4): 62-68 |
| |
| 作者姓名： | 吴烈善 韦龙明 |
| |
| 作者单位： | 有色矿产地质研究院,广西,桂林,541004 |
| |
| 基金项目： | 国家“九五”科技(攻关)项目!96-914-04-02A |
| |
| 摘 要： | 文章论述了八卦庙矿床围岩和含金石英脉的稀土元素及硫、硅、氢、氧、碳的同位素地球化学特征，结合合金矿床与深大断裂的时空分布特点，以及与秦只铅锌矿床和双王喷流沉积金床的对比研究，论证了八卦庙金矿的主要成矿物质来源于地壳深部，甚至上地幔。
|
| 关 键 词： | 金矿 稀土元素 同位素 下地壳 成矿物质来源 陕西 |
| 收稿时间： | 1999-05-24 |
| 修稿时间： | 1999-05-24 |
GEOCHEMICAL CHARACTERISTICS AND GENESIS OF BAGUAMIAO SUPER-LARGE GOLD DEPOSIT |
| |
| WU Lie-shan and WEI Long-ming. GEOCHEMICAL CHARACTERISTICS AND GENESIS OF BAGUAMIAO SUPER-LARGE GOLD DEPOSIT[J]. Contributions to Geology and Mineral Resources Research, 1999, 14(4): 62-68 |
| |
| Authors: | WU Lie-shan and WEI Long-ming |
| |
| Affiliation: | Research institute of geology for mineral resources, Guilin 541004, China;Research institute of geology for mineral resources, Guilin 541004, China |
| |
| Abstract: | Through the research on the features of REE,S,Si,H,O and C isotopes of Baguamiao gold deposit''s wall-rocks and auriferous quartz and comparing Baguamiao gold deposit with Qinling hotwater-sediment-hosted Pb-Zn deposits and Shuangwang spout sediment-hosted gold deposit, the authors conclude that metallogentic material was derived mainly form lower crust, even from upper mantle. |
| |
| Keywords: | gold deposit REE S Si H O C isotope material source lower crust Shanxi Province |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
| 点击此处可从《地质找矿论丛》浏览原始摘要信息 |
|
点击此处可从《地质找矿论丛》下载免费的PDF全文 |
