| 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,(4):62-68 |
| 八卦庙超大型金矿地球化学特征及物源 |
| GEOCHEMICAL CHARACTERISTICS AND GENESIS OF BAGUAMIAO SUPER-LARGE GOLD DEPOSIT |
| 投稿时间：1999-05-24 修订日期：1999-08-30 |
| DOI：10.6053/j.issn.1001-1412.1999.4. 010 |
| 中文关键词: 金矿 稀土元素 同位素 下地壳 成矿物质来源 陕西 |
| 英文关键词:gold deposit REE S-Si-H-O-C isotope material source lower crust Shanxi Province |
| 基金项目:国家“九五”科技(攻关)项目96-914-04-02A |
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| 中文摘要: |
| 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,结合金矿床与深大断裂的时空分布特点,以及与秦岭热水沉积铅锌矿床和双王喷流沉积金矿床的对比研究,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。 |
| 英文摘要: |
| 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. |
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