| 辽宁王家崴子金矿床地球化学研究 |
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| 引用本文： | 郝瑞霞,彭省临.辽宁王家崴子金矿床地球化学研究[J].黄金地质,1999,5(2):47-51. |
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| 作者姓名： | 郝瑞霞 彭省临 |
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| 作者单位： | 中南工业大学 |
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| 摘 要： | 王家崴子金矿床赋存于辽南古元古代浅变质岩系中。矿床的微量元素、稀土元素及稳定同位素地球化学天空表明，成矿元素和成矿热液具有多来源，盖县组地层和岩浆水分别是主要的矿源层和成矿流体；中生代的构造岩浆活动导致金的多次富集；成矿主要集中于燕山期。王家崴子金矿床是具有多来源的岩浆热液型矿床。
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| 关 键 词： | 金矿床 微量元素 稀土元素 稳定同位素 地球化学 |
GEOCHEMICAL STUDY OF WANGJIAWAIZI GOLD DEPOSIT IN LIAONING |
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| Hao Ruixia,Peng Shenglin.GEOCHEMICAL STUDY OF WANGJIAWAIZI GOLD DEPOSIT IN LIAONING[J].Gold Geology,1999,5(2):47-51. |
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| Authors: | Hao Ruixia Peng Shenglin |
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| Abstract: | Wangjiawaizi gold deposit occurrs in Lower Proterozoic opimetamorphic rock series. Geochemical studies of trace elements, REE and stable isotopes indicate that the ore forming elements and ore forming hydrothermal solution have multi source. Gaixian Group and magmatic water are respectively the main source bed and ore forming fluid. Mesozoic tectonomagmatic activities have led to the multi stage gold mineralization and gold mineralization mainly occurrs in Yanshan Period. Wangjiawaizi gold deposit is a multi origin magmatic hydrothermal deposit. |
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| Keywords: | gold deposit trace element REE stable isotope Liaoning |
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