| 北塔山三个泉一带金矿地质特征及其与岩脉的关系 |
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| 引用本文： | 高怀忠,张旺生,吕万军.北塔山三个泉一带金矿地质特征及其与岩脉的关系[J].新疆地质,1998(3). |
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| 作者姓名： | 高怀忠 张旺生 吕万军 |
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| 作者单位： | 中国地质大学!武汉430074 |
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| 基金项目： | 国家“305”项目!(96 - 915 - 0 2 - 0 6 - 0 1)研究成果 |
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| 摘 要： | 根据三个泉地区金矿与岩脉的空间关系和成矿流体盐度、成分及同位素的研究 ,认为金矿与岩脉具有成因关系。它们可能属同源、同通道上升的产物 ,因此 ,岩脉应是重要的找矿标志
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| 关 键 词： | 三个泉 金矿 岩脉 成矿流体 成因关系 |
GEOLOGY OF GOLD DEPOSITSIN SANGEQUAN AREA OF BEITASHAN AND ITSRELATION WITH DYKES |
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| Gao Huaizhong,Zhang Wangsheng,L u Wanjun.GEOLOGY OF GOLD DEPOSITSIN SANGEQUAN AREA OF BEITASHAN AND ITSRELATION WITH DYKES[J].Xinjiang Geology,1998(3). |
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| Authors: | Gao Huaizhong Zhang Wangsheng L u Wanjun |
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| Abstract: | The gold deposits in Sangequan area are believed to be associated genetically with the dykes based on the study of salinity,composition and isotopic data of ore fluid,and their spacial occurence with dykes. They are possibly comagmatic products rising along the same passage. Therefore these dykes are im- portant ore prospecting marks. |
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| Keywords: | Sangequan gold deposit dykes ore fluid genetic relationship |
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