| 冀西北四台沟金矿地球化学原生晕特征及晕扩散模式 |
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| 引用本文： | 魏俊浩.冀西北四台沟金矿地球化学原生晕特征及晕扩散模式[J].黄金地质,1995,1(3):67-71. |
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| 作者姓名： | 魏俊浩 |
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| 作者单位： | 中国地质大学 |
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| 摘 要： | 简要介绍了四台沟金矿的地质特征，在此基础上系统讨论了该矿床中Ｆ１０断裂主要控矿地段的地球化学原生晕的空间特征，最后归纳总结了热液型金矿床原生晕的扩散模式。
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| 关 键 词： | 原生晕 扩散模式 金矿床 地球化学 |
THE FEATURE AND DIFFUSION MODEL OFGEOCHEMICAL PRIMARY HALO IN SITAIGOU GOLDDEPOSIT,NORTHWESTERN HEBEI |
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| Wei Junhao.THE FEATURE AND DIFFUSION MODEL OFGEOCHEMICAL PRIMARY HALO IN SITAIGOU GOLDDEPOSIT,NORTHWESTERN HEBEI[J].Gold Geology,1995,1(3):67-71. |
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| Authors: | Wei Junhao |
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| Abstract: | Based on the geological features of Sitaigou gold deposit,the author systematically discusses the spatial features of geochemical primary halo in the main orecontrol section of F10 fault and finally puts forward a diffusion model for the primary halo of hydrothermaltype gold deposit. |
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| Keywords: | Hebei gold deposit primary halo diffusion model |
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