| 青海省肯德可克金矿热水沉积层矽卡岩特征及成矿意义 |
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| 引用本文： | 高章鉴,罗才让,井继锋.青海省肯德可克金矿热水沉积层矽卡岩特征及成矿意义[J].西北地质,2001,34(2):50-53. |
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| 作者姓名： | 高章鉴 罗才让 井继锋 |
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| 作者单位： | 西北有色地质研究所, |
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| 基金项目： | 中国有色金属工业总公司重点找矿科研项目资助(项目编号96-D-24) |
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| 摘 要： | 热水沉积成因层矽卡岩在青海省肯德可克金矿区非常发育。其产出特征，结构、构造及与岩体的关系等与接触交代型矽卡岩都有显著的区别，层矽卡岩是该区金矿化主要控矿因素之一，同时也是重要区域找矿标志。
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| 关 键 词： | 热水沉积 层矽卡岩 肯德可克金矿床 找矿标志 祁漫塔格 青海 |
| 文章编号： | 1009-6248(2001)02-0050-53 |
| 修稿时间： | 2000年8月7日 |
Features and mineralization significance of stratiform skarns of hydrothermal fluid sedimentary origin in |
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| GAO Zhang-jian,LUO Cai-rang,JING Ji-feng.Features and mineralization significance of stratiform skarns of hydrothermal fluid sedimentary origin in[J].Northwestern Geology,2001,34(2):50-53. |
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| Authors: | GAO Zhang-jian LUO Cai-rang JING Ji-feng |
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| Abstract: | The stratiform skarns of hydrothermal fluid sedimentary origin are well developed in Kendekoke gold deposit,Qinhai province And their development features,textures,structures and the relation with magma intrusion are obviously different from the skarns of contact metasometic origin type The stratiform skarn is a major factor of gold mineralization control and the regional ore-searching criteria |
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| Keywords: | Hydrothermal fluid sediment stratiform skarns Kendekoke gold deposit Qinhai |
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