| 驼路沟钴金矿床地质特征与成因初探 |
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| 引用本文： | 李琳业,许存胜,陈建洲.驼路沟钴金矿床地质特征与成因初探[J].中国工程科学,2005(4). |
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| 作者姓名： | 李琳业 许存胜 陈建洲 |
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| 作者单位： | 青海省地质调查院 西宁810012 |
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| 摘 要： | 驼路沟钴、金矿位于东昆仑褶皱系昆南断褶带内,产于晚古生代二叠系下统石英片岩中。矿床在区域变质作用的基础上,构造活动继续,现有的裂隙再次开启,后期中低温热液沿着构造薄弱带进一步将钴、金元素活化富集成矿。
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| 关 键 词： | 驼路沟 构造破碎蚀变带 绢云母石英片岩 |
The Geologic Characteristics and the Formation Cause of Cobalt and Gold Deposit in Tuolugou |
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| Li Linye,Xu Cunsheng,Chen Jianzhou.The Geologic Characteristics and the Formation Cause of Cobalt and Gold Deposit in Tuolugou[J].Engineering Science,2005(4). |
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| Authors: | Li Linye Xu Cunsheng Chen Jianzhou |
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| Abstract: | Tuoluogou cobalt and gold deposit is in the south of the east Kunlun drape. It formed in quartz schist in the forepant Permian of late vecent life. On the basis of regional metamorphism,the conformation activities continued,the cracks opend again. The middle and low temperatured hot liquid caused the gathering of the cobalt and gold elements,and finally the deposit was formed. |
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| Keywords: | Tuolugou sericite structure alteration enlope quartz schist |
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