| 杉松岗钴(铜镍)矿床地质特征及找矿远景 |
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| 引用本文： | 刘文香,王坤.杉松岗钴(铜镍)矿床地质特征及找矿远景[J].吉林地质,2006,25(3):24-28. |
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| 作者姓名： | 刘文香 王坤 |
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| 作者单位： | 吉林省有色金属地质勘查局六○二队,吉林,白山,134300 |
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| 摘 要： | 杉松岗钴(铜镍)矿床产于古元古代裂谷海槽褶皱地带,是国内新近发现的新类型矿床.它赋存于老岭群富硼、碳粘土岩夹硅质岩建造之中.通过对矿床的地质、地球化学特征研究,初步认为该矿床受后期变质热波的强烈叠加作用,形成沉积变质热液叠加改造型矿床.同时阐述了该矿床地质特征及找矿远景.
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| 关 键 词： | 富硼建造 沉积变质热液 叠加改造 杉松岗钴(铜镍)矿床 |
| 文章编号： | 1001-2427(2006)03-024-05 |
| 修稿时间： | 2005年8月5日 |
Geologic features of Shasonggang Co (Cu, Ni) deposit and prospecting perspective |
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| LIU Wen-xiang,WANG Kun.Geologic features of Shasonggang Co (Cu, Ni) deposit and prospecting perspective[J].Jilin Geology,2006,25(3):24-28. |
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| Authors: | LIU Wen-xiang WANG Kun |
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| Abstract: | Shasonggang Co(Cu,Ni) deposit occurs in Laoling Group,rich boron,carbon clay rock with siliceous rock formation,Paleoproterozoic rift trough folded belt,which is the domestic a new type deposit.Through the study for geologic,geochemical characteristics of deposit,it is preliminarily considered that strong superimposed metamorphism by the late hydrothermal metamorphism form a remarking sedimentary metamorphic hydrothermal superimposed deposit.Meanwhile,geologic features and prospecting perspective are expounded in this paper. |
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| Keywords: | rich boron formation sedimentary metamorphic hydrothermal superimposed remarking Shasonggang Co(Cu Ni) deposit |
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