| 红旗岭矿区2号岩体岩浆型硫化铜镍矿床成矿规律及找矿意义 |
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| 引用本文： | 刘俊梅,张宏,冯修云,周树亮.红旗岭矿区2号岩体岩浆型硫化铜镍矿床成矿规律及找矿意义[J].吉林地质,2010,29(4):39-42. |
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| 作者姓名： | 刘俊梅 张宏 冯修云 周树亮 |
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| 作者单位： | [1]吉林吴融有色金属集团有限公司资源开发公司,吉林磐石132311 [2]吉林省有色金属地质勘查局607队,吉林吉林市132105 |
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| 摘 要： | 红旗岭矿区2号岩体硫化铜镍矿床位于红旗岭矿区Ⅰ岩带上,辉发河深大断裂带北西侧,富家-何家-北兴隆-长胜断裂构造系统中,并侵位于北兴隆复背斜的轴面核心位置,是Ⅰ岩带上一个较大的镁铁—超镁铁质岩体。辉发河深大断裂为岩体的形成提供幔源岩浆上升的通道,其主要扮演了一种导矿构造,而在富家-何家-北兴隆-长胜次级断裂为2号岩体的形成提供了容矿空间,也是重要的容矿构造,同时矿体的富集受岩体岩相的制约。
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| 关 键 词： | 岩浆型铜镍矿床 成矿规律 找矿意义 2号岩体 红旗岭 |
Metallogenic regularity and prospecting significance of magmatic sulfide copper-nickel deposit of No.2 rock body of Hongqiling mining area |
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| LIU Jun-mei,ZHANG Hong,FENG Xiu-yun,ZHOU Shu-liang.Metallogenic regularity and prospecting significance of magmatic sulfide copper-nickel deposit of No.2 rock body of Hongqiling mining area[J].Jilin Geology,2010,29(4):39-42. |
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| Authors: | LIU Jun-mei ZHANG Hong FENG Xiu-yun ZHOU Shu-liang |
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| Institution: | 1.Jilin Haorong Nonferrous Metals Co.,Ltd,Jilin 132311,Jilin,China 2.Team 607,Bureau of Nonferrous Metals Geological Exploration of Jilin Province,Jilin 132105,Jilin,China |
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| Abstract: | The fulfi de copper-nickel deposit of No.2 rock body of Hongqiling mining area is located in the No.1 rock belt,the NW of Huifahe deep faulted zone,Fujia-Hejia-Beixinglong-Changsheng faulted structures,emplaced in the axial core position of the Beixinglong compositic anticline,which is a larger mafic-ultramafi c rock body in the No.1 rock belt.The rock body formation of Huifahe deep fault provides a channel-way for mantle-derived magma rising,acting as a structure as passage-way for ore fluid;Fujia-Hejia-Beixinglong-Changsheng secondary fault provides a space for the formation of the No.2 rock body,it also an important host structure,meanwhile,the enrichment of ore bodies is controlled by rock body and rock facies. |
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| Keywords: | magmatic sulfide copper-nickel deposit metallogenic regularity prospecting significance No 2 rock body Hongqiling |
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