| 新疆莫托萨拉地区铜矿地质特征及成因 |
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| 引用本文： | 李随领,欧长可,赵金洲,张志娜,李璨.新疆莫托萨拉地区铜矿地质特征及成因[J].矿产勘查,2018,9(10):1952-1956. |
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| 作者姓名： | 李随领 欧长可 赵金洲 张志娜 李璨 |
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| 作者单位： | 河南省有色金属地质矿产局第五地质大队,郑州 450016;河南省有色金属矿产探测工程技术研究中心,郑州 450016,河南省有色金属地质矿产局第五地质大队,郑州 450016;河南省有色金属矿产探测工程技术研究中心,郑州 450016,河南省有色金属地质矿产局第五地质大队,郑州 450016;河南省有色金属矿产探测工程技术研究中心,郑州 450016,河南省有色金属地质矿产局第五地质大队,郑州 450016;河南省有色金属矿产探测工程技术研究中心,郑州 450016,河南省有色金属地质矿产局第五地质大队,郑州 450016;河南省有色金属矿产探测工程技术研究中心,郑州 450016 |
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| 摘 要： | 莫托萨拉一带区域上受那拉提山南缘和北缘两条深大断裂控制,区内岩浆活动频繁,断裂构造发育。铜矿化位于花岗岩体内部、岩体边部接触带以及石炭系火山沉积地层内,赋矿岩体具有显著的正铕异常以及埃达克岩的地球化学特征,具有寻找铜矿的良好潜力。
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| 关 键 词： | 铜矿 地质特征 莫托萨拉 新疆 |
| 收稿时间： | 2018/5/31 0:00:00 |
Geological Characteristics and Genesis of Copper Deposits In Moto Sara,Xinjiang |
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| LI Sui-ling,OU Chang-ke,ZHAO Jin-zhou,ZHANG Zhi-na and LI Can.Geological Characteristics and Genesis of Copper Deposits In Moto Sara,Xinjiang[J].Mineral Exploration,2018,9(10):1952-1956. |
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| Authors: | LI Sui-ling OU Chang-ke ZHAO Jin-zhou ZHANG Zhi-na and LI Can |
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| Affiliation: | Henan Province Non-ferrous Metals Geological and Mineral Resources Bureau No.5 Geological Team,Zhengzhou 450016;Henan Province Non-ferrous Metal Mineral Exploration Engineering Technology Research Center,Zhengzhou 450016,Henan Province Non-ferrous Metals Geological and Mineral Resources Bureau No.5 Geological Team,Zhengzhou 450016;Henan Province Non-ferrous Metal Mineral Exploration Engineering Technology Research Center,Zhengzhou 450016,Henan Province Non-ferrous Metals Geological and Mineral Resources Bureau No.5 Geological Team,Zhengzhou 450016;Henan Province Non-ferrous Metal Mineral Exploration Engineering Technology Research Center,Zhengzhou 450016,Henan Province Non-ferrous Metals Geological and Mineral Resources Bureau No.5 Geological Team,Zhengzhou 450016;Henan Province Non-ferrous Metal Mineral Exploration Engineering Technology Research Center,Zhengzhou 450016 and Henan Province Non-ferrous Metals Geological and Mineral Resources Bureau No.5 Geological Team,Zhengzhou 450016;Henan Province Non-ferrous Metal Mineral Exploration Engineering Technology Research Center,Zhengzhou 450016 |
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| Abstract: | The region of Moto Sara is controlled by two deep faults in the north and south margina of Nalati Mountain. Magma activities are frequent and the faults are developed in this area. The copper mineralization is located in the inside of granite body, the contact zone at the edge of the rock mass and the Carboniferous volcanic sedimentary strata. The ore-bearing rocks have significant positive europium anomalies and geochemical characteristics of the adakite,with good potential for prospecting copper deposits. |
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| Keywords: | copper deposit geological characteristics Moto Sara Xinjiang |
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