| 祁漫塔格地区铁多金属矿床成矿特征及成因探讨 |
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| 引用本文： | 谭文娟.祁漫塔格地区铁多金属矿床成矿特征及成因探讨[J].地质与勘探,2011,47(2):244-250. |
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| 作者姓名： | 谭文娟 |
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| 作者单位： | 中国地质调查局西安地质调查中心,陕西西安,710054 |
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| 基金项目： | 国家科技支撑计划项目(2006BAB01A01); 中国地质调查局地质大调查项目(1212010813046和1212010881632及1212010911032) |
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| 摘 要： | 祁漫塔格地处东昆仑造山带西段,该区建造组成丰富,断裂构造发育,断层构造以北西西走向为主,华力西-印支造山旋回中酸性侵入岩浆活动强烈.在综述祁漫塔格地区成矿地质背景基础上,通过对区内肯德可克铁钴铋金矿床、野马泉铁锌矿床和迪木那里克典型铁矿床地质特征分析,并以肯德可克矿床为例,对比了不同成因类型铁矿床中磁铁矿的化学成分组成...
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| 关 键 词： | 祁漫塔格 铁多金属矿 矿床地质特征 矿床成因 |
| 收稿时间： | 7/7/2010 12:00:00 AM |
| 修稿时间： | 2010/8/26 0:00:00 |
Metallogenic Features and Genesis of Fe Polymetallic Deposits in the Qimantage region |
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| TAN Wen-juan.Metallogenic Features and Genesis of Fe Polymetallic Deposits in the Qimantage region[J].Geology and Prospecting,2011,47(2):244-250. |
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| Authors: | TAN Wen-juan |
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| Institution: | (Xi’an Center,China Geological Survey,Xi’an,Shaanxi 710054) |
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| Abstract: | The Qimantage region is situated in the west segment of the East Kunlun orogenic belt,which is characterized by abundant formations and compositions,predominant NWW trending faults,and intensive intermediate-acid intrusive magma activity during the Variscan-Indosinian orogenic cycle.In this paper,we make a review of geological setting for metallogenesis in this region,and analyze the geological features the Kendekeke,Yemaquan,and Dimunalike Fe polymetallic deposits.Taking the Kendekeke deposit as an example... |
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| Keywords: | Qimantage Fe polymetallic deposit geological feature genesis |
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