| 青海省祁连县热水沟铁矿地质特征及成因探讨 |
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| 引用本文： | 杨银成,周金玺,彭勇,沈刚刚. 青海省祁连县热水沟铁矿地质特征及成因探讨[J]. 黄金科学技术, 2007, 15(6): 30-34 |
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| 作者姓名： | 杨银成 周金玺 彭勇 沈刚刚 |
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| 作者单位： | 青海省有色地质矿产勘查院,西宁,810007;青海省有色地质矿产勘查院,西宁,810007;青海省有色地质矿产勘查院,西宁,810007;青海省有色地质矿产勘查院,西宁,810007 |
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| 摘 要： | 热水沟铁矿矿体主要受早奥陶世阴沟群地层控制，其成因为火山—沉积变质矿床，找矿标志为早奥陶世阴沟群及矿区内磁异常。
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| 关 键 词： | 铁矿床 基本特征 矿床成因 找矿标志 热水沟 |
| 文章编号： | 1005-2518（2007）06-0030-05 |
| 收稿时间： | 2007-08-28 |
| 修稿时间： | 2007-10-15 |
Geological Characteristics and Original Discussion of Eastern Reshuigou Iron Deposit in Qilian County, Qinghai |
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| YANG Yincheng,ZHOU Jinxi,PENG Yong,SHEN Ganggang. Geological Characteristics and Original Discussion of Eastern Reshuigou Iron Deposit in Qilian County, Qinghai[J]. Gold Science and Technololgy, 2007, 15(6): 30-34 |
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| Authors: | YANG Yincheng ZHOU Jinxi PENG Yong SHEN Ganggang |
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| Affiliation: | Geology and Mineral Exploration Institute，Qing Hai Provincal Bureau Geology and Mineral Exploration，Xi Ning 810007，China |
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| Abstract: | The Iron ore at east Reshuigou is form early ordovician epoch , the stratum is a mainly controlled by the stratum of Yingouqun which condition to find The Iron ore there. And another condition is abnormality of magnetism. The Iron ore form for volcanic-deposit metamorphose . |
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| Keywords: | iron deposit essential features cause of deposit formation condition of finding ore Reshuigou |
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