| 青海都兰吉给申地区铜铅锌多金属矿床地质特征及找矿方向 |
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| 引用本文： | 肖文进.青海都兰吉给申地区铜铅锌多金属矿床地质特征及找矿方向[J].矿产与地质,2009,23(1). |
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| 作者姓名： | 肖文进 |
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| 作者单位： | 有色金属矿产地质调查中心,北京,100012 |
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| 摘 要： | 吉给申铜铅锌多金属矿床处于柴北缘铅锌银铜金多金属成矿带东段,受上奥陶统滩涧山群(O3tn)地层控制,文章介绍了铜铅锌多金属矿床的地质特征,认为其成因为热水沉积—热液改造型铜铅锌型矿床,提出找矿标志,结合以往资料,指出了该区的找矿方向。
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| 关 键 词： | 铜铅锌矿床 地质特征 找矿方向 吉给申 青海 |
Geological characteristics and prospecting direction of the Jijishen Cu-Pb-Zn polymetallic deposit in Dulan County, Qinghai |
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| XIAO Wen-jin.Geological characteristics and prospecting direction of the Jijishen Cu-Pb-Zn polymetallic deposit in Dulan County, Qinghai[J].Mineral Resources and Geology,2009,23(1). |
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| Authors: | XIAO Wen-jin |
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| Institution: | XIAO Wen-jin (China Non-ferrous Metals Resource Geological Survey; Beijing 100012; China); |
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| Abstract: | The Jijishen Cu-Pb-Zn polymetallic deposit located in eastern section of the Pb-Zn-Ag-Cu-Au polymetallic mineralized zone on north edge of Qaidam Basin.The Jijishen deposit was controlled by the strata of Tanjianshan Group at Upper Ordovician(O3tn).The paper has introduced the geological characteristics of Cu-Pb-Zn polymetallic deposit,and believed that this deposit is formed by hydrothermal precipitation and hydrothermal alteration.The prospecting criteria in this area are proposed and the prospecting dire... |
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| Keywords: | Cu-Pb-Zn deposit geological characteristics prospecting direction Jijishen Qinghai |
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