青海省大柴旦镇红柳沟金矿床地质特征及其成因 |
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引用本文: | 吴正寿,邓元良,苏生顺.青海省大柴旦镇红柳沟金矿床地质特征及其成因[J].青海国土经略,2001(1). |
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作者姓名: | 吴正寿 邓元良 苏生顺 |
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作者单位: | 青海省第一地质矿产勘查大队,青海省第一地质矿产勘查大队,青海省第一地质矿产勘查大队 平安 810600,平安 810600,平安 810600 |
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摘 要: | 通过对红柳沟金矿床地质特征及围岩蚀变的研究,总结了金矿控矿因素及其富集规律,认为该矿床的成因为动力变质热液型。
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关 键 词: | 红柳沟 金矿床 动力变质热液型 |
GEOLOGICAL FEATURES AND ORIGIN OF HONGLIU GOUGOLD DEPOSIT, DACHAIDAN TOWN, QINGHAI PROVINCE |
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Authors: | Wu Zhengshou Deng Yuanliang Su Shengshun Qinghai No Team of Geology and Mineral Exploration Pingan |
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Institution: | Wu Zhengshou,Deng Yuanliang,Su Shengshun Qinghai No.1 Team of Geology and Mineral Exploration,Pingan 810600 |
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Abstract: | Through studies on geological features and country rocks alteration, thefactors of ores controlling and enrichment law have been summarized. The genetic type isbelonged to a dynamometamorphic hydrothermal type. |
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Keywords: | Hongliugou gold deposit dynamometamorphism |
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