| 新疆琼河坝铜金矿化地质特征及成因机理 |
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| 引用本文： | 陈仁义,刘海光,马文义.新疆琼河坝铜金矿化地质特征及成因机理[J].地质与勘探,1995(1). |
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| 作者姓名： | 陈仁义 刘海光 马文义 |
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| 作者单位： | 中国地质大学，中国地质科学院矿床所，新疆第二区调大队 |
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| 摘 要： | 通过研究琼河坝地区的含矿岩系、铜金矿化、流体包裹体和氢氧同位素，认为２０２铜矿为斑岩型矿床，绿石沟铜矿为夕卡岩型矿床，剥蚀程度是本区铜金找矿的关键。
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| 关 键 词： | 铜金矿化，夕卡岩，斑岩，剥蚀程度，琼河坝 |
Geological Characteristics and Genetic Mechanism of Cu-Au Mineralization in Qiongheba,Xinjiang |
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| Chen Renyi,Liu Haiguang,Ma Wenyi.Geological Characteristics and Genetic Mechanism of Cu-Au Mineralization in Qiongheba,Xinjiang[J].Geology and Prospecting,1995(1). |
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| Authors: | Chen Renyi Liu Haiguang Ma Wenyi |
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| Abstract: | After studying ore-bearing rock series,Cu-Au Mineralization,fluid inclusion and H-O isotopes,it is believed that 202 Cu deposit is a porphyry one,and that Lushigou Cu deposit is a skarn.Then,it is pointed out that the key to prospecting Cu and Au in studied area is the depth of denudation. |
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| Keywords: | Cu-Au mineralization skarn porphyry the depth of denudation Qiongheba |
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