| 浙江长兴大银山金矿成因探讨 |
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| 引用本文： | 殷虹. 浙江长兴大银山金矿成因探讨[J]. 浙江国土资源, 2000, 0(2) |
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| 作者姓名： | 殷虹 |
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| 作者单位： | 浙江省第九地质大队!湖州，313000 |
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| 摘 要： | 受燕山中晚期地质构造运动和岩浆活动的影响 ,在中酸性侵入岩体与钙镁碳酸盐岩外接触带 ,大银山金矿体呈扁平透镜状产于侵入体的舌状端部。是中低温热液型含金矽卡岩矿床。研究其成矿地质条件和控因素 ,对找矿和成矿预测均有重要意义
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| 关 键 词： | 含金矽卡岩矿床 燕山运动 矿床成因 找矿标志 |
Discussion on the Genesis of DayinshanGold Deposit in Changxing County,Zhejiang Province |
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| Yin Hong. Discussion on the Genesis of DayinshanGold Deposit in Changxing County,Zhejiang Province[J]. Zhejiang Land & Resources, 2000, 0(2) |
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| Authors: | Yin Hong |
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| Abstract: | Affected by geotectonic movement and magmatic activities in middle-late Yanshanian Period,the ore body of Dayinshan gold deposit is located in the exocontact of middle-acidic intrusive rock body and Ca-Mg-Carbonate rock,at the tip of the intrusive, occurring in flat lenticulat shapes. It belongs to gold-bearing skarn ores of middle-low temperature jucbrothermal type. research on the geological conditions of its.nineralinzation and the mineralization-controlling factors will have great significance for ore prospecting and mineralization forcast. |
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| Keywords: | gold-bearing Skarn ore deposit Yanshanian movement Gensis of ore deposit mark of ore propecting |
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