| 五龙金矿成因研究 |
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| 引用本文： | 彭艳东.五龙金矿成因研究[J].地质与资源,1994,3(1):21-31. |
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| 作者姓名： | 彭艳东 |
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| 作者单位： | 沈阳地质矿产研究所 |
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| 摘 要： | 五龙金矿是一大型脉状金矿床，金矿化与燕山期构造-岩浆活动密切相关，野外地质特征及大量岩石化学、地球化学及同位素资料表明，三股流岩体、脉岩和含金石英脉是古老含金矿源层重熔的产物，三者具有相同的来源。矿床成因类型为重熔岩浆热液金矿床。
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| 关 键 词： | 金矿成因 辽宁丹东五龙 |
| 收稿时间： | 1992-12-01 |
STUDY ON GENESIS OF WULONG GOLD DEPOSIT IN LIAONING PROVINCE |
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| Peng Yandong.STUDY ON GENESIS OF WULONG GOLD DEPOSIT IN LIAONING PROVINCE[J].Geology and Resources,1994,3(1):21-31. |
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| Authors: | Peng Yandong |
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| Institution: | Shenyang Institute of Geology and Mineral Resources |
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| Abstract: | Wulong gold deposit is a large scale gold lodes．The gold mineralization is close relatedto the Yanshanian period tecto—magmatisms．Geological，Petrochemical，geochemical andisotopic characteristics have been studied and indicate that Sanguliu intrusion、dikes and goldmineralization were the products of remelting of old gold—bearing source beds．They comefrom the same deep—seated magama chamber．Wulong gold deposit belongs to remelted mag－matic hydrothermal gold deposit． |
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| Keywords: | genesis of gold deposit Liaoning Dandong Wulong |
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