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    彭艳东. 五龙金矿成因研究[J]. 地质与资源, 1994, 3(1): 21-31. DOI: 10.13686/j.cnki.dzyzy.1994.01.002
    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. DOI: 10.13686/j.cnki.dzyzy.1994.01.002
    shu
    Peng Yandong. STUDY ON GENESIS OF WULONG GOLD DEPOSIT IN LIAONING PROVINCE[J]. Geology and Resources, 1994, 3(1): 21-31. DOI: 10.13686/j.cnki.dzyzy.1994.01.002
    Citation: Peng Yandong. STUDY ON GENESIS OF WULONG GOLD DEPOSIT IN LIAONING PROVINCE[J]. Geology and Resources, 1994, 3(1): 21-31. DOI: 10.13686/j.cnki.dzyzy.1994.01.002
    shu

    五龙金矿成因研究

    STUDY ON GENESIS OF WULONG GOLD DEPOSIT IN LIAONING PROVINCE

      摘要
    • 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。

       

      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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