ISSN 1009-6248CN 61-1149/P 双月刊

主管单位:中国地质调查局

主办单位:中国地质调查局西安地质调查中心
中国地质学会

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    高建伟, 刘文卿, 邓会娟, 申俊峰, 赵国春. 胶东三山岛北部海域金矿蚀变特征与微量元素迁移规律[J]. 西北地质,2023,56(1): 245-253.
    引用本文: 高建伟, 刘文卿, 邓会娟, 申俊峰, 赵国春. 胶东三山岛北部海域金矿蚀变特征与微量元素迁移规律[J]. 西北地质,2023,56(1): 245-253.
    GAO Jianwei, LIU Wenqing, DENG Huijuan, SHEN Junfeng, ZHAO Guochun. Hydrothermal Alteration Characteristics and Migration Rules of Trace Elements in the North Sanshandao Sea Gold Deposit, Shandong, China[J]. Northwestern Geology,2023,56(1): 245-253.
    Citation: GAO Jianwei, LIU Wenqing, DENG Huijuan, SHEN Junfeng, ZHAO Guochun. Hydrothermal Alteration Characteristics and Migration Rules of Trace Elements in the North Sanshandao Sea Gold Deposit, Shandong, China[J]. Northwestern Geology,2023,56(1): 245-253.

    胶东三山岛北部海域金矿蚀变特征与微量元素迁移规律

    Hydrothermal Alteration Characteristics and Migration Rules of Trace Elements in the North Sanshandao Sea Gold Deposit, Shandong, China

    • 摘要: 胶东地区是中国最重要的金矿矿集区,区内众多大型–超大型金矿集中产出,已探明金矿资源量占全国30%以上。构造蚀变岩型金矿是胶东区内重要的类型之一,三山岛北部海域金矿是该类型的典型代表。胶东三山岛北部海域金矿是近年来新发现的超大型金矿,对该矿床的蚀变岩石进行研究具有重要意义。通过详实地岩心编录与室内研究,查明了该矿床的主要蚀变类型及矿物组合特征,系统采集了典型蚀变岩石样品并进行了微量元素地球化学分析,运用质量平衡技术方法总结了热液蚀变过程中的元素迁移规律,同时探讨了黄铁绢英岩中微量元素特征。结果表明,在标高−1200~−1400 m 范围内蚀变强烈。蚀变类型有钾化、绢英岩化和黄铁绢英岩化等,其中与成矿关系最为密切的是绢英岩化和黄铁绢英岩化;从原岩到黄铁绢英岩的整个蚀变过程中,流体向围岩提供了大量(迁移量>2)的As、Sb、Te等低温元素,中量(迁移量为1~2)的Pb、Zn、Cu等中温元素,少量(迁移量<1)的Co、Ni、Cr等高温元素,表明在标高−1200~−1400 m处,流体以中低温元素组合为主,预测−1200~−1400 m处矿体仍处于中上部,深部还有很好的找矿潜力。

       

      Abstract: Jiaodong area, the most important gold province in China, is an area with concentration occurrence of large and super large gold deposits, the proved reserves in Jiaodong Peninsula account for more than 30% of the country. The fracture zone altered type gold deposit is one of the important types in the area; The Sanshandao North Sea gold deposit is a typical representative of this type. This gold deposit is a super-large gold deposit newly discovered in recent years, it is important to study the eroded rock of this deposit. Based on the detailed rock core compilation and interior study, the main corrosion type and mineral combination characteristics were identified. Samples of typical eroded rock were collected and underwent trace element geochemical analysis, the element migration rules in the hydrothermal erosion are summarized by mass balance technique, and the characteristics of trace elements in beresite are also discussed. The results show that, in the elevation range-1200 to-1400 m, corrosion types are kalification, sericitization and beresitization. Among them, the most closely related to mineralization are sericitization and beresitization. From the original rock to the beresite, the fluid provides a large number of low temperature elements (migration value > 2) such as As, Sb, Te, moderate medium temperature elements (migration values are 1~2) such as Pb, Zn, Cu, and a small number of high temperature elements (migration value <1) such as Co, Ni, and Cr. It is shown that at-20 −1200 to −1400 m, it is predicted that the ore body at −1200 to −1400 meters is still in the upper middle part, and there is still good prospecting potential in the depth.

       

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