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ZHANG Hai-quan, JI Wen-hua. Study on substance composition and cause of formation of Jincheng gold deposit, northwestern Jiaodong Peninsula[J]. Northwestern Geology, 2005, 38(2): 62-69.
Citation: ZHANG Hai-quan, JI Wen-hua. Study on substance composition and cause of formation of Jincheng gold deposit, northwestern Jiaodong Peninsula[J]. Northwestern Geology, 2005, 38(2): 62-69.

Study on substance composition and cause of formation of Jincheng gold deposit, northwestern Jiaodong Peninsula

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  • Received Date: November 09, 2004
  • Revised Date: March 20, 2005
  • Published Date: June 04, 2005
  • This paper studies the major elements and trace elements of altered rocks and the Au content and composition of altered minerals of Jincheng gold deposit and first studied the Fe-carbonate and the amygdale in lamprophyre in this deposit. The conclusions show that the metallogenetic fluid is general rich in Fe, Si, K, Au, Ag, Bi, Co and Cu etc.,expect for their difference. Pyrite is the main Au-bearing minerals but quartz is poor in Au. Fe-carbonate is closely related to the precipitation of pyrite and chalcopy rite.The last remain fluid of lamprophyre magma is similar to metallogenetic fluid in composition and precipitating sequence,showing their genetic relationship.
  • 杨敏之.金矿床围岩蚀变地球化学——以胶东金矿床为例[M].北京:地质出版社,1998.
    杨敏之,吕古贤.胶东绿岩带金矿地质地球化学[M].北京:地质出版社,1996.
    李兆龙,杨敏之.胶东金矿床地质地球化学[M].天津:天津科技出版社,1993.
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