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Two Phase Overprinting Mineralization in Huangbuling Gold Deposit in Northwestern Jiaodong Peninsula

ZHANG Yuan1, LIU Lian-deng1,SUN Jing-gui1,CHEN Guo-hua1,ZHANG Hong-xi2,YAN Fu-chuan2, YANG Kai-chun2   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;2.Zhaoyuan Canzhuang Gold Mine of Shandong Province, Zhaoyuan， Shandong 265400,China
  • Received:2007-06-22 Revised:1900-01-01 Online:2008-01-26 Published:2008-01-26
  • Contact: ZHANG Yuan

Abstract: Huangbuling gold deposit locates in the Zhaoyuan-Laizhou gold deposit belt in Northwestern Jiaodong peninsula, at the hanging wall of the Huangbuling-Fenghuangshan NE trending fault. It consists of 18 ore veins with different scales. The study shows that the NE faults controlled the early stage intermediate gold vein, and the NNE faults controlled the late stage shallow gold vein. The early phase mineralizations are different from late phase. The early stage intermediate gold deposit consists of quartz, pyrite, molybdenite, electrum, gold, chalcopyrite, sphalerite, galena and others； while the late period gold deposit consists of quartz, calcite, pyritogelite, electrum, silver, sulfosalt minerals and others. The overprinted part of the early and late stages is the ore shoot part in the ore area.

Key words: two phase mineralization, Huangbuling gold deposit, Northwestern Jiaodong peninsula

CLC Number: 

  • P618.51
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