Journal of Jilin University(Earth Science Edition) ›› 2012, Vol. 42 ›› Issue (6): 1656-1664.

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A Discussion on Genesis and Ore Prospecting of Dongshengmiao Deposit, Inner Mongolia

Zhou Chao-xian1,2,3，Zhang Yun-guo1,2，Tang Ping-zhi1,2，Chen Yan-miao3，Wang Shuang-lun1,2，Qi Ya-hui1,2，Yang Qiang1,2   

  1. 1.China Geological Survey of Nonferrous Metal Resource, Beijing100012, China;
    2.Sinotech Mineral Exploration Company, Limited, Beijing100012, China;
    3.Wulate Houqi Zijin Mining Company, Limited, Wulate Houqi015500, Inner Mongolia，China
  • Received:2012-04-20 Online:2012-12-26 Published:2012-11-26

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Abstract: Such the ideas on genesis and ore prospecting of the Dongshengmiao deposit proposed by Zhang et al. (2010) are questioned in this paper as the classification of orebodies (i.e., sulfur orebodies and zinc orebodies), shapes, structure and texture, REE pattern of both sulfur and zinc ore. It was negated in this paper that, in Dongshengmiao deposit, sulfur orebodies were resulted from SEDEX process and zinc orebodies were caused by hydrothermal reworking after sulfur orebodies forming, and the further exploration be here. In Dongshengmiao-Sanguikou area, there are mainly six zinc orebodies (i.e., orebodies 9, 2, 11, 3, 10 and 4) and four sulfur ones (i.e., orebodies 1, 3, 4, and 2). Orebody 9, occurring comfortably in schist and having the same REE pattern model with the wall rock, should be resulted from the SEDEX mineralization process, similar to the mineralization of other orebodies. It is proposed that further ore exploration should be concentrated upon the deeper boot orebody of SEDEX deposit.

Key words: Dongshengmiao-Sanguikou ore deposit, characteristics of orebody, zinc orebody, sulfur orebody, SEDEX, genesis, ore deposits

CLC Number: 

  • P611
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