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J4 ›› 2011, Vol. 19 ›› Issue (2): 13-17.

• article • Previous Articles     Next Articles

Analysis of Ore-controlling Mechanism of Gold Mineralization in Hadamengou Gold Deposit,Inner Mongolia

XIA Dong1,3,NIU Shuyin1,XU Guo2,CHEN Chao1,ZHAO Zhiyuan1,PENG Yuxuan4   

  1. 1.Shijiazhuang University of Economics,Shijiazhuang 050031,Hebei,China；
    2.China University of Geosciences,Beijing 100083,China；
    3.Geological Survey of Inner Mongolia,Huhehaote 010020,Inner Mongolia,China；
    4.Xinjiang Institute of Mineral and Experiment,Wulumuqi 050081,Xinjiang,China
  • Received:2010-02-15 Revised:2011-03-19 Online:2011-04-28 Published:2012-05-11

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Abstract:

Hadamengou gold mine has a large deposit scale by proven,gold deposit is strictly controlled by tectonic, also has its own unique,such as high gold background values of wallrock,piedmont red fragments altered belts, thick crystal biotite granite pegmatite,and multi-stage intrusion of magma,and it become an indispensable factor in the formation of gold.Take mantle branch theory as a guide,throughcomprehensive study of geological features and other factors,we consider that Hadamengou gold mine belongs to fracture-altered rock typedeposit,wulashan rock Group is an important ore source,EW-trending primary and secondary detachment is the main leading-host structures,multi-stage magmatic activity provide heating,hot water and some minerals for deposit,mineralization is close related with biotite graniticpegmatite and brittle deformation of quartz veins.We discuss metallogenic regularity of deposit,and propose ore prospecting.

Key words: Mantle branch structure, Ore-controlling mechanism of mineralization, Primary and secondary detachment belt, Brittle deformation, Hadamengou gold deposit

CLC Number: 

  • P618.51

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