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Reanalysis of the Ore-fluid Origin in Jiaodong Gold Deposits and Discussion on the Metallogenic Dynamics Process

  • ZHAO Zelin ,
  • LI Junjian ,
  • LIU Lishuang ,
  • DANG Zhicai ,
  • TANG Wenlong ,
  • FU Chao
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  • 1.Graduate Department of Chinese Academy of Geological Sciences,Beijing   100037,China;
    2.Tianjin Institute of Geology and Mineral Resources,China Geological Survey,Tianjin   300170,China;
    3.Institute of Geology Chinese Academy of Geological Sciences,Beijing   100037,China

Received date: 2015-04-22

  Revised date: 2015-06-09

  Online published: 2015-11-16

Abstract

For purpose of making a clear acknowledge of nature and origin of the Jiaodong ore cluster ore-forming hydrothermal,date regarding mineralization ages,hydrogen and oxygen isotopes,sulfur isotope,argon,helium and radioactive isotopes were collected and reanalyzed briefly.The results showed that ore-forming hydrothermal was characterized by mainly crustal origin with minor proportions of mantle involvement.It was found that hydrothermal fluid was caused by early Cretaceous magmatic activities(Guojialing rock mass and Weideshan super-unit),acted the role of provider of the ore-forming hydrothermal.Over the same period enrichment mantle-derived magma(mafic dike) likewise provided partially or hydrothermal ore-forming materials.In the process of the Pacific plate to Eurasian plate subduction,fluid was released,which led to  the partial melting of mantle lithosphere,the enrichment of lithospheric mantle source basic magma formation,and the bottom effect of magma resulted in partial melting of crust and formed parental magma for the Guojialing granite(Early Cretaceous).With continuous subduction plate,lithospheric mantle melted persistently,moreover,the sustained high temperature of mantle-derived basic magma caused the partial melting that happened at lower crust depth,and finally formed the mountain superelement Weideshan super-unite(late Early Cretaceous).Fluid appeared in the process the Early Cretaceous magmatic assault on precipitation,and the fluid circulated in the shell and extracted to ore-forming material.Finally,under the condition on favorable NNE pull-apart structure,the ore-forming material reacted with surrounding rock and become ore material precipitation as variation of  ore-bearing hydrothermal temperature pressure conditions.

Cite this article

ZHAO Zelin , LI Junjian , LIU Lishuang , DANG Zhicai , TANG Wenlong , FU Chao . Reanalysis of the Ore-fluid Origin in Jiaodong Gold Deposits and Discussion on the Metallogenic Dynamics Process[J]. Gold Science and Technology, 2015 , 23(4) : 8 -17 . DOI: 10.11872/j.issn.1005-2518.2015.04.008

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