Volume 14 Issue 3
Sep.  2008
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Article Navigation >  Journal of Geomechanics  > 2008  >  14(3): 263-273
WANG Hai-qin, HUO Guang-hui, 2008. CHARACTERISTICS OF MINERAL INCLUSIONS IN GRANITES CLOSELY RELATED WITH GOLD FORMING IN EASTERN SHANDONG PROVINCE. Journal of Geomechanics, 14 (3): 263-273.
Citation: WANG Hai-qin, HUO Guang-hui, 2008. CHARACTERISTICS OF MINERAL INCLUSIONS IN GRANITES CLOSELY RELATED WITH GOLD FORMING IN EASTERN SHANDONG PROVINCE. Journal of Geomechanics, 14 (3): 263-273.
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CHARACTERISTICS OF MINERAL INCLUSIONS IN GRANITES CLOSELY RELATED WITH GOLD FORMING IN EASTERN SHANDONG PROVINCE

  • 1.

    Shandong Institute and Laboratory of Geological Sciences, Jinan 250013, China

  • 2.

    Shandong Geophysical and Geochemical Exploration Institute, Jinan 250013, China

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  • Received: 2007-11-23
  • Published: 2008-09-01
    Abstract
  • In eastern Shandong Province (Jaodong area), there are distributed Linglong gneissic granite, Luanjiahe granite, Guojialing diorite and Shangzhuang monzonitic granite, which have close relation with Jiaodong gold mine.According to developing degree, type, size and characteristics of mineral inclusions, and based on temperature-measuring result by microscope, it is indicated that the Linglong rock mass was formed by remelting of granite caused by high regional metamorphism, the Guojialing rock mass was derived from crystallization of a high-temperature and high-viscosity magma, the Luanjiahe rock mass was crystallized from high-temperature, high-viscosity and CO2-rich magma at a relatively small depth, and the Shangzhuang rock mass was formed at a low-temperature and lowpressure condition.

     

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