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J4 ›› 2008, Vol. 16 ›› Issue (4): 33-37.

• article • Previous Articles     Next Articles

Geological Characteristics and M etallonic Condition of Shuangquan Gold Deposit， Xilnjian g Pl'rovimnc

ZHA0 Haibin 1，WANG Meijuan 2，WANG Xin2   

  1. 1．NO．8 Gold Geological party of CAPF，Urumqi  830057，Xinjiang，China；
    2．GD Geological Institute of CAPF，Langfang  065000，Hebei，China
  • Received:2008-06-20 Revised:2008-06-30 Online:2008-08-27 Published:2011-07-05

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Abstract:

The Shuangquan gold deposit，located in the Kalamaili metallogenic zone，is the important gold-polymetal metallogenic zone of East Junggar，and it occurres in the epimetamorphic ore series of Nanmingshui formation of lower carboniferous，which has higher gold abundance．Thei'e are frequent magInatic activity in this area and the incursion rock occurred in the north area as batholith．The Qingshui．Sujiquan falt and its subsidiary fracture were the 0re．c0n．trolling structure and ore-host space．Rocks in fracture zone had obvious plastic deform ation and strong schistosity
，mylonitization and had the character of ductile-brittle shear deform ation．The Shuangquan gold deposit belongs to the crushing alteration bearing gold-quartzvein type．Au element mainly from stratum，partly from deep source

Key words: Gold deposit, Metallogenic condition, Ductile-brittle, Shear deformation, Xinjiang

CLC Number: 

  • P618.51

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