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J4 ›› 2011, Vol. 19 ›› Issue (2): 26-30.

• article • Previous Articles     Next Articles

Isotope Characteristic and Ore Genesis of Guoluolongwa Gold Deposit in Qinghai Province

ZOU Dingxi1,YANG Xiaobin2,LU Wenquan3   

  1. 1.No.8 Team of Geology and Mineral Resources Bureau for Non-ferrous Metals of Qinghai Province,Xining 810012,Qinghai,China；
    2.Geo-exploration Bureau for Non-ferrous Metals of Qinghai Province,Xinning 810007,Qinghai,China；
    3.Land and Resources Department of Qinghai Province,Xining 810001,Qinghai,China
  • Received:2010-11-03 Revised:2011-03-26 Online:2011-04-28 Published:2012-05-11

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Abstract:

Guoluolongwa gold deposit is located Wangbaogou Group of the east Kunlun orogenetic belt.It is controlled by a ductile shear zone.Mineralized rocks are chlorite phyllite,siliceous slate,and so on.There are plenty of vein rocks in the metallogenic region.Mineralize type includes quartz vein,altered phyllite,fracture zone,vein-like mass.The ore is low content of sulfide,mineral composition is simple in the ores.The study results of sulphur and lead isotopes show that Guoluolongwa gold deposit is very like the others gold deposit of the east Kunlun minerogenetic region.It is a typical type of orogenic gold deposit.It is related to intermediate -acid magma intruded in Varisian-Indian-China periods and it belongs to medium-temperature hydrothermal type.

Key words: Ductile shear zone, Sulphur and lead isotope, Orogenic gold deposit, Guoluolongwa gold deposit, Qinghai Province

CLC Number: 

  • P618.51

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