ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
小西南岔金、铜矿床同位素地球化学
  
关键词:Xiaoxinancha gold-copper deposit  isotope magma  hydrothermal deposit
基金项目:吉林省科委资助项目(吉科033号)
作者单位E-mail
周燕 吉林大学吉林长春130026 wentong@jlu.edu.cn 
咸嘉泉 吉林大学吉林长春130026  
王铁夫 吉林大学吉林长春130026  
张延洁 吉林大学吉林长春130026  
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摘要:
Isotope Geochemistry of the Xiaoxinancha Gold and Copper Deposit
      Lying in Hunchun County,Jilin Province,the Xiaoxinancha deposit occurs in the contact zone between the Late Variscan diorite and Lower Paleozoic Wudaoguo Group. Based on the research of isotope ratios of lead,sulfur,oxygen and carbon in the ores and rocks of this area,it is held that Qinglongcun Group serve as the source bed of gold. The polymetallic deposits of porphyry,skarn and hydrothermal types were formed during the remelting of Qinglongcun Group in the Variscan period and the mixture of hydrothermal activity and atmospheric precipitation in the Yanshanian period. Isotopic analysis of gold-copper deposits is very important in prospecting for original deposits in Xiaoxinancha area and providing essential geological data for further research.
ZHOU Yan,XIAN Jia-quan,WANG Tie-fu,ZHANG Yan-jie.2004.Isotope Geochemistry of the Xiaoxinancha Gold and Copper Deposit[J].Acta Geoscientica Sinica,25(2):133-136.
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