ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
安徽铜陵大团山铜矿床层状矽卡岩矿体中辉钼矿Re-Os年龄测定及其地质意义
  
关键词:Re-Os isotopic age  Datuanshan copper deposit  Tongling  Anhui Province
基金项目:国家重点基础研究发展规划项目(编号:G1999043211);国土资源部专项研究计划项目(编号:20010103);中国地质调查局地质调查项目(编号:K1.4-3-3)
作者单位E-mail
梅燕雄 中国地质科学院矿产资源研究所北京100037 meiyx@sohu.com 
毛景文 中国地质科学院矿产资源研究所北京100037
中国地质大学北京100083 
 
李进文 中国地质科学院矿产资源研究所北京100037  
杜安道 中国地质科学院国家地质实验测试中心北京100037  
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摘要:
Re-Os Dating of Molybdenite from Stratiform Skarn Orebodies in the Datuanshan Copper Deposit, Tongling, Anhui Province, and Its Geological Significance
      The Datuanshan copper deposit in Tongling, Anhui Province, is located in the middle section of the Middle and Lower Yangtze Valley iron-copper metallogenic belt. The metallogenic epoch of the deposit was previously regarded as Yanshanian on the basis of the ages of intermediate-acid intrusive rocks related to the ore-forming process. The authors collected 6 molybdenite samples from stratiform skarn orebodies in the Datuanshan copper deposit for Re-Os precise dating. The isochron age is 139.1±2.7 Ma, and the Re-Os model ages vary from 138.0~140.8 Ma. These age data are concordant with 40Ar/39Ar ages, 135.8~139.8 Ma, of the ore-forming intermediate-acid intrusive rocks. The Datuanshan copper deposit and the copper-sulfur-gold deposits in Tongling area are products of Mesozoic large-scale metallogenic process in East China, coupling with the geodynamic event of the lithospheric tectonic regime transition.
MEI Yan-xiong,MAO Jing-wen,LI Jin-wen,DU An-dao.2005.Re-Os Dating of Molybdenite from Stratiform Skarn Orebodies in the Datuanshan Copper Deposit, Tongling, Anhui Province, and Its Geological Significance[J].Acta Geoscientica Sinica,26(4):327-331.
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