ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
东天山红柳河地区蛇绿岩U-Pb同位素年龄
  
关键词:East Tianshan Mountains  Hongliuhe area  ophiolites  U-Pb isotope age
基金项目:国土资源部1∶5万《红柳河站幅》、《芦苇井幅》和区域地质调查项目[甘地勘地发(1996)17号]
作者单位E-mail
于福生 中国石油大学石油天然气成藏机理教育部重点实验室北京102249 fushengyu@bjpeu.edu.cn 
李金宝 长安大学资源学院陕西西安710054  
王涛 中国地质科学院地质研究所北京100037  
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摘要:
The U-Pb Isotopic Age of Zircon from Hongliuhe Ophiolites in East Tianshan Mountains, Northwest China
      The U-Pb isotopic age of zircon from gabbro in Hongliuhe ophiolites is about 425.5±2.3 Ma. This age that can be considered to be the formation time of the gabbro shows that the ophiolites were formed in Early Silurian, corresponding to Gleedonian period of Wenlock. The result indicates that the central Tianshan Mountains were separated from the Tarim plate and formed a discrete terrain in Early Silurian.
YU Fu-sheng,LI Jin-bao,WANG Tao.2006.The U-Pb Isotopic Age of Zircon from Hongliuhe Ophiolites in East Tianshan Mountains, Northwest China[J].Acta Geoscientica Sinica,27(3):213-216.
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