ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
东天山红柳河地区晚加里东期花岗岩类岩石锆石U—Pb年龄及其地质意义
  
关键词:U-Pb age of zircon  the subduction of plate  later Caledonian  East Tianshan Mountains
基金项目:国土资源部1∶5万《红柳河站幅》、《芦苇井幅》项目;区域地质调查项目 [甘地勘地发(1996)17号]资助
作者单位
李伍平 中国科学院广州地球化学研究所长安大学资源系西安 
王涛 北京大学地质学系 
李金宝 长安大学资源系西安 
康旭 长安大学资源系西安 
于福生 中国石油大学研究生院北京 
韩庆军 长安大学资源系西安 
马忠平 西安地质矿产研究所西安 
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摘要:
The U-Pb Age of Zircon from Late Caledonian Granitoids in Hongliuhe Area,East Tianshan Mountains,Northwest China and Its Geological Implications
      Based on the Studies of the chronology, geochemistry of elements and isotopes of two granitoid plutons in Hongliuhe area, East eastern Tianshan Mountains,Northwest China,it is inferred that Hongliuhe pluton(zircon age being 441.4±1.6Ma) and Hongliuhebei pluton(zircon age being 440.9±3.1Ma)were formed in Late Caledonian .The ages determined not only confirm the existence of Late Caledonian magmatic activities in East Tianshan Mountains ,but also demonstrate the intimate relationship between the magmatic activities and the subduction of the Kazakstan-Junggar ocean plate beneath Tarim plate.
LI Wu-ping,WANG Tao,LI Jin-bao,KANG Xu,YU Fu-sheng,HAN Qing-jun,MA Zhong-ping.2001.The U-Pb Age of Zircon from Late Caledonian Granitoids in Hongliuhe Area,East Tianshan Mountains,Northwest China and Its Geological Implications[J].Acta Geoscientica Sinica,22(3):231-235.
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